CUMBERLAND RESOURCES LTD GEOL SURVEY JUNE … · WHOLE-ROCK ANALYSIS - ALTERATION SCORES...

SZK14ME0028 2.16847 GERRY LAKE Q..Q

2. 16247LTD.

GEOLOGICAL SURVEY

JUHE, SEPTEMBER 1994

gaT.T.g

HTS: 52K/14 ORTHNESTERH OHTARIO

RECEIVED

OCT 3 i 1995

MINING LANDS BRAN

C o i -L i b;^pu

Thunder Bay, Ontario SUBMITTED BT:NOVEMBER, 1994 M. P. LEWIS GEOLOGICAL SERVICES

S2K14NE0028 2.16247 GERRY LAKE

TAKLE OF i.

SUMMARY

1.0 INTRODUCTION

2.0 LOCATION, SIZE AMD ACCESS

3.0 PROPERTY SUMMARY AHD CLAIM DISPOSITION

4.0 PREVIOUS WORK

5.O REOIOHAL GEOLOGY AHD METALLOGEHY

6.0 PROPERTY GEOLOGY AMD MINERALIZATION

7.0 STRUCTURE

ALTERATION

01OC

Page

l

l

l

4

5

8

10

118.0 WHOLE-ROCK GEOCHEMISTRY8.1 HA208.2 HOSHIMOTO INDEX8.3 CU8.4 ZH8.5 COMPARISIOH OF ALTERATIOH PATTERMS TO OTHER VMS DEPOSITS8.6 TRACE ELEMEBT GEOCHEMISTRY

9.0 DISCUSSIOH

10.0 PROPOSED EXPLORATION PROGRAM AND BUDGET

REFERENCES

14

14

17

FIGURE l

FIGURE 2

FIGURE 3

FIGURE 4

FIGURE 5

LIST OF FIGURES

PROPERTY LOCATIOB

CLAIM SKETCH

SIGNIFICANT VMS OCCURREI

COMPILATION MAP

PROPOSED DEEPEN SURVEY

2

3

7

9

15

TABLE l

TABLE 11

TABLE 111

TABLE IV

TABLE V

TABLE VI

LIST OF TJ""-gS

SCHEDULE OF CLAIMS

Cu-Zn DEPOSITS AND PROSPECTS

WHOLE-ROCK ANALYSIS - ALTERATION SCORES

COMPARISIOH OF ALTERATION INDICES

PROPOSED BUDGET

4

6

11

13

13

16

APPENDIX l

APPENDIX 2

LIST OF APPrcHDIX

STATEMENT OF QUALIFICATIONS

CERTIFICATES OF ANALYSIS

18

19

PLAN 601-A

PLAN 601-B

PLAN 601-C

PLAN 601-D

PLAN 601-E

LIST OF DRAWINGS

GEOLOGY AHD ALTERATION

HA2O RESULTS

HOSHIMOTO INDEX

CU

ZN

SUMMARY

The Big Falls property is situated 50 km southeast of the mining community of Red Lake and 35 km north of the town of Ear Falls in Northwestern Ontario. The property is comprised of six contiguous mining claims, totalling 68 units. With the exception of 2 claims (18 units), which are part of an earn-in agreement with a local Red Lake prospector, the remaining claims are 100* wholly owned by Cumberland Resources Ltd. of Thunder Bay, Ontario.

The property position covers the eastern extension of favourable VMS hosting felsic stratigraphy which hosts numerous sub-economic massive and stringer base metal occurrences.

A property position immediately west of the Big Falls claims has been subjected to on-going exploration, including diamond drilling by Noranda, as part of a joint venture with a junior mining company, Major General. Two mineralized trends, which host significant massive and stringer base metal occurrences and associated stratabound and cross-cutting hydrothermal alteration, have been traced to the western boundary of Cumberland's Big Falls Property.

In June and September of 1994, a program of linecutting (25 Km), 50 km of geological mapping and lithogeochemistry (34 samples) was carried out on the Big Falls property. This program resulted in the discovery of a new and extensive proximal-type hydrothermal alteration zone in Fill type rhyolites. The alteration zone, which is 300 meters wide, and 1.5 km long, is characterized by a coarse anthophyllite-cordierite, garnet, biotite and chlorite mineral assemblage.

The results of a quantitative evaluation of the intensity of the proximal-type alteration, which is provided by determining alteration scores, and by comparing trace-element geochemistry from other known VMS deposits has greatly enhanced the probability of a VMS deposit on Cumberland's Big Falls property.

A phase 11 exploration program consisting of 16 km of DEBPEM geophysics is recommended at an estimated cost of $16,000.00. Diamond drilling would be contingent on the results of the geophysical survey.

Page l

1.0 IHTRODUCTIOH

During the period June 3rd-13th and September 26 th-October 9th , 1994 a geological survey was carried out on Cumberland Resources Ltd's Big Falls property which is located in the Red Lake area of Northwestern Ontario. The survey was controlled by extending Norex's Joy property baseline from 5100-E to 11000-E. Geological traverses were carried out over 25 km of pace and compass lines and an additional 25 km over a picket line grid established by Vytll Exploration Services of Thunder Bay, Ontario. During the course of the survey a total of 34 selected rock specimens were collected for whole-rock analysis.

2.O LOCATION, SIZE AHD ACCESS

The Big Falls property is located some 35 km north of the community of Ear Falls and 50 km southeast of mining community of Red Lake in Northwestern Ontario. The former producing South Bay Cu, Zn, Ag mine is situated some 35 km to the northeast (Figure 1).

The property is comprised of six contiguous mining claims totalling 68 units covering 7.0 km of a prospective base metal hosting stratigraphy. Excellent access is provided by the all weather South Bay mine road which traverses the center of the property. The Pickle Lake power-line corridor dissects the two most easterly claims.

3.0 PROPERTY SUMMARY AMD CLAIM DISPOSITION

Two of the six claims (114334 and 114348) are contained in an earn- in agreement between a local Red Lake prospector and Cumberland Resources Ltd. The remaining four claims are held 100% by Cumberland Resources Ltd of Thunder Bay, Ontario.

The claims are located in the Gerry Lake area. Map sheet G-1782 and consists of the following holdings (FIGURE 2):

UCHIGREENSTONE

BELT

WABIGOON \ GREENSTONE

BELT

CUMBERLAND RESOURCES LTDPROPERTY LOCATION

BIG FALL PROPERTY

CUMBERLAND RESOURCES LTD. BIG FALLS PROPERTY

CLAIM SKETCHICTRES

FIGURE 2

TABLE I: SCHEDULE OF CLAIMS

CLAIM l NO. OF UNITS RECORDING DATE

1144334 (JV)

1144348(JV)

1144362

1144365

1144373

1209260

TOTAL

16

2

16

16

6

12

68

OCT 13 r 1993

DEC 7, 1993

MARCH 16, 1994

MARCH 16, 1994

MARCH 16, 1994

JUNE 22, 1994

4.0 PREVIOUS WORK

The discovery of the South Bay Mine, a small but high grade Cu-Zn deposit (1.5 million tons grading 2.3% Cu and 14.0% Zn) by Selco in 1969, resulted in extensive base metal exploration which covered an area south from Confederation Lake and southwest to the community of Ear Falls.

To date, all prominent massive sulphide occurrences discovered in the Confederation Lake - Snake Falls area were the direct result of ground follow-up of vintage airborne electromagnetic (AEM) surveys conducted in the 1970's and early 80's. Since these discoveries were made by BP-Selco, the vast majority of base metal exploration has been confined to the immediate vicinity of the occurrences. Little or no effort has been made to extrapolate mineralized time breaks into areas of favourable felsic stratigraphy.

A review of the assessment records revealed that no work has been filed on the Big Falls property. This is likely due to absence of airborne EM targets. The Big Falls claims adjoin the east boundary of Noranda's Joy property, which host four massive sulphides occurrences that are located along two recogonized mineralized tii breaks.

Previous work on Noranda's Joy property is summarised as follows:

1969-1970

Five drill holes were drilled by Caravelle Mines Ltd. to test an airborne EM anomaly. Stringer Cu-Zn mineralization up to 5 m wide were intersected with local high grade narrow massive sulphide sections containing assays as high as Q.13% Cu and 21.6% Zn over 0.25 m. To the knowledge of the author the Caravelle zone has not been subjected to further drilling.

