Sewell TownBhip, NE Ontario - I 2UNITS J:.. · KEkUHKb L/K PtN U.N TIC F/5 UAICH COOES UUttwgy M 1...

' V- Sewell TownBhip, NE Ontario

S1 p --xi l" "

- I 2UNITS J...:.. *

1196940

iG UN;TS12 UNITS t r

7

f i x" l

.

t' 1 204646

Pt UfJ.'TSl 995

1129614

Looations,' /' !6 Juris - 6 UIJTS j

16 UNITS:-

K/ G No. :; 42-A/ SW

Vancouver, BC.; Driver Resources Inc.

TWP S AREA ; Sewell Twp. Porcupine Mining Division, NE Ontarion

TIMMINS FILE; TORONTO FILE;

DATE REG'D ; DATE OF WORK; Oct. 25th to Nov 12, 1995

TYPE OF WORK; 950 meters of Diamond Drilling on Akweskwa Grid.

42A04NW0072 2.17804 SEWELL 010 4

Summary

In October-November, 1995, Driver Resources Inc., of Vancouver, BC, explored their

Sewell-Kenogaming Property with 950 meters of diamond drilling. The six (6) drill hole sites

testing geophysical targets encountered significant data on the fabric of underlying terrain.

The drill holes did not intersect mineralization of economic interest.

Table of Contents

Introduction lProperty lPhysiography 2DDH Agenda 2Certification 5Drill Logs 12

List of SectionsSW-95-1 6SW-95-2 7SW-95-3 8SW-95-4 9SW-95-5 10SW-95-6 11

List of Plans1:10,000 Base Map with DDH locations (pocket) 1:20,000 Compilation Map page 4

42A04NW0072 2.17804 SEWELL l) 1 U U

(i)

IntroductionThe 1994 announcement of favourable gold intersections in Sewell Township, caused the

acquisition of six (6) contiguous claim blocks by Driver Resources Inc., of Vancouver, BC.

The six (6) claim block (65 units) property adjoins east of the property hosting the 1994

discovery. Contemporaneously with the work being done by Hemlo Gold of Timmins, ON,

on the discovery property, Driver Resources initiated an exploration program in the summer

of 1995. The Porcupine-Destor Fault is believed to be in close proximity to the property.

However, the results of the 1995 geophysical surveys (Mag SC IP) encouraged a pursuit of

an easterly extension of the Sewell Splay (horizon believed to host the gold discovery). This

presumed eastern extension was the area where the six (6) drill holes were targeted.

Property

The Sewell Property is found at the eastern limit of the common township line separating

Sewell at Kenogaming Townships. The six claim block property is comprised of the following

claims;

1203707 ( 5 units) Sewell Township Porcupine Mining Division

1203708 ( 8 units)

1203709 ( 16 units) "

1203710 ( 16 units) Kenogaming Township

1203711 ( 16 units)

1203713 ( 4 units)

The claims are held under the name M Caron, Timmins, ON, a local entrepreneur.

d)

PhysiographyThe property has been recently harvested for timber leaving an overall barren surface of

smooth rolling hills. There are numerous boulders scattered throughout the central area. The

highest elevations are along the meandering eskers, ranging from 30 to 40 ft above water

level. Robson Lake borders on the east, and is visible along the access road which leads to

a larger Akweskwa Lake. The latter is part of the Kamiskotia River System flowing northerly

via Opishing Lake and eventually reaches the Mattagami River. The till is generally made of

sand with an abundance of boulders with an average thickness of near l O feet.

DDH AgendaSummary of Drill Hole designation

DDH 1995 Grid Coordinates Azimuth DIP extent CLAIMSW-95-01

SW-95-02

SW-95-03

SW-95-04

SW-95-05

SW-95-06

1425

2100

2116

2375

2675

1625

East/

East/

East/

East/

East/

East/

1450

1150

1136

1325

1400

1275

North

North

North

North

North

North

N220

N135

N315

N360

N360

N180

0T

0 T

oy

0T

0T

0 T

-500

-500

-500

-700

-500

-500

181

158

.93m

.00m

077.00m

226

152

155

.50m

.00m

.00m

1

1

1

1

1

1

203708

203708

203708

203709

203709

203708

In consideration of the 1995 geophysical recommendations, DDH SW-95-01 targeted an

above background IP effect with a concurring resistivity low. It was believed that a prominent

near EW trending fault should occur at this location. The hole collared in a granitic porphyry

intersecting two minor fault gouges with little veining. The second hole, SW-95-02 also

targeted on the 1995 geophysical evaluation tested an interpreted north of east trending

lineament believed at the time to be an eastern extension of the said Sewell Splay (Cross Lake

Annual Report, Middleton 1995). The only significant mineralization was at the intersection

of bedrock in hole SW-95-02 where quart veining contained significant pyrite-pyrrhotite

mineralization prompting the drilling of SW-95-03.

(2)

DDH Agenda continuedDDH SW-95-03 a lso failed to intersect mineralization of economic

interest. The IP effects can only be explained by recrystallization

and alteration of the hosts rocks bordering a granite intrusion.

Since the DDH results and magnetic survey correlations inferred a

granitic batholith bordering south DDH SW-95-04 w as targeted

independently of the original recommendations and aimed towards a

high magnetic feature along strike of the north of east trending

lineament previously tested by SW-95-02/ 03. The magnetic high

features were well explained by several squeezed peridotite segments.

This hole intersected minor veins with no mineralization of interest.

DDH SW-95-05 i n pursuit of volcanics intersected an ancient fault.

However the fault zone failed to give significant assay results. The

last hole, SW-95-06 confirmed the controversy of possible Iron

Formation (said to exist on the Cross Lake-Hemlo Property bordering

west) by drilling through a intersection of Olivine Diabase.

(3)

CERTIFICATION

l Richard Daigje residing at 1115 Maclean Dr, U15 in the city of Timmins, ON, Certify;

1. l have received an Electronic Technologist Certificate in

1979 from Radio College of Canada, Toronto, ON.

2. l have been computer literate and utilized geophysical

equipment for fifteen years.

3. Experienced Max-Min ( HLEM ) interpretations along with field

operations under the supervision of john Betz, 1979- 81.

4. Geophysicist Assistant for Kidd Creek Mines under the

supervision of Mr. Doug Londry, 1981- 85.

5. Fulfilled geophysical contracts in NE Ontario, 1985-87.

6. Fulfilled geophysical contracts ( IP, HLEM, MAG, SP ) along

with property assessments in Eastern Canada, 1987- 92.

7. l have been employed by M.C. Exploration Services Inc as

Geophysical Evaluator for the past four years.

8. l have no direct interest in the property reported upon.

DATEiAx/^ f/ Timmins, ON

R. ]."Daigle

(5)

ffi

HOLES PLOIILD

199bGRlDCUQKmNA'lL

Losing, H25E Nortnng; 14UJN

Dip, -50" Awnutn; N22tf l

Oa.m 1 203706

y /3bm West A 2tiQm SouOi ot PUI.I jjf

ROCKCOOES L/S PEN L LN IK F/S UAICH CUtSLilholugy fi l O f f * *

KEkUHKb L/K PtN U.N TIC F/5 UAICH C OOESUUttwgy M 1 O F F T 7

SECTION SPtCS:Mtl FT t. M UMLXllNIi I&ObtCHON lOf . DOT OrOLLKWCt ./- 200 U

J l) IO 1i 20 25

H |.DtG) -

N

Driver Resources Inc Akweskwo Grid

DDH SW-95-01Clunn 120.37UH Sewell Township,

6,3 iS

l" C

~)

l.

