X Geology of Santo Domingo Pueblo and Santo Domingo Pueblo ...€¦ · 9 2????? X X c X X X X X c B...

282513

2215 24

Santa CruzSprings Tract

Well (BIA)

Si l e f a u

ral t a

Pe r a l t a f au

Si l e f au

c i s c o f au

Pa j a r i t o

f aul t

f a ul t

r r eg

F r a n c i s co

faul t

f a ul t

QalQalTglp

Qbo Qal

QTcQTc

QalQTc

QTslQTsl

QTslQtp4

QalQal

Qtp1Qe

QTcQTsl

QTslQTc

Qtp2Qtp3

Qtp4 Qtp4

QTc QTsl

Qc Qtp4

Tb1Tbv1

QalTb1

QeTbv1

QTsl QTsl

Qtp1?Qtp4

Qtp1?Qtp1?

QTslQtp4

QalQal

Qtp1Qta1

QalQal

QTcQta4

(QTslg)

Qtp4Tbt

QTslgQTslg

TbQtp4

QeQta4

QTslg QTslg

Qta4 Qta3

Qta3Qta4

QTslpQTslp

QTslg Qtp3

Qtp4Qtp4

QTsls QTsls

QTslsQTsls

Qtp4 Qtp4

(QTslg)

QTc Tbp

QboQTsl

QTcQTc

QTc Tglp

QTcQTsl

TglpTglp

QTslm Qta3

Qta3 QTslgQTslp

Qtp4QTslg

QTslpQTslpQTslp

QTslmQTslg

QTslmQTslm

Qtp4 Qtp3QTsls

QTsll Qbo

QboQtp4 Qtp4

A geologic map graphically displays information on the distribution, nature, orientation andage relationships of rock and surficial units and the occurrence of structural features. Thesedata are derived from geologic field mapping, compilation of published and unpublished work,analyses of borehole geophysics and well-cuttings, and photogeologic interpretation. Locationsof geologic unit contacts are not surveyed; therefore, the accuracy of contact locations dependson the scale of mapping and the interpretation of the geologist(s). Portions of the study areamay have been mapped at scales either smaller or larger than that depicted on the geologicmap; therefore, the user should be aware of significant variations in map detail. Any enlargementof this map could cause misunderstanding in the detail of mapping and may result in erroneousinterpretations. Site-specific conditions should be verified by detailed surface mapping orsubsurface exploration.

This map has not been reviewed according to New Mexico Bureau of Mines and MineralResources standards. Revision of the map is likely because of the on-going nature of work inthe region (Please note the date of last modification in the upper right of Plate I). The contentsof this map and associated report should not be considered final and complete until reviewedand published by the New Mexico Bureau of Mines and Mineral Resources. The views andconclusions contained in this document are those of the authors and should not be interpretedas necessarily representing the official policies, either or expressed or implied, of the State ofNew Mexico or the U.S. Government.

Acknowledgments

This mapping project was possible only because of the greatly appreciated interest andcooperation of the Governors and Tribal Councils of Santo Domingo and Cochiti Pueblos andthe Cochiti Environmental Protection Office. Consultations with Bill White, Dave Sawyer, andCharles Stearns were helpful for framing our ideas. Discussions of USGS geophysics studieswith Tien Grauch have been very beneficial.

(SAN FELIPE PUEBLO)

0° 46'

14 MILS

10.5°187 MILS

UTM GRID AND 1993 MAGNETIC NORTHDECLINATION AT CENTER OF SHEET

35° 30'106° 30'

T. 16 N.

(SAN A

PUEBLO)

T. 15 N.

R. 4 E. R. 5 E.20' 369 17' 30"

NEW MEXICO

QUADRANGLE LOCATION

106° 22' 30”430 000 FEET

106° 30' 365000m E. 367 R. 4 E. 27' 30” 25'

32' 30"

35° 37' 30"

Base from U.S. Geological Survey 1953, photorevised 19931927 North American datum, Projection and10,000-foot grid based on