1978-1985

BP-Selco carried out a number of geophysical surveys including Magnetometer, HLEM and UTEM. Diamond drill testing of a number of targets encountered best intersections of S.1% CU over 5.7 m in the Joy Zone and 17.2% Zn over 0.60 m in the South Zone.

1990-1994

Noranda acquired the property in 1990 and in 1993 entered into a joint venture with Major General of Vancouver, B.C. A four hole drill program in 1992 encountered a drill hole intersection which assayed 4.01^ Cu and G.17% Zn over 3.35 m. Drilling was also carried out in 1993 and the winter of 1994. Results of the most recent drill programs are unknown.

5.0 REGIONAL GEOLOGY ABD METALLOGENY

The metavolcanics - metasedimentary rocks of the Confederation Lake assemblage have been divided into three mafic to felsic volcanics cycles (Thurston, 1985). The upper sequence. Cycle III, host the South Bay deposit which is contained within what was commonly termed the Mine Series Rhyolite. These rhyolites, which consist of banded and amygdaloidal flows to thick quartz-crystal pyroclastic successions, extend from the South Bay Mine area south into Bowerman and Belanger Townships where they obtain a maximum stratigraphic thickness of 5 km. The supracrustal rocks are then bifurcated into a northern and southern belt by several large felsic intrusives.

The northern belt, which underlies the Big Falls property, extends west from Belanger Township through Fredart Lake, Gerry Lake, and Trout River to join the Red Lake greenstone belt at Gullrock Lake in Willans Township. These rocks are comprised of mainly pillowed and massive mafic flows with interbedded units of felsic pyroclastic tuff and flows. An oxide facies iron formation is located west of Fredart Lake and can be traced some 30 km west where it hosts the Dixie 18 Cu, Zn occurrence.

The southern belt, which extends west to the Dixie Lake area, is predominantly underlain by felsic and intermediate pyroclastics and subsidiary mafic metavolcanics.

In the Snake Falls area of the Confederation Lake assemblage base metal mineralization is largely hosted by strongly altered felsic to intermediate pyroclastic rocks. The mineralization is associated with a biotite - garnet - anthophyllite chlorite cordierite alteration mineral assemblage.

A single base metal deposit (former producer) and a number of significant massive sulphide prospects occur along specific mineralized time breaks in the Confederation Lake - Snake Falls areas (Figure 3). Some of major occurrences are listed in Table II.

TABLE II: CU- ZN DEPOSITS AND PROSPECTS

HORIZON

South Bay Nine

MIME/PROSPECT

South Bay

BP-Selco

TONNAGE/GRADE

l .6 million tons

2.3% CU, 14.(^ Zn, 3.5 opt Ag

Copper Lode A

Copper Lode A

Copper Lode

Joy

Joy

JOY

Joy

Dixie

SLATE LAKE

Copper Lode A Westminer

Dixie 18 Noranda

Copper Lode E Noranda

Joy Noranda

Dixie 17 Noranda

Dixie 19 Noranda

Moose Creek INCO

Dixie 3 Noranda

SLATE LAKE CUMBERLAND

425,000 tons1.56 % Cu, 0.98 opt Ag

150,000 tons J.4% ZN

276,000 tons Q.66% Cu, 4.8% Zn

DDH-19924.0^ Cu/3.35 m

DDHX.4% Cu, T.34% ZNX9.5m

DDHX.5% Cu, e.33% Zn/ 3m

DDH1.0* Cu, S.2% Zn70.37m

88,000 tonsQ.60% Cu, 14. 8% Zn

DDH S.7% Cu, Zn/ 0.50m

2. 3. 4.PRO

PER

TY

DIS

POSI

TIO

N1.

B

HP-

UT

AH

BREA

KW

ATE

R R

ESO

UR

CES

CUM

BERL

AN

D

RES

OU

RC

ES

GER

HA

RT M

EYER

5.

INCO

6.

MET

ALL

MIN

ING

7.

NO

RAN

DA

8.

PER

RY

EN

GLI

SH

9.

RIO

ALG

OM

10.

WES

TMIN

ER

SIG

NIF

ICA

NT

VM

S O

CC

UR

REN

CES

A.

SOU

TH B

AY

MIN

E B.

W

ASP

C.

TRIA

NG

LE

LAKE

D.

JIG

E.

HO

RSE

SHO

E LA

KE

F.

94-0

1

G.

94-0

2

H.

94-0

3

I. C

OPP

ER L

OD

E E

J.

CO

PPER

LO

DE

A

Q.

DIX

IE

19R.

D

IXIE

17

S.

DIX

IE

18

T.

MO

OSE

CR

EEK

U

. SL

ATE

LA

KE

K.

CARA

VELL

E ZO

NE

L

SOU

TH Z

ON

E

M.

JOY

l

N.

JOY

2

0.

DIX

IE

3

P.

HU

DSO

N B

AY

ZO

NE

CU

MB

ERLA

ND

R

ESO

UR

CE

S LT

D.

CONF

EDER

ATIO

N LA

KE -

SNAK

E FA

LLS

AREA

PRO

PER

TY D

ISPO

SITI

ON

-

1994

SI

GN

IFIC

AN

T VM

S O

CCU

RREN

CES

ME

TRE

S

FIG

UR

E "S

6.0 PROPERTY GEOLOGY AMD MINERALIZATION

During the course of the June and September, 1994 mappping survey, four major rock types were recognized on the Big Falls property: North mafic flow (andesite), Joy pyroclastic tuff. Power Line ash tuff. South mafic flow, and a dioritic intrusive. The Joy pyroclastic flow and the Power-line ash tuff are part of the same stratigraphic succession that have been dilated by a large diorite sill (Figure 4). From west to east in the direction of younging these stratigraphic units are as follows:

The North Mafic Flow(NMF) is exposed in two closely located outcrops immediately south of Trout Lake River. Both exposures were moderate to well foliated, dark green to black in colour with local speckled and patchy ID-15% feldspar porphyroblast. Numerous pink f elsite/granitic veinlets are randomly distributed through-out the outcrop exposures. Whole-rock analysis (samples 12954, 12955) averaged 49.(^ SiO2 , Q.61% TiO2 and S.42% Na2O.

The Joy Ash Flow tuff(JAFT), which hosts the Joy, Caravelle and the South base metal occurrences, is knowingly exposed in one lone location on line 5900-E. This unit is medium grey in colour, is aphyric and has a medium grained sugary texture. Crude banding is evident with a 740 bearing. The weathered surfaces has a rusty coloration due to the presence of pervasive biotite and muscovite. The whole-rock analysis indicates intermediate composition with a Si02 content of 68.10%, TiO2 content equal to Q.69%, and Na2o equal to S.56%. A unit of simi liar chemical composition exist as a xenolith within the southern felsic intrusive near the southeast corner of the property. The latter exposures differ in appearance from the JAFT in its alteration style. This alteration manifest itself as pervasive biotite, locally observed coarse-grained anthophyllite, and rare garnet porphoblast.

The Power Line Ash Flow Tuff(PLAFT) is exposed east from the South Bay mine road to the eastern boundary of claim 1144365 where the unit obtains a thickness of at least 400 meters.

The unaltered and altered equivalents of the PLAFT are substantially different in appearance. The unaltered PLAFT is finely banded, medium grained , light to a dark grey in colour and contains up to 5% sub 2mm size pink garnet. The altered variety, which is exposed in a number of outcrops over an open-ended strike length of 1.5 kms, is comprised of massive to coarsely bedded, coarse grained anthophyllite, biotite, cordierite, garnet, +/- chlorite. Garnets occur as pervasive sub 2cm porphyrobasts and heavily concentrated (5(^) sub 20 cm beds and palm-size aggregates or clusters. Coarse grained anthophyllite exists as heavily- concentrated tabular to lath-like and radial (half bow-tie) crystals generally in an off-white to grey cordierite-rich matrix. Garnet and anthophyllite mineral assemblage results in an extremely rough and knobby appearance on outcrop surfaces.

CUMBERLAND R

ESOU

RCES

LTD, (lOOX.)

