louis 010 REPORT ON PROPERTY CHESTER, BENNEWEIS AND ST ... · Apper lix "B". Hill, Goettler, De Laporte Limited accepted the materi al si imitted as factual, excepting some discrepancies

41P1PSW000? C3.4370 SI. louis 010

REPORT ON

MURGOLD RESOURCES INC.

PROPERTY

CHESTER, BENNEWEIS AND ST. LOUIS TOWNSHIPS

PORCUPINE MINING DIVISION ONTARIO

November 1983

Prepared by

HILL, GOETTLER, DE LAPORTE LIMITED Suite 904, 80 Richmond Street West

Toronto, Ontario, M5H 2C7 (416) 362-1474

ll l l lll l llll l l llll

t1Pl?SW000? 63.1370 ST. lOUl S

TABLE OF CONTENTS

SUMMA Y

INTRO UCTION

PROPK TY

Loc tion and AccessI.oc tion Map No. 3CI a .msTop graphy, Climate and Local Resources

H1STC :Y OF PREVIOUS WORK

GENEP J, GEOLOGY

Ger ;ral GeoJogy Map No. 2

ECONC I1C GEOLOGY

GEOPlt 'S3CS

CONCI IS10NS

RECOt 1ENDAT10NS

APPENDICES

Appei iix "A" - Recommended Diamond Drilling

Appei 3ix "B" - Data Reviewed

PAGE

l

3

4

A567

8

11

13

14

24

25

26

30

31

010C

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SUMMi X

Murgo]d Resources Inc. holds a group of 296 contiquous

claii 5 in Chester, Benneweis arid St. Louis Townships, Porcupine Mining

Divii ion of Ontario. This property lies 10 miles southwest of Gogama,

Onta: lo.

Fairly extensive field investigations including underground

deve. jpment, diamond drilling and trenching have been carried out

inte: nittently by various interests since 1931.

Gold, the on.ly mineral of economic interest yet found on the

propi rty, occurs associated with narrow quartz veins and stringers

whicl occupy portions of narrow, long, through-going shear fracture

zone; which traverse the property.

From 1979 on Murgold Resources Ltd. has undertaken an

exp^ ration programme over this claim group. These investigations

incli le geological mapping, extensive stripping, trenching,

geopl ?sical surveys, diamond drilling arid the taking of a 656 t on

undei ground bulk sample. The weighted average of this bulk sample is

repoi redly 0.34 oz. Au/ton.

Of the 8 shear zone structures seen by the writer, 2 in

part: :ular have indicated by diamond drilling and/or trenching inter-

estii * values in gold. These areas of considered interest are the

cent) jl and western portion of the No. 3 zone and the eastern exten

sion )f the No. l zone.

A diamond drill programme of approximately 8,500 ft. is

here: i recommended to further investigate these zones of interest. In

12.

Page 2.

lil addil Ion a moderate scale geochemical survey over some of the VLF-EM

indie ated conductors is also recommended.

The estimated cost of these recommended programmes is

l $300. )00.

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Page 3.

J NJTRC HJCTKJN

Hill, Goettler, De Laporte Limited was retained by Murgold

Resoi -ces Inc. to undertake a review of their gold prospect located in

Chest ;r, Benneweis and St. Louis Townships, Porcupine Mining Division,

Ontai .o.

The data reviewed as a base for this study is listed in

Apper lix "B". Hill, Goettler, De Laporte Limited accepted the materi

al si imitted as factual, excepting some discrepancies in the location

of se ne old diamond drill holes. A short field examination was made

of t e various showings on October 20th, 1983 by N. Firth in the

comps ty of D. Hoy, Murgold's field geologist.

This report covers the results of the review undertaken.

Page 4.

PRpPE: IT

1 .oca t jn and Access (Map 1)

The property is located in Chester, Benneweis and St. Louis

Towns! ips, Porcupine Mining Division, Ontario. More specifically the

claim; are approximately centred at 47 0 33'N, 81 0 51'E (N.T.S. 41-P-12)

some 3 miles southwest of the town of Gogama, Ontario.

Access to the property is very good as Highway 144, a paved,

2 lair road between Sudbury and Timmins, bisects the claims. To reach

the M rgold Resources camp one drives 6.6 miles past the junction of

llighw, ys 144 and 560 to the Mesomikenda Lake road. Turning left it is

1.2 m les along this good gravel road to the turn off for the camp.

One t en goes for 1.9 miles over a rough bush road to the camp site on

paten ed claims S20009.

Page 5.

46 0 00'

48*00'

- 470 00'

-460 00'

Murgolol property

Moinly \ (Iconic ond Sedimen ary rocks

.SCALE

l Inch * 25 MilesO 5 10 IS 20 25 50 Mi


LOCATION MAP

HILL,GOETTLER, DE LAPORTE LTD.TORONTO CANADA

OCT 1983

MAP-NO, i

Page 6,

Claln

The property reportedly consists of 296 claims in a conti

guous block.

These claims are as follows.

CLAIM NO.

S l 99 S 2 00 SI 21 P4 71 PA 7 3 P515 P51 f) P515 P538 P538 P538 P539 P539 P539 P539 P538 P539 P539 P507 P528 P543 P543 P543 P548 P546 P549 P549 P549

2 (patented) 9 (patented) 94 (lease) 52-471958 in 67-473746 in 48-515059 in 28-515330 in 35-515336 in 55-538059 in 8285-538089 in 05-539129 in 36-539155 in 79-539298 in 08-539328 in 23-538525 in 04-539421 in 81-539183 in 67-507669 in 8018-543824 in 2793-543996 in 9280-547000 in 01-549019 in 08-549117 in 94

TOTAL

NO. OF CLAIMS

111

elusive 7elusive 80elusive 12elusive 3elusive 2elusive 5

1elusive 5elusive 25elusive 20elusive 20elusive 21elusive 3elusive 18elusive 3elusive 3

1elusive 7

1elusive 4

1elusive 21elusive 19elusive 10

1

296

TOWNSHIP

ChesterChesterChesterChester

Chester S BenneweisChesterChesterChesterChesterChesterChester

Chester S BenneweisBenneweisBenneweisBenneweisBenneweisBenneweisSt. LouisSt. LouisChesterChesterChesterChesterChesterChesterChesterChesterChester

Titles and rights of these claims were not verified by the

write with the Mining Recorder in Timmins.

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Page 7.

-C2Po i raphy, Climate and Local Resources

The area is relatively high ( 1,300 ft. above sea level)

beinj near the height-of--land between James Bay and the Great Lakes.

The opography of the area is typical of the Canadian shield pene-

plair , that is the land surface consists of rolling hills and ridges

whicl: , with minor exceptions rise not more than 100 ft. or so. The

area under consideration is forested with a fairly dense growth of

sprue !, jack pine, balsam, birch and poplar.

The climate is characteristic of Northern Ontario, with long

cold ?inters (up to -40 0 C) and short summers ( 30 0 C). Heavy snow is

commc i in the winter.

There is no sign of logging taking place in the immediate

area j with the only resource being hunting and fishing.

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Page 8.

'Y OF PREVIOUS WORK

Gold was first discovered in Chester Township in 1930 on the

east shore of Three Duck Lakes. This discovery led to more intensive

searc i in 1931 which located other gold bearing quartz veins, chiefly

in tl ; environs of Three Duck Lakes and Clara Lake.

Since then in Chester Township 6 prospects and 11 occur

rence ; of gold have been found and briefly reported on (Mineral

Depoi .t Circular 18). Three of the prospects are located within the

Murgc .d claim group, these being the Kingbridge (Gomak) , Strathmore,

and eaverbridge prospects. There are no known gold showings in

Benn* ?eis or St. Louis Townships.

Since the initial discoveries there have been fairly exten

sive, though cyclic, investigations carried out within the claim group

area. This work was principally in 3 areas, the. Kingbridge (Gomak)

whicl relates to the Murgold No. l zone, the Strathmore which relates

to tl ; east end of the Murgold No. 3 zone, and at the west end of the

No. ; zone.

In essence the first work was undertaken in the 1 930 's by

Goma( ; Mines Ltd. on the No, l zone and by Strathy Basin Mines Limited

on tl ? No. 3 zone. From 1932 through 1938 Gomac.k M. L. did extensive

diaim id drilling, trenching and sank a 65" inclined shaft to a depth

of 8 ft., from which 215 ft. of drifting was done on the 65 ft.

level . Some 98 oz. of gold from 1,387 tons of ore was apparently

prodi :ed at this time. In the same period of time Strathy Basin Mines

Ltd. carried out exploration at the east end of the No. 3 zone. In

1937 a 116 ft. inclined shaft was sunk to the 100 ft. level and

286 j :. of development work was carried out. Channel sampling on this

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Page 9.

level returned the following uncut values; for 95 ft. east of the

shaft 0.30 oz. Au/ton over an average width of 3.13 ft., and for 120

ft. v st of the shaft 0.89 oz. Au/ton over an average width of 2.6 ft.

The next known investigations were carried out by Chesgo

Mines Limited from 1945 through 1948. This work was apparently mainly

diamc id drilling of which 8,000 ft. was completed along with some

strip ling and trenching. Of this drilling 3 holes totalling 512 ft.

were it the Strathmore portion of the No. 3 zone and 16 holes total

ling 1,785 ft. were at the west end of the No. 3 zone. It is not

knowr for sure where the rest of the drilling was undertaken, though

likel - at the Gomack (No. l zone) location. The logs for these drill

holes are very brief and there appears to be little correlation

betwe :n the sampling and the rock descriptions given. Murgold

Resoi 'ces Ltd. found and surveyed in 3 of the Chesgo drill holes so

that :he locations can now be plotted more accurately than has been

the c ise when the initial maps and sections were made.

]n 1963 the Icon Syndicate (Kerr Addison Mines Ltd., Newmont

Miriir ; Corp., Gunnar Mines and Rayrock Mines) optioned the Strathmore

showi lg (Rinaldi Option) and completed A diamond drill holes totalling

],24( ft. at this location. The results obtained from their assaying

were rery low.

From 1970 through 1975 Kingbridge Mines Ltd, in conjunction

with Olympian International Resources carried out an exploration

prog] imme which included geophysical surveys, bulk sampling, and

diamc id drilling. This work was apparently concentrated on the

cent] il portion of the No. l zone and the west end of the No. 3 zone.

/10,

ll Page 10.

l From 1979 to the present, Murgold Resources Inc. has carried

out a fairly extensive exploration programme. This includes bulldozer

l strip ing of large areas, trenching, diamond drilling, VLF-EM surveys,

soil eochemistry and geological mapping.

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The area under review is at the eastern extension of the

Swaze -Ridout greenstone belt. This belt has been cut off in part by

an i trusion of granite to diorite composition which occupies the

great :r part of Benneweis and a large part of central Chester Town

ships

The northern fringe of the claim group is underlain by a

thin ?and of east-west striking metasediments, principally greywacke

in cc iposition with some minor conglomerate sections. A second, small

zone if metasediments lies around Benneweis Lake.

There is only minor Keewatin type basic volcanics within the

genex .1 claim area, this consisting of a mile and a half long area,

strad .ling the Chester-Benneweis boundary south-west of Benneweis

Lake.

The majority of the claims are underlain by what Laird in

his i ;port calls the "Younger Granite". This intrusive has a number

of va iations ranging from alaskite granite, granodiorite and diorite.

As Le .rd states "field observations seem to indicate that the grano-

diori e, granite and alaskite are contemporaneous, and that they

repre ent differentiation phases of the same granite magma". All of

the a ove rock types are cut by Keeweenawan diabase dikes.

Gold is the principal economic mineral found in the area to

date. The main showings of gold occur within the granitic intrusive.

The g Id occurs in its native state in narrow quartz veins associated

with arrow, throughgoing shear zones. The majority of the fractures

strik in a direction a few degrees south of east and in general they

712.

Page 12,

show regional parallelism. Though the shears appear to be persis

tent n length the quartz veining is erratic along strike, pinching

and s 'el l ing and in part is completely absent. Pyrite and chalco-

pyrit are the common accessory mineralization.

/13.

Page 13.

f - N r\ i—\---

\\

NEVILLE ITWR i

GOGAMA

xx y^v--. '/' y////-???;

S s Y S s S-*'*. S'/-t^f.'.'.'r'. -S-4 X-rA-j':'/''..' 1''"'--'.' : .^ - /. : ' i-': ', ;'j; ?':'.-!; - ".r-wl," r~- -^'—: - i. '. ' , .' ' .'. ,j.'' 1\ l*-f j x * * '* i^ '

\

i-'..' .v^

,.\'V\

^l

\

CHESTER TWR

82"OO*

fiJTl Basic ) Ultrabasic Rocks

Acid In rusive Rocks.

ST LOUIS TWR

Metosf Jiments

Basic ^ )lconic Rocks

-——'Fault (i ssumed) N

Bound* 'y of Claim Group

H^ Kingbf jge(Gomock)

\2 S trath! ore SCALE

l Inch - 2 Miles l 2 4 Ml.


GENERAL GEOLOGY

H!LL,GOETTLER, DE LAPORTE LTD.TORONTO CANADA

OCT. 1963

GEOLOGY FROM O.D.M. MAP No. P. 151

MAP-2.

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Go]d is the only mineral of economic importance as yet found

on t Ir s Murgold property, though copper mineralization is often present

as at accessory mineral in the various showings. The gold occurs in

or n* ar narrow quartz veins and stringers, which occupy portions of

long, through-going shear-fracture zones. These shears are not

unifc :m along strike as they pinch and swell, increase and decrease in

inter ;ity and in places die out entirely. The most common strike

direc :ion for these shears is 110 0 -290 0 . The quartz veining asso-

ciatt l with these shears is also quite erratic in distribution,

formj lg more of a stockwork than one long vein. As such the writer

woulc call these shears and their accompanying quartz veining zones

rathe : than veins. In all 9 separate zones were seen during the trip

to tl ; property, the most important of which are considered to be the

No. ; and the No. l zones.

A synopsis of these investigations is as follows:

No.^J Shear Zone:

This zone consists of 2 to 3 narrow parallel silicified

shea: zones containing gold bearing quartz veins which vary in width

from a few inches to several feet as they pinch and swell along

st ri] s.

The zone has been traced for some 2,800 ft. along strike by

mean of surface sampling, underground investigations and diamond

dril ing. As per earlier reports, this zone can essentially be

divi' ed into 3 portions, an eastern, central and western part.

/15.

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Page

The eastern portion was investigated previously underground

(old Strathmore) and by diamond drilling. In all 21 diamond drill

holes , 7 by Murgold and 14 by other interests are located in this

sect] )n of the shear. Assays obtained by drilling are with few excep

tions quite low or negligible although the vein-shear zone is identi-

fiab: i. In 1937 an inclined shaft was sunk to 116 ft. with 286 ft. of

deve] )pment being done on the 100 ft. level. Channel sampling on the

100 t. level by Strathmore Gold Mines Ltd. returned the following

mie ut values; for a length of 95 ft. east of the shaft

0.30 )z. Au/ton over an average width of 3.13 ft. and for a length of

120 t. west of the shaft 0.89 oz. Au/ton over an average width of

2.6 i :.

Murgold dewatered these workings in 1981 and chip sampled

the ack. This sampling, over an average 3 ft. width, gave uncut

value i of 0.18 o?.. Au/ton for a 100 ft. section east of the shaft and

1.03 )z. Au/ton for a 100 ft. section west of the shaft. When a cut

to l ) oz. Au/ton was made the average in the west drift was reduced

to O, !8 oz. Au/ton. Subsequent to this sampling Murgold extended the

leve] for 100 ft. to the east and west. Channel sampling of shear

zone ilong these extensions apparently returned low values in gold.

MurgoJd then proceeded to take a 656 ton bulk sample from a

stopt developed in the better grade portion of the west drift, which

samp] ; reportedly average 0.34 oz. Au/ton. Chip channel (44) samples

taker from the back of this stope over a 3.55 ft. average width

aver* ;cd 0.69 02. Au/ton uncut and 0.58 oz. Au/ton cut.

The old trench located just west of the shaft is now

extet iively filled with debris so no examination could be made. No

/16.


Page 16,

addit .onal investigations are recommended at this time for this

l oca t .on.

The centra] portion of the vein system has been investigated

by si rface diamond drilling only, as there are no surface exposures

due l j overburden. All of the 18 drill holes in this 1,400 ft. long

sect:i in were drilled by Murgold. The shear-vein structure is readily

discs -liable through this section. Over a strike length of 500 ft. 9

drill holes returned appreciable values in gold over fairly narrow

widtt i, these being:

Hole No.

M-13 M-14 M-3 3 M-31 M-32 M-10

M-1 lM-16 M-8

These drill results are the most consistent of any drilling

under aken at the property, and therefore this section of the zone is

consl .ered as being the most promising from an exploration point of

vi ew.

Ten diamond dril] holes, totalling 2,640 ft. have been

recoin lended by the writer to further test this area to a depth of

1300 t.

UncutOz. Au j Ton

0.5540.002] .1760.3872.832.060.1921.494.080.106

Width

HU.

10.06.01.01.02.50.51 .251.51.21 .5

717.

Page 17,

The third part of the No. 3 zone, the western portion, is

indi ated over a l ength of 800 ft. It has been investigated by

tren hing and by 22 diamond drill holes, all of which were drilled

prev :)us to Murgold Resources Inc. acquiring the property. The two

trem nes known as the West Watts and East Watts were sampled by

Murgi Id, with the West Watts trench indicating a zone of 133 ft.

]engl i averaging 0.49 oz. Au/ton over an average with of 3.2 ft. and

the l ast Watts trench giving 0.203 oz. Au/ton for an average width of

3.03 :*ver a length of 80 ft. Samples taken by Murgold from two pits

sunk (etween the Watts West and East pits reportedly assayed 1.74 and

2.44 iz . Au/ton over 2 ft. The central parts of these 2 trenches were

inacc sssible to the writer due to water from recent rains. At both

ends .if the trenching the shear with the associated quartz veining

narrc 's down and dies out. There is however an indicated strike

lengt of 250 ft. at this locale.

Twenty-two diamond drill holes are located in the west end

of th zone, 16 were by Chesgo (1947), l by Kingbridge (1970) and 5 by

Olymp an (1975). Of these only 7 are in the immediate area of the

trenc ing. As Murgold Resources Inc. has found and surveyed in 3 of

the C ;esgo holes and l of the Olympian holes, the location of the

other can be placed approximately. The logs of the Chesgo Mines Ltd.

diamoi :1 drilling are very basic and lacking in detail, and it would

appea: that intercepts of interest were not sampled in their entirety.

]n 1974 Olympian International Resources forwarded 2 bulk

sampl* 5 to Noranda Mines Limited for testing. These samples from

veins l and 3A comprising 46.74 tons and 48.92 tons returned 0.172 and

0.30 c :. Au/ton respectively from estimated widths of 6 to 10 ft.

/18.

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*

Kight diamond drill holes totalling

recor oended by the writer to further investigat

Page 18

1,520 ft. have been

e this showing. Three

of tl 3se holes will be advanced far enough to cross-section the trend

of tt ; parallel No. 4 zone (vein).

No. ] Shear Zone

This zone, formerly known as the Kingbridge or Gomack

showj ig, has now been traced over a strike length of 2,500 ft. In the

centi il area of this zone, Gomack Mines Ltd. in 1935-1936 developed an

85 f . deep inclined shaft with 215 ft. of drifting at the 65 ft.

level It is reported that 1,387 tons of ore returned 98 oz. of gold

(0.05 oz./ton). A considerable amount of diamond drilling was appar-

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entl} done by Gomack Mines Ltd. and Chesgo Mines Ltd. in the vicinity

of tl i shaft but the results of this drilling

write '.

In a 200 ft. long trench, now filled

are not known to the

with debris and water,

exter ling west from the shaft, Jones ?? in 1939 averaged

2.04 iz . Au/ ton uncut over an average width of

Resot -ces Inc. in 1983 averaged 0.47 oz./ton Au

width of 2.8 ft.

In an 80 ft. trench 800 ft. east

repor :s the following assays:

Width

6.0 ft.6.0 ft.2.0 ft.0.7 ft. 4.0 ft.

1.4 ft., while Murgold

uncut over an average

of the shaft Murgold

Assay

0.271.030.0741.42 0.002

/19


Page 19,

Drill hole M-18 was drilled under this trench and encoun-

te.rec a 6 ft. section that returned 0.146 oz. Au/ton.

Two hundred and eighty ft. further east a 50 ft. trench has

been level oped on a shear containing quartz, pyrite and chalcopyrite.

Samp] Lng results here were 0.066 oz. Au/ton over 1.5 ft. and

0.54'I o z . Au/ton over 5.0 ft.

The shearing observed in these two trenches is of moderate

inter 5ity, with the quartz veining forming approximately 20% of the

zone,

Two trenches are located 900 ft. and 1,000 ft. west of the

shaft , In the first of these trenches there is moderate shearing over

a wi th of approximately 8 ft. The rock here is silicified and

conU Lns some pyrite and chalcopyrite throughout. There is only a

smal. amount of quartz as thin veinlets here. Three separate grab

samp! ?s assaying 0.2.04, 0.84 and 2.44 oz. Au/ton and one 8.0 ft. chip

chani ;1 sample of O.J19 oz. Au/ton was obtained by Murgold at this

site

The second trench is developed on a very weak shear only. A

grab sample here reportedly returned 0.75 oz. Au/ton.

Twelve diamond drill holes totalling 1,880 ft. are being

recoi nended by the writer to further evaluate the east end of this

zone from 900E to 1600E on the secondary grid baseline.

/20.

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Page 20

0

No. 4 Shear Zone:

This shear zone .lies north of and parallel to the

zone, It has been opened by 4 trenches along strike, one just

No. 3

south

of tl e new shaft collar, a second east near the location of diamond

dril] hole M- 14, and 2 small pits just north of the road near

pin ' -G. It appears as a weak shear containing intermittent

strir ;ers and lenses which are estimated to form ilC^ of the

Grab samples taken along the zone are reported to have returned

0.15! , 0.005, 0.78 and 0.12 oz. Au/ton.

survey

quartz

zone.

0.02,

No investigations are recommended by the writer for this

zone it this time.

No. 4 Shear Zone:

This shear is parallel to and lies approximately 75 ft.

sout? of the west end of the Watts trench. This not overly strong

sheai contains some irregular white glassy quartz veins. In all

probe dlity the Chesgo Mines Ltd. diamond drill holes Nos. 4, 6,

11 i itersected this trend, with the only assay of note

0.24 iz. Au/ton over 1.8 ft. from drill Hole No. 11.

7 and

being

Although this zone does not appear from indications to date

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to bc too promising it is recommended that three of the diamond drill

holes recommended for the: west portion of Zone No. 3 be extended far

enoup i to cross this shear.

/21

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Page 21

t

No. l Shear Zone:

This shear lies to the west and on

sheai , A large area, approximately 1,000 ft.

expoi ;d by bulldozing. The shear, which can be

strike of the No. 3

by 100 ft. has been

followed along strike

for onie 800 ft. varies in intensity from weak to moderate to

exisl ?nt . It pinches and swells from less than

ft. : n width. The quart?, veining is also quite

parti as minor stringers up to lenses 1 to 2 ft.

1 ft. wide to up

non-

to 5

erratic being seen in

in width and 5 t

ft, n length. There are some rusty, gossanous patches along

trem caused by minor disseminated pyrite and chalcopyrite. A

o 10

this

few

small trenches have been developed along this shear.

No additional investigations are recommended for this shear

at t l I s time.

No. ] j Shear Zone

An area of approximately 500 ft. by 100 ft. has been exposed

by M LI dozing running north-east from No. 16 shear to the access road.

No e: tensive shearing was seen in this area, rather there are a

near east -west striking, very weak fractures

cross the clearing rather than strike along i

noted, that is,

t. The outcrops

few

they

are

light -weathering intrusives with a few small slightly rusty patches on

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the s irface. Two diamond drill holes M-39 and M-40 showed no signifi

cant ninerali?.at ion. No further investigations

locat ôn.

are warranted at this

122

Page 2 2,

NO.

This ]]0 0 striking shear has been bulldozed clean along a

lengt i of approximately 800 ft. It lies north of and parallel to a

diab;; ;e dike. This shear of moderate intensity at its west end but

weakc ling to the east is approximately 2 to 3 ft. wide. As with the

othex shears seen the quartz veining associated with it is quite

irrej; ilar and overall would form 10% to 1 5Z o f the zone. There is

also a modest amount of pyrite and chalcopyrite associated with the

shear Four grab samples taken from small pits developed on its

weste -n end reportedly gave assay returns of 2.9, 3.30, 3.03 and 0.045

o?., t i /ton. Drill hole M-42 cross-cutting the shear in the vicinity

of tli ;se assays returned 0.24 oz. Au/ton over a width of 0.5 ft.

Of note at this location is the presence of a persistent

white quartz-carbonate vein l to 2 ft. in width lying approximately

20 ft north of and parallel to this shear. There is apparently no

mirier lization i.e., pyrite, chalcopyrite, associated with this vein.

]ts i tersection in the drill hole was not sampled.

No further investigations are recommended for this shear.

No. 2 JShjear JZone

This area consists of a number of weak to moderate parallel

shear that form the eastward continuation of the adjoining Chester

No. 2 zone of Kidd Resources Ltd. These shears have only very limited

quart associated with them but are in part moderately mineralized by

pyrit , chalcopyrite and pyrrhotite.

/23.

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l The adjoining Chester No. 2 zone has been extensively

invei ;igated by diamond drilling, the results of which are not known

l to t} j wri ter.

U No further investigations are recommended at this time.

m

^ A moderately strong shear 3 to 5 ft. in width is exposed on

B both ;ides of a rock cut in Highway 144.

l Within the shear is a 3 in. to 6 in. quartz vein with modest

pyrit : and chalcopyrite mineralization. Assays of 0.20 and

l 0.76 iz. Au/ton have been obtained from this site.

No further investigations are recommended at this time for

this .ocation.

J*?.aYjp 'bridge Prospect

l This prospect is a copper showing located in the north-west

porti m of the claim group at Weeduck Lake. It has been extensively

l inves :igated by geophysics and diamond drilling. No consideration was

given to this prospect during the course of the investigation.

l

l

l

l

l724.

l


Page 24,

GKOPj JS1CS

VLK-EM surveys were carried out over grids established at

Nos. l, 3, 20 and the highway shear. A number of conductors were

indie ited though in most instances they were not associated with the

narrc ? shear zones in question. Geochemical soil samples over these

condt :tors gave negative results.

It is recommended that some geochemical tests using organic

humus material as the medium be carried out over the better portion of

these VI,F-KM conductors.

/25,


Page 25,

CONCI [SIGNS

From the review undertaken it appears that there are

j niti i]3y 2 zones, i.e., No. 3 and No. l, that can be considered as

intei ssting with regard to the possible development of viable gold

depos .ts. As yet there is not enough available information for these

two 2 me s t o base concrete opinions as to depth extensions, continuity

of v i Lues, size etc. to warrant immediate underground investigations.

The l ;st method to acquire the additional data needed to further the

evalx it ion is believed to be diamond drilling.

/26,

11 111iiiiiiiiiiiiiii

Page 26

9

REC01* 1KNDAT10NS

It is herein recommended that a diamond drill programme of

apprc ;imately eighty-five hundred feet (8,500 ft.) be undertaken,

broke i down into the following:

1. lentral portion Zone No. 3-10 holes totalling 2,640 ft.

?. rest portion Zone No. 3-8 holes totalling 1,520 ft.

3. last end Zone No. 1 - 12 holes totalling 1,880 ft.

4. Jlowance for drilling extensions, fill in et al 2,500 ft.

For details of 1, 2, and 3 see Appendix "A".

In addition it is recommended that some geochemical tests

using organic humus material as the medium be carried out over the

trend of known gold bearing shears, and over the best of the VLF-EM

indie ted conductors. For gold, this medium, being analysed by

neutr n activation technique, provides better data than does

sampl ng of the B horizon.

Estimated Cost of Programme

Diamo d Drilling 8,540 ft. Cd $30/ft. $256,Assay 5,Repor , Maps, Sections 5,GeoJo i st S Helper 12, Geoch mi cal Sampling 8. Analysis 10,

288,

Conti gencies 11,

$300,

the

soil

200000000000 000

200

800

000

727

lll AU of which is respectfully submitted.

l

l

Page 27,

Toror :o, Ontario

Noven ter 1983

HILL, GOETTLER, DE LAPORTE LIMITED

c^.

* N. Firth, P.Eng.

l

l

l

l

l

l

l

l

l

l

l

l

l/28,


Page 28,

CKRTIFICATE OF QUALIF]CATIONS

], Norman Firt.li> hereby certify that:

1. [ am a Professional Engineer, registered as a Consulting Engineer ?ith the Association of Professional Engineers of the Province of hit ario.

2. i reside at 274 Juniper Avenue, Burlington, Ontario, L7L 2T3.

3. t graduated from the University of Toronto in 1950 with the iegree of Bachelor of Applied Science in Mining Geology.

4. [ have been engaged in mineral exploration and mine development for more than twenty-five years.

f). The Murgold claim group was visited by N. Firth on October 19th md 20th, 1983.

6. The foregoing report was based on data supplied by Murgold lesources Inc., and various Ministry of Natural Resources of )ntario reports.

