31M04SW0117 11 RIDDELL 010

Diamond Drilling

Township of Riddell Report NQ: 11

Work performed by: Goidex Mines Ltd.

Claim N9

L 317218

L 296696

Hole NO Footage DateG-l-72 G-2-72

G-3-72

748' 701'

865'

Aug/72 Sept/72

Sept/72

Note

(D (D

(D

Notes:

(1) 87/73

.004(T- 63) rev. 9- T2

oOQLDKK MDBS UMINE*

Report covering the diamond drill prograa ea the 30 dal* group in Riddel Tovnahip, Tavagaol Area, Ontario. During the period Auxaet aaft September 1972*

Addreas of Claim Owner* Page l

Locality l

Accciiibility l

Terrain d Vegetation l

O Oeneral and Economic Oeologjr l

Diamond Drill Program ft

Conclusions S

MAPS AOCOMPAiYOiQ THIS

Map No. l Surface geologjr and dianond drill hole looationa

Map No. X Diejiond drill holt ieotiont

REPORT ON BOULTON LAKE OLAD6, RIDDSL TOWNSHIP, TEMAOAMI ARIA, ONTARIO,

ADDRESS OF CLAIM OWNERS

Ooldox Minet Limited, Aulte 300-ttS Bay itreet, Toronto, Ontario,

LOCALITY

The group comprises SO contiguous claims in Riddel Township, Ontario* The claims are situated If miles southeast of Temagami Tevnslte and Boulton Lake lies almost wholly within the area of this claim group*

Claim Not. are 396696 to 296T08 inclusive (IS claims) and HttOS to nmo inclusive (1ft claims)

The dal* group may bo reached by light aircraft fro* Temagami, flying tine 10 minute* or bjr boat via Snake Lake and Cassel e Lake and by a li nile bush road from Cassels Lake to Boulton Lake. The diamond drill equipment was barged by water and hauled over the both road to the site of drill li*.

TERRAIN AUD VEOETATIOM

The eurfaoe elevatione vary rapidly between 1,000 foot and 1.150 feet above eea level on the eastern half of the group, while the western half of the area ia relatively flat lying, the f round ia thickly wooded by trees of spruce, Jack pine and birch.

The northern l /S of the claim group it overlain by Nipissing Diabase while the southern 1/3. by conglomerates of the Coltman Formation* A small patch of "slate-like-^greywecke" overlies the conglomerates on the east shore of Boulton Lake. The strike of the bedding ia northwest and dips IS** to 200 to the northeast.

On the east shore of Boulton Lake a prospect pit vat excavated at the foot of a cliff, in the face of which it a li* to IS* calcite breccia cone. The strike of this break, with aa atimuth of tt 0 and dip 800 H, has been followed eastward on surface by a trench and shallow pitt for 200'. 460 feet east of the main pit the taat break may bo toon in

a second cliff on the opposite side of a small valley where the "elate* like-Kreywacke" is fractured and calcite stringers art visible but without significant mineralization.

The breccia tone on which the pit was sunk it a strong structure but other than weak chalcopyrite and pyrite mineralisation no othor mineralisation of significance was observed. Vein material assayed tract of silver.

- 2 -

DIAMOND PRILL PROGRAM

Throe AxTcore diamond drill holts wort drilled for a totalfootage of 2,314 feet.

Hole* Ho, l and Ho. 2 are located on elaU 1117*18,

Hole No. l waa collared 416 foot north of It port and lil footeast of tho eaat boundary*

Hole Mo. 2 vat collared IK foot north of la poat and 1W footoast of the east boundary*

Hole No. 3 it located on claim 296696 mi Cellared 498 foot south of li post and 123 foot oast of the oast boundary,

The First drill hole was trilled, on an asiauth of 10** and dip at collar of -470, to out tho structure soon in tho prospect pit 220 feet down dip beneath tho pit. A weak 3/4" pink calcite structure was cut in the target area. Tho hole was continued beneath tho lake to 748'.

The second hole was drilled to intereseot the same structure 300 feet down dip from surface and 350 fotrt eastward along strike fro* the first hole. A 4" calcite breccia tone with quarts was cut in the target area. (This breccia tone maybe a flat lying structure) No'; mineralisation was noted. The length of the hole is 701 foot*

The third hole, collared 2.166* northwest of tho first holt and drilled on an asinuth of 300* and dip of -80*. Tho objectives wort to determine the attitude of tho Nipissing diabase sill, tho type of underlying basement rook and tho significance of gullies and degressions seen on surface at depth.

