RPT OB RCD NBR87 PROJ · (B-0) Fm. Essentially locally reworked 8-fl Fm created by late-glacial...

4aA08NEe082 2.10918 MICHAUD010

NQRANDA EXPLORATION CO. LTD

REPORT ON REVERSE CIRCULATION OVERBURDEN DRILLING

NBR87 PROJECT - BARNET PROPERTY

BARNET AND MICHAUD TOWNSHIPS. ONTARIO

NTS 42A/6

RECEIVED

WHOM

Preoared bv

J. A. Richard

Overburden Exploration Services Ltd

March S. 19B6 ;-

42A08NE0082 2.10918 MICHAUD 010C

1 INTRODUCTION

i - i

i. 2 Loc.a.t.i.o.nm arHJ i-Ac.c^ss. , , . . . . . . . , . . . . . . 2

iL . . . . . . i . . . . . . . . P 4

i - ^ Ac knp^w j^ed.0e.mejit.Sr. . . . . , . . . , . . . . . . . . . 5

J. 5 Pr e .YjjH!.s..Jj3rJ\. . . . . . . . . . . . . . . . . . . . 6

l - b feLQ.L9-Q.iL-QjJJitL!llLLv.-S.tr.a.tj, -g.r.aD.iiv. . . . . . . . . . . 6

2 NBR87 REVERSE CIRCULATION DRILLING PROGRAM . . . . , . . 12

2" i ^.C.Ly.LQ.Q.-L5.Q.i.l.tLC.i.-3[Ll-Si.*i.Lli.L9-E, . . . . . . . . . 12

3 BARNET PROPERTY RESULTS . . . . . . . . . . . . . . . . . 13

3. i L^XPIJL^jgjDJjioy. . . . . . . . . . . . . . . . . . . 13

3.2 G u e. t,e r ,r^a r.^ .G e o. LO .ov. . . . . . . . . . . . . . . . . . 16

3.2.1 uvertuirch-n Distribution and Stratigraphy . . . 16

3.2.2 Overburden Geochemistry and Results . . . . . . 18

4 CONCLUSIONS . . . . . . . . . . . . . . . . . . . . . . . 20

5 REFERENCES . . . . . . . . . . . . . . . . . . . . . , . 2 2

6 APPENDICES . . . . . . . . . . . . . , . , . . . . . . . 24

6.1 APPENDIX A. NBRB7 SUMMARY DRILLING REPORTS . . . . 24

6.2 APPENDIX B. SAMPLING AND ANALYTICAL PROCEDURES . . 26

6.3 APPENDIX C. HHC LABORATORY LOGS . . . . . . . . . 31

i) Regional Location Map - Barnet Property

H Summary ot Bedrock Descr i pt i ons-NBRS? Project

Barnet Project - NBR87 Drillhole Location Mao

Overburden Prof iles

Sheet i - Sections ft-Ai. B--B1, C-Ci

Sheet 2 - Sections B--D1, E-Ei. F-F1, 6-G1. H-H1

i INTRODUCTION

i. J fi.en.Rr.ajl

The following report, prepared by Overburden Exploration Services

Ltd -for Norande, Exploration Co., Ltd.. describes a program of

reverse circulation drilling \NBR87) carried out on the Barnet

claim group, situated in Barnet and Michaud Townships, Ontario.

The 1987 overburden drilling program, as reported herein, was

designed to assess the claim block's potential for economic gold

mineralization through the use o i r econnaissance overburden and

bedrock geochemistry.

Reverse circulation drilling operations on the Barnet property

claims were conducted over an eleven day period, commencing on

October 13, and finishing on October 24, 1987. THentyni ne holes

were drilled over a total -footage of 2305 ft which translates to

an average hole depth ccf 80 feet. A total of one hundred and

seven samples were taken, including twenty-nine bedrock chip

samples.

i. 2 Loc.iiL9.rL-,a.D..ci Acic ess

The Barnet claim group occupies the northeastern corner o* Barnet

Township. Ontario, and the adjoining southeast corner of Michaud

Township (Fig. i; see also Property Map, back pocket). It is

situated approximately 90 km east of Timmins and 30 km north of

Kirkland Lake. The general area is encompassed by National

Topographic Series map 42A/B, 1:50.000 scale. This region falls

within the jurisdiction of the Larder Lake Mining Division,

Ontario Ministry of Mines.

F'rimarv around access to the Barnet property is provided by

Highway 101 which traverses east-west across the south Abitibi

Lake area. At e, point 5 km east of Perry Lake Lodge, the

Dewhirst access road branches southward along the Munro esker.

Driveable ground access to the property, situated approximately 7

km south of Hiphway 101, extends to the south shore of Dewhirst

Lake via subsidiary bush roads, f r on t his point, a winter road

trends another 1.5 km southwesterly onto the Barnet claim group.

Helicopter access is readilv available to the property; during

the NBR87 drilling program, a Bell 206B was utilized to ferry

crews front Lava Mountain Lodge (H km west) due to very poor

summer road conditions. Barnet Lake provides an alternative

landino site for liqht floatplane service.

FIGURE l.

PROPERTY LOCATION MAPJAMES

BAY

Milti

Seal* li B 000 000

rnettTwp

GEORGIAHBAY

LAKE\

HURONONTARIO; r6'

l - 3 ?.LQJ..lLty^Df seQ.D.t i,on

The Barnet property reported on herein consists o-f 105 claims

which together comprise a contiguous, irregular land assemblage

covering approximately 6 km of bedrock strike. Included within

the western limit DI the claim block are eleven claims known as

the Leahv option. Assessment credits for the 1987 overburden

drilling program are being applied against the Leahy group which

specifically includes the followino claims:

L. 821225 L. 822590

L. 821226 L. 622591

L. S21227 L. 822592

L. 821228 L. 822593

L. 821229 L. 822594

L. 822595

s .o .ra j) h v

The Barnet property is essentially characterized by level to

gently undulating clay plain (less than 3m local relief) with

abrupt occurrences of bedrock outcrop rising up to 15 i* above the

surrounding terrain (south haH o-f property). The general area

lies 305-320 re (l 000- 1 050 -ft) above sea level.

Several snail tributary streams of the Pike River trend westerly

across the property. These poorly defined channels tend to be

choked with thick tanalder growth.

Vegetation on the Barnet property is typical of the poorly

drained Barlow-0jibway clay plain, dominated by black spruce

forest with minor stands of poplar occurring on better drained

surfaces. Large black spruce-sphagnum boos cover much of the

northern part of the claim group.

l - 4 Ac k n.GW.3 .edjjefi!.ejntj,.

This drilling program was completed on behalf of Noranda

Exploration Co, Ltd. Timmins field office. Program management

was carried out bv Overburden Exploration Services Ltd o i

Timmins, Ontario: G. Parkin, geologist (H.Bc), was responsible

for drill supervision and logging, assisted by D. Dunston and A.

Boudreau. samplers (DES personnel). Drilling operations were

completed under contract bv Bradley Bros Limited, Timmins (D.

Sussiere-dr i l S. er i ,

T. Babin of Norarida Exploration is acknowledged for his

assistance in planning this program.

J,A. Richard (GE5-author) is responsible for this reoort and its

cone i usi oris.

General geology of the Barnet property predominantly consists of

east-west trending Archean ma-fic metavolcanics. together with

minor met asedi raentsr v formations and cross-cutti no diabase

dikes. Gold mineralization has been previously encountered in

several discrete locations within Barnet Township.

Regional geological compilations have been produced by Pyke

fi.- aJL- U973) and HERD-DBS (1984) while more detailed mapping has

been carried out by Jensen (1985a,b). Numerous other geological

and geophysical studies have also been completed in the Barnet

property area, all of which have been summarized by the Kirkland

Lake Resident Geologist's office (QGS. 1967).

Previous, exploration activitv has been largely focussed on the

general area of the Leahy option shaft/outcrop area. Interest in

the area was generated in 1929 by reports of the Brett-Tretheway

discovery of coarse gold in porphry and diorite. Trenching over

the main discovery outcrop was carried out in 1975 by R. Bugow.

In 1978. 3 , L arche completed around EM surveys in the immediate

vicinity of the outcrop area. Recently in 19B6, H. Leahy and F.

Kiernicki -filed reports of an airborne electromagnetic survey

over the general area of Noranda's current Leahy option claims.

Elsewhere over the Barnet property. Dominion 6ulf Company

completed geological and ground magnetic s.urveys over

east-central parts of the Barnet property in 1950-51, including

some drilling. Later in 1965, Midrim Mining Co. Ltd conducted

AEM surveys over the eastern sector. Ground magnetic and EM

surveys were carried out in 1983 by Brinco Mining on a limited

number of eastern claims under the Tillicum Project. Canadian

Gold and Metals Inc: covered the entire Barnet Township area

during a 1980 airborne survey.

Recent exploration activity in Barnet-Michaud Townships and the

surrounding area have been spurred on by sonic drilling/gold

Drain results released by the Ontario Geological Survey as part

of the BRIM program. Sonic holes 67-33, 35, -36. and -37 were

drilled either on. or in close proximity to the Barnet property.

Preliminary gold grain results have been released (Baker and

Steele, 1987).

The use ci-f overburden dri 11 ino/cjeocheini Etry as an mineral

exploration technique is predicated upon an understanding of (i)

regional glacial history and deposit ional environments, (ii)

local property stratigraphy arid sedimentology, (iii)

inter~r el at ionshiOE between the above. The abililty to interpret

the sediffientological complexities of glacial overburden (ie.

lithogenetic identification and provenance) is crucial to the

final interpretation of results from any such program.

The following summary provides the context, of regional Quaternary

geology and pertinent reference literature.