-5-5

S 3 — s f

!oc

5

T

-,

00

, i i,,- .— , .-.

XI

ILW l

a:

1

"

0 U

-s^^^^^JIDViRByfc!f^.":^jT;r^~"jr*

\ ^

\V* jf

\ '\ j'*

\

2

g

|

r;

u.

s

— ~ ~~~ ~\ ' v _ t" *tf;^-i---- T^^r- | ^7^r..rV -

r̂ ai

ion z

HOLES PLOTTED m*, i

SW-95-03JTI JO \JvJ

1995 Grid Coordinate

Easting; 21 16E Northing; 11 36N

60m West i 61 5m South ol Post j iClaim 1203708

Azimuth; N315'T Dip; -50'

Kaaxtf lyn rt* lin ne F/S mot cueUttHtoyr R 1 0 F F * *

HUMS lyi PU UK ne F/S MIDI emo

SECTION SPtCS:BnWTS 110 - \M StCIlC* TOP. DOT 0 ISO HUHWCC 'A 200 y

SCALE -r;-/v \

i 0 S 10 15 M 25 gi \ W

' " vvDriver Resources Inc

Akweskwa GridDDH SW-95-03

Claim 1203708 Sewell Township, ON.Hateil 3.16.00 17-tMMtM 10Ji:*5

AJ3TTED ffi : M C D^tfotiofl Seivicei he GtQSOfT

OCLKQ) BY ; W hlmnn

-CLiS .-.:™D rotn i

SW-95-04

1995 GRID CQGRDiNATESEASTING; 2J75E NORTHING; 1225N

200m East and 400m South of Post f*

Cairn 1203709

Dip; -70' Azimuth; N360'T

-Onto*

L/S PO* LfM TC f/S MitX COOII 1 D r F i *

L/* PW LDI W r/S UAItH COOE311 t F F T f

SECTION SPECS:iff. PT. E. M 2J75 1.123Dram -oo -225SECTION TOP. id! tt US

t/- 200 H

SCALE

Driver Resources Inc Akweskwa Grid

DDH SW-95-04Claim 1203709 Sewell Township, ON.

a BY : y C gxpkxefonj

3 gr: Jf Gilmoa ~

O)

S iso i

HOUS PLOTTED ra*, i

SW-95-05

1995 GRID COORDINATEEasting; 2675E Northing; 1400N

460m East and 330m South of Post f4

Claim 1203709

HCKCGOG L/* IU IXN IK F/S UUCH COOBii l O F F . .

L/R PU) UN IK F/S IMCH COOOl 1 O F F T t

SECTION SPtCS:R0 PT. E, H 2U3 1400OTOflS ISO -ISOSEC1ION TOP. BOT O ISO

SCALES O S 10 15 B O

UHITH (Oat * MO N



~njma) m -. UTEijiliirulMi Sxvicn BC XSSSfr~

HOLES PLOTTED TOM. i

SW-95-06

1995 Grid Coordinates

Easting; 1625E Northing; 12/5N

teimuth; N18u*T Dip; -50'

MO m West i 460 m South of Pot ft

Claim 1203708

MCUXOB I/I PfX LUI K F/l WICH COOUMov II 1 O F f . .

BUMS l/R PU lil K F/S HKHaXBl l O F F t ?

-130 ISO

SECTION SPECS:ttf. PT. E, M tiUEXTEND 150StCnOB TOP. BOT OTQL0MCE V- 200 y

SCALEb I D 15 20 O

UMOH (OH) - TH



Diamond Drill Core Log M.C. Exploration Services Ltd. Page 1 of 5

Dip Tests

Grid Coordinate Elevation: Bearing: Dip at Collar:

Easting 1425 E Northing 145 ONSurfaceN 2200 T-500

Depth Dip Corr. DipO -50

181.93 -50

Hole No.: Property: Claim No: Core Size: Started: Finished:

SW-95-1AkweskwaP1203708BQOct. 27/95Oct. 27/95

Drilled by: Norex Logged Total Depth of Hole: 181 .93 Date log

Meters From

0.00

15.00

To15.00

27.80

!

Description

Till - largely boulders (200Xo) with intervening sand gravel,boulders ( as cored) 0 - 38 cm. Pink granite - 38 -58CM.

Sample No.

Magnetite Gabbro 58-62 pink porphyritic, aplite, 62 - 77 cm. finegrain andesite - 77-107 cm. Pink Granite 107-147 micacousaiotite andesite -147 -177 cm. Magnetite Gabbro - 177 - 200cmfine grain andesite, 200 - 270cm. pink granite 270 - 305 cm. biotiteandesite 305 - 325 grey hornblende Granite, information jre possible rock types encounter down holeactual bedrock contact at 17.0 M. (15to 17 boulders)Rock type grey Granite coarse grain hornblende, chlorite greyGranite - original grey is continually soaked with a pink phase oflater Granite - all degrees of colour change to pink by absorption- large angular inclusions of fine pink Granite in angular androunded fragments indicaters original grey is probable borderphase of intrusive, larger feldspar shows varying composition

in individual crystals supporting evidence of border phase,epidote permeates all crystals, feldspar, hornblende - as primealteration product.Foliation displayed by Granite matrix approximate 45" to corenormal indicates hole orientation good for max coverage - rock ;fabric indicaters border phase pluton - micro- pegmatiteabundant euhedral feldspar phenocrysts not incorrect toconsider this as Granite Porphyry innumerable imperceptibleand subtle changes to varieties of pink Granite of no significanceindicates permeation by influence of pink feldspar saturation j

From To Length (M)

Nl PPM

CD PPM

AG PPB

_________

by: W. Oilman ged: Oct 27/95AU PPB

Sample Description

SW-95-1

Page 2 of 5

Meters From

27.80

28.60

30.55

30.85

32.32

36.68

37.36

38.83

42.90

50.00

50.40

To28.60

30.55

30.70

32.32

36.68

37.36

38.83

42.90

50.00

50.40

53.13

Description

Aplite pink porphyry sugary fabric - pink feldspar mica, quartz 1 matrix-anhedral phenocrysts cream feldspar, epidote alteration of hornblende and mica. 27.80 - 28.6 no sulphides observed.

Grey Granite - increase saturation of matrix with pink feldspar and visible injectar.

Aplite - Pink porphyry.

Grey Granite - pink feldspar saturation of matrix grey Granite best 30.85 - 32.32 trace pyrite at contacts - rare 5mm. pyrite in matrix, epidote margins

Grey Granite - biotite flecked matrix

Aplite - Pink Porphyry banded epidotic margins, 36.68 - 37.36 movement and alteration post crystallixation, trace pyrite

Grey Granite - pink feldspar saturation pink, phase interpreted as later infusion of colour

Aplite - pink porphyry - a fingered contact several parallel lenses country rock, porphyritic, trace pyrite steep contacts bleaches lighter in center, 38.83 - 42.9 very siliceous, all sizes, shapes phenocrysts.

Grey Granite - cream white feldspar, 300Xo of matrix is chloritic amphibole, slight pink permeation, crude foliation 45" to core normal, orbicular fine grain Granite inclusions

Fault Gouge - schisted - chloritic - volcanic mylonite

Grey Granite same as 42.9 - 50.00, 1cm. orbicular fine grain Granite inclusions - random pink alteration.