7. t have no personal interest, nor do l expect to receive any Interests, directly or indirectly, in the property or the securi- :ies of Murgold Resources Inc.

Datei at Toronto this 1st day of November 1983.

N. Firth, P.Eng.

/29,

Page 29,

APPENDICES

/30.


Page. 30.APPENDIX "A 1

RECOMMENDED DIAMOND DRILLING

No.

Cent

123itb6789

10

West

12345678

East

123456789

101]12

Al lowfill

B

La t.

re Portion Zone 3

29355N29390N29390N29350N29350N29300N29300N29300N29285N29285N

Portion Zone 3

29600N29600N296I8N29635N29635N29580N29565N29565N

Portion Zone 1 (all

31060N3 1 06 ON31090N31120N31120N31155N31185N )31185N ",31220N31030N31000N31 DOON

nee for drilling ofins, etc. dependent

Dept .

169660E169750E169750E169900K169900E169955E169955E169955E170045E170045E

168967E168967E168922E168875E168875E169015E169062E169062E

S20 0W)

168240E168240E168145E168050E168050E167960E167870E167870E167775E168335E168430E168430E

extensions ,on first results:

Dip

-45"~45 0-65"-60 0-75 0-45 0-62 0-75 0-45 0-60 0

Total

-45 0-70 0-45 0-45 0-70 0-45 0-45 0-70 0

Total

-45 0-70 0-45 0-45 o-70 0-45 0-45 0-70 0-45 0-45 0-45 0-70 0 '

Total

Grand Total

DepthFt.

150215285300365210260350230275

.2,^640

210210130210210130210210

1,520

130210130130210130130210130130130210

1,880

2,500

8,540

/31.


Page 31

APPENDIX "B 1

DATA REVIEWED

J, l.D.M. Volume 41, Part 3, 1932,

Jeology of the Three Duck Lakes Area by H.C. Laird.

2. I.N.R. - Mineral Deposits Circular 18.

Jold Deposits of Ontario, Part ? - 1979.

3. 'he Chester, Benneweis and St. Louis Township Prospect of Murgold iesourc.es Inc. in Porcupine Mining Division District at Sudbury, )ntario by Watts, Griffis and McQuat Ltd. April 1983 (53 pages, 16 maps and sections).

4. look of diamond drill logs, Murgold, Chesgo Mines, Rinaldi Jption, Kingbridge Mine, Olympic Mine, Strathmore underground :hannels.

5. .983 Progress Reports D. Hoy.

6. lurgold Resources Inc. - Map No. l Vein, by T.D. Brown.

7. IcPhar Geophysics Induced Polarization and Resistivity Plan Map.

8. lurgold Resources ]nc. Surface plan diamond drill holes and assays October 1980, Map No. 8.

9. Preliminary map filtered VLF data.

4 ififswaaa? 6.3.1370 si. louis

REPORT

ON

THE 3983 EXPLORATION PROGRAM

MURGOLI) RESOURCES INC. PROPERTY

CHESTER, BENNEWEIS b S T. LOUIS TOWNSHIPS

PORCUPINE MINING DIVISION

ONTARIO

BY

D. Hoy, B. Se

JANUARY 3 984

-.JjLl. Jr.:_ iipi?sw000? 63.43/0 si. LOUIS

SUMM RY ................................................. 2

]NTR DUCT]ON ............................................ 4

PROP RTY 6, 'J'] TEE . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 6

HIST RY OF PREVIOUS WORK BY MURGOLD ...................... 20

THE 983 EXPLORATION PROGRAM .. .. .. . . . . . . . . . . . . . . . . . . .. .. 1 2

GENE AE GEOLOGY . . . . .. ... . .... .. . . .. . . . . . . . . . . . . . . . . . . . . . 16

ECON M]C GEOLOGY . . . , . . . . .. . . .. . . .. .. .. .. .. . . . . . . . . . . . . . . 19

TREK III NG 6- SAMPLING . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 25

GEOP YS] CS . . . . . . . . . ,, . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 36

GEOC EM1STRY . . . . . . . , . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 39

CONC US1ONS . . . . . . . . , . .. ... .. . . . . .. .. . . . . . . . . . . . . . . . . . . . . 40

RECO MENDATK)NS . .. ., . . . . .. . . . . . . . . . . . . . . . . . . . . .. .. .... . . 42

COST EST]MATE .. .. .. ,... . . .. .. . . . . . . . . . . . . . . . . . . . . . . . . . . . 44

REEF ENCES . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 45

LIST OF TABLES

Tab! i 2 CI ai ms Li st . . . . . . . . . . . . . . . . . . . . . . . . . . . . 7

- 8 'J

I'jgu: e J Sudbury 6 Timmins Regions Showing MurgojdProperty Location ...................... 5

I ( 'igu: e 7 P roperty Map Showing C2aims B2ock ...... 8I-'igu] ? 3 Genera] Geology of the Property ........ 27Figu: i - 4 Wat 1 5. Trenches { No . 3 Vein) k No . 4 Vein,

Geology k Sample Locations ............. 26T'igu: ? 5 No.] Vein (East Find), Geology 6t Sample

I .oc a t i on s .............................. 27Figui r 6 No . 8 Vein- Shear, Geology k Sample

I .oc ations .............................. 30Figui 'c 7 No. 20 ?,one, Geology f* Sample Locations .. 32 I-'igui -:- B Plan of No . 2 Shaft Dump. Sample

Locat i oris { Lower Level ) . . . . . . . . . . . . . . . . 34

LIST OF DRAWINGS Un back pockets )

Draw: rig No. 2 Composite Map, No. 2, 2 , 3 , 4, 5 &B Veins.Draw: ng No. 7. F 'l an of Grid A, Geology.Draw: ng No. 3 F'l an of Grid A, VLF-EM Survey.Draw: 'ig No. 4 Plan of Grid A, Soil Geochemistry Au ppb.Draw: ng No. 5 Plan oJ Grid B, Geology.Draw: ng No. 6 F'l an of Grid B, VLF-EM Survey.Draw: ng No. 7 F'l an of Grid B, Soi2 Geochemistry Au ppb.Draw] ig No. 8 P2 an of Grid C, VLF-EM Survey.Drawi ig No. 9 Plan of Grid C, Soil Geochemistry Au opb.

SUMMARY l .

Murgold Resources ]nc. owns 296 contiguous mining claims

total i ncj about 11,840 acres in area, located in Chester, Benneweis,

and S . Louis Townships, Porcupine Mining Division, Ontario.

Pants of the present property were originally worked in the

Thirt e-s and sic-cording to government records, production totalled 98

ounce, . Since 1979, Murgold has carried out extensive work on the

claim, , which has included surface exploration and underground

i rive S' i gat i on s .

The 1983 exploration program was largely concentrated on

inves i gat ing the No. l and No. 3 vein systems as primary targets.

Kxplo: at i on techniques employed during the program included core

loggiiq, trenching and sampling, geochemical soil sampling, VLF'-F,M 16

and m; gnetometer surveys in addition to geologic mapping.

Thjt- property is located on the south-eastern extension of

the Si axe greenstone belt. The claims are largely underlain by an

intru:ive complex consisting of dioritic, quart?, dioritic, granodiorite

and e\'. a skite phcises. These are intrusive into rhyolitic volcanic and

greyw; eke-type met asedi merit ar y rocks. Diabase dykes are the youngest

rocks on the property and cut all the aforementioned units.

To date at least l? gold bearing structures have been

identified on the property. The gold is hosted in relatively narrow

quart: veins, occupying persistent shear-fracture ?,ones which tend

to pi i c-h and swell along strike. The mineralization is structurally

contrt lied, as the veins and ore shoots are hosted in shear, fracture,

fault and contact zones. The most important gold-bearing structures

- 2 -

d 3 sco or od to date include the No s. l and 3 vein-shear systems,

which have been traced over strike lengths of 2,600 and 2,800 feet

r espC' t i ve] y .

Hand arid backhoe trenching was carried out at the site of

the NI s. ], 2, 3, 4, 8, and 20 vein-shear systems. The Watts portion

of t hi No. 3 vein was sampled in detail and returned an average value

of 0. 9 o ?./ion Au across a sampling width of 3.1 feet, along a strike

Jengtl of ?90 feet. Significant gold values were also obtained from

the o her veins sampled.

VI.F-FM16 and magnet ometer surveys were carried out over 3

grids covering portions of the Nos. l, 3, 20, and highway vein-shears.

A num] er of conductors were delineated in the surveys, however most

were , ttributable to the presence of conductive overburden, rather

than - he shear structures. Magnetics was similarly unsuccessful in

detec" ing the vein-sheers.

On the order of 1,000 soil samples were collected on the

grids to supplement the geophysics. The soils were analyzed for Au,

Cu, ai 3 Ag . Generally, the soil sampling yielded negative results;

which is probably the result of the presence of thick glacio-fluvial

overbi rden covering large areas of the property.

The 1983 exploration program was a success from a geological

point :)f view. Three zones in particular have been indicated by

surfac E- sampling and diamond drilling to be of economic interest.

These include the Nos. l, 3, and No. 20 zones.

A program of diamond drilling and trenching in addition to

geoloc ical, geophysical arid geochemical surveys is recommended as the

next , -l Jig e of exploration. The driving would consist of a 30,000

foot rograni primarily directed at the Nos. ], 3, and 20 zones. The

estini, ted cost of the program is S338,250.

4.

Murgold Resources Inc., owns 296 contiguous mining claims

iota]] ng approximately 31,840 acres, in the Porcupine Mining Division

of Nor hern Ontario. The property is 161 km north of the City of

Sudbur and 97 km south of the City of Timmins on Highway 144.

During the summer and fall of 1983, a comprehensive ground

explor t i on program was conducted on the property by Murgold personnel

The ex; l oration techniques employed included surface trenching, geo-

physic l, geochemical and geological surveying, in addition to core

relogg ng .

The purpose of this report is to outline the exploration

progra and the results obtained, and to recommend further work on

the su ject group of claims.

20 O 20 40 tO (O KILOMETRES t HW! -M -imt:

Sudbury and Timmins regions showing Murgold property location.

F'igure l

AND TI TLE 6.

^ ,o c fi l i i ri a n d Ac c e s s

The property j s located in Chester, Benneweis and St. Louis

Townsh. p s , 1G1 km north of Sudbury and 97 km south of Timmins {Figure l )

Specif reilly, the centre- of the claims is located 18 kilometres south-

west o: the town of Gogama at 47 0 33' N , 8 1 c 51' E.

The claims are bisected by Highway 144, thus providing

excel 1 1 nt access to the property. A system of good gravel roads

extend from Highway 144, a distance of approximately 5 kilometres to

the l o( at ion of the Murqold camp site. Alternate access i s by means

of air transport from Sudbury to Gogama, and from Gogama by ground

transpx rt to the camp. Numerous gravel roads and extensive areas of

bull do: E^r stripping are present on the property, providing relatively

easy ac ::ess to all parts of the claims block.

CI a ims St a tAij;

The property consists of a group of 296 contiguous mining

claims in Chester, Benneweis and St. Louis Townships, Porcupine

Mining Division, Ontario (Table l 6 Figure 2).

Two of the claims are patented (SI 9 99 2 and S20009 ) and

8 are rining leases (8323594, S51 5048-51 5052 , S51 5055-53 5056 ) . This

group) c f 10 claims covers the area containing the Nos. l and 3 vein

system* , the portion of the claims in which the major thrust of the

exp)lor; t i on program was directed.

The remaining 286 claims are unsurveyed and unpatented.

An exan i nation of government records indicates that all of the claims

TABLE l

C] fi i m s List

SI CJS20S3?851S51F' 51PSIP47P47P51P51P 5 3P53P53P53P53P53P53P53P53P 5 3P50P5?P54P54P54P54P54P54P54P54

CI a i m No .

92 (patented )09 (patented)594 (lease)048-515052 (leases)055-515056 (leases)053-515054057-515059952-471958667-473746328 -515330335-515336055-538059082085-538089105-539129136-539155279-539298308-539328523-538525404-539421181-539183667-507669680818-543824827993-543996092980-547000001-549019108-54911 7294

No . of CI aims

11152237

8032515

25202021

318

3317141

211910

1

Township

ChesterChesterChesterChesterChesterChesterChesterChester

Chester 6 BenneweisChesterChesterChesterChesterChester

Chester 6 BenneweisBenneweisBenneweisBenneweisBenneweisBenneweisSt. LouisSt. LouisChesterChesterChesterChesterChesterChesterChesterChesterChester

Total 296

8 -

ST. LOUIS TWP.

BENNEWEIS TWP.

Scale1 P345678910

Kilometers (approximate)

3 ^4___b 6 7

Miles (approximate)

P'igure 2

- 9 -

arc i n jood 5; t find ing, with sufficient work performed on them for

appi ice :3 on lo J e a se.

Physio: [/i ph y and Climate

The area of the claims is relatively high (i 3,300 feet

above ,c ;a 3 eve] ), and is located just to the north of the height of

]and de .ineating the interface between the Atlantic and Arctic

waters)- ;ds. Topographic relief rarely exceeds 100 feet, and in these

cases -t ic high ground consists of boulder till and glacial outwash

compris .ng esker s and kames. Generally, large areas of rock out-

croppir 3 are sparse, with exposure largely limited to small rocky

knolls. Overburden thickness is quite variable, however it is usually

l ess t)- m l 0-1 f. feet .

Short, warm summers, and long, cold winters with abundant

snow clr aracter j ?,e the climate typical of this area of Northern Ontario

Temperi :ures are extreme with summer temperatures exceeding 30 0 C and

winter :emperatures reaching lows of -30 0 to -40 0 C. Precipitation is

modera1 ? with an average total rain and snowfall of 48 inches per

annum.

The property is forested with relatively dense growths of

poplar, birch, spruce, jack pine, balsam and cedar. Low lying areas

abound îlh exlensive areas consisting of willow and alder swamp.

STORY OP PRKV3 PUS WORK BY MURGOLD 10.

The history of the property has been well described

in pro' ious reports prepared by Watts, Griffis 6, McQuat (April 12,

1983) ; -id by Hi]], Goettler, De laporte (November, 1983), and need

not be reported in detail here.

]n summary, to date considerable work has been carried out

on the olock of 296 claims. Parts of the present property were

origin; Jly worked i ri the Thirties with the original gold discovery

in the area, being made in 1930 by Alfred Gosselin. Two small shafts

were si 'ik in addition to numerous pits and trenches. Government

record.1 indicate that previous production totalled 98 ounces.

Since 1979, Murgold has carried out extensive work on the

claims, which has included comprehensive surface exploration and

undergi Dund investigations.

Surface exploration has included hand, bulldozer and backhoe

trench: ig , geological mapping, geochemical sampling, airborne magneto

meter, and VI iF surveys, and diamond drilling. Geological mapping and

V LI1 '- KM 16 surveys were conducted over the entire claim block in 1981,

howevei the major thrust of exploration has been directed at the No. l

and No, 3 vein systems.

A total of 12,776 feet of diamond drilling comprising 42

holes v as carried out by Murgold in 1982. Most of the total footage

was use 3 to drill the No. 3 vein system {about 8,000 feet), with the

remain] ig footage directed at drilling the Beaverbridge showing and

the NOJ . l, 2 , 4, 1 5, and 16 vein systems. The drilling delineated a

signifi :ant zone of mineralization in the central portion of the No. 3

-11 -

vein s; stem. Values ranging from .002 to 4.08 oz Au/ton over relatively

narrow widths were intersected to a depth of 280 feet, over a strike

length of approximately 400 feet. Included in these holes was hole

Ml 3 wh. r h returned a core length of 10 feet, assaying 0.554 o?, Au/ton.

Underground exploration has included detailed sampling of the

No. l ' -on at the site of the Gomak shaft and additionally on the

easteri portion of the No. 3 vein system at the Strathmore shaft.

Undergj :iund investigations were conducted on the east and west drifts

on the ]00 foot level at the Strathmore shaft in 1981. Detailed

channel sampling, geologic mapping and the extraction of a large bulk

sample (656 tons) were undertaken at that time.

3n 1982, the No. 3 shaft collar was excavated to a depth of

60 fee 1 and concreting of the collar was completed. This was work

carriec out in preparation for a three compartment shaft.

T ri K J 983 EXPLORATION PROGRAM J 2 .

Cei p Operatijons

'J'he exploration program commenced on June 20, 3983 with

the c i r i val of the students and project geologist. The exploration

crew c: nsisted of JO employees as listed below.

Project Manager W. Derek BullockProperty Manager Ted D. BrownProject Geologist Don Hoy'Student Keith BullockStudent Kevin BullockStudent C. Andrew Me AlpineStudent Michael FrancisProspector-Labourer Kenneth MonahanCar pent or-Labourer Bert SimpsonCook Lillian Therriault

The field camp situated in patented claim S20009 was

utili?. d as a base for the exploration program and to provide room

and bo rd for company employees. The camp facilities consist of 4

sleepi g cabins, an engineering office, a fully equipped cookery,

a gene at or shack, a core shack, and a trailer housing washroom and

shower facilities. Fuel and supplies required to support the camp

were o! tained from Timmins and from the nearby town of Gogama on a

regula basi s.

Camp operations were suspended on November 30, 1983 for the

winter nonths. A watchman has been retained on a temporary basis to

make pi riodical checks on the camp facilities.

Apj r o ac h jl o 1JS83 Explorati o n

Given the relatively short time frame of current management

and th( wealth of data eivailable from previous operators, the major

thrust :)f exploration in the past program was directed at verifying

and f o: low-up work of this data base. This included geological and

geophy; ical data, trenching and sampling data, and numerous diamond

- 23 -

d r i 3]i t 3 3 ogs .

A report prepared for Murgold by the consulting firm of

Watts, Griffis and McOuat (April 1 2, 3 983) was designed to draw

togethe r and review the work carried out on the Murgold property and

a3so t c outline work recommendations and budget for the No. 3 vein.

The rej Drt concludes that the No. 3 vein system is the most interesting

with rt gard to the possible development of a viable gold deposit.

Our feeling on the No. 3 vein system at the onset of the

3983 pi sgram was that there was not enough available information for

the xot ? to base concrete opinions as to depth extensions, structure,

siz,e ar 3 grade to warrant underground investigations. Accordingly, it

was fei t that the underground program proposed by WGM in their report

was son ?what premature.

The 3983 exploration program was largely concentrated on

invest] gating the No. l and No. 3 vein systems as primary targets.

The i rn sstigations were designed to increase the strike lengths of

the st:t jctures, obtaining a reasonable grade, and also to obtain a

better jnder st andi ng of the; structural and geological controls governing

minera] ization. The findings of the program would supplement our

ear 3 i ei knowledge of the ?.ories, in preparation for subsequent diamond

drill ir 3 and eventual underground exploration.

The program basics as set out at the onset of the program

were a; f o l l ows :

1) Complete additional test-pitting, trenching and

sampling on the No. 3 and No. l veins.

?) Re log all Murgold drill core, and resample any zones of

interest for assay purposes. Develop a structural and

- 14 -

geo]ogJ cal concept for the nature and mode of

m i nora] j ?.at j on .

3) Conduct prospecting and grass-roots exploration surveys

in the outlying and least explored areas of the claims.

4) Perform detailed confirmatory and follow-up geophysical,

geological and geochemical surveys in order to confirm

and more closely define the nature of the numerous

VIiK-KM 16 anomalies reported by Norminex.

Kx): .or at i on_Tpchni^jues

Kxploration techniques employed during the 1983 program

include l core logging, trenching and sampling, geochemical soil

samp] i r ), magnetometer and VL.F-EM 16 surveys and geological mapping.

The var .ous techniques are summari?,ed below.

Murgold drilled a total of 12,874 feet during the 1982

explore lion program. The cores were logged and sampled by the on-site

manager ; at the time. 3t was apparent that the sampling of the core

was con lined to the /ones comprising quartz veins and visible mineral

ization During the early stages of the 1983 program all of the pre

exist i r. j Murgold core was relogged to test for wallrock mineralization

and ale ) as a means of examining the geological setting of the ore

shoots. further sampling of the core was carried out in wallrock

alterat .on zones adjacent to the quartz veins where warranted.

Hand and backhoe trenching with subsequent sampling was

conduct ?d at a number of locales during the program. Trenching was

carried out on the Nos. l, 2, 4, and 8 vein-shear systems, the Watts

trenche ; on the No. 3 vein-shear, and on the No. 20 shear-alteration

zone. additionally chip-channel sampling was conducted in the locale

- 15 -

of the St r at hmor e shaft at the site of the ore stockpile taken from

the wc;: : drift of the Stratomere shaft and also the mine dumps.

Recent ground geophysical surveys conducted by Norminex Ltd.,

(3983 ) nit lined a number of target zones delineated by EM-16 anomalies.

Anomali ;s which coincided with a major structural linear (trending at

11 O 0 ) ?. id which were proximal to local showings were considered to be

first ]: "iority targets for potential zones of mineralization. Given

these j: irameters, follow-up surveys utilizing the EM-16 and magnetometer

were cc iducted on 3 first priority anomalies to confirm the targets

and fur ;her to determine the nature of the anomaly. Three grids

(grids ^, H and C) were cut and picketed to provide control for the

follow- i p work, on the No. l, the No. 3, and the Highway vein-shear

systems

Geochemical techniques that were employed during the program

include l l ithochemical sampling and soil sampling. In the order of

1,000 s )il samples were collected on the 3 above mentioned grids

cover in i the anomalous zones reported by Norminex. The samples were

collect ?d to supplement the geophysical surveys and to assist in

definir j the nature of the EM-16 anomalies.

Similarly, geological mapping was carried out on Grids A and

B t o su iplement the geophysical and geochemical surveys. Chip sampling

was add tionaly performed at a number of locales on the grids where

warrant id. Shortage of time towards the end of the program and snow

cover \: e vented geologic mapping from being completed on Grid C.

GENERAL GEOLOGY l 6.

The Murgold property is situated on the south-eastern

extens on of the Swaze greenstone belt. The greenstone be] t is comprised

of eas er]y trending bands of tight]y folded Archean metasediments and

metavo canics, termed the Temiskaming Sediments and the Keewatin

volcan cs. These are intruded by later Archean intrusive stocks of

graniti and granite-greiss. All of the above rock types are cut by

Keewee awan diabase dykes and si 3 l s.

Numerous gold deposits occur within the Swaze belt including

past p:oducers, the Ken t y Mine, and the Jerome Mine. Additionally

the Or fi no deposit in the northern portion of the Swaze belt is

curren ly under development.

The Murgold claim block is largely underlain by a large

intrus. ve cornple-x consisting of several phases including diorite,

quart 2 diorite, granodiorite and alaskite. These rocks are intrusive

into ri yolitic volcanic and greywacke-type metasedimentary rocks.

The no: them margin of the claims and an east-west trending zone

around Benneweis Lake a re underlain by greywackes and conglomerates.

The riv olitic volcanics are similarly restricted to these locales.

The yoi ngest rocks on t hie property are diabase dykes which occupy well

develo cd fracture zones trending both north and north-west (F'igure 3).

The quart?, vein-shear systems found to date on the Murgold

proper y are all hosted within the intrusive complex, largely in

di or iti s and alaskite units. Visible gold is hosted in relatively

narrow quart?, veins associated with shear and fracture systems. The

shear . ystem on the property spans a width of 5-6,000 feet following

a predi mi nant azimuth of 100-120 0 . This system appears to extend from

MUROOLD RESOURCES INC.

KEWEENAWAN

[]J ] Olivine d bose

ALGOMAN.——i Chester y inger granite withl l porphorili dioritic and grano-diorite1—— facies

TEMISKAMING

m Sediment schistose conglomerate greywacke arkose qi rtzite argillite serecite schist mica hornblend schist

KEEWATINVolcanics elsic to intermediate volconic flows and pyroc istics

,-. -. — p ou lt ;rred)


GENERAL GEOLOGY OF THE PROPERTY

SCALE: l'11 mi. FIGURE i 3 DATE: DEC. 83

- 38 -

the Yoi ig-Shannon property to the west to the Strathmore shaft on

the ea; :, with both ends st j] l open on strike. The shear and fracture

systems tend to display a regional parallelism.

ECONOMIC GEOLOGY 3 9 .

To date, at least 12 gold bearing vein-shear structures

have b( rn identified on the property. The gold is hosted in relatively

narrow quartz veins, which occupy persistent shear-fracture zones. The

structi res vary in width from a few inches to several feet in width and

tend t c pinch and swell along strike. The earlier gold discoveries

apoeart 3 to be individual isolated occurrences, however it is now

apparet t that the veins are hosted in a system of parallel shear-

fractui 2s. The veins which are located in the area between Mill Pond

and Art thusa Lake (Vein Nos. 1-5) are typical of this system of para

llel si ructures (Drawing l ). Additionally, the quartz associated with

the sh( ars commonly occur as parallel veins or in branching veinlets,

and as such should be referred to as vein-shear systems.

The dominant trend of the mineralized structures is prominent

at 110' -?90 D , largely dipping steeply to the north. However, there are

other fi ineralized shears on the property that trend at 045 0 (the No. 15

vein s} stem) and also at 090" (the No. 20 vein system). The mineral-

izatior appears to be structurally control led, as the veins and ore

shoots are hosted in zones of weakness, such as shear, fracture, fault

and cor tact zones. It is also apparent that there has been repeated

and prc longed deformation along the 110 0 trend as the degree of alter

ation ; id the strength of the structures are most predominant at this

azimuth . The persistent deformation was probably important in pre

paring :he groundwork in providing a plumbing system for the mineral

izing J l ui d s .

The structures crosscut geologic contacts at various locales

but ap{ sar to be strongest in gabbro-diorit e hosts as opposed to the

more f c isle, alaskite host rocks. Similarly the types and degree of

- 20 -

alterat .on differ between these rock types. Various phases are

evident in the gabbro-dior ite rocks and this is due in part to altera

tion, ['he various phases of the mafics grade into one another with

out wel . defined contacts and range from relatively fresh diorites to

intense .y altered chloritic schistose rocks. These highly altered

phases ire intimately associated with the vein-shear zones. Alteration

of the lafic rocks include propylitization, chloritization, carbonat

ization and silicification in varying degrees of intensity. Proximal

to quar :z veining the alteration is intense and pervasive, involving

the prc luction of chlorite and biotite schists and the introduction

of larg ; quartz eyes into the host rocks.

]n the more felsic granite-alaskite units, the alteration

is rest 'icted to silicification and sericitization adjacent to the

veins ;; id permeates the wallrocks for very short distances (1-2 feet).

General .y, regardless of the rock type, there appears to be a positive

cor r el;; .ion between the intensity of alteration and the gold content

of the 'ein zones.

There are at least two distinct styles of gold and associated

sulphic) i mineralization present on the property. The first is character

ized by the occurrence of visible gold and associated pyrite, chalco

pyrite md pyrhottite in relatively narrow quartz veins and veinlet

network ;. Most of the gold occurs as free gold, erratic in distribution,

usually accompanied by sulphides. Copper appears to be a very good

indioat )r mineral for the occurrence of gold and where chalcopyrite is

abundar . appreciable visible gold is usually present. In some instances

it was -eported that sampling of the wallrock adjacent to veining

carried significant gold values. However, relogging and subsequent

samp] i g of the 3982 drill core did not support this concept. Alteration

zones onlaining visible sulphide mineralization enveloping the veins

were s mpled during the relogging and failed to indicate significant wall

rock g Id mi nereil i ?,at i on . Values ranged from trace to .016 oz/ton Au.

The second style of mineralization is characterized by the

occur ri nee of gold associated with disseminated pyrite, chalcopyrite

and py: hottite in ore shoots. Locally the sulphides are semi-massive

and ar* commonly associated with quartz-carbonate veins. The mineral

ized zc ics appear to be substantially wider than the veins discussed

above. The host rocks for the mineralized zones are intensely altered

includ: -ig propylitic and silicic styles of alteration. The abundance

of l arc ? opalescent, bluish quartz eyes are apparent in the altered

minera! i zed zones. The gold may not all occur as free gold, as some

may be tied up in the associated sulphides. The No. 20 zone and the

Beaver! ridge showing are characteristic of this second type of

occurer re. The No. 20 zone is a continuation of the Chester No. 2.

gold-cc :)per zone contained within the adjacent claim block held by

Ki dd R* sources .

The most important and heavily investigated gold-bearing

struct*, res discovered to date on the property include the No. 3 and

No. l \ ?in-shear systems.

i

The No. 3 vein-shear has been traced over a strike length

of 2,8( )' by means of underground investigations, surface diamond

drillir 3 and trenching. The system comprises a series of 2-3 parallel

veins r at her than a single vein. Relatively high grade 'diamond drill

interse :tions have been obtained over a strike length of about 400

feet ir the central portion of the No. 3 vein-shear system. An

- 22 -

i-ntersc r. t i on of 4.08 o?, Au/t on over 1.2 feet was obtained at a vertical

depth c E 210 feet. The structure was additionally intersected at a

depth ( E 350 feet in the same general locale but yielded low gold

values. The results of the 1982 drilling on this section of the vein

were i l ? most consistent of any drilling undertaken on the property,

and t hi 5 this zone is considered as promising with regard to the possible

develop nent of a viable gold deposit.