B e n e r al Quaternary q e ol D o y and P v e n t s in northeastern

Ontario-northwestern Quebec have been described by Antevs (1928),

Hunhes (1959), Skinner (1973), Hardy (3977), Vincent and Hardy

(1979), Shilts (1960), Dyke e i., H.. ( 1982). and Veillette (19B6).

New concepts on the inception, growth and decay of Laurpntide

glaciation in east-central Canada are presented by Fulton and

Andrews (1987). Subsurface lithostratigraphy of the North

Abitibi region is discussed by Sauerbrei et.. al.. (1985) and

Bouchar d et... aJL.. (J 96M .

Surficial gecslogy of the Barnet-Michaud area reported on herein

has been (napped in detail by the Ontario Geological Survey

(Baker et al , 19BO), Sonic overburden drilling carried out under

the auspices of the GIGS's BRIM geoscience program has; produced

numerous oeol ooical/'geochemical data releases since 1984 (see

Baker arid Steele. J987).

Three phases of regional glaciation ere recorded in the

Quaternary lithostratigraphic record present throughout much of

the Abitibi region. In descending order of youngest to oldest,

the Quaternary units occur as -follows:

1) Cochrane Formation (Hughes, 1959)-Late Late Wisconinan

Tan to brownish-grey, non-compact silty clays and clayey

silts, locally pebbly, occurring as waterlain diamicton?.

(sediment debris flows), minor till and overlying

lacustrine silts and clavs. Paleozoic carbonates occur

20-50V.. Overlain by recent peat and humus, lower contact

typically gradational to lacustrine Bar low-Cljibway

(B-0) Fm. Essentially locally reworked 8-fl Fm created by

late-glacial Cochrane ice surging into glaciolacustrine

basins,

2) Barlow-0jibway Formation (Hughes, 1959) or Upper

Sediments (Sauerbrei et.al., 1985-Late Wisconsinan

fcuH-grey, laminated, v. non-compact silts and clays,

f-m.snds. These sediments reflect glaciolacustrine

deposition in proglacial Lake Ojibway following final

retreat of the main Laurentide ice sheet, but prior to

the late-til aci al Cochrane readvances. Also includes

10

c.snds and granule-pebble-cobble gravels deposited by

glaciofluvial processes during final ice retreat.

Polymictic, varied provenances, long-distance transport.

Conformably overlain by the Cochrane Formation,

conformably and unconforsiably underlain by glacial

Matheson Formation.

3) Matheson Formation (Hughes, 1959) or Upper Till

(Sauerbrei et.al., 198S)-Wisconsinan

Grev sandy to clayey silt tills, and diamicton-debri s

flow sequences. Tills are typically moderate to very

compact, fcO-95X local lithologies indicating proximal

sources where overlying bedrock. Unconformable active

ice deooEition by lodgement and conformable passive

melt out processes. Locally coloured by weathered

bedrock-derived clavs. Di amicton-debris f l ON sequences

consist of loose, v.poorly sandy-silty sediments,

v.pebbly, 30-60'/, local lithologies, gradaticmal upper

contacts, frequent complex interbedding with minor sorted

Glaciofluvial sediments. This unit reflects subaqueous,

ice-marginal and/or subglacial debris flow deposition,

local to distant provenances. South to south-

southeaster l v (155-180 azimuth) ice flow directions.

4) Lower Sediments (Sauerbrei e t.al.. 1 9B5)-Mid to Pre-

Wisconsinan?

Non-glacial sediments similar to Bar!ow-Ojibway Fm.

li

Consists of lacustrine silts and clavs. (v.dense

' superclays'i. -f-c.sands and gravels (fluvial to

glaciofluvial), v,polvraictic. Upper and lower contacts

oenerallv unconformable. Known to contain organics and

definite paleosols (interqlacial or interstadial?) in the

Timmins r eg i on,

5) Lower Till (Sauerbrei et.al., 19B5)-Mid to Pre-

Wisconsinan?

5 i 11 v to clavey till, pebbly, usually up to 95X local

litholooies. matrix coloured according to bedrock type,

v. local provenance. Lodgement and/or basal diel tout

till facies. Generally restricted in occurrence

to local bedrock depressions and areas of extensive,

v.deep overburden OiSOft). Recent evidence by

Veillette (1986) suggests southNesterlv (210-245 azimuth)

ice flow direction, possiblv related to early ice phases

of the Laurentide ice centre (Shilts, 1980; Richard,

1964).

2 N BR87 REVERSE CIRCULATION DRILLING PROGRAM

2. i . i) r ij J.i.DJ?. J:P.QAE.LI.jp.6..and...St.at.i.?JLi 5A

The NBR87 program of reverse circulation drilling on the Barnet

claim group was conducted over en eleven dav period, comment ing

on October 11. and finishing on October 24. 19B7. Twenty-nine

holes were drilled over s, t otal footage of 2305 -feet, indicating

an average hole depth o-f BO feet. Daily drilling production data

are H fcted under Appendices.

Downhole consumables amounted to seven tricone bits and one "sub"

adaptor. This represents an average bit life of one oer four

holes or 325 f t /bit.

Mechanical downtime.' totalling one day was experienced on this

job .

13

BARNET PROPERTY RESULTS

Preliminary identifications of bedrock chips recovered durino

drilling operations were initially performed on-site bv visual

examination. Binocular microscope examinations of chips were

later carried out at DES laboratory facilities to either confirm

or modi f v the preliminary rock identification.

Bedrock lithologies encountered on the Barnet property

or ed&mi nantl v consist tif Archean mafic metavol canics with lesser

occurrences of metasediments, syenite and diabase. Syenite was

cored st the bate of holes N'BF(87~li and -12 at the west end of

the property. Ketasediments consisting of greywacke and

argillaceous oreywacke were intersected in holes NBR87-13, -21,

-24. and oossiblv -22 and -26 (uncertainty due to alteration).

Minor disseminated sulphides were noted in several holes.

H descriotive bedrock summary based on binocular microscope

examinations is seoaratelv listed in Table 1.

14

Table I. Summary of Bedrock,.Descri.B.tiL ons - NBR67..Project.

Hole S

NBR-87

NBR-87

Bampl E

-0 1

-02

NBR-67-03

MBR-B7 -04

NBR-87-05

NBR-87

NBR-87

MBR- 67

1 6008

16013

1

1

1

-06 1

- 0 /'

-08

NBR-87-09

NBR-87

NBR-87

NBR-67

NBR-B7

NBR-87

NBR-87

NBR-87

NBR-87

NBR-B7

NBR-87

NBR-B7

HBR-87

-1

-1

-1

-1

-1

0

1

i

6016

6019

6022

6026

6028

6030

16038

1 6050

1 16053

2

3

4

-15

j 6

-17

1

-1

-2

~" jf.

B

9

0

1

S

1

6055

6060

16063

1

1

1

1

1

1

6069

6071

6073

6078

6060

6082

16084

Colour Texture HC1

md.

elk.

(fid.

dk.

dk.

It.

dk.

li.

d k.

dk.

bri

dk.

dk,

dk.

dk.

d k .

dk.

dk.

dk.

dk.

dk.

gr .

gr .

gr .

gr .

gr.

py -

gr .

D r .

gr .

bl.

c k. red

or .

bl.

gr.

gr .

bl.

bl.

qy.

gr .

ci r .

bl.

f . g.

f .g.

d. g.

f. q.

f. g.

f. Q.

f . g.

f .g.

f .g.

e.g.

e.g.

e.g.

f .g.

md. gr.

f. g.

rod. or .

f. g.

rod. gr .

i, g.

f. g.

f .g.

str.

str.

mod.

str.

str.

st r.

wk.

str.

wk.

wk .

str.

str.

wk .

wk.

str.

wk.

w k.

str

w k .

str

str

Min.

tr. pv.

tr . py .

tr. py.

tr. py.

tr. py.

tr. py.

tr. pv.

tr. py.

5X py.

tr. py.

tr. py.

t r . p y .

t. r . p y .

Di py.

tr. pv.

tr. py.

IX pv.

Other Rock-Type

Mafic

epidotized Mafic

Int.-

Mafic

epidotized Mafic

Mafic

Mafic

Alt.

10). epidote Mafic

Vole.

Vole.

f! a f .Vole

Vole.

Vole.

Vole.

Vole.

Maf .Vole

Vole.

25'/. magnet. Diabase

Byeni

25'/. magnet. Byeni

diss. py . Ara .

skel . tex Mafic

epidotized Mafic

Mafic

epidotized Int.

magnetic Mafic

Mafic

Mafic:

Arg.

te

te

Gwke.

Sub-i ntr

Vole.

Sub-i ntr

Vole.?

Sub-i ntr

Vole.

Vole:.

Gwke.

^"

D? 1 CO ~--.! I

f-J

•JO Cr-

H—

C"

O1-

a: w ri

CO

^4

N-.^

Od

Cr-

*~ *

.^;,

Ji

Z.

W j CO -J t ho --j

t? O1

--Ct

-^.1

s: w irr

i•-

sj i\~

--J 0 rs-

*o *-i'

c.fi

-z*-

w 1 CO --.t [ K3 en o-

C'

•-O C-'J

•z.

TO 7 CO ^j ! hO *" Cr- o •~0

fc—

z; o? iC

O•^

1 ! S-1 o'j

cr-

c- CO CCi

3S r^T

"i"

'

tSJ

^vl ! N.?

. JI

O- o CD O-

^

-O

'O

•S3

:O

iO

3

CX

f-1

O ex

3

O a.s o O

L

a- •aQ

.O

•O 3

ID

(f -o D,

O

ro

aum a.