Sample No.

15382

15383

15384

15385

From

27.80

30.85

36.68

38.83

To

28.60

32.32

37.36

42.90

Length (M)

0.80

1.47

0.68

4.07

Nl PPM

CU PPM

l

AG PPB

0.10

0.10

0.10

0.10

AU PPB

NIL

NIL

NIL

NIL

Sample Description

SW-95-1 Page 3 of 5

Meters From

53.13

53.85

57.90

60.10

83.46

83.56

105.25

To53.85

57.90

60.10

83.46

83.56

105.25

108.45

Description

Aplite-pink porphyry-epidote chlorite altered hornblende,hematite smeared joint planes 53.13 - 53.85, no visible sulphidesteep contacts.

Grey Granite-some coarse amphibole-sporadic pink segments(matrix permeation) at 56m and 57m, 4cm bands pink porphyry

Aplite-pink porphyry-hematite stained joints, turns grey Graniteto pink (feldspar near contacts).57.90 - 60.40 minute trace pyrite at contacts (all joints smeared

with chlorite).

Grey Granite, very slightly pegmatitic with large euhidral andanhedral pink to beige feldspar sporadic through matrix, alsoclustered granular amphibole clusters, all indicates a peripheralphase of main Granite mass.70m to 90m, gradual increase in pinkish hue to matrix,introduced hematitic alteration, iron enrichment produces pinkfeldspar, epidote increase, chlorite margins on amphiboleincrease, at about 90m reverts back to normal grey Granite,the larger feldspar phenocrysts, spectacular zoning, varyingstability of equilibrium, prime evidence of border phase ofGranite,-81m to 83.46 pink phase.

Fault-chlorite schist, mylonite, original Lamprophyre or possiblediabase intensity sheared, lenses white pink carbonate,parallel foliation, orbicular clots carbonate after feldspar,foliation 45 0 to core normal.

Grey Granite, as above, pink phase from 83.56 to 86.0.Intense pink phase 89m to 91m, 97.80 to 100 pink phase revertsrapidly to grey.

Grey Granite, Lamprophyre dyke.

Sample No.

153865,

15387

h

From

53.13

57.90

To

53.85

60.10

Length(M) ——

0.72

2.50

Nl PPM

-

-

cuPPM

-

AG PPB

0.10

0.10

AU PPB

NIL

NIL

Sample Description

i

SW-95-1

Page 4 of 5

Meters From To

108.45 j 108.95

108.95

116.42

i

120.44

i121.65

121.75

133.00

133.05

148.80

116.42

120.44

121.65

121.75

133.00

133.05

148.80

149.00

149.00; 156.65i

Description j

Lamprophyre, migmatized mix with remnants of originalabsorbed Granite, possibly original diabase with 50"Xoncorporated grey feldspar, amphibole, some rare pinkphenocrysts feldspar, wine coloured spinels, so much incor porated host rock gives porphyritic fabric, knots epidote,contacts 45" to core normal, very fine possible micro-pyrite.

Grey Granite, coarse grained, porphyritic, spectacular zonedfeldspar phenocrysts, abundant subhedral amphibole, takeson pink colouration at contacts, pink is alteration phenemena.

Aplite, pink porphyry, euhedral to anhedral pink feldsparphenocrysts, amphibole altered to chlorite, epidote, sharpcontacts medium grained at margin, indicates crystal mushinjected from below as relatively solid mush intruded perhapsafter Granite crystallized, no apparent sulphides, sharpcontacts, medium grained at contact, no guick chill.

Grey Granite, strong pink permeation of matrix coarse grained,euhedral feldspar phenocrysts.

Lamprophyre, highly silicic, epidotic, steep contacts.

Grey Granite, usual coarse grained, pink for 1m at uppercontact.

Lamprophyre, coarse grained, probable inclusion rather thandyke, strange coarse fabric unlike dyke.

Grey Granite, usual coarse grained, varying segments withpink permeation (alteration haloes) at 142m a roundish 5cmLamprophyre xenolith?

Lost core.

Grey Granite, coarse grained, distinct pink phase to fabric,large feldspar phenocrysts.

Sample No.

15388

From

116.42

To

117.42

ll

Length (M)

1.00

Nl PPM

-

CU PPM

.

ii ii l

AG PPB

0.10

AU PPB

NIL

Sample Descriptionjliii

SW-95-1Page 5 of 5

Meters From

156.65

157.13

160.50

160.55

160.60

160.85

161.35

165.87

166.62

166.87

167.10

To157.13

160.50

160.55

160.60

160.85

161.35

165.87

166.62

166.87

167.10

181.93

181.93

l

l

j

Description

Lamprophyre, very dark green, finer grain, coarse at contacts, large anhedral hornblende at and near contacts, ubiguitous pink feldspar as in all other Lamprophyre.

Grey Granite, coarse grained, random pink saturation.

Lamprophyre, skimming edge of Lamprophyre.

Aplite, small finger of fine grained pink dyke.

Grey Granite, coarse grained.

Aplite, porphyritic, anhedral, pink feldspar, sugary texture, contacts 45" to core axis.

Grey Granite, coarse grained, from 163.65 to 164.0 several angular wedges Lamprophyre, skimming dyke edge.

Aplite, high silica, pink porphyritic dyke.

Grey Granite, 500Xo grey, 500Xo pink feldspar.

Aplite, pink porphyry, steep contacts.

Grey Granite, coarse grained porphyritic, high silica Granite fabric and content unchanged from beginning of hole.

End of Hole

Sample No.

From To Length (M)

Nl PPM

CU PPM

j

AG PPB

AU PPB

Sample Description

l

Core stored at Al Taylor's warehouse

- s-/ ^ S \ Logged by: s7*L*.Js*' /^^,^Warren Gilman

Diamond Drill Core Log M.C. Exploration Services Ltd.

Dip Tests

Grid Coordinate Easting: 2100E Northing: 1450N

Elevation: Surface Bearing: 135 0 T Dip at Collar: -50

Depth Dip Corr. Dip

Hole No.: Property. Claim No: Core Size: Started. Finished:

Page 1 of 4

SW-95-2Akweskawa GridP1203708BQOctober 29, 1995October 31, 1995

Logged By: W. Gilman

Drilled By: Norex Total Depth of Hole: 158.00 Date Logged. November 2, 1995

Meters From

0.00

10.00

10.20

14.20

To10.00

10.20

14.20

Description

Overburden Casing. Till largely boulders (2007o) with intervening

sand gravel boulders, entirely coarse grain pink to grey Granite.

Same chloritic xenoliths rare, fragments of greenstone

remnants.

Quartz vein. 1 0cm quartz vein with clustered granular Pyrite at

45" to Core Axis of coarse grain pink grey granite country

rock, 10.0-10.20 suhedral clusteredvein.

Granite. Typical coarse grain granite as cored in SW-95-1 , but

pervasive pink hue, pink Feldspar, slight hematitic alteration,

random larger subhedral Feldspar phenocrysts, not as large or

as abundant as granite of hole # 1 . Amphiboles more distinct

(less chloritized) than preceding hole, minute xenoliths of

volcanic? rock at 13.23 skimming edge of Porphyritic

lamprophyre.

Sample No.