The western portion of the No. 3 vein-shear system is

indicat ?d over a strike length of 800 feet. The Watts trenches were

samplec during the past program, indicating a strike length of 290

feet a\ ^raging 0.49 oz Au/ton across an average sampling width of 3.1

feet. \ number of diamond drill holes were drilled by predecessor

compani ;s in the vicinity of the trenches, specifically by Chesgo

(1947), by Kingbridge (1970) and by Olympia (1975). Older plans and

drill l )gs indicate that significant intersections were obtained

during :hese periods of drilling in a number of holes with the

deepest intersection assayingO.94 oz Au/ton over a 2 foot width at a

depth c: 210 feet (Chesgo, DDH 13, 1947). Unfortunately the locations

of the )lder diamond drill holes are not accurately known and can at

best be approximated. Thus, based on the encouraging results obtained

from tfc s recent chip-channel sampling of the Watts trenches and the

IMAAII l l l l

A4V JAW AMI l

i i

- 22 -

inters* ction of 4.08 oz Au/ton over 1.2 feet was obtained at a vertical

depth ( f 210 feet. The structure was additionally intersected at a

depth ( f 350 feet in the same general locale but yielded low gold

values The results of the 1982 drilling on this section of the vein

were tl 2 most consistent of any drilling undertaken on the property,

and thi 3 this zone is considered as promising with regard to the possible

develof nent of a viable gold deposit.

The western portion of the No. 3 vein-shear system is

indical sd over a strike length of 800 feet. The Watts trenches were

samplec during the past program, indicating a strike length of 290

feet a\ sraging 0.49 oz Au/ton across an average sampling width of 3.1

feet. \ number of diamond drill holes were drilled by predecessor

companJ ;s in the vicinity of the trenches, specifically by Chesgo

(1947), by Kingbridge (1970) and by Olympia (1975). Older plans and

drill J )gs indicate that significant intersections were obtained

during :hese periods of drilling in a number of holes with the

deepest intersection assayingO.94 oz Au/ton over a 2 foot width at a

depth c: 210 feet {Chesgo, DDH 13, 1947). Unfortunately the locations

of the ilder diamond drill holes are not accurately known and can at

best be approximated. Thus, based on the encouraging results obtained

from tti s recent chip-channel sampling of the Watts trenches and the

signifi :ant gold values obtained in earlier drilling, the western

portion of the No. 3 vein-shear system is considered an excellent

target.

Located along strike to the west of the No. 3 system is the

No. 8 v in, situated to the immediate south of Mill Pond. Of signifi

cance i the very close alignment of this structure with the Gosselin

- 23 -

showinc to the west and the No. 3 system to the east. It is probable

that t} z No. 8 vein and the No. 3 vein are all part of the same system,

which j i effect would increase the total strike length of the structure

to appi jximately 4,700 feet. Sulphide mineralization is of moderate

abundat :e in the structure and some significant gold values were

obtain? 3 during recent sampling.

The No. l vein-shear system has been traced over a strike

length nf approximately 2,600 feet by means of trenching, underground

investj jations and some limited diamond drilling. This system, asis the

case fc r the No. 3 system can be divided into 3 sections.

In the central section Gomak Mines developed an 85 foot

deep ir :lined shaft with 215 feet of drifting at the 65 foot level in

1935-3( . It is reported that Gomak produced 98 ounces of gold from

500 1 ?ns of ore at that time. In 1939, Jones reportedly sampled

the 20C foot long trench located to the west of the shaft and obtained

an avei age value of 2.04 oz Au/ton over an average width of 1.4 feet.

Murgolc resampled the trench in 1980 and reported an average of 0.47

oz Au/1 ?n over an average sampling width of 2.8 feet. Olympia

Interne cional Resources drilled 2 holes in the locale of the Gomak

shaft j i 1975. The holes were intended to intersect the down-dip

extensi jn of the structure at shallow depths ( 45 feet). Shallow

inters* ;tions of 2.93 oz Au/ton and 0.42 oz Au/ton were intersected

over cc re lengths of 1.5 and 1.0 feet respectively at this locale.

Two large trenches have been developed on the shear at the

east er 3 of the structure. Drill hole M18 was drilled at this locale

in 198/ and produced a 6 foot length of core assaying 0.146 oz

Au/ton, Significant gold values were obtained from both of these

- 24 -

trench s during recent sampling which are consistent with earlier

sampli g by Murgold.

The western portion of the No. l system has been investigated

by ham and bulldozer trenching, in addition to very limited diamond

drillii g. A number of hand trenches returned significant gold values

and a , ingle drill hole which was drilled 650 feet to the west of the

shaft i long strike returned values of 0.45, 2.0, 1.0 and 0.10 oz Au/ton

respec ively. The hole was reportedly drilled in 1939 by Gomak Mines

Ltd. ' he widths of the intersections are not known, however it is

report* 3 that the mineralized sections of core were intersected at

depths 56 - 61 feet vertically.

Other vein-shear zones that have been investigated include

the No; . 2,4,5,11,15,16,17 and 20 systems in addition to the Highway

shear i hich is located on Highway 144, on the east side of Southcamp

Bay. r. D date a limited amount of work has been undertaken on them,

largely being restricted to trenching and sampling. Significant gold

values nave been obtained from the sampling, however their vertical

and lai gral continuity has yet to be established, and further work

is wan anted on these zones.

TRENCHING S. SAMPLING 25.

Hand and backhoe trenching was carried out at a number of

locale on the property. The following summarizes these operations

and th results obtained.

No. 3 ein-Shear (Watts Portion)

Blasting and subsequent mucking of the west Watts trench

reveal d a thin quartz vein (4-6" in width), hosted in relatively

unalte ed alaskite. The vein carries abundant chalcopyrite, pyrite,

malach te and azurite and appreciable visible gold locally (Figure 4).

Chip-channel sampling results of the west trench indicate

a zone 170 feet in length averaging 0.62 oz Au/ton over an average

sampli g width of 3.2 feet. The east trench assays 0.203 oz Au/ton

across an average width of 3.03 feet along a strike length of 120

feet. This indicates a total strike length of 290 feet averaging

0.49 o /ton Au over a sampling width of 3.1 feet. Grab samples

collec ed from the west trench returned values ranging from .054 to

4.57 o /ton Au. Visible gold is readily discernable at this locale.

The results of the above sampling confirm values which were

previo1 sly obtained by Murgold personnel and are in accord with the

result of two bulk samples collected by Olympian International

Resoun es in 1974. The two samples were comprised of 46.74 and 48.92

tons ai d returned values of 0.172 and 0.30 oz Au/ton from estimated

widths of 6 to 10 feet respectively.

No. l ' ein-Shear (East End)

Three pits were blasted and re-opened along the eastern

extens: on of the No. l vein shear along a strike length of about 375

26

LEGEND

Diaboi* dyk* - very 'ins g'oinsd to medium

T 20

Miatn't* granite - unatTTerenTfoTec, ffieaiutri TO coorte groined.

Trench Outline v.g. visible gold

Ou*cr op cpy cho'copy'*e

Geoiogicoi Contoc' py pyrite

Sêor Orien*otion mgi malochite

Strike - Dip oz azurite

Quartz- Vein iim iifnonite

chl chlorite

ler tericite

m.g. medium grained

l Chip chonnel

1.03/2.0' Au oz/ton/feet

O"---"l Proposed DDH

/\ Survey pin

/3.0'

py.cpy

JRCES INC.[N0.3 VEIN) 8 •IN

E LOCATIONS

DATE. DEC. 83

v.fg. very fine groined

-'... 638/2.5' l

j.303/4.0' .1.74/20' l

-i 210' at -450

20

9

.028/3.0' ^

MURGOLD RESOURCES INC.WATTS TRENCHES (N0.3 VEIN) 8

NO. 4 VEIN

GEOLOGY 8 SAMPLE LOCATIONS

SCALE-' l " FIGURE: 4 DATE: DEC. 832!0 of -4!

27.

Drilled by Vurgoid - 1978)

tN

Sheored Quartz Diorite

*-.. 2

Chlorite Schist

Assays/6.0' /6.0'

(grab)

(grab)

18573

Two Backhoe Excavations

did not reach bedrock

Thick Overburden

LEGEND

contains disseminated py, cpy

Altered Diorite - Quartz Diorite - prominent shearing,

pervasive propylitic alteration, appreciable disseminated

sulphides

18573

.246/6.0'

. 116

Trench Outline

Outcrop

Sample Number

Au oz/ton/feet

Au (grab sample)

Shear Orientation

Quartz Vein

py

cpy

qtz

v.g.

pyrite

chalcopyrite

quartz

visible gold

2."

I8577H.O06

I8575-I.O66/2.0J

q.v. py.cpy.po


NO.I VEIN (EAST END)

GEOLOGY a SAMPLE LOCATIONS

SCALE: \ -20 FIGURE.- 5 DATE: DEC.83

MIS (Drilled by Vurgold - 1978) N

Verfico! Projection

Surface

diss. py, cpy

Previous Murgold Assays

.27 oz Au /ton /6.0

l.OS oz Au /ton /6. Q'

4.11 oz Au/ ton (grab)

.92 oz Au/ ton (grab)

Sheared Quartz Diorite

Chlorite Schist

Two Backhoe Excavations

did not reach bedrock

To No. 3 Vein and Bates Shaft

\

18573

Thick Overburden

- 28 -

feet ( 'igure 5). The shearing observed in these trenches is of

modera e to strong intensity with widths ranging from 5 to 20 feet.

The qu rtz associated with the shearing is lenticular and discontinuous

in nat re. The shear and associated quartz contain pyrite, chalcopyrite,

malach te and minor visible gold. Sampling of the trenches yielded

the fo lowing results.

Assay (oz/ton Au) Sampling Width (feet )

0.074 2.0 )1.42 .8 ) .431/6.8'0.002 4.0 ).211 2.0.262 grab.066 1.5.018 grab.547 5.0

Previo s assays that were obtained by Murgold in these trenches were

.27/6. ' and 1.03/6.0'. In addition drill-hole M18 was drilled in

this l cale in 1982 and encountered a 6 foot section assaying 0.146

oz/ton Au.

No. l ein-Shear (West End)

A number of samples of interest have been obtained from a

series of trenches located to the west of the Gomak shaft. In a

trench crosscutting the vein-shear 900 feet west of the shaft the

follow ng assays were returned (Drawing 1).


0.119 8.0' 0.204 grab

A furt er 100 feet to the west, the shear was trenched and sampled

at wha has been referred to as the No. 17 showing. The following

assays were obtained from sampling.


0.134 grab0.294 grab0.052 3.00.010 3.00.020 grab

- 29 -

At thii locale the shear appears to decrease in intensity and thick

overbui 3en becomes prevalent to the west.

No. 6 ' sin-Shear

The No. 8 vein-shear was previously stripped by bulldozer

during L981 exploration by Murgold. The structure is stripped along

a stril 5 length of approximately 1,000 feet (Figure 6). The shear

lies tc the west and on strike with the Nb. 3 vein-shear. The discontin

uous si saring and associated quartz veining is of moderate intensity

and chc racteristically pinches and swells along strike. A number of

hand t] snches were blasted along the strike of the structure revealing

rusty i sctions containing minor to appreciable pyrite and chalcopyrite.

Chip-ct annel sampling and a few grab samples were collected from the

hand ti snches and returned values ranging from .002 to 1.56 oz Au/ton.

Two sar pies collected from the small exploration pit located at the

west er 3 of the structure returned assays of .219 and .263 oz Au/ton

resped Lvely. The sampling indicates that there is significant gold

contair sd within the structure and reflects the erratic distribution

of golc in these vein-shear systems.

No. 20 itein-Shear Zone

The following results were obtained from sampling the

mineral Lzed structures comprising the No. 20 zone (Figure 7).

Sample # Au oz/ton Sample Width (feet)

18561 .050 10.0 )18562 1.06 10.0 ) 0.38/30.0'18563 .084 10.0 )18564 .002 3.018565 .004 3.018566 .084 5.018567 .002 2.518568 .004 2.518569 .082 grab18570 .198 grab from Chester #2 zone

Bulldozer Stripped Area

q.v.,cpy, py y 18605 -To6873.0l",..,**---.--- f , , . sty-

18598-1.014/3.01-18599-1-002/6.0' l

I8600H 1.56 ' 1860H.00218602-1.002/3,5

18603 ,___^

LSite of two earlier grab samplesBulldozer Stripped Area

LEGEND

Sheared Diorite, intense, pervasive propylitic alteration schistose and foliated

Diorite, relatively unaltered, locally brecciated

Alaskite, unaltered, fine to medium grained

no

18596

-002/6.0 1

.004

KEY

Bulldozer stripped area

Outcrop

Shearing and foliation

Claim post

Rock trench

Quartz veining

Sample location

Au oz/ton/feet (channel)

Au oz /ton (grab)

cpy

py

ma l

bx

chalcopyrite

pyrite

malachite

brecciated


NO. 8 VEIN-SHEAR STRUCTUREGEOLOGY 8 SAMPLE LOCATIONS

CHESTER, BENNEWEIS 8 ST. LOUIS TOWNSHIPS

SCALE: l =50 FIGURE: 6 DATE: DEC.83"

9*00 E 8* 00 E 7+00 E 6 + 00 E

Azimuth 110*2,3

q.v.

.2 v

py.cpy 18598-1.014/3.0'!--^

18597^.004/5.0'

I8595H.002/5.01 l

18596 H. 002 l

Bulldozer Stripped Area

LEGEND

OOE

18599-1.002/6,0

18600-fl56~] 18601-1.002 J8602-T082

00 E

Deep Overburden

Sheared Diorite, intense, pervasive propylitic alteration schistose and foliated

Diorite, relatively unaltered, locally brecciated

Alaskite, unaltered, fine to medium grained

3+00 E

Bulldozer

18596

.OO2/6.01

.004

KEY

Bulldozer stripped area

Outcrop

Shearing and foliation

Claim post

Rock trench

Quartz veining

Sample location

Au oz /ton/feet (channel)

Au oz/ton (grab)

cpy

py

mol

bx

ch(

pyr

me

bn

- 31 -

The most significant values were obtained over the widest

sectio of the zone with three continuous channel samples of ten feet

length assaying .050, 1.06 and .084 oz Au/ton respectively. As a

compos te the width of this portion of the zone assays 0.38 oz Au/ton

across 30 feet. The other shears were sampled and returned values

rangin from 0.002 to 0.084 oz Au/ton across width ranges of 2.5 to

5.0 fe t. A grab sample taken by Murgold from the adjacent Chester

#2 gol -copper zone assayed 0.198 oz/ton Au. Norminex reported

assays from well-mineralized grab samples containing in excess of

2 oz/t' n Au. from the No. 20 zone.

Kidd Resources reports channel sampling values of up to

0.87 o /ton Au across 38.0 feet from the adjacent Chester #2 zone.

They ha e additionally intersected significant gold values in drill

holes o a vertical depth of 150 feet.

32

2*00 N —

ooo oo-J

o o o o o o•o-J

o o o o

MURGOLD RESOURCES INC. OVERBURDEN

00 N ——

Boundary Post No. 4 -

x Barren ot visible mineralization

BULLDOZER STRIPPED AREA

Silicified Diorite - Quartz Diorite

Chester Gold-Copper Zone No.2

KIDD RESOURCES

2+00 S —


NO. 20 ZONE

GEOLOGY S SAMPLE LOCATIONS

SCALE', l": 50' FIGURE: 7 DATE: DEC. 83

LEGEND

Sulphide Mineralization Zones - disseminated to semi-massive, py,cpy8po associated with shearing and discontinous qtz veins

Altered Quartz Diorite - pervasive chloritization and carbonatization, prominent bluish quartz eyes

KEY

qtz

DO

Trench Outline

Muck Piles

Outcrop

Shear Orientation

Prooosed DO H

quartz

pyrrhotite

l Channel Sample Location

j J Au oz/ton/teet

— Claim Boundary

—Q— Jointing Orientation

Au Gold

cpy chalcopynte

py pyrite

- 33 -

No. 2 haft Dump

Relatively fine material comprises the lower level "dump"

at the site of the No. 2 shaft. Observation of this fine material

indica. ed the presence of fine grained disseminated sulphides.

Sampli g of the dump was conducted in 10 foot lengths in channels.

Values ranged from .002 to 1.81 oz Au/ton and averaged .279 oz/ton Au

over l foot sampling widths (Figure 8 ). The results of the sampling

indica es that the lower level of the No. 2 shaft dump comprises ore

grade aterial. Based on dimensions of a 50 foot length, a 40 foot

width nd a 4 foot thickness, it is estimated that there is approximately

500 to s of this material present at the site.

The coarser material comprising the upper level was addition

ally s mpled. Channel samples returned values of .018 and .004 oz/ton

Au ove channel sample lengths of 6.5 and 6.0 feet.

No. 4 ein-Shear

This vein-shear was blasted and sampled over a strike length

of app oximately 40 feet. The structure is located approximately 85

feet t the south of the Watts trenches trending at an azimuth of

approx mately 115 0 (Figure 4 ). Trenching indicated a shear of moderate

intens ty hosting discontinuous and lensy quartz. The quartz veining

varied in width from a few inches to about 2 feet. Appreciable patchy

and di seminated pyrite and chalcopyrite were hosted in the quartz and

within the shear i'tself. Small amounts of visible gold were noted at

one of the sampling sites. Gold values ranged from .004 oz/ton Au to

a high of .221 oz/ton Au across sampling widths of 3 to 4 feet.

Unfort nately the presence of thick overburden at both ends of the

struct re prevented further trenching from taking place.

34.

.

LOWER LEVEL MUCK PILE

FINE MATERIAL

UPPER LEVEL MUCK PILE

COARSE MATERIAL

Average for sampling fin* muck pile "02 X ion Au for 18 samples across 10.0 fMt

40712 Sample number

Au 07 /ton /feet


PLAN OF NO. 2 SHAFT DUMPSAMPLE LOCATIONS - LOWER LEVEL


SCALE: ("-(O1 FIGUREJ 6 DATE' DEC. 83

- 35 -

Other ' eins Sampled

Trenching and sampling was carried out at a number of other

localej during the program. This sampling was conducted on the No. 2

vein-si ear, the No. 11 showing and from the remainder of the ore stock

pile ol tained from the No. 2 shaft.

The No. 2 shear is located approximately 300 feet north of

the No, 2 zone. The structure has been exposed by a number of small

hand tj 2nches over a strike length of about 400 feet. Grab samples

were cc Llected from these trenches and returned values of .468, .014,

.155, . 305, .78 and .12 oz/ton Au. Appreciable patchy sulphides are

presenl in the quartz vein which attains a maximum width of about 2

feet a1 a few locales.

The No. 11 showing is located on Grid C to the north of the

No. l \ sin system (Drawing No. 8 ). The zone is stripped along a strike

length 3f about 600 feet. The showing was discovered in 1981 in

respons ; to a strong gold in soils anomaly reported by Norminex. The

mineral tzation is comprised of patchy and disseminated pyrite and

chalcof 'rite, hosted in interfingered units of diorite and alaskite.

Three c rab samples were collected from the showing and returned values

of .006 , .020 and .016 oz/ton Au.

A few large grab samples (20-25 Ibs) were collected from the

remainc ;r of the ore stockpile in the No. 2 shaft locale. The samples

were re jresentative grabs of the ore and returned values of 2.21 and

.464 02 Au/ton. The results confirm our feelings with regard to the

grade c : the ore extracted from the stope in the west drift.

GEOPHYSICS 36.

VLF-EM and magnetometer surveys were carried out over grids

A, B, ; id C covering portions of the Nos. l, 3, 20 and highway vein-

shears. A Geonics VLF-EM 16 was employed for the electromagnetic

survey, using Cutler, Mains as the transmitter station. A McPhar

M 500A nagnetometer was used for the magnetic survey. The results

of the surveys are summarized below.

A number of conductors were indicated on the EM survey

carriec out on grid A {Drawings). The presence of 2 powerlines created

problen 5 of interference on sections of the grid, and readings are

only Ve Lid between crosslines 10+OOW and 10+OOE. The conductors

defined by the Fraser filtered contours are apparently not associated

with tt s quartz vein-shear which is bisected by Highway 144. The

major c inductor located between crosslines 2+OOE and 10+OOE is

coincic snt with an area of the grid underlain by swamp as are a number

of the Jther conductors. It is probable that the EM responses

obtaine 3 are a result of the presence of conductive overburden rather

than di s to bedrock conductors.

Three major conductors were defined by the EM survey on

grid B Drawing 6). The Fraser filtered contours and the in-phase

profile 5 indicate 2 very strong conductors located between crosslines

4+OOW e id 10+OOW. The in-phase readings were extremely high over these

zones c id when filtered using the moving average, the resulting data

were hj jh. It is apparent that these anomalies are generated by the

extreme Ly swampy conditions in these areas, and are probably due to

conduct Lve overburden. There is, however, one anomaly which is

conside red valid, in view of the absence of swampy terrain in the locale,

- 37 -

and it, proximity to the No. 2 shaft and No. 3 vein system. This

anomal; is located between lines 4+OOW and 18-fOOE, trending at an

azimut! of approximately 080 0 . Of significance is the apparent

intersi ction of the conductor with the projected strike of the No. 3

vein tt the east of the shaft. It is probable that this anomaly

repres* nts a bedrock conductor and follow-up work is warranted in

this c. se .

On grid C, there is one very prominent anomaly indicated

by the filtered contours, that spans the entire grid in an east-west

direct: o n ( Drawings). The portion of the conductor located between

crossl: nes 16+OOE and 24+OOE is interesting in view of its close

spatial relationship with the No. 11 showing. The showing consists

of dis.1 sminated and patchy pyrite and chalcopyrite hosted in fractures

and sht ars in interfingered units of alaskite and diorite. The showing

was dii covered by follow-up trenching,investigating a strong gold in

soils i lomaly in 1981. With the exception of one 10-contour anomaly

locatec between lines 12+OOE and 16+OOE, the conductors delineated in

the su] yey are not associated with the No. l vein-shear system.

VLF-EM 16 and magnetometer surveys were carried out on a

small c rid covering the No. 20 zone. A strong conductor was indicated

by the EM survey, which correlates very strongly with the mineralization

associi ted with the Chester #2 gold-copper zone and the No. 20 zone.

In addi tion the magnetometer survey indicates a prominent magnetic

high si perimposed on the sulphide zones. Of significance is the

continx ation of the EM conductor to the east beyond the extent of the

present L y exposed sulphide zones, indicating potential for additional

mineraJ ization.

- 38 -

Generally, the conductors delineated by the EM surveys are

not ass )ciated with the relatively narrow vein-shear systems tested,

which i icluded the Nos. l and 3 systems and the shear on Highway 144.

It is s jparent that the veins are too narrow and lack sufficient

sulphid is to eli cit an EM response. The exception of course, is the

No. 20 :one, which is of considerable more width than the veins and

contain i significantly more sulphide material.

By and large, the magnetic surveys are more useful in

providi ig geologic control than for detecting the shear zones. The

magneti : data are able to detect the trend and location of diabase

dykes a id the gabbroic-diorite intrusive phases in areas underlain by

overbur [en. In a few isolated cases, weak magnetic lows are situated

over th i strongest vein-shears, but this relationship is not always

consist mt.

GEOCHEMISTRY 39.

In the order of 1,000 soil samples were collected on grids

A, B, c id C (Drawings4, 7 and 9) to supplement the geologic mapping,

the VL! EM-16 and magnetometer surveys. Samples were collected from

the B s sil horizon at all stations on the grid that were not underlain

by swan ny ground. The samples were analyzed at Bell-White Analytical

Laborat )ries in Haileybury.

In general, the response obtained from the geochemical

samplir. j was poor. Geochemical sampling that was carried out over the

EM cone ictors yielded negative results. The results of the sampling

are son ;what surprising given the fact that even soils that were sampled

in clos j proximity to known gold bearing veins yielded negative results.

The poor results can be in part explained by the relatively

thick \ meer of overburden underlying major portions of the property.

Soil ge chemistry works best in thin horizons of residual soils which

have be m left undisturbed. The overburden covering large areas of the

grids s impled consist of glaciofluvial material such as sands and

gravels , This suggests that the responses obtained in the soils do

not ref .ect the "signature" of underlying bedrock mineralization.

Some consideration should be given to further geochemical

testing of organic material utilizing the neutron activation method.

This cc ild initially be carried out as a test survey with future

surveys contingent upon the earlier results. The advantages of this

method ire that the neutron activation system is much more sensitive

in terrr ; of a lower detection limit (to 0.1 ppb), the method is a

multi-el ment technique in that many elements can be readily analyzed

simulte teously.

CONCLUSIONS 40.

The 1983 exploration program has been a success from a

geoloc ical point of view. The results of the program have substantiated

and ac ded to the potential of the property with regard to the develop

ment i f viable gold deposits. The most important conclusions as yielded

by thi program are:

1. The No. 3 vein system has been explored by surface sampling,

trenching and diamond drilling, over a strike length of

2,800 feet. The investigations have delineated 2 zones

of interest for further exploration. The central portion

of the system contains relatively high grades of gold over

narrow widths, along a strike length of 400 feet at shallow

depths. The western portion of the system, at the Watts

trenches locale, was sampled in some detail during the

program, and indicates a zone 290 feet in length assaying

0.49 o z/ton Au, across an average width of 3.1 feet.

2. The No. l vein system has been traced over a strike length

of approximately 2,600 feet through trenching, sampling

and limited diamond drilling. Sampling of the eastern and

western portions of the vein-shear system has yielded

significant gold values across relatively narrow widths.

The structure is still open at both ends along strike.

3. The No. 20 zone represents a significan't zone of mineral

ization. The showing displays a style of mineralization

which differs from the relatively narrow veins. Sampling

of the zone indicates gold values of 0.38 oz/ton Au, over

a sampling width of 30 feet. The zone has never been

- 41 -

drilled and present indications are that mineralization

extends at depth.

4. There are numerous gold bearing structures present on the

property. Very limited investigations have been carried out

on these to date, however most of them contain siginificant

gold as indicated by preliminary sampling.

5. VLP-EM 16 surveys failed to respond to the relatively

narrow vein-shear zones. A number of conductors were

delineated in the surveys, with most of them responding to

the presence of conductive overburden rather than bedrock

conductors. The exception is the No. 20 zone where a

significant EM and magnetic response was obtained, very

closely spatially associated with the mineralized zones.

Magnetic surveys were similarly unsuccessful in outlining

the narrow vein-shears.

i. Geochemical soil sampling was unsuccessful in outlining

gold in soil anomalies. The presence of a relatively thick

veneer of overburden, glacio-fluvial in origin, is suggested

to be the cause of the negative response.

RECOMMENDATIONS 42.

It is herein recommended that a program of diamond drilling,

trencting, geological, geophysical and geochemical surveys be under

taken ?n the property, as the next stage in exploration. The elements

of the program are as follows:

L. A diamond drilling program be undertaken comprising 10,000

feet of drilling, primarily concentrating on the Nos. l and

3 vein-shear systems. The drilling is suggested to be

broken down into the following:Proposed

7ein System

to. 3 vein

to. 3 vein

to. 3 vein

to. l vein

to. l vein

to. 20 zone

Sub total 9,000' Allowance for fill-ins contingent

Portion

central

western (Watts trenches locale )

eastern

central S eastern

western—

Footage2,800'

1,600'

400'

3,000'500'

800'

No. of Holes

9

9

2

20

3

4

m earlier results 1,000'

Total 10,000'

The proposed drilling is designed to fill in, extend and

test the structures at depth. It is recommended that 2

drill rigs be used to carry out the drilling, with one drill

operating on each vein system.

It is recommended that the Weeduck Lake area, the No. 20

zone area and the adjacent claims to the north of the

property held by Kidd Resources be investigated by a program

of geological mapping, EM, I.P., magnetometer and geochemical

surveys. The prominent EM anomalies delineated by Norminex

- 43 -

in 1981 in these areas, and the excellent potential for

discovering additional zones of mineralization similar

in nature to the Chester Nos. l and 2 zones and the No. 20

zone, warrant a program of this nature.

Given the obvious association of the vein-shears on the

property with fracture, shear and fault systems, an air

photo structural study is recommended. An air photo study

can be useful in areas of heavy overburden outlining

lineament and regional fracture systems. This would be

useful on the Murgold property in view of the abundance

of overburden covering large areas of the claims block.

It is recommended that a test geochemical survey utilizing

humus sampling, with subsequent analysis by the neutron

activation method be carried out. This method is much more

sensitive with regard to detection limits for gold and

provides better data than does soil sampling of the B

horizon. Apparently the technique has been used with some

success in the Hemlo area.

44

COST ESTIMATE

For a program of approximate 3 month duration.

Diamor 3 Drilling, 10,000 ft @ $20/ft S200,000Assays , 500 @ S10.00 each 5,000I.P. i i rvey, @ Sl,00071ine kilometre, say 40 km 40,000 Linecv :ting, @ SISO/line kilometre, 40 km 6,000Geoche nical Sampling 6 Analysis 10,000Air Pt 5to Structural Interpretation 1,500Report, Map i Section Preparation 5,000Persor Jl and Administration Costs 40,000

Sub total 307,500 plus contingencies @ 10^ 30,750

Total S338,250

Don Hoy, B.Se, January, 1984

REFERENCES 45.

Bu!lock, W.D., 1983. Murgold Resources Inc., Various Memorandums 6* Reports.

