equity silver mines limited - aris.empr.gov.bc.ca

EQUITY SILVER MINES LIMITED

ASSESSFIENT REPORT

FOR THE

1986 DIAMOND DRILLING

ON THE

SG 19, 20, 21, 22, 23, 24, AND 30

MINERAL CLAIMS

OMINECA MINING DIVISION

NTS 93 ~/l\ihl, I€

o 11.4' LATITUDE 54 k W N

16.2' LONGITUDE 126 EY W

OWNED BY: EOUITY SILVER MINES LIMITED

WORK BY: EOLIITY SILVER MINES LIMITED

REPORT BY: R. B. PEASE

DECENBER 1986

G E O L O G I C A L B R A N C H A S S E S S M E N T R E P O R T

TABLE [IF CONTENTS

PAGE

INTRODUCTION

(i) Location and Access . . . . . . . . . . . . . . . . . 1

(ii) Claim Ownership and Status . . . . . . . . . . . . . 1

(iii) P u r p o s e . . . . . . . . . . . " . . . . . . . . . . . 4

PROPERTY DESCRIPTION

( i ) Geology. . . . . . . . . . . . . . . . . . . . . . . 5

(ii) Mineralization . . . . . . . . . . . . . . . . . . . 5

(iii) Alteration . . . . . . . . . . . . . . . . . . . . . 7

DRILLING PROGRAMME 9

RESULTS

(i) O v e r v i e w . . . . . . . . . . . . . . . . . . . . . . . 11

(ii) HopeArea . . . . . . . . . . . . . . . . . . . . . . 12 (iii ) Superstition Zone . . . . . . . . . . . . . . . . . . 15

STATEMENT OF EXPENDITURES 18

AUTHOR'S OUALIFICATIONS 19

REFERENCES 20

APPENDIX I - Diamond Drillhols Lagging Code Explanation

APPENDIX I1 - Diamond Drillho!e Geologic Loys and Assay Data

FIGURES AND TAHLES

PAGE

LIST OF FIGURES

. . . . . . . . . . . . . . . F i g u r e 1 - M i n e s i t e L o c a t i o n 2

. . . . . . . . . . . . . . . . F i g u r e 2 - M i n e s i t e Access 2

F i g u r e 3 - P r o p e r t y Layout . . . . . . . . . . . . . . . . 7 .-,

F i g u r e 4 - D r i l l h o l e Loca t ion r j . . . . . . . . . . . . . ( i n pocl:et)

F i g u r e 5 - P r o p e r t y Geology . . . . . . . . . . . . . . . 8

F i g u r e b - P r o p e r t y A l t e r a t i o n . . . . . . . . . . . . . . 8

LIST OF TAHLES

Tab le 1 Statement o f Expend i tu res . . . . . . . . . . . . 18

INTRODUCTION ------------

(i) Loca t i on and Access

The E q ~ l i t y S i l v e r m ines i t e i s l o c a t e d 40 km southeast o f t h e town

o f Houston, B r i t i s h Columbia (see F i g u r e 1 ) . The m i n e s i t e l i e s i n t h e

gen t l e , and o c c a s i o n a l l y steep, h i l l s of t h e Nechako P la teau

phys iograph ic r eg ion . Rccess i s gained t o t h e p r o p e r t y b y an a l l -

weather g rave l r oad f rom Houston (see F i g u r e 2 ) . The d r i l l h o l e s

discussed i n t h i s r e p o r t ar-e l o c a t e d i n t h e gener-a1 ar-ra sou th o f t h e

abandoned S o ~ ~ t h e r n T a i l p i t !see F i g u r e 5 ) . Access t o t h e d r i l l s i t e ;

i s v i a r e c e n t l y cons t ruc ted 4 :: 4 t r a i l s which r u n E O L I ~ ~ I fr-om t.he

S o ~ ~ t h e r n T a i l p i t and n o r t h f r n n t h e o l d BL I~~ : : F l a t s l ogg ing road (see

Figur-e 4 ) .

(ii! Claim Ownership and S ta tus

The E q u i t y m i n e s i t e p r o p e r t y c o n s i s t s of C e r t i f i e d Min ing Lease

# 1 and Min ing Lease # 6 surrounded by a b l o c k of 209 two-post m inera l

c la ims, 7 f r a c t i o n a l c la ims, and 3 mod i f ied g r i d c l a i m s (43 u n i t s ) .

I n add i t i on , 19 two-post c l a ims and one f r a c t i o n a re j o i n t l y h e l d w i t h

Teck Corpora t ion and Pioneer Meta ls Corporat ion.

The d r i l l i n g was conducted on t h e SG 19, 20 , 21, 22, 2 3 , 24, and

30 minera l c la ims. A l l of these c l a ims a r e who l l y owned by E q u i t y

S i l v e r Mines L i m i t e d and ar-e n o t sub jec t t o any vendor agreements.

T h e i r boundar ies a r e shown on F i g ~ ~ r e 4. For t h e purpose of r -ecord ing

assessment, severa l ad,oining cl.aims have been gro~lpecl t o form Che

06 -2 g r o ~ ~ p .

FIGURE 1 - IIINESITE LOCATION

I1

FIGURE 2 - MINESITE ACCESS

EQUITY SILVER MINESITE N.T.S. 93 L /I

- Clo~rn Block Outlinr

Southern f o i l Zone

FIGURE 3 - PROPERTY LAYOUT

The company h a s been c o n t i n ~ m ~ ~ s l y o p e r a t i n y s 5 5130 t p d open p i t

min ing and m i l l i n g complex a t t h i s s i t e s i n c e mid t.960. P r o d u c t i o n

was i n c r e a s e d t o 13 OOO t p d i n mid 1936. T h r e e ore d e p o s i t s are i::nown

t o o c c u r on C e r t i f i e d Mining L e a s e # 1. The S o u t h e r n T a i l d e p o s i t h a s

been mined o u t t o t h e economic limit of a n open p i t . The Main Zone

d e p o s i t i s c u r r - e n t l y b e i n g mined by an open p i t , and t h e W a t e r l i n e

d e p o s i t h a s y e t t o b e d e v e l o p e d . P roven o r e r e s e r v e s , a s of J a n u a r y

1966, were a p p r o x i m a t e l y 17.8 m i l l i o n t o n n e c a t a y a d e of 0.35%

c o p p e r , 106 g / t s i l v e r , and 1.04 g / t g o l d .

( i i i ) P u r p o s e

E i g h t e e n NO s i z e diamond u r i l l h o l e s , t o t a l l i n q 3 3 9 . 9 metres,

were d r i l l e d t o test p o s s i b l e m i v e r a l i m e d s t r - u c t u r e s . Ten h o l e s were

d r i l l e d n o r t h of S u p e r s t i t i o n Creek . T h r e e h o l e s had been d r i l l e d i n

p r e v i o u s y e a r s i n t h i s a r e a , and some weakly m i n e r a l i z e d s t r u c t u r e s

were d e f i n e d .

E i g h t h o l e s were d r i l l e d s o u t h of S u p e r s t i t i o n Creek . F o u r t e e n

h o l e s had been d r i l l e d i n p r e v i o u s y e a r s i n t h i s a r e a , and a low gr-ade

s t r ~ ~ c t u r e ( t e r m e d t h e S u p e r s t i t i o n z o n e ) was p a r t i a l l y d e f i n e d .

( i ) Geology

The g e o l o g y of t h e E q u i t y S i l v e r p r o p e r t y is b r i e f l y d e s c r i b e d

be low and i l l u s t r a t e d on F i g u r e 5. The r e a d e r is r e f e r e n c e d t o Cyr ,

e t a l . ( 1984 ) f o r a more d e t a i l e d d e s c r i p t i o n .

The d e p o s i t s o c c u r i n a hon ioc l i na l Upper J u r a s s i c t o C r e t a c e o u s

i n l i e r c o n s i s t i n g of s e d i m e n t r ) , p y r o c l a s t i c , and v o l c a n i c r o c k s

f l a n k e d by i n t r u s i o n s and s u r r o u n d e d by younger-, u n c o n f o r m a b l e

T e r t i a r y a n d e s i t i c t o b a s a l t i c f l o w s and f l o w b r e c c i a s . Fou r

s t r a t i g r a p h i c c o n f o r m a b l e s u b d i v i s i o n s , t e rmed t h e Goos ly Sequence ,

are r e c o g n i z e d i n t h e i n l i e r and c o n s i s t of a ba5;al c o n g l o m e r a t e and

a r g i l 1 . i t . e ( c l a s t i c d i v i s i o n ! ; int .er-calatecl c,ub-aeri a1 t u f f s and

b r e c c i a s ( p y r a c l a s t i c d i v i s i o n ) ; i n t e r b e d d e d v o l c a n i c c o n g l o m e r a t e ,

s a n d s t o n e , and bedded t u f f ! s ed imen t ry -vo l c a r t i c dl v i s i o n ) ; and

a n d e s i t e and d a c i t e f l o w s ( v o l c a n i c f l o w d i v i s i o n ! . The Goctsl y

s e q u e n c e h a s an o v e r - a l l stril'e of 0 1 5 and d l p s g e n e r a l l y t o t h e west.

A q u a r t z monzon i t e e t o c k (58 m.y.) on t h e west, and a gabhr'o-

m o n z o n i t e complex ( 4 9 m.y.) t o t h e e a s t , i n t r - u d e t h e Goos ly s e q u e n c e .

F 'os t -minera l a n d e s i t e and q u a r t z l a t i t e d y k e s ( 4 9 m.y.) c r o s s c u t t h e

Goos ly s e q u e n c e and t h e gabb ro -monzon i t e complex.

( i i 1 Eineralizat.gn_

E c o n o m i c a l l y s i g n i f i c a n t Ch-Ag-ALI m i n e r a l i z a t i o n o c c u r s i n t h r e e

d i s t i n c t z o n e s d e s i g n a t e d t h e Main, Wa te r - l i ne , and S o u t h e r n T a i l

o r e b o d i e s (see F i g u r e 5 ) . F y r i t e is most a b u n d a n t m e t a l l i c

minera l t h r o ~ ~ g h o u t t h e Goosly sequence r e g i o n a l l y , and w i t h i n the

zones o f Cu-Ag-Au m i n e r a l i z a t i o n i n p a r t i c u l a r . The p r i n c i p a l s i l v e r

minera l i s t e t r a h e d r i t e w i t h minor va lues c o n t r i b ~ ~ t e d by a v a r i e t y of

a r g e n t i f e r o u s minera ls . Cha l copy r i t e i s t h e p r - i nc ipa l copper minera l

and a smal le r b u t s i g n i f i c a n t p o r t i o n i s i n t e t r a h e d r i t e .

The o re m ine ra l s a r e g e n e r a l l y r e s t r i c t e d t o t a b u l a r zones

s~~bconco rdan t t o hos t r ock s t r a t i g r a p h y . They occur as

d isseminat ions, veins, f r a c t u r e f i l l i n g s , and l o c a l l y as massive pods

and ma t r i x m a t e r i a l i n b r e c c i a zones. The pr imary o r e c o n t r o l i s

s t r u c t u r a l , s i n c e "economic" su lph ides tend t o be bes t concentrated i n

zones o f i n tense f r a c t u r i n g and b r e c c i a t i o n .

I t i s be l i eved t h e Cu-Ag-Au m i n e r a l i z a t i o n i s ep igene t i c i n

o r i g i n . I n t r u s i v e a c t i v i t y r e s u l t e d i n t h e i n t r o d u c t i o n o f

hydrothermal me ta l - r i ch s o l u t i o n s i n t o t h e py r -oc las t i c d i v i s i o n o f t h e

Goosly sequence. Sulphides in t roduced i n t o t h e more competent and

permeable ash and l a p i l l i t u f f s of t h e Main and Water l ine zones formed

as s t r i n g e r s and d issemina t ions which grade randomly i n t o zones o f

massive su lph ide . I n t h e Southern T a i l Zone, su lph ides formed as

veins, f r a c t u r e f i l l i n g s , and b r e c c i a zones i n t h e b r i t t l e , l e s s

permeable f i n e g ra ined dust t u f f . Emplacement of pos tminera l dykes

i n t o a l l t ypes o f su lph ide - r i ch p y r o c l a s t i c r ocks r e s u l t e d i n

r e m o b i l i z a t i o n and concent ra t ion of su lph ides adjacent i n t r u s i v e

contacts . Hemob i l i za t ion , concent ra t ion , and con tac t metamorphism of

su lph ides occurred i n t h e Main and Water l ine zones a t t h e con tac t w i t h

t h e postminera l gabbro-monzonite complex.

(iii) flltewetFo~

Alteration assemblages in the Goosly sequence are characterized

by minerals rich in alumina, bur-on, and phosphorous. The distribution

of vario~~s alteration zones is illustrated on Figure 5. Four types of

alteration are recognized and briefly described below. The reader is

referenced to Wojdak and Sinclair (1984) for a more detailed

discussion.

1. Alumino~~c, alteration is characterized by a suite of al~~minous

minerals including analusite, co~.rundum, pyrophyllite, and scorzalite.

These alteration zones show a systematic spatinl relationship to areas

of mineral deposits.

2. Boron-bearing minerals consisti ny of taurmal ine and

dumortierite occur within the ore zones and in the harlg:ngwall section

of the Goosly sequence.

3. Phosphoro~~s-bearing mi!lerals including scorzal i te, apatite,

augelite, and svanbergite occur in the hanqingwal.1 zone, immediately

above and intimately associated with sulphide minera!~ - particularly

in the Main and Waterline zones.

4. Phyl lic a1 teration is characterized b y weal:: to pervasive

sericite-quartz replacement:. It appears to envelope zones. of intense

fracturing, with or without chalcopyrite/tetrahedrite occurences,

particularly in Unit 2 dust tuffs.

The proyramme cons i s ted of 3449.9 m of NCI w i r e l i n e diamond

d r i l l i n g spread over e igh teen (:8) holes. The c o l l a r l o c a t i o n s and

sur face p r o j e c t i o n s of t h e d r i l l t ~ o l e s a re shown on F i g u r e 4. A l l of

t h e d r i l l h o l e s were i n c l i n e d a t angles from -45 t o -70 degrees, and

o r i e n t a t e d i n an e a s t e r l y d i r e c t i o n . T h i s p a t t e r n was chosen t o bes t

i n t e r s e c t p o s s i b l e north-south, west d ipp ing , m ine ra l i zed s t r u c t u r e s

s t r i k i n g through t h e general area.

The d r i l l setup pacls and access roads were cons t ruc ted p r i o r t o

d r i l l m o b i l i z a t i o n by a con t rac ted DE t r a c t o r . The d r i l l i n g

c o n t r a c t c r was G & D Diamond D r i l l i n g of Kamloops, H.C. A s k i d -

mounted Longyear Super ZE w i r e l i n e d i g r i g was u t i l i z e d . The

cont racto l - supp l i ed a t r a c t o r t o move and a s s i s t t h e d r i l l . The

d r i l l i n g o f ho les X86CH233, X8hCHZ39, and X86CH240 commenced on March

20 and i i n i s h e d on march 29, IY36 . The remain in3 d r i l l h o l e s , X86CH260

t o X86CHZ74 wer-E d r i l l e d s e q u e n t i a l l y f rom J u l y 13 t o August 26, 1986.

The co re was t ranspor . ted t o t h e l ogg ing f a c i l i t i e s a t t h e

minesi t e immediat-el y f o l l o w i n g I ro lc complet ion. The co re was logged

by t h e author, M r . Dary l tianson and M r . Ray Westendot-f. M r . Hanson,

a g e o l o g i s t t e m p o r a r i l y employed by Equ i ty , has p reva len t academic and

p r a c t i c a l t r a i n i n g , h o l d i n g a H.Sc. degree i n geology and hav ing

over t e n years exper ience i n miner-a1 e x p l o r a t i o n . M r . Westendorf, a

Ca r l e ton U n i v e r s i t y geology s tuden t t e m p o r a r i l y employed by Equ i t y ,

i o g g ~ d t h r e e h o l e s under- t h e super-v is ion of t h e author . The d r i l l h o l e

l o g s have heen reproduced and a r e i n c l u d e d in t h i s r e p o r t as

Appendix 11. Assay r e s u l t s f o r t h e sampled i n t e r v a l s a r e recorded a t

t h e end of t h e logs . A l l assay r e s u l t s a re recor-ded i n percent,

e c i e p t s i l v e r and g o l d which a r e repo r ted i n grams/tonne.

A coded core l agg ing system was u t i l i z e d on t h i s programme main ly

t o improve t h e measure of o b j e c t i v i t \ , , consistency, measureab i l i t y ,

and r e a d a b i l i t y as compared t o h i indwr i t ten logs. The system a l l o w s

geo lcg ic and assay da ta t o be er l tered i n t o fo rmat ted computer da ta

f i l e s . These f i l e s can be accessed by programs which p l o t s e c t i o n s

and plans, per fo rm s t a t i s t i c a l analy*es, and a s s i s t i n reserve

c a l c u l a t i o n s . An exp lana t ion of t h e l ogg ing codes i s p rov ided i n

Append::: I .

The core was sampled top 'o bottom i n approx imate ly 3.0 metre

i n t e r v a l s . Barr-en dyke i n t e r s e c t i o n s wer-e gener-al l y omi t ted.

Sampling was dcne by a hand operated core s p l i t t e r . One h a l f was

p laced i n p l a s t i c sample bags and d e l i v e r e d t o E q u i t y ' s m ines i t e

l a b o r a t o r y f o r assay, and t h e o the r h a l f was r e t u r n e d t o t h e core box

f o r permanent s torage. The s p l i t core i s s to red i n t h e f a c i l i t i e s a t

t h e minesi te .

The core samples were assayec! f o r t h e meta ls CLI, Ag, Au, Sb, As,

Fe, and Zn. I n E q u i t y ' s assa) procedure, 1 gram o f p u l v e r i z e d

m a t e r i a l i s d i sso l ved i n 10 m l o f n i t r i c a c i d and 30 m l of

h y d r o c h l o r i c ac id . Th i s s o l u t i o n i s b o i l e d f o r f i f t e e n (15) minutes,

a f t e r which 10 m l o f 10% t a r t a r i c a c i d i s added and t h e sample i s

r e tu rned t o t h e ho t p l a t e f o r f i v e ( 5 ) minutes. The s o l u t i o n i s

a l lowed t o cool and q u a n t i t a t i v e a n a l y s i s i s done on an atomic

absorp t ion machine, except f o r Au which i s f i r e assayed f i r s t .

(ii Overview

The geology o f t h e d r i l l i n g area i s r e s t r i c t e d t o U n i t 2

( P y r o c l a s t i c D i v i s i o n ) and U n i t : (Sedimentry - Vo lcan ic D i v i s i o n ) o f

t h e Goosly sequence. The U n i t 3 U n i t 3 con tac t i s shown on F i g u r e 4.

The U n i t 2 r o c k s i n t e r s e c t e d i n t h e d r i l l i n g c o n s i s t ma in ly of

massi.ve, f i n e grained, green t o t a n dus t t u f f s . Some coarser g ra i ned

ash and l a p i l l i t u f f s were a l s n i n t e r s e c t e d . The U n i t 3 r o c k s

i n t e r s e c t e d i n t h e d r i l l i n y c o n s i s t of in terbedded chel-t pebble

conglomerate, quar tz sandstone, well-bedded dus t and ash t u f f s , and

some vo l can i c conglomerate and sandstone. The c h e r t pebble

conglomerate and quar tz sandstone tend t o dominate t h e base o f t h e

u n i t , w h i l e t h e t u f f s and sandc,tones a re more common h ighe r i n t h e

sec t i on . Both U n i t 2 and 3 a r e c u t by numerous andes i te and quar tz

l a t i t e dykes.

The Un i t r ; a r e b e l i e v e d t o be s t e e p l y f o l d e d and have an o v e r a l l

s t r i k e of 017 degrees. The f o l d i n g i s apparent i n U n i t 3 rocks, b u t

d i f f i c u l t t o i n t e r p r e t i n U n i t 2 p y r o c l a s t i c s due t o t h e i r massive

na tu re and l a c k o f wel l -preserved l d e n t i f i b l e bedding.

U n i t 2 i s cons idered t he main t a r g e t f o r h u s t i n g "e:onomis"

m i n e r a l i z a t i o n . The key gu ides t o l o c a t i n g m i n e r a l i z a t i o n i n t h i s

area a r e degree o-i f r a c t u r i n g , arid a l t e r a t i x i n t e n s i t y . Low grade

a l t e r a t i o n ( P r o p y l i t i c ) i s r-ha:-acterl-ed b y c h l o r - i t e l i n i n g f r a c t u r e s

(~nic:roveins! . E igher grade a l t e r a t i o n i s de f i ned by i n c r e a s i n g

i n t e n s i t y o f qua r - t z - se r i c i t e ( o r p h y l l i c ! r ep laceae r t . That i s ,

"economic" m i n e r a l i z a t i o n cou ld he ecpected t o occur i n a zone of

in tense f r a c t u r i n g and pervasive phyl ! ic a1 t e r a t i o n . The "economic"

m i n e r a l i z a t i o n an t i c i pa ted i c c h a l c o p y r i t e and/or t e t rahedr i t -e

occur r ing i n microveins. Accesscry at inerals coulcl i n c l u d e spha le r i t e ,

arsenopyr i te , and specular hemati te. P y r i t e o c c u r r i r q i n micr.oveins

and d isseminat ions i s common th rougho~t t U n i t 2 and 3. The

d i s t r i b u t i o n o f l i t h o l o g y , f r a c t u r e i n t e n z i t y ? a l t e r a t i o n , and Cu-Ag

m i n e r a l i z a t i o n i s summarized i n t h e f o l l o w i n g h o l r hy ho le discus5ion.

Descr ip t ions o f the frequent, pcs t -m ine ra l i za t i on dykes are g e n e r r i l y

omit ted.

Some of t h e holes d r i l l e d n o r t h of S u p e r s t i t i o n Creek (see

F igu re 4) i n te rsec ted a new minera l i zed s t r u c t u r e which has been

termed t h e Hope zone. The ho les d r i l l e d i n the S u p e r s t i t i o n zone lead

t o f u r t h e r d e f i n i t i o n o f t h e zone. Both of these zones r e q u i r e

f u r t h e r s tudy and a d d i t i o n a l d r i l l i n g t o determine f e a s i b i l i t y o f

mining. The Hope zone i s poo r l y def ined, and t h e gr-ade of the

S u p e r s t i t i o n zone appears t o be below an economic l e v e l .

(i i ) Hope Area

Hclles X86CH23R and X8bCH?ZC' were d r i l l e d t:, i n t e r s e c t a poss ib le

southern extension o f a weal: ! . t ructure p rev ious l y defi,ned t o t h e

nor th. The rock types i n te rsec ted were U n i t 2 dust t u f f s , w i t h minor

ash u n i t s towards t h e end of t h e holes. Both ho les d i s p l a y low

f r a c t u r e i n t e n s i t i e s , bu t r a t h e r pervasive q u a r t z - s e r i c i t e a l t e r a t i o n .

A few sporadic: very low Ag assays were obtained, hut they cannot be

a t t r i b u t e d t o a s i g n i f i c a n t s t ruc tu re .

Holes X85CH250 and X86CH251 were d r i l l ed on the same section a s

238 and 239 b u t fur ther t o the eas t . T h i s location tes ted a possible

southern extension of the So~rthern Tail s t ructure . Mainly Unit 2 dust

t u f f s were intersected, w i t h some ash t u f f near the top of 250 and a

few in te rva l s of l a p i l l i t u f f near the bottom o+ 1 The f r ac tu re

intensi ty was re la t ive1 y low throughout both holes. In hole 260, weak

t o moderate quar tz-ser ic i te a l t e ra t ion was observed above 51.0 metres,

and only chlor-ite a l t e ra t ion occurs below. Hole 261 displays a very

s imil iar a l t e ra t ion pattern with weak t o moderate quar tz-ser ic i te

above 101.0 metres, and ch lor i te below. Weal:. sporadic chalcopyrite i n

microveins was noted above 47.0 metres in hole 260. Twa low grade

intersect ions were found in hole 251, from 103.0 t o 105.0 metres

( 0 . 8 % CLI, 28 g i t Ag) and from 124.0 t o 125.3 (0.24% Cu, 15 g / t Ay)

metres.

Hole X8bCH240 was d r i l l ed t o t e s t a possible up-dip extension of

a small mineralized zone located by a hole d r i l l ed i n 1770. Hole 240

intersected Unit 2 ash t u f f s which displayed re l3 t ive ly high f r ac tu re

in tens i ty and moderate t o pervasive quar tz-ser ic i te a l t e r a t i on . No

s ignif icant mineralization was located. A t 3 l a t e r date, hale

XObCH262 was d r i l l ed on the same section b u t down-dip of the 1970

hole. A re la t ive1 y good mineralized intersection was found, and

termed the Hope zone. Hole X86CH273 was dr i l l ed fur ther down-dip on

t h e same sect ion, and holes X85CH272 and X86CH274 were d r i l l ed

appt-o;:imatel.y 100 metre.; t o the south and north respectively, i n an

attempt t o t r ace the zone.

Ail of these holes (262, 272, 273, 274) were collared in

interleveled U n i t 5 chert pebble con~lomerates, quartz sandstones, and

well-bedded ash and dust tuifs, and passed in to Unit 2 dust tuffs t o

the end of the hole. In hole XB6CH262, the Unit 2 dust t~lffs display

medium to high fracture intensity and moderate to strong phyllic

alteration down to appro::imatel)r 270 metres. Below this point, the

tuffs display only low to medium fracture intensity and chloritic

alteration. Mole 262 contains a zone approximately 100 metres long of

sporadic Cu-Ag mineralization broken by a few post-mineralization

dykes. Two ;rf the better intzrsoctions include; 167.0 to 194.0 metres

averaging 0.57% Cu and 14 g/t Ag, and 235.0 to 256.3 metres averaging

0.?9% CLI and 278 g/t Ag. These zones contained chalcopyrite and

tetrahedrite in microveins.

The Unit 2 dust tuffs in hole X86CH273 displayed relatively high

fracture intensity and pervasive quartz-sericite alter-ation to the end

of the hole. However, only sporadic low grade mineralization was

intersected. The interval from 228.0 to 267.3 metres averaged 0.23%

Cu with a few low Ag assays. In hole X86CH274, the Unit 2 dust tuffs

displayed the same fracture and alteration pattern as hole 273. Two

sections of chalcopyrite and tetl-ahedrite occurring in microveins were

located from 229.0 to 236.8 metres (0.50% Cu, 109 g/t Ag), and from

291.0 to 299.1 metres (0.26% CL~, 75 g/t Ag).

The Unit 2 portion of hole X86CH272 is dominantly dust tuff, but

contains some interleveled ash tuff. The tuffs display a medium to

high fracture intensity and moderation to pervasive phyllic

alteration. Only low grade mineralization was intersected. A zone

from 164.0 to 251.0 metres contains sporadic chalcopyrite in

microveins with a few tetrahedrite occurences.

Farther to the south, hole X86CH263 was drilled up-section from a

1970 dri 1 lhnla . U n i t ? dbmt ~ L I Q + B were ~lncnuntlered throt-qheut the

h o l e (except dykes). Down t o 55.1 metres, on l y low f r a c t u r e i n t e n s i t y

and c h l o r i t i c a l t e r a t i o n was obsrrved. Fr-om 55.1 metres t o t h e end of

t h e hole, medium f r a c t u r e i n t e n s i t i e s and weak t o moderate p h y l l i :

a l t e r a t i o n was encountered. A zone from 57.0 t o 119.0 metres con ta ins

sporad ic c h a l c o p y r i t e i n microveins. A few patches of cha l copy r i t e ,

numerous occurences of t e t r a h e d r i t e , and r e l a t i v e l y h i g h amounts o f

s p h a l e r i t e , a l l occur i n microveins f rom 159.0 t o 196.2 metres.

(iii) S u p e r s t i t i o n Zone

Hales X86CH264 and X86CH265 were d r i l l e d t o i n t e r s e c t t h e

n o r t h e r l y t r a c e o f t h e S u p e r s t i t i o n :one s t r u c t u r e . Hole 264 was

c o l l a r e d i n U n i t 3 vo l can i c sandstone and c h e r t pebble conglomerate,

and passed i n t o U n i t 2 dus t t u f f s w i t h minor ash t u f f u n i t s t o t h e end

o f t h e ho le . Hole 265 i n t e r s e c t e d U n i t 2 dust t ~ ~ f f s t h rnugho~ ! t ,

except f o r some ash t u f f unit.5 towards t h e end of t h e ho le . Both

ho les a r e c u t by numerous dykes.

