RPT ON PHASE I EXPL PROG€¦ · Fluorite Deposits in Harrington Sound Resources Property Area...

31CiaSE0e85 2.1 2688 MADOC

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l RECEIVED Z . l 2 S g 8^* N!J v^

/.IM-i^'-W ' - '^' - '

I* WP1HG LANDS SECTION

l j REPORT ON THE

l

1989 PHASE I EXPLORATION PROGRAM

FLUORITE-BARITE PROPERTIES

MADOC AND HUNTINGDON TOWNSHIPS. ONTARIO

PREPARED FOR

HARRINGTON SOUND RESOURCES INC.

NTS 31C/5. C/6. C/ll. C/12

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l

lDERRY, MICHENER, BOOTH fc WAHL

T. B. Dickson, B.Sc.

.3-I. D. Trinder, M.Sc.

lm Toronto, Ontario l August 11, 1989

M Ref.: 89-38

^ This report may not be reproduced, in whole or in part, without the written m permission of Derry, Michener, Booth ic Wahl.

DERRY, MICHENER, BOOTH ft WAHL

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TABL ...a.iseae MADOC

Fage

SUMMARY (i)

INTRODUCTION l

PROPERTY LOCATION, DESCRIPTION AND ACCESS l

ECONOMICS OF FLUORITE AND BARITE 3Barite 4

REGIONAL AND PROPERTY EXPLORATION HISTORY 5

REGIONAL GEOLOGY 13

PRESENT EXPLORATION PROGRAM 15

PROPERTY GEOLOGY 16Jarvis Lake Block 16Banker Lake Block 17Southern Block 18

DISCUSSION OF RESULTS 18Jarvis Lake Block 18Banker Lake Block 20Southern Block 20

CONCLUSIONS AND RECOMMENDATIONS 22

REFERENCES 24

CERTIFICATES OF QUALIFICATIONT. B. Dickson, B.Sc. 25I. D. Trinder, M.Se. 26

LIST OF APPENDICES

APPENDIX li SOIL SAMPLE ASSAY CERTIFICATESAPPENDIX 2s PROPOSED DIAMOND DRILL PROGRAM - DETAILED BUDGETAPPENDIX 3s TECHNICAL DATA STATEMENT

LIST OF TABLES

Table Is Claim List , 2

Table 2: Description of Previous Work Conducted on 7-12 Fluorite Deposits in Harrington Sound Resources Property Area


TABLE OF CONTENTS

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LIST OF FIGURES

Figure 1: Location Map

Figure 2: Claim Map

Figure 3: Fluorite Occurrences in the Madoc Area

Figure 4: Regional Geology Map

LIST OF MAPS (see map pockets)

89-38-01: Jarvis Lake Geology

89-38-02: Banker Lake Geology

89-38-03: Southern Lake Geology

89-38-04: Jarvis Lake Soil Sample Location Map

89-38-05: Jarvis Lake Soil Geochemistry

89-38-06: Southern Soil Sample Location Map

89-38-07: Southern Soil Geochemistry

After Page

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DERRY, MICHENER. BOOTH ft WAHL

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SUMMARY

Harrington Sound Resources Inc. holds twenty unpatented mining claims in three separate blocks in the Madoc areai southern Ontario. Access to all claims is

excellent via highway or country road.

The aim of the 1989 summer exploration program was to prospect all

documented past-producing fluorite-barite veins within the properties' limits and

to explore for potential, as of yet undiscovered, fluorite vein mineralization. The

program consisted of geological mapping, geochemical soil sampling and follow-up trenching.

The geological mapping program was successful in delineating the

distribution of the various rock types underlying the property and in locating

numerous old exploration pits and shafts representative of past fluorspar

production by previous exploration interests in the area. Prospecting of these old

workings failed to locate any fluorite-barite vein material at surface.

The results of the geochemical soil sampling survey presented several coincident fluorine-barite-zinc target anomalies well above background values.

Lalonde (1974) states that the dispersion patterns above known veins in the area

are restricted to 30 m, and as such the target anomalies obtained during the present program represented definite targets for further investigation by

trenching. Several target anomalies were further enhanced in that they

represented the possible on-strike extensions of known veins on the properties.

Subsequent trenching of the best target soil anomalies, both above known

veins and their possible strike extensions, failed to uncover any fluorite-bearing

vein material at surface. The program was successful, however, in identifying

fault structures at surface, thereby explaining the soil anomalies and providing

well-defined targets for further investigation by diamond drilling.

Consequently, DMBW recommends that a 700 m diamond drilling program be implemented. This program would be performed to test the subsurface extent


(H)

of the fluorite veins and provide the necessary data to determine if further

definition diamond drilling, bulk sampling and preliminary metallurgical testing

would be warranted.

The cost of the proposed program is estimated at S67,500 as detailed in

Appendix 2 and summarized below:

Pre-field PlanningSite VisitMobilizationDiamond Drilling {all inclusive)DemobilizationData Compilation and Reports

Total

Contingency

GRAND TOTAL

$ 2,4701,940455

46,950430

9.120

61,365

6.135

S 67.500


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1NTRODUCTION

This report, prepared by Derry, Michener, Booth ic. Wahl (DMBW) on behalf of Harrington Sound Resources Inc. (Harrington), summarizes the results of

the 1989 Phase I exploration program carried out on the Madoc area fluorite-

barite properties located in Madoc and Huntingdon townships, Ontario. The

program was carried out in two stages, the first, from May 23 to June 7, 1989, consisted of detailed geological mapping and geochemical soil sampling. The

second stage, carried out from July 7 to July 16, 1989, consisted of trenching.

Linecutting and geophysical surveying were completed prior to the

implementation of the geological program. Mr. T. B. Dickson, DMBW contract geologist, performed the geological mapping and field supervision and is first

author of this report. Mr. I. D. Trinder, DMBW staff geologist, supervised the

program.

PROPERTY LOCATION. DESCRIPTION AND ACCESS

The Harrington fluorite-barite properties are all located within 4 km of

the town of Madoc, Ontario (Figure 1). The Jarvis Lake and Banker Lake

properties are located in Madoc Township, west of the town of Madoc, along

Highway 7. The Southern property is located in Huntingdon Township, approximately 3.5 km south of the town of Madoc.

The Jarvis Lake claim group consists of 12 unpatented contiguous mining

claims totalling approximately 228 hectares, the Banker Lake claim group consists

of 3 unpatented contiguous mining claims totalling 57 hectares and the Southern

block is comprised of 5 unpatented contiguous mining claims representing an area

of 95 hectares, as shown in Figure 2 and detailed in Table 1.

DMBW has not examined title to the claims nor substantiated their physical boundaries and, accordingly, expresses no opinion as to validity of title

and property description.

DERRY, MICHENER. BOOTH St WAHL

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BANKER LAKE

BLOCK

JARVIS LAKE

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JARVIS LAKE BLOCK

BANKER LAK BLOCK

748 K8 j 998774r

998780 i 998775

998781

998T82 {740067

998779199877*

998778 '998777

MADOC TWP.

HUNTINGDON TWP

Moira ' '. :.

•.Lake • •^1XA*f"

1234 56789 10

2Km

12 13 14 15 16 lot

FIGURE 2 CLAIM MAP

no.

SCALE 1:^280

-2-

Table l - Claim List

Block

Jarvis Lake

(Madoc Twp.)

Banker Lake

(Madoc Twp.)

Southern

(Huntingdon)

Claim Number

SO748523

SO748524

SO748526

SO748527

SO748528

SO998774

SO998775

SO998776

SO998777

SO998778

SO998779

SO998780

SO748067

SO998781

SO998782

SO748521

SO748522

SO748525

SO748560

SO748561

Location

NW T, Lot 4, Con. I

SWT, Lot 4, Con. I

SWi, Lot 5, Con. I

NWi, Lot 5, Con. I

NW i, Lot 3, Con. I

NET, Lot 3, Con. I

SEi, Lot 3, Con. I

NEi, Lot 2, Con. I

SEi, Lot 2, Con. I

SWi, Lot 2, Con. I

NWi, Lot 2, Con. I

SWT, Lot 3, Con. I

SEi, Lot 3, Con. Ill

NW T, Lot 3, Con. Ill

SWi, Lot 3, Con. Ill

SWi, Lot 14, Con. X

SE?, Lot 14, Con. XI

Pt. NWi, Lot 15, Co

NWi, Lot 14, Con. 3*

SWi, Lot 14, Con. X

Note;

* - As of May 26, 1989.

Anniversary Date*

November 5, 1990

November 5, 1990

November 5, 1990

November 5, 1990

November 5, 1990

March

March

March

March

March

March

March

22, 1991

22, 1991

22,1991

22, 1991

22, 1991

22, 1991

22, 1991

March 17, 1990

March 22, 1991

March 22, 1991

September 24, 1990

September 24, 1990

November 5, 1990

October 5, 1990

October 15, 1990

DERRY, MICHENER. BOOTH A WAHL

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All the properties are easily accessible year-round using two-wheel-drive

vehicles. The Jarvis Lake and Banker Lake properties are accessed via Highway 7 west from Madoc. The Southern Block is accessed via Highway 62 south from

Madoc and east on the Quin-Mo-Lac Road. Numerous bush roads and paths provide easy access by foot over the entire extent of the properties.

ECONOMICS OF FLUORITE AND BARITE

Fluorite is the only common mineral that contains significant amounts of

the element fluorine. In its pure form, fluorite contains 51.196 calcium and 48.996

fluorine (Guillet, 1962). Fluorite is a semi-hard, glassy, non-metallic mineral that exhibits a wide range of colour varieties; from green to amber to purple to

transparent. Commercial products of fluorite are marketed under the name

fluorspar and are classified as acid or metallurgical grade, depending primarily on

the CaF2 (fluorite) content.

Fluorspar is of value to industry because of its fluxing power in

metallurgical and ceramic batches, and the physical and chemical properties of its

acid in the aluminum and chemical industries. The most lucrative markets for

fluorspar lies in the production of a hydrous hydrogen fluoride and aqueous

hydrofluoric acid (HF) and, consequently, the specifications for acid-grade fluorspar (acidspar) are the most critial: a minimum of 9796 CaF2 is required with

196 maximum each of SiO2 and CaCO3. Other factors include low sulphur and

arsenic content (less than 0.1096) and a certain fineness of the ground material

(Ind. Min., Nov. '88). The largest volume consumer of hydrogen fluoride (HF) is

the manufacturing of fluorocarbons which account for about 6796 of North

American demand (Ind. Min., Nov. '88). Chemical intermediates such as

herbicides account for some 1496 of the demand for HF production. In the metallurgical field, where fluorine compounds are used as a flux in steelmaking

and in rare metal refining, HF consumption accounts for 1496 of the total United

States consumption of about 290,000 tonnes in 1988: 896 was consumed as aqueous

hydrofluoric acid for stainless steel, glass and metal processing, 496 in uranium

processing, and 296 was used to manufacture aluminum fluoride. The current


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price for acid-grade fluorspar from the Illinois District of the U.S.A. is in the

range from US$168.00 to US$173.00/ton {Ind. Min., Apr. '89). Metallurgical grade

fluorspar requires a CaF2 content of not less than 7096 with low SiO2 contents and, as the specifications are not as stringent for that of acidspar, sells for between US$70 to US$77/tonne from Mexico.

The only current producer of fluorspar in Canada is Minworth Ltd. whose

mining operations at St. Lawrence, Newfoundland, have recently been expanded.

The material is of extremely high grade and purity; ore grades as high as 9596

CaF2 have been noted in the deposit (Ind. Min., Nov. '87). Approximately three-

quarters of the North American fluorspar demand, however, has to be met by non-

domestic producers. A profitable niche, therefore, exists in this market for a

reliable, efficient domestic supplier of high quality fluorspar, provided that

potential products are aggressively marketed.