Hi! l, Goettler, De Laporte Ltd., 1983. Report on Murgold Resources Inc. Property, Chester, Benneweis S St. Louis Townships, Porcupine Mining Division, Ontario.

Ho? , D., 1983. Murgold Resources Inc., Progress Reports.

Mil istry of Natural Resources, 1979. Gold Deposits of Ontario, Part 2, Mineral Deposits Circular 18.

Mu] gold Resources Inc., 1980. Report on Chester, Benneweiss, St St. Louis Townships, Porcupine Mining Division, Sudbury District, Ontario.

NOJ ninex Limited, 1983. Second Report on Fraser Filtered Data,Murgold Resources Inc., Gogama, Ontario, Norminex Limited,

No] ninex Limited, 1981. Report on Fraser Filtered Data, Murgold Resources Inc., Gogama, Ontario.

Noi ninex Limited, 1981. Geology S Gold Deposits, Murgold Resources Inc., Gogama area, Ontario.

Onl ario Geological Survey, 1983. The Geology of Gold in Ontario, Ontario Geological Survey Miscellaneous Paper 110.

Waibs, Griffis 6t McCMat Ltd., 1983. The Chester, Benneweis ASt. Louis Township Prospect of Murgold Resources Inc. in Porcupine Mining District at Sudbury, Ontario.

REPORT

ON

THE 1983 EXPLORATION PROGRAM

MURGOLD RESOURCES INC. PROPERTY

CHESTER, BENNEWEIS S, ST. LOUIS TOWNSHIPS

PORCUPINE MINING DIVISION

ONTARIO

BY

D. Hoy, B. Se.

JANUARY 1984

VOLUME II - DIAMOND DRILL LOGS

DIAMOND D RECORD

SHEET NUMBER

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fa+t^ i 't*~~*e*. '. ^,*,is â **.* ! ^*~ jLui7 ' f r t ^ f vfa*** * s**. y i t,*-t'\ w . f-*'\ so- s f -4 ^/"/^

-^* 'v^^r^ 1 ** 0 (**. '*~t ^ *f*~-V u J C^"^

^ ,^ ^, ,,,.^,,^ /r' ^..ff. ^ ^^,.v4v xj.rW ^ .-,^.^C

t . v? ^ 'X /* ,-f -'

j^^^ tlAstr ^ ; ^ ^W,^f^ -W ****4*.

SAMPLE No.

mSTARTED ^-^ '-V"-

COMPLETED rf*"*- "*~*

ULTIMATE DEPTH s /a. o'

PROPOSED DEPTH


SLUDGE

GOLD S

DIAMOND D •LI RECORDPROPERTY HOLE No..

SHEET NUMBER..

LATITUDE ____

DEPARTURE ——

ELEVATION ^^.

SECTION FROM.

DATUM ————

.TO. STARTED

COMPLETED —

BEARING

DIP ——

ULTIMATE DEPTH

PROPOSED DEPTH.


OF SAMPLE GOLD SSLUDGE GOLD i

—— -V----T

st '

A, frv

Au

is~ t-s-

"^ ^ 1* ;-/f

-r ' A ^-

DIAMOND D RECORDPROPERTY HOLE No..

RHFFTNUMBFR 5 ^3 SECTION FROM TO

1 ATITlinF DATUM

DFPARTURE BEARING

ELEVATION DIP

DEPTH FEET

/if.o- * "-o'

f

FORMATION

-7/Qt/X' Z tfi^L' , Xû. '^ irfiA*- î&f^-SL- Mr36t4***- fa- /xy*y

j f V

G (rv^'0' f'w-4 - X^K^M^ tf^^*^^tti &L I9vt*04^' 4*4îst^ 4*}(2 ^14^*0- ^46^*,

9

W-t - 9IH ' ^ O^^C *s**L ^^.*L Û^^, , s[s6*#*j f f j

tt

'^* s J*^*y . . ' tp .jvj^ . ^ *7?

^nZ ' r 7? tf *-~^ff'Q r /^^t^Û-t ^ "Â-^v44^ *^^*M^*-- ' di^&i&ff'A,, flfî '•fi.i-t'U' *ZsQ ^^^f^-^f.

f J

l f-

s^tf?' to ' ^5^P 0 ^"\^- 'fyiS-*-tyjsj'L , ^**f4~-i- Jfec' j*Jljfa,'i''lL™ /',^^^y*^ti'ô ^* F ^/^^•^^~j r

.'i?.o ; :,j,'^ , ^^ ^ 1^ *'j..-.**.o , y,^ ^,^' , ' : T ''

Û^Mbi "^**'T ''^'-/4 , St**4~t. ^ 741 -O'', (S, Sorjfi'}

E. (-'D *^ /W* g ?'J'

SAMPLE No.

P******.f

•1*6, iS'Sf

STARTED

COMPLETED

ULTIMATE DEPTH

PROPOSED DEPTH

WIDTH OF SAMPLE

tA^tv*

W+'Vt*

GOLD S

-TV.

/•a-'

SLUDGE

GOLD S

•77^

DI AMON D D •LL RECORD

SHEET NUMBER .

p . , . ~*-~ ,--^,-Js/. S, H DDrtDCDTV ' fj-afav , C^rlTJ'-dv/c) Ar.ft SX i4-ffw3 t fit*' 46*4^3 LI^M C Kl^v Ai V ^^ — — ~ _ — —ffi\*tr en li - r ^ . ' jT riviLC TVD. ' i

7 ^ i SECTION FROM TOD

1ATITUDE 2-9 ^ k , ., DATUM A/8. 3 /w^~ i^xKv-

DFPARTURF \b")-7C)^ BEARING 2 A3 ' l 3 ****0

EIFVATION 9994.71 DIP -^'W ^//"-

DEPTH FEET

0-î

W .^0

i 5 *- f r. S

f-:'- "r.,;

- ; 6 . /S: ;

FORMATION

.'X-J-.-.j) . .

,v.w yv 4. , ; -A//^. ,r/ ^'^^ ..,,..',..y * -5-^-i,^; ".,^,-.^ .'' ,-.r ', , -^^^ *s'-'*:4ff /•./M .s,*. ^ ,'.*,-.. . .^ ^:,,..--

r•j. fi, Mi S f. i, - .' ' -" J '-i'J. : Ji-.-.t '-'--' " f.rs''j:'- s-'- /**''* ••^j.-ii /îff--'^

i ff ^ ^ ^ ^

f i -, W- v4,.y^x f.^,.^1^^, t/'.- 1 -, s. p.*.* .t,,-. :S /e^x^

^^' -1*4 t .^ -c,' . -,h s*-* ^.^^ ^ s**- t, ^' ' f

;., vi , -^

——— ^ —— J •••••'•i ———— t- ——— i —————— ———————————— -^ —— r-

./" '' -

.,, ;'

,,.^..^ ^ ;r, ^^, ^v^*' ^ Jf-'/i.'

.- ; ' ' ••-..- - ^.w ,, */,^. ^ , .- .-' l-'

,.,.,^ , . ", f y .^.,-' - . --.

— LL —— L.- ————— : — L — —L-Li — i — •'r!?.''-":.- — —————— i;: —— - —— : '———

SAMPLE NO

-±J^

STARTED //A/^ Âz-

COMPLETED v/-^ /'?^^

ULTIMATE DEPTH f '*-o'

PROPOSED DEPTH


SLUDGE

GOLD S

DIAMOND D.•LL RECORD

SHEET NUMBER

PROPERTY HOLE No

Z J t SECTION FROM TO

LATITUDE DATUM

DEPARTURE BEARING

ELEVATION DIP

DEPTH FEET

rfci - /' e-"S 0

'

Y

*

2-03. d- 35*0

251s)- -,*,',r s

FORMATION

•3 'if: * ,*^7,W^ -VUx Z Jo-*'. i .*u ,..- ^^^.^î

J fi fi

h', ,,,^,; J y /^vv^v .:*,^,,,Ww. ^*,,v,U~ ^y,,,^,.^ X^-HL

h* A x .,'-, .W ;.'Vs, ^ .' ^, , 5 ,^.^*^ .-^ *,*u

j-'. /'.•-^) .,. A ^7 ../- J- :' X ,-;-- fo-ffa:- ^*^T*^./'

S^/s-./V.jT. ^ ^.-,,,,1 y-v^-^V., ^-A, ir^y ^5,

d? /^.5- '/^' ' /.v, -A- - ^'.**

r '.' i- f- c " ^ - ^ ^ ' x ^ ~ fr:f e'ft * o . ^ '^ '" "' ' ~"*--*^*f;-\ /y&te, ^tt^ô/t; yC*-3,/

^^ ; ^ , ,.,, i:X( ^/,X;,^ y,..,^,^ ^.^

^r,.^, f- ^-—— ;, * ~ ...f' -....^( j--"-'-'- - - ^/- ,- '.-^ --'

^vvi/,^, . y; ' ^ u ^^w,,-,-^. ^,. A ^^,, v ^:^J., M^ ' " l/~-"T ",- ' " -^-fy x '^'

' -, :' ( ^ f , ! -

SAMPLE NO

* /.r/ 7 ?*)Slto

llS~1t-

/f 5"^5

n#Hlifts'

i* *ni^î

ASTARTED

COMPLETED

ULTIMATE DEPTH

PROPOSED DEPTHWIDTH

OF SAMPLE

I1\.S'*3*

W.* y?, sJtf.v H / -S

!-)7.0 ~ /fi-f

' Jy S ' ~tn.y

rtejj-m. ,

2 S' a- z fi J

:.^^.i

GOLD S

^.5"'

i, o 'J.*'

*S'

2..T

" ^

S.-

SLUDGEGOLD S

. aii -j.

.0**

-T**.-t

-^ffi f

, (j(j 2"

-v.'.-,r

-;,,v

J r It f

i,tlM

DIAMOND D0LL RECORD

SHFFT NUMBER

PROPERTY HOLE No

5 V ^ SECTION FROM TO

LATITUDE DATUM

DEPARTURE BEARING

ELEVATION DIP

DEPTH FEET

ZSS.f 2 S J S,'

2S1.S- 7^0

2St.O-?6t.O

v*M- J Tl-S

f 73. 5"- 'J&f'-S''

?8SS- ,-^.c

W.O- 3 /S 5

FORMATION

.X^ ^^; ,,^.. t^,vx i r #,.^ Ml^ ^ ^..^^ h^^,, It y i*.'.* y^/*, ,- ,*W,,,. ^,XW -' ,,,^.^.

^,u^J, ^.^.,^ , ^ ^^(^ ,^;^;^*Kt/ ^ /-"i

t' - ' 'r? *"

*^,x /,,; V -. ,^;... v, .v- .^ , ,,;^ , . ,,. :, ^, (î- '

'fa :*SS* Q ^ '."C/ r V'J , ^l^t^^V^Î f'^ -' -'C^ X* ? ^^ ; 'î't'* 4^ X^Vlî-V' '

X - V

* ? /'I f'

J , r' \ ^"fctf 'W.-jx' , . -: "s- j'.6f*-t*t" x^r" X^;-? -^ . ' --J I^^w-X- . i AtA- /; st&M*'-*-'

j^/'^tf* x;; ,-c. " xx,. ,-' '" i **-jf 'X v* '-'^ , .'X* J '-^ j/i.-.XvV^ -f'î //: /fff^ .^ ^ p "/5

^^ ^4- ^ ^;W . '^-.^ ,^,^. i/^r- ../,W^r

,^,,/-., /.v,, ^^,^ ^x^ n .^^ ^ ^,^.;^- ---Wî7 ; X

^ ^.,,- ^J.,-; y, ^ .;^^rf {^J^ ^4 ^^,;.r. i^t^

^.^ A. sA S.*'.*.~f -^ ;,,M /,.^/i-yW Z-^^-^ fe

"5-^.- ' 7 ' (/v, , x , . ti . /, . . .f^ , ^;^ ^ ^,^ y,v , /,., 4 ^ ^

f"S!S; s ' '' ^ i-'^1 ^'^•f^' '-'{b* ' -^-* ' ,tî' S'k-; 'S -t X^'-- ^ T* ^2. X^^ -^C5^**-*S^^**^-

ytV*uC toi4*Cls ' , 'Q *'{?t'6*-*6u ] PUU "44X4^ Aj^5 ^ ^l^C^J

SAMPLE No.

,ê

tfg41

lî,6Q

I1{,6\

A^

STARTED

COMPLETED

ULTIMATE DEPTH

PROPOSED DEPTH

WIDTH OF SAMPLE

,^..-^.r

757. f -?5 go

*-i^-7*.'.0

^t/.C- 3'S.c

GOLD S

i.-T

cJ V

?.o

/j

SLUDGEGOLD S

v^*

,:- ^

,-^

DIAMOND DJ0L L RECORD

SHEET NUMBER.. .

PROPERTY HOLE No

f f t SECTION FROM TO

t.ATITUDF DATUM

nFPARTURF BEARING

FI FVATION DIP

DEPTH FEET

3IS.S- 3 'to'

S7f.O- 53-7.0

.V576- 365.0

3CS-0- Mo-0

W*- 3f6 .s",

FORMATION

f~} v y x y fc^t^C*^* t X***-p ^t-^-f -fa-fttmSt-' -^^ ••fa^j*' -J'lî'W^ C^-^-Cf^^- 4.'*f3'J9t-'. '

y -' ' /9 y 'rf o-^c- y j^'r ,' 7 '

/ . '"

7 x /* ^ ^.' ' ^ .^

/' ^

/O^^^^r^ ^,., v ^ xXv,^V ' ^ ^^ ^,-^.

^,,^#a ^ ../^^, ^^x. ^-U. x^v y^W^sy

i- rf j

pi ,/ -7

^wfc, ' i,-/-, ^.A,^ -^ â*,^^* ,:*H* *dL-' S*,^* .Ith'f f1 r j

"^ V y '^ ^' ^.^ ' ",; , /, ; ^ ^C|3 S 'lfV- - *2- x f -J''/ ^ ^ , i -^îî-^;;/ ^ /*^t c^* P"*O^ * ffi f,. ^^^^^rt^fcjf 4 *0^

6s 411.2-' f ^** X^V/ ^ 4 /t' j*- j, ^"'!^/*^ t /i^tî. ty-d + l&Vv^ /C^^^^\ ^

ft , - 1 3 vt w. *-*',t fi .^. y ^' A ^-J. .(3 '.i? i' ' ^4j , ;. . ^ ',:,' Vi/ -s/i/ir : i' jr ^ '•^' : /^" j: .^,^

//^/^ L'W/* - ,,^,^ ^^^^v:^,.,v, û,-^.. ^,.^x

SAMPLE No.

/7^0 Z'

/W-J

/^^v/itof

/w.fr)

/Wfl6

/f^7

ASTARTED

COMPLETED

ULTIMATE DEPTH

PROPOSED DEPTH

WIDTH OF SAMPLE

3^..-l*7.0

3z?.0 -33^.0

•^.30. 0-33 ra

37^,0 "i?^.^

57^.0 - 3 d? ? ^

3/?.* •SA'-i'

GOLD S

7.0

*.o

3. o

^.0

3. "

55

SLUDGE

GOLD S

. 60 Z-

.^8

-V^

.oft-

,*cz

D l A M O N D D *L L R E C O R D

SHFFT NUMBER

PROPERTY HOLE No.

-f "^ SECTION FROM TO

LATITUDE DATUM

DEPARTURE BEARING

FI FVATinN DIP

DEPTH FEET

if^, , *0

&1.0- MW.O

*h*0- W.O

y-ru. i- *J?V j

4*.a- "St-o'

i/S^-i- J If 5-0

FORMATION

—— ———————— ^ —————— *-**-" —————————————————————————— ' —— — —— —— —— —— ———

J^.Jf , ,. '' . .^ ' ^

^.-^ v -s*' t+i+fr,* ^ ***t ** ^ ,^Jw, ' d-' u j f "V r * ^ '^^^

..^..L s* te*,v*f. } *

/;-,., 4 -, **~* ^;^ '^^ ^.-~#~4-, *tte~u/' V v j

'f ,y~± t'J.tx^ /--^ r- rt jS-'-^t&.i.-Xtt,

J-/'-,* ^'^- r,^f ^ " '^ a^

^.^ ^ - ),". t l**^ ,*S~*** ^,.^J . 1^^ ZZ X^v,^,y " ' j fi ~* ^{)

/*,-, t .;.-,:.- ^^ ,^f. ,..-t*. ^^ ^.^^ t+rJX,.

\^^.f^t't .' '^tf":.fff' ^'•'•"'-4^ j'"'iîf*L i*-' ftr t^.^^f-i ..''J J,'^.t. 'rf^vf.l'^fl" , faj&^&^s*^-' ' f (-

o L' n,,, /,,,, t. s /^^, L*.**t-,^ f* J j 'fi '

(j V iT.ci'. **'t-f( /-/vrt , a s .?' .4 i--M i x*^L.v'iA 4" ^5 1

® 'W fi' j ' ^''.'M ..'.^ tV SO-YC.' Jij^v-.-~C;*ttA' Li* ?f^2

nî ; r-v^ A *--. JJt fv^^, ^^^ ^^ê *,, y -'** ^ /yÂ/ , iwsl ^ ^ y * ^. *^^.

SAMPLE No

IWI

lUo1

rftlto

m

STARTED

COMPLETED

ULTIMATE DEPTH

PROPOSED DEPTHWIDTH

OF SAMPLE

ifft.a-t/zj.u

tll/l .0 - UU\. Q

rt**-"^

GOLD S

T. 0

'•O

3.0

SLUDGE

GOLD S

^'P

.C "f

,**z.

D l A M O N D D .•L L R E C O R DPROPERTY HOLE No..

RHFFTNUMRFR i .f SECTION FROM TO

LATITUDE DATUM

DEPARTURE BEARING

ELEVATION DIP

DEPTH FEET

M.e- W. 6

utf.O -e/tO'

FORMATION

@ '/i*/.**' V/^V - C Z^-4^ //.r.t-bt?,-*!,-*^. f^'.-frtt-.'Tj.'^ tijt'f-} J'-4tAt*- ^Jrf**- *^Xt ^*^-XXî..^'

f 1 f J *"(/

i'*,.^' ^. l,*fc*t-, ^ *,**t **^*t(, . r?.^^ ^*tS**-

f. ^ -

ff^v,.^*; /,/^ ^j,^ ^1, i,^ Ai*. V*-^ /w^,y

J rr.(\t(sMt .t.'^d-i^'Cuc. sjs*'. ^r'' \' . ' ; s/^fttr *6*- ' as-H*f'iv6*d2C-- ''" j

f- f ^ f f

f f J 7 S

3 ' - ' r x 0. )'zu fsiSM**s S-- ' ' -''3^4-1 , ** f.9-fsjj s,' ^4, '':'"~- * -*3- ( 2 *ii /w J ; sCtfu&C'r ' f

INK j r /,V;C ^ ^..'

SAMPLE No

STARTED

COMPLETED

ULTIMATE DEPTH

PROPOSED DEPTH

WIDTH OF SAMPLE GOLD l

SLUDGEGOLD l

DIAMOND D, *-L RECORD

SHFFT NUMBER.. . }

PROPERTY ''iijfri., bih-.uo^ #'*y ^ 1.-***, -^^j*, HOLE No. . 1/0

l * Z SECTION FROM TO

LATITUDE .92-0*0 DATUM A/* 3 i/^- zfft*^

DEPARTURE 1 1, 0) 74 O BEARING 02^' ^ ft/ Z*'E)

ELEVATION :95B,8ft. DIP "^ ^ ^*""

DEPTH FEET

0-7/0

re- f.*

•1,1- z**

" 2*-*- t?.i

li.l- '(.c-

•S t -i - i S -S

; ,,5 . w

FORMATION

j"** 3

y , V, f f t ^ f ,f ^, A 4

i*'f**, ' * , ^ ,^ ; t*. - w . ft 7'-**'J 7) '' - !

J *i*vr.l* A ,*'te*- :""t t^t--;, ^'^.i- W .r ,V

1'.,^ /, , . ,^,,^ ^rf;^ -' ,^v^

:..- ?: ,/ - ' ,., , .v,:-,'..:^ ^ " •.f-^^/.fr3^,.-* ' " - :.^*.,i* ^-^ . --., ^v.,^, ,^H ^ -*t***-"11 - :^', , -, ..,.'.-.Kl ;, .-J.*.!* - ^ ——— ^ f,-,'"-^

/v,,t Xi /-./.-, .''.f....:/,, 9y',-ijL, " ' ^/v/.-^-i '-''.': "

^^^: .,,,,,c- ,^*, ^ .^' * ^, ,.;'.. . ,/^.vv, .^^..-^c

,./.: v,-^^•-.^.'•- -: ^ .^ ,,r-^ .'-.^.- -..v^ ,,^. *,^v-4 -^-/-'I. J*''' ' ^-^ '- f't-.t', J j. "-.j .-? -i'^'-i1 /'Z ,'*3 -i- J . ? ' '"X , ' . --5-i-ttt '^^C.

/•f -*/^ r **'C ' ' ~ ' s ^-f'.tt '. f") x" - 'J's'tt tf ?3 . r /(fv( ' .-.'s .'.ff -~ S '^ r^,\ 3**.tfJ.; V-, ^

t 3 S*..; ^ , y.-v^,^, ^^^^ ^,-.^ ^ --^^ ,v-'/^ ' ^ i g W , 6 y1 ^ - - " ,/ , /^ r y, ' .- -^ X ^ , ^^ ',^ .

JU-'-*-.- -X':^ ^ 'A?^. ^}^^, /...v^*.v ^'X ^,^^,'-

V/'i'îif* p ftij* -S ' -'^ ( jf/^.f-i t '^^'Cv A^tr*fZfff' f t ifa ' ff.ffi6\ .y*jhtt-jj- f •J*** "^J rf) '^*v^1*v*' -^

SAMPLE No

7 f 5"'^"

",5/fl/

i Iff l

i*S'7

1 3 S* b

-'"')

1 35 ' /f

\ STARTED, /p

COMPLETED

'^tt-VjJ.. ft ÂB^\

ULTIMATE DEPTH 52* *'

PROPOSED DEPTH

WIDTH OF SAMPLE

^-^5,0

^.,- 23.1

3 3.-?.7 7. 0

* j 0 ' 5 7- ^

-*7. 0 -*'

^7 fl - if'tf .3

GOLD S

S C

i.'?

3.)

?, 0

3, c '

z- f

SLUDGE

GOLD S

-y/y*-. i 'li'

.W/

Jl-Jf

Iff* 4,

J* ' e

- — - - —

C,ii,n^ ^^/^

DIAMOND D *LL RECORDPROPERTY HOLE No..

RHFFT NUMBER * ^ ^ SECTION FROM TO

1 ATITIinF DATUM

DEPARTURE BEARING

ELEVATION DIP

DEPTH FEET

740- *K.t

K-l, " ? o

'•g..',- /W, o'

•r,:...;- i?*.* 1

/-J./.- 'W'

/tW 0-/V? 0

FORMATION

/. ,.A ^ ^ ^ y ,/' ' ' r

f C X^^-' ' 7 ^ ' ' ' y

^ 4tf.V^-

vv ,' '3 fi - ^ ^ , Sft'J M * :P. ^ ' ^.' l , 7^v^ :V v -J4 j/ '^ vt^t -tî^r^f'^.' ^f -fî.

••ê lvl, f ,.-*,-*. *'.-i'o^ ? .^^,a~.^,, . ^-^^^,^.'ev/;'.'*f

J '

f T ( ^ .., ^ ^'^ ' ^.' ^ 7 /?

^,, f- ^, -^-y .x-,/ - • -••^.^ / /.v A^^,,,^,../J/.*,, ^.-^,-- ^--,y,^' ^,i.-,./ .;-4:-A /.G,,^

rt , - .'i- i'; .^ J ,^.,t ' ^t*v*. ^^.

^ ,./^- X ,.,/x ,/;,, ' /.- ,^.^x ii^^ tetu*.t4~ .v •^1.

^

7 '

^ *'-. .v..t^ -

* ^"**^ ^tyrs ' x"'V /''i c^ -^vA*^^^ , i i^tfi t r^'-4 ***^-^VT^ ^w-i*^3*i ^ ff'i?4\

SAMPLE No.

i 1 5? 6

/ffZ/

" ,^/ez-

/f5Z*

/f^3

/•f^y

^5?r

STARTED

COMPLETED

ULTIMATE DEPTH

PROPOSED DEPTH

WIDTH OF SAMPLE

***- ^

^- ^.^

/'*.*-W.O

'"O * -/730

/4^.a- rio

v-w /?fe.o

7* .0 -/?',

GOLD S

i. 6.

'f

l. o'

*.v'

3.0'

r o '

Z" '

SLUDGE

GOLD S

. W

-f- f 4 C "t.

. 4fJ-

,6'l

.601,

, c /o

.00-2,

DIAMOND D. 10LL RECORDPROPERTY HOLE No..

RHFFT NUMBER 5/5" SECTION FROM TO

lATITUDF DATUM

DEPARTURE BEARING

ELEVATION DIP

DEPTH FEET

'yso - 'w

t"7 5 ; "^ * ^

V? f- "' o

FORMATION

X, W * ^' ter****7 r

/y ,'

^ * .- ,,-; : ; ^ /?

* ,' 7 /* '' /7

^ ^ ' 7 v ' y ; y w ;

0^0-1^-0; ''--v,^ ^W* - -x^t, ^ s,'^, ^ ,,J ^y*^ ^' f r •/e'

(f rj~5- '{ t' d*,^. /~ '&-HH A, V Aie*tt irtjjt-*:-- u SSa , "C./4.1-Q

r ' , X* J t^f'Sftiftts -*î -Vi '/t j l * plf.itt' , •^•-•'-it ':--X P*. /•^'•'/^-**3——— L........ i . ..., //- . y i . .,. t r^ ( /-.,r f

s ,'^f.*' '-'{i b' '?j.xx -•y^îffi. ^-îv/tc, yyk , , ../*, ^•."''^ 40.5*'.i - /'

e/?^.^; ' /4 ., v ,^ ,-^x: . ^/* ,,,x f^ ../^^, r-x5, -'A y-, - -V-i- ^^^,, ...-.4- î* * f''^ " .-.^.',.A*'

,/ y . ^ 1 , ;± '

•,.' ^-,. '. ; * /^,/X . ( ''y ^r*'**l 4t**~ rt fttf,J.a*.

'/^ -x,/.,-. ,/ ' " y -' fi- tlf .,j ,,- - v ,.; . , c /,,/,.,,,?, . /. ^.7^4.

fi 7

^ ^ l'

SAMPLE No

tlfil

11 5-2-7

/^52?

/f^1/^30

n&iIW2

1 9 5-33

•^ /s /ft j

;* 5-s-/

x f 5- J r

STARTED

COMPLETED

ULTIMATE DEPTH

PROPOSED DEPTH

WIDTH OF SAMPLE

•VJo- .4.0

M.o-.vu

'i/fa-ASj.O

/*7.0-^s-4

,,i*-^-*. 3

-w.*-/*'*

/*^ - iw. o

liV,0-H7- ^

't T s - t 7 1

,*?r- w, t

/-tin- / -Ti/a

GOLD S

r.

3 0

3.0

3. 0

?,S

r. o•s o

5 s'

*.V

5/

5.4

SLUDGE

GOLD S

.^^

-M"*

-i1 /a t -t

.610

J{***

,iOT,

-hace.

.061,

f*±

.002*

.Vis

DIAMOND D0LL RECORDPROPERTY HOLE No..

SHEET NUMBER.

LATITUDE -^

DEPARTURE.

ELEVATION .

SECTION FROM,

DATUM _^__

BEARING ____

DIP ———————

.TO, STARTED

COMPLETED

ULTIMATE DEPTH .

PROPOSED DEPTH.

DEPTH FEET FORMATION SAMPLE NOWIDTH

OF SAMPLE GOLD lSLUDGE

~f^———r-

-fi

77 ii~

6-5. 3 0

2.6-

.-^ * 3s .06 t

D l A M O N D D WL L R E C O R DPROPERTY HOLE No..

RHFFTNUMRFR S~ 0/V SECTION FROM TO

LATITUDE DATUM

DEPARTURE BEARING

ELEVATION DIP

DEPTH FEET

7 S *1. f f fi -C.

Zto*- 3,16

S'^-*-,.*,

5/7- 5" - 32 y.o

Zzi.t- i'"-' J

FORMATION

4753.6-^**'; ^,^. /^4r, '^*** '..-^^ ^ ^-Jfc',/'f . f?

jfy^j.? S&+ A* 4 iHitj ^t#ytt4s fitj^ A A 'Sr/tttt tS*jfyr*MV AS*rV ij ' r

f*ft 4 ' "rf 7) ' -^tX r/

i **j* ^ ^ '*' M y / A7 ^ ^^ ' t **s r*

\ f t S-, .0 * , , f

'p'ltA'*^ tftt'dd fsf.,fa**- tstffyUi jt*ft'd^ ^ s?2 6 s tp f:* 464.4^4*f r f u f tf -s

VH'A- : ^,VA /vx^. W^. *W ^/4-.,,/^ , ^^"4, ***4^-4/ tS'.*^"6s -y^/v^ tnwi, 1/ J^tte- A ses'-zo' ?'*'--rs'

- y '

fra o'' : ;w. .L/^C^r 1 C

^' v '' f-'* @ ,' 7

f"f~^)i f rt ' ^f'^- .c Y ^ ' ^"^' ^rff^- y* " fVi/

-/^V a,,--v; /, ,1 ^^ ,f; rf ,,^(, ^,V^'VXH ^f ^

Z--* X, -' ,. Ji&i**. l''.-*'- O "^ rf'

^•....-..-i ^ ,.^, ^,^t x^,^ V..VAXr ' '

CWO (5^ ^/Lff ^ ^"7^-^

SAMPLE No

MS1I

HW

US**

15 W

STARTED

COMPLETED

ULTIMATE DEPTH

PROPOSED DEPTH

WIDTH OF SAMPLE

zrto.i* o

r e*. W*

W.t'**o

vtS'fv.