The U n i t 2 p o r t i o n of h o l e 264 from 89.0 t o 130.0 metres,

d i s p l a y s low f r a c t u r e i n t e n s i t y end p r o p y l i t i c a l t e r a t i o n , w i t h a few

Sporadic c h a l c o p y r i t e occurences i n mici 'oveins. From 130.0 metres t o

t h e end of t h e hole, a medium t o h i g h f r -ac tu re i n t e n s i t y was observed,

w i t h weak t o moderate p h y l l i C a l t e r a t i o n . The zone f rom 133.0 ' t o

145.0 metres con ta ins numerous c h a l c o p y r i t e and t e t r a h e d r i t e i n

micruveins, averaging 0.21X CLI and 40 g / t Ag. Hole -265 con ta ins

medium t o h i g h f r a c t u r e i n t e n s i t y and moderate p h y l l i c a l t e r a t i o n

throughout. The zone f rom 48.8 t o 51.3 metres averaged 0.49% C u w i t h

a low fig grade o f 9 g / t . S p h a l e r i t e occur-ences i n mic ruve ins were

found towards t h e end o f bctth ho les ( p a r t i c u ! a r l / 255) w i t h no

associated c h a l c o p y r i t e o r t e t r a h e d r i t e .

H o l e X86CH266 was d r i l l e d down- sec t i on of a 1994 h o l e . U n i t 2 - dust . t u f f s were i n t e r s e c t e d t h r o u g h o u t t h e h o l e . The z o n e f r o m 1Cll.O

t o 203.0 metres d i s p l a y e d m o d e r a t e t o h i g h f r a c t u r e i n t e n s i t y w i t h

some b r e c c i a t i o n , and p e r v a s i v e p h y l l i c a l t e r a t i o n . The b a l a n c e of

t h e h o l e c o n t a i n e d medium f r a c t u r i n g and weal: t o m o d e r a t e p h y l l i c

a l t e r a t i o n . S p o r a d i c c h a l c o p y r i t e w i t h o c c a s i u n a l t e t r a h e d r i t e was

f o u n d i n m i c r o v e i n s f r om 101 .0 t o 203.0 metres. The s e c t i o n f r o m

108.0 t o 203.0 metres a v e r a g e d O.Z;2% Cu, and 37 g!t Ag.

H o l e X86CHZ67 was l o c a t e d i n b e t w e e n two p r e v i o u s l y d r i l l e d h o l e s ,

b u t was p r e m a t u r e l y t e r m i n a t e d a t 108.2 $metres d u e t o d r i l l i n g

pr-oblems. The h o l e s h o u l d h a v e c o n t i n u e d t o a t l e a s t 1513 metres t o

h a v e p r o p e r l y t e s t e d t h e t a r g e t . U n i t 2 d u s t t u f f s w i t h c o n s i d e r a b l e

a s h t u f f i n t e r l e v e l e d were i n t e r s e c t e d . Down t o 4 0 . 2 metres, t h e

f r a c t u r e i n t e n s i t y was low, a n d weak q u a r t z - s e t - i c i t e a l t e r a t i o n was

o b s e r v e d . From 40.2 metres t u t h e end of t h e h o l e , t h e f r a c t u r e

i n t e n s i t y i n c r e a s e d and t h e p h y t . l i c a l t e r a t i o n became p e r v a s i v e . A

few s p o r a d i c c h a l c o p y r i t e o c c u r e w e s i n m i c r o v e i n s were e n c o u n t e r e d .

H o l e X36CH269 was d r i l l e d u p - s e c t i o n ( a l b e i t 30 m t o t h e s o u t h ) ,

and h o l e s X86CHZ68 and X06CH271 were d r i l l e d down- sec t i on of a

p r e v i o u s h o l e . H o l e 268 was abandoned i n a f a u l t z o n e a t 72.9 metres,

and h o l e 271 was d r i l l e d la ter a t a s t e e p e r a n g l e t o t e s t t h e s ame

zone .

Ho le 269 i n t e r s e c t e d U n i t 2 d u s t t u f f s . A medium f r a c t u r e

i n t e n s i t y and m o d e r a t e t o o c c a s i o n a l l y p e r v a s i v e p h y l l i c a l t e r a t i o n

was e n c o u n t e r e d down t o 56.1 metres. Elelow t h i s d e p t h , o n l y low

f r a c t u r i n g and weak t o m o d e r a t e p h y l l i c a l t e r a t i o n were obser -ved . A

few c h a l c o p y r i t e a c c u r e n c e s i n j n i c r o v e i n s were n o t e d n e a r t h e t o p of

the hole. Hole 271 inter-sected U n i t 2 dust t u f f s w i t h some

i n t e r l e v e l e d l a p i l l i t u f f towards t h e end of t h e hole. A low

f r a c t u r e i n t e n s i t y w i t h genera l l y o n l y c h l o r i t i c a l t e r a t i o n was

observed down t o 88.0 metres. From 88.0 t o 162.0 metres, a medium t o

h igh f ractct re i n t e n s i t y and moderate t o pervasive p h y l l i c a l t e r a t i o n

w i t h a few s i l i c i f i e d i n t e r v a l s was encountered. I n t h e balance of

t h e hole, a low f r a c t u r e i n t e n s i t y and prop;,!itic a l t e r a t i o n was

found. Hole 271 was e s s e n t i a l l y devoid of cha lcopyr i t e / t e t r a h e d r i t e

minera l i za t ion .

Hole XabCH270 was d r i l l e d inbetween two prev ious holes. I t was

c o l l a r e d i n U n i t 2 ash t u f f t o 39.0 metres and passed i n t o dust t u f f

t o t h e end o f 'he hole. Down t o 54.0 metres, a low f r a c t u r e

i n t e n s i t y , and p r o p y l i t i c w i t h some weak p h y l l i c a l t e r a t i o n was

observed. I n t h e zone from 54.8 t o 98.0 metres, t h e f r a c t u r e

i n t e n s i t y increased and moderdte p h y l l i c a l t e r a t i o n w i t h a few

i n t e r v a l s o f s i l i f i c a t i o n was encountered. Below 98.0 metres, t h e

f r a c t u r e i n t e n s i t y was low and on l y p r o p y l i t i c a l t e r a t i o n was noted.

Sporadic, bu t some good grade, c h a l c o p y r i t e and t e t r a h e d r i t e

m i n e r a l i z a t i o n was i n te rsec ted i n t h e zone from 54.8 t o 98.0 metres.

The sec:tion from bl.e:l t o 76.0 metres averaged 0.29% Cu and 28 g l t Ay,

and the sec t i on from 82.0 t o 88.0 metres averaged 0.35% Cu and 118 g / t

A9 -

1. Cons t ruc t ion o f D r i l l s i t e s and Access Roads D8 T rac to r , 190 h o ~ l r s @ 117.50

2. Diamond D r i l l i n g 3449.9 metres I2 35.27/m Consumables

3. Sample Assaying 998 samples 12 l5.@O/sampl1?

4. S a l a r i e s R. Pease, 1 clgging and s u p w v i s i on March 20, 21, 24 J u l y 15, 16, 17, 22, 23, 74, 25, 29, 29, 30, 31 August 12, 13, 14, 15, 19, 20, 17, 28 22 days B 185. @0!day

D. Hanson, l ogg ing and supe rv i s i on March 24, 25, 26, 27, 31, A p r i l 1 J u l y 14, 15, 18, 21 C I L I ~ L I ~ ~ 5, 6, 7 , 8 , 11, 18 16 days @ 165.@@/day

ti. Saretsky, s p l i t t i n g and sampl ing March 20, 21, 24, 25, 26, 27, 31, A p r i l 1, 2 J u l y 17, 22, 29, 31 August 5, 7, 11, 12, 13, 22, 25, 26, 27, 29, 29, Sept. 2 25 days O 115.00/day 2 875.00

R. Westendorf, s p l i t t i n g , sampling, and l ogg ing J u l y 16, 25, 30, 31 A ~ ~ g ~ t s t 1, 7, 15, 19, 20, 21, 25, 25, 27, 28, 29 16 days @ 95.00Iday

R. Barnes, s p l i t t i n g and sampl ing J u l y 16, 23, 25, 2R, 30 August 1, 6, 8, 14, 25, 2.1, 27, 28 13 days I@ 95.00/day

M. Nelesk i , s p l i t t i n g and sampling J u l y 17, August 6, 8, 15, 16, 29 6 days 13 lOO.C!O/day

5. Veh ic le Renta l and Fuel 50 days 12 50.00/day

6. Report Prepara t ion

I, Robert B. Pease, do hereby c e r t i f y t h a t :

1. I am a g e o l o g i s t r e s i d i n g a t R. H. # 1, Ke r r Road, Telkwa, B r i t i s h C o l ~ ~ m b i a .

2. I am a 1981 graduate of t h e U n i v e r s i t y o f Waterloo, Waterloo, Onta r io , w i t h an Honours Bachelor of Science degree i n E a r t h Sciences.

3. As a s tuden t , I spent some twenty ( 2 0 ) months employed i n t h e minera l e x p l o r a t i o n f i e l d w i t h severa l m in ing companies i n v a r i o u s r e g i o n s of Canada.

4. I was employed as an e x p l o r a t i o n g e o l o g i s t w i t h Duval I n te r -na t i ona l Corpora t ion i n Vancouver fr-om May 1981 t o January 1902.

5 . Since February of 1982, I h a w been con t i nous l y employed as an e x p l o r a t i o n g e o l o g i s t w i t h E q u i t y S i l v e r Mines L i m i t e d in Houston, B r i t i s h C o l ~ ~ m b i a .

6. I am an Assoc ia te Member of t h e Geo log ica l Assoc ia t i on of Canada, and a Member of t h e Canadian I n s t i t ~ ~ t e of M in ing and Me ta l l u rgy .

7. I p e r s o n a l l y superv ised t h e work programmes as descr ibed i n t h i s r e p o r t .

R e s p e c t f u l l y submit ted,

EOUITY SILVER MINES LIMITED

H. B. Pease, B.Sc. E x p l o r a t i o n Geo lag i s t *

REFERENCES ----------

Cyr, J. H.; Pease, R. B.; and Schroeter, T. G. (1984): Geology and Mineralization at Equity Silver Mine. Journal of Econ. Geol., Vol. 79, pp. 947-968.

Wojdak, P. 3 . and Sinclair, A. J. (1904): Equity Silver Ag-Cu-Au Deposit: Alteration and Fluid Inclusion Studies. Journal of Econ. Geol., Vol. 79, pp. 969-990.

AEPENDLX-L

Diamond Drillhole Logging Code Explanation

Column 1 is a key which indicates the type of data or information on

each line.

I - Identity infarmationldata S - Survey data / - Upper tier geologic data L - Lower tier geologic data R - Free form remarks A - Assay and analysis data

I DATA ------ Each drillhble has two I lines at the start.

The first line indicates:

Col. 17 to 24 - Drillhole Name Col. 26 to 27 - Size of Core Col. 29 to 35 - Day/Month/Year Logged Col. Jb to 3E - Logger's Tniti als Col. 39 to 41 - Helper's I~?it:ials (if any' Cal. 42 to 45 - Drilling Contractor Col. 46 to 50 - Month/Year Hole Drilled Cal. 51 to 57 - Drill Aig Type Col. 63 to 68 - Grid Azimuth (O.0 if True North)

The second line indicates:

Col. 5 to 45 - Company Name Col. 46 to 80 - Zone and type of Geocodel used.

NOTE: 1 Equity uses two type-, of Geocodes, ST and MN. The ST geocode is used when a hole is drilled houth of t.he Wain Zone, and the MN geocode is used to the north of, arrd incl~uding, tlhe Main Zone. This is done to reflect. the differ-ing host rock and style of nrineralizat~c~n'alteratioi~ between the nrirthern and rjouther-n sections of the j r-opel-ty.

E-PBLL!

The SO00 line is the collar survey data. Subsequent S lines

(S001, 5002, etc.) are down-the-hole surveys.

Col. 5 to 10 - From (a decimal point is inferred between column 8 and 9)

Col. 11 to 16 - To ( a decimal point is inferred between column 14 and 15)

Col. 17 to 18 - Units; MT (metres), FT (feet) Col. 20 to 26 - Total Length Col. 27 to 32 - Azim~~th Cnl. 33 to 38 - Dip Col. 51 tn 60 - Northing Col. 51 to 70 - Easting Col. 71 to RO - Elevation

/ AND L DATA ------------ Disregard the /SCL and LSCL lines, they are only for computer

processing. Two lines are available to describe a geologic interval,

the upper line ( / ) and the lower line (L). The /NAB line defines the

mineral fields for the upper line, and the LNAM defines the lower'

line. These mineral fields change according to the type of Gencode

(ST or MN) used.

ST Geocode - upper (/NAM) line Col. 57, 58 MS - Muscovite (sericitel Col. 59, 50 CL - Chlorite Col. 61, 62 PZ - Ouar-te Col. 63, 64 PY - Pyrite Col. 65, 56 CP - Chalcopyrite Col. 67, 68 TT - Tetrahedrite Col. 69, 70 AS - Arser~opyrite Col. 71, 72 PR - Pyrrhotite

- lower (LNAM) l j ne

Col. 57, 58 CB - Carbonate Col. 59, 50 GY - Gypsum Col. 63, 64 MG - Magnetite Col. 65, 66 HE - Hematite Col. 67, 58 SL - Sphalerite Col. 69, 70 GL - Galer~a Cnl. 71, 72 NO - Mnlyhdenum

MN Geocode - upper ( / ) l i n e

Col. 57, 58 QZ - Quar tz Col. 59, 60 S2 - S c o r z a l i t e Col. 61, 62 TO - Tourmal ine Col. 63 t o 72 - Same as ST Gemcode

- lower (L) l i n e

Col. 57, 58 DM - D u m o r t i e r i t e Col. 59, 60 CB - Carbonate Col. 61, 62 CL - C h l o r i t e Col. 63 t o 72 - Same as ST Geocode

Upper ( / ) Geologic Data

Col. 5 t o 10 - From idec imal i n f e r r e d between 8 and 9 ) Col. 11 t o 16 - To (der:imal i n f e r - r ed hetv~een 14 and 15) Col. 17 t o 10 - Hecoi.et-y i n Metres (deciina! i n f e r r e d between

18 and 19) Col. 24 t o 27 - Rock Type Code - See Rock Type Chart Col. 28 t o 29 - T y p i f y i n g M ine ra l 1 - see M ine ra l Char t Col. 30 t o 31 - T y p i f y i n y Minera l 2 - see Minera l Char t Col. 35 t o 36 - Te::ture 1 - see Texture Char-t Col. 37 t o 38 - Tex tu re 2 - see Te::t.ure Char t Col. 47 - E s s e n t i a l l y always a "P" which s tands f o r

F ' r i i x i p l e Geologic I n t e r v a l . If "D", :t stands f o r D i t t o I n t e r v a l which means a l l of t h e above i n t e r v a l d e s c r i p t i o n app l ies , except as noted.

Col. 49 t o 50 - S t r ~ i c t ~ l r e 1 - see S t r u c t u r e Char t Col. 55 t o 56 - Angle t o Core Axis o f S t r u c t u r e 1 Col. 57 - Minera l F i e l d * Node o f Occ~irence - see How Char t Col. 58 - Minera l F i e l d , Amount o f Occirrence - see Amount CIhart Col. 59 t o 72 - Minera l F i e l d s , same p a t t e r n con t inues ( i s .

How, Amount) as i n columns 57, 58.

Lower (L ) Geologic Data

Col. 17 t o 20 - RQD i n Metres (decimal i n f e r r e d between 13 and 19)

Col. 23 t o 29 - Colour Code - see Colour Char t Col. 35 t o 36 - Typ i f y -ng M ine ra l 3 - see Minera l Char t Col. 37 t o 38 - T y p i f y ~ n g Minera l 4 - see Minera l Chi-rt Col. 43 - Count o f F r a c t u r e s a t Steep Angle t o Core

Axis - See Amount Char t Col. 44 - Count of F r a c t u r e s a t Medium Angle t o Core

A x i s - See Amount Chart Col. 45 - Count o f F rac tu res a t Low Angle t o Cor-e f k i s

- See Amount Chart. Col. 46 - Couiik ~ ; f To ta l F rac tu res - See Amo~mt Char-t

NOTE: Columns 43 t o 46 not. always used

Col. 49 t o 50 - S t r u c t u r e 2 - see S t r u c t u r e Chart Col. 55 t o 5h - Angle t o Core Ax i s of S t r u c t u r e 2 Col. 57 t o 72 - Mjneral. F i e l d s , as i n upper ( / ) Data

These a r e f r e e form remarks w r i t t e n by the logge? t o f u r t h e r

descr ibe t h e ge log i c i n t e r v a l . Note t h a t Rock Type Codes (see Rock

Type Char ts) a re o f t e n used.

Th is l a s t t ype o f data l i s t s t h e assay i n fo rma t i on f o r t h e hole.

Note t h a t remarks ar-e a l s o used.

The f i r s t l i n e , A001, de f i nes a " s e t " of assay data. eg. A002

would d e f i n e a d i f f e r e n t set , etc:. The f o l l o w i n g l i n e s descr ibe and

l i s t t h e assay data.

ALAB Col. 17 t o 80 - Def ine Labora to ry ATYP Col. 17 t o 80 - Def ine Type of Determinat ion AMTH Col. 17 t o 80 - Def ine A n a l y t i c a l Method AUMM Col. 17 t o 80 - Def ine Assay F i e l d s A001 Col. 5 t o 10 - From (decimal i n f e r r e d between 8 and 9)

Col. 11 t o 16 - To (decimal i n f e r r e d between 18 and 19) Col. 23 t o 26 - Sample Number Col. 33 t o 38 - Percent Copper Col. 59 t o 44 - Grams/Tonne S i l v e r Col. 45 t o 50 - Gr-ams/Tonne Gold Col. 51 t o 56 - Percent Antimony Col. 57 t.o 52 - F'ercent Arsenic Col. 53 t o 68 - Percent I r o n Col.. h9 t o 74 - Percent Z inc

1. Rock Type Chart

A f ou r d i g i t code i s used t o desc r i be rock types. The f i r s t and

second d i g i t s a r e common t o bo th ST and MN Geocodes. The f i r s t d i g i t

(number! de f i nes s t r a t i g r a p h i c u n i t , and t h e second d i g i t ( l e t t e r )

de f i nes a l i t h o l o g y unique t o t h e s t r a t i g r a p h i c u n i t . I n t h e ST

Geocode, the third d i g i t ( n~ t sbe r ) de f i nes t h e i n t e n s i t y o f f r a c t ~ ~ r i n g

or brecciation, and the fourth digit (number-) defines the type and

intensity of alteration. In the NN Geocode, the third digit (number)

defines the alteration, and the fourth digit (number) defines the

mineralization.

One special code, OVBN, is used for overburden.

1 Clastic Division

Pyroclastic Division

Sedimentry - Division

A Polymictic Conglomerate B Cherty or Silty Conglomerate C Chert Pebble Conglomerate D Quartz Sandstone E Cherty Arqillite F Silty Argillite

Volcanic A H C D E F G H I J I.:

Flow Breccia Ash Flow Dust Tuff Ash Tuff Lapilli Tuff Volcanic Breccia Volcanic Sandstone Volcanic Conglomerate Welded tuff Interbedded Dust and Ash Tuff Lahar Tuff aceous Si 1 tsone Claystone

Chert Pebble Conglomerate Quartz Sandstone Laminated Dust Tuff Volcanic Conglomerate Volcanic Sandstone Dust Tuff Ash Tuff Lapilli Tuff Volcanic Siltstone Interbedded Dust and Ash Tuff Silty Argillite

Volcanic Flow Division A Andesite Flow B Daci te Flow

Quartz Nonzonite A Fresh Quartz Monsonite B A1 tered (Potassic) auartz

Monzoni te

Gabbro-Monzoni t e Complex A B C D E

P r o p e r t y Dykes

T e r t i a r y V o l c a n i c s (Goos ly Lake Fm)

ST - Geocode

T h i r d D ig i t :

F o u r t h D i g i t

Gabbro D i o r i t e Monzoni te Hypabyssal Monzoni te Prophyry Gabbro - Monzoni te T r - a r ~ s l t i o n Phase

Andesi t e T rachyandes i te Ouartz L a t i t e

l r a c h y a n d e s i t e F low Amygdaloidal Andes i te Flow F low B r e c c i a Reddish-Purple F low Massive Andes i te Flow Uuar ts-eye Porphyry ( L a t i t e ) Tu f f aceo~cs Sandstone/Si l ts tone

I n t e n s i t y nf F r a c t i ~ r i n g o r B r e c c i a t i o n

No F r a c t u r i n g Weak F r a c t u r i n y Moderate F r a c t u r i n g Nod t o S t r o n g F r a c t u r i n g S t r o n g F r a c t u r i n g Weak B r e c c i a t i o n Weak t o Mod B r e c c i a t i o n Moderate B r e c c i a t i o n Mod t o Str-ong B r e c c i a t i o n S t r o n g B r e c c i a t i o n

Type and I n t e n s i t y of A l t e r a t i o n

U n a l t e r e d Wsak P r o p y l i t i c (CHL - CLAY) S t rong P r o p y l i t i c Waak P h y l l i c (OTZ - SER.) Moderate P h y l l i c P e r v a s i v e P h y l l i c Advanced A r g i l l i c Weak P o t a s s i c S t rong P o t a s s i c S i l i c i c (OTZ)

MN - Geocode

Third Digit Alteration

Unaltered Propylitic Scorzalite Pearing/Argillic Andalusite Bearing/Argillic Moderate Silicification Strong Silicification Biotite Hornf els I'yrite Porphyroblast Bearing I'hyllic (auartz-Seri,cite) Uuartz - Tourmaline

Fourth Digit Sulphide Mineralization

None Disseminated Pyr-ite +/- Chalcopyrite Pyrite - Magnetite Intergrowths Sulphide Bearing (CP+/-PY+/-SL) Stringers Sulphide Bearing (CP+/-PY) Patches hassivr Sulphide (CP+/ -PV+I-TT+/ -F'D+/- SL) Replacements or Remobilized Grey, "Dusty" Sulphides (fine grained mixture of sulphides and quartz Sulphides in Breccia Matrix (CP+/-PY+/-IT+/-SL)

2. Mineral Chart (ie. Mineral short-forms)

OZ Cluartz CL Chlorite CY Clay CB Carbonate PY Pyrite MS Muscavi te CP Chalcopyrite TT Tetrahedrite AS Arsenopyrite PR Pyrrhotite MG Magnetite HE Hematite SL Sphalerite GL Gal end MO Mnl ybdeni te GY Gypsum EP Epidote FL Feldspar' EI Biotj 1.e

3. Tex tu re Char t t i e . T e x t u r e Short-Forms)

.<. .. .. MX BR P I A l: TC WP VU AD HI:

M i c r o Ve ins Massive B r e c c i a t e d P o r p h y r i t i c Amygdaloidal T r a c h y t i c Wispy vugs A d h e r r i n g / P y r o c l z s t i c C h i l l e d R i n d / P y r o c l a s t i c

4. S t r u c t u r e Char t ( i e . S t r u c t u r e Short-Forms)

C/ Contact BD Bedding V / Ve in F / Fac11 t BN Banding FB Flow Banding CU Upper Contact CL Lower Contact SH Shear

5. How Char t

Symbol

A n # C Xc D E F G H I 3 t: L M N 0 a R S $

T U

Most Daminant Mode o f Occurence

f imygdaloids, c a v i t y f i l l i n g s B l ebs B r e c c i a f i l l i n g s C o a t i n g s & e n c r u s t a t i o n s C l a s t s D i s s e m i n a t i o n s & s c a t . x ' l s Enve lopes Framework c r y s t a l s Gouge Hal a s Eyes, augen I n t e r s t i t i a l Stockwork Laminated/bedded Massive Nodules Spats Patches, a s i n q u i l t s R o s e t t e s & x ' t l s c l u s t e r s Se l vaqes Shee t ing S t a i n i n g s , a s i n t a r n i s h Euhedra l c r y s t a l s

Veins Macroveins Microveins Box wor I:: Massive and/or lsminated/bedding Da lmat ion i te Fresh, pr imary rock Flooding

6. Amount Chart

Code Assigned Value

Range

100 85 t o 99 75 t o i 8 5 55 t o (75 55 t o (65 45 t o <:55 35 t o : 4 5 25 t o (35 15 t o (25 7 t o i 1 5 4 t o < 7 2 t o < 4

.5 t o < 2

.2 t o <.5 .05 t o .:.2 .02 t o i . 0 5 Trace = ,<.02 N i l , Absent Present: Est imate impossib le Poss ib ly Present

7. Colour Chart

The co lour c h a r t can be used i n two ways. A l i g h t n e s s can be

combined w i t h a co lour , o r two co lou rs can be combined.

eg. 3U - Dark Brown

RU - Reddish Brown

Lightness

Symbol Value

9 p a l e s t

Col our

Symbol Col our

R Red

p a l e l i g h t 1 i g h t e r medi u m d a r k e r d a r k v e r y d a r k d a r l c e s t

brown (Umber) Q r a n g e Tan ( k h a k i ) Yellow Lime (Y-G) Green Aqua (8-P) B l u e Violet (B-P) P u r p l e Mauve (P-H) W h i t e Gray B lack ( N o i r )

Diamond Drillhole Geologic Logs

and

Assay Data

NOTE: All Drillholes were logged using ST Geocode

IPRJ SO00 00 SO01 419 so02 1206 /SCL LSCL /NAM LNAM / L R R / L R / L R / L R / L / L / / L R / L / R R / L / R R / L R / L R / L R / L / L / L

E W I T Y SILVER MINES LTD SOUTH OF S.T. - ST GEOCODE 419 MT 157.3 090.0 -45.0 6227.50 7677.82 1281.18

1206 157.3 090.0 -42.0 1573 157.3 090.0 -44.0 MT. 2MT. I

MT.?

OVBN

MSCLDZPYCPTTASPR CBGY MGHESLGLNO

P

CASED TO 15.2 M. NO OXIDE I N FIRST CORE. SUSPECT CASING WELL INTO BEDROCK. ACTUAL. BEDROCK DEPTH LIKELY 2 TO 3 M. 2 0 2C13MS ;. P .:: ) .< ( <: 8 0 0 5T

CORE I S VERY BROKEN. NO OXIDE ZONE. 5 4 2C12CL C c. P <+ < (

0 6 TG CORE STILL VERY HR0E:EN.

3 5 2Cl3MS (i P E ) < ( ( 8 05 5T

CORE ST ILL VERY BROKEN. GOOD TYPICAL 2C13. 2 1 2C34MS ( i: P E ( < ) < + < ( 13 6T ++=I <- 16 2C45MS << P <(<I 0 9 7T +1=2 < (

D F / 5 4 2C34MS <<BR P E ( O < ) 15 6T 12=4 < (

SPOT OF OXIDE AT 35.9 M. 0 9 2C45MS < < P D) D) 00 7T

D F/ RUMBLE FROM 39.8 TO 40.8, VERY LOW RECOVERY, LIKELY FAULT ZONE.

439 11 2C34MS <(BR P E(++D)<. 00 6T

459 D F / RUMBLE FROM 42.0 TO 43.9, VERY LOW RECOVERY, LIKELY FAULT ZONE.

497 5 5 2C23MS C .c P E l < ) < : + 13 5T ++23

MINOR 2D AT 47.6 M. = -? 1 6 2C75MSDZ BFC< P # I # +

13 6T ) I + = NICE STRUTURE, BUT b!HERE'S THE BEEF!

532 27 2C13MS < i. P C X O 19 T A =1+2

CONSIDERABLE DISSEMINATED PYRITE I N THIS INTERVAL. 566 3 2 2C14MS < < P <: #<: )

11 ST =2=3 590 2 2 ZC55MSOZ BH<C P ': (#=#+

0 9 5T +== 1 674 77 2C24MS < : P E l < $ < )

19 6T 1214

CHLORITE GIVES BLUE COLOUR TO <<'S. CORE BUITE BROKEN, BUT UNIFORM.

689 15 2C13 << P O< (<I 13 TG ) 1+2

725 26 2C24MS CCBR P <IV) V+ 00 6T MINOR BRECCIATION. CDRE BUITE BROKEN, POOR RECOVERY.

813 80 2C14MS < < P OW<) 2 1 6T 1 1+3

820 07 2C55MS BR<< P : ) #+#= 0 3 T A BLUE TARNISH ON SOME PYRITE GRAINS.

831 10 2C23 < < P : ) O O 00 5T 1102

856 23 2C13 <<RR P C ) VIV+ 06 AT 11=3 MINOR BRECCIATION.

912 51 2C24MS < < P E)O)B+ 03 AT 12=4 CORE QUITE BROKEN, DISRUPTED. IE. MINOR DISPLACEMENT ON <i'S.

942 29 2C14MS << P E)<)<:) 03 ST 1 1+3

1001 56 2C24MS .< < BR P E) V+B= 11 AT VU 12=4

CORE VERY BROKEN. VERY SIMILIAR TO 85.6 TO 91.2 M. 1073 55 2C14MS < SPOT OF ASH TUFF AT 112.0 M.

1137 1146 09 2C29QZ ( ...: BR P 06 AW +=) 1 MINOR BRECCIATIDN - DISRUPTION.