H.I

I44M

5

[CUM

BERL

AND

- EN

GLIS

H/OP

TION

KRL

1144

334

NDRA

NDA

/ MAJOR

GENERAL

JV

HO

RtT

t IN

TKU

StVC

t <

KB

SO

LC F

LOW

GM

MT

t

SOUT

H H

tfK

FLO

W

JOY

ASH

PLOW

rur

rPO

WER LDC ASH PLOW TUFF

NORT

H K*nC PLOW

JOY

ZONE

4,

0 X

Cu

X

VE

LLE

ZO

NE

4.4X

ZnX1

4n

CUM

BERL

AN

D

RES

OU

RC

ES

LTD.

B

IG

FALL

S PR

OPE

RTY

GEO

LOG

Y

A

ALT

ERA

TIO

N20

0 40

0 60

0 80

0 10

00

Average SIO2, TIO2, and MA2O content for the altered PLAFT is Tl.38%, D.76% and G.62%, respectively.

The South Mafic flow (SMF) overlies the PLaft and is mainly exposed along the southern portion of claims 114365 and 1209260. This unit ranges from dark green, fine grained and massive to a more dioritic appearance from west to east. The more easterly exposures display a typical salt and pepper dioritic texture composed of mainly hornblende and feldspar. SiO2 , TiO2 and Na2O average 52.1^, X.02% and S.22%, respectively.

Intrusive rocks occur in the form of a diorite sill which extend along the entire 7.0 km strike length of the property. This sill appears to be rather consistent in thickness (approx 300m) and separated Northern Mafic Flow from the felsic ash flow tuffs to the south. Text ur ally the intrusive is typically dioritic consisting of a characteristic salt and pepper -like appearance and is composed of 50% feldspar and 50% hornblende. The unit is generally massive with minor locally observed foliation. Chemically the sill averages 49. 7(^ SiO2 , 1.543; TiO2 , and a.00% NaO2 .

With the exception of minor pyrite no other known mineralization exist on the Big Falls property. Noranda's Joy property to the immediate west hosts four stringer and massive base metal occurrences. These metal rich occurrences appear to be associated with two separate mineralized time breaks. The Joy conductive trend has been delineated geophysically over a distance of approximately 2 km. The Joy Occurrence, which is located at the western end of the delineated mineralizing trend, is a Cu-rich stringer and massive sulphide zone with a reported best intersection of 4.01^ Cu over 3.35 m. The Caravel le trend is located just 500 m south of the Joy trend and contains two massive and associated stringer sulphide occurrences with best intersection of 21.6% Zn/0.25 m and 4.44% Zn/ 1.1 m (Caravelle zone) and 17. 2% Zn/0.60 m (South zone). The known limits of both the Joy and the Caravelle conductive trends extend to the eastern boundary of Noranda's Joy property and hence to the western boundary of Cumberland's Big Falls property.

7. STRUCTURE:

A weak to moderate mineral f oliaton( hornblende, minor biotite and chlorite) is present in most of the mafic rocks. The felsic units (JAFT, PLAFT) display a crude to a moderately well-developed banding and/or bedding. Both foliation and banding are consistentely orientated at 70-800 with a near vertical dip. Personal communications with present day workers in the area indicated that known sulphide lenses dip 650 to the east and plunge at a shallow angle to the northeast.

Inferred faulting south of Trout Lake River and near the eastern limits of the property is based solely on the sudden termination of rather thick stratigraphic units.

8.0 WHOLE-ROCK GEOCHEMISTRY : ALTERATION

The felsic volcanics, which host the former producing South Bay Cu, Zn, Ag mine, extend west to the Snake Falls area where they play host to a number of sub-economic massive sulphide occurrences. These massive sulphide occurrences typically display stratabound and cross-cutting hydrothermal footwall alteration which is consistent with all Archean VMS deposits.

During the course of the Big Falls mapping survey, a total of 34 rock samples were collected for the purpose of whole-rock analysis. These samples were analyzed for various major, minor and trace elements by Chemex Labs of Vancouver, B.C. Analytical results are appended as Appendix 2.

Selected elements and combinations of elements were plotted on a digitized base map. The most effective and accepted way to determine and interpret hydrothermal alteration processes that are commonly associated with volcanogenic massive sulphide deposits is through the identification of depletion or enrichment trends in total Fe and the alkalis. Alteration trends of this nature are known to occur around or, more usually, stratigraphically underlying proximal massive sulphide ore bodies. Trends of MgO, total Fe and less typically K2O enrichment and depletion of Na2O and CaO in felsic volcanic rocks are recognized to form integral parts of the overall ore-forming process. A quantitative evaluation of the alteration processes is best provided by generating alteration indices such as Hoshimoto, Chlorite, Sericite and Spits (Table III). Only the Hoshimoto index will be briefly discussed in this report.

The whole-rock geochemistry and the above mentioned alteration scores define a rather extensive area of massive sulphide-forming type alteration which extend east from the South Bay Mine road for a distance of 1.5 km. This alteration zone, which defines itself mineralogically as a anthophyllite-cordierite-biotite-garnet +/- chlorite mineral assemblage, is 300 meters wide with a 1.5 km open strike length.

8.1 Ha2O: PLANl 6O1-B

A plot of Na2O values shows the alteration zone to be defined by the 1.5% Na2O contour. Of the 11 whole-rock samples which displayed varing degrees of alteration three of the samples contained <0.5% Na2O. Plan 601-B display a typically zoned alteration system with an open strike length of 1.5 km.

8.2 HOSHIMOTO INDEX: PLANf 601-C

The Hoshimoto Index(HI) is derived from the ratio of those oxides (MgO and K2O) expected to be enriched due to alteration versus the total alkali content. As MgO and K2O content of a volcanic rock increases with respect to the total alkali content, the Hoshimoto

88

s: S

S

S

S S 8 800

888 S 8 8

•Jo

88 900

s s 8

88?oboo

8

88? •ve 323 8 88 8*rim

ui

8 32SSS

558

3UI

8III UI UI III 111 111 III

8

8

33885 8 8 S

889SZ

88

ui w

8

f

ii

Index approaches 100. Average Hoshimoto values for subalkaline mafic to felsic volcanics lie between 35 and 50. Highly altered volcanics rocks will have a value in excess of 80.

All samples within the alteration zone have values greater than 70 with the exception of sample 12918 which has an abnormally high CaO value(10.801). Values greater than 80 occur throughout the alteration zone.

8.3 Cu: PLAN! 601-D

Cu values are extremely low ranging from l to 146 ppm. The lone anomalous value of 146 ppm was obtained from the Joy ash tuff outcrop and can probably be attributed to the processes that formed the numerous copper-rich massive sulphide occurrences in the general area.

8.4 Zn: PLAN 601-E

Samples from the newly discovered alteration zone generally contain Zn values greater than 50 ppm. A weakly anomalous area is defined over a continous strike length of 1.2 km with highs of 212 and 136 ppm Zn.

8.5 COMPARISON OF ALTERATION PATTERNS TO OTHER VMS DEPOSITS.Table IV demonstrates the comparison between alteration indices for the rhyolitic tuffs of the Big Falls property and those of footwall rocks of well known VMS deposits.

TABLE IV COMPARISON OF ALTERATION INDICES

LOCATION HOSHIMOTO CHLORITE SERICITE SPITS

BIGFALLS*(UNALTERED) ? ? ? ?(ALTERED) 93 95 85 49STURGEON LAKE(UNALTERED) 46 ? 52 4(ALTERED) 75 ? 90 42WINSTON LAKE(UNALTERED) 16 ? 3 2(ALTERED) 82 ? 63 10LYNN LAKE(UNALTERED) 14 ? 15 2(ALTERED) 75 ? 41 14HORNE MINE(UNALTERED) 26 ? 17 3(ALTERED) 99 ? 99 22

8.6 TRACE ELEMENT GEOCHEMISTRYArchean felsic metavolcanic rocks which host most of major massive sulphide deposits have a distinct geochemical signature which accounts for their association with massive base-metal mineralization. Table V compares trace element geochemistry of typical VMS hosting Fill type rhyolite and those of the Big Falls property:

COMPARISON C

Zr/Y ratio

Fill RHY 2-6

IF TRACE ELEMENT GEOCHEMISTRY

Sr Se Y Zr

7-88 2-13 50-200 200-700

Big Falls 3.5 18 ? 133 459 AV. 9 samples

8.0 DISCUSSIONThe 1994 program has resulted in the discovery of a new and extensive proximal-type hydrothermal alteration zone on Cumberland's Big Falls property. Hydrothermal ore-forming processes have altered the felsic rocks, forming a well defined zone of Na2O depletion and Fe2O3 and MgO enrichment. At the prevailing amphibolite metamorphism this alteration has formed a mineral assemblage consisting of anthophyllite-cordierite, garnet, biotite +/_ chlorite.