3

CO

^f

3?

o lult n

-c om ••o

n •c

o n •••J

CD Z m "J

tn

toc

-*-cr

v- en

3 , 2 iy.at er nar,y

3,2.1 Overburden Distribution end Stratioraphy

Overburden thicknesses and Quaternary stratigraphy as determined

bv re-verse circulation drilling on the Barnet property are

depicted on the overburden profiles (sheets l fc 2) found in the

back pocket of this report.

Depth to bedrock over the property ranges -from nil (outcrop) to

155 ft below ground surface. In the north half of the property,

a moder stel v undulating bedrock topography ranging 50-100 ft

below surface is indicated. Conversely, a highly irregular

bedrock topography is clearly reflected in southern sectors by

numerous bedrock outcrop Juxtaposed next to deeply buried bedrock

l D W S .

In general, a simple Quaternary stratigraphic package

representing the final south-southeasterly (Late Wisconsinan')

glacial advance and retreat phases is present over the Barnet

property,

17

Quaternary stratigraphy on the claim group is dominated by

glaciolacustrine sediments o-f the Bar low-0jibway Formation. This

unit typically forms a ubiquitous mantle up to 150 ft thick over

the property, contpr i sing 70-907. of the entire overburden section.

Glaciofluvial pebble-cobble gravels are also widespread and

frequently coiiiprise the cm l y coarse clastic sediments cored

within drillholes. Upper level sandy gravels deposited as

subaqueous outwash are typically polymictic in l ithological

composition, and reflect diverse, distant source areas from

plutonic terrains. Coarser basal gravels reflecting more

proximal, up-ice metavolcanic/metasediment source areas (8G7.+ of

clast content-few exotic species) frequently form the bottom

sample, sctino as a reasonable sampling proxy where glacial

di ami c tons are absent,

Abnormally thick sequences of sorted/bedded sands and gravels

more than 100 ft thick were intersected in holes NBR87-09 and

-10. suggesting the presence of a buried esker-outwash svsteiti.

Tills d lodgement and meltout types) and other glacial diamictons

of the Matheson For mat i on - primary geochemical sampling targets

of this drilling program - are sporadically distributed across

the Barnet property. AE depicted in profile (sheets 1&2, back

pockets), these sediments were cored in onlv twelve of

twentv-ninc drillholes. Till thicknesses tvfiicallv range less

than 10 ft. although hole N6R87-01 cored approximately 35 ft of

18

glacial sediments. Proximally derived clast lithologies

characteristically comprise B0~95*/. of total semple content in

subgla.ci al lv deposited tills, thus reflecting their importance as

valid geochemical samplings o f up-i ce bedrock terrains.

3.2.2 Overburden Geochemistry and Results

Saniole processing techniques and geochemical methods are fully

explained under Appendix B.

Date produced by lire assay and esther geochemical analyses are

statistically compiled to (i) assess overall patterns of

geochemical distribution within the glacial overburden, and (ii)

to detect the presence of anomalous results from within the

general data population.

Anomalous results sre determined bv integrating both

statistically processed geochemical values with empirically

ranked data. Raw assay data normalized to bulk assay form assist

in determining geochemical anomaly thresholds. Bulk assay

results are then subjected to a ranking procedure which factors

together the lithogenetic host, position in-the-hole and total

ooid orains within the sample.

19

Ranked anomalous results are finally evaluated in the context of

ail available oeolcipical information to draw final conclusions

and recommendations. Significant concentrations of anomalous

results within glacial overburden are usually recognized as

dispersion fans which warrant follow-up work to define specific

bedrock targets-,

Geocheinical data produced bv the NBR87 drilling program will be

evaluated according to the above procedures to determine the

Dotential for bedrock mineralization on the Barnet property

claims. Recommendations for anv additional follow-up work on

these c.laius will be made on the basis of these evaluations.

20

4 CONCLUSIONS

A program o{ reverse circulation drilling has been completed on

behalf of Norande. Exploration on the company's Barnet claim group

in Barnet end Michaud Townships. Ontario. A total of 2305 ft.

were drilled to evaluate the property s bedrock and overburden

geochemistry for indications of economic gold/base metal

mi nerali z at i on.

The following conclusions have been reached with respect to the

Barnet property reported on herein:

i) Archean mafic: metavol carii cs. together with lesser

metasediment s, syenite and diabase, were intersected in bedrock

during this drilling program.

2i Thin to moderately deep Quaternary (glacial) drift ranging

in average thickness from 50 ft to 150 ft covers the Barnet c l a i ITI

group. Numerous prominent outcrop are present in southern parts

o-f the property. A single phase of Late Wisconsinan glacial

advance (south-southeasterlv movement) and retreat is represented

in t.tie overburden section. Proximal!y derived till and glacial

diamicton deposits of the Matheson Formation are sporadically

distributed in onlv 12 of 29 drillholes completed, in thicknesses

generally less than 10 feet. Glaciofluvial deoosits related to

ice retreat are widespread but typically thin. Glaciolacustrine

21

s i 11 s and clay s i B e r l o w - O j i b w a y Formation) form a thick drift

mantle (up to 150 ft) over the entire Barnet property, except

over prominent bedrock outcrops.

3) Overburden samples collected during the NBR87 drilling

proorani underwent heavy minerals concentration by tabling and

heavy liquids, and ooid grain evaluations. Concentrates

were ultimately subjected to geochemical analyses by fire assay

and atomic absorption for gold, zinc, copper, lead and nickel.

Follow-up work to this drilling program is to be recommended on

the basis of full geochemical/geological data analyses.

R&spectful l y sub m i 11 e d.

OVERBURDEN EXPLORATION SERVICES LTD

s A. Richard, H.BBS

March 8. 1988

5 REFERENCES

Antevs. E.(1928): The last glaciation, with special reference to the ice

retreat in northeastern North America? A RI. Geog. Soc..Res. Ser. no. 17. 281p.

Baker. C. L. and Steele. K.G.(1987): Bold Grains in Sonic Drill Core Samples (1987) -from the

Lake Abitibi-Matheson area. District of Cochrane! Ontario Geological Survey, Nap P.3097. Beophysi cal /Geochenti cal Series-Preliminary Hap, scale Is 100,000. Geology 19B7.

Baker. C.l... Seaman, A. A., and Steele, K.G.U960): Quaternary Geology of the Ramore Area. Districts of

Cochrane anci Ti mi skami no; Ontario Geological Survey Preliminary Map P.2381. Geological Series. Scale 1:50,000. Geology 1979.

Bouchard. H.. LaSalle. P., David, P., Bouillon, J.J (1986): Pleistocene stratigraphy of northwestern Abitibi from

boreholes and excavations at Selbaie mine, Quebec: Abstracts, of the GAC-MAC-C6U, May 19-21, 1986, Carleton University, Ottawa. Ontario, v.ll, p.47.

Dyke, ft.S., Dredge, L.A.. Vincent. J.S.(1982): Configuration and dynamics of the Laurenti.de ice sheet

during the t.ate Wisconsin maximum: Geographic Physiqueet Quaternaire, v.36. nos.1-2, p.5-14.

Fulton, R.J. and Andrews, J.T, (eds)(1967): The Laurentide Ice Sheet; Geographic Physique et

Quaternaire, v. XLI, no. 2, 318 p.

Hughes, O.L.(1959): Surficial geology of the Smooth Rock and Iroquois

Falls map-area. Cochrane District, Ontario? Unpubl.Ph.d dissertation. University of Kansas, Lawrence,Kansas, 190p.

MERQ-OGS(1964): Lithostratigraphic Hap of the Abitibi Subprcivinces

Ontario Geological Survey, Map 2464, scale 1:500.000.

Ontario Geological SurveyU986): Rotesonic Drilling Operations U984) and Overburden Heavy

Mineral Studies. Matheson Area, District of Cochrane;Ontario Geological Survey Open File Report 5569, 60 p.

(1987): Barnet Township, District of Cochrane: Ontario Geological Survey, Geological Data Inventory Folio 349, compiled by staff of the Resident Geologist's Office, Kirkland Lake,27 p. and 2 maps.

(1988): Michaud Township. District of Cochrane: OntarioGieol DO) cal Survey, Geological Date Inventory Folio 382, compiled bv staff of the Resident Geologist's Office, Kirkland Lake. 60 p. and 3 maps.

Pyke, D.R.. Ayres. L.D. and Innes, D.G.(1973): Ti mini ns-k'i r kl and Lake, Geological Compilation Series, Map

2205. Cochrane, Sudbury and timiskaming Districts, scale1:250.000.

Richard, J,A.(1964): Quaternary Geology o-f the Porquis; Junction (42A/10) and

Watabeag River (42A/7) Map Areas, District of Cochrane;in Summary of Field Work, Ontario Geological Survey,Misc. Paper 119, p.2B3-285.

Sauerbrei. J., E.F. Pattison, Averill. S.A,(1985): Till sampling in the Casa-Berardi area, Quebec; a case

history in orientation and discovery; Paper presented at the lith International Geochemical Exploration Svniposi Lin, Toronto. April 30, 1985.

Shilts, W.W.U980): Flow patterns in the central North American ice sheet;

Nature, v.286, no. 5770, p.213-218.

Skinner. R,G.(1973): Quaternary stratigraphy of the Moose River basin;

Geol. Burv. Can. Bull. 225, 77p.

Veillette. J.(3986): Former southwesterly ice flows in the Abitibi-Timiskaming

region: implications for the configuration of the late Wisconsinan ice sheet; Can. J. Earth Sci., v.23, no, 11,p.1724-1743.

Vincent, J. and Hardy, L. (1979): The evolution of glacial

Quebec and Ontario; Geollakes Barlow and Ojibwav in Surv. Can. Bull, 316, IBp.