1146 1161 15 8810 TI: P CLI 13 36 +=)I CL

1161 1198 37 8A10 M < P CU 29 BG +=)I F/

CONTACT BETWEEN DYKES IS FAULTED. 3c-' 1198 1226 27 - ha <<BR P

23 BT 11=3 ~- ~

SLIGHTLY BRECCIATED NEAR LOWER CONTACT. UNIT MAYBE XENOLITH. 1226 1252 24 8Cll VUNX P CU 70 D-

16 YW SMALL XENOLITH OF DUST TUFF AT 125.0 M.

1252 1267 34 BROO MX P F: 66 <: (D. 27 GR

1287 1293 06 8C10 MX P D- 06 AW

CONTACT BETWEEN TWO ABOVE DYKES GRADATIONAL. 1293 1304 11 2CS5MS BR P #=#+

06 5T ) ) ) +

1304 1332 26 2C24MS <<BR P EX<).<+

0 9 5T =1+2 MINOR BRECCIATION.

1332 1344 11 2C13 <<VU P E l i + < + 03 5T +=+ 1

VUGS HAVE COARSE GRAINED PYRITE CRYSTALS (EUHEDRAL). 1344 1354 10 2D13 d: < P < ) < )

0 3 7A 1 ) ) +

1354 1389 3 3 2C14 < G.; P E I O C ) 0 9 5T =1+2

1389 1409 19 2C23 ?:<BR P I ) <+ 03 AT =1+2 < -

MINOR BRECCIATION. 1409 1438 27 2C13 < < P EX< l< )

03 5T 1450 11 2D13 < < P E ( < ) < +

0 3 AT ) + + I 1488 3 4 2C23 < < P E ( < X O

0 3 ST 5 CORE VERY BROKEN. HAKD TO ESTIMATE FRACTURES.

1515 25 2C34MS CiER P V / 10 1(0)<+ 0 6 5T 1214

MINOR BHECCIATION. 1540 23 2C24MS << P EX.:*< )

0 5 4T 1124 MINOR EUHEDRAL PYRITE I N <<'S.

1573 3 2 2C13 .., I % <, P V/ 48 E I < (0

11 AT 11+2 <. PATCH OF ASH TUFF AT 156.3 M., AND AT VERY END OF HOLE, 157.3 M.

EQUITY NINESITE LABORATORY ASSAY WET EXTRACTION A.A. - AU FIRE ASSAYED FIRST

IDEN6B02r)l IPRJ SO00 00 SO01 457 5002 1350 sO(j3 7112 /SCL LSCL /NAM LNAN / 00 R / 46 L R / 79 L R R / 110 L R / 140 L R / 170 L K / 200 L R / 230 L R / 260 L R / 290 L R / 320 L R / 350 L R / 380 L R / 390 R / 410 L R I 440

XBbCH239 NO 24MAR8bDJH GLD MARBbS38 0.0 EOUITY SILVER MINES LTD SOUTH OF S.T. - ST GEOCODE

457 MT 245.7 090.0 -45.0 6224. h5 7591.57 1264.62 1350 245.7 090.0 -44.0 21 12 245.7 090.0 -46.0 2457 245.7 090.0 -44.0

NT.?NT. 1 MT. 2

MSCLQZPYCPTTASPR CBGY NGHESLGLMO

46 OVRN P :TRICONED - NO CORE

79 30 2C24HSCL .<< P 00 GT

:HEAVILY BROKEN UP CORE W / FE OXIDES ON FRACTURES :TO 2C12 LOC. 110 30 2C23CLNS << P E.EI<.+:X

02 TG D1: : TO 2C12 AND 2C24 LOC : MINOR FE OXIDES ON FRACTS. : HEAVILY

BROKEN UP CORE 140 18 2C13CLMS ::.: P <:*<.<*

00 TG :NO FE OXIDES :TO 2C12 AND 2C15 Ill[:.

170 28 2C12CL , , i - P c: 8 .:: . <: * 18 5G <.

: TO 2C25 LOC. W / 5T COLOR 200 28 2C23CLMS (( P c:X<Yt<I

11 TG i % .

: TO 2C25 LOC. W / 55 COl.0R 230 29 2C24CLMS <:< P : <$<.

24 TG : TO 2CZ5 LOC. W / 5T COLOR

260 30 2C34MSCL <i P < a < ) < = 26 GT : TO 2C35 LOC.

290 29 ZC12CL << P < I < . < $ 09 56 : TO 2C23 LOC.

320 28 2C13CLMS ,<< P <. < (

02 TG <. : HEAVILY BROKEN CORE W / MINOR GOUGE : TO 2C12 LOC.

350 28 2Cl3CLNS (< P < ( .:: ( ,: .$ 08 56 <. : TO 2C25 LOC.

380 28 2C12CL .: .: P <.<.<( 05 5G <. : TO 2C13 AND 2C25 LOC.

410 28 2C24CLMS << P ':IC<.<t 04 TG <. : TO 2C25 TOWARDS EOI

390 X D F/ 060 : 1 CM CLGY GOUGE

-, m 440 29 LCL~MSCL i C P <. +':*< $

15 GT <. : TO 2C25 AND ZC23 LOG.

470 28 2C13ClMS <f I) < X < (<+

19 TG : LOCAL CL SPOTS (ZD?)

500 30 2C24CLMS << P < (<.< (

23 TG : TO 2 C 1 3 LOC. : TO 2C25 TOWARDS E O I

530 29 2C1JCLMS <,< P c: (<.<I (

1 6 6G : LOCAL CL SPOTTING

= 7 doL X VU D4V/ 030 V4Vb 560 27 2C25MS c: < P <. V*V+

03 5 T : TO 2 C 1 3 TOWARDS E O I : NUMEROUS T H I N ClZ+PY VE INS

5 9 0 29 2C14CLNS i< P ,<.<:.<* 1 J GT

: 20% 2 C 2 5 620 27 2C25MS .<. % : .. P .:.<((+

03 6 T : TO 2 C 1 3 LOC. : NUt.iEHOUS QZ+PY VEINS :CL I N 2 C 1 3 MICRO VEINS

650 29 2C25MS .:i .. .: . P < (*:+<.

0 7 6 T : TO 2C33 TOWARDS ED1 W / CL I N << t TH. CP

6 3 4 X 6 8 0 30 2CJ:ZCLMS <:.<

2 4 5G 676 X 7 1 0 29 2C33CLMS <I

2 1 TG : TO 2C35 LOC. W / 5 T COLOR

740 28 2C23CLMS <i 19 TG

: TO 2 C 3 5 LOC. W / 5 T COLOR 770 2 9 2C24MSCL < C

2 4 GT 800 29 ZC24MSCL G:.:

23 GT

: TO 2 C 1 2 TOWARDS E O I 530 27 2C25MS , , <.. <

18 b T : TO 2 C i 2 AT SO1

860 29 2C25MS c c 0 7 b T : TO 2 C 2 4 LOC.

557 X 890 28 2C24MSCL C

19 GT 920 28 ZC34MSCL <I

21 GT 950 26 2C24MSCL < :

05 GT : HEAVILY EIROKEN CORE W / CLAY (GOUGE?) AND LOST CORE 94.0-94.9 : TO 2 C 1 5 LOC. W/O CL ON <<

923 X D2V/ 0 3 5 VbV4 980 2 7 2C35MS . ... P ~< .< (

, , ,: ,.

05 6T : TO 2C55 77.0-98.0 N W/ MINOR CY

1010 2 9 2C25MS << P < (< (

05 b T : TO 2C35 LOC.

1040 2 9 2C24MSCL << P C(<.<$ 11 GT

1070 2 9 2C24MSCL <:< P < ( < . < X 09 GT : TO 2C25 AND 2C12 LOC.

1100 2 9 2C13CLMS << P <(.<.<$ 0 3 TG

1130 2 8 2Cl3CLMS << P c: ( < # < ) 1 0 TG

: TO 2C25 TOWARDS EOI 1160 2 9 2C25MS << P <L<+

04 5T : NOTE ABSENCE OF CL.

1190 2 5 2C25MS < < P < (<+ 0 2 5T : HEAVILY BROKEN AND LOST CORE 117.0--117.7 M : QZ+PY ENVELOPES

i 2 2 0 2 8 2C25MS <.' <. % ~ P <: ( < *

00 5T : FAULT ZONE 121-122 M (NO ATTITUDE) CLAY GOUGE

1250 15 2C25MS < ; P < (<:% 0 0 5T : HEAVILY BROKEN CORE W / NUMEROUS ZONES CLAY GOUGE

1280 2 5 2C25MS ~, P .: ( ( # , , .: <

00 5T : HEAVILY BROKEN CORE W / NUMEROUS ZONES OF CLAY GOUGE

1310 2 0 2C25MS .: , .., <> P < ( r t

0 5 5 5 : HEAVILY BROKEN COKE W / LOCAL CLAY GOUGE

1340 2 9 2C25MS CL <i P +(<(<Is 0 4 51 : V. MINOR CL AS FLOUDING :NO CL I N MICROVEINS

1370 2 9 2C25MS ( ( P <: ( <: # 00 5 T : MOD. BROKEN CORE W:O GOUGE

1400 2 8 2C25MS CL << P +(.<; ( < *

0 3 5T :PY ALSO AS SPOTS TO 0.5 MM : LOOKS L I K E 2D LOC. : TR CL LOC.

1430 29 2C25MS /( . ~ P .:(<:$ <. 0 4 5T : TR. SHINEY GREY SDE. MINERAL W / QZ (T I -? )

1460 1 9 2C25MS .' , i ... P < ( < (

0 5T : HEAVILY BROKEN CORE

1490 1 3 2C25MS CL << P +.< (': ( OCI 5T : LOST AND BROKEN CORE W / CLAY GOLIGE 146.0-147.8 M (0.2 M CORE) : MINOR LOCAL CL ALT'N

1520 28 2C25MS , .. , c.. P .< ( ': ( tji;) 5T : LOC'LL'I PY SPOTTED : HEAVILY BROt<EI\I CORE W/O GOUGE

1550 26 2C25MS < .; P -< ( <: (

04 5T

: HEAVILY BROKEN CORE : LOC. PY SPOTTING 1550 1580 2 9 2C25MS < < P <)<:+

0 0 5T : TO 2C35 LOC. : HEAVILY BROKEN CORE : MINOR TECTONIC BXIA W /

CLAY GOUGE 1 5 8 0 1 6 1 0 2 7 2C25MS .: i P

0 0 5T : LIGHT GREY OZ. RICH ENVELOPES

1585 1585 X D3V/ 0 6 2 1610 1640 2 9 2C25MS ,, ./ , '.. P

0 4 5T : S T I L L NO CL ON MICROVETNS

1640 1670 2 5 2C25NS <: .% P

CtO 5 T : HEAVILY BROKEN CORE IJ/ PATCHES GOUGE

1728 1767 3 4 2C45NS QZ C: P 2 5 4T : NOTE STRANGE COLOR- UNLIKE TYPICAL 2C : TO 2D45 LOC. : TR.

TO? W / SDES. :LIGHT GREY QZ RICH ENVELOPES 1750 X D F/ 0 5 0 178h 1 6 8A02CL PY P CIJ 045

08 5G : 20% FLAG PHENOS TO 1 0 MM : LOWER CNT. NOT OBSERVED

1798 1 1 BA06CY P 00 7T : TOTALLY ALTERED TO CLAY : 8A? : CNTS NOT OBSERVED

1820 2 1 2C45MS QZ (CRR P : <. ( )

16 4T : TO 2C55 AT SO1 : UT COLOR LOCALLY : TR TO? I N SDE PATCHES :LIGHT GREY QZ RICH ENVELOPES

1844 2 4 2C45MS QZ C < P c: . <: . e: )

2 0 4T : TO 2C35 LOC. : UT COLOR LOC. : TO 2D LOC. : NOTE SAME

STRANGE COLOF: AS ABOVE : LIGHT GREY QZ RICH ENVELOPES 1919 7 3 8CU3MS P 1 P CU 06(1

r LJ 1 7 c : 10% PLAG PHEWOS TO 3 MN : 7 6 COLOR LOC. : LOWER CNT. NOT

OBSERVED DUE TO BROKEN CORE 1950 2 9 2C25NS PZ <:< P .< . +: +.: +

0 6 4T : TO 5T COLOR TOWARDS EOI : NOTE TR CL

1980 2 9 2C25MS i : P i : : 0 4 5 <*<+ 02 5T

2010 2 8 2C25MS < < P i<: 0 6 0 <$<+

0 3 5T 2 0 4 0 2Y 2C15MS / . c .. P B D 0 6 0 < L < (

0 2 5T : 10% INTERLEVED 1D : LIGHT GREY QZ RICH ENVELOPES

2064 23 2C25MS ({ P <*$:+

0 0 ST : MINOR I D INTERLEVSD

2079 14 BA02CL A L P CU 070 A( 1 4 46 A ( : LOWER CNT. NOT EXPOSED

2110 30 2C25MS i % ., ,~ P < X c.: + 0 3 5T : LIGHT GREY az RICH ENVELOPES

2140 3 0 2C35MS < .:: P < t C = 0 5 5T : TO 2C25 LOC. : LIGHT GREY QZ RICH ENVELOPES

2170 28 2C35MS <,:BR P <x<= 0 7 5T : 2C85 LAST 0.2 M OF INT.

2166 X D F / : CLAY GOUGE - NO ATTITUDE

2179 0 9 8 ~ 0 2 ~ ~ A I P CU 065 0 7 46 CL 055A= : GOOD CHILLED INTRUSIVE CNTS.

2184 0 4 2C85MS BR P #=#= 0 2 5T

2246 t l BAO2CL A$P$ P CU 039 5 7 46 CL 051 D. : TO 8A06 W / BG COLOR AT SO1 AND EOI

2270 2 2 2C35MS <<RR P <)<= 0 5 5T : 2C85 (TECTONIC BXIA) AT SO1

2300 28 2C25MS 0 4 ST : TR DARK GREY

2330 28 2C25MS 02 5T : 2D? (PHYLLIC

ORIGINAL 2330 2360 29 ZC15MS

0 0 5T : TR DARK GREY

2360 2390 28 ZCISMS 00 5T : TR DARK GREY

2390 2420 28 2D25MS 05 ST : TO ?C LOC. :

24215 2457 3 2 ZD15MS 00 5T : TO 2C LOC. END OF HOLE.

ALT'H MAY MAKE I T DIFFICULT TO DETERMINE TEXTURE! ! )

< C P < (<)

SDE? AS ABOVE 227-230 M : TO 2 0 LOC. :, , ~ \ P < ( < )

<. SDE? AS AROVE : 2D?

< <; P C : 060 <I<+

TO =Dl5 LOC. < .: P < < 047 < ( < )

ALAB EDUITY MINESITE LABORATORY ATYP ASSAY AMTH WET EXTRACTION A.A. - AU FIRE ASSAYED FIRST AUMH RCDVSAMPLE ROD % CU G/TAG G/TALJ % SB % AS % FE % ZN AClOl 46 7 9 5331 0.036 1.0 0.010 0.005 0.005 4.370 0.005 A001 7 9 110 5332 0.022 1.0 0.Ob0 0.005 0.005 3.430 0.005 A001 11'2 140 5333 0.023 2.00.0700.005JO.0053.9100.0~s

170 200 230 260

320 1.50 380 410 440 470 5oo 530 560 5 5 1:) 620 65O 504 7 10 740 17il ROO 83lj 8612 89U 920 950 9811

1 0 1 0 11140 1 C17I:l 1 101:l 1130 l i b 0 1 l5lS

1220 1250 1280 1310 1340 1370 1400

1460 1490 1520 1550 1580 16 1 0 1640

1700 171.0 1757 1820

290

14.Xl

1670

6

1844 5389 1950 5390 1980 539 1 20 1 1:) 5392 2040 C 7 ( -

.Jd ?A

2064 5394 2110 5395 2140 5396 2170 c7 .,.>97 2184 5398 2270 c-7 d i99 - 7 . L...~~Q 5400 2331:1 5401 2360 c J ~ J L ,. e,

2390 5403 2420 5404 2457 5405

END OF ASSAYS -

/SCL LSCL /NAM LNAM / R / L R R / L R / L R R / L R

L R / L R R / L R / L R R I

L R R / L R R / L R / L R / L

EQUITY SILVER MINES LTD SOUTH OF S.T. - ST GEOCODE 457 MT 148 .1 @90.0 -45.0 5029.20 7648.38 1258.98

1198 140.1 090.0 -44.0 1481 148. 1 090. 0 -45. CI MT. 2MT. 1

MT.2 MSCLPZPYCPTTASPR CBGY MGHESLGLMO

280 OVEN P : TRICONED AND CASED - NO CORE

3 0 2 1 1 2C25MS .... t P .:: # .:.: ) ... ,

1313 5T : HEAVILY BROKEN CORE : NO FE OXIDES : CLAY GOUGE? ZONES : NO CL ON MICROVEINS -,.. 2 2 1 2C35MS <.. ~ :, ... F .:[ $ r: ) 0 0 5T : HEAVILY BROKEN UP CORE W/O CLAY ZONES : TO 2C55 LOC.

3613 2 0 2C55MS .<<[[R P < ) <.: = <;

0 2 5T : MOD.-STRONGLY BR0KE:N UP CORE W/O GOUGE : TO 2C45 LOC. : NOTE TR. GREY SDE. (TT?)

370 2 2 2C45MS i .. .:, ., P : # : ) .[ . 01:) 5T : MOD. BROtKEN UP CORE W!O GOUGE : TR GREY SDE (TT?)

418 2 1 2C45MS ... L P .:: y .:: ) ., ,

00 5T : MOD. BROKEN UP CORE h1/0 GOUGE

445 0 5 2C25MS ... ... '. . ... P .<%<)

0 0 ST : HEAVILY BROKEN AND LOST CORE W/O GOUGE : 1 QZ+PY VEIN > 50 MM

- NO ATTITUDE POSSIBLE 456 1 0 2C45MS ( .. <.' ~ P .:, % .:: =

0 0 5T : MOD. BROKEN UP CORE W/O GOUGE : LOST CORE

485 11 2C45MS ;'BR P .:t.[= .:. I:IO 5T : MOD. BROKEN CORE W/O GOUGE : LOST CORE : TO 2C55 LOC. : TR

GREY SDE? (TT?) 5 0 5 0 5 2C45MS .: < BF: P .:#<= .:.

0 0 5T : MOD. BROKEN UP CORE W/O GOLIGE : LOST CORE : TO 2C55 LOC. :TR

GREY SDE? AS ABOVE 5 5 0 17 2C45MS . < BR P .: L .; = <: .

0 2 5T : MOD. BROKEN UP CORE W/O CLAY GOUGE : LOST CORE : TO 2C55 LOC. : TR GREY SDE? (TT'?)

5 6 0 2 5 2C45MS (.. .. ?: .. P ': #.:= x::.

0 4 5T : MOD. BROKEN UP CORE - W/O GOUGE : TO 2C55 LOC. : TR TT?

5 9 0 2 9 2C45MS : < P <t.<= <:. 0 4 5T : LESS BROKEN UP THAI ABOVE INTS. : TO 2C85 LOC. : TR TT?

5 2 0 2 9 2C35MS ( ( P <8.:= <. 02 ST

: TR TT? 6 5 0 2 4 2C35MS <: <: P .;xi) <.

0 4 5T : TR TT?

6 4 2 X D F / : CLAY GOUGE (FAULT?) - NO ATTITUDE POSSIBLE

6 8 0 1 8 2C35MS << P I I .0 C. (12 5T : HEAVILY BROKEN UP CORE : LOST CORE 56.2-68.0 M : TR TT?

7 0 1 1 7 2C45MS .:: i P :I<) .<. 0 0 5T

: HEAVILY BROKEN CORE W/O GOUGE : LOST CORE : TR. TT? 735 17 2C45MS 6 - ./ .% P i t 0

0 2 5T : HEAVILY BROKEN UP CORE W / MINOR CLAY GOUGE : LOST CORE : TO

2C55 LOC. 7 . 2C45MS , .. < , P ,eO 2 4 ~ ... :.).;= <.

1 4 5T : TR TT?

P 7 9 0 2 8 2C35MS <': i : )C= C . 0 9 5T : HEAVILY BROKEN UP LOCALLY : TR TT?

8 2 3 2 4 2C45MS .< C BH P < j < = <. 0 2 5T : HEAVILY BKOKEN UP LOCALLY W / SOME GOUGE : TO 2C55 LOC.: TR

TT? 8 9 2 6 1 8AOlCL PI: P

4 5 4 6 D. : CNTS OBCJCURREL) I N WOKEN CORE : 5% ALTERED, UNALIGNED FLAG

PHENOS TO 10Y2 MM : POST-MIN DYKE 9 1 7 20 2C45MS <:(BF( P .:%.:::) .:,

0 0 5 1 : TR TT? : 8A 91.1-91.4 N W / MG

9 5 0 3 2 8AO2CL hxl F CLJ 0 5 2 0) 2 8 4G CL i:IDSAl : 5% AMYGDS. W! CB+CJZ I N F I L L I N G

, , P 9 7 2 1 6 2C45MS . e.. ' X C ) .:.! . 05 ~r : TR TT? : HEAVILY BROKEN UP CORE EXCEPT FOR DYKE 95.4-95.9 M

9 9 7 1 2 2C25MS .:: ' P <*o <:. 00 5T : V. MINOR 2D INTERLEVED : TR. TT? : HEAVILY EROKEN UP CORE

1027 2 5 2C25MS .< .< P < ( < X <. 00 5T : MOD.-STRONGLY BROKEN UP CORE : TR TT?

1061 2 6 2C15MS : , c.. .:.. P <:: ( ~: $ .< ,

00 5T : TR TT?

1090 2 7 2C25MS C < P < X < ) /:. 0 2 5T : HEAVILY BROKEN UP CORE : TR. TT?

1120 2 7 2C25MS C C P <I<) <. 011 ST : HEAVILY BROKEN UP CORE LOCALLY : TR. TT?

1150 27 2C25MS . .. i % P <:;go <,a

03 5T <. : HEAVILY BROKEN UP CORE TO 114.0 M : TR. TT?

1123 X D4V/ 025 V5V5 1180 28 2Cl3CLMS < < P <.<: (<:)

07 TG <: ( <. : TO 2C15 LOC.

1210 25 X15MS .< < P <.! ( < *

02 5T ... . : TO 2C13 TOWARES El11

1231 20 2C13CLMS << P <.<(<:l: 00 TG : MOD. BROKEN UP CORE : TO 2Ci5 LOC.

1243 11 8A02CL AL P FB 050 A ( 1 0 6G CL 080A ( : POST-MIN DYKE : UPPER CNT. 1HREG.-NU ATTITUDE

1254 11 2 ~ 2 3 ~ ~ i <. P c: (.< ( < # , ,

1 9G <. : TO 2C25 I? ED1

1274 12 2C25MS ( i P i . < ( < X 00 5T

1302 25 2C25MS < < P < ( < ) <. 02 5T < ( : TR. TT?

1332 29 1D20DZ < <: P ((0 <. 13 AW < ( : TR. TT'? : MINOR 2C INTERLEVED AT SO1 & EOI

1360 27 2D25MSCL <:< P << 045 r (<: ( < +

22 5T : TO 2D23 % 2C LOC.

1390 29 2C23CLMS C < P 4 ( < ( C + 14 TG : TO 2C25 % 2D L.OC.

1420 30 2C24CLPIS <.: P < ( < ( < )

12 TG C . 1450 29 ZC13CLMS <l ACKI 1 A001 A001

EOUITY MINESITE LABORATORY ASSAY WET EXTRACTION A.A. - AU FIRE ASSAYED FIRST RCOVSAMPLE RcID % CU G/TAG G/TAlJ % SH % AS % FE % ZN

302 5406 0.005 0.5i1.2~101:1.005U.0052.bbOC1.!:105 332 5407 0.005 0.5 0.010 6.010 0.005 2.590 0.005 360 5408 0. 1:11!:1 0 . 5 0. 100 0. 010 0 . c105 3. 990 0. crc15 390 5409 0.635 2.0 0.030 0.010 0.005 6.140 0.010 418 54 10 0. #.:105 0. 1 0. 0515 0. 005 (:I. 005 5. 500 0. O 1 I:] 445 541 1 o.005 13.1 CI.IOIO 0.005 0.005 4.600 0.1:111:1 466 5412 0.005 0.1 0.010 1:1.01:15 I:I.I:I~I~ 4.4200.011:l 506 5413 0.001 0.1 0.020 0.005 0.005 5.640 0.010 c- - .L:,I.I 54 1.5 0.001 0.1 ~ . ( I ~ ~ ~ . ~ : I o ~ o . ( I ~ I ~ ~ . ~ ~ ( I o . ~ o ~

R END OF ASSAYS

0.005 0.1 0.0200.005 0.005 3.8300.060 0.005 0.1 0.010 0.005 0.00510.040 0.005 0.005 0.1 0.020 0.005 0.005 5.5800.005 0.001 0.1 0.030 0.005 0.005 2.840 0.005 0.001 0. 1 0.090 0.005 0.005 3.690 0.005 0.001 0.1 0.040 0.005 0.005 1.770 0.005 (1.005 2.0 0.030 o.010 n.cm 5.140 cr.005 0.005 1.0 0.040 0.010 0.005 8.560 0.005 0.005 (I. 1 0.030 0. (105 0.005 7. 980 0. 005 0.005 0.1 0 . 0 ~ 0 0.005 0.005 2. 9.50 0.005 0.005 1.0 0.0400.~:11~0,l:1055.i1700.005 0.005 0.1 0.020 0.010 0.005 2.2B0 0.005 0.005 0. 1 0.020 0.010 0.005 4. 1CIO 0.005 0.005 1.0 0.020 0.005 0.005 4.240 0.005 C1.0(15 1.0 0.010 0.005 O.005 5.420 0.005 0.005 0.1 0.030 0.005 0.005 5.430 0.005 0.0(15 1.0 0.050 0.01U 3.001 5.080 0.005 0 . ~ 1 0 0.5 0.050 0.0112 0.001 5.430 0.005 0.03Ij 0.5 0.05Cl0.005 0.OIl5 4.1700.005 0.605 3.1>0.oB00.0U50.l>054.240Cl.Olj5 0.605 1.o 0.060 O . C I ~ ~ I O . C I ~ C I 4.090 0.0i15 0.040 4.0 0.090 0.010 0.005 5.680 0.020 0.005 18.0 0. 1251 0.005 O.l:r<rl 3.280 l : l . l j l C I

0.<!05 3.0 0. 100 0.010 0.005 5.890 0.005 0.005 2.0 i:1.050 0.005 0.005 4.11:Iij 0.005 8:j.i)o; 1.0 0.050 0.005 0.005 4.060 0.005 0. 005 2. 0 0. 070 0. 005 (11. (105 3. 540 il. 0.005 5.00.050 0.0lOd.005 5.320 O.005 I . 010 1.0 0. 060 0.005 CI.OO5 5. 220 0.005

END OF LOG

IDEN6B0201 XBbCH260 NO JULBbDJH G&D JUL86S38 0.0 EQUITY SILVER NINES LTD SOUTH OF S. T A I L - ST GEOCODE I P R J

soim 5001 /SCL LSCL /NAN LNAM / R / L R / L R / L R , L R / L / L R / L R / L / L R / L R / L R / L / L / L R / L R / L R /

1161 116.1 090.0 -43.C. MT.2MT. 1

WT.2 MSCL!3ZPYCPTTASPR CBGY NGHESLGLMO

152 OVBN P :TRICONED - NO CORE

2 1 2 3 4 2C25MSOZ << P i (<I+.:. 0 0 5T

:LIMONITE ON FRACTURES FROM 20.1 - 2 1 . 2 225 12 8A02CLCB A f P A)

0 6 4 6 A ( :1-2% AMYGDS :CNTS NOT OBSERVED (GOUGE I3 UPPER CNT)

2 5 0 2 5 2C24MSCL <<: P < I <:+ 0 0 GT

:10% 2D INTERLEVED :LIMONITE ON FRACTS 2 8 0 2 8 2D24MSCL i< P <.<:(<)

0 0 GT :LIMONITE ON FRACTS

3 1 0 2 9 2D23CLMS <:( P <.<(<:)':.

0 0 TG 3 4 0 2 6 2D23CLNS <:< P i ( < ( O

00 TG :10% 2C INTERLEVED

3 7 0 2 7 2D23CLNS %<%< P . < ( < ) < (

0 0 TG :10% 1 4 INTERLEVED (;OX CHERT CLASTS)

1 8 TG :"25% 2D INTERLEVED

4 4 6 15 2C24MSCL << 0 9 GT

:LOWER CNT V SHARP 4 6 2 1 5 l ~ 1 0 a ~ <<

12 5 A :LOWER CNT V SHARP

4 9 0 2 7 2C24MSCL << 13 GT

5 2 0 2 9 2C23CLM5 << 2 4 TG

5 5 9 2 9 ZC23CLM5 << 2 0 TG

:TO STRONG << TEXT LOC 5 8 0 2 7 2C23CLMS C <

20 TG :TO STRONG << TEXT LOC

6 0 9 29 2C23CLMS << 1 1 TG

:TO 2C15 LOC 6 1 4 0 5 8A20CLCB A X

0 4 4 6 CL 060 :LOWER CNT IRREGULAR

637 22 2C22CL < < P < ) < . < (

10 b G 673 36 8A20CLCB P I P

31 1 4 6 CL 070 D) :UPPER CNT IRREG W / MINOR 8 x 1 4 :LOWER CNT WEAKLY IRREGULAR

<< P < : ) < . < ( 700 26 2C22CL 18 56

:TO 2 C 2 5 LOC : 7 3 0 30 2C22CL

19 5G :TO ZC25 LOC : HANDING

760 30 2C22CL 1 6 5G

: l o % 10 INTERLEVED :V IRREGULAR GREEN/TAN COLOR

:AS ABOVE W / 2C25 LOC AND TAN/GREEN COLOR BANDING 790 2 7 2C22CL <( P HD 071 < ) < ( < (

20 5G <: . : 5 % 1D INTERBEDDED

820 29 2C22CL << P < ) < X < ( 1 9 5G <.

