GEOLOGY AND GROUND WATER RESOURCE S - … GROUND WATER ... separate parts of the bulletin ... (or...
Transcript of GEOLOGY AND GROUND WATER RESOURCE S - … GROUND WATER ... separate parts of the bulletin ... (or...
North Dakota Geological Surve yE.A. NOBLE, State Geologist
BULLETIN 5 5
North Dakota StateWater Commission
MILO W . HOISVEEN, State Enginee r
COUNTY GROUND WATER STUDIES 1 4
GEOLOGY AN DGROUND WATER RESOURCE S
of Burke and Mountrail Countie s
PART I IGROUND WATER BASIC DAT A
b yC.A. ARMSTRONG
Geological Surve yUnited States Department of the Interio r
Prepared by th e
in cooperation with th e
the North
and the Burke and Mountrai l
Y%rte : . . .~
United States Geological Survey
North Dakota State Water Commission ,
Dakota Geological Survey ,
Water Management District s
1969
North Dakota Geological SurveyE .A. NOBLE, State Geologist
BULLETIN 5 5
North Dakota StateWater Commission
MILO W . HOISVEEN, State Engineer
COUNTY GROUND WATER STUDIES 1 4
GEOLOGY AN DGROUND WATER RESOURCES
of Burke and Mountrail Countie s
PART I IGROUND WATER BASIC DATA
byC .A. ARMSTRON GGeological Survey
United States Department of the Interio r
Prepared by the United States Geological Surve yin cooperation with the North Dakota State Water Commission ,
the North Dakota Geological Survey ,
and the Burke and Mountrail Water Management District s
1969
Introduction '--'
"=»= " =nd scope
°ell-n"*",ing system .
^~"" w`edoments '
uxplanation .*tables '— '
°=°~m"^itr^at"---'---'---'----' '----
xin.raz "on" it"ents in solution '---'
Prmprtie" an* characteristics "' water
1 0
ILLmTRATIONS
?late 1 . Map showing location m °ells . spung` , and test holes m *=^ tr"i l
County, North Dakota '--' '(in pocket )
2 . Map showing location of wells, springs, and test holes in Burk e
Figure 1 . Map showing county ground-water studies in North Dakota 2
2 . Diagram showing system of numbering wells, springs, and test holes-
4
TABLES
Table 1 . Records of wells and test hole s
Mountrail County 1 3
Burke County 4 o
2 . Records of springs
Mountrail County 66
Burke County 6 8
3 . Water levels in selected well s
Mountrail County 6 9
4 . Logs of test holes and well s
m°ntr"unoun^y 8 5
Burke County 177
5 . Chemical analyses of selected water sample s
Mountrail County 274
This is one of a series of county reports published cooperatively
by the North Dakota Geological Survey and the North Dakota State Wate r
Commission . The reports are in three parts ; Part I describes the geology ,
Part II presents ground water basic data, and Part III describes the groun d
water resources . Parts I and III will be published later and will be dis-
tributed as soon as possible .
Buy North Dakota Products
GEOLOGY AND GROUND WATER RESOURCES OF BURKE AND MOUNTRAIL COUNTIES, NORTH DAKOT A
PART II - GROUND WATER BASIC DAT A
B y
C . A . Armstrong
INTRODUCTION
Purpose and Scope
The purpose of the investigation was to determine the quantity and quality of groun d
water available in Burke and Mountrail Counties, N . Dak . (fig . 1) for municipal, domestic ,
livestock, industrial, and irrigation uses . Specifically, the objectives within the scop e
of financing and time available were to : (1) determine the location, extent, and nature of
the major aquifers ; (2) evaluate the occurrence and movement of ground water, including th e
sources of recharge and discharge ; (3) estimate the quantities of water stored in th e
aquifers ; (4) estimate the potential yields to wells tapping the major aquifers ; and (5 )
determine the chemical quality of the ground water .
The investigation was made cooperatively by the U .S . Geological Survey, North Dakot a
State Water Ccmmussion, North Dakota Geological Survey, and Burke and Mountrail Countie s
Water Management Districts . The results of the investigation will be published in thre e
separate parts of the bulletin series of the North Dakota Geological Survey and the count y
ground-water studies series of the North Dakota State Water Commission . Part I is an
interpretive report describing the geology, Part II is a compilation of the ground-water
basic data, and Part III is an interpretive report describing the ground-water resources .
Part II makes available hydrologic data collected during the county investigation an d
functions as a reference for Parts I and III .
The information in this report was collected chiefly between 1965 and 1968, and con -
sists of the following: (1) data on about 2,100 wells and test holes ; (2) data on 5 8
springs ; (3) water-level measurements in 63 observation wells ; (4) logs of about 570 tes t
holes and selected wells ; and (5) chemical analyses of 504 water samples .
The data in this report are useful for predicting geologic and ground-water condition s
in Burke and Mountrail Counties . For example ; a person considering the construction of a
new well can locate the proposed site on plates 1 and 2 (in pocket) . The characteristics of
nearby wells and springs may be determined from tables 1 and 2, and the water-level fluctu -
ations in the area may be determined from table 3 . The type of material encountered in
nearby wells may be determined from table 4, and the chemical quality of water in adjacen t
wells may be determined from table 5 . Extrapolations based on these data should be con-
servative because of the irregular distribution of the water-bearing rocks .
1
MC KENZIE:I~
fq
BILLINGS1
MC HENR Y
0
20
40 MILE S
THIS REPORT
ALL OR PART OF THE REPORT PUBLISHED
IN PROGRES S
FIGURE 1 .-County ground-water studies in North Dakota .
Well-Numbering Syst- m
The wells, springs, and toot horde in the tables are numbered according to a syste m
based on the location in the public land classification of the U .S . Bureau of Land Manage -
ment . It is illustrated in figure 2 . The first numeral denotes the township north of a
base line, the second numeral denotes the range west of the fifth principal meridian, an d
the third numeral denotes the section in which the well is located . The letters a, b, c ,
and d designate, respectively, the northeast, northwest, southwest, and southeast quarte r
sections, quarter-quarter sections, and quarter-quarter-quarter sections (10-acre tract) .
For example, well 157-90-15daa is in the NE-!E4SEy sec . 15, T . 157 N ., R . 90 W . Consecu -
tive terminal numerals are added if more than one well is recorded within a 10-acre tract .
In T . 164 N ., Rs . 88-94 W ., secs . 25-30 are only about a quarter of a mile wide . Thes e
sections are considered as though they are only the southern part of a normal square-mil ,
section .
Acknowledgments
The cooperation of the residents of the county and the municipal and county official s
is gratefully acknowledged . Thanks are also due to the numerous well drillers who contrib -
uted logs and information for this report . Well-site logs were prepared principally by
L . L . Froelich and C . E . Naplin of the North Dakota State Water Commission . The early
stages of the investigation were under the direction of J . L . Hatchett of the U .S .
Geological Survey .
EXPLANATION OF TABLES
Water levels in observation wells were measured periodically beginning in the sunnie r
of 1966 . During most of 1967 and 1968, from 60 to 70 wells were measured each month, an d
2 wells were equipped with continuous water-level recorders . About 20 of these observation
wells will continue to be measured as part of the Statewide observation-well network . The
locations of observation wells are shown on plates 1 and 2 .
The logs given in table 4 are the descriptions as given by the source shown, otherwis e
they are composites of the well-site geologists' and drillers' descriptions, sample analyse s
and electric logs (where available) . Visual examination, where the samples were obtaine d
during drilling of the hole, was made by using a binocular microscope . Color description s
were determined by comparing the sample with the Geological Society of America rock-colo r
chart (1963) . Grain-size determinations used in the logs refer to the Wentworth (1922 )
size scale . All of the samples of glacial drift reacted (effervesced) when treated wit h
diluted hydrochloric acid and therefore were considered calcareous . Any large variation i n
the amount of calcareousness was noted on the sample logs in table 4 .
3
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The term " til l " indicates an unsorted, unstratified, cohesive, agglomeration of roc k
particles ranging from clay to boulders . In Burke and Mountrail Counties, silt and cla y
are the dominant particle sizes . If other particle sizes are present in appreciable amounts ,
they are used as modifying terms . Consequently, such terms as sandy or gravelly are textural
terms used to indicate that the material described contains an appreciable, but not a
dominant amount of the modifying material .
Observation wells were constructed in selected test holes . These, for the most part ,
were cased with 1},-inch plastic pipe, slotted in the lower 10 or 20 feet or screened i n
the lower 2 feet . They were pumped from 5 to 8 hours and a water sample was collected fo r
chemical analysis (table 5) .
The stratigraphtc nomenclature used in this report is that of the North Dakota Geolog -
ical Survey and, in some instances, differs from that of the U .S . Geological Survey .
WATER-QUALITY DATA
All natural waters contain dissolved mineral matter . Water in contact with soils o r
rock, even for only a few hours, will dissolve some mineral matter . The quantity of dis -
solved mineral matter in a natural water depends primarily on the type of rocks or soil s
with which the water has been in contact and the length of time of contact . Ground water
is generally more highly mineralized than surface water because it remains in contact wit h
the rocks and soils for much longer periods .
The mineral constituents and physical properties of natural waters reported in th e
table of analyses include those that have a practical bearing on the value of the water s
for most purposes . The analyses generally include determinations of silica, iron, calcium ,
magnesium, sodium, potassium (or sodium and potassium together calculated as sodium) ,
alkalinity as carbonate and bicarbonate, sulfate, chloride, fluoride, nitrate, boron ,
dissolved solids, pH, and specific conductance . Many of the specific conductances from
1947 through 1950 apparently, were not adjusted for temperature and, therefore, should not
be used to estimate dissolved-solids content . The source and significance of the different
constituents and properties of natural waters are discussed in the following paragraphs .
Mineral Constituents in Solution
Silica (SiO2 )
Silica is dissolved from practically all rocks . Some natural waters contain less than
5 ppm (parts per million) of silica and few contain more than 50 ppm, but the more commo n
range is from 10 to 30 ppm . Silica affects the usefulness of a water because it contribute s
to the formation of scale in pipes, water heaters, and boilers .
5
Iron (Fe )
Iron compounds are very common in rocks and they are easily leached by ground water .
On exposure to air, normal basic waters that contain more than 1 ppm of iron soon becom e
turbid with the insoluble reddish ferric oxide produced by oxidation . Surface waters ,
therefore, seldom contain as much as 1 ppm of dissolved iron, although some acid water s
carry large quantities of iron in solution . Ground waters commonly contain as much a s
10 ppm . Rarely, concentrations over 50 ppm may occur in waters with a pH of 5 to 8 (Hem ,
1959) . Iron causes reddish-brown stains on porcelain or enamelware and fixtures and o n
fabrics washed in the water . The U .S . Public Health Service (1962) recommends an uppe r
limit of 0 .3 ppm of iron in drinking water .
Calcium (Ca )
Calcium may be leached from all rocks, but limestone and dolomite fragments in th e
glacial drift provide the largest amount of calcium in Burke and Mountrail Counties .
Calcium is a major cause of hardness and forms scale on utensils and on boilers and pipes .
The calcium content of ground water may be as high as several hundred parts per million .
Magnesium (Mg )
Magnesium is dissolved from many rocks, particularly from dolomitic rocks . It s
effect in water is similar to that of calcium . The magnesium in soft waters may amoun t
to only 1 or 2 ppm, but water in areas that contain large quantities of dolomite or othe r
magnesium-bearing rocks may contain more than 100 ppm of magnesium . Sea water contain s
more than 1,000 ppm of magnesium .
Sodium and potassium (Ha and K )
Sodium and potassium are dissolved from practically all rocks . Sodium is the pre -
dominant cation in some of the more highly mineralized waters found in the western Unite d
States . Natural waters that contain only 3 or b ppm of the two together are likely t o
carry almost as much potassium as sodium . As the total quantity of these constituent s
increases, the proportion of sodium becomes much greater . However, the potassium concen -
tration in water does not usually exceed 50 ppm . Moderate quantities of sodium an d
potassium have little effect on the usefulness of the water for most purposes, but water s
that carry more than 50 ppm of the two may require careful operation of steam boilers t o
prevent foaming . More highly mineralized waters that contain a large proportion of sodiu m
salts may be unsatisfactory for irrigation . The presence of several hundred parts pe r
million of sodium in water makes it unsuitable for use in sodium-restricted diets use d
as therapy for cardiovascular diseases .
6
Bicarbonate and carbonate (HCO3 and CO3 )
Bicarbonate and carbonate are sometimes reported as alkalinity . Since the major cause s
of alkalinity in most natural waters are carbonate and bicarbonate ions dissolved fro m
carbonate rocks, the results are usually reported in terms of these constituents . Although
alkalinity is primarily due to the presence of carbonate and bicarbonate, other ions als o
contribute to alkalinity such as silicates, phosphates, borates, possibly fluoride, and
certain organic anions that may occur in colored waters . The significance of alkalinity
to the domestic, agricultural, and industrial user is usually dependent upon the nature o f
the cations (Ca, Mg, Na, and K) associated with it . However, moderate amounts of alka-
linity do not adversely affect most uses .
Sulfate (SO4)
Sulfate is dissolved from many rocks and soils--in especially large quantities fro m
gypsum and from beds of shale . It is formed also by the oxidation of sulfides of iron an d
may therefore be present in considerable quantities in mine waters . Sulfate in waters that
contain much calcium and magnesium causes the formation of hard scale in steam boilers an d
may increase the cost of softening the water . The U .S . Public Health Service (1962 )
recommends that 250 ppm of sulfate should be the upper limit for drinking water .
Chloride (Cl )
Chlorides are generally very soluble compounds and are found in most rocks so that
chlorides are found in all natural waters . Large quantities of chloride may affect th e
industrial use of water by increasing the corrosiveness of waters that contain larg e
quantities of calcium and magnesium . The U .S . Public Health Service (1962) recommends an
upper limit of 250 ppm of chloride for drinking water .
Fluoride (F )
Fluoride has been reported as being present in igneous and some sedimentary rocks t o
about the same extent as chloride . However, most fluorides, unlike the chlorides, are low
in solubility so that the quantity of fluoride in natural waters is ordinarily very smal l
compared to that of chloride . Hem (1959) reported that fluoride concentrations in exces s
of 10 ppm are rare . Investigations have proved that fluoride concentrations of about 0 . 6
to 1 .7 ppm reduce the incidence of dental caries, and that concentrations greater than 1 . 7
ppm also protect the teeth from cavities, but cause an undesirable black stain (Durfor an d
Becker, 1964) . U .S . Public Health Service (1962, p . 8) states, "When fluoride is naturally
present in drinking water, the concentration should not average more than the appropriat e
upper control limit (0 .6 to 1 .7 ppm) . Presence of fluoride in average concentration s
7
greater than two times the optimum shall constitute grounds for rejection of the supply . "
Concentrations higher than the stated limits may cause mottled enamel in teeth, endemi c
cumulative fluorosis, and skeletal effects .
Nitrate (NO3
)
Nitrate in water is considered a final oxidation produce of nitrogeneous material an d
may indicate contamination by sewage or other organic matter . U .S . Public Health Service
(1962) sets 45 ppm as the upper limit for nitrate . Ingestion of water containing excessive
quantities of nitrate may result in infantile methemoglobinemia . If the concentration is
sufficiently great, both man and animals can be poisoned by nitrate .
Boron (B )
Boron in small quantities has been found essential for plant growth, but irrigatio n
water containing more than 1 ppm boron is detrimental to navy beans and other boron -
sensitive crops .
Dissolved solid s
The reported quantity of dissolved solids--the residue on evaporation--consists mainl y
of the dissolved mineral constituents in the water . It may also contain some organic matte r
and water of crystallization . Waters with less than 500 ppm of dissolved solids are usuall y
satisfactory for domestic and some industrial uses . Water containing several thousand part s
per million dissolved solids are sometimes successfully used for irrigation where practice s
permit the removal of soluble salts through the application of large volumes of water o n
well-drained lands, but generally water containing more than about 2,000 ppm is considere d
to be unsuitable for long-term irrigation under average conditions .
Properties and Characteristics of Wate r
Temperature
Temperature is an important factor in properly determining the quality of water . Thi s
is very evident for such a direct use as an industrial coolant . Temperature is also impor -
tant, but perhaps not so evident, for its indirect influence upon concentrations of dissolve d
gases and distribution of chemical solutes in ground water . Normally, the temperature o f
ground water within 60 feet of the surface approximates the mean annual air temperature an d
increases 1°F for each 60 to 100 feet of increase in depth .
Hardnes s
Hardness is the characteristic of water that receives the most attention in industria l
and domestic use . It is commonly recognized by the increased quantity of soap required t o
8
produce lather . The use of hard water is also objectionable because it contributes to the
formation of scale in boilers, water heaters, radiators, and pipes, with a resultan t
decrease in rate of heat transfer, possibility of water heater or boiler failure, an d
decrease of flow .
Hardness is caused almost entirely by caspounds of calcium and magnesium . Other con -
stituents--such as iron, manganese, aluminum, barium, strontium, and free acid--also caus e
hardness, although they usually are not present in quantities large enough to have an y
appreciable effect .
Generally, bicarbonate and carbonate determine the proportions of " carbonat e " hardnes s
of water . Carbonate hardness is the amount of hardness chemically equivalent to the amount
of bicarbonate and carbonate in solution . Carbonate hardness is approximately equal to th e
amount of hardness that is removed from water by boiling and is termed temporary hardness .
Noncarbonate hardness is the difference between the hardness calculated from the tota l
amount of calcium and magnesium in solution and the carbonate hardness . If the carbonat e
hardness (expressed as calcium carbonate) equals the amount of calcium and magnesium hard -
ness (also expressed as calcium carbonate) there is no noncarbonate hardness . Noncarbonate
hardness is about equal to the amount of hardness remaining after water is boiled . Th e
scale formed at high temperatures by the evaporation of water containing noncarbonate hard -
ness commonly is tough, heat resistant, and difficult to remove .
Although many people talk about soft water and hard water, there has been no fir m
line of demarcation . Water that seems hard to ap leasterner may seem soft to a westerner .
The U .S . Geological Survey has adopted the following classification :
Hardness range(calcium carbonat e in ppm) Hardness description
0-6o
Soft
61-120
Moderately har d
121-180
HardMore than 180
Very hard
For public use, water with hardness of about 200 ppm generally requires softening treatmen t
(Durfor and Becker, 1964) .
Sodium-adsorption ratio (SAR )
The term "sodium-adsorption ratio (BAR ) " was introduced by the U .S . Salinity Laboratory
Staff (1954) . It is the ratio expressing the relative activity of sodium ions in exchang e
reaction with soil and is an index of the sodium or alkali hazard to the soil . Sodium-
adsorption ratio is expressed by the equation :
SAR = Na+
J Ca+++Mg++
2
9
where the concentrations of the ions are expressed in miliiequivalents per liter (o r
equivalents per million for most irrigation waters) .
Waters are divided into four classes with respect to sodium or alkali hazard : low ,
medium, high, and very high, depending upon the SAR and specific conductance . Water varie s
in respect to sodium hazard from that which can be used for irrigation on almost all soil s
to that which lo generally unsatisfactory for irrigation .
Specific conductance (micromhos per centimeter at 250C )
Specific conductance is a convenient, rapid determination used to estimate the amoun t
of dissolved solids in water . It is a measure of the ability of water to conduct an
electrical current . Commonly, the amount of dissolved solids (in parts per million) i s
about 65 percent of the specific conductance (in micromhos) . This relation is not constant
from well to well and it may even vary in the same source with changes in the compositio n
of the water (Durfor and Becker, 1964) .
Specific conductance of most water in the eastern United States is less than 1,00 0
micromhos, but in the arid western parts of the country, a specific conductance of more tha n
1,000 micromhos is common .
Hydrogen-ion concentration (pH )
Hydrogen-ion concentration is expressed in terms of pH units . The values of pH often
are used as a measure of the solvent power of water or as an indicator of the chemica l
behavior certain solutions may have toward rock minerals .
The degree of acidity or alkalinity of water, as indicated by the hydrogen-ion conce n -
tration, expressed as pH, is related to the corrosive properties of water and is useful i n
determining the proper treatment for coagulation that may be necessary at water-treatmen t
plants . A pH of 7 .0 indicates that the water is neither acid nor alkaline . Readings pro -
gressively lower than 7 .0 denote increasing acidity and those progressively higher than 7 . 0
denote increasing alkalinity. The pH of most natural ground waters ranges between 5 .5 and
slightly more than 8 .
SELECTED REFERENCES
Abbott, G . A ., and Voedisch, F . W ., 1938, The municipal ground-water supplies of North
Dakota : North Dakota Geol . Survey Bull . 11, 99 p .
Dingman, R . J ., and Gordon, E . D ., 1954, Geology and ground-water resources of the For t
Berthold Indian Reservation, North Dakota, with a section on chemical quality of water :
U .S . Geol . Survey Water-Supply Paper 1259, 113 p .
10
Durfor, C . N ., and Becker, Edith, 1964, Public water supplies of the 100 largest citie s
in the United States, 1962 : U .S . Geol . Survey Water-Supply Paper 1812, 364 p .
Geological Society of America, 1963, Rock-color chart : New York, Geological Society o f
America .
Hem, J . D ., 1959, Study and interpretation of the chemical characteristics of natural
water : U .S . Geol . Survey Water-Supply Paper 1473, 269 p .
Jensen, H . M ., 1962, Geology and occurrence of ground water near Bowbells, Burke and War d
Counties, North Dakota: North Dakota State Water Conservation Comm . Ground Water
Studies, no . 42, 65 p .
LaRocque, G . A., Jr ., Swenson, H . A ., and Greenman, D . W ., 1963a, Tables of hydrologic data ,
Crosby-Mohall area, North Dakota 1945-1951 : U .S . Geol . Survey open-file report, 508 p .
_1963b, Ground water in the Crosby-Mohall area, North Dakota : North Dakota State Wate r
Conservation Comm . Ground Water Studies, no . 54, 57 p .
Paulson, Q . F ., 1954, Geology and occurrence of ground water in the Stanley area, Mountrai l
County, North Dakota : North Dakota State Water Conservation Comm . Ground Water Studies ,
no . 23, 59 p .
Schmid, R . W ., 1962, Ground water conditions in the vicinity of Parshall, Mountrail County ,
North :Dakota, with pump test analysis by V . E . Ziegler: North Dakota State Wate r
Conservation Ccmm . Ground Water Studies, no . 41, 31 p .
U .S . Public Health Service, 1962, Drinking water standards, 1962 : U .S . Public Health
Service Pub . 956, 61 p .
U .S . Salinity Laboratory Staff, 1954, Diagnosis and improvement of saline and alkali soils :
U .S . Dept . of Agriculture, Agriculture Handb . 60, 160 p .
Wentworth, C . K ., 1922, A scale of grade and class terms for clastic sediments : Jour . of
Geol ., v . 30, p . 377-392 .
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LOCAL WELL 016IF NETNOD DATE WATER LEVEL WATER TYPE COIF TOOE- QI AVAIL- PER- LEVEL TOTA .WELL
IRIIISLEOWNER DEPTH
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ISINONW13DAA H . ANDES 6S 16 ! 1911 27 6-66 H J S 6 -- K -- - 01SEM069Y 14000 J .JENSON SO S 6 195* OG Sl 20 H J S 6 -- K -- -- NIIINDMIG66A L .9 .ENLEE7 151 S -- - -- 130 S -- -- -- -- -- -- NISINOME19000ISINOOOW24UDA
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ISIM69WSDAA N .PETERSON SE 24, 6 - 32 -- H P S 6 K -- 43 NISIME9Y306001 E .YANNER 110 4 6 1932 TL OC 36 6-66 S P 5 5 K D 43 0IIINOSg3066E2 E .YANIIER N 5 C 1962 TL ,OC 57 6-66 H J S 5 K -- 0131N0691300DD Y .H .VORYEEK 100 4 0 1917 SO - H P S 6 K -- 41 NISINO09WDIOCA J .YOKEN 36 16 6 1921 04 Sl 7 6-66 H P S 5 K -- 40 0
ISIN01PIW33000 E .I .ANENUO 127 4 C 1917 -- 110 K S S 4 -- K D - NISIN0f9W3•A00 K .STEELE 66 6 11901 -- 40 N P I S -- K -- 43 N1SIN00NlWM K .STEELE 40 24 • 1960 -- 20 S P F -- - K -- 43 NISEN0~911360N U .S .G .S. 140 H 1966 U
-32076 GE N 140
IS1N090W03A66 A .HEDGEKG 96 6 C 1924 06 51 52 K P T 6 -- K -- 44 N
ISINO90Y03/AA N .O .S .W .0 S2 - H -- -- -- -- U -- -- -- -- 0 -- N 52ISIND9E11OS00O E .6RENOLE 154 6 K NISIN090VOSCN C .M .JOINS0N 140 4 H 1963 105 -- K S S 4 K -- -- NISINONIONA01 P .A .HILLEEEN 27 16 6 1941 TL OC 24 H P S 4 K -- N151N0901106DA02 P .A .HILLEREN 13 IS 0 1944 TL OG 11 6-66 5 C S S K -- 43 0
ISIN090614ACAI J .O .SARTEL5ON l6 4 H 1960 TL OC 7 -- N P 5 5 -- K -- NISINSNWI4ACA2 J .D .SARTELSON iD 4 0 1949 TL OC 7 - S P 5 5 - K 42 N1SI11090Y/MY C .S .VANIIORN 160 3 C 1920 TL OC 150 -- K P S S -- C NISSNONY20DADI 6 .J .WALDOCK SO 24 6 1926 TL -- - S P 5 6 -- K 42 N1511019ON200A02 O .J .WALDOCK 235 3 H 1954 TL OC 221 -- H P S 6 -- K -- - N
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CASING WATERAPE -CIPIC ALTI- LOG TEN-
FREQUENC YOF WATER-
LOCAL WELL OIAM- METHOD DATE WATER LEVEL WATER TYPE CON- TUDE- OY AVAIL- PER- LEVEL TOTAL
WELL OWNER DEPTH ETER DRILLED DRILLED AQUIFER LEVEL DATE USE LIFT POWER DUCT OF LSO TYPE ABLE ATURE MEASURE- OE/TM
NURSER IFT .) 11N.) 'YEAR) IFT .) MEAS . AMCE (FT.I I
Fl MENU
1SINO91WOISIC L .ANTON 80 30 8 -- -- 60 -- -- N
SSIM091MO280C1 WOILENSCNLAGER 126 4 C 1962 TL OC 37 S P S 6 -- K 47 N
1310091W0210C2 WOLLENSCHLAGER 122 4 C 1965 TL OC 37 H S S 6 -- K N
ISSN091MI11SS R .A .ORENOLE 160 4 C 1956 K P 7 6 -- K - 43 N
IVINONIW26CAA C .A .LEE SS 4 C 1917 TL OC 40 K J S 6 -- K - N
ISSN092003000 U .S .G .S . 300 - H 1967 - U -- 1900 - - GE - N 300
151N092004S80 J .P .MOST 152 4 1927 06 51 145
, -- K P S 6 -- K 46 N
ISIM092MO6AAO L .O .ANOERSON 150 4 C 1920 0G 51 135 - - M P S 6 -- K 46 N
151N092M0S088 U.S .G .S . 220 -- H 1967 -- -- -- U 1925 -- G N 22 0
1SIN09281SAD0 D .LITTLEFIELD 265 6 -- -- -- 120 -- S P S 7 -- K - 47 N
ISINO92WIS800 M.SAND 6S 4 C 1964 OG S1 60 - H P 6 K M
531N091822000 U.S .G .S . 240 -- H 1967 -- -- -- U -- 1899 - - GE -- N 240
I51N092623CCA L .LUNO SR . 125 4 -- -- TL OC 44 10-66 U P -- -- -- 0
ISIN092W30AIC L .L .STOUT 26 IS 0 1925 OG 31 l4 10-66 H P 5 -- K 45 0
ISlN092831AAA U.S.G .S . 60 -- H 1967 -- -- - U -- -- 1968 -- G -- N 60
151N092831500 0 .R.HAMSON 62 24 8 -- -- 51 --N
151110921233C0C M.NIVA 44 24 -- -- -- 7 -- N
1S1M092W340AA U .S .G.S . 138 1 M 1966 OG 51 76 9-66 U N - 4 1891 C GE 47 M 20 0F.."
1310093003080 L .E.PENNIMGTON 109 4 C 1963 TL OC 84 10-66 S S 5 7 -- K 47 ' O
131M093W030E0 L .E.PENNINGTON 30 24 8 1948 TL OC 16 10-66 S P S 6 -- K -- 44 0
1510093W09AC8 C .B .SMDBE 180 4 C 1954 TL OC 160 -- S P G __ - -- N
ISIN093W0908A C .5.5HOBE 38 1 V 1960 06 31 30 -- S P P -- -- --
1510093814065 0 .0 .0010106 50 24 8 -- TL OC 38 -- U P 1 -- --
IS1N093WISCDA P .EVENSON 172 -- C 1962 TL OC 166 10-66 K S S K - O
ISIN090116K0 C .8 .SM08E 150 6 C 1951 TL OC 36 10-66 K P S 5 2185 C SO 0
1S1M09SW2108A C .1 .SH00E 129 4 C 1952 -- 69 - - S P 1 -- - -- 0 -- N
1510093022000 U .S .G .S. 450 -- H 1967 -- -- -- U -- -- 1986 - - GE - N 45 0
1510093023000 U .S .G .S . 120 -- -- 1966 -- -- - - U -- -- 1935 - - GE N 120
1501093W280CD A .BANGPN 56 24 8 1952 TL OC 43 -- H P F 4 -- K 47 N
151N093828000 A .EANGPN 94 4 C 1951 TL OC 80 K P S S -- K 0 47 N
1510093W29A00 C .8 .SHOSE 270 4 C 1952 TL OC 253 K P S 5 K.. -
0--
40
--
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N
300151N0931133C88151N093N34AAC
G .LARSENE .WENINGER
7 834
424
- --
195 2--
- ---
2024
US N
1310693053009 M .S .SANGPN 274 3 C 1950 TL OC 170 K P S 5 K 0 SO N
552N08080260C1 A .C .LVNNE 48 24 D 1906 43 H J S S K -- - N
I52008EW02ADC2 A .C .LYNNE 48 6 D 1960 -- 44 -- U P 1 S K 44 N
132810S0804118 PLAZA 90 12 H 1959 -- 45 4-67 P S T S C D 45' 0 100
ISZNOSSWOSOAD R .VANECKMOUT El 4 C 1957 TL OC 34 - - H S S 6 K N
152N088W06AAC1 W .A .SPLETSTOSER 60 6 C 1951 TL OC 12 6-66 U N -- -- -- 0
152N088W06AAC2 W .A .SPLETSTOSER 65 6 C 1936 -- -- -- U P 1 -- -- N
LOCALWELLNUMBER
OWNERWEL LDEPT HIFT .)
CASINGDIAM-E'E R(IN .)
METHODDRILLED
DAT EDRILLE D(YEAR)
AQUIFERWATE RLEVE L(FT .)
WATERLEVELDATE -MEAS .
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SPE -CIFE CCON-DUC TANCE
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152N088W23ADA2 E .J .GIESEN 115 4 C 1961 -- 40 -- S P S 6 K -- -152N088M23ADA3 E .J .GIE5EN 60 18 8 1962 -- 10 6-66 U P L 7 K -- 4 1152N088W24ABA B .S .SHAW 100 6 C -- TL OC 54 -- S P S 6 K -- 4 2152NO88W28888 M.A .KREFT 191 5 C 1952 OG 51 -- -- K P S 6 K 4 4152N088W328AA O .SPLETSTOSER 140 6 C 1940 -- 110 -- S P S 7 -- K 4 4
152NO88W35AAAl R .E .CHRISTEN50N 120 6 C 1920 -- 110 U P S -- -- -- -- - - NE5ZNO88W35AAA2 R .E .CHRISTEN50N 24 24 a 1912 -- 6 6-66 U P 1 5 -- K 44 0152N089W018RB U .S .G .S . 120 -- -- 1966 U -- -- -- 2091 -- GE - - N 120152NO89WO288B1 O .BRAAFLAT I50 4 C 1957 TL OC 142 -- H S S 5 -- K - - N152N089K028B82 0 .8RAAFLAT 60 18 8 -- TL 0C 55 -- S T S 5 -- K -- -- N
I52N089WO4A8A R .SCHNASE 85 24 B 1914 TL 0C 72 K P 6 5 -- K -- --152NO89W05BAC L .EYENSON 119 4 C 1920 -- 89 K P 5 5 -- C 4 5
T152N089W06AA0 U .S .G .S . 40 -- H 1966 -- -- -- U -- -- -- 2111 -- C - - 40152N089WO60AO J .A .MANLAL 90 4 C 1958 TL 0C 75 -- K S S 5 -- K -- - -152NO89W08000I G .RUUD 125 24 B 1964 TL OC -- H P S 5 -- K -- 4 5
152N089WOBCCC2 G .RUUO 110 6 B 1928 TL OC 90 -- S P S 5 -- K152N089WI3CDC C .A .HOLMSTRON 120 4 -- 1956 -- 41 6-66 K S S 6 -- K -- 44 0I52N089NSSC88 8 .8AARDSON 125 6 -- 1909 TL OC 100 -- U P 1 6 K 4 3152NO89W19ADC M .WERLINGER IO -- g -- OG 31 - -- 5 P F 5 -- K 78 N152N089W19BCC E .AVERY 155 4 C 1960 -- 67 -- H 5 5 6 -- K 4 8
I52NO89W228BC1 D .L .WENIEL 80 -- 8 -- -- -- S P S 6 -- K 4 31S2NO89W22811C2 D .L .WENZEL BO 4 8 1957 -- -- U P S 6 K -- --152NO89W23CDB1 8 .CD-CLOUGH 10 6 V 1946 -- H J S 6 K - -152N089W23CD82 R .COLCL000M 12 32 D -- -- 30 6-66 5 P 5 6 K 3 9152N089M23CD83 R .COLCLOUGH 7 48 D 1964 -- 4 6-66 5 P 1 6 -- K 4 2
1S2NO89R25DAA A .WOESSNER 101 18 8 -- -- 59 6-66 U P S 6 K - - 0I52NO89W27AB8 N .D .S .W .C . 52 -- H U N 52I52NO89H2TC80 K .NESS 23 42 0 1933 LI H P 1 4 K -- 41 N152N089W29CCCI S .ESTVOLD 30 24 8 1920 OG 51 -16 -- S P 5 5 -- K 41 N152N089W29CCC2 S .ESTVOLO 30 24 B 1950 OG 51 16 -- H J S 6 K - - N
152N089W290AD N .D .S .Y .C . 74 U -- -- -- -- P D N 65152N089W30ACA N .D .S .W .C . 65 -- -- -- u -- -- 1949 -- D N6 5152N089M30 C
152N089Y 30C RC BCN .D .S .W.C .N .D .S . M.C .
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1I52N089W3008A N .O .S .Y .C . 63 U 1933 -- 0 -- N 63
SPE- FREQUENCY
CASING WATER CIFIC ALTI- LOG TEN- OF WATER-LOCAL WELL DIAN- METHOD DATE WATER LEVEL WATER TYPE CON- TUDE- OW AVAIL- PER- LEVEL TOTA LWELL OWNER DEPTH ETER DRILLED 'DRILLED AQUIFER LEVEL DATE USE LIFT POWER DUCT OF LSD TYPE ABLE ATURE MEASURE- DEPTH
NUMBER IFT .1 1111.1 IYEARI IFT .l MEAS . ANGE IFT .1 1
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IE2NOW9W30006 N .D .S .W .C . 73 1964 P 0 N 7 3132N089W30000 S .ESTVOLD 30 24 6 1953 OG 51 16 - 5 P S 6 K 42 N1S2NOB4WSIAAA N .D .S .W .C . 52 U » -_ _- 1964 -- D N 52152N089W31A$A N .D .S .W .C . 63 1940 - D - N 6 31S2N089WS16ARl W .L .NELSON 34 24 B 1950 -- 19 - H P S 6 - K - -- N
L52NOA9WS18AB2 W .L .NELSON 57 4 C 1956 -- 19 - 6-66 U N -- -- 0
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IS2NO90WOICOD N .MOVDA 45 24 8 1963 12 10-65 H P S 6 K -- 01S2N090W02CDO R .BARTELSON 225 4 C 1954 TL 0C 140 -- K P S 6 C 45 NI52NO90NO3ABA U.S .G .S . 140 -- H 1966 -- -- -- U - -- - 1956 GE -- N 140152ND90WOBACD N.D.S .W .C . 105 -- P 0 - N 10 5152N090W12ABB J .NERMANSTAO 80 24 8 -- TL OC 78 -- H P 6 -- - N
1S2N090WI31BC W .EVANS 50 24 42 -- K NIS2B090WI3CCCI S.HOFF 66 24 6 - 60 - K S S S C 47 NI52N090W130002 U.S.G .S . 120 H 1966 -- - U -- -- 2057 - 0 - N 12 0152N090WI30AA O.SKOGEN 450 2 C 1921 -- 200 -- 5 P 6 6 -- K 45 N152N090WI4CDC H .GEVING 60 24 6 1945 -- 54 - H P S 5 K -- N
152N090W14DDO N.O.S .W .C . 21 __ -- -- U » -- - D - N 21152N090W153AA M.NONSON EST . 64 24 B 1914 TL OC 57 -- U P S - -- -- N152N090W17CDO C.CLENENSEN l2 48 D 1940 -- 9 -- K P 5 S -- K -- - N152N090W17000 F .CLENENSEN 12 48 D -- - 9 K P S NIS2N090WI8CCC U .S.G .S . 79 1 H 1966 QG 51 14 5-66 U N - 6 1800 C EG 46 N 9 5
152N090WIBDDO B.H.DETIENNE 81 24 - - - '32 - K -_- -_ -- N
152N090W19000 E.I .DANIELSON 80 24 B 1912 60 -- H S S S __ K -- -- N152N090W20AOC H.F .OEBERTIN 120 4 C 1957 TL OC 80 - K P B 6 K -- 46 N152N090W20A0 0152N090W20000
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CASING WATERSPE -CIFIC ALTI - LOG TEN-
FREQUENC YOF WATER -
LOCAL WELL DIAN- METHOD DATE WATER LEVEL WATER TYPE CON- TUDE - OW AVAIL- PER- LEVEL TOTA LWEL L
IWINGEROWNER DEPT H
IFT .1ETER11N .1
DRILLED DRILLE D(YEARI
AQUIFER LEVE LIFT .)
DAT EMEAS .
USE LIFT POWER DUCTANCE
OF LS DIFT .1
TYPE ABLE ATUR E1
FlMEASURE -
RENTSDEPTH
1S3N090WIOBBA S .SKAAR 104 4 -- 20 NIS3N090WIIDOC S .SJOL 100 6 -- TL OC 16 N153N090WISDOD U .S .G .S . SO H
--2101 GE N BO
153N090Nl6BBC H .FEVOLD lBS 4 -- 75 -- NI330090WI9BOA O .WEFLEN 136 4 -- TL OC 72 S C - 4T N
ISSN090N20BCB H .NESHEIM 200 6 130 K _- _- N153N090W23BAB D .DISSERUO 116 6 C 1966 TL 0C 99 H S 5 4 K 42 NSS3N090W26BBB H .TYGE 7l 24 -- -- 64 - - --
MIS3N090W29CBB F .HAUGE 100 -- -- 1942 -- 35 K -' -- -- NI3)NO90N30BAA J .MCNAMARA 165 4 -- -- - 2 K
1S3N090W32AB0 G .MCNANARA 320 4 C 1965 TL OC 170 - K S S 6 K 44 N153N0EOB36AD E .OLNSTEAD 25 42 B 1964 OG 31 22 K P S 5 K 43 NIS3N091W04AAA J .LABRANT 25 16 8 7 B-67 H B t 4 K 01S3N091W09660 H .OLSON IS 24 -- I9S9 QG 31 10 -- K NIE3NO91BI0BB6 C .DOCKEN 169 6 C -- TL OC 153 -- K P S 6 K 44 N
1S3N091W1000A L .LOCKEN 60 24 -- 20 -- K NIS3N091Wl1BBA A .LONTO 20 24 0 OG 31 17 - H P S 4 K 42 NIS3N09IWIS$B6 H .WELK 9l l4 0 1907 TL OC 60 -- S P S 4 K 42 N
Ir 1S3N091WI7ABA F .SANO 312 C -- 2S0 S P 5 6 C 42 NISSN09IW19CAC E .JOHNSONBERG 60 l6 6 1956 - 2B -- H P 5 S K 42 N
ISDN09IW210BBI L .ANNALA 30 24 B 1950 0G 31 16 -- H J S 4 K 43 NI53N041N21DBB2 L .ANNALA 90 24 6 - OG 31 70 - U P l - -
--N
IS3N09IW2NCCC K .OLSON 40 24 6 1944 QG 31 23 -- K S S 4 K - 43 N1S3N091W26AAD D.MCNAMABA 200 6 -- 1960 TL OC 163 K S S 4 K 4S N1S3N091M21CCC U.S .G .S . 100 -- R -' -- -' -- U
207W -- GE -- N 10 0
IS311091W32CBC U.ANNALA 240 4 C 1960 -- 120 - U -- -- D -- N 25 9IS3N091W320C R .CEYNAR 60 4 40 S N15311091W340A0 E .TOLLEFSON 100 24 8 TL OC 93 -- K S S 4 K -- 44 NIS3N091W3SOCC . C .NONSON 155 4 C 1960 9S -- K S S 6 -- K -- 4S N153N092V17BCA R .MAN 32 6 C 1960 0G 51 20 -- S S 11
1RI11092WI2BBC L .FLAOELAND 20 40 0 1914 06 31 12 11-65 K S 4 K 45 0IS3NO92WITBBB U.S .G .S . 41 I H 1967 00 Sl 6 B-67 U N 1978 G N 601S0M092W17B0A R.MAN 56 6 C 1960 TL OC 26 -- K S S 6 C - NIS3N092Wl9CCC U.S .G .S . 40 H 1967 -- -- - U 1964 -- OG N 60IS3M093W11AOC D.MAN 10 . 72 0 -- -- 6 -- K N
I5DN093W14AAA L .CURREN 44 S -- -- - 36 -- H NISSNO93W2SCCA B .B06GENBUCK 62 24 -- -- - SO -- K N1S3IO11OVI9BA0 W.EDWAROS 7S 46 - - - SS K N1S4NOBBWOICBB J .SAN000IST 100 3 -- -- -- 100 K S 4 C - 44 N1S4MOBBW02BM N.CARLSON SS 24 -- -- -- BO K N
LOCA LWEL L
NUMBEROWNER
WEL LDEPT HIFT.1
CASING01A8-ETE RTIN .)
METIIOODRILLED
DAT EDRILLE DITEARI
AQUIFERWATERLEVELIFT .1
WATERLEVELDATEMEAS .
WATERUSE
TYP ELIFT POWER
SPE-CIFI CCON-DUC TANCE
ALTt -TUDE-
OF LSDEFT .,
O WTYPE
LO GAVAIL -ABLE
TEN-PER -ATUR EI
Fl
FREQUENC YOF wATER-
LEVE LMF4SURF -
8ENT5
TOTALDEPT E
154NO88N048C8 L .RINGOEN 85 24 B -- -- 40 P .5 6 K 441546088405000 G.AAS 40 24 -- 3 5154NO88W0TCNC H .TRULSON 22 18 0 1951 16 S 5 -- K -- 44154N088WOT000 H .TRULSON 264 4 -- -- TL 0C 8 0154NO85WO98AA COMMON 130 24 8 0
154N088W118WC F .JDIINSON 185 4 C -- TL 0C 80 S 6 K 43 N1545700 .11D0C G .JDNNSON 92 24 -- -- -- 7 5154NCBdW14C(C V .JOHNSON 149 4 90 -- N154MO55NI5CBB F .PEASE 145 4 C -- -- 127 P 5 7
K
44 , NI54N085N10C88 G .STIND 128 4 C 1963 -- 90 S 5 5 K 43 N
IS4NC88M20ADD E .THUNSHELLE 220 4 C 1963 TL OC 150 S S K 45 N1S4NOR8K2I000 H .THUNSHELLE 60 4 -- -- -- 45 N154N088422CBC 0 .058E10 24 24 -- -- -- 15 A1541088425000 L .SWANSUN 170 4 -- -- -- 88 8-67 P n154N08882500 L .SMANSUN 180 4 -- -- 12 0
I54MC88W29CTC W .ASHLEY 115 24 8 -- 90 8-67 U PI5ANO88W72AB6 C .OLSON 6S 24 8 35 S p S 5 4 3
3 1S4NO89WG20DA I15440598020002
J .MOE NJ .MO7JT
3625
2 448
8D
1950 -- 3 114 10-65
HS
PP
sS
-5
I54NCB9WO8R58 E .HA18F 115 24 8 1941 100 K P S 6 K
1S481084814COD J .EOWARDS 28 24 8 1916 - - S P S 4 - - K 4 5154N089W1+000 U.S .G .S . 40 -- H 1966 -- -- - - U 2050 UG Sc154NOS9W15COD U .S .G .S . 100 -- -- 1966 -- -- - - U 2096I54N089N15005 U .S .G .S . 58 1 H 1967 -- 15 8-67 U 6 2(m:' C
E46 18800
1548089819000 L .HORST 65 z+ B 1919 OG 31 59 S P S 6 - - K 45
154N089W240A01 R .GROTTE 254 6 -- 1964 TL OC 80 H P S 6 K _ _15411089W240602 R .GROTTE 65 24 6 1912 -- - - 5 P S K -- 44154NO09W288CC H .WOESSNER 107 4 C 1963 TL 0C 67 H P 5 6 K - -I54NO59W70D00 A .KULLANO 132 6 C 1956 -- 107 S P S 7 C 4 5154010899350811 O .HALLINGSTAD 91 24 8 1918 -- - - H P S 6 K - -
154M09OW03AAAI M .JOHNSON 100 24 B 1917 98 -- S P S 44 N1S4N090W03A8A2 M .JOHNSON 50 24 B 1954 -- -- -- H P 1 N134110908036A83 M .JOHNSON 145 4 C 1967 95 -- K S S 45 N154NC9OW04DDD H .HOSETH 82 24 B 1941 64 -- S P S N154N090W068801 WM .WIIITMORF 177 3 C 1935 161 6-67 U P 5 44 0
15481090W065802 MM .88ITMOR2 30 24 B 1955 OG
31 75 K P S 6 K 44 N1549090W068809 WM .WHITMORE 207 4 C 1967 -- 160 - - S P S 7 K -- 44 N154N090W06CCA WM .WHITBOME 217 4 C 1961 -- - - S P F 7 C D 45 N154NO90WE2000 C .NEWMR7 60 1B 30 H P S s K - -154N090W14000I 0.1808108 30 IB 8 1943 -- 13 10-65 S P F K -- 0
SPE- FREQUENC YCASING WATER CIFIC ALT1- LOG TEM- OF MATER -
LOCAL WEIL 01AM- METHOD DATE WATER LEVEL WTER TYPE CON- TUOE- OW AVAIL- PER- LEVEL TOTALNCLL
NUWNhK0WNFk DEPT H
IFT .)FIF E11N .)
',KILLED DRILLF O(YFAR)
AQUIFER LEVE LIFT .)
DAT EMEAS .
'SSE LIFT POWER DUC TANCE
OF LS DIFT .)
TYPE ABLE ATON E1
FlMEASURE -
MENTSOEPT H
ISNSON04IwCCC2 G .JIMYSUN 70 24 B 1941 10 I0-65 S P 1 -- -- -- -- UI54NC9Q .17CWBI S .MOSFTN 7S IB X 1954 46 -- K P S 7 -- K -- 44 N1545090 .I7CBB1 C .HOSETH 75 24 B 1933 65 U P S N
154N097819COD J .FINGFR IGO 24 B 1940 -- - - -- S P S 6 - C 44 N154N091813000 U .S .G .S . 120 -- H - - -- U -- -- -- 2300 -- GE -- N 12 0
I54NC9C .74CC.O MRS.JENSON 18 48 - - -- - - K P 1 5 K -- N1S4N09C .27CCH H .WOESSNFR 4? 74 B 1957 OG 51 9 K P 5 6 -- K -- N154809C .12XAB1 L .DIHRLE 81 -- D -- OG 51 4 S S S -- -- -- -- NISnNC90.24MA62 L .DIBBLF -- 49 D 1957 OG 31 - - H P 5 4 -- K NI54NC91 . 1CLA F .FVANS 17 24 B 1962 TL OC 14 S N -- -- -- -- N
I54NC918C600C F .WILKE 97 24 B 1914 -- 92 -- K P 5 6 K -- N1548C91 .10AA8 R .JOMNSU4 22 14 B 1948 -- - - -- H P 5 5 -- K -- N154NC41411000 W .HENNING 2B 24 X 1909 OG 31 25 -- K P S 6 K -- 43 N1549C91 .150001 N .LAUKKALA 46 24 X 1961 EL OC 42 -- K P S 6 K 44 N154NO918I5CDC2 N .LAUKKALA 30 24 D 1919 TL OC 24 -- K P I 5 C 44 N
1548091k19CBA1 E .TILISTO 35 24 B 1928 -- 22 10-65 H B 1 5 K 45 01548091W2CAOAl E .80MER 93 4 C 1965 -- 73 U P S -- N154NC9182CADA2 E .BOIW ER 69 IB B -- - 43 K S S 5 15 -- -- NI54N09IN21DUCl S .GREEN 15 24 B -- OG 31 7 10-65 K P I 5 K 01544C91 .21DOC2 S .GREEN 15 24 -- -- 'AG 31 4 10-65 K S S -- -- 0
154N091827AOO A .JORGENSON 88 18 B 1942 -- - -- K P S 6 -- K -- -- N154M091830AAA U .S .G .S . I01 I H 1966 -- l9 8-66 U 6 2121 C G 48 M 1 W154N091W32CCB H .KANNIANFN 350 3 C 1953 TL OC 300 -- K P S 6 -- C -- 45 NI54N092803DAR A .NIELSON 138 4 C 1917 TL OC 1)0 U P 6 M
ISA8092WC4CCC F .NARTENS 70 4 C 1960 IL OC 8 -- K S S 5 -- C D -- N
1S4N09280708C 5 .ANDFRSON 203 6 C 1950 -- 113 K S 5 6 K D N154NC92WIOCDDI A .FLAOELANO 44 24 B 1929 TL OC 24 S P 5 N
154N092WI00002 A .FLAOELANO 32 24 B 1956 20 H J 5 N
- -1S4N092W126CC N .D .G .S . 94 -- -- 1966 85 8-66 U -- -- -- G 0 yB154N092W14CA8 J .CARKUFF 40 24 B 1941 -- 28 K P 6 4 K -- N
':;LD : 's2V 2 :X98 U .S .G .S . 100 -- H 1966 ._ U -- ._ 2120 -- DC -- R 10 0TL OCIS4N092M23DO0I C .ARNDT 35 24 8 1958 20 11-65 H P S -- -- -- -- 0
1S4MC92W310AC GIBS SPRINGS 0 -- -- F 5-67 K 5 C 4 5
1S9N093W04DOC A .UNREIN 39 4 C 1964 Q0 31 15 -- I --
- -- 4 K 42 NIS4N093W0S6U0 U .S .G .S . 80 -- H 1961 -- - - -- U -- -- -- 2330 -- .GE -- N 0 O154NG9SWC5CDD H .FRETHEIM 30 24 -- -- -- S P S 5 K 44 N
ISRN093WOS000 M .FRETBEIM 39 4 C 1964 14 H P S 5 C D 45 N
I54M093A09AC0 M .RANBEL SO 6 -- TL OC 44 K -- 4 NIS4N093W1511CC J .DIDIU 140 24 B — TL OC 11S S P S 7 C -- 48 N
194N093WZOCCD P .WEYRAUCN 85 4 1954 -- 70 K S S 6 K -- -- N
IS4N093N23AAD E .FRANOSDN 138 4 -- -- 125 K N
M91M9SdM--------4
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0--99SS9S9-99615 90266194Z5411539'S00,6006906451N91--9FSd9--SE1S 9051£6199E050595N364'90000006006641N11--99SdS------916109EItSNOS 1 503N'92339100690N041N9S5fH--SZ0E6109E2ESNOS 1 553N'91379119680N561N0M9SS9--OS.1S 9061617E141S3NAO'l9901099900651
N,SSn--16 00-09E21NO30N19'N,400E09909551OILN39--OSOZ------A----9961H-041'5'9'5'09090090908061
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002N39--4012------IT------9961H--010•5'9'5'099vS1MB909561001N37--1112------n----L961H--001S'9'S'A3334109908501
N------9SfN--1961--400163043'09941190908551
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002N--39I61Z----n99-BE£11S 909961N1E915•9'S'n00090909305015dS------956E--4051109.09909589900541
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-90198 10-831901-111V71117931909N1SV3£383110103-3dS
SPE- FREQUENCY
CASING WATER CIFIC ALTI- LOG TER- OF WATER-
LOCAL WELL DIAM- METHOD DATE WATER LEVEL WATER TYPE CON- TUDE- OW AVAIL- PER- LEVEL TOTAL
WEL LNUMBER
OWNER DEPT H01 .1
ETE RIIN .1
DRILLED DRILLEDIYEARI
AQUIFER LEVE LIFT .)
DATEMEAS .
USE LIFT POWER DUC TANCE
OF LSOIFT .I
TYPE ABLE ATIM E1
FlMEASURE -
MENfSDEPTH
I9SMO89W24ABS A .STRAND 30 24 0 - - -- H -- 1 N
ISSN089W25AC81 L .OYNES 80 6 H 1965 OG SI 12 10-66 I S T 6 C 44 N
ISSN08W25AC82 L .OYNES 60 1 H 1965 OG 51 14 9-66 U N -- 5 2036 -- G 46 M
I3MN089W2SACB3 L .OYNES 56 l_ H 1966 OG 51 15 9-65 U N -- 5 2037 K GO - 0
I5SNOB9W25AC84 L .OYNES 46 t ' H 1965 OG 51 12 9-65 U N -- 5 2034 K GO 47 0
ES5N08W2SECC U .S .G .S . 89 1 H 1965 OG 51 0 9-66 U -- -- 6 2028 C G M 100
15SMO$9W25B00 L .OYNES 54 1 H 1965 0G 31 8 9-65 U N - 5 2029 K G 0
IQNMOW9W25000I E .MAHLUM 12 36 0 1907 -- 7 7-65 K P F 5 K 47 0
1SSM089W2QCCC2 E .MAHLUM 12 l8 0 1959 -- 9 -- S P F 5 K 45 NISSMOSMY260CB1 W .MEYER 67 6 -- -- -- F -- -- N --
l3IMOS9W260C82 W.MEYER 22 24 B 1959 OG 51 9 9-65 S S 5 K -- 48 0
15SN089W260CB3 W .MEYER 20 2 V 1948 -- -- -- H 1 4 -- K -- 46 N
INQMOR9W27DOD O .SDLBERG 80 24 B TL OC -- S F 5 K 46 N
ESSMOSVW32AAA U .S .G .S . 38 1 H 1966 OG 51 13 9-66 U -- -- 6 2035 K GE 56 M 700
ISSIIOSW34AAAI C .SHERVA 22 48 D 1935 -- 20 -- K S
1SNMOS9W34AAA2 C .SHERVA 12 8 D 1964 5 -- S P S N
ISSN089W33AEA U .S .G .S . 38 I H 1966 W 31 20 8-66 U -- 4 2030 C G 47 N 60
17SNO90W02ABOL M .KVAMME 290 3 -- 1925 -- 100 -- U P 1 5 -- C -- 43 N
,'K ISQMOMOW02AB02ISSN09OW03AAA
M .KVAMM EU .S .G .S .
2 6240
1 8--
BH
- -1966
-- 1 7--
7-6 7--
UU
N--
---- 2135 -- GE --
ON 24 0
I5SN09WOS000 C .RHODES 28 24 8 -- OG 51 25 H P 5 4 K -- 44 N
15SN090WI10AOI K .RUGLAND 68 24 B 1949 58 8 J S 6 K 44 N
1SBN090111DA02 K .RUGLAND 232 3 C 1925 IL OC 80 -- S P S 6 -- K -- 43 N
ISSN090W12CAA A .OSTDAHL 12 48 -- -- -- 6 -- H -- -- 4 C 49 N
155N090112DDD U .S .G .S . 178 1 H 1966 OG 51 24 8-66 U N -- 6 2090 C GE 44 N 200
ISSN090W13ABC T .00LAN 65 24 B 1929 20 -- S P 1 5 -- K -- 44 N
1SSN090W15A0C A .OSTDAHL 26 24 B -- 11 7-67 S P 1 5 -- K -- 41 0
ISSN090W23C8CI DUNHAM BROS . 45 24 D -- 36 -- H J S 6 -- K -- 45 N
IS5N09ON23CBC2 DUNHAM BROS. 325 3 1932 225 -- S P 5 7 K 44 N
155N090W290DC 0 .1MUGEN 75 24 -- -- 65 -- K -- -- N
IS5N09ON30BBB1 O .HARSTAO 55 l8 B 1963 18 -- H J S 5 K 44 N
ISSN090W308882 O .HARSTAO 90 24 B -- 45 - 5 P 5 6 K -- 43 N
157NO90W31ABA L .WRIGHT 7S 24 B -- 28 7-67 K P S 5 K 40 O
153N090W33AA8 W .P .JOHNSON 16 48 -- -- 10 -- H - -- N
ISSN090W34000 C .LIEN 69 18 B -- 13 7-67 U P 1 6 K -- O
I55N090135BCC G .N .SAUBER 210 4 -- 1963 -- 150 K -- -
155M091W04ABA G .ENANDER 183 4 - -- 100 H S S 6 K 46 N
I55N091W04CAC D .JARMIN 120 4 C -- -- 5 P S 6 C 48 N
I5SN09LW04CCB D .JARMIN 128 24 B 1936 121 S, P 5 6 K 43 N
I55N091WIISAA S .SEVERSON 70 24 B -- 50 K -- - -
CASING WATERSPE-CIFIC ALTI- LOG TEEN-
FREQUENCYOF WATER-
LOCAL WELL DRAM- METHOD DATE WATER LEVEL WATER TYPE CON- TUOE- OW AVAIL- PER- LEVEL TOTALWELL OWNER DEPTH ETER DRILLED DRILLED AQUIFER LEVEL DATE USE LIFT POWER DUCT OF LSO TYPE ABLE ATURE MEASURE- DEPT HMONGER IFT .) 11N .) 1YEAR) IFT .1 MEAS . ANCE (FT .) 1
Fl MEN' S
1SSN091W11000 A .RUGSTAD 196 4 -- TL OC 100 — K P S 6 K — 44 N1SSN091K12AD8 A .KURTERUO 20 3Q B -- 12 -- K P 5 4 K 45 N15SN0OIW13CCA O.ARNOUR 27 24 C 10 K - - MISSN09IW15EEB155N091M1/ABA
J .HARSTADK .JOHNSON
5090
1818
e8
TLOC--
2 751
7-6 77-67
SU
JN
S--
6--
K 4S
_
00
1SBN09IW21ACA H .JDNNSDN 124 24 B - - 104 7-67 K P S 6 K 43 0155H0911123008 M .AMUNDSON 16 36 D - - 14 K NESSN091M2SBBBl ENGE BROS 14 48 0 10 — S P 1 5 K N15I$O91W25R8E2 ENGE BROS ITS 4 C 1966 80 -- H $ S 6 K 45 N155N091N25BBB3 ENGE BROS 210 3 H - - 100 -- S P S 6 K 44 N
ISSN091M260C6 R .CRAFT 18 24 -- - - 12 — K --N
ISSN091M278AC S .CRAFT 135 4 -- 1966 110 -- H -- -- — MISSM091W2ESAA H .MYNRA 70 18 a 1910 60 S P 6 -- — N155N091W31000 D .HILL 135 24 - - 85 5 -- NISSN092WO188C M .TNOMPSON 145 3 C 70 S P S 6 K 44 N
15SN092WO16RD J .TNONPSON 160 C -- S P 5 6 C 44 NIS50092W02AOA L .PIEPKORN 59 15 8 10 K P S S K 43 NISSN092W04C66 R .SIMONSON 134 3 C 49 6-67 S P S 6 K 44 0IS9N092W09AAA E .TABBERT 72 24 B 30 -- S -- -- - - _ N155N092W09ECA S .SORENSON 108 24 B 80 -- S — -- - - -- -- -- N
1550092Wl40AA1 J .ANDERSDNS 40 24 B 1928 35 K P S 6 K -- 44 NISSN092W14DAA2 J .ANDERSON 221 4 C 1956 194 7-67 S S S 6 K 01S5N092W17AAA H .LUNO 57 24 8 - - 37 -- S P S 6 K 42 N155N092WIBBEA G .GRAHAM 47 4 34 -- S - - -- NSSSN092MIRCDD J .CVANCARA 63 4 C 1960 40 -- K P $ 4 K 44 N
1SSN092W21DA01 C .PAN2ER 156 18 B -- 112 -- S S S 6 K -- 44 N15SN092N210A02 C .PANLER 60 18 8 56 H P S K -- 43 NISSN092W23000 U .S .G .S . 180 A 1967 U — - - 2274 -- 6E -- N 18CISSN092W24B6C BAKKE BROS 192 4 152 K -- -- - - N155N092W270AD H .STROEBECK 160 S 1908 125 K P S -- K -- 44 N
1SSN092V33DA R .OGDEN 230 4 -- 175 -- S -- -- - - N15511092W34D00 R.OGDEN 66 18 e - - 77 7-67 K S 5 5 K -- 43 0I55N093VOSAAD L .INGERBRET50N 320 4 C 1923 160 -- K $ 5 6 K -- 44 NISSN093WOSADA L .ENGEBRETSON 320 K S 5 6 C 49 NISSN093WOSRO0 N .O.G .S . 69 1966 60 8-66 U -- -- -- 6 -- 0
1SS1109IW0EOCC H.REHAK 144 4 C 1964 BS — K 5 5 6 K -- 44 NISSM093W0960C .. .PROCHASKA 89 11 6 1965 47 K $ 6 K 43 NISSN093WIORAA G .N.RV .ET AL 210 2395 -- 6 — N *501S5N093WIOBBR U.S .G .S . 60 H 1966 2416 06 N 601SSN093W12ABA C .SORENSON 42$ 2 C -- 300 K F S S -- K -- 44 N
CASING WATER CIFIC ALTI- LOG TEN-FREQUENC YOF WATER -
LOCAL NELL DIAM- METHOD DATE WATER LEVEL WATER TYPE CON- TUOE- ON AVAIL- PER- LEVEL TOTM
WELLNUMER
OWNER DEPT HIFT .l
ETER11X .1
ORILLL0 DRILLE D(YEAR ;
AQUIFER LEVELIFT .l
DAT EMEAS .