Comparing alteration geochemistry (alteration indices) and trace element geochemistry from various archean VMS deposits has significantly enhanced the possibility of the Big Falls property as a probable host to a VMS deposit.

9.0 PROPOSED EXPLORATION PROGRAM AND BUDGET

To continue with a systematic and intergrated base metal exploration program a DEEPEN geophysical survey is recommended and should cover two defined areas of the favourable VMS hosting stratigraphy (Figure 5). Area l is located immediately east and adjacent to the known Joy and Caravelle massive sulphide zones and subsequent mineralized time breaks. Area 2 would cover the entire strike length of the recently discovered alteration zone. The survey would be carried out at 200m line interval for a total of 16 km. Estimated cost is 316,000.

Respectively submitted,

Patrick7 Lewis

xRESOURCES LTD. (1007.)

NDRANDA 7 MAJOR GENERAL?

LEGEND

NEW

JOY ZDC44 Z Cu X 3L9n

rassoLC FUIW

l————laum imc FLOWJOT ASH FLOW TUFF

FfMOt UC ASH FUM TUFF

MRTH NmC FUIW

SOUTH

LMC JOT

CUMBERLAND RESOURCES LTD. BIG FALLS PROPERTY

PROPOSED DEEPEM SURVEYFIGURE

TABLE VI

PROPOSED BUDGET - 1994

PROJECT: BIG FALLS PROJECT PN: 601

GEOLOGY

GEOPHYSICS

DEEPEM (16KM X S700)

6EOCHEMSTRY

DRUJNG

Salaries

Travel Expenses

Contract Payments

Field Expenses

Analyses

Salaries

Travel Expenses

Contract Payments

Field Expenses

Salaries

Travel Expenses

Contract Payments

FieUExpenses

Analyses

Salaries

Travel Expenses

Contract Payments

FieUExpenses

Analyses

S1.50D

S2.500

S11.2DO

seoo l si6.ooo|

50 KM X 9350 Line Cutting

Propotty A/QutsHion

Opfcn Payments

REPORT WFOTING - DRAFTHG

TOTAL HRECT

Adnmistrabon

TOTAL EXPENDITURE

PARTNERS SHARE

CUMBERLAND SHARE BFALLS.XLS

10*

l ?16.000|

*1.600

l S17.eOD|

MACDOUQAL, C. (1992)

REFEREHCES

HORAHDA EZPLORATIOH: REPORT OH DIANOHO DRILLING - JOT PROPERTY: ASSESSMENT LIBRARY - RED LAKE

APPENDIX l



I, M.P. Lewis, hereby certify that:

1. I am a practicing Geologist and sole proprietor of M.P. (Pat) Lewis Geological Services, with an office at 269 Chercover Drive, Thunder Bay, Ontario.

2. I am a graduate of Memorial University of Newfoundland (1976) with a Bachelor of Science Degree - Major in Geology.

3. I have practiced my profession as an Exploration Geologist continuously for the past 17 years.

4. I have an indirect interest in the Properties described in this report.

Signature:M. P.

Date:

APPENDIX 2

CERTIFICATE OF ANALYSIS

Che

mex

Lab

s Lt

d.An

alytic

al Ch

emist

s * Q

eoch

emlst

s * R

egist

ered

Ass

ayer

s51

75Ti

mbe

rlea

Blvd

., M

issisa

auga

, O

ntar

io, C

anad

a L4

W 2

S3

PHO

NE: 9

05-6

24-2

806

To:

LEW

IS, M

.P. G

EOLO

GIC

AL S

ERVI

CES

269

CHER

COVE

R DR

. TH

UNDE

R BA

Y, O

N P7

Q1A

2

Proj

ect:

Com

men

ts:

ATTN

: PAT

LEW

IS

lPa

g* N

uh.w

er

: 1 To

tal P

ages

: 1

Certi

ficat

e Da

te: 2

8-JU

N-94

In

voice

No.

: 1

9418

093

P.O.

Num

ber

: Ac

coun

t : L

VP

SAMP

LE

1290

1 12

902

1290

3 12

904

1290

5

1290

6 12

907

1290

8 12

909

1291

0

1291

1

PR1

CO 205

205

205

205

205

205

205

205

205

205

205SP DE 22

6 22

6 22

6 22

6 22

6

226

226

226

226

226

226

CERT

IFIC

ATE

OF A

NALY

SIS

A941

8093

A120

3 Ca

O Ct

203

Pe20

3 K2

0 Mg

O Mn

O Nt

20

P205

Si

02

Ti02

LO

I TO

TAL

Ba

Kb

St

Mb

Zr

Y \

\ \

\ \

\ \

\ \

\ \

\ \

ppi

ppi

ppm

ppn

ppm

ppa

11.2

6 2.

49 <

0.0

1 6.

31

0.46

2.

96

0.14

3.

56

0.14

66

.10

0.69

0.

99

99.1

1 IC

O 5

100

40

550

90

14.4

3 9.

44 <

0.0

1 13

.96

0.38

5.

38

0.18

2.

81

0.12

49

.00

1.44

0.

58

97.7

3 11

0 <

5 23

0 10

13

0 40

14

.71

9.59

< 0

.01

13.0

8 0.

50

.16

0.18

2.

97

0.14

48

.40

1.27

0.

88

97.8

9 12

0 S

260

< 10

11

0 30

14

.63

9.89

< 0

.01

13.0

1 0.

35

.20

0.15

2.

81

0.14

49

.30

1.27

0.

68

96.4

4 11

0 <

5 25

0 <

10

100

20

9.59

0.

33 <

0.0

1 8.

28

0.60

.6

9 0.

07

0.31

0.

17

72.4

4 0.

65

2.64

99

.78

110

10

< 10

20

40

0 90

10.1

4 O.

S8 <

0.0

1 10

.72

0.32

.7

2 0.

06

0.81

0.

15

70.0

5 0.

66

1.05

99

.47

90

< S

20

30

490

140

14.3

7 7.

78 <

0.0

1 13

.06

0.55

.7

0 0.

18

3.20

0.

13

51.7

1 1.

75

0.52

97

.96

160

< 5

250

10

110

40

10.9

0 0.

18 <

0.0

1 8.

49

1.37

.5

6 0.

04

0.25

0.

14

72.4

1 0.

69

1.05

100

.10

170

20

< 10

20

40

0 11

0 10

.44

0.49

t 0

.01

10.9

4 0.

11

.06

0.08

1.

11

0.09

70

.69

0.86

0.

49

99.3

7 10

<

5 20

30

50

0 16

0 16

.49

10.2

2 <

0.0

1 10

.48

0.41

7.

41

0.16

2.

92

0.07

48

.40

0.81

1.

14

98.5

2 60

<

S 2

50

< 10

20

10

13.6

6 9.

81 <

0.0

1 12

.50

0.30

6.

19

0.16

2.

62

0.16

51

.13

1.10

0.

63

98.2

7 30

<

5 16

0 <

10

130

30

CERT

IFIC

ATIO

N:^

Che

mex

Lab

s Lt

d,An

alytic

al Ch

emist

s' Qe

oche

mlsl*

* Re

gister

ed A

ssay

ers

5175

Tim

berle

a Bl

vd.,

Miss

issau

ga,

Ont

ario

, Can

ada

L4W

2S3

PH

ONE

: 905

-624

-280

6

o:

LEW

IS, M

.P. G

EOLO

GIC

AL S

ERVI

CES

269

CHER

COVE

R OR

. TH

UNDE

R BA

Y, O

N P7

G1A

2Pr

ojec

t:Co

mm

ents

: AT

TN: P

AT L

EWIS

Page

i oe

r :1

Tota

l Pag

es

: 1 Ce

rtific

ate

Date

: 03-

JUL-

94

Invo

ice N

o.