GOLD S

?, 0

3..0

^ , o

r^ '

SLUDGEGOLD S

.0*1,

.00^

•Htt*

,06^

DIAMOND D0LL RECORDPROPERTY HOLE No.

RHFFT NUMBER ? ^ SECTION FROM TO

LATITUDE "?Z04 DATUM ^* 3 V^ *^s.

DEPARTURE ifo97VJ BEARING 02*' (Hfe)

FIFVATION 79^9.6.7 DIP '*-** 0 ^^

DEPTH FEET

0 -/o.?'

,.,. 3 - :,^

.-:-'^- 7'1- D

- ,:V;.. -/JT

^.•T- ^1

V 7*Z- 3*. S

".',-r- ,;'.o

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'.'' . S ' " '\' '-'

r- i- y-o

/f

FORMATION

'.-.^; ,)

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C* ^ p

!^;^; ^.^,. J* .-.^- t ;,,,,^ . - '-4 ' ,^- , /-, ^ ,v

4 ' y' V 6 SS S ' ' -' ' " '"j ' f i

7 f !

"^ , y - ' - ' / '

1*.'.* ^'- , n,....:^ s.^:- .'.,:~ *~.^ S.*'.:*Py** J ^ ,,

^.,H , v,d. fc ^ /V .v^^ '

; . ;.:.', . - ,,., . ..r,;. ,. ,, '-•••. ' .

/', . r / .^ - rr/.A 1^ '' t'^.

' ' ' ' . ^ ' ' - - t'-'' ' ; s - - -" -^ /V ' ' ,- ' ' ' '' *, ' J ! . " - " J'"*"- *'

- ' .' x1 - * ' ^- ax ' ' .^*y*^ ^ /;'*' ' '

^ ,-/ . '-j ' 'J ' 'f ' ' '- i * - S \ ' ' ' - '-^ -"^ ' '"' '^- * S t "' '" '

,-.-,' ,- ,/,. - '-. ,v-?r. ,-v^'-. -^ - ^-y v.. ;,/,. f ; ,-y - -v:. ^^.. - , ,-, .,.,^...^ ., ..,. ;. y.. -,

' i ( i ' : * i ' ' ^' -z"^' *)s'

1 " ' ^

SAMPLE No

nsyf/fSVt

'StKf

/t^7

" IS"ZC g

* / S'te

't'^g

*/.- : -.iJ

'W1

'•if*0

*sst

•-' .-."l, i

Jf !f l "8 7

STARTED V v '^ y/WK/"^

COMPLETED ty'J !^^

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PROPOSED DEPTH

WIDTH OF SAMPLE

/8. a- z/ j

Z''^ - ?t:0

?ij,0 *"Z ^'i

z^-2-2

23^-;'2-^.i-^.f

^,r- M .

.S..-7? ^

72.!)--"!,-.^

7<.5- ^ :-

-.V .' - - "

ac.-*'.o

^.* - iy.5-

GOLD J

?. 4

?. i

O. i"

3. 6"

- 2.

^..C

. J

?. :

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i, T

a r

SLUDGEGOLD 5

-If AC -f.

,c*G

z.o*

,60-t.

, Ctb

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, 002,

^

^^-•r'-- J.

.00

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.//i

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T /^

DIAMOND D ALL RECORDPROPERTY HOLE No..

SHFFT NUMBER ^ f ^ SECTION FROM TO

LATITUDE DATUM

DEPARTURE BEARING

FI FVATION DIP

DEPTH FEET

y Sv.f' ftf-fl 1

'f /. 0 - 7/4"

r -7?.f~ ''fi. f)

* ff.O ' 1*5-0

•SiT. c- l -'-i. t,'

//f f - l*.?/)'

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FORMATION

^^. X *:** j***,*,'. . S,,,.'''*u^

2*#* ^ *' "^-^ ^ 3 * /***** W* #rX***,*r ' / 7 j/ ? r

s

ty.fa'J-*-!/ ' .'•'Pdc'yh*.- **--- ./4 , /lk*3-\ ^*'; tA- i*7 -#'\f3 g ^S

'C)itv'JL. ' X^,/ V.^y. -^ X^^/ ' ' -A*. /* •^'••^ J'^-.;^ A/iA***^^

Jt-r-t'L tt* '' ' ~'^***-* ?-'"l ' .''.-f.'bl t'-', *' .j.'.ttfa/fZ.s- f l/'j^j&T rf ,to/* W?Sl~*J

J j

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l/

,, '-,-^ ,- :-t: .6*',.' /^ *,.-',^ ±.,,''-s.-(~ s - ';- M .."s "6^

-,, t ^,.,,. , y,/,, /f . ^ ^

fa ' ?, i ' 1} ' f l- ^f'.'i '*t '. -f'.-

-" A"' -'' '^/v- -y-^ ', x ( ./•••V i-: /,- ,-^yf .^? î*.---.' 'f

- . ^^ .-. y '' ' ~ ( ^/^y 1 - ^ ^" '.'. ..y ; '^.•'•^ '7 •/,-'v!. X l' ^^- •*y ' * -' '^ - '.V. . s ' .V.-' ^

y. 1 -' ' . ,. '- ''X ^ . ^lff ^'f/s-.t'-- *, t, :."' '- * . ^ : , , rf - x",

.,A ; .,A *xx, v,..v, ,^Jv^ 4yfc*^ A,^ .^ ^.,. /* • !^rf,.v*,' ' /'

SAMPLE No

"/r?^'.sin*,61t*

'ISit*

* /JJ*f" /f 3 /O

/^*

^52,1

.-W3

y^?'/

•fwr

/*5S*

W

STARTED

COMPLETED

ULTIMATE DEPTH

PROPOSED DEPTH

WIDTH OF SAMPLE

#.*-#.*'

?^5--f/^

•?^-^.8

•#8. -^,r

W A -'Off. f

/tt -S- KS. 5

*f..S- W

'li 3-13 -1.]'

j

!ty f."jf 4

•J*..,-'*. d-.vj-.y,'..

•^/••'^.d

/^•/53 -

GOLD S

5". o

^~i b

4.3"

(.•s-

f. .0

S*

2..T

)

? J

?.d

' 3

*0

3. (5

SLUDGEGOLD S

-Tt.-rt.

.6/2-

Vy

.OSi

"TV.

-*W

.frz.

-1 /tt*-

•/'••"-li

.^

,MZ-

-Vw^-c


SHFFT NUMBER ? ysr SECTION FROM TO

LATITUDE DATUM

DEPARTURE BEARING

ELEVATION . DIP

DEPTH FEET

17? ^ -7-21. i

FORMATION

1 " ' 7 ' t1 f;

' 3 c'

vs.^ '.-rg.* , t ^/^^^^^^..a. y**,,,*. y jâ, - ^t,,i xw*. t j. -y ——

M t-', t* f ,,-^ .* -t.*- 4-^: ,-'..t - . ; /, ,- v,i ,;y^ /—

f^/if trf^' f"

••-"•— - -~ ' " r / T 7

,'*5.*..' k f.', 'VA, y- 'O:- ^W .;/^^-^^;.^^ ,.X-..^

^.^,,/ ^ ^. .^-,1 '

w,4.. '--i ^t.

,..,;j ^.^ , ( '...^ # , /^J ^^ v.^v. /!î y^ J'***j

2 'l 5 " T'^'. Z ' \i'-',?' f, /-l^ j '-S: ' ff*'*'*''^ • '- 1 rfi^.'i.tv ' A'fJfjt^ .'-{i- x ;X7 f'.1 r ^ ''

SAMPLE No.

14 653

K5*9

I4SLQ

tff*l

list*

,*st*

p *-J9*

STARTED

COMPLETED

ULTIMATE DEPTH

PROPOSED DEPTH

WIDTH OF SAMPLE

a? . 8 - /j*.*

-^. 3 -'rt,jffi.*-'"."T';-^y.^

/;v.o -/if 7,0

'-:~! ' f 7? O

GOLD l

J .

?.o

"5 'O

70

7. o

•To

SLUDGEGOLD S

,^*/

-lit* -e,

-4 1 a ce

Jrtx-e,

J,6C*

Ml.

D l A M O N D D m i L R E C O R DPROPERTY HOLE No..

SHEET NUMBER

LATITUDE ———

DEPARTURE__ ^

ELEVATION __ ——

SECTION FROM,

DATUM ^^^^

.TO- STARTED

COMPLETED

BEARING

DIP -——

ULTIMATE DEPTH

PROPOSED DEPTH.


OF SAMPLE GOLD SSLUDGE GOLD S

^^, -P-

(

'•7

0 .2-

(F ?

S? It-

s 7.*

l \ DIAMOND D0LL RECORD

SHEET NUMBER

PROPERTY HOLFNo

f f f SECTION FROM TO

LATITUDE DATUM

DEPARTURE BEARING

ELEVATION DIP

DEPTH FEET

537.0 - s te.o

FORMATION

#i*s*-W7.'; ^,,^, ^ /.^^^Jt ^jt, ^ tftAr-y+HA,

*~A' r'' ' * J-^. AÂflj yy^ ; ^ t? 4^ ^ ^, X^t ^5 fi- -c ^"-^^ -* rf. cs/otA , . ' **xx i *

a J r l?rf^-dfa. /VV^ c , 'S'tS't^ - s? : ^^ A( X^^^x t 'T'^C'-sSt ^^ /\) '/S-* 3^*4*^

syfrf&t '#' V *S*ff fi fyS'ff/f^d ^'"t-t/A^ -a *4^' .(^ ? ^-?C ^ 7

P fjF"' df~ jlCLi fP3t@tf *

SAMPLE No.

^*f

A

STARTED

COMPLETED

ULTIMATE DEPTH

PROPOSED DEPTH

WIDTH OF SAMPLE

??f.a.jf70

GOLD f

/i 2.

SLUDGEGOLD t

^^

DIAMOND D*LL RECORDPROPERTY HOLE No..

SHEET NUMBER,.

LATITUDE

SECTION FROM l * ^

DATUM y* 3

STARTED

COMPLETED

DFPARTURE ^ ? VÔ BEARING zc** L* 2't '^)

FIFVATION * "5S7.^ DIP -^' */ ^//'

DEPTH FEET

0 - / C - G

,o.a. w

l-O.t)- ~.,', u'

- i s1 - - ;; 7.

V.2- "1.0

* v ;.*- -*.ai-y.s - :^.^

rv, o - in 1-'

FORMATION

-^ ZSf *6, fc*^^} 'futî-.^ff -Wf-.V.'j-C .^'"'l /I-^S^rv . /V*t(, -C/^JÔ

y ' /y '

•7*,. r '•'•"••i1 ' /^'/t^ -*^..i^t -^ ^t-M, -A* -i; K*-?i^ ^'^,sua**U

X'^y /v: ^ XV. ^ ;"*X^,V --^: vVW syS^*r^:*

^-.o";

^,^fl t*,.^, - ^..^ ^,,V -^*... '- ^-^ n-^".7 f

^^ ^ '' ' t f (

^•', j^^.-',.t -.^-/., ,v,i ' '

W"/ r '. d*X '//' .J?**' fr^t.&MS'sS L2tS':t*s . . .vJv î-y, î-vX x^ -fS-t* ^/'.,s-^/

;-'",S. 3*, b- *.^, r,-^. ^ -^ ^ --,^;^,\:^,^6-' r

/xj,^. . /'-'.of Xr ff-e.^. ^••^•^.'.'S.. '^"^t/fa /.'//ft- 'Jt^f^.f^

^.^

/' rV."!- '"i ' ,: -' --.x .x'.''-.- i-'*/ ^-.-y /••': su,;itt- ' - - . -fi-

- . .-. - i. A,

; ---.-X-^ ,,vy^,, /^ ,-^^ ^ _ :x, J â /*s*-**-4fi '

S '.^-fflft .•'•'•'''*' •'•.'•t * '. * ^ x .'^-*y'Or /S^^ tfl^t&i , ' ^~^'-*4 -^.'-f. X':f ." . "^-*-- i*!.Y '*'^^-Vv'

SAMPLE No

. -,^'

^.^/^

*- /5.'-.^

ULTIMATE DEPTH ^'

PROPOSED DEPTH

WIDTH OF SAMPLE

J?.*-S*2,

^-W.^

^^^y.-5

GOLD S

2.2.

' 0

--.o'

SLUDGE

GOLD S

-T/.^

S" '

-7^,

•PA

DIAMOND D^LL RECORD

SHEET NUMBER

PROPERTY HOI F Mn

' ^ SECTION FROM TO

LATITUDE . DATUM

DEPARTURE . BEARING

ELEVATION DIP

DEPTH FEET

,,*.;- z* d

FORMATION

f.';-,. " V X/:.- -is.tt. "•f'.'.&C-i . ' "'-'' '-' /vif-v .V'Ô/'X^-

' 70 f -7 2.0. ,-;/ .j' rf''''-", 4.**-Jt,. ^Sf,:?:*- -V -^ '" •''•' ,J C [

^^5-^'; .,, /.. '^,'.^ -//,,/,, ./^^ ^^ ^.W -./.^

.^•-.•.,.-. -^ ^,'/ ^.-^-,. - , ,-.,'*/-', '

* i? 11*0 i 2" f St 6*. -s^'/, v^^ y ^,.v'V^r;.^y'

' 2^.*". ^" /'.*-l-J --^- J.-^frtXt,^

* (f .^.o- ;;.i.; *.v--i, ,' S-? r'; r^j^/î - v/ -^4. ' ^/.v i-" ^ A'-^'- ^ ^ : ^ .*/,^-' -, . ^,.-. '' . -.,/. z • s-.-r -r .^ ,- -:, -^

: . /y,;',,,,-.

y'W /•'''- r. '' ^-•:^- A -^- •••-./u .-^. ;.-,, ,-.^v.^,;... .nv,y; ,,/,,- . X -' ' -V;,', ',' ;v? - '-.•:- ''t ,- -'.-

- . ' :. '-,' ~'- '' , /'-^.." ' - r -,./, '- '-i-

. . . . . ,, . -' - ' ^

-; . " t . , ,/ - ',^, .-:., , * ,,c . A,//'-' x .^', ^*:r

^^, ' --'S ^ W± '-~- s-k~* .4 ~**'*i'J* -,; ,H

SAMPLE No

; -?5-78

/4571

'/S'-f?

* IS W

* -m* / C 2 00

* .'^0,

* ,s?^

' ^6

A

STARTED

COMPLETED ^

ULTIMATE DEPTH ^

PROPOSED DEPTH ____

WIDTH OF SAMPLE

•,o.e-n.o'

&.J--V i

ll^.O" Ci, c.

/M o - M .o

//If. i/- //g,^ '

/Av^-î ?

/^-/*?o

'i?.-- c,e.o

.Vi- J'S'.'.'

GOLD l

-s . C. '

2, c , '

?.o-

?. 0 '

0,*'

' 0 '

.r.*'

-r, o 1

7,0

SLUDGEGOLD I

4r***

±,4*

"tsLî r r

, cc,-

- a -5 - f.

, J O t

.-'.i

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J *

u——— r-

V

V

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.i

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DIAMOND D,9LL RECORD

RHFFT NUMBER

PROPERTY HOLFNo

3 f 'J SECTION FROM TO

LATITUDE DATUM

DEPARTURE BEARING

FIFVATION DIP

DEPTH FEET

r w- r^

FORMATION

yr^.r-^': v., .- ,,..' ft . yy,,. :v, x,, :#.,^ ^.,4 ^^

;,-fc* e* .~'.' .,. *,; , y^,,.,-V r,,,^ ^^;,,:W/;^

X^V/^X ;^ -J'Vtf.*^/*^*"- "- ? y v

y ^0 '^ "' ^ • 'A-r '.-,'{tf:^ i- X, , w?x ' -^ ' *-t *s-^*''vt(^, X^* l*A'.jrJ';'- ^ , . ^•vXv*^*^^y /V

,-/^- :^'i: /. -,, ' y..-:. ', ., . -. ,A'-,,^ ^ : ...-; . y

/, -^ ' ' /- '.?. ,- ,, -'.i ' .'-,' •••' -t** , . ' '.' ^ -'. . ' . j-iV- - 1 j -- '-''-

1J: VX .' y, . #v...'-' . ••-.- . - V, ..yX,^ V^; Vxiv/V .

"y . /-'•i, ^ /' ' -f'f

,., :/,. - , ' i~* . .v'^ ;'.-. v . ,,.-.-,-y- ,,y ,/^-'-. x. . ^

-W.,. .-". - -- -' . .'••••^'.^•- - ;,, -^.v, ,..', /. ,-^-.^.y - ,.

••^•;- ' --: ./,, - .- - ;- ,.,, ..,, y,c. .^.,? ,^ , v..... v .^, V, -,. vA

C/ -^ , ' - v -' - : ;,.,^,,-^/ . -,^- r^ ^ .''X.-...X -a^.,,.,/,.'^, ?' ./^../^1

,. . . ,.. t , . . ; : . ', ;., , . . ,- ,; ,. y ,.. . f , ,,,, ^ , , ,.,

, - - , r '.

i\" A.' -

^ .v,,. -.-.•,- ; ,. ., ( .^^y^.^^y^^ ^^

SAMPLE NO

/^s"8/

/î"8z-

tist*

t cis B 1/

j 4585

ttstt

/4ZB7

,^ntfStt

11516

If ffi l

STARTED

9

COMPLETED

ULTIMATE DEPTH

PROPOSED DEPTH

WIDTH OF SAMPLE

/4W---7U

nc-o-2-7-,.0

'K.Q--i-rt.s

m.j-m.l

z7-v;-7*'.-

.^,-^.'.0

g j. o-3f..;,o

25 *^-!W.7 0

?09!^S^J

-Oj^â

?T***5

GOLD S

; ,5-

sr

?.o

.: . /;

7.0

-zo

*. as.o*:j

< ,

SLUDGEGOLD S

**tt,

4 H! i -f.

M**

-hut

Jt et-t

J,o( i

1*.*,

-h f. i

.m

^

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DI AMON D D *LL RECORD

RHFFT NUMBER

PROPERTY HOLFNo

V w :/ SECTION FROM TO

LATITUDE DATUM

DEPARTURE BEARING

FI FVATION DIP

DEPTH FEET

s,.? f- . v

3ii.O- y-'*.,.' 1

FORMATION

'•*'- f.* .l* f -**-t -t ^fr Wnr\ -S'#"L '"-} -f- "t- /*-*^

•' -.s' l x .y*,'*?^ ^^ *i'^- W^/ ^X. t i,. ...^-.y ,/

'

••••i /' i-'ic/.' .-•,-.r-, ''-' -, '//- , /-"i- r. "-j x ^j.vV^', /-;.'.

,, ', y ^ ^. x^ û- j Al -,, - -i,:./ ^^X 'x^,^x ' x * ;,,lj - ' 'j,. " :-'-'-:/ ' t..'*{'; . ;.'*'. . '-' ":)-yi''4 -^J .

i " !) ;f" //a i'' \F 'MG-V'

SAMPLE No

A

STARTED^

COMPLETED

ULTIMATE DEPTH

PROPOSED DEPTHWIDTH

OF SAMPLE GOLDS SLUDGE

GOLD S

DIAMOND D. •li RECORD

SHEET NUMBER , ^

LATITUDE i 9t

PROPERTY y^V . 62,- ,,~-:-* -* ;-*^ 7^,^ HOLP No rt 'S \?**"*'

7 y ^ SECTION FROM TO

^ ~r R DATUM A/*. 3 x*^t- *^*t-

DFPARTURF &99-S-4, BEARING 0 10'

FIFVATION 5S-5". o? DIP '^'

DEPTH FEET

C - ?1 0

7 1*' 3 ?- 5

, , >s _ c gvr

M.S-- 7 '*

w -'

FORMATION

C.^^

^*~ -jiW; ...^... f,.,,,v^. :^,/. /-^c. ^.*, 4^^., ^- t ' , , .' ; J ' ' i,***

1 - 'X ,/

',. .^ , , J :/,^, ^ /; :i .,.,,.,y, x-. - -^ *..aw.^-

^/,,,^, ^ li

^.v.î , /;,^ ~-^.. ^ v,^ .{-.^^. ' -—— ,^4 , ^^^..#'" ' -*- f - ' ,- t ('

^ ;/-.^.,^, .^^.,;/^^ --^ .v.*V.',.V*r- ^ -^-^^

, •..--'••..f' '-*. ,i;*'^' , - I,Y^..' 'r. . i^toiv'v*' x,i -'' V • U^'--*f* **ffi6~3.7" " " '

f., —, 6"::,' - vs"

. , e ,:r... . ^ 9ii . S ;-ii 7 ..., ,. ,..- .^...^ ,, U ...*V. 4S .'.r7 ' ""

r,,,..,.,; , ,^ ti ^.t ; ,, -;^ ;,..:-., ,,jt M, ^' f.

1- ' . '/r' . ''"t,

. . ' . ^. .^ y ^ ,. t (, ^ - ^ ,..

1 -- '-'

. . - - j , y y y . t- ? ' - - , f - ;- . '. ^/^'F-* ,-(.-

SAMPLE No

"r." '2-

V64V5-

i/.jM

MV

")^t

*' -,--?

".^/V

STARTED /1 0 ,.l *^-

'-oB^v)—- — _ . __

COMPLETED ^ w ;/ V^

ULTIMATE DEPTH ^• d '

PROPOSED Dt

WIDTH OF SAMPLE

'•3 -5- --'f ";

I A : ' - ,

^L-'^C

75 ''-~7 G. O

••; ;ic

Z,.?-n*

GOLD l

-~ c

-, .

'-- '"

T; "

.^ '

f. (

EPTH

SLUDGE GOLD S

TT

-4{fi-e

J s j i- -t-

.001,

• ;^

.•t

.632.

DIAMOND D 0L L RECORDPROPERTY HOLE No..

SHEET NUMBER Z f ^ SECTION FROM TOi/

LATITUDE DATUM

DEPARTURE BEARING

FLFVATION DIP

DEPTH FEET

* 8~l-D- V-C

' no- ^-0

' - ~'-\-j- ^7,0 '

-r? o- ••an.

i"1 "t, y

'•y..*). ;-'ji

FORMATION

,-W^.-, ; ^ ^,r ^ /, ^ ^^ ^.,tf sstt ,,^,,/-T', ,.' -i-;', y^-. '' '- f ,/.' VAj^tt ' s?ys.4'.,l4(

"2ir.J*\ Jr.- •y^-.^C " : - ^ . r-fe^ ^ ^-., ^-.m-ttC t,:*w*t~

,^^ ' ''to *,,..,; -.,...-,,.,,, n-. ,, ,. t -x ,/,. , -,,,,^^ n^l{ ^,^.. ^ Ae frfi - , z.

7 ' ? ' ' 7

f

'*~- ' 2 '' ' x J " ' "

'0,j ^,. { sS ssef,^ Cj,^^(. ^ ^^,-..,,v, ^ ..^"* 1 f ' ' y

^•'* , :.. -'- -v .y ;,^,..:' --^ ,^.^; -- ''^^r

' j -^"y s s^.- 1- '.'. ' e. ' ' "f,, - 1 ' - - y " " '' ' ' [ s ~- ^ j' ,' - i ;; :^-^-v ^ 'f t* t- ^ fi/ 1*0* x^**^^*^

^/i." .' . *- ^ ^/' •• J'-' *- f ' ''r t f -- -

f - f,V. ; ...-, a- ,,.^': ^;- y ^' v ^. ;; .,,:^ ^. .

-,.. : ..' - ,- . .-" .,, ^/^ . '.:..,ff '' '-. ,', ——f.

/' ' J':'' . ''^ J'/'/ ,l . . -- '" ./,'y'\ ^•fffJ'Jf^, * ;V.-*. ^ ^X L -J, X-''-^ ."/.^ . '.'

SAMPLE No

^5-j..r

*"*'r-v

•"' V./7

if t, ty it 9

^0t 5 b

145* l

i^ôZ'H?*'W*

H&f

H Sob

,W7

ns*t

STARTED

COMPLETED

ULTIMATE DEPTH

PROPOSED DEPTHWIDTH

OF SAMPLE

3*0-6*0

•^.f-ric'

11.C-07.0

-//. - - -i L"

/((l). 1 - '* 5 '(J

K*' m.*

Kt.*- "-'-f

k t. ,'' ' W

1-7,6- I'ô

//fi j- -fa

•:f.J"?i,6

•5*.*-.'i'-0

GOLD t

2 o'

^••'

: -. y 1

T C'

^ O

7. O

"i. c

T. -^

^,-o

?.d

-:,t

•7.6

?'- C

SLUDGEGOLD S

Z..-TS-

. ' "f Z

. S- 'j -,

,^2

,ao~Z

^*

~j 'n t -t

.Ml

JlK-L

.00^

,oc*

^-*.p^

DIAMOND D AL L R E C O R DPROPERTY HOLE No..

SHFFT NUMBER ?- "'f SECTION FROM TO

LATITUDE DATUM

DEPARTURE BEARING

ELEVATION DIP

DEPTH FEET

IU.o- Z"'

ZK.o - ; .v-5

r -^ s - : '' ' .c

;tS.,- : -,",

2"',o- 3 -' r

FORMATION

l, ^ ;, f l. 'f* f l ^ j

st''S^ ~~ - f-'^J " ' ,-' . x * fî'l/i f ,*'fe^ xC''-/! EKT- ^ .- ' J - J^ P^*\Jt.

T/) //i fej) 1- ' V1 ' ' "' ^ ^ " ?O* 'j S" W* /^5'^ * '•r-?

/v-.v-"A y ,/^^ ,,...^, ^^.r' ." ^' -^-^ ^.^ .^.T:*-?'

^'.•y - -" .4 -t.-* i ' l i r'~,'. -rf, x "'--^

,.--.. AiH /1^.7 ,' ^ ,.. ,.^',--^^. -î^

.. - -;. -./'- , .. . t-.*,.,*. ,,.*., y^;-t ^-. (y -".,.. '. i; ^-,;^ r, 7 ... y -

C, :-w., ' y 7 :,y,. ..,.,./,

js'/j'x/t ^.c ,,'f, p/- r .'^..•^'î' -îVi ^,,,tîst Al-4*- f^f~t' ,

.^ ,. ,,,-, -' . v;^ y... ./ p : , ,,. ;,AL ,.

/' ' ' - ,- - - ' 7^,V " ^/..^' . ' . "./ : t. . :.. -\

/, -.,.-,' ,.,i: * ,.-;..v, /-.,,:^ X ^'4,., ^ ^ . ;-/*.-^^

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,. . f .'-;.. .ff j, /v/... ,^,^ v^, ; -,.v t, ^. /, , ^. ^ , v•V V -' v V,

;,--;.j i , - . - '.. ,; : , ,,/, *. -. .. - (. ^ , i ..- ' . ^,.,t //. .^

•^,' i/t/,'.- , ,,, ^-.v.'^s'-^',

# ".? ? .-^y^--, ^. ,1.^ -^^, ;^^ , o.v,^ ^^

SAMPLE No

/?5*f

fi f /o

I45rt' o-^

^ ./z/ ?

STARTED

COMPLETED

ULTIMATE DEPTH

PROPOSED DEPTHWIDTH

OF SAMPLE

-i w /**a

^,, -/.^.^

^.S -^,..c

r.^.,.7^.4

77^ 7^0

GOLD 5

7. 0

T.,

/.tf

' u

/.^r

SLUDGE

GOLD S

-4r~

-//•^t*

Jrt't

.60*,

TS

DIAMOND D *LL RECORD

SHEET NUMBER

PROPERTY HOLE No

V ^ ^ SECTION FROM TOi/

l ATITUDF DATUM

DEPARTURE BEARING

FI FVATION DIP

DEPTH FEET

J//, 4- J-? i

5*0- **t

's 2,1.0 - *'-',, C

W;- V'-,,;

^SV..*3*.6

FORMATION

fi 2ft-Z ~yl-*', ///*KV"^ X'- . A/'^-JS* ,'f* j* . .;- rf,wX, aen^^j d-ffi-t*'

^/^ _ :^ ,,T ,,^ , .7.^'^ A/*,^ '^;^ -K^/^ ^

Cl-ryv "i*- .^yi A. * 1 fix"'-- / -t t^-^^ctf-- 3 jttt+vf^ f^lt /J 1 / / :'t r ^ V-Xi-i' ^

/*fj , y .j ;. 3 . 7^

"^ Ji ''r ^' ~ " ** *' ^ -^ i .' v / -t/^f^',^ jt. ^'^C't^-'Âff '^•^rfi**'Ot^*t*^''L- **? "^" ^' j - (i^^'jA^*— ,

f.'^J' ' . --". . ft **' ~ -^^"jf/f ^S*''* '-' ' 'J'"" Jfr 'l '&T ^/* ' ' ,-

^ V'u?"*. '-' ' 'l . •V*'- '-* i i'' ' T1 . "j* '' '' jXv .•Z'A''* , . f "''^r , ,^r~f 1'-ty,-^C.** 1 ' - Cii'V* 'i'*-*^."

xV-' 1 '' ^ ' -••"^ ^•"--' ^- :^ ' ^-^ ^'^ -^^v*r ; ^

^ jtjfaf*', (t#s'ef .-K^T'''- V . / Iv* i'ifî' /S^xJfe^-j *fal*-(*^3 i f'ltt^l ^Zf'/'d/t \^^

''*^f{ftf*^L /t'/j^ ~fpj**' -* ' O"-- ^ V*"-''v SS-t'tr t*'** ' ^-i^^vfo" *i*4*-s J^î -O .