8 4 6 26 2C22CL < < P C ) < l i : X 07 56 <.

:LOWER CNT F A I R L Y SHARP BUT IRREGULAR (NO ATTITUDE 857 10 1D12CL < .< P <.<.

03 AG :TUFFACEOUS MATRIX? :V WEAK << TEXT : 3 0 % 1C ( E O I )

880 23 2C21CL < < P < ) < ( < (

18 G A < ( 910 28 2C23CLMS <i P < ) < ( C (

19 TG :10% 2D INTERLEVED

9 4 0 30 2 C 1 0 < C: P <:(<: ( < (

2 1 4M :PROPYL IT IC ALT 'N CNV ON << :TO 2 C 2 2 I3 START OF I N T

970 29 2 C l 0 c: < P < ( < ( < (

1 4 4M :TO 2 C 2 2 LOC

1000 29 2C22CL < c: P < I < ( < $ 23 AG

:LOCAL IRREGULAR GREEWEIUFF COLOR BANDING 1030 28 2C22CL < < P < ) < ( < $

19 AG :PY ALSO I N PATCHES

1060 30 2C21CL < S: P < I < ( < ( 21 GM

1 0 8 4 2 4 2C21CL << F <)<:<.

0 7 6M <. 1096 12 8A02CLCB A l P

0 8 AG :CNTS NOT OBSERVED

1125 27 2C22CL << P 1 4 5 G

iMINOR EXIA B 112.5 M

L R R R A00 1 ALAB ATYP AMTH AUMM R 00 A001 152 A001 186 R AD01 225 A001 250 A001 280 A001 310 A L l O l 340 A001 370 AOCl l 400 A001 430 A001 460 A001 490 A001 520 A1001 550 A M 1 580 A001 610 R ACIOl 673 A001 700 AljOl 730 A001 76il A001 790 A001 820 AClCll 850 A001 880 A001 910 A001 940 AClOl 970 A001 10430 A O i l l 1030 A001 106lI R 1084 A001 1096 R 1125 A O O ~ 1132 F4 R

0 2 5G <. :MINOR BXIA @ 113.2 M : l D 115.8 - 116.1 :EOH @ 116.1 M END OF HOLE.

EPUITY NINESITE LABORATORY ASSAY WET EXTRACTION A.A. - AU FIRE ASShYED FIRST RCOVSAMPLE RQD % CU G/TAG G/TAU % SH % AS % FE % ZN

152 :OVHN - NO CORE (TRICONED) 186 6782 0.100 212 6783 0.11

:DYKE - NO SAMPLE 250 6784 0.19 280 6785 0.08 310 6786 0.22 340 6787 0.07 370 6788 il. 17 400 6789 0.08 430 6790 0.03 460 6791 0.09 490 6792 0.19 520 6793 0 . C15 550 6794 0.03 580 6795 0.04 610 6796 0 . i12 637 6797 0.02

:DYKE - NO SAHPLE 701) 6778 0.005 730 6799 [I. 1j2 760 6800 0. ir2 790 680 1 0.02 820 6802 0. o:! 850 6803 0. 1005 880 6804 0. !:W5 910 6B05 0. 10:; 940 6806 0 . 005 970 6807 0. 005

1000 68i18 0 . 005 1030 6809 0. 005 l ~ t b i j 6810 0. C105 1084 681 1 0.005 1096 :DYKE - NU SAHPLE 1125 6812 0. 005 1132 :DYKE - NO SAMPLE 1161 6813 0. r : l i l l

:EOH P 116.1 M END OF ASSAYS - END OF LOG

IDENbB02lI l X86CH261 NQ JUL86RBP GbD JUL8bS38 0.0 IPRJ SClO0 SO01 /SCL LSCL /NAM LNAM / R / L R

L R / L H / L R / L R / L / L R R / L R / L R / L R / L R / L R / L R / L / L / L

EQUITY SILVER MINES LTD SOUTH OF S. T A I L - ST GEOCODE

WT. 2MT. 1 MT. 2

MSCLQZPYCPTTASPR CBGY MGHESLGLMO

183 OWN P CASING TO 18.3 , HOLE I S LIKELY WELL INTO BEDROCK.

2 1 0 2 0 2C14QZMS <i P .< + <: ) 0 0 6T

CORE I S VERY BROKEN. 240 2 6 2C24QZMS << P <+ <+

00 6T CORE VERY BROKEN. WEATHERING (FE-STAIN) ON FRACTURES TO 22.9.

2 7 2C54PZMS <<BR P .::+< ) # + 0 2 6T

BR'X MOST INTENSE FROM 24.0 TO 25.0. BH'X TYPICAL OF 2C.. 2 0 2C24QZMS << P V/ 5 0 < + i f < + CIO 6T

POSSIBLE SS ON FRACTUKE. 2 9 2C13QZMS <.< P < <:+ 0 0 GT

PYRITE OCCURS I N SMALL WISPS AS WELL. CORE S T I L L VERY BROKEN. 2 2 2C330ZMS <<Hi? P I)<)<+ <)(:I 7T 1 1 2C24QZMS << P <1 0 0 0 6T

VERY BROKEN CORE, VERY POOH RECOVERY. NO CLAY GOUGE, I SEE NO REASON FOR BROKEN AND POOH RECOVERY.

21) 2C33QZMS (CVU P < )

0 0 6T VERY BROKEN POOR RECOVERY.

3 0 2C1': ;< P o.:$'$ 00 b T

CORE S T I L L VERY BROKEN. 2 8 ZC23QZMS I < B R P <)<I<+ 05 6T VU

CORE GETTING MORE SOLID. MINOR BRECCIATION. 2 9 2C14QZMS << P < ) < X O 05 6T

MINOR DISPLACEMENT OF SOME <<. 2 0 2C13QZMS << P <+<)<) #- 0 3 5T

LOST CORE FROM 5 5 . 9 TO 56.7. SMALL BR'X AT 55.0 WITH TT/PY/QZ. 2 6 2C13 < < P < ) . I S < ) i l c l AT

PATCH OF 2D AT 58.0 2 9 2C13 < < P <+ < X 0 3 b T 2 9 2C13 .: < P < + < I < $ 11 GT 29 2C13 << P <:+ < X 03 GT < (

TYPICAL 2C13. 720 29 2C14 < < P < I < Y

08 AT 754 33 2Ci3 <<IF P < < (

09 GT 763 09 COO PL P FB 40 D.

05 8A FAULT GOUGE ON UPPER CONTACT, LOWER CONTACT NOT PRESERVED.

788 24 2C54MSQZ BR<< P I ) O Q - 08 AT 0 .

ZONE WEAKLY BX'D. 802 13 8AOO NS P I =

09 2A 830 27 2C14 < < P *:)<+<)<:.

09 AT PATCH OF 1C AT 80.4

860 29 2C13 < < P OO<+ 09 7A

PATCH OF 1C AT 85.2. 895 34 2C23 <<BR P <)<+<)

06 70 CONTAIINS OCCASIONAL CLASTS OF Q Z PEBBLES.

917 21 l C l i i< P C U 55 < < $

07 AW D. LOWER CONTACT GRADATIONAL INTO 2C.

950 32 2C13 << P V / 35 O<+O 11 AT

PATCH OF 1C AT 93.2. OCCASIONAL QZ CLASTS 980 29 2C13 < < P Vf 45 <)V+V+

1 i 5A PATCH OF 1C AT 95.8 AND 98.0.

1010 29 2C23 .:<3R P (+<) <+ 09 54

CLASTS OF CITZ I N 2C. SLIGHTLY BX'D. 1040 28 2 ~ 2 2 <<BH P <+ <+B(

00 5A PATCH OF 1C AT 102.7.

1070 28 2C22 < < P <= <XB( 0 0 bA

CORE VERY BROKEN. SOME CP I N << AS WELL. 1100 29 2C22CL .: < P < l<)<+B.

0 6 GT 1123 22 2C22CL <.< P <l<L<+B.

03 GT 1140 17 2El2 << P C U 85 < $ D+

07 2A 1160 20 2C29 << P <(<I<+<:)<-

06 5A < ( CP BLEBS AS WELL, GOOD INTERVAL.

1190 29 2C19 < < P <1BtV+B( 09 5A

OCCASIONAL LAPILLI. 1209 19 2E12 < < P V) V)

05 AG SOME LAPILLI SILICIFIED.

1209 1240 30 2C12 <i P 17 AG

ROCK CONTAINS OCCASIONAL LAPILLI. 1240 1263 21: 2C22 < < P BN

05 AG 1247 1248 X D

A001 ALAH ATYP AMTH AUMM 0001 183 A001 210 AOCll 240 13001 270 &Oil1 1.00 A001 330 A001 360 A O O l 390 A O O l 440 A001 480 A001 510 A001 540 A001 570 A001 600 ALIOl 630 A001 660 A001 690 A001 720 A001 750 A001 802 A001 829 A001 860 AClCll 8911 A001 920 AClOl 950 A001 980 AEm1 101CI

05 AG SOME LAPILLI, DISRUPTION, BX'D. SMALL 8< 131.0 TO 131.1.

1350 29 2C22 .: < PBN 55 <+B1< 06 G A

OCCASIONAL LAPILLI. 1381 30 2C29 << P <+B(B)<.

11 G A STILL CONTAINS OCCASIONAL LAPILLI.

1388 07 8A00 MS PCU 75 <- 07 1 A CL 40 D )

1393 05 2C22 -( < P <+ 8) 02 GA

END OF HOLE.

EQUITY MINESITE LABORATORY ASSAY WET EXTRACTION A.A. - AU FIRE ASSAYED FIRST HCOVSAMPLE RQD % CU G/TAG G/TAU % SB % AS % FE

210 604 1 0.001 0.5 0.005 0.005 0.001 2.60 240 6842 0.001 0.5 0.005 0.005 0.001 5.14 270 6843 0.001 0.5 0.07 0.005 0.001 5.09 300 6844 0.001 0.5 0.005 0.005 0.001 4.76 330 6845 il.Cl05 0.5 0.03 0.005 0.0~11 2.51 3611 6846 0.02 0.5 0.31 0.005 0.04 5.13 390 6847 0.001 0.5 0.03 0.005O.OCIl 1.64 440 6848 0.001 0.1 0.01 0.001 0.001 0.72 480 6849 <).Oil1 0.5 0.03 0.01:15 O.CICII 2.21 510 6850 0.001 0.5 o.i)? 0.065 0.001 5.19 540 6851 il.001 0.50.06 0.0050.03 3.24 570 6852 0.001 0.5 0.08 0.005 0.01: 2.31 6r:10 6853 0.001 0.5 0.04 0.005 0.001 3.11 630 6854 0.005 0.5 0.03 0.005 0.001 3.44 66CI 6855 0.Cl05 0. 5 O.CI3 0.005 0. 001 5.27 690 6856 0.02 0.5 0.05 0.005 0.001 5.00 720 6857 il.005 0.50.03 1:1.0050.001 4.26 750 6858 o . 0 ~ 5 0.50.03 0.00;o.ooi 4.60 788 6859 0.040 0.5 0.05 0.005 O . C l i l l 2.95 8J1j 6860 0.050 Z.O 0.22 0.020 0.050 5.45 860 6861 0.0:!0 0.5 0.13 0.005(1.(14i13.71: 890 6862 0.020 0.50.05 0.0200.0053.0Y 920 6863 0.030 3.00.12 1:1.<1200.05r:12.46 950 6864 0.005 0.5 0.12 0.020 0.050 4.55 980 6865 0.001 0.1 0.03 0.005 il.CK11 3.60

lOI0 6Rbb 0.020 0.1 0.03 0.005 0.001 3.03 1040 6867 O.OEl0 0.1 0.1.73 0.Crg5 0.0(:11 2.55

1070 6868 1100 6869 1130 6870 1160 6871 115'0 6872 1220 6873 1240 6874 1263 6875 1320 6876 130 6877 1370 6878 1393 6877

END OF ASSAYS -

0.130 2.0 0.03 0.070 3.0 0.04 0.005 3.0 0.06 0.380 28.0 0.05 0.080 4.00.05 0.030 4.00.05 0.ObO 4.0 0.04 0.240 15.0 0.16 0.050 3.00.03 0.030 2.00.05 0.080 5.0 0.04 0.010 1.0 0.03 END OF LOG

IDENbB0201 X86CH262 NQ JUL86DJHRBPG&D JUL86S38 0.0 IPHJ EOUITY SILVER MINES LTD SOUTH OF S. T A I L - ST GEOCODE

- /SCL LSCL /WAM LNAM / R / L R H / L R / L H R / L R R R H R / L R R / L R R / L R / L H / L R / L R / L R / L

MT. 2MT. 1

OVBN P :TRICONED - NO CORE 20 3AlOI2Z <<VU P

MSCLL2ZPYCPTTASPR CBGY MGHESLGLMO

:FE OXIDE STAINS ON FRACTS :VUGS MAY BE CAUSED BY DISSOLUTION OF PY.

3 0 3A20QZ i< P < I < ) 0 6 AN

:FE OXIDE STAINS ON FRACTS. 1 8 3A10QZ i( P <: ( < $

0 0 AN :TO 3A?O/OC :FE OXIDE STAIN ON SOME FRACTS :NOTE -CHERT CLASTS ARE LOCALLY INDISTINCT (S IL IC IF ICAT ION?) .

22 3AiOI2Z id ~ .. P <:(< (

1 0 AN CL 0 7 0 :AS ABOVE 3 0 0 TO 3 3 0 :MINOR FE OXIDE STAIN ON FRACTS :CORE HEAVILY BROKEN TO 34.1 M. :MOST OF CORE LOSS FROM 33-34.1 M. :LOWER CNT SHARP AND REG. :TO 3B LOCALLY :AGAIN THERE SEEMS TO BE A S I L I C A OVERPRINT ON THE CLASTS.

:TO 3 F LOC. :MINOR OXIDE STAINS ON FRACTS. :LOWER CNT NOT OBSERVED.

0 9 AN < ( :AS ABOVE 33.11-37.2 M :LOWER CNT GRADATIONAL :TR FE OXIDES ON FRACTS.

4 5 0 1 3 3B103Z < < P < (< (

OS AN < ( :W/10% 1C INTERLEVED :LOWER CNT SHARP YUT VERY IRREGULOR.

480 2 9 3G12CL .:, % / .% P < ( < ( < ) < )

04 5G :TO AG LOCALLY :TO MOD FRACT LOCALLY.

5 1 0 2 9 3G12CL .:: < P .<)<:(< (

0 6 5G < ( :REMARKS AS ABOVE.

5 4 0 3 0 3G12CL < ( P <X<$<$ 0 5 5G

:HEMARKS AS ABOVE. 5 7 0 30 3G12CL << P < I < ( < (

11 5 6 < ( :REMARKS AS ABOVE : NOTE-FINE ASH

6 0 0 29 SG12CL ': < P < ) < ( < (

5G

:REMARKS AS ABOVE. 628 2 8 3G12CL i i

\ '% P ':+<)C) 2 2 5G < (

:REMARKS AS ABOVE :LOWER CNT NOT OBSERVED. $50 3 1 ~ A ~ O I J Z , .. <, <, P < (i+

27 AN :DISTINCT CLASTS TO 2 0 MM. (WHITE AND GREY)

690 1.0 3A10QZ .< < P i (.:+

15 AN :REMARKS AS ABOVE.

7 2 0 3 0 3A12QZ i: ~, P <.<. 1 0 AN

:VERY WEAK << TEXT :OTHER REMARKS AS ABOVE. 7 5 0 31) 3A10DZ . .< P <.<.

0 5 AN :REMARKS AS ABOVE

735 2 5 3A10IJZ ( c P ,: i < y 0 4 AN

:MOD << TEXT LOC. 797 X D F/ 0 1 0

:CLAY GOUGE. 83:1 21:1 3G22CL c: <: BS P <.:$<)<)

I 11 I; r i :LOCAL ZONES OF BRECCIA BETWEEN 78.5 & 80.2 M. (50%) W / QZ 4

PY MATRIX. :CL ALSO I N <( ENVELOPES :FAULT @ 80 .2 M.

2 0 3G22CL .: < BR P <:*<)<)

1 4 AG :LOCAL BRECCIA ZONES 84.4-85.1 M W / QZ + PY MATRIX. :CL ALSO I N < < ENVELOFES. 0 9 8A02CL A* P CU 0 7 5 0 8 AG CL 0 6 0

:LOWER CNT SLIGHTLY IRREGULAR :AMYGDS CONCENTRATED NEAR CNTS. 2 8 3G22CL .:, ; P < : ) < ) < )

15 5G :CL ALSO I N <i ENVELOPES i. - d.1 1.G22CL C: < P < ) < * < X 2 5 5G <$

:TO WEAK << TEXT LOC. :CL << ENVELOPES. 20 3G12CL .. ... P : ) .< $ .. ... .:

15 5G CL 054 :CL ALSO I N ii ENVELOPES. 3 7 ZAI(:IQZ < ( P B D 0 5 8 <(<(<:. -7 3 .J AN

:CP AT TOP OF INT ONLY :U.1 M. 3 6 INTERBEDDED e94.6 M. 3 4 JAlOQZ <( P < (<.

1 6 AN :VERY WEAK TEXT :NOTE-NO CORE 100.9-101.5 (TUBE DIDN'T LOCK) :LOWER CONTACT NOT OE,SERVED

3FZ4 LAC : CL RLSO I N (< ENVELOPES .< ,,

% % P <:)<)<:)

16 TG :CL ALSO IN C i ENVELOPES

:TO 3F25 LOC. : 3FKG CONTACT IS ARBITRARY(V.GRADATIONAL) 1216 26 3G24CLMS i P < ~) <=

29 AW 1280 29 3A200Z .:: C VU P .: ) (: +

14 AW 1310 29 3A20QZ < % i % P .:)<+

13 AW <. 1340 30 3A2OCIZ << P < ( ( 8

23 AW <. 1370 30 3AZOQZ << P <(<)(:.<.

24 AW :TR. TT?

1400 30 3A2OQZ . - ,, .< P < ( < )

26 AW 1430 30 3A20QZ ,: ... .... .~ P < (0

-,= i r l AW

1472 42 3A20QZ i: < P < (< )

25 AW CL 035 :VL I? LOWER CNT. THEREFORE NOT NECESSARILY BEDDING . . 1503 31 3620CIZ < .. .: . P < +%: + 18 AN :LOWER CNT. NOT OHSERVED

1536 33 3A20QZ ;: <': P < ) < + -7 A& AW CL 022 . < ( . . % RUNS RIGHT ALONG LOWER CONTACT

1580 44 ZC23CLMS .<<: P < )< )%<+<.

36 TG 1610 30 2C25MS << P < ((=<=

26 5T :TO 2C23 LOC :UPPER CNT GRADATIONAL

1658 30 2C24MSCL iC P <)Cl<+ 15 GT \. : 10-15% 3B INTERLEVED

1686 28 1D13 (( P <: (<).<+<:-

2 1 AG :LOC 2C INTERHEDDED, NO SHARP CONTACT

1730 42 2C24MSCL .<< P < (<+<:+<#

GT - :LOC 2C44, GOOD CP MINERALIZATION

1720 1760 30 2C24NSCL <i P <:(%:+<:I<( 21 GT

1760 1790 30 2C34MSCL << P ( -o i+Ct

17 GT :LDC 2834 INTERBEDDED. SOFT, GREEN, GREASY MINERAL IN <<

1820 Z9 2C34MSCL i.< P < - < ) < ) ~ < * < -

21 GT :MINOR TT OCCURING WITH CP IN <<

1850 29 2C44MSCL C<BR P (-0 <=<*<- 17 GT <- :MINOR BRECCIA

1880 30 2C34MSCL <<BH P <-<$<=<- 21 GT

1910 29 2C44MSCL C C P <-<)<:+< ( 11 GT

1940 30 2C34MSCL << P <(O<+<( 2 1 kT

1970 30 2C23MSCL << P <+<#<)<:.<. 19 TG <. :TT AND SL IN <i AT 196.6

2000 30 2C34MSCL <<BR P <-< (<)<.< ( 21:1 AT < - :MINOR BX'D. GOOD TT IN <<

2030 30 2C34MSCL <( P .<-<)$:+<.<- 15 GT :ROCK BECOMING SILICIOUS TOWARDS BOTTOM OF INTERVAL

2057 26 2C44MSCL <(BR P 11 GT :MINOR RR'X

2062 05 8C00 HXCM P CL 02 9T

2082 20 8BOl TCCM P CL 16 AG

2110 27 ZC~JMSCL I':BR P F/ 06 GT :CLAY RICH FAULT GOUGE

2140 28 2C53MSCL X B R P ' 09 GTCY

2160 19 2CS3MSCL (CBK P 03 GTCL

2185 24 2C44MSCL <<BR P 06 GT

2194 09 8COlFL P 1: P CU 06 GY CL

2230 34 ZC44MSCL <<Hi3 P 03 GTCY :BR'X ON UPPER CONTACT WITH DYKE

2260 29 2C44MSCL < I P 06 GT

2290 30 2C24MSCL << P 09 6T

2320 29 2C25MSCL << P 08 bT :BX FILLING PY AT 229.1

2350 29 2C25MSCL ::.: P 06 5T :CLASSIC 2C25 !

2380 29 2C24MSCL (:< P

05 GT C - :VERY FINE TT I N WITH HE I N <C'S

2410 29 2C24MSCL i:< P < (<$<)<-<-

02 GT 2440 29 2C34MSCL C < P C (<LC+< ( C (

11 GT < ( :TT, HE I N <C7S

2470 30 2C55MSCL C<BR P < (<$<+<-<$

19 GT *: . : GOOD LOOKING ROCK ! !

2500 29 2C34MSCL P C ( O < ) 05 GT .: -

2530 30 2C34MSCL P ~< (*:)<+<.<. 11 GT C: -

-c ha63 33 2C34MSCL <<HH P < (<+<+ <. 09 GT / -

:MINOR RR'X AT CONTACT WITH DYKE BELOW 2582 19 8A0O CM P C U ' 45 < (

11 BG CL 60 D ( 2600 18 8CClO CMP$ P < (

0 6 9T CL 60 2617 17 8A00 CM P < (

11 RG D ( :LOWER CONTACT IRREGULAR

2636 19 2C55MSCL BR<< P #+#= 15 5 1 <-

:COULD BE XENOLITH 2663 26 8A00 MSCM P C U 60 < ) < -

17 CL 50 D ( 2669 06 ZCSJMSCL BR<< F #=#=

03 5T #. 2675 06 8A00 MS P CU 70

04 2R CL 50 D ( 2700 23 2C35MSCL <<BR P F / <$<:$<+

11 5T :MINOR RR'X UNDER DYKE. FAULT GOUGE 268.3 TO 268.5

2723 23 2C24MSCL < C P < X i * < ) Ob GT

2760 36 2Cl2CL C < P q:)<-C)

06 46 :BANG! GREEN ROCK, FASTEST TRANSITION I 'VE SEEN!

2790 28 2C24MSCL << P C X < ) < ) CICI GT

:CORE VERY BROKEN 2820 28 ZC24MSCL <:<: P < ((+<+

00 GT 2850 30 2C12CL C < P C ) C - < t

11 TG 2880 30 2Cl2CL < C P <)<+<+<.

17 TG 2910 30 2C12CL < < F (+<-<I)

13 56 2940 30 2C12CL < < P <+<-<$

11 5G 2968 27 ZC23CLMS <<: P < # < ( C +

L / 2997 L / 3031 L / 3044 L H R R A00 1 ALAB ATYP AMTH AUMM R A0101 244 A001 270 A001 300 A001 1.30 A001 360 A001 390 AO01 420 AClCll 450 A001 480 A001 510 A001 540 At101 570 A001 600 A001 630 A001 660 A001 690 A001 720 A001 750 A001 780 AGIO 1 8 10 A001 830 R 85 1 A001 850 A001 896 A001 920 A001 950 A001 980 R 1009 A00 1 10 15 A001 1040 A001 1070 A001 1100 A001 1130 A001 1160 A001 1 190 A001 1220 ALICIi 1250

06 GT 29 8B01 <<P I P C L 25 < - 19 BG CM D ( 33 2C23CLMS << P <+CY<+<. 08 GT < - 13 1C12CL ,< < P <-< (<: (

03 56 8 1 2C12CL .% , P <+< (C$c:.

...' .,

36 TG - :CONTAINS TO SMALL (0.1 M) INTERVALS OF 1C. TUFF ALSO CONTAINS :OCCASIONAL CHERT PEBBLES. :END OF HOLE AT 312.7 M

EPUITY NINESITE LABORATORY ASSAY WET EXTRACTION A.A. - AU FIRE ASSAYED FIRST RCUVSAMPLE RPD % CU G!TAG G/TAU % SH 7. AS % FE % ZN :TRICONED - NO CURE

6820 0.15 0.5 0.08 6821 0. 1 1 0. 5 0. 08 6822 0.13 1.0 0.07

540 6823 0. 04 0. 5 111. f:15 570 6824 0.01. 0.5 0.03 6ClO 6825 0. 1113 1 . 0 0. U4 630 6826 0.07 1.0 0.01. 660 6827 0.05 1.0 0.05 690 6828 0.06 0.5 0.04 720 5929 0 . 02 0.5 0.04 750 681.0 0.05 0.5 0.05 730 6831 0. 08 1.0 0.07 810 6832 o. 11 4.0 0.08 830 6833 0. 02 0.5 0.04 85 1 6834 0.06 2.0 0.07 860 :DYKE-NO SAMFLE 890 5835 CI . 01. 1.0 0.05 920 6836 0.05 1.0 0.09 950 6837 0. 1J 0.5 0.07 180 6838 0.05 1.0 0.03

1009 681.9 0.03 1.0 0.04. 1015 :NU CORE-TUBE DIDN'T LOCK 1040 6840 0.05 0.5 0. 05 1070 6880 o. 07 1.0 0.06 1 100 6881 0.04 0.5 0.03 111.0 6882 0.19 9.0 0.05 1 160 6883 0.14 ;.o 0.05 1 190 6884 0.31 = a.0 0.05 1220 6885 1 . 5 5.0 (3.04 1230 6UU6 0.03 2.0 0.05 1290 A087 0.03 ?.(:I 0.04

1310 6888 1340 6889 1370 6890 1400 6891 1430 6892 1460 6893 1490 6394 1520 6895 1550 6896 1580 6897 1610 6898 1640 6899 1670 6900 1700 6901 1730 6902 1760 6903 1790 6704 1820 6705 1850 6906 1880 6907 1910 6908 1940 6909 1970 6910 2000 69 11 2030 6912 2057 6913 2082 :DYKE-NO SAMPLE 2110 6914 2140 6915 2160 6916 2185 6917 2194 :DYKE-NO SAMPLE 2230 6918 2260 6919 2290 6920 r r - 7 i j L O 692 1 2350 6922 2380 6923 24 10 6924 2440 6925 2470 6926 2500 6927 2530 6928 2563 6929 2617 :DYKE-NO SAMPLE 2636 6930 2663 :DYKE-NO SAMPLE 2669 6931 1675 : DYKE-NO SAMPLE 2700 6932 2730 6933 2760 6934 2790 6935 2020 6936 2850 6937

2890 6938 0.97 2910 6939 C,. 02 2940 6940 0.02 2968 6941 0. 07; 2997 :DYKE-NO SAMPLE 3030 6942 0 . 1 0 3060 6943 0.03 3090 6944 0.02 3127 6945 0.133

END OF ASSAYS - END OF

0.5 0.04 0.5 0.05 0.5 0.07 0.5 0.03

LOG

/SCL LSCL /NAN LNAM / H / L / L R

L R / L / L R / L / L / L / L R

L / L / L R / L H / L R / L / L R / L / L

EQUITY SILVER MINES LTD SOUTH OF S. TAIL - ST GEOCODE 552 NT 195.7 Ob2.0

1515 195.7 062.0 1957 145.7 062. 0 MT.2MT. 1

MT. 2

3 7 OVBN


:TRICONED - NO CORE 61 2 0 2C12CL <.I P

00 6G 8 5 15 2C12CL << P

0 0 6 6 :CORE BROKEN, FE STAIN

140 0 0 NREC P 00

:TRICONED AGAIN DOWN TO 14.0 - NO CORE 170 22 2C 1 2CL , -. P < ..1

00 TG 198 23 2C22CL .:: ( P

0 3 5G :FRACTURES STILL RUSTY

238 3 2 8C00 PY P BN 40 0 9 9G

270 27 2C12CL .: ( P 0 0 6G

300 28 2Cl2CL < C P

0 9 AG :FRACTURES STILL RUSTY

360 29 2C12CL I .., '\ '.. P

00 AG 390 27 2Ci2CL ( <: P

0 0 AG 420 28 2CiZCL << P

0 0 AG :SOME BLEACHING ON (C'S

2C12CL << P < ( < $ AG

FRACTURES END I N THIS INTERVAL. CORE VERY BROKEN. 2C 12CL ..: / ... %.. P r * . :a< .