New Mexico coordinate system, cental zone (Transverse Mercator)1000-meter Universal Transverse Mercator grid ticks, zone 13, shown in blue

D. J. McCraw and G. E. Jones: digital cartographic production

374 460 000 FEET371(CANADA)

(BEAR SPRINGS

1 0.5 0 1 MILE

1000 0 1000 2000 3000 4000 5000 6000 7000 FEET

1 0.5 0 1 KILOMETER

NATIONAL GEODETIC VERTICAL DATUM OF 1929

CONTOUR INTERVAL 20 FEET

SCALE 1:24,000

PONDEROSA 30 MI.366

Mapping of this quadrangle was funded by a matching-funds grant from the 1997 STATEMAPprogram of the National Geologic Mapping Act coordinated by the U.S. Geological Survey

and the New Mexico Bureau of Mines and Mineral Resources.

NEW MEXICO BUREAU OF MINES AND MINERAL RESOURCESA DIVISION OF NEW MEXICO INSTITUTE OF MINING & TECHNOLOGY

SANTO DOMINGO PUEBLO SW QUADRANGLENEW MEXICO

Geology of Santo Domingo Pueblo andSanto Domingo Pueblo SW quadrangles,

Sandoval County,New Mexico

Gary A. Smith and Andrika J. Kuhle

April 19986 April 2000 Revision

Plate I of II.

Department of Earth and Planetary Sciences, University of New Mexico,Albuquerque, NM 87131

R. 5 E.

SAN FELIPE PUEBLO 5 MI.

1 640 000FEET

3943000m N.

366 371 374000m E.

367 368

372 373

(SAN FELIPE PUEBLO NE)2.8 MI. TO INTERSTATE 25R. 5 E. R. 6 E. 20' 380 17' 30"35° 30'

106° 15'

3930000m N.

T. 16 N.

T. 15 N.

32' 30"

35° 37' 30”106° 15'

(MONTOSO

1 680 000FEET

470 000 FEET

106° 22' 30" 376000m E. 378R. 5 E. 20'379 17' 30" 386000m E.385490 000 FEET382(COCHITI DAM)377

SANTO DOMINGO PUEBLO QUADRANGLENEW MEXICO

R. 6 E.

.M. 14

21 MI. TO N.M. 44ALBUQUERQUE 39 MI.

COCHITI PUEBLO 2.1 MI.

376 382 383 385000m E.

NMBMMR Open File Map SeriesMaps OF–GM–15 and OF-GM-26

Map last modified on 6 April 2000Plate I of II.

David J. McCrawDigital Cartography

0° 50'

15 MILS

10.5°187 MILS

UTM GRID AND 1993 MAGNETIC NORTHDECLINATION AT CENTER OF SHEET

Base from U.S. Geological Survey 1953, photorevised 19931927 North American datum, Projection and10,000-foot grid based onNew Mexico coordinate system, cental zone (Transverse Mercator)1000-meter Universal Transverse Mercator grid ticks, zone 13, shown in blue

D. J. McCraw and P. Brown: digital cartographic production

(MADRID)

4,800'

5,000'

5,600feet ASL

5,200'

4,800'

5,400'

5,000'

RioGrande

5,600feet ASL

5,200'

5,400'

5,000'

QTslpQTslpQTslp

QalQal

QTslgQal

dfQtp4Qal

QTslgQTslg

Vertical Exaggeration = 2.0

Projection ofBIA Santa Cruz

Springs WellCochitiDam

N.M. StateHwy. 16

N.M. StateHwy. 22

Vertical Exaggeration = 2.0

?Qal Qal

RioGrande

QoaQTslg QTslgQTslg

N.M. StateHwy. 22

QTsls QTslm QTslm

Qalm Qal

QboQTslp

QTslpQTslp

Qalm QalmQalm

These cross sections are constructed based uponthe interpretations of the authors made from surficialgeologic control and subsurface and geophysicaldata, where available. They should be primarilyused as an aid to geologic frameworkunderstanding and not be the sole source ofinformation used in locating or designing wells,buildings, roads, or other man-made structures.