A review of the historical documentation on the Madoc area fluorspar

production shows that ore concentrates ranged from 7196 to 9396 CaF2 (Guillet,

1964). The inability to reach acidspar grade concentrates were hampered largely

by the presence of barite as a vein constituent and antiquated metallurgical

processes used to beneficiate the ore. Improvements in metallurgical techniques

coupled with a better understanding of the structural setting of the fluorite veins

combine to make the Madoc area an excellent prospect to meet the demand for a

domestic source of fluorspar.

Barite

Barite is a semi-hard, very heavy mineral that can exhibit a range of

colours from colourless, yellow, red, green and rarely black.

In North America, over 9096 of the demand for barite stems from the

American oil and gas well drilling industry which uses ground barite as a filler for weighted drilling rnuds. However, because of great distances from the major

drilling areas, Ontario's deposits are not well-located to compete in this market.

DERRY, MICHENER, BOOTH 8t WAHL

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Instead, barite produced in Ontario is used as filler in products such as paint,

plastic, paper and rubber. It is also used in the chemical and glass industries where whiteness and high purity are of consequence. In 1985 Canada produced

about 35,000 tonnes of barite. The April 1989 edition of Industrial Minerals

Magazine quoted a retail price of USSSS/tonne for regular ground barite (FOB, Gulf Coast).

Barite is of secondary importance in the Madoc fluorite-barite deposits.

In most of the deposits, barite constitutes about 1596 or less of the vein material.

Three mines south of Moira Lake, however, contain up to 5096 BaSO4. In most cases the two minerals are interbanded making hand-cobbing difficult or

impossible, but with modern gravity separation techniques, it should be possible to extract a relatively high grade barite product suitable for the fillers industry.

REGIONAL AND PROPERTY EXPLORATION HISTORY

Madoc has been a centre of mining in Eastern Ontario for well over 100

years (Hewitt, 1968). In 1837 Uriah Seymour built a furnace for smelting iron ore

and opened the Seymour iron mine which operated from 1837 to 1845. In 1866, the first gold discovery in Ontario was made at the Richardson Mine near

Eldorado. Two gold mines operated in the Eldorado area during the period from

1894 to 1901. Lead, copper and pyrite were also produced from small operations

in the early 1900's.

The area is best known, however, for the production of industrial minerals

and building stone. Talc, fluorspar, marble, slate, granite, sand and gravel have been produced intermittently since the year 1900. Current producers of industrial

minerals in the Madoc area include the Canada Talc Limited talc mine located

just east of Madoc and the Grenville Aggregates marble quarry located just north of Madoc.

The bulk of Ontario's fluorspar production has come from 24 properties;

all mined at various stages and by varying methods between 1905 and 1961 in the


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Madoc area (Guillet, 1964). Approximately 150,000 tons of fluorspar ore have

been mined and produced 121,919 tons of metallurgical-grade fluorspar

concentrate, the most active periods occurring between 1916-1921 and 1940-1951.

Several of the documented past-producing fluorspar mines in the Madoc

area occur within, or proximal to, the Harrington Sound Resources properties.

Table 2 provides a complete description of each of these occurrences and

condenses information on the geology of the deposit, exploration and mining

history, extent of workings, the exploration potential and, if the deposit does not

occur directly on the property, the deposit's significance to exploration along

strike. Additionally, the location of each fluorite deposit is illustrated, in

reference to the subject property, on Figure 3.

DERRY. MICHENER, BOOTH ft WAHL

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Figure 3 —Fluorite occurrences in the Modoc oreo. (from Guillet, 1964)

Table 2

DESCRIPTION OF DEPOSITS INHARRINGTON SOUND RESOURCES

PROPERTY AREA

BLOCKAREA

Southern(HuntingdonTwp.)

NAME OF MINE/PROSPECT

Noyes Mine

Johnston Hine

LOCATION

Con XII, Lot 13- about 300m

along striketo the north west

Con. XI, Lot 14northeast 1/4- occurs onproperty

DEPOSITDESCRIPTION

- Moira Lake granite hostrock

- Vein-filled lenticularfault cavities up to60m in length and 5min width

- Principle pod averaged60 m by 2.5m

- Proportion of bariteincreases with depth

- There are no rockexposures in the shaftarea

- Country rock is lime stone to 53m thengranite below

- 1943 government drillingoutlined vein up to 2.1mwide (0.9m average) over245m strike length

- Vein consists of about50% fluorite, 35% bariteand 15^1 calcite

PRODUCTION STATISTICSAND HISTORY

- 1916: Discovery- 1917-1918: Fluorite

and minor bariterecovered fromsurface cuts

- 1918-1920: Under ground mining ofabout 15,500 tons

- 1941-1943: Under ground mining ofabout 9,000 tons

- TOTAL PRODUCTION:25,000 tons

- Prior to 1943:discovery by diamonddrilling

- 1943 s 2 compartmentshaft sank to 17m(55 ft.); recovery of"several hundred tonsof ore"

- 1944-1947: deepeningthe shaft to 19m andmore small scaleproduction

- 1949: deepening ofshaft to 24m (78 ft.)

- TOTAL PRODUCTION:187 tons hand-cobbedfluorspar

EXTENT OF WORKINGS

- Shaft to 84m (275 ft)- 663m of drifts- 17 m of crosscuts- 242m of raises- Underground develop ment extends toabout 65m fromproperty boundary

- Shaft to 24m (78 ft)- 85m of drifts at the

17m (55 ft) level

EXPLORATION POTENTIAL/SIGNIFICANCE

- Pods of barite-fluorite veinmaterial upto 2m in widthplunge southeastwardtowards the SouthernBlock(see Figure AI.l)

- 1050m of diamonddrilling in 26 holeswas performed in theJohnston propertyarea over a strikelength of about 425m

- A large tonnage ofunmined vein materialexists at shallowdepths

- Better intersectionsinclude:-451 CaF over 3.2m-50% CaF over 2.3m-35% CaF over 2.7m-45% CaF over 3.3m

- barite contents werenot given

- trenching and diamonddrilling is warranted(see Figures AI . 2 andAI.3)

Table 2


PROPERTY AREA

BLOCKAREA

Southern(HuntingdonTwp. )

continued

NAME OF HINE/PROSPECT

Howard Mine

WrightProspect

LOCATION

Con XI, Lot 14northeast 1/4- within 175malong strike(in bothdirections)from theproperty

Con XI, Lot 15- occurs on

southernblock

DEPOSITDESCRIPTION

- Wall rock is limestoneto 55m

- Vein is parallel to,but displaced 90m tothe northeast of, theNoyes-Johnston vein

- Vein dips 75^ SW- Vein ranges from 0.3m

to 0.9m wide over 130mstrike

- Bulk samples containedup to 67% CaFj and 25*BaS04

- Recovery of up to 78*CaF 2 was achieved

- Average mining gradewas about 41* CaF 2over 0.7m


- 1917: Discovery- 1918-1920: open cutmining and some shaftdevelopment work

- 1929: shaft deepened- 1940-1944: mining of

about 2,500 tonsfluorite ore


- 10 pits were excavatedto explore for thestrike extension of theHoward Vein

- 1 of the pits reportedlyuncovered a vein

- NO PRODUCTION RECORDED

EXTENT OF WORKINGS

- Two shafts, one 13m(60 ft) and the otherllm (36 ft)

- 130ra of drifts

- 10 pits


- Vein appears to betoo narrow to be ofeconomic interest

- The strike extensionshould be explored,however.(Wright Prospect)

(see Figure AI.4)

- Prospect has notundergone adequateexploration

- Prospecting, trencliinand possible diamonddrilling is warranted

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Table 2

DESCRIPTION OF DEPOSITS IUHARRINGTON SOUND RESOURCES

PROPERTY AREA

BLOCK AREA

NAME OF MINE/ PROSPECT LOCATION

DEPOSIT DESCRIPTION

PRODUCTION STATISTICS AND HISTORY EXTENT OF WORKINGS

EXPLORATION POTENTIAL/ SIGNIFICANCE

Banker Lake (Madoc Twp)

Lee Junior Mine

Con III, Lot 2- northernworkings about 300m south of the property

The vein cuts "blackrhyolite"(amphibole basalt?) inthe northern zone, andlimestone in thesouthern zoneThe vein strikes at3000 to 3100 ; the dipis unreportedThe vein is up to 0.55mwide and has a typicalmineralogy

- 1917: "three car loads" of fluorspar produced

- 1940-1941: 1,100 tons recovered from open cuts and shallow shafts

- 1943-1945: 684 tons produced

- TOTAL PRODUCTION: 2,000 tons

Two areas of workings about 400m apart Northern area consists of two shafts, 12m and 15m deep, about 100m apart with 42m and 12m of drifting respectively 180 m of open cut mining in area Southern area has 14m shaft with 5m o f drifting at the bottom The vein was mined from a surface cut 60m long, 0.9m wide, and 1.5 to 9m deep

The vein is narrow but it produced about 2,000 tons of ore and it has not been drill tested along strike Prospecting, trenching and diamond drilling are warranted on the Banker Lake property along strike from the vein

McBeath Prospect

Con III, Lot 3 southeast 1/4 - occurs onBanker LakeBlock

Fluorite-barite vein about 0.3m wide cutting limestone

- Unknown l trench near south boundary of property

- Vein may represent the extension of the Moira Lake Fault

- No appreciable surface work or diamond drilling has been reported

- Prospecting, trenching and diamond drilling is warranted

VD

Table 2


PROPERTY AREA

BLOCKAREA

Jarvis Lake(Madoc Twp)


Rooks Mine

William-ReynoldsMine

Ponton Hine

LOCATION

Con I, Lot 6- about 150m

north of theproperty

Con I, Lot 5- occurs in the

northern partof theproperty

Con I , Lot 3- occurs onproperty

DEPOSITDESCRIPTION

- Fluorite vein up to0.75m wide cuttinglimestone

- Vein strikes at 3050 ,dip not reported

- Vein strikes at 3200through limestone

- Vein varies in widthfrom 0.3 to 0.8m andconsists of about30i fluorite, 20%barite and 50%calcite

- Fluorite-calcitevein trends 3 IS0 andcuts limestone

- up to 0.75m wide


- 1916-1918: 100 tons ofore was shipped fromopen cut

- TOTAL PRODUCTION:100 tons

- 1920s Discovery- Prior to 1940: 6 test

pits excavated- 1941-1942: 88 tons

fluorspar shipped- TOTAL PRODUCTION:

100 tons

- 1917: Discovery andminor workings

- 1929-1942: 1,200 tonsshipped from seriesof open cuts


EXTENT OF WORKINGS

- Open cut 90m long andup to 6m deep

- 6 test pits spacedfrom north to southat 27m, 17m, 27m,17m and 24m

- Series of open cutsalong strike lengthof 120m and up to 6mdeep

- Workings are nowfilled in


- The strike extensionof the vein shouldbe explored on theproperty

- Prospecting andpossible trenchingand diamond drillingis warranted

- The vein lias neverbeen drilled

- Prospecting, trenchingand diamond drillingis warranted

- Surface work anddiamond drilling iswarranted

Table 2


PROPERTY AREA

BLOCKAREA

Jarvis Lake(Madoc Twp)continued


Miller Mine

StewartProspect

Wallbridge-llarringtonMine

LOCATION

Con I, Lot 4- occurs onproperty

Con I , Lot 2northeast 1/4- occurs onproperty

Con I, Lots 1S2north part ofmine- occurs onproperty inpart

DEPOSITDESCRIPTION

- The vein strikes at3500 through lime stone

- The vein is over 120mlong and up to 1mwide consistingmostly of fluoriteand calcite

- "Narrow" barite-fluorite vein

- The mine consists oftwo ore bodies: thesouth vein that is acontinuation of theLee Senior vein, andthe north vein thatincludes the Harring-ton Mine (on theJarvis Lake Block)