AG <i AT 53.7 CORE I S RUMBLE, NO FAULT GOUGE THOUGH. 8B0 lFL PtCM P

6 A <<VU 2C24MS << P < a < - 0

GT CONTACT WITH DYKE IRREGULAR 2C2JMS Z: ( F' .:%.: ( < )

GT

600 637 35 2C13MS << 03 AG

637 652 15 8B0l PXTC 09 4A

652 680 27 2C23MS <: < 00 GT

:CORE VERY BROtKEN 680 710 29 2C34MS < q:

02 GT 710 740 29 2C34MS <<BR

00 GT 740 770 25 2C23MS < <

00 GT :MASSIVE CG. PYRITE SEAM AT

800 26 2C23MS < < 00 GT

830 29 2C22 <: <: 00 GA

860 29 2C24MS << 03 AT

890 28 2C34MS ((

03 6T 944 43 2C35M6 <<BR

0 3 6T :POOR RECOVERY

961 17 8B00 TCCM 08 2A

986 24 2C65 << 09

:MINOR 88 AT 96.7 1038 8BOO CHTC

3A 1052 14 2C44MS < <

00 1100 47 8BO1FL CM

2 1 54 :CONTACTS NOT PRESERVED

1130 29 2C44MS < < 09 GT

:LOTS OF DISSEM PV AS WELL 1160 27 2C44NS ((B4

00 AT 1190 29 2C33MS <<

00 AT 1199 09 8400 MS<:<

06 G A CM 1209 09 2C95MSaZ BR<<

03 6T 1262 52 8A00 MS

26 GA :CONTACTS NOT PRESERVED

1304 40 2C34MS <<BR 08 AT

1316 12 8A00 CMI: < 08 GB

P C U 45 <- CL 50 D-

P < I < - < )

75.3. BUT POOR RECOVERY

L / 1590 L R / 1620 L R / 1650 L / 1680 L / 1710 L R / 1740 L / 1770 L R / 1800 L R i 1830 L R / 1862 L / 1890 L / 1923 L H A001 ALAB ATYP AMTH

1350 33 2C?4MS <<BR P < ) < ) < +

09 AT 1380 29 2C34MS <<BH P < ) <+<+

Oh AT 1410 30 2C34MS <<BR P < (':+<+

15 AT 1440 30 2C34MS < < V/ 65 <X.:=<+

17 AT 1470 30 2C34MS << P V/ 70 <)<=<+

05 AT :BIG VEINS I N LAST TWO INTERVALS ARE QZ-PY, 5 CN WIDE

1500 30 2C24MS < < P < ( < ) < + 07 AT

1530 29 2C24MS ( < P V / 65 05 AT

:VEIN I S PY-QZ, 5 CN WIDE 1560 29 2C34MS .< .: P < (<+<+

05 6T 1590 30 2C34NS e: < P <-<+<+ <.

09 AT 1620 30 2C34MS <<BR P <-<+<+<.<X

11 6T < ( :GOOD TT, I N << AND ANGULAR RX AT 161.3

1650 30 2C55MSQZ i<HR P <.,:=:+ < ( 1.6 AT C (

: BX WEAK., TT I N << 1680 30 2C34MS <<BR P < (<+<:+ < (

09 AT <- 1710 30 2C33NSCL << P < t < ( < S

15 GT 1740 28 2C34NS <<BR P < ( < ( < ) < (

03 AT :MINOR RX'D

1770 28 2C34NS << P <X<+<+ <- 00 AT < (

1800 29 2C33MS < < P <$<+<+ <. 05 AT <.

:<<: WITH TT-SL AT 178.6, ONLY OCCURRANCE 1830 30 2C23MSCL << P < ) < ) < )

09 GT :ROCK TURNING GREEN!

1862 31 2C33NS << P <$<+<+<.< ( 00 GT <-<-

:ESSENTIALLY ALL TT, SL, CP OCCUR FROM 185.8 TO 186.1 1890 28 2C34MS < < P < (<=<+

1119 AT < - 1923 32 2C33MSCL << P <$<+<+<.

09 GT < ( 1957 33 2C23MSCL << P < I I < ) < )

12 AT :END OF HOLE

EQUITY MINESITE LABORATORY ASSAY WET EXTRACTION A.A. - AU FIRE ASSAYED FIRST

RCDVSANPLE RQD % CU G/TAG G/TAU % SB % A9 % FE % ZN 37 :TRICONED - NO CORE 61 6946 0.03 85 6947 0.02

140 :TRICONED - NO CORE 170 6948 0.03 198 6949 0. 02 238 :DYKE - NO SAMPLE 270 6950

421j 6955 0.06 450 5956 0.119 540 5957 0. Oh 570 6958 0.06 600 6959 0.11 639 6Y 60 0 . 0 3 652 :DYb'.E - NO SAMPLE 681:~ 6961 0. 05 710 6962 0. 39 740 696:: (I. c13 770 6964 0.14 800 6965 0. 11 030 6966 0. Oh 860 b957 0. (18 890 6968 0.27 944 6959 0.19 961 :DYKE - NO SAMPLE 986 5970 0.16

1038 :DYKE - NO SAMPLE 1052 597 1 0.47 11150 :DYKE - NO SAMPLE il;o 6972 (:I. :a 1160 6973 0.51 1 19CI 6974 0. 14 1199 :DYKE - NO SAMPLE 1209 6975 0.02 1262 :DYKE - ND SAMPLE 120; 6976 11. 03 1304 6977 0 . 05 1316 :DYKE - NO SANFLE 1;51:1 5978 CI. 07 138l? 6979 0.08

1710 6990 1740 6991 1770 6992 1800 h993 1830 5994 1862 6995 1890 6996 1922 6997 1957 6998

:END OF ASSAYS - END OF ASSAYS -

0.04 5 . 0 0 . 0 8 0.04 13.0 0.04 0.01 2.0 0.03 0.005 2 . 0 0 . 0 2 0.02 3.0 0.04 0.25 99.0 0.06 0.02 5 . 0 0 . 0 2 0.09 0 . 5 0 . 0 6 0.01 0.5 0.02

- END OF HOLE END OF LOG

IPRJ SO00 /SCL LSCL /NAN LNAM / R / L R / L / L R / L / L / L R / L / L R / L / L / L / L / L / L R / L R / L R R / L / L R /

X86CH264 NQ JUL86RBP EQUITY SILVER MINES LTD

488 MT 251.5 090.0 -45.Q MT. 2MT. 1

MT.2

104 OVBN :TRICONED - NO CORE

130 26 3F11CL < < 0 5 GA

:VERY LITTLE RUST ON <<

G&D JUL86S38 0. 0 SUPERSTITION ZONE - ST GEOCODE

5611.87 7435.93 1107.05

MSCLQZPYCPTTASPR CBGY MGHESLGLMU

15 G A :MINOR MS-QZ ALT'N ENVELOPE ON <<

220 3 0 3F12CL c: < P <+< (< (

17 G A 247 27 3F13CLMS << P < )<+<(

09 TG 280 3 3 3A11QZ < < P < (<+<$

1 2 AW :TYPICAL, VERY SILICOUS, CHERT PEBBLE CONGLOMERATE

310 3 0 3A21QZ < <: P < ( < + < a 14 AW

340 3 0 3A21QZ < < P V/ 25 < (<=<:+ 1 0 AW

:NOT SURE ABOUT ARSENU, VERY SMALL OCCURRANCE WITH 370 3 0 3A21QZ << P < f < + C )

09 AW 397 27 8C02CY P$CM P CU 4 5 < -

09 WT CL 45 4.30 3 3 3 A l l Q Z << P < ( < ) < f

15 AW 460 29 3A21QZ C < P < (<+<)

09 AW 499 38 3A21QZ << P <: ( < + < I

0 8 AW 505 0 6 3 E l l < < P B D 50 < ( < ( < : X

0 4 TG CL 50 :TOP CONTACT GRADATIONAL, BOTTOM SHARP!

569 53 3A11QZ < < P < ( < X < ) < . 18 AW

:MINOR CP I N << AT 53.1 616 4 6 3B11QZ < < P BD 50 < % < I < ) < .

2 1 AG CL 9 0

<. QZ-PY

:TOP CONTACT GRADATIONAL, BOTTOM SHARP. MINOR CP AT 58.5 :BOTTOM CONTACT IRREGULAR

670 5 2 3A1182 <:I P < ( < ) < : I : 1 4 AW < (

700 29 3A l lQZ << P <.<:+<( 06 AW <: -

:RUST ON FRACTURES (MINOR) 729 28 3A21QZ <i P C . < + < Y

11 AW :LOWER CONTACT IS SHARP, BUT IRREGULAR 31 3F 12CL << P <)<+< (< .

19 AG :SMALL (0.1 M) 3B AT TOP OF INTERVAL. STRAT COULD BE UNIT 2? 30 3F22CL *: < P <+.:+i (<.

17 AG 30 3F22CL < < P V / 40 <(<+<*<. 15 AG :TUFF CONTAINS ABUNDANT BLACK SHARDS. MINOR QZ-SER ALT'N ON : SOME :: < 25 3F23CLNS << P <XrOi(<. 09 T6 11 3B12CL << P < (O< (<. 0 3 AG :UPPER CONTACT IS GRADATIONAL OVER 0.3 M 05 8A01 ,~ ./

\ .~ P <: * 0 2 76 CL 70 <K)<- 09 3B12CL < < P BD 70 03 AG :LOWER CONTACT GRADATIONAL, CONTAINS 0.2 CM WIDE 2C. TO BEDDING 17 3J12CL . .: P B D 70 i(<)<( 09 AG :INTERBEDS ARE JUST OVER 1.0 CM WIDE 49 ZC23CL ./ , '%. ' P C (<+<:$<- 20 TG :SLIGHT OZ-SER ALT'N ON <i. THIS IS LIKELY THE ACTUAL :TRANSITION INTO UNIT 2 -. . ;u 2C22CL << P <+oo 11 AG 30 2C23CLMS << P ti$<+<:+< (

19 AT :MINOR 2D INTERBED 30 2C22CL << P <*< (< )< : -

2 1 AG :MOST OF CP AT 100.4 30 2C12CL << F O O i I 11 AG :MINOR 2D 30 2ClZCL < i P < < #? 09 AG :MOST CP IN SMALL UX AT 107.7 M. MAYBE SOME ARSENO TOO 28 2C13CLMS << P <+<)< )< -

06 TG 30 2C12CL < < P <:+<),<(<. 14 AG

1180 29 2C22CL <* , <. % P <:+<I .<)<I-<- 15 AG .< - < ( :MINOR PZ-SER ALT'N AT 117.6, WITH TT, SL, CP

1210 30 2C22CL << P <)<+<)<. 19 AG :AGAIN, MINOR 02-SER ALT'N

1240 JO 2C23CLMS << P O < ) < X 19 AG

1270 30 2CZSCLhS << P <)<+<#< -

1270 1300 3 0 2C22CL < r: 1 7 FIG

:NO VISIBLE T i BUT COULD BE LOW GRADE AG 30 2C54MSDZ <<HR P V/ 65 < I#+#$ 12 AT 29 2C34NSQZ <<BR P V/ 6 0 < = < I + < - 0 5 AT 2 0 2C44MSQZ <<BR P <+<) <-<:? 0 6 AT 7 0 5BO1CY (<:PX P CU 50 D ( 36 G A CN CL 6 5 D-

:CL-CY REPLACE FL LATHS 17 2C64MSOZ <<BR P # 1 #+B- 0 6 AT 0 6 8A02CL ((CM P CU 5 5 ; = 03 bG CL 6O

:PERSAVSIVE CL ALT' N 23 ZC6411SUZ BR<< P + 1 #=B-B (

0 6 bT :0.1 M OF 8C AT 160.4. BOTTOM 0.4 M CY RICH BX; LIKELY FAULT : GUUGE 0 4 5C12CY << P CU 50 0 0 CL 6 0 20 ~ C ~ ~ M S Q Z BR<.:< P <=#)B. 0 3 AT 10 8A10 <<CM P CU 6 5 A= 10 46 CL 65AY

:0.1 R 5C MARGINS. SOLID PIECE OF CORE 27 2C43MSQZ < iBR P #=O=B (B ( 14 AT B- 29 2C34MSQZ << P < )< l<=<-< - 13 AT < - 3 0 2C34MS < < P .:)<+<+.:.<- 2 1 AT <* 3 0 2C34MS <: <: P <)<=<+<-<-B? 17 AT < X 3 0 2C34MS << P <)<:+<)<Y<- 11 AT < (

:TT OCCURS I N << WITH SL, IDENTIFICATION DIFFICULT 29 2C33MS < < P <t<=<+< (<$

0 8 AT < )

:MOST SL, TT, CP OCCURS I N TOP HALF OF INTERVAL 3 0 2C33MS .I . i ., P v/ 6 5 <l<)<+<-<. 17 AT < )

3 0 2C23MS << P < X I < + < + < - 11 AT

1890 1920 3 0 2C23CLMS << P 1 4 GT

1920 1950 2 9 2C23CLMS << P 0 7 GT

1950 1980 3 0 2C33CLMS << P 0 9 GT

:MINOR 2D 1980 2010 3 0 2C43CLMS << P

0 9 TG :GENERAL REMARK: MOST OF ABOVE SL, :GASHES. ALL THE WAY BACK TO 168.0

2C43CLMS <<: P GT

2C43CLMS <<BH P TA

FX, NOT NOT AT DYKE CONTACT 8C00FL PXCII P

9G CL 2C44MSQZ <:I P

AT 2C43CLMS << P

TA

I )<+<=< (<? < (

CP, TT OCCURS I N IRREGULAR

:MINOR XI, SPOTTY STRONG DISSEM. PY 3 0 2C43MS .-:<BR P <)<+<=<)<? 1 3 AT

:VERY F I N E GRAINED GRAY-BLUE I N << WITH CP, TT ? 3 0 2C33CLMS << P <+<l<+<-<? 15 AT <.

:AS ABOVE 3 0 2C33CLMS << P <+<:)<+< ( < -

2 1 AT < - 30 2C33CLMS <<BH P <:+<$<+<- 1 2 AT

:CP OCCURS ONLY AT 227.0 3 0 2C33CLMS <<BR P <+<+<=< ( 1 5 AT

2C33CLNS << P <+<=<=< (<? 1 5 AT #+

:MINOR 2D. LOTS OF SL, NO POSITIVE I D OF TT, BUT SUSPECT SOME : I N WITH THE SL

3 0 2D23CLMS c:~: P (+<=<+ <? 12 TA <-

:SOME INTERBEDDED 2C. SL OCCURS ONLY I N FIRST 0.2 M OF INTERVAL 2 8 2CZJCLMS << P <=<+<+ 0 5 T A 0 9 8 A l l C L <<PC P D+(+D) 0 9 7 6

:CONTACTS SHARP, BUT IRREGULAR 2 4 0 8 2 4 4 0 31 2D22CL .: .: P B D 6 0 <=<X<)

09 T A <. :INTERBEDDED 2C

2440 2462 2 2 2C44CLMS << P < = < X < ) <? 12 AT < t

:NO POSITIVE I D ON TT, BUT SUSPECT I N WITH SL 2462 2484 22 2C44MSCL << P < = < * < a <?

L R R R R a00 1 ALAB ATYP ANTH AUMM R oo A001 104 A001 130 A001 160 A001 190 A001 220 AClOl 250 A001 280 A00 1 310 A001 340 R 370 A i l i l l 397 A001 430 A001 460 A001 490 A O O l 520 A001 550 A!:rOl ;no Ah01 610 A O O l 640 A001 670 A O O l 700 AC101 730 A001 760 A001 790 AClOl 920 A001 850 A001 880 A001 910 AClOl 940 A001 970 AOCI 1 1t)CIO A001 1030 AOCll 1060 A001 1090 A001 1130 A001 1150 A001 1130 A001 1210 A001 124C1

L 05 GT < )

R :AS ABOVE, SL OCCURS ONLY I N TWO i < ' S / 2484 2515 3 1 8A10 <<A* F C U 40 A=<-

28 %A D+ :OTZ ALSO OCCURS I N <<'S. HOLE ENDS I N DYKE :HOLE LIKELY SHOULD HAVE BEEN CONTINUED. I SHUT I T DOWN BECAUSE :OF THE INCREASE OF CL :IN <<'S :END OF HOLE

EQUITY MINESITE LABORATORY ASSAY WET EXTRACTION A.A. - AU FIRE ASSAYED FIRST RCOVSAMPLE RQD % CU G/TAG G/TAU % SB % AS % FE % ZN

104 :TRICONED - NO CORE 130 6999 0.05 160 71:11:10 0. 04 190 700 1 0. 04 220 7iXl2 0. 04 250 7i)i:lz 0.03 280 7004 0.04 310 71305 0. i j5 340 7006 I). 02 370 7007 0. 06 397 :DYKE - NO SAMPLE 43i3 7008 0.06 460 7009 0.10 490 7010 0. 05 520 7 rJ l l 0.05 550 7012 0. 10 580 7013 0.07 6 l i l 7014 0.14 640 7015 0.07 570 7016 0.05 700 71:) 17 I.:> . 0 6 730 7018 0.09 760 7019 0. 136 7Y0 7020 0. OY 8211 7021 0. 06 850 7022 0 . 13 880 71125 0.10 910 7024 0. 1 I. 940 7025 0.07 970 7026 0. 09

1000 7027 0.26 1030 7028 0.13 1060 7029 0.05 1090 703il . 17 -. 1 120 7031 0.09 1150 7 . - 7 , 02% 0. 07 1180 ?I>?.: 0.11 12 1 0 7i:17.4 0.11

1360 7039 0.28 1390 7040 0.14 1420 704 1 0.19 1450 7042 [j. 22 1480 7043 <I . 07 1500 7044 0.06 1571 :DYKE - NO SAMPLE 1588 7045 0.33 1594 :DYKE - NO SAMPLE 1619 7046 il. 29 1623 :DYKE - NO SAMPLE 1643 7047 0.04 1653 :DYKE - NO SAMPLE I680 7049 (] -:?! . .dd 1710 7049 1). 17 1740 71150 0. 06 1770 7051 0.05 1800 7052 0.04 1830 7053 0.12 1860 7054 0 . 1 3 1890 70% 0.16 1920 7056 0. 12 1950 7057 0.10 1980 7058 0.12 2010 7059 0. 17 2040 7060 0. (18 2078 7061 0.10 2096 :DYKE - NO SAMPLE 2130 7062 0.09 2160 7063 0.26 2190 7064 I:] . i a 2221) 7065 0.07 2250 7066 0.08 2280 7067 IJ. 07 2310 7068 0. oa 2340 7069 0.10 2370 7070 0.06 2399 707 1 0.06 2408 :DYKE - NO SAMPLE ?440 7072 0. 04 2462 7073 0.04 2484 7074 0.05 2515 :DYKE - NO SAMPLE

R :END OF HOLE - END OF LOG R END OF ASSAYS - END OF LOG

IDEN6B0201 X86CH265 NO JULBbRWW G&D JUL86S38 0.0 IPRJ EQUITY SILVER MINES LTD SUPERSTITION ZONE - ST GEOCODE SO00 00 457 MT 168.9 090.0 -45.0 SO01 457 1302 163.9 090.0 -44.5

/SCL LSCL /NAN LNAM / H / L R / L R / L / L H / L H / L R H / L R / L / R / L R R / L R H / L H / L H / L / R /

1689 168.9 090.0 -42.5 MT. 2MT. 1

MT.2


520 29 2C34MS <<:BR P ':< AT

INTERBEDDED 20 2D44CL <<BR P

&A INTERBEDDED 2C 8Cll <: < F CU

Y T VU 2C44MS .:(BR P

AT

MSCLPZPYCPTTASPR CBGY MGHESLGLMO

6O <(<+<=El.

< (<=<=B.

65 <.

< (<=<=<-<.

INTERBEDDED 2D. :SOME FE STAINING 2C34MS .; .: BF( P < (<+<=Q*<.

AT INTERBEDDED 2D 8B13MS .:<AA P

5T < ( MAFIC COMPOSITION FROM 61.8 TO 62.2 M. FELDSPAR INFILLING

: AMYGDS 27 2C44MS +:<AH P .:f<:+<=B. 11 AT :SOME CP IN << 37 2C44MS <IFF: P < (<=<;=p- 11 AT

X D +4 :OTZ FLOODING CONTAINS PATCHY PY 25 2C44MS <IBR p <: e: 60 <(<=<= 08 AT

:.l M OF PATCH FELDSPAR FROM 71.3 TO 71.4 M :POSSIBLE GL BUT MAY BE TARNISHED PY 28 2D44CL <<UR P <+<= 03 TA :SOME FE STAINING. :SOME INTEHBEDDED 2C. SOME PY STAINED BLUE :SIMILAR FELDS TO ABOVE 24 2D44CL .:<BR P 06 TA :SOME PATCHY PY. :STILL SOME FE STAINING 28 2D44CL <<BR P 08 TA :SOME PY DUITE MASSIVE. :SOME INTERBEDDED 26 2C44MS z:<BR P 03 AT

X D V1 6CI :PTZ-PY VEIN FROM 80.3 TO 80.5 28 2C34MS .:<BR F

06 : SOME 25 00

:.l M 26 02 :SOME :ROCK :SOME 27 02

AT FE STAINING. :AGAIN SOME STRANGE FELDSPARS AS BEFORE 2C34MS < < P .: ((+(+

AT X D Vl 55 OF PTZ-PY VEIN FROM 86.4 TO 86.5 M 2C43-E c:<:BR P < (<:+<+<.

AT PATCHY PYRITE. :IDENTIFIED BLUE-GRAY MIN. (CHLORITE?) CONTAINS FINE GLASS SHARDS. :ALSO SOME FE STAINING. VEINS OF ALTERED FELDSPAR(?) 2C44MS (.:: BR F' C: (<+<=<-

AT :SLIGHT FE STAINS. :AGAIN FELDSPAR AS ABOVE. :SOME PY PATCHY - -8 2C44MS ,.. .., 1 ... P <.:a<+<+ 02 AT :SOME MASSIVE PY AND SOME MINOR QTZ FLOODING. :SOME FE STAINS 27 2C34MS (.<'R P W P 35 .<(<+<+ <. Ob bT a- :SOME FE STAINING. :SOME CARONATE AGAIN FELDSPAR TOO :TT ONLY AT 97.2 M 27 2C44MS <iBR P < (<+<+

00 AT :AGAIN ALT. FELDSPAR. :FE STAIN AT BEGINNING OF INT 29 2C44MS <<BR P r!;+i+ 0. CICI AT a. :MINOR FE STAINS :TT ONLY AT 105.9 M :DTZ-PY VEIN FOR 0.1 M :FROM 107.4 - 107.5 M 27 2C44MS <<BR P < (<+<=

05 AT :GOOD BRECCIATION FROM 107.5 - 107.7 M 28 2C43MSCL <<BR P <+<+<. 03 ATAG :0.1 M OF OTZ-PY VEIN FROM 112.9 - 113.0 M :AGAIN FELDS PATCHES

INTERBEDDED 2D :GOOD HR'N AT START OF INT 2C44MS <<BR P < (<+<=<-

AT <.<. FE STAINING :SL MAYBE QUESTIONABLE 2C44MS ,: .< UR P <:#<+<=

AT FE STAINING 2C43MS s: <: P <*<+<+

AT B. FELDSPAR BLEBS. FE STAINS 2C44MS <i:ER P < (<+<+<.

AT 0 . . . . -. :CP ONLY FROM 124.0 - 124.1 M :MINOR FE STflINS :LAST METER :MAINLY ASH :OTZ-PY VEIN .1 M - CANNOT DETERMINE C1 27 2C43MS i .: BR P <#<+<+<. 00 AT <.H. :SP & GL ONLY AT 127.8 M 28 2C44MS .:CBF( P ( ((+i:= 00 AT < 1: :GY FROM 129.8 - 130.5 M 26 2C44MS << P < (<+<=Q(<.

08 AT < ( :GREY-BLUE HIGH LUSTRE MIN - UNIDENTIFIED TT(?)

1360 23 2C44MS .< .: BR P <: (<+<c+.< ((.

03 AT <. 1379 19 8AllCL <<FB P <.<.

11 AG AX 1389 09 2C44MS <<BR P C U 50 <+<+<+<.<)

Oh AT <:.<X :STRONGLY BRECCIATED AT BEGINNING OF INT

1415 25 8AllCL < ' , \ P CL 45 < ( ,7 L 1 AG <.<. :CARBONATE AMYGDS :INTERIOR 8A DYKE WITH SLIGHTLY DIFF. TEXT

1445 28 2C44MS <<BR P .<+.<+<= 03 AT <.a( :HE ONLY AT 144.6 M :PY-QZ VEIN (.2 M) FROM 143.7 - 143.9 M

1475 29 2C44MS < < P <)<:+<+

08 AT :SOME INTERBEDDED 2D

1505 29 2C44MS C<BR P < (<+<= 05 AT < )

:SOME SL IN PATCHES 1535 29 2C44MS /.:(HF: P i, (.<+<=<.<.

08 AT < ( :HE MAY BE MIXED WITH SL :CP ONLY IN 2 PLACES (IN < < I 14 2C44MS C: .< BR p .: .: 55 <(i t<+(.<.

A001 ALAR ATYP AMTH AUMN R 00 488

06 AT <?< ( :BLUISH GRAY MIN WITH SL <:< - MAYBE SPECULARITE - CAN'T TELL! 07 BAllCL <: <: P 06 5G :CARBONATE AMYGDS :COI4TACTS NOT MEAS. DUE TO BROKEN CORE 29 2C44MS (.<BI~ P <(<+/=<.<.

08 AT '. . :BRITTLE FURPLE-BLUE MIN. AGAIN(?) :3 CM PY-OZ VEIN AT 158.6 M 31 2C44MS < < Bl? P i (c+=i.$<- 09 AT .: ?.: )

:AGAIN BLUE GRAY MIN WITH SL - COULD BE SPECULARITE :0.4 M OF STRONGLY BRECCIATED CORE WITH GOOD TT, CP, SL :FROM 161.6 M 3 1 2C44MS <<BR P << 50 <: (<+<+O-<- 14 AT 0. <?< (

:SOME GOOD FRACTURING :ROCK STARTING TO TURN GREENER AT END :OF INTERVAL 17 2C33MS ,: < P O<+O i,. 06 AT <?<- :TT AT 165.7 M 16 2C43MS <<BR P <).<+<:)<:.<.