32

14.95 Lamprophyre, medium grain green-uniform fabric, medium grain

persists at contacts; indicates dyke intruded as crystal mush,

abundance of pink anhedral Feldspar phenocrysts absorbed

from the intruded Granite, minute pink crystals probably sphene,

contacts flat to 45" to Core Axis.

From

10.00

To

10.20

Length (M)

0.20

Nl PPM

CD PPM

AG PPB

AU PPB

Sample Description

SW-95-2

Page 2 of 4

To

28.88

28.93

52.10

52.22

84.30

84.50

90.20

Description

Granite. Coarse grain pink, usual coarse grain with some

spectacular zoned Feldspar phenocrysts, hornblende clouded

and rimmed with chlorite, unnumerable joints with hematite

chlorite slips, at 23.70 micro dyklet of altered lamprophyre

absorbed much of intruded granite.

Quartz vein. Barren vein, contacts 450 to Core Axis. Much

absorbed pink Feldspar, 2cm at 29m.

Granite. Typical coarse grain pink hornblende granite, random

reldspar phenocrysts, inclusions of lamprophyre at 29.63 and

32.80, several random clots of 1cm. Xenoliths altered

lamprophyre lath like xenolith at 39.05. At 45m-2cm Granite dykelet at 50m, at 49m-2cm Granite

dykelet 1cm quartz vein running along parallel to Core Axis.

Quartz vein, barren with some absorbed pink Feldspar.

Granite coarse grain pink-same as previous logged granite

at 57.80 and 63.50 metasomatized wedges at probable

original lamprophyre, orbicular pink Feldspar inclusions

indicative of original lamprophyre, at 72.65 metasomatized

wedge of lamprophyre 8cm, at 81 .40 xenolith of chloritic

schist (lamprophyre).

Dual vein-pegmatite quartz vein and typical lamprophyre at

very steep angle-parallel segments, each 2cm.

Granite, coarse grain pink-subhedral amphiboles with

chloritic margins, large phenocrysts zoned plagioclase. At

Sample No.

j l

From To Length (M)

Nl PPM

CU PPM

AG PPB

AU PPB

Sample Description

SW-95-2Page 3 of 4

Meters From

90.20

90.38

118.70

119.00

119.13

121.40

124.37l

i

To

90.38

118.70

119.00

119.13

121.40

124.37

124.92

Description

88.40 -1cm steep smoky quartz vein.

Lamprophyre-recrystallized with central inclusions remnant

granite, porphyritic-Feldspar and hornblende.

Granite. Predominantly grey to pink, several segments of 1 to

3m of very pink, some pronounced pink with zoned Feldspar

sporadic, chlorite schist xenoliths of 1 to 3cm. The

Feldspar subhedral phenocrysts persist at 93-90-97.20

at 98.95 wisps of chloritic schist could be dyke margin.

Aplite pink medium to coarse grain mush of individual crystals-

many euhedral, dyke came in nearly cold along zone of

weakness as a partly crystallized mush, hematite stained joints.

Granite-grey, pink, coarse grain.

Lamprophyre-light green finer grain large resorted

phenocrysts of xenoliths of chlorite, after amphibole crude

foliation (orientation of large fragments) 45" to Core normal,

upper contact flat, lower contact 85th to Core normal. Very

fine schistose upper contact, joints lined with chlorite, pink

hue indicates permeation with granitic pink fluids; lack of pink

Feldspar disseminations, as found in smaller dykes.

Granite, grey pink porphyritic, amphibole with margins of

chlorite, vary rare minute Pyrite.

Lamprophyre identical to 119.13 to 121 .40, possibly same

dyke as above.

Sample No.

From lo Length (M)

Nt PPM

CU PPM

AG PPB

AU PPB

Sample Description-J

SW-95-2

Page 4 of 4

Meters From

124.92

149.70

149.90

To149.70

149.90

158.00

158.00

Description 1

Granite, grey pink coarse grain porphyritic, some large zoned

Feldspar. From 128-129, strong hematite alterations, pink

permeation. At 133.70,4cm wedge of lamprophyre, from 140.50

:o 141.50, strong pink permeation. At 146.80, 4cm wisp

of chlorite schist or skimming of dyke. 140.50 to 141 .50

strong pink permeation to Granite. At 146.90 wedge 4cm, mica

rich lamprophyre.

Lamprophyre, large incorporated pink Feldspar in hornblende

rich dark green dyke, contacts 45" to Core normal.

Granite, grey, slight pink, large Feldspar phenocrysts persist,

amphiboles constitute 15 to 2007o of matrix (with chlorite),

remaining percentage nearly entirely quartz and Feldspar.

End of Hole

Sample No.

*

From To Length (M)

Nl PPM

CDPPM

.

AG PPB

AU PPB

Sample Description

Core stored at Al Taylor's warehouse* -

Logged by: ^-v^^^. v̂/s&srs*Warren Gilman


Dip Tests

Grid Coordinate Easting: 2116mE, Northing 1136mN Elevation: Surface Bearing N315 Degrees T Dip at Collar: -50

Depth Dip

77.00

Corr. Dip

-50.00

Hole No.: Property: Claim No: Core Size: Started: Finished: Logged by: Date Logged:

SW-95-3 Akweskwa Grid P1203708 BQOctober 31, 1995 November 1, 1995 W. Gilman November 10, 1995

Drilled By: Norex Total Depth of Hole: 77.00Meters

From0.00

9.00

61.23

To9.00

61.23

61.86

Description

Overburden. Till boulders comprise 2007o with intervening sandand gravel. Boulders as cored 90 0Xo grey granite, 100Xo lampro phyre. Accurate reflection of underlying bedrock.

Grey Granite. Coarse grain hornblende chloritic granite, originalgrey is sporadically and continually soaked with pink hermitic

Sample No.

Feldspar to varying degrees-seems to be close to border phaseof granite intrusive-larger zoned plagioclase ubiquitous withgranite in all these holes. Wisps of chloritic lamprophyre sporadicthrough core.e.g. 13.15m and 15.0m - either margins of dykesor undigested xenoliths of lamprophyre. From 20.25 to 23.25,pervasive strong pink matrix due to alteration zones in graniteintrusive.At 22.60m, Feldspar quartz, coarse grain vein in granite seam.At 27.90, 10cm inclusion of lamprophyre with coarse pinkFeldspar (undigested) from host granite.At 46.50 - 52.50, wisps of chloritic schist-metamorphosedlamprophyre-1 cm smoky quartz bands at 45" to Core Axis, 1 en-wide at 10cm below and above 52.50.Granite becomes progressively more pink-large phenocrystszoned Feldspar persist.From roughly 59.50 to 61 .23, strongly pink to red - alterationzone.

Lamprophyre. Dark grey black - medium grain with abundant

.

il

larger amphiboles and typical vary-sized orbicular pink Feldsparabsorbed from invaded Granite, random rare Granite stringers i

From To Length (M)

Nl PPM

CU PPM

AG PPB

AU PPB

Sample Description

SW-95-3

Page 2 of 2

Meters From

61.86

73.90

74.16

To

73.90

74.16

77.00

77.00

Description l

hrough lamprophyre dyke, late stage granitic injecta.

Pink Granite. Same coarse grain granite as above, but bright pink due to pervasive alteration.

Lamprophyre. Skimming along dyke edge, core 50"Xo granite parallel Core Axis.

Pin k Granite. As above.

End of Hole

Sample No.