USE LIFT POWER DUC TANCE
OF LSDIFT .l
TYPE ABLE ATURE1
FlMEASURE-
MEN'SWEPTM
ISSN013W13AAA U .S .G .S . 223 4 H 1967 TL OC 121 6-67 U -- -- 5 2365 C GE - N 9501S90O951113 ► AA J .CVANCERA 175 3 C 1959 -- 90 S -- S 6 K -- 44 N15911093W17600 0 .808E5 90 3 8 - -- SO K $ 6 K -- 42 N13SN093821860 T .D08R080LNY 290 ' 2 C 1943 -- 200 K P S 6 -- K -- -- N1910093W22006 L .VACMAL 170 18 -- 1930 -- 160 K -- N
ISS0093W23AAA L .STETTNER 215 4 C 1964 - 151 7-67 K S S 4 C P 48 0ISSN09)W2SABA G .LAPICA 9l 24 8 1941 TL OC 70 K S S 5 K 42 N1810093H27800 L .CVANCARA 214 - 1964 -- 184 K 5 K -- NISSM093W28E88 R .008ROVDLNY 35 18 8 1964 -- 31 K S S 5 K 44 N
ISSN093W30A80 C .SPAfNY 97 24 8 -- -- 75 K P 6 5 K 43 N
13SN0931132000 F .CVANCARA 275 3 1962 -- 175 K -- __ 5 K -- N15511094W05858 U .S .G .S . 80 - H 1966 -- -- U 2232 DG N 8D
15311094W05808 M .HEGLAND 23 18 -- 1961 6 10-65 K P 3 4 c -- 48 0TL OCIS1WO94WOSCSA M .MEGLAND 76 '24 8 1911 5l 10-65 5 P S 6 K 45 0
1009094803808 8 .J0184504 15 24 1956 00 31 4 10-65 H J S 4 K -- -- 0
IS5N094W06DAA 8 .NESVIK 47 -- 8 -- OG 5l 11 10-65 S P 1 K 44 015511094W07868138N094WO68OC
9 .9E501 8V .THOMPSON
3 035
2418
8 1945 - ---
930
10-65 KH
- - K__
-- 4 7__
0N
3 15841094W140A01 D .REMAK 325 6 C 1943 TL OC 135 K . P S K -- N
IMO 444444444 O .REHAK 145 24 8 1930 TL OC 135 U P 6 -- __ N
15811094N150CA1 C .SLEMIN 16 24 0 1950 00 31 11 H J S 6 K
15SN0948158CA2 C .SLEMIN 14 36 D 1942 GIG 31 10 S P 6 K 46 N
1S511094M31DAD U .S .G .S . 60 -- H 1968 -- - - __ 2005 -- DG -- N 60
195N094H328C8 U .S .G .S . 80 -- H 1966 -- - - 2025 -- GE -- N 80
IS4M08WOS000 O .SVENNINGSON 410 4 C 1962 TL OC 130 K P S 6 K -- 44 N
ISWN088WO8DAA C .MALGRIMSON 445 3 C 1955 TL OC 100 S P S 6 K 43 N
(SW08WI288* 0. .GRANT 100 4 -- 38 K S S 5 K -- 44 N
1519018M126DA1 E .EVENSVOLD 101 4 C 1958 -- - H S 5 5 C 50 N
IS6N068N128DA2 E .EVENSVOLD 60 4 C 1966 -- 45 S 5 5 5 K 47 N
1SWNO88WI20CN TAGUS 130 6 C -- -- 60 P P 5 5 C -- 48 N
18111088W198C8 C .WIRT2 20 4 C 1963 -- 12 H J 5 4 K 44 N
1SWOSMW21WED R .MOEN 80 24 8 1926 -- 60 H P - 5 K 45 N
1S4M088W24DAA B .KILENE 200 4 C -- -- 125 K P S 6 K 44 N
1519088W318C8 J .LEE 64 4 C -- -- 56 H P S 5 K -- N
156N088N35C88 M .MUNTINGTON 18 24 D 1936 15 H P 1 6 K 42 N
156NO89NOIAADI 0 .8907505 18 12 0 1962 00
31 16 H J S -- N
1569089WOIAA02 G .KNUTSON 12 48 D 1910 00 31 7 S P S N
156N089WOIDA8 R .LIN08ERG 485 3 - TL OC S P S 4S N
15611089W02CCD1 6 .0L505 180 4 C 1961 00 51 70 S S S -- N
156NO89W02CCD2 G .OLS8N 35 24 R 1935 00 51 12 S P S 44 N
CASING WATERSPE -CIFIC ALTI- LOG TE M.-
FREQUENC YOF WATER -
LOCAL WELL DIAM- METHOD DATE WATER LEVEL WATER TYPE CON- TUOE- OW AVAIL - PER- LEVEL TOTALWELL OWNER DEPTH FIER DRILLED DRILLED AQUIFER LEVEL DATE USE LIFT POWER DUCT OF LSO TYPE ABLE ATURE MEASURE- DEPT HNUMBER 1E7 .1 IIN .1 1YEARI 1E7 .1 MEAS . ANCE IFT .1 {
fl MENT S
156NO89W020003 G .OLSON 20 24 8 1964 OG 51 6 K J S 5 K — NI56N089M06AAB U .S .G .S . 179 1 H 1967 -- 2 8-67 U N -- 6 2138 C G 46 M 30 0156NO89WIOBBBI F .BIERE EST . 40 24 B 1941 -- -- -- S P 5 4 -- K -- 44 N156N0B9WI08882 F .BIERE EST . 21 48 D 1954 -- -- -- H J S 6 -- K -- NISbNO89NIOBMB3 F .BIERE EST 18 24 O 1917 -- -- -- S P S 5 -- K -- 44 N
1S6N089W1368 1 G .ALVSTAD 220 4 1964 -- 100 S -_IS6MO89MI3BB 2 G .ALVSTAD 200 4 C -- -- 5 5 5 5 K 47 N15611089W13CBC1 E .GORSETH 214 4 C 1964 BN 7-68 H 5 5 5 K -- 49 0156NO89WI3C8C2 E .GORSETH 226 4 C 1963 TL OC _ -- K S S 5 -- K -- -- NI56N089WI4AC BLAISDELL 230 -- C 1967 5 5 5 C -- N
15w089ML4888 L .ROCK EST . 190 4 -- 1950 TL OC'-' -- K S S -- -- -- -- N156NO89Wl40AB E .ROCK 241 4 C 1965 TL OC -- S P F -- - -- -- NIS6NO89W19CCAl J .TANK 222 4 C 1962 QG 51 ILO -- K S 5 6 C 0 48 N156NO89W19CCA2 J .TANK 16 48 0 __ P __ __ N156NO119W20AAAl C .SIGLOH 55 24 B 1950 -- 40 K P 5 5 -- K 44 N
15BN089W20AAA2 C .SIGLOH 19 36 0 14 S P __ N156N0B9W2ODCA L .JONES 355 2 -- 1956 TL OC 155 H P S 6 -- K -- 44 NIS6NO89W230001 J .BIERE 50 4 C S -_ N1S6NO89Y24DAA U .S .G .S . 12o - - H 1966 -- -- -- U -- -- -- 2180 -- DG N 120156110B9W25ADDI P .LEE .JR . 14 4 V 1957 -- -- H S 5 4 -- K -- -- N
I5601OB9W25A002 P .LEE .JR . 18 4 V K P S __ NIS6NO89N245CB A .N00RE 345 4 -- 1956 TL 0C 90 -- K P S 6 C -- 48 N156NO90WOIAD8 M .KNUTSON 68 24 -- 1962 QC 51 20 -- K P S 6 K 44 N156NO90W020CD G .KUAHNE 100 3 C 1929 -- IB -- S P S 5 K 44 N
IS6NO90WO3BMA u .S .G.S . 180 H 1968 -- -- -- U -- -- 2268 -- GE -- N 18 0156M090W0380C E .WALHAUG 88
4
C 1965 OG 51 36 -- K J 5 6 -- K 0 44 NISBNO90WO4ABB U .S .G .S . 66 l H 1967 0G 51 37 6-67 U -- 4 2225 C GE 46 N 14 0156N090W048AB U .S .G.S . 140 N 1968 -- -- -- U -- -- 2320 -- GE -- N 14 0156M0901108CCAI E .NYBERG 40 24 B 1958 -- 12 -- N L S __
ISMU0HOW09000 W .HALVERSON 112 6 C 1965 TL OC 35 5 S 6 C -- NI56NO90WI000C H .GRINOLDS 50 24 D -- -- 30 -- S S 5 -- K 44 N1561109OM12CCD R .GRINOLDS 30 24 D 12 K S 6 K 44 NL56NO90B14CB8 A .HOLLEKIM 200 -- -- TL OC -- -- $ S 6 K 44 NIS61109OW15AA8I O .DUNHAM 30' 24 __ __ __ 13 _- H 5 -- N
I56NO9OWISAA82 C .RHODES 32 18 1968 9 7-68 H P 5 5 K -- 0156NO90MISAAC PALERMO 35 C -- 22 7-68 P P 1 5 -- L .I56N090W1588B156MO90W19DAC
U .S .G .S .O .NYHUS
10 0157
4 NC
19671959
----
----
US ' P S 6
2176 - -K
G E0
-45
NN
100
1S6110901119DOD U.S .G .S . 180 H 1966 -- -- -- U 2161 -- GE -- N 180
CASING WATER CIFIC ALTI- LOW TEN-FREQUENCYOF WATER-
LOCAL - WELL DIAM- METHOD DATE WATER LEVEL WATER TYPE CON- TUDE- DW AVAIL- PER- LEVEL TOTAL
WELLNIMBEA
OWNER DEPTHIFT .)
ETER11N .)
DRILLED DRILLE D(YEARI
AQUIFER LEVELIFT .I
DATEMEAS .
USE LIFT POWER DUC TANCE
OF LSOIFT .)
TYPE ABLE ATUEE1
FlMEASURE -NENTS
DEPTH
IS6NO90W210A8 G .RAINOAHL 120 4 C 1963 -- 75 -- K J S 6 -- K -- 44 N
I56N090W2688C U .S.G .S . 120 -- R 1967 -- -- -- U -- -- -- 2155 --
- GE -- N 120
1S6NO9OW3388A
' M .8INGEN 312 4 C 1938 TL OC 100 -- K P S 6 -- K -- 44 N
I56609IW02000 U .S .G .S . 214 1 H 1967 DG 51 55 6-67 U N -- 6 2185 C G 45 M 21. 0
156NOTIWC3C55 U .S .G .S . 240 -- H 1967 -- -- - U N -- -- 2220 - -- GE -- N 240
156NO91wC4CRC U .S .G .S . 230 -- -- 1952 -- -- -- U -- -- -- -- -- DG -- N
156NC9IW04000 U .S .G .S . 160 -- -- 1952 -- -- -- U -- -- -- -- OG -- N
156NO91w05AAA U .S .G .S . 90 -- -- 1952 -- -- -- U -- -- -- -- DG -- N
156NC91WO5C88 U .S .G .S . 220 -- H 1967 -- -- -- U -- -- 2240 -- GE -- N 220
1SANO9IwCSDAA U .S .G .S . 196 1 H 1967 OG 52 22 6-67 U -- 6 2180 C G 46 N 420
I56NC91w06ADO R .HADOEN 49 24 B -- QG S1 33 7-52 U
' P 1 -- -- -- -- O
1S6N091W06000 DRURY C OAVIK, 34 -- 0 1952 25 7-52 S P S -- -- -- -- 0
156N091w078AA 8 .HEMSTAO 40 -- B -- -- 26 8-52 K P -- -- -- -- -- 0
156NC91W08DAA W .RUDOLPH 46 24 8 -- -- 33 7-52 K P F -- -- -- 0
IS6N091w09888 U .S .G .S . 180 -- H 1967 -- -- U -- -- 2260 GE -- N 180
I56NC9IW09VCA B .INGEBRITSON 65 24 B -- -- 27 7-52 K P 6 -- -- -- -- ----
0
I56N091w090A0 U .S .G .S . 220 -- H 1967 -- -- -- U -- -- -- 2292 -- GE M 220
,x 156509IAI088 e1S6NO9IWIO00C
U .S .G .S .T .SCHJERVHEIM
12 860
124
MB
196 61915
OG 5 1QG 51
5 723
8-667-52
US
--P
--S
- 5 2303 C GE 45 N0
340
156N091W*ICDC U .S .G .S . 140 -- H 1952 -- -- -- U -- -- -- -- -- DG -- M
1S6N09IW138AA U .S .G .S . 140 -- H 1952 -- U -- -- -- DG N285
156N091W14AAA U .S .G .S . 284 -- H 1967 -- U -- -- 2197 -- GE N
1S6NO91W16AC8 U .S .G.S . 90 -- H 1952 U -- -- -- -- DG N
IS6NO91W16888 U .S .G.S . 140 -- H 1952 -- U -- -- -- DG N
1S6N09IW16CCA U .S .G .S . 250 -- H 1952 -- U -- -- -- DG N
156NO91W178CC S .JAHA 40 24 8 1940 -- 18 8-52 K C 6 -- -- -- 0
156NO91WIBDAA A .HASSEN 16 48 D -- — 10 8-52 U C 6 -- -- -- O
156N091W19AAA U .S .G .S . 120 -- H 1967 -- -- -- U -- -- 2317 -- GE N 120
156$0918200D0 U .S .G .S . 70 -- -- 1952 -- -- -- U -- -- -- -- DG N
156NO91W21CBAI STANLEY NO .1 180 S -- 1915 TL OC 98 -- P -- -- -- -- -- N
156149111210362 STANLEY NO .2 200 8 -- 1947 TL OC 127 11-48 P -- -- P D 0
1S6NO91W2ICCA1 U .S .G .S . 70 -- -- 1952 -- -- -- U -- - ---
-- ----
0 6DG
NM
156NO91W21CCA2 U .S .G .S . 60 -- -- 1952 -- -- -- U
ISAN091W2ICDU R .EDWARDS 48 24 B
. 1924 -- -- -- N -- — P -- -- N
SS6N091W21DC81 C .KOESSENG 50 24 8 1922 QG Sl -- -- H -- -- P -- -- N
156NO91N210C82 L .BACKER 20 24 B 1949 15 -- H P 1 P--
-- N
IS6NONINZP000 U .S .G .S . 40 -- -- 1952 -- U -- ---- C
DGD6
M
15AN091W220DC U .S .G .S . 20 -- -- 1952 -- U -- N
156N091W22D00I U .S .G .S . 30 -- -- 1952 -- U -- -- - ---
OG N
156NO9IW2200D2 U .S .G .S . SO -- -- 1952 -- U -- -- 06 N
SPE- FREQUENC YCASING WATER CIFIC ALTI- LOG TEN- OF WATER -
LOCAL WELL SIAM- METHOD DATE WATER LEVEL WATER TYPE CON- TUDE- 0W AVAIL- PER- LEVEL TOTALWELL OWNER DEPTH ETER DRILLED DRILLED AQUIFER LEVEL DATE USE LIFT POWER DUCT OF LSO TYPE ABLE ATURE MEASURE - DEPTH
NUMBER IFT .1 IIN .I (YEAR) (FT .) MEAS . ANCE CFI .) 1
Fl RENT S
IS6NO9IW230AB A .NELSON 60 24 B 1933 -- 36 7-52 K P 3 0156NO91W23000 U .S .G.S . 8D -- H 1952 -- -- -- U -- -- D6 NI36NO91W23CCD U .S .G .S . 100 -- H 1952 - U DG NIS6NO91W258CC J .FIT2PRTRICK 230 3 H 1952 TL OC 140 -- D P 3 P -- NL56N09IW26ABB1 W .NELSON 95 18 B 1930 -- 75 7-52 S P S 0
156N0910266882 W .NELSON 23 24 D -- -- 14 7-52 H P 1 0ISAWOO1W26888 F .CORRIGAN 54 24 8 -- - 40 7-52 U C 1 0I56N091W26DAAI R .STALNECKER 205 3 -- 1948 TL OC 94 7-52 S P S 0156N09IW26DAA2 R .STALNECKER 100 24 B 1917 -- 57 1-52 H -- -- 0I56NO91W27888 U .S .G .S . 280 -- H 1952 -- -- -- U - - - OG N
IS6N091W2TBCC U .S .G .S . 60 - H 1952 -- -- U -- -- DG - NSS6NO91W27BCD A .PETGRSON 40 24 0 1948 27 7-52 H P I - 0I56N09IW2TCBB U .4 .0 .S . 90 -- -- 1952 -- -- U -- -- 06 N156N091N27CC8 U .S .G .S . 60 - H 1952 -- -- U - -- DG N156NO91W27000 U .S .G .S. 40 -- -- 1952 -- U -- -- OG N
I56NO91W28ABA STANLEY 190 8 -- 1949 95 -- U M U P D -- N156NO91W28ABB J .SMITH 26 36 D 1928 14 9-52 K P 1 -- 0156N091N288ACL STANLEY 185 -- -- 1953 85 -- P M U 6 C D 45 NIS6NO91W288AC2 U .S .G :S . 350 -- -- 1952 -- -- U -- -- -- OG -- N156N09IW2W000 U .S .G .S . 350 -- -- 1952 -- -- U - -- DG -- N
156N09IW2800A M .KINCANON 26 24 0 1925 -- 15 7-52 H P 5156NO91W29A88 E .JELLESED 100 . 36 0 1902 56 7-52 K P 6 0156NO91W298A6 A .JOHNSON 52 36 -- 1902 0G 51 32 7-52 K P 5 0156N091W29888 U .S .G .S . 350 -- -- 1952 -- -- -- U - -- DG N1560091W29000 O .HOLM 70 30 B -- -- 37 7-52 U -- -- 0
I56N09IW3ICBC J .CR .ENANOER 53 20 B 1947 33 7-52 K P 5 0I56N091N32BAD U .S .G .S . 80 -- -- 1952 -- -- U -- -- DG N156NO9IW3280AI U .S .G .S . 70 -- -- 1952 -- -- U -- -- -- DG N136N091W328DA2 U .S .G .S . 20 -- -- 1952 -- -- U -~ DG N1568(091W33AAA 68 24 B -- 2 1
Q7-52 U -- 0
IS6NO9IW33ACA U .S .G .S . 20 -- -- 1952 -- - -- U -- -- -- 06 -- NI36NO91W33ACC STANLEY 25 86 -- 1964 -- 9 5-66 P N U 6 C 40 0I56N091W33BAD U .S .G .S . 60 -- H 1952 -- -- -- U - -- -- D6 -- N1S6N09IW33BMI W .NFLSON 11 20 0 0G 3l 4 8-52 U . P -- 2157 C -- -- 0I56N09IW3388C U .S.G .S . 30 -- -- 1952 -- -- -- U -- -- DG N
I56NO91W33BBD U .S.G .S . 20 -- -- 1952 -- -- U - - DG -- N156NO91W33BDA2 U .S .G .S . 50 -- -- 1952 -- -- U - - OG -- N156NO9IW33CAB U .S.G .S . 80 -- -- 1952 -- - U - - 06 - NI56NO9IW330A0 U .S.G .S . 140 -- -- 1952 -- -- U -- -- DG -- NI56NO91W34AAA J .JAC08S 120 18 B 1913 97 7-52 K P 5 -- 0
SPE- FREQUENC YCASING WATER CIFIC ALTI- LOG TEN- OF WATER -
LOCAL WELL D1AM- METHOD DATE WATER LEVEL WATER TYPE CON- WUDE- OW AVAIL- PER- LEVEL TOTAL
NELL OWNER DEPTH ETER DRILLED DRILLED AQUIFER LEVEL DATE USE LIFT POWER DUCT OF LSD TYPE ABLE ATONE MEASURE- DEPTH
NUMBER IFT .) 414 .1 1YEAR1 IFT .) MEAS . MACE 1FT .) 1
Fl RENT S
S4910 66666666 U .S .G .S . 20 -- -- 1952 --
- -- -- DG N
13611091W34C88 U .S .G .S . SO - 1952 -- DG NlS6NO91W34CRC H .HAGEN 16 36 D 1930 OG 31 4 7-52 P 5 0
1 S64092WOSAAA U .S .G .S . 160 -- H 1967 -- - 2358 GE N 160
IS618092WO9A88 M .FARHART 74 24 8 -- -- 51 8-52 0
1S64092WL000C J .HORNE 175 24 8 1925 TL OC 99 7-52 S 0
lSMM092WIIDCD C .JUMA .SR . 61 24 B -- -- 39 7-52 U O
l S6R092N128AB SULLIVAN ET .AL . 62 24 B -- -- 42 8-62 S 0
140109Z 666666 C .JUNA .SR . 35 24 D -- -- 33 7-52 0
IS611092WI666 8 A .HORNE 20 24 B -- -- 18 7-52 0
1S6N092W19ABA U .S .G .S . 80 -- H 1966 2290 DG N BO
156NO9210208CC J .4EIERS 100 36 9 1920 98 8-52 S 0
1365092W20000 U .S .G .S . 102 -- H 1952 -- -- U DG
15640921122000 U .S .G .S . 100 -- -- 1952 -- -- -- D G
1544092W23000 U .S .G .S . 130 -- -- 1952 - - U O G
I564092V23000 U .S .G .S . 160 -- - - 1952 U P DG N
1564092W24C88 U .S .G .S . 172 - - 1952 U DO N
I56M092W24000 U .S.G .S . 160 - - 1952 U DG N
I564092W2SAAA 27 D QG 31 17 7-52 K 0
156M092W266CL U .S .G .S . 70 - - 1952 U OG N
13614092W26600 U .S .G .S . 135 -- 1952 - -- U -- O G
15611092W260A6 A.SEVERSON 64 24 6 1919 -- 12 7-52 U --
1S6M092N35DOC S .JAHA 90 20 8 -- 39 7-52 S --
1565092W330001S6M092W36OOD
S .JAH AU .S .G .S .
4 5200
I B--
8H
-1967
2 8-
7-67--
UU
N-- 2328 GE 200
IS6MO53N01B68 O .N.HAGEN 309 2 C 1952 -- 276 K P 5 6 -- K -- 46
IS6NO93NO3ADC W .MEIERS 12 46 0 -- -- 8 K -- N
/SAN09SN0600 0ISAN093WO6000
J.J .BELI KU .S .G .S .
14180
6--
CH
--1968
TL O C--
13 1--
----
KU
S--
5 6--
--2263
K--
- -GE
4 S--
NN s o
I56M093NO8CBA W .CHAMELY 128 6 -- -- UG 52 50 -- K P N
lSAN093WIOAAA W .MEIERS 240 3 -- -- -- 40 A -- 6 -- C -- 49 N
ISA409IVLOSS8 G .N.RY .ET AL 210 -- -- -- -- U -- 2295 -- G -- N 21 0
GNWNOOSW1OCIAISAM083WI000A
R .REIRSGAR DW .MEIERS
ISO130
318
----
- ---
- ---
4040
KK
P
-P N
ISAN093W11AAA U .S.G .S . 180 -- H 1967 -- U - -- -- GE -- N 180
lSMN93W13000 E .EVANS 200 3 15 K P S 5 -- C 45 N
E5A4893W1S000 U.S.G .S . 60 -- H 1966 -- U -- -- 2299 -- DG -- N 60
1SANO95WIA000 G.N .RY .ET AL 165 -- -- -- -- U -- -- 2300 -- G -- N 165
ISAN093WI6OAAlSA01093N170C0
A.MALVORSONJ .SMOLA
30105
24S
--C
- -1958 --
2 470
KH
--S S 4 -- K -- 46 N
SPE- FREOUENCYCASING WATER CIFIC ALT!- LOG TEN- OF WATER-
LOCAL WELL 01AM- METHOD GATE WATER LEVEL WATER TYPE CON- TUDE- OW AVAIL- PER- LEVEL TOTALWELL
NUMBEROWNER DEPTH
IFT .1ETE R118.1
DRILLED DRILLE DIYEARI
AQUIFER LEVELIFT .1
DAT EMEAS .
USE LIFT POWER DUC TAMCE
OF LSDIFT .l
TYPE A8LE ATUR E1
F)MEASURE -
MENTSDEPTH
156N09311 66686 R .MELANO 158 C 1952 -- -- — K S S 6 -- K - 46156N093W24000 R .ONSTAD 30 24 8 1964 -- 14 - - H J S 5 K - 4 5IS60093W2580815611093826800
G .N .RY .ET A L0 .8NSTAO
14 524 24 -- -- 12 --
US
2240 :: G 1450G 3 1
156N093W27A00 W .TEXEL IO 8 -- -- -- 4 6-67 U P 1 3 -- K - 37
156PI093827000 1 .C .REYNaDS 23 18 -- 17156N093W3110C R .QUANMEN 235 4 C 1963 TL OC 190 S S b — K 46136N093M321RR G .N.RY .ET AL 90 2365 G 90I56N093W34AAA L .TEXEL 26 24 -- 0G 51 1 6156N0934134BC0 N .SKA80 150 5 C 1959 TL OC 90 S S 6 -- K 45
15611093834006 E .SANDERSON 30 H156M094V03AA 6 .N.RY .ET AL 210 2120 G 210I5ANO94W05CC8 G .N.RY .ET AL 225 U -- -- 2365 G 22 515811094110186 G .N.RY .ET AL 210 U — -- 2260 G 210IS6NO94WI2AA6 G .M .RY .ET AL 210 U — -- 2260 G 210
1S6NO9WI2BAC E .J .JOHNSON 9 42 0 -- -- 4 10-65 U P 1 -- -- -- -- 00568094812000 G .N.RY .ET AL 210 U -- -- 2195 -- G N 210
TL O C1S6NO94Wl6CAD W .HANSON 125 4 H 1962 40 K J S 6 K - - 45 N156NOV4W16DIA U .S .G .S . 50 1 H 1966 0G 51 16 8-66 U N -- 6 2050 C G 47 M 80156N094619000 .G .N.RY .ET AL 210 U — -- -- 2332 -- G N 210
I56N094W20018 D .JOYCE 28 36 D -- -- 18 6-67 H J S 4 -- K - - 45 0ISAN09421248DD G .N.RY .ET AL 210 U -- -- -- 2215 -- G N 210156N0941124C58 U .S.G .S . . 40 M 1968 -- U -- -- 2165 GE N 401368094124010 U .S.G .S . 179 l H 1968 06 52 99 7-68 U N -- 6 2173 C GE 47 O 220156N094W26ARC T .WATSON 41 lB 8 1949 -- 17 10-65 H J 5 6 -- K -- --
156N094W29BC0 N .OAHL 1O1 24 - -- TL OC 36 -- K __ __ _ _156M094W3006A O.S .HANSEN 52 24 D 1946 TL OC 29 - - K P 5 5 K19080941031AAA J.NANSOM 80 8 -- TL OC 65 -- S P 6 5 K 45
157N088WOSA0A J .J .FLAHERTY 30 20 D -- -- 12 K P 5 5 K 39
1530080W060101 L .J .GOETTLE 14 36 0 1938 OG 31 8 H P I 4 -- K 38 N157N0R$0060002 L .J .GOETTLE 34 24 8 1957 18 7-66 H J S 6 K 0
0G 5 1137N081WO68803 L .J .GOETTLE 182 7 C 1950 150 - - S P S 6 C 43 N157NO88WO6808 L .J .GOETTLE 180 3 J 1940 OG 51 80 - - U P 6 NI57MOSBW09CSCI A.L .CHARNIT2KI 18 24 B -- — 6 — H P 6 6 K 45 N
I57NOUWO9CIC2 A.L .CHARNITZKI 279 4 C 1927 TL OC 100 - - S P 6 -- -- N157NO118WIOCN O .A .GANORUD 300 S C 1954 200 -- 9 P S 6 -. K N
0G 3 11518086W11S80 O .A .GNORUD 8 1 V K P S 5 -- K 39 NI57NO88WI3CN O .T .ALVSTAD S 48 0 1961 -- 0 7-66 U N 4 K 58 0157NOSON1400D B .T .ALVSTAD 20 48 D 1951 -- 9 7-66 K J S 4 C 47 0
CASING WATERSPE -CIFIC ALT1- LOG FEN-
FREQUENC YOF MATER- '
LOCAL WELL 01AM- METHOD DATE WATER LEVEL WATER TYPE CON- TUOE- Q . AVAIL- PER- LEVEL TOTA LWELL OWNER DEPTH ETER DRILLED DRILLED AQUIFER LEVEL DATE USE LIFT POWER DUCT OF LSD TYPE ABLE ATTIRE MEASURE- OFPT H
NUMBER 1FT .) TIN .) IYEARI (FT .) MEAS . ANCE IFT .) 1
Fl PIPIT S
1S7FNO68N17ADA O .G .SCMAEFER 325 4 C 1965 TL 0C 140 -- K S S 6 K -- NLS7NO88W20ADC L .L .ANDERSON 24 24 B 1963 0G 51 8 7-66 J 5 6 K 0I57NO88W2ICAA L .L .ANDERSON 24 24 B 1961 OG 51 8 -- S P F - - N
I57NO88W23AC8 6 .64.85760 447 4 -- 1962 -- 200 -- K S 5 6 K -- NIS7NO68W24CA6 C .G .ALVSTAD 9 4B D 1963 OG 31 5 -- U P 1 N
I57NO8BW2708B T .R .STAVE 420 4 -- -- -- 170 -- K157N088W33A6C1 A .E .STAVE .SR . 28 48 0 1936 - 10 K P S 5 K -- 40I57NO6BW33ABC2 A .E .STAVE .SR . 16 24 8 1961 QG 51 10 U P s --I57N068W34BCC A .V .KJELLBERG 317 2 C 1939 TL OC 67 S P S 6 K -- 4 3I57NO88W35ADA O .M .RLVSTAO 403 4 C 1960 TL OC 200 S S S 6 K -- - -
157NO88W3688B U .S .G .S . 340 -- H 1966 -- -- -- U 2342 -- GE 340157NO89WOIODC L .J .GOETTLE 16 24 B 1957 OG 31 8 -- S
_ P 6
4 K 40 NIS7NOB9NOSBA8 1 .KNUTSON 352 4 -- 1957 TL OC 100 -- S S 5 K 4 2157NO89WO58CB L .ANDERSON 380 4 -- TL OC 200 S
1S7NO89WON000 H .D .JOHNSON 140 24 8 1920 TL OC -- K P S 5 K 4 3
I57NO89MI$000 V .D .HALVORSON 103 24 8 -- -- 96 -- K v S 5 -- K 42 N157N0B9W20ACC HAUGEN BROS . 93 5 C 1961 -- 60 -- K S 5 6 K NI57NO11910040C U .S .G .S . 141 1 H 1966 OG 51 14 8-66 U N - 6 21_72 C G 45 M 20 C157NO89W24AC0 C .C .GUSTAFSON 16 48 D 1951 OG 51 5 7-66 U P 1 6 -- K 39 0157N089W240B6 C .C .GUSTAFSON 9 48 D 1936 OG 51 4 7-66 K J S 4 K 0
I57NOESW26CDA E .ANDERSEN l8 48 D 1934 "KG 51 4 H P 1 4 K
157NO89N30DCB M .A .HALVERSON 82 4 C 1959 TL OC 25 -- K S S 5 K 0 4 2157N089W3ICDA C .O.HANSON 90 18 B 1923 70 -- S S S 5 K -- 4 3LS7NO89W31CD B157N089W328C0
C .O .HANSONB .RUGLAND
1 4133
362
DC
190 21934
OG 3 1TL OC
1 035
UK
NP S 5 K -- 4 3
IS7N090W03BBD I .J .NAHLUN 32 24 - 1961 OG 51 20 -- K P S 3 K 40 NI57NO90WO48CD R .METTINGER 126 3 C 1932 IL OC 90 -- K P S 6 K NI57N090N11080 H .D .JOHNSON 180 4 C 1944 -- 110 S P S 6 K 43 NI57N09010I20AC A .JOHNSON 25 IN -B 1950 -- 5 -- U N N15711090W12DOC A .JOHNSON 197 6 -- 1929 -- 40 K P S 5 K 42 N
167N09W14CAD H .HALV08SON 70 4 C 1959 TL OC 30 -- S P 5 5 K D 4 3137N090W14C0A H :HALVORSON 20 24 B L928 QG 51 30 -- H v I 4 K 4 4157NO90W15888 U .S .G .S . 38 1 H 1966 QG 51 26 8-66 U 2270 -- 0 801579090WI50AA R .G .BALL 65 24 B 1928 -- 34 11-66 S P 1 6 C 4 2
157M050R1508D R .G .BALL 30 36 D -- -- -- -- S P 5 5 K
157N09OW19AOA T .NEETHER 37 30 D 1950 -- 15 -- K P S 5 K -- 43 N157N090W21CCA L .NEETHER 28 -- 8 OG S1 14 -- K P 4 K 44 NI57N090W2200A U .S .G .S. 40 -- H 1968 - U __ 2200 -- DG - - N 40157NO90r26868 A .N .JOHNSON 21 48 0 1936 OG 31 11 11-66 K S 5 K 44 0157N090026000 S .KING 18 48 -- -- -- 14 -- K N
CASING WATERSPE-CIFIC ALTI - LOG TEN-
FREQUENCYOF WATER-
LOCAL WELL DIAN- METHOD DATE WATER LEVEL WATER TYPE CON- TUDE- ON AVAIL- PER- LEVEL TOTALWELLMASER
OWNER DEPTHIFT .)
ETER11N.)
D61LLE0 DRILLEDIYEARI
AQUIFER LEVE L(FT .)
DAT EMEAS .
USE LIFT POWER DUC TANCE
OF LSD(FT .)
TYPE ABLE ATUI E1
FlMEASURE-
RENTSDEPTH
I31N090N31CDC S .NtTCHELL 7S 24 8 1933 -- 60 K P S 5 -- K -- 43 N137009011)31188 0 .5 .6.1 . 80 -- R 1967 -- U - -- 2227 06 -- M 8D157N090N)40CDI L .HAGEN 130 4 C -- 70 H S S 6 -- C 8 43 N
TL OC151N090W340002 L .HAGEN 220 4 C » 110 S P S 6 -- K -- -- N151009180486$ L .JOMISON 213 -- -- -- TL OC -- X N - N
IS7NO9IWIIC88 G .VAAGE 263 4 C 1949 IL OC - - -- K P S 6 -- C -- -- N157N091WI)0D0 U .S .G.S. 160 0 1966 - - -- U -- -- -- 2320 -- GE -- N 1601S7N091N12000 A .AIINESON 20 36 0 1954 QG SI 12 -- K S S S -- K -- 45 NIS7N09IWISAAD J .JOMSON 162 2 1942 TL OC 100 S P S 6 -- K -- 43 N1375091W18000 N .KUSTER 145 3 C 1957 TL OC 80 K P S N
15711091M2300D
. RUDOLPH BROS . 46 24 O 4916 -- 20 S P 5 6 K -- 43 NIS1N091026C88 C .NELSON 100 24 8 1918 -- 90 K P 5 6 -- K -- 44 N157M091N310001 B .HOLLINGER 404 4 C 1956 TL OC 100 X P S 6 C -- 48 N1S7N091W31000 215TN091W3SBAA
8 .NOLLINGERU .S .G.S .
9 550
24--
8--
19121952
--- -
90 -- SU
P S 7 -- K06
44 NN
15111091036000 U .S .G.S . 187 1 N 1966 OG 51 42 8-66 U 6 12200 C GE 48 M 2001STN09200388A O .ENERS02 78 3 C 1915 TL OC 70 -- K P S S -- K -- » N157N092M040AA L .ENERSON 240 2 C 1914 TL OC -- K P S 6 K 43 N
'Xr 1STN092NOS8AA M .S .G.S . 120 - H 1966 -- - - U -- -- -- 2210 -- GE » N 120157M090005S8B U . S .G .S . 120 - H 1968 -- - - U -- - -- 2213 -- GE -- N 120
1STN092NOSSDA C .COLSENSON 90 3 C 1910 TL OC 60 R P S 4 -- K -- -- N1576092MOTCC IIS711092609SCC
C .ERI E1 .11A55E
13590
33
-C
19451914
-- 11 760
HK
SP
SS
S6
----
KC
----
--44
NN
TL O C1S7NO92WIOSC8 D .AIN/E 46 4 C 1964 26 R S 5 N157N0928I3000 F .CROWDER 62 18 8 1946 -- 47 S P S S -- K -- - N
157N092M13DOD1 F .CROWDER 161 4 C 1962 IL OC 118 -- H S T 6 -- K -- -- N15TO92M130002' F.CROW0ER 121 4 C 1959 TL OC 50 -- N157N092014AA6 F .05000E5 313 4 C 1961 TL OC 252
_ S -F- F N
15TM092NI60001 U.S.G .S . SO l M 1966 56 51 9 7-66 U - -- 2204 - GE -- N 6 515710926160002 U .S.G .S . 360 - K 1966 -- -- U - - -- 2204 -
-- GE - N 360
1SOM092WITCCA O.ROISE ITS 3 1914 TL OC 155 » R - _- __ -- N15TN092018SOC H.HOLLET 134 4 C 1930 -- R I 5 S R -- 43 N
--13100928100A8 U.S .G .S. 80 0 1968 U - -- 2326 DG -- N 60157N092819AIHI A .ERIC 14 24 0 1935 -- 12 K J S 6 -- K -- -- N1S7M092825C0C J .PAIN05T 59 4 C 1965 - P -- K -- S -- K » 44 N
ISTM092A2IOAD V.PAPPA 230 4 C 1963 TL OC 200 K S S 6 -- K -- - N1575053W29000 B .IOPKINS 259 4 C 1961 TL OC 210 K S S 6 -- K - 45 N13TM0928320CC G .N .NV .ET AL 210 U 2300 6 N1STN092833ADA O .PAIIMIT 19S 4 C 1963 TL OC 125 S S 6 C 45 N1STN0018011148 U .$ .8.5. 100 -- D 1967 -- » U - -- -- 2245 - GE -- N 100
SPE- FREQUENCYCASING WATER CIFIC ALTI- LOG TEN- OF WATER-
LOCAL WELL DIAM- METHOD DATE WATER LEVEL WATER TYPE CON- TUDE- OW AVAIL- PER- LEVEL TOTA LWELL OWNER DEPTH ETER DRILLED DRILLED AQUIFER LEVEL DATE USE LIFT POWER DUCT OF LSO TYPE ABLE ATURE MEASURE- DEPTH
NUMBER IFT .1 (IN .) 1YEAR) IFT .1 MEAS . ANCE IFT .1 1
Fl RENTS
t17N093Y028CD J .ROSENCRANS 110 3 C -- -- 80 K P S 5 K 44 N/S1N093Y080AA1 G.N.RY .ET AL 195 -- -- -- -- -- U -- -- -- 2290 -- G -- N 1951S7N0938080AA2 E .MORSTEOT 200 3 -- -- TL 0C 82 N -- -- -- -- -- -- -- N1S7N093W09ACD L .NORSTEDT 160 3 C 1910 TL 0C 135 K P S S K AS NIS7N0936SIR80 G.N.RY .ET AL 121 -- -- -- -- -- U -- -- -- 2335 -- G -- N 12 1
157N093WISDAA U.S.G.S . 60 -- H 1967 -- -- U -- -- -- 2260 -- 0G -- N 6 01S7N093Y128RC A .ERIE 130 3 -- -- -- 50 K -- -- -- -- -- -- -- N157N09361)BDB1 M .N.NOROBY 132 3 C 1963 -- 117 S P S 5 -- K -- 44 NI57N09)Y13B082 M .M.NORDBY 12 30 D 1964 A H N 3 -- K -- - NIS7N093WISOCCI LEE BROS . 100 3 C 1916 QG 51 85 5 P S 6 -- K -- 43 N
157N093W1SOCC2 LEE BROS . 96 4 H 1953 OG 51 78 H P S S -- K -- 44 N157N093E150CC3 LEE BROS . 96 4 C 1964 OG 51 83 5 P S 6 -- K 0 43 NISTNO93A2IAAA U .S .G.S . 120 - H 1967 -- -- U -- -- -- -- -- GE -- N 120157NO93W27A88 LEE BROS . 180 4 C -- TL OC 140 S P F -- -- -- -- -- NIS7N093W28000 U .S .G.S. 160 -- H 1966 -- -- U -- -- -- 2115 -- GE -- N 160
157N093U28DCO A .FURING 150 3 C -- -- -- -- S P 1 6 -- K -- 46 N157N093W29AAA G .N .RY .ET AL 180 -- -- -- -- -- -- U -- -- -- 2235 -- G -- N 18 0157M093Y 31C D8 8,KJOSEN 25 36 D 1918 TL OC 11 10-65 S S S 4 -- K - 44 01S7N093Y32CCC C .XAL V00.50N 200 7 8 1954 OG 51 I20 -- K P S 6 -- K D -- N157N093W338AB R .FEIRING 94 2 -- -- TL OC 66 -- N P S =- -- -- -- - N
I57N093Y368AA U .S .G .S. 340 -- H 1967 -- -- U -- -- -- 2480 -- GE -- N 34016TN094W02888 0 .l .SATHER 39 21 8 1963 OG 51 31 H J 5 4 -- K -- 48 NI57N094W04800 E .NE55 52 6 -- 1910 -- 30 -- -- - S -- -- -- -- -- N157N094W0400D1 A .J .LEE 49 36 0 1951 OG 5l 41 H J S 5 -- K -- 47 N157N0948040OD2 A .J .LEE 19 24 0 -- OG 31 -- 5 N -- -- -- -- -- --. N
1S7N094YO58AA O .P .LOKKEN 70 4 C 1942 - 40 - K P S 4 -- K -- 45 NIS7ND94YD68C M .f RICKSOM 210 6 H 1952 TL OC 156 7-53 U N -~ -- -- -- D -- 0IS7N094YDBCCC V .AENST AD 58 4 C 1960 OG 51 28 -- K P S 4 K - 45 M151N094Y09AAB U .S .G.S . 40 -- H 1966 -- -- -- U -- -- -- 2280 -- OG -- N 40157N094WIOBA8 M .JO8STAD 136 3 C 1938 TL OC 115 -- K P 5 5 -- K -- 45 N
IS7N094WI3000 O .C.STENBAK 10 24 0 1966 -- 5 X P 1 4 K -- 45 M157N094Y14ABB G .N.RY .ET AL 225 -- -- -- -- -- U -- -- -- 2290 -- G -- N 22 5I57Np94W11AM G .N.RY .ET AL 180 -- -- -- -- -- U -- -- -- 2275 -- G -- N 180l57NO94M1888C C .A.SYVERSON 62 5 8 1945 TL OC 59 H P S 5 -- K -- 45 NIS7NO94WI8CCA J .NWSS 60 1 -- -- -- 50 K -- -- -- -- -- -- N
I57NO94WI9000 G.L .MESET 98 S C 1942 TL OC 66 -- K S S 5 -- K -- 45 N157M094W20DCC G.N.RY .ET AL 135 -- -- -- -- -- -- U -- -- -- 2200 -- G -- N 1157N094W238A8 U.S.G .S . 40 -- H 1966 -- -- -- U -- -- -- 2290 -- OG
N
4'
15711094112 66666 3.ROXOE l2 24 D -- TL OC 4 10-65 U P 1 -- -- -- -- --N837N094825A882 H.ROHDE 67 4 C 1950 TL OC 58 -- U N -
CASING WATER
SPE-CIFIC ALTI - LOG TEM-
FREQUENCYOF WATER-
IOCAL WELL DIAM- METHOD DATE WATER LEVEL WATER TYPE CON- TUDE- OW AVAIL- PER- LEVEL TOTA L
WELL OWNER DFPTH ETU DRILLED DRILLED AQUIFER LEVEL DATE USE LIFT POWER DUCT OF LSD TYPE ABLE ATURE MEASURE- DEPTH
NUMBER 1FT .1 11N .1 IYEARI IFT .I MEAS . ANCE 1E1 .1 1
fl RENT S
157N094W250BA U .S .G .S . 60 -- H 1966 -- -- U -- -- 2090 -- GE N E C
157NO94W26DAA G .N .RY .ET AL 90 -- -- -- -- -- U -- -- -- 2110 -- G N 9 0
157N094w26UAD E .H .DANNEWITZ 153 5 C -- TL OC 136 U N -- -- -- -- N
157NC94W298CC S .S .OLSUN 146 6 C 1964 -- 66 -- K 5 5 5 C -- 47 N
157NC94w32BC8 L .HEYER 35 24 B 1944 -- 25 -- K P -- 4 -- K -- 44 N
157N094w34A00 R .IVERSON 202 5 C -- -- 15 H J 5 -- -- -- 0I57N094W368CC H .RICE 23 -- V -- -- -- -- H 5 5 4 -- C -- --
I5MOWHRO28BA H .S .JACOBSEN 125 3 C 1960 OG 51 7 H J S 6 -- K -- 4 5158NC8ANO2CCC O .JDNNSUN 320 2 -- -- -- 70 K -- -- -- -- -- --158NO88w03AAA O .C .ERICKSON 150 4 C 1960 -- 14 -- P N -- 6 -- K 4 6
1S8N088w06CA C .ERICKSON 250 3 -- -- 200 -- S -- -- '- --158N088N09CWH A .WILLOCK 250 2 -- -- -- 160 K -- -- '- -- --158N08RWIIRDU P .WILLOCK 250 2 -- -- -- 130 -- S -- -- -- - -- - -158MO88w13ADU C .GREGOIRE 160 3 -- -- TL OC 100 -- K -- -- -- - -158N088WI48881 L .J .ERICKSUN 160 3 C 1918 TL OC -- -- U P 5 6 -- K 4 6
ISM088w1488B2 I .J .ERICKSON 10 24 0 1910 -- 6 -- U J 5 4 -- K -- 41 N
IS8NO88NI7ABA U .S .G .S . 260 -- H 1966 -- -- U -- -- -- 2260 -- GE - - N 2EC
I58NOBtlNIIA00 I .J .IVERSON 260 4 - C 1928 230 -- K P - S _5 - C _ - N
ISMO88w1 BCCA N .ELOEVIK 290 7 200 K N
I5M088WIBCCB N .ELOEVIK 24 24 -- -- 10 S -- -- -- -- ' - N
15M088w218AA 5 .1 .ULSUN 70 4 C -- -- 50 -- K J S 6 K -- - - N
I58NOMMW2I000 L .SMITH 300 3 -- -- -- 252 -- S -- -- -- -- '- - - N
158AIG88W24COD A .H .CIIONS 235 4 C 1963 OG 52 155 K 5 5 6 -- K - - N
158NO89W27AAC D .L .PULLEN 550 2 C 1916 TL OC 100 5 P T 6 K 44 N
158N08Bw29A88 S .L .IILSON 300 -- -- 1961 -- 150 -- S S S 6 -- K 46 N
1SRNOWAW32DUC W .CHAFER 12 -- D -- -- 6 -- K -- -- -- -- '- -' -' N
15M088W320DD U .S.G .S . 300 -- H 1967 -- -- -- U -- -- -- 2239 -- GE -- N 9M
I58NO88w3 C .C .CHARNETIKI 132 24 C 1962 15 -_ K S 5 4 K N
ISMDBRw34ADC BUC1 H .M .VURASSUGSD
N MISSONIA
24 B 1964 OG 15 -- H J 5 5 -- K -- 42 N
158N088N34BOC2 H .M .NASMUSSON 242 4 C 1952---- -- 5 P 5 -- '- ' - N
158NC89WOLAAAI D .000NS 14 24 D -- 8 H J 5 4 -- 44 N
158NO89WOIAAA2 D .000NS 240 4 C - 125 -- S P S 6 -- K 43 N
158NC89W02ADD A .SANDE 118 -- C 1966 30 -- K 5 5 5 K -- 42 N
158NC89W048VDI 5 .V000E 216 3 -- -- -- 150 S -- -- -- -- -- -- - - N
15M089W04M802 S .V000E 30 48 -- -- 10 H -- -- -- -- - - N
15MG89WGVCCDI C .KRUEGER 218 4 -- 100 -- S -- -- - - N
I58N089wC40002 C .KRUGER 16 36 D -- -- 8 -- H -- -- - - N
158N089W06DDDI A .ANUERSON 20 36 -- 6 K C -- -- -- '- - - N
158N089W060002 A .ANUERSON 16 24 -- -- 2 1 -- -- -- -- - - N
IS8NO89w07G0A F .HAUGEN__ -- 4 -- -- S P F 6 K 43 N
CASING WATERSPE -CIFIC ALTI - LOG TEN-
FREQUENC YOF WATER-
LOCAL WELL SIAM- METHOD DATE WATER LEVEL WATER TYPF CON- TUDE- OW AVAIL- PER- LEVEL TOTALWELL OWNER DEPTH ETER DRILLED DRILLED AQUIFER LEVEL DATE USE LIFT POWFR DUCT OF LSD TYPE ABLE ATURE MEASURE- DEPTH
NURSER IFT .) 11N.) IYEARI IFT .) MEAS . ANCE (FT .) 1
Fl MENT S
ISM089WIOAOD J .LINDOUIST IT 36 D 6 8-67 SISM089W12888 R .KING 36 36 0 1926 18 -- S P S 6 -- K -- 44 N15M08W14DOA J .GUINN 22 24 0 - - 8 K J S 5 K -- 43 NI5MO89WI7COA1 W .JOMSON 53 24 B 1920 18 7-68 K P S 6 2310 C -- -- 0ISM089WIYCDA2 W .JOINSON 50 24 B 1913 15 -- K P S 6 -- K -- 44 N
LSM08WI9AAAI U .S .G .S . 220 -- H 1968 U N 2315 -- GE -- N 22 0188NO89WI9AAA2 U .S .G .S . 80 -- H 1968 U 2315 -- OG -- N 8 01SM089W22CCC U .S .G .S . 280 -- H 1967 U _- 2308 -- GE -- N 280ISMOUW24CCC N .HELWIG 2S 24 - - - 10 K -- NIS8N089W26AAA R .RLDEVIK 12 24 B - - 9 -- K P 4 -- C -- 43 N
158M089W28ADD O .HANSON 90 12 B 45 -- K J S 4 K 43 N)S8MO89W3000CI H .LUNDT 60 24 B - - 25 -- H J S 6 -- K 44 NlS1IN0O9W3000C2 H .LUNOT 165 4 TL OC 90 -- S P S 6 -- K - 43 NISON089W3SOAC L .JOINSON 25 24 B 12 H P I 5 -- K -- 43 N1SM090WO/AAA O .6NDERSON 54 24 1945 13 7-65 S P S __ __ 0
1S801090WOIAAC O .M .ANDERSON 138 4 1962 K P G __ N1S8M090W0I8AC O .HAUGEN 426 3 TL OC 165 -- K S S 5 -- C 44 NISM090W0208B O .M .ANDERSON l4 42 D 1962 7 -- S P __ NISBN090W04BAC M .BRYANT I10 4 C 1959 50 -- K P S 5 -- K NISM090WIO8DB M .8AYANT 70 - - F S --
ISM090N12DDD U .S .G .S . 340 - - H 1966 U -- -- 2270 -- GE -- N 340ISM090W13CAA S .REID 241 4 150 -- K -- D -- N1S8N09DWIH8BA U .S .G .S . 94 1 H 1967 29 9-66 U N -- 6 2240 C GE 46 M 12 01SIN09M2188B K .MADER 17 24 D 1960 8 -- K J S 4 -- K -- 42 NI88M090W22AAA J .BOMSTAD 160 3 30 -- K --
IS801090W22ACC J .DORAN 212 3 18 -- K P 43 NI8M090W23DCD A .NELSON 208 2 TL OC 150 -- S --1S8N090W240CD H .OLAF 221 3 C 190 K P S 5 K 43 N158MO90W29000 U .S .G.S . 200 - - H 1968 - - U -- -- 2318 -- GE - N 20 0158N090W32A88 E .JOMNSON 12 24 B 9 K P 5 4 -- K -- 43 N
I51IN0IIWOSC U .S .B .S .F .W . 145 4 C 1959 - - S P 6 5 -- K 0 47 NI5M091WO88B U .S .B .S .F .W . 162 4 C 1961 S P 6 4 K 0 47 NISM09IW10AA0 A .ANOERSON 140 3 -- 1910 TL OC 110 K P S 5 -- K -- 43 N18NONIWSICCC A .WESTBY 38 24 28 K NIS8N09IW12AAD H .ROGNE 20 24 LS -- K J 42 N
I5MDNIWI4000 M .MICKELSEN 40 24 B 30 -- K J S 6 -- K -- 42 NI88N09IW19000 R .LUMBLY 169 4 140 -- K S 5 -- K 41 N181N091WI90D0 U .S.G .S . 160 - H 1967 - - U -- -- 2359 -- GE -- N 180ISM091WI000C158M091W218CC
W .ERICRSMJ .KRAUSNAUG
14 014
4-- D 1960 W 31
1208
- -6-67
KK N
CASING WATER CIFIC ALTI - LOG TEM-
FREQUENC YOF WATER -
LOCAL WELL OIAM- METHOD DATE WATER LEVEL WATER TYPE CON- TUDE- OW AVAIL- PER- LEVEL TOTAL
WELL DEPTH ETER DRILLEO DRILLED AQUIFER LEVEL DATE USE LIFT POWER DUCT OF LSD TYPE ABLE ATURE MEASURE- DEPTHOWNER
NUMBER IFT .) 11N .) IYEARI IFT .) MEAS . ANCE (FT .) 1
F1 MENT S
I58N091W2ICCD H .JACKSON 96 4 -- -- -- 90 K158N091w2288 DESBN09IW2400C
N .ERICKSO NL .JOINSON
20218
304
--C
- ---
- ---
8150 --
HK
N
I58N09IW26CC8 E .W .SPOONER 23 24 B 1957 OG 31 8 K J 5 6 K -- 41 N20 6
158N091w27ADD U .S .G .S . 206 -- H 1961 -- -- U 2328 -- GE -- N
158N091W27CA8 A .AFSETH 201 3 C 1965 TL 0C 140 K S S 6 K N
158N091W30AD0 R .E .REYNOLDS 160 3 -- -- -- 120 -- KN
15BN09EW31AA0 L .ELEFSON 320 2 -- -- -- 150 K 6 C 47 N
158N09IW348B5 U .S .G .S . 140 -- H 1966 -- -- -- U 2332 -- GE -- N 14 0
I5BN09IW3500A B .THORVIG 40 24 -- -- -- 25 H N
I5INO92W02CBC O .SORENSON 160 4 H 1914 -- 100 K P S N
I5BN092WOSAAA H .SORENSON 160 6 -- -- -- 80 H P S 5 -- K -- 43 N
158N092WI30BC E .FODTH 24 30 0 -- 19 K J S 6 K -' N
I5BNO92WI7DCC A .MOEN 64 4 C 1939 IL OC -- H S 6 -- K 43 N
158N092W20088 J .PAULSON 100 4 H 1924 -- V K P 5 4 -- C -- 44 N
ISBN092W21BAA A .COLBENSON 120 4 H 1964 -- K S S 4 K -- N
158N092W24DCD L .PYAN 172 2 -- 1918 132 S P S 5 K -- 43 N
158N092H25CCC C .SOLGJELD 30 48 D 1914 15 H J S 5 -- K N
158N092W26ABA W .PAULSON 180 3 H 1944 150 K 5 6 K N
158N092w29AAA U .S .G .S . 140 -- H 1967 -- U -- 2223 -- GE -- N 140
158N092W29CCB U .S .G .S . 70 -- H 1966 -- -- U 2230 GE -- N 70
IS8N092W31DCC U .S .G .S . 120 H 1968 -- -- -- U -- -- 2212 -- GE -- N 120
158N092W31DAD HOVLAND BROS . 50 24 -- 1939 TL DC 30 K P S 6 -- K -- 43 N
158N093M01A00 36 -- 0 -- -- 18 K P l 6 -- K -- 45 NG .HEGSTA DO .HEGSTA D158N093W02AAD 80 -- -- -- -- 70 -- K
N
158N093W020CC U .S .G .S . 140 -- H 1967 -- -- U 2302 -- GE N 140
158NO93W03BBC J .NELSON 120 6 -- - 110 -- KN
I58N093W04AAB C .HOLMAN 45 4 C 1956 DG 51 30 H J S 6 K - 44 N
I58NO93WOTA8 0
1588D93W07R08
U.S .G .S .H.JORGENSON
5060 6
H
--
1966
--
--
-'
--40
-- UH
2235 -- GE -- NN
5 0
158N093WOBAAA G .N .RY .ET AL 116 -- -- u 2330 -- G -- N 11 6
I58N093WIICCD N.TRONDSON 130 3 -- 80 -- K N
158N093WI2AAA 8.5EM 120 5 80 5 P S 6 -- K -- 45 N
158NO93W13CCD M.TANDE 165 6 128 H
158N093W14CBC D.BUNESS 80 4 70 -- K
150N093W16888 U .S .G .S . 140 -- H 1966 -- -- -- U -- -- 2354 - - GE -- N 140
158N0931421DDC158N093W22CCA
C .ENGE TT .ALBERTSON
10 0165
53
----
- -
--
TL D C
--
96155
----
KK N
IS84093W22CCD T.ALBERTSON 132 4 C 1966 TL OC 122 -- H S S 5 -- C D 45 N
I58N093W2408A E .ERICKSON 133 3 C -- TL OL 40 6-67 C P 6 5 -- K 44 0
SPE- FREQUENCYCASING WATER CIFIC ALTI- LOG TEN- OF WATER-
LOCAL WELL DIAN- METHOD DATE WATER LEVEL WATER TYPE CON- TUDE- OW AVAIL- PER- LEVEL TOTA LWELL OWNER DEPTH ETER DRILLED DRILLED AQUIFER LEVEL DATE USE LIFT POWER DUCT OF LSD TYPE ABLE ATUNE MEASURE- DEPTH
NUMSER IFT .I I1N.1 I7E6R1 IFT .l MEAS . ANCE IFT .) 1 Fl RENTS
156N093N2SAC0 H .JGNNSON 30 36 B -- 26 K P S S K 45 NISSN093W26AAA U.S.G .S . 60 -- R 1967 -- -- -- 2310 -- DG — N 601S$N093W2711A G .N .RY .ET AL SOS U 2430 6 N LOSIS1N093W2710CISINO93W26061
E .AL$ERTSONG .N .RY.ET AL
36506
C 1927 TL OC 29S SU
P S 62375
K--
-G
43—
NN 06
lSBN093W291AA J .N .HOLLET 273 3 C 1942 TL OC 256 -- K P S 6 K 4S NIStlM93W30ARS U .S .G.S. 6O N 1966 -- U 2270 -- DO M 80151M093W34000 N .ROSENCRANS 212 3 C 1946 TL 0C 162 — K P S S K 43 NISM094WOSD00 J .HANSON 1S0 6 C TL OC 130 -- K ► S 6 K 4S N1SRN094N06000 A .O .BLIKRE 92 l2 C 1920 0G 3l 62 6-66 K P S 6 44 0
LSM094W09CC5 W.R10E 156 4 -- -- -- 120 -- K -- -- -- -- NISM094W10610 NORSTESY BROS . 22 24 6 K NISON094WI000RI A .L .TORGERSON 15 24 0 1940 QC 31 13 6-66 S J S 6 K 40 0LSBN094WI000A2 A .L .TORGERSON 16 16 0 1954 Q: 31 1S -- H P S 4 -- NISM1091888888 G.N.RY .ET AL 22S U — 2415 -- 6 - N 225
13M094YI1000 U .S.G .S . 160 H 1966 -- - -- U 2434 -- GE N 180ISENO 4N11DCA H.JGINNSON 16 1S 1S H MIS5N094W16B/6GSEN094WIASCE
U.S .G .S .C .HAASON
S E100 i
H 1966 AG 5I 2 3TS
9-66—
uK
N—
4 2305 C GE 4 7--
MN
100
ISMOMWISDAA J .RICE 13 24 -- -- 5G 31 5 -- N N
ISON094WISADD1 O .FOSSAA 23 0 1927 -- 16 -- H S 4 -- K -- N191N094M19A002 O.FOSSAA 26 0 1916 — 20 -- S 1 6 S - K 44 N1S1N094W2000D H .FROSTAD 66 24 _ 53 -- M -- N1S1N09440216A01 P.SKA6R 75 6 C 1955 -- 45 -- H J S S -- K N1SM094W210AD2 P .SKAAR 20 21 C 1963 -- 14 -- S P 1 4 — K 39 N
1SM094M21CDO U.S.G .S . 160 M 1966 -- -- — -- 2305 -- GE -- N 1601SM094W22000 E.LEE 36 22 - 26 -- -- N19BN0941121000 C .1110E 200 C 1933 -- 100 -- P 6 __ -- N1SON094W2AAAA G.N .RY .ET AL 210 2375 - - 6 -- N 21013M094W2916A 6.90RN ES 16 5 1933 OG 5l 70 P S 4 -- K 44 N
1SM09411295AO A .BOKN 67 4 C 1964 62 — H J S 4 -- K -- N15M094U21000 0.07E5550 130 6 5031 20 .- s — N1SM094N30505 U.S .G .S . So H 1967 -- — — — — 2360 -- DO N BO
ISM594N32ADO N.HUL9ERG 30 16 25 — H NlGMM4N325CC O.E .KNOSHMK 90 4 C 1933 — 15 S P S 6 -- K -- 44 N
1SNN94N3HCD I .LOCKEN SS 4 TL OC 14' -- N15ON094W)3000 N.T6NDE 135 6 C 1949 60 — H S SIN N WNUSBAC N .R ICE TS 24 5 1939 — 69 U P S
LOCALCASING MATER
5PE -CIFIC ALT!- LOG TEN-
FREQUENC YOF WATEP -
WELLWELL SIAM- METHOD DATE WATER LEVEL WATER TYPE CON- TUDE- OW AVAIL- PER- LEVEL TOTA LOWNER DEPTH ETER DRILLED DRILLED AQUIFER LEVEL DATE USE LIFT POWER DUCT OF LSD TYPE ABLE ATURE MEASURE- DFPT HNUMBER IFT .1 11N .) IYEARI (FT.) MEAS. ANCE (FT .) 1
Fl DENT S
MCOOSPY
159N090W02DA5159N090W04BCC
R.ANDERSON 23 24 8 1940 OG 31 - -- H P S 6 K 43 N
159N090W06000U .S.G .S. 178 1 H 1966 OG 51 82 9-66 U 4 2298 C GE 45 240J.STAAEL 70 24 1952 -- -- -- K P 5 4 •- K -- 45 N15911090W10AAA1 W.EGGER 40 24 B 1940 00 51 15 -- S P 1 6 -- K -- 47 N
1S9N090W10AAA2 W .EGGEA 40 24 8 1940 00 51 12 -- S P 1 47 N159NO90WIOAAA3 W.EGGER 40 24 B 1959 OG 51 17 - H P 1 5 K 47 N159N090W18BBBI O.KALLBERG 37 24 B 1961 OG 51 16 7-65 K P S 6 K -- 47 0I59N090W180B02 O.KALLBERG 40 24 B 1955 0G 51 -- --S
P S 6 K -- 44 N159N090W26DDD G.CAROLINE 240 3 C 1917 TL 0C -- -- K P 5 6 C 44 N
1S9N090W2788C R.ECKERT 27 24 0 -- -- 10 -- S N N159N090W28CDDI L .RENNER 30 24 8 1947 OG 51 23 K -- S 6 -- K -- 42 N159N09OW28CD021S9N090W29CCC
L.RENNER 39 24 B 1962 OG 51 22 7-65 5 P 1 7 K 42 0
1S9N090W33CADU.S .G .S. 160 -- H 1966 -- -- -- U -- -- -- 2300 -- GE -- N 160R .ECKERT 12 4 -- 1961 -- 23 7-65 K -- S 5 -- K -- 44 0
159N090W35DDD139N091W02DAA1
U.S .G .S. 260 -- H 1966 -- -- U -- -- -- 2298 -- GE -- N 260159N09LW020DA2
J .ECKERTJ.ECKEDT
903C
2424
BB
194 31945
TL O COG 31
--25
SH
PS
55
6S
----
KK
----
4 5--
NN159N091W07ADC
139N091W126AAU.S .B.S .F .W . 175 4 H 1961 Tl DC 15 5 P 6 6 K 46 NU.S .G .S . 120 -- H 1966 -- -- U -- -- - 2290 -- GF - - N 120
159N09IW14BDC A .LINOBERG 76 24 B 1951 -- 40 -- K P S 6 C -- 44 N159N09IW23CBAI MA1110BE0G 88 24 B -- TL OC 86 7-65 S P S 6 -- K -- 44 0159N091W23CBA2 H.LINDBERG 12 -- -- -- OG 31 - -- H -- - 5 -- K -- 46 N159N091W25AAAI59N091W30000
D .LINDBERG 163 4 -- 1950 TL 0C 50 -- S P S 6 K 43 NU.S .G.S . 220 -- H 1966 -- -- -- U -- -- -- 2345 GF -- N P20
1S9N091W33BA A159N091W34BCA
U .S .G.S . 120 -- H 1966 -- -- -- U -- -- -- 2282 -- GE -- N 120
159N0OIW358BCU .S.G.S . 259 -- H 1968 OG 52 14 8-68 U -- -- 5 2250 C GE -- 0 400J .VAAGE 54 24 -- 1932 TL OC -- -- K P S 6 -. K 44 N159N092WDICDC1 S .EDWARDS 90 -- C S P S 5 -- K -- 44 N139N092WOICDC2 S .EDWARDS 90 4 C 1960 TL OC -- -- H J S 5 -- K -- -- N
159N092W04CC6 E .NIELSEN 60 16 B 1912 -- 50 -- K S S 6 -- K -_ 43 N159NO92WODAAA O .VAN BERKOM 77 12 B -- -- 64 6-66 U P 01S9N092WOBDCO A .VAN BERKON 110 6 C 1913 -- 80 -- K S 5 S -- K -- 44 N
159N092W17ADA U .S.G .S . 120 -- H 1967 -- -- U -- -- -- 2335 -- GE -- N 12 0
139N092W17ADD U .5 .4 .S . 4C -- H 1967 F 7-67 U -- -- 4 2271 C OG 46 0 4 0IS9N092W18AB81SVN092W24AAA159N092W31AA0
C .BJERGAAR DU.S .G .S.H.HEGSTAD
18 0140
6--
--H
--1966
140
-- -- U -- -- -- 2350 -- DO --N
N 16 050 ♦ 1924 22 -- K J 5 S -- K -- 44 N159N092W31BCB1 J .ANDERSON 80 4 C 1935 6 -- SP S S -- K -- 42 N
CASING WATERSPE -CIFIC ALT1- LOG TE M .-
FREQUENCYOF WATER -LOCAL WELL DIAM- METHOD DATE WATER LEVEL WATER TYPE CON- TUDE- OW AVAIL- PER- LEVEL TOTALWELL OWNER DEPTH ETER DRILLED OPILLED AQUIFER LEVEL DATE USE LIFT POWER DUCT OF LSD TYPE ABLE ATURE MEASURE- DEPTH
NUMBER 1PT.1 11X .1 (YEAR) IFT .1 MEAS . ANCE 1FT .1 1
F1 RENT S
15960920 310682 J .ANOERSON 65 4 N 1951 F 7-66 S N S K -- 4 3159N092M31BCN3 J .ANOERSON 65 4 C 1954 10 -- U P 1 5 -- K -- 43159N092W310004 J .ANOERSON 80 4 C 1962 6 -- N 5 5 5 --I5911092W32A10 U .S .G .S . 90 -- H 1966 -- -- U -- -- -- 2280 -- GE -- 90159N092W33AAD K .HEGSTAD 168 6 C 1913 13 -- K P S 4 -- K -- --
139M092W34A88 E .AN9ERSON 180 4 C 1962 50 K S S 4 -- C 0 471S9N09UW020CSI O .ENGET 42 6 B OG 31 34 S P 6 5 -- K -- 43159N093MO20002 O .ENGET 42 6 C 1965 OG 31 35 M J S 5 -- K -- - -159N093WI2604 W .SUMMERS 141 3 -- -- -- 40 KIS9N093WIZ00 01590093W10OD1
U .S .G.S . 140 2330 -- GE N 160
19990930120AU .B .G.B . 220 H 1266_ U _
3 8 220
159N093W120A0J .SKALICKYJ .SKALICKY
86130
46
--C 1914 --
--91
----
KK
PP
55
55
- ---
CK
---
4 84 2
139N093W21000 G .N .RY.ET AL 180 -- -- -- -- -- -- U -- -- -- 2215 -- G -- N 18 0159N093W220CC 1199N0930228CC2
N .POWEL LM .POWELL
4040
621
CB
--1964
- -06 31
2 833
-6-66
SS
PJ
SS
55
- ---
KK
----
4 2- - 0
I53NO93W220003 M .POWELL 11 3 V 1946 OG 31 M P S 4 K - -159N093023000 G .SLOTSVE 100 4 C 1934 TL OC 20 S P S 5 K 43 N559N093W23005 G .SLOTSVE 120 4 N 1964 TL OC M P S 5 -- K N153N093W25COA POWERS LAKE 103 -- H -- -- -- P C 47 N159N093W25008 C .BJ ERKNESS 140 4 -- 1908 OG 51 -- K P 5 5 K 44 N
159N090026D0D POWERS LAKE 103 10 C 1940 OG 31 13 -- P M T -- p N193N093W2RHAA U .S .G.S . 140 -- H 1967 -- -- -- U -- -- -- 2200 -- GE N 160159N0931129000 U .S . G.S . 140 -- H 1966 -- -- -- U -- -- -- 2261 -- GE N 140159N093W320AD A .JORGENSON 135 3 C -- -- 119 -- K P S 6 •-- K -- N15911093W330A0 6 .008.1A9 50 S C 1962 06 51 36 6-66 K J S 6 -- K D 0
159849930348A8 U .S .G.S . 68 1 H 1967 0G 31 13 8-67 U N -- 5 2303 C GE 46 M 160139N093W35AAA POWERS LAKE 101 8 C 1959 13 -- P M T 5 -- P -- 46 N159N093W358CA C .SREDING 60 4 C 1962 -- 40 -- K P 5 5 K 43 N159N093W36A0A U .S.G.S . 78 1 N 1966 0G 31 51 8-66 U 5 2258 K GF M 12015SNO94WOIC881 J .MELBERG 210 4 M 1957 TL OC -- -- K P 5 6 -- K -- 44 N
153N094M01C0B2 J .MELBERG SO 30 0 1922 0G 31 -- N p 1 6 K - 44 N1S9N09WOI000 O .OL SON 30 24 D -- OG 31 22 K P S 5 K 43 N159N994W05AAA U .S.G .S . 140 -- H 1966 -- -- U -- -- -- 2350 -- GE -- N 160I99NO94WO8RAA M .PETERSON 22 36 0 1930 -- 18 -- K P 5 5 N1S0N094Y10BCB E .CAVLSON 214 4 C 1917 TL 0C 55 S P S 6 -- K -- 44 N
159N094W110001 H .FARSTAO 65 24 8 -- TL OC 37 S P S N159N09411110002 H .FA9STAO 66 4 H 1955 TL 0C 35 H J 6 _ N159N094M128CCI R.BLOOMOUIST 112 4 C 1909 TL OC -- S p 5 6 K 45 N159N994W126CC2 R .0LOOMO4JIST 32 48 D 1940 0G 51 20 H P 5 6 44 N159N094W12CD0 R.OLOOMQUIST 34 24 6 1958 OG 31 21 S 5 5 N
SPE- FREQUENC Y
CASING WATER CIFIC ALTI- LOG TEN- OF WATER -
LEVEL TOTALLOCAL WELL 01AM- METHOD DATE WATER LEVEL WATER TYPE CON- TUDE-
OF LSDO W
TYPEAVAIL -ABLE
PER -ATURE MEASURE . DEPTH
WEL LNUMBER
OWNER DEPT H(FT.)
ETE RITN.)
DRILLED DRILLE D(YEAR)
AQUIFER LEVEL(FT .)
OAT EMEAS .