00 GT <.<. :0.1 M CJZ-PY VEIN AT 167.5 M :TUFF ASH HAS GREEN COLORATION :END OF LOG

EOUITY MINESITE LABORATORY ASSAY WET EXTRACTION A.A. - AU FIRE ASSAYED FIRST RCOVSAMPLE RQD % CU WTAG G/TAU % SB % AS % FE % ZN :TRICONED - NO CORE

520 7081 0.31 550 7082 0.44 579 7083 0.35 613 7084 0.85 523 :DYKE - NO SAMPLE 653 7085 o. in 683 7086 0.22 712 7087 0. 02 742 7088 0.01 772 7089 0.01 8 0 7090 13.02 833 709 1 o.O? 863 7092 0.04 893 7093 0.03 923 7094 0. 08 953 7095 0.12 983 7095 0.06 1013 7097 0. (13 1043 7098 0.03 1073 7099 0.02 1103 7100 0.03 1133 7101 0.05 1163 7102 0.04 1193 7103 0.04 1223 7104 0.04 1253 7105 0.06 1283 7106 0.11 1313 7107 0 . 03 13.56 7100 0.28 1360 7109 0.05 1379 :DYKE - NO SAMPLE 1389 7 1 10 0.05 1415 :DYKE - NO SAMPLE 1445 7111 0.02 1475 7112 0.05 1 505 7113 0.01 1535 7114 0.06 1550 7115 0.09 1558 :DYKE - NO SAMPLE 158Y 7116 0. 07 1621 7117 0.27 1553 7118 0.10 1671 71 19 0.04 1689 7120 0.03