: 194

1861

2 P.

O. N

umbe

r :

Acco

unt

: LVP

CERT

IFIC

ATE

OF A

NALY

SIS

A941

851 2

SAMP

LE

1291

112

912

1291

312

914

1291

5

1291

612

917

1291

8

PREP

CODE

205

205

205

205

205

205

205

205

226

226

226

226

226

226

226

226

A120

3 Ca

O Cr

203

Pe20

3 K2

0 Mg

O Mn

O Na

20

P205

Si

02

T102

LO

I TO

TAL

B*

Rb

Sr

Nb

Zr

YX

X X

X X

X X

X X

X X

X X

ppm

ppm

ppn

ppn

ppn

ppa

11.4

1 0.

34

0.02

9.

90

0.67

4.

06

0.08

0.

59

0.21

70

.40

0.70

1.

44

99.8

3 17

0 5

10

20

460

130

12.6

3 0.

27 <

0.0

1 12

.31

0.95

5.

49

0.07

0.

55

0.17

64

.28

0.77

1.

43

98.9

3 30

0 S

10

30

500

180

13.9

5 9.

56 <

0.0

1 13

.48

0.39

5.

84

0.19

3.

18

0.31

48

.98

1.72

0.

65

98.2

6 13

0 <

5 29

0 <

10

140

3022

.67

1.73

0.

02

4.48

4.

74

2.23

0.

07

2.98

0.

23

59.0

0 0.

63

2.34

101

.10

1170

12

0 35

0 <

10

ISO

1015

.93

8.94

< 0

.01

11.6

3 0.

54

5.69

0.

17

3.62

0.

2S

50.2

9 1.

42

0.63

99

.12

140

< 5

310

* 10

10

0 30

10.1

6 0.

66

0.01

13

.77

0.72

3.

94

0.07

1.

38

0.18

67

.59

0.78

0.

19

99.4

5 19

0 <

S 20

20

48

0 11

010

.64

0.64

0.

04

3.38

0.

07

7.17

0.

01

1.37

0.

14

72.1

0 0.

83

3.65

100

.05

20

< 5

30

30

460

130

10.8

0 0.

88

0.03

8.

84

0.34

5.

00

0.05

1.

49

0.15

70

.00

0.69

1.

71

99.8

7 60

<

5 40

30

44

0 15

0

CERT

IFIC

ATIO

N:

Che

mex

Lab

s Lt

d,An

alytic

*! Ch

emM

t * Q

*och

*mliu

" H*g

l*t*r*

d As

wyer

*51

75 T

imbe

rtea

Blvd

.. M

lMlsu

uga.

On

tario

, Can

ada

L4W

2S3

PH

ONE:

905

-624

-280

6

To:

LEW

IS, M

.P. Q

EOLO

QIC

AL S

ERVI

CES

269

CHER

COVE

R OR

. TH

UNDE

R BA

Y, O

N P7

Q1A

2

Proj

ect:

Com

men

ts:

ATTN

: PA

T LE

WIS

Page

Nui.

,r :1

Tota

l Pag

es

: 1 Ce

rtific

ate

Date:

17-

OCT-

94

Invo

ice N

o. : 1

9427

976

P.O.

Num

ber

: Ac

coun

t : L

VP

CERT

IFIC

ATE

OF A

NALY

SIS

A942

7978

SAMP

LE

1295

4L2

955

1295

612

957

PREP

CO

DE

205

205

205

205

226

226

226

226

A120

3 \

CaO

\Cr2

03 W

e203

\

K20 \

MgO

\ Mn

O \

Na20

\ P

205 \

8102

\ T

i02

\ LO

I X

TOTA

L Au

ppb

Cu

Zn

Ag

ppn

XRF

XRF

XRF

XRF

XRF

XRF

XRF

XRF

XRF

XRF

XRF

XRF

* FA

+AA

ppa

ppn

Aqua

R

18.3

2 11

.65

0.06

9.

33

0.59

(.

15

0.14

3.

02

0.03

48

.87

0.56

0.

72

99.4

4 <

5 3

16

< 0.

218

.6*

11.6

2 0.

03

8.85

1.

07

4.39

0.

16

3.83

0.

04

49.0

8 0.

67

1.43

99

.83

< S

32

60

< 0.

211

.03

1.45

0.

02

6.88

1.

70

3.3C

0.

06

2.61

0.

08

(9.1

6 0.

49

1.50

98

.34

< 5

14

151

< 0.

29.

74

0.15

0.

03

7.75

0.

12

4.70

< 0

.01

0.20

0.

10

73.2

7 0.

65

2.26

98

.97

< 5

43

94

< 0.

2

CER

TIFI

CAT

IO

Che

mex

Lab

s Lt

d.An

alytic

al Ch

emte

tt* Q

wxhw

nMt "

R*g

M*ra

d As

tayv

ra51

75 T

imbw

tea

Blvd

., M

iatiu

auga

, O

ntar

io, C

anad

a L4

W2S

3 PH

ONE

: 005

-624

-280

6

To:

LEW

IS, M

.P. Q

EOLO

QIC

AL

SER

VIC

ES

269

CH

ERC

OVE

R O

R.

THU

ND

ER B

AY, O

N

P7Q

1A2

Pro

jtct:

Com

man

ta:

BIG

FAL

LS

ATTN

: PA

T LE

WIS

Paga

Nw.n

iwr

:1 To

filP

aoM

:1

Certi

ficat

e Da

te: 2

5OC

T-94

In

volo

tNo.

: 1

0428

511

P.O.

Num

ber

: Ac

coun

t :L

VP

SAMP

LE

1295

812

959

129(

012

9*1

129(

2

129C

312

9(4

129(

512

9((

129(

7

129(

812

9(9

1297

012

971

PR CO 20S

20!

205

20!

205

205

20!

205

20!

205

205

20!

20!

205EP DE 22

622

122

C22

422

6

22C

221

22(

224

226

226

224

224

226

A120

3 \

CaO

XCx2

03 *

F*20

3 \

K20

\ Ng

O *

MnO

* Na

2XR

F XR

F XR

F XR

F XR

F XR

F XR

F

14.4

9 10

.28

O.OS

9.

18

0.40

.3

5 0.

13

313

.84

9.89

0.

01

13.7

0 0.

41

.(4

0.19

3

10.3

4 2.

18

0.03

9.

81

0.88

.9

4 0.

05

29.

15

0.97

0.

02

11.8

1 2.

28

.51

0.13

1

14.5

4 12

.54

0.02

11

.41

0.41

.5

8 O

.K

2

14.8

3 7.

78

0.01

12

.06

0.84

.5

9 0.

15

314

.43

10.7

8 0.

03

12.1

4 0.

53

.55

0.17

3

14.3

5 9.

29

0.02

11

.94

0.58

.(

1 0.

14

315

.78

8.77

0.

01

12.5

3 0.

50

.22

O.K

4

13.4

5 10

.82

0.01

13

.68

0.46

.(

0 O

.K

2

10.3

* 0.

70

0.01

12

.85

1.80

.4

5 O

.K

112

.01

10.9

7 0.

12

10.6

0 0.

40

.96

O.K

2

15.1

9 5.

45

0.05

7.

05

0.18

.2

5 0.

10

311

.92

0.26

0.

01

1.47

8.

04

0.57

0.

02

0

CERT

IFIC

ATE

OF A

NALY

SIS

A942

851 1

0 \

P205

* 8

102

It T1

02 \

LO

I *

TOTA

L An

ppb

Cu

Zn

Ag

ppi

XRF

XRF

XRF

XRF

XRF

\ FA

+AA

ppi

ppi

Aqoa

R

.50

0.12

53

.39

0.81

0.

90

99.6

1 10

33

20

*

0..0

1 0.

19

50.2

3 1.

36

0.96

99

.43

< 18

56

<

0..0

9 O

.K

(8.9

* 0.

92

0.66

99

.04

< 40

71

x

0..6

0 0.

04

(6.8

8 0.