USE LIFT POWER DUC TANCE (PT .) 1
F) MENT S
159N094813B8B1 W.RYSTEDT 175 3 H 1940 TL OC 50 K J 5 6 N
159NO94W13BBB2 W.RYSTEOT 28 48 D -- OG 31 20 H J S --
I59N094W2008 R159N094W20000
J .MOMBERGJ .NOHBERG
1 446
3 6
24
8B
195 91963
OG 31--
1 229
-- KH
JJ
SS
35
- ---
- -- - N
159NO94W21BBB U .S.G .S . 120 -- H 1966 -- -- U -- -- -- 2200 GF N 120
159N094W23CD BATTLEVIEW 17 -- V 1930 -- 10 -- M P 1 5 -- C - - -- N
1S9NO94W23000 U .S.G.S . 40 1 H 1966 OG 51 12 7-66 U -- -- 4 2195 C GE 44 W 110
159NO94W24BBB G .N .RY.ET AL 232 -- -- -- -- -- -- U -- -- -- 2275 -- G N 23 2
159N094W24DD0 G .POWELL 22 24 R 1964 fl OC 10 H J 5 4 -- K - - 45 N
1S9N094W26BC R .SETTERLUNO 30 24 B -- -- 14 -- S -- -- 5 -- P -- N
1S9NO94W34888 G .N .RY .ET AL 210 -- -- -- -- U -- -- -- 2350 -- G N 21 0
159NO94WDA000160N090WO1BCC
U.S .G .S.G.N .RY .ET AL
200165
----
H--
196 7
--
UU
----
----
- ---
242 02010
- ---
GEG
NN
200I6 S
1AONO90W01000 M .GRANLUND 28 36 0 1900 -- K P S 6 2032 K -- 44 N
16ON09OWO3BBB G .N .RY .ET AL 180 -- -- -- U -- 2040 G N 18 0
160N090W05DA01 C .ALBERTSON 160 3 M TL OC F -- S P S 6 2077 K ----
45 N
I6ON09OW05OAD2^(-o C .ALBERTSON
JACOBSON BROS .16 060
33
HH
193 0--
I LTL
OC00
FF
- ---
HS
CN
S-
6--
207 7--
K
-- -- NL6ON09OW06ABA 1160N090W06A862 JACOBSON BROS . 21 4 C -- -- 1 7-65 K P S 6 2050 K -- 44 0
SROWONOW07DD0 U .S .G.S . 90 -- H 1966 -- -- -- U -- -- -- 2025 -- GE N 90
16ON09OW09AAA C .HEGLANO 185 5 -- -- -- -- H P 1 -- 2062 --
160N000W10ADAI G .EKBERG 65 4 -- 1951 TL OL 9 -- K S S 6 2052 K 46 N
16ON090W10ADA2 G .EKBERG 19 36 0 -- 2 7-65 U P S -- 2052 -- - -
TL- -0 C160N090WLOBBB1 E .ALBERTSON 220 4 -- 1957 30 M P 5 5 2062 K N
16ON090WLOBBA2 E .ALBERTSON 210 4 -- 1914 TL nC -- -- S P S 5 2062 K 44 N
16ON090WIODODI U.S .G .S. 80 -- H 1966 OG 51 F 8-66 U -- -- 6 2171 C GE 44 0 80
1AON090WL00D02 G.N .RY .ET AL 190 -- -- -- -- -- -- U -- -- -- 2070 -- G -- N 19079
160N090W1IA88 G.N .RY .ET AL 75 -- -- -- -- -- -- U -- -- -- 2053 G N
16ON090W11CBA A.HEDLIN 86 4 C 1959 OG 51 19 -- K P S 5 2062 K -- 44 N
160N09OW128CC G.N.RY .ET AL 75 -- -- -- -- -- -- U -- -- -- '2059 -- G N 75
16ON09OWIORCC G .N.RY .ET AL 75 - - U 2064 -- G - - 75
160N090WIS000 E .CNRISTIANSON 217 4 TL OC H P S 5 2075 K 4 6
L60NOHOW14CBC G .N.RY .ET AL 75 U -- -- -- 2100 -- G - - 7 5
160N09BW1400D G .N.RY .ET AL 135 U -- -- -- 2085 -- GJ - - 13 5
16ON090WL5800 G .N.RY .ET AL 75 U -- -- -- 2100 -- G - - 7 5
16ON0901117000 G .N.R7 .ET AL 180 U 2150 -- GJ -- N 18 0
16ON090W18AOB R .SORLIE 63 4 1933 TL OC -- H P 5 6 2170 K -- 48 N
16ON090W2IROO G .N.RY .ET AL 135 U 2173 G N (135
160NOHOW2100D I .MOGREN 38 24 1948 TL OC 7-6SKU
P--
$--
6--
22002170
K--
--G
4 5- -
0N l35
L6ON090W22000 G .N .RY .ET AL 135
CASING WATERS ► E -CIFIC ALTI- LOG TEN-
fREOUENCYOf WATER.'
LOCAL WELL OIAM- METHOD DATE WATER LEVEL WATER TYPE CON- TUDE- OW AVAIL- PEN- LEVEL TOTALWELL OWNER DEPTH EVER DRILLED DRILLED AQUIFER LEVEL DATE USC LIFT POWER DUCT OF LSD TYPE AISLE ATURE MEASURE- DEPTH
NUMBER IPT .I 1111 .1 IYEARI IFT.) MEAS. ANCE IFT .1 1
Fl NEWTS
160N090W220DA W.JOWNSON 65 4 1958 TL OC 8 H J S 6 2140 K - - NIAOMOVOW23BOA C .LINDOUIST 6 -- -- TL OC F N C S 6 2110 K N160N09OWD300 0160N090W24DDA
G.N.RY .ET ALG .N.RY.ET AL
105120
----
----
----
----
- ---
UU
-- - - 213 52085
-- GGJ
- NN
10 512 0
14OM09OW2SAIS8 L .CHRISTIANSDI 40 30 0 1946 -- 30 K P S 6 2115 -- 44 N
1A0M090W2SADD G .N.RY.ET Al 172 -- -- -- -- U -- -- -- 2126 GJ N 11 216ON01OW2ESES G .N.RY .ET AL 140 -- -- -- -- U -- -- -- 2118 G N 1401600090W250D0 G .N.RY.ET AL 135 -- -- -- -- U 2160 6 -- N 13 516001090W26SCC G .N .RY.ET AL 16 5I
2160U
GJ N 16 3AON09OW26000 G .N .RY.ET AL 195 -- -- -- -- U -- -- -- 2143 GJ N 19 5
160N090W36RCC G .N .RY.ET AL 100 -- -- -- -- -- -- U -- 2180 -- G N ISOSAON09IWO58D6 V .GODEJAHN 160 3 C 1935 TL OC 140 -- K P 5 5 -- K -- 45 N160N091W0708C C .GLEAVE 365 4 C 1962 -- 100 -- K P S 6 -- K -- 45 NIAON0V1WO8888 C,ERICKSON 285 4 C -- -- -- -- K P S 6 -- K -- 45 N1{ON011W09CCD J .GLEAVE 32 18 B 1938 -- 6 7-6S S P 5 6 -- K -- 45 0
1{ON091W13AC0I U .S .G.S . 229 1 H 1966 06 52 21 7-66 U -- -- 5 2240 C GE 48 M 360160N011W13ACD2 U .S .G.S . 328 1 H 1966 OG 52 24 7-66 U -- -- 5 2240 C GE 45 M 360140N091024106 U .S .G.S . 60 -- R 1966 06 5 1
---- -- U -- -- -- ,2233 -- GE N 6 0
160N091W24C88 U .S .G.S . 460 -- H 1966 -- -- U 2265 GE N 46 0TL OC160N091V258C6 W .STEWART 100 4 C 1950 50 -- K P ' 5
-4 -K45 N
160MO91W358CA U .S .B.S .F .W. 289 2 H 1939 -- 40 3-67 U N -- -- -- __ -_ 0SAONDS1WISNCA U . S.O. S .F . W. 321 4 C 1959 OG 51 165 -- H 5 S S K 0 -- N16ON092WOT000 U .S.G.S . 200 -- H 1968 -- -- -- U - -- -- 2423 -- GE N 20 016ON092WO90DA R .CLARK 78 4 C -- -- 19 -- K P S 5 -- K - - 43 N1600092W10ADC K .LUCY 88 4 -- 1962 25 -- S S S 6 -- K - - -- N
160N092813868 A .JDNNSON 160 4 C -- K P S S -- K N16014092017RA8 U .S .G.S . 120 -- H 1967 -- U -- -- -- -- -- GE N 12 01A0NO92W200DO U .S .G.S . 120 H 1967 -- U -- -- -- 2346 -- GE N 12 016011092W2111C81 C .WE1NMANN 120 4 C -- 50 S P 5 6 -- K - - 44 N160M0928210182 C .WEtNMANN 30 18 0 1935 28 N J S 6 -- K - - 47 N
16ON012W2900A O .ENGET 85 12 B 1943 -- 40 -- K J 4 K160N092W35606 U .S.G .S . 120 -- N 1966 -- -- -- U 2395 - GF N 1201{ON09)Y02AA1 H . KLEVFNBERC 16 36 D -- -- 4 8-67 X N 1 S -- K - - 0LRON0950S0000 A .SKALICKY 38 10 8 -- 2626 -- K ► 1 4 -- C 42 N160NO93W12CAA R .TITUS 95 4 C -- 06 51 73 -- K P 5 4 -- K - - 42 N
16ON093W1300D S.KULSTAO 120 4 H 1961 -- 60 S P S 6 - K 42 N16ONO9OWI4DOC U .S.G .S . 200 -- K 1966 -- - U -- -- -- 2365 -- GE N 20 01AOM016W216COI E .GRU86 167 6 C 1961 06 51 97 S P 5 6 -- K - - 42 N160N093W21ACO216ON093W21ACD3
E .6RU6 8E .GRU88
4 040
3636
08
195 81958
----
2025
5H
5S
5S
66
----
KK
- ---
-- NN
CASING WATER CIFIC ALT1- LOG TEM-FREQUENCYOF WATER-
LOCAL WELL DIAM- METHOD DATE WATER LEVEL WATER TYPE CON- TUOE- OW AVAIL- PER- LEVEL TOTAL
WELL OWNER DEPTH ETER DRILLED OPILLFD LEVEL DATE USE LIFT POWER DUCT OF LSD TYPE ABLE ATURE MEASURE- OEPTMAQUIFER
NUMBER IFT .1 IIN .1 IYEARI IFT .1 MEAS. ANCE (FT .! I
Fl MENT S
160N093W22AAA1 E .PIXLEY 40 4 C 20 K P S 7 K 44 N
160N093W22AA62 E .PIKLEY 140 3 C OG 51 110 S P 6 K 43 N
160N093W23AC4 C .SWANSON 150 4 C - 85 K P S 5 K 42 N
I60N093W25BCB A .SKALICKY 140 4 C TL 0C 65 K J 5 6 K 43 N
160N093W290CD1 P .TITUS BC l5 B OG 51 40 H P 1 5 K 41 N
160N093W290002 P .TITUS 135 4 C 1918 OG 51 100 S P S 5 K 43 N
160N093W290CD3 P .TITUS 205 4 C 1958 TL OC 100 H J S 5 K -- N
160N093W31AAA E .NELSON 101 4 C - Tl OC 70 S P S 5 K 43 N
160X097 Y370CD1 M. GRUBB 37 IB D 192C OG 51 14 N J S 4 K -- N
I60N093W33DCO2 M.GRUBB I3C 3 C 1942 OG 51 80 S P S 6 K 43 N
I6ON093W35BAC R .SKALICKY 92 5 OG 51 40 K S 4 K 44 N
160N094W07DD0 U .S .G .S . 68 -- H 1966 0G 51 49 9-66 U N 5 2267 C C+F 47 M 28 0
160N094M12B80 R .G00DMAN 180 4 C 195P OG 51 30 -- S P D -- N
I60N094W1308 A160N094W15BCCI
R .GOODMANL .GROTE
18 0237
45
CH
196 0--
IL DCTL OC
3 080
-- KK
SP
5S
66 --
KK __ -- N
ILON094WI58CC2163N094MIBBA8
L .GROT EE .BARMOEN
4 055
2 126
8B 1964 OG 51
3 012
HK
JJ
55
65
-- KK N
r
160N094M2000C U .S.G .S . 80 H 1966 -- -' -- U - -- -- 2118 - - GE N 8 0
160N094W23CAD A .MARUSKY 28 24 B 1958 -- 8 K P S 5 -- K 48 N
169N094W25CBB1 A .MELBERG 50 24 8 1964 OG 51 -- H P S 6 -- K N
160N094W25CBB2 A .MELBERG 100 B 192B TL OC S P S 6 K 65 N
160N094M26CDD1 A .01SON 150 6 C 1925 TL 0C 70 S P N
160N094W26CDD2 A .OLSON 4C 24 B 1934 0G 51 20 H J S N
160N094W260003 A .OLSON 30 24 B 1934 OG 51 20 H J S N
160N094W27CCD K .SATMRE 124 4 C 1947 IL OC 40 S P 5 6 -- K 45 N
160N094K28DDC A .FREDRICKSON 126 3 C 1943 0G 51 -- -- S S 5 -- K 44 N
16JN094W29BBB A .THOMPSON 112 4 -- 1959 OG 51 S P S 4 v 44 N
169N094M29000 F .FREDRICKSON 101 - - OG 51 41 K P S
I6DN094W30A0A1 O0RLE8 BROS . 134 4' C 1963 TL 0C 40 K J S 4 N
160N094M30ADA2 OVERLEE BROS . 80 24 B 1939 OG 51 60 -- H P S
160NO94W31AOO WOLO BROS . 130 B C 1962 TL 0C 50 H S S 0 N
160N094W34BBB U .S .G.S . 100 H 1967 -- -' U -- 2393 GE N 10 0
16ON094M35AAA16IN089WOICDC
A .ESSE NP .KELLY
30130
243
D--
- ---
-- --40
HK
P-- 6 -- N
16INOB9WO28BC J .KOCH 20 36 0 -- -- 18 H --
I61N089WO38B8 R .AUFF0RIH 85 -- -- -- -- -- -- S P 6 6 K 41
161NO89W030C C .SWENSON 94 4 H -- TL OC 40 7-46 S 6 6 1933 C
161N089W04AAAI N.D .S .M.C . 22 -- -- -- - ---
- ---
- -'- UU
- -1946 --
00161NO89M04AAA 2
161N089W048CN.D .S .W.C .P .THOMPSON
6092
--4
--H
195 2-- 21 7-46 U P 6 1955 PTI 9C
SPE- FREQUENC Y
CASING WATER CIFIC ALT!- LOG TER- OF WATER-LOCAL WELL DIAM- METHOD DATE WATER LEVEL WATER TYPE CON- TUOE- OW AVAIL- PER- LEVEL TOTA LWEL L
NUMBEROWNER DEPT H
IFT .)ETE RIIN.1
DRILLED DRILLE DIYEARI
AQUIFER LEVEL1E7 .1
DAT EMEAS .
USE LIFT POWER DUC TANCE
OF LS OIFT .1
TYPE ABLE ATUR E1
FlMEASURE -MEN'S
DEPT H
1AIN0S0W04CCC N.D .S .W.0 50 -- -- 1952 -- -- U -- -- -- 1962 -- 0 -- N1AIN009W04000 G.N .RY .ET AL 153 -- -- -- -- -- U -- -- -- 1950 -- G -- N 153
161N0BWOSAAD N.D .S .W .0 600 -- -- 1952 -- '- U -- -- -- 1956 -- D N161M0E9WOSAC 1 BOWBELLS 710 M -- TL OC 110 P T 5 6 1957 C D 50 N161N009WOSAC 2 BOWBELLS 227 B -- -- 7L OC 220 P T 5 6 1957 P -- -- B
IBIM009W05ACO 00WBELLS 45 -- 1967 -- P -- -- 6 -- C -- 46 N16IN009WOSADC WOMBELLS 101 -- 1961 TL OC P '- -- 6 C -- -- N
I6LNO89WOS03616INOW9WOS8CC
N .D.S.M.C .N .D.S .W .C .
4021
- ---
195 2--
- --- --
UU
----
195 71955
----
00
- ---
NN
161N009WOSCADI N .D.S.W.C . 21 -- -- -- U -- 1945 -- 0 -- N
16INOS9WO5CA02 N .D .S.W .C . 17 -- U 1940 D N161N0WMWOSCR U .S.G.S . 65 5 H 3 8-47 U N 1945 0 0
16INO89WOSCBCI N .D .S.W.C . 67 -- -- -- U -- 1948 0 N161N089WO5CWC2 N .D .S.W.0 21 -- -- -- U -- 1955 -- 0 N16IN089EOSCDAI N .D .S.W.C . 17 -- -- -- U -- 1953 D N
161N069YO5CDA2 N .D .S .M.C . 11 -- -- -- -- -- -- U -- -- -- 1950 -- 0 -- N
161M 089WO9DAB U .S .G.S . 100 -- -- -- TL OC '- -- U -- -- -- -- P 0 -- N161N089W0500 I A .CHRISTIANSON 97 4 H -- 25 7-46 K - 5 6 1958 C -- -- 016IN089WOS00 2 A .CHRISTIANSON 00 5 M TL OC 26 9-45 U N 6 1958 P -- 0161M089MOSDDA A .CHRISTIANSON 133 4 C 1944 TL 0C 32 - S P S 6 -- K -- 45 N
161N089Y06600 U .S .G.S . 40 -- M 1968 -- -- -- U -- -- -- 1960 -- DG -- N 40161NOB9WOACC M .ROSS 58 6 H -- TL OC 22 7-46 U P -- 6 1962 P -- -- 0161N089W06CCD H .ROSS 51 6 -- -- -- 22 -- K J S 6 -- K -- -- N161N089W060A C .MASTRUO 70 -- H -- -- -- '- S P -- 5 1956 C -- -- N161N089W060AA1 N .D .S .W.C . 17 -- -- -- -- -- -' U -- -- -- 1961 -- D -- N
161N009WO6DAA2 N .D .S .W.C . 12 -- -- -- -- -- U -- -- -- 1965 -- D NI61NO89WO85A J .000M 100 5 H -- TL OC 25 7-46 U P -- 6 1960 P -- 016LN089WOW06 A .FISMER 102 5 TL DC 29 7-46 U P 6 6 1964 C 016IM0891N10CCC G .N .RY .ET AL 180 --
-'-'m-- -- '- U -- -- -- 1960 -- S N 100
16IM089W098B 1 R .WIPER -- 6 -- -- 24 7-46 S P 3 6 1959 P -- 0
I6IN089WOHEW 2 R .WIPER 190 4 H -- -- -- S P 1 6 1960 C -- N16IN089W090CC N .D .S .W.C . 115 -- -- 1952 -- -- -- U -- -- -- 1961 -- 0 -- N161N089M09COD G .N .RY .ET AL 165 -- -- -- -- -' -- U -- -- -- 1955 -- G -- N16IN009WI0DD L .PETERSON 273 3 H -- TL 0C 130 7-46 S P 6 5 1955 P -- -- 016INOW9W11AAA L .CHRISTIANSON 134 4 C 1965 -- 79 -- H P S 6 -- K -- 45 N
I6INOW9MIIDAA N .D .S .W.C . 327 -- -- 1952 -- - '-'
- ---
U - -P
-- -- 1940 -- 0 -- N
I6INOIVWI2B B16IN009W13CC
C .BRYANW .OUANBECK
11 2170
26
M
--
H- ---
- -TL OC , 118 8-46
US 0
--6
56
194 11957
PP
----
- ---
N0
I61N009Y14AAA B .ORMISTON 120 6 -- -- 60 -- S -- -- 6 -- P -- -- N
16INOW9W14DAA P .JORDY 285 4 H -- TL OC 100 7-46 S P 3 6 1957 P -- -- 0
CASING WATERSPE-CIFIC ALT1 - LOG TEN-
FREQUENCYOF WATER -
LOCAL WELL DIAM- METH00 DATE WATER LEVEL WATER TYPE CON- TUDE - OW AVAIL- PER- LEVEL TOTA L
WELL OWNER DEPTH ETER DRILLED DRILLED LEVEL DATE USE LIFT POWER DUCT OF LSD TYPE ABLE AZURE MEASURE- OFPT NAQUIFERNUMBER (FT .) IIN .I (YEAR) (FT .) MEAS. ANCE IFT .) 1
Fl RENT S
161N089W14000 N .O.S .W .C . 140 -- -- 1952 -- -- -- U -- -- 1958 0 -- N161N089M15CCD J.8E0.G 160 6 H -- TL OC 110 -- N P 5 6 K - 44 N
161N089WL688B N .D.S .W .C . 295 -- -- 1952 -- -- U -- -- 1945 -- D -- N----161N089W168CB N .D.S.W.C . 180 -- -- 1952 -- -- U -- -- 1950 0 -- N
161N089WI68CC N .D .S.M.C . 300 -- -- 1952 -- -' -- U -- -- 1960 -- D N
161B089W16CBC 5.O.0 .5 .2 . 120 -- -- 1952 U -- -- -- 1968 -- D -- N
161N089WI6000 N .D .S.M.0 100 -- -- 1952 -- -- __ U -- -- -- 1971 -- D -- N
161N089W19DA J .OLSON 1B0 -- H -- 31 7-46 K P 5 5 1977 P -- -- 0
TL O C16IN089W19DAA J .OLSON 90 6 -- -- 20 H N
16IN089N20AA T .JACOBSON 96 5 H TL OC 27 9-45 U P -- 6 1970 P -- 0
161N089W20AD0 N .D .S.W.C . 80 -- -- 1952 -- -- -- U -- -- -- 1972 -- D N
16IN089M21BA T .JACOBSON 150 H -- Tl OC 48 7-46 S P 6 6 1972 P -- 0
16 N 8921BB A161N089W21DA
T .JAC083U NF .HAENHOUSE
10 0100
45
--H
----
9041 7-46
HS P 6 5 1975 C -- --
N
0TL O C161N089W23AA T .BYSTEOT 180 4 H TL OC 70 8-46 5 P 6 6 1961 P -- 0
16IN089M24C8 H.OLSON 180 6 -- TL OC 105 8-46 S P 6 6 1963 P -- 0
16IN089W24OD R .HANSEN 600 3 H 120 7-46 U P 6 6 1955 P -- 0
161N089W24DDA1 R .HANSEN 360 4 M 1920 TL 0C IBO -- Z P 6 6 -- K -- N
161N089M240DA2 R .HANSEN 220 5 H 1963 TL OC 180 H S S 6 K -- -- N
16IN089W258C C .NELSON 274 4 -- -- TL OC 130 7-46 S P 6 6 1966 P 016LN089W26CCAI C .CARLSON 20 48 0 -- -- 8 -- H P 5 5 -- K 45 N
161NO89W26CCA2 C .CARLSON 265 2 H 1920 TL OC 165 -- H P 6 6 -- K -- N
16IN089W26DDD HANSEN 8005 . 237 3 -- -- TL OC 157 -- H -- -- 6 -- C -- N
161N089M2788 L .BERG 136 10 H - TI OC 4l 7-46 U P 6 6 1972 v 0161N089W27BB8 U.S .G .S . 100 -- H 1966 -- -- -- U -- -- -- 1974 -- GE N 100
I6IN089W28AA A .ECKSTROM -- 3 H -- -- 120 8-46 S P 3 6 1971 P -- 0
161N089W28AAA A.ECKSTROM 100 4 -- -- TL OC 60 -- H -- -- -- -- -- -- -- N
I6IN089M28D00161N089W308DA1
A.CH4ISTIANSO NA.SAGNESS
2 240
1 836
0B
- -1948
----
1014
5-6 59-66
UH
PP
1S
--6
198 2--
--K
- ---
- -44
N0
161N089M308DA2 A.SAGNESS 185 2 C 1962 -- 32 -- K P S 6 K 0 46 N
16IN089M33AAA G.N .RY .ET AL 105 -- -- -- -- -- '- U -- -- -- 1944 -- G -- N 10 5
161N089W338BB I .SAGNESS 24 48 D -- -- 20 -- K -- -- -- -- -- -- -- N
161N089W330A0 F .BORGESON 19 18 B 1955 -- 11 9-66 H P 1 6 -- K -- 46 0
161N089W34DAA M.IHMELS 304 3 J 1945 -- 70 -- H P 5 6 -- K -- -- N
161N089W358A8 T.ERICKSON 18 48 -- -- -- 12 -- M -- -- -- -- -- -- -- N
161N089W3600 U.S .G .S . 315 4 H -- TL 0C 5 8-47 U N -- -- 1963 -- 0 -- 0
161N091WO73AA L.PETERSON 80 8 B -- -- 12 S P S 6 -- K -- 42 N
16INO90WOIBB8 U.S.G .S . 60 -- H 1968 -- -- -- U -- -- -- 1955 -- DG - N 60
161N090W03ORDI C.MELBY 187 6 M TL 0C SO 9-45 K P 6 6 1956 P -- 0
I61N090W030OD2 C .MEL8Y 65 6 -- 1912 -- 7 6-67 K P 5 6 -- K -- 43 0
16IN090W08NC8 G.N .RY .ET AL 165 -- -- -- -- -- -- U -- -- -- 1962 -- G -- N 165
N--J59611--d0--------HE65NNTNN13M'dVV60M16CN191
N--dOLOZ99aS-----HE591435N860344'443090616049191
019dZLO2SSd5--6130 119161
_31602150083'92030208160N191
N11M--S1dH--51--236102911S3863•8103010816049191
N--d--9----S91-961----'-56021S3b3•V3000M160N19T
NdEOJ29EaS----30 11H509Sb3A3 3N •9935081609191
N--d1561L1dn------H5021i4lll1V9•f99E091609191
00--L561----N0L4-LLI--H156•S•9'T•n9820M160N191
SGlN7--5961------0--------501lV 13•Ab•N•9333I0MT60N191
0----a640059M91-19Z--HEZLNO510.3035E906CN191
N99--b--9SaS------4561--1OBNOS10.3033SEM060N191
OZIN--9--9561------0------------021l9 13'A0•N•93339EM0609191
327N--i9--O9JZ------0----9961H--OZI•S•9'S•00032£90609191
U----d--S9a0L9-561--H9tE00S10•9900660609191
0--aEE3299d991-15E00 11H15918135d0.9998260609191
0--a1E009--a991-10130 11--HtOilNION01.1999200609191
N21--9--95fH--Of04 11--E021W091SN11.36992M060N191
U----d20029S994-11EJO 11H061NO31SN11•0989080609191
SJlN--9--6861------n----------SOSlV 13'Ab•N'9e3952M060N19I
N51M5SSH--IS 909961350015S00•999912M060N191
0--d916195d991-181--H1E91103.5991290609191
0-d40619SaM91-10130 11--HE00ZN05013099•6908290609191
N219-l1aH--91--09E9Z010503IMS•96090280608191
0--dE20Z99dS94-1ZE--H10981060V1300080609191
591N--9--0661------0------------59116 13'09•9•93992090608191
0----------Ia029-112----991690N81898•39992260606191
0----d040Z95db91-.51130 11-H--301399809•8300260608141
NSt--J--9SSH--OL30 114961J9911N3593f'90006160009191
Nd590Z9Eaa----MES21NOSd3f•N2 006180609191
0d9102S9a599-12230 11NS2660503f•31006190609191
0d6102SEa991-LOL30 11HE21E635030•9032180609191
Nd99019--Nb9E-30 11H92SN051980•39VL1906091910600615--d--91-102--H1--A1134'r304180609191
O-d996199d991-LSl---H161#31910.680109060N191
001N39--OLdl------0----ZS 001961H--015•S•9•S'n00001906661910--a196199dS91-101--N1--113HSl3.0990180608191
0--309619--d091-11130 11--HS6009136•9031190608191
51N9--0561------0------'-----St1V 13•Ab•N•98901160608191
51636Ai
11.1313090•59361.131(993011•N1)1'131039908
01030-39009363601931983301051 401300836031311350319013A3193310080311160031116093131410303380011398
19101132431-930-18909MO-3001-60333016319613A313319631900094136-991011361'301
-6319830-631901-11193191333196990163
036300393-3dS
SPE- FREQUENCYCASING WATER CIFIC ALTI- LOG TEN- OF WATER-
LOCAL WELL DIAM- METHOD DATE MATER LEVEL WATER TYPE CON- TUOE- OW AVAIL- PER- LEVEL TOTALWELL OWNER DEPTH ETER DRILLED DRILLED AQUIFER LEVEL DATE USE LIFT POWER DUCT OF LSD TYPE ABLE ATURE MEASURE- DEPTH
NUMBER IFT .1 UN .) IYEARI 1FT .1 MEAS . ANCE (FT .) 1
Fl MENT S
16LN091WI000 C .GULLICKSON 180 2 H -- 20 6-46 S P 5 6 2017 P -- 016IN09IWI0DDC G .GULLICKSON 100 5 H -- TL 0C 14 -- H N161NO91WL2CC A .KISTLER 90 4 H -- TL OC 3 6-46 U P 6 1995 P -- -- 016111091W138AA1 A .KISTLER 119 3 C 1919 TL OC 13 6-46 K P S 6 1996 P 43 0161N391WI30642 4 .KISTLER 22 8 8 1925 OG 31 18 H P S 6 -- K -- N
16IN091W138BB 5 .0 .RY. ET AL 165 -- -- -- -- -- -- U 2005 G N 165I61NO91W145A J .THIES 165 4 H -- Ti 0C 15 6-46 K P 5 6 2016 P 016IN091WIAAAB J .THIES 190 -- -- -- TL OC 7 H N
161N091W140C B .ANOERSON 19C 4 H TL 0C 55 6-46 K P 6 2043 P 0161N091M143CC B .ANOERSON 159 4 C 1959 TI 0C 50 7-66 K J S 6 -- K 0
L61NO9IW1500A E .GULLICKSON 200 3 C 1928 TL OC 15 H P S 6 K 44 N161NO91W17AA G .BRYAN 235 3 H -- TL OC -- -- P 6 5 2073 P -- -- N161NO91W17CC C .BUTGERITE 104 5 H -- TL OC -- -- P -- 6 2118 P -- N16IN091M19BAO G.BRYAN 185 4 C -- -- F K
I6IN091W20CAC F .HANSON 142 4 C 1945 TL OC 10 K P S 6 K 43 N16IN091W2IBA A .CHRESt 75 3 N -- Ti CC -- S P 1 6 2098 P -- Na
16IN09IW25OA41 J .DIGMAN 110 4 C 1941 5 K P 1 5 -- K 44 N161NO91M250AA2 J .DIGMAN 151 4 C 1963 TL OC 5 K 5 S 6 -- K 45 N16IN091W25DCC C .BUTGEREIt 200 3 -- -- -- 40 K -- -- -- -- -- -- N
16IN091W26A0C E .CHREST 260 3 C 1951 TL OC F -- K P S 5 K 44 N16IN091W28DAA O.CHRISTIANSON 260 4 C -- TL OC 100 K -- -- -- -- -- -- N161N091M33ACC M.KRISTIANSON 180 4 C 1920 100 K P S 5 K 42 N16IN09IW34888 M.MARTINSON 140 3 -- -- TL OC 120 K -- -- -- -- -- N1619091W34C80 D.BE400 160 3 C -- -- 150 K P 5 5 K 44 N
161N092WOI000 M.SERNSEN 40 24 B 1930 -- 6 - H 5 6 -- K 42 N16N092MO28AA J .NESS 73 30 B -- -- 39 6-67 U P -- -- -- -- -- -- p16IN092MO38118
1 .8AKK54 12 B -- -- 32 K P 6 6 K 42 N
16N092W0300
DDE .6ELHE
125 0 -- -- 35 9-45 K P 6 6 2073 K -- 016IN092W09 BCA C .EGGEN 28 36 0 -- -- 11 6-67 K P S 4 -- K 42 0
I6IN092WIHCCA1 J .GRIFFITH 85 3 C 195C 0G 51 F -- S N 5 -- K 45 N16IN092WI000A2 J .GRIFFITH 35 36 B 1958 -- 21 -- H J S 5 K 42 N161N092W1218 P .WEINMANN 165 5 H -- -- 23 6-46 K P 6 6 2087 P -- 0161N092W120001 M.8EARD 44 18 8 9 8-65 H P 5 -- 2007 -- M161N092W12DCD2 M.BEARD 53 4 C 1952 TL 0C -- -- H P S 6 -- K 44 N
161NO92WI3DD R .OWNINGS 220 5 H -- -- S P 5 6 2159 P -- N161N09244444 J .STEEN 125 5 H -- -- 30 6-46 5 P 6 6 2113 P 0161NO92W1BBAA N.EGGEN 27 30 D -- 7 -- H J S S -- K 41 N161N092W25000 W .SMITH 14 36 D 1963 6 H J S 4 -- K 42 N161N092W35CAC J .SMITM 242 4 C 1959 TL OC 150 -- K S S S -- K -- N
CASING MATERSPE -CIFIC ALT1 - LOG TEN-
FMEOUENCYOF WATER-
LOCAL WELL DIAM- METHOD DATE WATER LEVEL WATER TYPE CON- TUDE- OW AVAIL- PER- LEVEL TOTAL
WEL LNUMBER
OWNER DEPT H(FT .)
ETE R11N .)
DRILLED DRILLE D(YEAR(
AQUIFER LEVE LIFT .1
DATEMEAS.
USE LIFT POWER DUC TANCE
OF LS D(PT.l
TYPE ABLE ATUR E1
F)MEASURE-
RENTSOMPTM
16INO92WIS000 U .S.G .S . 38 1 H 1967 OG 51 13 6-67 U 3 2400 C DG -- M 200
161N093W33A88161M093NOI000
1 .085C .HOLTER
20880
4l8 R
196 4__
-- 13035
----
KK
S--
5__
5__ K
161NONOMO588A ► .YOUNG 132 3 1929 -- 125 -- K -- -- N
161N09IM0SCCA I .WATTERUD 40 24 O 1962 OG 51 0 -- H P 1 5 -- K -- 42 N
5 6 K 42 N161MO93WO60AD161N093WI000C
I .MATTERUOU.S .G.S .
28 8260
3-- H 1968
__
266 U - P2435 -- GE -- N 260
161N093M11CD0 A .NOGA 85 22 B 45 K -_ --
161M093W1188C W.MILLER 220 6 C 1921 TL OC 180 S P S 6 -- K 42 N
161NO93MISOAC G.MARTINSON 11 24 B -- '_ 5 S __ -- N
1618093814000 N.MOFF 15 8 B 1956 OG 31 13 -- H J 5 4 -- K N
161N093W17000 8.0150N 150 4 C 1950 TL OC 110 -- 5 P 5 6 -- K 4L N
I6LN093W21BAA U.S.G .S . 260 -- H 1968 -- -- -- U -- -- -- 2410 -- GE -- N 260
161N091W22608 V .HOFF 25 42 D 1954 OG 31 15 -- K P S 4 -- K 44 N
10IM093W23CDC M .MOFF 160 4 C 1962 TL OC 125 -- S P S 6 -- K -- 43 N
1A1NON3W24A8C F .VELO 264 4 C 1961 TL OC 154 6-66 K P S 5 43 0
16INON3W24CAD O .OAS OS 12 B 1935 -- 40 -- K J S 4 K -- -- N
'0 161N093W26608 A .WESTERNESS 90 18 8 __ -- 30 K __ __ __
161M093W31860 F .HASS .JR. 187 4 -- 150 -- S -- -- -- -- N
161N093W350A0 C .WESTE0NESS 130 4 C 1961 -- 110 -- K P $ 5 K N
IMLM094WO2AAA D .WATTERUD 264 4 C 1961 239 H P S 6 K 0 45 N
I61NO94WO3000 N .IVERSON 34 8 8 - 11 6-67 U P 1 - __ 0
16IMO94W04AAA M.BURAU 355 4 C 1964 255 -- K -- S 6 K -- 44 N
IWINO94W0S0B0 M .PRIIE 30 27 -_ 15 -- K_- __ __ -- N
1618094806A00 S .0000AL 325 4 C 1949 313 -- K P S 6 K -- N
161N094M09AAA O.ANDERSON 23 36 B -- -- 9 6-67 U N - - __ 0
161N094M100ACI E .TMINGVOLD 63 48 -_ 3 6-67 S P 3 - - 0
161N094M108AC 2161M094M10DA
E .TMINGV0L OSERLIE OROS .
6 3278
B--
5 --TL OC
5218
6-67--
US
P 1 - -
" N
16IN094W130CD 0.01506 29 12 B -- -- 8 6-67 S P 1 6 K 42 0
16LN09481OACA1 L .GILBERTSON 12 48 D 1966 -- 6 -- K S S 4 K 42 N
161NOV4WI4ACA2 L .GILOERTSON 75 12 8 40 -- H J $ 6 K 43 N
161MO94M200IR E .RUNNING 286 6 C 1964 TL OC 196 -- K 5 S 7 K 45 N
161M0948220W C .ROMMOLDT SO 24 5 -- -- 15 -- S -- -- -- __ N
I6IN094M23D0C J.ORMISTON 18 36 D __ -- 7 -_ K __ -_ __
I6INO94W26ODD R.O.NEIL 22 18 B 1954 11 6-67 H -- S 4 -- K 42 O
10111054M66666 R.HOLTE 320 4 -- 200 __K -- '- -- N
162NOBBWOI000I J .DURICK 225 2 -- 1941 -- H P S 6 - - K N
►62N008W030002 J.DURICK 200 2 1941 50 7-46 5 P S 6 P 43 0
162NO66WD4C6 P.STEFFAN 2S0 5 H -- 35 7-46 S P 3 6 1876 P O
00NN0
0N0N0
a0
00N
--
Z9
------
--
0
--
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--
0
NN0N0
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092N51390----0----
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----------
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191d30-390593939018319V1910113A01-63d-11469
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d51619EdS94-LOEHE021930039•V0920061094291 M--99dM91-19530 11391N019949•63311296000291--5E61------n----0561--OLT'3•M•S•0•14990100690N291 9__S--9E------E06N1310•1009100690N29131E6199dS94-119H1002N9A99.6091106100291
0--4IdH99-9E----0246N093.19994.1969094291-0261-----n----0561--812•3.8S•0•93999111690NZ9Td126199S99-10930 11--HZ09293a1M•33861069092910955H--0630 1159613422IOWOOH.38984186860291--0161----Nn91-11I----HS062•5.1S•011E106104291
d11619Ed94-10930 11HZ612593N31S•339E10696N291 _--1d59-8L--0B452N901.09991196909291dE16199d99-8OLHES9Z5699•9996006100291d926199d91-1ZS30 11--H909t901931303001000009291--1061----------0561--Oft•3•9•5.0•N98990916909291
O016199S----H2OS133l•N03L00610NZ919--9Sd0901613522A1136•99091606900291dZ£6199dN94-10130 II--H9961ON1193AI5.309909690N091--2161Nn59-9IL--JE46EN093.10900006908291 d916199dN54-60630 11--HZBLE911NS•N9950M600NZ91
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SPE- FREOUENC Y
CASING WATER CIFIC ALTI- LOG TEN- OF WATER -
LEVEL TOTA LLOCAL HELL DIAM- METHOD DATE WATER LEVEL WATER TYPE CON-
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PER -ATURF MEASURE- DEPT H
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El NEWT S
162NO89W22604 A.REDMER 95 4 -- -- 27 -- S N
162N089W2300 150 4 M -- ----
50 9-45 S P 6 6 1912 P 0N
I62N089W230D0I62N099M24000
M .AUFFORTHH .AUFFORTH
36510
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- -TL O C162NO89W24DAA J .REOMER 300 4 C -- -- -- K P S 6 -- K 45 N
162NO89W25AAA U .S .G.S . 160 R 1967 -- -- -- U 1925 GE -- N 16 0
1626089W25A8 J .AUFFORTH 35 30 25 -- SN
TL D C162N089M27CCD E .KLEIN 295 -- C 1965 75 -- H S 5 6 K N
162NO89M288C J .KOCH 160 4 H -- 30 7-46 5 3 6 1940 P -- 0- -- -162NO89W2800 U .S .G .S. 145 5 H -- 4 7-47 U N -- -- 1941 -- D -- 0
I62N089W29AAA N.D .S .W .0 230 -- -- 195C -- -- U 1940 0 N
162N089W29CC J .KOCH 100 2 H -- TL OC -- -- U P -- 6 1951 P N
162NO89W3000 J.KOCH 150 5 H -- TL 0C 18 7-46 S P 6 6 1957P
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1626089M310A 4.OLSON 270 3 H TL OC 22 7-46 K P 6 6 1957 C - 0
162N089833889 N .D.S .W .C . BO -- -- 1950 -- -- -- U 1949 D N
162NO83W33000 T .PETERSON 68 6 -- -- 58 -- H 5 -- P -- N
1626089634A89 5 .969015 100 4 C 1909 56 7-46 K P 5 6 K -- 42 0
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162NO89W34CC A .BOLLSMAYER 83 3 H -- 10 7-46 S P 5 6 1947P 0
1626589W34000 R .AUFFORTH L8 3 1890 IC 7-46 K v S 6 1947 R -- 43 0
I62N089W3588C1 C .WILKES 22 48 V -- 20 -- H P 6 5 -- K -- 42 N
I62NO89W3588C2 C . WILKES 79 4 C 1962 45 -- S P S 6 -- K -- 43 N0
162N089W358BC3 C .WILKES 22 18 8 1952 -- 7 6-66 U N
162NO89M35000 N .O .S .W.C . 90 -- -- 1952 - U -- -- -- 1937 -- 0 -- N
162N089W35000 N .D .S .W.0 120 -- -- 1952 -- -- U 1933 D N0
162N090W01AAB U .S .S .R. 24 3 H -- -- 7 9-49 U N 9 1032 P D
162N390W01A06 U.S .S .R. 24 3 M 10 9-49 U N 8 1935 P D 00
162N090WOIADD U.S .G .S. 26 3 H 10 1-50 U N 6 1934 P D
I62NUNOW01BAA U.S .G .S. 26 3 H 8 I-SO U N 7 1938 p D 0
162N090WOIBAB U.S .S .R . 24 3 H 12 9-49 U N 7 1939 p D 0
I62M090WOIBCC U.S .G .S . 22 1 H 12 9-49 U N 4 1938 P D 0
162N090WOIUAD U .S .S .R . 24 3 H 11 9-49 U N 8 1934 p D 0
1629090801088 U.S .G .S . 12 1 H -- 10 9-49 U N 4 1929 P D 0
I626090601000 U .S .G .S . 24 1 H 9 10-49 U N S 1938 P D 0
I62N090WOID0D U .S .G .S . 16 1 H -- 11 9-49 U N 7 1941 P D 0
162N090MO2AA0 U .S .S .R . 23 3 H -- -- U N -- 19 33 -- D N
1626590602606 U .S .S .R . 22 I H 8 9-49 U N 4 1917 P D
I62NO90W02ACC U .S.G .S . 24 3 H 15 11-49 U N 6 1937 P D
162N090W028AA U .S.G.S . 26 3 H - N 1937 D
162N090W028AB U .S.S .R . 24 3 13 9-49 U N 7 1942 P P
162N090W02C88 U .S.G .S . 24 1 M 12 8-49 U N 7 1946 P D
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CASING WATERSPE -CIFIC ALTI - LOG TEM-
FREOUENCEOF WATER -
LOCAL WELL DIAM- METHOD DATE MATER LEVEL WATER TYPE CON- TODE- OW AVAIL- PER- LEVEL TOTAL
WELL OWNER DEPTH ETER DRILLED DRILLED LEVEL DATE USE LIFT POWER DUCT OF LSO TVPF ABLE ATURF MEASURE- DEPTHAQUIFE RNUMBER (FT .) 11N .) (YEAR) (FT .) MEAS . ANCE 1FT .) 1
Fl RENT S
162N090815C0C U .S .S .R . 24 3 H 17 11-49 U N 7 1963 P D 0162N090W15064 U.S .G .S . 24 1 H 19 11-49 U N 6 1957 P D 0
162N090WI5DAD U .S.S .R . 22 3 H -- 16 11-49 U N -- 6 1965 P D 0I62NO90WISDCC J.NVGAARO 60 6 H 40 7-46 S P 6 1958 P 0I62NO90WISDCD U .S.S .R . 24 3 H 15 11-49 U N 7 1966 P T) - 0
162ND9OW16CC U .S.G .S . 195 5 H -- -- 23 7-47 U N -- -- 1958 -- D -- D
162N090W160DD U .S.G .S . ID 1 N 7 7-49 U N -- 5 1952 P D 0
00 5 1I62N09OW19AAD1 T .OLSON 125 4 C 1941 -- -- S P S 6 -- K -- 43 N162N990W19AAD2 T .OLSON 201 4 C 1965 TL DC H S S 6 K - -- N162N990W22AAA U .S .G.S . 12 1 H -- -- 7 8-49 U N -- 5 1954 P D -- 0
162NO90W22BAA U .S .G.S . 24 1 H -- -- 11 11-49 U N -- 3 1958 P D -- 0
162N090W23AAD O .FERM 3C 24 -- -- -- 23 -- S -- -- -- -- -- -- -- N162N090W23BB A162N090W238DD
U .S .S.R .L .HANSEN
2 0200
32
--C
--1949
- -TL DC
96
1-50--
UK
NP
--S
--6
1966 --K
D --43
0N
162N090W24AAB U .S .S.R . 22 3 H -- -- -- -- U N -- 6 1950 P D -- N
162N090W24BA6 U .S .G.S . 24 1 H -- -- 11 10-49 N -- 6 1 948 D -- nI62NO90W2ABAB U .S.S.R . 24 3 H -- -- 7 9-49 N -- 6 1°44 D -- 0162N09CW30AD N .PETERS ET .AL . 80 4 H -- -- 26 6-46 K P 6 6 1967 P . -- -- 0162N090W3000 W .KUNOIGER 80 4 H -- 34 6-46 K - P 6 5 1970 P -- -- 0
Tl O C162N090W31ADD1 R .NINDS 42 14 8 -- 22 -- S P S 7 -- K -- 41 N
16?N090M31ADD2 R .HINDS 76 4 C 1952 TL OC 12 -- K J S 6 K -- N162N090W3100 M . PE IERSON 80 5 H -- TL DC 10 6-46 -- -- -- 5 1953 P -- 01626090W32B6162N090W33BA6
G .BE9GN .NELSON
6556
64
H--
- ---
----
2 226
7-4 6--
KN
P--
6--
6--
1961--
P--
- ---
0N
162NO90W3300 P .PETERSON 120 4 H -- -- 20 7-46 K P 6 6 1955 P -- -- 0
162NO90W34006 L .FUNK 45 6 -- -- -- 25 -- K -- -- 6 -- P -- -- N162N090W34DDD N .D .S.W.C . 20 -- -- 1952 -- U -- -- -- 1950 -- D -- N162NJ90W35ADA R .PETERSON 55 6 B 1910 TL OC 15 K P S 6 -- K -- 41 N
1624090W366DD N .MAGEDANL 236 4 -- 1920 TL OC 30 K P S 5 -- K -- 43 N
162N091W01BAA W .PETERSON 285 6 -- -- TL DC 80 H -- -- -- -- -- -- -- N
162NO91W03CAA I .NELSON SC 12 -- -- -- 38 -- K -- -- -- - -- -- N162NO91W0300 C .KALLBERG 360 3 H -- TL OC -- -- K P 6 6 1956 C -- N
162NO91W0300A C .KALLBERG 170 3 -- - TL OC 70 -- S P S 6 K 44 N
I62NO91W04DDD A .KOSTAD 385 2 -- 1912 Tt 0C 160 -- K -- -- -- -- -- -- N
162N091W05AA W .MDNSON 40 -- B -- OG 51 28 6-46 5 P 6 6 1942 P -- 0
162N091W0SBAB H . SORENSON 151 4 -- -- -- 30 -- S -- -- 6 -- P -- N162N091W050R W .NOLTE 74 2 H -- TL 0C 30 6-46 U P -- 6 1960 P -- -- 0
162NO91W06AB M .ST6ALESON 160 6 N TL OC 100 6-46 K P 6 6 1953 P -- -- 0
162N091W06CBB A . STAALESON 2D 36 1905 OG 51 14 -- H J S 5 K 42 N
162NO9IW06000 U .S.G.S . 80 -- H 1966 -- -- -- U -- -- -- 1973 -- DC -- N SO
5PE— FREQUENCY
CASING WATER CIFIC ALTI- LOG TEM – Oi YATfR-LOCAL WELL DIAM- METHOD DATE WATER LEVEL WATER TYPE CON – TUOE- OW AVAIL – PER– LEVEL TOTALWEL L
NUMBEROWNER DEPTH
(FT .)ETE R11N.)
DRILLED DRILLE D(YEAR)
AQUIFER LEVE LIFT.)
DAT EMEAS.
USE LIFT POWER DUC TANCE
OF LS OIFT .1
TYPE ABLE ATUR E1
F1MEASURE–
MENTS
DEPTH
162N011 NOBBA C .BLON 231 3 H TL OC 60 6–46 5 P 3 6 1960 P 0162NO91N0800A E .BUNTING 135 3 C 1934 TL OC 35 -- 5 P S 6 -- K 43 N162NO91W098A8 W .RERG 65 8 B -- OG 51 10 -- P 6 5 K 42 N162N011WIOAO P.PETERSON 127 2 H -- -- -- -- U P 6 5 1951 P -- N
162N091NSOOAD N .UNDHJEM 40 18 8 1945 -- 20 -- K -- -- -- -- -- -- N
162NO91W11AA C .BLOM 130 3 N 40 6– 46 S P' 3 6 1955 P 0IAZNOM1W13AAA F .INGERSON 107 2 -- 1911 TL OC 15 -- K -- -- -- -- -- N162N091W13C0 D162N091M130C
F .SCHIEL EJ .LARSON
27120
24
--H
----
- ---
1 513
- -6–46
K --P
--6
--5
- -1949
--P
N0
162N091W148C D .BENGE 160 2 H- -- -- 40 6– 46 S P 6 6 1955 P -- 0
162N09IW1SAOA D .BENGE 240 4 -- -- TL OC 25 -- K -- -- -- -- -- -- N162N091W1588 O .HOST8JOR 90 2 N -- 5 P 1 6 1948 P N
TL O C162N09IW1SDDD V .NELSON 70 4 – 1955 20 -- K P 5 6 K 42 N
162N091W17C8 A .FREORICKSON 105 D -- TL 0C 7 6 – 46 U P 6 1963 P 0162N091W18B88 J .ANDERSON 44 36 B -- TI OC 3 6–67 5 P 5 6 -- K 42 0
162N091W19CCA1 F .SAWYER 45 4 C 1953 TL OC LOG -- S P 5 6 -- K -- 43162N091W19CCA2 F .SAWYER 26 36 D -- -- 1B -- S J S S -- K -- --
.~n
162N0911120AEA N.SCOTT 17 48 D 1958 -- 15 -- K -- -- -- -- -- -- --162N091W20CD0 U.S .G .S. 160 -- H 1968 -- -- -- U -- -- -- 1939 -- GE -- N 18 0162N091W21A8 H.BUNTING 195 3 H -- TL OC 20 6 – 46 S P 3 6 1937 P -- -- 0
162N091W23C00 A.MYREN 26 18 B 1952 10 H J 5 6 K 42162N091W24AAA U.S .G .S. 38 1 H 1967 0G 51 8 8 – 67 U N -- 5 1940 C GE 46 280162N091N23AD 120 -- H TL 0C 50 9 – 45 N P – 6 1945 P - -
162N091W25AD01 FAIRVIEW MILL 94 5 -- 1921 TL OC 6 6–67 P 1 5 -- K -- 44162N091W25A002 COMMUNITY HALL 54 5 -- -- TL -- 1 6 – 67 H P 1 5 -- K
162N091W2500 H.LUCKMAN 80 4 H -- TL OC B 6 – 46 K P 6 6 1958 P -- -- 0162N091W26CBB N.RYKKEN 110 4 -- -- TL OC F -- K -- -- -- -- -- -- -- NL62NO91W27AC H.BUNTING 106 2 H TL OC 40 6 – 46 K P S 6 1953 C -- 0I62N091W33C88 A.MONSON 45 3 C 1953 TL OC 15 – U P 1 6 K -- 43 N162N091W34BD A.JOHNSON IOC 6 H -- TL OC 30 6–46 K P 6 6 1969 P -- -- O
162N092WO1BCC U .S.G .S . 260 -- H 1967 ----
-- U -- 1960 GE N 260162N092WOLC C162N092WOUCBB
M.CAMPBELL
U .S.G .S .4 138
41
--H
- -1966
2 427
- -8-66
MU 1968 GE
NM 160OG 31
162M092WO2C001 U .S.G .S. BC – H 1966 U 1967 GE N BD162N092W02CDD2 U .S .G .S. 42 4 H 1967 QG 31 27 6—67 U 1967 -- N 62
162N092MO2DDA H.HERMANSON 42 30 -- -- 35 -- K -- -- -- -- -- -- -- N
162N092W03ADD S.RIESTAD 70 3 -- -- 40 -- H -- -- -- --
162N092W0300A1 C.CHMISTIANSON 50 5 C 1960 15 -- C J S 5 -- K -- N
162N092W03DDA2 C .CHRISTIANSON 40 12 B -- -- -- U P 1 4 -- K -- 44 N
162N092W040D0 U.S .G .S . 80 -- H 1967 '– -- U -- -- -- 1950 -- GE -- N 80
50E- FREOUENC Y
CASING WATER CIFIC ALTI- LOG TEN- OF WATER -
LOCAL WELL OIAM- METHOD DATE WATER LEVEL WATER TYPE CON- TUDE- OW AVAIL- PER- LEVEL TOTA L
WELL OWNER DEPTH ETER DRILLED DRILLED LEVEL DATE USE LIFT POWER DUCT OF LSD TYPE ABLE ATURE MEASUPE- DEPT HAQUIFERNUMBER 107 .1 110 .1 IYEAPI 107 .1 MEAS. ANCE IFT .1 1
FI MENT S
162N092W05CO B .DANL 225 3 H -- TL 0C -- S P 6 6 1960 P --16200920050AB A .BOMSTAD 12 24 1946 H P l 3 -- K 3816200920060A6 t .HUNSTAD 10 24
4K
162N992WOTDOC E .BVWATER 65 45 P 5 6 -- K 42162N092010BAB R .LAR$ON 45 30 B 1965 10 S N 7
1620092010005 E .A0UNDSON 37 12 1920 TL OC 3 6-66 U N -- 6 -- K162NO92W110A A1620092012850
C .BLOOM
LIGNITE4060 10
--
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00 51
3 6
35
- -
--
H
P T Y 5 -- C 46162N092W1TBBA W .BUSCH 90 6 IS S16200920240001 0 .GL0SPEY 13 36 -- -- 9 8-65 H -- $ -- 1945 --
1620002W240002 0 .01A50EY 94 4 -- -- TL OC 84 -- H N162N092W26AC A162NC92W2ACC
L .MERMANSO NG.CRANDALL
127120
43
--H
-- -- 6 015
- -6-46
SK P 6 6 1964 P
N0
TL O C162N092W29DC01 HERMANSON EST. 55 18 B 1918 9 6-66 S P S 5 -- K 40 0162N092W290CD2 HERMANSON EST. 90 5 B 1955 TL 0C 12 6-66 H J S 6 -- K 0
162N092W30AC E .ESSEN 108 4 1962 TL DC 40 -- H 0 -- N16200920350A162N092W35DAB
W.PETER$O NM .PETERSON
1 0120
242
p -- - -
TL 0C
713
6-4 6--
SK
PP
65
66
195 0--
P- - 44
0N
162N092W75DAD A.BOMSTAD 165 2 C 1904 TL 0C 30 -- H P 5 6 -- P N
162N093002C00 H.RUDE 25 24 0 1955 -- 20 -- H P 1 4 -- K 38 N
162009300588 J .0AY 140 2 H -- -- 20 5-46 5 P -- 6 1930 P 0162N093W06CB E .ALOEN BO 5 H -- -- 8 5-46 S P 6 6 1932 P -- 01620093W0600 1 U.S .G .S. 100 5 H -- -- 9 8-47 U N -- -- 1937 0 -- 0162N093W0600 2 N.HEITZ 100 2 N -- 20 5-46 S P 6 6 1939 P 0
TL OC1620093W070AD V.JACOBY 150 4 -- 20 -- S N
162N093007000 JACOBY BROS . 12 24 B 1950 7 8-65 S P 1 -- - - MI62N093WOBAA 0 .BJ00NGJELD 26C 3 H TL OC 20 5-46 K P 6 6 1941 P 0162N093W09A8A C .THOMPSON 100 2 C 1913 TL OC 12 H J 5 6 K 44 N
16200930098A C .TH000SON 100 3 H -- TL OC 18 5-46 S P 6 1940 P 0162009301088 O.UNDHJIM 100 2 H -- -- 20 5-46 S P 1 6 1930 P 0
1620093W11AA U.S .G.S. 95 5 H -- 12 8-47 U N -- 1935 -- D - 0162N093W11ABA H.RUOE 175 2 -- -- TL OC 20 -- K P 6 -- K 44 N
1620093W140DC162N093W158081
J .KOPPELSLOE N0 .00NSNESS
4 580
182
B - -1906 TL
--OC
3 510
----
KK P S 6 -- K
NN
162N093W155082 O.BONSNESS 80 18 B 1923 TL OC 10 -- S P 5 6 -- K 42 N
162N093W19BAA 00N .OAK .UTIL .CO 445 6 TL OC U D -- N162N093W196A0 MON .DAK .UTIL .CO 446 B H -- TL OC 129 10-66 U -- -- 1973 -- 0 I 48 71620093W1966B MON .OAK .UTIL .CO 530 -- -- TL OC -- -- U 0 N162N093W19CA MON .DAK . U7IL . CO 700 6 TL OC 190 -- U 6 -- P N162N093MI9CC MON .OAK .UTIL .CO 400 12 H 1948 TL OC -- -- U N 1023
CASING WATERSPE -C.IFIC ALTI- LOG TER-
FREOUFNC YOF WATER -
LOCALWELL OWNER
WELLDEPTH
DIAR-FTER
METHO DDRILLED
DAT EDRILLED
WATE RLEVEL
LEVE LDATE
WATERUS E
TYPELIFT POWER
CON -DUCT
TUDF. -OF LSO
O WTYPE
AVAIL -ABLE
PER-ATURE
LEVE LMEASURE -
TOTA LDEPT HAQUIFE R
NURSER 1E7 .1 1119 .1 IYEARI IFT .I MEAS . ANCE IFT .) 1
El RENT S
162NO93112000 KINCAID MINE 180 6 N -- F 5-47 D -- -- 6 202 8162N093M248AA J .BUSCH 180 4 -- - TL OC 20 -- S -- -- 6 -- P16280938260001 J .GRARUD 1B 12 D 1924 12 -- H P 1 4 -- K 3 8162NO93M2W000D J .GRANRUO 275 2 19116 TL OC 60 -- K o S 6 -- r1621g93W27AD T . MF STF0.NE 55 160 2 H -- -- -- -- -- P 6 6 202 1
162N093M27A0A T .NESTERNESS 85 4 -- 30 K -- -- -- -- -- N162N093M31DB O .WATTERUD 170 3 H -- S P 6 6 2235 P N162NO93W32ADC N.YOUNG S5 14 8 -- H P S 5 -- K 43 N162NO93W328AA A .BE950N 26 12 8 6 K -- -- -- -- -- N
1628093W330A G .ELIE 100 18 B -- S P 6 6 2138 P - -16280938346A81 K .RUOE 83 4 C 1956 TL OC 50 K J S 6 -- K -- - -1628093W34AA8 2162N093W35CAB
K .RUD EN.OAS
34980
418
HB
195 1--
- ---
9 418
6-66--
UK
162N094M01D0C A .ULSRUD 17 36 D -- -- 13 K J S 5 K 4 3
162N094W026AD G.JOHNSON 107 4 C 1947 TL OC 70 -- S 5 6 -- K ♦ 3
4162N09AWO28A8162809480308
M.DIHL EU.S .G .S.
70100
125
-H
- ---
----
122 6-47
KU N -- — 1923 -- D - -
1628094809000 D.OLSON 30 12 P -- 10 -- K
1628094810CA0 R.ELY 201 3 C 1932 -- 12 -- N S 6 -- K 4 3
162N094811000 R .IVERSON 300 4 C 1917 -- 13 H J 5 6 K 44 N16211094W13DDC A.ULSRUDE 20 36 0 -- -- 14 K N1628094W22A0C 8.8I110 12 36 0 -- 5 H NI62N094M26A8B N.FAGERBAKKE 9 24 D 1948 5 -- H C 5 5 K N
IL OC16280948200011 R.PETERSON 310 3 C -- 210 K P 5 6 K -- 46 N
162N094W29AAA U.S .G .S . 160 H 1967 U -- 2210 -- GE -- N 160162N094M33AAA T.WITTY 382 3 -- -- TL OC 246 ,6-67 S p S __ __ __ 0
1628094833000 G.BURAU 295 4 -- -- TL 0C 80 -- K
162009483450163N088MOIC8
A .WITTYE .JOMNSON
6 5180
44
--H
- ---
----
5370
--7-46
SK P 6 6 1P.52 p -- -- 0
163808880280 C .OLNEY 125 4 N -- 73 7-46 K P 6 6 1860 P -- 01638088802888 C .OLNEY 300 4 H 1933 -- 30 K P 5 6 -- K -- 43 N163NO88W04BB T .KNUTSON 120 3 M -- 80 7-46 K p 6 1859 C -- -- 01638008804888 1.6801508 180 4 C 1905 -- 20 -- P S 6 K __ N
16380888038* F .MOEN 200 4 N - 60 7-46 P 6 5 1859 P -- 016350&1114000 B . 8190]. 40 18 B 1914 QG 51 10 6-66 P 1 6 -- K -- 42 01638081W0908D M.NELSON 12 18 B 1949 OG 31 8 -- P 1 3 K -- N163NO88W/ICCC U.S .G .S. 120 -- H 1966 — -- -- -- -- 1868 -- GE -- N 12 0
TL O CI63N0$MW12AAA163N080W19AC
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39 5200
4
2
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PP
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65 1870
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43__
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163NO 99999 0C G.SWENSON 212 3 3 -- -- 48 9-45 P 6 5 1874 8 -- __ 0
SPE- FHEOUFNC Y
CASING WATER CIFIC ALIT- LOG TFM- OF WATER -
LOCAL WELL DIAM- METHOD DATE WATER LEVEL WATER TYPE CON- TUOE- OW AVAIL- PER- LEVEL TOTAL
WELL OWNER DEPTH ETER DRILLED DRILLED AQUIFER LEVEL DATE USE LIFT POWER DUCT OF LSD TYPE ABLE ATURE MEASURE- DEPTH
NUMBER 1ET .) 11N .) (YEAR) 1FT.) MEAS . ANCE 1FT.) 1
El MENTS
163N088W248B G .FOX 440 2 H 61 7-46 U P 6 6 1858 C 0
163N088W25CC8 K .BEISCHLE 22 22 8 8 K __ __ __ - - N
L63N088W26AD W .KALMRACH 40 4 M 23 7-46 K P 6 5 1861 P 0163N088W2800 E .8618 200 6 H 44 7-46 K P 6 6 1857 C 0163N088W2988 W .SWENSON 180 2 H 40 7-46 5 P 6 6 1869 P 0
I63NORMW3000 E .NEILSON 140 2 H 50 7-46 K P 6 6 1881 P 0
163N088W328A A .BAUER 180 2 H -- -- 60 7-46 5 P 6 6 1871 P -- 0
163NOB8W3388 E .GINS 101 4 H -- 40 7-46 K P 6 6 1866 P 0163N088W35DAA M .WADE 464 4 C 1962 -- 50 4-67 K S S 6 -- C 0I63N089W048CB D .BURKE 90 2 C -- TL OC 23 U P 1 6 -- K 45 N
163N089WO58C F .FREED 180 2 H 90 9-45 K P 3 6 1872 P 0
163N089M068CD J .PETERSON 115 2 C - - 70 S P S 6 K 44 N163N089WO18C 8 .841R 200 5 H 130 7-46 S P 6 6 1901 P 0
163NO89WOBAD J .EMERSON 153 5 H - - 79 7-46 K p 6 6 1893 C 0
163N089WO8B8 G.GANSKOP 170 4 H - - 100 7-46 K P 6 6 1896 P -- 0
163N089W10BBB U.S .G .S. 100 -- H 1967 -- U -- -- -- 1870 -- GE -- N 10 0
163N089W10DCD G .GUEROETTE 12 42 -- 8 __ H __ N
m
163NO89MI0DOD U.S .G .S. 140 H 1966 -- -- U -- -- -- 1882 -- DG -- N 14 0
163NO89WIIACD163N089W130A41
T .GAGNUMC .OLSON
3 012
6024
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5
8
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6-66
KH J
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N0
163N089W130AA2 C .OLSON 10 24 - - 9 6-66 S - 5 -- K 61 0163N089W17ADD163N089M17DA
C .KNUDSONU.S .G .S.
200300
45
CH
196 5- -
806
--7-47
SU
PN
S--
6-- 1876
K- - O
44 N0
163NO89WIBBCA T .HARM 22 24 B 15 __ __ N
163N089W198BB A.GANSKDP 190 4 C 1954 150 -- K P S 6 -- K N
163N089W21888 N .D .S .W.0 240 -- -- 1950 U 1903 __ 0 NL63N089W218C M.KNUTSON 300 4 H -- TL OC -- -- U P 6 6 1909 P N
163N089W210AA A. SWENSON 130 2 -- -- -- 80 -- K __ N
163NO89W22000 O.PETERSON 240 2 -- -- -- 90 K 6 P N
163N089W2300 E .KIELHACK 126 2 H -- -- 60 7-46 K P 6 6 1884 P
163N089W24CC E .KIELHACK 195 2 H -- 90 7-46 5 P 6 1887 P
163N089W240C 0.946109 150 4 M -- 50 7-46 K P 6 6 1881 P
163N089W25A0 0.SWEN50W 200 6 H -- 52 7-46 S P 6 6 1881 C 0
163N089W25CB B.BAIR 167 2 H 40 7-46 S P 6 6 1898 P
163N089W26ABB1 G.SWENSON 130 4 C 1964 40 -- K P S 6 -- K N
163N089W266882 G.SWENSON 120 2 - - 65 6-66 U -- -- -- -- -- 0
163N089826000 U.S .G .S. 120 H 1967 -- -- U -- -- -- 1900 -- GE N 12 0
163N089W27DA 5 .000NS 132 2 H -- 100 7-46 K P 6 6 1920 P 0
I63N089W288C R .SWENSON 186 4 N 138 7-46 S P 6 6 1916 P 0
163N089W29A00 N.O .S .W.C . 170 -- -- 1950 __ __ U -- -- 1925 - - N
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163N093W060CB E.PE7ERSON 255 2 C 1909 26 K P 6 6 1907 K 43 N163N093WOBAD R•ULEBERG 204 5 H TL OC 73 5-46 5 P 3 6 1919 C -- 0161NO03WOBCC6163N095W09DA8
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91-5BL--H--96N0Hlbui•333Z1696u9691
9,-5S8----H16Z19H0093000.36(1199606691
59-602----66191N1533130.900301a,636691
99-901--U90ZZ6]106.329996099606691
LI--0b181HJSn6•iI9d96JM160NE91 --
--0900 110,61L991SNIS'M2U99L0M160NE91
--S1It JO92610l0Z5615.610901J01609E91
--09----91016115606.03939099909191
99-595----N939Z9IJS8ON•U9390M960N691
------HS011•S'.'S •nZ 9990M960NE91
91-5663a ll--52133191a9•81 99609,6UN(91
91-509----fJOEN05a3190930•0969)996CN691__----'0961H--RI'5.0'5'00001069606191
----5OilJb30.801Z0#960NE91
19-801----S531•S•J•S•0009EME609691
L1-e9----N60S1'S•0'S•n9896MEbONt91
9,-59E----08111SS3NSN06.19VEEM669NE91
19-6L1130 110901HtlZ5Z509Nnl63009ZC9(bONt9l
--30 ll99613905Zsn9Nnw3Zx18ZkMEo0N491--09130 11L561399105096010313090E96609E91
--3U 11056139S1E509981030360E9666NE91
99-911----8Z1SiSVb9V0.309081(96618691
----
SZ--
----
L161L961
dH
9Z--
S9091
199900'3•3•M•5.0•N
119918ME60N6916000690618191
------L901H--001•5.3.5'03300LMf6UNE91
69-819ZS 008961NlJ99•3'6•5.0.6689990E6060889969-860ZS JO8961H1005•3•9•0•0•1a09991690699E91
89-899
.ZS 008961H9505909601030699069E609191----
El--
----
91619961
9H
91--
9Z011
905609•0•S•01S•n
699669669869100062ME60Nt91
•S8391.1311803111•N111.131899606
3190139319331009'0311190031119093139183083NM01136
138319316931100019136-60101131119301
S319M061533
061N
30U
CASING WATERSEE -CIFIC WTI- LOG TEN-
FREQUENCYOF WATER-
LOCAL WELL 01AM- METHOD DATE WATER LEVEL WATER TYPE CON- TUDE- OW ' AVAIL- PER- LEVEL TOTA LWEL L
NURBEROWNER DEPTH
(FT .'ETE RIIN .1
DRILLED DRILLE DIYEARI
AQUIFER LEVELIFT .1
DATEMEAS.