6,200feet ASL

5,200'

5,400'

5,000'

QTslQTsl

Qal Qal

QTslQTsl

6,000'

5,800'

5,600'

Tb2 Tbt BorregoFault

QTcQTslQtp4

BorregoCanyon

TbtTglp

QalQtp3 Qtp4 Qtp1

??? ? ?

QTcQTc

QTc QTcQTc

QoaQoa

GEOLOGIC CROSS SECTIONS

6,200feet ASL

5,600'

5,200'

5,800'

5,400'

BorregoFault

Qal6,000'

PeraltaFault

QTslQTc

CañonSanto

DomingoCamada

FaultQtp5Qal

SileFault

0 10 20 mi

0 10 30 km20

INDEX MAP OF NMBMMR’S

STATEMAP GEOLOGIC QUADRANGLES

McCLURERESERVOIR

SANDIACREST

PLACITAS

ROSILLAPEAK

ASPENBASIN

COWLESTESUQUE

BERNALILLO

LOMAMACHETE

ARROYODE LAS

CALABACILLAS

VOLCANORANCH

LA MESITANEGRA SE

LOSGRIEGOS

ALAMEDA

WINDMESA

ISLETA HUBBELLSPRING

SANDIAPARK

TIJERASSEDILLO

ESCABOSAMOUNT

WASHINGTON

TAOS SW

CARSON

BERNALILLONW

CERROCONEJO

JEMEZPUEBLO

SANFELIPEMESA

COLLIERDRAW

SANTAANA

PUEBLO

SANFELIPE

PUEBLO

SANFELIPE

PUEBLO NE

OJITOSPRING

SANYSIDRO

LOMACRESTON

SANTODOMINGO

PUEBLO SW

SANTODOMINGOPUEBLO

TETILLAPEAK

HOLYGHOSTSPRING

GILMAN PONDEROSABEAR

SPRINGSPEAK

CAÑADA

COCHITIDAM

MONTOSOPEAK

GLORIETA

RANCHOSDE TAOS

TRESRITOS

PEÑASCOTRAMPAS

HORCADORANCH

REDONDOPEAK

JEMEZSPRINGS

SANMIGUEL

MOUNTAIN

LAVENTANA

AGUAFRIA

SANTA FE

TURQUOISEHILL

SETONVILLAGE

WILDHORSEMESA

ROWEGALISTEO

OJOHEDIONDA

BULLCANYON

RENCONA

PICTUREROCK

GOLDEN CAPTAINDAVIS

MOUNTAIN

SANPEDRO

EDGEWOOD

CHILILI

RIOPUERCO

LOSLUNAS

SETAJIQUE MILBOURN

RANCHDALIESBOSQUE

DALIESNW

LA MESITANEGRA

BENAVIDEZRANCH

LAGUNAORTIZ

NORTHSAN YSIDRO

LOWERCOLONIAS

ELKMOUNTAIN

HONEYBOY

TAOSJUNCTION

VELARDE

JICARITAPEAKEL VALLETRUCHASCHIMAYO

SANJUAN

PUEBLOCHILI

SANPABLO

RANCHODEL

CHAPARRALSEVEN

SPRINGSVALLE

TOLEDO

VALLESAN

ANTONIOGUAJE

MOUNTAIN

PUYESIERRAMOSCA

CUNDIYO TRUCHASPEAK

PECOSFALLS

ESTANCIA

MORIARTYSOUTH

MORIARTYNORTH

KINGDRAW

ESPAÑOLA

WHITEROCK

LOSCORDOVAS

TAOSTRES

OREJAS

BELENNW

TOME TOME NE TORREON EWINGBELEN MOUNTAINAIRNE

BELENSW

TURNPUNTA DE

AGUAMOUNTAINAIR

VEGUITAMANZANO

PEAKWILLARD

LA JOYANW BLACK

BUTTEBECKER

ABEYTAS

SCHOLLE

ALBUQUERQUEWEST

ALBUQUERQUEEAST

TOME SE

SHADYBROOK

PUEBLOPEAK

WHEELERPEAK

ARROYOSECO

ARROYOHONDO

CERRODE LOSTAOSES

RAYO HILLSCERROMONTOSO

BECKERSW

LA JOYASAN

ACACIASILVERCREEK

SANLORENZOSPRING

MESADEL

SIERRADE LACRUZ

SOCORROLOMA

DE LASCANAS

BUSTOSWELL

WATERCANYON

LADRON

COMANCHERANCH

LOS ALAMOS 1:100,000

OF-DM–18

GM–45GM–33

GM–28 GM–34