From To Length M)

Nl PPM

CU PPM

AG PPB

AU PPB

Sample Description


Loaded by: *^s..^is.j^*f x^/x/^?**/?,*/.Warren Oilman


Grid Coordinate Easting 2375E, Northing 1325N Elevation: Surface Bearing: N 20 " T Dip at Collar: -50 degrees

Depth

Dip Tests

Dip Corr. Dip


SW-95-4Akweskwa GridP1203709B.Q.November 2, 1995November 7, 1995

Logged by: W. Gilman Drilled by: Norex Total Depth of Hole: 227.00 Date Logged: November 12, 1995Meters^ From

0.00

9.00

24.18

24.22

To9.00

24.18

24.22

65.24

Description

Overburden, till boulders comprise 200Xo (as cored ) with inter vening sand and gravel, boulders 200Xo Lamprophyre, 800XoGranite accurate reflection of underlying bed rock.

Pink Granite, coarse grain uniform, hornblende Granite withabundant pink feldspar, quartz, larger Feldspar phenocrystsnot as abundant or as large as in previous holes, probablyprobing deeper into intrusive, at 15.86 wisp of chlorite schistderived from Lamprophyre, probable xenolith.

At 16.0, barren 4cm, flat vein of smoky quartz, (hematite) nosulphides.

Vein, quartz epidote, feldspar.flat vein, faulted and displacedfew cm.

Pink Granite, very coarse grain, pink pegmatitic granite, throughto 30m, then reverts to more normal granite, coarse grain butslightly less pink feldspar phenocrysts, epidote rims nearly allhornblende crystals from 46m to 52m reverts to more pinkhematitic.

At 48.12 to 48.22, slice of Lamprophyre with characteristicscattered pink orbicular feldspar in dark green fine to mediumgrain matrix.

Sample No.

From To Length (M)

Nl PPM

CU PPM

AG PPB

i

iji

|

AU PPB

Sample Description

SW-95^Page 2 of 5

Meters From

65.24

65.83

104.70

104.80

116.35

116.52

116.50

116.65

116.98

117.02

ToDescription \

65.83 Lamprophyre, very dark green, typical Lamprophyre dyke,

104.70

104.80

116.35

116.52

116.50

116.65

116.98

117.02

119.27

scattered pink anhedral and subhedral feldspar phenocrysts,some to 1cm. , medium grain contacts, not affected by intrudedrock , some grain size throughout, contacts flat, perpendicularto core Axis.

Pink Granite, pink hematitic, slight red persists through! to 83m,hematite stained joints, at 76.60 angular wedge of Lamprophyredyke, assumption is dyke injections causes pink alteration haloin Granite.

A 83m, reverts back to more usual pale pink granite, at 85.40and 85.5 wisps of chlorite schist. Some lone feldsparphenocrysts to 2cm. From 96.0 - 96.1 0, wedge of Lamprophyreat 97.3 wedge of lamprophyre. At 102.7 vein like fracture withchlorite schist at steep angle.

Peridotite, dykelet invading fracture in Granite.

Pink Granite, same as described above.

Aplite, bright pink, slightly porphyritic aplite, typical crystal mushno fine contacts coarse to tim.

Pink Granite.

Lamprophyre, characteristic fabric, laths hornblende, mg.with acicular pink feldspar random throught matrix, muchincorporated fragments Granite in dyke.

Pink Granite.

Quartz vein, frosted white, hematite stain, flat contacts.

Pink Granite at 1 18.6, 1cm fracture with chlorite schist with2cm frosted quartz vein at 118.65

Sample No.

From To Length (M)

Nl PPM

CU PPM

AG PPB

AU PPB

Sample Description

j

i

i

SW-95-4Page 3 of 5

Meters From

119.27

119.50

134.80

136.57

136.90

137.15

158.35

158.72

162.53

162.96

163.90

164.90i

To119.50

134.80

136.57

136.90

137.15

158.35

158.72

162.53

162.96

163.90

164.62

184.15

Description j

Aplite-pink medium grained samll orbicular feldspar phenocryst!

Pink Granite, as described previously.some secondary granitic njectors along joints at 123.85,1cm wisp chlorite schist also at 126.5, at 131.5,8cm sliver chlorite schist. From 134. 5 to 134.8C

continual wisps and slivers of schisted Lamprophyre in pink Granite.Lamprophyre, predominantly fine grain schisted displays typical Finer grained version of the dyke, a crystal mush of finer aggregate, slight pink permeation of fabric near fractures, foliation of matrix at 45 degrees to Core.

Pink Granite.

Lamprophyre,, very typical with articular pink feldspar inclusions near vertical contact, 500Xo granite, 5007o dyke.

Pink Granite, coarse grain, some larger feldspar phenocrysts, hornblende with chloritic margins, typical of all this granite, only minor variations (colour), 140.1 a 1cm flat quartz epidote vein, 507o plus chalcopyrite, at 147.35, 3cm pink aplite dykelet.

Aplite, sugary fabric, innumerable thin fractures coursed with hematite stain, near flat vein contacts.

Pink Granite, usual features, at 159.54 to 159.68 wedge of Lamprophyre in Granite, at 162.09 composite flat vein, aplite quartz, epidote, green mica, finely and distinctly banded.

Pink aplite, flat dyke, retains coarse grain right to contact.

Pink Granite.

Peridotite, 25cm of slice of dyke in Granite, remainder is very fm grain dense brittle peridotite.

Peridotite, very fine grain hard brittle, strongly jointed, dark green peridotite, so fine difficult distinguish individual crystals,

Sample No.

^

From To Length (M)

Nl PPM

CU PPM

AG PPB

AU PPB

Sample Description

SW-95-4

Page 4 of 5Meters

From

184.15

192.55

195.45

196.15

To

192.55

195.45

196.15

208.95

l

Description

Pyrite in clustered aggregates in crude cubes, about 2 0Xoaverage, disseminated uniformly, some 1cm serpentinous joints^rite to .5cm in size.

164.9 - 166.0 little granular crystals Pyrite

1 83.0 - 1 84.1 5, minor Pyrite near both contacts. Pyrite scarcethrought central part of sill to trace, hard siliceous matrixthroughout, some seams serpentine to .5mm.

Pink Granite, from 184. 15 to 188.50 , unique fabric of orbicularfeldspar (pink ) in finer matrix, probable influence of peridotite,sill with some remelt of granite matrix and some recrystallizationsome random Pyrite within matrix, threaded with epidote.

184.15 - 185.5 ultra siliceous, uniform fine Pyrite, from 192.15to 192.55 sliver of peridotite along Granite contact.

Peridotite, dark green very fine grain, blocky, brittle, 192.55 to195.45 rare clusters fine Pyrite to .5mm.

Lamprophyre or migmatized peridotite could be either, eitherpassage of peridotite along a zone of weakness paralleling thelamprophyre or a portion of peridotite absorbed sufficientforeign material to produce a migmatized basic rock, the formersuggestion seems more plausible with injection along a zoneof weakness.

Pink coarse grain Granite, actually red Granite from contact to1 meter. At 197.05 wisp of chlorite schist skimmed branch

of dyke, pink Granite retains coarse grain throughout and tovarious contacts, at 197.31 and 197.46 fingers coarse grain

Sample No.