USE LIFT POWER DUC TONCE
OF LS D(FT .)
TYPE ABLE ATONEI
FPMEASURE-
NESTSDEPTN
163N094W190AA U .S.G .S . 60 -- H 1968 -- -- -- U -- -- -- 1913 - DG -- N E .16311094820008 U .S.G .S . 160 -- H 196M -- -- -- U -- - -- 1909 -- GE -- N 16 0163N0940200D 0163N094M20CA
C .GRAVE SS .OAHL
2 8240
162
8M
1912 OG 3 1TL OC
560
6-665-46
HS
PP
1S
36 1912
KP
----
42--
00
I63N094W20CAA S .OAHL 88 4 C 1962 TL 0C 30 -- H S S 6 -- K -- -- N
163N094W21CBB U .S.G.S . 400 -- H 1968 -- -- -- U - -- -- 1910 -- GE -- N 4001630094W22000 U .S .G.S . 240 -- H 1968 -- -- -- U -- -- -- 1905 -- GE -- N 240163N094W22C0R1 U .S.G.S . 190 -- H 1968 -- -- -- U -- -- -- 1900 -- CE -- N 190163N094W22CB82 U .S .G.S . 98 1 H 1968 OG 52 24 8-68 U N -- 1900 C DG -- 0 160163N094W22000 D .009NTVEDT 88 2 -- -- TL OC 48 5-46 K J S 6 1911 P -- 41 0
163009402200 C .HAUGSTAD 98 3 H -- 55 5-46 S P 6 6 1912 P -- -- 0I63N094N23AB E .8RENN0 110 18 B -- 68 5-46 5 P 6 6 1927 P -- -- 0163N094W23CD U .S .G.S . 231 5 H -- 33 8-47 U N 1918 -- 0 -- 0163N09402466 H .BRENNO 200 4 H 94 5-46 S P 5 5 1917 P -- 0
TL O C163N094W24A6A H .BRENNO 110 3 C -- -- S P S 5 -- K -- 44 N
161N094N25AAB N .D .S .W.C . 290 1 H 1967 OG 52 46 9-68 U - 1915 -- GE 300163N094W26C8 L .LUNSTAO 90 S H 1946 -- 52 5-46 S P 6 5 1917 P -- - 0163N094W26CB81 L .LUNSTAD 70 4 OG 51 35 -- S P 5 5 -- K -- 44 N163N094426002 L .LUNS7AD 68 4 C 1965 OG 51 40 -- H J T 6 K 48 N163N094W27C08 U .S .G .S . 120 N 1968 -- -- -- U -- -- -- 1914 -- GE -- N 120
163N094W27000 U .S .G.S . 40 -- H 1968 -- -- -- U -- -- -- 1915 -- DG -- N 401630094029AAA U .S .G.S . 40 -- H 1968 -- -- -- U -- -- -- 1912 -- OG -- N
45
163N094839AD R .SLATER 309 4 H TL OC 47 5-46 K P 6 6 1915 P -- 0163N094W31DCC1 L .AABERG 16 18 8 1961 0G 31 10 10-65 5 P S 6 -- C -- 46 0163N094W310CC2 L .AABERG 18 24 0 -- -- 10 8-65 U N -- -- -- -- -- -- N
163N094M33AA S .N0800UM 270 2 H -- -- 40 9-45 S P 6 1922 C -- 0163N0948336AB S .NORORUN 200 2 -- -- -- -- U P S 6 -- K -- 44 M160N094W33AAC 5 .9050900 15 12 B -- 8 6-66 H P 1 4 -- K -- 44 0163N0940340DC W .BRENNO 53 18 0 32 6-66 S S S 6 K 44 0161N094U366BB N .O .S.W.C . 100 -- H 1967 -- -- U -- -- -- 1930 -- GE -- N 100
164N0080338C 0 .JOHNSON 140 3 N -- 41 7-46 5 P 6 6 1053 P -- 01641108883500 C .OLNEY 205 4 H -- 41 7-46 K P 6 6 1072 P -- 0164N0N903000 U .S.CUSTOM STA . 135 4 H 60 9-45 P 3 6 1043 P - 0I64M089W30D00 C .WOLEM 19 48 D 1938 4 6-66 U P 6 K -- 0164NO09W31AC M .NC GILLIRUAV 156 2 H -- 79 7-46 K P 3 6 1812 P -- 0
164N009031AD C .tHOMPSON 165 2 4 -- -- -- - -- -- 6 1867 P -- N164N009031000 U .S.G .S . 00 -- H 1961 -- -- U -- -- -- 1875 -- DG N 8016400894320 [164404983200
G .N.R .M .C .MCINTEE
10690
62
HH
----
5 020
9-657-46
SS
PP
-
-6
66
10611056
PP
- ---
00
164M089034C0 R .HANSEN 150 2 H 40 7-46 K P 6 6 1841 P -- 0
CASING WATERsum-CIFIC ALTI- LOG TEN-
FREQUENC YOF WATER -LOCAL
WELLWELL OIAM- METHOD DATE WATER LEVEL WATER TYPE CON- TUOE- OM AVAIL- PFR- LEVEL TOTAL
NUMBEROWNER DFPT H
IFT .IETER1111 .1
DRILLED DRILLE D1YEAR1
AQUIFER LEVEL(FT .!
DATEMEAS .
USE LIFT POWER DUCTANCE
OF LSOIFT .1
TYPE ABLE ATON E1
FlMEASUPE -
MENTSOERTIP
16441090W25DC P .TALELMEYER 152 4 N -- 90 9-45 S P 6 6 1865 P 0164N090W250CD1 O .TVEIT 22 30 D 1904 7 N P 1 6 K 41 N164N090W25DCO2 O .TVEIT 170 4 C 1934 OG 51 110 7-46 K P 5 6 1873 P164N090M26CDC R .GANSKOP 170 4 -- -- TL OC 60 -- K -- -- 6 1873 P N164N090M32C00 H .BENSHOOF .JR . 280 2 TL OC 120 -- K -- N
164N090W32DC N .WILSON 200 2 H 150 6-46 S P 6 6 1918 P 0164N090W3300C A .WOLKENHAUER 205 4 C 1956 TL OC 135 K P S 6 K 45 N164N090W34CC R .NANSEN 200 6 H 96 6-46 S P 3 6 1897 P 0164N09083568A U.S .G .S. 81 I H 1966 OG 51 7 9-66 U -- -- 6 1869 C GE 47 M 12 0I64N091W328C8 W .KELLER 18 36 D -- -- 10 -- H -- -- -- -- -- __ -- N164N091W320CC1 S .ERICKSON 362 1 H 1917 -- 100 S P S 5 -- K 44 N164N091W320CC2 S .ERICRSON '20 36 D 15 H P 1 6 -- K 41 N164N091W340CC A .LUND 83 2 C 1953 OC 51 16 H -- S 6 K 43 N164609202550 500 LINE RR . 708 P H -- TL OC -- A -- 6 1950 P 0 -- N1646092W29DDA W .CLINGMAN 290 3 -- -- TL OC 150 K
064609260408 J .RUPPERT 400 3 H -- -- -- -- U P 1 5 -- P164M092M340C J .RUPPERT 345 4 H -- -- -- -- S P 3 6 1959 C N164N092W35A60 L .CEGOMSKI .SR. 17 30 -- -- -- 6 -- K - - N164N092W36AA6 PORTAL 625 -- H -- TL OC 260 -- P -- -- 6 -- C 46 N164600283600 U .S .G.S . 265 5 H -- -- 7 8-47 U N -- -- 1950 - - D -- 0
164N093W270001 C .LARSON 26 12 8 1902 TL OC 16 H J S 6 -- K -- N164N093W270002 C .LARSON 16 30 D 1920 -- 7 6-66 2 P 6 4 K 39 0164N093W3I00 U .S.G.S . 50 5 H -- 10 8-47 U N -- -- 1903 - - D 0164M093035CCC U .S.G.S . 40 -- H 1966 -- -- -- U -- -- -- 1917 - - DG -- N 60164N093N3S0DC OLSON EST . 26 36 0 -- -- 4 8-65 U P 1 -- -- - -
164N094M32CC
' V .WRIGLEY 12S 4 H -- -- 70 5-46 K P 6 6 1907 P 0164N0448306D D .EARLV 110 3 N - 100 5-46 K P 3 6 1905 P1646094633D001 J.KNUTSON 110 4 - 1905 OG 51 90 -- U P 116460949330002 J.KNUTSON 18 18 B 1936 -- 14 -- U P 1 6 -- K 44 N
TABLE 2 .--Records of springs
EXPLANATION
Use of water
Lithology
H, domestic
S, stock
L, lignit eK, domestic and stock
U, unused
S, san d
Location
Owner or name
Use of water
Lithology
Flow range
Conductance
Temperature
Remarks(gallons per
(micromhos per
°Fminute)
centimeter at 25°C )
MOUNfRAIL COUNTY
150-92- 8dda D . Drags Wolf U L 0 . 8150-92- 9dab L . No Arm S L 6150-92- 9dbc Otter S 4150-92-12aca D . Stevenson S L 3 . 5150-92-ltbac R . Dancing Ball S S 3
150-92-22dad L . Medicine U L . 2150-92- 2 7bbd J . Berries U S . 1150-92-34aad S L . 8150-92-35bdc Young Woman S S . 8150-93- 2abd W . Big Head S L . 4
150-93- bade M . Evans S L 6150-93- 8aba D . Driver S L . 1150-93- 8bbb N . Eagle S L 1150-93- 9dbbl M . Red Feather S . . . 1150-93- 9dbb2 M . Red Feather S . 1
150-93-10acd L . No Arm S L . 2150-93-10cab Otter S L 2150-93-10daa Otter S . . 2150-93-llbec J . Horn S 1151-90- Sdad3 P . Hilleren S L 1-4 1,050
Location Owner or name Use of water Lithology Flow range Conductance Temperature Remarksnumber (gallons pe r
minute)(micromhos pe r
centimeter at 25°C)
O F
151-90-14aca3 J. Bartelson S 8 1,680 4 3152-90-24bcc F . Maurer S •S 35 1,420 Several outlet s
152 -92 - 3dbb M. Ruland K S 1-1 .5 800 4 7152-92-llbdc M. Ruland S S 100 1,200
153-90-33acd J. Casey K L 3 66o
153-92- 6caa E . Satterthwaite S L 2,160
153-92- 6dcc E . Satterthwaite S L .1-1 3,000 45154-91- 4dab F . Evans S L .1- 1154-91-17acbl J. Baaken H L .3 580154-91-17acb2 J. Baaken S 3 43o 46
154-91-19cba2 E . Tilisto S L 1-10 1,15 0
154-91-3odc c W . Evans S L 1-10 1,810 40154-92-23ddd2 C . Arndt S L 1,020 39154-92-25daa F . Evans K L 1-10 2,950154-92-31dac Gibb Springs K . . 16o 1,310 45 Several outlet s
154-92-35aba W . Evans S L .1-1 3,990 4 5154-92-35cac W . Evans H L .1-1 4,600154-92-35dca W . Evans K L 1-10 2,210 4 5
155-90-13ada T . Dolan S 10 4,300 4 6
156-89-23ddb2 J . Biere H 3,000 4 4
156-93-31c dc R . Quammen S L >100 2,900 -46
156-94- 9bda L . Lund K L 1-10 1,390 45156-94-23cac T . Watson U 11-100 2,900 48 Several outlets156-94-23ddc T . Watson S 1-10 2,550 47
156-94-33aac H . Ortlof£ 1-10 1,570 47
Location Owner or name Use of water Lithology Flow range Conductance Temperature Remarksnumber (gallons pe r
minute)(micromhos pe r
centimeter at 25°C)
OF
156-94-34bda G . Williams K L .12-1 990 46157-89- 9daa L. Goettle S . . 1 530 4 5157-89-15aad L. Goettle S 5 560157-89-20dcd M. Nelson U S 50 1,940 44157-93-18bbb J. Moore H . . . . 1,910 49
157-93-30bba J . Moore S L .1-1 1,620 50157-93-3obbc J . Moore S 1-10 1,130 47157-94- 9dad M . Jorstad S S 50-75 1,580 40157-94-13aac M . Leichtie U . . 20 1,470 45 Several outlet s157-94-25bbd J . Enger K . . 1 1,110 50
157-94-26dac E . Dannewitz S L 25-30 900 4 1158-93-19ca c
BURKE COUNTY
J . Blikre K L 10 1,500 4 7
160-90-22bba W . Johnson K S 10 1,620 45
TABLE 3 .--Water levels in selected wells
MOUNTRAILCOUNTY
Depth to water, in feet below land surfac e
151-89-12add
Date
Wate rlevel
Date
Water
Date
Wate rlevel
leve l
June 3, 1966 5 .45July 22 7 .11Oct . 14 8 .56Nov . 14 Froze nDec . 14 Froze nApr . 25, 1967 2 .72May 15 3 .57June 12 5 .36
July 17 6 .89
May 13 7 .92Aug. 9 7 .94
June 6 8 .28S ept . 12 8 .80
July 3 8 .60
Oct . 10 9.23
Aug .
5 9 .23Nov . 14 9.56
Sept . 4 9 .82Dec .
4 9 .64
Oct .
2 9 .81Mar . 13, 1968 7 .50
Nov .
5 9 .87Apr . 10 7 .6 1
151-90-36dda
June 7, 1966 68 .80Nov . 14 68 .4 7Dec . 14 68 .44Jan . 23, 1957 68 .08Feb . 20 68 .26Mar . 16 68 .52Apr . 20 A/72 .34Apr . 20 68 .04May 15 68 .03
June 12 67 .74
May 13 68 .20July 17 1183 .27
June 6 67 .7 9Aug. 9 68 .50
July 8 68 .99Sept . 12 1179 .14
Aug . 5 67 .5 3Nov . 14 68 .01
Sept . 4 68 .2 1Dec .
4 68 .86
oct .
2 67 .3 1Feb . 6, 1968 67 .86
Nov .
5 67 .6 0Mar . 13 67 .66Apr . 10 67 .86
11 Pump had been operating .
151-92-34daa
Sept .Sept .Oct .Nov .Dec .Jan .Feb .Mar .
2, 1966 73.8323 73 .4712 73 .1014 73 .0714 72 .8323, 1967 73 .3 020 73 .2 716 73 .59
Apr . 25 72 .84
Dec . 4 72 .2 1May 15 72 .31
Jan . 9, 1968 72 .6 6June 12 71 .74
Feb . 6 70 .4 0July 17 71 .52
Mar . 13 70 .08Aug . 9 71 .98
Apr . 10 70 .07Sept . 12 70 .96
May 13 69 .59Oct . 10 71 .07Nov . 9 70 .44
152-90-18cc c
May 27, 1966 14 .16June 2 14 .10June 8 13 .7 9June 17 13 .6 4July 22 12 .6 8Aug .
2 12 .7 5Aug . 24 21 .91Sept . 23 13 .31o ct . 14 13 .59Nov . 14 14 .04Dec . 14 14 .40Jan . 23, 1967•••• 14 .85
Feb . 20 15 .2 6Mar . 16 15 .5 7Apr . 20 14 .59May 15 14 .39June 12 13 .90July 17 11 .60Aug .
9 11 .24S ept . 12 11 .81o ct . 1o 11 .94Nov .
9 12 .30Dec .
4 12 .5 5Jan .
9, 1968 13 .23
Feb. 6 12 .6 4Mar . 13 13 .6 4Apr . 10 13 .3 8May 13 13 .48June 6 13 .75July 3 12 .55Aug .
5 11 .40S ept . 4 10 .95Oct .
2 10 .74Nov .
5 11 .11
69
Depth to wattae . In feet below land surfac e
152-92-17bbb
lao
Wat•r
Date
Water
Date
Waterlevel
level
leve l
A. , . .
,
i 96 .23
Nw .
9 91 .97
Jon? 13 91 .551, 95 .73
Dec .
4 92 .13
July
1 91 .7 1on 12 95 .24
Jan .
9, 196 8 — 92.34
Aug .
5 90 .5 3July 17 94 .41
Feb .
6 92 .70
Sept . 4 90 .08Aug .
9 94 .01
Mar . 13 91 .87
Oct .
4 89 .6 3S ept . 15 93 .10
Apr . 10 91 .80
Nov .
5• 89 .4 2Oct . 10 92 .75
May
13 91 .2 4
1'-92-19aab
Aug .
9, 1967 48 .8 4Sept . 13 50 .50Oct . 10 50 .2 3Oct . 26 50 .7 3Oct . 31 50 .8 3Nov .
5 51 .28Nov . 10 51 .2 5Nov . 15 51 .4 5Nov. 20 51 .48Nov . 25 51 .50Nov . 30 51 .96D ec .
5 52 .52Dec .
7 52 . 09Jan .
9, 1968 54 .21Jan . 10 54 .17Jan . 15 54 .53Jan . 20 54 .92Jan . 25 55 .08Jan . 31 55 .3 5Feb .
5 55 .5 5F eb . 10 55 .6 7Feb . 15 55 .83
Feb . 25 56 .4 7Feb . 28 56 .6 5Mar .
5 56 .5 5Mar . 10 56 .6 5Mar . 13 56 .36Apr . 10 53 .1 0May
5 54 .2 0May 13 54 .17June 10 55 .8 3June 15 55 .8 0Jaw 20 53 .97 'June 25 53 .4 3June 30 51 .87July
5 51 .28July lc 51 .03July 15 50.68July 2o 50.79July 25 49.83July 31 49.68Aug .
5 50.01Aug . 10 49.64Aug . 15 49.13
Aug . 20 48 .8 5Aug . 25 48 .4 5Aug . 31 48 .1 7Sept . 5 48 .0 0Sept . 10 47 .9 2S ept . 15 47 .7 2Sept . 20 47 .4 5S ept . 25 47 .60Sept . 30 47 .5 1Oct .
5 47 .7 5Oct . 10 48 .0 5oct . 15 48 .53Oct . 20 48 .54Oct . 25 48 .4 5oct . 31 48 .95Nov .
5 48 .95Nov . 10 49 .00Nov . 15 48 .95Nov . 20 49 .0 0Nov . 85 49 .08Nov . 30 49 .9 4Dec .
5 49 .52
152-92-20ad d
May 27, 1968 90 .82
Feb . 20 96 .00
Jan .
9, 1968 89 .5 9June
2 90 .60
Mar . 16 97 .35
Feb .
6June 17 89 .29
.Apr . 20 96 .12
Mar . 13 91 .54July 22 88 .69
May
15 94 .92
Apr . 10 90 .37Aug .
2 88 .70
June 12 92 .46
May 13 91 .08Aug . 26 88 .42
July 17 86 .19
June 6 92 .10S ept . 23 8 9 .93
Au ;- .
9 84 .44
July
8 87 .02Qct . 12 89 .34
:ept . 12 86 .22
Aug .
5 85 .80Nov . 14 91 .09
Oct . 10 55 .74
Sept . 4 83 .6 6Dec . 14 9 2 . 6 0
N . .
9 86 .77
Oct .
2 83 .3 3Jan . 23, 1967 94 .24
n 1 37 .57
Nov .
5 84 .4 9
152-92-29dd d
July 17, 1967 41 .48
Jan .
9, 1968 . . . . 43 .48
July
8 42 .26Aug .
9 41 .45
Feb .
44 .48
Aug .
5 40 .92S ept . 12 41 .64
Mar . 13 44 .80
Sept . 4 39 .7 3Oct . 10 41 .53
Apr . 13 44 .23
Oct .
2 39 .3 1Nov .
9 41 .76
May 13 44 .68
Nov .
5 39 .6 9Dec .
4 42 .21
June
6 45 .2 1
70
90 .86
Depth to water, in feet below land surfac e
152-92-31cc c
Date
Water
Date
Water
Date
Waterlevel
level
level
(t- .
9, 1967 23 .46
Feb .
6 22 .56
Aug .
5 22 .3 5pt . 12 22 .35
Mar . 13 22 .34
Sept . 4 22 .3 94 . 10 22 .43
Apr . 10 22 .39
Oct .
2 22 .3 8Us .
9 22 .41
May 13 22 .30
Nov .
5 22 .374, 22 .44
June
6 22 .4 0:-at .
9, 1968 22 .44
July
8 22 .4 4
1 53-92-17bbb
Aug .
9, 1967 6 .11
Jan .
9, 1968 6 .37
July
1 5 .4 7Sept . 15 6 .51
Feb .
6 5 .93
Aug .
5 6 .02Sept . 23 6 .23
Mar . 13 5 .35
Sept . 4 5 .6 3Oct . 10 6 .19
Apr . 10 5 .29
Oct .
2 5 .6 3Nov .
9 6 .09
May 13 5 .32
Nov .
5 5 .6 2Dec .
4 6 .05
June 13 5 .3 2
154-89-15ddd
Aug . 10, 1967 15 .3 8S ept . 13 15 .64Oct . 11 15 .7 0Nov .
9 15 .6 8Dec .
4 15 .7 2Jan .
9, 1968 15 .77
Feb .
6 15 .75
Aug .
6 15 .8 5Mar . 12 15 .52
Sept . 5 1- .80
Apr . 10 15 .43
Oct .
2 15 .6 0May 15 15 .33
Nov .
5 15 .5 5June 11 15 .57July 3 15 . f
154-9l-3Oaa a
Aug . 25, 1966,,,, 19 .11
June 12 19 .19
Apr . 10 19 .4 1Sept . 23 19 .28
July 17 19 .34
May 15 19 .3 4O ct . 12 19 .18
Aug .
9 19 .38
June 11 19 .3 7Nov . 15 19 .29
Sept . 13 19 .24
July 3 19 .4 8Dec . 14 19 .25
Oct . 11 18 .42
Aug .
6 19 .8 2Jan . 23, 1967 19 .23
Nov .
9 19 .41
Sept . 5 19 .4 4Feb . 20 19 .32
Dec .
4 19 .35
Oct .
2 19 .4 0Mar . 16 19 .46
Jan .
9, 1968 19 .50
Nov 519.4 1Apr . 20 19 .10
Feb .
6 19 .60May 16 19 .28
Mar . 12 19 .5 3
l54-94-3bb a
A ug .
9, 1967 10 .74
Feb .
6 10 .57
Aug .
5 10 .52Sept . 15 11 .00
Mar . 13 10 .23
Sept . 4 10 .02O ct . 10 10 .82
Apr . 10 10 .18
Oct .
2 9 .94Nov .
9 10 .60
May 13 10 .29
Nov .
5 9 .87D ec .
4 10 .55
June 13 10 .35Jan .
9, 1968 10 .58
July 1 10 .41
71
Depth to water, in feet below land surfac e
155-88-6dd d
Date
Waterlevel
Date
Water
Date
Waterlevel
leve l
Aug . 25, 1966 133 .35S ept . 22 133 .53Oct . 14 133 .94Nov . 16 133 .38Dec . 14 133 .30Jan . 23, 1967 133 .75Feb . 20 133 .74Mar . 16 134 .36Apr . 20 133 .03May 16 133 .69
June 12 133 .30
Apr . 10 133 .46July 17 133 .42
May 15 133 .50Aug . 10 133 .88
June 11 133 .63Sept . 13 133 .08
July 3 133 .91Oct . 11 133 .30
Aug .
6 133 .65Nov .
9 133 .30
Sept . 5 133 .6 4Dec .
4 133 .51
Oct .
2 133 .7 3Jan .
9, 1968 134 .04
Nov .
5 133 .93Feb .
6 134 .18Mar . 12 133 .71
155-89-25acb l
Sept . 20, 1965 11 .6 9Oct .
4 11 .6 4Dec .
8 11 .6 7Mar . 18, 1966 12 .00Apr . 15 11 .69
May 13 11 .49
Jan . 23, 1967 12 .56June 17 11 .64
May 16 11 .5 8Oct . 14 12 .45
June 12 11 .73Nov . 16 12 .38
July 17 12 .28Dec . 14 12 .5 0
155-89-25acb2
Sept . 20, 1965 14 .01Oct .
4 13 .98Sept . 22, 1966 14 .7 2Oct . 14 14 .7 8Nov . 16 14 .7 6Dec . 14 14 .8 5Jan . 23, 1967 14 .93
May 16 13 .99
May 15 . 1A 14 .96June 12 14 .10
July 3 15 .58July 17 14 .63
Aug .
6 16 .24Aug . 1 : 16 .12
Oct .
2 15 .26Oct . 11 15 .78
Nov .
5 15 .04Nov .
9 15 .6 2Dec .
4 15 .5 9
155-89-25bc c
Sept . 15, 1965 +0 .09Sept . 21 + .16Dec .
8 Froze nJan . 20, 1966 Froze nMar . 18 Froze nAp r . 15 Froze nMay 13 + .3 7June 17 + .2 2July 22 + .09Aug . 31 + .04Sept . 22 07
Oct . 14 0 .10
Dec .
4 Froze nNov . 16 Frozen
Mar . 10, 1468 FrozenDec . 14 Frozen
Apr . 10 0 .01Apr . 20, 1967 + .43
May 15 + .02May 16 + .33
June 3 0 8June 12 + .29
July 3 2 5July 17 08
Aug . 6 4 9Aug . 10 21
Sept . 5 3 8Sept . 13 34
Oct .
2 3 3Oct . 11 38
Nov .
5 2 5Nov .
9 Froze n
72
Depth to water, in feet below land surfac e
155-89-32aaa
Date
Wate rlevel
Date
Wate rlevel
Date
Wate rleve l
Sept . 2, 1966 13 .3 5Sept . 22 23 .1 9Oct . 14 24 .3 5Nov . 16 24 .3 3Dec . 14 Snow plugFeb . 20, 1967 25 .27Mar . 16 24 .86Apr . 20 23 .98May 16 23 .48
June 12 23 .31July 17 23 .89Aug . 10 24 .75Sept . 13 25 .48Oct . 10 25 .70Nov .
9 25 .65Dec .
4 25 .55Jan .
9, L968 Snow PlugFeb .
6 25 .88
Mar. 12 25 .3 1Apr . 10 25 .1 0May 15 24 .47June 11 24 .2 8July 3 24 .3 5Aug. 6 24 .9 6Sept. 5 24 .6 6Oct .
2 24 .37Nov .
5 24 .12
155-89-35aaa
Aug .Sept .Oct .Nov .Dec . 14Jan . 23, 1967Feb . 20Mar . 16Apr . 20 19 .0 2May 16 19 .08
June 12 19 .38July 17 20 .24Aug . 10 20 .82Sept . 13 21 .30Oct . 11 21 .00Nov. 7 20 .87Dec .
4 20 .83Jan .
9, 1968 20 .87Feb .
6 20 .65Mar . 12 20 .27
Apr . 10 19 .80May 15 19 .7 0June 11 20 .08July 3 20 .4 8Aug .
6 21 .2 2Sept. 5 20 .6 7Oct .
2 20 .2 9Nov .
5 20 .02
31, 1966 20 .1 322 20 .3 2
20 .2 420 .0520 .2 420 .1 720 .0 119 .9 0
1416
155-90-12ddd
Aug . 24, 1966 24 .1 0Sept . 22 24 .3 0Oct . 14 24 .3 4Nov. 16 24 .26Dec . 14 24 .1 9Jan . 23, 1967 24 .1 3Feb . 20 24 .05Mar. 16 24 .1 0Ap r . 20 23 .90May 16 24 .06
June 12 24 .13July 17 24 .30Aug. 10 24 .4 5Sept . 13 24 .44Oct . 11 24 .50Nov .
9 24 .50Dec .
4 24 .33Jan .
9, 1968 24 .6oFeb . 6 24 .42Mar . 12 24 .38
Ap r. 10 24 .2 8May 15 24 .2 5June 11 24 .2 5July 3 24 .3 9Aug. 6 24 .5 2Sept. 5 24 .4 1Oct .
2 24 .3 4Nov .
5 24 .3 3
155-93-13aaa
Jun e 29, 1967 121 .26July 17 125 .1 2Aug .
9 16 .6 5Sept . 14 128 .4 2Oct . 1( qi8 .( 5Nov .
9 129 .06
Dec .
4 129 .48Jan. 10, 1968 129 .92Feb . 6 129 .37Mar . 13 129 .40Apr . 10 129 .41May 15 129 .88
June 11 129 .3 6July 3 130 .1 1Aug .
5 130 .1 0Sept. 4 129 .4 8Oct .
2 129 .6 3Nov. 5 130 .17
156-89-6aab
Aug. 10, 1967 1 .5 4Sept . 13 1 .4 7Oct . 11 1 .5 0Nov .
9 1 .5 4Dec .
4 1 .52
Jan .-Apr ., 1968 Froze nMay 15 1 .45June 11 1 .45July 3 1 .61Aug . 6 1 .70
Sept. 5 1 .5 9Oct .
2 1 .6 0Nov .
5 1 .6 7
73
Depth to water, in feet below land surfac e
156-90-4ab b
Date
Wate rlevel
Date
Waterlevel
Date
Waterleve l
June 20, 1967 37 .14July 17 37 ."1Aug. 10 37 .42Sept . 13 37 .60Oct. 11 37 .7 4Nov .
9 37 .79
Dec .
5 37 .82Jan . 10, 1968 37 .88Feb .
6 38 .0 4
Mar. 12 38 .0 0Apr . 10 37 .8 0May 15 37 .84
June 11 37 .8 1
July 8 37 .7 8Aug .
6 37 .90Sept. 5 37 .98Oct .
2 37 .99Nov .
5 38 .02
156-91-2cc c
June 20, 1967 35 .26July 17 35 .4 1Aug. 10 35 .52Sept . 13 35 .5 9Oct . 10 35 .5 9Nov .
9 35 .46
D ec .
5 35 .47Mar . 12, 1968 35 .48Apr . 10 35 .43May 15 35 .41June 11 35 .36July 3 35 .52
Aug .
1 35 .56Sept. 4 35 .58Oct .
2 35 .33Nov .
5 35 .41
156-91-5da a
June 15, 1907 21 .8 3June 18 21 .7 9July 17 21 .9 6A ug. 10 22 .0 6Sept . 13 22 .03Oct. 10 22 .08Nov .
9 22 .04
Dec .
5 21 .99Jan . 10, 1968 21 .91Feb .
7 21 .94Mar . 12 21 .96
Apr . 10 21 .85May
15 21 .89June 12 21 .93
July 3 22 .0 0
Aug .
1 22 .1 0Sept . 4 21 .93Oct .
2 21 .8 8Nov .
5 21 .96
156-91-10bbb
Aug . 10, 1966 56 .72Sept . 22 56 .64Oct. 14 56 .78
Nov. 16 56 .50Dec . 15 56 .66Jan . 23, 1967 56 .73Feb . 20 56 .6 5Mar . 17 56 .94Apr . 20 56 .39May 19 56 .78
J,m° 12 56 .52July 17 56 .59Aug . 10 56 .89S ept . 13 56 .53Oct . 10 56 .92Nov .
9 56 .79Dec .
5 56 .77Jan . 10, 1968 56 .70Feb .
6 57 .3 5Mar. 12 56 .97
Apr. 10 56 .89May 15 56 .90June 12 57 .00July 3 57 .11Aug .
1 57 .02Sept. 4 57 .03Oct .
2 57 .07Nov .
3 57 .14
156-94-16db a
Aug . 10, 1966 16 .2 2Aug. 12 15 .77S ept . 21 15 .9 3Oct . 12 15 .78
Nov . 15 15 .66Dec . 15 15 .6 8Jan . 24, 1967 15 .7 5Feb . 21 15 .77Mar . 16 15 .87Apr . 27 14 .54
May 17 14 .80June 13 15 .2 3July 17 15 .76Aug. 10 16 .12Sept . 15 16 .40Oct. 10 16 .3 1Nov .
9 16 .1 5Dec .
5 16 .0 8Jan . 10, 1968 16 .16Feb .
6 17 .09
Mar . 13 15 .44
Apr. 10 15 .60May
13 15 .88
June 11 16 .04July 1 16 .17Aug .
5 16 .50Sept. 4 16 .41Oct .
2 16 .15Nov .
5 15 .90
74
Depth to water, in feet below land surfac e
157-89-20adc
Date
Water
Date
Water
Date
Wate rlevel
level
leve l
Aug . 22, 1966 14 .12
May 16 14 .01
Mar . 12 14 .28
Sept . 22 14 .19
June 12 14 .07
Apr . 10 14 .18
Oct . 14 14 .20
July 17 14 .23
May 15 14 .14
Nov . 16 14 .13
Aug . 10 14 .36
June 11 14 .13Dec . 15 14 .12
Sept . 13 14 .29
July 3 14 .34
Jan . 23, 1967 14 .05
Oct . 11 14 .30
Aug .
6 14 .36
Feb . 20 13 .93
Nov .
9 14 .33
Sept . 5 15 .06
Mar . 16 14 .05
Dec .
5 14 .27
Oct .
2 15 .03Apr . 20 13 .89
Feb .
6, 1968 14 .28
Nov .
5 14 .98
157-90-15bb b
10, 1966 5 .82
June 12 25 .90
Apr . 10 27 .6 6,pt .
:r .. .21
July 17 26 .31
Jey
15 27 .4 4
'et . 14 76 .33
Aug . 10 26 .68
June 12 27 .2 5Nov . 16 26 .41
Sept . 13 27 .10
July 3 27 .3 7
15 26 .54
Oct . 11 27 .37
Aug .
5 27 .7 2
Jan . 23, 1967 '6 .70
Nov .
9 27448
Sept . 5 27 .7 4
F•b . 20 2( .78
Dec .
5 27 .56
Oct .
2 27 .6 5`.!ar . 16 ( .'30
Jan . 1,, ,, 1968 27 .73
Nov .
5 27 .6 1
Apr . ?0 ?E .
Feb .
3 27 .87277
16 4. .05
Mar . 12 27 .76
157-91-362d d
Aug . 10, 1960 42 .42
June 12 42,22
Apr .
Sept . 22 42 .38
July 17 42 .87
nayOct . 14 42 .40
Aug . 10 43 .07
JunoNov . 16 42 .31
Sept . 13 43 .03
JulyDec . 15 42 .34
Oct . 10 43 .03
Aug .Jan . 23, 1967 42 .22
Nov .
9 42 .98
Sept .
Feb . 20 42 .09
Dec .
5 42 .99
Oct .Mar . 17 42 .16
Jan . 10, 19(8 42 .89
n? ;v .Apr . 20 42 .03
Feb .
6 42 .9 9May 19 42 .16
Mar . 12 42 .9 8
157-92-16ddd 1
July 21, 1966 9 .26
June 13 8 .60
Mar . 13 11 .4 3
Sept . 21 9 .04
July 17 9 .31
Apr . 10 11 .1 4
Oct . 12 9 .17
Aug . 10 10 .23
May 15 10 .84
Nov . 15 9,33
Sept . 14 11 .88
June 11 10 .84
Dec . 14 9 .49
Oct . 13 11 .14
July
3 10 .94
J an . 24, 1967 9 . 6 9
Nov .
9 11 .14
Aug .
5 11 .56
Mar . 16 9 .86
Dec .
4 11 .23
Sept . 4 11 .4 9Apr . 18 8 .77
Jan . 10, 1968 11 .47
Oct .
2 11 .5 9May 17 8 .37
Feb .
6 11 .62
Nov .
5 11 .( 3
75
Depth to water, in feet below land surfac e
158-90-17bba
Date Water
Dat eWater
Date Waterlevellevel
leve l
Sept . 13, 1967 28 .66
Feb . 7 28 .89
July 3 29 .05Oct . 17 28 .91
Mar . 12 28 .92
Aug .
6 29 .05Nov .
9 . ., : 28 .85
Apr . 11 28 .83
Sept . 5 29 .02Dec .
5 28 .75
May 14 28 .77
Oct .
2 28 .94Jan . 10, 1968 28 .74
June 12 28 .92
Nov .
5 29 .02
158-94-16bbb
Sept . 21, 1966 23 .49
June 12 23 .33
Apr . 11 23 .21Oct . 12 23 .23
July 17 23 .29
May 14 23 .22Nov . 15 23 .28
Aug . 10 23 .51
June 13 23 .30Dec . 15 23 .40
Sept . 14 23 .33
July 10 23 .37Jan . 24, 1967 23 .42
Oct . 17 23 .51
Aug .
1 -23 .4 6Mar . 14 23 .53
Nov .
9 23 .31
Sept . 5 23 .3 5Apr . 18 23 .52
Dec .
5 23 .19
Oct .
3 23 .4 3May 17 23 .29
Mar . 12, 1968 23 .47
Nov . 6 23 .2 5
76
BURKE COUNTY
Depth to water, in feet below land surfac e
159-90-4bc c
Date
Water
Date
Water
Date
Waterlevel
level
leve l
S ept . 21, 1966 82 .04
Aug . 22 81 .72
May 14 81 .3 8Oct . 13 81 .97
Sept . 13 81 .54
June 12 81 .87Nov . 16 81 .74
Oct . 12 81 .34
July 3 81 .95Dec . 16 81 .56
Nov .
7 81 .73
Aug .
6 81 .91Apr . 17, 1967 82 .01
Dec .
5 81 .53
Sept . 5 81 .83May 17 81 .58
Feb .
7, 1968 81 .8o
Oct .
2 81 .98June 13 81 .68
Mar . 12 81 .84
Nov .
6 82 .1 3July 18 81 .69
Apr . 10 81 .3 8
159-93-34baa
Aug . 10, 1967 13 .30
Feb .
7 13 .22
Aug .
1 13 .3 0S ept . 14 13 .69
Mar . 12 12 .76
Sept . 5 12 .8 6
Oct . 12 13 .27
Apr . 11 12 .27
Oct .
3 12 .7 8Nov .
7 13 .22
May 14 13 .42
Nov .
5 12 .7 5Dec .
5 13 .10
June 13 12 .40Jan . 10, 1968 13 .16
July 10 12 .88
159-93-36aaa
Aug . 15, 1966 51 .10
MayS ept . 1 51 .29
Jun eS ept . 21 51 .36
Jul yOct . 12 51 .20
Aug .Nov . 15 51 .24
Sept .Dec . 15 51 .45
Oct .Jan . 24, 1967 51 .44
Nov .Feb . 21 51 .24
Dec .Mar . 14 51 .44
Jan .Apr . 18 51 .16
Feb .
17 51 .00
Mar . 12 51 .52
13 51 .21
Apr . 11 51 .1718 51 .29
May 14 52 .3710 51 .47
June 13 51 .3014 51 .45
July 10 51 .4 012 51 .31
Aug .
1 51 .5 27 51 .48
Sept . 5 51 .4 9
5 51 .38
Oct .
3 51 .6 210, 1968 51 .34
Nov .
5 51 .5 07 51 .49
159-94-23dd c
July 21, 1966 11 .92
May 17 10 .40
Mar . 12 13 .13Aug . 12 11 .55
June 13 11 .53
Apr . 11 12 .28
S ept . 21 12 .95
July 18 12 .98
May 14 12 .10
Oct . 12 13 .07
Aug . 10 13 .67
June 13 12 .29N ov . 15 13 .16
Sept . 14 14 .23
July 10 13 .20
Dec . 15 13 .56
Oct . 17 14 .14
Aug .
1 13 .80J an . 24, 1967 13 .83
Nov .
7 14 .08
Sept . 5 13 .00
Feb . 21 13 .84
Dec .
5 14 .18
Oct .
3 13 .0 5
Mar. 14 13 .96
Jan . 10, 1968 14 .56
Nov .
6 13.10
Apr. 18 10 .84
Feb . 7 14 .69
77
Depth to water, in feet below land surfac e
160-91-13acd l
Date
Water
Date
Water
Date
Wate rlevel
level
leve l
July 21, 1966 21 .01
May 17 21 .90
Mar . 12 22 .75Aug . 18 21 .11
June 13 •• 21 .96
Apr . 11 22 .6 2Aug . 19 21 .13
July 18 22 .06
May 14 22 .6 0Sept . 21 21 .34
Aug . 23 22 .18
June 12 22 .7 5Oct . 13 21 .38
Sept . 13 • 22 .17
July 10 22 .9 1Nov . 16 21 .46
Oct . 12 22 .25
Aug .
6 22 .97Dec . 16 21 .50
Now .
7 22 .39
Sept . 5 22 .86Jan . 25, 1967 21 .65
Dec .
5 22 .38
Oct .
2 22 .7 3Mar . 13 22 .76
Jan . 10, 1968 22 .41
Nov .
6 22 .64Apr . 17 21 .97
Feb .
7 22.61
160-91-13acd 2
July 21, 1966 23 .84
May 17 24 .63
Mar . 12 25 .52Aug . 18 24,03
June 13 24 .66
Apr . 11 25 .3 9Aug . 19 24 .42
July 18 24 .66
May 14 25 .38Sept . 21 24 .16
Aug . 23 24 .90
June 12 25 .58Oct . 13 24 .19
Sept . 13 24 .85
July 10 25 .59Nov . 16 24 .25
Oct . 12 25 .01
Aug .
6 25 .7 1Dec . 16 24 .29
Nov .
7 25 .17
Sept . 5 25 .6 1Jan . 25, 1967 24 .53
Dec .
5 25 .15
Oct .
2 25 .4 3Mar . 13 24 .60
Jan . 10, 1968 25 .18
Nov .
6 25 .4 2Apr . 17 24 .79
Feb .
7 25 .38
160-94-7ddd
Sept . 1, 1966 49 .30
June 13 48 .22
Mar . 12 48 .95Sept . 21 48 .27
July 18 48 .16
Apr . 11 48 .5 0O ct . 12 48 .09
Aug . 10 48 .58
May 14 48 .56Nov . 15 48 .14
Sept . 14 48 .73
June 13 48 .4 9Dec . 15 48 .44
oct . 17 49.03
July 10 48 .5 2Jan . 24, 1967 48 .55
Nov .
7 48 .72
Aug .
1 48 .7 5Mar . 14 48 .79
Dec .
5 48 .62
Sept . 5 48 .7 5Apr . 18 48 .55
Jan . 10, 1968 48 .53
Oct .
3 49 .0 4May 17 48 .13
Feb . 7 48 .59
Nov .
6 49 .0 0
161-89-28ddd
Aug . 13, 1965 9 .89
Nov . 16 14 .29
Dec .
6 17 .3 0Oct . 28 12 .15
Dec . 16 14 .73
Feb .
8, 1968 18 .09Dec .
7 12 .57
Jan . 25, 1967 15 .43
Mar . 11 17 .90Jan . 18, 1966 12 .88
Mar . 13 15 .80
Apr .
1 17 .48Mar . 17 12 .79
Apr . 18 12 .78
May 14 17 .17Apr . 14 10 .18
May 17 11 .70
June 12 17 .46May 11 8 .65
June 13 11 .96
July 10 17 .66June 15 8 .33
July 18 13 .33
Aug .
2 17 .77July 21 9 .91
Aug . 11 14 .60
Sept . 6 17 .2 8Aug . 17 11 .27
Sept . 13 15 .70
Oct .
3 17 .4 4Sept . 20 12 .80
Oct . 12 16 .42
Nov .
6 17 .3 3Oct . 13 13 .60
Nov .
7 16 .93
78
Depth to water, in feet below land surfac e
161-92-12dcdl
Date
Waterlevel
Date
Water
Date
Wate rlevel
leve l
Aug . 13, 1965 8 .7 2Oct . 28 10 .0 8Dec .
7 10 .8 5Jan . 18, 1966 12 .00Feb . 18 14 .37Mar . 17 15 .22Apr . 14 15 .42May 12 13 .00June 16 19 .33July 21 7 .87Aug . 18 11 .97Sept . 19 11 .89
Oct . 13 9 .47
Nov .
6 15 .4 2Nov. 15 13 .24
Dec .
5 15 .1 1Dec . 15 15 .05
Feb .
7, 1968 18 .43Jan . 24, 1967 16 .13
Apr .
1 19 .43Mar . 14 19 .11
May 14 19 .96Apr . 17 1.3 .23
June 12 18 .31May 17 9 .93
July 10 16 .98June 13 9 .16
Aug .
1 19 .84July 18 8 .41
Sept . 6 21 .40Aug . 11 11 .54
Oct .
3 12 .2 6Sept . 14 11 .54
Nov .
6 13 .0 3Oct . 17 16 .16
161-92-35cc c
June 29, 1967 13 .17July 18 13 .59Aug . 23 14 .36Sept . 14 14 .7 0Oct . 12 15 .05Nov .
6 15 .25
Dec .
5 15 .39
June 12 14 .5 0Jan . 11, 1968 15 .60
July 10 14 .8 1Feb .
7 15 .80
Aug .
1 14 .91Mar . 11 14 .98
Sept . 6 14 .91Apr .
1 14 .37
Oct .
3 15 .0 6May 14 14 .48
Nov .
6 15 .2 0
162-88-25bbb
Aug . 10, 1965 66 .0 9o ct . 28 66 .1 3Dee .
7 66 .16Jan . 18, 1966 66 .2 3Feb . 17 66 .27Mar . 17 66 .2 9Apr . 14 66 .3 1May 11 66 .3 3June 15• 66 .3 3July 21 66 .2 9Aug . 17 66 .3 oSept . 19 66 .27
Oct . 13 66 .30
Nov . 13 66 .6 6Nov . 16 66 .37
Dec .
6 66 .6 8Dec . 16 66 .40
Feb .
8, 1968 66 .6 9Jan . 25, 1967 66 .47
Mar . 11 66 .7 1Mar . 13 66 .50
Apr .
1 66 .7 5Apr . 17 66 .45
May
14 66 .78May 17 66 .46
June 12 66 .78June 13 ••• 66 .50
July 10 66 .80July 18 66 .47
Aug .
2 66 .7 4A ug . 22 66 .50
Sept . 6 66 .56Sept . 13 66 .58
Oct .
3 66 .52Oct .
9 66 .63
Nov .
6 66 .52
162-89-3bbb
Aug . 19, 1966 87 .70S ept . 1 87 .37Sept . 19 87 .48Oct . 13 87 .47Nov . 16 87 .53Dec . 16 87 .51Jan . 25, 1967• 87 .47Mar . 13 87 .43Apr . 17•• 87 .4 7May 18 87 .34
June 13 87 .43
Apr .
1 87 .63July 18 87 .59
May 14 87 .34Aug . 11 87 .68
June 12 87 .3 7Sept . 14 87 .70
July 10 87 .5 7Oct . 12 87 .61
Aug .
2 87 .6 5Nov .
7 87 .68
Sept . 6 87 .4 8Dec .
6 87 .68
Oct .
3 87 .5 0Jan . 11, 1968 87 .62
Nov .
6 87 .5 1Feb .
8 87 .61Mar . 11 87 .66
79
Depth to water, in feet below land surfac e
162-89-5dad
Date
Waterlevel
Date
Waterlevel
Date
Waterleve l
Aug .
9, 1965 71 .42Oct. 28 71 .36Nov. 18 71 .6 4
Jan . 18, 1966 72 .0 1
Feb. 17 72 .1 8Mar . 17 72 .26
Apr. 14 72 .3 3May 12 72 .4 4June 16 72 .04July 21 71 .86
Aug . 18 71 .87Sept 19 71 .87
Oct . 13 72 .01
Nov. 16 72 .2 3
Dec . 16 72 .3 5Jan . 25, 1967 . . Discontinue d
162-90-5cc c
Aug . 11, 1965 6 .88
O ct . 28 8 .5 0Dec .
7 8 .9 1Jan . 18, 1966 9 .5 1Feb. 17 9 .9 9Mar . 17 10 .4 4Apr . 14 10 .7 1May 12 10 .1 9June 16 8 .22July 21 7 .82Aug . 16 7 .90Sept . 19 7 .95
Oct . 13 8 .03Nov . 16 8 .3 9Dec . 15 8 .6 9Jan . 24, 1967 9 .3 7Mar . 14 10 .52Ap r . 17 9 .63
May 18 7 .07June 13 7 .26July 18 7 .95Aug . 11 8 .76S ept . 14 9 .2 1Oct. 12 9 .57
Nov .
6 10 .1 4
Dec .
5 10 .29Feb .
7, 1968 11 .45Mar. 11 11 .06Ap r .
1 11 .84May 14 11 .2 7June 12 10 .98July 10 10 .62Aug .
1 10 .4 3Sept. 6 9 .93oct .
3 9 .38Nov .
6 9 .23
162-91-24aaa
Aug . 11, 1967 8 .4 oSept . 14 9 .05O ct . 12 10 .06
Nov .
6 10 .1 6Dec .
5 9 .14Jan . 11, 1968 9 .42
Feb .
7 9 .4 2Mar . 11 8 .94
Ap r .
1 8 .7 1May 14 6 .86
June 12 6 .76
July 10 7 .63
Aug .
1 8 .32Sept. 6 7 .90Oct .
3 8 .00Nov .
6 8 .12
162-92-2cbb
Aug . 18, 1966 27 .48S ept . 19 27 .3 9Oct. 13 27 .37Nov. 15 27 .37Dec. 15 Ice plugJan . 24, 1967 27 .4 5Mar. 14 27 .5 9Apr. 18 27 .5 2May 18 27 .46
June 13 27 .4oJuly 18 27 .4 3Aug . 11 27 .7 3Sept . 14 27 .7 9Oct . 17 27 .8 8Nov .
7 27 .8 4
Dec .
5 ..
. 27 .8 4Jan . 11, 1968 27 .92Feb .
7 27 .97
Mar. 11 28 .0 5Apr .
1 28 .07May 14 28 .0 0June 12 28 .05July 10 28 .1 1Aug .
1 28 .1 1Sept . 6 28 .2 3Oct .
3 28 .2 1Nov .
6 28 .2 2
162-92-2cdd2
June 28, 1967 27 .42July 18 27 .48
Aug . 11 27 .58S ept . 14 27 .66O ct . 17 27 .71Nov .
7 27 .74
Dec .
5 27 .7 0Jan . 11, 1968 27 .7 6
Feb .
7 27 .7 1Mar . 11 27 .90Ap r .
1 28 .1 9May 14 27 .82
June 12 27 .88July 10 27 .90Aug .
1 27 .93Sept. 6 28 .01Oct .
3 28 .04Nov .
6 28 .05
80
Depth to water, in feet below land surfac e
162-92-24ccc l
Date
Water
Date
Water
Date
Wate rlevel
level
leve l
Aug . 13, 1965Oct . 28Dec .
7Jan . 18, 1966Feb . 18Mar . 17Apr . 14May 12June 16July 21Aug . 18Sept . 19
8 .68
oct . 13 9 .43
Nov .
6 9 .36
8 .71
Nov. 15 9 .16
Dec .
5 9 .6 0
8 .65
Dec . 15 9 .22
Feb .
7, 1968 9 .2 0
8 .73
Jan . 24, 1967 9 .32
Ma
11 8 .96
9 .17
Mar . 14 9 .36
A r . 11 8 .7 3
8 .28
Apr . 18 8 .85
ay 14 8 .4 9
7 .68
May 18 8 .27
June 12 8 .6 0
7 .47
June 13 7 .98
July 10 9 .3 2
7 .75
July 18 9 .79
Aug .
1 9 .08
8 .23
Aug . 11 9 .02
Sept . 6 9 .3 0
8 .58
Sept . 14 9.37
Oct .
3 9 .98
9 .21
Oct . 17 9 .39
Nov .
6 10 .1 2
162-93-7ddd
Aug . 12, 1965Oct . 28Dec . 7Jan . 18, 1966Feb . 18Mar . 17Apr . 14May 12June 15July 21Aug . 18Sept . 19Oct . 13 •
6 .89
Nov . 15 8 .71
Jan . 10, 1968 9 .5 9
6 .57
Dec . 15 9 .08
Feb .
7 9 .87
7 .22
Jan . 24, 1967 9 .45
Mar . 12 10 .06
8 .05
Mar . 14 10 .09
Apr . 11 8 .8 9
9 .09
Apr . 17 8 .37
May 14 7 .6 6
9 .38
May 18 5 .74
June 13 7 .4 0
8 .00
June 13 6 .09
July 10 7 .9 0
6 .11
July 18 7 .11
Aug .
1 8 .4 3
6 .15
Aug . 10 8 .00
Sept . 5 7 .1 8
6 .64
Sept . 14 9 .10
Oct .
3 7 .3 9
7 .41
Oct . 17 9 .39
Nov .
6 7 .5 9
7 .87
Nov .
7 9 .38
8 .46
Dec .
6 9 .5 <
163-91-4ddd l
Aug . 11, 1965••• 14 .8 5Oct . 28 14 .93Dec .
7 15 .7 8Jan. 18, 1966 . . . . 16 .7 5Mar . 17 16 .2 4Ap r . 14 16 .5 1May 12 16 .2 3June 16 16 .47July 21 16.87S ept . 19 16 .76Oct . 13 16 .68
Nov . 16 16 .65
Feb .
8, 1968 18 .7 3Dec . 15 17 .15
Mar . 11 19 .24Apr . 18, 1967 18 .73
Apr .
1 18.08May 18 17 .74
May 14 19.3 3June 13 20 .52
June 12 19.2 9July 18 18 .60
July 10 19.0 2Aug . 23 19 .26
Aug . 2 18 .3 9Sept . 14 18 .55
Sept . 6 19 .91Oct . 12 20 .17
Oct .
3 18 .90Nov .
7 20 .26
Nov . 6 17 .76Dec .
6 19 .02
81
Depth to water, in feet below land surfac e
163-92-9cc a
Date
Water
Date
Waterlevel
levelDate Wate r
leve l
14 .' '14 .5 614 .7615 .1 815 .4 015 .4 515 .9 115 .9 215 .5 915 .3 115 .0 914 .9 114 .7 1
Aug . 11, 195Oct . 28
Jan . 18, 196F . b . 17Mar . 17Apr . 14May 12June 16July 21Aug . 166_.p t . 19Oct . 13
Nov . 15 14 .90
Jan . 11, 1968 14 .7 7Dec . 15 15 .11
Feb .
8 17 .0 2Jan . 24, 1967 15 .45
Mar . 11 16 .36Max . 14 16 .02
Apr .
1 16 .36Apr . 17 16 .05
May 14 16 .1 8May 18 15 .43
June 12 16 .34June 13 14 .78
July 10 16 .30July 18 14 .57
Aug .
2 16 .26Aug . 11 14 .72
Sept . 6 16 .09Sept . 14 14 .57
Oct .
3 15 .89Oct . 17 14 .99
Nov .
6 15 .78Nov .
8 15 .02Dec .
6 15 .1 4
163-92-24daa
Aug . 11, 1965 9 .32
Jan . 24, 1967 10 .53
Feb .
8 12 .38Oct . 28 9 .45
Mar . 14 10 .77
Mar . 11 11 .96Mar . 17, 1966 9 .73
Apr . 18 8 .51
Apr .
1 10 .49Apr . 14 8 .48
May 18 7 .33
May 14 9 .30May 12 7 .71
June 13 8 .04
June 12 9 .82June 16 7 .80
July 18 10 .04
July 10 10 .45July 21 6 .89
Aug . 11 11 .24
Aug .
2 11 .21A ug . 16 8 .53
Sept . 14 12 .25
Sept . 6 11 .79Sept . 19 9 .87
Oct . 17 12 .15
Oct .
3 11 .94Oct . 13 9 .95
Nov .
7 12 .03
Nov .
6 11 .7 9Nov . 15 10 .05
Dec .
6 12 .1 3Dec . 15 10 .29
Jan . 11, 1968 12 .1 8
163-92-35dd d
Oct . 28, 1965 12 .60
Nov . 15 13 .98
Dec .lee .
7 12 .85
Dec . 15 14 .15
Jan .Jan . 18, 1966 12 .85
Jan . 24, 1967 14 .48
Feb .Feb . 17 13 .60
Mar . 14 15 .19
Mar .Mar . 17 13 .62
Apr . 18 13 .18
Apr .Apr . 14 12 .27
May 18 11 .05
MayMay 12 10 .95
June 13 11 .25
Jun eJune 16 10 .80
July 18 13 .00
JulyJuly 21 11 .23
Aug . 11 14 .10
Aug .Aug . 16 12 .42
Sept . 14 14 .92
Sept .Sept . 19 13 .67
Oct . 17 15 .27
Oct .Oct . 13 14 .13
Nov .
7 15 .09
Nov .
5 15 .1 511, 1968 15 .4 5
7 15 .6 311 15 .89
1 14 .8114 13 .4 212 13 .3 110 14 .08
1 14 .986 15 .1 33 15 .5 86 15 .3 8
82
Depth to water, in feet below land surfac e
163-93-8ccb
Date Wate rleve l
Date
Wate rlevel
Date
Waterlevel
Aug . 12, 1965 15 .00Oct . 28 15 .92Dec .
7 16 .26Jan . 18, 1956 16 .30Feb . 17 16 .75Mar . 17 17 .09Apr . 14 17 .10May 12 15 .78June 15 15 .01July 21 15 .40Aug . 16 15 .7 5Sept . 19 16 .21Oct . 13 16 .52
Nov . 15 16 .69Dec . 15 17 .04Jan . 24, 1967 17 .37Mar . 14 18 .00Ap r . 17 16 .76May 18 13 .67June 13 13 .7 0July 18 14 .5 2Aug . 11 15 .3 4Sept . 14 16 .04Oct . 17 16 .7 0Nov .
8 16 .6 4Dec .
5 16 .80
Jan . 10, 1968 16 .8 2Feb .
7 17 .5 0Mar . 11 18 .02Apr .
1 17 .64May 14 16 .00June 12 15 .7 0July 10 15 .7 2Aug .
2 16 .12S ept . 5 16 .68Oct .
3 16 .85Nov .
6 16 .79
163-93-17ddd
June 29, 1967 15 .6 9July 18 15 .7 3Aug . 11 15 .7 5S ept . 14 15 .7 7Oct . 17 16 .13Nov . 14 16 .22
16 .2216 .22
Feb .
8 16 .86Mar . 11 17 .2 3Ap r .
1 17 .2 4May 14 17 .05
June 12 17 .2 3July 10 17 .0 9Aug .
6 17 .1 3Sept . 5 17 .0 5Oct .
3 17 .0 0Nov .
6 16 .7 6
Dec .
6 ..
. .Jan . 10,
163-93-20aaa
Apr . 11, 1568 49 .2 9Apr . 15 49 .36Apr . 20 49 .3 8Apr . 25 49 .4 2Apr . 30 49 .4 2May
5 49 .4 2May 10 49 .3 0May 15 49 .2 6May 20 49 .3 3May 25 49 .35May 31 49 .30June 5 49 .30June 10 49.30June 15 49.32June 20 49.27June 25 49 .39
June 30 49 .3 2July 5 49 .36July 10 49 .33July 15 49 .33July 20 49.28July 25 49 .36July 31 49.35Aug .
5 49.33Aug . 10 49.50Aug . 15 49.74Aug . 20 50.07Aug . 25 52 .70Aug . 31 51 .27Sept . 5 50 .60S ept . 10 50 .2 5Sept . 15 49 .95
Sept . 20 49 .8 9Sept . 25 49 .7 4Sept . 30 49 .66Oct .
5 49 .5 8Oct . 10 49 .5 2Oct . 15 49 .5 1Oct . 20 49 .4 9Oct . 25 49 .4 4Oct . 31 49 .4 1Nov .
5 49 .5 1Nov . 10 49 .4 8Nov . 15 49 .3 7Nov . 20 49 .3 4Nov . 25 49 .4 1Nov . 30 49 .3 2Dec .
5 49 .4 1
163-93-32bdd
May 18, 1967 116 .6 2June 13 116 .3 8June 27 119 .3 4June 29 123 .1 0July 5 118 .4 6July 6 123 .09July 18 136 .08Aug . 11 140 .44
Sept . 14 126 .1 2Oct . 17 127 .6 8Nov . 14 127 .64Dec .
6 119 .57Jam . 11, 1968 128 .00Feb .
8 121 .32Mar . 12 123 .63Apr .
2 105 .87
May 14 99 .80June 12 101 .37July 10 133 .40Aug . 21 100 .56S ept . 5 102 .57O ct .
3 104 .7 0Nov .
6 113 .03
83
Depth to water, in feet below land surfac e
163-94-15bab
Date Wate rleve l
Date
Wate rlevel
Date
Waterlevel
Oct . 28, 1965 17 .66
Dec . 15 17 .9 0Dec .
7 17 .62
Jan . 24, 1967 17 .95Jan . 18, 1966 17 .70
Mar . 14 18 .1 4Mar . 17 17 .68
Apr . 18 17 .7 5Apr . 14 17 .50
May 18 17 .43May 12 17 .31
June 13 17 .3 5June 15 17 .47
July 18 17 .50July 21 17 .70
Aug . 10 17 .74Aug . 16 17 .80
Sept . 14 18 .00S ept . 19 18 .05
Oct . 17 17 .9 9Oct . 13 18 .05
Nov .
7 17 .86Nov . 15 17 .85
Dec .
6 17 .92
163-94-31dcc 2
A ug . 12, 1965• 9 .82
Oct . 13 10 .10
Nov .
8 10 .43Oct . 28 9 .63
Nov . 15 10 .13
Dec .
6 10 .7 4Dec .
7 10 .10
Dec . 15 10 .19
Feb .
7 . 1^68 10 .3 9Jan . 18, 1966 9 .74
Jan . 24, 1967 10 .19
Mar . 12 10 .3 9Feb . 18 9 .8
Mar . 14 10 .18
Apr .
1 10 .3 3Mar . 17 9 .67
Apr . 18 9 .90
May 14 10 .08Apr . 14 9 .55
May 18 9 .55
June 12 10 .08May 12 9 .40
June 13 9 .50
July 10 10 .2 7June 15 9 .43
July 18 9 .81
Aug .
1 10 .5 7July 21 9 .77
Aug . 10 10 .14
Sept . 5 10 .4 0Aug . 16 9 .89
Sept . 14 10 .35
Oct .
3 10 .3 3Sept . 19 10 .03
Oct . 17 10 .64
Nov .
6 10 .2 9
164-90-35ab a
Sept . 2, 1966 7 .43
July 18 8 .41
Apr .
1 8 .87S ept . 19 9 .18
Aug . 23 8 .58
May 14 8 .89Oct . 13 8 .43
Sept . 14 8 .63
June 12 9 .04Nov . 16 8 .16
oct . 12 8 .61
July 10 8 .18Dec . 16 7 .96
Nov . 7 8 .65
Aug .
2 9 .28Jan. 25, 1967 7 .78
Dec .
6 8 .62
Sept . 6 9 .17Apr . 17 8 .11
Jan . 11, 1968 8 .47
oct .
3 9 .15May 18 8 .12
Feb . 8 8 .53
Nov . 6 9 .04June 13 8 .16
Mar . 11 8 .7 8
84
Jan . 10, 1968 17 .87Feb .
7 18 .08Mar . 12 18 .1 5Apr .
1 18 .23May 14 18 .17June 12 18 .14July 10 18 .2 1Aug .
1 18 .3 7S ept . 5 18 .4 7oct .
3 18 .6 1Nov .
6 18 .48
TABLE 4 .-Dogs of test holes and wells
MOUNTRAIL COUNIT
150-92-2ab a(Log from Dingman and Gordon, 1954 )
Geologicsource
Altitude :
1,933 fee t
Material Thickness De th(feet) feet )
Topsoil 2 2Sand and gravel 3 5Clay, with pebbles 25 30clay , gray 4o 70sand 34 l0 4Clay, gray and brown 6 noLignite 5 11 5Sand and clay 5 120sand 5 12 5Lignite 5 130sand 3 13 3clay , gray 4 13 7Lignite 3 14 oclay, gray 9 14 9sand 36 18 5Lignite 5 190Sand and clay, gray 10 20 0Clay, gray 33 23 3Lignite 2 23 5Clay, sandy, gray 20 25 5C lay, gray 6o 31 5Clay, sandy, gray 13 328Lignite 17 34 5Clay, gray-green 22 36 7Lignite 3 370Clay, sandy, gray-green 7 377
-------------------------------------------- - 3 38oClay, gray-green 8 388Lignite 2 39 0Clay, gray-green 3 39 3Lignite 2 395Clay, gray to brown 10 405
8 5
150-92-14ab d(Log from Dingman and Gordon . 11954 )
Altitude :
1,950 fee t
deelogi csource Material li:ickness Dept h
0ravel
(feet )
`i
(feet )
5Gravel and clay 10 1 5Clay, gray 40 5 5Lignite 2 5 7Cla y, gray 18 7 5Clay, silty, brown 25 10 0Silt, brown 15 11 5Clay, gray 30 14 5Lignite 5 1 5 0Cl ay, gray 30 18 0Sand 20 20 0Lignite 5 20 5Clay, silty and sandy, gray 28 23 3Lignite 2 '35Clay, gray 10 245Sand 10 255Lignite 8 263Clay, gray 4 267Lignite 3 270clay, gray 55 _ J
Lignite 15 340Clay, gray-green 5 345 --Sand 35 380Lignite 5 38 5C la y, gray 10 39 5Sand 10 40 5Lignite 5 410Cla y, gray 5 41 5Sand and tan sandy clay 5 420
C la y, gray and tan 15 43 5Lignite 15 4 5 0Sand 26 476Clay, gray 4 48 0Lignite 5 48 5
Clay, sandy, gray----° 7 49 2Lignite 8 50 0
150-93-ldda(Log from Dingman and Gordon, 1954 )
Altitude :
2,179 fee t
Topsoil 3 3Clay, silty and sandy, with gravel 7 10Clay, silty, gray-brown 5 1 5Sand 6o 75Lignite ' 5 8 0Clay, silty, dense, gray 55 135(No sample) 1 5 1 50Sand 62 212
Lignite--"' 3 21 5Clay, silty, gray 5 220Lignite 5 22 5Sand 5 2 30C lay, gray 10 240
Clay, gray, with lignite streaks 15 25 5Sand with lignite streaks 15 270Sand 4o 310Lignite 5 31 5
Clay, sandy, gray 15 330
86
150-93-2adc(Log from Dingman and Gordon, 1954 )
Geologi csource Material Thickness Depth
Topsoil
(feet )
5
(feet )
5Clay, brown with gravel 25 30Sand 10 40
Lignite ° 1 41
Sand 18 59Lignite 4 6 3Clay, gray 53 116
Lignite 4 120
C lay, gray 26 146
Lignite 8 15 4
Clay, gray 129 28 3
Lignite 7 290C lay, gray 25 31 5Clay, gray and brown, with thin lignite beds 15 330Clay, silty, gray 60 39 0
Sand 15 40 5
150-93-'cbb(Log from Dingman and Gordon, 1954 )
Topsoil 3 342 45Clay, yellow, with pebbles
Clay, gray 5 5oClay, sandy, yellow 16 66
Clay, carbonaceous, and lignite 2 68C lay, gray 9 77Lignite 3 8oClay, silty, gray and brown 90 170
Lignite 3 17 3C l ay, gray and brown 26 199Clay, brown, with small amount of lignite 5 20 4
Clay, sandy, dense, gray 26 230Sand 1 23 1
Clay, gray 89 320
Iignite 3 32 3Clay, gray 77 40 0sand 10 410Clay, gray 16 142 6
Limestone 14 430
sand 8 438
Limestone 1 1439
Lignite 11 450
Limestone 3 45 3Lignite 9 462clay, gray 33 495
8 7
(Log from
Gordon , Dingman and
1954 )
Geologi csource Material Thickness Depth
(feet) (feet )
Topsoil
---'--'-- 3 3' '---- 17 2 0
--------------- 13 3 3—'--''--' '--'
S~~~~y,
~~°lignit e~~_.