50

1.4*

99

.35

< <

1 30

0 *

0..3

3 0.

11

51.5

2 1.

13

0.97

100

.72

< 95

33

<

0.

.73

0.12

51

.76

1.41

0.

66

98.9

6 <

26

71

* 0.

.05

0.15

49

.77

1.19

0.

70

99.4

9 <

80

31

< 0.

.84

0.15

50

.65

1.20

0.

89

96.8

6 <

32

45

4 0.

.02

0.15

51

.45

1.43

0.

56

99.5

6 <

49

66

* 0.

.26

0.14

52

.32

1.52

0.

75

99.1

7 <

18

79

< 0.

.20

0.08

68

.06

0.78

0.

16

99.6

3 <

< 1

132

< 0.

.81

0.11

50

.36

0.96

1.

16

98.6

2 <

9 31

*

0..3

9 0.

14

5C.3

3 0.

61

4.52

99

.29

* 43

88

<

0.2

.31

0.03

73

.42

0.29

1.

62

97.9

6 <

< 1

43

* 0.

2

CER

TIFI

CA

TIO

N:

OCT.-25'95(0) 13 = 12 MINING/GEOLOGY-KEN

j J^X OCT.-2rttnED) 12:57 HIIIW-IECOUOMU,

*r

TEL:8074682823

TEL:107 727 3553

P. 002

P. 002

Report of Work Conducted After Recording Claim

OnUfta•ir at

i

W* or print aid i to M Mrthg M tnd H^ttUloM Mr r

w or Mi tom mm M

M eWrat ta worn b

52K14NE002a 2.16247 GERRY LAKE llfenBlir~~ "

900

t *- fcc* Ml M*i In Mi MM

LJg^/f \tf MKtCM

\GtT 7/9S

DP

Ministry ofNorthern Developmentand Mine*

Ontario


MlfilnQ Act

Tronttction Numbor

IAJ153.0.

i cclsctsd on ttito lonn is obtained under Hw eultiurlty of Ine Mnlnoj Act. Thle infuinielion wil bo ueod for corroopondenco. 4•^u - — a.— — *; —— mhjij- ,tii *-— ^C0^kj^^M4 tsi M*A DMMMMMSA! ftAttM^rf^^v ftCfl^^M* l ^MM^B ft^b^MAM* j^ U*M4f*Aa** n^*^MbMM**A*rfIras OOMCDOn snoun 00 OHOCWQ n vw rroMncw Manager, Mrang Laraa, Naraaoy OT Nonnarn uovwopmoni Sudbury. Ontorto. P3E 6A5. totaphom (705) 670-7264.

4CA ^^Amm Ot*M^4, iav veoar awoi,

Instructions: - Please type or print and submit in duplicate.- Refer to the Mining Act and Regulations for requirements of filing assessment work or consult the Mining

Recorder.-A:- Technical reports and maps must accompany this form in duplicate.- A sketch, showing the claims the work is assigned to, must accompany this form.

mot WJ amt Mminy nn tuiu rKHjuwuun* MN rOTjunaiiiauKi m IIMIIJJ inrouumiioiu nw* m vwiauH um

ecorder. t^, separate copy of this form must be completed for each Work GroupjB e l ft O" X

echnteaJ reports and maps must accompany this form in duplicate. ** ^ 4c

Telephone No.

"* ITnmal

P7S 3P9MWngOwWon

L/HtE.orQPlMiNo.

From: ocwit 3 ,/99V &UTT

lv.

Work Perfonned (Check One Work Group Only)WorkGroup Type

Geotechnical Survey Li/vfeu Try/vfi-PhysMsal Work, Inctudbig OriHing

RECEIV̂Other Authorized OCT 3 1 199 f; '-T 1 1 la*- s^^ v- * l*?*/*^

Assays MINING LANDS

Reserve

Total Assessment Work Claimed on the Attached Statement of Costs3-7

Note: The Minister may reject for assessment work credit all or part of the assessment work submitted H the recorded holder cannot verify expenditures claimed in the statement of costs within 30 days of a request for verification.

Persons and Survey Company Who Perfonned the Work (Give Name and Address of Author of Report)

(attach a schedule If necessary)

Certlflc atlon of Beneficial Interest * See Note No. 1 on reverse sidel oertny that at the ome the work waa performed, the dairna covered in into work report ware recorded In the currant holder's name or held under a l by the current recorded holder. as/frs

Hotter or Agent (SHimttura)

Cei lineation of Work Reportl certify that l ham a personal fcnowtedge of the facts eat forth in this Work report, having performed the work or Ha completion and annexed report to true.

ourinQ wid/or

of Poroon CejwyiriQ P ~76

TetaponsNo.

For Office Us* Only

&CT

ToM Value Or. Recorded Doto Recorded

//*Deemed Appnwel Data

MMng Recorder

Dale Approved

Notice ter AnhdmenC Sem

OCTAM PM

j:. 16*47

fi

irOo

si

'K oc

MINING l

JE' 1•31

ANSJ

^Qi

J 0.-- v. .

5s.

^

|

^ >

LP

1

es.^ Js0

s 1

^N.

0*

sb

5 O

s**iff ffi*

r®otal Value

l •Sf<

^lCredits you are claiming in this report may be cut back. In order to minimize the adverse effects. , which claims you wish to priorize the deletion of credits. Please mark (^) one of the following: -. - l L \̂

^1. D Credits are to be cut back starting with the daim listed last, working backwards.

2. D Credits are to be cut back equally over all daims contained in this report of work.

3. D Credits are to be cut back as priorized on the attached appendix.

In the event that you have not specified your choice of priority, option one wM be implemented.

deletions, please indicate from

Hotel: Examples of beneficial Interest are unrecorded transfers, option agreements, memorandum of agreements, etc.. wHh respect to the mining claims.

Note 2: rf work has been performed on patented or leased land, ptease complete the foOowing:

l certify that the recorded holder had a beneficial interest in the patented or leased land at the time the work was performed.

Dale

ocr

MmistryofNorthern Devetopment

OntarioMMsteredu Dovotoppomont du Nord aides mines

Statement of Costs for Assessment Credit

(ztat des coOts aux fins du credit devaluation

Mining Act/Lol sur les mines

Transaction NoJN* de transaction

Personal information coltocted on this twtn is obtained under the authority of the Mining Act. This information wMI be used lo maintain a record and ongoing status of the mining daim(s). Questions about this collection should be directed to the Provincial Manager. Minings Lands. Ministry of Northern Development and Mines. 4th ROOT. 159 Cedar Street. Sudbury. Ontario P3E 6A5. totophono (70S) 670-7264.

624?s dans to presente formutoLes renseignements personnels contenus dans to presente fonnuto sort

recueims en vertu de b Loi sur tos mines et serviront a tenir a jour un registre des concessions minieres. Adresser toute quesiton sur to cottoce de ces renseignements au chef provincial des terrains miniars. ministere du Devetoppemert du Nord et des Mines. 159. rue Cedar. 4* etaga. Sudbury (Ontario) P3E 6A5. telephone (705) 670-7264.

1. Direct Costs/CoOts directs

Type

Wagaa

Contractor's and Consultant's

Drafts do1 OflvVpfVfMMII'etderexpert-

Supples Used

Location de

Doscnption

Labour Main-d'oeuvre

Field Supervision Supervision sur te terrain

Type

Lflflf,Type

misc.

TUP*

Amount Montant

1 66?

Totals Total global

df l fs t'

tf3'S7^3/330

Total Direct Costs Total des coats direct*

2. Indirect Costs/CoOts indirects* * Note: When claiming Rehabilitation work Infract costs are not

allowable as assessment work. Pour to rembouraement des travaux de rehabilitation, tos coOts indirects ne son! pas admissMes en tant qua travaux d'evaluation.

Type

Transportation Transport

RECE&OCT3

Description

-h

Amount Totato Total global

Alo

Sub Total of Indirect Costs Total partial des coOts indirects '

sbto (not greater than 20* of Direct Coats)t (n'sxcodsnt pas 20 9ft des cuflta dJrecta)

Total Vi(Total of Direct and

Note: The recorded holder win be required lo verify expenditures claimed in this statement of costs within 30 days of a request for verification. If verification is not made, the Minister may reject for assessment work

' aH or part of the assessment work submitted.