15390

15391

t

15392

15393

i

From

164.90

183.00

184.15

192.55

To

166.00

184.15

185.50

195.45

Length (M)

1.10

1.15

1.35

2.90

Nl PPM

43

50

21

32

CU PPM

152

144

15

133

AG PPB

7

nil

nil

nil

AU PPB

7

nil

-

3

Sample Description

SW-95-4

of 5

Meters From

208.95

209.40

209.60

209.90

210.38

216.15

216.35

220.78

220.90

To

209.40

209.60

209.90

210.38

216.15

216.35

220.78

220.90

226.50

226.50i

Description

aplite at 199.30 to 199.40 barren smoky chloritic quartz vein.

Peridotite, very fine grain, dark green, blueish alteration alonginnumerable jagged fractures in blocky dyke.

Pink Granite.

Quartz vein, smoky chloritic quartz with some Pyrite, 209.60 to209.90 quartz heavily fractured gives smoky effect.

Pink to red coarse grain Granite.

Peridotite, very fine grain dark green dyke, very hard (not asblocky and brittle as previous dyke intersections). 2 types ofjoint linings, hair like, carbonate and very hard serpentinousalteration zone.

Pink Granite, peridotite, core is half of each rock type, drill cutalong dyke margin.

Pink Granite.

Lamprophyre at steep angle, characteristic phenocrysts orbicu lar pink feldspar in dark green matrix.

Red Granite, to 224.5, normal pink hornblende Granite to end o

hole.

Marked as 227 End of Hole

Sample No.

15394

|

From

209.60

To

209.90

Length (M)

Nl PPM

cuPPM

i0.30 30

AG PPB

32

i

AU PPB

nil

Sample Description

i


Logged by: Xx^xjV^x: s^/'/???/!/*w ' —— yt—L — r e c- f f ——— ̂ ——— f ir- ——— -

Warren Oilman


Grid Coordinate Easting 2625E, Northing 1400N Elevation: Surface Bearing: N O degrees Dip at Collar: -50 degrees

Depth

Dip Tests

Dip Corr. Dip


SW-95-5 Akweskwa Grid P1203709 B.Q.Novembers, 1995 November 10, 1995

Logged By: W. Gilman

Drilled By: Norex Total Depth of Hole: 152.00 Date Logged: November 18, 1995

Meters From To

0.00

21.80

26.00

29.00

35.45

35.60

21.80

26.00

29.00

35.45

35.60

55.10

Description

Overburden, 15cm of lamprophyre kernels, above bed rock,overburden composition unknown, sand or clay or both.

Granite, grey white, all bleached, Feldspar in process of alteringto clay, not the usual very coarse grain cut by innumerableenstatite echelon FAULTS, represented by gravel Granite,breaks at 22.0(1 Ocm) at 23.85(1 5cm) to 24.0 at 24.90 to 25.10(20cm), next 90cm represented by 20cm core(80cm ground up

to 26.0; 21.80-23.0, gravel, pink peak epidotic Granite.

Lost core, 3 meters represented by 20cm gravel granite.26.0 - 29.0, rare trace fine Pyrite, epidotic granite gravel(actually 20cm gravel).

Sample No.

15400

15146

15147

Pink Granite.

Lamprophyre, dark green, larger laths amphibole in medium Q Kmatrix.

lin

Pink Granite, pink partly altered bleached Granite, red hematite |permeation, through matrix of original hornblende Feldspar,

From

21.80

23.85

26.00

To

23.00

26.00

29.00

Length l (M)

1.20

2.15

3.00

Nl PPM

24

-

.

cuPPM

3

-

.

AG PPB

.

-

.

AU PPB

.

NIL

NIL

i

Sample Description

SW-95-5

Page 2 of 4

Meters From

55.10

55.80

59.00

i

j

To

55.80

59.00

61.50

Description

Granite with rims epidote around Feldspar, chlorite matssmeared along joints, rare trace Pyrite.

35.60 - 36.50, pink bleached Granite, clay film on Feldspar.

36.50 - 38.00, bleached Granite, heavily fractured.

43.0 - 44.0, slight bleached epidotic red Granite, blocky.

50.00 - 51.00, slight bleached altered red Granite, rare veryfine Pyrite very red hematitic Granite to dyke contact.

Lamprophyre, dark green, medium grain, many slender lathsamphibole, abundant ovoidal pink Feldspar characteristic of thislamprophyre throughout all drill holes, contacts 45" to Core,fine grain contacts.

Red Granite, dark red Granite, hematite saturated fabric,partly silicified, some foliation, some brecciation.

Ancient recrystallized fault zone, lit par lit injection oflamprophyre stringers and quartz, in foliated silicified redGranite and hematitic alteration(jasper?)in foliated zone at 45"to Core normal, some brecciation with white carbonate fillingsome disseminated very fine Pyrite.

59.0 - 60.50, recrystallized, silicified, melange of sericite,lamprophyre stringers, quartz, carbonate, rare Pyrite, filigreeof fine quartz parallel foliation.

60.50 - 61 .00, silicified mylonitic melange of quartz with

Sample No.

15148

15485

15149

15150

15396

15398

interlayered mica schist, hematite alteration.

61 .00 - 61 .50, recrystallized fault breccia, trace fine Pyrite. 15397

From

35.60

To

36.50

36.50

43.00

50.00

38.00

44.00

51.00

;

59.00 60.50

i

i

60.50 61.00

i

61.00 61.50

Length (M)

0.90

1.50

1.00

1.00

1.50

0.50

0.50

Ml PPM

-

-

.

cuPPM

-

-

-

.

60

28

3

4

AG PPB

-

-

-

~

-

-

27' 3

AU PPB

NIL

-

NIL

5

-

-

-

Sample Description

SW-95-5Page 3 of 4

Meters From

61.50

91.90

92.07

104.75

107.00

j

To91.90

92.07

104.75

107.00

137.00

Description

Pink Granite, coarse grain, intergrowth quartz, pink Feldspar,aths amphibole rimmed with epidote some very fine Pyrite rare

through matrix, joints are matted with film of chlorite, constantlycontains large Feldspar phenocrysts.

3eridotite, dense black very fine grain peridotite, some hair likefractures of serpentine, contains fine Pyrite (30Xo?) very finescattered Pyrite or chalcopryrite.

Pink Granite, more medium grain than usual coarse grain, palepink abundant green hornblende, less large phenocrysts, morenormal looking Granite, some random fine Pyrite, at 102.60quartz epidote hematite vein.

Peridotite, very fine grain, blocky brittle, abundant fractures withhematite carbonate and fractures with Pyrite, some Pyrite cubesto .5mm, heavy Pyrite smeared on some joint planes, nearvertical upper contact, very fine grain against coarse grainGranite.

104.75 -107.0, test of meagre Pyrite in blocky dyke.

Pink Granite, more normal appearance than usual, coarse grainwith large phenocrysts Feldspar, lighter pink than usual, veryfine pinpoints Pyrite anhedral laths amphibole rimmed withepidote.

From 115 to 116.42, varying degrees of migmatized Granite,abundance of green amphiboles with very different fabricfrom the normal Granite, some wisps and fragments of dyke in

Sample No.

15399

From

104.75

To

107.00

Length (M)

2.25

Nl PPM

26

i

cuPPM

71

AG PPB

-

AU PPB

-

Sample Description j

SW-95-5

Page 4 of 4

Metres From

137.00

139.00

To

139.00

152.00

152.00

Description

Granite, dyke was probably original lamprophyre, fine pinpoints Pyrite.