.~~~~~~~~~~~~~~~~~~~~~~~~~~
6 3 96135 13 5
----' ' m 14 5--' '—'--'—' 10 15 5--'—'----'--'--'—' 4o 195
_._—. .—.--.— .—._--.--.— . zv 205---'—' '—' 8 213
_"—~ . .---._. . 2 215—'---'—'—'—'--'—' 15 23 0-------------------------------------------- - 2 23 2
clay , = ay 3 23 5Lignite 3 23 8
31 26 9z 270
---------------------- -` la' gray— .—.---_ .—.----.— .— .---.--.
691
34 o30
3705
37530
Altitude : 2,118 fee t
Glacial drift :Sand, -- 1 1Sand, very clayey, white to yellowish-gray 3 4
Sand, medium, brown, well-sorted, subangular to27 8 9subrounded-------------------------------------- -
Sentinel Butte Formation :
12 10 1ohale, silty, various shades of yellow, light-green ,
and grayLignite, black 4 10 5
151-88 .12ab b
Altitude : 2,105 fee tGlacial drift :
Soil, pebbly, silty, black 1
1Till, yellowish-gray to moderate-olive-brown,
4o
41oxidizedTill, olive-gray 19
ooTill, dusky-yellow to moderate-olive-brown, oxidized
41
101Sentinel Butte Formation :
Shale, yellowish-green to medium-gray; a thi n
88
1
151-88-29bbb
Altitude : 2,115 fee t
Geologic source
Material Thickness
Depth(feet)
(feet )
Glacial drift :Soil, silty, black 1
1Till, yellowish-gray to dusky-yellow, oxidized 17
18Till, dusky-yellow to moderate-olive-brown ,
oxidized 19
37Sentinel Butte Formation :
Sand, fine, yellowish-green, lignitic 25
62Lignite, black, fissile 2
64Shale, silty, light-to medium-gray 16
80
151-89-ldaa(Log from D . Jahnke )
Black loam 3
3Yellow clay 63
66Darker sandy clay 6
72
Yellow sandy formation 2
74
Yellow soft sandstone with soft layers 9
83Yellow soft clay 2
8 5
151-89-19cc c(Log from D . Jahnke )
Missing 7
7Yellow clay 28
3 5Blue clay or shale 19
5 4Coal 1
5 5
Gray clay or shale 3
5 8
Coal 1
5 9Gray clay or shale 31
90
Rock 3 .5
93 . 5
Gray sandy clay 8 .5
102Soft lignite and water 3
105Gray clay 3
108
Coal 2
110
151-89-30bbb l(log from D . Jahnke )
Drift clay 5 2
52
Moist clay 5 3Lignite coal 1
5 4Sandy clay 5
5 9
Blue clay or shale 21
8 0
Gray clay or shale 18
98
Sandy clay 12
110
Lignite 3 .5
113 . 5
Blue clay or shale 3 .5
117
89
151-89-33ddc(Log from D . Jahnke )
Geologicsource Material Thickness Depth
Yellow clay with small stones and pebbles
(feet )
24
(feet )
24Boulder or rock 3 2 7Sandy yellow clay 27 54Lignite 3 5 7Blue clay or shale 7 .67 64 .6 7Lignite coal 2 .33 6 7Gray shale or clay 20 87Hard rock or limestone 3 .5 90 . 5Sandy formation .5 91Soft sandstone 30 .5 121 . 5Hard rock or limestone 3 124 . 5Soft clay-like formation 1 .5 12 6Soft sandstone or petrified sand 10 136
151-89-36dd d
Altitude : 2,076 feet
Glacial drift :Till, dusky-yellow, oxidized 2 2
Sentinel Butte Formation :
35 3 7
Sand, medium, yellowish-brown to reddish-brown ,well-sorted, subangular to subrounded, oxidized ;contains
ironstone chips and concretions Silt, dusky-yellow, limonitic, oxidized 3 40Sand, fine, clayey, yellowish-green 5 4 5Shale, yellowish-gray to medium-gray and greenish -
27 72graySand, fine, greenish-gray to bluish-gray, calcareous 16 88Silt, bluish-gray 11 99Shale, medium-gray 13 112Lignite, black 10 122Shale, medium-gray and brownish-black 18 14o
151-90-3baa
Glacial drift :Sand,
(Log from Schmid, 1962 )
gravelly to clayey, oxidized 6 6Till, light-olive-brown, oxidized 6 12Till, olive-gray 19 31Sand, very fine to coarse 5 36
Tongue River Formation :3 39Lignite
Clay, greenish-gray to light-bluish-gray 13 .5 52 . 5
90
151-90-26ddd
Altitude : 2,192 fee t
Geologi csource
Material Thickness Depth
Glacial drift :Till, dusky-yellow to moderate-olive-brown, oxidized
(feet )
8
(feet )
8Till, moderate-olive-brown, oxidized 12 20Boulder 2 22Till, moderate-olive-brown, oxidized 13 3 5
Sentinel Butte Formation :46 81Sand, silty and clayey, light-olive-gray, bedded
Shale, silty and sandy, interbedded, light-olive-grayto medium-gray 27 Io8
Sand, fine to medium, clayey, bluish-gray to dark-greenish-gray 18 12 6
Shale, bluisn-gray 4 130Sand, fine to medium, bluish-gray to dark-greenish -
gray 4 134Shale, bluish-gray 6 140
151-90-35baa(Log from D . Jahnke )
Black loam 2 2Yellow clay 14 16Yellow sand 20 3 6Rock or boulders 2 3 8Hard sandy formation or yellow sandstone 32 70Hard yellow sandy clay 28 98Darker clay with smell pieces of lignite 10 108Yellow sandstone or hard sandy clay, some water at
125 ft . 17 12 5Darker sand or blue sandy clay 8 13 3Blue sandy formation 12 14 5Rather hard rock, light colored 1 .5 146 . 5
151-90-36dda(Log from D . Jahnke )
Drift clay 29 .75
29 .75Boulders and smaller stones 2 .25 32Medium hard sandy formation 29 61Blue clay or shale 19 80Reddish coal .5 80 . 5Gray clay or shale 21 .5 102Gray sandy clay 6 108Harder sandstone 1 109Softer gray sandstone 8 117
91
151-92-3cc c
Altitude : 1,900 feet
Glacial drift :Soil, silty, loam, black Silt, sandy, yellowish-gray Till, yellowish-gray to dusky-yellow, oxidized
Till, dusky-yellow to moderate-olive-brown, oxidized
Till, moderate-olive-brown, oxidizedSand, coarse with fine gravel, moderately well-sorted ,
subangular to subrounded ; pebbles are mostlylimestone and dark shale
Clay, silty, olive-gray Clay, dark-olive-graySand, very fine, light-olive-gray, subrounded ,
1ignitic
Clay, silty, olive-gray Sand, very fine to medium with interbedded silt an d
sandy clay, generally light-olive-gray, but varie s
to blackTill, olive-gray
Tongue River Formation :Shale, silty, medium-graySand, very fine, clayey, dark-greenish-grayShale, silty, greenish-gray Lignite, leonardite, and black oily sandy clay
Shale, black
151-92-8bbb
Altitude : 1,925 feet
Glacial drift :Loam, silty, dark-brown Sand, coarse and fine to medium gravel, subangula r
(dry)Till, yellowish-gray, oxidized
Till, dusky-yellow, oxidizedTill, moderate-olive-brown, oxidized Clay, silty, light-olive-gray Claystone, gray, iron stained
Till, olive-brown to olive-graySand, medium to coarse with some fine gravel ,
lignitin
Till(?), olive-graySand, medium to coarse with some fine gravel ,
lignitic
Tongue River Formation :Shale, medium-grayShale, light-greenish-gray Sand, very fine to fine, well-sorted, subangular t o
subrounded, calcareous, contains some lignit e
grainsSand, very fine to fine, clayeySand, very fine to fine, well-sorted, subangular t o
subrounded, calcareous, contains lignite grainsLignite, brownish-blackShale, light-olive-gray
92
(feet )
1 1
3 46 10
22 32
20 52
19 7126 9712 109
5 114
9 12 3
35 158117 27 5
5 280
3 28 32 28 5
9 29 46 30 0
2 2
4 6
3 912 2 113 3 4
6 40
3 4 311 54
4 583 61
10 7 1
5 764 80
62 142
11 15 3
42 1955 200
20 220
Geologi csource
Material
Thickness )attifeet )
-E
52 I 14
2-A.
ww
nK
r.
S
14
R
wG1
C]
4~1
]- 1~-
rG
6ro
Gg
wy°
~1 ~
~"M
GK
~ro
G~
,~~
Por
..
aI+
R O
'nw
~a/~
e~
d R
~IC
~R
~ n
p 6
~E6 6
S.4,
r7
1
R A
1 1
`~kCii
tV
1
-R
1GS.r
°1,+
m g
r4&
oRv
ml
Sbym
o4
4W
V.
W
•'i H'•••444
®-
Ng
ppPp.~
pm
of
4°a'0°
i H
O.
k1D1
1R
p
:'
::
O
R f
iR
ymr
o0y
a
r ~ R
Sp
10a
l~4
Kr•
arwj
6
:
y'
i''
1 ~~+
1+
Y00
0o
~+
o
C
A.
14
' !C
4 as i
ll!b
o°i
WiO1
"~O
I
'ai
P.i
gaI
IEi•
..
!
I
G•
1
w
a i~
oo
oI
~ro
r
wad
..
R O
ro a
a
a o
m
gq5 $
.Vm
r
~~
aN
GN
~
go
$
11eoG
Ga
—A
r ! ¢ 16
q°
ga
n
1 ~
O
~
Ii1
PF
IU
~
4
m'
ie
PoG
R a
Q ~j
t6f
O yCn
rm~s
!i! a
f
le H
P P
O
Illµ+++O
es
1
1
•1
a.
l
a ''
1
iig
g.4
1 1
R
2i0°j
i0 d
0"b
ppwl
$a
o!
mH
.sp•
R
a1
11
n
i
~
1P
1i
1
~
11
1
1
1
1L
i
I
2
WOD
H
OF
NW
NI
Nvr
VF
iFI's
F'O
F F
O,
CO N
DO
H
H H
rz) v
FiN
FAO
V ii •
0co 7
w
00~
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ON
H8
m..n
o,.
wvl S
a a
IN
8
HW
Oi-
4 v
l a
a►0
N r
W
151-93-21bb a(Log from D . Jahnke )
Geologi csource
Material
Thickness
Depth(feet)
(feet )
Dark sandy clay or soil 1
1Fine yellow dry sand 72
73Fine gray wet sand 29
102Fine gray wet sand, mixed with small pieces of coal 9
111Gray wet sand 15
126Sand mixed with slack coal and coarser sand towar d
bottom 3
129
151-93-22ddd
Altitude : 1,986 fee t
Glacial drift :Till, dusky-yellow, oxidized 22
2 2Sand, medium to coarse, silty to gravelly, poorly
sorted, subangular to subrounded, interbedded ,oxidized 29
51Sand, fine, silty, interbedded with medium to coarse
sand and gravel, oxidized 27
78Silt, clayey to sandy, dusky-yellow, oxidized, inter
bedded with fine to medium sand 20
98Sand, fine, interbedded with lenses of silt and
medium sand, oxidized 26
12 4Sand, fine, dark-green, very poor sample 43
167Sand, fine, clayey, dark-greenish-gray 21
188Sand, fine to medium, dark-greenish-gray, well-sorted,
subangul.ar 24
212Lignite, black, detrital 5
217Sand, medium, dark-greenish-gray, well-sorted ,
lignitic 14
23 1Lignite, clayey, black, detrital 4
23 5Sand, fine to medium, dark-greenish-gray, well -
sorted, subangular 63
29 8Gravel, fine to medium, dark-brown, predominantl y
iron stained siliceous and sedimentary pebbles 9
30 7Till, dark-olive-gray, contains many small lignite
fragments 92
39 9Sand or gravel (from 8-log and drilling) no samples 23
42 2Tongue River Formation :
Shale, dark-brownish-black, oily 12
43 4Silt, clayey to sandy, light-greenish-gray 16
450
151-93-23bc c
Altitude : 1,935 fee t
Glacial drift :Loam, sandy, black 1
1Sand, very fine to very coarse, clayey, yellowish -
gray, drilled as though interbedded 8
9Till, dusky-yellow, oxidized 22
31Till(?), clay, silty, sandy clay, lignite, and car -
bonaceous clay, variegated, light-gray to black ,principally moderate-olive-brown, oxidized, con -tains a few sandstone boulders ; till apparentlycontains many inclusions from the Fort Union Group-
54
8 5Tongue River Formation :
Sand, fine, rusty-yellowish-gray, well-sorted, sub -rounded, micaceous, oxidized and iron stained 9
94Shale, silty, light-olive-gray, oxidized 13
10 7Shale, silty, medium-gray 13
120
94
151-93-28ddd(Log from D . Jahnke )
Geologicsource Material Thickness De t h
Black loam with some gravel
(feet )
3
feet )
3Yellow clay with gravel 24 2 7Seemed to be a layer of gravel 1 2 8Yellow clay 8 3 6Sort of hard pan or rock of some kind 2 38Yellow hard sandy clay or sandstone 6 44E[arder sandstone with soft layers 34 78blue sandy clay or sandstone 13 91Iignite coal and water 2 .5 93 . 5Dark clay .5 94
151-93-29add(Log from D. Jahnke )
Black loam 1 1Yellow clay mixed with gravel 37 3 8Darker clay 4 42Yellow clay 9 5 1Petrified sandy clay or soft sandstone 9 60Yellow sandy clay 34 94Darker sandy clay 8 102Still darker clay 14 116Lighter sandy clay 31 147Reddish clay, rocks and gravel 9 156Yellow sandstone or sandy clay 22 178Dark,green, and muddy 9 18 7Blue sandy mud 29 216Dark gray clay, not so muddy 30 246Gray soft sandstone or hard sand, water from 256 t o
259 ft . 15 26 1Hard rock 1 .5 262 . 5Sandy hard clay or soft sandstone 7 269 . 5Very hard rock 2 271 .5:Not quite so hard rock 2 273 . 5Very hard rock 2 275 . 5Sandy blue . clay ° 14 .5 290Gray sticky clay or shale ll 301,Almost black clay .5 301 . 5Fairly hard lignite coal 5 306 . 5Gray clay ° ° 2 308 .5
95
151-93-35bbb(Log from D . Jahnke )
Geologi csource Material Thickness De t h
Black soil mixed with gravel
fee t
1
feet )
1Gravel and sandy clay 3 4Rocks, gravel and sand It 8Yellow clay 13 2 1Rock and gravel 4 2 5Sandy mud 31 5 6Quite a lot of gravel 2 58Gray clay or shale 1 5 9Hard formation of some kind 2 6 1Sticky gray clay 15 76Light-green clay 6 82Dark-green clay or shale (some seepage) 13 9 5Very dark clay 2 9 7Very dark clay like coal but softer than coal 2 9 9Very sticky dark clay 3 102Greenlike very sticky clay 6 108Dark-gray clay 7 11 5Dark limestone 1 .5 116 . 5Dark clay 4 .5 12 1Black clay mixed with coal 2 12 3Lighter clay, sticky, noticed some seepage at 145 ft . 22 14 5Still light colored clay 10 15 5Coal .5 155 . 5Sticky gray clay 16 .5 17 2Brownish clay, not sticky 5 177Layers of thin coal, some seepage 2 179Gray clay 4 18 3Sandy clay 1 .5 184 . 5Fairly hard coal 2 186 . 5Gray clay ° 17 203 . 5Rock .5 204Sticky dark-gray clay 26 230Sandy and some water 4 234Still sandy clay and a little more water 4 238Layer of clay 2 240More sand and a little more water 10 25 0Gray clay or shale 5 255Hard rock, probably dark lime rock 1 .5 256 . 5Sticky gray clay 13 .5 270Loose coal and water 2 272Hard lignite, no more water 2 274Gray clay or shale 1 275
152-88-4bbb(Log from C . A . Simpson & Son)
Topsoil 1 1Yellow clay 38 39Gray clay 6 45Yellow clay, rust colored in places 9 54Gray clay '----° 4 58Hard layer 2 60Gray clay 5 65Slightly sandy gray clay 8 73Coal chunks, gray clay or shale 2 75Gray shale with coal particles 10 85Coal 1 .5 86 . 5Gray shale with coal particles 13 .5 100
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152-89-lbbb
Altitude : 2,091 feet
Geologi csource
Material Thickness De thfeet feet)
Glacial drift :Till, moderate-olive-brown, oxidized 27 2 7
Sentinel Butte Formation :5 3 2Leonardite, black, oily
Shale, variegated 23 5 5Lignite, black 2 5 7Shale, variegated 24 8 1Lignite, black 2 8 3Shale, variegated 7 90Lignite, black 3 93Shale, variegated 8 10 1Shale,variegated, lignitic, interbedded 19 120
152-89-6aa d
Altitude : 2,111 feet
Glacial drift :Loam, sandy, black 1 1Till, sandy, yellowish-gray to dusky-yellow, oxidized 24 25
Sentinel Butte Formation :Lignite, black 2 27Sand, fine, black, carbonaceous and medium-gray
shale, interbedded 7 34Shale, bluish-gray 6 4o
152-89-27abb(Log from Schmid, 1962 )
Glacial drift :Gravel, fine to coarse, sandy, oxidized 8 8Till, moderate-yellowish-brown, oxidized 4 12
Till, olive-gray 20 32Sand, medium to very coarse, gravelly 7 39Till, olive-gray 10 49
Tongue River Formation :Clay, dark-greenish-gray, lignite seams 3 .5 52 . 5
152-89-29dad
(Log from Schmid, 1962 )
Glacial drift :Gravel, fine to coarse, sandy, oxidized 12 12Till, olive-gray 34 46Gravel, fine to very coarse, sandy 8 54
Tongue River Formation :Clay, brownish-gray and grayish-blue-green wit h
lignite fragments 19 .5 73 . 5
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152-90-18cc c
Altitude : 1,870 feet
Geologi csource
Material
Glacial drift :Loam, sandy, blackSand, fine to coarse, subangular to subrounded ,
oxidizedTill, dusky-yellow, oxidizedTill, moderate-olive-brown, oxidized ; grades int o
olive-gray till at about 15 ft .Sand, medium to very coarse, and fine to coars e
gravel, interbedded in well-sorted lenses Till, partly oxidized ; poor samples
Tongue River Formation :Shale, medium-graySand, fine, greenish-gray, calcareous, friable
152-90-24ddd(Log from Schmid, 1962 )
Altitude : 1,993 fee t
Glacial drift :Till, moderate-yellowish-brown, oxidized 9
9Tongue River Formation :
Clay, dusky-yellow, oxidized 7
16Clay, greenish-gray ° 4
20Shale, grayish-yellow and dusky-yellow with ligniti c
seams 10
30C lay, greenish-gray 16
46Sandstone, very fine to fine, medium-bluish-gray wit h
lignitic seams 12
58Shale, grayish-yellow and dusky-yellow with ligniti c
seams 5
63
152-90-25ab d(Log from Schmid, 1962 )
Altitude : 1,986 feet
Glacial drift :Till, dark-yellowish-orange to moderate-yellowish -
brown, oxidized 28
28Tongue River Formation :
Clay, light-olive-gray to olive-gray with ligniti cseams 10
38Clay, dusky-yellow, sandy 4
42Shale, greenish-gray 6
48Lignite 4
52Sandstone, medium-bluish-gray, fine 13
65Shale, greenish-gray, sandy with lignitic seams 4
69Sand, grayish-green, very fine to fine with shale ,
moderate-olive-brown with lignitic seams It
73Siltstone, pale-green to dusky-yellowish-green with
lignitic seams 9
82Clay, light-olive-gray with lignitic seams 9
91Shale, greenish-gray 9
100Sandstone, pale-green, clayey 5
10 5
102
Thickness
Depth
(feet)
(feet )
1
1
3
4
5
9
55
64
11
758
83
6
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95
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152-90-26cdd(Log from Schmid, 1962 )
Altitude : 1,909 feet
Geologicsource
Material Thickness D tfee tPeet
Glacial drift :Clay, medium-gray, oxidized 5 5Sand, fine to very coarse, sparse clay 6 11Sand, fine to very coarse, gravelly 10 2 1Gravel, fine to coarse 2 2 3Till, olive-gray 10 33
152-90-26ddc(Log from Schmid, 1962 )
Altitude : 1,918 fee t
Glacial drift :Sand, fine to very coarse, gravelly, oxidized 15 15Gravel, fine to very coarse, oxidized 2 17Till, olive-gray 8 2 5Sand, very fine to very coarse 13 38
Tongue River Formation :Lignite with greenish-gray clay lenses 8 46Clay, olive-gray with greenish-gray areas 17 63
152-90-27caa(Log from Schmid, 1962 )
Altitude :
1,905 fee t
Glacial drift :Clay, moderate-yellowish-brown, sandy, oxidized 5 5Clay, dark-greenish-gray to greenish-gray, silty 3 8Clay, yellowish-gray, silty 3 11Till, olive-gray 42 53Gravel, fine to coarse 2 55
Tongue River Formation :Lignite 2 57Shale, dark-greenish-gray 7 64Clay, pale-blue-green, silty with greenish-gray and
dark-greenish-gray clay with lignite lenses 18 82Sandstone, medium-gray, very hard 2 84
152-90-27ddd(log from Schmid, 1962 )
Altitude : 1,909 feet
Glacial drift :Clay, dusky-yellow, oxidized 5
5Gravel, fine to coarse, sandy, oxidized 2
7Gravel fine to coarse, sandy 13
2 0
Till(?), rock at 22 ft ., abandoned hole 2
2 2
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152-90-35bac
(Log from Schmid, 1962 )
Altitude : 1,918 feet
Geologicsource
Material
Glacial drift :Till, dusky-yellow, oxidizedGravel, fine to coarse, sandy, oxidized Till, olive-gray
Tongue River Formation :Shale, dark-greenish-graySandstone, greenish-gray, fine to very fine
152-90-36aaa(log from Schmid, 1962 )
Altitude : 1,932 feet
Glacial drift :Till, moderate-yellowish-brown, oxidized 16
16Till, olive -gray, gravel 15
31Gravel, fine to coarse, sandy 10
41Gravel, bouldery, poor samples 5
46Tongue River Formation :
Clay, light-greenish-gray to bluish-gray, sandy, verypoor samples 17
6 3
152-90-36aba(Log from Schmid, 1962 )
Altitude : 1,919 feet
Glacial drift :Sand, very fine to medium, silty, oxidized 6
6Sand, very fine to very coarse, silty 10
16Gravel, fine, very sandy 12
28Till, olive-gray 15
43Sand, medium to very coarse, granule gravel 2
45Till, olive-gray 3
48Gravel, fine to medium, sandy 12
60Tongue River Formation :
Clay, greenish-gray, lignitic seams 24
84
152-90-36abb(Log from Schmid, 1962 )
Altitude :
1,919 fee t
Glacial drift :Till, moderate-yellowish-brown, oxidized 7 7Gravel, fine to medium, sandy, dark stained 24 3 1Clay, light-bluish-gray to medium-bluish gray with
brownish-black clay with lignite seams (Tongu eRiver Formation??) 6 3 7
Clay, olive_gray 20 57Gravel, fine to medium, sandy 3 60
Tongue River Formation :Clay, light-bluish-gray with brownish-black clay 3 6 3Clay, pale-green to grayish-green with light-olive -
gray sandstone 11 74Clay, greenish-gray to dark-greenish-gray 31 105
106
Thickness
Depth{feet)
(feet )
11
11
7
i8 .
44
62
6
685 .5
73 . 5
152-90-36ab c(Log from Schmid, 1962 )
Altitude : 1,950 fee t
Geologicsource
Material Thickness Depth
Glacial drift :Topsoil, black
feet
2
(feet)
2Gravel, fine, sandy, clayey, oxidized 7 9Till, dark-yellowish-orange, oxidized 9 18Gravel, fine to medium, sandy, oxidized 2 20Till, olive-gray 60 80
Tongue River Formation :4 8 4Cla y, greenish-gray
152-90-36add(Log from Schmid, 1962 )
Altitude :
1,931 feet
Glacial drift :Sand, very fine to coarse, silty, oxidized 7 7Sand, very fine to coarse, clayey 4 11Sand, medium to very coarse, gravelly 4 1 5Till, olive-gray 30 4 5Gravel, fine to medium, sandy 5 50Till, light-olive-gray to olive-gray 10 60
Tongue River Formation :3 63Shale, light-bluish-gray, silty, lignitic seams
152-90-36ddd(log from Schmid, 1962 )
Altitude : 1,977 feet
Glacial drift :Till, dark-yellowish-brown, sandy, oxidized 6 6Till, moderate-yellowish-brown to dark-yellowish -
orange, oxidized 8 14Till, dark-yellowish-brown to dusky-yellowish-brown ,
oxidized 13 27Till, olive-gray 10 37
Tongue River Formation :
15 52Clay, light-olive-gray with lignite lenses Clay, pale-blue-green to grayish-blue-green 6 58Shale, light-olive-gray 5 63
10 7
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Geologicsource
152-92-19aaa l(Log from C . A . Simpson & Son )
Material Thickness Depth(feet) (feet )
Topsoil 1 1Light-gray clay 1 2Light-gray clay, rocks and gravel 1 3Gravel, rocks 2 5Yellow clay 33 3 8Gray clay 78 116Muddy gray sand 31 14 7Medium-fine sand and fine gray sand 10 15 7Sand and small gravel with coal and scoria particle s 2 15 9Sand with coal chunks 1 160Sand and gravel 15 175Sand 5 180Muddy fine gray sand with a few coarser particles an d
coal 5 18 5
152-92-19aaa 3
Altitude : 1,896 fee t
Glacial drift :Soil, silty and sandy, brownish-black 1 1Gravel, fine to medium, clayey, angular to sub -
rounded, oxidized 3 4Clay, silty, dusky-yellow, calcareous, (fluvial
sediments), cracks at 10-12 and 46-48 ft . 46 5 0Clay, silty, light-olive-gray, (lost circulation in
interval, apparently in cracks) 57 10 7Till, olive-gray 13 12 0Sand, fine to medium, moderately well-sorted ,
angular to rounded ; 70 to 80 percent quartz 22 14 2Gravel, sandy, moderately well-sorted, angular t o
subrounded ; gravel is fine near top and grades t ocoarse near bottom, and contains about 15 to 2 5percent coarse to very coarse sand 16 158
Tongue River Formation :
4 162
Sandstone, fine to medium, light-bluish-gray t omedium-bluish-gray
Shale, medium to dark-gray ; contains some lignite 18 180
152-92-19aab
Altitude : 1,892 fee t
Glacial drift :Silt, sandy with pebbles, dusky-yellow, oxidized 4
4Silt, clayey to sandy, dusky-yellow, oxidized 24
28Clay, silty, olive-gray 90
118Sand, medium to coarse with fine to medium gravel ,
generally subrounded ; pebbles are composed pre -dominantly of limestone,granitic rocks, and shale 13
131Sand, medium, well-sorted, subangular to subrounded ,
lignitic 18
149Gravel, coarse ; pebbles are predominantly limestone
and claystone 12
161Tongue River Formation :
Shale, light to medium-gray ; interval also containsthin lenses of interbedded lignite 19
180
109
152-92-20ad d
Altitude :
1,926 fee t
GeologicThickness Depthsource
Material(feet )(feet )
Glacial drift :Silt, pebbly near surface, dusky-yellow, oxidized 5 5
Silt, sandy to clayey, dusky-yellow, oxidized 14 19
Silt, clayey with lenses of pure plastic clay and188 207very fine sandy clay, olive-gray
Clay, sandy with pebbles and gravel stringers, oliv e
gray , (till?) 28 23 5
Sand, very fine to fine, dark-greenish-gray to black ,highly micaceous and lignitic, moderately cal -careous, contains some gravel lenses and detrita l
lignite ; has strong H2S odor 38 273Sand, coarse and very coarse, some fine gravel, sub -
rounded, light-brown color, well sorted, the sand
is mostly clear quartz with minor amount of gree n
silicates and brown
ironstone,
shale, limestone ,
and lignite 34 307
Tongue River Formation :Sand, very fine to fine, light-greenish-gray, cal -
careous 4 31 1
Shale, medium-gray to olive-black 3 314
Lignite 5 319
Shale, medium-gray to olive-black 6 325
152-92-20bb a
Altitude : 1,901 fee t
Glacial drift :Soil, silty and sandy, brownish-black 1
1
Gravel, fine to medium, poorly-sorted, angular t osubrounded, oxidized 4
5Clay, silty, dusky-yellow, calcareous, oxidized 50
55
Clay, silty, light-olive-gray to greenish-gray, (los t
circulation at 60 ft . and drilled blind, E-lo g
indicates similar material through interval) 53
108
Till, o live -gra y ° 16
124
Sand, fine to medium, lignitic 17
141
Sand, fine to coarse, about 25 percent gravel 9
150
Gravel, fine to coarse, about 25 percent sand 67
21 7
Boulders and cobbles ; predominantly limestone and
sandstone 2
21 9
Tongue River Formation :Shale, medium-to dark-gray ; siliceous ; slightly cal -
careous near bottom of interval 21
24 0
110
152-92-20bbb2
Altitude :
1,898 feet
Geologicsource Materia l
Glacial drift :Soil, silty and sandy, brownish-blackSilt, gravelly, dusky-yellow, calcareousSilt, clayey, dusky-yellow, calcareous ; contains a
few limestone pebbles, oxidized (fluvialsediments)
Clay, silty, light-olive-gray to greenish-gray, cal -careous ; a few thin yellowish-gray layers in somesamples (fluvial sediments)
Clay, silty, olive-gray, calcareous (fluvia lsediments)
Till, olive-gray to dark-greenish-gray Sand, fine to coarse, moderately well-sorted, angula r
to rounded ; 75 to 80 percent quartz grainsGravel, fine to medium (grades to coarse with depth) ,
moderately well-sorted in lenses, angular to sub -rounded ; predominantly subrounded ; contains about20 percent coarse to very coarse sand
Boulders ; greenish-gray, calcareous sandstone an dpale-orange limestone
Tongue River Formation :Shale, medium-to dark-gray, siliceous ; slightly
calcareous in top 10-15 ft . of section
152-92-29dd d
Altitude : 1,877 fee t
Glacial drift :Loam, sandy, blackSilt, sandy, dusky-yellow, oxidized Silt, clayey, light-olive-gray, laminatedClay, silty, moderate-olive-brown, oxidized Till(?), moderate-olive-brown, partly oxidized ;
contains a few silt and clay streaks Till, olive-graySand, fine to coarse with some gravel, lignitic (san d
is coarser and cleaner with depth) Tongue River Formation :
Sand, very fine, silty and clayey, greenish-grayClay, sandy, white, calcareous Lignite, black, fissileSandstone, fine-grained, greenish-gray, hardShale, light-graySand, fine, clayey, dark-greenish-gray
152-92-31cc c
Altitude :
1,968 fee t
Glacial drift :Till, yellowish-gray to dusky-yellow 20Gravel, fine to medium, moderately well-sorted 5Sand, medium to very coarse with some gravel, well -
sorted in lenses, subangular to subrounded 1 7Sand, coarse, gravelly, subangular to subrounded 8
Sentinel Butte Formation(?) :Sand, very fine, clayey, light-greenish-gray 8Sandstone, fine-grained, lignitic, calcareous 2Shale, light-olive-gray 20
111
2 02 5
4 2
5 0
5 8608 0
Thickness
Dept h(feet) (feet )
1 1
3 4
44 48
48 96
14 11013 12 3
31 154
61 21 5
3 218
22 240
4 412 1620 364 40
10 5053 10 3
19 12 2
4 12 62 1284 13 22 13 43 13 73 14 0
152-93-idea
Altitude :
2,004 feet
Geologi csource
Material Thickness Depth(feet )(feet )
Glacial drift :Gravel, fine to medium, sandy, iron-stained 8 8Clay, sandy, black, oily 1 9Gravel, fine to medium, sandy, iron-stained 9 18Clay, silty, black, oily 1 1 9Sand, medium to very coarse, well-sorted in lenses ,
iron-stained ; contains some gravel 28 4 7Till, moderate-olive-gray to olive-gray 20 6 7
Sentinel Butte Formation :
3 70Lignite, black, hardShale, sandy, greenish-gray to light-olive-gray ,
brittle 30 100
153-88-6ddd
Altitude : 2,036 feet
Glacial drift :Loam, sandy, black 1
1Sand, very fine to fine, clayey to silty, yellowish -
23
24grayGravel, fine, sandy, reddish-brown, well-sorted, sub
10
34angular to subrounded, iron-stained Sentinel Butte Formation :
26
60Shale, variegated,contains sandstone, lignite, and
leonardite, probably in thin beds
153-88-15ddd
Altitude : 2,071 feet
Glacial drift :Loam, silty, black 1
1Till, moderate-olive-brown, oxidized 17
18Till, light-olive to olive-gray 7
2 5Till, olive-gray 20
4 5Sentinel Butte Formation :
Lignite, black, fissile 2
4 7Shale,variegated grays and greens 13
6o
153-88-23ddd
Altitude : 2,089 feet
Glacial drift :Till, yellowish-gray, oxidized 9 9Till, moderate-olive-brown, oxidized 41 50Till, olive-gray 24 74
Sentinel Butte Formation :10 8 4Silt, clayey, dusky-yellow, micaceous, oxidized
Silt, clayey, medium-gray, micaceous 16 100
112
153-88-30cdc(Log from D . Jahnke )
Geologicsource
Material Thickness Depth
Iark yellow clay mixed with stones
Pee t
20
(feet )
20
Darker clay 11 3 1
Yellow clay 7 38
Dark clay, almost black like coal 7 4 5Sticky gray clay 5 5 0Lignite coal, some loose coal above lignite 2 52Gray clay 5 57
153-89-16ddcN .D .G .S . auger hole
Pebbly sand; dark-yellowish-brown, outwash 60 60Gradation between outwash and bedrock 2 62
Fort Union Group :Clayey sand, gray 12 74
153-89-21cc c
Glacial drift ;:Loam, gravelly, dark-brown 1
1Gravel, fine and medium, sandy, poorly-sorted, sub -
angular and subrounded, iron-stained 7
8Till, dusky-yellow, oxidized 3
11Sentinel Butte. Formation :
Silt, clayey, moderate-olive-brown to light-olive -
gr'ay 10
2 1
Limestone, gray 2
23Shale, silty, medium-gray to light-greenish-gray 17
4oSand, very fine to fine, very clayey, dark-greenish-
gray, slightly friable 13
5 3Idgnite, black, hard 2
5 5Shale, Br'a.Y ° 5
60
153-89-31cb c
Altitude : 1,910 fee t
Glacial drift :
Loam, clayey, black ° 2
2Sand, coarse, well-sorted 4
6
Clay, light-olive-gray 2
8Gravel, fine and medium, sandy 24
32Till, olive-gray 33
65Gravel, fine and medium, sandy, moderately wel l
sorted in lenses, subrounded 31
96
Fort Union Group :Shale, silt, and sand, generally olive-gray wit h
some variegatedbeds 46
142
Shale, silty, medium-gray 18
160Sand, very fine, silty, light-gray, calcareous 20
180
113
153-89-33dda(Log from D . Jahnke )
Geologi c source
Material
Thickness
De t h(feet)
feet )
Black loam 3
3Yellow drift clay 41
44
Yellow clay mixed with sand 4
48
Slush coal, mud, some black dirt with water 3
5 1Hard like coal with water below coal .5
51 . 5
Yellow clay 1 .5
53Dark clay 5
58
Gray clay or shale 22
80
Darker clay 10
90Slush coal and water 2
92Hard lignite with water 3
95
153-89-35dd dN.D .G .S . auger hole
Silty loam soil 1
1Till, slightly gravelly 26
27
Fort Union Group :Clayey silt (some thin, fine sand lenses), dusky-
yellowish-brown 7
34
153-90-7ccc
Altitude : 2,191 feet
Glacial drift :Loam, pebbly, dark-brown 1
1Till, yellowish-gray, oxidized 14
1 5
Till, dusky-yellow to moderate-olive-brown 17
32Gravel, fine and medium, moderately well-sorted, sub
angular to subrounded, iron-stained 7
3 9Till, moderate-olive-brown, oxidized 20
5 9
Till, olive-gray 25
8 4
Gravel, medium, sandy, subangular to angular ,lignitic, iron-stained 5
8 9Clay, sandy, olive-gray ; contains numerous lignite
specks 15
10 4Clay, silt, and sandstone . Probably a large boulde r
of Fort Union sediments 13
117
Till, olive-gray 93
210
Sentinel Butte Formation(?) :Shale, silty to sandy, slightly calcareous ; contains
minor quantities of lignite 16
22 6Shale, brownish-black, and gray, carbonaceous 4
23 0Shale, variegated,grays, greens, and brown 16
24 6Lignite, black, fissile 3
24 9Shale, light-greenish-gray 3
252Sand, very fine, clayey, light-greenish-gray 5
25 7Shale, light-greenish-gray 3
260
114
15i-`0-15ddd
Thickness
Dept h
. 7
drift
(feet) (feet )
Loam, sandy, dark-brown 1 1Pill, yellowish-gray, oxidized 5 6
:A!t,
layey, dusky-yellow, oxidized 6 12
1 v,l, fine, sandy,
iron-stained ; contains many8 2 0iron-oxide and iron carbonate pellets
2 do n,•l Butt
or:nation :
16 36G .m i . very fine to fine, clayey, yellowish-green ,
lienitic, and micaceous, friable
silty, dusky-yellow 8 44
S n i, very fine to
'in, . light-greenish-gray to
14 58brownish-black . calcareous, licnitic, micaceous ,
friableLi*nite, black,
fissile 7 6 5Clay, sandy, light-olive-:ray to greenish-gray 15 80
153-91- 2 7cc c
Altitude : ',078 feet
llacia]
drift :Loam, gravelly . dark-brown 1 1
Gravel, medium, brownSilt, sandy, yellowish-gray 4 6
Till, dusky-yellow, oxidized 8 14Sand, medium to coarse, gravelly, well-sorted in
lenses, subrounded, iron-stained 10 24Till, moderate-olive-brown, oxidized 16 40
Sentinel Butte Formation :10 50Gilt, clayey, dusky-yellow, oxidized
Sand, fine, slightly clayey, yellowish-green ;contains some lignite grains 12 62
Sandstone, fine grained, light-greenish-gray,4 66calcium-carbonate cement
Sand, fine, greenish-gray, lignitic 24 90Shale, sandy, medium-gray 10 100
153-91-32ch c(Log from E . H . Prather)
3 3TopsoilBrown sandy shale 32 35Gray sandy shale 10 45Gray sand 15 60Coal 2 62
Gray sandy shale 8 70Blue sand (rolling sand) 80 150Gray shale 78 228Gray sand (fine sand and some coal in the sand) 31 25 9
11 5
153-92-17bb b
Altitude :
1,978
C~~ .f7 s
Geologi csource
Material Thickness Dept h
Glacial drift :Loam, silty, black
(fens : )
1
(j•.
Silt, dusky-yellow, oxidized 9 l ugravel, fine to medium, sandy, well-sorted in lens m ;
40 percent subangular, 60 percent sabre ndea 4 6Tongue River Formation :
7 5 3Lignite, black, fissile Shale, silty, medium-Fray to ir-. garish-: .ray, and
black, carbonaceous 7 60
153-92-19ccc
Altitude : 1,964 fee t
Glacial drift :Till, yellowish-gray, oxidized 21
2 1Tongue River Formation :
Shale, silty, dusky-yellow, oxidized 4
2 5Shale, silty, light-olive-gray 15
40
154-89-14dcd
Altitude : 2,050 fee t
Glacial drift :Till, moderate-olive-brown, oxidized 20
20Sentinel Butte Formation(?) :
Shale, variegated,yellows, greens, and grays ;contains a few thin lenses of lignite 20
40
154-89-15cdd
Altitude : 2,096 feet
Glacial drift :Loam, pebbly, black 1 1Till, moderate-olive-brown, oxidized 37 38Till, olive-gray 10 48Gravel, fine to medium, sandy, subangular, iron -
stained 5 53Till, olive-gray 7 6oShale, light-greenish-gray 5 65Sand, clayey, dark-greenish-gray, micaceous 6 71Gravel, fine, sandy, subangular to subrounded ,
iron-stained 9 8 oSentinel Butte Formation :
20 100Shale, variefated,contains leonardite and lignite--- -
116
154-89-15ddd
Altitude : 2,002 fee t
(feet) feet
Glacial drift :Loam, sandy, brown--- 2 2Gravel, fine to medium, sandy, moderately well-
sorted in lenses, subangular to subrounded, iron -stained to 17 ft . 58 60
Sand, medium to coarse, fine gravel interbedded ,generally subrounded 11 7 1
Tongue River Formation :Shale, silty, light-olive-gray 3 74Lignite, black, fissile 2 76Shale, medium-tray, thin carbonaceous and ligniti c
shale 4 80
154-90-6cca(Log from E . H . Prather )
Brown clay 15 1 5Gray clay, rock and gravel 61 76Brown clay and rock 65 14 1Brown sand 3 144Brown clay 17 16 1Brown clay and small trace of coal 3 164Brown sandy clay 12 176Green clay 6 .5 182 . 5Hard shell 1 183 . 5Gray sandy clay 12 .5 196Gray clay 16 212Gray sand 5 217
154-90-18ddd
Altitude : 2 ,300 feet
GlaAal drift :Till, dusky-yellow to moderate-olive-brown, oxidized 19 19i-i 11, olive -g ray 19 38Till, gravelly, olive-gray 11 49Till, olive-gray ; contains some yellow, oxidized,
31 80silty bouldersSand, very fine to fine, silty, light-olive-gray 8 88Clay, olive-gray 6 94
Sentinel Butte Formation :7 10 1Silt, light-olive-gray
Idgnite, black, fissile 6 10 7Shale, silty, light-gray to brownish-black, sandy
13 120near bottom, darker color is due to carbonaceousmatter
117
oologi csource
Material
Thickness
Depth
154-91-30aaa
Altitude : 2,121 feet
Geologi c source
Material
Topsoil, blackSilt, clayey, variegated, mostly greenish-graySilt, light-olive-gray, soft, calcareousSand, fine, gray, well-sorted, subrounded Silt, sandy, light-olive-grayClay, olive-gray to olive-black, some greenish-gray Clay, silt, and fine sand, olive-gray ; generally i n
lenses 2 to 3 ft . thickClay, olive-gray, olive-black, and dark-greenish-gra ySilt, slightly sandy, olive-grayGravel, fine and medium, poorly sorted, angular an d
subangularClay, very silty, greenish-gray and olive-gray
Sentinel Butte Formation :Sandstone, medium-grained, light-greenish-gray t o
dark-greenish-gray, fairly well-sorted, calcareouscement
Sand, medium-grained, dark-greenish-gray, very well -sorted, micaceous and lignitic
Lignite, black, fissileShale, silty, calcareous
154-92-4cc c(Log from E . H. Prather )
Brown clayGray shale and sandCoalGray shale (water)
154-92-7db c(Log from J . F . Bruton )
Yellow clay 75 75Gray sandy clay 4o 115Some coal and muddy water 10 12 5Gray sandy clay 65 190Coal and water 6 196Gray sandy shale 7 203
118
Thickness(feet)
feat!feet )
2 214 16
7 2 32 2 57 3 27 3 9
26 6 57 726 78
3 8 111 9 2
5 9 7
29 12 64 13 0
10 14 0
25 2 539 64
4 6 82 70
154-92-25bbb
Altitude : 2,120 fee t
Geologi csource Ms .terial Thickness De t h
feet )(feet )
Loam, sandy, dark-brown 1 1Sand, fine to medium, clayey, silty, yellowish-gra y 13 1 4
Silt and clay, sandy, yellowish-gray, interbedded,
15 2 9softSand, coarse, some gravel, poorly sorted, sub -
4 3 3angular and subroundedSilt and clay, sandy, yellowish-gray to moderate -
15 48olive-brown with variegated streaks, interbedded-- -Clay, silty to sandy with occasional pebbles--mostly
30 78lignite chips--variegatedyellows, grays, an d
greens, (till?)Gravel, fine and medium, sandy, "dirty " , poorly
sorted, angular to subrounded, iron-stained 2 80
Sentinel Butte Formation :
20 10 0
Sand, fine, slightly clayey, yellowish-green, highl ylignitic and micaceous ; becomes dark-greenish-grayand more clayey with depth
154-92-32bc c
T:ul 13 .5 13 . 5
Salty clay, with scattered pebbles 17 30 . 5
Silty clay, brownish 5 .5 36
Yellowish bentonite 5 .5 41 . 5
Clay with scattered gravel pebbles(?) 2 .5 44
Bentonitic clay and bentonite 3 4 7
Silty clay, brownish 7 5 4Clay, bentonite, waxey, yellowish 1 5 5
Silty clay, bentonitic, brownish 2 5 7
Silty clay, reddish-yellow 1 58
Silty clay, brownish 3 6162Clay, purplish (1 in . lignite at top) 1
Clay, tan .5 62 . 5
Clay, bentonite, orangish .5 6 3
Clay, bentonite, tan ; with silty clay 4 6 7
Clay, bentonite, purplish 2 6 9
Clay, bentonite, tannish ; lignite chunks 4 73
Silty clay and clayey silt, tan to bluish 21 9 4
154-93-5add
Altitude :
2,330 feet
Glacial drift :Gravel, fine to coarse, sandy, poorly sorted, sub -
angular and subrounded, iron-stained 12
12 19Till, dusky-yellow, oxidized
26
19Till, olive-graySentinel Butte Formation :
13
58Sand, fine, silty, and clayey, light-olive-gray Shale, silty, medium-gray to light-greenish-gray 7
6 5
Lignite, black, fissile 3
6 8
Shale, brownish-black and medium-gray 6
74
Shale, greenish-gray 6
80
11 9
154-93-5dc c(Log from E . H . Prather )
Geologi csource Material Thickness Ik th
(feet) feet )
Brown clay 6 6Brown sandy clay 22 2 8Black clay ° 2 3 0Gray clay 2 3 2Coal, sand and water 5 3 7Gray clay 2 3 9
154-93-25aaa
Till, oxidized 52 52Clayey silt and silty clay, scattered pebbles ,
oxidized 16 68Clayey silt and silty clay, oxidized 8 76Silty clay, oxidized, more reddish 4 80Silty clay or clay; oxidized ; dark-grayish-brown 3 8 3Bentonite, greenish-bluish 2 8 5Clay, brownish and yellowish 3 88Silty clay, dark brown 8 96Clayey silt, light brown 7 103Clay, olive-greenish 4 107Silty clay or clayey silt, greenish 11 118Clayey silt, greener 6 12 4
154-94-3bb a
Altitude : 1,938 fee t
Glacial drift :Sand, very fine, clayey to silty, yellowish-gray t o
dusky-yellow, oxidized, (dry) 9
9Gravel, fine and medium, sandy, interbedded ; contain s
some marcasite ; pebbles are predominantly lime-stone and sedimentary rocks 48
5 7Tongue River Formation :
23
80Shale, silty to sandy, light-olive-gray to light -
greenish-gray
154-94-4dd d(Log from E . H . Prather )
Brown sandy shale 30 30Gray shale ° 10 4oGray sandy shale 17 5 7Hard shell 3 6oGray sandy shale 14 74Gray sandy shale (small amount of water) 11 8 5Gray shale 5 90Gray sandy shale 11 101Goal 3 l04
12 0
155-88-2add
Altitude : 2,103 fee t
Geologi csource Thickness DepthMaterial
Glacial drift :Clay, black
(feet )
2
(feet )
2Clay, yellowish-gray, oxidized 14 1 6Clay, silty, dusky-yellow, light-olive-gray, and
14 30yellowish-gray, interbeddedClay, silty to sandy, gray, bedded 22 52Till, olive-gray ° 52 104Gravel, fine to very coarse 15 119Till, olive-gray 42 16 1
Fort Union Group :Shale, silty, various shades of gray and green ;
contains some thin seams of white bentonite and39 200black lignite
155-88-3aaa2
Altitude : 2,182 feet
Glacial drift :Till, yellowish-gray, oxidized 10 10Till, moderate-olive-brown, oxidized 52 62Sand, medium, tan, well-sorted, subrounded to sub-
4 66angular, micaceous, oxidized Trill, olive-gray ° 22 8 8
Sentinel Butte Formation :
9 97Sand, fine to medium, dark-greenish-gray, micaceou s
and ligniticSand, dark-green ; indurated, light-greenish-gray
23 120sandstone ; and yellowish-gray, bentonitic, siltyshale
155-88-6dd d
Altitude : 2,191 feet
Glacial drift :Sand, silty and clayey, yellowish-gray, oxidized 4 4Till, moderate-olive-brown 25 2 9Till, olive-gray 81 110Gravel, medium to coarse, sandy, poorly sorted ,
angular to subrounded ; contains thin lenses of21 13 1silt and clay
Gravel, fine and medium, well-sorted, subangular to29 160subrounded
Gravel, medium to very coarse, poorly sorted 18 178Sentinel Butte Formation :
22 200
Shale, silty, variegated grays and greens, and inter bedded dark-greenish-gray sand and brown carbon-aceous silt
121
155-88-7dd d
Altitude : 2,123 feet
Geologicsource Thickness Dept hMaterial
Glacial drift :Loam, sandy, black
(nett )
.I .
(Peet )
1
Sand, fine, clayey, yellowish-gray 9 10Till, dusky-yellow, oxidized 7 1 7Till, moderate-olive-brown, oxidized 4] 58
Till, olive-gray 70 128
Till, olive-gray, contains many thin streaks of28 15 6limestone gravel
Gravel, fine to medium, subangular to subrounded 4 16 0
Till, olive-gray, contains thin streaks of sand and25 18 5gravel
Sand, fine to medium, gray, moderately well-sorted,15 200subrounded ; contains many lignite chips
Till, olive-gray 5 205Tongue River Formation :
7 21 2Sand, very fine, clayey, greenish-grayShale, silty, light-olive-gray to light-greenish -
8 220gray
155-88-14cc c
Altitude : 2,117 fee t
Glacial drift :Clay, sandy, yellowish-gray, oxidized 3 3
Till, moderate-olive-brown, oxidized 15 18
Sand, fine, silty, reddish-brown 8 26Gravel, fine to medium, poorly sorted, subangular to
9 3 5subrounded ; pebbles are iron-stainedTill, moderate-olive-brown to olive-gray, partly
30 6 5oxidizedSentinel Butte Formation :
13 7 8Silt and very fine, clayey sand, light-greenish-gray Shale, silty, light-olive-gray to light-greenish-gray 14 92Limestone, dark-gray 2 94
Shale, silty, medium-gray 6 100
l55-88-15abb
Altitude :
2,104 fee t
Glacial drift :Till, yellowish-gray, oxidized 3 8Till, moderate-olive-brown, oxidized 10 18
Till, olive-gray 144 162
Fort Union Group :Shale, silty, light-gray 9 171Sand, silty and clayey, light-gray to greenish-gray ,
micaceous ; interbedded 54 22 5Lignite, black, fissile 99
2234
Shale, medium-gray 40
12 2
155-88-26ccc
Altitude : 2,077 feet
Geologi csource Material Thickness Depth
(feet )(feet )
Glacial drift :Clay, silty to gravelly, yellowish-gray to dusky-
yellow, (till?), oxidized 8 8Till, moderate-olive-brown, oxidized 23 31Till, olive-gray 118 149Sand, gray, well-sorted, lignitic 3 152Till, olive-gray 17 169Sand, fine to medium, silty, light-gray, well-sorted
in lenses 7 176Clay, olive-gray 4 18oSand, fine to medium, light-gray, well-sorted, sub -
11 19 1roundedClay, sandy, white 3 194Gravel, fine to medium, moderately well-sorted,
10 204angular to subroundedSilt, clayey, white 3 20 7Gravel, fine to medium, sandy, poorly sorted 6 21 3Silt, clay, and very fine sand, intercalated, olive -
gray and light-olive-gray (possibly Tongue River64 27 7Formation)
Tongue River Formation :3 280Sandstone, very fine, greenish-gray, cemented
Sand, clayey, very light-gray to light-greenish-gray 20 300
155-88-30ad a
Altitude : 2,050 fee t
Glacial drift :Till, yellowish-gray, oxidized 5 5Till, dusky-yellow to moderate-olive-brown, oxidized 9 14Gravel, sandy, reddish-brown, with thin lenses o f
dusky-yellow silt 18 3 2moderate-olive-brown to olive-gray, partly
oxidized 14 46Gravel, fine to very coarse, poorly sorted 8 54Till, olive-gray 35 8 9Gravel, fine to coarse, sandy, poorly-sorted ,
angular to subrounded 6 9 5Trill, olive-gray 15 110Gravel, fine and medium, sandy, moderately well -
sorted in lenses, angular to subrounded 13 12 3Tongue River Formation :
17 140Shale, silty, light-to medium-gray, interbedded with
greenish-gray to dark-greenish-gray, sand
12 3
155-88-31aaa(Log from D . Jahnke )
Geologi csource Material Thickness Depth
Dark soil mixed with some gravel
(feet )
3
(feet )
3Yellow clay, some gravel and sand 27 30Yellow clay 7 3 7Dark clay, rock at about 51 and 63 ft . 37 74Harder formation, varied color 3 77Gray clay 17 9 4Harder formation mixed with sand 4 98Gray clay 3 10 1Gray clay and darker 20 12 1Dark muddy clay with some water 13 13 4Fine blue sand with water 2 13 6Sand became gradually coarser with some gravel 8 144Soft clay mixed with sand 2 146
155-89-22bbb
Altitude : 2,015 feet
Glacial drift :Sand, silty and pebbly, yellowish-gray, oxidized 4 4Silt, clayey, moderate-olive-brown and reddish-brown ,
contains lenses of medium to coarse sand and finegravel 8 12
Gravel, fine and medium with interbedded medium t overy coarse sand, subangular to subrounded 18 30
Till, moderate-olive-brown, oxidized ; contain sseveral thin lenses of rusty sand 27 5 7
Till, olive-gray 66 12 3Tongue River Formation :
4 12 7Clay, light-olive-gray, laminatedSand, very fine, clayey, greenish-gray 15 142Shale, reddish-brown 4 146Lignite, black, fissile 2 14 8Shale, medium-gray, lignitic 8 156Lignite, black ; fractured and takes much water 4 160
l55-89-25acb2
Altitude : 2,036 feet
Glacial drift :Soil, black 2
2Sand, medium to coarse, gravelly, yellowish-brown ,
poorly sorted ° ° 7
9Till, yellowish-brown, oxidized 8
1 7Clay, silty to sandy, olive-gray, calcareous ,
lignitic 18
3 5Sand, coarse, gravelly, moderately well-sorted 2
3 7Gravel, medium to coarse, sandy, moderately well -
sorted, subangular to subrounded ; about 50 percentlimestone pebbles 9
46Sand, coarse, gravelly, angular to subangular 24
70Tongue River Formation :
Clay, silty, greenish-gray, contains lignite flakes--
10
80
12 14
155-89-25acb 3
Altitude : 2,037 fee t
Geologicsource
Material
Thickness
Depth
Glacial drift :Soil, silty, blackGravel, sandy, yellowish-brown, poorly sorted Clay, silty and sandy, yellowish-brown ; drilling
indicates a few cobbles or small boulders (till?)Clay, silty and sandy, dark-blackish-gray Clay, dark-blackish-gray interbedded with thin lense s
of sand and gravelGravel, fine to medium, moderately well-sorted, sub -
angular to subroundedGravel, fine to very coarse with boulders, poorly
sortedClay, silty, medium-gray ; poor returns
155-89-25acb 4
Altitude : 2,034 fee t
Glacial drift :Soil, blackClay, silty to sandy, yellowish-brown, oxidized
Gravel and sand, poorly sorted, subangular to sub -
roundedClay, silty, dark-olive-gray, slightly calcareous
Gravel, sandy, poorly sorted ; contains two thin clay
lenses between 40 and 45 ft .
feet (feet )
5 54 9
7 1611 2 7
11 38
12 50
11 61
9 70
1 16 7
6 1 312 2 5
33 58
155-89-25bc c
Altitude : 2,028 feet
Glacial drift :Soil, black 4 4
Gravel, medium to coarse, yellowish-brown, poorly
sorted 14 18
Clay, slightly sandy, dark-olive-gray, calcareous ;
contains several thin lenses of sand 65 83
Sand or gravel 11 94Tongue River Formation :
Clay, silty, light-greenish-gray ; contains lignite
flakes 6 100
155-89-25bd d
Altitude :
2,029 feet
Glacial drift :Soil, silty, black 4 4
Gravel, sandy, fine to medium, subangular to sub -
rounded, poorly sorted, oxidized, a thin cla y
lense at 4 and 9 ft . 11 15
Gravel, sandy, fine to medium, subangular to sub -
rounded, poorly sorted 7 22
Sand, medium to fine gravel, well sorted in lenses 10 32
Gravel, fine to coarse ; contains some sand and
gravel 27 59
Fort Union Group :Clay, dark-greenish-gray, contains lignite flakes--- 11 70
125
155-89-32aaa
Altitude : 2,035 fee t
Material
Thickness
Dept h(feet)
(feet )
Glacial drift :Sand, medium to coarse, reddish-brown, subangular t o
subrounded, contains some fine to medium gravel 23
23Gravel, fine to coarse, sandy, reddish-brown 15
38Till, olive-gray 34
72Tongue River Formation :
Shale, variegated greens, grays, and dark-browns, anddark-greenish-gray, carbonaceous, fine sand 28
10 0
155-89-35aaa
Altitude : 2,030 fee t
Glacial drift :Loam, sandy, black 2
2Sand, fine to medium, silty, yellowish-gray 3
5Till, dusky-yellow, oxidized 14
19Gravel, fine to coarse, sandy, angular to subrounded ,
most pebbles are iron stained 20
39Tongue River Formation :
Leonardite, black 2
41Shale, variegated grays and greens, contains a fe w
black and brown carbonaceous beds 19
60
155-90-3aa a
Altitude : 2,135 fee t
Glacial drift :Loam, pebbly, black 1
1Till, dusky-yellow, oxidized 9
10Till, moderate-olive-brown, oxidized 35
45Till, olive-gray ; contains a few streaks of peaty
clay, and small particles of wood and roots 169
214Sand, fine to very coarse, gravelly, poorly sorted ;
interval is predominantly coarse sand 7
22 1Tongue River Formation :
Shale, silty and sandy, variegated 19
24 0
155-90-12ddd
Altitude : 2,090 feet
Glacial drift :Loam, silty and pebbly, yellowish-gray 2 2Silt, clayey and clay, yellowish-gray, oxidized 21 2 3Clay, olive-gray 60 8 3Till, olive-gray ; contains a few thin lenses of
75 158gravel
Gravel, fine to coarse, moderately well-sorted in
22 180lensesTongue River Formation :
4 184Shale, sandy, brown, carbonaceous Sand, light-greenish-gray, with black and brown
5 189carbonaceous streaksShale, sandy and silty, light-olive-gray to light -
11 200greenish-gray
126
Geologi csourc e
155-92-23ccc
Altitude : 2,274 fee t
Geologi csource
Material Thickness De thfeet )(feet)
Glacial drift :Loam, pebbly, black 1 1
Clay, gravelly, yellowish-gray and dusky-yellow
(oxidized till?) 5 6
Till, reddish-dusky-yellow, oxidized 22 2 8
T:L11, moderate-olive-brown to light-olive-gray 31 5 9
Gravel, fine to medium, sandy, subangular, iron
stained 2 61
Till, olive-gray ° 83 144
Silt, clayey, sandy, light-olive-gray, calcareous 5 149
Gravel, fine to coarse, angular to subrounded, iro n
stained 5 X54Clay, sandy, white, calcareous 2 156
Tongue River Formation :Sandstone, fine, dark-greenish-gray, calcareous
3 15 9cementSand, fine, greenish-gray 14 17 3
Shale, silty, light-olive-gray -
7 180
155-93-5bd dN .D .G .S . auger hole
Till, oxidized 28 2 8
Silty clay, with pebbles, till(?) 32 60
Silty, very fine sand, grayish 3 63
Clay, gray, purplish 2 65
Silty sand 1 66
Cl ay, greenish 3 69
155-93-loba a(Log from Great Northern Railway an d
Baukol-Noonan Inc . )
Altitude :
2,395 feet
Sandy brown till, small boulders and gravel 26 2 6
Blue till 66 92
Gray clay with green tint 39 1 31
Hard coal .5 131 . 5
Gray clay with green tint 3 .5 13 5
Silty gray clay ° 57 192
Hard coal 1 19 3
Gray clay 17 210
l55-93-10bbb
Altitude :
2,416 feet
Road fill 4 4
Glacial drift :Till, yellowish-gray to moderate-olive-brown, oxidized 17 21
Gravel, fine to medium, sandy, poorly sorted, sub -
angular, iron stained 15 36
Fort Union Group :24 60Shale, light-gray to yellowish-gray, bentonitic
12 7
155-93-13aaa
Altitude : 2,365 feet
Geologicsource
Material Thickness Depth(feet) (feet)
Glacial drift :Loam, silty, pebbly, black 1 1Till, yellowish-gray to reddish-brown, oxidized 6 7Till, dusky-yellow grading to moderate-olive-brown
and light-olive-gray, oxidized 43 50Till, olive-gray 52 102
Fort Union Group :Sand, very fine, clayey and silty, yellowish-green 8 110Shale, silty and sandy, light-gray, light-olive-gray
42 152and medium-graySand, fine, silty, dark-greenish-gray 8 160Shale, silty, greenish-gray and brownish-black 18 178Lignite, black, fissile 2 180Clay, black, carbonaceous 2 182Shale, silty, light-gray 3 18 5Lignite, black 2 18 7Shale, silty, greenish-gray 10 19 7Sand, clayey to silty, greenish-gray 29 226Sandstone, fine, light-greenish-gray, calcareous
cement ° 2 228Sand, light-greenish-gray, well-sorted, subrounded 59 287Shale, silty, greenish-gray, platy 5 292Sand, light-greenish-gray, well-sorted, subrounded 32 324Clay, gray 5 329Sand, and carbonaceous shale, variegated, interbedded 11 340
155-93-23aaa(Log from E . H. Prather)
Topsoil 3 3Gravel 34 3 7Sand and gravel 3 4oGray clay 18 58Gray clay 12 70Brown sandy clay and gravel 13 83Yellow clay 24 107Brown clay and gravel 12 119Gravel, sand 2 121Gray clay, gravel 9 130Brown clay, gravel, some coal -
12 142Gray clay ° 42 184Gray sandy clay 29 213Gray sand, water 2 215
155-94-5bbb
Altitude : 2,232 feet
Glacial drift :Loam, silty, black 1
1Till, reddish-brown, oxidized 17
18Till, moderate-olive-brown, partially oxidized 28
46Fort Union Group :
Lignite, black, fissile 4
50Shale, medium-gray, light-gray, light-olive-gray,
30
80greenish-gray and yellow-gray, bentonitic
128
155-94-31dad
Altitude : 2,005 feet
Geologicsource
Material
Thickness
Depth(feet)
(feet )
Glacial drift :Loam, silty, black 1
1
Till, grades from dark-yellowish-gray through dusky-yellow to light-olive-gray, oxidized 24
2 5
Fort Union Group :Limestone, gray 4
2 9Shale, silty, reddish-yellow-brown ; contains some
lignite 11
4oSand, very fine to fine, clayey, medium-gray to dark
greenish-gray, micaceous and lignitic ; and light -gray, bentonitic shale 20
60
155-94-32bcb
Altitude : 2,025 fee t
Glacial drift :Loam, silty, black4111, yellowish-gray, oxidized Till, moderate-olive-brownTill, olive-gray
Fort Union Group :Silt, medium-light-gray, calcareous ; contains lenses
of white and gray limestoneSilt, brown, ligniticSilt, medium-light-gray, calcareousShale, dark-greenish-gray ; lignitic from 65 to 72 ft .