The hole collared in Nipissing diabase out the lower oontact at 510 feet and continued in greywacke, pebble greywacke and conglomerate bods to 865* when the hole was stopped in a break filled with sand. No veins were encountered and the baatatnt rode typo was not penetrated.

CONCLUSIONS

The break on which tho pitting and tronohing was carried out in the original prospect appears to bo well developed in tho vloinity of the contact with the Nipissing diabase sill but beoonos loss well defined in depth below the contact, so that it was difficult to recognise in the core*

CONCLUSIONS COOT'D

The attitude of the diabase is a at lying, thus the linn of the diabase rock type in this area as portrayed onO.D.M, aap |34b by A.O. Burrows are probably all lower contact. Whether the basement rook type is volcanic or granite was not detendned.

Further drilling on the break tested by this exploration progran is not expected to be beneficial, since theekreajc is thought to post date the diabase intrusive and probably developed as a result of the intrusion and further, the area aost favoured for Mineralisation is adjacent to the Nipissing diabase contact which in this area has been eroded away.

B, K. Thomiley, P, Bm., Cobalt, Ontario*

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ram

DIAMOND DRILL RECORDPROPERTY

SHEET NOMMt.

LATITUDE. ..

DEPAtTUKE .. . .

ELEVATION

SECTION FftOM

DATUM .

•EAKING

..DIP........ ........,...

TO

HOLE No.

..STARTED

COMPLETED

ULTIMATE DEPTH.

PKOPOSED DEPTH

DIAMOND DRILL 1TECORDt.PROWY

SHCET HUM

LATITUDE

DEPARTURE

EIEVATION

..SKTION FROM. TO

HOLE No,

STARTED

•3; -

..DATUM ......................................,.... .....,.......... ,.,,...., .................., ........ COMPUTED

..MAKING..

..DIP.... .....

ULTIMATE DEPTH

PROPOSED DEPTH

DCPTH FEET

567-

FORMATION

- -

^ S j.

D k?

r \TV', "^

SAMPLE NO.

^ V-yJv^.

•T-O*-, rv

-

FROM TO WIDTH

t .V

MINK* rO*M *O9 N IV./S4

ASSAY VALUES

DIAMOND DRILL RECORDPROPEF

SHEET NUMBER

LATITUDE .........

DEPARTURE ......

DATE .................

HOLE No.

.F/W TO COL. IN FT.

..COLLAR EL. ...............

..AZIMUTH ........................................

.DIP ............................ CORE TYPE.

LEVEL ..........,

WORK PLACE

DEPTH ...........,

HORIZ. PROJ.

DEPTH FEET

~ L'' O

ROCK TYPE

Ca) ^T 8 2 '

-' o r\6cy*-\ C

-^w

6/ ? -

G*

.rtMJO l———^

Sample No.

ASSAY VALUES

From To . Width Ozs. Ag. per Ton

SIGNED

''A '

DIAMOND DRILL RECORDPROPE

SHEET NUMBER

LATITUDE ........

DEPARTURE .....

DATE

HOLE No.

.F/W TO COL. IN FT. ............,.......................................... LEVEL

..COLLAR EL ....................................................,................... WORK PLACE ....

..AZIMUTH ..................................................................;......... DEPTH ................

.DIP ............................ CORE TYPE.................................... HORIZ. PROJ. ....

Cassels Twp.l ,M

I7M

I6M

l? Ml W

Askin Twp200

ci

cu

32LU

THE TOWNSHIP OF

RIDDELLDISTRICT OF

NIPISSING

LARDER LAKE MINING DIVISION

SCALE:1-INCH-4O CHAINS

LEGEND

PATENTED LANDCROWN LAND SALELEASESLOCATED LANDLICENSE OF OCCUPATIONMINING RIGHTS ONLYSURFACE RIGHTS ONLYROADSIMPROVED ROADSKING'S HIGHWAYSRAILWAYSPOWER LINESMARSH OR MUSKEGMINESCANCELLED

NOTES

This Twp Lies Within The

TIMAGAMI PROVINCIAL FOREST

4Q0 1 Surface Rights Reservation around all Lakes and Rivers.