From 127 to 129m, zone of red saturation, alteration, epidote permeates every amphibole and rims margins.

Peridotite, very fine grain, dark green, homogeneous, contacts at 45" contacts very sharp (no apparent effect on Granite), margin of peridotite of finer grain, fractured brittle, blocky, laced with pink and white carbonate, minute pinpoints Pyrite. Random rare chalcopyrite.

137.0 - 139.0, very brittle with abundant micro fractures.

Pink Granite, unusual pink, coarse grain Granite, no extraordi nary features, local areas, pink hematitic alteration, usually diffused out wards from joints, coarse grain 148m to 149. Zone of red saturation 151 .50 - 152.

End of Hole

Sample No.

15395

From

137.00

To

139.00

Length (M)

2.00

Nl PPM

27

cuPPM

54

AG PPB

-

AU PPB

-

Sample Description


Logged by^^x^ ^^//'/y^^^W. Oilman


Grid Coordinate Easting 1625E, Northing 1275N Elevation: Surface Bearing: N1800 T Dip at Collar: -50

Depth

Dip Tests

Dip^—^ Corr. Dip


SW-95-06 Akweskwa Grid P1203708 BQNovember 11/95 November 12/95

Logged by: W. Gilman Drilled by: Norex Total Depth of Hole: 155.00 Date Logged: November 30, 1995Meters ~ — -! - i: — ~ From

0.00

20.00

|

To20.00

144.35

Description

Overburden. 60cm, small ground pebbles of great variety fromaplite to amphibolite, rock in sandy overburden transportedover great distance, 1 fragment of 15cm very fine grain andsite indicates no significant boulders as indicators.

Olivine Diabase. Coarse grain grey diabase with ophitic texture,intergrowth of pyroxene and grey basic plagioclase withaccessory magnetite and ilmenite and leucoxene, skeletalleucoxene intergrown with ilmenite, great homogeneity, welljointed with black film on joints (probable melange of hematite,manganese, chlorite?) Probable hypersthene amongpyroxene, bronzite only identifiable with petrographic stedly,disseminated uniform fine Pyrite, clustered Pyrite on joints to.5m m, differential movement along all joints, some rare

ultra-saturated highly feldspathic patches (common in diabasedykes and sills) called pegmatitic phase eg. 39m from about130m grain size gradually diminishes until medium grainbecomes nearly very fine grain at lower contact, very finebronzy Pyrite, Pyrrhotite increases gradually toward lowercontact. Contact very sharp and abrupt with large Feldsparsappear cut by knife some isolated granular green patches onlyof intrusive later injection into Granite.stringers of medium graingranite invade diabase contact, appear to have remobilizedand invaded diabase after the intrusion.N.B. It is an old mystery as to high heat injection has little effecton low minerals temperature of Granite.

Sample No.

From To Length (M)

Nl PPM

CD PPM

i

AG PPB

AU PPB

Sample Description

SW-95-6Page 2 of 2

Meters From

20.00

144.35

To

144.35

155.00

155.00

Description

20.0 - 22.0 coarse magnetite, bronzite, very rare Pyrite39.0 - 40.0, pegmatitic phase, very coarse grain, large Feldsparntimately fractured.73.0-74.50, short pegmatitic phase, 1 0Xo Pyrite on rims Feldsparrare pinpoints Pyrite.125.0 - 127.0, coarse grain pegmatite phase, classic ophitic

texture, rare sulphides.

Sample No.

1548615487

15488

15489

133.0 - 135.0, medium grain homogeneous, bronzite, pinpoints 15490sulphides essentially devoid of any suggestion of orepossibilities.137.0-140.0 persistent medium grain approaching lower

contact, contents remain uniform, homogeneous.fine pointssulphides.

Olivine diabase. Strange condition that olivine proper cannot beidentified with hand lense.this is well known olivine diabaseand will continue to be called that but the primary accessoryappears to be absent or very small.

142.0-143.0, sporadic clustered Pyrite in medium grainedphase, bronzite.

143.0-144.35, fine grain lower contact, pinpoints Pyrite,chalcopyrite

Pink coarse grain Granite, unaffected by contact with olivinediabase, except for reddening of matrix for 2 meters fromcontact, hematitic alteration, fractured diabase at contactinvaded by stringers of medium grain Granite. Granite is ahomogeneous intergrowth of coarse quartz, pink Feldspar,amphibole, some epidote on crystal margins, (Granite is amultiple or pulsing injection) fine pinpoints Pyrite.

End of Hole

15491

15492

15493

e.g.. large euhedral Feldspar rimmed by finer Granite as laterstage injection.

From

20.0039.00

73.00

125.00

133.00

137.00

142.00

143.00

To

22.0040.00

74.50

127.00

135.00

140.00

143.00

144.35

Length (M)

2.001.00

1.50

2.00

2.00

3.00

1.00

1.35

Nl PPM

CU PPM

AG PPB

AU PPB

l

Sample Description


-^S^" Js/Logged by: Ss^jst* A^/ffTrtrrtWarren Gilman

M g P __—S-—K- Q-?i^~~?r *T

1203

—±^:W^IL I.WEoNgarninq Twp

Summary of D rill Hole dejlpiaclon

Lg95-CrM CouidiiiitBi Ailmuiii DIP txasnt

SW-95-01

SW-95-02

SW-95-03

SW-95-O4

SW-95-05

5W-9S-06

HZ5 East/ l 4SO North

2 1 OO East/ l l 50 Ncnh

2116 tait/ 1 1 36 Nor*

2375 East/ 1325 North

2675 EJSC/ 14OO North

1625 East/ 1 275 Nonti

Good Gravel Road

Old Haulage Road

1995 DDH Road

DDH Location 6c Azimuth

DRIVER RESOURCES lac.

Sewell oc Kenogaming Townships NTS: 42-A 7 SW Porcupine MWng Dwsion

Ministry of Declaration of Assessment WorkNorthern Development —--j . .., . . jand Mines ^ Performed on Mining LandMining Act, Subsection 65(2) and 66(3), R.S.0.1990

Transaction Number (office use)'Assessment Res Research Imaging

Personal information Mining Act, the infori Questions about th

nn this form is obtained under the authority of subsections 65(2) and 66(3) of the Mining Act. Under section 8 of thev work and correspond with the mining land holder. f Northern Development and Mines, 6th Floor,

SA d t : •••'V" ,:" ; :

900 claim, use form 0240.^AMNVWTO 2. 17S04 SEWELL

Recoded holder(s) ^Attach a list ifi irWr- "^ — ——11.1 ——— — ————— — — ——— -' ''"" "l" i" ' " '

2. Type of work performed: Check ( ^ ) and report on only ONE of the following groups for this declaration.Geotechnical: prospecting, surveys, assays and work under section 18 (regs)

no/ Physical: drilling, stripping, j k-Hrenching and associated assays Q Rehabilitation

Work Type H, Office Use* :.--Commodity/' * :— . *... , , ,- .^.,., -. .f. . V.i,*-,.-^ V' - - '"- -

Total S Value of Work Claimed

DaytO .

| Month | Yev Dty | MoMli | YewNTS Reference.l

Global Positioning System Data (if available) Township/AreaMining Division

M or Q-Ptan Number' " ' Resident Geologist District

Please remember to: - obtain a work permit from trie Ministry of Natural Resources as required;- provide proper notice to surface rights holders before starting work;- complete and attach a Statement of Costs, form 0212; "- provide a map showing contiguous mining lands that are linked for assigning work;- include two copies of your technical report. ..