6 APPENDICES

6.1 APPENDIX A. NBR67 SUMMARY DRILLING REPORTS

OVERBURDEN EXPLORATION SERVICES LTD. Progress Report: Norandi Exploration (Tiuins) Oct. 27, 1967

1 OVERBURDEN FT6 I BEDROCK FT6 1

INBR-87 MIE I OVFROM I OVTO I BRKFROH I BRKTO I TOT FT6 J CUH FTG I OVSHPLS I BRKSHPL I

-

01

02

03

04

-

05

06

07

OB

09

10

10

11

1!

12

13

14

15

16

17

16

19

13.10.87

14.10.87

14.10.67

15.10.87

15.10.87

16.10.67

17.10.67

17.10.87

17.10.87

17.10,87

18.10.87

19.10.87

20.10.87

20.10.87

21.10.67

21.10.87

21.10.87

21.10.87

21.10.87

22.10.87

22.10.67

22.10.87

22,10.67

-

0

0

0

0

.

0

0

0

0

0

0

123

0

0

0

0

0

0

0

0

0

0

-

108.6

93.5

36.8

97

-

94.2

76

57

11

80

123

135

54

0

41.5

71.4

60

94

111.6

61

64

38.6

-

106.6

95.5

36.6

97

.

94.2

78

57

11

60

-

135

54

56

41.5

71.4

60

94

111.6

61

64

36.6

-

112

97

40

102

.

96

61

il

14

81

-

138

56

61

45

75

64

97

115

64

71

42

-

112

97

40

102

.

98

81

61

14

81

123

15

58

3

45

75

84

97

115

64

71

42

-

112

209

249

351

-

449

510

591

605

686

809

824

882

865

930

1005

1069

1186

1301

1365

1436

1478

-

?

?

?

2

.

2

3

1

I

7

.

11

-

-

i

4

2

5

1

1

3

1

-

?

?

16016

16019

-

16022

16026

16028

16030

16038

-

16050

~

16053

14055

16060

16063

16069

16071

16073

16078

16080

BRKTYPE

Halle Hetivolc.

Mafic Hetavolc.

Malic Metavolc.

Malic Netavolc.

.

Malic Metavolc.

Malic Metavolc.

Malic Metavolc.

Malic HetavDlc.

Malic Netavolc.

.

Malic Netavolc.

-

Syenite

Basalt

Sandstone

Malic Vole.

Basalt

Basalt

Malic Vole.

Int. Vole.

Malic Vole.

I REMARKS I

Mob. to hole 101

Old hole f 03

Old hole 129

Old hole 128

Dozer stuck, drillpulls out, no holes.Old hole 104

Old hole 105

Old hole 106

Old hole 107

40i east ol old hole108; trouble crossingcreek; bit breaks inhole at 81'.

Hydraulic clutchblDnnj take bridgenhile repairs going(old hole 109)

Old hole 109) verybldry. last 12'Old hole 110

Old hole 110

Old hole 111

Old hole 112

Old hole 113

Old hole 114

Old hole 115

Old hole 116

Old hole 117

Old hole 118

, 5

OVERBURDEN EXPLORATION SERVICES LTD. Frogrtii Report: Noranda Exploration ITinins) Pj. 2

I OVERBURDEN FT6 1 BEDROCK FT6 I

INBR-87 DATE I DVFRON I OVTO 1 BRKFROH 1 BRKTO I TOT FTB I CUH FT6 I DVSMPLS I BRKSHPL l BRKTYPE

20

21

22

23

24

25

26

27

28

29

22.10.87

23.10.87

23.10.87

23.10.87

23.10.87

23.10,87

23.10.87

24.10.87

24.10.87

24.10.87

0

0

0

0

0

0

0

0

0

0

55

52

152

34

119.4

70.5

122,5

46.7

95.5

46.5

55

52

152

34

119.4

70.5

122.5

46.7

95.5

46.5

se

55

155

37

124

74

126

SO

98

50

SB

55

155

37

124

74

126

SO

98

50

1536

1591

1746

17B3

1907

19B1

2107

2157

2255

2305

1 I60B2 Hafic

1 160B4 Hafic

1 16086 Hafic

1 16088 Hafic

2 16091 Hafic

1 16093 Hafic

1 16095 Hafic

Vole.

Hetavolc.

Hetavolc.

Hetivolc.

Httavolc.

Hetavolc.

Hetavolc.

1 16097 Hetivolc.

6 16104 Hafic

1 16106 Hafic

Hetavolc.

Hetavolc,

1 REMARKS

Old hole

Old hole

Old hole

Old hole

Old hole

Old hole

Old hole

Old hole

Old hole

Old hole

119

120

121

122

123

125

126

127

124

12

OVERB DEN EXPLORATION S E R*v* I C E CIRCULATION DRILL HOLi*T D

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6.2 APPENDIX B. SAMPLING AND ANALYTICAL PROCEDURES

Bradley Bros, Drilling o •f Timmins, Ontario provided a reverse circulation Acker drill svEtem. mounted on a GoTrack BT-3000 and enclosed -for all-weather operations. This fully hydraulic Acker rio features a direct-drive connection to the GT-3000, resulting in exceptional drilling performance.

The dual-tube drill rods used bv Bradley Bros Drilling measure 10 it l one by 2.75 inches (--outer rod. i inch inner rod), and are fed in 10 ft strokes bv the Acker drill. A controlled mixture of compressed air end water is pimped down the outer annulus of the drill rod string to a tricone bit, measuring 2.94 inches in diameter, which is adapted to the rods bv a l ft 'sub'. The bit cones are fitted with tungsten carbide buttons, the configuration of which reduces boulders and bedrock to chip size. The pressurised air-water mixture ensures that sediment/rock chip returns are brought to surface almost instantly through the l inch inner tube, thus enabling the geologist to accurately correlate overburden lithostratigraphy with downhole depth.

The- returning sample slurry produced by reverse circulation is slowed down at surface by a cyclone which discharges directly into the sampling equipment. The sample passes through a 10 mesh (1,7mm) screen which collects sediment globules and coarse, mul ti -mi ner al l ic rock -fragments, thereby enabling the petrolooical details of overburden units to be noted. A small cut D -f the +10 mesh fraction is saved for later examination in the event of anomalous geochemical results. The 10 mesh sieve is supported over the primary sampling bucket by a larger l cm screen .

Samp l e col lection by OES emplovs a three-bucket system. The sample slurry is directlv dispensed in a plastic bag which lines a 20 litre- primary bucket. Overflow decants into a second unlined bucket where the fines (silt and minor clay) are collected. TD reduce the suspension of fines bv turbulent churning, the decant spout is dispersed against the side of the second bucket, thereby maximizing the settling out. of predominantly silt sized fines.

To maintain data control and accuracy, sampling intervals are confined to individual lithostratigraphic units, keeping overlap to a minimum. Sampling intervals generally average 2-2.5 m in thicker, sorted (glaciofluvial) units, but were reduced to a maximum of 1.5 m in till or diamicton units. In cases where drill penetration through glaciofluvial sediments produce verv high volume returns, samples are reduced on-site to a representative size. Where similar high volume returns were experienced over short intervals in dense, compact till units. total samples are not reduced, but split into A and B subsamples.

Contamination controls are strictly maintained bv OES personnel. All sampling equipment coming in contact with sample materials are constructed o -f stainless steel. To minimize sample handling and the possibility of cross-contamination, samples are captured directlv into bags, thereby eliminating the step of arbitrarily "grab sampling from bucket to bag. Sample bags are sealed iff! HI e d i ste! y and placed in metal cans on-site for shipment.

f-.E.r- OS. f..! s i.n.Q

Bulk overburden samples obtained during this program were shipped to the heavy minerals laboratory of Overburden Exploration Services in Timmins. Ontario. No sample splits were taken. A flow sheet depicting DES heavv mineral concentration procedures is shown in F i our B 2.

HEAVY MINERAL CONCENTRATION FLOW CHART

FIELD SAMPLE

C REGISTRATION BULK (WET) WEIGHT (kg)

OPTIONAL SUB-SPLITS

*10 MESH STORED (OPTIONAL)

TABLE LIGHTS STORED (OPTIONAL)

C +IO MESH SCREENING

SHAKER TABLE Preliminary V.G. Grain Count

Praconcantrata Drlad

MAGNETICS STORED (OPTIONAL)

0.3 S. G. STORED (OPTIONAL)

MAGNETIC SEPARATION

HEAVY LIQUID SEPARATION Methylana Iodide (S.G. 3.3)

C SUPERPANNERJ

\ B INOCULAR MICROSCOPE EXAMINATIONOoid Count A Mlneraloglcal Examination

A

j SPLIT STORED *-

C NON- MAGNETIC HEAVY MINERAL CONCENTRATE

Optlonal 3:1 Split

REPORT - SHIP TO ANALYTICAL LABORATORY

* PROCESSING SPLITS WEIGHED AND RECORDED AT EACH STAGE

Bulk samples are first weighed (wet); the entire sample is then wet-screened through s 1 0 mesh (1.7mm) sieve to remove any t2mm rock fragments and sediment, globules present. The remainder is passed through a classifier before release onto the specially modified Beister shaker table where the combined action of continuous water flow and controlled agitation on the riffled table surface causes the samole to partition into discrete mineral bands according to specific gravity. Heavv minerals larpely consisting of horneblende. epidote, pamet, pyrite, and magnetite (ascending order) form distinct bands higher up on the table deck, all of which are captured as the table preconcentrate.

Visible gold grains coarser than 125 microns generally ride 5-lOcm above the magnetite band on the shaker table, with finer gold i)ess than 125 microns) riding peripheral to, or within. heavv mineral bands of lower specific gravity. In monitoring the partitioning of heavy minerals under magnification, free gold grains are readilv observed on the table and counted.