- Both veins mayrepresent the samestructure

- North vein has beentraced for over 150mwith widths up to2.1m


- 1917: Discovery andopen pit excavation

- 1918-1919: Furtheropen cut mining andshipment of ore

- TOTAL PRODUCTION:460 tons

- History Unknown- NO PRODUCTION

- 1918: Discovery- 1920-1922: Fluorspar

produced from opencuts and shafts onboth veins

- 1941-1943: North veinmined on both theWallbridge andHarrington properties


EXTENT OF WORKINGS

- 120m long open cut onthe main vein that was1.5m wide and up to 3mdeep

- Also, a 23m shaft with12m of drift work atthe bottom

- "Several" prospect pits

- North vein explored by3 shafts of 15m, 38mand 6ta and numeroustrenches

- 310m of drifts and 38mof crosscuts on 3levels


- Trenching andprobable diamonddrilling is warranted

- Probably theextension of theMiller Vein

- Prospecting andtrenching warranted

- About 8,000 tons ofore have been producedfrom Lee Senior-Wallbridge- Harringtonstructure; most ofwhich came from withinor very near theJarvis Lake property

- Diamond drilling andtrenching isdefinitely warranted

-If possible, the mineshould be dewateredand re-evaluated

(see Figures AI.5 andAI.6)

Table 2


PROPERTY AREA

BLOCK AREA

Jarvis Lake(Madoc Twp)continued

NAME OF MINE/ PROSPECT

Lee SeniorMine

LOCATION

Con I, Lot 1- occurs just

south ofproperty

DEPOSIT DESCRIPTION

- Property consists of5 veins cutting lime stone - two were minedfor fluorite

- Wallbridge extension(main vein) :Lenticular massesof fragmental or"gravel"fluorspar; 27mlong by up to2.5m wide

- East vein cuts lime stone at 3230

- Vein is narrowerthan main (western)vein

PRODUCTION STATISTICS AND HISTORY

- 1916-1918: Period ofproduction from opencut and minordrifting on Main Vein

- 1942-1943: Developmentand production fromeast vein

- TOTAL PRODUCTION:Main Vein; 1,200 tonsEast Vein; 400 tons

EXTENT OF WORKINGS

- Main Vein:- 15m long/ 2.5m deepopen cut

- 18m shaft with 30mof drifts

- East Vein:- 60m open cut tomaximum depth of12m

- 15m shaft with 48mof drifts

EXPLORATION POTENTIAL/ SIGNIFICANCE

- Both veins strikeon to the property

- Prospecting, trenchingand diamond drillingis warranted

1h-"NJ

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REGIONAL GEOLOGY

The regional geology of the Madoc area is described by Hewitt (1968) and

shown in Figure 4.

The Madoc area straddles the Paleozoic-Precambrian unconformity.

Medium to high grade metamorphic rocks belonging to the Central

Metasedimentary Belt of the Grenville Province lie to the north and younger,

essentially unmetamorphosed sedimentary rocks of Middle Ordovician Age lie to

the south. Flat-lying outliers of Ordovician limestone rest locally upon

Grenvillian rocks north of the unconformity.

The oldest rocks in the area are the Tudor volcanics, a series of

greenschist facies, dark green mafic lavas of andesitic composition. These rocks

lie in the eastern and northern portions of Madoc Township and are overlain by

calcitic and dolomitic marbles, conglomerate, argillite and pelitic schists. This

mafic volcanic event ended with rhyolitic flows and tuffs and, based on the

intercalated relationships between the volcanics and sediments, it is apparent that

there was a gradual transition from volcanism to sedimentation.

In south-central Madoc Township, the Madoc volcanics occupy a domal

structure of approximately 23 sq. km. They range from andesite to rhyolite in

composition. Massive, pillowed, vesicular and amygdaloidal, tuffaceous and

agglomerate facies are all common in these volcanics. Volcanism and

sedimentation were concomitant in the area as there is no erosional unconformity

between the volcanics and sediments which consist primarily of conglomerate,

slate and dolomitic and calcitic marbles.

Intruding the volcanics and sediments in the area are four bodies of pink

granite and syenite. The two main intrusions in the Madoc area are the Deloro

granite, which forms a stock of pink medium-grained granite in west-central

Madoc Township and the Moira granite, which is a pink medium to coarse-grained

granite outcropping in the vicinity of Moira Lake. Minor intrusions of gabbro and

diorite are locally present.


BANKER BLOCK*

15 16

SOUTHERN BLOCK

O NHUNScale l: 31.680 or l Inch to V2 Mile

LEGEND

CENOZOIC*

PLEISTOCENETill. sand, grave!, clay, mar!.

UNCONFORMITY

PALEOZOICORDOVICIAN

7 1 Black River limestone, 11 a Basal conglomerate.

UNCONFORMITY

W Diabase.

9 Granite and syenite ^indifferent. ated.

9a Granite.9b Syenite.

S Grey granodiorite.

7 Diorite and gabbro undifferentiated 7a Gabbro.

INTRUSIVE CONTACT

METASEDIMENTS AND METAVOLCANICSMETASEDIMENTS

6 Quartzite and Quartzo-feldspathicrocks.

6a Felsite.5 Pelitic rocks.5a Argillite, greywacke.5b Paragneiss.5c Schist.5d Conglomerate.

4 Marble undifferentiated.4a Dolomitic marble.4b Calcitic marble.4c Lime silicate rock.4d Limestone conglomerate.

3 Para-amphibolite.3a Garnet amphibolite.

METAVO1-CANICS Basic Metavolcanics2 Undifferentiated.2a Amphibolite, amphibolite schist.2b Massive andesite.2c Agglomerate.2d Tuff.2e Pi/low lava.

Acid MetavolcanicsT Rhyolite.fa Rhyolite tuff.1b Felsite.1c Felsite breccia.1d Rhyolite breccia.

SYMBOLS

140 ' Shaft; depth in feet.

Location of mining property and occur rence. See list of mines, properties dr.rl occurrences.

NOTE: Locotions of shafts and trench es ore approximate.

FIGURE 4

PROPERTY GEOLOGY MAP

Feet 1 000 O

After 06S Mao 2I54


-14-

The Grenville rocks in the area underwent a period of deformation

resulting in folding; the principal folds are the northwest-trending Queensborough

syncline and the northeast-trending Madoc syncline.

Following a protracted period of erosion, the Paleozoic marine

transgression deposited a series of terrigenous clastic and carbonate rocks of

Middle Ordovician age in the Madoc area {Williams and Thompson, 1986). These

sedimentary rocks consist of the following lithologies: the basal Shadow Lake

Formation consisting of sandstone and siltstone; the Gull River Formation

comprised of thin to medium-bedded limestone; the Bobcaygeon Formation thin to

massive bedded limestone and finally the Verulam Formation consisting of

interbedded limestone and shale.

The last event to affect the Madoc area was a period of post-Ordovician

normal faulting which provided the structural environment for the emplacement

of the Madoc area fluorite-bearing veins. This structural zone is approximately

15 km long and 5 km wide and trends southeasterly through the Madoc area

paralleling major rift zones (Ottawa Valley) in the region (Thompson and Williams,

1987). Vertical fault displacements of more than 90 m have been detected and

their traces have been shown to be gently curved to distinctly curved in the

vicinity of fault junctions.

The Madoc area fluorite veins occupy lenticular fault cavities both above

and below the Precambrian-Paleozoic unconformity with a common left-lateral,

en echelon mode of occurrence. The vein material consists essentially of banded

fluorite, calcite and barite with minor amounts of accessory minerals. The veins

have been subdivided into the Moira Lake group, historically the more economic in

the area, and the Lee-Miller group which represent smaller deposits occupying

parallel, subsidiary fractures west of the town of Madoc.

Two distinct conjugate vein sets have been recognized: one striking at

135 0 to 1400 and the other at 105 O to HO0; both are vertical to steeply dipping

(Williams, pers. comm.).


-15-

PRESENT EXPLORATION PROGRAM

The geological program was carried out in two stages; the first, from

May 23 to June 7, 1989, consisted of detailed geological mapping and geochemical

soil sampling and the second stage, from July 7 to July 16, 1989, consisted of

follow-up stripping and trenching. Please refer to Appendix 3 for the technical

data statement regarding this program. The geological program was implemented

subsequent to the completion of linecutting and complete geophysical coverage of

the properties consisting of magnetometer and VLF-EM surveys. The results of

the geophysical survey are presented in a previous DMBW report (ref. 89-33).

Geological mapping was controlled by cut grids on each of the properties

and allowed easy access over their entire extent. The properties were mapped at

a scale of 1:2,500 (Map 89-38-01, -02, -03) to gain an understanding of the various

rock types underlying the properties and to locate old workings associated with

previous exploration interests in the area. All pertinent geological data was

recorded on scaled sheets amenable to in-field use and, subsequently, transferred

onto a base map. Every attempt was made to cover the area in between the

100 m spaced grid lines to ascertain additional geological data on all outcrops

encountered.

Geochemical soil sampling was implemented on the Jarvis Lake and

Southern claim groups. The Banker Lake claim group was initially sampled,

however, due to extensive swamp coverage on the property, coupled with poor soil

development in areas where Paleozoic limestone formed extensive outcroppings,

the samples were not submitted for analysis.

Based on the comprehensive and extensive research conducted by Lalonde

(1974) on geochemical prospecting methods for fluorite deposits in the Madoc area,

sampling of the soil profile was restricted to the uppermost A horizon. Lalonde

(1974) states that the A horizon exhibits a greater contrast than either the B or C

horizons over areas of known mineralization and accentuates the contrast between

background and anomalous fluorine contents. In addition, sample intervals of

25 m were used because dispersion patterns of known fluorite veins are restricted



-16-

to a relatively narrow zone of about 20 m on either side of the veins. Samples

were bagged and shipped for analysis for the following three elements: fluorine,

barium and zinc. Lalonde (1974) states that the barium and zinc contents in the A

horizon of the Madoc area soils are useful tracers for fluorite veins and their

contents were shown to correlate extremely well with those of fluorine.

A total of 644 soil samples were collected; 536 from the Jarvis Lake

property and 108 from the Southern property and shipped for analysis to the

Bondar-Clegg facilities in Ottawa, Ontario. The elements were analyzed using

the following methods: fluorine - Specific Ion; barium - DC plasma and

zinc - Atomic Absorption.

The geochemical soil assay certificates are presented in Appendix l, and

the results from the soil survey are presented on Map 89-38-05 and -07. Sample

locations are presented on Map 89-38-04 and -06.

Subsequent to the soil sampling survey, a number of trenches were

escavated on the Jarvis Lake and Southern claim blocks. Trenches were located

on the basis of the following criteria; firstly over soil anomalies exhibiting the

best potential, particularly where anomalous fluorine values coincided with high

barium and/or zinc values and, secondly, proximal to known vein deposits or their

inferred strike extension. Trenches were escavated using a backhoe and then

manually cleaned to bedrock with shovels. A total of 5 trenches were escavated

on the Jarvis Lake property and 4 on the Southern property, as illustrated on Map

89-38-01 and -03.

PROPERTY GEOLOGY

Jarvis Lake Block (Map 89-38-01)

The oldest rocks underlying the property are mafic volcanics (Unit 1).

The unit outcrops between L3+OON and L6+OON between 4+OOE and 8+OOE and

forms a prominent topographic high. In hand sample, the rock is very fine to fine-



-17-

grained, dark grey and magnetic due to the presence of discreet magnetite

crystals and veinlets. Texturally, the rock varies from massive to moderately

foliated and moderate to weak carbonate alteration is ubiquitous. Agglomeratic

facies dominates over massive facies and consists of rounded to angular, 5 cm to

50 cm diameter fragments of mafic volcanic, tuff and pink felsite, in a fine

grained mafic matrix.

Granitic rocks (Unit 2) belonging to the Deloro granite occur on the

extreme western edge of the Jarvis Lake property. In hand sample the rock is

pink in colour, massive and varies from medium to coarse-grained.