3. Person or companies who prepared the technical report (Attach a list if necessary)Name Telephone Number

Fax Number

Name Telephone Number

Fax lumber :~Address

Name Telephone Numberajus ea o? aAddress Fax Number

4. Certification by Recorded Holder or Agent

l,(Print Name)

or after its completion and, to the best of my knowledge, the annexed

, do hereby certify that l have personal knowledge of the facts set

duringforth in this Declaration of Assessment Work having caused the work tp be performed or witnessed the same dunireport f^true,B':r^tVs-i"' '' ' r^?: - ,*.

Signature of Recorded Holder or Agent s V Date .' i i J

's Address n Telephone Number Fax Number

0241 (02/96)

5. Work to be recorded and distributed. the'minincj land where work was performed, must accompany this form. -

Work, pan only be assigned to claims that are contiguous (adjoining) Jto^~at the time work*wiis peffolrrned. A map showing the coritiguolisflrtkiW:. r^inm em fcstfdfetvv-?. " v ^.,ws ,u- -" -***v V. vv

Mining Claim Number. Or if work was done on other eligible mining land, show in this column the location number indicated on the claim map.

Number of Claim Units. For other mining land, list hectares.

Value of work performed on this claim or other . mining land. :

Value of work applied to this claim. .u;.

Value of work assigned to other mining claims, , 0

Bank. Value of work to be distributed at a futu/e date.,-^ir-";!!^,?;^"'-.-*.,1' f'*-.xS8 SUMP?.'. X

eg TB 7827 16 ha S26, 825 N/A S24,000 S2,825

eg 12 ^24,000T2—J- * W,

f"m tci oq^ :^-r '"eg S 8, 892 S 4,000

120370"?

y//2037/3 ^^ GC

10

11

12 f\VI.

13

149*

OS

15

Column Totals

do hereby certify that the above work credits are eligible underf,1 * ift'sirVi^ sns f;f'-' 'i.i'i - -. .v. ;, iiasteo * .o"* ••;*ci;ut- v-: ",-M-;.l, .^^—^^—^^^-^^— (Print Full Name)

subsection 7 (1) of the Assessment Work Regulation 6/96 for assignment to contiguous claims or for application to the claim where the work was done.Signature of Recorded Holder or Agent Authorized in Writing

6. Instructions for cutting back credits that are not approved. -.ft

Some of the credits claimed in this declaration may be cut back. Please check ( ^ ) in the boxes below to show how you wish to prioritize the deletion of credits: ~* ,' V - . , A i T;

1. Credits are to be cut back from the Bank first, followed by option 2 or 3 or 4 as indicated. O 2. Credits are to be cut back starting with the claims listed last, working backwards; or CH 3. Credits are to be cut back equally over all claims listed in this declaration; or _ CD 4. Credits are to be cut back as prioritized on the attached appendix or as follows (describe):

Note: If you have not indicated how your credits are to be deleted, credits will be cut back from the Bank first, followed by option number 2 if necessary.,, , v;~"f?ft c. S /^\ js

For Office Use OnDeemed Approved Date Date Notification Sent

/V^*.. ft'

Received Stamp

0241 (02/96)

20 19976 farr frJ PORCUPINE MINING DIVISION

Date Approved Total Value of Credit Approved

Approved for Recording by Mining Recorder (Signature)

Ontario Ministry ofNorthern Developmentand Mines

Statement of Costs for Assessment Credit

Transaction Number (office use)

Personal Information collected on this form is obtained under the authority of subsection 6(1) of the Assessment Work Regulation 6/96. Under section 8 of the Mining Act, the information is a public record. This information will be used to review the assessment work and correspond with the mining land holder. Questions about this collection should be directed to the Chief Mining Recorder, Ministry of Northern Development and Mines, 6th Floor, 933 Ramsey Lake Road, Sudbury, Ontario, P3E 6B5.

Work TypeUnits of Work

Depending on the type of work, list the number of hours/days worked, metres of drilling, kilo metres of grid line, number of samples, etc.

Cost Per Unit of work

Total Cost

Associated Costs (e.g. supplies, mobilization and demobilization).

Transportation Costs

Total Value of Assessment Work

Calculations of Filing Disc

1. Work filed within two years of performance is claimed at 1000Xo of the above Total Value of Assessment Work.2. If work is filed after two years and up to five years after performance, it can only be claimed at SO'Vb of the Total

Value of Assessment Work. If this situation applies to your claims, use the calculation below:TOTAL VALUE OF ASSESSMENT WORK x 0 .50 Total S value of worked claimed.

Note:- Work older than 5 years is not eligible for credit.- A recorded holder may be required to verify expenditures claimed in this statement of costs within 45 days of a request for verification and/or correction/clarification. If verification and/or correction/clarification is not made, theMinister may reject all or part of the assessment work submitted.

Certification verifying costs:

l, , do hereby certify, that the amounts shown are as accurate as may(please print full name)

reasonably be determined and the costs were incurred while conducting assessment work on the lands indicated on

the accompanying Declaration of Work form as

to make this certification.(recorded jToldat. aqeni. or state company position with signing authority)

l am authorized

0212(02/96)

Signature Date

Ministry ofNorthern Developmentand Mines

Ministers du Developpement du Nord et des Mines Ontario

November 18, 1997

MICHEL GEORGE CARON 99 BRUCE P.O. BOX 362 SOUTH PORCUPINE, Ontario PON-1HO

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

Telephone: (888)415-9846 Fax: (705) 670-5863

Dear Sir or Madam:

Subject: Transaction Number(s):

Submission Number: 2 .17804

StatusW9760.00578 Deemed Approval

We have reviewed your Assessment Work submission with the above noted Transaction Number(s). The attached summary page(s) indicate the results of the review. WE RECOMMEND YOU READ THIS SUMMARY FOR THE DETAILS PERTAINING TO YOUR ASSESSMENT WORK.

If the status for a transaction is a 45 Day Notice, the summary will outline the reasons for the notice, and any steps you can take to remedy deficiencies. The 90-day deemed approval provision, subsection 6(7) of the Assessment Work Regulation, will no longer be in effect for assessment work which has received a 45 Day Notice.

Please note any revisions must be submitted in DUPLICATE to the Geoscience Assessment Office, by the response date on the summary.

If you have any questions regarding this correspondence, please contact Lucille Jerome by e-mail at [email protected] or by telephone at (705) 670-5858.

Yours sincerely,

ORIGINAL SIGNED BYBlair KiteSupervisor, Geoscience Assessment OfficeMining Lands Section

Correspondence ID: 11571

Copy for: Assessment Library

Work Report Assessment Results

Submission Number: 2 .17804

Date Correspondence Sent: November 18, 1997 AssessonLucille Jerome

Transaction NumberW9760.00578

Section:16 Drilling PDRILL

First Claim Number1203708

Township(s) l Area(s)SEWELL

StatusDeemed Approval

Approval Date

September 18,1997

Correspondence to:Resident Geologist South Porcupine, ON

Assessment Files Library Sudbury, ON

Recorded Holder(s) and/or Agent(s):MICHEL GEORGE CARON SOUTH PORCUPINE, Ontario

Page: 1Correspondence ID: 11571

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