R :END OF HOLE - END OF LOG AT 168.9 M R END OF ASSAYS - END OF LOG

IPRJ SCl0O SO01 so02 1 /SCL LSCL /NAN LNAM / R / L R / L R R / L R / L R / L R R / L R / L R / L R / L R / L R / L Fi / L R / L R / L R

~~~

ECJUITY SILVER MINES LTD SUPERSTITION ZONE - ST GEOCODE 457 MT 230.4 090. 0 -45.0 5523.54 7452.69 1128.68

1470 230.4 090.0 -43.0 2304 230.4 090.0 -45.0

MT.2MT. 1 MT. 2

MSCLCJZPYCPTTASPH CRGY MGHESLGLMO

OVBN P :TRICONED 0 - 9.8 M NO CORE :CORED A FEW BOULDERS 9.8 - 10.0 M 25 2C24MSCL <( P < ) , : I < : . 0 0 GT

:LI ON FRACTS :TO 2D LOC 29 2C23CLMS (( P << 028 < ) < ) < .

CICI TG :ONLY MINOR L I PAST 13.7 M :2C24 13.0-13.7 M (GRADATIONAL CNT) : 10% MS AS <<: ENVELOPES 26 2C23CLMS <( P << 024 <+<) ( )

0 9 TG < ( : 10% MS AS << ENVELOPES :5% CL AS << ENVELOPES

2 0 2C23CLMS << P < 036 <+()<+ 0 5 TG < (

:5% MS AS <% ENVELOPES : 10% CL AS <i ENVELOPES 2 2 8COSMSCL P I P 18 GT

:TYPICAL POST-MIN LATITE DYKE :CNTS NOT OBSERVED DUE TO :BROKEN CORE 29 2C23CLMS <:< P <(<:)<+<:.<:.

00 TG :Ti MS AS << ENVELOPES :TT? 28 2C23CLMS << P < (< )%+< .

02 TG :TO 2C15 LOC :10% MS AS << ENVELOPES 3 0 2C23CLMS << P < ) < + < (

05 TG : 10% MS AS i< ENVELOPES

2 0 2C24MSCL (< P < ) < ) < . 00 GT

:HEAVILY BROKEN UP INTERVAL :60% MS 25 2C24CLMS << P < ( < ) < ) < (

0 4 TG :TO 2D LOC :30% MS

3 0 2C24CLMS <% P < ( < ) O 15 TG

:30% MS 28 2C23CLMS << P << 025 < ( < ) < )

12 TG :5% MS AS << ENVELOPES :1% CL AS << ENVELOPES

3 0 2C23CLMS << P 09 TG < +

:5% MS AS << ENVELOPES :2% CL AS << ENVELOPES :TO 2C23 LOC 2 6 2C23CLMS <:< P .: (<)<+<.

12 TG :TO 2ClS @ END OF INTERVAL :10% MS AS << ENVELOPES

540 29 2C23CLMS << P <:(<)<:+

05 TG :TO 2C15 @ START OF INTERVAL :10% MS AS i C ENVELOPES

563 23 2C44MSCL <<BR P .:: ) ( +( + 08 GT i ( :TO 8A FROM 54.6 - 55.1 M

598 35 8AllCLCY <<P$ P CU 020 < ( 30 G A CL 015<( :FLAG PHENOS TO 15 X 3 MM (ALTERED TO MONT)

611 13 2C34MSCL << P < (<+<+ 05 GT < (

624 13 8AllCLCY <<P$ P CU 025 < ( 00 G A i ( :SIMILAR TO 56.3 - 59.8 EXCEPT LOCALLY BLEACHED WHITE :LOWER CNT NOT OBSERVED DUE TO GROUND CORE

650 24 2C24CLNS << P <+O<+ 04 TG < ( :2% CL AS << ENVELOPES

680 28 2C24CLMS << P <:(<)<+<:. 02 TG i+

710 29 2C34MSCL << P <(00 13 GT <+ :TO 2C54 LOC

740 28 2C34NSCL Ci P I+<).:. 05 GT < ( :TO 2C12 LOC (EOI)

770 29 2C24MSCL << P O O < . Oh GT :TO 2C12 LOC (Sol)

800 28 2C25MS << P ($0 00 5T :5% PZ AS << ENVELOPES

812 11 2C25MS (: < P < a < ) < . ClCt 5T :AS ABOVE 77.0 - 80.0 M

822 10 8AOlCY PS P CU 07C1 04 5A :LOWER CNT NOT OBSERVED DUE TO BROKEN CORE

860 36 2C25MS < %: <1<)<.<? 02 5T :MINOR GOUUGE @ 83.5 M :5% QZ AS << ENVELOPES

890 28 2C24MSCL << P <SO<(<? 19 GT :BROKEN CORE AND GOUGE 88.8 - 89.0 M :TO 2C34 LOC

915 24 2C24MSCL < < P CS<)<( ~13 GT :TO 2C35LOC

925 09 8A0lCY PSCM P CU 048 06 AU CL 045 D ( :GOOD INTRUSIVE CNTS W/ CHILLED MARGINS :.l M XENOLITH @ :UPPER CNT

950 23 2C24CLMS <:.< P < : % < ) < I < . 03 TG :TO 2C45LOC

900 25 2C34CLMS << F < ( < + < I < (

0 6 TG < ( 18 2C24MSCL P <(<+<)<. 00 GT

:POOR REC - SMALL CHIPS OF CORE - NO GOUGE 40 2C45MS < ( P < ) < )

05 AT :GOUGE @ 103.6

x D F/ 080 :2 CMS GOUGE 5 6 BAI~CLCY P ~ A X P cu 070 < X 42 AG << < X

:GOUGE & RXIA 109.6 - l lO.1 M :NOTE 2 TYPES OF ANDESITE DYKE : (AMYGDALOIDAL ONE CUTS PORPHYRITIC ONE) :UNALIGNED FLAG PHENOS (15 X 2 MM) ALTERED TO SAUSS :LOWER CNT OBBSCUHHED I N GOUGE :.08 M XENOLITH @ 109.6 M

27 2C55NS BR<< P #+#+.< (

13 AT :TO 2C35 LOC

3 0 2C55MS 0 9 AT 27 2C35MS 17 5T 28 2C35MS 0 2 5T

:8A FROM 115.1 25 2C35MS 0 8 ST 3 0 2C35MS 0 5 5T

BRr( P

(( P

< <: P

115.81 (PREVIOUS INTERVAL) < < P < i 058

<< P C < Oh0

1310 3 0 2C35MS %< < P C < Oh0 0 3 5T

:TO 2D LOC :OCC PY + OZ V/ 1340 29 2C35MS <<BR P

05 5T 1331 X D F / 015 1370 27 2C35NS << P

0 6 ST :8A FROM 134.2 - 134.8 M

1400 30 2C35MS << P 10 ST

1416 16 2C35NS <: < P 0 0 ST

:TO 2C45 LOC :TO 2D LOC 1428 12 8A02CLCB PXAI P CU 060

10 5G CL 085 1460 3 2 2C25MS .< <: P << 060

03 5T :TO 2D LOC

1490 30 2C25MS < < P V/ 050 0 4 5T

:4 - V/ OZ + PY 2 - 4 CMS WIDE 1520 30 2C35MS <<FIR P

13 ST :TO 2C55 LOC

1550 29 2C55M9 0k.c: P

14 ST :TT POSSIBLY IN W / SL - DIFFICULT TO :TO 2C35 LOC :POSSIBLY HE (HS) IN W /

1580 30 2C65MS BR<< P 04 5T :TO 2C35 LOC :APPEARS TO BE TECTONIC

1610 29 2C35MS i .: P c: <: 07 5T

1640 29 2C55MS FIR:< P 22 5T :TO 2C35 TOWARDS EOI

1670 29 2C35MS << P << 16 5T

1700 30 2C35MS << P << 12 5T

1730 30 2C35MS < i p (( 15 5T

1760 29 2C35MS < < P <;< 04 5T

1790 26 2C55MS C < P 02 5T :GOUGE @ 177.3 M

1820 30 2C35MS ( < P 04 5T

1850 28 2C45MS << P OF3 5T

1880 30 2C55MS << P 19 ST

1910 27 2C45NS < < P 02 ST :TO 2C55 LOC

1940 26 2C45MS < < P 20 5T

<?< t IDENTIFY POSITIVELY SL

#+#+#. #? a c #?

BXIA W / SOME GOUGE i140 <)<:)<;(

<?< ( #+#+

:TO 2C55 LOC :TT OBSERVED TO CROSS-CUT PY :LOST CORE @ 191.1 M 1940 1953 13 2C45MS << P 0 0 C 1

0 7 5T <. 1953 1965 12 RA02CL A1 P CU 042

0 9 5G CL 045 D ( 1965 2000 35 2C45MS <<I< P O<+<t

17 'JT < ( 2000 2030 30 2C45HS < < P < ) < + < a

0 4 5T 2030 2060 30 2C24CLMS << P <X<Y<t< (

09 TG :2C?S TO 204.2 :8A 203.7 - 203.9 M :CP ONLY TO 204.2

2060 2090 30 2C24CLMS << P <t<$<*<.<? 22 TG <. :GREY UNIDENTIFIED MINERAL W / SL :NOTE COLOR CHANGE @ 204.2 M

2090 2120 29 2C24CLMS << P < * < Y < t c < . 04 TG

2120 2150 29 2C24CLMS << F' < ( < 1 .... t 05 TG :TO 2C25 LOC

2150 2170 20 2C24CLMS <:< P < ( < # i t 08 TG <.

R / 2170 L / 2195 L R / 2225 L Fi / 2255 L R I 2285 L R A001 ALAB ATYP AMTH AUMM

:TO 2C25 LOC 2195 20 2C24MSCL << P <:.I*<*

12 GT < X 2225 -' JU BA02CLC.B A#<< P

29 46 CL 050<. :V WEAK << TEXT W / CB :UPPER CNT NOT OBSERVED

2255 30 2C24CLMS << P < ( < X < X < . 03 TG

:TO 2C25 @ END OF INTERVAL 2285 30 2C24MSCL << P < ( < X C )

02 GT :TO 2C25 LOC :TO 2D LOC

2304 19 2C24CLMS << P < ((:X<) 03 TG

:EOH @ 230.4

EQUITY HINESITE LABORATORY ASSAY WET EXTRACTION A.A. .- AU FIRE ASSAYED FIRST RCOVSAMPLE ROD % CIJ G/TAG G/TAU % SH % AS % FE % ZN

100 :OWN - NU CORE 130 7161 0.13 160 7162 0.09 190 7163 0 . 05 212 7164 0.06 240 :DYKE - NO SAMPLE 270 7165 0.05 300 7166 0 . 08 77 - .,.,,.I 7167 I:! . 07 360 7168 0.09 590 7169 11. 06 420 7 1 70 0.12 450 7171 0.11 480 7172 0. (J4 c ~ l i . 1 7173 0. (17 540 7174 0.09 563 7175 0. 135 598 :DYKE - NO SAMPLES 622 7176 0. Oh 6515 7177 0.10 680 7178 0. 07 710 7179 (2.18 740 7 180 0.09 770 7181 0.07 8ilO 7182 0. 14 812 7181: 0.12 860 7184 0. 07 890 7 185 0. C7 915 7186 0.14 925 :DYKE - NO SAMPLE 9511 7187 0.12 980 7188 0.17

1 01 CI 7189 0.07 1045 7190 0.03 1101 :DYKE - NO SAMPLES

~TDDD~DDDDDDDD~DDDDDDDDDDDDDDDDDB~DDDDDDDDDDD

30

3

0C

03

00

00

~

~0

0C

~3

0.

~.

0~

20

00

OO

O0

C

30

00

00

00

30

O

00

0

OC

00

00

GC

0

00

CO

~G

~~

~0

OO

~0

C0

0

OO

OO

O0

00

CO

O

r-r

C

-C

C-

CC

-

rr

rC

CC

--C

Cr

rr

r-r

r-

rr

rr

rr

r-r

--

I PRJ S000 SO0 1 /SCL LSCL /NAM LNAM / R / L R / L R / L R / L R / L R / L R / L R / L R / L R / L H / L R / L H / L H / L R 1 L R

XBbCH267 NQ AUGDbDJH G%D AUG86S38 0.0 EQUITY SILVER MINES LTD SUPERSTITION ZONE - ST GEOCODE

434 MT 108.2 090.0 -45.0 5421 .68 7507.98 1131.07 1082 108.2 090.0 -44.0 MT. 2MT. 1

MT. 2 MSCLQZPYCPTTASPR CRGY MGHESLGLMO

5 2 OVBN P :TRICONED - NO CORE

8 0 2 6 2C13CLMS <.: P <.<(<:$<. 0 0 TG

:FE OXIDE ON FRACTS :MS AS << ENVELOPES 110 2 9 2C13CLMS i<: P < ( < ( < I

00 TG :FE OXIDES ON FRACTS :MS AS C < ENVELOPES

140 2 9 2C13CLMS <<: P < ( < ( ( 1 : 1 2 TG

:MINOR FE OXIDES :MS AS << ENVELOPES 1 7 0 27 2C13CLMS i< P < (< (~<I<.

1 1 TG :MS ON << ENVELOPES

2 0 0 27 2C13CLMS << P < ( < ( < X < . 0 7 T 6

:MS ON << ENVELOPES 2 3 0 2 8 2C13CLMS << P <(<(<I<.

0 2 TG :MS AS << ENVELOPES

2 6 0 2 8 2C13CLMS << P < (<; ( < X < . 0 9 TG

:MS AS << ENVELOPES 290 2 9 2C13CLMS << P < (< ( < $

0 4 TG :MS AS << ENVELOPES

3 2 0 2 8 2Ci3CLMS << P < ( < ( < X < . 0 4 TG

:MS AS << ENVELOPES 3 5 0 2 8 2C13CLMS << P < (<*<I<.

18 TG :MS AS << ENVELOPES

3 8 0 2 8 ZC13CLMS <<: P < ( < X < t < . 0 5 TG

:MS AS << ENVELOPES 4 0 2 1 2 2C13CLMS <:< P < (<I<*<.

0 0 TG :8A 38.0 - 38.4 M :V RUBBLY INTERVAL :DIFFICULT TO TELL RX TYPE

428 19 2C65MSQZ BR P #=#a 00 5A

:FAULT ZONE - GOUGE HX TYPE UNCERTAIN :TECTONIC BXIA 4 7 4 4 2 BA02CLCB PX P

18 5G D ( :NO CNTS OBSERVED D U I TO BADLY BROKEN CORE

- : aoul 25 2C35MSQZ q:; P a3 5T

:BADLY BROKEN UP

29 2C25MSQZ << P a+o+ 09 5T :PY + QZ ALSO IN <i - STRANGE HX TYPE - POSSIBLE 2C557 :MINOR GOUGE ZONES 30 2C35MSOZ << P <)C) -q LL 5A :TO 2D LOC 3 1 2C35MSQZ <.: P OO<. 19 5T :TO 2D LOC 32 VEINQZPY P V8V2 24 AW :A FEW SHORT SECTIONS OF 2C35 :NO CNT ATTITUDES POSSIBLE 23 2C35MSQZ <<RR P 12 5A :TO 2C75 LOC 29 2C25MSQZ (,. P 14 5A :TO 2D LOC 29 2D25MSQZ <C P =. L 1 5A :TO 2C L.OC 29 ZD25MSQZ *:< P 13 5A :TO 2C65 27 2D25MSOZ <.< P

820 18 2D25MSOZ << P 10 5A :TO 2D55 LOC

840 17 2C25MSQZ << P 03 5T

858 15 BA02CL AI P CU 12 6G CL

:CL AS AX ENVELOPES 889 31 ZC25MSOZ c:.: P

04 5T - .

:TO 2C22 @ END OF INTERVAL W / CL ON << 937 45 8B02CLCB PIAl! P TC 044

38 46 A. A . :NO CNTS OBSERVED BUT PROBABLY / / TO TC

970 31 2C25MSDZ <+: P <: (< )< )< .

14 5T :TO 2C22 @ START OF INT :TO 2D LOC

1000 25 2C25MSQZ (< P < ) < )

00 5T :CORE HEAVILY BROKEN UP

1033 31 2C25MSQz (i. P < ) < )

04 5T :V BROKEN UP CORE :TO 2C23 LOC

lCl60 27 lD1OQZ <( P <*<LC:. 19 54

1082 20 ZD25RZNB C < P < ) O < .

L R R R R R R A00 1 ALAF ATYP AMTH AUMN R Arm1 A!:iO 1 A001 AOOl A00 1 AGIO 1 A001 A00 1 A00 1 AOO 1 A00 1 A001 A001 R A001 AOOl AOO l AOOl AClO 1 A001 A001

08 5A :UPPER CNT GRADATIONAL OVER 0.2 M - ENTIRE INT MAY HAVE :QZ GRAINS (IE - COMFORMARLE TRANSITION ZONE) :EOH iLd 108.2 :RODS STRUCK WHILE TRIPPING OUT OF HOLE - :BLASTED OFF :COLLAR LOCATION LOST WHILE MOVING DRILL (RE-POSITIONED :WITHIN 0.5 M RADIUS)

EQUITY MINESITE LABORATORY ASSAY WET EXTRACTION A.A. - AU FIRE ASSAYED FIRST RCOVSAMPLE RQD % CU &/TAG G/TAU 7. SF % AS % FE i! ZN

52 :TRICONED - NO CORE 0 0 721.1 0.11

1 1 0 7237 0.10 140 7x3 0.06 170 72P, 0.07 200 7--C

1 -..,a 0.1, ?-. isCl 7236 0. 1;: 266 ,".7 I ->, 0.1:; 290 721.8 (:I" (1:; T-, . i 0 7239 0.0'> 7 E - .-,dCI 7240 0. 07 380 7241 0.15 402 7242 0.11 428 7243 0.15 474 :DYKE - NO ASSAYS 500 7244 0.05 530 7245 0.01 560 7246 0. C105 590 7247 0.02 620 7248 0.01 650 7249 0. DL) 680 7250 !:I . (:).a 7 1 0 725 1 0.01 740 7252 0 . 02 770 7251. 0.01 800 7254 0. (105 820 7255 CJ. 840 7255 0. 1:105 858 :DYKE - NO SAMPLE 889 7257 O . !:I 6 937 :DYKE - NO SAMPLE 970 7258 0.11 1000 7259 0.05 1030 7260 (1. 0'7 1060 7261 0. 19 1982 7262 0. 08

:END OF ASSAYS - END OF HOLE :HOLE TERMINATED DUE TO STUCK RODS - BLASTED OFF @ 200 FT END OF ASSAYS - END (IF LOG

IDEN660201 IPRJ S0UO 00 /SCL LSCL /NAN LNAM / 00 R / 183 L R ,' 210 L R / 240 L R / 270

X86CH268 NQ AUG86DJH G%D AUGBbS38 0. 0 EQUITY SILVER MINES LTD ' SUPERSTITION ZONE - ST GEOCODE 729 MT 72.9 090.0 -45.0 5340.99 7399.62 1100.40 MT. 2MT. I



210 22 2D13CLMS << P ( . ' ~ r $ 12 TG <. :MS AS CC ENVELOPES

240 28 2ClJCLMS .<< P < ' ( < X < $ 08 TG <. :TO 2D LOC

270 25 2C13CLMS << P <.< (( (<.

05 TG <. :HEAVILY BROKEN 25.3 - 27.0 M :TO 2C12 LOC :TO 2D LOC

300 15 2C12CL ( r; P <.<.<. (XI 5G :V HEAVILY BROKEN UP CORE :TO 2C13 LOC -,-,-

2 10 2C12CL <: ; P ': (G: (< ( < (

00 56 :HEAVILY BROKEN UP CORE :TO 2C13 LOC :CP IN ONE SMALL VEINLET :TO 2D LOC

~ ~ . .

:HEAVILY BROKEN UP INT :SAND SEAM REPORTED BY DRILLERS @ 34.1 374 21 2C24CLMS < C P < ( < I < * < (

05 TG :TO 2C12 LOC

393 19 BAO2CLCB AI P 10 46 A$ :NO CNTS OBSERVED :XENOLITH 2C23 W / MINOR CP 38.3 - 38.6 M

420 22 2C12CL <( P <: (<*<#<: (

00 56 :TO 2C13 LOC

450 24 2C12CL < c P < ( < ( < ( < .

00 56 :TO 2C24 LOC

480 29 2C13CLMS < < P < ( i $ < X < ( 02 TG :ONE PZ + PY + CP VEIN

510 27 2C13CLNS <.:: P <.<(<(<.

00 TG :TQ 2D LOC :TO 2C14 LDC

540 28 2C13CLMS << P 08 TG < ( :TO 2D LOC

570 29 2Cl3CLMS << P C (< (< (<. 06 TG < ( :TO ZC14 LOC

600 27 2C13CLMS << P < ( < ( < (<.

Ok TG :TO 2D LOC

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IPRJ SO00 so0 i /SCL LSCL /NAM LNAM / H / L H / L R / L R R / L R / L / L R / L R / L / L R / L R / L R H 1 L R / L / L R / L / L

X86CH269 NO AUG86DJH EQUITY SILVER MINES LTD

364 MT 72.9 090.0 -45.0 729 72.9 090.0 -42.0 MT. 2MT. 1

MT. 2

OVHN :TRICONED - NO CORE 26 2C24MSCL <:< 0 9 GT

:TO 2D LOC 29 2CZ4M5CL << 0 7 GT

G%D AUGBbS38 0.0 SUPERSTITION ZONE - ST GEOCODE

5309.99 7554.41 1137.79


P

P < Z . < * < * < . < (

P r 1 . - -

:TO 2C45 LOC :TO 2D LOC z 0 2C24MSCL <i P <.<+<+ 0 4 GT

:TO 2D LOC :NUMEROUS QZ + PY VEINLETS :LOOKS L I K E A TRACE OF :NATIVE CU? ON FRACTS

30 2C24NSCL .<;< P I 6 GT

:TO 211325 LOC 26 2C24MSCL << P 0 6 GT 1 9 ZC24MSCL << P 0 4 GT

:TO 2D LOCbLLY :OZ + FY VEIN 29.7 27 2C24MSCL << P 02 GT

:TUBE DIDN'T LOOK @ 33.5 M 3 0 2C24MSCL << P 0 6 GT

:2C24 TO 39.0 M :PY + OZ V/ 40.8 - 41.0 (CONT'D NEXT INT) 18 2C35MSQZ << P <)O 0 4 5A

:TO 2C55 LOC :30% QZ + PY - VEINS? PODS? 07 2C35MSQZ << P 00 0 0 5T

:TUBE DIDN'T LOOK @ 46.0 M :HEAVILY BROKEN UP CORE :60% QZ + PY VEINS?/PODS?

- :TO 2C23 LOC 3 0 2C13CLHS << P < (< ( < (

11 TG

- .

:TO 2C3'3 LOC 10 2C24MSCL << P < . < t < t 00 GT

R / 57s L / 600 L / 630 L / 660 L / 690 L R R A001 AL AB ATYP AMTH AUMM R 00 A001 152 A001 180 A001 210 A C l i l l 240 A001 270 A001 297 A001 317 A001 348 A001 380 A001 410 A001 430 A00 1 460 A001 490 AC!O1 520 A001 550 R 561 A001 578 A001 600 A1!01 630 A001 660 AClOl 690 R

:NO CNTS OBSERVED 600 20 2C14CLMS <.<

00 TG 630 28 2C14CLHS <i

03 TG 660 29 2C13CLMS <<

05 TG 690 25 2C13CLMS <<

03 TG 729 23 2C14CLMS <<

02 TG :TO 2C24 LOC :EOH @ 72.9 M

EQUITY MINESITE LABOHATORY ASSAY WET EXTRACTION A.A. - AU FIRE ASSAYED FIRST RCnVSAMPLE ROD % CU G/TAG G/TAU % SB % AS % FE

152 :TRICONED - NO CORE 180 7132 0.15 1.0 0.01 0.005 0.001 2.00 210 7133 0.10 2.0 0.03 I . 0.001 3.46 240 7134 0.03 3.0 0.04 0.02 0.00114.50 270 7135 0.08 5.0 0.04 0.<12 O . O i l l 6.80 297 7136 0. J 1 2.0 0.02 0.005 0.001 3.13 317 7137 0.07 4.0 0.10 0.005 0.00114.90 348 7138 0.03 2.0 0.02 0.001 0.001 2.52 380 7139 0.02 2.0 0.01 0.001 0.C101 6.69 410 7140 0.001 0.1 0.02 0.001 0.001 5.63 430 7141 O.OO1 0.5 0.03 0.005 0.00111.75 460 7142 0.005 5.0 0.20 0.005 0.00118.30 490 7143 0.07 0.5 0.02 0.005 0.001 2.13 520 7144 0.05 0.5 0.02 0.001 0.001 2.87 550 7145 0.07 0.5 0.01 0.ClOl 0.001 2.80 561 7146 0.113 0.5 0.111 0.001 0.001 3.31:) 578 :DYKE - NO SAMPLE 600 7147 0.03 0.5 0.01 O.ClO1 0.001 3.96 630 7148 0.06 0.5 0.01 0.001 0.001 1.63 660 7149 (1.02 0.5 0.01 0.001 O.<101 2.96 690 7150 0.03 0.5 0.01 0.001 0.001 3.18 729 7151 0 . 03 0.5 0.01 i1.001 <1.1:101 1.8.5

:EOH @ 72.9 M R END OF ASSAYS - END OF LOG

IPRJ s o 0 0 so01 /SCL LSCL /NAM LNAM / R / L R / L R / L R / L R H / L R / L H / L R / L R / L R / L R / L / L R / L R / L R / L /

EOUITY SILVER MINES LTD SUPERSTITION ZONE - ST GEOCODE 535 MT 119.5 090.0 -45.0 5185.05 7440.19 1110.85

1195 119 .5 090 .0 -43.0 MT.7,MT.l

MT. 2 MSCLOZPYCPTTASPR CPGY MGHESLGLMO


150 23 2D13CLMS << P < ( < ( < Y 0 0 TG

:MINOR MS SERICITE ALT'N :TO 2C LOC 180 2 8 2D13CLMS << P < ( < (<I

05 TG : V WEAK MS ALT'N :TO 2D12 LOC

210 2 6 2D13CLMS .:< P <: ( < ( < %

0 2 TG <. :V WEAK MS ALT'N TO 2D12 LOC

2 4 0 2 9 2D13CLMS << P < .< .< (

09 TG :V WEAK MS ALT'N AS << ENVELOPES :AMYGDALOIDAL 8C 22.0 - 22.4 :AND 23.3 - 23.8 M W / DISS MG

2 7 0 3 0 2D13CLMS C < P < . < ( < f 0 4 TG

:V WEAK MS ALT'N AS .<< ENVELOPES :TO 2C LOC 3 0 0 2 7 2D13CLMS .<< P G: . G: ( *: $

0 3 TG :TO 2C LOC :TUBE DIDN'T LOOK @ 27.4 M

3 3 0 2 9 2D12CL i< P <.<: ((1s 0 3 4 6

:TO 2D13 LOC :BORDERLINE CALL BETWEEN 2C B 2D 3 5 0 2 7 2D13CLMS <:.< P

00 TG :TO 2D25 LOC

3 9 0 2 4 2D12CL < < P <.<.<(

0 0 4 6 <. :TO 2D13 LOC

420 2 4 2C12CL <: P <.<(<L 00 4G <.

:TO 2C13LOC 450 2 3 2C12CL << P

0 0 4 6 <. 475 2 0 2C13CLMS << P <.<.<.

0 0 TG :MINOR 8 8 FROM 46.6 - 47.5 M :TO 2 C i 5 LOC

506 2 2 BCl lCLCY P I < < P <. 00 9G <: .

:NO CNT ATTITUDES OBSERVED 548 4 2 8AIZCL Pt<:< P

05 AG <. D. :V WEAK C < TEXT

5 8 0 3 0 2C34CLMS <.< P <=<(<. 0 7 TG

6 1 0 27 2C24CLMS <:< P < ( < (

0 3 TG :TO 2C25 LOC

6 4 0 2 6 2C24CLMS << P <+<(<.<. 00 TG < ) < -

:NO POS I D ON TT, BUT SUSPECT I N << WITH HE 6 7 0 2 0 2C24CLMS <<: P <=<+<-<-

00 TG :POOR RECOV FROM 64.3 TO 65.5

7 0 0 2 7 2C390Z <<BR P OO<-<( 0 3 T A < (

:MINOR BR'X. ,LOC 2C24 7 3 0 2 7 2C59QZ BR< < P < ) < ) < - < t

0 4 TA < )

:TT-SL BR'X AT 71.0 7 6 0 2 9 2C44MSCL << P it<:+<. < (

00 AT < $ 7 9 0 2 6 2C34MSCL <<BR P < $<+<-<-

0 0 AT <- <. :MINOR BR'X

8 2 0 1 5 2C34MSCL << P <#<+<.<- 0 0 AT I <- < -

:POOR RECOV 8 5 0 1 4 2C34MSCL <<BR P <)<)<.<.

0 0 AT <. :POOR RECOV

8 8 0 2 9 2C59QZ i < B R P +I+= #+<- 0 9 TA # )

8 5 0 X #i # 4 #2

:TT-PY-SL BR'X FROM 85.0 TO 85.2, TT ALSO OCCURS I N C < I N :REST OF INTERVAL

9 2 0 1 1 2C23CL << P v+< ) 0 0 AG

:TERRIBLE RECOVERY 9 5 0 2 7 2C45 <<BR P V+#+ #a#-

03 #* :TT-PY-QZ BR'X AT 94.8

9 8 0 2 9 2C33CLMS

0 3 GT : TERRIBLE RECDV

100 2 9 2C22CL 08 AG

130 2 9 2C12CL 0 3 AG

:LOC 2C33 160 29 2C12CL

0 9 AG

IDENhB02i l l IPRJ SO00 00 5001 514 SO02 1347 /SCL LSCL /NAN LNAM / R / L R / L R / L R / L R / L R / L / L R / L R R / L R / L R / L R / L R / L R / L / L R

X65CH271 NQ AUGBbRBP G&D AUG85S38 0.0 EDUITY SILVER MINES LTD SUPERSTITION ZONE - ST GEOCODE

5 1 4 MT 189 .9 090.0 -75.0 5339.84 7431 .17 1113 .81 1347 189.9 090.0 -78.0 1899 139.9 090.0 -74.0 MT. 2MT. 1


9 1 OVBN P :TRICONED - NO CORE

1 4 0 2 8 2C11CL < < P < (<8< (<,

0 0 AG :POOR RECOVERY, VERY BROKEN.

170 2 7 2C13CL < < P < . < a < ( < , 0 2 AG

:VERY MINOR OTZ-SER ALT-N. 200 2 0 2C13CL ( <: P < ( < - < t

00 TG :VERY BROKEN

230 2 8 2C23CLMS << P < ( < ( < % < -

0 5 TG : LOC 2C23

270 2 8 2C23GLMS << P < $ < ( < ( < .

0 0 TG :POOR RECOVERY

3 0 0 29 2C12CL < < P < I<-< ( 00 AG

3 3 0 2 7 2C12CL << P < ( < (< -

0 0 AG :LOC 2C23

3 8 0 2 4 2C22CL < < P < (< -

0 0 G A :SOME CORE VERY FRACTURED, ALL BROKEN, SUSPECT FAULT ZONE :BUT NO CLAY GOUGE.

4 1 0 2 8 2C12CL C < P < $ < ) r : ( < . 0 3 AG

:LOC 2C13 4 4 0 29 2C l2CL < < P <t<(<-

0 0 :ABUNDANT SHARDS

470 2 9 2C12CL << P < t < (< -

0 5 G A < - : LOC 2C13

500 29 2C12CL < < P +:(<$<(<-<. 08 G A

:LOC 2Ci3 . LOW ALT'N AND FRACTURING, BUT A B I T OF MINERRL = - ~ 1 . 3 1 2 2C12CL <c:RR P < X < - < (

or: G A :DTZ-PY BR'X FROM 51 .1 TO 51.3

5 4 1 2 7 BC00FL PtCM P CU 50 1 7 TW CL 80

5 7 0 2 7 2C23CLMS (< P <)<+<= 0 0 TG < -

:LOC 2C25

6 0 0 2 5 2C22CL << P <+< (< (

00 AG < X 6 4 0 2 5 2C22CL < < P <=< (< (

no AG 6 7 0 2 7 2C i2CL c: < P < ) i t < (

0 0 AG < - 7 0 0 2 9 2C12CLMS << P <:-<:)<)

09 AG :LOC 2C13

7 3 0 30 2C12CLMS << P <-<:I<*<. 2 1 AG

:LOC 2C13. FIRST REASONABLY SOLID CORE INTERVAL. TRACE CP 7 6 0 3 0 2C22CLMS << P <-<X<$<.

1 2 AG :LOC 2C23

7 9 0 3 0 2C22CLMS <:< P < - < ) < * % < .

1 2 TG :LOG 2C23, CLOSER TO BOTTOM OF INTERVAL

8 2 0 2 7 2C22CLMS (:< P 0 9 AG

:LOC 2C23 8 5 0 30 2C22CL < 3:

11 AG :LOC 2c2.3

8 8 0 3 0 2C22CLMS << 17 AG

:LOC 2C32 AND 2C23 9 1 0 3 0 2C29PZ <<

0 6 7A :TT I N ONE << AT 89.4

9 2 9 1 9 2C33CLMS << 0 3 GT

9 5 3 2 4 2C89QZPY BR 07 AW : QTZ-PY-2C BR' X

9 6 0 0 7 8 C I I F L <<CM 0 5 GW

9 6 1 0 1 2C8SQZPY BR 0 1 AW

9 6 9 0 8 D B l l F L < < P I 05 AG CN

1000 3 1 2C54MS BR< < 18 T A

:BR'X LESS INTENSE TOWARDS BOTTOM OF INTERVAL 1030 30 2C54MS BR<< P #=#=

1 3 TA :PTZ-PY I N Cc: AS WELL

1060 3 0 2C54MS DR.: <: P #+#+ 06 T A

1090 3 0 2C55MS BR< < P #1#+ #? 0 0 TA

1120 2 9 2C44MS <<:BR P ($0 0 0 T A

:MINOR BR'X, LOC 2D 1150 2 8 2C45MS <<BR P 00

1560 2 9 2E2bMS < <: P 1 7 AW

:AS ABOVE 1590 3 0 2E26MS < : P

15 AW :AS ABOVE

1620 3 0 2E26MSCL << P 2 1 AW

:AS ABOVE, SOME CL RIMS ON L A P I L L I 1643 2 3 2E12CL .; < ,* .. P

1 3 GW :ALT7N ?

1650 0 7 8BEllFL PX P CU 0 3 TA CL

1662 1 2 2E12CL < ( P 0 6 GW

1725 2 0 2C22CLCY <i P F / 0 0 GA

:FAULT ZONE, POOR RECOVERY 1750 2 4 2C12CL <: C: P

03 TA :LOC 2C23

1780 28 OC21SC << P 0 0 TA

0 3 AT 1190 3 1 2C35MS < i P B+<

0 3 3T 1224 3 2 2C390Z < <: P < X < ) < - < .

1 4 6A :TT OCCURS AROUND 121 .0

1263 3 9 B B l l C L I < T C P <t 28 2A CM CL 70

1290 2 5 2C39QZ <<AH P <+0 0 0 6A

:SMALL BK'X UNDER DYKE. GRADES INTO 2C34 1320 2 5 2C34MS (( P < )< )< .< -

00 AT <- :TT-SL I N ONE +:< AT 130.0

1350 2 8 2C34MS < < P <) * :$<( 0 0 AT

1380 2 9 2C33CLMS <i P < ) < ( < (

06 AT 1405 2 3 2C22MSCL << P < ) < (

0 9 AT :LOC 2C33

1440 2 7 2C23MSCL << P O(:( <- 0 0 AT <.

1470 2 7 2C22CL ( : P < ) < X <? 0 0 TA <-

1496 2 0 2C22CLCY << P <l< (

0 0 TA :CLAY RICH FAULT GOUGE

1530 3 3 2E26MS << P B= D ( 11 AW D (

:STRANGE ROCK. COULD BE FLOW INTENSELY ALT'D TO SERICITE <$El=<-D-

D (

D= D ( D-D-

D=D.D. D(D.

D t

/ 1780 L / 1800 L / 1829 L / 1840 L R / 1870 L R R A00 1 AL AB ATYP ANTH AUMM

1800 19 2C22CL < < P <+< ( CIO T A

1829 28 2C22CL < C: P <+< (<.

00 TA 1840 11 8BOlCL <<TC PCU 70 < (

04 56 CM CL 75 D- 1870 28 2C42CLMS <<BR P <+i: f<-

00 T A :LOC 2C43, MINOR BR'X

1899 27 2C32CL << P ':#< (

6 0 TA :END OF HOLE AT 189.9. WOULD HAVE LIKED TO DRILL INTO GREENER :HOCK, BUT WE WERE PA2T THE TARGET

EQUITY MINESITE LABORATORY ASSAY WET EXTRACTION A.A. - AU FIRE ASSAYED FIRST RCOVSAMPLE ROD % CU G/TAG G/TAU % SB 7. AS % FE % ZN

91 :TRICONED - NO CORE 140 7287 0.100 170 7288 0.07 210 72E9 0.11 240 7290 0.12 270 7291 0.05 30r:r 7292 0.12 330 7293 0.14 380 7294 0. 09 410 7295 0.07 4 4 0 7296 0.04 470 7297 0.04 500 7298 0.08 513 7299 0.05 541 :DYKE - NO SAMPLE 570 7300 0. 06 600 7301 0.05 540 7302 0.04 570 73113 0. Gb 700 7304 0.07 730 7305 0.09 750 7305 0.05 790 7307 0 . 07 8x1 7308 0. 04 850 7309 0.10 880 7310 <I . c:rq 910 731 1 0.07 929 7312 0.05 q 5 .: 7313 0.001 959 :DYKE - NO SAMPLE 1nc1o 7314 0. 03 1030 7315 0.005 1060 7316 1:). 005 1090 7;17 fj . 1:~j5 1 170 7318 0 . OU5 1 1510 7319 0.02 115'0 7320 0.01

1224 7321 0. 13 1263 :DYKE - NO SAMPLE 1290 7322 0. 09 1320 7.223 0.05 1350 7324 0.12 1380 7325 0.09 1405 - -- 1.2~6 I:). (15 1440 7327 cj.nt 1470 7328 1:). 03 1 500 7529 0.04 1530 7370 0.02 1560 7331 0.08 15VO 7332 0 . 08 1620 7353 0.04 1643 7334 0. CICI 1 1650 :DYKE - NO SAMPLE 167.5 777C

3rd <I. 001 1716 7336 0.02 1750 7337 0.04 1780 7338 0. 0E. 1800 7339 0. 04 1829 7340 0.09 1040 :DYKE - NO SAMPLE 1870 7341 6.03 1899 7342 0.02

:END OF HOLE - END OF SAMPLES END OF ASSAYS - END OF LOG

IDENbB0201 X8bCH272 NO AUGBSRBPDJHGGD AUG86S38 0. C1

IFFiJ EOUITY SILVER MINES LTD SOUTH OF S. TA IL - ST GEOCODE SC!CiCl 0 0 914 MT 266. 7 090.0 -45.0 5939.73 7480.12 1201.18

/SCL LSCL /PIAM LNAM / R / L R / L R / L R / L R i L R / L R i L R / L / L R / L R R / L / L R / L R / L i L R /

1713 266.7 090.0 -45.0 2667 266.7 090.0 -45.0

HT.2MT.1 MT. 2

MSCLDZPYCPTTASPR CBGY MGHESLGLMO

122 OVZN P :TRICONED - NO CORE

186 2 0 3G11CL i <; P < (< -

0 0 AG :VERY BROC:EN, RUSTY. NO RECOVERY AT ALL FROM 13.6 TO 14.2

220 20 3 G l l C L .. , .:.. i P C / 7 0 < ( < $

00 AG BD 7 0 :LUC 3D, POOR RECOV

293 25 3 H l l C L i <: 0 0 AG P < (0

:POOR RECOV, LOC 3G 332 23 3G11CL <:: .: P <-<$

(>(I AG :POOF: RECOV, VERY BROKEN, SUSPECT CHIPS FROM FARTHER UP HOLE

367 20 3Hi1CL !, (HR P .:-.I y 0c1 AG

:SOME 3H MAYBE BRECCIA. RUST ON FRACTURES ENDS 395 27 8C11FL .: .: p 1: P i (

13 GW :CONTACTS NOT PRESERVED

4;1 23 3 H l l C L .:. .. \. , P < $

0 0 AG :FAULT GOUGE AT 41.0. LOC 3H21

463 29 3A21CJZPY (< P < - < * 03 AW

492 29 3811OZ < .<. P <-.< (<:. * 13 AW

:OCCASIONAL CHERT CLAST 540 3 3 3A21OZ G: c P <;-.! .. - C $

0 6 AW :TYPICAL 3, CLASTS UP 'TO 2.0 CM, SOMETIMES CLAST BORDERS : INDISTINCT. 3A-3B CONTACT GRADATIONAL

553 11 3 B l i a z , '.. P , ... :

0 3 G A 580 25 3AllCJZ <% +., P *..-<-<: (C. , ..

15 AW :CLASTS SOMETIMES INDISTINCT, ONE TINY SFOT OF CP I N <.<

.. ,.. .:. . P 610 28 3A l lDZ . .. c i -.: ; ( ( $ 1; AW

:LOC 38 AND 3F INTERHEDDED. BLACK TARNISH ON SOME PY 640 2 8 3k21QZ : .~

: .. , .. P <: -.:; *<: )

09 AW , ... P 670 29 3A21QZ c .; <. -*.'-!, . i?

08 AW :POSSIBLE TT I N <<

719 4 1 3AllCJZ \ -. P i.-<-<)<' * , ..<. . .I

0 9 AW :8A FROM 58.0 TO 68.2. LOWER CONTACT GRADATIONAL OVER 0.3 M

7 5 0 39 2C22CLMS .<< P < X ( ( < * 09 TG

:LOC 2 C 2 3 790 3 0 2C22CLMS <<: F' <%i)i)

1 4 TG :LOC 2C23, ?C24

820 30 2C lZCL I IS << P < *.:.I ) .< ) d.: . .< - 1% TG

1 4 TG :LOC 2C23, 2C24. CP I N ONE << AT 82.6

6 8 0 2 9 2CI;zCLMS .<.< P <:-?:#.::=<-<,

09 GT :LOC 2 C 2 2 i

910 30 2C23MSCL (.< P <(<)<:+

11 GT :LOC 2 C 2 2

938 28 2 ~ 2 3 ~ s ~ ~ <.< P <- . ; : )< )<-<? !j& GT (: .

:LOC 2C22, 3 2 2 4 . T T I N <<, COULD BE SPECULARITE 976 38 3A2013Z .:; <: P <l<) ( -

05 AW < . :LOWER CNT NOT OBSEFNED DUE TO BROKEN UP [:ORE

1OOO 22 2C23CLMS <:< P < ( < : ) < ) < -

1 1 TG :TO 2 C 2 4 LOC :CL ALSO AS i: ENVELOPES

1036) 31) 2C24MSCL < ( P <: -.< ) < ) <: * 06 GT < -

:TO 2 C 3 4 LOC :TO 2D LOC 1060 29 2C34MSCL <.< P < (<*<*<:*

10 GT <. :SPEC. HE

1090 30 2C24MSCL ::<: P < ( < $ < X < - 16 GT

:TO 2 C 1 2 LOC 1170 30 2C24CLMS << F < (<$<#.:-

05 TG <-.I. :TT OR SPEC HE (BLUISH GREY COLOR W / METALLIC LUSTER :TO 2C?2 LOC :TO 2D LOC

1 1 6 1 4 1 ~C~:CLMS <( P CL 035 <:-<#<:*<:. 7 2 TG < -