The youngest rocks, which underlie the remainder of the property, are

Paleozoic limestone of mid-Ordovician age. They are pale grey to grey,

microcrystalline to fine crystalline, thin to medium-bedded limestones

representative of the Bobcaygeon Formation. They are flat-lying and form

extensive outcroppings in the central portion of the property. Jointing is

prominent in this unit varying between HO0 and 140 O.

Banker Lake Block (Map 89-38-02)

The Banker Lake block is predominantly underlain by mafic volcanic rock

displaying massive, foliated, agglomerate and amygdaloidal facies. In hand

sample the rock is dark grey green, fine-grained and, in the northern portions of

the property, displays an intense degree of amphibolitization.

Thin to medium-bedded, microcrystalline, grey limestone, representative

of the Bobcaygeon Formation, overlies the mafic volcanics on the eastern portion

of the property. Extensive outcropping of flat-lying limestone displays prominent

jointing at 135 O to 140 O.

DERRY. MICHENER. BOOTH ft WAHL


-18-

Southern Block (Map 89-38-03)

The oldest rocks on the Southern Block are granitic in composition and are

restricted to the extreme northwestern portions of the property between L16+OON

and L2(HOON. Representative of the Moira Lake granite, the rock is pink, medium

to coarse-grained and massive.

Overlying the granite and underlying the remainder of the property is a

unit of flat-lying mid-Ordovician limestone. Chocolate-brown to grey in colour,

the limestone is thinly to massively bedded and ranges from microcrystalline to

fine crystalline. Jointing patterns are pronounced and vary from 110 0 to 140 O .

DISCUSSION OF RESULTS

Jarvis Lake Block

During the course of geological mapping conducted on the property, a

number of old workings were located and mapped in detail (Map 89-38-01). The

Herrington Mine (LO+00/0+25W) consists of a timbered shaft to a depth in excess

of 5 m and is now completely water-filled. In addition, a number of old test pits

and trenches exist in the vicinity of the shaft. The Herrington and Wallbridge

Mine, located 30 m south of the property, produced approximately 6,600 tons of

fluorspar from veins hosted in limestone. No vein material was found during the

course of surface prospecting. The Stewart Prospect (L4+OON/4+50E) consists of

two old pits in limestone. No production was recorded from this showing and

prospecting failed to discover any vein material in outcrop. The Ponton Mine

(L11+OON/1+50W) produced 1,500 tons of ore by open-cut method. Exposed for

over 150 m on surface, the vein and the structure responsible for it was emplaced

in limestone. Surface prospecting did not encounter any vein material.

The results from 536 soil samples collected and analysed from the

property are presented on Map 89-38-05 and the basic statistics are tabulated

below:

DERRY, MICHENER, BOOTH A WAHL


-19-

Fluorine (ppm)

536

466.4

413.8

479.1

*950

Barium (ppm)

536

807.5

762.1

443.8

*1,200

Zinc (ppm)

536

106.1

82.02

70.56

*250

Number of Samples

Mean

Median

Standard Deviation

Target Anomaly Value (Mean + Standard Deviation)

*greater than

The results from the survey were excellent insofar that a number of

coincident fluorine/barium/zinc anomalies were identified. Not surprisingly,

anomalous values were recorded from samples taken directly over old prospects

on the property, however, in addition, several 2- and 3-point target anomalies

were identified in locations which coincide with inferred strike extensions of past-

producing veins on the property.

A total of five trenches were escavated on the property; three to test the

Herrington vein and its possible extension and two to test the Ponton vein

(Map 89-38-01). Trench J-l was excavated 5 m south of the Herrington shaft

(LO+00/0+25W) in an attempt to locate the vein and/or the host fault. Dug to a

depth of 4 m, water was encountered on strike from the vein extension and

further trenching was abandoned. Trench J-2 (L3+OON/2+OOW) was escavated to

test a coincident fluorine/zinc target anomaly thought to represent the possible

strike extension of the Herrington vein. The trench was 30 m in length and

although prominent 135 0 trending fractures were encountered in limestone, no

vein material was found at surface. Trench J-3 (L5+OON/2+90W to 3+85W) was

escavated to test a series of highly anomalous and coincident fluorine/barium/zinc

anomalies thought to represent the possible extension of the Herrington vein.

Limestone bedrock was exposed the length of the trench, however, apart from

highly fractured limestone possibly representative of a fault structure, no vein

material was encountered.



-20-

Trench J-4 and J-5 were escavated on the south and north extensions of

the exposed Ponton vein respectively. Trench J-4 is comprised of two separate

trenches, north and south of a forest access road. North of the road the old l m

wide open cut workings were exposed to reveal remnant vein material on the

limestone wall rock. South of the road trenching did uncover the fluorite vein

extension, striking at 1350, however, it pinches out to a width of approximately

8 cm over its 2 m exposed length and no sampling was undertaken.

Trench J-5, escavated on the north extension of the Ponton vein, was dug

to a depth of 4 m to reveal a 1.5 m wide open cut with minor amounts of remnant

fluorite, barite and calcite on the brecciated and vuggy limestone wallrock.

Banker Lake Block

The McBeath prospect (LO+00/7+75E) was located and prospected during

the course of geological mapping on the property (Map 89-38-02). The 0.75 m

wide open cut was exposed for over 150 m in strike length, however, no vein

material was encountered at surface. Low angle slickensides, developed in the

limestone wall rock, attest to possible post ore movement or a minor horizontal

component to the normal faulting. As previously mentioned, soil samples were

not submitted and, due to the lack of adequate targets, trenching was not

undertaken.

Southern Block

Several old workings were located and prospected on the property, two of

which were previously undescribed in the literature. Two old timbered shafts

(L19+OQN/1+75W) which were blasted in granitic rock to a depth of 5 m were

prospected, but no vein material was found in situ. In addition, a pit in excess of

6 m deep (L20+45N/0+10E) was discovered and, although no vein material was

encountered it seems apparent that the previous exploration interests had some

indication of vein material to undertake this degree of work. The Johnston Mine



Fluorine (ppm)

108

354.3

332.9

237.5

*425

Barium (ppm)

108

996.3

787.2

746.1

*1,400

Zinc (ppm)

108

106.7

146.3

66.5

*275

-21-

(L13+50N/2+50W) workings were located although no outcropping exists in the

vicinity of the shaft due to low-lying swampy terrain.

The results from 108 soil samples selectively collected and analysed from

the property are presented on Map 89-38-07 and the basic statistics are tabulated

below:

Number of Samples

Mean

Median

Standard Deviation

Target Anomaly Value (Median -t- Standard Deviation)

""greater than

The results of the soil sampling on the Southern property were not as

definitive as those from the Jarvis Lake block, however, several coincident

fluorine, barite and/or zinc anomalies were identified. A number of these

anomalies were located along inferred strike extensions of old workings and,

therefore, represented definite targets for further investigation by trenching.

A total of four trenches were escavated on the property, all north of

Quin-Mo-Lac Road {Map 89-38-03). Trench S-l (L19+OON/1+50W to 2+25W) was

escavated to test a coincident fluorine, barium and zinc soil anomaly and the

possible strike extension of any vein structure south of two old timbered shafts

collared in granite. The trench exposed granite bedrock over its entire length and

although no vein material was encountered at surface, a strong shear/fracture

trending at 120 0 on strike with the old shafts attests to the continuation of the

structure. Trench S-2 (L20+OON/1+25W and 1+75W) was dug to test isolated

fluorine soil anomalies. Both were escavated to a depth in excess of 4 m without

encountering solid bedrock and were abandoned. Trench S-3 (L20+OON/0+00 to

0+50W) was located to test a coincident fluorine/zinc soil anomaly and the on-

DERRY, MICHENER, BOOTH A WAHL


-22-

strike extension of an old pit located approximately 40 m to north. The trench

exposed limestone bedrock over its entire length and an intensely fractured

interval of limestone with the bedrock horizontally offset in excess of 2 m. This

zone, trending at 140 O , coincides with the on-strike extension from the old pit

located to the north and is probably representative of a fault, although no vein

material was seen at surface. Trench S-4 (L21+OON/0+00) was escavated to test

the northern extension of the forementioned pit and a coincident fluorine/zinc

anomaly. Limestone bedrock was encountered and a pronounced offset in the

limestone trending at 140 0 was located directly beneath the soil anomaly and on-

strike with the old pit. Again, no vein material was seen at surface, but the

offset probably represents the fault structure.

CONCLUSIONS AND RECOMMENDATIONS

The geological mapping program was successful in delineating the

distribution of the various rock types underlying the property and in locating

numerous old exploration pits and shafts representative of past fluorspar

production by previous exploration interests in the area. Prospecting of these old

workings failed to locate any fluorite-barite vein material at surface.

The results of the geochemical soil sampling survey presented several

coincident fluorine-barite-zinc target anomalies well above background values.

Lalonde (1974) states that the dispersion patterns above known veins in the area

are restricted to 30 m, and as such the target anomalies obtained during the

present exploration program represented definite targets for further investigation

by trenching. Several target anomalies were further enhanced in that they

represented the possible on-strike extensions of known veins on the properties.

Subsequent trenching of the best target soil anomalies, both above known

veins and their possible strike extensions, failed to uncover any fluorite-bearing

vein material at surface. The program was successful, however, in identifying

fault structures at surface. The presence of the faults explains the soil anomalies

and provides well-defined targets which will require diamond drilling to

investigate their potential for fluorite mineralization down-dip.



-23-

The fluorite-barite veins in the Madoc area have produced the bulk of all

fluorspar production in Ontario. Past production from the area was largely by

small-scale, individually run mines and, consequently, many of the known deposits

remain superficially explored, particularly at depth.

To enable a further assessment of the economic viability of the fluorite

veins, additional information is needed. DMBW recommends that a diamond drill

program be implemented on the Jarvis Lake and Southern properties, the results

of which would provide information on the down-dip continuity and variability in

width and grade of the fluorite veins.

Emphasis will be placed on drilling three of the past-producing mines on

the properties. These are: the Herrington and Ponton Mines on the Jarvis Lake

property and the Johnston Mine on the Southern property. In addition, two fault

structures identified by trenching and on-strike with old timbered shafts and pits

in the northern portion of the Southern property represent targets for diamond

drilling.

DMBW, therefore, recommends that a 700 m diamond drilling program be

implemented. This program would be performed to test the subsurface extent of

the fluorite veins and provide the necessary data to determine if further

definition diamond drilling, bulk sampling and preliminary metallurgical testing

would be warranted.

The cost of the proposed diamond drilling program is estimated at S67,500

as detailed in Appendix 2 and summarized below:

Pre-field Planning S 2,470Site Visit 1,940Mobilization 455Diamond Drilling (all inclusive) 46,950Demobilization 430Data Compilation and Reports ___9,120

Total S 61,365

Contingency ___6,135

GRAND TOTAL S 6 7.500


l l l l l l l l l I l l l l l l l l l

-24-

REFERENCES

Guillet, G. R.1964: Fluorspar in Ontario, Ontario Department of Mines,

Industrial Mineral Report No. 12.

Hartwick, P. A.1988: Report on the Madoc Area Fluorite-Barite Properties,

Madoc and Huntingdon Twps., Ontario, NTS 31C/5, Prepared for Harrington Sound Resources Inc., DMBW unpublished report, 20 p.

Hewitt, D. F.1968: Geology of Madoc Township and the North Part of

Huntingdon Township, Ontario, Department of Mines, Geological Report No. 73, 45 p.; includes ODM Map 2154.

Industrial Minerals MagazineApril 1989 issue

Lalonde, J. P.1974: Research in Geochemical Prospecting Methods for

Fluorite Deposits, Madoc Area, Ontario; Geological Survey of Canada, Paper 73-38, 56 p.

Thompson, L. G. and Williams, D. A.1987: Geological and Geophysical Studies of the Madoc Fluorite

Area, Southern Ontario; in Summary of Field Work and Other Activities, 1987, Ontario Geological Survey, Miscellaneous Paper 137.