156-89-6aab
Altitude : 2,138 feet
Glacial drift „Loam, silty, blackSilt, sand, and gravel, yellowish-gray to reddish -
brownTill, yellowish-gray to moderate-olive-brown ,
oxidizedClay, light-olive-gray and olive-gray, laminated ;
contains lenses of silt, and very fine sand, als osome gypsum crystals
Sand, light-gray, well-sorted, subrounded, lignitic
Gravel, fine and medium, moderately well-sorted, sub angular to subrounded
Clay, silty, light-olive-gray and olive-gray ,laminated
Till, olive-graySand, medium, well-sorted, subroundedGravel, fine, sandy, moderately well-sorted, sub -
roundedSand, medium; contains many lignite chips of various
sizes
Gravel, fine to coarse, moderately well-sorted ; predominantly limestone pebbles, but also contain sas much as 20 percent pyrite, marcasite, andpyritiferous lignite
Fort Union Group :Shale, silty, light-gray Silt, white to medium-gray Shale, silty, medium-gray; interbedded with white
bentonitic,silty shale
129
14
1 5
25
556
19
1
520
4 5
505 56 180
1 1
7 8
8 16
28 4 48 52
4 56
80 136
1 3 X496 15 5
-
39 194
74 268
9 277
4 2815 286
14 300
(log from E . H . Prather)
Geologi c source
Material Thickness
litEgi(feet)
feet )
Gray clay 5
5Brown clay ' 5
10Gray clay, rocks and gravel 69
79Rock, gray clay, gravel (small seep of water) 16
9 5Gray clay, rock and gravel 123
218
156-89-24daa
Altitude : 2,180 feet
Glacial drift :mavel, fine to very co=se ' sandy, reddish-brown ,
poorly sorted, angular to subrounded 25
2 5Till, dusky-yallow to moderate-olive-brown, oxidized 4
29Till, olive-gray 24
53uu* , cl yer olive-gray; contains very fine sand
lenses o^
nFort Union Group :
o=* 'in" yellowish-green, micaceous, oxidized 18
95male
yell= gray, green, and black 10
10 5Lignite, black 1
IomSand, clayey, dark-greenish-gray 14
120
156-90-3bba
Altitude : 2,268 fee t
Glacial drift :Till, yellowish-gray, oxidized 14
14Till, moderate-olive-brown, oxidized 9
23Gravel, clayey, iron-stained, poorly sorted 14
37Till, moderate-olive-brown and olive-gray, partly
oxidized 16
53Till, gravelly, olive-gray
' 7
mTill, olive-gray 4o
100Till, moderate-olive-brown, oxidized 10
110Till, olive-gray 32
142Fort Union Group :
Shale, silty and sandy, medium-gray to dark-greenish gray, interbedded with thin bentonite and siltston elenses 31
173Lignite, black '--'-' ' ' '
3
176
(Log from E . H . Prather )
Gray clay and gravel 19
19Sand and gravel 25
44Gray clay and rock 43
8 7gravel 1
88
130
156-90-4abb
Altitude : 2,225 feet
Geologicsource
Materia l
Glacial drift :Sand, clayey and gravelly, brown, poorly sorted Gravel, fine to medium, brown, well-sorted Till, moderate-olive-brownSand, fine, clayey to silty, olive-grayGravel, fine to coarse, moderately well-sorted in
lenses, angular to subroundedClay, sandy, olive-gray, till(?)Clay, olive-grayTill, olive-gray
Fort Union Group :Shale, silty, light-greenish-grayLimestone, gray °Clay, sandy, dark-greenish-gray to olive-gray ; con -
tains carbonaceous streaksLignite, black, fissile
156-90-4bab
Altitude : 2,320 fee t
Glacial drift :Gravel, fine to coarse, sandy 24 24
Till, olive-gray 10 34Boulder, granitic 3 37Till, moderate-olive-brown to light-olive-gray,
30 67oxidizedTill, olive-gray 23 90Silt, clayey to sandy, olive-gray 16 106
Fort Union Group :Shale, medium-gray 6 112
Lignite, black, fissile 2 11 4Shale, medium-bluish-gray 20 134Lignite, black, fissile 2 13 6Shale, sandy, dark-greenish-gray 4 140
156-90-15bbb
Altitude : 2,176 fee t
Glacial drift :Gravel, fine to coarse, poorly sorted, subangular t o
subrounded 14 14Till, moderate-olive-brown 17 3 1Till, olive-gray 39 70
Fort Union Group :Shale, silty to sandy, medium-gray and light -
greenish-gray 10 8 0
Sandstone, fine, light-greenish-gray 1 8 1
Shale, silty, greenish-gray 19 10 0
131
Thickness
Dept h(feet) (feet )
6 66 12
11 2 312 35
24 595 645 69
39 108
13 12 13 12 4
12 13 64 140
156-90-19dac(Log from E . H . Prather )
Geologi csource Material Thickness Depth
(feet )(feet )
Brown clay 2 2Sand and gravel 13 1 5Brown clay 31 46Muddy sand and gravel 38 84Gray clay, sand and gravel 24 108Gray shale 42 150Gray sandy shale 2 152Gravel and sand 2 154Gray water sand 3 157
156-90-19ddd
Altitude : 2,161 fee t
Glacial drift :Spil, black 1 1Silt, sandy, yellowish-gray to reddish-brown 6 7Till, yellowish-gray, oxidized 23 3 0Till, olive-gray 35 65Till, olive-gray; contains thin lenses of sand 10 75Till, olive-gray 63 13 8Sand, coarse, gravelly, light-brown, subrounded 4 142Till, olive-gray 18 16 0
Fort Union Group :Shale, silty, medium-gray, brownish-gray, and
13 173brownish-black, carbonaceous Sand, fine, light-greenish-gray to greenish-gray ;
contains some brown carbonaceous streaks 7 18 0
156-90-26bbc
Altitude : 2,155 feet
Glacial drift :Till, yellowish-gray to moderate-olive-brown,
oxidizedTill, olive-gray
Fort Union Group :Shale, silty, light-olive-gray to olive-gray,
laminated ; contains streaks of white bentoniticshale
156-91-2cc c
Altitude : 2,184 feet
Glacial drift :Sand, medium to coarse, well-sorted 10 10Till, moderate-olive-brown, oxidized 14 24Clay, olive-gray ; contains lenses of silty clay and
116 140sandy clay and a few rocks, till(?)Silt, sandy and clayey, olive-gray, lignitic 24 164Till, olive-gray 14 178Gravel, fine to medium, sandy 34 212
Fort Union Group :Shale, silty, greenish-gray 10 222Sand, clayey, olive-gray 11 23 3Shale, medium-gray 7 240
132
12
1257
69
51
120
156-91-3cbb
Altitude : 2,220 feet
Geologicsource
Material
Thickness
Depth
feet
(feet)
Glacial drift :Till, yellowish-gray to dusky-yellow, oxidized 10
10
Till, moderate-olive-brown 15
2 5
Till, olive-gray 108
133
Gravel, moderate-olive-brown 3
136
Till, olive-gray ° 25
161
Gravel, fine, sandy, subangular to subrounded, pre -
dominantly limestone pebbles 2
16 3
7111, olive-gray 52
21 5
Fort Union Group :Shale, silty to sandy, light-greenish-gray to light -
olive-gray 15
230
Iimestone, gray 2
23 2
Sand, very fine, silty, light-olive-gray; contains a
white sandy clay bed 8
24 0
156-91-4cb c
(Log from Paulson, 1954 )
Glacial drift :Clay, yellowish-gray 7
7Clay, medium-gray, silty, uniform . Appears to be
lake deposits 55
62
Till, medium-gray, sand; few pebbles 126
188
Gravel, fine, and very coarse sand . Hard drilling 24
21 2
Till(?), samples consist mostly of very coarse san d
and carbonaceous clay 12
224
Fort Union Group :Shale, light-gray 6
230
156-91-4ccc
(Log from Paulson, 1954 )
Glacial drift :Clay, gray 3
3Sand 1
4
Clay, gray, and gravel ° 5
16Till, yellowish-gray 7Till, gray 38
54
Sand, fine, and clay, gray . About 50 percent sand 28
82
Sand and gravel, cleaner than material from 54 to 82
ft . 9
9 1
Till, gray 55
146
Fort Union Group :Lignite 1
147
Shale, light-gray, sandy 13
160
133
156-91-5aaa(Log from Paulson, 1954 )
Geologi csource
Material
Glacial drift :Clay, yellowish-grayTill, yellowish-graySand, fine, clayeyTill, gray . Boulders at 72 and 78 ft .
Fort Union Group :LigniteShale, light-grayLignite --------------------------------- -
156-91-5cbb
Altitude : 2,240 fee t
Glacial drift :T111, yellowish-gray to dusky-yellow, oxidized
Till, dusky-yellow, oxidizedTill, moderate-olive-brown, oxidized Till, olive-grayTill, white, pink and salmon colored, oxidized
Till, olive-grayClay, sandy, white, calcareous Sandstone, greenish-gray Till, olive-gray
Fort Union Group :Shale, silty, light-olive-gray Lignite, black, fissileShale, light-gray to black, carbonaceous
156-91-5daa
Altitude : 2,180 fee t
Glacial drift :Loam, silty, black 2 2Till, yellowish-gray to moderate-olive-brown,
12 14oxidizedTill, olive-gray 11 2 5Clay, light-olive-gray; interbedded with silt and
35 60fine, sandy clayTill, olive-gray 18 7 8Sand, very fine, clayey, olive-gray 7 8 5Till, olive-gray 34 119Clay, silty, olive-gray 11 130Till, olive-gray 56 18 6Gravel, fine, sandy, subangular to subrounded ; pre -
18 204dominantly limestone, remainder principallylignite and shale pebbles
Till, olive-gray ; contains a few thin sand and gravel154 358lenses
Sand, fine, clayey, light-olive-gray, calcareou s(possibly Fort Union sediments) 14 372
Fort Union Group :
11 383
Silt, light-olive-gray, with thin beds of brownish -black, carbonaceous sand
Lignite 7 390Shale,
silty, light-gray ; contains thin blackcarbonaceous clay and lignite beds 16 406
Lignite, clayey, black, oily 3 40 9Sand, fine, clayey, greenish-gray to black 11 42 0
134
Thickness
Depth(feet )
162 5
1 525
153
(feet )
1641
568 1
828 79 0
26 2 612 3812 5045 9518 11323 1361 1371 138
52 190
24 21 4
3 2173 220
156-91-9bbb
Altitude : 2,260 fee t
GeologicThickness alsource
Material ftfeet )fee t
Glacial drift :Till, yellowish-gray and dusky-yellow, oxidized 14 14
Sand, fine to medium, brown, well-sorted, subrounded 5 19
Till, olive-gray 6 2 5Silt, moderate-olive-brown and light-olive-gray,
27 5 2laminatedTill, olive-gray 78 1 3 0
Fort Union Group :Sand, clayey, white, yellowish-gray, yellowish-green,
29 15 9and dusky-yellowShale, silty, greenish-gray 10 169
Lignite, black, fissile 5 169Shale, medium-gray 6 180
156-91-9dad
Altitude : 2,292 fee t
Glacial drift :Till, yellowish-gray to moderate-olive-brown ,
oxidized 38 38Till, olive-gray 22 60
Silt, moderate-olive-brown, calcareous 20 80
Silt, sandy, moderate-olive-brown, calcareous 22 102
Till, olive-gray ° 64 166
Fort Union Group :Sand, very fine to fine, clayey, yellowish-green,
oxidized 15 18 1
Shale, silty, medium-gray 24 20 5Lignite, black, fissile 2 20 7Shale, silty, medium-gray 13 220
135
156-91-10bbb
Altitude : 2,303 feet
Geologicsource
Material
Glacial drift :Loam, pebbly, dark-yellow-brownTill, yellowish-gray, oxidized Silt, clayey to sandy with some pebbles and rocks ,
yellowish-gray, oxidized Sand, very fine to fine, well sorted, subrounded ,
some silty streaks, dry Silt, clayey, sandy in upper portion, dusky-yellow to
moderate-olive-brown, oxidized Sand, very fine and fine, very silty with streaks o f
clay, light-olive-gray to olive-gray Clay, silty, olive-gray Silt, clayey, olive-gray ; contains streaks of very
fine sandSand, very fine and fine, interbedded with silt an d
clay, light-olive-gray to olive-gray Sand, medium, well-sorted, subrounded, quartzose Gravel, fine to coarse, sandy, moderately well-sorted
in lenses, generally subangular, about 25 percen twell rounded
Till, very sandy and gravelly, olive-gray Till, silty, olive-gray, contains many specks o f
lignite, pebbles mainly limestone Till, olive-graySand, fine,
medium-gray, moderately sorted Clay, silty, olive-gray, till(?)Sand, with gravel
Sentinel Butte Formation(?) :Silt, light-gray, highly calcareous Shale, medium-graySand, fine, greenish-gray, slightly friable Shale, olive-gray and dark-greenish-graySand, fine, greenish-gray to dark-greenish-gray ,
carbonaceous
156-91-llodc
(Log from Paulson, 1954 )
Glacial drift :Till, pale-yellowish-brown, sandyTill, medium-grayTill, moderate-yellowish-brown Till, light-gray
Fort Union Group :Clay, light-gray, sandy
136
Thickness Depth(feet)(feet )
1 16 7
14 21
19 40
14 54
18 72
7 79
18 97
11 108
6 114
17 13112 143
113 25636 292
11 30 35 30 8
10 318
4 32 2
4 32 64 3304 33 4
6 340
27 2755 826 88
43 1 31
9 140
156-91-13baa(Log from Paulson, 1954)
Geologicsource
Material Thickness Depthfeet (feet )
Alluvium and glacial drift :Soil, dark-brown 1 1may, graY-' 2 3Clay, grayish-white .
Contains alkaline salts 4 7Till, yellowish-gray 4 11Till, gray ; much sand and gravel 112 12 3Sand and gravel, hard, drills like cemented gravel 12 13 5
Fort Union Group :Shale, light-gray 4 13 9Shale, dark-brown 1 140
156-91-14aaa
Altitude :
2,197 fee t
Road fill 9 9Glacial drift :
Till, moderate-olive-brown, oxidized 20
, 2 9Till, olive-gray 25 514Sand, medium to very coarse, gravelly, subangular to
subrounded 9 63Till, olive-gray 177 2140
Fort Union Group :S :Llt, olive-gray and light-olive-gray, calcareous 20 260Sand, fine, silty, olive-gray, calcareous 20 280Sandstone, light-olive-gray, calcareous cement 4 2814
156-91-16acb(Log from Paulson, 1954 )
Glacial drift :Soil 1 1Till, yellowish-gray 18 19Till, light-gray • 35 54Till, yellowish-gray 27 8 1
Fort Union Group :Shale, gray, sandy 9 90
156-91-16bbb(Log from Paulson, 1954)
Glacial drift :Soil, dark-brownTill, yellowish-gray 41 4 1Till, light-g ray, sandy 21 6 4
Sand, medium; much clay 5 6 9Till, light-gray, sandy 33 102Till, yellowish-gray 24 126Till, gray, hard 11 13 7
Fort Union Group :3 14 0Shale, light-gray
13 7
156-91-16cc a(Log from Paulson, 1954 )
Geologicsource
Material Thickness
Depth
(feet)
fee t
Glacial drift :Soil, brown 2
2
Till, yellowish-gray 16
18
Sand 2
2 0
Till, yellowish-gray 18
3 8
Sand and gravel 10
48
Till, yellowish-gray 29
77Till, gray, harder than above 29
I0 6Fort Union Group :
Shale, light-gray, sandy 9
115
Shale, light-gray, clayey 30
14 5
Shale, light-gray, hard 12
15 7Lignite 2
15 9Shale, light-gray, clayey 49
20 8
Indurated rock, probably concretion 1
20 9
Shale, light-gray, hard 39
248Shale, brown 2
25 0
156-91-19aaa
Altitude :
2,317 fee t
Glacial drift :Gravel, sand, silt, and clay, yellowish-gray an d
dusky-yellow, interbedded, oxidized 11 11Till, moderate-olive-brown, oxidized 11 2 2Till, olive-gray 41 63Clay, olive-gray (no inclusions) 9 72Till, olive-gray 12 84Till, olive-gray and gravel 10 94
Fort Union Group :Shale, yellowish-gray, yellowish-green, and light -
26 120gray, interbedded
156-91-20ddd
Glacial drift :Soil,
(Log from Paulson, 1954 )
dark-brown------ 1 1Till, yellowish-gray 20 2 1Sand and gravel 6 2 7Till, yellowish-gray 33 6 0Till, light-gray 6 6 6
Fort Union Group :Shale, light-gray 4 70
138
156-91-21cba 2(Log from Paulson, 1954 )
Geologi csource
Material
Glacial drift :soilClay with cobbles (till)Sand, medium to coarseGravel, fine, clayeySand, medium to coarse ; mostly shale fragmentsSand, medium to coarse ; mostly shale fragments ,
clayey °Clay and sand-°°
Fort Union Group :Clay, gray, tough ° °Sand, clayeyClay, grayClay, brownClky, gray, sandySand, gray, clayey ; hard and soft layers Sandstone, gray, fine
156-91-21ccal(Log from Paulson, 1954 )
Glacial drift :Soil, black 2
2
Till, yellowish-gray 45
47Fort Union Group :
Shale, yellowish-gray 11
58
Shale, light-gray 12
70
156-91-21cca2(Log from Paulson, 1954 )
Glacial drift :Soil, dark-brown 2
2
Till, yellowish-gray 2
4
Sand 3
7Till, yellowish-gray 42
49Fort Union Group :
Shale, yellowish-gray 5
54
Shale, light-gray 6
6o
156-91-22dc d(Log from Paulson, 195 4)
Glacial drift :Soil, dark-yellowish-brown 3
3Till, yellowish-gray 25
2 8Fort Union Group :
Shale, light-gray 12
40
139
Thicknes sfeet
feet
1
113
144
184
22
8
30
8
3827
6 5
49
11 44
118
35
15 37
16 0
l0
170
5
17525
200
156-91-22ddc
(Log from Paulson, 1954 )
Geologi csource
Material
Thickness
Depthfeet
(feet)
Alluvium and glacial drift :Soil, dark-brownClay, brownSand, very coarseGravel, very fine to coarse ; average diameter about
* inchClay, carbonaceous, dark-brown ; contains bits of
vegetationFort Union Group :
Shale, light-gray
156-91-22ddd1
(Log from Paulson, 1954 )
AJJ uvium and glacial drift :Soil °° ° 1
1clay 2
3Sand, very coarse 2
5Till(?), yellowish-gray, much very coarse sand 5
10Till, yellowish-gray 5
15Till or lake clay, grayish-orange, contains small
amount of pebbles or sand (could also be weathere dshale, more orange than oxidized till) 7
2 2Fort Union Group :
Shale, light-gray (streak of dark brown clay an dlignite from 24-26 ft .) 8
30
156-91-22ddd 2(Log from Paulson, 1954 )
Alluvium and glacial drift :Soil, dark-brown 1
1Clay, brown 2
3Sand, fine to medium 4
7Till, yellowish-gray 13
20Till, yellowish-gray, much sandier than above= 27
47Fort Union Group :
Shale, light-gray, sandy 3
50
156-91-23cc c(Log from Paulson, 1954 )
Alluvium and glacial drift :Soil, dark-brown 1
1Clay, yellowish-gray 2
3Sand, medium to coarse 2
5Sand, very coarse 3
8Gravel, very fine to coarse ; average diameter about
* inch 8
16Till, yellowish-gray 58
74Fort Union Group :
Shale, brown ° 2
76Shale, light-gray 1
7 7Lignite °' 1
78Shale, light-gray 2
8 0
140
1
12
32
5
5
10
4
14
6
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156-91-27cbb
(Log from Paulson, 1954 )
Geologi csource
Material
Thickness
le tLR;7EY--
feet
Alluvium and glacial drift :Soil, brown, sandy 1 1Clay, brown 2 3Gravel 2 5Cobbles ; average diameter 2 to 3 inches 5 10
Sand and gravel 4 14Till, yellowish-gray, sandy 64 78
Fort Union Group :Shale, light-gray 12 90
156-91-27coh(Log from Paulson, 1954 )
Alluvium and glacial drift :Soil 1 1clay 3 4Sand, very coarse, and gravel 6 10Gravel, very fine to coarse 6 16Till, medium-gray 12 28Till, yellow, gray, and orange (streaked) ; very sandy,
appears to be a weathered zone, shows evidence ofgreater weathering than in the overlying till ;contains limonitic nodules 21 49
Fort Union Group :Shale, light-gray °---°-°---- 11 60
156-91-27cc c
(Log from Paulson, 1954 )
Alluvium and glacial drift :Sand and gravel 5 5Gravel 4 9Till, medium-gray 13 22Gravel 4 26Till, medium-gray 3 29
Fort Union Group :Shale, light-gray, core, about 5 percent recovery---- 11 40
156-91-28aba(Log from Paulson, 1954 )
Glacial drift :Till, yellowish-gray 60 60
Fort Union Group :
10 70Clay, yellowish-gray, silty Clay, light-gray 10 80Silt, pale-brown 10 90Silt, yellowish-gray 20 110Silt, dark-brown, carbonaceous 10 12 0Silt, light-gray ° 10 130Clay, dark-brown, carbonaceous 10 140Clay, light-gray, silty 10 150Sand, very fine, clayey, loosely consolidated 12 162Sand, very fine to fine, relatively clean, loosel y
consolidated 11 173Sand, very fine, clayey 27 200
142
Geologicsource
Material
156-91-28bacl
(Log from Paulson, 1954 )
Glacial drift :Clay, yellow, sandy
Fort Union Group :Clay or shale, grayShale, greenShale, grayShale, gray, sandySandstone, fineShale, gray, sandySandstone, fine, hardShale, gra y, sandySandstone, fine, hardShale, gray , sandySandstone, hardShale, gray, sandyShale, brown, sandyShale, gray
156-91-28bac 2
(log from Paulson, 1954 )
Glacial drift :Soil, dark-brownTill, yellowish-gray, sandy
Fort Union Group :Shale, light-grayLigniteShale, light-graySand and sandy clay, light-gray, and thin layers o f
hard sandstoneSand, cleaner than from 117 to 190 ft ., but, sample s
still contain much clay; washed sample obtaine dfrom pits consisted mostly of medium grained ,angular sand, about 75 percent or more quartz ;remainder consisted mainly of basic igneousrock fragments
Lignite °Shale, light-gray ; core obtained from 240 to 250 ft .
with about 60 percent recovery . Consisted mostlyof light-gray clay-siltstone and 1 ft . of veryfine, dirty sandstone
LigniteShale, light-gray, with hard layers
143
Thickness
De thfeet feet
76 76
32 1086 1144 118
42 1602 1628 1701 17 1
14 18 53 188
17 20 52 20 7
28 23 53 23 81 23 9
1 1
71 72
20 92
2 9423 11 7
73 190
46 23 61 23 7
37 2741 275
75 350
156-91-28ccc
(Log from Paulson, 1954 )
Geologicsource
Materia l
Alluvium and glacial drift :soilSand, medium to coarse---'---'—' ' 'Till, yellowish-gray '
Fort Union Group :Shale, yellowish-grayShale, light-gray
--'—'—'--' 'oano light-gray, very fine to fine, much clay 'Lignite
Clay and sand, very fine, light-grayLignite
~~~~~.~~.~
.—243_~~-~~~~ ~Clay, sandy, gray ;
Shale, light-ora' not sandy ' 'Lignite
Shale
~~~~~~=~na~"~298 ft .
Lignite
Shale, light-grayLignite
Shale, light-grayLignite --'--" 'Shale, light-gray
156-91-29bb ^
(Lug from Paulson, 1954 )
Glacial drift :Soil, dark-brownTill, yellowish-gray, sandyTill, grayer than aboveTill, yellowish-gray, sandy
Fort Union Group: Clay, yellowish-gray '
Clay, very light-purplish-gray, 'Clay, yellowish-gray, sandyClay shale, light-gray, alternating with layers o f
sandy clayClay, very sandy, light-graySandstone, very fineSand, very clayey, light-graySandstone ,xano . very clayey (50 percent or more clay) —'Clay, light-gray, sandyclay , grayLignite
Clay, light-grayClay, brownish-gray '—'---'--' 'Lignite
'—'
~~-32bad
(Log from Paulson, 1954 )
Alluvium and glacial drift :_san dSand and gravel ' 'rol.yellowish-gray yellowish-gray Till, gray
Fort Union Group :Shale, light-gray, sandy
Thickness-TT;;Ty--
Depth(feet )
1 112 1332 4 5
95 14o20 mv52 2122 21 4
23 23 7
3 240248
16 mw3 26 7
54 54 30 12 30 3
12 31 52 31 711 3283 33 1
19 350
1 145 4 610 5 624 8 0
5 8 5
5 9013 10 3
92 19 529 22 44 22 8
18 24 63 249
41 290
5 29521 3162 3189 32 78 33 53 33 8
5 57 12
26 3815 53
27 8o
156-91-32bdal(Log from Paulson, 1954 )
Geologicsource
Material Thickness
Depth(feet) (feet )
Alluvium and glacial drift :4 4Sand
Gravel 10 14Till, yellowish-gray 14 2 8Till, medium-gray 28 56
Fort Union Group :Shale, light-gray 14 70
156-91-32bda2(Log from Paulson, 1954)
3 3Alluvium and glacial drift :
Soil and slopewash, dark-brown, clayeyTill, yellowish-gray 6 9
Fort Union Group :Shale, light-gray, clayey 3 12Shale, light-gray, sandy 8 20
156-91-33aca(Log from Paulson, 1954)
Alluvium and glacial drift :Soil, dark-brown 2 2Clay, sand, and gravel 3 5Sand, very coarse 4 9
Fort Union Group :Shale, clayey, yellowish-gray 11 20
156-91-33ba d(Log from Paulson, 1954 )
Alluviumand glacial drift :1 1Soil, brown, sandy
Clay, light-tan 1 2sand 5 7Till, yellowish-gray 49 5 6
Fort Union Group :4Shale, light-gray
156-9l-33bbc(Log from Paulson, 1954 )
Alluvium and glacial drift :1 1Soil, dark-gray, clayey
Clay, moderate-yellow, uniform ; probably lake14 1 5deposits
Sand, medium to coarse 7 22Fort Union Group :
8 30Shale, light-gray
145
156-91-33bb d(Log from Paulson, 1954 )
Geologi csource
Material
Thickness
De thfeet
feet
Alluvium and glacial drift :Soil, dark-brown, clayey Clay, yellowish-gray, with few pebblesSand, medium to coarse
Fort Union Group :Shale, light-gray, sandy
156-91-33bda 2
(Log from Paulson, 1954 )
Alluvium and glacial drift :Soil, dark-brown, clayey 1
1Clay, sand and gravel 2
3Gravel, fine to coarse ; average size about 3/8 inch ;
consists of limestone (about 1/2) ; granite (1/4) ;basic igneous concretions, and shale (1/4) 18
21
Fort Union Group :Shale, light-gray, sandy 29
50
156-91-33cab(Log from Paulson, 1954 )
Alluvium and glacial drift :Soil, dark-brown 1
1
Till, yellowish-gray 32
3 3Sand, fine 7
40Sand or sandy clay, yellowish-gray, soft 15
5 5Sand, coarser than from 40 to 55 ft . 5
6 0
Fort Union Group :Shale, dark-gray, clayey 20
8 0
156-91-33dad
(Log from Paulson, 1954 )
Glacial drift :Soil, brown 1
1Till, yellowish-gray 35
36
Till, medium-gray 3
39Sand and gravel 1
40
Till, medium-gray 38
78Fort Union Group :
Shale, gray, sandy 32
110
Shale, yellowish-gray 19
12 9Shale, light-gray, clayey 11
140
156-91-34bbb(Log from Paulson, 1954 )
Alluvium and glacial drift :Soil and slopewash 3
3Clay, tan 1
4
Sand and gravel 4
8Fort Union Group :
Shale, light-gray 12
2 0
146
3
36
99
18
2
20
v
;stw
rV
et'
Us
,.'s
156-92-20ddd(Log from Paulson, 1954 )
Geologi csource
Material Thickness De t hfeet(feet )
Glacial drift :Clay, yellowish-gray 3 3
sand 6 9
Till, yellowish-gray 25 3 4
Till, gray 36 70
Till, yellowish_gray 30 10 0
Fort Union Group :Shale, yellowish-gray 2 10 2
156-92-22cc c
(Log from Paulson, 1954)
1 1Glacial drift :
Soil, dark-brownTill, yellowish-gray 17 18
Till, gray 14 32
Sand, coarse 6 38
Till, gray 46 3 8Till, yellowish-gray 2 86
Fort Union Group :Clay, light-gray ° 4 90C lay, yellowish-gray 10 100
156-92-23cc c
Glacial drift :Soil,
(Log from Paulson, 1954 )
dark-brown 1 1
Till, light-yellowish-gray 34 35Sand, fine, clayey 6 4 1C lay, gray 5 46
Sand, clayey 4 50
Clay, dark-gray 6 56
Sand, clayey ° 8 64Till, Bray 38 102
Till, yellowish-gray 20 122
Fort Union Group :Shale, yellowish-gray, sandy 8 130
148
156-92-23ddd(Log from Paulson, 1954 )
Geologicsource
Material Thickness Depthfeet (feet )
Glacial drift :Soil, dark-brown 1 1Till, yellowish-gray 30 31Sand, medium to coarse 4 3 5Gravel, medium 5 40Gravel, fine to coarse ; average diameter about }, inch 12 52Till, gray-'-'-' 5 5 7Gravel, medium ; average diameter about 3/8 inch 11 68Till, gray and tan 7 75Sand, very fine, brawn, streaked with black carbon -
aceous zones 5 8 0Clay, dark-brown to black (as in soil), carbonaceous ;
pieces of carbonized wood 5 85Till, gray, very sandy 16 101Till, yellowish-gray 7 108Till, medium-dark-gray and brown 36 144
Fort Union Group :Clay, light-gray, sandy 16 160
156-92-24cbb(Log from Paulson, 1954 )
Glacial drift :Soil, dark-brown 1 1Till, yellowish-gray, sandy 18 1 9Till, medium-gray, sandy 10 2 9Sand, fine to medium 7 3 6Till, medium-gray '---' 49 8 5Till, pale-yellowish-Bray--
- 18 103Till, medium-gray, gravelly 27 130
Till or bedrock, medium-gray, sandy clay ; few pebbles 37 167Fort Union Group :
Shale, light-gray, moderately sandy 5 172
156-92-24ddd(Log from Paulson, 1954)
Glacial drift :Soil, dark-brown 1 1
C lay, yellowish-gray, sandy 2 3Sand 3 6Till, yellowish-gray, sandy 22 2 8
Till, gray '--
----" 90 118
Till, yellowish-gray 8 126
Ti11, BraY 28 154
Fort Union Group :Shale, yellowish-gray 6 160
156-92-26aca(Log from Paulson, 1954 )
Glacial drift :Clay, yellowish-gray, lake deposits 12 12
Till, yellowish-gray 3 15Sand ° 1 16
Till, yellowish-gray 26 42
LY11, gray 11 53Gravel, fine 4 57
Till, gray 13 70
149
156-92-26add(Log from Paulson, 1954 )
Geologicsource
Material Thickness Depthfeet (feet )
Glacial drift :Soil, dark-brown 1 1Clay, yellowish-gray, lake deposit 13 14Till, yellowish-gray, clayey 14 2 8Till, gray 48 76Till, yellowish-gray, bouldery 38 114
Fort Union Group :Clay, yellowish-gray, sandy 21 135
156-92-36ddd
Altitude : 2,328 feet
Glacial drift :Loam, gravelly, dark-brown 1 1Sand, fine to coarse, reddish-brown, subrounded 7 8Till, yellowish-gray, oxidized 6 14Till, dusky-yellow, oxidized 19 3 3Till, moderate-olive-brown, oxidized 35 68Clay and sand, variegated,predominantly green and
gray laminae (bedrock boulder?) 22 90Till, olive-gray 37 12 7Sand and silt, clayey, olive-gray, light-olive-gray ,
interbedded 39 166Gravel, fine and medium, dark-brown, moderatel y
well-sorted, angular to subangular 8 174Fort Union Group :
7 18 1Shale, silty, light-olive-gray, calcareous Sand, dark-greenish-gray, calcareous 12 19 3Shale, silty, light-olive-gray to light-greenish-gray 7 200
156-93-6dc d
Altitude : 2,263 feet
Glacial drift :Sand and gravel, iron-stained 8
8Till, yellowish-gray to moderate-olive-brown,
5
1 3oxidizedTill, olive-gray 32
4 5Fort Union Group :
Shale, silty, brownish-black, organic 6
5 1Lignite, black 2
5 3Shale, silty, medium-gray 7
60Sand, fine, clayey, greenish-gray 7
6 7Shale, silty, greenish-gray, fissile 13
80
150
156-93-10bbb(Lag from Great Northern Railway and
Baukol-Noonan Inc . )
Geologicsource
Material Thickness Depth(feet )feet
Sandy brown till 9 9Gravel - fair 5 14
Blue till, small boulders 40 54Gray clay with green tint 6 .5 60 . 5Hard coal .5 61
Gray silty clay with green tint 41 102
Hard opal 2 .5 104 . 5Gray clay with green tint 35 .5 140Hard coal 4 144
Gray silty clay with green tint 49 193Gray sandstone .5 193 . 5Gray silty clay with green tint 16 .5 210
156-93-llama
Glacial drift :Till, yellowish-gray to dusky-yellow, oxidized 8 8
Till, dusky-yellow to moderate-olive-brown, oxidized 37 45Till, olive-gray 35 80
Till, moderate-olive-brown, oxidized 20 } 100
Till, olive-gray 36 136Till(?), predominantly reworked bedrock (Fort Union) ,
clay and sandy clay with pebbles 14 150
Fort Union Group :8 158Shale, silty to sandy, greenish-gray
Lignite, black, fissile 4 162Shale, reddish-brown 4 166
Shale, silty and very fine sand, greenish-gray to
light-gray 14 180
156-93-15ccc
Altitude : 2,300 fee tGlacial drift :
Gravel, fine, reddish-brown, moderately well-sorted ,subangular to subrounded ; contains medium to very
coarse sand 5
5Till, yellowish-gray to dusky-yellow, oxidized 4
9Till, moderate-olive-brown, oxidized 7
16Till, olive-grey ° 26
42
Sentinel Butte Formation :18
60Shale, greenish-gray, noncalcareous
151
156-93-16cc c(Log from Great Northern Railway and
Baukol-Noonan Inc . )
Altitude : 2,300 fee t
Geologi csource Material Thickness De th
Sandy brown till with small boulders, some gravel
feet
37
feet )
37Silty gray clay with streaks of coal 29 66Gray clay with green tint 2 68Coal, hard 5 7 3Gray clay 8 8 1Silty gray clay 28 .5 109 . 5Coal - fair 2 .5 112Gray clay with green tint 21 13 3Gray sandstone .5 133 . 5Silty gray clay with green tint 12 145 . 5Coal - fair 3 148 . 5Silty gray clay with green tint 16 .5 16 5
156-93-25bbb(Log from Groat Northern Railway and
Baukol-Noonan Inc . )
Altitude :
2,240 feet
Sandy brown till 16 16Sandy blue till 92 10 8Blue till with some gravel and small boulders 12 12 0Blue till boulders 25 145
156-93-32bbb(Log from Great northern Railway and
Baukol-Noonan Inc . )
Altitude :
2,365 fee t
Sandy brown till - small boulders 35
3 5White clay 20
5 5Blue silty clay 16
71Orange and gray silt, clay 9
80
152
156-94-3aa(Log from Great Northern Railway and
Baukol-Noonan Inc . )
Geologicsource
Altitude :
2,120 feetMat e rial Thickness D h
Sandy brown till--some gravel and small boulders
feet
29
feet
29Boulder ° 1 30
Brawn till with small boulders 4 34
Blue clay 14 48
Woody coal 0 .5 48 . 5
Gray clay 37 .5 86
Woody coal ° .5 86 . 5Gray clay ° 9 .5 96
Woody coal .5 96 . 5
Gray claY ° ° 13 .5 110
Fair coal ° 3 113Dark brown clay 28 141
Very silty gray clay 35 176
Gray clay l0 186
Coal, woody .25 136 .2 5
Gray clay 3 .75 190Hard sandstone .5 190 . 5
Gray clay 19 .5 210
156-94-5ccb(Log from Great Northern Railway an d
Baukol-Noonan Inc . )
Altitude : 2,365 feet
Sandy brown till - small boulders Blue till - small boulders Tan and orange claySilty gray clay----' '----•Coal, hardSilty gray clay with green tintGray clay - green tintCoal, fairGrey. clay - green tintGray clay ' ' 'Coal - hardGray clay with green tintGray clay
2 6
3441646710713914015 717 117 520 722 5
153
156-94-10bba(Log from Great Northern Railway an d
Baukol-Noonan Inc . )
Altitude : 2,260 fee t
Geologi csource
Material
Thickness
Depth
Sandy brown till 27
2 7
(feet)
(feet )
Silty brown "la'-' 9
36Woody coal .5
36 . 5Brown silty clay 6 .5
43Gray clay 13
5 6.5
56 . 511
67 . 5Woody coal 1
68 . 5Gray clay- . 2 .5
71Hard gray sandstone 2
736
793
826
88Woody coal 2 .5
90 . 5Gray clay 6 .5
9 7Woody coal 1 .5
98 . 5Gray clay with green tint 55 .5
154Gray silty clay 16
170Woody coal
----'--'-'-' '
1
171Gray clay with green tint
---'--' '
14
18 5Woody coal 1 .5
186 . 5
(log from Great Northern Railway an dBaukol-Noonan Inc . )
Altitude :
2,260 fee t
Sandy brown till ' small boulders 37
3 7Blue till - small boulders 62
9 9Silty gray clay ' 16
115Lost circulation - drilled like coal 5
120Gray clay with green tint
' 15
13 5Gray clay 53
188Coal ' fair 4 .5
192 . 5Gray clay with green tint 17 .5
210
156-94-12ddd(Log from Great Northern Railway an d
Baukol-Noonan Inc . )
Altitude :
2,195 fee t
Sandy brown till, small boulders 19
19Blue
4o
59Large boulder 1
60Blue till, small boulders 38
98Blue clay
---' 55 .5
153 . 5Streak of woody coal .5
15 4Silty gray clay with green tint ' ' 17
171Gray clay with green tintCoal,
-hard
~~~~~~~~~~~~~~~
~
209
154
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156-94-24cbb
Altitude : 2,165 fee t
Geologi csource
Material
Thickness
De h
feet
feet
Glacial drift :Till, moderate-olive-brown, oxidized 21
2 1Fort Union Group(?) :
Lignite, fractured (may be reworked) 5
2 6Clay, yellowish-brown 11
3 7Lignite, slack(?) ; lost circulation at 38 ft . 1
3 8Missing 2
4o
156-94-24cbd
Altitude : 2,173 feet
Glacial drift :Loam, dark-brown 1
1Till, yellowish-gray to brown, oxidized 6
7Till, moderate-olive-brown, oxidized 31
38Clay, silty, yellowish-greenish-gray, partiall y
oxidized 9
47Clay, silty, olive-gray, calcareous 8
55Sand, coarse, well-sorted, subangular 4
59Clay, silty, medium-gray, olive-gray and olive-black ,
calcareous 64
123Clay, silt, and fine to medium sand, interbedded 18
141Sand, medium to coarse, gravelly 33
174Gravel, fine, sandy, subangular 17
191Fort Union Group(?) :
Shale, medium-gray ; contains thin bentonitic seams 23
214Shale, silty, light-gray 6
22 0
157-88-36bbb
Altitude : 2,342 fee t
Glacial drift :Clay, silty, yellowish-gray, oxidized 7 7Clay, silty, yellowish-gray to moderate-olive-brown ,
oxidized 31 38Till, moderate-olive-brown, oxidized 4o 78Till, olive-gray 88 166Till ,
mediumolive-gray ; contains numerous lenses of fine to
sandy gravel 49 215Till, olive-gray 30 24 5Silt, clayey and sandy, olive-gray 17 262 'Till, moderate-olive-brown, oxidized 19 28 1Till, very sandy, moderate-olive-brown, oxidized 19 30 0Till, olive-gray 20 320
Fort Union Group :Sand, very fine, clayey to silty, olive-gray, cal -
8 328careous, micaceousShale, light-to medium-gray 4 332Sand, clayey, dark-greenish-gray 8 34o
156
157-89-20adc
Altitude : 2,172 feet
Geologicsource
Material
Thickness
De th
feet
feet )
Glacial drift :Loam, pebbly, black 1
1Till, yellowish-gray, oxidized 5
6Till, moderate-olive-brown, oxidized 24
30Till, olive-gray ; contains streaks of moderate-olive
brown oxidized till 23
5 3Till, olive-gray, contains a few thin gravel and sand
lenses 22
75Silt, light-olive-gray to olive-gray ; grades downward
into olive-gray to dark-greenish-gray, very fine ,silty sand 13
88Sand, fine to medium ; contains a few lenses of dark-
greenish-gray, very fine, clayey sand and silt .May be a preglacial post Fort Union deposit 75
163Fort Union Group :
Sand, very fine to fine, greenish-gray ; containsblack and brown carbonaceous zones and is inter -bedded with carbonaceous clay 22
185Shale, silty and sandy, medium-gray, light-greenish -
gray to dark-greenish-gray and brownish-black 15
20 0
157-89-3odcb(Log from E . H . Prather )
Brown shale 5
5Brown sand 25
30Sand and gravel 8
38Clay and gravel ° 14
52Rolling sand (water) 22
74Gray clay 6
80Coal, water 2
82
157-90-14cad(Log from E . H . Prather )
Topsoil °°° ° 2
2Gravel sand 8
10Yellow sand 17
27Gray clay 8
3 5Brown sand 20
5 5Brown sandy shale 4
59Coal, water 5
64Light-gray clay 5
69Garay sandy shale 1
70
157
157-90-15bbb
Altitude : 2,270 fee t
Geologi csource
Material Thickness Dept h(feet) (feet )
Glacial_ drift :Gravel, fine and medium, sandy, subrounded 4
Clay, sandy, yellowish-gray 2 6
Gravel, sandy , poorly sorted '-' ' = ?Gravel, fine and medium, sandy, moderately well -
sorted in lenses 12
Till, moderate-olive-brown to olive-gray, partiall y
oxidized 9 ;0
Fort Union Group :
90Shale, silty, and clayey, fine sand ; various shade s
of yellow, green, and gray Shale, silty to sandy, medium-gray to dark-greenish-
gray ; contains black and brown lignitic lenses---- `%2
157-' 2-22dda
Altitude : 2,200 fee t
Glacial drift :Sand, gravel, and cobbles, poorly sorted, heavil y
irea stained to 36 ft .
- 157-90-33bbb
Altitide : 2,227 fee t
Glacial drift :Till, yellowish-gray, oxidized
Gravel . reddish-brown, subangular, iron stained
Till, olive-gray °Fort Union Group :
Clay and silt, variegated ,partially oxidize I
Shale, greenish-gray; contains lignite seams
157-90-3 ld,- ~(Log from E . H . Pratrler )
Brown clay and gravelGray shale, sand and rocks, trace of water
Gray shale and gravel °
Brown sand and gravel r
Black sand and coalGray shale, gravel and sand
Gray sandy shale`Gray shaleCoal and water `
158
157-91-llddd
Altitude : 2,320 feet
Geologi c source
Material Thickness
Depth(feet)
(feet)
Glacial drift :Loam, pebbly, black 1
1
Till, moderate-olive-brown, oxidized 26
2 7
Till, olive-gray ; contains oxidized moderate-olive -brown streaks 15
42
Till, olive-gray 13
5 5Gravel, fine and medium, sandy, subangular to sub -
rounded 4
59Till, olive_gray 28
8 7Silt, clayey, and very fine sand, olive-gray 26
11 3Till, olive-€ ;raY 22
13 5
-ort Union Group :Shale, medium-gray, and greenish-gray, contain s
brownish-black carbonaceous layers 16
15 1
Sandstone, greenish-gray 3
7.5 4
Shale, medium-gray, calcareous 6
16 0
157-91-35baa(Log from Paulson, 1954 )
Glacial drift :Soil, blackClay, yellowish-gray °Till, yellowish-gray ^
Fort Union Group :ihale
157-91-36dd d
Altitude : 2,200 feet
Glacial drift :Sand, fine, silty, dark-brownish-gray 6
6
Till, clay, very silty, dusky-yellow to moderate -
olive-brown, oxidized 26
32
Till, silty, olive-gray, lignitic 40
72
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80
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101
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112
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170
;ravel, fine to very coarse, some cobbles, generall y
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192
Fort Union Group :Clay, highly carbonaceous, oily and lignitic ,
leonardite(?) 4
196
Shale, medium-to light-gray, slightly hard, cale :•.r -eons it
200
159
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157-93-lbbb
Altitude : 2,245 feet
Geologi csource_
Material Thickness Depth(feet )(feet )
Glacial drift :Sand, silty, yellowish-gray 3 3Till, dusky-yellow to moderate-olive-brown, oxidized 16 19Sand, very fine and fine to medium ,
dusky-yellow to yellowish-green,clayey to silty ,interbedded 29 48
Fort Union Group(?) :10 58Clay, sandy, yellowish-green
Sand, very fine to fine, clayey, medium-yellowish -
3 1 89green, oxidized °Shale, light-to medium-gray 11 100
157-93-8daa 1(Log from Great Northern Railway and
Baukol-Noonan Inc . )
Altitude :
2,290 fee t
Gravel " ° 7 7Sandy blue till, small ':oulders 54 61Blue and orange sand till - silt(?) 76 137Silty blue till 58 195
l57-93-llbbb(Log from Great Northern Railway and
Baukol-Noonan Inc . )
Altitude : 2,335 fee t
Sandy brown till, small rocks 29 29Silt, brown and gray 6 3 5Tan and gray clay 5 40Woody coal 6 .5 46 . 5Gray clay, green tint 10 .5 5 7Soft coal 1 58Silty gray clay ° 22 80Brown clay 6 86Hard gray clay with green tint 35 12 1
157-93-llda a
Altitude : 2,260 feet
Glacial drift :Till, yellowish-gray to dusky-yellow, oxidized 25
2 5Fort Union Group :
Shale, silty, medium-gray to greenish-gray 7
32Lignite, black, fissile 2
34Sand, very fine to fine, greenish-gray to brownish -
black, well sorted, subrounded, carbonaceous i nlayers 26
60
162
157-93-15dcc 3(Log from E . H . Prather )
Geologicsource
Materia l Thickness
De th
(feet)
feet )
Brown sand and gravel, mixed clay 30
30
Small trace of water 2
32
Gray clay, rock and gravel 50
82
Gravel (water) 13
95
157-93-21aaa
Glacial drift :Clay, silty and sandy, yellowish-gray, oxidized 4
4
Till, dusky-yellow, oxidized 18
22
Till, moderate-olive-brown to light-olive-gray ,
partially oxidized 28
50
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5 2
Till, olive-gray 10
62
slightly sandy, yellowish-green (reworke d
bedrock?) 4
66
Clay, yellowish-gray (reworked bedrock?) 3
69
?rave L, fine,and medium to very coarse sand, dark-brown, angular to subangular, heavily iro n
stained 6
75
Fort Union Group :Silt, clayey to sandy, laminae of various light
shades of gray, green, and yellow 21
96
Shale, greenish-gray 5
101
Silt, clayey and very fine sand, buff, laminated 16
117
Shale, gray 3
120
157-93-28cc c
Altitude : 2,115 fee t
Glacial drift :Eoam, sandy, black 1
1
Silt, sandy, yellowish-gray, calcareous 1
2
Gravel, fine and medium, sandy, subangular to sub -
rounded 14
16
Till, olive-gray 42
58
Sand, fine to medium with some coarse, moderately
well-sorted in lenses, subrounded 70
Port Union Group :Sand, very fine to fine, silty and clayey, light -
olive-gray and olive-gray, micaceous and lierit''c--
40
110
[aonardite, black, oily 11
72 1
Sand, very fine, cleyey to silty, olive-era', 15
136
Male, light-greenish-gray to green'sr,-?rav 8
144
Silt and very fine sand, clayey, ligh t -greenish-gray ,
calcareous, interbedded 16
16 0
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l57-94-23bab
Altitude : 2,290 fee t
Geologi csource_
Material Thickness hPeet ( feet )
Glacial drift :Till, reddish-brain to moderate-olive-brown, oxidized 23 2 3
Fort Union Group :Shale, yellowish-green to light-greenish-gray and
olive-gray 17 40
157-94-25dba
Altitude : 2,090 fee t
Glacial drift :team, sandy, black 1
1Sand, very fine, silty, dark-gray 5
6Silt, clayey, yellowish-gray 8
14Clay, yellowish-green, and yellowish-gray 17
31Sand, fine, gray 2
33Clay, silty, light-olive-gray 8 41Gravel, fine to medium, moderately well-sorted, sub-
rounded 6
47Fort Union Group :
Shale, silty, light-gray to light-greenish-gray 12
59Lignite, black 1
60
157-94-26daa(Log from Great Northern Railway and
Baukol-Noonan Inc . )
Altitude :
2,110 feet '
Sandy brown till 19 19Brown silt ° ° 2 2 1Gray clay 10 3 1Tan and orange clay 5 .5 36 . 5Limestone .5 3 7Gray clay 3 40Gray clay with streaks of coal 28 68Coal, fair ° 4
- 72Gray clay 18 9 0
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158-90-29cc e
Altitude :
2,318 feet
Geologi csource Thicknes sMateria l
Glacial drift :Till, yellowish-gray, oxidized
(feet )
8
Till, moderate-olive-brown, oxidized 2 3
Till, olive-gray 5 9Till, moderate-olive-brown, oxidized 2 4
Till, olive-gray----- 4o
Fort Union Group :Shale, silty, light-gray 2 1
Lignite, black 3Shale, silty, greenish-gray . 4
Lignite, black, fissile 2
Shale, light-greenish-gray 5Shale, sandy, greenish-gray 11
158-91-5 c
(Log from E . H . Prather)
Brown elay 8
Gravel 4
Brown clay and gravel 3 4
Gravel 2 5
Brown sand and water 71
Gray shale 3
158-91-8bb.
(Log from E . H . Prather )
Brown sandy shale 30
Yellow sand 78
Hard sandstone 6Yellow sand 42
Yellow sand (partly red in color) 6
158-91-19ddd
Altitude : 2,359 feet
Glacial drift :Till, yellowish-gray to reddish-brown, oxidized
(reworked?) 9
9
Till, moderate-Olive-brown Sand, medium to coarse, yellowish-green, well-sorted 5
69
Till, moderate-olive-brown 31
100
Sand, silty and clayey, dusky-yellow to yellowish -green 32
132
Fort Union Group :Sand, medium, yellowish-green, well-sorted, sub -
angular, micaceous and lignitic 10
142
Sandstone, greenish-gray 2
144
Sand, medium, dark-greenish-gray 16
16 0
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Depthfeet)
8
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175178182184189200
8124 6
7 114 214 5
30108114156162
158-91-27add
Altitude : 2,328 feet
Geologi c source
Material
Glacial drift :Silt, clayey and sandy, yellowish-grayGravel, sandy, reddish-brownTill, moderate-olive-brown and light-olive-gray ,
partly oxidizedSand, medium to very coarse, moderately well-sorted ,
subangular to sabroundedGravel, medium to coarse, moderately well-sorted ,
subroundedTill, olive-grayGravel, fine to medium, sandy and clayey, poorly
sorted, subangularTill, moderate-olive-brownClay, silty to sandy with pebbles, •:aria ;:atedyellows ,
browns, grays, and greensRocks .
Fort Union Groip :Shale, silty, medium-gray and brownish-black ,
laminated `Lignite, black, fissileShale, olive-gray to olive-black
158-91-34bbb
Altitude : 2,332 fee t
Glacial drift :Loam, silty, dark-brownish-grayTill, yellowish-gray to dusky-yellow, oxidizedTill, olive-gray
Fort Union Group :Shale, light-greenish-gray, greenish-gray, and
medium-gray, interbedded
158-92-29aa a
Altitude : 2,223 fee t
Glacial drift :Clay, blackGravel, fine tc medi .:m, sandy, subangular to sub -
rc nieaTi11, ausky-yellow, ox_dizedGravel, fine tc me —am, satiy, moderately well-sorte d
in lenses, s .:ba :rular, iron stainedCiay, greenish .-gray, laminatesSang., fine to very coarse, some gravel, well-sorted
in lenses °Forr, Union Grc .:p :
Sara, 'ine, dark-greenish-grayCsy llak, oilyL gtc, black, fissileShale, silty, light-oliv,--gray to brownish-gray
171
Thickness Depth(feet )(feet )
4 45 9
11 20
6 26
6 326o 92
6 9834 132
47 1793 182
6 1882 190
16 206
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158-94-llbbb(Log from Great northern Railway an d
Baukol Noonan Inc . )
Altitude : 2,415 fee t
Geologicsource Material Thickness Depth
Ss•awy till, small boulders
feat
21
(feet)
2 1
Blue till, smell boulders 183 20 4
Silty gray clay 21 225
158-94-llcc c
Altitude : 2,434 feet
Glacial drift :Loam, silty, black 2 2
Till, yellowish-gray to moderate-olive-brown ,
oxidized 20 22
Till, olive-gray-•--
--° 76 98Till, yellowish-gray to moderate-olive-brown ,
oxidised •- 24 122
Fort Union Group :
47 169sand , very fine, silt and sandy clay, interbedded ,
yellowish-green and buff
Shale, greenish-gray 11 180
158-94-16bbb
Altitude : 2,305 feet
Glacial drift :Loam, silty and pebbly, black 2 2
Till, yellowish-gray to moderate-olive-brown ,
oxidised 16 18
Till,olive-gray • 15 33Clay, olive-gray to olive-black 3 36
Till, olive-gray-• 5 41
Santd, medium, gray, well-sorted • 6 47
Till, olive-gray ° 29 76Fort Union Group :
Sand, very fine to fine, greenish-gray to dark -15 9 1greenish-gray, calcareous
male, light-to medium-gray and greenish-gray 9 100
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159-94-24bbb(Log from Great Northern Railway and
Baukol-Noonan Inc . )
Altitude : 2,275 feet
Geologic_source
Material
Thickness
Depth
feet
(feet )
Sandy brown till, small boulders 62
62Blue till, some floating coal 13
75Blue till 62
13 7Silty grey clay with streaks of coal 26
16 3Gray clay, green tint 8
171Gray sandstone .5
171 .5Silty gray clay 33 .5
20 5Coal, hard ° 4 .5
209 . 5Silty gray clay ° 22 .5
232
159-94-34bbb(Log from Great Northern Railway and
Baukol-Noonan Inc . )
Altitude : 2,350 feet
Sandy brown till 17
17Blue till, small boulders, some floating coal 166
18 3Gray silty clay 3 .5
186 . 5Gray sandstone .5
18 7Silty gray clay'--° "---
23
210
159-94-34ccc
Altitude : 2,420 feet
Glacial drift :Loam, dark-brown 2
2Till, light-olive-gray 7
9Till, moderate-olive-brown, oxidized 4o
4 9Till, olive-gray 17
66Silt, clayey, light-olive-gray, laminated 16
82Till, olive-gray 59
14 1Gravel, medium to coarse 3
14 4Till, olive-gray 20
164Fort Union Group :
Silt and sandy clay, dusky-yellow to reddish-brown 13
177Shale, silty, light-gray 14
191Sand and sandstone, fine, ligh t-greenish-g ray 5
19 6Shale, light-gray 4
20 0
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161-89-5ac l(Log from LaRocque and others, 1963a )
Altitude : 1,957 feet
Geologi csource
Material Thickness Depth(feet )feet
Glacial drift :soil 2 2Clay, yellow 13 15Sand and gravel 3 18Clay, hard, gray 3 2 1Clay, with stones 7 2 8
Fort Union Group :Shale and lignitic shale 15 43Sandstone, gray 8 51Shale, hard, blue 27 78Lignite '-'-' '-"'--"' 3 8 1Shale, soft, with thin lignite beds 41 12 2Lignite '° 4 12 6Shale, hard, brown 4 130Shale, very hard, gray 20 150Limestone, gray 2 152Shale, hard, gray 43 195Shale, soft 10 20 5Shale, hard gray, with thin lignite beds 208 413Shale, sandy, gray with thin lignite beds ; water 17 430Lignite ---"' '°' 3 43 3Shale, very hard, with thin lignite beds 41 474Shale, hard, gray 2 476
Shale, very hard with soft layers 87 56 3Shale, gray, and gray sandstone, fine ; small amount
of water (cased out) 5 56 8Limestone 5 57 3Shale, gray, with thin beds of fine sandstone, gray 51 624Shale, very hard to hard 46 670Shale, sandy, soft 25 69 5Sandstone, hard 3 698Sandstone, soft ; water and small amount of gas 4 702Shale, hard, gray 8 710
161-89-5bbb(Log from Jensen, 1962 )
Glacial drift :Topsoil, dark-brown 1 1Clay, gravelly, yellowish-gray (till) 22 2 3Clay, gravelly, light-gray, and coal fragments (till) 10 3 3
Fort Union Group :Shale, light-gray 7 40
161-89-5bc c(Log from Jensen, 1962 )
Glacial drift :Soil, silty, brown 2 2Clay, pebbly, tan (till) 10 12Clay, gr avelly, yellow (till) 5 17
Fort Union Group :Clay, 1 18Lignite 3 21
198
161-89-5cad l(Log from Jensen, 1962 )
Geologicsource
Nal.prial
Thickness
feet
fht
Glacial drift :Topsoil, sandy, black 1
1
Clay, sandy, tan (till) 2
3
Clay, sandy, gray (till) 2
5Fort Union Group :
Lignite •5
5 . 5Lignite, black, and interbedded light-gray clay 8 .5
14
Rand, very fine, light-gray, clay 3
17
161-89-5cad2(Log from Jensen, 1962)
Glacial drift :Topsoil, sandy, black 1
1
Clay, sandy, pebbly, tan (till) 15
16
Fort Union Group :Lignite 1
17
161-89-5cb
(Log from LaRocque and others, 1963a)
Altitude : 1,945 feet
Glacial drift :Soil 2
2
Cl ay, sandy, yellow 8
10
Gravel and fine sand 7
17Clay, sandy, gray °° 5
22
Fort Union Group :Clay, sandy, gray with some .gravel
5
27Lignite 4
31Clay, sandy, gray 14
SLignite 2
47Cla y, sandy, gray 6
5 3Lignite 3
5 6Sand, gray, and clay 9
65
161-89-5cbcl
(Log from Jensen, 1962 )
Glacial drift :Topsoil, sandy, dark-brown 1
1Clay, pebbly, tan (till) 20
21
Fort Union Group :Clay, silty, gray 17
38
Lignite 1
39Clay, light-gray ; a little gypsum 13
52Sand, very fine, silty, light-gray 10
62
Cl a y, light-gray ; lignite 5
67
199
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161-89-9bcc(Iog from Jensen, 1962)
Geologi csource
Material
Thickness
Depthfeet (feet )
Glacial drift :Soil, dark-brown 1 1
Clay, sandy, yellowish-gray (till) 18 19Clay, gravelly, light-olive-gray (till) 7 26
Sand 2 28
Clay, bouldery, medium-gray (till) 64 92
Clay, sandy, dark-yellowish-orange, many limoniticshale pebbles (till) 3 9 5
Fort Union Group :Lignite 3 98Clay, light-gray 17 115
161-89-9cdd(Log from Great Northern Railway and
Baukol-Noonan Inc . )
Altitude : 1,955 fee t
Till, sandy brown clay with some gravel 33 3 3Till, blue and brown clay with some gravel 9 4 2Till, blue sand with floating coal and gravel 41 8 3Till, lots of gravel with little blue clay 2 8 5Till, blue clay and some gravel 5 9 0Till, blue clay and some gravel, very little floating
coal 45 135Till, blue clay with floating coal 30 165
161-89-lldaa(Log from Jensen, 1962 )
Glacial drift :Clay, very bouldery, yellowish-gray (till) 34 34Clay, very bouldery, light-gray (till) 43 7 7Clay, sandy, yellowish-gray (till) 13 9 0Clay, light to medium gray (till) 120 210Clay, hard, light-olive gray (till) 40 250C lay, grave lly, yellowish-gray (till) 5 25 5
Fort Union Group(?) :Clay, sandy, light-gray, samples consist of cavings 72 32 7
161-89-14ddd
(Log from Jensen, 1962 )
Glacial drift :Topsoil, dark-brown 1 1Clay, gravelly, yellowish-gray (till) 39 4oClay, sandy, light-gray (till 90 130
Fort Union Group :
4 134LigniteClay, shaley, light-gray ° 6 14o
202
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161-89-16cbc(Log from Jensen, 1962 )
Geologicsource
Material Thickness De thfeetfee t
Glacial drift :Topsoil, dark-brown 1 1Clay, sandy, yellowish-gray (till) 3 4Clay, gravelly, yellowish-gray (till) 31 3 5Clay, bouldery, light-gray (till) 57 92Gravel, fine to medium, clayey 15 10 7
Fort Union Group :Clay, very sandy, very light-gray 13 120
161-89-16ccc(Log from Jensen, 1962 )
Glacial drift :Soil, dark-brain 1 1Clay, gravelly, yellowish-gray (till) 31 32Clay, gravelly, light-gray (till) 49 8 1
Fort Union Group :12 9 3Clay, sandy, light-gray
Lignite 7 100
161-89-20add(Log from Jensen, 1962)
2 2Glacial drift :
Topsoil, dark-brainClay, sandy, yellowish-gray (till) 24 26Clay, sandy, light-gray (till) 36 62Clay, gravelly, grayish-yellow (till) 8 70
Fort Union Group :Clay, light-gray 10 80
161-89-27bbb
Altitude : 1,974 fee t
Glacial drift :Loam, silty, black 1 1Till, yellowish-gray to dusky-yellow, oxidized 20 2 1Till, yellowish-gray, oxidized ; contains lenses o f
medium sand 16 37Till, light-olive-gray 16 53Till, bluish-gray 7 6oSand, fine to medium, clayey---° ' ' 7 67Till, olive-gray 16 83
Fort Union Group :Shale, medium- to dark-gray and various shades of
green 11 94Lignite, black, fissile 2 96Sand, fine, greenish-gray ; micaceous, lignitic and
calcareous ° 4 100
204
161-89-30bds 2(Log from A . Sagness )
Geologi csource Material Thickness Depth
Clay
(feet )
14
(feet )
14Fine sand and water 7 2 1Clay and rocks 17 38Coarse sand and water 5 43Rocks and yellow clay 7 50Blue clay and small gravel 63 113Coal, no water 4 117Blue clay 31 1148Coal, no water 3 151
15 166Coal 3 169Blue clay 9 178Coal ° 2 180Sand, salt and pepper 5 185Coal 1 .5 186 . 5Blue clay or shale 186 . 5
161-89-33aaa(Log from Great Northern Railway and
Baukol-Noonan Inc . )
Altitude : 1,944 feet
Till, brown sandy clay with boulders7111, dark-blue clay with some brown clay, boulders
and some floating coal7111, blue clay, not so sandy, some bouldersTill, blue clay with boulders and floating coal
161-89-36dd(log from LaRocque and others, 1963a )
Altitude : 1,963 feet
Glacial drift :Soil, sandy, brownClay, sandy, brown, with some gravelClay, sandy, gray, with some gravelClay, sandy, gray, with strips of limestoneBoulder, graniteClay, sandy, gray, with boulders and small strips o f
limestoneClay, sandy, gray, with some gravelClay, sandy, gray, with strips of brown sandy clay
with some gravel and ligniteBoulder, graniteClay, sandy, gray, with some gravel and lignite
fragmentsClay, sandy, gray, with small strips of gravelClay, sandy, gray, with small strips of lignite an d
gravelLignite, hard, with small strips of gravelLignite, hardLignite, hard, with small strips of gravelLignite, hard, with strips of gravel and gray sandy
c1.aY° 'Clay, sandy, gray, small strips of ligniteBoulders and gravel, small strips of ligniteBoulders and gravel
Fort Union Group :Lignite and some gravel (wash-down)C lay, sandy, Bray '-__°"'---°---' "
20 5
22
84 035
22
3070
10 5
1 114 1 533 48
4 5 21 5 3
12 6517 8 2
13 951 96
44 14 06 146
19 1655 1709 179
30 209
15 22434 25832 29 020 310
4 314
1 315
161-90-lbbb
Altitude : 1,955 fee t
Geologi c source
Material
Thickness
Dept h(feet)
(feet )
Glacial drift :Loam, silty, dark-brown 1
1Till, yellowish-gray, oxidized 6
7Till, moderate-olive-brown, oxidized 16
2 3Till, olive-gray 15
38Fort Union Group :
Shale, silty, light-gray, light-olive-gray, andlight-greenish-gray 22
60
161-90-8bcb(Log from Great Northern Railway and
Baukol-Noonan Inc . )
Altitude : 1,962 feet
Till, clay and sand 19
19Till, blue clay, floating coal 6
25Till, blue clay, little gravel 5
30Till, layer rock, light-gray, hard 3
33Till, gray clay with little gravel 19
52Coal, till 2
54Till, gray clay and silty 1
5 5Gray sandy clay 25
80Soft rock, light-gray 2
82Gray clay with a green tint 28
110Coal, drilled hard 4
11 4Gray sandy clay ' 6
120Gray clay, not so sandy 27
14 7Coal, drilled hard 7
15 4Dark-gray clay 11
16 5
161-90-llbbb(Log from Great Northern Railway and
Baukol-Noonan Inc . )
Altitude : 1,950 fee t
Sandy brown till with some gravel 13
13Blue till with floating coal and gravel 24
3 7Sandy blue clay with a green tint 8
45
206
161-90-13ddd
Altitude : 1,970 feet
Geologi csource
Material
Glacial drift :Silt, clayey to sandy, dusky-yellow ; contains
pebblesSand, medium to coarse, gravelly, subangular t o
subroundedClay, silty, moderate-olive-brown to olive-gray ;
contains numerous streaks and lenses of medium to
very coarse sand, oxidized
Till, olive-grayGravel, fine to medium, sandy, moderately well-sorted ,
subangular to subrounded Clay, silty to sandy, olive-gray, contains thi n
gravel lensesTill, olive-gray ; contains numerous lignite chips
Sand, fine to medium, silty, subrounded, lignitic
Gravel, medium, brown, subrounded Clay, sandy, light-olive-gray Gravel, sandy, subroundedClay, sandy, olive-gray Gravel, fine to medium, brown
Clay, sandy, olive-gray Gravel, fine to medium, brown Silt, clayey, olive-grayGravel, fine to medium, brown
Clay, silty to sandy, olive-gray ; contains thi nlenses of gravel
Sand, medium to coarse, locally siltyClay, silty to sandy, olive-gray Sand, medium to coarse, well-sortedClay, silty to sandy, olive-gray Gravel, coarseClay, light-olive-grayGravel, medium, well-sorted
Clay, olive-graySand, fine, siltyClay, silty, olive-gray Silt, clayey, light-olive-gray, calcareous Sand, fine, olive-gray to greenish-gray ; contain s
brown carbonaceous streaks Silt, clayey to sandy, olive-gray, calcareous
Till, olive-gray ; contains a few sand and grave l
lensesClay, olive-gray to olive-blackSilt, sandy, light-olive-gray Sand, coarse, well-sorted, subroundedSilt, clayey, light-olive-gray, calcareous Sand, fine, ligniticSand, coarse, well-sortedGravel, fine and medium, sandy, moderately well -
sortedClay, light-gray, calcareousClay, silt light-olive-gray
Sand, fine ,silty,
greenish-gray - --Lignite, black, rounded, (apparently detrital)
Clay, sandy, brownish-black, carbonaceous ; containslignite
Sand, very fine or silt (from drill action) ; lignitecirculating in drilling fluid
Clay, white and medium-gray, calcareous
Silt or very fine sand (from drill action)
Gravel, medium and coarseSand, coarse ; contains limestone and lignite pebbles
Clay, silty, olive-gray Sand, coarse, brown, well-sorted
207
Thickness
De
hPeet feet )
8 8
10 18
14 32
9 4 1
7 48
9 5 78 6 58 734 775 8 2
4 8 6
8 942 96
5 101
3 1042 1063 109
13 12214 13 611 14 74 15 1
11 162
3 165
3 168
8 1762 178
3 181
12 19 312 20 5
9 21410 22 4
57 28 110 29110 30 1
6 3074 311
3 314
9 323
18 34 16 34 7
3 350
4 35 46 36 0
36 396
62 458
7 46 531 49 66 50 2
5 5073 510
5 515
161-90-13ddd, Continued
Geologi c source
Material Thickness
Depth(feet)
(feet )
Fort Union Group :Sand, fine, clayey, light-greenish-gray 1
51 6Sandstone, fine, light-greenish-gray 2
518Silt, sandy, light-olive-gray, calcareous 5
52 3Sand, fine, light-olive-gray, micaceous 6
529Shale, silty, light-gray 3
532Shale, greenish-gray 4
536Shale, medium-gray 4
540
161-90-22bbb(Log from Great Northern Railway and
Baukol-Noonan Inc . )
Altitude : 1,990 fee t
Brown clay with boulders Brown clay with blue streaksTill, brown clay with floating coalTill, layer rock, white with light-grayTill, blue sandy clayTill, bouldersTill, blue clay with some boulders Coarse blue siltRock °Blue silty clayHard sandCoalGray clay '
161-90-25bc b(Log from Great Northern Railway and
Baukol-Noonan Inc . )
Altitude :
1,980 feet
Till, brown sandy clayTill, brown sandy clay with floating coalTill, brown clay, gravelTill, blue clay and gravelTill, blue clay, bouldersTill, blue clay with some small rocks and floating
coal
161-90-32cdd
Altitude : 2,080 fee t
Glacial drift :Loam, sandy, blackSand, fine to medium, dark-brown, well-sorted Clay, silty, white, calcareous ; clay, dark-brownish-
black, carbonaceous
Till, dusky-yellow to moderate-olive-brown, oxidized Till, olive-gray (bluish tint)Sand, medium to very coarse, gravelly, well-sorted in
lenses, subroundedGravel, fine to coarse, poorly sortedTill, olive-gray
Fort Union Group :Shale, silty, light-gray, calcareous
3015
61 . 5
22 . 525
432158--
30455152 . 5757782
12 512 712 813 314 116 5
20 208 282 305 3 54 39
66 10 5
2 24 6
6 1223 3 526 6 1
14 755 80
22 102
18 120
208
161-90-34cc c(Log from Great Northern Railway and
Baukol-Noonan Inc . )
Altitude : 1,956 feet
Geologicsource Material Thicknes s
Till, brain clay with gravel
(feet )
15
1)2221feet )
1 5Till, brown clay with floating coal 5 20Till, blue clay with gravel 15 3 5Till, boulders 2 3 7Till, blue clay with some gravel 27 6 4Till, boulder 1 65Till, blue clay with some sand and some gravel 24 8 9Till, boulder °° 1 90Till, blue clay with sand and gravel 12 102Gray, silky clay 12 114Coal 2 116Gray clay 4 12 0
161-91-lccc(Log from Great Northern Railway and
Baukol-Noonan Inc . )
Altitude :
1,965 feet
Till, sand with some gravel 19 19Lost circulation 1 20No returns 5 2 5Till, blue-gray clay with gravel 5 30Till, blue clay with floating coal 5 3 5Till, blue clay with little sand 40 75Dark gray clay, bedrock 7 8 2Coal ° 8 90Gray clay 15 105
161-91-2aa(Log from IaRocque and others, 1963a )
Altitude : 1,957 feet
Glacial drift :soil 1
1Clay, sandy, yellow, with some gravel 18
1 9Clay, sandy, yellow, with fine sand and some gravel 5
2 4Clay, brown, with some gravel 6
3 0Gravel, with yellow sandy clay 3
3 3Fort Union Group :
Clay, sandy, gray 10
43Lignite 10
53
Sand, Bray- 39
92Lignite 3
95
209
(Lag from Great Northern Railway andBaukol-Noonan Inc . )
Altitude : 2,005 feet
Geologi csource
Material Thickness Depth
Till, brown clay, some sand
(feet )
15
(feet )
1 5Till, boulders 15 30Till, floating coal, blue clay ' 10 +vTill, blue clay with boulders 5 ^*
Till, coalTill, blue clay 16 6 1
Till, blue clay, silty 13 75Gray clay, silty 20 9 5Dark-gray clay, silty 5 100coal 6 IoeLight-gray clay, silty ' ' 12 118Dark-gray clay, silty 15 13 3coal 7 1 0Gray clay with little silt 25 16 5
(Log from D . Tandeski )
Brown clay anmgravel 32 3 2Gravel --' ' 2 3 4Brown sand and gravel 11 45Gray shale and gravel 20 65
Brown clayGray shale 26 91
Gray shale and gravel 50 145Gray sandy shale 35 18 oBrown sand 17 197Brown clay 12 209Green shale 15 22 4Gray sandy shale 14 238
161-92-35ccc
Altitude :
2/00,ee^
Road fill 6 6Glacial drift :
32 38Gravel, fine to medium, sandy ; heavy iron stained to
21 ft .Till, olive-gray 20 58Gravel, 'in" 2 60Till, olive-gray
_– . .–.~~~
6 66Gravel, medium, well-sorted 3 69Till, olive-gray
-- 9 78Gravel, fine to coarse, sandy, subangular to sub -
rounde^---" '--" 10 88Sand, coarse, well-sorted, subrounded, lignitic 5 93Sand, medium, slightly clayey, well-sorted, 29 122Till, olive-gray 20 **
6 14mTill, olive-gray
' 7 155Gravel, fine t ^ meu "". ^ar,-br=" ' 3 1 8
Fort Union Group :Silt and very fine clayey sand, yellowish-green ,
micaceous, oxidized 20 178Shale, silty, light-olive-gray to greenish-gray and
210
161-93-locdc
Altitude : 2,435 feet
(feet) feet
Glacial drift :Till, yellowish-gray, oxidized 7 7
Till, yellowish-gray to moderate-olive-brawn 11 18
Gravel, fine and medium, iron stained 3 21Till, moderate-olive-brown, oxidized 12 33
Till, olive-gray 14 47
Till ,lenses
olive-gray ; contains many thin sand and gravel30 77
Gravel ,gray
fine and medium, sandy ; contains lenses o f
silty and sandy clay 53 130
Till, o live -gray ° 39 169
Gravel, medium, well-sorted, subrounded 5X79
Till, olive-gray 50 22 4
Fort Union Group :Sand, very fine, silty, clayey, light-olive-gray,
17 241micaceousShale, silty, light-gray 7 24 8
Sand, clayey, black, carbonaceous 6 254
Lignite, black 3 257
Shale, medium-gray 3 260
161-93-21baa
Altitude : 2,410 fee t
Glacial drift :Loam, silty, black 2 2
Till, yellowish-gray and dusky-yellow 9 1 1
Till, moderate-olive-brown to light-olive-gray ,
partly oxidized 50 6 1
Till, olive-gray 64 12 5Gravel, fine to medium, moderately well-sorted, sub -
angular to subrounded 4 12 9Till, olive-gray ; granitic boulder at 168 ft . 55 184
Gravel, medium 3 187Till, olive-gray 20 207
Fort Union Group :Shale, medium-gray ° 7 214
Lignite, black 3 217Sand, fine, clayey, dark-greenish-gray, carbonaceou s 8 225Silt, light-greenish-gray ; light-brownish-gray silt ;
and silt, light-brownish-gray ; clay, sandy ,greenish-gray 24 249
Shale, silty, light to medium-gray 11 260
161-94-2aaa(Log from E . H . Prather )
Brown clay, rock, gravel 69 69Gray clay, rock, gravel 14 8 3Brown sand, gas, little water 14 97Gray clay, boulders, rock and gravel 122 219
Yellow clay 9 228
Brown clay, coal mixed 11 239Gray sandy clay 23 .5 262 . 5Loose coal, sand mixed, water 1 .5 264
211
Geologi csource
Material
Thickness
De th
162-88-31cdc(Log from Jensen, 1962 )
Geologi csource Material Thickness Depth
(feet) (feet )
Glacial drift :Topsoil, dark-brown 1 1
Clay, sandy, yellow to gray 2 3Clay, sandy, yellowish-gray (till) 7 10Sand, medium to coarse, clean 12 22
Clay, gravelly, medium-gray (till) 62 84
Clay, very sandy, yellowish-gray (till) 11 9 5Clay, bouldery, light-gray (till) 38 13 3Gravel, granular 3 13 6
Clay, gravelly, gray (till) 22 158
Gravel and boulders 25 18 3Clay, sandy, bouldery, yellowish-gray (till) 22 205
Clay, gravelly, medium-gray (till) 95 300Fort Union Group :
Clay, shaley, light-gray .