Note:LeMula egjstrei Denude venter les daple present etat des coots dans tes 30 jours suivant une demande a cet eftet. Si la verification n'est pas effectuee. le ministre peut rejeter tout ou une partie des travaux d'evaluation present**.

Hang Discounts

1. Wort filed wiminWwo years of completJon is daimed at 1(XWb of the above Total Value of Assessment Credit.

Rsfnlsss pour dJspot

1. Les travaux deposes dans tos deux arts suivant tour achevement sort rembouTsesalOOttdetovaleurlotatesusntertiora^

2. Work filed three, four or five years after completion is claimed at 50* of the above Total Value of Assessment Credit. See calculations below:

Tow Value of Assessment Credit

X 0.50

Certification Verifying Statement of Costs

l hereby certify:that the amounts shown are as accurate as possible and these costs were incurred white conducting assessment work on the lands shown on the accompanying Report of Work form.

that asrded Hoktor. Agent. Position in Company)

to make this certification

2. Les travaux deposes trois. quatreoucinqansapres tour achevement sort rembourses a 50 y deja jtajnuf inlala du rrflfBl d'evaluationaim.a*jmi.jm^A l/jtl.fc^j H^^bJL^M 4W9^MjMA*^*L^^ 3 nsusmennonne. votrnes ua"j|{iajQjge3laa,yay. ̂ ^

P- ̂ ' '^ 4 - ' E'ratMRon Male demand*!Vatour totato du credit i

AMAttestation de v

J'atteste par la presente :que tes montants indiques sort te plus exact possible et que ces depenses ont ete engagees pour effectuer tes travaux d'evaluation sur tes terrains indiques dans la formute de rapport de travail ct-joint.

l am authorized Et qu'a litre deropfAMntovii. posto occup*) (tans te

a faire cette attestation.

je suis autorise

Signature

Nota : Dans cette formuto. kxsqu'il designe des personnes. to masculfh est au sens neutre.

DENNIS SMITH T2T 3393 p.etMMetryofNorthern Developmentand Mines

mtario


Mining Act

TfeWMCtsOA

poo

waonalirilOrmatmcoaMted on thto tom) ia obtained under to* ooUectton should be directed lo the Provincial Manager. Mining Land.. MMtouy oi Northern Development md Mine*. Fourth Floor. ISO Cedar Straatjdbury, Ontario. P3E GAS. telephone (TOO) S70-78S4. jy

2e) l fi 9 4wtructJons: - Please type or print and submit in duplicate. * w *v "X

- Refer to the Mining Act and Regulations for requirements of fiing assessment work or consult the Mining Recorder.

- A separate copy of this form must be completed for each Work Group.- Technical reports and maps must accompany this form in duplicate.- A sketch, showing the claims the work is assigned to, must accompany this form.

VMmef SP LMdL . O/vT.TownohifiMrea '

ffeu

Client No./gy^/reiephone MoT

~D3ST weft±6*6-

U or o Plan No.

From: To: '3,/ffV

Voffc Performed (Check One Work Group Only)WorkGroup Typo

Geotechnical Survey **- -*- -. lifnji,rnyeicei wonc. IndurMne OrMng

ReheMtaiion

Other Authorized Work

Assay* UCT 31 1995

Assignment from Reserve MINING LANDS

? *7/Total Assessment Work Claimed on the Attached Statement ofNote: The Minister may reject for assessment work credit aH or part of the assessment work submitted if the recorded

holder cannot verify expendftures claimed in the statement of costs within 30 days of a request for verification.

Persona and Survey Company Who Performed the Work (Give Name and Address of Author of Report)Name Address

Y#r m. E. MM ,

P7G-

/JT-

(anaoli a schedule H necessary)

Certification of Beneficial Interest * See Note No. 1 on reverse eMol certify thai at the time the work wet performed, the daunt cowered m Wa work fepOrtwerereooidadinôurrenlhotoVsnameorheklunoâbenelKMlnttraet byMcunwineoordedhaWer_____ _______________ l

Certification of Wortc Reportl certify that l have a poraonal knowledge of the facts cot forth kt this Work report, having performed the work or Ma completion end annexed report ia true.

or PeieiNi CoiWykiu

269

9/9Sfor Office Use Only ^^

TotelVaVieCr. Recorded IBete Recorded"RPCPJVFQ itweivgsW^ *- -. F-r:RED LH \E ivllî^G O!V.

OCT. -25' 95(VED) 13:12 MINING7GEOLOGY-KEN

OCT.-25-93(10) 12:51 HIKIKC-lECOOEI-iL

OCMMI* 9HITH

TEL: 8074682823

TEL.-II7 727 3SS3

T TST 9*99

P. 003

p. M,

Report of Work Conducted After RMOrdlng Ctolm

into

-Ptono lypo or prtni Md- Rktor to die MninB Ad Md ffcojMtons far nojriranMnn of m* i loreoMoiMMMng 7- A Mparato copy of tMt tom* mull b*

VB^kAlM^ MWMA^kB -~ "* MM^M MH^A AM- T cnnioii rapora m nupt mm Mt- A fltattti, fhmlno 8* cWiw BM wM li

far took Vtofc froup.^^ ̂ A^JL^^Mwn n (NimMiilo^ IMM Hoontppny Mi MIIL

oric nrfHBWd (Ctitck Oiw Woift Oioiip OnM

LlP/t CuTTXMS- m/lftVm? — tuft*Lt

l AMHQTttoMntabi tahtorcvir l In KM

i*OTp*j1 al VMof COM vrfMi 30 i"y* of c

Kit*

Md Survey Company *"o PvrfoniMd VM Wtorit (ttvt NMO Md AdMw of AufnroTRmon)

QffflndPolt Of DOfWnCWl BlwMVOt SM llQVB NO* l

l

2. 1 6 2 h r.•^\

^k

^Q&

"1(M Ul

\

-

ill!

fili

iH

l

fiUo\J

M00

- REGOCT

i^lNINIG L/

E(\SI

NOS

.err

99F

dh,: .' ; -

4

OfcCAI en

^

fbabOD

Si

S**

*

tiff

o3

00

19

Credits you are claiming in this report may be cut back. In order to minimize the adverse effects fTfttiftiflalsJipnni rf iyta radrntir which claims you wish to priorize the deletion of credits. Please mark (f) one of the following:^ !U- ^ i i^j j 11

__ P * JT*;-" *ae^ ^"^- J ** fce^^

1. D Credits are to be cut back starting with the claim Ksted last, working backwards. i-'fO LA^E wil^'O Oiv/.2. D Credits are to be cut back equally over all claims contained in this report of work. -li- -

UC l * * '^^^ AM P.M

3. D Credits are to be cut back as priorized on the attached appendix

In the event that you have not specified your choice of priority, option one will be '"iplemente^r,8j9jK)j!!tI2ilj'?'3j'lj5|5

Hotel: Examples of beneficial Interest are unrecorded transfers, option agreements, memorandum of agreements, etc.. with respect to the mining claims.

Note 2: H work has been performed on patented or leased land, please complete the following:

l certify that the recorded holder had a beneficial interest in the patented or teaaod land at the time the work was performed.

Date

OntarioMinistry ofNorthern Developmentand Mines

Ministers duDeveloppement du Nord et des Mines

Geoscience Approvals Office 933 Ramsey Lake Road 6th Floor Sudbury, Ontario P3E 6B5

Telephone: (705) 670-5853 Fax: (705) 670-5863

January 08, 1996Our File: 2.16247 Transaction /: W9520.00068

.00069Mining RecorderMinistry of Northern Development t MinesOntario Government Building227 Howey Street, Box 324Red Lake, OntarioPOV 2MO

Dear Sir:

Subject: APPROVAL OF ASSESSMENT WORK CREDITS OH MIMIMO CLAIMS KRL. 1144373 BT AL IM THE 6ERRT LAKE AREA

Assessment work credits have been approved as outlined on the original submission. The credits have been approved under Section 12, Geology, Mining Act Regulations.

The approval date is January 3, 1996.

Please disregard the Notice of Credit Reduction of December 20, 1995.