Table preconcentrates are subjected to a magnetic separation procedure which typically reduces the sample by another 25-30?.. Dnlv materials with the highest magnetic susceptibil ies (i.e. drill steel and magnetite) are removed to vield a non-magnetic preconcentrate; pyrrhotite and most ilmenite remain.

This fraction is further refined by a heavy liquid separation (methylene iodide, S.G. 3.32) to produce the final non-magnetic heavy mineral concentrate (HMD) ready for assay.

Panning Procedures

HMD's noted on the shaker table to contain visible gold grains and/or significant sulphides are specially panned and examined under the binocular microscope. Individual gold grains are measured three dimensional!v to calculate the expected Au ppb values based upon their apparent volume related to concentrate weight .

Visible gold grains are classified by DES according to the current industry standard as outlined in Ontario Geological Survey Open File Report 5569. but. only to the extent of 'pi aeon-hoieing ' typical grain shapes for comparative u u r f o s e s.

Under this classification, "delicate", "irregular", "abraded" and "rounded" forms comprise a morphological continuum that attempts to directly relate grain shape with glacial transport distance (up-ice distance to auriferous bedrock sources). While seemingly convenient, this classification strictly assumes that originally, all free gold grains were mechanically liberated at the bedrock-ice interface, englacially transported down-ice, and

deposited by subglacial lodgement processes. The simpler thethree dimensional grain shape, the greater the distance ofmechanical abrasion and hence, distance to bedrock source.

In fsct. this popular gold grain classification scheme -fails to consider the effects of several important factors, including;

(i) the complex diversity of sediment transport/deposi ti onal mechanisms and ice dynamics which exist in the glacial environment, and their multiple impacts upon ooid grain shape;

iii) original ooid form within rock; (iii) gold liberated directly from mineralized rock fragments

in the overburden upon impact by the drill bit; (iv) possible effects of hydromorphic precipitation upon gold

grain shape.

In considering the above points, the validity of the current gold grain classification scheme is suspect. OEB therefore does not use nor recommend interpretation of distance to bedrock sourcesbased upon grain shape alone,

Non-magnet i c heavy mineral concentrates from the MBR B 7 overburden drilling program were shipped directly to Minen Laboratories of Ti mains. Ontario. Heavy mineral concentrates were analyzed for gold bv fire assay (whole sample); a 2g split was subjected to a multi-acid digestion, then analyzed by atomic absorption for C;u, Zn . F'b and K'i .

Bedrock chips were subjected to standard pulverization and fireassay procedures.

6.3 APPENDIX C. HHC LABORATORY LOGS

P6.1 of 2OVERBURDEN EXPLORATION SERVICES LTD.

REPORT DATE: Nov. 5, 1967 CLIENT: Noranda Exploration Coipany Ltd.

SERIES: MBR

EaaaBaasaEaasEaaaEaaaEEBaasssaEsasBsaaSBBBBBBaBBsaaBBa BSBaasaaaaKg.(wet) Grans (dry)

Saiple No.

160001600116002160031600416005160061600716009160301603116012160341601516017160181602016021160231602416025160271602916031160321603316034160353603616037160391604016041160421604316044160451604616048160491605116052

Bulk

6.686.426.144.196.235.955.332.669.617.109.245.357.8010.276.437.458.135.769.849.996.067.335.977.684.78B. 807.407.386.8411.1310.501.195.738.53B.439.007.266.675.846.566.03B.90

+30 Hesh

.63

.25

.30

.59

.74

.38

.63

.25

.53

.27

.69

.26

.24

.07

.26

.83

.71

.66

.56

.60

.64

.44

.301,01.00.35.04.14.18.53.39.05.89.90.80.69.71.12

1.971.711.09.49

Table Feed Tat

6.056.175.843.605.495.574.702.419.066.838.555.097.5630.206.156.627.405.109.289.395.426.695.676.674.768.457.367.246.6610.6010.111.144.847.637.638.316.556.553.876.856.946.41

ile Cone.

93.5091.75100.2550.8562.8675.5248.4434.23123.0577.43

226.8057.2893.0876.4463.4771.7584.0066.97101.0675.3761.8091.7067.07116.11109.6577.81126.0456.4963.2182.2385.2610.0654.1677.6343.67101.1443.74202.6136.3946.4046.4162.86

Hags.

12.689.327.743.405.896.114.452.1317.2713.2516.506.62

11.8714.446.337.4111.035.1714.0413.066.7010.396.339.075.6510.768.727.4616.6918.9914.61

.336.0621.8713.4024.7911.55122.5310.1319.988.6412.07

NonHags.

80.8282.4392.5147.4556.9969.4143.9932.10105.7864.18

208.3050.4681.2162.0055.1464.3472.9761.6067.0262.3155.1061.3160.74107.04103.6067.03117.3249.0146.5263.2470.659.73

46.1055.7630.4776.3532.1960.0826.2626.4239.7770.81

H.I.Lites

58.2664.6772.7540.1541.4056.9733.6625.6671.0035.93173.6535.6156.2333.0937.5948.1250.7347.5651.6736.6939.2556.9746.5986.5585.0245.4694.1635.5926.4829.5636.706.41

33.2731.6817.1043.6617.4253.9315.1912.3519.7245.71

H.I. H.

22.5417.7619.767.3015.5912.4410.136.44

34,7828.2534.6514.6524.9626.9117.5516.2222.2414.2435.1525.6215.8524.3414.1520,4916.7821.5523.1613.4220.0433.6633.951.32

12,6323.8613.3732.6914.7726.1511.0714.0720.0525.10

Con. F. i

268347296493352448464374261242247343303353350408333358264367342263401326255392316539332315298864377320571254443250350487346335

1) N.I.K. - Final non-aagnetic heavy lineral concentrate.

21 Con.f. - Concentration factor.

P6.2 of 2OVERBURDEN EXPLORATION SERVICES LTD. REPORT DATE: Nov. 5, 1987

CLIENT: Noranda Exploration Conpany Ltd.SERIES: N8R

SSBESSSEEEB3BSESSSEESEBSEBBESEEBEBBSBB*B*8B*BBBSBSBSES BESBBBSBEBKg.(wet) Grais (dry)

Saiple No.ssiEESsrsr:

16054160561605716058160591606116062160641606516066160661607016072160741607516076160771607916081160831608516087160891609016092160941609616098160991610016101161021610316105

Bulk *irzrzrsrssrsr

6.006.255.958.103.169.275.789.176.54.67

5.064.685.0310.457.794.232.547.128.679.459.412.171.60

11.143.617.B29.6412.2211.064.799.406.632.998.85

10 Mesh l iE^rzrsssESi:

.48

.66

.34

.55

.22

.26

.24

.12

.36

.23

.31

.691.09.71.82.13.13.85.88

1.52.95.32.37

1.44.10.81.69.34.57.35.18.52.06.48

ible Feed TatSSEESSEBSEES'

5.525.595.617.552.949.015.549.056.18.44

4.753.993.949.746.974.102.416.277.797.938.461.851.239.703.517.018.9511.8810.494.449.226.112.938.37

ile Cone.ESBBBEaBBES:

55.8761.7567.1695.1546.03100.5671.4595.3353.957.70

54.1662.0253.6685.2564.7237.1429.4879.66117.7983.6380.4232.2813.3297.5278.6194.4099.99104.44137.9329.2168.1046.4134.1272.96

Hags, iEESBSEBSEBB

10.087.058.298.953.8014.597.2412.387.86.48

4.906.707.2813.208.614.372.729.5813.7514.0312.421.62.90

14.485.8411.6813.6710.5522.564.7212.3710.455.4511.10

BonHags..SBBSSBSBBE!

45.7954.7058.8786.2042.2385.9764.2182.9546.097.22

49.2655.3246.3872.0556.1132.7726.7670.08104.0469.6068.0030.6612.4283.0472.7782.7286.3293.89

115.3724.4955.7335.9628.6761.86

H.l.LitesssEBBaiBXBESB:

27.7937.5339.6560.8831.5446.4245.6053.6827.675. 98

33.7923.2925.7939.8431.2021.0119.1345.0770.1441.1036.2627.4410.3851.3460.1753.6254.0670.9576.3116.1835.1321.6519.3238.68

Avirigi -

Standard -Deviation

H.I.K.:SSBBBBBBSaS:

18.0017.1719.2225.3210.6939.5518.6129.2718.421.24

15.4732.0320.5932.2124.9111.767.6325.0133.9028.5031.743.222.04

31.7012.6029.1032.2622.9439.068.31

20.6014,319.3523.18

20,45

9.26

Con. f.SaBESSEE

307326292298275228298309336355307125191302280349316251230278267575603306279241277518269534448427313361

347

109

1) H.I.H. : Final nonmagnetic heavy lineral concentrate.

2) Con.F, - Concentraiion facior.

Dec iarat i on of Qualifications

l, James A, Richard, do hereby certi-fv that:

i) I am a Quaternary geologist, and reside at 576 Gordon Street. Timmins. Ontario. P4N 764:

ii) I hold an H.BE5 decree (1981) from the University of Waterloo. Waterloo, Ontario:

iii) I have completed two years H.Se course wort; (geology) at the University of Waterloo. Waterloo, Ontario:

iv) I am an associate member o-f the Geological Association ofCanada:

vi 3 have been actively engaged as a Quaternary geologistthroughout northern Ontario-northwestern Quebec since 197B. both as field party leader and consultant for the Ontario Geological Survey (1981-1985). and as an exoloration consultant to private industry since 1985.

vi i I have not received, nor will I receive, an interest.directiv or indirectly, in the properties of the client, orany affiliate:

vii) l was personally involved with the technical supervision of the orooram. and wrote this recort.