Poor samples 3 303
162-88-34aa a
Altitude :
1,886 feet
Glacial drift :Till, dusky-yellow, oxidized ; contains several thin
34lenses of iron stained, fine to medium sand Till, olive-gray ; contains some thin lenses of fine
to medium sand 19
Till, olive-gray 39Sand, medium, moderately well-sorted, subrounded 18Till, olive-gray 16Sand, medium to coarse, moderately well sorted ;
contains some interstitial clay 16
Till, olive-gray 76Fort Union Group :
Lignite, black 3Clay, black, oily 4
Shale, silty, medium-gray to light-greenish-gray 1 5
aceous 6
182Sand, fine to very coarse, gravelly, dark-brown ,
poorly sorted ; predominantly siliceous grains andpebbles 36
218Clay, sandy, light-gray, calcareous 8
226Sand and gravel, dark-brown ; predominantly siliceou s
rocks 10
236Fort Union Group :
Shale, light- to medium-gray, and black ; contains athin bed of lignite 18
254Shale, sandy, light-greenish-gray 10
264
Limestone, tan 5
269Shale, medium-gray 11
280
212
34
5 39 2
110
126
14 2218
22 122 5240
162-89-3bbb
Altitude :
1,918 fee t
Glacial drift :Till, dusky-yellow to reddish-brown, oxidized ;
contains a few lenses of sand and gravel Till, olive-graySand, medium to coarse, slightly clayeyTill, olive-graySand, medium to coarse, clayey, dark-brown, carbon -
26
26101
12 79
13640
176
162-89-4bbb(Log from Jensen, 1962 )
Geologi csource
Material
Thickness
Dept h(feet)
(feet )
Glacial drift :Topsoil, sandy, blackClay, very sandy and gravelly, tan (till)Sand, fine to very coarse, and some fine gravelClay, sandy, pebbly, tan (till)Clay, sandy, pebbly, gray (till)Clay, sandy, hard, gray, numerous boulders (till)Clay, sandy, hard, gray ; cavings predominant i n
samples (till)
162-89-8aaa(Log from Jensen, 1962 )
Glacial drift :Topsoil, sandy, blackClay, yellow, sandyClay, sandy, gravelly, tan (till)Clay, sandy, pebbly, bouldery (till)Gravel, medium to coarse Clay, sandy, boulders, gray (till)Sand, medium and coarse, clayey, grayClay, sandy, gray, with lignite fragments (till)Clay, smooth, grayish-brown (till)Clay, sandy, gray, lignite fragments (till)Clay, sandy, yellowish-brown (till)Clay, sandy, gray, sand and gravel, cavings in
samples (till)Fort Union Group :
Clay, grayClay, shaley, blackClay, smooth, gray
111
71 7849 5
69
1121936
12021 5
284
1 13 4
10 1 424 3812 5 0
171 22 111 23 222 25 411 26572 33 7
8 345
65 410
5 4155 420
10 430
213
162-89-13cc(Log from LaRocque and others, 1963a)
Altitude : 1,910 feet
Geologicsource
Material
Thickness
De th(feet)
feet )
Glacial drift :Soil 1 1Clay, sandy, yellow 4 5Clay, sandy, yellow, with some gravel 11 16Clay, sandy, gray, with some gravel 5 2 1Sand, fine and gravel 2 2 3Clay, sandy, gray, with some gravel 15 38Gravel 2 40Clay, sandy, gray, with some boulders 3 4 3Boulder ° 1 44Clay, sandy, gray, with some gravel and boulders 4 48Clay, sandy, gray, with some gravel and lignite frag
ments 44 92Sand, fine 1 93Clay, sandy, gray, with some gravel and lignite frag
ments 3 96Boulder, granite 2 98Clay, sandy, gray, with some gravel 7 105Clay, sandy, gray, with some gravel and lignite frag
ments 4o 145Gravel ° 1 146Clay, sandy, gray, with small strips of gravel and
lignite fragments 16 162Gravel and lignite fragments, with strips of gray ,
sandy clay---°° 6 168Clay, sandy, gray, with small strips of gravel and
lignite fragments 17 185Fort Union Group :
Lignite 3 188Lignite, with strips of white clay 30 218Clay, white, with strips of lignite 20 238Limestone, gray 3 241Sand, Bray 9 2 50
162-89-16bbc(bog from Jensen, 1962 )
Glacial drift :Topsoil, sandy, black 1 1Clay, sandy, light-gray 2 3Sand, fine to medium 1 4Clay, yellow, with interbedded sand and gravel (till) 6 10Clay, sandy, pebbly, tan (till) 8 18Clay, sandy, pebbly, dark-gray (till) 26 44Clay, pebbly, yellow (till) 1 45Clay, pebbly, dark-gray (till) 45 90Clay, sandy, and very gravelly, dark-gray (till) 90 180Clay, sandy, tan (till) 12 192Clay, very sandy, tan and gray .
A lot of coarse sandand gravel (till) 17 209
Fort Union Group :9 218Clay, smooth, light-green
214
162-89-21bbb(Log from Jensen, 1962 )
Geologicsource
Material Thickness
f'2 22-)ifeetYee t
Glacial drift :Topsoil, sandy, black 1 1
Clay, sandy, pebbly, tan (till) 17 18Clay, sandy, pebbly, brown (till) 12 30Clay, sandy, pebbly, gray (till) 128 158
Fort Union Group :Clay, sandy, gray 12 170
162-89-25aaa
Altitude : 1,925 fee t
Glacial drift :Till, moderate-olive-brown, oxidized 33 33Gravel, fine and medium, well-sorted 2 3 5Till, moderate-olive-brown, oxidized 7.8 5 3Till, olive-gray ; contains a contorted bedrock
boulder between 75 and 86 ft . 46 9 9
Gravel, medium, well-sorted ; pebbles are predominantly limestone 4 10 3
Sand, coarse, well-sorted 3 106
Till, olive-gray 15 12 1Fort Union Group :
19 140Silt, clayey, light-olive-gray, calcareous ; locally
carbonaceousShale, silty, light-gray 2 14 2Lignite, black, fissile 2 14 4
Shale, gray 2 146
Lignite 3 149Shale, medium-gray 7 156Sand, fine, greenish-gray, subrounded 4 16o
162-89-28dd(Log from IaRocque and others, 1963a )
Altitude : 1,941 feet
Glacial drift :Soilclay, Yellow 'C lay, sandy, gray, with some gravelSand, fine and gravelClay, sandy, gray, with some gravelClay, sandy, gray, with some strips of limestone
Clay, sandy, gray, with some gravelLimestone and "sand " rockClay, sandy, gray, with some gravel and lignite
fragmentsFort Union Group :
Clay, Lignite
Light clay, gray
215
3
310
1338
5 14
5 511
666
7228
1001
101
14
115
5
1202
12223
14 5
162-89-29aaa(Log from Jensen, 1962 )
Geologi csource
Material Thicknes s(feet) feet )
Glacial drift :Topsoil, sandy, black 1 1Clay, pebbly, tan (till) 23 24Clay, gravelly, tan (till) 16 40Clay, sandy, tan (till) 6 46Sand, cemented, tan 5 5 1Clay, sandy, gravelly, tan (till) 2 5 3Clay, sandy, pebbly, bluish-gray (till) 51 I04Sand, fine silty, clayey, light-gray 13 11 7Clay, sandy, pebbly, bluish-gray (till) 50 167Gravel and rock fragments, predominantly dolomitic 4 17 1Gravel, fine, mixed with clay 4 17 5Clay, sandy, pebbly, bluish-gray (till) 33 208
Fort Union Group :1 209Lignite
Clay, sandy, gray 7 216Clay, sandy, brown---- 4 220Clay, sandy, gray 10 230
162-89-33bbb(Log from Jensen, 1962 )
Glacial drift :Topsoil, sandy, brown 1
1Clay, gravelly, tan 2
3Sand, fine 1
4Clay, sandy, pebbly, tan (till) 26
30Clay, sandy, bouldery, gray (till) 16
46Fort Union Group :
2
48LigniteClay, 30
78Clay, very sandy, light-gray 2
80
162-89-35cc c(Log from Jensen, 1962 )
Glacial drift :Clay, sandy, yellowish-gray (till) 17
1 7Clay, bouldery, medium-gray (till) 64
81Fort Union Group :
Clay, shaley, sandy, light-gray 5
86Lignite 4
90
162-89-35ddd(Log from Jensen, 1962 )
Glacial drift :Clay, sandy, yellowish-gray (till) 34 34Clay, sandy, bouldery, medium-gray (till) 66 100Gravel 4 I04Clay, bouldery, medium-gray (till) 12 116
Fort Union Group :Clay, shaley, light-gray 4 120
216
162-90-laab
(Log from IaRocque and others, 1963a)
Altitude : 1,932 fee t
Geologicsource Material Thickness Depth
feet (feet )
Soil, clayey, dark-brown 1 .3 1 . 3Clay, dark-brown .8 2 . 1Clay, calcareous, grayish-brown to yellowish-brown,
2 .4 4 . 5with limonitic mottling and lignite fragments Clay, calcareous to depth of 10 ft ., olive-brown with
15 .5 20limonitic mottling, lignite fragments and thi nsand lenses
Clay, slightly silty, olive-brown, with limonitic4 24mottling and thin sand lenses
162-90-lad a(Log from LaRocque and others, 1963a )
Altitude : 1,935 fee t
Soil, sandy and clayey, light-gray to brown, with2 .6 2 . 6small amount of salt
Clay, silty and sandy, olive-brown .9 3 . 5Sand, fine, yellowish-brown .1 3 . 6Clay, silty
and sandy, olive-brown, with limonitic3 .4 7mottling
Clay, olive-brown, with limonitic mottling ; water
seep at 17 .6 ft . 14
2 1
162-90-lad d(Log from le.Rocque and others, 1963a )
Altitude :
1,934 fee t
Soil, clayey and silty, brown to grayish-brown 3 3Clay, silty, calcareous, brown, with limoniti c
mottling and salt pockets 1 .5 4 . 5Clay, calcareous, olive-brown, with limoniti c
mottling and lignite fragments 2 .9 7 . 4Clay, silty, calcareous, olive-brwn,with limoniti c
mottling and lignite fragments 2 .6 10
217
162-90-lbaa(Log from LaRocque and others, 1963a)
Altitude : 1,938 feet
Geologicsource
Material
Thickness
f''2211:5(feet)
fee t
Soil, silty and clayey, brown, with salt pocketsbelow depth of 1 ft . 2 .3 2 . 3
Clay, silty, varved, grayish-brown, with salt pockets 1 3 . 3Sand, fine, clayey, stratified, varved, light-olive -
brown, with salt pockets and limonitic mottling 3 .3 6 . 6Sand, poorly sorted, yellowish-brown .4 7Clay, silty, olive-brown, with salt pockets an d
limonitic mottling 3
10Clay, sandy, olive-brown, with lignite fragments 16
2 6
162-90-lbab(Log from LaRocque and others, 1963a )
Altitude : 1,939 fee t
Soil, silty and clayey, brown 1 .3 1 . 3Clay, silty, olive-brown, with limonitic mottling 4 .6 5 . 9Clay, very sandy, olive-brown, with limonitic
3 .6 9. 5mottling and lignite fragments Clay, sandy, olive-brown, with limonitic mottling 5 .5 1 5Clay, very compact, olive-brown, with limonitic
5 2 0mottlingSand, silty, olive-brown 4 2 4
162-90-lbcc(Log from LaRocque and others, 1963a )
Altitude :
1,938 fee t
Soil, silty and sandy, grayish-brown to brown 3 .1 3 . 1Sand, medium, clayey, dark-yellowish-brown .4 3 . 5Clay, silty, pebbly, olive-brown, with lignite frag-
6 .5 10mentsClay, slightly sandy and pebbly, grayish-brown, with
10 2 0limonitic mottlingSand, coarse, poorly sorted, yellowish-brown ;
2 2 2contains water
162-90-ldad(Log from LaRocque and others, 1963a)
Altitude : 1,934 fee t
Soil, clayey and sandy, dark-brown 2 2Clay, calcareous, olive-brown, with salt pockets ,
varved from depths of 3 .3 ft . to 4 .5 ft ., lignit efragments and limonitic mottling 8 10
Clay, silty, olive-brown, with limonitic mottling 5 15Clay, sandy, and silty, olive-brown, with limonitic
mottling ; water seep at 18 ft . 5 20Clay, olive-brown, with salt pockets and limoniti c
mottling 4 24
218
Geologi csource
162-90-ldbb
(Log from LaRocque and others, 1963a )
Altitude :
1,929 feet
Material Thicknes s(feet)
Soil, silty and clayey, grayish-brown, with limoniti cmottling 1 . 1
Clay, black 1 . 4
Clay, calcareous, olive-brown, with limoniti c
mottling and lignite fragments 7 . 5
Silt, light-brown ; moist . 2
Sand, coarse with some gravel, poorly sorted, brown ;
saturated 2 . 3Clay, very dense and pebbly, olive-brown, with
lignite fragments, gypsum crystals and salt
pockets 1 . 5
162-90-ldc c(Log from LaRocque and others, 1963a )
Altitude : 1,938 fee t
Soil, silty and clayeyClay, silty, light-gray, with limonitic mottling Clay, silty, brown, with limonitic mottling
Clay, brown, with limonitic mottling Clay, brown, with limonitic mottling and salt pocket s
Sand and clay, silty, brown, stratified with salt
pocketsClay, brown, with limonitic mottling and salt pocket sClay, pebbly, olive-brown, with limonitic mottling ;
becomes more pebbly with depthClay, pebbly, olive-brown grading downward to gray,
with limonite mottling
162-90-lddd(log from LaRocque and others, 1963a )
Altitude :
1,941 fee t
Soil, silty and clayey 1 .4 1 . 4
Clay, very silty and sandy .6 2
Clay, silty, highly calcareous from 2 to 3 ft . ,
pebbly, varved, olive-brown 2 .5 4 . 5
Sand, medium, pebbly, yellowish-brown 1.5 6
Clay, gravelly and silty, olive-brown, with limoniti c
mottling 2 8
Clay, silty and gravelly, olive-brown, varved withlignite fragments and limonitic mottling 2 10
Clay, sandy and pebbly, tan to olive-brown, varve d
with lignite fragments and pockets of silt 3 13
Sand, coarse, poorly sorted, clayey, light-brown,
with lignite fragments ; saturated from 14 to 15 ft . 2 15
Clay, light-brown 1 16
219
Depth(feet )
1 . 12 . 5
1 010 .2
12 . 5
14
1 .5 1 .51 .1 2 .61 .1 3 .71 .4 5 .1
3 .9 9
.5 9 . 5
.5 10
8 18
7 25
162-90-2aad(Log from taRocque and others, 1963a )
Altitude : 1,933 fee t
Geologi csource
Material
Thickness
Depth(feet)
(feet )
Soil, silty and clayey, dark-brown 3
3Clay, silty, olive-brown, with salt pockets to dept h
of 10 ft ., limonitic mottling and lignite frag-ments °° 17
20Clay, olive-brown, limonitic mottling 3
2 3
162-90-2aba(Log from LaRocque and others, 1963a )
Altitude : 1,917 feet
Soil, silty, dark-brown 1 .5
1 . 5Clay, silty, varved, dark-grayish-brown .8
2 . 3Silt, clayey, calcareous, gray 2 .2
4 . 5Gravel, poorly sorted, olive-brown .7
5 . 2Sand, fine, clayey, olive-brown 1
6 . 2Clay, silty, calcareous, olive-brown, with limoniti c
mottling 3 .8
10Clay, olive-brown, with limonitic mottling and
lignite fragments 12 .5
22 . 5
162-90-2ac c(Log from LaRocque and others, 1963a)
Altitude : 1,937 feet
Soil, silty and clayey, grayish-brown 1 .1
1 . 1Clay, calcareous to depth of 6 ft ., pebbly below
depth of 5 ft ., light-brown to olive-brown, withlimonitic mottling and lignite fragments 14 .9
16Clay, very compact, pebbly, dark-olive-brown, with
salt pockets, lignite fragments, and limoniticmottling 8
2 4
162-90-2baa(Log from LaRocque and others, 1963a)
Altitude : 1,937 feet
Soil, silty and clayey, calcareous, brown toyellowish-brown 2 .5
2 . 5Sand, medium, silty, yellowish-brown 2
4 . 5Clay, sandy, silty, laminated, pebbly, olive-brown 1 .6
6 . 1Gravel, poorly sorted, silty, olive-brown .5
6 . 6Clay, silty, olive-brown, with limonitic mottling 3 .4
10Clay, silty and sandy, pebbly, olive-brown, with
limonitic mottling 16
26
220
162-90-2bab
(Log from LaRocque and others, 1963a)
Altitude : 1,942 fee t
Geologicsource Material Thickness Depth
Soil, silty, dark-brown
(feet )
2 .3
(feet )
2 . 3Clay, silty, valved, pebbly, very compact, olive -
brown, with limonitic mottling 3 .7 6Clay, silty, light-olive-brown, with limoniti c
mottling and lignite fragments 1 7Clay, silty, olive-brown, with salt pockets 3 10Clay, olive-brown, with limonitic mottling an d
lignite fragments 14 2 4
162-90-2cbb
(Log from LaRocque and others, 1963a )
Altitude : 1,946 fee t
Soil, silty, dark-brown to grayish-brown 1 .3
1 . 3Clay, silty, calcareous to depth of 5 .5 ft ., alkaline
below 5 .5 ft ., olive-brown, with limoniti cmottling 8 .7
10Clay, very pebbly, olive-brown, with limonitic
mottling 3
13Clay, pebbly, gray to buff, with lignite fragment s
and gypsum crystals ° 10 .5
23 . 5Sand, radium-grained, silty, saturated, brown 3
26 . 5
162-90-2ccb(Log from LaRocque and others, 1963a )
Altitude :
1,945 feet
Soil, silty and clayey, brown 1 .6 1 . 6Clay, silty, calcareous, sandy with depth, olive -
brown, with limonitic mottling, lignite fragmentsand salt pockets 8 .4 10
Sand, fine, clayey, olive-brown 5 1 5Clay, silty and pebbly, olive-brown 8 23
162-90-2cdc(Log from LaRocque and others, 1963a )
Altitude :
1,944 fee t
Soil, silty, dark-brown 1 .5 1 . 5Sand, clayey, yellowish-brown .8 2 . 3Clay, silty, olive-brown, with lignite fragments,
17 .7 2 0limonitic mottling and salt pockets
22 1
162-90-2dad(Log from LaRocque and others, 1963a )
Altitude : 1,941 feet
Geologi c source
Material Thickness
Depth(feet)
(feet )
Soil, silty and clayey, gray to brown 2 .1
2 . 1Clay, silty, stratified, yellowish-brown 2 .1
4 . 2
Clay, very compact, calcareous, olive-brown, wit hlignite fragments and limonitic mottling 2
6 . 2Silt, sandy and clayey, yellowish-brown, with
limonitic mottling 1 .6
7 . 8
Sand, fine, yellowish-brown 1
8 . 8Clay, silty and sandy, olive-brown, with limonitic
mottling and lignite fragments 14 .2
2 3
162-90-2dcc(Log from LaRocque and others, 1963a )
Altitude : 1,945 feet
Soil, silty, brown 1 .3
1 . 3Sand, medium, silty, grayish-brown to yellowish -
brown 3 .7
5Sand, medium, silty, varved, olive-brown 1 .5
6 . 5Sand, medium, silty, varved, yellowish-brown 1 .7
8 . 2
Silt, sandy, varved, yellowish-brown 1 .8
10Clay, silty, moderately compact, olive-brown 7 .5
17 . 5Clay, pebbly, very compact, olive-brown, with gypsum
crystals 4 .5
2 2Clay, olive-brown, interbedded with thin lenses of
saturated silt 6
2 8
162-90-2ddc
(Log from LaRocque and others, 1963a )
Altitude : 1,938 fee t
Soil, silty and clayey, grayish-brown 1 .9
1 . 9Clay, silty, calcareous, olive-brown, with limoniti c
mottling 1 .8
3 . 7Clay, calcareous, olive-brown, with limonitic mot -
tling, lignite fragments and salt pockets 6 .3
10Clay, silty, olive-brown, with limonitic mottling 5
15Sand, clayey, brown, with limonitic mottling 2
17Clay, silty, olive-brown, with limonitic mottling 7
2 4
162-90-3aab
(Log from LaRocque anc others, 1963a )
Altitude : 1,943 fee t
Soil, silty, dark-brown 2 .4
2 . 4Clay, silty, calcareous, olive-brown, with limoniti c
mottling and lignite fragments 13 .6
16
222
162-90-3aad(Log from LaRocque and others, 1963a )
Altitude : 1,946 feet
Geologi csource Material Thickness De th
feet(feet )
Soil, silty, dark-grayish-brown to brown 1 .2 1 . 2Clay, silty, calcareous, brown to olive-brown 2 .5 3 . 7Clay, silty, calcareous, olive-brown with limoniti c
mottling 6 .3 10
162-90-3baa(Log from LaRocque and others, 1963a )
Altitude :
1,922 fee t
Soil, clayey and silty, brown 1 .1 1 . 1Clay, very silty, calcareous to 2 ft ., varved from 2
to 2 .5 ft ., boulders at 5 ft ., yellowish-brown---- 3 .9 5Sand, fine-grained, well-sorted, light-brown ;
saturated from 13 to 13 .5 ft . 8 .5 13 . 5Clay, pebbly, unweathered, dark-brown 3 .5 1 7
162-90-3bba(Log from LaRocque and others, 1963a )
Altitude :
1,916 feet
Soil, silty, dark-brown 0 .8 0 . 8Silt, calcareous, organic, black 4 .2 5Clay, olive-brown .8 5 . 8Sand, fine-grained, clayey, grayish-brown .3 6 . 1Gravel, clayey, brown .3 6 . 4Clay, limonitic mottling, olive-brown 16 .1 22 . 5
162-90-3bbb(Log from LaRocque and others, 1963a )
Altitude :
1,921 feet
Soil, silty, dark-brown 3
3Sand and gravel, poorly sorted 2
5Clay, friable, olive-brown, with lignite fragments ,
limonitic mottling 15
2 0Clay, olive-brown, as above but more moist an d
plastic 4
24
162-90-3bb c(Log from LaRocque and others, 1963a )
Altitude :
1,923 fee t
Soil, clayey and silty, brownClay, silty, calcareous, grayish-brown
2 . 3.7
2 .33
Unsampled 7 10Clay, silty, olive-brown, with limonitic mottling 6 16Clay, very compact, olive-brown, with limonitic
mottling 6 .8 22 .8
22 3
162-90-3bd d(Log from LaRocque and others, 1963a )
Altitude : 1,946 feet
Geologi csource Material Thickness Depth
Soil, silty and clayey, grayish-brown
(feet )
1 .5
(feet )
1 . 5Clay, silty, calcareous to 3 ft ., salt pockets below
3 ft ., olive-brown 8 9 . 5Sand, silty, Isminated, yellowish-brown .5 10Clay, pebbly, buff-colored, with crystals of gypsu m
and limonitic mottling 4 1 4Clay, silty and sandy, pebbly, grades to unweathered
material with depth 12 2 6
162-90-3cbb(Log from LaRocque and others, 1963a )
Altitude : 1,939 feet
Soil, silty, brown to yellowish-brown 1 .9 1 . 9Clay, dark-yellowish-brown 1 .1 3Clay, silty, very compact, olive-brown 7 10Clay, pebbly, olive-brown 6 16Silt, sandy, light-brown 2 18Clay, sandy, pebbly, olive-brown 3 .5 21 . 5Clay, sandy, unweathered, olive-brown to gray 10 .5 32
162-90-3ccb(Log from lahocque and others, 1963a )
Altitude :
1,942 feet
Soil, silty, dark-brown 0 .5 0 . 5Soil, sandy and clayey, dark-brown 2 2 . 5Clay, silty, olive-brown, with limonitic mottling and
12 .5 15lignite fragmentsClay, silty and pebbly, olive-brown 7 .5 22 . 5
162-90-3ccc(Log from LaRocque and others, 1963a )
Altitude :
1,945 fee t
Soil, silty to clayey, dark-brown 1 .5 1 . 5Clay, silty, olive-brown, with salt pockets an d
limonitic mottling 8 .5 10Clay, pebbly, olive-brown, with lignite fragments 14 24
162-90-3cdc(Log from LaRocque and others, 1963a )
Altitude : 1,940 feet
Soil, silty, brown to yellowish-brown 1 .8
1 . 8Clay, olive-brown, with limonitic mottling 1 .9
3 . 7Silt, sandy, grayish-brown, with limonitic mottling 2 .4
6 . 1Silt, sandy, laminated, yellowish-brown, with
limonitic mottling and salt pockets 1 .6
7 . 7Clay, sandy, olive-brown, with limonitic mottling
and lignite fragments 15 .3
2 3
224
162-90-3dc c(Log from LaRocque and others, 1963a)
Altitude : 1,939 feet
Geologicsource Material Thickness Dth
fee t(feet )
Soil, silty, dark-brown 2 2
Clay, silty, calcareous from 2 .5 to 4 ft ., olive -brown, with limonitic mottling 8 10
Clay, sandy, olive-brown 4 14
162-90-3ddc(Log from LaRocque and others, 1963a )
Altitude :
1,943 feet
Soil, clayey and silty, brown 1 . 5Clay, calcareous, sandy, grayish-brown 1 . 5Clay, sandy, olive-brown, with salt pockets and
7limonitic mottlingClay, olive-brown, with limonitic mottling and
9lignite fragments
162-90-9aad(Log from LaRocque and others, 1963a )
Altitude : 1,940 fee t
Soil, silty, black 0 .8
0 . 8
Clay, silty, brownish-gray, with limonitic mottling 2 .5
3 . 3Silt, sandy, brown to gray, with limonitic mottling .7
4Clay, olive-brown, with salt pockets and limoniti c
mottling 6
10
162-90-10aaa(Log from LaRocque and others, 1963a)
Altitude :
1,950 fee t
Soil, silty, olive-brown 3 3
Silt, yellowish-brown, sandy .5 3 . 5Clay, silty, olive-brown, with limonitic mottling and
salt pockets 6 .5 10
Clay, very compact and pebbly, olive-brown 8 18
Sand, medium, clayey, light-brown 2 20
162-90-10bcc(Log from LaRocque and others, 1963a )
Altitude :
1,950 fee t
Soil, silty and clayey, dark-grayish-brown 1 .5 1 . 5
Clay, silty, olive-brown, with limonitic mottling ,salt pockets, and lignite fragments 8 .5 10
Clay, pebbly, olive-brown, with lignite fragment sand limonitic mottling 12 22
22 5
162-90-10caa
(Log from LaRocque and others, 1963a )
Altitude :
1,946 feet
Geologicsource Material Thickness Depth
Soil, silty, brown
(feet )
1 .1
(feet )
1 . 1Clay, silty, grayish-brown, with limonite fragment s 2 .9 4Gravel, sandy and silty, stratified, olive-brawn 2 6Clay, silty, olive-brown 4 10Clay, sandy, olive-brown ; contains very thin lense s
of fine sand 2 12Clay, pebbly, dark-brown 2 14
162-90-10cbc
(log from LaRocque and others, 1963a )
Altitude :
1,950 feet
Soil, silty, brown 1 .7 1 . 7Clay, silty, olive-brown, with salt pockets 13 .3 15Sand, clayey, stratified, olive-brown 1 16Clay, silty, olive-brown 6 .5 22 .5
162-90-locc c(Log from LaRocque and others, 1963a )
Altitude :
1,948 feet
Soil, silty, calcareous, grayish-brown = 3 3Clay, silty, olive-brown, with salt pockets and
limonitic mottling 3 6Sand, medium, yellowish-brown .3 6 . 3Clay, silty, olive-brown, with limonitic mottling an d
salt pockets 2 .7 9Clay, pebbly, laminated, olive-brown, with gypsum
crystals and salt pockets 8 17Clay, shaly cleavage, olive-brown 4 2 1Clay, shaly cleavage, unweathered, dark-gray to black 3 2 4
162-90-10cdc
(Log from LaRocque and others, 1963a )
Altitude :
1,942 feet
Soil, silty, brown 1 .2 1 . 2Sand, coarse, stratified, brown 2 .8 4Sand, medium, brown .7 4 . 7Sand, clayey, medium, brown .3 5Sand, medium, brown .4 5 . 4Clay, silty, olive-brown, with limonitic mottling,
.8 6 . 2salt pockets and lignite fragments Not sampled 3 .8 10Clay, very compact, unweathered, dark-gray 11 .7 21 . 7
226
Geologi csource
162-90-llaad(Log from LaRocaue and others, 1963a )
Altitude :
1,938 feet
Fbterial Thicknes sfeet
Soil, silty, brown 2 . 3Clay, silty, olive-brown, with salt pockets,
limonitic mottling and lignite fragments 2 . 7Not sampled 5Clay, silty, calcareous, olive-brown, with lignit e
fragments, limonitic mottling and salt pockets 4Clay, very compact, olive-brown 2
(Stopped by boulder at 16 ft .)
162-90-llbbc
(Log from LaRocque and others, 1963a )
Altitude : 1,946 feet
Soil, silty, brownClay, silty, calcareous, olive-brownClay, silty, calcareous, olive-brown, with sal t
pockets and limonitic mottlingClay, silty, olive-brown, with limonitic mottling ,
salt pockets, and lignite fragments
162-90-llbc c(Log from LaRocque and others, 1963a )
Altitude : 1,944 feet
Soil, silty, calcareous, grayish-brown Clay, silty, calcareous, olive-brown Clay, calcareous, olive-brown, with lignite fragments ,
limonitic mottling, and salt pockets Clay, very compact, pebbly, buff-colored, with
lignite fragments(Boulder at 13 .5 ft . prevented further sampling )
162-90-llbdd(Log from laRocque and others, 1963a )
Altitude : 1,944 feet
Soil, silty, dark-brown Clay, silty, dark-brown Clay, calcareous, black, with limonitic mottlingClay, silty, olive-brown Clay, calcareous, olive-brown, with limoniti c
mottlingClay, silty, calcareous, olive-brown, with limoniti c
mottling and lignite fragments Clay, sandy, olive-brawn
(Stopped by boulder at 17 ft . )
227
De thfeet )
2 . 3
510
1416
1 . 3.9
1 .4
19 .1
1 . 32 . 2
3 . 6
22 . 7
1 .6 1 . 6
.9 2 . 5
7 .5 10
3 .5 13 . 5
1 1
.9 1 .91 .4 3 .3.7 4
3 .5 7 . 5
2 .5 10
7 17
162-90-llcc b
(Log from LaRocque and others, 1963a )
Altitude : 1,950 feet
Geologi csource
Material
Thickness
Depth
(feet)
(feet )
Soil, silty, brown 1 .8
1 .8Clay, silty, calcareous, olive-brown, with limoniti c
mottling and lignite fragments 22 .2
24
162-90-llcc c
(Log from LaRocque and others, 1963a)
Altitude : 1,942 feet
Soil, silty and clayey, dark-brown 1 .8 1 . 8Clay, silty, pebbly, grayish-brown .7 2 . 5Gravel, silty, brown .9 3 . 4Clay, silty, olive-brown, with limonitic mottling and
lignite fragments 6 .6 10
162-90-llcdd
(Log from LaRocque and others, 1963a )
Altitude :
1,942 feet
Soil, silty, calcareous below 1 .5 ft ., grayish-brownto brown 3 3
Clay, calcareous, olive-brown, with salt pockets an dlimonitic mottling 7 10
Clay, friable, very compact, pebbly, grayish-brown,with lignite fragments and gypsum crystals 12 .5 2 2 .5
162-90-lldda
(Log from LaRocque and others, 1963a )
Altitude :
1,942 feet
Soil, silty, dark-brown 0 .9 0 . 9Clay, dark-brown 2 2 . 9Sand, medium-grained, olive-brown .4 3 . 3Clay, silty, very compact, calcareous, olive-brown ,
with lignite fragments and limonitic mottling 6 .7 10Clay, silty, olive-brown, with salt pockets an d
limonitic mottling 4 14
162-90-llddc
(Log from LaRocque and others, 1963a )
Altitude : 1,944 fee t
Soil, silty and clayey, gray-brown 2 .5
2 . 5Clay, olive-brown, with limonitic mottling 1 .6
4 . 1Silt, sandy, yellow-brown, with limonitic mottling 1 .8
5 . 9Clay, calcareous, olive-brown, with limoniti c
mottling and lignite fragments 3 .9
9 . 8Clay, silty, calcareous, olive-brown, with limoniti c
mottling 13 .2
23Clay, unweathered, dark-gray 1
24
228
162-90-12aba
(Log from LaRocque and others, 1963a )
Altitude : 1,933 feet
Geologi csource Material Thickness Depth
Soil, silty, grayish-brown
feet
2 .8
(feet )
2 . 8
Clay, silty, brown, with gypsum crystals 2 .7 5 . 5Clay, brown, with limonitic mottling and salt pockets 2 .2 7 . 7Clay, silty and sandy, brown, with limonitic mottling 1 8 . 7
Not sampled 1 .3 10
Clay, silty, olive-brown, with limonitic mottling an d
lignite fragments 5 1 5Clay, olive-brown, with limonitic mottling and
lignite fragments 7 22
162-90-12ac c
(Log from LaRocque and others, 1963a )
Altitude :
1,942 feet
Scil, silty and clayey, grayish-brown 3 .5 3 . 5Clay, silty, friable, grayish-brown, with limonitic
mottling 1 .5 5
Clay, friable, very compact, grayish-brown 11 16
162-90-12ada
(Log from laRocque and others, 1963a)
Altitude :
1,933 feet
Soil, silty and clayey, dark-gray 2 .8 2 . 8
Clay, extremely compact, light-brown 5 .2 8
Clay, light-brown, with salt pockets and limoniti c
mottling 1.5 9 . 5Clay, extremely compact, olive-brown, with limoniti c
mottling 14.5 24
162-90-12add
(Log from LaRocque and others, 1963a)
Altitude :
1,937 feet
Soil, silty, grayish-brown 1 .3 1 . 3Clay, olive-brown, with limonitic mottling and
lignite fragments 3 .4 4 . 7C:Lay, very friable, brown 13 .3 18
Sand, vew fine, light-brown 1 19
Clay, pebbly, brown 3 22
162-90-12bab
(Log from LaRocque and others, 1963a )
Altitude :
1,934 fee t
Soil, silty and clayey, brown 2 .6 2 .6Clay, very compact, gray-brown, with limoniti c
mottling 7 .2 9 .8Clay, silty, olive-brown, with lignite fragments an d
limonitic mottling 3 .2 13Sand, silty, olive-brown, with lignite fragments 3 .5 16 . 5
229
162-90-12bbb
(log from LaRocque and others, 1963a)
Altitude : 1,941 feet
Geologi csource Material Thickness De th
Soil, silty and clayey, grayish-brown
(feet )
1 .4
feet )
1 . 4Clay, silty, olive-brown, with salt pockets ,
limonitic mottling and lignite fragments 8 .6 10Clay, sandy and pebbly, dark-brown, with lignite
fragments 5 .2 15 . 2Sand, coarse to medium, poorly sorted, saturated,
light-brown 1 .8 1 7Sand, as above but better sorted 1 .5 18 . 5Clay, sandy and pebbly, olive-brown 1 .5 20
162-90-12bcc(Log from LaRocque and others, 1963a )
Altitude :
1,943 feet
Soil, silty and clayey, grayish-brown 5 .5 5 . 5Clay, calcareous, olive-brown, with limoniti c
mottling, lignite fragments, and salt pockets 4 .5 10Clay, pebbly, friable, very compact, olive-brown ,
with lignite fragments and gypsum crystals 5 1 5Sand, clayey, saturated, medium, olive-brown 2 1 7Clay, olive-brown 1 18
162-90-12dad(Log from LaRocque and others, 1963a )
Altitude :
1,936 feet
Soil, silty, dark-grayish-brown 1 .3 1 . 3Clay, silty, calcareous, dark-brown, with limoniti c
mottling and salt pockets 8 .7 10Clay, olive-brown, with limonitic mottling, grade s
with depth to dark-brown 5 .5 15 . 5Clay, dark-grayish-brown 2 .5 18
162-90-12ddd
(log from ImRocque arid others, 1963a )
Altitude :
1,940 feet
Soil, silty and clayey, yellowish-brown 2 2Clay, silty, pebbly, calcareous between 2 and 3 ft . ,
salt pockets below, olive-brown, with limoniticmottling 8 10
Clay, silty, pebbly, olive-brown, with gypsumcrystals and lignite fragments 8 18
230
162-90-13aad(Log from LaRocque and others, 1963a )
Altitude :
1,940 feet
Geologicsource Material Thicknes s
Soil, sandy and silty, brown
feet
1 . 3Clay, very compact, grayish-brown . 7Clay, calcareous, very compact, olive-brown, with
limonitic mottling and lignite fragments 6 . 5
Clay, sandy and silty, olive-brown, with limoniti c
mottling and lignite fragments 1 . 5Clay, very compact, olive-brown, with limoniti c
mottling 11 .5
162-90-13aba(Log from LaRocque and others, 1963a )
Altitude : 1,944 fee t
Soil, silty and sandy, grayish-brown to yellowish -
brown 2 .7
2 . 7
Clay, calcareous, grayish-brown, with limoniti cmottling and lignite fragments 7 .3
10
Clay, olive-brown, with limonitic mottling 14
24
162-90-13add(Log from LaRocque and others, 1963a )
Altitude : 1,936 feet
Soil, sandy and silty, dark-brown 1 .5
1 . 5
Clay, dark-brown .6
2 . 1
Clay, calcareous, olive-brown 1 .6
3 . 7
Sand, light-yellowish-brown, with lignite fragments 1 .8
5 . 5
Sand, very fine, silty, light-brown 1 .3
6 . 8
Clay, olive-brown, with lignite fragments and
limonitic mottling 1 .6
8 .4
Sand, fine, stratified, saturated, reddish-brown 1 .1
9 . 5
Clay, sandy and pebbly, olive-brown .5
10
162-90-13baa
(Log from LaRocque and others, 1963a )
Altitude :
1,942 fee t
Soil, silty and clayey, brown 2 .1 2 . 1
Clay, silty, calcareous to 5 .6 ft ., light-brown to
olive-brown, with limonitic mottling 7 .9 10
Clay, pebbly, olive-brown 6 16
Silt, olive-brown 1 17Sand, clayey, wet but not saturated, olive-brown .5 17 . 5
Clay, sandy, pebbly, olive-brown, with lignit efragments and limonitic mottling 2 .5 20
231
Depth(feet )
1 . 3
2
8 . 5
10
21 . 5
162-90-13bb a(Log from LaRocque and others, 1963a )
Altitude :
1,940 fee t
Geologicsource Material Thickness Ce th
Soil, silty and clayey, grayish-brown
(feet)
2 .4
fee t
2 . 4
Clay, silty, calcareous, olive-brown, with sal tpockets, limonitic mottling and lignite fragments- 7 .6 10
Clay, sandy, olive-brown, with limonitic mottling 3 13Clay, dark-brown, with limonitic mottling .7 13 . 7
162-90-13bbc(Log from LaRocque and others . 1963a)
Altitude :
1,944 fee t
Soil, silty, brown 3
3Clay, silty, calcareous, pebbly, olive-brown, with
lignite fragments and limonitic mottling 13
16
162-90-13dad(Log from LaRocque and others, 1963a )
Altitude :
1,934 feet
Soil, silty, dark-brown 1 .3 1 . 3Clay, sandy, gravel from 2 .7 to 3 .1 ft ., calcareous ,
olive-brown, with limonitic mottling and lignit efragments 4 .1 5 . 4
Clay, extremely compact, olive-brown, with limoniti cmottling 11 .6 17
162-90-13dbb(Log from LaRocque and others, 1963a)
Altitude :
1,946 fee t
Soil, silty, dark-brown 1 .7 1 . 7Clay, silty, calcareous to 4 ft ., olive-brown, wit h
salt pockets and limonitic mottling 8 .3 10Clay, olive-brown, with lignite fragments, limoniti c
mottling, and very thin lenses of lignite sand a t12 .5 ft . 3 .5 13 . 5
Sand, pebbly, poorly sorted, saturated, brown 2 .5 16Clay, pebbly, friable, very compact, dark-grayish -
brown 2 18
162-90-13ddd(log from LaRocque and others, 1963a )
Altitude : 1,944 feet
Soil, silty and clayey, calcareous from 0 .7 to 1 . 7ft ., brown to yellowish-brown 1 .7
1 . 7Clay, silty, olive-brown, with salt pockets ,
limonitic mottling and lignite fragments ; cal -careous from 2 .5 ft . 8 .3
10Clay, pebbly, olive-brown, with lignite fragments ,
limonitic mottling and gypsum crystals 5
1 5(Boulder at 15 ft .)
232
162-90-14aaa(Log from taRocque and others, 1963a )
Altitude : 1,940 feet
162-90-14add
(Log from LaRocque and others, 1963a )
Altitude : 1,949 feet
Soil, silty and clayey, brown, with limoniti cmottling
Clay, sandy and silty, olive-brown, with limoniti cmottling
Sand, fine, silty, yellowish-brownClay, calcareous, salt pockets below 7 ft ., olive -
brown, with limonitic mottling
162-90-14bba
(Log from laRocque and others, 1963a )
Altitude : 1,944 feet
Soil, silty and clayey, grayish-brownClay, grayish-brown, with salt pockets and limoniti c
mottlingSand, silty, fine, yellowish-brown, with limoniti c
mottlingClay, calcareous, olive-brown, with salt pockets ,
limonitic mottling, and lignite fragmentsClay, sandy and silty, grayish-brownClay, reddish-brown, with limonitic mottling
Clay, silty, olive-brown Clay, silty, unweathered, dark-gray
162-90-14bdd
(Log from laRocque and others, 1963a)
Altitude :
1,961 feet
Soil, silty and clayey, grayish-brown to brown 2 .1 2 . 1
Clay, silty, calcareous, light-grayish-brown, wit h
limonitic mottling 2 .2 4 . 3Clay, silty to sandy, olive-brown, with limoniti c
mottling and gypsum crystals 11 .2 15 . 5Sand, fine, well-sorted, saturated, light-brown 1 .5 1 7Clay, sandy, pebbly, olive-brown, with lignite
fragments and gypsum crystals .5 17 . 5
23 3
Geologicsource
Material
Thickness
Dept h
Soil, silty and clayey, dark-gray Clay, olive-brown with limonitic mottling Send, silty, calcareous, medium, yellowish-brown ,
with limonitic mottling Clay, silty, calcareous, pebbly, olive-brown, with
limonitic mottling ; boulder zone at 10 ft .