Williams, D. A. and Thompson, L. G.1986: Structural Setting of the Fluorite Vein Deposits of the

Madoc Area, Southern Ontario; in Summary of Field Work and Other Activities, 1986, Ontario Geological Survey, Miscellaneous Paper 132.

DERRY, MICHENER, BOOTH St WAHL


-25-

CERTIFICATE OF QUALIFICATION

I, Timothy B. Dickson, of 105-212 St. George Street, Toronto, Ontario, do hereby certify that:

(1) I am an exploration geologist working as consultant for Derry, Michener, Booth 6c W ahl, Consulting Geologists and Engineers of Toronto.

(2) I am a graduate of the University of Western Ontario, London, Ontario, in Honours Geology with the degree of B.Sc. in 1985.

(3) I have been practising my profession since 1982 and full-time since graduating in 1985.

(4) I have not received, nor do I expect to receive, any interest, directly or indirectly, in the properties or securities of Harrington Sound Resources Inc.

(5) The statements contained in this report and the conclusions and recommendations made are based upon my review of all data available. I supervised and visited the properties during the exploration program.

(6) I hereby consent to the use of this report in a Statement of Material Facts of the Company for the preparation of a prospectus for submission to the Ontario Securities Commission and other regulatory authorities.

Timothy B. Dickson, B.Sc.

Toronto, Ontario August 11, 1989


l l l l l l l l l l l I l l l l l l l

-26-

CERTIFICATE OF QUALIFICATION

I, lan D. Trinder, of Apt. 2025, 30 Denton Avenue, Scarborough, Ontario do hereby certify that:-

1. I am an exploration geologist employed with Derry, Michener, Booth 6c Wahl, Consulting Geologists and Engineers of Toronto.

2. I graduated from the University of Manitoba in 1983 with a degree of Bachelor of Science, Honours Geology and from the University of Western Ontario in 1989 with a degree of Master of Science, Geology. I have been practicing my profession since graduation.

3. I have not received, nor do I expect to receive, any interest, directly or indirectly, in the properties or securities of Harrington Sound Resources Inc.

4. The statements contained in this report and the conclusions and recommendations made are based upon my review of all data available. I have not visited the properties.

5. I hereby consent to the use of this report in a Statement of Material Facts of the Company for the preparation of a prospectus for submission to the Ontario Securities Commission and other regulatory authorities.

lan D. Trinder, M.Sc.

Toronto, Ontario August 11, 1989



APPENDIX l

SOIL SAMPLE ASSAY CERTIFICATES


l5420QuttfkRc

I Ottawaj^Bmo K1J8X5^

Boodtf-CltQ 6 Compuy Ltd.:Road

(613) 749-2220 Tdex 053-3233

Geochemical Lab Report

7 REPORT: 089-51466.0 ( COMPLETE )

C CLIENT: DERRY, MICHENER, BOOTH t KAHL PROJECT: HSR103

REFERENCE INFO:

SUBMITTED BY: TIM DICKSON DATE PRINTED: 15-JUN-89

! NUMBER OF LOiiER ORDER ELEMENT ANALYSES DETECTION LIMIT EXTRACTION METHOD

1 Zn Zinc 242 1 PPM HCL-HN03, (3:1) Atone Absorption 2 F Fluoride 242 20 PPM NA2C03-KN03 FUSION Specific Ion

3 Bs Bariug

SAMPLE TYPES NUMBER

242 1 PPM Hf-HC104-HN03-HC1 OC Plasoa

SIZE FRACTIONS NUMBER SAMPLE PREPARATIONS NUMBER

REPORT COPIES TO: I.D. TRINOERFAX TO TORONTO OFFICE

INVOICE TOs I.D. TRINDER

l

11f1

Boadv-Ckg A Company Ltd.5420 Gmgtk RoadOttawa^Birio K1J 8X3^^(613) 749-2220 Tetec 053-3233

REPORT: 089-51466.0

SAXPLE ELEHENT NJK8ER UNITS

ZnPPH

F PPN

f^9fiMk^K^^^K^^K ^KA ^UM-^bBQNDMH1EG6

Ba SAMPLE PPH NUMBER

GeocfaemicalLab Report

PROJECT: HSR103 PAGE 1

FLESENT Zn F Ba UNITS PPM m m

JS001DUPLICATEJS002JS003JS004

57608196

105

506526561

1072508

955 JS037932 JS038918 JS039898 JS040

1010 3S041

319 111 1020266 1607 8000160 411 891143 325 741133 338 7511- JS005

JS006JS007JS008JS009

190117243559212

849556284266173

760 JS042705 JS043611 JS044622 DUPLICATE436 JS045

152 362 697161 441 850

77 530 77883 540 81381 470 785

JS010DUPLICATE3S011JS0123S013

7378

1197377

408410404354*25

793 JS046745 JS047737 JS048818 JS049637 JS050

113 449 1760112 556 112066 366 100071 464 123075 369 793

JS014JS015JS016JS017JS018

3409565

134133

196361361

16172340

445 JS051731 JS052774 DUPLICATE872 JS053

1170 JS054

93 401 585209 476 902220 486 862174 135 25986 626 808

DUPLICATEJS019JS02QJS021JS022

13875647990

2390404504447601

1120 JS055869 JS056982 JS057

1080 JS0581550 JS059

53 396 783220 464 661121 624 691

82 373 53699 484 572


7178

2046752

306222523540411

1000 JS0601030 JS061824 JS062882 JS063777 JS064

84 403 60560 432 71689 444 74384 297 75440 282 738

JS028JS029JS0303S031JS032

127122119

54327

377425430322202

754 JS065764 JS066762 JSC67666 JS068634 JS069

69 341 801119 377 666501 J83 611152 530 732

59 412 648

1JS033JS034JS035DUPLICATEJSQ36

135259460476278

411383355346126

780 DUPLICATE 100 413 883870 JS070850 JS071825 3S072

1690 JS073

116 174 965144 466 953J51 6C4 831

94 Sil 889

1

11L"

l1

Bond* -Clegg 4 Compuy Ltd.5420 Camtek Road

(613) 749-2220 Idex 053-3233

REPORT: 089-51466,0

SAMPLE ELEMENT NUMBER UNITS

JS074 3S075 JS076 JS077 JS078

DUPLICATEJS079JS080JS081JS082

ZnPPM

84 76 68

103 123

1233182

10877

Fm

440 337 383 475 520

536409411519438

Et^mmBOM

Ba PPM

1000 804 869

1020 1150

1170985857997743

9f*9^wuknnsB MHIfUOb

SAMPLE NUMBER

.

JS111 3S112 DUPLICATE JS113 JS114


PROJECT: HSR103

GeochemicalLab Report

PAGE 2

ELEMENT Zn UNITS PPM

82 33 36 53 98

80103925477

F BaPPM PPM

531 872 384 789 377 765 3*6 811 371 777

422 7il297 703*53 761337 721331 795

JS083JS084JS085JS086DUPLICATE

27455615352

462395374374360

880863880860822

JS120 308DUPLICATE 299JS121JS122JS123

29577

190

115 386110 383

3540 466429 689251 547


55149

6274

191

365399454357336

8162860943916

1160

3S124JS1253S126JS127JS128

23249

29122893

77 205457 719

76 33091 169

404 605

i JS092 JS093 JS094 JS095 JS096

189 171

77 171 165

745 902 339

1422 557

878 414 822

1630 5420

JS129 JS130 JS131 JS132 JS133

226 82

316113 121

147 564 543 1030 204 600 449 796 483 835

JS097 JS098JS059JS100JS101

69 23tt8075

r443355504

869 788844822993

JS134 JS135JS136JS137

183 9973

113DUPLICATE 119

5*1 975 459 957365 942439 8144*9 835

JS102JS103DUPLICATEJS104JS105

7780855945

474546541464402

97314101400999

1000


97204

93129140

395 757465 880669 880531 705651 651


8062

1077893

603.551

493523429

768835953909805

JSH3JS144J SI 45JS146

12786

103125

DUPLICATE 129

471 690701 811280 6SO279 74?291 766

l

lI Ottawa^kirio

K1J8)^ (fil^ 749-2220 T*

Boodv-Ckn A Company Ltd.5420 Canotek Road Geochemkal

Lab Report(613) 749-2220 Tdex 053-3233

^ REPORT; 089-51466.0

1 SAMPLE ELEMENT NUMBER UNITS

ZnPPM

F PPM

Ba SAMPLE PPM NUMBER

PROJECT: HSR103

ELEMENT Zn F UNITS PPM PPM

PAGE 3

BaPPMJ~

JS147 JS148 JS149 JS150 JS151

80 88 75 79

131

393 385 478

1034 422

744 J Si 84 823 JS185 600 JS186 591 JS187 666 JS188

96 587 78 395

103 309 145 287 60 425

835 856 768 785

1120W

JS152 JS353 JS154 DUPLICATE JS155

100 83 56 60 37

475 498 580 563 639

832 DUPLICATE 660 JS189 940 JS190 910 JS191 765 3S192

66 429 68 417 85 395 67 404 62 326

1160 969 963 981

1090hiJS156 JS157 JS158 JS159 3S160

JS161 JS162 JS163 JS164 JS165

52 42 52 71 67

61 57 52 30 29

601 566 632 476 642

493 533 610 784 768

729 JS193 598 JS194 750 JS195 711 JS196 809 OS197

785 JS198 875 JS199 940 JS200 643 JS201 890 JS202

62 349 122 530 138 489

94 891 89 402

153 670 94 627 76 460 61 413

283 581

1200 897 900 944 775

812 778 762 726

1100

1iii-ii- i

JS166 JS167 JS168 JS169 JS170

JS171 DUPLICATE JS172 JS173 JS174

JS175 JS176 JS177 JS178 JS179

JS180 DUPLICATE JS181 JS182 JS183

85 111

89 93 72

242 255 137 118

87

54 56 97 98

257

360 374 144 1C4

75

788 471 409 479 404

345339 535 622 442

360 372 378 373604

438 444518 393315

952 JS203 97 439 878 JS204 86 465 762 JS205 69 461 762 DUPLICATE 94 482

1110 JS206 83 517

732 JS207 714 JS208 829 JS209 992 JS210 800 - JS211

81 523 83 684 58 261

134 506 135 471

862 JS212 74 410 809 JS213 127 595 886 JS214 119 444

1020 *v DUPLICATE 123 411 2050 JS215 80 493

2230 JS216 2250 JS217 1130 JS218 1170 JS219

924 JS220

126 519 95 521

100 427 312 658118 396

940 768 8SO 837 801

893 768 679 804 655

780 885 843 852 825

861 873744 532

i

1Boodtt-Uttt 4 Company Ltd. Bp^Bl5420 Cjttek Roed Hl^E

I ottaw^Burio B^^^M K1J 8)^^ ^^^^^^(613) 749-2220 Idee 053-3233 BONDM

1REPORT: 089-51466.0

M.