GM–26 GM–27

(SKY VILLAGE SE)

(SKY VILLAGE NE)

(SKY VILLAGE)

(SKY VILLAGE NW)

GM–71

GM–73

OF-DM–12 OF-DM–33

OF-DM–22

OF-DM–31

OF-DM–11

OF-DM–32

OF-DM–23OF-DM–15OF-DM–26OF-DM–25

OF-DM–14

OF-DM–19 OF-DM–37

OF-DM–39

OF-DM–2

OF-DM–16OF-DM–9

OF-DM–10 OF-DM–6 OF-DM–1 OF-DM–29

OF-DM–35

OF-DM–20OF-DM–4

OF-DM–3OF-DM–17

OF-DM–8OF-DM–5OF-DM–13

OF-DM–24OF-DM–21

OF-DM–28

OF-DM–34

OF-DM–7

NMBMMR STATEMAPQuadrangles

Santo DomingoPueblo SW,

Santo DomingoPueblo

LosAlamos

Santa Fe

SOCORRO 1:100,000

35°30'

36°00'

105° 30'

36°30'

35°15'

106°00'

35°00'

106°30'

34°22'30"

34°30'

107°00'

ALBUQUERQUE 1:100,000

SANTA FE 1:100,000

VILLANUEVA 1:100,000

TAOS 1:100,000

BELEN 1:100,000

ABIQUIU 1:100,000

Location Map

Socorro

Grants

LasCruces

Deming

109° 107° 105° 103°

SANTA FE

Albuquerque

EXPLANATION OF MAP SYMBOLSSanto Domingo Pueblo and Santo Domingo Pueblo SW

7.5' Quadrangles

Exposed geologic contact

Approximate or inferred geologic contact

High-angle normal fault, tick showing dip, bar and ball indicates downthrown side

Normal fault, approximately located on the basis of outcrops, bar and ball indicatesdownthrown side

Normal fault, approximately located on the basis of well logs, D indicates downthrownside

Concealed normal fault, D indicates downthrown side

Strike and dip of bedding

Peralta Tuff Member biotite - rhyolite pumice lapilli (upper Miocene) abundant influvial sediment.

Tschicoma Formation dacite pumice lapilli (Pliocene) abundant in fluvial sediment.

Bandelier Tuff rhyolite pumice lapilli (lower Pleistocene) abundant in fluvial sediment.

Prominent zone of calcite cementation. Generally located along exposed fault planes orin coarse-grained beds in close proximity to faults.

Approximate positions of vents from which units Tb and Tbt were erupted .

Location of 40Ar/39Ar geochronology samples

OF-DM–43

FRIJOLES

OF-DM–42

OF-DM–47

OF-DM–48OF-DM–36

OF-DM–41

OF-DM–49

MADRIDOF-DM–40

OF-DM–46

OF-DM–45

CAPILLAPEAK

OF-DM–27

LEMITAROF-DM–38

MEXICO

TATE M A

auof Mines & Mineral R

Earth Science for the 21st Century

Ne w Me x i c o Tech

Dr. Peter A. ScholleDirector and State Geologist

Dr. Paul W . BauerGeologic MappingProgram Director

COMMENTS TO MAP USERS

X Geology of Santo Domingo Pueblo and Santo Domingo Pueblo ...€¦ · 9 2????? X X c X X X X X c B...

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