^ ' -f

•:, X/.Vr* '-^ -

:^^ ,, ^,.-,;i-; 1 ,'.^ : -^;^ . -v—^. ^.,..^,t ./. rv ^.,, ,-^ .., ...:-. f -t r^^;/ /i^,.^^ .e* x,..,.

X^vV ; . ^ //p^, /.--i ^ ^ ,i^6 x,-^- y- •/•I./y^X. -l^.A-*^

' ' j s ' '^"\,/. , .- //y ' -', L/ /i '" '' ~ ^ x" ~

. v,.-^ /^,, ;,, ^., i/, , ,.^ ; ,,,;^ ,-,-.. ,. , : ',-. x./^' ''.'-- • P !T-.'*/^ i'' 7'* i'" '.'--1

SAMPLE No.

/-7SV2-

/^/3

^•y/V

^

ms^

STARTED

COMPLETED

ULTIMATE DEPTH .

PROPOSED DEPTH

WIDTH OF SAMPLE

s, r 4. ^ ?r- :'i

c;,^-,;-.^

. V a- "\'V J

GOLD I

?.c ''

T C

V 6

SLUDGE

GOLD S

• flOZ.

^^

4,M

D l A M O N D D •l L R E C O R D

SHEET NUMBER

PROPERTY HOLE No

5 ''^ SECTION FROM TD

LATITUDE DATUM

DEPARTURE . BEARING

ELEVATION DIP

DEPTH FEET

S*.* - ,,S5.0

' 385.*- M -6'

&I.*' 31*0

jr'W.i- *it C

FORMATION

A^; ,.w,,U ^ ^*^ ^^. ..-V-* -A *:*^^ .^,^-c.,' y

:' C

tt I7t. t '-* 7 ''-6 - ?... s"-' .'Ss*i yi i *" Va' ^ j^ Wi . I/AC,, y/..-; jS-^.^/c

.'0* t"^ ,-^^^-y-' ..r^l ^V,,

/i*I^r^^^ 6 OW-tt- Ssffjfi. r* j* 7j \4JKf(. /'- "'V. JL 4-4* t Inpi+'J**.- ^Xx-^^v/* ^** ? ;X'

j^Xx'^.A/ v,'^ 6 A;A.U**s S-efiXfC. *~'--- J- J**t*A**Ct* s'fs'.i,-.-r d f r

Dt*;.fc- - KX*',- A "**~ *^-x. ^.'x^^ /'^y.v-r

''•^ r^jSv-' ' CijV * ' ' * , î-'/ ** ^'/^ ' f •^^-' 2t\ S* f^Jy&XJZ// . ^/'

EiVto (jp âtf (^) w/ig 1

SAMPLE No

" '^37 O

MSTARTED

COMPLETED

ULTIMATE DEPTH

PROPOSED DEPTH

WIDTH OF SAMPLE

Stt.o- 3*.0

GOLD S

t.O '

SLUDGE

GOLD I

T^K

DIAMOND D ALL RECORD

SHEET NUMBER

PROPERTY V I&UD Ceôfctt TM. H OLE No * ^ (^^

1 'f ^ SECTION FROM 7 * 06? tf/fl/ TO

LATITUDE 112.9^ DATUM ^0 3 \U^- i***^

DEPARTURE 17OO&8 BEARING /-^'

ELEVATION 9*3-66. Z& DIP -^ ffi - * ^ - l? (K* ffi)

DEPTH FEET

•^ - / /.ft'

'1.0 '

FORMATION

"x^;

'Dlf.Jh ; ,^; , //, {: , /^ ;^,.v Ut -UiCK.vX ^ y^; ^ ..^vj.. X, J^y y

X ' /r

7 f c 7 f - ^ r

1 -' 7 . - 1 , ( 'v ^^- **.-;'-i'*.- : ,.;.' 4*4 ^L , .,^- -*,^ ^ .^'^ ^

*";-.*- --.? ' -- -'.- '^.-/. :.v , , V -- y^v, 1^,S- ,*.tt, ^ ^ A*iA

•^ " '' ^ ' " J' J S&*-"' s* s\\' -^ }-^t -tst *JS'.-A S.^ X-T/!'^ r^ -vv:V '-'^-f'-S^'ly ^3 *-J'-Sf\

r

X-v VV ^.f v ^^ ^^ .v.^4 ^,r^ tf) ^' .

A,:,, ,5,;,v^

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-'^' - -if : / :,. .^ V ^*^. ^K .'. ^ . ,. -.. ^--w .^..4, M.^,,,w^ --Ôv,^;^ -, / ^.^t*. s";tt44***~0~

''•' . ,*.'.' #. - ,, ,' ^.'.;.' -' ^

1 {

SAMPLE No

'6.

^ -75 1

4*:*

i' t- 5 753

t: 1 75"'

^' 755'

--: 75t

HtfSl

STARTED ^P/ 'iV'* 2-

rt M^ \- •i9/!"^ J

-~ — . ——— ~s

COMPLETED /IP"/ ?/^

ULTIMATE DEPTH ^'

PROPOSED DEPTH

WIDTH OF SAMPLE

ft f f 1.0

iV.j- ^7.0

i? 3 ' 7() 6

790-7T.O

'J. 5 - 7i 0

•/^ /- - n o

IS. C- f 1-6

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,-S'

:*'

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;.9'

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SLUDGEGOLD t

^ ' - " '

: ^

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DIAMOND D •L L RECORD

SHFFTNUMBFR

PROPERTY HOLE No

2 'f ^ SECTION FROM TO

1 ATITUHF DATUM

DFPARTURF BEARING

FI FVATION DIP

DEPTH FEET

'*.t ' l-Jf.!,'

i*.*- - z/**

FORMATION

fs.v- ft--: M, M^;,,x. ./.^ x:/,,.. ; ;^,x^ - ^? ,. /* ,/./,**.,,,...**-,* ' s* *w- .',{{. ,; JS^,-f -'^'.^6- f"-,*'-'- *f**i 'S'''**

• J S ' ' ' ' - '' ' "'

" " y/'/ A /'( . f ' - '

f' * ^ ' ^ /* ^ r^

^ ^ .r

... .. , ^ /' ^ f . f^ •^*r

-'*.,*x? ^ -^/, i .^^ ^^- ' ^s'JjJ*^ —— ^ 7, . f r7

^ //*^ iC^Ct-. 1 ^ - ss/A,: -, **r *fy l^-^^ff.- ^*t*.*J*~ , f* "j f j /'"*^f lb'-*'SlStJ(- 'tûtt'f^( .r ; r c y t-'j*

/, ,^ ^ ^ -^ * -"w^" ^ ' JZ,*4 K'.,.* 1' ^, f.Ht. i: I.''**-- A 'W , ,.-'. , : *.**y*/ f' -' '/,'..' .'. J-/ . f' /': "* .','f *1 'f.'':- •'^j'if/V'/X - . f',- ji 'S'ltS , , :/

'.l ' -' ' f -' ' " ' " ' - ^ S ' ' '

J -, -^ :-*J -' --" --' -' ^. /-,. ^ ' ; " ^r--^

a, o fl .-: ,,-,y '-'^ ^ ^^ ^,^,^ 2 .r

-- v..:..* ^,, /^;,y -'.^. ^^-' ^^

SAMPLE No

^75-e^ itf

*ito•-'i, 7 i Z

407*3

4 W/

',:.J

. :\.r-';7.6

m

STARTED

COMPLETED ,

ULTIMATE DEPTH \

PROPOSED DEPTH

WIDTH OF SAMPLE

i*.*-***.o - *e. 0

/i^-f,1.*

'/It- H™W Mo

tlf.t'IZtQ

,^.-.,'.--4

/s*. i - ' t'rs

GOLD S

.?. a '•z. o '

w3.0-

2.0

?,*'

•', ;J '

S,.' 1

SLUDGEGOLD I

. (-'l

. 5 C 2-

( ' C ".'

. ' ' 7

-^/.'' .'-tf

^' i -' S

, . '•

, : : *~

}f


RHFFTNUMRFR J ^ '' SECTION FROM TO

LATITUDE DATUM

DEPARTURE BEARING

FI FVATION DIP

DEPTH FEET

Z'V 5 - 775.S"

2.2 i , i" - 3';-)

f 7 ? 0 . J't' 0 '

^ 3/i.ft- ?M.3'

FORMATION

^ 7 sf,'

^s*.-t 'sJfa- * T /#i ^ c^* j?-/ -f'te*-- 3,-v#**,/^ Xi^-tfiîz- ^;-— /t^J^2g^-^j jt^*C ^^4t-

/V- ———— r ——— - —— — —— ^"'r3"'-'^ — : — ij^r —— f ———— i — ; ———** - V X ' st** f

s.-.;i, .-.,, (± "i) , *-- x*r ././J* 1 /,-^. ^ -^^ ^y^—^.^ - ;,,.^ -;^;.A : ,,^ x* ^ ^^;,^. ^.^^^^s*,^ , ,~,.. ^ }^,^- ~s^ /^. ^y -^/J^,-

f '' - ^' ' " ; ' ' '' ^ '

Q774.0- ?n~/- ^ }.^,^ ^ ,f!J /^ y^,,,^^ ^v/^y;

J^.^ ^tf^-' ^ "^ - 6'^ ' ," ,^.-.^*4v ^ tf/* 1 finJdJ* 'S'

9 ,.D - -'V jo-. TTo ^.^. , n a;-/-/ -^ y^/:^**-•' ^ . X , ;-.,,.,,^ . /J,'^'.;..^;,; î'''(t. .--î'-d/^, . syt'Sfte.,

.1 y -x "' - '.' . .-/•'/./s/.'..

i'.-.- -'./-i ^./v, , - yy ^...v, ,, /y ^,:, ,' ^v.'.^- ' /.'. . '- x' /''',, - 3 /v x ..'/..- ?)/-^/,/ ^-.v// y.?i

^./•/-o-.'^ . -r 0^^/41.'

SAMPLE No

w.\wuitMl

"t-'/tf

'572'

V0776

ô7l(

wn?.

, K!

c '''St

STARTED

COMPLETED

ULTIMATE DEPTH

PROPOSED DEPTH

WIDTH OF SAMPLE

^•45-^7

^/7.a- ^74,6

22*.0 -^/T.6

7JPO - 2?S~.S

2*1- f**.*

?4*.*'Z#*

gio 5 " 2~"?t.2-

2^71*2' 2 ~f'r^

•: - -- - --.'He

?'i*-3^

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y.f '

"S v '

"5. a '

Z.f

^

2.0'

; 7 '

2. 3 '

•:. 6 '

': - '

SLUDGEGOLD S

. f.f-z.

,., -,,v

-.;,.--'.'*r

-^

1 ^ ^

y ' ' f'

.-' .'

i ..-if

* . ,v ;-

* . t ' '2

'

tfi.. H&i .

DIAMOND D •l L RECORDPROPERTY HOLE No.

RHFFTNUMRFR ^ ^ ^ SECTION FROM TO

IATITIIHF DATUM

DEPARTURE BEARING

ELEVATION DIP

DEPTH FEET

St*.*-

FORMATION

^ J* ^, f

j J ,A v ^ j j . ^^•:. '^sf*r-* ***f \ ' ' * s , ffa-t'jC. l/'s**'- -* *^X*'- /y\ ^Jt^- jC^-ti *~f- 2n^4frt--4*

ft x** ' - "t -y - -i L\,-~ Q k]

"~ ' '~ ~;"^"'.^'~~~~/ ~,~f r x"i^^T7^^^~

X c f 0 - Si'

U -*7.t - ^--,/y ^ , ,.,^ w M*** **S 6'***'-

,1* r'-'- n*w A '' ^ -5'' /- ,^-7

t-^ *r .^ 0 W.*-

SAMPLE No

^?V?

V'77*/

•X4775

4^

STARTED

COMPLETED

ULTIMATE DEPTH

PROPOSED DEPTH

WIDTH OF SAMPLE

SVi-.*iS*

4 b ?,6 ~ "^trt,Q

3^-3 ' f? ft

WtS^.*

GOLDS

j- O'

ff

! fi

3' 6

SLUDGEGOLD S

- - , , -r

. ' '- ~

,--2-

. -••7-

D l A M O N D D •L L R E C O R DPROPERTY - "fytgxj. Z***^ AM..,___________ H OLE No. * iS

SHEET NUMBER '^ SECTION FROM TO

LATITUDE P9i/*- . - DATUM ^- 3 ^^ ^^

DEPARTURE ___ 24

ELEVATION '9

*xSO BEARING 2^' Cs**' 1V

S8.i7 D IP "tt*

DEPTH FEET

6 - ' 1-*'

/l, t - SZ.5

3?.*' ,i,1

?r./?- (,1-t)'

(,1-b- (.J.*

* , ^'- ti.D

FORMATION

''OVh-

r

v /:,^ x;v /.^' /Â. W'v/,^/.?, ^ ^^-v^, v^..^J* f^W, ^^ ^ /,. :4,.r s,.:.*',.. ,^-" ™- J * **""'-

xVu*. /^-^ /M,^:',y ^,.:,''4S.^ s,^ls S*'**.

^nj;^. p*M'f f.*.'., -' w^ .^ ^^^ foy^;/* M ' f*

: -J, /. , ' S 1 r .

. .. ..'... . j? t J^- f

^^.o-;ti.f, s~*4 W 7 . //,, sJ*^ jj^t 0 /j- 4 c**.

l:.-*u* y.^; /,u 4w-^ //^ -i^ 4 ^^ ^^ ^s/^*^ r 7 f (Df

v.o- -t. a : ,;r*-*t ,* { fff^ ,^:t:i -t*-î

•J', y , , V l ( j , , ^4^

••-'" "y, ' ; i *\•- ' ' f ^ * - - *"-f , ' i* , *' -^ -* ff jsS- ' ^ 4r t s v f.-j, ' i ; .i'- 1* isff i -1 -',' * - *' ,— -

/' i ' t ' 't - f '' t ' , ' S f ''-f i C^f"' '44-îf* fS^' ' *^f'^} ' f ' -&'''*1 - -X i^j&f f ''4 1 'Stt f f\.f1

•f '

SAMPLE No

W 71

4577 8

Vo77f

^766

40761

,.,

^7te

v '5723

* /572V

•" /5 ?- 5

* /ffZ'4* /5-77 7

STARTED cV^ z ' //*s-1

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ULTIMATE DEPTH -?*6 '

PROPOSED DEPTH

WIDTH OF SAMPLE

^7.0- "2 e*, o

r. -S,.*

-21 a - ?t.b*

2i.o - y o;x,. 0 -:^

il.9-tt.O

Hit, - 1,1-0

61.0- 7^,0

',V.O'-*,D

^.0-n*g4t~ tt o

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-5.0'

^, j '

1.0-

S'. O'

r. s '

,' ;'

5" c

?.6

J.*

5".o

2-0

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--W-e

-/M,*

V/^-*

~-,:,:t

.til-

.'.,01s

Tf.

rr

ri2

.*W4

7 r .


SHEET NUMBER

PROPERTY HOLFNo

2 ^ SECTION FROM TO

LATITUDE DATUM

DEPARTURE BEARING

ELEVATION DIP

DEPTH FEET

gf.o - 'H, O

"'.ft- -i i-O

J '01,0- I'lj'S'

S 04,0- -0,6'

v /.'d, 3 - f i?. l) '

''3. C' "i t. 6

. , . . . 7

FORMATION

U^********. *y(*: *™**t*a ^^/^ .^,'n^ ^^tb.r.K.L*' ' AS, t ^G*t "

&&X-- z,.,.,/., f'*:*- : v*~~*s*, ^.^ ^.^. xV/ *Y;,J +-+J ,t'-'''."'; ,, t ,,,//,^. , ,/V.t. /^ /"x-î. ^^^.^ ^ "/J

f f ' sr

,^^-x. Or-ui; ^.v^/^t x^^ -^5^ -^5^ 7x;^ ," f1 7 iJ'xV/ 1 ''

"'"' '*' ^ * V

t-, ' - - -V-i/ /^^ -".-^ , .-' " ' -x; v,,, -.

/v/^ , ^ ^- x^ -i-^ x.y.-^ ^ -*-- •.••^^^^..w^//,/ ,^/,^/ ,* ,^, ^:. .--/^^^ x -,. .^^,^.

-A x ^ -

*" -c^- -- - ! -- . .., , ,, -. -v^'- ^yi -:,,

/- -x , -, ' s o-* .t*,.* . v^ f -*'

—— f— , r ————— /^ ——— ————————f? 1^4 ' W{ /ITJ"

SAMPLE No

^-'?3

* '5-724

" I5JZ1

* ,-s2ia* 16-2 SI

MM

* 1 5 2 3 2.

mSTARTED

COMPLETED

ULTIMATE DEPTH

PROPOSED DEPTH

WIDTH OF SAMPLE

gt.0-^1,0

U.O-V.O

5 ——— ^

W.o-,01.0

{6i.o~ 110,0

110,6-113-0

,^,-,- ,^-

&.6-M.O

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S,6 '

T.o '7 i,., *WV

r.*'

•/.o5.6

-7.0'

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GOLD S

. J 0 l-

.606•v

7r

Tr

If.

.'..'•'^

rri

t^-t,. -ir*-.

DIAMOND D mi RECORDPROPERTY HOLE No..

SHEET NUMBER.

LATITUDE ———

SECTION FROM.

DATUM ———

TO STARTED

COMPLETED

DEPARTURE__ m

ELEVATION __ ^

BEARING

DIP ,^,

ULTIMATE DEPTH

PROPOSED DEPTH.


OF SAMPLE GOLD S SLUDGE GOLD l

'V?0 f SO, o .y. e.,,. e ft,f c

/.o

Q

/sc.o *___&L.705" ft.*- ffi 0

f S*

/Sg

fif.^tti,-. ff -'tt-o' { O 6 '5?.o' ; 55- is' T t f 8-0 ~ W-D f.o

f 'f

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-f- i-^.t

- " 35 '••'-' ---*~

D l A M O N D D m i L R E C O R DPROPERTY HOLE No..

SHEET NUMBER ^ ^ SECTION FROM TO

LATITUDE DATUM

DEPARTURE BEARING

ELEVATION DIP

DEPTH FEET

t 79.0- z;*.

W- 2 33.-f

2*3.7- 7^.0'

FORMATION

A.*!* r&M*- Aw&ii**; '^^ .y.**.* S~** *~ step X /7 f f

^•t,.A(St*' /•//r*S'*ssXfa /^, A/faujC //t.sA,t /G p.rtfet+fa- ^k&t&i-Lf,-^' ' l ' S f fi/.••I'.f /ic^ft'Âu ^^t-^^L hr'^t&t /itÂ^ tsJfU*^? X3^-t* fi-t&f'tti. .

~ 7 j 7 ' ' " ' ^

r f

? 'j* 'f / ^- '" f ^ ^ f j *' ' -. j t '

f.r

ew f; '-.-.c 0 2*8,*'

SAMPLE NO

^6 7ff

STARTED

COMPLETED

ULTIMATE DEPTH

PROPOSED DEPTH

WIDTH OF SAMPLE

/^g-A*,

GOLDS

' Z

SLUDGE

GOLD S

f:', Z-

DIAMOND D*L L RECORD

SHEFT NUMBER

PROPERTY ^s.-. , S- xx,^ ^ ^ .'^ ^..v^r, HOLENo. /^/^.

- . SECTION FROM / 43 '0 v'w" TO

LATITUDE i 5^-5" Z. DATUM A/a- 3 ^— 4^^*-

HFPARTIIRF , ;9 #0^ BEARING --^' (^ 2*'**)

ELEVATION ) 9*) f . 1 7 D IP '^' '

DEPTH FEET

0 - 2.0'

7.0- 7S.Q

-?.o- :SS

* ?fJ- i*-f

?*.r- 6?.S

*?.S. :,' '

-1 .'. r 5 ' ' ' )

; * , . - . -: '. "i

FORMATION

C^^- i

t^,^ ( - -^xi.,. 4 -.*.^*. t,^v* ^X*^.^ ^v-v^.-^r/

^ j, .^6 , r* F/- *

Q **'; *,,^ ^, 3 35-6 ^. ^-^ x^vi/^4./T r '^

jj rf'.&lJ.ji" j*-.' b-fJ-Jj, ^ -'*: . ' *jr4t^4# -' d .(r*; f^s^+if*, / 'j^-^dMf^ ' y i*^V-*W^*6 ^? ^J^ r y'

i^ Tt P " ? g- ^ ' /tn*^. fai*j**- f p' S-*' s^,' /'fmt sbr&r-tL ^f^^^ A4t

^ '(*/fi? i"

V rj , -f. '•j.ttr.s l ! '.-'i ^ --' :'-'-f- ''.{{if t'lir*. '.'.-- '''.-''- ,'- ' "A, 'X J11 ^ y*T ^/'tt^*' ' ^^'U^-

^ '.r-.1,4-\f.- " '* U ^ ^ # ; ^ 'O* / f^*' i^^ i^-^*''-'^^ A3 flC+tr^jt f*\. {llAtf'l't** "^

/.-t ' ^ t t*~ j it, p ^'71 j(jji w S&4& /t 'f1/" ' X r '. r^, sAs(sf*'~jP^--**' i y **'j ,'Oj'V^^'vd'J. -^ ' 0

^ j * —— : — ' —— —— — — —— L*22*. ——————————————————————————————

: -V U,, /x, W,i. ^., ' ,^.^ ^,~,

,v, '....•..,.,, --'-r j t/r / - -*~,' S..4K ^ -î^

^ -v'r - : - " -'^ ' r.:-- -o - '-- ' - ' - ' •.-^.;. /' - -- ; - .-.- ,-.^- .,0 7'. '"' /' - :'''S-'S' }, t '••/x-.,/: r/ ' ', 'f j

SAMPLE NO

^-7*Z-

Ma 7/3

w,7W

K ' r ?- -: j?

i/o? ^5"

W07^

W0747

# --'''

.'r^

C '' ;v*7 /' , ly ,,,A ,.i^... rt . f .** '"tt (f,.'^. ' -. '1

STARTED t*

{ [sZSfad-' rs- --^^^B^N.V ^T'l \. H^/6 H/A/U7 yrfJW*^ ——— -- -^

COMPLETED 'v',v -' ^

ULTIMATE DEPTH ? ;* c

PROPOSED DEPTH

WIDTH OF SAMPLE

,2.*-24.6

?4.*-*7*'

??.*-?8r

?gr - ?6-, c

i^-i*.-

3f.i- 31.0

f. f. f -iS i

Si-i- "'-i

GOLD t

-z, ft

S (5

/•i"

-:,. 5 -

t.f1.0

~ . -

- , -

SLUDGE

GOLD S

-^,. ,

.1'*

,V ^

, / ? ?

./,,V

-' C '/.'f

.-'-i.

1

kx


SHEET NUMBER

PROPERTY HOIFNn

- t' , SECTION FROM TO

LATITUDE DATUM

DEPARTURE BEARING

FI FVATION DIP

DEPTH FEET

•' j /, o . . r 3. c

* 3-9.5 - / 'i V. o'

i 7 . J ' '"' ' ' ''

-. -- -J - . ,

IU.S-- . .,v.r

FORMATION

(? * o- *t? ; l ^.jt, {^(^( J

j f( f Vi-* ,/ V C 1 ' l

U- '/7.iO x- -,.V,... ^'.U/'!^. , . A.:^. ^"/....- ^ Xv//',-^

5^:^x svV; At, A -v-^ ^^ A^,^ *

^ " 7 ' V xv'* '* ' ^ f) *

j ,***-,7i.s': :f:,-m. *,^,v /^.*y*:/* ,'î* x^-6*^ ^*^

,,*A^ ^ V^-* '^,^ /i-:-/' . ,,,.;,,, 7 O 0 . r / ^,^y

'/A . ^.: ^ v -.-.'- i^'i.- . , A' f- - ^ ' ' - : •-••\ J t'jr:-;"^ '-f*}*'*-

" 1 '--'r " v . ^ 'i rfj-/;,',. ^.;.. - , . . V ,, . /f,^ : , ;j.t f'-1

f

'--' -X v ?-;'-'.'/ -iVi-..^ . s'*' 'I'-'.' .,.;J- /i/./l.^V

. ; . /, ^ ^ , ',.-,^ . ^M,r-.,.f ,: ".' ^-;^

- -; ' . ! " ' -' ' '- ' ,/ - . -'- ' . ^.:V,. .' -;. '-'.t -i i :-v.x

.--'•^ - ' . ' - j : ''''s / ^ "'' - . -.. 2 'j--.. -y -' :.--^,-^ c-'/ ' ' '

' . . , f , ''vx'l-'',-. c^ "'J ' -J .^ ' ,-' ' ' 'jfjt1 ..i-y ^/"ll"'.- - :'*(.

.^ .-s^TJ ..f-!., f *.f/.-,,; •'•,~' 1 S~'Z, /:'^''-''

SAMPLE No

^67^1

Vo Soo

^84f

^.^2^r^8.2.

W63

i/6 8i"^

MSTARTED

COMPLETED

ULTIMATE DEPTH

PROPOSED DEPTH

WIDTH OF SAMPLE

121.0- IZ ,,.0

W izl-t

W '76.6

'?tf :-7.6

/^r.,- ~-l.*

'-^,;.- -f. f

/.•^.r- /^-.

GOLD S

r. ^

s.O'. 0

. f ;

r. ^

v.,-

3.5"

SLUDGE

GOLD S

.--,.:-^

. . lit.

't -r*"

"•' 'd

'' i-'-f *L

-~ 1 . ' L^

-"l." t

; - '


SHEET NUMBER

PROPERTY HOI F Mn

~ y d SECTION FROM TO

1 ATITUDF DATUM

DEPARTURE BEARING

FI FVATION DIP

DEPTH FEET

1 - ' j ' - ''"-,',

','C.O- - -'.1

•fi.-} - 7 *.r

-1.1 - '.:.-

- r' - : 5

FORMATION

y,A-,,Y s s^^ * ,S7s^.u **-** ./,^X /**~"**^,

' ' y " " ' ' '*" j' - ' "i*tfi ''r ' .V- : -4*- ,* ft /'' \\.btl l/ts*!' ±1?Tl.'!'-'t,-4'. ,'"' :''f •r^rsssfa )yf^'- ' ' '- - 'i

1C (* i

'•^ ';. -,.--, -^ x--/^x - -; .' -- ^- ," i '.' '- - ' ;,-:^' y--'*'-''. p ^ . '. '. f^-^'^^-^-f^l

' ^ ,

t 7 ' ' - j '''

' ^ x

St-.~ x , :.^ -/r,- -.A-/ , : .J- - s, •:,'S*(rt. *^^-^^

, ' ^'

fy ri,'-s ^ jf J 1 V ' '^- - l ^.-.f't^'^ ' /ft f-^ f^t ' 'A&Att* /^•-/.-'•!'*JZ~,

j

•' W w .---'s-..,. ;.-.*.- S - :^ x-v-/,^ v-~ -' *.vfrv4^ *afc

^,,,f ^ A,,-, -.'-/i .•;.'/'; ,.,. ..-.^ ^..^. ^^^W*.iM

f f ' '

•' , , , .' - f

l^;.-* -, . ,/-, - ---.' .':,-'.,-' - -, - ' "-'-

^,, ,. ', . - ,; s,- * .' ,~'s..~jt s.,.-,.', ,^ s^*,,.(j 7 - c '

SAMPLE No

V 0 &0 T

^08^6

^^7

Votot

iya 8^7

, T n

L/o 6/D

, v otil

1/09/2

^*tfwu*wr

A

STARTED

COMPLETED

ULTIMATE DEPTH

PROPOSED DEPTH

WIDTH OF SAMPLE

^.. ' **.0

•*?*.M.*

Kfif-f^S 0

.'Vf.i- 'jf-'O

/f/c.^.'.-

5?. S- '.5S.3

•5-J.7-.it.fl

/Si 0 - '.^3

/.-•.-v:.*

;^*-;^D

;;,;. ' - '.'.i .

GOLD S

J.O

.T. D

T, a

?. G

.'.o

J. i"

2-,

Td

? s

;.i

;.5

SLUDGE

GOLD S

-//Y('"i

- 1.', ' f.

.U'Z

-i if- 1 e.

-l, 'i.' -f

-h"' ^

J,.,*

•S,.':^

, ' t 2-

. '-J'-' Z-

-'/rf '4

DIAMOND D •L L R E C O R DPROPERTY HOLE No..