1 SAMPLE ELEMENT Zn F 6d^ NUMBER UNITS PPM PPM PPM

JS221 176 436 730JS222 116 481 822DUPLICATE 121 489 791JS223 92 472 788JS224 172 449 720

JS225 115 423 590JS226 88 453 782JS227 88 495 1080JS228 93 388 958JS229 126 561 1620

JS230 75 301 1970JS231 151 562 1530JS232 107 632 1640JS233 75 415 949JS234 75 529 893

C GeochemicalLab Report

fc tmm M^^MHUB


SAMPLE ELEMENT Zn F 6aNUMBER UNITS PPM PPM PPM

JS235 127 588 912JS236 117 709 1110JS237 113 436 841JS238 185 656 1140JS239 170 446 797

I

1

I

1

1

1

1

DUPLICATE 176 443 788 ^ JS240 222 843 714JS241 105 1094 810JS242 108 576 800

1

11

BoMtafClea A Compuy Ltd.5420 Carattk RoadssP*(613) 749-2220 Idd 053-3233

J REPORT: 089-51466.0riSTANDARD ELEMENT NAME UNITS

8CC ROCK PULP 1989-1

Zn PPM

55 55 53 57 57

F PPM

374 383 396 374 403

E^V^^^

mSmmJUBNKUB

8a STANDARD PPM NAME

450 BCC CHEMICAL 450 469 505 474

GeochenucalLab Report

PROJECT: HSP.103 PAGE 5

ELEMENT zn F BaUNITS PPM PPM PPM

BLANK (1 (30 (1 (1 (30 (1 (1 (30 (1

585858

437348382

447 Nuiber of Analyses 8 8 8455 Mean Value 0.5 12.5 0.5488 . Standard Deviation 0.00 2.67 0.00

Lowest Value 1 ' 20 1Highest Value 1 30 1

Nuiber of AnalysesMean ValueStandard DeviationLowest ValueHighest Value

856.41.85

5358

8387.126.01

348437

8467.320.91

447505

BCC ROCK PULP 1988 409 675 995*Q7 654 587389 781 946i09 645 1030

I11

BCC ROCK PULP 1989-2

Nunber of AnalysesMean Value Standard Deviation Lowest ValueHighest Value

454 499 511 513

4494.3 27.54

454513

313 331 348 303

4323,1-19.89

303348

546 Nuiber of Analyses 4 4 4 550 Mew Value 403.5 688.8 989.5 598 Standard Deviation 9.71 62.77 34.49 612 Lowest Value 389 645 946

Highest Value '09 781 1030

4576.5 33.44

546612

! i

BCC CHEMICAL BLANK

d (i

(20(20 (20 (20 (30

(1

d

l l l

Boodir-Ctegg ft Compuiy Lid.5420 GMtic Road

KU8X5(613) 749-2220 Tdex 053-3233


REPORT: 089-51489.0 ( COMPLETE ) REFERENCE INFO:

CLIENT: DERRY, MICHENER, BOOTH t KAHL PROJECT: HSRlOi

SUBMITTED BY: T. DICKSON DATE PRINTED: 30-JUN-89

I ORDER

1 2

Ba Zn

ELEMENT

Bariuc Zinc

NUMBER OF ANALYSES

299299

LOJiER DETECTION LIMIT

1 PPM 1 PPM

EXTRACTION

Hf-HCi04-HN03-HCl HCL-HN03, (3:1)

METHOD

DC Plasra Atonic Absorption

3 F

SAMPLE TYPES

SOU———

Fluo-ide 299 20 m

NUMBER

—m-SI2E FRACTIONS

•80

M2C03-KN03 FUSION Soscific Ion

SAMPLE PREPARATIONS NUKBE*

Drv.iiPTB -8Q m

REMARKS: SAMPLES JS-300,430 AND 431 WERE NOT RECEIVED. < *EANS LESS THAN

REPORT COPIES TO: LO. TRINOER INVOICE TO: I.D. TPIMOER

l l l l

11ffr

Boodar-Ckgg 4 Company Ltd.5420 Cajêk RoadOttawajj^wio K1J 8X5^(613) 749-2220 Tdex 053-3233

REPORT: 089-51489.0

SAHPiE ELEMENT WBE* INI "S

JS-243 DUPLICATE JS-244 35-245 JS-246

6ap PH

928 910 635 584 691

InPPI

87 65

120 124 103

PW*E*M•^ÂA^^hM^M ^Â a^^k^hBONDMHUGG

F SW'LE PP* 'Jl'WE*

562 JS-279 595 jS-260 481 JS-281 280 JS-282 423 JS-283

GeocfaemkalLab Report

PSOJECTs HS9J03 PAbE 1

ElEKtN! 63 Zn FUNITS PH P-^ PP**

703 52 352 7iO 50 254

1070 81 3i7 778 56 /56 733 66 292i JS-247

JS-248 35-249

' JS-250JS-251

778 619 673804780

113 70

1747651

331 3S-284 371 JS-285 403 JS-286

1105 DUPLICATE556 JS-287

937 79 333818 85 738 808 44 342835 48 350764 66 349

JS-252DUPLICATEJS-253JS-254JS-255

734761600

1155945

9398

3175852

281 JS-288303 3S-289310 JS-290566 JS-291416 JS-292

742 57 357816 61 370

1470 242 399782 64 351995 150 270

JS-256JS-257JS-258JS-259JS-260

756717745350749

6762479275

388 JS-293365 JS-294324 DUPLICATE513 JS-295634 JS-296

792 70 iC6804 66 47 1787 74 WO607 87 389648 J3 J14i DUPLICATE

35-261 JS-262 JS-263 JS-264

774 752 725 764 713

81 53 70 68 55

647 JS-297 366 JS-?98 456 JS-299 476 JS-J01 445 JS-302

797 52 5J8 719 60 i93 734 63 373 547 *8 374 719 121 81

1- JS-265JS-266JS-267JS-268JS-269

734722725634712

**-:758856

426 JS-303392 JS-304

: 455 jS-305406 JS-306393 JS-307

668 114 3:6943 194 338873 70 383869 102 537763 83 Ji4

I- - -JS-270JS-271JS-272JS-273JS-274

7bb676783766671

485455

104114

403 JS-308357 JS-309356 JS-310369 JS-31135? JS-312

690 ' 78 434840 113 476847 97 544808 45 353583 56 m

1JS-275JS-276JS-277DUPLICATEJS-278

693239655672706

103218

778281

391 DUPLICATE105 JS-313555 JS-314579 JS-315375 JS-316

^94 62 361540 143 'M602 84 529634 75 310670 55 s59

1

11

Boodir-Qeg A Compwiy Ltd.5420 Ca^k RoadOttawal^pirio

(613) 749-2220 Ida 053-3233

j REPORT: Q39-51489.0

r SAMPLE ELEMENT IYJK3EP UNITS

3a ZnPPH

^^^^^•I^^^^BE5w^

F SAHPtE PPH NijrtSEP


PPOJiCT: HS*103 PAGE 2

FLE*ENT 5a in FUNITS PPH P?* PPH

i JS-317 JS-318 3S-319 JS-320 JS-321

DUPLICATEJS-322JS-321JS-324JS-325

565 617 576 572 756

743823737219854

34 31 74 48 39

4222957355

299 JS-J54 293 JS-355 480 DUPLICATE 310 J S- 356 281 JS-357

288 J S- 358317 JS-359377 JS-360

96 JS-361312 JS-362

S55 70 392 714 62 3 ?1 718 65 3*5 595 66 513 768 77 ?G5

1010 70 472796 55 4178?3 69 w*

1 847 58 490817 78 451

JS-376JS-327jS-328JS-329DUPLICATE

836830692645605

11662

156209m

3i8 JS-:63281 DELICATE3iO JS-364519 JS-365517 JS-366

657 79 *23684 76 472622 54 49675 76 491618 47 47

JS-33035-331JS-332JS-333JS-334

110021 40889703703

8894

13583

135

227 JS-3677G8 JS-368466 JS-369489 JS-370369 JS-371

403 282 144731 76 "74725 81 518666 51 583678 77 421

i JS-335 JS-336 JS-337JS-338JS-339

616 777

1500590662

239 188 456105140

147 JS-372 520 JS-373 152 JS-374382 JS-375340 JS-376

523 J8 349 528 62 383 606 83 506606 113 451659 101 475

JS-340JS-341JS-342JS-343JS-344

630703742593712

637278

17289

401 JS-377348 J S- 378470 JS-379601 JS-360

737 149 500757 75 325727 41 332794 70 378

293 DUPLICATE 746 77 is3

JS-345JS-346DUPLICATEJS-34?JS-3J8

224724668795752

26531336864

130 JS-j&l281 JS-332276 :S-:83366 JS-334349 JS--65

m 7 9 J37544 20i 2i9779 66 i52731 6- 629758 54 i? 2

JS-349JS-550JS-351JS-352JS-353

750623574383531

53169179; 0366

383 JS-386468 :-S-:87524 JS-333371 JS-369

703 63 406150 233 *i713 55 4o:975 106 545

394 DELICATE 1020 114 5i.

l

11

Boodar -Clegg A Compuy Ltd.5420 CaMgk RoadKuix!^"0(613) 749-2220 Tdex 053-3233

?EP09T: 089-51489.0

riSANPiE ELEHENT

35-390 35-391 35-392 35-393 35-394

63PH

753 778 822 750 742

ZnPPI

60 54 63 62 71

WS&f^^^s^^BONOAR-OEGG

f S .A^.EPPH fU'SE*

410 35-427

465 35-429 4)9 35-432 389 35-433


PROJECT: KSRI03 PAGE 3

ELEMENT e? i n f

775 6J JiC :52 65 i&tf 764 92 4.9 7iO r',9 356 743 60 3-54i 35-395

35-395 35-397DUPLICATE3S-3S8

676 704 777720601

70 94 818658

395 DUPLICATE 370 JS-434 398 3S-435409 OS-436353 35-437

721 67 379 766 130 451 791 65 346724 69 423763 83 358

35-39935-40035-40135-40235-403

634618651755727

697058

11736

412 OS-438384 J S- 439359 OS-440435 OS-441316 OS-442

837 58 445816 117 iOO652 38 440812 75 413682 99 540

35-40435-40535-406OS-40735-408

691707793707614

3560428453

317 OS-443393 3S-444391 OS-445349 OS-446418 OS-447

506 127 658780 73 826762 142 *69747 62 324770 75 353

j 35-40935-4*0 05-411 35-412 . 35-413

3S-4;4

DUPLICATE35-4)535-416JS-4]7

686651 684 7C4 710

793 795 693775775

6971 92 68 62

SO 97 767181

414 JS-448374 3S-449 381 33-450 355 DUPLICATE 353 3S-451

336 35-452 328 OS-453 374 3 S- 454416 05-455410 3S-*56

715 360 538760 122 S29 294 128 155 'M 1 35 176 704 65 500

729 64 J63 729 73 10-54 686 93 '09720 83 416833 87 35 i

35-41835-41935-42035-42135-422

581791780766825

6382

1057075

374 3S-457356 3S-458

1777 35-459

1230 382 495822 182 J0118624 88 398

408 DUPLICATE 656 87 *13532 35-460 690 158 i?9

i

35-423DUPLICATE35-42435-42535-426

823752BOO797752

71768957SO

454 35*^61458 35-462481 35-^63391 35-464454 3S-J65

678 74 4j5609 62 395574 61 3:0621 69 395792 121 659

l

11

BMdv-Cfea A Company Ud.5420 CaMttjc Road

SumP*(613) 749-2220 Tdra 053-3233

^9^^| Geochemkal

J REPORT: 089-51439.0

r SAMPLE ELEMENT h'J'dER UNITS

8aP?H

ZnPPH

"^ - - K^^BM^^BK im m aa*^fc^^

BMMR-CLEfiG

F SAMPLE

Lab

PROJECT: HS*1Q3 PAGE

Report

4

ELEMENT Ba in F PPC,

IJS-466 JS-467 DUPLICATE JS-468 JS-469

JS-470JS-475JS-476JS-477JS-478

603 585 665 594 647

709602633555594

71 98

107 58 64

756879

10675

397 3S-506 416 JS-507 422 JS-508 519 JS-509 563 JS-510

475 JS-511484 JS-512450 JS-513532 JS-514434 JS-515

832 168 807 72 183 1?3 618 225 663 85

605 147659 138648 48648 83475 105

393 80

153 411

293343312470544

JS-479JS-430JS-481JS-482JS-483

645551697549608

7383777956

388 JS-516376 JS-517452 JS-S18448 JS-519367 JS-520

655 106793 234768 2C4719 76613 143

344309378465iCO

JS-484JS-485JS-486JS-487JS-488

521537563540771

7077788090


564 188729 39681 42661 50673 39

414'03391315386

1

1

DUPLICATE JS-489JS-490JS-491JS-492

776 744810746701

96 59524562

362 JS-525 469 JS-526434 JS-527574 irv JS-528329 JS-529

622 114 580 217619 1*0514 130619 71

927240452266779

JS-493JS-494JS-495JS-496JS-497

750804860848658

5361,.676672


371 322780 57808 59783 39731 57

91328353347378

DUPLICATEJS-498JS-499JS-500JS-501

7021440693

1030727

76255

78185

S6

627 JS-534596 JS-535502 JS-536659 JS-537379 35-538

826 i 00863 44777 61706 627 i i 12

'61355; B6i a'05

JS-50ZJS-503JS-5GSJS-505DUPLICATE

838565635677654

10092

205180186

473 JS-539362 DUPLICATE295 JS-540261 JS-5*i275 JS-542

111 55671 '8

4304J5

927 227 1077838 71165 373

2KB161

l

l l

BoMtv-Ckf8 4 Company Ltd.5420 CMttk Road

K1J8X5(613) 749-2220 Tdex 053-3233


REPORT: 089-51489. 0 PROJECT: HSR103 PA6E 5

l

SAMPLE ELEMENT UNITS

JS-543 JS-544 JS-545 JS-5J6 JS-547

8aPPI

IsT610 570 6?3 61?