:TO 2 C 2 2 LOC :CB << X-CUTS t2Z + PY << 1180 1 9 3A20t2Z .< .: F' < . < % < I

05 AW :SOME < < ARE VUGGY

1215 36 3A2OaZ <I .. / .. P <.<:)<:)

09 AW <. :SPEC. HE? OR T T

1 2 2 4 08 8A12CLCY < < P I P 07 TG

:MICRC-PORPHYRITIC TEXT :NO CNTS OBSERVED 1250 25 3820QZ ,.. ,.\v'U ... a F.' <:#($

11 AW 1250 1280 29 3AZOClZ i . i .. P <$.<$<:-

05 AW 1280 1310 28 3A10QZ , ... ~, . < P < ( < (

22 AW 13i!:l 1340 30 3A2ClCIZ .., ... (.. , P < I < : )

25 AW 1340 1358 18 iA2OCIZ .... ,, ... .~ P < ( < (

12 AW :LOWER CNT GRADATIONAL OVER 0.3 M

1358 1387 28 3R20ClZ .<; .: F' ~ : # 4 : # < : (

1 CI AW :2C FROM 138.3 - 138.7 M. W / CL ON .<< :LOWER CNT IRREGULAR :(NO ATTITUDE) - 2C/3A CNT

1387 1397 10 3A2OaZ q:: c:: P 09 AW :LOWER CNT GRADATIONAL OVER 0.2 M

1397 1410 13 3B100Z :.: i 8 D P LID 05 AW CL. :KC. CHERT PERBLES

1410 1430 16 3A100Z .: ,.. I.. '... P

05 AW 1430 14b0 30 ~ 2 0 a z i .: P

24 AW 1460 1490 30 3A20QZ i < P , ..

15 AW 1490 1528 37 3A30aZ c:: <: P

18 AW :LOC 3A20

1528 1550 21 2D23MS c .; P 04 TA :UPPER CONTACT SHARP! HUT IRREGULAR

1550 1500 30 2D23MS << P 08 TA

1580 1610 29 2D24MSCL i< P 12 TA

1610 1640 30 2D12CLNS << P V / 11 TA :LOC 2C23

1640 1670 30 2D13MSCL <(BR P V / 12 TA :LOC 2C23, MINOR BRECCIA

1670 1700 J0 2C23MSCL ..:.< P 18 TA

1700 1730 30 2C34MSCL i< P 21 AT

1730 1754 24 2C34MSCL << P 12 AT

1754 1790 36 ZD23MSCL << P 23 TA : LOC 2C23

1790 1SZO 30 2C34MS < ; P 11 AT

1820 1850 29 ZD23MSCL << P 14 AT

:CLAY RICH FAULT BX AT 184.6 1880 29 2C34MSCL .::< P < ( ( ) ( ( < .

09 AT :CLAY RICH FAULT BX AT 197.1

1910 30 "EMS .< . ' P <+.'=( (<? 11 AT < (

1940 30 2C45MS ..,I, ... .\ P .+.<=c (<? 12 AT < *

:FINE HE I N i*:, COULD BE TT AS WELL 1970 30 ZC55fiS (CBR P <+(=(-<?

15 AT < - 2000 28 2C44MS c ... i \ P <.:.<(<+<.<.

09 AT 203!:1 29 2C44MS <:<BR P < ( C ) < . < .

13 AT < - :MINOR BR'X

2!:16O 30 2C55MS ( c:: FIR P <:LC)<-.<- 15 AT <.

2090 30 2C55MSCL <:.::EjH P <: (<: (<).<-*:-

11 AT < - 2120 27 2C35MSCL <: <: P :-<: (<)<.<-

03 AT <. :LOST CORE AT 211.2 SUSPECT MORE TT THAN VISIBLE I N THIS :INTERVAL AND THE FEW ABOVE. TT COULD BE I N SMALL ;:C WITH : BLUEIISH TINGE

P 2150 29 7C34MS ii .:: * <: ) <: . <: - 12 AT

2191 31 2C35MSCL <<BH P .:$<+<-( (

18 AT <. :MINOR BR'X

2207 28 8R1OFL ((OM P CU 30 < ( 2 1 56 CL 30

2236 21 2C65MS ( <: BR P #)#+#.#- ,

03 AT <- :SANDY FAULT ZONE FROM 222.9 - 223.6

2286 50 8810FL .<.<EM P < ( -7 ,r 1 5 G CL 40

2310 23 2C55NS .:; (HR P <( t i )< ( < X 13 AT < -

:MINOR RR'X. BA FROM 230.4 TO 230.5 2335 15 2C55MS RR<C P # ) # = I # . # .

03 AT 2359 23 2C55MS <: ': E)R P < (<+<:-<-

17 AT :MINOR BR'X

2375 17 8A10 C<:CY P CU 30 C ( 13 AG CL 65

2377 02 2C55MSCL C<BR P <I#+(:=<.<.<. 0 2 AT <.

:MINOR BR'X 2394 17 9010 < <: CM P CU 50 c:(D(

11 66 CL 65 2410 16 2C55MSCL (:iBR P < ) #=#+#-#.

09 AT #. #- :LESS BR'X TOWARDS BOTTOM OF INTERVAL

2410 2448 38 BBlOFL <<TC P CU 35 < ( 25 46 CM CL 50 D-

2448 2480 30 2C45MSCL <s;HR P < # < I < + ( ? 05 AT < t :LOTS OF (i HE, MAYBE MINOR TT IN WITH HE

2480 2510 29 2434MSCL C,: P <)<)<+.<.<? 00 AT ,: - :AS ABOVE CONCERNING HE

2510 2540 29 2C35MSCL i<BR P .< ) <; - .* - <? 11 AT C - :LOC 2C55, BUT MINOR. AS AHOVE CONCERNING HE

2541:) 2570 30 2C23HSCL (< PBD 50 ) ( (? 06 AT .: - :GRADES INTO ZC12, MINOR 2D - BEDDING CONTACT

2570 2600 30 2C24MSCL .<.< F' <:)<; ( < (

05 AT .: . 2671) 3CI 2C23MSCL .<<: F <;+<-<;-

00 GT :GREEN F:OCK, VERY LITTLE PY, NO HE

2657 37 2C23MSCL <( P <+< (C ( 03 GT :GRADES INTO 2C12 AT END OF HOLE - LAST 0.5 M :END OF HOLE @ 266.7

EUUITY MINESITE LABORATORY ASSAY WET EXTRACTION A.A. - AU FIRE ASSAYED FIRST RCOVSAMPLE RDD % CU GITAG GITAU % SH % AS % FE % ZN

122 :TRICONED - NO CORE 186 7343 0 . 05 1.0 0.02 0.001 0.001 3.86 0.005 220 7544 0. 08 1.0 0.02 0.001 0.0i!l 3.61 (1.005 293 7345 0.16 0.5 0.05 0.001 0.005 3.51 0.01 777 .. ii 7346 0 . 12 0. 5 O. 06 I:]. 001 0 . i:Kjl 3. 50 0. 1:11:15 367 7347 0.135 0.5 0.01 0.001 0.ij01 3.86 0.005

END OF ASSAYS - END OF LOG 395 :DYKE - NU SAMPLE 4j l ) --

/ ~ 4 8 0.12 460 7.349 cr.03 490 7350 (I. 1115 520 735 1 0.07 =c - JJC~ 7352 0.09 5RQ 7353 0.06 6 1 0 7354 0.11 640 7355 0.04 670 7356 O. 06 700 7357 0. 05 730 7'1.58 0.06 760 7357 0.09 770 7360 0.08 820 736 1 0.05 850 7362 0. ?<I 8e0 7363 0.09 910 73i4 0.04 940 7365 11. Ob 970 7366 <I, (1s

1000 7367 0.09 1030 7368 0.24 1 l:l60 7 7 . ,009 1:). 24 1090 7370 0.10 1120 7371 51. 14 1150 7372 0.14 1180 7373 1:). 03 12011 7374. 0.03 1216 7775 , ... . -, 0.01 1224 :DYKE - NO SAMFLE 1250 7376 0.02 1280 7377 0.08 1310 7378 0. 154 1340 7379 0. 06 1379 7380 C! . (13 14OO 7381 I) . .,T L -,

1450 7332 0.03 1460 738; 0 . 0; 1490 -- . . -, ;.>a4 LI. C i j

1520 7385 0.02 1550 7584 0.14 1500 7387 0. 05 1 6 1 0 7388 0.04 1640 7389 0.09 1 b7il 7390 0 . 1 0 1 700 739 1 0.14 1730 7392 0.07 1760 7393 0.13 1790 7394 0. 17 1820 7395 0.17 1350 7396 0.06 1880 7397 0.28 1 9 1 1:) 77 , r . i 5 d 0. 1 :; 1940 7399 O.X 1?76 ;400 il.i.19 2000 7401 0.04 203i:r 74112 0. 14 2060 7405 0.11 2~190 7404 0. l i t

2 120 7405 13. OT 2 1 50 741'16 0. 158 2181 7407 0.13 2209 :DYKE - NO SAMPLE 2 2 3 ~ 74051 0. 21j 2286 :DYI:KE - NO SAMPLE 23 11:) 7409 0.15 23:; 7410 0.91 2353 731 1 0.06 2375 :DYKE - NO SAMPLE 2377 7412 0. 1j2 2394 :DYKE - NO SAMPLE 2410 7413 0.03 2448 :DYKE - NO SAP1PL.E 2483 7414 (:I . il 6 2510 74 15 0 . h 5

IDEN600201 X86CH273 NQ AUG86RWW G&D AUG86538 0. 0 EOUITY SILVER MINES LTD SOUTH OF S. TAIL - ST GEOCODE IPRJ

5000 0 0 SO01 541 SO02 1584 SO03 2759 /SCL LSCL /NAN LN AM / R / L R R / L R / L R R / L R / L R / L R / L F: R R / L R / L R / L Fi / L R / L R / L R

541 MT 343.2 092.0 -45.0 1. 584 343.2 1:192.!:1 -44.0 2759 343.2 092.0 -43.5 3537 343.2 092.0 -43.5

MT.2MT. 1 MT. 2


OVBN P :TRICONED - NO CORE, CASING TO 21.3 25 3A21:laZ CT,;< P :) <:tR. 12 2 ?A

:MAINLY BOULDERS AT BEGINNING OF INTERVAL :SOME FRACTURES CON- TAIN CLAY 29 3A30QZ CT/ <: P < < B. 0 6 7A

:5OME THIN INTERBEDDED 3F AND 3B :CLAY PRESENT AGAIN 28 303002 CTI<: P C) i$B . <I o 7 A

:AGAIN SOME CLAY FILLING FRACTURES :CP ONLY AT 27.2M :SMALL ZONE OF 36 AT END ON INT. 29 3Al0OZ CTi: i P ~ : Z < W . 11 ?A

:CP ONLY AT Z1.9M :AGAIN SOME INTERBEDDED ZF AND 3B. 29 3A20OZ C T i i P S: ) < t .<: . 06 7A BR

:AGAIN SOME INTERBEDDED 3B :SMALL BE'N I N VEIN AT 35.6H. 29 3A20QZ c T i i P < + . < X (

14 7A :AS ABOVE 28 3A21QZ C T i i P .;:-C+<LB> 0 5 bA

:AS ABOVE :CL ALSO PRESENT :SMALL ZONE OF 3F FROM 39.8 TO 40.2 :CP ONLY AT 40.5 M :.3M OF 8C HEAVILY ALTERED TO CY AT 41.7M.

29 3B210Z CT.; i P <.'-.:;+< ( <

09 6A :SOME CHERTY PEBBLES SCATTERED THROUGHOUT INT. 28 3B21QZ CT< C F' <-<+.< (<.

11 767 :SOME INTERBEDDED 2C :ALSO MUCH 3A. 3 6 3BZlUZ CT<< P < . < + . : x < . 11 7A

:CP ONLY AT 49.3M :AGAIN INTERBEDDED 34. 21 8b00 0 8

:CLAY FHENOS PRESENT :CONTACTS NOT MEAS. DUE TO BROKEN CORE. 28 3B l lQZ CT<-: f' < . O < X B 0 5 6 A

:CP ONLY AT 56.8M :AGAIN INTERBEDDED 3A 29 3A21DZ CT<:C P <%$:($<. 0 8 7A

:SOME INTERBEDDED 3F

630 27 3AllOZ CT<< P 03 7A :AS ABOVE

660 28 3A20QZ CT<< P <+<# B. :TT ONLY AT 63.2 M

690 28 3A2082 CT< < P <+<$ B? 05 7A :BLUE TARNISH ON PY.

720 29 3AllQZ CT.I.: P <.<+<(<. O 6 7 A :STARTING TO GET 2D MIXED IN WITH 3A.

750 28 7C33MS 02 ST < ( P O < + < $ C . :MAINLY 2D AT BEGINNING OF INTERVAL.

780 28 2C32MS < C P <:I 25 <)(+<)<.B. 05 TG i.

810 29 2C32CL <: <: P < ) <:+<) <. 09 TG <.

840 28 2C21CL , , <. <.. P .:)<+<$

03 GA :SOME INTERBEDDED 2D

870 29 2C33MS .. , , .. , % P ~O<=,<+<. 05 GT B.

900 28 2C22CL .( < P ,:+<=.{)(. 0 3 TG 0) U-< . :HE IN NEEDLES - MAYBE SUME TT MIXED IN.

930 29 2C32CL < .< P <+<=(=B.EI. 05 TG <: - U. :HE AS ABOVE :CP AND TT MAINLY IN LARGE aUAHTZ <:<

960 29 ZC22CL .< .. c % P < .:: 25 .:+!:=.<)(. 08 TG a ~. .

990 29 ZC32CL < ( P <::+.:=<:) '. C ? 14 TG < ) < - :HE AS ABOVE, SOME IN PATCHES.

1020 29 2C21CL .: .: P c:(C+i)<. 14 GA < (

1050 29 2C22CL <.. , ,... ~. P <)<=<+ 08 TG C. :SOME MS ALTERATION.

1080 29 2C21CL ir: P Cl 62 < ( < ) i t 0 9 AG :CONTACT MEASURED BTWN A2C AND G2C WHERE 62C HAS STRONGER ALT.

1110 29 2C21CL ,:< .( ~ P .., x % < > ( ;. +.- ) c - 09 TG 4: ( El..:. :HE IN CE-CB VEIN :PAKT OF INT MAGNETIC

1140 29 2C22CL .. .. P <, <> if<+<).:. 1s -r G B)B. :SOME COKE QUITE MAGNETIC

117i) 29 ~. , .. .. P 2C22CL ... .. ;:+<:+().:. 11 TG '%. . a(.:. :AS ABOVE (MAG NOT AS STRUNG).

1200 29 2C21CL i ( P c: (<:+<$

04 TA <- B-a. : MG AS ABOVE

1230 28 2C23M5 c ( P <(,;+<:)<-

0 9 GT <. :MG FOUND WITH PY-DTZ VEIN.

1230 1260 28 2C22CL . ..' '.. ,. P <).:+<) 0 2 TG B- i .

:AGAIN CORE SLIGHTLY MAGNETIC 1260 1290 3 0 2C22CL r. ... ,, .% P < ) < + < : I < .

14 TG B. <- :AS ABO'JE

1290 1320 29 2C23CL < < P < + < + < I < . 11 TG B-< .

:AS ABOVE 1320 1350 28 2C33CL i < P <)<+<+!I-<?

0 6 TG <. 0 . i - :AS ABOVE :HE SUSPICIOUS - MAY BE SOME TT I N I T

i l i=.:)B.<? .: . 1350 1380 28 2C44MS .: .:

0 4 AT :AGAIN HE MAY CONTAIN TT

1380 141i:l 28 2C44MS (<

0 4 GT :SL ONLY AT 139.OM

1410 1440 29 2C44MS < <: 14 GT

:STARTING TO GET GOOD MS AL 1440 1470 28 2C44MS <.<BR

0 6 GT : . lM BHECCIATION AT l 4 b . 9

1470 1500 28 2C33MS .: .. .... <..

11 TG

.T'N. :CORE SLIGHTLY MAG AGAIN P < ) .:=<:+.:. .: .

:.3M RC FROM 148.2M. :TT ONLY AT 148.6M 15UO 1520 29 2C44MS i c P CU 35 (+.::=i+.<.~.

17 AT Q. :UPPER CONTACT IRREGUI.AR :.7M OF 8C FROM 153.7M

1530 1560 29 3A410Z <: <: c.; P < :$<+(= i t 14 6 A

:BEGINNING 1M MAINLY 2C WITH ALT'N 4 :GHAD'NAL CNT BTWN 2C & 3A 1560 1590 2 0 2AJOGZ .< < CT F' C + ( )

11 7A 1590 1620 26 3A30Q; i (CT P *:+< (

12 7A B- :HE MORE COMMON THAN TT BIJT HE MAY CONTAIN TT (CAN'T TELL)

1710 1740 29 3A2ijQZ <.;cT P .:+< ( <. OY ?A , .

:SOME INTERBEDDED 3B. :ALSO SOME 2C FRAGMENTS. :TT ONLY AT 173.5M.

1746 1770 28 3A31QZ <: c CT P s.. . .4 . +( .).:. 11 7A *: .

:TT I N SMALL CB'TIZED VEINS 1770 1800 28 3A31QZ < r: CT P <.(+',+ i.

0 4 7A <. 1800 1830 2 8 3A3lPZ (.;cT P <-<+<=

:SOME INTERBEDDED 2 0 AND SOME 2C FRAGS. 1830 1 8 5 1 ~ 2 9 3A30PZ (<CT P <.<+<= B.

0 8 BA :SOME TINY SILVER SPECS BUT CANNOT TELL WHAT?

1860 1890 2 7 3A3202 <: i CT P .:-<+<:=(. 1 1 7A H F:

:FINAL 1 . lM OF INT 2C WITH CP AND ACT'N 3 :GOOD . i M BRECCIATION AT BEGINNING OF 2C

3 0 2C43MS .:< P <+<+<$<)<:.

1 8 GT <. :TT MAY BE MOSTLY HE BUT GAVE A DULL GRAY STREAK (V. GRANULAR)

2 8 2C34flS .< .c P :+<=.;)<. 08 AT <. 2 8 2033MS .:: < P <+<=<+<. 11 T A

:SOME INTERBEDDED 2C :FIRST PART OF INT ZC,LAST 2/3RDS 2D 2 9 2C44MS .: -: [ j ~ P <:#<:+<:)<- 15 GT < - B.B.

:BIG PATCH OF CP AT 200.8M :CORE SLIGHTLY MAGNETIC 7 9 - 2(:mNS ?: .< P <:-<+<)in 15 TA

:INTERBEDDED 2C AND 2D 2 8 2C44MS .: i P *:)<(<:(<.<.

0 9 GT <. :LARGE QTZ-PY VEIN AT END OF INT. QZ PART CONTAINS GRAY-BLUE FLECKS-MAY BE TT BUT TOO SMALL TO TELL

2 8 2C45MS < .: P <:)<=<:)<*

0 9 AT B. <. :THIS TIME HE AS BLUE-GRAY PATCHES I N BTZ-VEIN 2 9 2C45NS c L; BR P <.(+(=(-<:. 14 AT B d .

:ALONG WITH << PY ALSO FINELY DISSEMINATED PY. 2 7 2C34MS < < P <: +.... -~, , ...-. ) < .

0 5 T A 2 8 2C44MS P .:) <=<+ 0 5 AT

:LARGE TPZ-PY VEIN WXTH 2C FRAGS AT 215.7M ALONG WITH BRECCIA. 2 8 2C43MS I (I

~ .. P <*;:+.:)<- 04 TA 2 9 2C33NS ~ .. P <+C=<+ B. 3 ,' .. ..

0 8 TG B- :TT LOOKED L I K E I T HAD HE HUT DIN 'T GIVE RED STREAK XI 2C44MS : < P ?:)<=<:)<.

0 7 T A .: . 30 2C22MS ( c P < ) < + < ) < )

15 TG 27 ~ 4 4 ~ s C ~ I J R P <t(+<+<$

15 AT :BIG PATCH OF CP AT 237.5M.

2430 3 0 2C44MS <: < P <)<=<+< ( 0 9 AT

:SOME INTERBEDDED 2D. 2460 29 2C44MS <<BR P < ( < = < = < I < -

0 6 AT :STRONG << AND BRECCIFTION THROUGHOUT INTERVAL

2490 2 9 2C45MS '..:BF. P <,+:=<=<)<(

0 6 AT < - :SOME TT MAY CONTAIN HE AND VISA-VERSA - NICE CORE!

2520 2 9 2C45MS <<: P c:) .<+.<=<: (<:-

1 4 AT :MOST TT AT BEGINNING OF INTERVAL

2550 3 0 2C44MS G: < BR P ()<+(=<:-(.B? 1 7 AT B-

:MOST BLUE-GRAY LOGGED AS HE 2580 2 9 2C45MS <<B4 P ,I - ., - .-I,-<. <-

12 5T <: - :HARD TO GELL I F HE OR TT - BURGUNDY STK.

2610 2 9 2C44MS .< (RR <..:+(+<.<, 1 2 AT < -

:AS ABOVE 2640 2 8 2C44MT ., 3 -. -.. P (.(=<)<.<-

1 2 AT 2673 30 2C44MS (<BR P <. .::=<+B. ‘:.

0 6 AT :CP ALSO I N <<

2705 3 1 8A20CL <<BR P CU 7 0 2 1 5G

:FELDSPAR PHENDS :BR OF 2C INTO PART OF DYKE 2740 3 3 2C44MS .< '. BF: P <.<=<+ <.

1 7 AT < - :SOME 8A I N SAMPLE AT START OF INTERVAL

2770 2 6 2C44MS .< ( BR P <.<=';+ <. 123 AT <.

2800 2 8 2C44MS <I BF. P <::<=<+<.<. 05 AT < -

2830 2 9 2C44MS i < B K P < . ,./=.,- .k \-Q.Q. 1 4 AT <.

:SOME BLUE-GRAY HARD TO TELL BTWN HE t TT 2860 2 7 2C44MS < < ElK P <. (=<=B-B.

1 1 AT B. 2890 28 2C4SMS <:<BR P ‘ : . < : = < + < . < .

01j AT 2920 2 9 2C44MS (':BK P <.<=<=B.B.

05 AT R . 2950 2 9 2C44MS c: l BH P <.<+<=

0 6 AT :GOOD ALT'N BUT ONLY PY MINERALIZATION

2980 2 9 2 ~ 4 4 ~ ~ +: .:: BR P <.<=l;+

09 AT :2 PY-OTZ VEINS ABOUT 2CM WIDE - NO MINERALIZATION

3010 2 9 2C44MS .< <: BR P (=<= B. 06 AT 0.

28 2C44MS c : BK P (. (=<:= 11 AT 8. 29 2C44MS ((BR P (.(+(= 04 AT B. 29 2C44MS i<BR P i . .<+<:+ 06 AT 77 A, 8Ali:lCL <<A* P CL 50 <: - 18 TG <: . :UPPER CONTACT NOT MEASURED DUE TO BROKEN CORE :FELDSPAR AMYGDS 25 2C44MS I<BR P (..:=:+ 09 6T < -

: SOME CH PRESENT IN i ?: 14 SClOCL (<:A* P <: 1 08 TG .: . B. :CL AHYGDS :BANDS OF DARK GREEN (ANDESITE) 05 2C44MS <:<:BR P i-,- x - x -

0 3 AT < ? :SHORT SAMPLE SINCE ENCASED BY DYKE ON TOP & BOTTOM 37 8A1OCL <<A$ P O<. 15 5G ... . Ei ( :CL & HE ANYGDS :SON,: TYPE OF SOFT RED MINERAL (? )

3224 3250 24 2C45MS ... ... ..% ..% B3 P ( +<+

06 AT 3250 2280 27 2C34M3 < < P (-.:+<:+

05 7T :CORE STARTING TO LOSE FRACTURING

3280 5310 29 2C33MS ': < P <)<+<)B. 09 TG i. :SOME CLY F'RESENT :ROCK TURNING QUITE GREEN

3310 3326 15 2C22MS ( ( P ?:+<=?:)::.

03 TG . . ~ -

3325 3349 22 ElAlClCL << P i - 12 46 :CL PHENOS

3349 3380 29 2C;2MS < < f .(+<+<)

08 TG <. 3380 3410 27 2C32MS <1BR P <+<+iSB.

02 TG i - :SOMETHING CAUSING A PURPLE COLOR (UNIDENTIFIABLE MINERAL)

3410 3432 21 2 ~ 2 1 ~ ~ i.! % < P <+<+(SO- il 5 AG :CP BECOMING MORE PROMINENT :END OF HOLE - END OF LOG

A001 ALAB ATYP AMTH AUMM R A00 1 A001 A00 1 AClCll A001

EQUITY MINESITE LAHOEATORY ASSAY WET EXTRACTION A.A. - AU FIRE ASSAYED FIRST RCOVSAMPLE RQD % CLI G/TAG G/TAU % SB % AS % FE % ZN :TRICONED - NO CORE 10 21.3

213 243 7441 0.0'0 0.1 0.010 0. 005 0.001 1.270 0.001 243 271) 7442 I . 1 . 0. ; 0. 02 0. 005 0. <101 1. 57 0. ClOl 270 3~10 7443 0.0h 0.5 0.0': 0.i105 0.001 1.57 ir.1>01 300 390 7444 O.Ob 0. 1 0.01 0.Cl05 O.CIIS1 1.24 0.001 3x0 ~ A U 7445 0.04 0.1 o.01 0.005 0.1:mt 1.09 0.Q01

I . 5 . I l l 2. 13 0. .00 0.005 0.001 1.53 0.001 0. <I05 0. C I C l l 1.21 0.001 0.005 0.001 1.69 0.001 : : : 1 1:1.:111 1 . 1 C1.001 I). l:105 I). 005 1 . 12 0. 005 I . : 1 1 I . : I : . 56 0. C105 0. 0i15 11. 005 4. 39 0. 01j5 . . . o. i .1~5 O. ~105 3.53 <I. 005 0.005 0.01 3.71 0.005 0. 005 0. 005 3. 54 0.1jil5 0.1305 0.005 4.96 0.005 c j . 005 0. 0115 4. 78 0. Oil5 0.005 0.005 4.16 0.005 0. Qi); (1.005 4.05 0.(:1<15 0. 005 0. 065 5. 65 0. 005 0.005 r:1.005 4. 7 3 0. 005 0.005 1j.01j5 3.81 0.005 0.005 I:I.O~I~ 3.14 0.005 13.005 0.005 4.41 0.005 0. i 1 1 E (I. i1O5 3.89 0.005 0 . m o . m 5 4-15 0.005 : 1 . 1 Cl.01 4.20 0.01 0.01 0.005 4.81 0.005 0. 005 0. 005 4. 19 0. OCl5 0.005 0.005 4.28 0.005 I:I.C13 0.005 4.48 Cl.l : I l 0.03 0.02 4.26 0.03 Cl.05 l:l.Ol 4.4& 0.07 0.01 0.01 4 . ~ 2 0.03 0.01 0.01 4.65 0.04 0.01 0.01 5.10 0.04 0. I:)? 1:). i105 3. 94 0. 07 0.01 0.005 5. 12 0.01 0 . 01 (1. 01 2. 32 I:]. 1x15 0.04 0.01 1.59 0.01 0.I:IZ 0.02 2.97 0.(,l 0.01 0.0ij5 4.29 0.01 0.02 1 . 1 3.33 <l.<l5 0.02 0.005 1.82 0.01 0.01 i:r.1:1!:1:15 1.95 0.~14 0.01 0.005 4.26 0.02 0 . 01 0. 005 6. 1l:l 0. 005 0. 13135 (j.Uij5 5.54 1).005 il. 005 (11. l:ll:l5 2 . 83 !:I. O<15 0 . 1 ~ 0.1j1:); 3.48 n.Cll 111. 605 (1. 1:1<15 3. 75 <I. 1:11:)5 Cl. l:li:r; lj. lj95 3.37 11. c105 0. 01 I:. i l l 3. 4 (1. 1:1!:15

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iSCL LSCL /NAN LNAM / R / L R / L H / Fi / L R / L R / L H / L F< R / L R

L Fi / L R / L H / L R / L R / L R /

EQUITY SILVER MINES LTD SOUTH OF S. TAIL - ST GEOCODE 375 MT 310.9 090.0 -45.0 6131.61 7484.28 1224.09 1276 310.9 <)90.C1 -44.0 2375 310.9 090.0 -42.0 3109 3151.9 090.0 -42.0 MT. 2MT. 2

MT. 2 MSCLPZPYCPTTASPR CHGY MGHESLGLMO

a 1 OVEN P :TRICONED - NO CORE

105 24 3FiOPZ <( P <I<% 00 S A :FE STAINING ALONG FRACTURES, SOME MANGANESE OXIDATION

127 2ij 3FlOPZ '.. ... . ,% ... P .:+< )

02 S A i-

:AS ABOVE 140 NREC P 140 :MISLATCH - NO CORE :SOME QZ PEBBLES 170 25 3FlQI3Z <: ('R P i + C )

00 SA :SOME FE STAINING ON FRACIS :ALSO SOME 3D

200 25 3F10QZ ... < .... c., P i ) < l 02 S A :AS ABOVE

2 27 3F10QZ i / ,: . P FB 5Ci <+<)

03 4A :FE STAIN HAS JUST ABOUT DISAPPEARED :SOME LARGER FRAGMENTS

260 28 3F10QZ < .:; P .<+< ) 05 SA <: - :BEGINNING OF INT FE STAINED, SOME AT END :MANY CLASTS TOWARD END OF INT.

290 27 3F11CL. .:.:cL P I=,+<: ( 00 AG .:; ( H.Y. :AGAIN SOME 3D MIXEI) IN :CORE SLIGHTLY MAGNETIC

320 27 3F21CL <*:EL P $:)<+<) 03 AG :FE STAINING ALONG FRACTURES

350 27 3F21CL : .:. P ,<)<+<I 03 3A :MINOR FE STAINING

380 28 3F32CL ,.. ... ... .., P .:+<+<. 06 T A :AS ABOVE

410 23 3F43MS P <:)i+OB.B. 05 AT :AS ABOVE :GRAY SULPHIDE - MAYBE TT

440 27 3F42CL. i ./ ... . .. P (+<=<)

05 TG i _ :AS ABOVE

470 28 3F33MS <<BR P .:)<=<l: 05 TG <- :AS ABOVE

500 27 3F33MS <: < P .:+.:+<)El.

02 [i T < ( :AS ABOVE

530 27 3F32MS ,, .. %. c.. P *:)<+<$H.B.

05 GT i ( 550 27 3F34MS ... ,

..< c.. P <: (<I+<:- 00 GT

590 29 3F33MS ( .: P FB 30 <+i+(f 00 TG <.

520 28 3F33MS < c:: P <:=<+<:)(.El, 00 TG <; - :TT QUESTIONABLE - VERY TINY SILVER-GRAY BLEBS

650 25 3F33MS <: <: P :=<+<)B. 05 TG B.

580 29 3F32CL .< < P .:+<=.<*El. 05 < ( :CORE QUITE GREEN

710 28 3F32CL ..: .- .... ,.. P ,:) <:,=<.%% .B? 0': TG i) B.

740 27 3F32CL .< < P <+<+i$H. 0; 56 < ( <: - :HE ONLY AT ?l.7M

770 29 3F43MS : .: P i+/=<+B.B. 12 TG i (

790 1% 3F33MS +<BR P 03 TA

801 10 OF00 P 0 0 :CONTACTS SOMEWHAT IRREGULAR

830 28 3F32CL < :: HR P < ) < + < #

02 AG :SOME CLAY FILLING FRACTURES

890 29 3031QZ <: ?: P 06 6A :INTERVAL STARTS AS 3C GOES TO 30 THEN 3D AND FINALLY INTO 3A :GRADATIONAL CONTACTS :CLAY FILLING SOME FRAC'S.

920 78 SAlORZ C.':BR P < +.:: ) .:: . 0 5 5A CL :ONE HAND OF 3C AT 90.5M

950 78 iAl0OZ [(ICL F .<+!:)H. 06 7A < ) :SOME CLASTS OF ARGILLITE :SOME CLAY INFILLING FRAC'S.

980 28 3A218Z <<CL P .< +<:: ( 12 GA <: )

:SOHE CARB INFILLING FRAC'S :ALSO SOME ZH AT END OF INTERVAL 1010 78 3A2082 C C L P .+. . - -- , (i.

1" bA .: . u- 1040 27 3A10QZ r; .<EL P .:. .:+< (

11 5A <" - :FIEST .7M IS 3C

1070 30 3A21CL I ;: OL P C U 100 (-<+<(

15 5CI i) : 2 BANDS OF 3C-UPPER QNE MEASLIRED :SOME FE STAINING

1 1 0 0 2 9 341082 X C L P ?: )<+

1 1 6A i. :CL PRESENT BUT NOT I N FRAC'S

1130 29 3k10OZ ((CL P O C ) 11 6A

1 15O 2 9 3A20QZ ::EL P <:I(<)

0 9 6A 1190 2 8 3G10QZ t.: < CL P <:) < 1 B. B.

0 9 5A e: . :FIRST .7M 3A - CONTACT GRADATIONAL :LAST .1M 3F.

1220 2 9 3F32CL .< . .! .. P q.: ) <.? ) < ) 0- 1 7 4G .: . R. E-

:SOME IHTERHEDDED 3 6 1250 2 8 3F22CL <: : P

0 9 TG < - 1280 3 0 3F22CL .:; < 8H F' i) i + . < S C -

1 1 TG <. 1310 29 J F l l C L < < P < ( < ) ( $ < -

1 1 TA :SOME INTERBEDDED 3 6 - PERHAPS b L ITTLE 3E

1340 2 8 3F22CL i: .< P I )<+.<)<. 14 TG .: . B-

:AS ABOVE - NO 5E 1370 33 3E21CL ... ... P <:)<+<:)El:::. ,.. ,..

2 1 AG ? - :SOME 3F MIXED I N

1400 2 8 3E32CL i .. .<. , P c : . ) ? : (<+<.B. 05 TG <- El-<.

:AS ABOVE 1430 2 8 3F33MS ,: < P : ) .LC + ) .

0 5 AT :SOME 3E MIXED I N

1460 2 8 3E22CL .( .. ,* .% P c:)<)<*l3. 0 9 TA < -

1490 2 7 3E33MS ~ c B H P .T'-C+C+ 8. 08 AT .< .

:SOME 3F MIXED I N 1520 2 8 3E34MS C C P ( . .: ) <:+a .:: -

06 AT 1550 2 9 3E33MS <* , .., .% P C ( O C (El.<.

1 2 TG i. :HE GIVING OFF A BURSUNDY STREAK

1580 2 9 3E32CL .c $ ., .< P < ( . O i ) < - C . 1 8 TG (3

:TT GIVING OFF REDDISH-GRAY STREAK 1610 2 7 3E48MS ( .' . '.. P <:. <+<:)O-.::.

0 6 TR <: . C . :HUGE PATCH OF CP AT 133.05M

1640 29 3A30DZ ((EL P O C = B? 1 4 7A R-

:SOME INTERBEDDED 3E :HE MAY CONTAIN TT 1670 3 33A3OZ .:CCL P .: ) .:= 0-

1 7 ?A 0. 1700 28 3A310Z ::ILL P c:.C)<+ B.

08 6A :FINAL METRE OF INT GRADATIONALLY GOES TO 2E

1700 1730 28 3A200Z f iCL P < ) < + < $

02 7A <.<- : INTERBEDDED 3E

1730 1760 25 262002 < q: P <)<:+ <. 03 4A :MAY BE HARD 2C

1760 1790 30 2C21QZ <: *.: P c . ( X < + 0; AT :ROCK SEEMS TO HAVE CHANGED FROM HARD 26 TO SOFTER 2C

03 AT f . 28 2C44MS .<.; BR P <.<+(+ <. 0.5 AT <. 28 2C44MS .I( P i.i+<+ 0 5 AT i. 28 2C43NS ( .< P . 0. 14 AT r; . ., . :TT ONLY AT 192.0M 28 2C33MS r' , c .. P <.<.:)<+<. 09 AT I 5 .

29 2C43NS .: .:: P <: . <:+.::=a. 06 AT c ~. <. :GOOD CP AT END OF INTERVAL :HE MAY CONTAIN TT 29 2 ~ 3 3 ~ ~ G: <: P <.<+<+<.<? 06 AT c. . 29 2C44MS ( <' . .. P <..:+<+ <- 0 9 AT i. 28 2C45MS (( P .:.:=(+ <. 09 5T <: . :HE MAY CONTAIN TT 19 2C44MS <:fBR P <.(=<+Q.<. C) 5 AT <. 28 2C45MS <<Be P q : . f + < + O < (

06 AT <. 28 X45MS +: <.; BK P !:.<+<+<)((

05 5T C . :EXCELLENT CP AT START OF INT & TT IN MIDDLE OF INT. 29 2C34MS ., i ., i P .< . s.: +<: +( < . 14 AT i.

28 X44MS .: ( P <: . .< +z: ) w; . 0 3 AT i <. :HUGE PATCH OF CD AT 217.6M 30 2C44MS .< ( P c: . <: ) c:: + <: < . 12 AT :GOOD CD THROUGHOUT INTERVAL 79 2C45MS (.<BR P <.<+<=<.<. 05 AT 28 ZC45MS (, < BR P <.<=<:+<:.<. 00 7T 25 2C55MS .:;c BR P :: +< = <: 03 6T <. :WELL BRECCIATED ROCK WITH GOOD TT 30 2C55MS :Z:HR V ( ) (= C )

2 1 ST / \. < )

:MAY BE MORE TT THAN HE BUT DON'T WANT TO OVERESTIMATE :.7H OF 8C AT 229.6M WITH CB-QTZ AMYGDS

2368 16 2C45MS :: rg~i P .I ) .... %.-<.. - ' ( .. 02 5T *' .. . <.

2432 51 8Al0 P CU 65 r: ) 18 *: . B. :DYKE CHONGES AT0 8C AT 240.0 WITH ALTERED FELDSPAR PHENOS :FIRST PLHT OF DYKE CONTAINS SOME CL WITH MA1NL.Y FELDSPAR :PHENOS UP TO 1CM IN LENGTH

2460 26 2C55MS .: .:BH P . ( 2 .:. 17 5T <'-

:HE MAY CAF:RY TT 2490 29 2C45MS <<BR P <+*: (

14 5T 2520 29 2C45MS <<:BE P +:+(+ .:,

09 c dT 2550 28 ZC34NS .< .< BF; P ;:+(+ <:-

06 ST <.;? :SOME TYPE OF COATING ON TT-SOME LOOKS LIKE SL

2580 29 2CZ4MS .< .:: BF: P < : ) < # <:7

12 6T <: ? :AS ABOVE

2610 28 2C45MS .: .: P <+<+ C . 06 6T < ? :AS ABOVE-GIVES BROWNISH-BEIGE STREAK!

2640 29 2C44MS <( P .:+<+ 08 5T

2670 28 2C44MS .: < P <+<+ .:. 08 AT <. :AS ABOVE

270C) 17; 2C34i'lS :; <- 05 BT . - - .

2820 29 2C44MS <: <: p .<BR P 14 AT :CP ONLY AT 287.9 M

2910 29 2C45MS <CBR P 08 hT

2940 29 2C45MS .: < BR P 0 9 AT :GOOD TT & CP IN MIDDLE OF iNTERVAL

2965 24 2C45MS <<RR P 14 7T

:STRONGLY ALTERED ROCK AT END OF INTERVAL 2965 2991 2 4 2C55MS <<PR P < . < ) < ) a.

1 0 4T Q- :EXTREME BRECCIATION t ALT'N

2991 3039 47 BAl0QZ << P CU < )

2 6 bG <. :DYKE CONTAINS MAINLY BTZ - CL PHENOS :FROM 299.6M 8A CONTAINS BLEACHED 8C FOR 1.9M - 8C CONTAINS SOME FRAGMENTS OF 2C AND THE UPPER CONTACT I S IRREGULAR - COLOR I S CREAMY TO 6G - LOWER CONTACT ALSO GRADATIONAL WITH SLIGHT ALT 0 5 2C55MS .:: .:: 5. R p cu 141) .:..::+.:= 0 0 6T <I % .

:SMALL SAMPLE BECAUSE BTWN 2 DYKES 1 4 8C21OZ i:< P CU 5 5 8 .. -.,' %. . 03 9T

:BOTTOM CONTACT NOT MEASURED DUE TO BROKEN CORE 1 0 2C45MS s.: < P < ) C + 00 6T

:CORE VERY BROKEN - SOME 8C MIXED I N 2 9 8C10UZ .: .: F' C ) 0. 15 ', .

:OZ AND CB AMYGDS :COLOR FROM CREAM TO GRW( TO PALE GREEN :MANY CB AMYGDS WEATHERED OUT

0 7 2C45MS .:.: - BR F <: . 2: ) <: ) <: . 0 2 bT ~. .

:HOLE ENDED ON DRILLER'S CONVENIENCE - S T I L L HIGH ALT & V IS IBLE TT :END OF HOLE AT 310.9M - END OF LOG - BACK TO SCHOOL!

EQUITY MINESITE LABORATORY ASSAY WET EXTRACTION A.A. - AU F IRE ASSAYED FIRST RCOVSAMPLE ROD % CU G/TAG &/TAU % SB % AS % FE % ZN :TRICONED - NO CORE

7424 0.070 7425 0 . 1 1

:HISLATCH - NO RECOVERY 7426 0. 1 3 7427 0.07 7428 0 . 0 6 7429 0 .06 7430 0.04 7431 6 .03

A001 680 710 7544 0.04 A001 710 740 7545 0.04 A001 740 770 7546 0.17 A001 770 790 7547 111 . 1 5 R 790 801 :DYKE - NO SAMPLE

0.13 0. 10 0.09 (7 . 109 0.07 0.0tr 0.11 0.05 0. 1114 0. 01 il. 0'5 0 . 0 5 0. 1 3 0.12 0 . 2 ? 0 . I2 7 Ci. l t r 0. 125 0.04 0.11: O.CI4 0. (28 0. 08 0. 0B 0 . 04 0.13 0.14 0.05 [I . 02 0.05 0. It, 0.06 !j. 02 0. l h 0.16 0.15 0 . n2 0 . m O.C8 0 . IQ8 0.07 1:) . 112 0.10 111 . 1 2. € 9 0.21 0.13 0.31 0. OY 0.15

7

2320 7598 0 . 2 2 126.0 0.19 2350 7599 0.95 139.0 0.18 2368 764:lil 0.45 62.Oi1.22 2432 :DYKE - NO SAMPLE 2460 75d l 0.13 38.0 0.43 2490 76132 13.01 4.0 I?. 12 252g 7,503 0.05 2.0 (1.07 2550 7604 0.0' 4 .00 .1 j3 2580 7605 0.03 7.0 0.04 2610 7 t06 0.02 3.0 0.03 2640 7607 O.11iOl 0.5 0.04 2670 7608 0.005 0.5 0.01 270111 7609 C1.fji15 0.5 0.1:12 2750 7610 0.02 8 . 0 0 . 0 1 276i:I 761 1 I . 62.0 0.02 2790 7612 0.06 2.0 0.03 282~1 7613 0.02 0.5 0.11 2850 7614 0.24 18.0 0.OR 2890 7615 r:~ . ~14 2.0 0.08 2910 76 1 6 (1.04 7 . 0 0 . 0 3 2940 7617 0.39 97.0 0.11 2965 7618 0.11 63.0 0.09 2551 7 t i 9 0.29 64.0 0.12 31X9 : D W E - NO SAMPLE 3042 7620 0.005 8.0 0.06 3057 :DYKE - NO SAMFLE - . -.. :,I.I, 2 7621 0.005 2.0 0.11 3101 :DYKE - NO SAMPLE 2.1 Oc) 762'5 O.OCl1 3.0 0. 17

:END OF HOLE - END OF ASSAYS END OF ASSAYS - END OF LOG

equity silver mines limited - aris.empr.gov.bc.ca

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