LG H d MMinistry of Report of Work Northern Development

_ and Mines (Geophysical, Geological, Ontario , Geochemical and Expenditures)

. s* A ir

\fiffot- on M 42A88NE0882 2.109)8 MICHAUD 300Type of Survay(s)

Overburden Drilling Sec. 77-^ *| fl f\ 1 O BarnetClaim Holder(s) ^W S 1 \^ fjf JL \^ /p V

Noranda Exploration Company, Limited/ Michael Leahy'"fi

1^18263^1958Address

Suite 1300-4'.King St. W., Toronto, Ontario M5H 1B6Survey Company

Bradley Bros. Ltd., Box 485, TimminsDate of Survey (from tt to)\V \* VI l **-\ v* *nDay l Mo. | Yr. ] Day l Mo. l Yr.

Name and Address of Author (of Geo-Technical report)

Jim Richards, c/o Overburden Expl. Services Ltd. 43 Iroquois Rd.

Total Miles of line Cut

vi/ *^

Timmins, Ont.Credits Requested per Each Claim in Columns at right Mining Claims Traversed (List in numerical sequence)Special Provisions J Oeophytic8|

For first survey: R.fiCElVcD' IN 1* ^••TflettromagneticEnter 40 days. (This includes line cutting) 1 vyapne^ftOOer

J LA N LI i IN/WV'

For each additional survey: using the same grid: . L

Enter 20 days (ffdtHMK

Man Days

ar

A

î^(Mfmlittm'vmfffiPRfeflWUJcacî-5 ' -'

J" JAN 18 It^"~

•ne Credits

•e: Special provisions credits do not apply to Airborne Surveys.

- Radiom

IAAII&

Btric

SEfiTlOGeological

Geochemical

Geophysical

iZi^ i Electromagnetic

•la 1 Magnetometer

'li i paojf metric

^ - Othel

Geological

Electromagnetic

Magnetometer

Radiometric

Expenditures (excludes power

Days per Claim

1

Days per Claim

Days per Claim

stripping)Type o ( Work Performed

Overburden Till Sampling, Sec. 77-19Performed on Claim(s)

L-821229, L-822592-93-94

Calculation of Expenditure Days Credits

Total Expenditures

S511,225.35 -i- 15

Total Days Credits

= 748Instructions

Total Days Credits may be apportioned at the claim holder's choice. Enter number of days credits per claim selected in columns at right.

DateJanuary 15/88 -

Recorded Holder or Agent (Signature)

. ^-~" — ,a m ^^ ^^ - j^

Mining ClaimPrefix Number

L 821225H^fi 821226•^jffiffi*! Q91O'9"7 iffiji'ihr VuV J O*C \ i-LI

^^{ 821228S^ 821229'^S\feft 822590rfft*^' 822591

Jf5"i 822592

f*:-r-i ! 822593

J:;,".! 822594

k- -:.^ 822595- 1

i

'

H

!1

'

Expend. Days Cr.

6060

60

6060

6060

60

60

60

60

Mining ClaimPrefix

I i^v^l

For Office Use OnlyTotal Days Cr. Date Recorded ^W . Recorded /^ ^^

v7*2^x 'fS/i^\P\eQ , jXste Approved as Recorded

IIP

Sf^fj; iigrja

P

Number

1" "~ti

SiiÊi•w2*V{!

^|3

-y-

- -'-S -' "

J,' VsJj3 ..•SV"

- , - p ' .1*4 ' .

' V ' '

'

i —————————

——— —

— - -- - -

Total number of mining claims covered by this report of work.

Expend. Days Cr.

i

11

•Mining Recorder

Branch O\r^c\gf^^y

Certification Verifying Report of Workl hereby certify that l have a personal and intimate knowledge of the facts set forth in the Report of Work annexed hereto, having performed the work or witnessed same during and/or after its completion and the annexed report Xs true.

Name and Postal Address of Person Certifying

R.C. Denommee, P. 0. Box 1205

Timmins, OntarioDate Certified Certified by (Signature)

January 15/881362(65/12)

odrue LMinistry of

- Northern Development l Mines

Report of Work(Geophysical, Geological, Geochemical and Expenditures

ions: — Please type or print.- If number of mining claims traversed

exceeds ipace on this form, attach a list. : — Only days credits calculated in the

"Expenditures" section may be entered In the "Expend. Days Cr." columns.

1 IP . .-S rf W 'Mfi^#*t^\f^!\ - '""""V"" ^'KType of Survey(s) l -4

Overburden Drilling (Sec. 77-19)Claim Holder(s)

Noranda Exploration Company, LimitedAddress

Suite 1300 - 4 King St. W., Toronto, Ontario M5H IB*Survey Company Date of E

Bradley Bros. Ltd., Box 485, Timmins, Ontario i^y l iName and Address of Author (of Geo-Technica! report)

Jim Richards, c/o Overburden Exploration Services Lt(

) 1 1 is - uo not use shaded areas tTownship or Area

Barnet tt M ichaudProspector's Licence No.

A-34387

)urvey (from 81 to) [Total Miles of

J. 43 Iroquois Rd., Timmins,

MlOW.

line Cut

OntarioCredits Requested per Each Claim in Columns at rightSpecial Provisions

For first survey:

Enter 40 days. (This includes line cutting)

for each additional survey: using the same grid:

Enter 20 days (for each)

Man Days

Complete reverse side r.^^lflf.npllr1hnfP

n)IF' '^MAR le isfr-

q.e^o^vi*^^

Note: Special provisions credits do not apply to Airborne Surveys.

Geophysical

- Electromagnetic

- Magnetometer

- Radiometric

- Other

Geological

Geochemical

Geophysical

^, - Electromagnetic

"1Geol

Geo

adiometric

ither

gical

lemical

Electromagnetic

Magnetometer

Radiometric

Days perClaim

Days per Claim

Days per Claim

Mining Claims Traversed (List in numerical sequence)

Expenditures (excludes power stripping)TVP* of work Performed 29 Reverse Circulation

Overburden Till Sampling, Sec. 77-19Performed on Claim(s)

see attached list

Calculation of Expenditure Days Credits

Total ExpendituresTotal

Days Credits

35,314.13Instructions

Total Days Credits may be apportioned at the claim holder's choice. Enter number of days credits per claim selected in columns at right.

DateMarch 10/88

Recorded Holder or Agent (Signature)

Certification Verifying Report of Work

Total number of mining claims covered report of work.

Date Approved as Recorded

l hereby certify that l have a personal and intimate knowledge of the facts set forth in the Report of Work annexed hereto, having performed the work or witnessed same during and/or after its completion and the annexed report is true.

Name and Postal Address of Person CertifyingR.C. Denommee, P.O. Box 1205

REPORT OF WORK

cm* NO.L. 805117 TL. 805118 TL. 805119 TL. 805120 TL. 805121 TL. 805122 TL. 805123 TL. 805124 TL. 805125 TL. 605126 TL. B05127 TL. 805128 TL. 805129 TL. 805130 TL. 805131 TL. 805132 TL. 80513? TL. 805134 TL. B05I35 TL. 605136 TL. 805137 TL. 805138 TL. B05139 TL. 805140 TL. 805141 TL. 805142 TL. 805143 TL. 805144 TL. 805145 TL. 805146 TL.' 805147 TL. 805148 TL. 805149 TL. 805150 TL. 805151 TL. 805152 TL. B05153 TL. 805154 TL. 805155 TL. 805156 TL. 805157 TL. B05158 TL. 805159 TL. 805160 TL. 805161 Tl. 805162 TL. 605163 TL. 805164 TL. 805165 TL. 605166 TL. B05167 TL. 605168 TL. 805169 TL. B05170 TL. 805171 T

List of MiningPats Credit 40.00 40.0040.0040.00 40.0040.0040.0040.0040.0040.0040.0040.00 40.0040.00 40.00 40.0040.00 40.00 40.00 40.0040.00 40.0040.0040.0040.0040.0040.0040.0040.0040.0040.0040.0040.0040.00 40.0040.0040.0040.0040.0040.0040.0040.0040.0040.0040.0040.0040.0040.00 J40.00 j40.00 J40.00 f40.00 l40.00 j40.00 Ci40.00

Claims

dal* No.L. 805172 L. 805173L. 805174L. 605175 L. 805176L. 805177L. 805178L. 805179L. 805180L. 805184L. 805185L. 805186 L. 605187L. 605188 L. 805189 L. 604591L. 804592 L. 604593 L. 804594 L. 804S9SL. 804596

, L. 804597L. 604598L. 804599L. 604600L. 804601L. 804602L. 604603L. 804604L.. 804605L. 804606L. 805756L. 805757L. '805758L. 805759L. 805760 L. '805761

[jf^[p3Jg3gCE5rlit/ 1 lC /fnJr*'iJuBS'**"* J **' " W/JBM

J-v — 1^w^v^*B )J56fQ U ^^M-j^o-^v^

TTTT TTTTTTTT TTT TT T T TT TTTTTTTTTTTTTTT T

.

-----j

J331J1 l m f*'//rSit1 '-

71

Days Credit 40.00 40.0040.0040.00 40.0040.0040.0040.0040.0040.0040.0040.00 40.0040.00 40.00 40.0040.00 40.00 40.00 40.0040.00 40.0040.0040.0040.0040.0040.0040.0040.0040.0040.0040.0040.0050.0050.005 Q 00 17.00

Ministry ofNorthern Developmentand Mines

Ontario

Geophyslcal-Geological-Geochemlcal Technical Data Statement

File—

TO BE ATTACHED AS AN APPENDIX TO TECHNICAL REPORTFACTS SHOWN HERE NEED NOT BE REPEATED IN REPORT

TECHNICAL REPORT MUST CONTAIN INTERPRETATION, CONCLUSIONS ETC.