~734~

ZnPPI

~75~

75 71

147 57

~9T

fPPIH

446478555577432

SAMPLE ELE-ENT '.'"HS

8? Zn F PF1

l

11

Boodv-Ckjg 4 Company Ltd. ••^iU*) Cj^jk Road Kg^P^^^ GeocbemkaiOttawa,^Pbio ^^^^tf^^^^B Iflfr RCpOTt K1J 8X5 ^^^^^^^ ^^^^^^ (613) 749-2220 Tdex 053-3233 BONDAIM1EGG

I RcPQPT: 089-51439. 0

STANDARD ELEMENT Ba Zn FNA^E t'Nl'S PPC, PPM P?*

PROJECT: Hj*103 PAGS 6

STANDARD ELEMENT Ba Zn FNAdE L* US PPK P?* PP*

BCC ROCK PULP 1S69-1 450 53 365460 53 417460 52 331473 53 379490 54 449

BCC CHEMICAL BLANK ci ci cjOd ci c30<l ci cjOd ci c30<l ci c30

562 53 399485 52 393569 53 401464 53 400

<l <l <30*:1 <l <30<l <l ^0<l ci <30

Nunber of Analyses 999*ean Value 490.3 52.9 392.7Standard Deviation 44.46 0.60 32.95Lowest Value 450 52 331Highest Value 569 54 449

Nurber of Analyses 999Hean Value 0.5 0.5 15.0Standard Deviation 0.00 0.00 0.00lowest Value 1 1 30Highest Value 1 1 30

BCC ROCK PULP 1989-2 540 56? 550 450 500

458441447428414

276241268276282

BCC ROCK PULP 1988 1030500

10231024

376381373375

655715678675

Nuwber of Analyses 4 4 4Hean Value 894.3 376.3 680.8Standard Deviation 262.85 3.40 25.01Lowest Vaiue 500 373 655Highest Value 1030 381 715

Ninber of Analyses 5 5 5Mean Value 520.6 437.6 268.6Standard Deviation 45.95 17.07 16.21lowest Value 450 414 241

Va'iue 563 458 282

l

11™

1!

Bmdv-Ckgg 4 (Jompuy Ltd. •••M Uttr^lcRnaH KjgfOttawa^Bario ^T^^J| K1J 8X^^ ^^^^^^^(613) 749-2220 Telex 053-3233 BONDAI

REPORT: 089-516:6.0 ( COMPLETE )

CLIENT; DERRY, MICHENER, BOOTH i WAHL PROJECT: HSR103

NUK8ER OF LOiiE ORDER ELEMENT ANALYSES DETECTION

1 Ba Barium 108 1 F 2 Zn Zinc 108 1 P

3 F Fluoride 108 20 f

SAMPLE TYPES NUMBER SIZE FRACTIONS

SOIL - _ . ..—1B&— , ,.,,,-..,...,,...,,...-aa. ........ -. .

REMARKS: SAMPLES SS-48 TO SS-52 REC'O EXTRA.< MEANS LESS THAN

C GeochemicalLab Report

fc ^^m M^^AMUGG

REFERENCE I'-FG:

SU5C.ITTEO BY: TIM DICK'SO* DATE PRINTED: 6-.-OL-89

R L WIT EXTRACTION "EThCD

?M Hf-HC10'!-HN03-HC] DC Pi3SB3 PM HCL-HN03, (3:1) Atonic Absorotion

?M NA2C03-KN03 FUSION Specific Ion

NUMBER SAMPLE PREPARATIONS NUMBER

———— m ———— Qcyr&Uva -ifl ————— 108 .- — -..

REPORT COPIES TO: 1.0. TRINOERFAX TO TORONTO OFFICE

INVOICE TO: 1.0. TRINOEP

;

l

11

Bowhf -Clegg Si Company Ud.5420 C^ttk RoadKU8X5^

(613) 749-2220 Tdex 053-3233

J REPORT: 089-51636.0rL

SAKPLE ELEMENT NUMBER UNITS

SS01 DUPLICATE SS02 SS03 SS04

BaPPH

300 336

848690

ZnPPH

201 228

98 150 122

^^^^J*^^^^"*^^^^^•^^^^JB

BONDMHUGG

F SAKPLE PPH NUMBER

77 SS37 79 SS38

263 SS39 359 SS40 353 SS41



ELEMENT Ba Zn F UNITS PPH PPH PPH

841 150 371 1049 150 353 834 109 303 787 123 349

1144 189 )54

SS05SS06SS07SS08SS09

61718481380596727

132283283286139

351 SS42294 SS43330 SS44176 DUPLICATE329 SS45

1554 134 372832 209 718935 143 317994 155 283

1144 119 351

SS10DUPLICATESS11SS12SS13

634611491

1067945

171187228208133

348 SS46356 SS47194 SS48396 SS49351 SS50

1050 109 2481848 239 226

641 100 292801 93 353S84 191 343


18205936106418902814

227138132190272

375 SS512650 SS52

378 DUPLICATE333 SS53153 SS54

692 115 380833 343 i03805 363 406476 208 267511 205 227

•~~

1\i

DUPLICATESS19SS20SS21 SS22

2926204415261085 620

291169159123

56

135 SS55325 SS56302 SS57323 SS58 267 SS59

710 86 248682 99 535720 98 303682 97 312 575 99 *86


639759

184810211582

5287

160111154

256 SS60301 SS61328 SS62307 SS63355 SS64

668 191 424531 122 362594 114 395643 160 :BO666 290 523


2254973

147013311133

217101172131129

331 SS65297 SS66339 SS67314 SS68402 SS69

601 m 3 33827 320 379738 171 315725 158 265797 90 282

SS33SS34SS35DUPLICATESS36

16805012

983J028

855

106185189209129

-308 DUPLICATE 846 98 255238 SS70391 SS71360 SS073382 SS074

753 170 567920 414 235813 291 432676 203 411

l

1Boodtr-Oegg 4 Company Ltd. ••A

— 5420 Cg^k Road K^f 1 Ottawa^Hario ^^^^tf l K1J 8X5 ^^^^^^^

(613) 749-2220 Telex 053-3233 BONDAffi

1

1

1

j 'EPOST; 089-51636.0

( SAMPLE ELEMENT Ba Zn F M*W U NITS P?*" PPM PP*

i sS075 673 224 383 SS076 707 245 432 SS077 806 155 536 SS078 724 ]06 329 SS079 626 145 425

DUPLICATE 658 158 J?0SS080 633 98 339SS081 805 119 445SS082 763 136 369SS083 606 ?00 282

D Geochemical Lab Report

K. ^ m V4MMt-OHJG

PRO:?CT: sSRiOi PA5E 2

SA*"LE E'.EKEKT 8a Zn fNU^BE* UNITS ^PI ??i PPM

SS084 703 231 339SS085 533 150 299SS086 623 62 204SS087 714 69 251DUPLICATE 798 79 260

SS088 844 93 297SS089 721 120 314SS090 986 187 227SS091 680 255 190SS092 939 144 262

I SS093 1023 278 233 SS094 788 97 237 SS095 895 136 346 SS096 592 100 257 SS097 862 201 285

SS098 794 89 322SS099 752 151 353SS1CO 706 128 295SS101 612 181 478SS102 617 104 337

SS103 556 245 459SS104 655 209 420DUPLICATE 640 201 420SS105 629 116 405SS106 777 88 365

SS107 1233 208 515SS108 703 109 4525S1C9 718 65 492

1

l l

Bowkr-Cka 4 Company Ltd.

K1JI(613) 749-2220 Tdex 053-3233


T REPORT: 089-51636.0

1 STANDARD ELEMENT Ba Zn F Y NAHE UNITS PPM PPH PPM

1 8CC ROCK PULP 1969-1 409 59 369 412 60 351 4i3 60 303 428 58 375

Nufiber of Analyses 444 Mean Value 415.4 59.3 349.5 Standard Deviation 8.56 0.96 32.63

' Lowest Value 409 58 303 Highest Value 428 60 375

BCC ROCK PULP 1989-2 606 484 254 517 503 270

I Nunber of Analyses 222 Nean Value 561.6 493.5 262.0 Standard Deviation 63.07 13.44 11.31 Lowest Value 517 484 254 Highest Value 606 503 270

PROJECT-. HSR1Q3 PASE 3

STANDARD FLEHENT Ba Zn F NAME UNITS PP* PPM m

BCC ROCK PULP 1988 965 A 12 557 946 398 557

Nurber of Analyses 2 2 2 Hean Value 955.5 405.0 557.0 Standard Deviation 13.44 9.90 0.00 Lowst Value 946 398 557 Highest Value 965 412 557

lT BCC CHEMICAL 8LANK ci

^(1(1

ci c30ci c30ci c30ci c30

1

Nunber of Analyses 4Mean Value 0.5Standard Deviation 0.00 Lowest Value 1 Highest Value 1

1

4 40.5 15.0

0.00 0.00 1 30 1 30


APPENDIX 2

PROPOSED DIAMOND DRILL PROGRAM - DETAILED BUDGET

DERRY. MICHENER. SOOTH a WAHL

l l l l l l l l l l l I l l l l l l l

DERRY, ENER, BOOTH i. WAHL

REPORT DATE 10AUG89 RUN NO. 1714:49

PROJECT - DETAILED COST PER ACTIVITY

FINEST HOUR

COST CONTROL ACTIVITY REPORT

HARRINGTON SOUND - PHASE II EXPL PRG

START DATE 1SEP89 FIN DATE 80CT89

DATA DATE 1SEP89 PAGE NO. 1

COST ACTIVITY ID RESOURCE ACCOUNT

HSR103Z101 PREFIELD PLANNINGRD 5 ES 1SEP89

GEO PROJ M20GEO SR M20

TOTAL :

HSR103Z111 SITE VISITRD 4 ES 16SEP89

GEO SR F30MEALS 8300TRUCK 8304LODGING 8300

TOTAL :

HSR103Z701 MOBILIZATIONRD 1 ES 6SEP89

GEO PROJ F38MEALS 8313TRUCK 8304

TOTAL :

HSR103Z702 DIAMOND DRILLINGRD 15 ES 7SEP89

GEO PROJ F34LODGING 8322MEALS 8313TRUCK 8304ASSAYS 8332D/MOB OR 8336DRILLING 8336CORE BOX 8338DRIL KIT 8315FD SUP 8315OFF SUP 8314