If you have any questions regarding this correspondence, please contact Lucille Jerome at (705) 670-5858.

Yours Sincerely, ORIGINAL SIGNED BY:

Ron C. GashinskiSenior Manager, Mining Lands Section Mining and Land Management Branch Mines and Minerals Division

.LJ/J1\Enclosure:

cc: Resident Geologist Red Lake, Ontario

ssessment Files Library Sudbury, Ontario

SOU

TH

OF

OTT

EFLA

KE

G

-1888

FRE

DA

RT

LAK

E

G-1

77

9

Q ?

.

ERLAND RESOURCES LTD. CIOOX)

CUMBERLAND -- ENGLISH DPTIDN

GENERAL JV

ROCK LITHOLOGIES

DIORITE: INTRUSIVE?GRANITE - ' '

SOUTH-HAFIG

JOY ASH FLO W* TUFF

-SPRUCE:.- ^ ' .iViv-* -:-' : V ** -*""'A--.V^-^v-V^:- ",*''Vt V*: '"--J 'NEW ZDlstE

300,000 TONS H 4X CDWBINED

-* ' ^ ."~- * 'S- "i,.^^,v^^?V POVER LINE t&H FtlJV. Wf ^ .. .

NORTH MAFIC FLOW < NOT QBSCRVtPv ^ ^ i-^* e ^

STRINGR CPY.i^!^^^r, -\*

•v -- -•,. -. -•u*:^:?'** j-r-v *-.r-r- .^"- '. r J ,.-, . * ^ , ' * -^TW **r fc , " ,* *' ^. r^ *4. * *-^ ^^ ' ' ~-

CU 1.0k ZN/ i

ZN/0.60M

^^;?" ^*-^.ft, -at** 4 -^ -- -?s- ^. -' - w * ~ S-^B .-,..e;*^f*.-"- * .-, ,î--^S

g^^'^^^l•' V^ -" "•.i--'- *.-J?^"- 7** , . 1"* ^- "-V-- ^-, j , **^^ ,-~* êlt *^l

j^ ^K~ t~ * .v - J.* a ^;- . -^ .-JÂ _ n

SYMBOLSGeology

^"•^-:

^te^Sa?fî Geological Contact

Lineament -

Property Boundary

Fault , ,

Outcrops '"

SUpNd* BoUders

Br*t: Hot*

11449:73

i^38?ss^s^^

52K14NE002B 2.16247 GERRY LAKE52K14NEQ01Q 2.16247 GERRY LAKE

1144365 CUMBERLAND RESOURCES LTD, (100X)

12^0+00 N'

mo*

l TpO+OQ N

\' ' v\

1144334 ENGLISH DPTIDNCUMBERLAND 1144362

NDRANDA-MAJER GENERAL JV

LEGENDROCK LJTHOLOGIES

AIN 'JCfY' CDNTOUCTpnpL^

DIORITE INTRUSIVE? C POSSIBLE FLOW

GRANITE ' * . '

SOUTH MAFIC FLOW

JDY ASH FLOW TUFF -

POWER LINE ASH FLOW TUFF

NOfcTH,MAFIC FLOW

NEW ZONE300,000 TONS4X CDMBINEDBu-Zn

' \t POPLAR' l\ r SPRUCE: t

JDY ZDNE4.0 7. C LL 0.17X Zn X 3,5m

MINERALOGY

, 4.4XZNXl.lnSTRINGER CPY,r^- a fc

cu i.ote

pyrite

pyrrhotrte

aaleno

ondotusite

biotite

garnet

corecerrte

anthophyllite

chlorite

STRINGER CP SPH, p.

,aX ZN/O.GOnOCT311995

MINING LANDS BRANCH~~ ^

Structural

SYMBOLS

Geotoo*cal ContactLineanerrt

Property Boundary

FaultOutcrops

Sulphide Boulders

Dtonond ft-ttl Hole

BeddJriQ

Lineatkw

Lloeatiotv

1144373 Alteration Zone

HLDt Conductor

'S' Tot*

Fold, treqri i ptwo^e of hinge line'

**p . *

R p^o n i- 4 rs* o r*" "o i "-"^ IF* t^ b ̂ OtiRGES,.: ti^B*

FALKS PR0J

52K14NE0028 2 16247 GERRY LAKE

H44365 CUMBERLAND RESOURCES LTD (100X)

1144334 ENGLISH EIPTIQNCUMBERLAND 1144362

•NQRANDArKAJ R GENERAL JV

LEGENDROCK LITHOLOGIES

DIORITE: INTRUSIVE? t POSSIBLE f?et3tf * * *:GRANITE

ORDOC

SOUTH MAFIC FLQV

POWER LINE ASH FLOW TUFF

NORTH HAFie

.^..- y -. :JOY ZD0,177. Zn X 3,Sn 6XZN/0

col colctte

act actmottte

anthophy44ite

cWorrt*

0.50 l -

MINING LANDS BRANCHSYMBOLS

~ Geoiogy

Property Boundary

FoUt

Outcrops-

Sulphide loulders

Dtonond DrfU Hole

Mtcro-bor•^

HLEM Conductor

114437344348

BIG

if V\ fr*.;' r ;-;v:"'"- -.u*-'""" ~t ?*f..^•"S"i* :-"i,.* -"-"-' *-' ' si** * N - "^"'j^'^-i ' L ^- - -"^ * **V? 4 * * ^ ". -"'.i *T " fc * -

J*^*-^ , p * t- * T ^" "J^i*" .'"w

52K14NE0028 2 16247 GERRY LAKE52K14NE0010 2 16247 GERRY LAKE

s^-^V,iV *ztf~Y*:-? ; lVvi 'V!^i' ̂ ^'^'".

a*

H44365 r IMBERLAND RESDL S LTD, (1007.)

0 i 10+00*

ENGLISH DPTIDNCUMBERLAND 1144362

NDRANDA-N AJDR GENERAL

- MAIN "

JQV ZONEX Cu, 0.17X Zn X 3,5m

13XCU 31.6XZN/0* . *- ^ -^ *"^—.**-4 w 4---^ - *- -* -•'SM.-Vii'

\_x' k-ySTRINGR CPY, *y. PQ, *H

CU, l.OiX ZN/ Ii5n

RECEIVED200 -7.2X ZNX0.60n

SYMBOLSGeology

f oliotioft Vertical

Fottetwa IrtetowdProp*r-ky Boundary m

Tautt

Outcrops

Sulphide Boulders

Btanond Drill Hote

'S' rdtjt

Fot* ,*r*n* t pKinge o*LAKE ZDY

UMBERLAND BIG FALLS

52K14NE0028 2 16247 GERRY LAKE

jo^'^b^s; ̂ ^ * *

BORLAND RESOURCES

1144334 J p TIjNCMMEE 1144362

GENERA!NDRANDA-MA

LEGENDROCK LITHOLOGIES

- RENDDIORITE INTRUSIVE? ( POSSIBLE FLDV )

GRANITEV

SOUTH MAFIC FLOW

JOY ASH FLOW TUFF

POWER LINE ASH FLQV TUFF

NORTH MAFIC FLOW

NEW ZONE 300,000 TONS

'/. C OMBINED CL

JOY 2DM 4,0 y. C u 0,177. Zn 13XCU 31.6XZN/

0.21X/CU 4 ,4XZNXl.ln siliceous

calcite

actioolite

cordierite

anthophyllite

chlorite

chalcopyrite

sphalerite

pyrite

pyrrhotite

galena

gahnite

calcsiticates

STRINGER CPY, . SPH 7

andal andalusite

bio btot.te

garnet

cRop diopside

x cu i.oix ZN/

7.2X ZN70.60nOCT 311995

TL5+00 S

SYMBOLSGeology

11443731144*8

UHBERLAND RESOURCE^ BIG FALLS PROJECT :.:

GEOLOGY.DRAVt*Revistons*

52K14NEO010 2 16247 GERRY LAKE

CUMBERLAND RESOURCES LTD GEOL SURVEY JUNE … · WHOLE-ROCK ANALYSIS - ALTERATION SCORES...

Documents

Transcript of CUMBERLAND RESOURCES LTD GEOL SURVEY JUNE … · WHOLE-ROCK ANALYSIS - ALTERATION SCORES...