(feet)
0 .751 .2 5
1
15
(feet )
0 .752
3
18
1 .5 1 . 5
1 .4 2 . 9.6 3 . 5
6 .5 10
2 .1 2 . 1
3 5 . 1
1 .1 6 . 2
1 .2 7 . 4.8 8 . 2
1 .8 107 177 24
162-90-14dcc
(Log from LaRocque and others, 1963a )
Geologicsource
Altitude :
1,953 feet
Thickness Depth(feet )
Material(feet )
Soil, silty, dark-grayish-brown 1 .1 1 . 1Silt, sandy, dark-grayish-brown 1 2 . 1
Silt, clayey, friable, light-gray 1 .3 3 . 4Clay, silty, calcareous, olive-brown, with limonitic
1 .6 5mottlingClay, calcareous, olive-brown, with limonitic
1 .6 6 .6mottlingSand, medium, olive-brown, with limonitic mottling
1 .5 8 . 1and lignite fragmentsSilt, sandy and clayey, calcareous, olive-brown, with
limonitic mottling and lignite fragments .9 9Sand, clayey, fine, saturated below 11 .5 ft ., olive -
brown 3
12
Clay, olive-brain 1
13
162-90-14dda
(Log from LaRocque and others, 1963a )
Altitude :
1,953 feet
Soil, sandy and silty, brown 2 .3 2 . 3Clay, silty, olive-brown, with limonitic mottling an d
lignite fragments 6 .7 9Not sampled 1 10Clay, sandy and silty, olive-brown 1 11Sand, medium, saturated, brown 7 18
162-90-14ddc
(Log from LaRocque and others, 1963a)
Altitude : 1,948 fee t
Soil, silty, dark-brown 1 .3 1 . 3Clay, silty, sandy, light-yellowish-brown with
limonitic mottling and lignite fragments 4 .9 6 . 2Sand, clayey, fine, poorly sorted, light-yellowish-
brown, with limonitic mottling and lignite frag -ments 2 .3 8 . 5
Clay, silty, laminated, olive-brown, with limoniti cmottling and lignite fragments 1 .5 10
Sand, clayey, poorly sorted, stratified, olive-brown 2 12Sand, medium, saturated, brown to light-gray 6 18Silt, sandy, unweathered, wet but not saturated, gray 6 24
162-90-14ddd
(Log from taRocque and others, 1963a )
Altitude :
1,952 feet
Soil, silty and clayey, brown 2 2Clay, silty, calcareous, olive-brown, with sal t
pockets and limonitic mottling----S 3 .2 5 . 2Clay, pebbly, brown, with lignite fragments an d
boulders 11 .8
1 7Sand, fine, well-sorted, saturated at 24 ft ., black 7
24
234
162-90-15aab(Log from LaRocque and others, 1963a )
Altitude : 1,952 feet
Geologi csource
Material
Thickness
De h
feet
fee t
Soil, silty, brown 1 .8
1 . 8Clay, silty, calcareous, olive-brown, with limoniti c
mottling and salt pockets 19 .9
21 . 7
162-90-15abb(Log from LaRocque and others, 1963a )
Altitude : 1,945 feet
Soil, silty and clayey, dark-brown to yellowish-brown 3 3
.5 33 . 5Clay, silty, calcareous gra
ish-brwn - -Clay, sandy and silty, ,
,
salt pockets 1 . 5Clay, very sandy and silty, stratified, yellowish -
brown with limonitic mottling 1 .2 5 . 7Sand,
silty, saturated, yellowish-brown 1 .8 7. 5Clay, silty, olive-brown 2 .5 10Clay, sandy, olive-brown 2 12
162-90-15ada(Lug from LaRocque and others, 1963a )
Altitude :
1,948 feet
Soil, silty, dark-grayish-brain 1 .7 1 . 7Clay,
andsilty and sandy, olive-brown, with salt pocketslimonitic mottling 17 .3 19
162-90-15bcb(Log from IaRocque and others, 1963a )
Altitude :
1,945 feet
Soil, silty and clayey, gray to brown 1 .3 1 . 3Clay, silty, friable, grayish-brown, with limoniti c
mottling and salt pockets 1 .2 2 . 5Clay, silty, olive-brown, with limonitic mottling,
salt pockets and lignite fragments 4 .5 7(Stopped by gravel at 7 ft . )
162-90-15bdd(Log from LaRocque and others, 1963a )
Altitude :
1,957 feet
Soil, clayey and silty, dark-grayish-brown 1 .1 1 . 1Clay, pebbly, olive-brown, with salt pockets,
limonitic mottling, and lignite fragments 14 .4 15 . 5
23 5
162-90-15cbb
(Log from LaRocque and others, 1963a )
Altitude : 1,948 fee t
Geologi csource Material Thickness Ge
h(feet) feet )
Soil, silty, dark-grayish-brown 1 .1 1 . 1Clay, silty, olive-brown, with salt pockets an d
limonitic mottling 3 .9 5Sand, silty, medium, yellowish-brown 1 .5 6 . 5Clay, pebbly, silty, olive-brown, with salt pockets
and limonitic mottling 1 7 . 5Sand, fine, interbedded with clay, olive-brown 4 .5 12
162-90-15cb c
(Log from LaRocque and others, 1963a )
Altitude : 1,953 feet
Soil, silty, dark-brown 1 .9
1 . 9Clay, silty and sandy, olive-brown 3 .1
5Sand, clayey, fine, olive-brown, with limoniti c
mottling 1 .1
6 . 1Clay, silty, olive-brown, with limonitic mottling 11 .9
18Sand, medium, well-sorted, saturated, olive-brown .2
18 . 2Clay, silty, olive-brown, with limonitic mottling .8
19Sand, medium, well-sorted, saturated, olive-brown 3
22Clay, sandy, very compact, olive-brown 1
2 3Clay, sandy, very compact, unweathered, gray 1
24
162-90-15cdc(Log from LaRocque and others, 1963a )
Altitude :
1,963 feet
Soil, silty, dark-brown 1 .1 1 . 1Clay, silty and sandy, olive-brown, with lignit e
fragments, salt pockets, and limonite mottling 18 .9 20Sand, clayey, stratified, olive-brawn 4 24
162-90-15daa
(Log from taRocque and others, 1963a )
Altitude : 1,957 fee t
Soil, silty and clayey, brown 1
1Clay, silty, pebbly, olive-brown, with salt pockets ,
limonitic mottling and lignite fragments ; become smore compact with a depth to a maximum at 14 ft . 14
1 5Gravel, poorly sorted, material ranging from sand t o
boulders, saturated, dark-olive-brown 3
18Clay, sandy and pebbly, dark-olive-brown, wit h
lignite fragments and limonitic mottling 6
24
23 6
162-90-15dad(Log from LaRocque and others, 1963a)
Altitude : 1,965 feet
Geologicsource Material Thickness Dept h
Soil, silty, dark-brown
fee t
2 .1
(feet )
2 . 1Clay, silty, olive-brown, with salt pockets and
limonitic mottling 11 .9 14Sand, medium, olive-brown 7 21Clay, very compact, unweathered, dark-gray 1 22
162-90-15dc d(Log from LaRocque and others, 1963a)
Altitude :
1,966 feet
Soil, silty, dark-brown 0 .6 0 . 6Clay, silty and sandy, olive-brown, with limoniti c
mottling and lignite fragments and salt pockets 17 .4 18Not sampled 6 24
162-90-16cc(Log from LaRocque and others, 1963a)
Altitude : 1,958 fee t
Glacial drift :foil ° 2 2Clay, sandy, yellow 7 9Gravel, sandy, fine 2 11Clay, sandy, yellow, with some gravel and fine sand 16 27Clay, sandy, gray, with some gravel and lignit e
fragments 50 77Gravel and strips of limestone in gray sandy clay 7 84Clay, sandy, gray, with some gravel 8 92Gravel 2 94Clay, sandy, gray, with some gravel and lignite
fragments 61 155Gravel, with lignite fragments 6 161Clay, sandy, yellow, with lignite fragments 9 170
Fort Union Group :
sand, gray 25 195
162-90-16ddd(Log from LaRocque and others, 1963a)
Altitude :
1,952 feet
Soil, silty, grayish-brown 1 .3 1 . 3Clay, silty, olive-brownClay, very silty, pebbly, stratified, calcareous,
.7 2
olive-brown, with limonitic mottling and saltpockets ; very thin lenses of sand at 6 and 8 ft .--
8
10
23 7
162-90-22aaa(Log from LaRocque and others, 1963a )
Altitude : 1,954 fee t
Geologi csource
Material
Thickness
Depth(feet)
(feet )
Soil, silty, black 0 .9
0 . 9Clay, very sandy, saturated, olive-brown 1 .8
2 . 7Clay, silty, olive-brown 6 .6
9 . 3Clay, silty, olive-brown, with lignite fragments 1 .5
10 . 8Sand, medium, well-sorted, saturated, light-brown 1 .7
12 . 5
162-90-22baa(Log from LaRocque and others, 1963a )
Altitude : 1,958 fee t
Soil, silty and clayey, dark-brown 1 .5
1 . 5Clay, calcareous, friable, brown 4 .5
6Sand, medium to fine, wet but not saturated, brown 5
11Clay, brown, with limonitic mottling 3
14Sand, pebbly, coarse-grained, poorly sorted ,
saturated, brown 10
2 4
162-90-23bba(Log from LaRocque and others, 1963a )
Altitude : 1,966 fee t
Soil, silty, dark-grayish-brown 2
2Clay, very silty, calcareous, light-gray to brown ,
with limonitic mottling ; laminated phase from 5 . 6to 7 .9 ft . 6 .4
8 . 4Sand, clayey, calcareous, yellowish-brown 1 .6
10Clay, silty, olive-brown, with salt pockets and
limonitic mottling 10
20(Stopped by boulder at 20 ft . )
162-90-24aab(Log from LaRocque and others, 1963a)
Altitude :
1,950 fee t
Soil, silty, dark-brown 1 .9 1 . 9Clay, silty, gray-brown to brown, with limoniti c
mottling, salt pockets and lignite fragments ;laminated from 3 .1 to 5 ft . 5 .6 7 . 5
Sand, light-yellow-brown, with limonitic mottling .6 8 . 1Clay, sandy and silty, light-olive-brown, with
limonitic mottling and lignite fragments 1 .9 10Clay, silty, olive-brown, with limonitic mottling 3 13Clay, olive-brown, with limonitic mottling 5 18Gravel, clayey, poorly sorted, saturated, olive-brown 4 22
238
162-90-24baa
(Log from LaRocque and others, 1963a )
Altitude : 1,948 fee t
Geologi csource
Material
Thickness
Dept h(feet)
(feet )
Soil, silty and clayey, dark-brown 1 .6
1 . 6Clay, silty, light-brown .9
2 . 5Clay, calcareous, grayish-brown, with limoniti c
mottling and lignite fragments 7 .5
10Clay, pebbly, olive-brown, with lignite fragments an d
limonitic mottling 8
18Sand, coarse, pebbly, clayey, saturated, light-brown 2
2 0Clay, very compact, friable, unweathered, dark-gray 4
2 4
162-90-24bab(log from LaRocque and others, 1963a )
Altitude :
1,944 feet
Soil, sandy and clayey, brown 1 .5 1 . 5Clay, olive-brown 1 2 . 5Clay, sandy, calcareous, olive-brown 1 3 . 5Sand, calcareous, varved, olive-brown, with lignit e
fragments and limonitic mottling 1 .7 5 . 2Clay, silty, olive-brown, with lignite fragments and
limonitic mottling 2 7 . 2Not sampled 2 .8 10Clay, sandy, calcareous, very compact, olive-brown 3 1 3Clay, very compact, unweathered, dark-gray 11 2 4
162-90-34ddd1
(Log from Jensen, 1962 )
Glacial drift :Topsoil, dark-brown 1 1Clay, gravelly, yellowish-gray (till) 10 11
Fort Union Group :
Clay, light-grey 1 12Lignite 6 18Clay, light-gray 2 2 0
162-91-6cc c
Altitude : 1,973 fee t
Glacial drift :Till, dusky-yellow to yellowish-gray 16
16Silt, very sandy, yellowish-green ; contains a few
pebbles 16
32
Fort Union Group :48
80Shale, variegated and thin lignite beds
239
162-91-20cdd
Altitude : 1,939 feet
Geologi csource
Material Thicknes s(feet)
]ethfeet )
Glacial drift :Loam, clayey, black 2 2Silt, clayey and interbedded sand, light-olive-gra y
to brownish-gray 10 12Sand, fine, clayey, green, interbedded with medium-
gray 18 30Till, olive-gray 99 12 9Till, very gravelly, olive-gray 8 13 7
Fort Union Group :Shale, black 3 140Lignite, black 3 14 3Shale, medium-gray 4 14 7Silt, light-gray ° 6 15 3Shale, silty, medium-gray 7 160Shale, medium-gray 3 16 3Shale, silty, light-gray 5 168Shale, medium-gray 5 17 3Sand, fine, dark-greenish-gray, lignitic,micaceous 5 178Sandstone, light-greenish-gray, calcareous 2 180
162-91-24aaa
Altitude : 1,940 fee t
Glacial drift :Till, dusky-yellow, oxidized 9 9Sand, medium to very coarse, gravelly, iron stained 5 14Gravel, fine and medium, moderately well-sorted,
20 34subroundedTill, olive-gray ; contains many sand and gravel
24 58lensesTill, olive-gray 64 12 2Sand, coarse, moderately well-sorted, subrounded 9 131Till, olive-gray 42 173Sand, very fine, clayey, interbedded with olive-gra y
to brownish-black, laminated silt 26 199Clay, silty, light-oligray to olive-gray 9 208Silt, clayey, light-olive-gray 7 215Clay, sandy, olive-gray 10 22 5Sand, very fine, clayey 8 23 3Till, olive-gray 14 24 7
Fort Union Group :Shale, silty, light-gray 7 25 4Lignite, black, fissile 2 25 6clay 1 25 7Lignite, black, fissile 2 25 9Siltstone, light-gray, micaceous 7 26 6Shale, silty, medium-gray 2 268Sand, fine, well-sorted, subangular, micaceous 12 280
240
162-92-lbcc
Altitude : 1,960 fee t
Geologi csource
Material
Thickness
Ge th(feet)
feet )
Glacial drift :Soil, silty, blackish-brown 1
1Clay, silty and sandy, yellowish-brown; calcareous ,
oxidized 17
18Sand, coarse to very coarse, gravelly and silty ,
poorly sorted, angular to subangular 3
2 1Gravel, medium to coarse, silty and sandy, poorly
sorted, angular 6
27Till, olive-gray 73
100Till, medium-dark-gray 100
200Till, gravelly, medium-dark-gray 6
206Till, medium-dark-gray to dark-gray 14
220Till, gravelly, medium-dark-gray 8
228Gravel, medium to coarse, silty, moderately well -
sorted, subangular to subrounded, lignitic 15
24 3Fort Union Group :
Clay, sandy, light-gray ; calcareous 11
254Shale, brownish-gray to brownish-black 6
260
162-92-2cbb
Altitude : 1,968 feet
Glacial drift :Silt, sandy, yellowish-gray, oxidized 6
6Till, dusky-yellow to moderate-olive-brown, oxidized 6
12Gravel, fine and medium, sandy, moderately well -
sorted, subangular and subrounded 17
2 9Sand, fine and medium, lignitic ; contains some silt ,
clay, and very fine sand lenses 76
105Till, dark-olive-gray 24
12 9Gravel, fine to medium, dark-brown, moderately well-
sorted, subangular and subrounded, iron stained 8
137Fort Union Group :
Shale, silty and sandy ; variegated greens and grays 23
160
162-92-2cddl
Altitude : 1,967 feet
Glacial drift :Soil, silty, black 1
1Till, yellowish-brown, oxidized 26
27Sand, medium to coarse, gravelly, moderately well -
sorted in lenses 19
46Clay, sandy and silty, brownish-gray to brownish -
black, calcareous, oxidized 9
5 5Fort Union Group :
Siltstone, dusky-yellow, calcareous 9
6 4Shale, light-gray to medium-light-gray 16
80
241
162-92-4ddd
Altitude : 1,950 fee t
Geologi csource
Materia l
Glacial drift :Soil, silty and sandy, dusky-yellow-brown, oxidized- -Clay, sandy and silty, moderate-brown, calcareous--- -Sand, medium to coarse, clayey, yellowish-brown ,
poorly sorted, angular to subangular Till, medium-dark-gray
Fort Union Group :Lignite, black
Sandstone, greenish-gray ; contains numerous yellowishgray streaks
162-92-30ac(Log from E . H . Prather )
Brown sandGray shale, trace of coalHard panGray shaleCoal, water
162-93-6dd1(Log from LaRocque and others, 1963a )
Altitude : 1,937 feet
Glacial drift :Soil, sandy, brown 3
3Clay, sandy, brown, with angular limestone pebbles 24
2 7Fort Union Group :
Clay, gray, with some strips of lignite 33
60Clay, sandy, gray 30
90Sand, gray 10
100
162-93-llaa(Log from LaRocque and others, 1963a)
Altitude :
1,935 fee t
Glacial drift :Soil 3
3Clay, sandy, yellow 11
14Clay, gray 2
16Gravel 8
2 4Fort Union Group :
Clay, sandy, gray 5
2 9Lignite 2
31Clay, gray 4
35Sand, fine, gray 14
49Lignite 2
51Sand, fine, gray 8
59Lignite 1
60Sand, fine, gray 10
70Clay, brown 11
81Lignite 1
82Sand, fine, gray 12
94Lignite, hard 1
95
242
Thickness
Depth(feet) (feet )
1 122 2 3
17 4 o27 67
4 71
9 80
10 1041 5 1
1 5250 1026 108
162-93-19baa(Log from Montana-Dakota Utilities Co . )
Geologicsource Material Thickness De th
feetfeet
Topsoil 18 18Clay, sand and gravel mixed 2 20Blue like clay, some sand 4 .5 24 . 5Side rock ° .5 2 5Bluish clay 5 3 0Side rock .5 30 . 5Blue clay and sand with hard Streaks 3 .5 3 4Coal, some water .5 34 . 5Gray clay and sand, hard streaks 24 .5 59Hard rock, water 1 60
Gray sandy clay 10 .5 70 . 5Coal, some water 1 71 . 5Green clay ° 3 .5 75Brown-blue clay, hard 11 8 6Coal 1 8 7Bluish clay 3 90Coal .5 90 . 5Bluish-gray clay 15 .5 106Bluish clay and sand, some water 12 .5 118 . 5Coal, water 4 122 . 5Brown clay 1 .5 124
Coal 1 125Brown and blue clay in layers, very tough 10 135Sandstone and clay, no water 9 144Hard brown rock .5 144 . 5Tough brown clay 7 151 . 5Coal, slight trace of water 4 .5 156Tough brown clay 2 158Light-gray clay and sand 2 160Dark-blue clay 4 .5 164 . 5Coal, no water ° 1 .5 166Blue-brown clay ° 6 172Coal .16 172 .16Very hard sandstone .50 172 .66Hard blue clay 4 .34 177Light sandstone 2 179Gray sandstone with trace of clay 9 18 8Hard rock .5 188 . 5Soft sandstone 3 191 . 5Sandstone 4 .5 196Sandstone, salt and pepper 14 210Sand and clay 1 211Sandstone, salt and pepper 3 214Sandstone, brown-blue 4 218Soft sandstone 8 226Sandstone, blue, salt and pepper 4 230Dark-blue clay 5 23 5Dark-blue shale 12 .5 247 . 5Blue clay 5 .5 253coal .5 253 . 5Blue-brown clay, hard 2 .5 256
Coal, trace of water 1 .5 257 . 5Blue-brown clay, hard 3 .5 26 1
Coal, trace of water 2 .25 263 .2 5Brown clay 12 .75 276
Sandy blue clay 1 277Fine sandstone 3 280Hard dark clay 1 .5 281 . 5Dark-blue shale 5 .5 287Fine texture sandstone, no water 6 293Dark-blue shale 11 304
Hard blue clay 6 310
Light-blue clay 2 312
Sandy clay, brown 4 31 6
Hard gray slate rock 1 .75 317 .75
Chalk stone 22 .25 34 0
Clay and chalk stone 3 343243
162-93-19baa, Continue d
Geologi csource Material Thickness
le2t—)thfeet(feet )
Chalk stone 6 3491 350
noal ' slight trace of water 1 3512 353
Blue clay ' ' ' 4 3578 365
Blue clay 2 367Sandy clay
—'—' ' 3 opoan^ st" ne .water 7 377
2 .25 382 .2 5.75 383
3 386Ha, 2 388Brown. sandstone, hard spots, water 28 416Brown-blue sandstone, coarser, water 4 42oBlue sandstone, coarse, water 13 433Brown 3 436
4 44onoaz .some water 1 .5 441 . 5
u62(Log from Montana-Dakota Utilities Co . )
Gumbo 10 10Gravel and sand 24 34Hard rock 2 36clay
' 21 5 7coal----'----'----'--'--'---' 3 ^oRock"~---'--' ' '—' z 61
20 81coal -' '---' ' 4 8 5Sandy claycoal -'--'—' '----'--'—' 2 .5 127 . 5Light colored clay ----' '--' ' 37 .5 165sand 30 195Rook----'---'--"--'--'—'---' 3 .5 198 . 5oanu ' ' 43 .5 242coal ' 8 250clay 78 32 8coaz ' 1 329Sandy clay 30 359
8 369
clay -- . .-- .--.— .—.-- . 11 383rine sand 12 395Coarse sand 27 42 2Hard sand 19 441Clay and sand
~~~~~~~~~~~~~~~~~~~~2
3 ~~cla,—'—'--'---'--' '---'—'--- 17 118 7
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162-94-29aa a
Altitude : 2,210 fee t
Geologi csource
Materia l
Glacial drift :Silt, sandy with pebbles, yellowish-grayTill, moderate-olive-brown, oxidized Gravel, fine and medium, sandy, moderately well -
sorted, iron stainedTill, moderate-olive-brown to light-olive-gray ,
oxidizedGravel, fine, sandy, moderately well-sorted, sub -
roundedSand, medium, siltyTill, olive-grayGravel, fine to coarse, moderately well-sorted, sub -
angular to subroundedTill, olive-gray
Fort Union Group :Sand, fine, light-greenish-gray, chalky Sand, fine, clayey, greenish-gray Sandstone, greenish-grayShale, silty, medium-gray
163-88-llccc
Altitude : 1,868 feet
Glacial drift :Till, silty, dusky-yellow to moderate-olive-brown 28 2 8Till, olive-gray ; contains a few sand and gravel
12 40stringersTill, olive-gray 54 9 4
Fort Union Group :Clay and silt, dark-brown to brownish-black, carbon -
16 110aceousShale, medium-gray to light-greenish-gray 10 120
163-89-lobbb
Altitude : 1,870 feet
Glacial drift :Sand, medium to coarse, reddish-brown, well-sorted ,
subangularTill, moderate-olive-brown, oxidized Till, olive-gray
Fort Union Group :Silt, clayey, very-light-gray, calcareousShale, silty, medium-graySilt, light-gray to white, highly calcareousSand, fine, dark-greenish-gray, lignitic, micaceous
246
Thickness Depthfeet (feet )
4 448 52
4 56
14 70
3 735 78
36 114
8 12 26 12 8
16 1447 1512 15 37 160
6
6
9
1 56o
7 5
3
785
8312
9 55
100
163-89-1oddd
Altitude : 1,882 fee t
Glacial drift :Sand, fine to medium, brown, well-sortedSilt, clayey to sandy, dusky-yellow, oxidized
Clay, silty to sandy, moderate-olive-brown, oxidized
Till, moderate-olive-brown to olive-gray, partiall y
oxidizedSand, fine, slightly clayey, dark-greenish-gray ,
micaceousTill, olive-gray
Fort Union Group :Shale, silty and sandy, very-light-gray, micaceous ,
highly calcareous
163-89-17da
(Log from LaRocque and others, 1963s )
Altitude : 1,876 feet
Glacial drift :Sand, brown, and bouldersClay, sandy, brownSandstoneClay, sandy, brown, with strips of limestoneClay, sandy, grayClay, sandy, brownClay, sandy , gray , with lignite fragmentsClay, sandy gray, with some gravel and lignite frag -
mentsSand, fine, and gravel with boulders and lignit e
fragmentsBoulderSand, fine, and gravel with boulders and lignit e
fragments °Boulders, with gravel and fine sand Gravel, with lignite fragments Gravel, fine sand with boulders, strips of clay an d
lignite fragmentsFort Union Group :
Sand, fine, gray
163-89-21bbb(Log from Jensen, 1962 )
Glacial drift :Topsoil, sandy, blackClay, sandy, light-brown and gray Clay, sandy, pebbly, tan (till)Sand, coarse, clayeyClay, sandy, bouldery, tan (till) Clay, gray with sand, gravel and numerous boulder s
(till)Clay, yellow and white ; sand, gravel, and numerous
boulders (till)Gravel and boulders . Hole abandoned
24 7
Yeet
3129
33
182 6
39
(feet )
31524
57
75101
140
10 1016 261 2 73 30
17 4 71 48
60 108
51 159
30 1892 191
9 200
3 20 38 211
71 282
18 300
1 12 3
17 2 06 2 6
16 42
175 217
18 23 55 240
Geologicsource
Material
Thickness
Depth
163-89-26ddd
Altitude : 1,900 feet
Geologicsource
Material
Thickness
De th
Glacial drift :Sand, fine to medium, reddish-brown, well-sorted ,
subroundedSilt, clayey, dusky-yellow ; contains thin lenses o f
sand and gravel, and locally contains pebble s(tin)
Clay, silty, light-olive-grayTill, olive-graySand, coarse, brown, well-sorted, subangular to sub-
roundedTill, olive-grayGravel, coarse ; contains cobbles and small boulders ,
principally granitic rocksFort Union Group :
Silt, clayey, white to very-light-gray, highly cal-careous
Sand, very fine, silty, light-olive-gray to light -greenish-gray
163-89-29add(log from Jensen, 1962 )
Glacial drift :Topsoil, sandy, blackClay, sandy, light-tan (till)Clay, sandy, tan (till)Sand, fine, medium, and coarseSand, fine to very coarse, clayeySand, fine and mediumGravel, fine and considerable clayClay, very gravelly, dark-gray (till)Clay, gray ; numerous limestone, dolomite, and other
rock fragments scattered throughout sample (till)Fort Union Group :
Clay, light-gray to whiteClay, light-brownClay, dark-grayClay, very light-greenish-gray, becoming nearly whit e
in placesClay, sandy, dark-gray to black
(feet) feet )
5 5
14 194 2 3
20 4 3
15 5827 8 5
6 9 1
11 10 2
18 12 0
1 118 1911 30
5 3 55 40
10 505 55
15 70
77 147
8 15 55 16o2 162
7 .5
169 . 5
.5
170
248
163-89-31c c(Log from LaRocque and others, 1963a )
Altitude : 1,933 feet
Geologi csource Material Thickness De th
Soil, silty and clayey, calcareous, brown
(feet )
3
feet )
3Clay, silty, calcareous to 4 ft ., olive-brown, with
lignite fragments and limonitic mottling 7 10Clay, pebbly, olive-brown, with salt pockets, gypsu m
crystals, lignite fragments, and limoniti c
mottling 9 19Send, very silty, light-brown 1 20Gravel, sandy, poorly sorted, saturated, olive-brow n 1 2 1
163-89-36ddd
Altitude : 1,895 feet
Glacial drift :Sand, fine to medium, reddish-brown, well-sorted ,
subrounded 10
10Till, dusky-yellow to moderate-olive-brown, oxidized 19
29Till, moderate-olive-brown to olive-gray, partiall y
oxidized 12
41Sand, medium to coarse, light-brownish-gray,
moderately well-sorted 7
48Till, olive-gray 18
66Sand, coarse, gravelly, moderately well-sorted, sub -
angular and subrounded 12
78Till, silty, olive-gray 193
271Rocks or very coarse gravel (drilling action an d
E -log) 5
276Till, olive-gray 37
313Send, drill action and E-log (no samples) 4
317Till, olive-gray 25
342Gravel ; drill action and E-log (no samples) 7
349
light-olive-gray 24
422
Fort Union Group :Sand, dark-greenish-gray (very poor samples and
E-log) 30
45 2Shale, drill action and E-log (no samples) 8
46 0Lignite, black 5
465Shale (poor samples) 15
48 0
249
Till, olive-grayClay, olive-blackSilt and clay, olive-gray, interbeddedSilt, clayey, olive-gray; sand, very fine to fine,
25
3748
38216
398
163-90-15c c
(Log from LaRocque and others, 1963a )
Altitude : 1,926 fee t
Geologicsource
Material
Thickness
Depth(feet)
(feet )
Glacial drift :Soil 1
1
Clay, sandy, yellow, with some gravel 18
19
Clay, sandy, gray, with some gravel 28
4 7
Gravel 2
49Clay, sandy, gray----- 1
5 0Gravel 9
5 9Clay, sandy, gray, with some gravel 31
90Clay, sandy, gray, with some gravel and boulders 20
110Clay, gray, with some gravel, boulders, and lignit e
fragments 62
172
Boulders, with gravel and lignite fragments 50
22 2Fort Union Group :
Lignite, hard 8
230
163-90-30dad
Altitude : 1,946 fee t
Glacial drift :Till, yellowish-gray, oxidized ; contains stringer of
coarse sand 16
16Till, moderate-olive-brown, oxidized 11
2 7Till, olive-gray 69
96Gravel, fine, sandy, moderately well-sorted, general
ly subrounded 6
102
Clay, silty and sandy, olive-gray ; contains pebble s(till?) 7
109Gravel, fine, sandy, lignitic 3
112Clay, silty and sandy, olive-gray 3
115Sand, medium, gray, lignitic 3
118Clay, silty and sandy, olive-gray 6
12 4Gravel and cobbles, subrounded 6
130Till, olive-gray 22
152Sand, fine, slightly clayey, gray 5
15 7Till, olive-gray 40
19 7Fort Union Group :
Sand, very fine to fine, light-green ; silt, light-gray and light-olive-gray, calcareous ; shale ,gray ; lignite (2 thin beds) 43
240
163-90-31cc e(log from LaRocque and others, 1963a )
Altitude : 1,934 feet
Glacial drift :soil 3
3Clay, sandy, brown, with some gravel 22
2 5Clay, yellow, very sandy 11
36Clay, sandy, gray, with some gravel 4
40Gravel, fine 8
48Clay, sandy, gray, with some gravel and lignite frag
ments 147
195Gravel 6
201Fort Union Group :
C lay, gray 17
218Lignite 2
22 0Clay, sandy, with strips of lignite 35
255
250
163-90-32cb c(Log from C . A . Simpson & Son)
Geologi csource Material Thickness Ge th
feet(feet )
Topsoil 1 1Yellow clay 37 38Gray clay 81 11 9Sand and gravel 12 13 1Gravelly blue clay 4 13 5Gravel with clay 3 13 8Gravel 4 142Bissing 137 279Coarse gravel and fine sand 4 283Sand 5 288Coarse sand and gravel 3 291Sand and clay 3 294Coal and 1 295coal 9 304Missing 321 62 5blue clay 10 63 5Clayey sand 29 664bark-gray shale 11 67 5Clayey sand 40 71 5
163-90-34ddd(Log from LaRocque and others, 1963a)
Altitude :
1,946 fee t
Soil, silty, grayish-brown 2 2Clay, calcareous, grayish-brown to olive-brown, with
lignite fragments and limonitic mottling 8 10Clay, pebbly, very compact, olive-brown, with
limonitic mottling and lignite fragments 5 1 5Boulder, dolomite " 2 .5 17 . 5Sand, clayey, medium, saturated, olive-brown 4 21 .5
163-90-36cb(Log from LaRocque and others, 1963a )
Altitude :
1,913 feet
Glacial drift :Soil 3 3Clay, yellow 6 9Clay, brown, with some gravel 19 28
Clay, gray 8 36Clay, sandy, gray, with some gravel and lignit e
fragments 114 150Boulder, limestone 1 151Clay, sandy, gray, with some gravel and lignit e
fragments 18 169Gravel, with strips of gray sandy clay 3 172Clay, gray, sandy, with lignite fragments 8 180
Gravel and boulders 21 20 1Clay, sandy, gray, with some gravel 5 206
Fort Union Group :Lignite, hard 14 220Sand, gray 15 23 5
25 1
163-90-36cc c(Log from LaRocque and others, 1963a)
Altitude : 1,938 feet
Geologi csource Material Thickness Depth
Soil, silty, dark-brown to olive-brown
(feet )
1 .5
(feet )
1 . 5Clay, silty, calcareous, olive-brown, with sal t
pockets, limonitic mottling and lignite fragments 6 .5 8Clay, olive-brown, with limonitic mottling and salt
pockets 3 11Clay, very friable, pebbly, brown 1 12Sand, pebbly, poorly sorted, olive-brown 1 13Sand, clayey and silty, poorly sorted, more claye y
with depth, light-brown 2 15Clay, sandy and pebbly, olive-brown 4 19Clay, pebbly, olive-brown, with lignite fragments 2 2 1Sand, fine, well-sorted, saturated, olive-brown 2 23Clay, dark-brown 1 ?4
163-91-4bbb
Altitude : 1,940 fee t
Glacial drift :Loam, clayey to sandy, black 1
1Till, yellowish-gray 3
4Till, moderate-olive-brown 19
2 3Clay, silty, black, oily 3
2 6Sand, slightly clayey, moderate-olive-brown 7
3 3Till, olive-gray 28
61Till, gravelly, olive-gray 30
9 1Till, olive-gray 73
164Till, gravelly, olive-gray 21
18 5Gravel, fine and medium, well-sorted, subangular an d
subrounded 5
19 0Clay, silty and sandy, olive-gray 6
19 6Gravel, fine and medium 4
20 0Till, olive-gray 47
247Sand, very fine to fine, clayey, light-olive-gray t o
olive-gray 23
270Silt, clayey, olive-gray 6
276Till, olive-gray to dark-olive-gray 81
35 7Sand, medium to very coarse, gravelly, moderately
well-sorted in lenses, generally subrounded 16
373Clay, sandy; contains some thin sand and gravel
lenses 36
40 9Sand, medium to very coarse and clay, light-olive -
gray to tan 7
416Clay, sandy, olive-gray to dark-greenish-gray, cal -
careous 4
420Till, olive-gray 11
43 1Cobbles and boulders 5
43 6Fort Union Group :
Sand, very fine and fine, dark-greenish-gray, lignite
13
44 9Shale, light-olive-gray 8
45 7Sand, very fine and fine, dark-greenish-gray 3
46o
252
163-91-4ddd 1
Geologicsource
Materia l
Clay---_' "Boulders and coarse sandBlue clay__° '---'-'Fine sand
163-91-21aa(Log from IaRocque and others, 1963a )
Altitude : 1,939 feet
Glacial drift :soil ° '--' 'Clay, sandy, yellow, with gravelClay, sandy, gray, with gravelGravel and bouldersClay, sandy, gray, with narrow strips of gravelC lay, sandy, gray, with gravelGravel and boulders Clay, sandy, gray, with gravel and bouldersGravel °Clay, s andy, gray °GravelClay, sandy, gray, with bouldersLimestone, fine grained, hard, grayClay, sandy, gray, with gravel and boulders
Fort Union Group :sand, compact, gray, with strips of lignite
163-92-8ddd
Altitude : 1,930 feet
Glacial drift :Till, yellowish-gray, oxidized 8
8Till, moderate-olive-brown, oxidized 59
67TL11, olive-gray 7
74Gravel, fine to medium, sandy, unsorted, subangular
to subrounded 5
79Till, olive-gray 23
102Fort Union Group :
Silt, light-gray, light-olive-gray, and light -greenish-gray, locally carbonaceous ; contains someinterbedded very fine sand 34
136L9g:Ate, black 3
13 9dale, silty, light-gray ° 9
148Sand, very fine, light-olive-gray and light-greenish
253
Thickness11-11V—)''feet
202 72838
fee t
2071
10
1 130 3 138 692 715 764 8 05 85
10 951 961 971 988 1061 107
41 14 8
22 170
12
160
163-92-14bbb
Altitude : 1,938 fee t
Geologicsource
Material Thickness Depthfeet (feet )
Glacial drift :Till, yellowish-gray, oxidized 8 8Till, moderate-olive-brown, oxidized 50 5 8Till, olive-gray 40 98Clay, silty, olive-gray 8 106Clay, very silty, olive-gray, contains sand grain s
and pebbles (till?) 60 166Clay, very silty, olive-gray ; contains numerous sand
and fine gravel lenses (lacustrine?) 71 237Till, olive-gray 42 279Clay, olive-gray to olive-black 11 290Till, olive-gray, contains many lignite chips 46 336Gravel, medium and fine, sandy, moderately well -
sorted, subangular and subrounded 8 344Till, olive-grey 25 369
Fort Union Group :Sandstone, fine grained, dark-greenish-gray 3 372Sand, very fine to fine, slightly clayey, greenish -
gray to dark-greenish-gray 28 400
l63-92 - 20 dd d
Altitude : 1,934 fee t
Glacial drift :Till, yellowish-gray to moderate-olive-brown ,
oxidized • 20
2 0Silt, clayey, moderate-olive-brown, contains lense s
of very fine and fine, light-brownish sand 25
45Gravel, fine to coarse, sandy, generally subangular 4
4 9Till, olive-gray 44
93Till, gravelly, olive-gray 12
105Till, olive-gray 81
18 6Fort Union Group :
Sand, fire, very light-greenish-gray; locally clayey 34
22 0
163-92-21sa(Log from LARocque and others, 1963a )
Altitude : 1,927 feet
Glacial drift :Soil 2
2Clay, yellow, with some gravel 3
5Clay, brown, with some gravel 16
21Clay, gray, with some gravel 18
39Clay, sandy, gray, with some gravel, lignite an d
limestone fragments 110
149Clay, sandy, gray, with hard strips of limestone 27
176Clay, sandy, gray, with some gravel, lignite an d
limestone fragments 18
194Gravel ° 6
200Clay, sandy, gray with some gravel 4
204Gravel 12
216Clay, sandy, gray with some gravel 29
245Fort Union Group :
Clay, sandy, grey 40
285Sand, fine, gray 10
295
254
163-92-28ddd
Altitude : 1,950 feet
Geologi csource
Material Thickness Depth(feet) (feet )
Glacial drift :Till, yellowish-gray, oxidized 7 7Till, moderate-olive-brown, oxidized 29 3 6Till, olive-gray 36 72Clay, silty and sandy, olive-gray ; contains numerou s
sand and fine gravel lenses 42 114Gravel, fine and medium, sandy, moderately well -
sorted in lenses, subrounded 12 126Clay, silty and sandy with pebbles, olive-gray ;
contains numerous thin sand and fine gravel lense s(till?) ° ° 62 188
Fort Union Group :
Lignite, black, fissile 7 19 5Shale, sandy, medium-gray 7 202Limestone, gray 2 204Shale, medium-gray to light-greenish-gray, lignitic 16 220
163-92-32ddd
Altitude : 1,947 fee t
Glacial drift :Soil, silty and sandy, brownish-gray 1
1Clay, sandy and silty, calcareous, oxidized 16
17Clay, sandy, oxidized ; gravel, medium to coarse,
7
24sandy, poorly sortedClay, yellowish-brown, calcareous, oxidized 2
26Till, medium-dark-gray 34
60Clay, sandy and silty, medium-light-gray, calcareous 11
71Fort Union Group :
5
76LigniteShale, brownish-gray to brownish-black, carbonaceous 4
80
25 5
(Log from E . H . Prather )
Altitude : 1,960 feet
Geologi csource
Material
Thickness
Depth
(feet)
,==, /
Brown topsoil 5 5Brown sandy 18 2 3
Lighter sand (caving
rolling sand)
_. 21 w~
Gray "hale ' ' ' 16 ^«Gray sand (small amount of water) 8 68Gray clay 2 70
Gray sandy shale (some gravel) 17 8 7
Coal (water) 2 8 9Fine sand 11 100
Gray clay 6 Io6coal 3 109Gray sandy shale 7 116Gray clay 22 138Gray sandy shale 7
owGray clay . 5
150
Hard shell (gray) 2
152clay
_.— . . .__ .---' '
16
1 8
Gray sandy shal
e Gray
16
ua
coal 6
1 0Gray shale 50
wmHard shell 6
*w
Gray clay ' '
6
252
Coal 7
259
Gray clay 1
260
Coal (water) 11
271Gray clay 3
274Hard shell 1
27 5
16s-92 ' sm^m
Altitude : 1,940 feet
Glacial drift :Till, yellowish gray to
oxidized m
14r -~moderate-olive-brown, oxidized ; "~~~"" fe wTill, moderate-olive-brown ,
thin sand lenses 32
ws
Till, olive-gray 50
96Gravel, fine, sandy, "dirty" , poorly sorted 11
10 7Sand, medium, well-sorted, "ubro"nd°^ '
6
113Till, olive-gray ; contains numerous lignite chip~ ' 65
178Fort Unio
Lignite, black, fissile nGroup :
Clay, sandy, black, oily 3
184Lignite, black, fissile 3
187
256
163-92-36dd(Log from LaRocque and others, 1963a)
Altitude : 1,947 feet
Geologicsource
Material
Thickness
Depth(feet)
(feet )
Glacial drift :Soil 2
2Clay, sandy, brown, with gravel 10
12Boulder 1
1 3Clay, sandy, brown, with gravel 15
28Clay, sandy, gray, with gravel 2
30Gravel 1
31Clay, sandy, gray, with gravel and lignite fragments 9
40Gravel and boulders 1
4 1Clay, sandy, gray, with gravel 20
61Fort Union Group :
Clay, sandy, gray, with strips of fine sand andlignite fragments 23
84Lignite 4
88Clay, gray, with strips of lignite 2
90Clay, gray 25
11 5Sand, compact, gray, with strips of gray clay 5
120
163-93-13aaa
Altitude : 1,925 feet
Glacial drift :Till , yellowish-gray, oxidized 8
8Till, dusky-yellow to moderate-olive-brown 25
3 3Till, olive-gray 24
5 7Till, olive-gray ; contains much locally derived
bedrock clay, sand, and silty shale 20
7 7Till, olive-gray 40
11 7Fort Union Group :
Shale, silty, light-olive-gray to brownish-black ;contains thin seams of lignite 10
12 7Sand, very fine, clayey, light-olive-gray ; inter-
bedded with carbonaceous material 8
13 5Shale, silty to sandy, light to medium-gray 11
146Sand, fine, clayey, greenish-gray, well-sorted ,
subangular, micaceous and lignitic 14
160
163-93-17ddd
Altitude : 1,917 fee t
Glacial drift :Soil, silty and sandy, yellowish-brown 1
1Clay, silty, yellowish-brown to medium-dark-gray ,
calcareous, oxidized (till?) 22
2 3Sand, coarse to very coarse, silty, poorly sorted ,
angular to subangular, oxidized 15
38Till, moderate-olive-brown, oxidized 10
48Gravel, medium to coarse, sandy, silty, angular t o
subangular 9
57Clay, olive-gray, calcareous 5
62Gravel, medium, and medium to coarse sand, moderatel y
well-sorted in lenses, angular to subrounded 11
73Till, olive-gray 7
80
257
163-93-18aaa
Altitude : 1,917 feet
Geologi csource
Material Thickness Dept h
Glacial drift :Soil, silty and sandy, brownish-black
(feet )
1
(feet )
1
Till, moderate-yellowish-brown, oxidized 23 24
Till, olive-gray 65 89Fort Union Group :
Lignite ° 1 90Shale, light-gray to light-bluish-gray, siliceous 30 120
163-93-19aaa
Altitude : 1,916 feet
Glacial drift :Soil, silty and sandy, brownish-black 1 1
Till, moderate-yellowish-brown, oxidized ; contains a11 12few reddish-brown zones
Till, olive-gray 93 10 5Sand, fine to coarse, moderately well-sorted ,
angular to subrounded 2 10 7
Till, olive-gray 27 13 4Clay, very silty and sandy, olive-gray, calcareous
(fluvial) 116 250
Clay, silty and sandy, olive-gray to dark-greenish -gray, calcareous ; contains some interbedded san dlenses (fluvial) 65 31 5
Till, olive-gray 36 35 1Gravel, fine to coarse, moderately well-sorted ,
angular to subrounded 5 356Till, olive-gray 24 380Till, olive-gray to moderate-brown, partially
oxidized 68 448Fort Union Group :
Shale, light-bluish-gray, siliceous 12 460
258
163-93-19ad d
Altitude : 1,919 feet
Glacial drift :Soil, silty to sandy, brownish-black Till, sandy to silty, moderate-yellowish-brown t o
reddish-brown, oxidized :Gill, silty, olive-grayClay, sandy, olive-gray and light-gray lenses, cal -
careous (fluvial) Till, silty and gravelly, olive-gray Clay, very sandy and silty, olive-gray, calcareous ;
contains a few light-gray clay lenses (fluvial)
Till, olive-gr'ayClay, very silty and sandy, olive-gray to dark -
greenish-gray, calcareous ; contains some brownishblack (organic) and light-gray clay lense s
(fluvial)Gravel, fine to coarse, moderately well-sorted ,
angular to rounded ; 40 to 50 percent limestone and
dolomite pebbles, 50-60 percent granitic, quartz ,shale,and calcareous sandstone pebbles
Till, silty, olive-gray Gravel, fine to coarse, moderately well-sorted ,
angular to roundedClay, very sandy, olive-gray to light-gray,
calcareousGravel, fine to coarse, moderately well-sorted ,
angular to roundedTill, olive-gr'ayClay, very sandy, olive-gray, calcareous (fluvial) Clay, silty and sandy, olive-gray, contains a few
pebbles (till?)Sand, fine to medium, gravelly, poorly sorted Clay, sandy and silty, olive-gray, calcareous
Sand, medium to very coarse, gravelly, poorly sorted Gravel, fine to very coarse, sandy, angular t o
roundedFort Union Group :
Sandstone, fine to medium, light-bluish-gray togreenish-gray
163-93-19bcc
Altitude : 1,925 feet
Glacial drift :Soil, silty and sandy, brownish-black 1
1
Till, moderate-yellowish-brown 24
25
Till, sandy (about 45 percent), olive-gray to dark -
greenish-gray 49
74
Till, olive-gray 66
144
Clay, very silty, sandy, olive-gray, calcareous ;contains a few light-gray laminations (fluvial) 72
212
Till, olive-gray 24
236Clay, very silty, sandy, olive-gray ; contains a few
light-gray lenses (fluvial) 6
242
Fort Union Group :Sandstone, fine to medium, clayey, medium-bluish -
gray, slightly calcareous 15
25 7Shale, medium-dark-gray, siliceous and slightl y
calcareous 8
265
25 9
Geologi csource
Material
Thickness
De th(feet) feet
1 1
19 2 018 38
50 88109 197
10 207
43 250
25 27 5
10 28 515 300
7 30 7
3 310
17 32 7
23 35025 37 5
5 38015 39 51 39 624 420
56 476
4 480
163-93-19ccc l
Altitude : 1,916 fee t
Geologi csource Thickness Dept hMaterial
Glacial drift :Soil, silty, sandy, brownish-black
(feet )
1
(feet )
1Till, moderate-yellow-brown to dark-yellowish-brown,
24 2 5oxidizedTill, olive-gray 75 100Till, olive-gray to dark-gray 50 150Clay, very silty, sandy, olive-gray ; contains a few
30 180light-gray clay lenses (fluvial)Till, olive-gray 33 213Sand, medium to coarse, clayey, moderately well -
4 21 7sorted, angular to subrounded Till, olive-gray 51 268Gravel, fine to coarse, sandy, moderately well-sorted
in lenses, angivlar to subrounded 30 298Clay, gravelly, medium-gray 4 302Gravel, fine to very coarse ; contains cobble size
28 330material
163-93-19ccc 2
GlacialAltitude :
1,916 fee tdrift :
Till, oxidized 19 19Till 155 174Gravel 2 9 203Till, sandy 18 221Gravel and rocks 10 231Till ° 32 263Gravel 2 7 290
163-93-19dda
Altitude : 1,923 fee t
Glacial drift :Soil, sandy, silty, brownish-black 1 1Till, moderate-yellowish-brown, oxidized ll 1 2Till, olive-gray 48 60Clay, very silty, sandy, olive-gray ; contains light -
olive-gray lenses (fluvial) 13 73Gravel, fine to medium, sandy, poorly sorted, angula r
to subrounded 1 74Till, olive-gray 59 133Gravel, fine to coarse, sandy, moderately well -
sorted in lenses, angular to subrounded ; pebble sare 60 to 70 percent limestone and dolomite an d30 to 40 percent shale and granitics 11 144
Till, olive-gray 40 18 4Gravel, fine to coarse, sandy, moderately well-sorte d
in lenses, angular to subrounded ; pebbles areabout 50 percent siliceous rocks 33 21 7
Fort Union Group :
43 260Shale, light-gray to medium-gray, calcareous
260
163-93-20aaa
Altitude : 1,919 feet
Geologicsource
1aterial Thickness De
hfeet )(feet)
Glacial drift :Soil, sandy, silty, brownish-black 1 1
Clay, silty and sandy, yellowish-brown, calcareous ;
(probably till) 32 33Gravel, coarse, moderately well-sorted, angular to
subangular 10 43
Clay, very silty, sandy, moderate-olive-brown ,
oxidized 8 51Gravel, medium to coarse, sandy, moderately well -
sorted in lenses 18 69
Till, medium-dark-gray to dark-gray 31 100
Till, gravelly, medium-dark-gray to dark-gray 20 120
Silt, light-gray, calcareous 16 136
Gravel, coarse, moderately well-sorted, angular t o
subrounded ; predominantly limestone 5 14 1
Silt, very sandy, light-gray, highly calcareous 6 14 7Sand, very fine to fine, well-sorted, subangular to
subrounded 16 16 3Till, silty, medium-light-gray 37 200
Gravel, medium to coarse, sandy, poorly sorted ,
angular to subangular 3 203
Clay, medium-dark-gray, calcareous 26 229
Gravel, coarse, sandy, moderately well-sorted ,angular to subangular 4 23 3
Clay, medium-dark-gray, calcareous ; contains thinlenses of medium to coarse sand 7 240
Boulders and medium to coarse sand 7 24 7
Gravel, medium to coarse, moderately well-sorted ,
angular to subrounded ; pebbles are predominantlylimestone and shale 9 25 6
Till, dark-gray 24 28 0
Till, medium-gray to medium-dark-gray ; contains a few
inclusions of black oily, organic material 18 298Clay, silty, grayish-black to brownish-black, cal -
careous ; contains a few thin lenses of light-grayclay 55 353
Sand, coarse to very coarse, well-sorted, subangula r
to subrounded ; pebbles are about 30 percent shale
and 35 percent limestone and dolomite, remainde rare principally granitic and sandstone 26 379
Clay, silty and sandy, light-gray, calcareous 4 383
Gravel, coarse to very coarse, well-sorted, sub -rounded to rounded 37 420
Sand, very coarse, clayey 14 43 4
Gravel, coarse to very coarse, well-sorted, sub -
rounded to rounded 49 48 3
Fort Union Group :
7 4 90Shale, sandy, very pale-blue to light-blue, cal -
careous
26 1
163-93-2occ c
Altitude : 1,924 fee t
Geologicsource
Material
Thickness
De th(feet)
fee t
Glacial drift :Soil, silty, sandy, brownish-black 1
1
Till, moderate-yellowish-brown, oxidized 19
20
Till, olive-gray 12
32Gravel, fine to coarse, sandy, clayey, poorly sorted 4
36
Clay, very silty, olive-gray, calcareous ; containsnumerous light-gray clay lenses (fluvial) 40
76
Till, olive-gray, locally gravelly i4
190 90
Till, olive-gray 58Sand, very fine to fine, clayey and silty, poorl y
sorted, angular to rounded 12
16 0
Clay, very silty, sandy, olive-gray, calcareous
(fluvial) 7
167Gravel, medium to coarse, sandy, moderately well -
sorted in lenses, angular to rounded ; pebbles are
20 to 30 percent limestone, 15 to 20 percent shale ,25-30 percent chalcedony, the remainder is quart zite, granitic, and sandstone 8
175Fort Union Group :
Sandstone, fine to medium, light-bluish-gray, cal-careous 25
200
163-93-21cbb
Altitude : 1,916 feet
Glacial drift :Soil, silty, sandy, and clayey, brownish-black 1
1Till, moderate-yellowish-brown, oxidized 21
2 2Till, olive-gray 66
8 8Gravel, medium to coarse, sandy and clayey, poorl y
sorted, subangular to subrounded 4
92Till, olive-gray ; gravelly near bottom 62
15 4Gravel, fine to coarse, sandy, moderately well -
sorted in lenses, subangular to rounded 46
20 0Fort Union Group :
Sandstone, fine to medium, clayey, medium-bluish -gray ; contains a few thin lignite beds betwee n200 and 208 ft . 40
24 0
262
163-93-22cdd
Altitude : 1,920 feet
Geologicsource
Material
Thickness
Depthfeet (feet )
Glacial drift :Soil, silty and sandy, brownish-black 1 1
Till, moderate-yellowish-brown, oxidized 35 3 6Till, olive-gray 92 ]2 8
Clay, silty and sandy, olive-gray; contains thinmedium-gray and light-olive-gray lenses (fluvial) 34 162
Till, olive-gray 12 174
Gravel, fine to medium, sandy, angular to subrounded ;
contains interbedded clay lenses 20 194Clay, silty, sandy, medium-gray to medium-dark-gray,
calcareous, lignitic (fluvial) 4 198
Sand, fine to coarse, poorly sorted, angular to sub -
rounded-------- 2 200
Till, olive-gray 14 214Fort Union Group :
Sandstone, fine to medium, clayey, medium-bluish -26 240gray, slightly calcareous
163-93-23aa
(leg from laRocque and others, 1963a )
Altitude : 1,918 fee t
Glacial drift :Soil 1 1
Clay, yellow 18 19Sand, fine and clay 4 23Clay, sandy, yellow 4 27Clay, sandy, gray, with some gravel and lignite frag
meats 59 86
Boulder, granite 2 88
Clay, sandy, gray, with some gravel 12 100Gravel 2 102
Clay, sandy, gray, with some gravel 28 130
Boulders, limestone and granite 2 132Clay, sandy, gray, with some gravel and lignite frag
ments 27 159Clay, hard 1 160
Clay, sandy, gray, with some gravel 21 181
Gravel, with stripe of limestone 4 185Clay, sandy, gray, with some gravel and lignite frag
ments 5 190Fort Union Group :
65 25 5Clay, silty and sandy
26 3
163-93-291dd
Altitude : 1,925 feet
Geologi csource
Material Thickness DepthZfeet )(feet )
Road fill 3 3Glacial drift :
31 3 4Till, moderate-olive-brown, oxidized Till, olive-gray 49 8 3Till, sandy and gravelly, olive-gray 18 101Till, olive-gray ° 15 116
Fort Union Group :Shale, light-olive-gray 8 12 4
Sand, very fine, clayey, light-greenish-gray,16 140micaceous, locally carbonaceous
163-93-30bbb2
Altitude : 1,915 feet
Glacial drift :Till, oxidized 13 13Till 122 135Gravel 14 149Till 49 198Gravel 10 208Till 34 242Till, sandy and gravelly 33 275Gravel 25 300
163-93-30bbb 3
Altitude : 1,915 feet
Glacial drift :Till, oxidized ° 18 18Till ° 107 12 5Gravel 8 133Till or fluvial sediments 75 208Gravel 14 22 2Till 29 251Gravel, sandy 14 265Till 14 279Gravel 24 303Till, gravelly 12 315Gravel and cobbles 32 347Till, gravelly 2 3Till 66 436Gravel and cobblesL 30 466
Fort Union Group :shale 5 471hignite 4 475Shale 4 479
264
163-93-30dc c
Altitude : 1,924 feet
Peet (feet )
Glacial drift :So:l, silty, sandy, brownish-black 1 1Till, moderate-yellowish-brown, oxidized 19 20
Till, dark-greenish-gray 9 29
Till, olive-gray 37 66
Fort Union Group :Shale, medium-bluish-gray, siliceous 14 80
Shale, grayish-brown, siliceous 6 86
Sandstone, clayey, light-bluish-gray 14 100
163-93-30dd d
Altitude : 1,927 fee t
Glacial drift :Soil, silty, sandy, brownish-blackTill, moderate-yellowish-brown, oxidized
Till, olive-graySand, fine to coarse, poorly sorted, angular to sub -
roundedTill, olive-graySand, fine to coarse, poorly sorted, angular to sub -
rounded °Till, olive-gray
Fort Union Group :Shale, light-olive-gray to medium-dark-gray ,
siliceousSandstone, fine to medium, silty and clayey, light -
bluish-gray
163-93-34ba
(Log from LaRocque and others, 1963a )
Altitude : 1,926 fee t
Glacial drift :Soil, sand, fine, brown Clay, sandy, brown, with some gravel Clay, sandy, brown, with strips of gravel and gra y
sandy clay and lignite fragments Clay, sandy, grayClay, sandy, gray, with lignite fragments and strips
of fine sandSand, fine, with lignite fragments
Fort Union Group :Lignite with thin strips of clay Clay, sandy, gray ° °Sand, fine, grayClay, sandy, grayLignite with strips of gray sandy clay Boulder, graniteClay, sandy, gray
26 5
Geologicsource
Material
Thickness
Depth
1 1
39 4 0
15 55
1 5611 67
2 6949 118
24 142
18 160
6
' 610 16
12 28
17 4 5
6 5 17 5 8
23 8 11 8 2
3 8 855
3 921 93471 193
Sand, compact, gray 10
150
163-93-36dd ;(Log from LaRocque and others, 1963a)
Altitude :
1,946 fee t
Geologi csource
Material Thickness DepthZfeet )(feet )
Glacial drift :Soil, sandy, brown 3 3Clay, yellow, with gravel 17 20Gravel and fine sand with some clay 4 24
Fort Union Group :Clay, brown 3 27Clay, sandy, gray 1 3 40Clay, sandy, gray, with some gravel and lignite frag
ments 17 57Gravel and gray clay 7 64Clay, sandy, gray, with limestone and lignite frag -
ments 9 73Clay, gray, with lignite fragments 18 91Lignite with strips of gray clay 6 9 7Sand, fine, gray, with some clay 8 10 5
163-94-3ddd
Altitude : 1,892 fee t
Glacial drift :Loam, clayey, black 1 1Till, dusky-yellow to moderate-olive-brown, oxidized 21 2 2Till, olive-gray 65 87
Fort Union Group :Shale, very silty, light-gray 11 98Limestone, silty 3 101Shale, very silty, light-gray 19 120
163-94-6aa2(Tog from LaRocque and others, 1963a )
Altitude : 1,902 feet
Glacial drift :Soil ° 2 2Clay, brown, with some gravel 4o 42Clay, sandy, bluish-gray with some gravel and lignite
fragments 50 92Fort Union Group :
Clay, gray, with strips of lignite 6 98Clay, brown to black 1 99Clay, gray, with strips of lignite 17 116Lignite 7 123Clay, brown, with strips of lignite 2 125Clay, gray, with strips of lignite 35 16oLignite 2 162Clay, gray 8 170
266
163-94-15dd
(log from PsRocque and others, 1963a )
Altitude : 1,907 feet
feet (feet )
Glacial drift :Soil, sandy, brown 1 1
Clay, silty, yellow 18 19
Clay, sandy, brown, with some gravel 15 34Clay, sandy, gray, with some gravel 26 60
Fort Union Group :clay, gray 7 67Clay, sandy, gray, with strips of lignite 98 165Clay, shale, white 1 166
163-94-16daa
Altitude : 1,909 fee t
Glacial drift :Till, yellowish-gray, oxidized 5 5Pill, moderate-olive-brown, oxidized 33 38
Till, olive-gray 18 56
Sand, medium to coarse, moderately well-sorted,87 14 3subrounded, lignitic
Gravel, coarse ; drill action indicates some cobbles8 15 1and small boulders
Fort Union Group(?) :Silt and very fine sand, light-gray ; contains thi n
carbonaceous laminae (possibly reworked bedrock29 180material) °
163-94-19daa
Altitude : 1,913 feet
Glacial drift :Loam, pebbly, black 1
1
Till, yellowish-gray, oxidized 6
7Till, moderate-olive-brown, oxidized 26
33
Fort Union Group :Shale, light-gray 15
4 8Limestone, dark-gray 1
49Shale, medium-gray 6
5 5Shale, silty, light-greenish-gray to light-olive-gray ;
contains some lignite 5
60
26 7
Geologicsource
Material
Thickness
Depth
163-94-20bbb
Altitude : 1,909 fee t
Geologi csource
Material Thickness Depth
(Teet) (feet )
Glacial drift :Till, yellowish-gray, oxidized 5 5Till, moderate-olive-brown, oxidized 12 17
Sand, medium, well-sorted, subangular and subrounded ,iron stained ; contains much detrital lignite 14 31
Sand, medium to coarse, gravelly, moderately well -sorted in lenses ; sand is principally quartz and
lignite 40 71Till, olive-gray 20 91Sand, medium, gray, well-sorted ; apparently inter -
bedded with some fine and coarse sand 14 10 5Till, olive-gray 22 12 7Gravel, fine to coarse, brown, generally subrounded ;
pebbles are principally siliceous, limestone an ddolomite, and granitic rocks 11 138
Fort Union Group :3 14 1Shale, very silty, nearly white
Lignite, black, fissile 3 14 4
Shale, medium-gray 4 148
Sand, fine, clayey, green 5 153Shale, silty, light-greenish-gray 6 159Limestone, silty, light-brownish-gray 1 160+
163-94-21cbb
Altitude : 1,910 fee t
Glacial drift :Till, yellowish-gray, oxidized 8
8
Till, light-olive-gray 15
23Sand, medium and coarse, reddish-brown, moderately
well-sorted, subrounded 18
41Clay, very silty, dusky-yellow, oxidized 4
45
Sand fine clayey, gray 7
52
Till , olive-gray 11
6 3Sand, medium to coarse, gray, moderately well-sorted ,
subrounded 23
86
Silt, clayey 16
102Gravel, fine, sandy, gray 6
108
Clay, silty 7
11 5Sand, medium, gray, well-sorted, lignitic 7
122Clay, silty, olive-gray 6
128Sand, fine to medium, gray, lignitic 2
130
Clay, silty, olive-gray ; contains some interbedde dsilt and clayey fine sand 67
19 7Silt, clayey and very fine to fine sand, olive-gray;
contains detrital lignite 107
30 4Clay, silty, olive-gray 15
319Till, olive-gray ; contains a few sand and gravel
streaks 34
35 3Fort Union Group :
Sand, very fine to fine, greenish-gray ; shale, silty ,light-gray ; lignite ; shale, carbonaceous ; silt ,white ; limestone and sandstone, very thin 47
40 0
268
163-94-2 2bbc
Altitude : 1,905 feet
Geologi csource
Material Thickness Depth
Glacial drift :Clay, silty, yellowish-gray, oxidized ; contains sandy
(feet) (feet )
lenses 5 5Pill, moderate-olive-brown 33 38Pill, olive-gray 31 69Gravel, fine and medium, moderately well-sorted ,
subangular and subrounded 10 79'Pill, olive-gray 46 125Gravel, coarse, subrounded 10 135Sand, medium to coarse, light-brown, well-sorted ,
subrounded, lignitic 68 203Fort Union Group :
9 212Shale, very silty, light-gray Sand, very fine, clayey, dark-greenish-gray, locall y
carbonaceous 6 218Lignite, black 3 221Silt and very fine sand, light-gray 19 240
163-94-22cbbl
Altitude : 1,900 feet
Glacial drift :Gravel, fine to medium, sandy, reddish-brown, sub -
angular to subrounded-` 5 5Silt and very fine sand, clayey, dusky-yellow 14 19Sand, fine ; silt and lignitic sandy clay, moderate -
olive-brown to gray, interbedded 35 54Sand, medium to coarse, gray, well-sorted in lenses ,
subrounded 41 9 5Gravel, fine to coarse, sandy, subangular to sub -
rounded 95 190
163-94-22cbb2
Altitude : 1,900 feet
Glacial drift :Gravel, fine and medium, clayey, reddish-brown ,
poorly sorted 7 7Silt, dusky-yellow, oxidized, powdery 14 2 1Silt, moderate-olive-brown ; interbedded with fine and
medium sand 16 37Sand, medium to coarse, well-sorted, lignitic 44 81Gravel, fine and medium, sandy, subangular to sub -
rounded 79 160
26 9
163-94-23c d(Dog from LaRocque and others, 1963a)
Altitude : 1,918 fee t
Geologi csource
Material Thicknes s(feet )
Glacial drift :Soil, clay, brown, with some gravel 18
Gravel, with strip of clay 2
Clay, sandy, gray, with some gravel 2 5
Boulders, with gray sandy clay 2
Limestone 2
Clay, sandy, gray 2Clay, sandy, gray, with gravel and thin strips o f
gravel 9
Fort Union Group :72Clay, sandy, gray
Lignite--- 3Clay, sandy, gray, with strips of lignite 1 4
Lignite with strips of clay and fine sand 2 9
Clay, sandy, gray 5Lignite, with strips of gray sandy clay 15
Clay, sandy, gray, with strips of lignite 12
Lignite with thin clay strip 8Clay, sandy, gray with strips of fine sand and strips
of lignite 10
Sandstone, gray 2
Limestone, buff colored 1
163-94-25aab
Altitude : 1,915 fee t
Glacial drift :ClayTill, oxidized 11 16
Sand, silt and gravel 11 2 7
Till ; contains a few sand and gravel stringers 133 160
Gravel 10 170
Till, gravelly 29 19 9
Gravel 43 24 2
Till 18 260
Gravel 40 300
163-94-27cbb
Altitude : 1,914 fee t
Glacial drift :Till, yellowish-gray, oxidized 5
5Till, moderate-olive-brown, oxidized 32
3 7Sand, very coarse, reddish-brown, well-sorted, sub -
rounded ---" 2
3 9Till, olive-gray 58
9 7
Fort Union Group :Shale, medium-gray 5
102
Shale, very silty, light-gray 7
109Sand, fine, slightly clayey, dark-greenish-gray ,
lignitic 11
12 0
270
fSallfeet )
182 045474951
6o
13213 514 917818 3198210218
22823023 1
163-94-27cc c
Altitude : 1,915 fee t
Geologic source
Material
Thickness
Depth(feet)
(feet )
Glacial drift :Till, yellowish-gray, oxidized 4
4Till, moderate-olive-brown, oxidized 24
28Fort Union Group :
Shale, silty and sandy, reddish-brown, yellowish -green, and dusky-yellow to yellowish-greenish -
gray 8
36Lignite, black 4
40
163-94-29aa a
Altitude : 1,912 fee t
Glacial drift :Loam, sandy, yellowish-gray 1
1Sand, medium to coarse, gravelly, moderately well-
sorted in lenses, subangular to subrounded 15
16Till, silty and sandy, moderate-olive-brown, oxidized
7
2 3
Fort Union Group :Sand, very fine to fine, clayey, yellowish-green ,
oxidized 12
35Sandstone, very fine-grained, light-bluish-gray ,
calcareous cement 1
3 6Shale, very sandy, medium-bluish-gray 4
4 0
163-94-36ab b
Altitude : 1,930 feet
Glacial drift :Soil, sandy, silty, brownish-black 1
1Till, moderate-yellowish-brown, oxidized 27
2 8Boulder, granitic 1
2 9Till, olive-gray 4
3 3Till, olive-gray to brownish-gray, partially oxidized
15
48Clay, very sandy, silty, olive-gray, calcareous
(fluvial) 14
6 2Gravel, fine to coarse, poorly sorted, angular t o
subrounded 4
66Till, olive-gray 12
78Fort Union Group :
Shale, light-bluish-gray to medium-bluish-gray ,siliceous 11
8 9Sandstone, fine to medium, light-bluish-gray, cal -
careous cement 6
95Sand, fine to medium, light-bluish-gray, slightly
calcareous 5
100
271
164-89-31cc c
Altitude : 1,875 fee t
Geologi csource
Material Thickness Depth
Glacial drift :Till, moderate-olive-brown, oxidized
(feet )
20
(feet )
2 0Till, olive-gray 17 3 7Till, pink 2 3 9Till, olive-gray, contains numerous cobbles and smal l
boulders 19 5 8Fort Union Group :
8 66Clay, silty, medium-gray, calcareousLimestone, gray 5 71Clay, silty, very light-gray, highly calcareous 9 80
164-90-35aba
Altitude : 1,869 feet
Glacial drift :Till, yellowish-gray to dusky-yellow, oxidized 26
26Silt, dusky-yellow, oxidized ; contains some san d
grains and pebbles (till?) 15
41Sand, medium and coarse, light-brown, well-sorted i n
lenses ; contains a few thin silty lenses 44
85Fort Union Group :
Shale, silty and sandy, variegated grays and greens ,interbedded 35
120
164-92-25dd(Log from LeRocque and others, 1963a )
Altitude :
1,950 fee t
Glacial drift :Clay, yellow 8 8Clay, blue, and gray sand 172 180
Fort Union Group :Sandstone, gray, and hard gray shale 60 240Sha]e, gray 40 280Lignite 3 28 3Shale, gray 17 300Shale, sandy 115 41 5Shale, gray 55 470Shale, sandy 30 500Shale, sandy ; water 18 518Shale, gray 80 598Sandstone, fine ; water near base 108 706Shale, gray 2 708
272
164-92-36dd(Log from LaRocque and others, 1963a )
Altitude : 1,950 fee t
Geologic
Thickness
lle t h
source
Material
(feet)
feet )
Glacial drift :Soil 2 2
Clay, yellow, with gravel 10 1 2
Sand, fine, with lignite fragments 2 1 4
Clay, sandy, gray, with some gravel 24 3 8
Gravel 2 4 0Clay, sandy, gray, with gravel 55 9 5Boulder, granite 1 96Clay, sandy, gray, with gravel and lignite fragments 149 24 5
Fort Union Group :clay,
graY '-' ° 1 246
Sand, fine, gray 10 256
Lignite, black 9 26 5
164-93-31d d(Log from LaRocque and others, 1963a )
Altitude : 1,903 fee t
Glacial drift :soil 2
2Clay, yellow 6
8Clay, brown, with gravel 8
16
Fort Union Group :Clay, yellow 5
21Clay, gray, with lignite fragments 4
25Sand, fine, gray 25
50
Shale 50
164-93-35cc c
Altitude : 1,917 feet
Glacial drift :Clay, silty, yellowish-gray 2
2Clay, silty and sandy, dusky-yellow, oxidized ;
material is predominantly reworked bedrock 5
7Fort Union Group :
9
16Sand, fine, slightly clayey, yellowish-green ,
micaceous, oxidizedLignite, black, fractured 3
1 9Shale, light- and medium-gray ; sand, clayey, light -
21
4 0greenish-gray, carbonaceous
27 3
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1625090013000 34 10-17049 300 355 90 5 6n, -- 3500 20 -- 5950 5350 7. 4162090313550 -- 16 01-10-90 -- -- -- -- 1707 -- -- -- -- -- -- 13100 1".0 00 7. 5
102400OY13000 11 10-21-09 -- 000 1540 1301 -- -- 0260 04 -- 04400 000 05 ,1A2N090Y13D0016240501101000 --
1 011
07-1B-S007-16-50 --
----
----
3 5055 --
----
- ---
- --- --
2406020
3000400
0. 30. 0
102X090014000162109001406
- ---
1 024
10-24-4510-17-50
91325
43040
353100
37 6,010
-- 2690000
2 0290 --
09 210600
,11737 50
0. 30. 0
1620090014DCC 12 10-25-50 -- -- 61 1280 000 600 404 40 -- 2760 2500 0. 51020010010000
> 1620900140DC --1 124
10-21-4010-21-49
-- -- 46 1203
35 0147
27535
04 2740
26001080
3202
---
- ---
----
411 01090
30002500
7. 47. 0
16218090316000102,00001000t --
2 322
07-10-3007-14-50 --
----
----
5011150
---- --
- --
- ---
-- - ---
-- 356 07030
5000000
5. 07 . 3
102N090115001 12 10-25-40 -- -- 000 000 700 -- 510 -- 4640 96 7710 34 .0 0 . 01621090Y0500 0162505001000
1 00
10-21-4010-23-40 --
13 4042
15 1310
13 2000 --
32 7615
-- 0364350
5672
-- 100 06170
170 05005
7 . 50. 0
1A25030353000102N00001SC0
1 612
07-20-0010-21-49 -- 300 --1000
0102700
__--
_ _051 -- --10500 296 -- --
12 016200
1110130 00
0. 00. 0
1625100015C0C 24 10-21-40 400 410 010 -- , 00 354080 -- -- 3660 01 0 0 0 . 110000,0111500 230 06-06-47 -- -- -- -- 604 -- Il -- - - 274 0100000MISCOCIA2090Y190AA --
2 424
07-14-5001-10050
----
----
----
045400
- ---
-- ----
----
----
--
620 02330
00 02501
1. 00 . ]
1620030015000 22 07-18-50 -- -- 700 -- -- - -- - 5130 4005 7 . 5
1625090015000 60 06-10-47 -- -- -- -- -- 655 -- -- 150 04 01620050015000 24 10-21-49 -- 413 550 102 105 -- 4200 200 0050 400 1 . .1 .-10090111600162001112200
----
1 012
10-20-4510-25-69
- --
14 963
0 151
12 5225
-- 44 4440 --
500168
4096 -
-- 127 01100
100 01200
8 . 00 . 5
1600501122180 -- 24 07-19-50 -- -- -- 03 -- -- - -- -- -- 240 300 7 . 4
162210501224660 - 22 10-21-45 -- 200 500 204 -- 203 -- 3160 24 -- -- 4120 000 0 1 . 61021109011200*02(105002400
----
2 025
07-10-5010-21-00
-- --442
--200
415144 -- 210 --
__2410 24 -
03001140
470 53000
7 . 11. 0
1620040060I62NOMY0000 --
0 000
0-10-4100-10-07
____
0_ 04 0095
-- ---_
2221
207 01 010 _
16205011310 net 00 06-1e-42 -- -- -- -- 1400 - 0s -- -- -- 1000 0 0162000110213 -- 05 06-10-47 740 -- 49 - 20 0020154053501020401130003
---
12 045
0-10-4000-10-47 -_ __ __ __ _
101 0900 --
---
730 -- -- --
212203000
16200•10000 TLOC MD 00-02000 0 .S -- 1 .0 1 .3 540 le 0 22 19 458 24 1.0 .l5 1530 23 w
3621104100900 5052 40 06-20-47 010 -- 140 3550 -202510410000162001104000 040
U106
05-26-4705-25-47 --
70 01000 --
1270
24700000
----
161004111040 0204 00 00-20-07 -- 730 -- - IS 2500 --
0155-00YE0 000- 400606
550CI -010
66100040000 9OF TOTAL CAL-
004 -40-
00-00S- 01040_ 0 00_ 6010- 0000-
50110 510000- 4600-
CAB-80000E
00-5090-
CONO -0606400 0000000000
000000 AQUIFER YELL 001E SILICA 1004 CIUR 0I00 SODIUM 4106 00110 0 0 80000E 5ULF*TE 810E 010E NI0000E 80805 00E AT 0055 0000- T100 0006007 193680- 04 0000000100 .1 101021 1001 1001 1001 1001 101 100031 10011 1404) ICLI 101 10001 181 180 CI 100 .001 NESS 0,010 400100 .8051 1 06 6. 6 1
662609130300 TLOC 211 05-28-07 1620 -- - 657 242 0162009101000 - - 120 05-26-47 259 10 110 0
162009101100 130 06-10-47 3 , 44 -- -- -- 241 ,1627109301000 120 06-10-47 640 3 3 198 016200910148C -- 160 05-2e-47 1409 23 237 016250910156 81025090013C0
- -TLOC
9 0135
05-29-4700-29-47
04 01040
44 350 0
162009102166 TLOC 195 05-29-47 1 000 __ 5 192 __050 02500 _ _1620001024006 0651 38 08-02-67 2 .3 159 Il 351 671-- 11 .0 3 .3 .00 6320 663 360 2 .5 ++ lt9^. 7 . 9
16200910256 0162009102500
TLO CTLOC
62 180
06-10-416-10-47 1 0 0 0
1490.2 727
210 0
1027109132761 9106 106 00-11-40 .32 9.0 712 14 1050 4.0 40 1 .0 5 .10 1722 42 C -- 0 5
21 0 0
0020 9 . 31020091034041625092000-0
1106TLOC
10 0225
05-20-6 705-26-47
005 01700
__3 2130
_ . 230 0203 6
1620092012886 0001 60 04-10-07 81 297 64 .39 915 548 22 1102000202000 100 05-26-07 -- -- 1080 ST_I 1_5 131'
162009201500 13 05-26-47 1 950 46 2600162559235004 0100 165 05-28-47 197^ -- -- 60 2'1 1162009300908102609300660
14 080
05-26-4705-26-47
214 ^
102' 6220002420162009300600 2
162009300000 TIOC10 0200
05-26-4705-29-47
2 .2 01779
21 8132 3 , 1 ,
2070
162009100980 TLO - 170 05-28-47 1 9 19 140 2000662539301086 100 05-29-47 1050 46 0000162439101310 l162409382000
TL06 70 0180
05-28-4 705-28-07
01 . 0,000
24 234
046001001 62009 3024000 TLOC 180 05-21-47 9 64 i s^e
16260933260002 0000 275 05-29-07 95 2570162009303100162009303306
- ---
170100
05-27-4705-20-47 000
108.0
3060
163408800118 -- 180 06-18-47 69 . 160 0 200103000800286 -- 125 06-1 0-47 305^ 330 2590
163408800680163000000000
----
12 0200
06-12-4706-19-40
.60 44 653 1J 070 6660-- 1 8I1
3_5 .50 2010 156 2 0601 7 00
0 . 41636108901960 -- 200 06-09-47 1010 40 191 016340686190C6638089024881
-- 21 2440
06-09-4 706-12-47 23 423 307 245 23
1330095 36 1110
4 4299 1180 .23 3000 2020 2010 -- 19
190 04600
-8 . 0
063008002000 -- 40 06-19-47 405 16 1 020 - -163000802800 -- 207 00-05-07 3 .3 002 7.2 1090 150 38 1 .2 1 .5 .52 2230 58 0 0 6 330 0 0163000002908163608803000 --
18 0140
06-09-4 706-10-47
2^10 3 738
319 03630
- -169609003280 -- 080 06-10-47 065 35 365 ,163008003388 -- 100 06-09-47 1090 55 __1630000035000 -- 464 04-19-67 1 .1 7.6 1 .2 700 2 .5 103 1 .2 365 .7 1 .9 1740 24 , 90
321 06960 0 . 2163608990566
163401900710-- 180
20006-16-4706-10-47
1 0 100990
6248
:0 303 0
163608980860 -- 153 06-05-47 I3 -- 45 21 120 3 .2 844 35 i 50 .6 1 .5 .46 2200 199 0 00393 03 .39 B . o
163601960886 170 06-16-47 1'40 73 315 0663906982186 TISC 300 06-16-47 200 36 292 01639089622400163906902300
----
24 0126
06-09-4 706-09-47
99 4530
2 031
3040333 010330606266 -- 195 06-09-47 000 23 200 0
04369199240[ 150 06-09-47 639 30 346016380193250 03638019325c8
200167
00-0204806-10-47
2 . 5-- 56 6
6653 1,10__ 3 4
21 .6 1 . 6__
3080 176 0 4070
160908932000 132 06-10-47 -- 406 __29
30003060163N0190288C 186 06-09-47 -- 35 0030
40.0561.1•6'160905UY II9•L119ll1901•2Z19-92-00541259019NO15000M11
6'9--
0682OCOZ0152
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99•__
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[f9Ifi6Y6211
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1201-00-90L.-60-60
09002
----
OWiM605 0003605[6MK99
6'60691Ll610999006Z--61'
--1•
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1100046OM91S910011[61199
4.0006E2021O606091096'9'1101096u0602.611406JO4.26009-90-01211209061171Z06004601
0.601120962609l091602116669'
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6-6-
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61649f------19-90-605L--901050609491
601Ll
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612611
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1.-12-6000-02-10
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----
19-06-60L1-42-50
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6664
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91'0'1If199461on16l9-6.1-0J09-60-90
042642
----
19011906090191306290605691 .6.L
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9Z19-51.9009-01-90
009111
----
191200101091302600006991 6661
1616020.--6,6
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0125401611
33100060509133020010.691
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16
63(116666663611 001101160411311131110511.6110,666)“1,11619.1193113311101111.131601060
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50110503610
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0155 -011E0 60X- SODIUM
S1EC1-007
MAJOR OF TOTAL CAL-NAG-NE-
F0 -T0S- MO- FLINT-
SOLIDS10951- N000-
CAR -BIIN27E
A0-S00E-
CDND -UCT*NCE 1FNFLOCAL
NUMOER 40UI0E0 NEL L101 .1
DATE 51110 6151021
19035911
0100ICAI
5I001911
$00119INAI
1IU0101
9T[2a -001101 EI X0931
Cio-0011*7 71[051
SULFATE15041
010E,CL'
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917607 E10031
0000N101
000 60190 CI
NESS100 . .01
0200 -NESS
110406110
760005 0500100
101000-99051
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1630091100811111 0032 105 09-22-69 21 .17 6S 15 630 7.6 1200 447 99 2 .1 1.0 .39 1690 216 0 13 96 2000 0. 11431609001210 0163N09193200C1
TLOCTLOC
11 5275
11-16-6704-10-67
6. 16 .3
.3 4
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2 . 11 .2
861061
3. 12.0
10601161 G7
2 .1 236204
2 . 92 .5 .4
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2 016
00 94
9990
33403270
0. 26 . 521
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21 340 05-29-47
10 .15 .7_ 4.4 050 __ 1031500
-- 21 2115
3 . 6- -
l. 3__
-- 2110 20__0
-- 99 --6120
-
16171014110200 -- 110 05-27-47 720 - 11 - - 3 0 9 0164909440490161509490666 1 TLOC
30 0125
05-20-4T05-29-41 __
ae9
041
3320
271040 1 0
1631109400601169409421181
----
25 0129
06-02-4005-26-41
5 .5 .55 1.6 51 0615
-- 1140 2 8la
1.2 1 .4 .16 2220 119 0 92 30203910
0. 3
14330949120[ -- 96 05-29-47 040 0 .0 ,10169X09491442 -- 20 05-29-47 015 4a 2,9 0163110946150016390949150*
TLOC 15 0200
05-29-4105-26-47 - -
740750
12991962
175 D
14340940110* Tl0C 160 05-27-47 1211 µ121 0320 0
161900192006 TLOC 240 05-26-47 1,40 99 256:164909402209 1163N094822000
005 21100
9390
07-14-6105-29-47
.60 9.9 716140,
693 l492
.2 1750 523 59 22602400
, . 5- -161900462209
1649094021*0----
9 B110
05-29-4705-26-47
- - 429,l5 0.
250 [1,00
- -
16310944246* -- 200 05-26-41 - - 4.0 10701e4901402641163409411102014311094*310001
TLlt1631
9 010 916
05-29-4105-29-4704-19-67
- -
17 .62 A9 iB92
S1 5101 9253
- ---
---
962
1. 012041
--.1
- -.23
--2040
----
5))-'0
--- -
9.2
- -- -66
.66020702710 0 . ; :163909493302
1640609193390
--
--
27 0
140
0e-04-41
06-10-47
II 26 6 .1 41 106 . 2.9 133 4.0 .41 -
640
1020 00 0 -- 02 1040
251 0416w0B1*1500 -- 205 06-1.8-41 1140 --20
310 2100164900903000164901901180
----
11 5156
06-L6-4706016-47
192 010
7 190
20 6222001649099931*0 -- 165 06-16-47 1030 00 2200
164309943210 -- 146 06-16-47 1020 -- -- 73 2,00144909063200164999491400
----
9 0150
06011-4106-16-47
104 1940
---_
T 433
32003000
16410900250014490900250002 0031
15 2170
06-16-4106-22-66
1121 -- ----
9 796
25302300
1640090226000 9104 110 06-L-47 1100 - 96 2400164109093206164909021400
- ---
20 0230
06-16-4 706-16-47 -- -- -- -- __
155 01600
-- -- 4 164
211 02730
-_
114N000M358B4164X09242500
04 .1TLOC
9 1TOO
09-02-6 605-26-47
20--
.4 0--
3i--
0_ 653 __ 6 . 1__ .1 9
11100
--710-
0. 5163
. 7- -
.30 1770 129 253 02550
O .t--
164909243400 -- 490 05-27-11 -- -- __ 120 14 330 01649092236408164609263 4 ^_'
TLO C--
625345
06-23-6 609-11-40
0 . 00 .0
.1 6--
3 . 133 50 0
66 9040
1 . 912
131 0412
f12
11 31810
15 919
1.7 1 . 6.30
170 03100
1 3317
00
a 261 04010
0 . 20 . 2
I6N6D9w3I64N09w334 0 360
----
125110
05-26-4709-29-47
--01 51120
--- - -- 2 529
_ _- - 3400