SHFFT NUMBER ^ ^ 6 SECTION FROM TO

LATITUDE DATUM

DEPARTURE BEARING

FI FVATION DIP

DEPTH FEET

• H.O- w

,KM- .'t*.*

•*-..o - '".*

/6f^~ ' ?*5-t

*:*,.t- i***

*1W 7^.0

FORMATION

S*.WW /^ : fft .. f,. * W(, A..Y .?,v,. .v ixW , .^/,,^

s* S l ' i l Cr.*~'~- '; -J ' . ~/ '-"-j. *5*f" -J* *~* Ss-f't** i ' s T.'~* .'f • '..-i:.**) ^ ^ ^*5 *^ /TW *— ———— : —— ' ——————— -J ——— '- — 7 ————— T1 ———— — ' ———————————— ' ——————————————————

/ * y v

/i 'V ' T fiS-CtljrÂ X/ 1/*/ -t? t~ff** ^ ' ^/fW^S*' r 'X ^* > ' i"it. 'f f J- S r '^^ -^ J^^V** ^'-

' . ' J

x- 4.. W . v/ ^- -.^. ^,/-^ ^ ^-Vr'." /

t* 7

A^:,.- ^v- ^-^X ^^-,,,, ^-cx. ,x-,r,i- ^-,r..^ ' '

/;.*.-xe**JL /x-" -*^^^fTU^- , ffJSl4\4^ VtJ 6#f*slG.t* "^l^t*t-e^ i ^ftyfai. 'K&M/Ztj- Y 6*ftf*S*-*^5

tb tfjij*'.^ fa /.l -** , 3**t f) : X xix-^ .rJJ^- ^ trtis.* /M ab ^^ *^fa~ , t'Jt&db.

Akutu* ~M ^J'/ -'i,:V, s,^ ^ S,^--i A^vW^lf,f J .

t3 fo-k*''*i^. 0 ': ****t i" ^^,M ^ ^..^ v.xvt, o ff.

/f f 'f. ' ,, v

.7 ^f i (*V^' ^-l'/ 1- ?'I ^ - V ' j^*^1

(T -^? r? ' 5 " ? x" o -.4 (' o-yx ^r yx/^ .^-fi^ ^^* X/' ^v Zst&ici^ ^-t-t^-v^ *

r '. y vj^/Xfe-'"^ (;,;, . - '-: . y.;. -* •••Vî X y/^-,^

^Vfr'- ,.:, t ''./, V/ ,.'x^ .,,.,-v^ ^.,'.-^ ,^^ , t .r -'

SAMPLE No

V.8/C

f

' ' 7 i'

"48/7

* .'237

^ '5753

STARTED

COMPLETED

ULTIMATE DEPTH

PROPOSED DEPTH

WIDTH OF SAMPLE

/6-**-MS*

^7/-?:.^

2*' A : " 'J, ^ 8

r.v/d -?^

GOLD S

2. s-'

f. o '

.0

A 2-

SLUDGEGOLD S

Jr"*

" f -

,,,-,2,

, : .:z

d. d t

D l A M O N D D L R E C O R D

SHFET NUMBER

PROPERTY HOI F No

'' ^ f. SECTION FROM TO

LATITUDE DATUM

nFpARTURF BEARING

FI FVATION DIP

DEPTH FEET

* W -*' 7 3*0

* 3 W 7 58^'

Z 5-8.*- **'.' '

.-'4*5.0- -7,4'

^3.6- i/f.O

If

?rt.fl- S'* a *

3'?.*- ,Wl. 0

*?*fi- KO.O

FORMATION

:',^ ,/'.'/ V-Û f-S'f I., ,' ^r^,:' ''i,-.. / . i ,.,-,^

;

j/At^ .,iWt; ^^ ^^^ xw,. -j _ *r U*Jt

r,.**^* ."t* ri SM.^t* ^^^^ *U*~. ^ U^ ,^fi

/*M*. ''Û*. w *^^ 4*v*uuj*M** 0* &&HJL. e***.' f - -7 i i \ t J

' W4. y,/-, ^ * '^- .v*~S , o^c,^ /,#A **~ ^

! JL ' 4**n *.Sx*6 ^ Q 4i ' us \ **~* f W ^' 1 .' t

" ^ ' ^f.s,fSff sjtt- s "- p p^V'^jf^ff. ' fnrtdes i3-5 h) /s^)tj. yi&i&su

f , t , f , , j U/2 7 7^. v 'Z 7i - 0 ', /.t/i-j-:.!. Cft?-'-*'^ *j^-y-'.!:,\'*-!*- rib t r,y r^-iy^r^ "fif

/ft -li' i' ? 5 ". VvjJ •'' lf:' lj, lt(4--', /f ffi : i xiAy^V-I r f

'Mx " -^ ^^ ^, ^ w**^^ J*u*- -. 'V - X. . , S-

f

J f 7 ' f

4 ^ t /-^ lj A* x^ ^ oD ^ '

/- ^ /x ^ ^.

SAMPLE No

^ ''2^f

*-v*^

V^S/8

^*e.i*','7^

^870

*J2 ^r

* )5" 7 ^

ASTARTED

COMPLETED .

ULTIMATE DE

PROPOSED Df

WIDTH OF SAMPLE

w*x*^'iij-?l4rj

fW-k -7^(3,0

^•^"^ t- ~ 2s ft Q

2. b&iO' îO @

2 tu. 0 - V V

^/.fl- ?â^.r-o-a

3'85-â

^.,.A-.o

GOLD S

3.0'

J.fl '

•y. s— J^5 ————

.--.o

-EO'

~.O '

S-O'

j. r''0'

5:o

PTH

EPTH

SLUDGE

GOLD S

.we..a/a..0*

. wfe.ô^

.^zT/..001

, 03i

•06&

.

D l A M O N D D L L R E C O R D

SHEET NUMBER.. ^

LATITUDE

PROPERTY HOLE No

^ !? If. SECTION FROM TO

DATUM

DEPARTURE BEARING

ELEVATION DIP

DEPTH FEET

Ji'-?.*' 9 li 0

2*3- 1' -*7S.C

FORMATION

W*** -Zx*-^ ; ^ A *^,, yu**n. ^^-^ frl f , '

v ' c /

! . )^5 fa C*l* ( (^"•^^'f^^&r- j /Vv^vvfV ^^^^Wî^ f' 0! /V Ô&V"

/T ,- ' ' ! 1 ' 1

2***', ' "'Vi, -^ A--0* VW^V '^W——4 x,xs**O.^C '

i ^r r f'

Qut-s-m-e: fr**~ }*** r^Suf*** y-*- x/^-v^^*^

IjrfaA, , j/Sff) /r.'stt ^'JfÂ. R fS'

0 34* -f" ?7',4.' •fVjAj*i'i, K- 'i. y&.vtf'.t-î' s*Ai**-C*j SM&*.

T r i

eto *r tine g W

SAMPLE No

!S?f7

VOST-I

W 6"

^ftj

mSTARTED

COMPLETED

ULTIMATE DEPTH

PROPOSED DEPTHWIDTH

OF SAMPLE

Wl- 359.0

9X.I-3S*.'

*w*-5* ie

3H.C-W

GOLD t

:f 0

s-.a•so

?.a

SLUDGEGOLD S

7^.

-V/VJ/-*

*^S0f-G

&O ^^

1

DIAMOND D^LL RECORD

SHEET NUMBER.

LATITUDE ^^^

DEPARTURE^^

ELEVATION __

PROPERTY1

HOLE

SECTION FROM

DATUM \|o

TO STARTED

3 COMPLETED

o go ^

9?AO s

BEARING

DIP

ULTIMATE DEPTH

PROPOSED DEPTH.


OF SAMPLE GOLD tSLUDGE GOLD l

C -.TV

JLJ?—— 2 ':*

jf 1 3 X' X. f y*

/" 68 S"-

X,

70,3- ?r.i' z. s-

77 -S-

SHEET NUMBER.

LATITUDE ———

DEPARTURE ——

ELEVATION ——

DIAMOND DAL L RECORDPROPERTY HOLE No..

SECTION FROM.

DATUM ————

,TO. STARTED^,

COMPLETED

BEARING

DIP ___

ULTIMATE DEPTH

PROPOSED DEPTH.


OF SAMPLE GOLD SSLUDGE GOLD l

ff.o- it?, D

V*-?*. , t J,, y

*-

" II) .t* JT&VJ4

- /'t -0 '

'-"i. t, -t•^-r^*^ ,-r, d '

1 2?, t- J '0

r**, o- ^ -i. ff&.a- /l'-.}

^.^ -h it ''-C

1 15. f

.cot,

^-;- Q

X*'---**

(g

***. y

DIAMOND DMLL RECORDPROPERTY HOLE No..

RHFFTNUMRFR "f" SECTION FROM TOJ

\ ATITUDF DATUM

DEPARTURE BEARING

FI FVATION DIP

DEPTH FEET

ILftj - Ml, 6

t"*-*- IK.1

'-k. 7 - li**. l

/jjn. i' - -!3,0'

'

/7O.O ~ "*~*. O

^..' - / V.C,

",-', ' ' - :. -r

FORMATION

U*^- f ^^ ^ ff.^ t^* ,,*^~ 4 , u.^4**lI

r ft X . fa A * y . r-?/Î'.i/itt- # -v-5* i*,j3f*\ ' ik'+e*. :*.' .'i-s/f, ^/-^*p (2 ?o-ôj ' '

Q lil.o- 'i?. i ' ; f-. -f.,/ ^ '.^ -j :ti~s(L J/t-'r ,,-,u. )ln, ,/*,^ sJttÂ

x;-' ' '**- .

fr.*,***tf*.- :.t~M. v-; ^--? ^-^ ^-.-c, x,^^, ^^..^r /?-

jftpy1* tt 4^** -S s*-/ *5*~*4**,fa- J,l0-3**.l'^(-4Js44~3 j /.,-'~~-*t''bt /S ^ ^' -^fD*' * *- ** /^H^*^v

^^^-; ,^.-;^ ^^/-^X^^*--^* ^^- ,^H,-r-"^

*f \ s ^ s *

,.:.:,.(/^!}:

••' f".' I-*-''*'. iv***..* .y^,'"-. ^.^.,,t S^'J,

s- " y

^ ^ t ' * ^ ./'^

,.':-', •'•*. ' -,*. "l

' f

- . :. ' - -l-', r -''. . '.•••t'x-^-

•^••^ ' ;.,' . ,^.-^ , '.-f *'.;-~ * "f.

SAMPLE No

W**

:-*.-3.

WZJ'/

mz..^7o

-J4237

STARTED

COMPLETED

ULTIMATE DEPTH

PROPOSED DEPTH

WIDTH OF SAMPLE

',^",(C

'^.'••'j.j

f (.a- tei'ts

,81.0-s??*

,1?. 0-^.0

/tSt-WS

GOLD S

r-.cf '

T. 0

?.-J

?,o

.v -J

i r

SLUDGEGOLD S

,oo-^

*lf3( -e

,00^

,*z

•*(f,.-'.

.to ^

DIAMON D D •L L RECORD

RHEFT NUMBER

PROPERTY HOLE No

if f -c . SECTION FROM TO

LATITUDE DATUM

DFPARTURF BEARING

F( FVATION DIP

DEPTH FEET

/,V^ '^" " , ^ 3 f, 0

"3-&T , O ' 2 t ^/, fi

^•/.a- ;*ra

.--•fc*J~ ,,3^

FORMATION

j , ?y j^*s . -Pw* ^

l P '

•ca^ -pfJ :.{. \' ^^^ , : U,L ,6S'*'#* *-?''s6

:-fJ . ^-U s-.As.X,^ •^vA'vS. S*.,.,'^* X^ru^.

^^ ^,1,...^' r , - ..:y.

- - -i" y"' —— j—— ——— - ———— '—"-^ ———— ——— ^ ' ——— ——

(^ '-^-;--': ^-. .,. A^y "/^^ .^ * - ,H" .-'*-^**-. ' '

L. t l*.\ '.^, - T -.^.^ r- 'f ,^.,,/^V i ^^

.., ,,^ ,.,v/ ^ ,/^ ,-.- .-^— ,'^ ,,^- --^ ^^

i ; .-''.: - - - - •'••' . ,;--.',. ^ ''--r-'. :'.:^-' *"-' •'•'- .

, /T i''. . '' -''f .'^ , '.. -' V ' ^ .^.'.(.^ 'J t 'S" i '-' V -^

" . - f ' ..'.,-,t j ,^fj - x ^-^ t-.-

,-'v,^

.- . ' ' -y /,, /'A,.^ o- ;^, x'{

v - /- '. ' ..) '^' : -^.•'^^. ^/^- /.^ j- .^-., .,v. .-r* y^r^.^^*.v 9 w .'- -A p -, ^,xJr ^,w û^l^ ^î

*4n^ , , . ,^.V /y^^. ^^ /^K^^ ^ ^Wi

SAMPLE No

M? 83 8

V^3?

V3?^

v*gv/T'dlg 1/?

/^7D

'^57/

^r2

/-/5-J

^5*3

A

STARTED

COMPLETED

ULTIMATE DEPTH

PROPOSED DEPTH

WIDTH OF SAMPLE

!^6.S~ 15 to

'l*h'Z*.*

Sfil.flm~"' * M ' C

i*.t'7*.C

tt4o-M.t

2il-o~2(*1'0

?W?*to

2*13-3313

wrf-s

GOLD l

•2. r?.a

•/.a

r..

/•A

3,4

7-6

5'f)

3-0

0 g'

SLUDGE

GOLD t

. (59 T-

-J f'' t -^

, 00^2-

^//^ /'•i

.^•z-

,^-T.

.W)^

x/.):^

^.-v*

.^2-

DIAMOND DAL L RECORD

SHEET NUMBER

PROPERTY HOLE No

-^' ^ . SECTION FROM TO

1 ATITUDF DATUM

DEPARTURE BEARING

ELEVATION DIP

DEPTH FEET

50-5"- f r i. *

i f 9 - ;;}.a

-Z3.0- , ;0

5Lrt.3- 3-V,,

FORMATION

-- — -" ' ' f f

^\sW^- A/- 3" ^tei2**V~*'y\jt4*lCt ^-^L 1 ^f2tti^f y5M ^0 ^sl{?frf*"tt-4'fyC' st^Jvl**

'Sj/sVt*-' /t'-t'tjjfafe S-1'^ ^yy.tt^ jiÂ**l-c*j t ftjsf^fts -ffc^^tv^ -^*^^ .

J l

-Dt*^ **^ t* L**^ ^,^ ft** ;af, A, 4^^,

(r^M- , v,-****,*. , /i^ tlbvtu, ^^ jJ*L*^ /wt^x.

-^f-j **Âî*3 X J^'^Hi 3*44*** t x?* wU^ JJ^4*'*-^^*^"W^*c/ ^w/jfe sty&Uvtd

l j -'' f.

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^-;,..,'* tv-M, ' M.,,.*,'^ f *v*J-S*ti. "pt*, tft**! "f 'f /f '

r-? i "*, /-v^^^-v X/'-*' :V ^*x

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t ' '

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^ , .y

jf

'l^-'i- ' c^^ W' - '

y^ ,^ v-'W ^ **' llJL J* ^.^ AH -

SAMPLE No

145^4

tfSlS

14571

I4S77

WK

WWJ

t**..

b

A

STARTED

COMPLETED

ULTIMATE DEPTH

PROPOSED DEPTH

WIDTH OF SAMPLE

50(^*0

3t4* -307-0

W W*

WM.f

atS'-tt.S-

359.iT-*tff

GOLD t

s.o

5-0

R. d

?.r

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X (5

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GOLD t

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.661-

JKH*

^^

.CCL

~îfi c j

DIAMOND D^LL RECORD

RHFFT NUMBER

PROPERTY :/**^, i*w/^ y X^. /^^ , 3*,*Lf^ H OLE No ft /S

; *' ^ SECTION FROM TO

LATITUDE DATUM S**- *v* # ^ J .- ^s*-

DFPARTURE W 5^'^^ BEARING -w '

FIFVATION DIP ' *' 3- t* ;l*'

DEPTH FEET

(5 - 1 j . t'

'5".0 " /" ?. 8

^? 4- .v -y

WO- ^.0'

V? 0 - 510'

53. -5- !*{p

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;,,Wf

/X^^y^vQ. , Xl v*-ô fs's&^&Jtd * f-* **iG'4 '' , i1- . y'/jtt'f. fJ-jfjtJjgA,ft f l ' r ^

y stT-tiwZi •(rr'.f-d ^--/rf.-* ,^-**,44 "v!yC '.' '-'^.^' ft- '' -' -" " *"*"-j *firx^7 ^

j --f '-^f 's/J&s /^f-".^'-:^ st'. 'î-C." ^.5 /:(s^*2 tf .5 ",5^* ^7 J^W -1 ^^*

y'A'-Û^ 'i^f^'KV- /r/ C*l^**"'^ jX"^' sfy^-^-C**. •^''^'•^fJ^. t ^sfr*-:* •fy-^*v^tf*^ j^V

sf-tfytfa f^X'-*.^-^^^ -}. .*-fj '# *(-'',f jf^Ji rf-^- 5-0 - 5-*''* si^-'-f', ' •'rV'-'t

Â^V--) , : v;-? - ' ^ ' J-" X/; ^;v /z^y**. ('z.- 5 Vi j

(? 7^5'; ,:/--, ,,; - ^^ ^ i.'/î ^.' J ' - S 'Jr 1

j y x ,. A^ .'.'-- ,v . ' ;\ 'i., : , ,. -' ". .r'-' 'X ** ic ' .y,, .-x;

y , J ^, ,

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'; ,-, ; ; ' , /i v - :i ,. (| . t, ^ : J *... /j.^t. ; ", : '^fj.''.- \ : -' v .1

; . . -? ; : .'S' f , r i' -' . ,.' .^V, ^ . , y^.

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SAMPLE No

y ^f/3/f i?*'

tfi*5

rtirtI*ili7

,*b?tv :,-^3•'.-.w

i?lilh&ti*W

l*(52

^rtt

STARTED 'W ') /0

i-'-Vf-

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PROPOSED DEPTH

WIDTH OF SAMPLE

Zi.0-25.0

WU.'

r 9.0 -3tO

y.o - ?*o

S V, J ' ^ i, o

3 7.0 -r M

v;,*-v7.o"'^'J5.fl'

r^-.^--rt.,- ^.--.

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,,.3.1

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53

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, tf/^

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HA

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DIAMOND D *L L R E C O R DPROPERTY HOLE

SHEET NUMBER

LATITUDE

SECTION FROM TO

DATUM ik/A^W -^vic. A^

DEPARTURE V J^-VV-^ BEARING 0 3-6"

ELEVATION DIP -s** (2 *x^v

DEPTH FEET

O- f -6

ST, a - 58 D

bf. J- :- *

- ' - ; .^V

•r, rv -V* 0

•,j.5 - i " "

FORMATION

/V^,..,

,6^W.^ - ^^ ^.^ ; ^r^ ^,-vc x^Ût A ^Xf ^ ^ P

.tt y fi , /' ..-'•''5-^ vf 1* ^ //T, tvftif -' ^ ie- /z^^^ Î*S-"îr -^^^^ x^5rfKit. x5r ^-^-^^-

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~^ —— i^ —— - —— — - ————— — - -iJ-^" —— : —— - —— - —— -^ ——— ' .1 ————————————

SAMPLE No

'S-J&2

ST/i

COI

ULT

PRC

WIDTH OF SAMPLE

f94.*i.f

iRTED J^^/3 -z

^PLETED JW- /rf z

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)POSED DEPTH

GOLD S

-x-^r

SLUDGEGOLD S

—^^

DIAMOND D 0LL RECORD

RHFFTNUMRFR

PROPERTY HOI F No

SECTION FROM TO

[ ATITIJHF DATUM

DEPARTURE ^ BEARING

ELEVATION DIP

DEPTH FEET

"V ;, - Z 7' '•

.-".o ----"

.---f ':- ~-' "

FORMATION

- / - , *SA, ~*.# ^...- - ;.*s,-. f v,*.J.-/ ' /, ' ' ' ;; r

x/ /- - , - '/r/v /(.vit,' t.j-.A X}v., 't.

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5/, , J ^ ,,^.--; ^' ^ - ,, X,.,. J, '., X-A ,'.W

,,,.. ^/-,^ x*^*' ^,.y xx-^:, - , — - ''- ^- — f i ^

?'-* "' ' ' * '

-i .-l , v,.'.^,:4 ; .^,. t ^,..v; ,.,- ;., -v .'.-.v. ^/^^

s'**~' 1 - - -' ' * ' ' ?rf y f ' -f

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^'- , /. ,^^ J ,^*t. -U ^ -V -/^

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f.., tJ *T .-.'.- i' .y ---

SAMPLE No

4^

STARTED

COMPLETED

ULTIMATE DEPTH

PROPOSED DEPTH


SLUDGE

GOLD S


SHFFT NUMBER

PROPERTY 7^ SW-..J ' -^ ^^ 77,,.v,^ HOLE No M ^3

' '' 3 . SECTION FROM TO

LATITUDE DATUM !,W V /V,

DEPARTURE ^ 3* if/ft. BEARING 2 *0 '

ELEVATION DIP ~so ' ^ - )jl*'

DEPTH FEET

'. ,- ;

,,J- -';,. 4

7*a- ..c'

~,.- va

FORMATION

' 0~*

'•'^.^: ,..^,. *v,;,* ^.'-H,,,, /W A *^.~ ,-~. if J " ' - r

' i- ' /ij&t, - .'/M" . rr /. , P/f^t- * /''-f^t ')stf*t^ , Ji-,xT j l ^, ; , ; x,,../,. ,.-, , ,,^ ^^ ,, s,. ^^,,-.-? M.OC ^ l? ,, (i . .'

•' - ' S ' i (-

i

;-W ^ , i'.v. ,'^,,, -,, ,-.l 7 'l r , X l' ' ' A ' ' . -'

•~ -J /. •C' s * -f --vCx ^-^ •,".,", . "^> ,, (- j . -f- -f,' f^ff ...'f.

J ; . . ,,. y, ,, , X (^

ri ^v.o- •"'/•"' \,;*^~ ,, .-î. ., ^^ ^ ^., .^..^ "*'

:. ,; ,,,.. tf /I/.5 1

,.,. ,.,,., , .,L " ,^,^ ^' /,, ,,.,'x /-,.-:I.I

J-:?.,. ,'*AxA **#.± - -,, ,, ^ ^---1 -^ -.X'.

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; -. . ^ - -/' ; .--., , . .y V^ ... s ,, -' , , ;

. . '' : V' ...' . - '- -'/' ,- 'i - , -

s .,-lsutl. . '''.•••i

.- , '5.t' "'"'J .^4 x^s-

SAMPLE No

-;^7

A

STARTED

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PROPOSED DEPTH

WIDTH OF SAMPLE

'^)- -. : '

Jl*--.**

GOLD S

: -f,'

b

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GOLD S

-^

D l A M O N D D M l L R E C O R DPROPERTY HOLE No.

RHFFT NUMBER SECTION FROM TO

LATITUDE DATUM

DEPARTURE BEARING

FI FVATION DIP

DEPTH FEET

&0 - :,-, J9

' -,w j - - - ,

-(.i-.ci - - -Hi 0

FORMATION

.*:io-W; *.:** t~*z* - -••— " --*^ *#*î , ,

gr f J

-,, ,^ ^ H .,, / .^ , , '. f ,: ,S f' ^ ,,-,v. , t __ , . -;,/ ' f ' i

•-**-4- .*^; S;.-L-'*^ r---*' ^-' "^ ^ ^" *

J /If. ^ M*A '^^, * f,^.*.,t fuo.S, ^

, /'''''••^Lt 'r ^'J . '"^ ' '' ' - ^ ' ' ' "** ' j Str.fr- " ' ^-t 'j . t'- - ~*jL Xfe^l*l*^''i^

t/ j' '

. ' " "" ' ' f

J

X"

^.,^ ^. 0,.., ,,,^^ '

f '/D i! P J ':j L f (3 UtiCi V'

SAMPLE No

IW*

111X

STARTED

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ULTIMATE DEPTH

PROPOSED DEPTH

WIDTH OF SAMPLE

" ' J

•• ; /.," ••••.•.•

GOLD I

' . ,~ '

SLUDGEGOLD \

1, VI

.(.-IT-

DIAMOND D *L L R E C O R DPROPERTY HOLE No.

RHFFTNUMRFR SECTION FROM TO

1 ATITUDE DATUM

DEPARTURE BEARING

FI FVATION DIP

DEPTH FEET

•^- f?:*

•70 ' / j 75

f': S- ~-~ ~" J

.- '-'c -so*

FORMATION

J"*Jir.*is- fft&b' ~/; i /t ^XW- -;^'-.VC ;Vj /?*- /ssji.'i. ^'••? ••'•jjl( .. ^..,.j ' . ^' ^7 ; x ;^ " x,. yy - . - .' f s ^ '

f ;vv""^ —

7 ••','-?,* 0'6'*^ '-'^} .*L. \ -{'''.ft -,; * ^:*'^

S -x X ^ ^^1

, ''.l * 3*' *" ^

y ^ f ^,,/ ^^j x ' y'^, ' 4^lM.^ ,-^-y^tf;. 1 ^ /yi^-ii- â^ , ; i.

#.'5? S'.' :"' -v-./. -v^,^, ,. ^^ , ...-.^.^ ^, .-,.;,.x.x

•'r*v ''-'' ' -"'- ' -) ,-,,., - -' .-i ^r, ,,s.-'b*- i Or. .' *.Ue,.- . . s, ,- *...-

•'••'••- " ' i .'f - ,/, ,. /r '-, /.f,.;. . .

-' v - ' . ^ 7 y -

-^" '--^ ' /I-'^ /, . j;j,'. /J ^ j^J- ' ^./-J/. ' S -l . ' ^ '^ .t'

' 7

^. :/,, V -' /- vX-,X/^ /'

^;-v.'.' : .'.-v,y ;;A ' J,-a , ^ ///t'

SAMPLE No

STARTED

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ULTIMATE DEPTH

PROPOSED DEPTH

WIDTH OF SAMPLE GOLD t

SLUDGEGOLD J

D l A M O N D D •LLRECORD

RHEFT NUMBER

PROPERTY C/^frv -5**w**4 W. ^ ^, ^J-:,fx HOLFNn h Z?

li 3 SECTION FROM TOJ

l ATITUDE DATUM filufavfi *^ 3™*-

DEPARTURE A/W J^rvf BEARING ft**

FI FVATION DIP -MS' ^ c*X*.

DEPTH FEET

O - IS.O

1 5,0- ^ o

fio. ,;o -f

*3o- ,3ifl0

/•;i/, a - 137.1)'

-.7.0

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^s^.^

A'.wsc-A' - Wu*- r^*, ,,-j**i*4, //x^*. ^ *4*^t^ "

f t/ 1 p ' 415 Q- l* t . fr'^l^f •^•ii /J., /-/^*t^j ^*l^*1**r ^ ^ t-S'

'

J ^ ^ '

rs ^ j ^ v r

t ^ -y^.

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,,,,, Ab^-Ôut -^V,^ *' ^^ ^^^^^ S ,-3'/,)^ __ ^MW*. ^ 7*1"""

/^ ^y., v, 1 ^ y^^ ,, y^-^^.jj ( * ' ^

' /^ (!x7 ^ \

^jj'.tf " '- " ^ , //Ss "'V'jt^fe^^' i ff^v^) " '.st/jfjb. sj'^'-'fyt^ C C^ X ^--0 i/'-S*^1 "-*

1 rfL/// '-A/-^/* Wf(4-

^,;r^'^ - '/i- .' ^-^ / l&A ' ' j/,* Sstt-x. /^ . '-fi.--i-r4t, f yt4 j,i .'-/^^,"' \^' ' C'

-i^jit^? ^**'C*/^ ' J ' jf ^ ??***-\ '^v/^R^-î jjd T^ * ^^ li-yi* ,*"/^^' .7 ^

^.^^ ^^K. /V ^*C-t r^-X. Û^Ki- ^/^^ ' ^

SAMPLE No

/5^#7

^

STARTED ^^ /*i

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WIDTH OF SAMPLE

f2 e V?.o

GOLD S

/.^

SLUDGEGOLD S

•7^

Â ?^

D l A M O N D D L R E C O R DPROPERTY HOLE No..

SHEET NUMBER.

LATITUDE ,———.

DEPARTURE..^

ELEVATION ——

SECTION FROM.

DATUM .-^^.

-TO. STARTED.^

COMPLETED

BEARING

DIP ——

ULTIMATE DEPTH

PROPOSED DEPTH.

DEPTH FEET FORMATION SAMPLE No WIDTH OF SAMPLE GOLD t

SLUDGE GOLD l

2 /i'- *- ? 't -ov \ ^ ^ "x

? It,. t

Ar

'****!j. ^^y^^J...-.- ^1^...

^^?.S-~ *-f~5-w, fa

r i'- 2 lf.it, S i fi t

frr-H. Afc*'*,,.O

f f

_^__L_^^±L '^ t? ^

364 -t- 2 "g (j

J&Sj ,jt. "X* -fro' /x

-j**Z——7 i f -f- i'/.