Flooding Rights on Rabbit Lake to contour 5' LO. 1597- File 1165

Ball a st P its o Jo rg On l Noii(;:and Ra l i way chy Order- In-Ccuncil 24 Jar '906 File- 3170/06

•ri

PLAN NO.-M. 578DEPARTMENT OF MINES

— ONTARIO —

Str

ath

y T

wp.

M.5

96

Q

5 CL Q.

CD "O CJl

-J

00

CD CD CO H

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296701 BOUUTON

LEGEND

NIPISSING DIABASE SLATE LIKE GREYWACKE CONGLOMERATES KEEWATIN ROCK TYPES CALCITE STRUCTURES

}

SYMBOLS

CLAIM LINES

BUSH ROADS

LAKES

SWAMP

TOPOGRAPHIC CONTOURS

DIAMOND DRILL HOLES

DO TRAILS

AREA MAP

LAKETIMISKAMING

31M045W0117 11 RIDDELL 230

SUDBURY

GOLDEX* PROPERTY

'WORTHBAY

81

SCALE- I^

GOLDEX MINES LIMITED

TORONTO—ONTARIO

PLAN

LOCATION

SCALE

DATE

MAP No.

SURFACE GEOLOGY ft D.O.HOLES

BOULTON LAKE-RIDDELL TW'P

l 10,000 or l11 -* 833'

AUGUST — 1972

r

BOULTON LAKE

HOLE-G-l-72 DIP - 47 0 (ColIar) AZM. - 209 0 Compass

OVERBURDEN

CONGLOMERATE

a

HOLE- G-2-72 , DIP -60 0 (Collar)

AZM. - I15 0 Compass STREAM BED

lPORTAGE

CLIFF OF BEDDEDGREYWACKE

U R F A C E

VERTICAL SECTION

THROUGH D.D.H. G-i-72

GREYWACKE

BADLY BROKEN

GROUND-CEMENTED

-o- PEBBLE GREYWACKE

3/4" RED-PINK- WHITE CALCITE

PEBBLE GREYWACKE

/GREYWACKE

-— O ——o — ,. PEBBLE GREYWACKE

HOLE- G-3-72DIP - 80'yfiP (Collar)AZM. - 305 0 Compass

OVERBURDEN

GREYWACKE

748

VERTICAL SECTION

THROUGH DO H G-3-72

DIABASESEOIMENT-X^^-CONTACT \\MUO SEAM WITH

\ l" r A i PtTCl CALCITE

VERTICAL SECTION

THROUGH

l

R O F l L E

69

D.D.H. G-2-72

^ X

^SLIPS WITH

HEMATITE STAIN

ZONE OF. CALCITE STRtNGERSV 6*

4"BRECCIA ZONE WITH QUARTZ MATftTx NO MAJOR CALCITE STRUCTURE

N TARGET AREA

PLAN OF RELATIONSHIP OF G -i-72 T O G-2-72

AND MAIN SURFACE FEATURES

COLLARCOLLAR ELEV'S G l"72

V 2i' ABOVE LAKE WATER LEVEL

COLLAR G 3-72

\r A

VEIN S TRUCTURE -200'

25 V ERTICAL. DROP TO LAKE

B O U L TO N

LAKE

-\v \ o

MAJOR BREAK t-160) ^ ^ vx ^ ^^.\ -9,

VEIN STRUCTURE - 220*

A'

\\/\

\

\ •^ ^\

FRACTURED Z ONE

6 WIDE- VUGGY-WlTH

CALCITE S TRINGERS

N.V. M.

701'

VERTICAL SECTIONl"-l MILE

ti-flLba.sC- I A PPROX. 500

SECTION PERTAINING TO AREA ON MAP l /r

^•C\\O**.Gf0.'-

VERTICAL SECTION ON LINE A-B BEING PART OF MAP No.34BACCOMPANYING REPORTS BY E.W.TODD - O.D.M, REPORT XXXIV— PART 3, 1925,

73

CONGLOMERATE BED

GOLDEX MINES LIMITED

TORONTO-ONTARIO

PLAN

LOCATION

SCALE

DATE

SAND -f CAVE 868' MAP No

D.D.HOLE SECTIONS AND PLANS

BOULTON LAKE- RIDDELL TW'P50'

AUGUST-1972

31M04SW0117 1 l RIDDELL 230