Type of Sui Township o Claim Hold

Survey Con Author of 1 Address of Covering D.

Total Miles

'vey(s) N^v)^l2vfc

r Area O A '

er(s} M O/ÂisiPA

ipany Q\Jk.#6^

Jeport NJ^M^

UltfCUJ-AT'O/J U^/^flU/lO^'0 l/^ti-*-^rJg-T A/^D /\*cHÔ '(VAI/'^

IA) S

Â-oÂTio/o Co Uro X MICHAELf- KUtÂlicKi

ôt/^ lr^Û)(?rt-riorJ ^tôicc^•^ A . /VKlrMfcP

LTD

Author P.O. 6oxr lO'-H.'Twtirfvif; OrsiT. Pf/vJ^Htl 1

irwnf Survey IV^'^ to 24" - ^ - VI

of Line Cut

SPECIAL PROVISIONS CREDITS REQUESTED

ENTER 40 days (includes line cutting) for first survey.

ENTER 20 days for each additional survey using same grid.

AIRBORNI Magnetome

PATF.r 0^

Res. Geol.

(Unecutting to office)

DAYS~ , , . per claim Geophysical

—Electromagnetic... . ... —

—Radiometric .., ,., —

P.^lo 5r,I

r rhpmiral

l CREDITS (Special provision credit! do not apply to airborne (urveyi)

ter Rlertromagnetir RaHiomftrir(enter dayi per claim) ^^.^.^ rf

M //Y^? * S1\A# ) H-?-g SinNATIIRF- M . L^^~~^~^^7

Previous SurveysFile No.

—

/^/Author of Report or Aftent

Qualifications

Type Date Claim Holder

MINING CLAIMS TRAVERSED List numerically

L- 39H9a5(prefix) (number)

L*' ^? 3 1 99*^

U o r\ i O O L 9 o if* i ^ o~ O

L * O Cr* i (/* Oî

L. ^9^515^0L * v 0^ 0^ ^) 1 l

i ^QCi. ^^lil

L. ^5*) 3L. ^9^5^^L ^ A /\ CCQ^ * o o^ fi j lO

TOTAL CI -AIMS li

1

iS3

GEOPHYSICAL TECHNICAL DATA

GROUND SURVEYS — If more than one survey, specify data for each type of survey

Number of Stations—————————————————————————Number of Readings Station interval ____________________________Line spacing .-—-^— Profile scale________________________________________—Contour interval.

Instrument _

o

Accuracy — Scale constant. Diurnal correction method.Base Station check-in interval (hours). Base Station location and value ———.

Instrument

ECTROMAGNETK Onjl ^"figuration

fV.il separation

Accuracy. ,. ,.,.,,..,,, .. , . -,,.,,,,. ,, , .,,,, ,.,,,,, , .....,,,,,.,,Method: O Fixed transmitter Q Shoot back Q In line Frrnumrv

CD Parallel line

WParameters measured.

Instrument.Scale constant.Corrections made.

Base station value and location .

Elevation accuracy.

Instrument ———————————————————————————————————————————————— Method D Time Domain D Frequency Domain Parameters - On time ___________________________ Frequency —————

- Off time ___________________________ Range ————————— Delay time ——————————————————————————— Integration time

Power.r Ele ctro de array

Electrode spacing . Type of electrode

SELF POTENTIALInstrument_______________________________________ Range.Survey Method —————————————————————————————————————————

Corrections made.

RADIOMETRICInstrument ———

Values measured.

Energy windows (levels).——————.—————.———.—.^—^———..—^——^...—-

Height of instrument____________________________Background Count,

Size of detector__________________________________________

Overburden —-———-^—-——^^-^^————^———.——-.^.————...—.——-.^—^—(type, depth - include outcrop map)

OTHERS (SEISMIC, DRILL WELL LOGGING ETC.)

Type of survey^————.—————^————————-—

Instrument ——————^—^—————^—^—^-——

Accuracy——————————————————————————Parameters measured.

Additional information (for understanding results).

AIRBORNE SURVEYS

Type of survey(s) ———

Instrument(s) —————(specify for each type of lurvey)

Accuracy———————————————.(specify for each type of survey)

Aircraft used________________________________

Sensor altitude-Navigation and flight path recovery method.

Aircraft altitude________________________________Line Sparing Miles flown over total area________________________Over claims only.

GEOCHEMICAL SURVEY - PROCEDURE RECORD

Numbers of claims from which samples taken.

ton

Total Number of Samples. Type of Sample.

(Nature of Material)

Average Sample Weight——————— Method of Collection————————

Soil Horizon Sampled. Horizon Development. Sample Depth———— Terrain————————

Drainage Development——————————— Estimated Range of Overburden Thickness.

SAMPLE PREPARATION(Includes drying, screening, crushing, ashing)

Mesh size of fraction used for analysis———

ANALYTICAL METHODSValues expressed in: per cent D

p. p. m. Qp. p. b. d

Cu, Pb, Zn, Ni, Co, Ag, Mo, As.-(circle)

Others ——^-^————.——.—————————Field Analysis (.

Extraction Method. Analytical Method- Reagents Used——

Field Laboratory AnalysisNo. ——————————Extraction Method. Analytical Method . Reagents Used——

Commercial Laboratory (. Name of Laboratory—. Extraction Method- Analytical Method - Reagents Used -————

.tests)

.tests)

.tests)

GeneraL General.

anil MinusOntario

(Geophysical, Geological, Geochemical and Expenditures)

Mining Act

exceeds space on ihu lorm, attach .1 Only days credits calculated in "Expenditure*" lection may be entt in the "Expend. Otyi Cr." colun Do not use shaded areas below.

t

*

Tijp* o( SurveyU)

'^^ Overburden Drilling Sec. 77-19Township or Area

BarnetClaim Holder(t) /— -.

Noranda Exploration Company, Limited/ Michael Leahy I^3S8KuL826^19EAddress

Suite 1300-4* .King St. Vf., Toronto, Ontario M5H 1B6Survey Company Date of Survey (from Si to) Total Miles of line Cut

Bradley Bros. Ltd., Box 485, Timmins D^MO-LY?. oayjVio. vr. \^l *.Name and Address of Author (of Geo-Technical report)

Jim Richards, c/o Overburden Expl. Services Ltd. 43 Iroquois Rd. Timmins, Ont.Credits Requested per Each Claim in Columns at right Mining Claims Traversed (List in numerical sequence)Special Provisions . Oavs Der Geophysical â'm

For first survey: . , - Electromagneticfintpr 40 days. (This . -includes line cutting) . M,gnelometer

For each additional survey: ' R adiom"tricusing the same grid: |...........

Enter 20 days (for each) i jGeological

Geochemical

Man Oavs Oavs per Geophysical culm

^ r^^^SJSfefJlra f-6^ 'omagnet.c /^\3r ft^l^^TFPiMIcfrni I \n HP t. J ' \v ' r U J * UJ Ha U3 ^ -- S j HB e lom"" f111 i Q0d metric M

^ IS.. ^ - oth. \^

vi Geologica

Airnorne Credits - - -* Days per — Claim

Note: Special provisions | Electromagnetic :

to Airborne Surveys. Magnetometer !

Radiometric j

Expenditures (excludes power stripping)Tvpe of Work Performed

Overburden Till Sampling, Sec. 77-19Performed on Claimls)

L-821229, L-822592-93-94

Calculation of Expenditure Days Credits Total

Total Expenditures Days Credits

511,225.35 H- 15 * 748nstructions

Total Days Credits may De apportioned at the claim holder's choice. Enter number of days credits per claim selected in columns at right.

Oate Recorded Holder or Agent (Signature)January 15/88 --^- ^ — —j,, __ ___

Certification Verifying Report of Work

0


L 821225&&3P 821226

L^&il&l VL\LLI**^5ê"Ji.f*

i-SlBlf 821228821229

S 1™ lx-X-tiXiiy I338& 822594p.s-"3^ ^S^, R?2595-i^"-** - /. f , fi.1 w^-^1%.: t.-; ' .-^ ——————————— — ———

; '" ••:. !'grixfJ

' -" !

*. - '* *.4 ' " ' '

'"." ' *' '

•.^...;. i***-" ' !

3'î ———————

• ,-;'*, .

Expend. Days Cr.

6060

60

6060

• 60 [60 f 60

6060

*n

0/0 ®For Office Use Only

Total Days Cr.iOate Recorded -^W , Recorded /"J. , . V*25ot '/f/jH(o (o O , tetit Approved as Recorded


*j|BjgjjSy83 •aa'.jji— -*- .- . -K j S S2 *~"* U- -,.s i.. i .'ijjjj (j^ji

lwife ' AN 29 19!

^ JCÂNr \ GXPLOR,

P i^7 ?i.'- ••'iNQ.'oNT•vfi&J* ii * -(uac.^-. ,.."V/, 'T^J

sSaS(•i.v.MwJT•^ST"ttr&oaSfl

•^N

^^]

p4;YJ^vVN

'•.- * "-'t: -^: '.^::1..-s-, 'V '; '^' -.

' J~"v'"- t,. . .,.ST.'-- !

•'" ; .' - ^ ,••-.V.'.v i

: i ' : :v ! ,-,:.;?J j'

^ : , . j ——————'-*'*. .*. *

Exper Days (

TD

8

JIO.v

Total number of mining claims covered by this 1 1 report Of work.

Mining Recorderj* \

Branch Director

i hereby certify that l have a personal and intimate knowledge of the facts set forth in the Report of Work annexed hereto, having performed the work or witnessed same during and/or after its completion and the annexed report is true.