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DIAMOND D •LL RECORDPROPERTY HOLE No..

SHEET NUMBER.

LATITUDE ———

SECTION FROM.

DATUM ————

-TO. STARTED.

COMPLETED

DEPARTURE.

ELEVATION ———

BEARING

DIP ___

ULTIMATE DEPTH

PROPOSED DEPTH.

DEPTH FEET FORMATION SAMPLE No WIDTH OF SAMPLE GOLD S

SLUDGE GOLD t

i*,-*.

Ci

A

-b , "7————7~ir/z~*v -j e/ _fe_

3.0

^ ^ g /7?.o-_/2^-o l f -ft 50

4 / /r

vt /tr

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"fif.o- 2.0 .OOT-.

/5•3.0 • UO 2-

.'frJ.i* .1 X

(V 7 X***-, - i'lt.JO z/lu - z' 3 o

7/5.0- ;iS

(P 50' x*

DIAMOND D0LL RECORD

SHFFT NUMBER

PROPERTY J***,. ^:— - * l*~- T^^fi* - HOLE No rt so

i tf 3 SECTION FROM TO1

LATITUDE DATUM U/,,.^**. L *to- fa*

DEPARTURE ^ ^-"^ BEARING ?^"

FI FVATION DIP " ' 3 '^^

DEPTH FEET

O - M.O '

no ' •"' f'

.-•-,- v,,y

4" 4- -v,

"' '•". " r " '' ' ~- 2- J '

FORMATION

.'^^•r

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^•/,,^ *~**,*H, ^ ^ J^^n*-^ ^.^ J\ t . ^^

^^ ^ *jJL /*^'4 fr,^ JW,K* /-A^. (,.,,,- . ^^,, ^^' ^.^s ,-t 'w* t.' ** ^

J

t-vtA,- M* tp. X *^^ x^. X,,/ /^:^. ^-^ ••/^-^^ ' i r r" jfr**, t*, fA*^.atonA,; /*^ r,^f- ^.Â Y^-

F ?t 7

^ A- A . r /-..^ ^-^ /"-A*. î~-, ' ^ -,

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/ivv^.' /y, ^y- k ^ ^, ^:^^7

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1 ,-,/^ /•-.-? ' x'* y'. -o -'t* j, si. -i K.;-!-.-..'# j.f ,jL ^,. , ; -.r",.,.

i x ,. ' ^

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SAMPLE No

r j*,? g ^

tr /.5?Sf

A

STARTED ^,^ //a*.

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ULTIMATE DEPTH ÔA

PROPOSED DEPTH

WIDTH OF SAMPLE

^.a-A"j

..' 08 'X -/t f. Q

GOLD S

•' O

..r

SLUDGEGOLD t

• ts-z.

~T**,^

l y

DIAMOND D0LL RECORD

SHEET NUMBER ,

PROPERTY HOLE No

?- 'f SECTION FROM TO

LATITUDE DATUM

DEPARTURE BEARING

ELEVATION DIP

DEPTH FEET

if y. e- 2^1t>

75-7,- ?S S9

rzsa- *,*.0

3 i 3, o- fpJ S

FORMATION

ua*^ A&L,- ]^^*u^: /*^ r,^^ r^,,^ . , vu**.j? r y

C- ,- f

jr . ~. ' y

•*- ^ ~* , -\ "t*;, f-' ~jf,^ f'' ' ^ i ; ' •^•îi^t^^ , i^T.^vVî'i^-' g 1.' .yxV*-'-* T"- . ' *f *.~ ^

i , ,J-i A*- /jtS'St ZS./'tf.^r /^~ffj ., ' •'•f-

-f(t*^ ??t.O /e 4*^1 *? j.,.''. - i-y,' j.4zr* /-/^-ie r' st&s-a/ts.f ' t X ) ,

y' , .^-^^ . t/^-* "- - - "^

^ ^ ^ " ! ^ 1 ^ ' .TVJO . .^^, C ' f *

f f

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. , , ^ ' '/r, ,y.-'-.ri: ^ ^, ,*o^ r*™* *-* f*'.*^ "-'^

f f' ^

^/St*. "' —— ^ ^K^'^ (Zo'i) /,...^ .y^-y'. -;', 4

' ^ ' -a- fe -^ f

.'///x-/ ,/.^- ^fd /^ x-^. ' '*t*6~ ^^, *****.V

SAMPLE No

*.

A

STARTED . . .

COMPLETED

ULTIMATE DEPTH

PROPOSED DEPTH


SLUDGE

GOLD S

D l A M O N D D 0L L R E C O R DPROPERTY HOLE No..

SHFFTNUMRFR SECTION FROM TO

LATITUDE DATUM

DEPARTURE BEARING

FI FVATION DIP

DEPTH FEET

41-TS' ^" 0

FORMATION

^.3.0- 5.Y.0 1 ; aAJI* X , X **4*y *K* rt ^'A ^ **C J s

'

f s 7 v i (^

.''•^^- /fÂ. fi*^ f^,X ^^K- t* ^ , *'*a

r 0*1^*6) ^ l^TtuJj, 3f:^-A 'sJtfati ^f'/Avt (-2 3*'A CA*. .

* f ' . .xf*t^l^tj /î2**v 'i^*i '' /"-*-**^SM?X ^y^5*y,i{** /lt-\Y'i l f -^^^5*^';**i^yW^^-^r

-^ky- ijfis' C ' "" ^ fr^^*24.rr*Jt^, ,'''#Ut 4*4* t ^fet*fr* — v&i^T^L -/4^to

y , . ,. 't, * U l f '1 fi

f V ' V ir . f/ ^f

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y ^^(' ^ 4uA ' *"/* '-i

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^^-,-:^ t ^'t9 **a : ^,/r^., .X~* *4J**,

fMO of M,c* ^J0f.d'

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STARTED

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ULTIMATE DEPTH

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SLUDGE

GOLD l

. 9

SHEET NUMBER.. ^

LATITUDE i 1 '

DIAMOND D •L L RECORDPROPERTY iX*wSL. S^ —— ~ X A /^^ 7^^ HOI F No A1 ?* 7

J' SECTION FROM TO

^0 DATUM ^0 5 ^ *^^•)

DEPARTURE ^Soft BEARING ^ ' ? ^'*/

ELEVATION o, ^ ? '* O DIP ^' * "''^

DEPTH FEET

0 -Z'.O'

21.0 - ^3.5"

*?5- /-V.

•**. .we

FORMATION

C^*^**î

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,^w^ -4***^ ^^wij^ ^ .^^JM ^-^^4 a s--,^.*M*uv*t ix^X ^-^ xotof ™^ v^^CX -^y-6 w __

y f x

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. ',^' r- j

y^/H^ ^-.^^ /W- x* ^;—— a*U***ti, /t4t j**^

ffitlO-; *;:, :., f'*") .^-^ ^ t* l/.î ,^1..,:7;/, ^:^;,

. '^. ^îf^ *t^ -5^ /x? iXY ft&JS .

7 S o- f,' c ' ' X' ' - y/ ' X x- y' j ''- ^^Syj ' s '''-

" **.*A* ,W A,^ /.^H^

X'/i.^; :^y^ ,^,:^. .:A-X-'.- -- -^ ^-A x,^, '- ^/;- .Ky ^

/-.'..^ 3*,;^; ,^,,, i. ^ ,,:-ri,.. i .^^jt*. •S^.^.^

/4-A .fXr.^ •-'- tfff&i sSxi. ..-'t S*6--Q*6. â.:*i jv)te, 4*, rf.'r-.-'t7 j s- t/

' , ^ S'

' f r ' f ''

SAMPLE No

/sx//

94t

STARTED ^ /**-

COMPLETED ^*5t. V*2'

ULTIMATE DE

PROPOSED Df

WIDTH OF SAMPLE

VZ.O-HH

GOLD S

2-5-

PTH ' 6^'

EPTH

SLUDGE

GOLD S

2^7 V/ s*. M

1

*,WKMfVl

\SS

D l A M O N D D L R E C O R DPROPERTY HOLE No..

SHFET NUMBER SECTION FROM TO

LATITUDE DATUM

DEPARTURE BEARING

ELEVATION DIP

DEPTH FEET

'•!9,0- GS.O

iff.o - /eva

FORMATION

5W6 . #44*. ^ ,,Wt ^^, *^*6G*4, ^^ ^

ieuw. *x^, ^ t&tjs fa Jo*. Q - *-*' Jk^L ^f ? t' ^ S+- A*

^l

fyt&W^- 6**4-tVi^^ . styjfo.*t0v^6\ J-vO 1*^^ Jsf'&lfy*^, . ^w^^-fi- -^c J-ftft^S**—

-ViX^ry**' 'fptyft'f* '.is*'-^ ty4s*.-fas*fy. st&ttQ j ^^jiXx^ 1 -**^ 4i*i*-tXx7/ i 'd*-jfrf(^

r X s ( *~-

*"*~~ ^ t^W* t*^ ^^ *^J*4,. '

/7

^^ ^P #*ue e /ei-o't)

SAMPLE No

STARTED

COMPLETED

ULTIMATE DEPTH

PROPOSED DEPTHWIDTH

OF SAMPLE GOLD lSLUDGE

GOLD I

DIAMOND DALL RECORDPROPERTY HOLE No.

SHFFTNUMRFR t f ^ SECTION FROM TO

LATITUDE i?4-8C* DATUM v 3 vW jtpZ^f/

DEPARTURE h^SOfe BEARING 7^'

ELEVATION '990,^,4 DIP ~*f 0 *4*,

DEPTH FEET

6- 1,1,

•f.o- f 7.0

•7.0 ' If.

''..S- #.f

S'-f' /5/r'j'

-r

V

FORMATION

CA^

* " t^ - -A 1 *4,J *' ' ' 4,

r. __ . ^ j^, * *a^ /^^ x ^; ./,;-^ " -a^t .fa.-b*. ^ -w ja ^ ,,x^ . !

CJf'iirt - *-C /s&t'*- ( -J ' ,J ^ ff'f" 1 9 -0 ", '"/(^/-'Xtv /*^V*V ^*i-i'ijjt'^ -^^l^C ^*-tiV^*^

Aitfysbt ^\ f7 -^J^C^ff^t l ' X^ "i-CX. J&tdZ* f* /VArf X"'*" j^*t^' -i*i *Xî ^"J^D -

7 ^ y. .^ 7 . '"7 ,

1/5 " ' 7 /T --' - ,'Y

^/^• ; w, y.-^^, ,^, .,,v* ^-r,. x^ ^ y^sv-^.7 y ^

(5'7?o *r^; ,v ?.. ^ -U, - ,,'.. t ^ /^^.-,^.,--.'0

^X. -i.^-, .V/-^ , -^

...W. .^ ...' - ,-, ^ ^',^ ;,... .*/,;

.'* ^ J' * p - j' ' rf ' p H4-x. -^ ^Siî'-'''^* 'iv .•'-'*' X l-Sî*-'^l ^ r /-T-^,' iX"*^ 7"^*T . - ^ -- ' ( . - ~f JL\.** - - '^-

r. *^- ^ - ;"' .': w ..,, 7

•;^- r-3': /^..,' -.,-x ,v,.-^ ^-^ J"*--.-,. ^ -' ^,.vs^•5 1 ' - ^ y - ' -. 0 ' /v: . r. ; . i : . - ,, . '.- .p-* '-" '•••.- --VC -.X . ^ ^

^-/"?.s- i M ,^Wy* ^^t jxrni*** ' *#**'*ct* (r*~* ^

SAMPLE No

* ^.52*^

7? ^^7

;??^

^RTED ^ ^ W

COMPLETED . ^-^ ^./A'SJ

ULTIMATE DEPTH s"-*'

PROPOSED DEPTH

WIDTH OF SAMPLE

-le - /? -0

/?.*VJ.J-

/,.^/i.o

77^ -r- i

GOLD S

S. (D

'•6-

•z-tr

:*1- 5 '

SLUDGE

GOLD i

,^^ 8

•- -~Y

-2

-

—

—

DIAMOND D L RECORDPROPERTY HOLE

SHFFTNIIMRFR SECTION FROM TO

1 ATITUDF DATUM

DFPARTURF BEARING

FI FVATIDN DIP

DEPTH FEET

'S/-*' /l 3 , fl

'536- .~.to.0

-30.0- ?i* ^

FORMATION

x5^v^. x,/^ ^^( /xvX^v -^ i t"^Lr^~f^~ sCb*^ x-*"- t'/^V-v-- , X^.^v^ ^ .^^ /•'

yfcl *3 //-CfV'Cv* /l ' n^JX. XV* ^f^Q!Z4tf- s^tf~-4. ^'^•fw- ^..c'-V "^ S '^:;'-{*f- /ri-^T^, ^ff,.f-fn* •fl&tC

, X7^ T 7

•-•--/" ---- --— — --- — — -- - -----^ - ————— ——————*^^ x1"^:^ t y ' ^.-r- '".- f t-^î {,-tfit-f'^ ^LAjfrf ^'-t-- "Cf^^^tô tffj. yOi*i^li i1^ tt^~ '-l .

•iw-v c ~" ' *-' i ' . -- V '^- z ^2f-t'~-!iZ , f- * 'jJ--i.-At , '^t/iS1-.*'' - '-- j*s-^ ' i 'L 'r' * - ^ t*y

.v/^ -^--^ --^ ;- -^^*. ^-*-^ -/-' ^ ^X--^,, ,,,f,^ ^-.^ ^^^^î. ^,i^,v -,^,, v ,.v-, -^44

. r ; r f ' f- s

* X f 3 "^^ 'C? SF,4t^fa.t'\*\3 Ji+^lL ^t&djs XY'-fttJ; ^ ji/) '^5' X5" ^"U? ^-Mi?

^xXX* VV* '*--4 jf j- (. Gt' ' /WttfCjCtrSj, X*0 L* ^tf'O^- -?O-A-J*V ^v- . AI'*^^^*^tJ5^ ^^

s-J'fjitAMs ?^.\I'-J-iGtJf* , -'S'- S A-* t'i^sjt-- ( /C# !yj. ';~ ..'^V'.^'W' ^Î'-Ctx-p } - "~ ^^

tJU'J** ,',*^ ^.,.s^,*t it*^ w. S, ,* ^,r~ -^-;*f f , '^

'li' f J*

, 7*7.*'? W; * t,...t ^ZL :/*/***^ ' f*jsJ-*U*

9 W* * ?M'.' sJ^^ * fa*^ 4 *? A x*

SN& df !'-uf 0 7*4.1'

SAMPLE NO

••51-*?

STARTED

COMPLETED

ULTIMATE DEPTH

PROPOSED DEPTH

WIDTH OF SAMPLE

iv*-*'*.?;

.-^*-.-^.J

GOLD t

C-f

-'•3

SLUDGEGOLD t

.^•s

DIAMOND D L RECORDPROPERTY HOLENo^ /.'3S-

SHEET NUMBER..

LATITUDE ____?

DEPARTURE__L

ELEVATION ___ S". L \

SECTION FROM——

DATUM _____^

.TO, STARTED -T^V-'-?

BEARING

DIP ^^..

COMPLETED —^

ULTIMATE DEPTH .

PROPOSED DEPTH.



GOLD l

A - 11.0

HJ^faf——7~

0-&

57.4-3?7

- nl.otlr* -f

DIAMOND D *L L R E C O R D

SHEET NUMBER

PROPERTY cVU^k- CWî^w ^,,x- ^- )Wi \ 3*,^** H OI F Nn ^-^

' ? . f SECTION FROM TO

LATITUDE ; #9 7 If- DATUM ^ s V-^ Jû-

DFPARTURE -70*87 BEARING

FIFVATION 99S"O,f4 DIP '^"* 0 c'o^

DEPTH FEET

(3- 7O

7-0- /33-0

;x?.d -;?7.3

,'??.;-

FORMATION

X

^ G/iîy 5***-- -^^*^* /^V^wot- ,' '-^2 '~be,, -2'xi*w^c- /xt^v s&^'fitjfc -t^v*?*'^*- .

yT ' [ ' V f'/*^ ^ ^ ,., , y". ^v * A. ^

7 7" ^ rc? ^^ ^ '' V-" " 4A. x"*i- ^ 35"'^"' Xis- ^J - M /fa^ r-^Vv^v*.

V' ' L '

J , /, , Z ' ^ ' -

^^-a 1 ' -^ j,*e^...*te ^n^0 T r^. , ''.y ' 'x

^ ^ . / j'jfjt Ar^^/^v- (2* ^•5 * ^ ^^ ^"^

/9 ;r/, 0 ' x'X^ty ^ J^-'S* /hSr--*~ ^C- "^5' ^ j^^t ,^txE^^ 7

y/ 7^ ' s^-Ct-tffît, S3ff^dt4j -fcttA&s ^ h-f.-s^ ' **A(ste'fy.*-^t' ^t^^f' s*Ztir f ^ *

/f ftv- 12 1-6 ~*d Ji'-J y / .rt* ' A/^^C ^W/^4* " x'Vfj^'.^ ^/.^**-* ,

U)/*^*"-^ ^--~ '. /;-V^,. / ',-fr^/A, fT^^^^^t /^0 ^'i^ 1-^ V'^."^- .'-^r/J^t^X^*^ i-

/^ ^'.f,. fab /. ~7-5' -^ ^' i*ti''

^/.,,'^4- ^ * - ^^^ ^/^ A^VS /U- 'A'/i , X^---**-,-^

-'•^.: -'^ î^ y A** ^ ^tA t Y,'**. *^-A*f ' '

, ^ XJ i

SAMPLE No

. ^ ^S/a.

fc.

M3S-OOJ,

-mi

fllSf-ov3

J^

STARTED '^ ^ ?* 2

COMPLETED .^ .* -*2.

ULTIMATE DEPTH -^ :''

PROPOSED DEPTH

WIDTH OF SAMPLE

-fr'^ '

tfS.a- "3 S

^7 a-/'?. 6

/33. o- /33 -5

GOLD S

Oi.-? '

4. f

^.-s

SLUDGE

GOLD S

-v-*..

.0*1s

~z*^.

2*fi- }-pf

DIAMOND D. •LL RECORD

SHEET NUMBER.

LATITUDE ———

PROPERTY

V______

lato, ~^'- HOLE No..

SECTION FROM.

DATUM A/J

.TO. STARTED .

COMPLETED /?8s

DEPARTURE__l

ELEVATION __5

BEARING

DIP ..—. -s" (9 jULTIMATE DEPTH

PROPOSED DEPTH —

DEPTH F EET FORMATION SAMPLE NoWIDTH

OF SAMPLE GOLD I SLUDGE

GOLD S

(5 -

Z '-0- ^

33. /^

y -~* ;. o

S.T.3-

DIAMOND D0LL RECORDPROPERTY HOLE No..

SHEET NUMBER..

LATITUDE ———

DEPARTURE ———

SECTION FROM.

DATUM ————

STARTED,

COMPLETED

ELEVATION ——

BEARING

DIP ,,^..

ULTIMATE DEPTH

PROPOSED DEPTH.


OF SAMPLE GOLD SSLUDGE GOLD t

3S.0 ; AtjC^TjCi -~^tjf,

#-y^M*-S */,

~^r /f

t S.o- 6S.S

^y--~T

0

T- ^

fc-s- -A3 2-

^ri

s v /r

D l A M O N D D mi L R E C O R DPROPERTY HOLE No..

SHEET NUMBER.

LATITUDE ———

DEPARTURE ——

ELEVATION ——

SECTION FROM.

DATUM ..^^

-TO.^ STARTED^^

COMPLETED

BEARING

DIP -——

ULTIMATE DEPTH

PROPOSED DEPTH.

DEPTH FEE! FORMATION SAMPLE NOWIDTH


GOLD t

(S - 70-75' 0^-3

0.3.

f 67.6 -/tt. i \ *-j~

o* A

f/il-HU 0-2 • OOZ-

-f**i*.

Ad

l r *ss, s - '-i

t/v^

DIAMOND D0LL RECORD

SHEET

LATITUDE

PROPERTY

J4-J-———

HOLE No..

SECTION FROM.

DATUM ____

-TO.

DEPARTURE__]

ELEVATION —— - 67

BEARING

DIP ___

STARTED__

COMPLETED

ULTIMATE DEPTH

PROPOSED DEPTH.



GOLD S

0 ~ /i Q

/S .0 - /Q. o

f B .0 ~ 5V 0

— - "7™—"

. - . - . . . .. . ' . 'SI.O

S?

•~-':*u~ 4u*:

5,0

^-^

/--s-

5 li

-78,0-5-''.

SO

.i? 6-rf&

DIAMOND D •L L RECORDPROPERTY HOLE No..

SHEET NUMBER.

LATITUDE ^__^.

DEPARTURE ——

ELEVATION ——

SECTION FROM.

DATUM ______

BEARING -——

DIP —————

-TO. STARTED__

COMPLETED

ULTIMATE DEPTH

PROPOSED DEPTH.

DEPTH FEET FORMATION SAMPLE No WIDTH OF SAMPLE GOLD t

SLUDGE GOLD t

1*7*' 'I/to', Ao

3'

' s St 4'

-2*^

-f

'±-?***————

CA, •222.0 -J Jf 6

r 1 1 Z o

771,0 -

.'-23 -1 -23* -

26f.s f 7 T

3 .i'

/57.0 - 0

DIAMOND D L RECORD

SHFFTNUMBFR

PROPERTY HOLE No

5 ^-? SECTION FROM TO

LATITUDE DATUM

DEPARTURE BEARING

FI FVATION DIP

DEPTH FEET

2cio- ?~i7.d

777-0 ' Z 30-0'

2 ' JQ - Q ' ^52 ! ()

FORMATION

6^*- O^: u^, a *A _ 4^*5 xû aW 2SiS'

sU&XJ'MjILf L-J^C^^^^ ' fllA&Ctj**'^ *fy*'^4#\4^s t ^Ct^^^ft ft**fM- PÔ^t^ **^-^*f P

,X-A^w* .îrftÂ^ , hlsftX-^'b&^'fGty gfas*O0t'Ml'^4*^4t' /^'t'X* ^T^titîCf^' Jty,**^#fieJ*~

*t 75' t'' 4, ^L M**, ^^ 4****.L** -Py^*

sj^^ , _______ ^^ ^JM ^ ^^^. /^^ ^^

^r^JL trttX*, if wJ*6L/^ j A/7

f-

'

Z,MO tr ê- j w. t'

SAMPLE No

'^

A

STARTED

COMPLETED

ULTIMATE DEPTH

PROPOSED DI

WIDTH OF SAMPLE

2ft*'2i6.0

GOLD S

•3-0'

EPTH

SLUDGE

GOLD S

"f, - ' t-t

NO.20 ZONE0.38 13D 1

MURGOLD RESOURCES INCMURGOLD RESOURCES INC.

RESOURCES

HARGOR RESOURCES27/6.0

1.03/6.0 92

Appro*.location of only Murgold hoi* on No 0.146/6'

800 western portion 4 Sub-parallel veins including Walts

Appro*, location or Section24-I32WNWHole No. KI-70, O.32/I2 1(not Murgold hole -confirmed by B. Hommerstrom)

Watts vein Locale 290' strike length grading at 0.49

Ton Au over 3.Approx 900 exposed and sampled Approx. 1000 gap [.221

Deeper overburden5

1400 Central portion 8000'of d,drilling (M)

(1937) 116 al 65 0 N 286' ol latera! development Additional drifting on d bulk sample by Murgold

600 Eastern portion 6 bulk sample

Appro* location Section 1*064 WNW Hole No. MI3- 0.554/10' (slant Intersection) Hole drilled from south side

same direction as dip of vein)

CANADIAN GOLD CREST

THREE DUCK L AKES

Appro*, location of Snep - Mac D.D.H. vein intersection at I374 1 VLF E M-16 Anomaly

Vein- Shear S ystem N o. .364 Au (oz/ton) Grab S ample

219/3.G' Au (oz/ton)/feet Chip Sample

MURGOLD RESOURCES INC.l. Muraold drilled 42 holes - 12,776

2. W.G.M. Report, p.39 " it has been established that the No.3 vein Is not a single vein but a system of narrow veins located within o NMO0 structural trsnd (shear. ) at least 2,8OO' long and same 2001 wide'

COMPOSITE MAP

NO. 1 ,2,3,4,5,8 VEINS

CHESTER, BENNEWEIS 8 ST LOUIS TOWNSHIPS3. Bill Hammerstrom recently indicated thot he

feels the No. l vein system is o priority target

SCALE- l = 1 000 DATE- DEC. 1983DRAWING NO.: l

41P12SW0002 63.4370 ST. LOUIS 200

BERNICE LAKE

MURGOLD RESOURCES INCORPORATEDCHESTER, BENNEWEIS ft ST. LOUIS TOWNSHIPS

PORCUPINE MINING DIVISION, ONTARIO

PLAN OF GRID A

SOIL GEOCHEMISTRYCONTOUR INTERVAL = 1 0 ppb Au

N.T. S. : 41- P/12 SCALE : l" = 200'

MAPPED BY: D. H. DRAWING NO. : 4

DRAWN BY-' M. B. DATE : DECEMBER 1983

41PI2SW0002 63.437® ST. LOUIS 210

SOUTHCAMP

BAY

2 f DON

BERNtCE L AKE

0 + 00

- 2t00 S

- 4+00 S

- 6 * 00 S

8 + 00 S

IN - PHASE PROFILE - OPERATOR FACING NORTH CONTOUR INTERVAL = 20 U NITS

SURVEY WITH GEONICS EM-16 BY BULLOCK

TRANSMITTER NAA, CUTLER. MAINE. 17.8kHz

50 "/o - 50 7o

MUR60LD RESOURCES INCORPORATED

CHESTER, BENNEWEIS a ST. LOUIS TOWNSHIPS


PLAN OF GRID AVLF-EM SURVEY

FRASER FILTERED CONTOURS S IN-PHASE PROFILES

N.T. S. : 41- P/12

MAPPED BY: D. H.

DRAWN BY: M. B.

SCALE : l" s 200'

DRAWING NO. : 3

DATE : DECEMBER 1983

B. 5,

4 l P 1 2SIYC002 63.437® ST. LOUIS 220

- IO+ DON

- 8 *00 N

00 N

00 N

- 2 + 00 N

- 0 + 00

- 10 + 00 S

- 5 + 00 S

- 10 + OOS

CONTOUR I NTERVAL ~ 1 0 ppb Au

MURGOLD RESOURCES INCORPORATED

CHESTER, BENNEWEIS a ST. LOUIS TOWNSHIPS


PLAN OF GRID B

SOIL GEOCHEMISTRY Au ppb

N.T. S. : 41- P/12

MAPPED BY: D. H.

DRAWN BY-. M. 8.

SCALE: l" . 200'

DRAWING NO. : 7

DATE : DECEMBER 1 983

T L. 5 +00 N - 5+00 N

ARETHUSA


CHESTER, BENNEWEIS S ST. LOUIS TOWNSHIPS

PORCUPINE MINING DIVISION, ONTARIOCONTOUR INTERVAL = 20 UNITS

SURVEY WITH GEONICS EM - 16 BY BULLOCK

TRANSMITTER NAA, CUTLER, MAINE, 17.8kHz

IN-PHASE PROFILE - OPERATOR FACING NORTH

PLAN OF GRID BVLF-EM SURVEY

FRASER FILTERED CONTOURS 8 IN-PHASE PROFILES

SCALE: l" - 200N.T. S. : 41- P/12

MAPPED BY: D. H. DRAW NG NO. : 6

DRAWN BY: M. B. DATE: DECEMBER 1983

41P12SW0e02 63.4370 ST. LOUIS 240

12 + 00 N -

10+OON -

8 + 00 N -

6 + 00 N -

4 + 00 N -

2 + 00 N

0+00

IN-PHASE PROFILE-OPERATOR FACING NORTH

50 7o - 50 7o

CONTOUR INTERVAL = IO UNITS

SURVEY WITH GEONICS EM-16 BY BULLOCK

TRANSMITTER NAA, CUTLER, MAINE, 17.8 kHz

^—* V EIN EXPOSURE

•/,''; BULLDOZED AREA

/rr4^? TRENCH LOCATIONS




PLAN OF GRID CVLF-EM SURVEY

FRASER FILTERED CONTOURS a IN-PHASE PROFILES

N.T.S.: 41- P/12

MAPPED BY: D. H.

DRAWN BY: M. B.

'SCALE: l" s 200'

DRAWING NO. : 8

DATE: DECEMBER 1983

l?*-

12*00 N -

10 + OON -

8 + 00 N -

6*00 N -

4*00 N -

2-00 N -

0 + 00

NS

NO. i SHAFT (GOMAK)

41PI2SW0002 63.437(2 ST. LOUIS

CONTOUR INTERVAL - l Oppb

* Contours increase in increments of 50ppb


CHESTER, BENNEWEIS ft ST. LOUIS TOWNSHIPS


PLAN OF GRID C

SOIL GEOCHEMISTRY Au ppb

N.T. S.: 4!- P/12

MAPPED BY; D. H.

DRAWN BY: M. B.

SCALE: f" * 200'

DRAWING NO. :

DATE: DECEMBER 1983

Documents

louis 010 REPORT ON PROPERTY CHESTER, BENNEWEIS AND ST ... · Apper lix "B". Hill, Goettler, De Laporte Limited accepted the materi al si imitted as factual, excepting some discrepancies