Name and Postal Address of Person Certifying

R ;C : " Denommee , P . ' 0?"B6)P1 205 7Date Certified Ccr,,t,.o BV .Signature,

POST DRILL SUMMARY

PROJECT: DISTRICT: TOTAL METERAGE: CONTRACTOR:

BARNET 112 STARTING DATE: OCT. 13/87 DRILLING TYPE: RCEAST ABITIBI DIVISION: N.E. ONTARIO702.57 DRILLING BUDGET: $48,300.55BRADLEY BROS COST/M: S68.75

HOLE NO.

NBR 87-01NBR 87-02NBR 87-03NBR 87-04NBR 87-05NBR 87-06NBR 87-07NBR 87-08NBR 87-09NBR 87-10NBR 87-11NBR 87-12NBR 87-13NBR 87-14NBR 87-15NBR 87-16NBR 87-17NBR 87-18NBR 87-19NBR 87-20NBR 87-21NBR 87-22NBR 87-23NBR 87-24NBR 87-25NBR 87-26NBR 87-27NBR 87-28NBR 87-29

CLAIM NO.

L-805757L-805178L-805153L-805157L-805148L-805147L-805144L-805143 'L-822592L-822593L-822594L-821229L-805124L-805129L-805125L-805126L-805126L-805130L-805131L-805133L-805176L-805175L-805174L-805173L-805165L-805166L-805138L-805163L-805179

ANGLE

VERTICALVERTICALVERTICALVERTICALVERTICALVERTICALVERTICALVERTICALVERTICALVERTICALVERTICALVERTICALVERTICALVERTICALVERTICALVERTICALVERTICALVERTICALVERTICALVERTICALVERTICALVERTICALVERTICALVERTICALVERTICAL

. VERTICAL' VERTICAL

VERTICALVERTICAL

DEPTH (M)

34.1429.5712.1931.0929.8724.6918.594.2724.6942.0618.5913.7222.8625.6029.5735.0519.5121.6412.8017.6816.7647.2411.2837.8022.5638.4015.2429.8715.24

TOTAL 29 HOLES TOTAL METERS 702.57

-V 400 surface rights reservation along the shores' ' of a ll I dkes and, rivers. ' i•,..-V. ;V . - v - . . , .•-'- '- -. -t ' ' :

-:. : ' SAND ond GRAVEL,., - - L '''.-1'. . *7——————

(?D - fcl.T.C. Crai'ti PI* N ft.7BZ

X

'a*

..S:*--,--(r

f. RESERVATIONS

-^ - . )

\-.^;. y^ i

'. ; .; N' ;F ,l .. ;;v

. .* " ' '.,; j :v f'/

1 -- ' ^ : '-':-- ' " -'-^ " ' '

:7 v AREAS WITHDRAWN. FROM STAKING : ' s.R..J-SURFACE R tGHT9 M.R.- MINING

Stcllan Offl*r Uo - Oitpotilion Fin.

S.f) "- 164566

\ (-

l nj.

OJ IDro

o. I-

T)i.O

-Q3 O

\

s MG Cool' Tp.

725103 '7?5I04783683 I7B366078*4677 (783676

B3880., ^83673 78368'^ J 78386 l

L " l L y i L lil

801872 .U001383681 783682 783665 l 783662

7Z5I36[725I37J 2SI38 [723JI39

1'V^^WilAO

f j 4 9 a i 7 ? a 9 o n803911 803906

8034)00 , 3CJ9CH

803891 1801884*

i L '804SOO i 804493 803899 8038^2

-l- J- "':

806031' 806030

40925 .40929B06023 j BQ6J2I

L ^^.If-^tKf LJt^. ^^* /.j*- rr^

321427 l 521428586490 586489 52(396 ." "" "

979900 I 979689-" - "f"' —."~

L L

586486 1586485

s#**si. i 5T^-raa714128 '714129,^'"•J. ' l •~-A-*-*—r r: r

V V ^^"" lUJ^^^V ^A"-*! J ^ ^ l V i

979848 ^79849

L L*

714126 !7I4070| 714073 ' 714076-979880 j 979879 805759 ' 8057567KI 15 7i4tl6

BQ5758 'B03TS7714114 i 714113 714(25 [714071 . TI4072 l 714077

800 00'43"opproi "

12

S00

9 ^8 , 7 6 . , 5

Barnet Tp. M.322 -* -r

r P\ucruVr 'J4-1924

1 LEG-END!r :

HIGHWAYMNB ftOUTE No,

ROADS ,TRAILS ^

SURVEYED LINES; ' . - , 7 ( TOWNSHIPS, BASE LINES, 'ETC.

; LOTS, MINING CLAIMS, PARCELS, ETC.-"7^

UNSURVEYED LINES' 'tOT LINES ^ \

PARCEL BOUNDARYWINING CLAIMS t-TC

RAILWAY AND RIGHT, OF WAY

UTILITY LINES ^

NON-PERENNIAL STREAM

FLOODING QR FLOOpING RIGHTS

SUBDIVISION ,. , - f

ORIGINAL SHORELINE -^ ^

MARSH OR MUSKEG '

MINES rf' \~* •

^\

^

\. ' i

DISPOSITION OF CROWN, LANDS

i,.pf D OCUMENT

PATENT. SURFACE A MININp RIGHTS

SURFACE RIGHTS'ONLY

MINING

•!SYMB

LEASE, SURFACt 4 MINING RIGHTS .A* "\

( SURFACi RIGHTS ONLY" ^V

MINING MIGHTS ONLY " ^L c *

LICENCE OF OCCUPATION^

CROWN LAND

•ORDER,!N-QOUNCIL

[ -,,; ,-. SCJALE : r l I NCH - 40 CHAINS ' ^ O/ v^v'^ i

f l ' ' ,- l " h * l **. T**^***^**N

X - o soo LOOO looo

'v

TOWNSHIP 4 r

MIGHADISTRICT

M l N l N fi/ l V PS l O NT

LARDER LAKEX - ',

Ministry of Natural ' Respurces v

Ontario ' Surveys and Mapping^Branch^"plafTNoT" -———

V.

Date S3 , JUNE /,74

Wlnlnny Block .-OO'S Park, Toronlo M .372

r Michaud Twp.

BARN;,DI STRICT, OF

COCHRANELARDER

MINING' DIVISIONSCALE: I-INCFK4Q'CHAINS

f ' - ' ^ . *F809 IS9 Uo5l60

l L

LEGENDPATENTLD LAND CROWN LAND SALE r

LEASES . ' LOCATEp ; LAND

tlCENSE-^OF OCCUPATION

MINING RlGHtS ONLY ~

SURFACE RIGHTS 'ONLYROADSIMPROVED . ROADS

?C 3 C 9 v' o O il c fr & 1•RAILWAYS' - '. POWER LINES

MARSH OR MUSKEG

u 9 ^ r r o i wy t{t r—— t- 4-"

NOTES*.- v .' ' (**r V-right* r*9*rva,tioo a rourtd all lak*s -'onrt' '- - '1030740 l M30T4I

F- E 7? 10 l f F ^pl B

Surfoca and Mining RlbhtiS taking, section 36/80 orrfir No JJLJliafi. . . , - . ^-,j, .~-- '. ,- - 4 -~ -,- -* 1 •"***fti."i*'

"050M4 *030M3

^^.034974

PLAN O-Melba Twp. ONTARIO

42A08NE00S2 2.10918 M ICHAUD

59/4 1805756

l| 805758 1805757

804591 ' 804592

804603 '804604 j 8 04605 . 804606H 80517 805179 805180

GRID B

85134 B65r*63 i'B05l62 BQSIt

— A- i — -t— — tb-805169 | 805170 ^05171 .805172

805128J/805127 805134 l 805133zo

805129805130 80C131 805132

IMllllimiiMii........42A(BBNEBC82 2.1*918 MICHAUD

LEGEND

3 shaftO OGS overburden d rilling

———" trail ( not driveable) . - - . road (driveable)

* swamp*— beaver dam

fltBR-97 f noranda overburden drilling

BARNET PROJECTOVERBURDEN DRILL HOLE LOCATION MAP

BARNET TWP.SCALE: 1:20,000

x

D e whirs t i oke

o

Q1 O

O Or"\

to O Or\

;-- . .v

tDO O

01 i

O Q O

e/^RNET

1 x

LEAHY OPTION'

-L

XX\

^s

2,18918 MICHAUD 230

'A s haftO OGy overburden drilling

--- -—- trail (not driveoble)- . rond (driveable)

* swamp*~. beaver dam

NBft-8? 0 noronda overburden 'drilling

BARNET TWP.

BARNET PROJECTOVERBURDEN DRILL HOLE LOCATION MAP

SCALE: 1:20,000

•RID B

00TH

Oi O

OG

S8

7-3

6 s

onic

295 a

z A 12

275

az.

B 00

-

150

.

0901

DD

1315

1617

B

95 a

z

27

o'a

z.

CC

90

az

SH

EE

T

ON

E

LEG

EN

D

O

OO

O

•l

Peo

r ,

HLJ-

MJS

,

Wate

r

S'lT

X C

lay

and

7 G

rave

l'.

flu

via

l,

gloc

io 'l

uvia

l

Dia

mic

Ton.

Un s

ort

ed

X S

emi-

sort

ed

su

baq

ueo

us

gla

cial

deb

ris

, underr

rett

an

d

flo

ws

"ill -

B

asal

Me

lto

uT

or

Lo

dg

em

en

t

Bould

er/

Bed

rock

2CL

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42A08NE0082 2.10915 MICHAUD

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RPT OB RCD NBR87 PROJ · (B-0) Fm. Essentially locally reworked 8-fl Fm created by late-glacial...

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Transcript of RPT OB RCD NBR87 PROJ · (B-0) Fm. Essentially locally reworked 8-fl Fm created by late-glacial...