ACCOUNT UNIT PCT ACTUAL ACTUAL ESTIMATE TO CATEGORY MEAS BUDGET CMP TO DATE THIS PERIOD COMPLETE

EF

LL

EF

LXXX

EF

LXX

EF

LXXXXXXXXXx

5SEP89 LS 1SEP89

/HR/HR

17SEP89 LS 20SEP89

/HR/DAY/DAY/DAY

6SEP89 LS 6SEP89

/HR/DAY/DAY

21SEP89 LS 7SEP89

/HR/DAY/DAY/DAYEAUNIT

L F 5SEP89 T F

1699.95770.00

2469.95

00

0

LF 21SEP89 TF

1540.00100.00180.00120.00

1940.00

0000

0

LF 6SEP89 TF

339.9925.0090.00

454.99

000

0

LF 21SEP89 TF

5099.85600.00375.001350.001400.002000.00

/FT 34500.00/FTUNITUNITUNIT

575.00250.00750.0050.00

00000000000

0

.00

.00

.00

4

.00

.00

.00

.00

.00

0

.00

.00

.00

.00

0

.00

.00

.00

.00

.00

.00

.00

.00

.00

.00

.00

.00

.00

.00

.00

.00

.00

.00

.00

.00

.00

.00

.00

.00

.00

.00

.00

.00

.00

.00

.00

.00

.00

.00

1699.95770.00

2469.95

1540.00100.00180.00120.00

1940.00

339.9925.0090.00

454.99

5099.85600.00375.001350.001400.002000.00

34500.00575.00250.00750.0050.00

FORECAST VARIANCE

1699.95770.00

2469.95

1540.00100.00180.00120.00

1940.00

339.9925.0090.00

454.99

5099.85600.00375.001350.001400.002000.00

34500.00575.00250.00750.0050.00

.00

.00

.00

.00

.00

.00

.00

.00

.00

.00

.00

.00

.00

.00

.00

.00

.00

.00

.00

.00

.00

.00

.00

TOTAL 46949.85 .00 .00 46949.85 46949.85 .00

l l I l l l I l I l l lIl l l l l l

DERRY, H^^ER, BOOTH 8, UAHL

REPORT DATE 10AUG89 RUN NO. 17 14:49

PROJECT - DETAILED COST PER ACTIVITY

ACTIVITY ID RESOURCECOST

ACCOUNT

FINEST HOUR

COST CONTROL ACTIVITY REPORT

HARRINGTON

START DATE

DATA DATE

ACCOUNT UMIT PCT ACTUAL ACTUAL ESTIMATE TO CATEGORY MEAS BUDGET CMP TO DATE THIS PERIOD COMPLETE

SOUND -

1SEP89

1SEP89

PHASE II EXPL PRG

FIN DATE 80CT89

PAGE NO. 2

FORECAST VARIANCE

HSR103Z706 DEMOBILIZATIONRD 1

GEO PROJTRUCK

TOTAL :

ES 22SEP89

F388304

HSR103Z707 DATA COMPILATION iRD 15

GEO PROJGEO SRDRAFTWPROCESSCADDPRINT

TOTAL :

ES 23SEP89

M20M20M21M22M278356

EF 22SEP89

LX

REPORTE F 70CT89

LLLLLX

LS 22SEP89

/HR/DAY

LS 23SEP89

/HR/HR/HR/HRHRUNIT

LF 22SEP89 TF

339.9990.00

429.99

00

0

L F 70CT89 T F

5099.85770.00900.00900.001250.00200.00

9119.85

000000

0

0

.00

.00

.00

0

.00

.00

.00

.00

.00

.00

.00

.00

.00

.00

.00

.00

.00

.00

.00

.00

.00

339.9990.00

429.99

5099.85770.00900.00900.001250.00200.00

9119.85

33990

429

50997709009001250200

9119

.99

.00

.99

.85

.00

.00

.00

.00

.00

.85

.00

.00

.00

.00

.00

.00

.00

.00

.00

.00

HSR103Z999 CONTINGENCYRD 0

OWING

TOTAL :

ES 80CT89

REPORT

E F 80CT89

X

TOTALS

LS 80CT89

UNIT

L F 80CT89 T F

6135.37

6135.37

67500.00

0

0

0

0

.00

.00

.00

.00

.00

.00

6135.37

6135.37

67500.00

6135

6135

67500

.37

.37

.00

.00

.00

.00


APPENDIX 3

TECHNICAL DATA STATEMENT


1 1 1 1 1 I 1 1 I 1 1 1 1 1 1 1 i i i

Ministry of Geophysical-GeologicaJ-Geochemicai Northern Development Technical Data Statement and Mines

W O ntario File

! TO BE ATTACHED AS AN APPENDIX TO TECHNICAL REPORT j i FACTS SHOWN HERE NEED NOT BE REPEATED IN REPORT }

TECHNICAL REPORT MUST CONTAIN INTERPRETATION, CONCLUSIONS ETC. i

Type of Survey(s}

Township or Area 'f)ftOCC avicL )tU A^T l iVC\ O o *J T tv/^ .

Claim Holder(s) Hrlv'/'irw K.-."\ OC^VicL KCSCU. VGLS WC

5~CC - (s'l R.lcl\kV\CiVtt Sk W. lovartrC

Survey nompanv De V i y | "J'cAe^*!/ ; RcoTtv ^ tUakl

Author of Report flM DlCKiOAj*

AHHress of Anthor H 10 - 2o f? ick^WTv^t ^1- - S . TbrcTK ft)

^ ' (linecutting to office)

Total Miles of T.ine Cut

SPECIAL PROVISIONS DAYS ; CREDITS REQUESTED Grnphysiral P"^*"" i

1 j

Electromagnetic. . -,.., } ENTER 40 days (includesline cutting) lor lirst B

i survey Rndiomftric.... . i

1 F.NTF.R 20 days for each -Othrr |

j additional survey using r.eo|oojral ^ O )i same grid. " . -i/*. j| l*enrherm'-?M.., ,fcV, '

AIRBORNE CREDITS (Special provision credit! do not apply to airborne turveyi)

Magnetometer. Elertromagn**'^ . .,,.,., ,. ,. R^HjometiHr(enter dayt per daim) *-

HATR: /ffi'/ '0 /fe^ S jr.rCATTIRF.: /tfi^l^C^^—-J ' Author of Report or Agent

Res. Geoi. Qualifications Ai J 1 O *.) (f?

Previous SurveysFile No. Type Date Claim Holder

MINING CLAIMS TRAVERSED List numerically MfVOoC

S /T) i tJ cf er^J 3 \^ f [ Q J f- J

(prefix) (number)

T48 *26

?27^^ J Of ^ ^ o

c^cjy 7 7 ^ 1M

e uV 7 f-* -

. ............................7..7.Z... \77^ 1771

7^0

"7V J

7?2.HM/ur^j^/v;

so 7^ a ^ i^? 2.

7^57r74*5^0

..............................S.!...

!37 185/12)

lGEOCHEMICAL SURVEY - PROCEDURE RECORD

Numbers of claims from which samples taken.cHg77 (7 , 393-778. W 8 77H . HK777, 31* 776 . 133777, -7*85^1

iS*

l

l

Total Number of Samples Type of Sample____oL-

(Nature of Material)

Average Sample Weight Method

I

I

l

Soil Horizon Sampled— Horizon Development—Sample Death———' " ~*

4- f -VTVrraip T KXT————————

Drainage Development——Q.Estimated Range of

O.jO -^ H

cccL

l

I

l

l

l

l

ANALYTICAL METHODS

Values expressed in: per cent CLp. p. m. [Zfp. p. b. D

Cu, Pb, (^ZnJ) Ni, Co, Ag, Mo, As.-(circlc)

Othrr* F I

Field Analysis .tests)Extraction Method.

Field Laboratory AnalysisNo. (-—^—————— .tests)

SAiMPLE PREPARATION (Includes drying, screening, crushing, uhing)

Mesh size of fraction used f c

F.vtrartjon

Commercial LaboratoryOf Laboratory 6o.-X?(c,v C l**3f

Extraction t/Cl ^ ?O

Xt A- 4-

General.

Ministry ofNorthern Developmentand Mines

Report of Work DOCUMENT NO.(Geophysical, Geological, VV8909Geochemical and Expentlriui'ti)' ' "

Mining ActType of S urveyts)

— .JSri^'-Claim H older(s)

Township o r Area (.tY]IOL,\

Address

Prospector's Licence No.

Survey Company

, .Name and Address o f Author (of G eo-Technical report)

..; f TR,~±iZJ2- 4tQ - 2c

TDate of Survey (from sTtoT"HS M l 2iTotal Miles o f line Cut

Credits Requested per Each Claim in Columns at right Mining Claims Traversed (List in numerical sequence)Special Provisions

For first survey:

Enter 40 days. (This includes line cutting)

For each additional survey: using the same grid:

Enter 20 days Ifor each)

Man Days

Complete reverse side and enter total(s) here

Airborne Credits

Note: Special provisions credits do not apply to Airborne Surveys,

Geophysical

- Electromagnetic

- Magnetometer

- Radiometric

- Other

Geological

Geochemical

Geophysical

- Electromagnet

- Magnetometer

- Radiometric

- Other

Geological

Geochemical

Electromagnetic

Magnetometer

Radiometric

Days per Claim

ZQ

Days per Claim

Days per Claim

Expenditures (excludes power stripping)Type of Work Performed

Performed on Claim(s)

Calculation of Expenditure Days Credits

Total Expenditures

S * 15

CTotal

Jays Credits

Instructions Total Days Credits may he apportioned at the claim holder's choice. Enter number of days credits per claim selected in columns at right.

Date Rii orded HokrtrrrÂge-it (S^gnature\

^

Mining ClaimPrefix

2':- 1 '

•^t-M''"' ' "' J

XAt^^1

.yJtJ1

ONTAK AS

Number

•f 4ft S z S

^4852.^^46 ^"2-T-^48^2.69ê?7.4^87-?-^

^^ft't^C*tfjc^ feT-T-l,

^9 E"??6^677-î

?-4fto4?*ttB?e/O o CL tiC^ *"?

9-4 B si \^48bZZ?-46^2.5"

-H&s&oL tT" \i J 4* 1

0 OIOLOOICAL 1SESSMENt Fit

OFFICE

Expend Days Cr

v,-

^^^l/V

Vsss

V

S

^

^-s

v'

,V1

v

y

uRvevBS

uti z 4 iyoy

R [*r*i-iitfr\

Total Djys C i. Recorded

^-JCertification Verifying Repolt of Work

1 hereby certify that 1 have a personal or witnessed same during and/or after

K)ffic! iXefent^^^

Mining ClaimPrefix

sour

AM-36

'*

- - .

Number

iERfroNrARio^fjrntOElVEI

-AUG4-5 19

18110.11.12,1, sg

U!

; --nqn'"W

-

——— ~ ' ——

'

Expend. Days Cr.

iGoTvisio)

.9 ——— PM-

aifr*L

9-

'. * - . i-

Total number of mining claims coverea by this *2 f*' report O* work, ^-V— .

/iDate Recorded ^'f'ln fl ^ e

PUiou?.Jl^

[Date ApprbvecTas Recorded '"'Bra*h tfcrbafor f g j jyî ^/c*^p*v**-* — * '

Qr^

and intimate knowledge of the facts set forth m the Report of Work annexed hereto, having performed the work us completion and the annexed report is true.

Nome and Postal Address of Person Certifying

^ * . ™ . .-^ ., MC

r 4lo - 2o T.c^ô^ Sree&r &KT

c 9\^qDate Certified Cfiflified by iSiqoajxire) \

V T \

•a

^

Ministry ofNorthern Development

Mines

tc&ff •Zfx-tX'i'~ ? ,Zb

Report of Work

(Geophysical, Geological, Geochemical and Expend!

DOCUMENT No. W8909*-??uresT

Mining Act

Instructions: — Please type or print. "^ '— If number of mining claims traversed

exceeds space on this form, attach a list.Note: — Only days credits calculated in the

"Expenditures" section may be enteredin the "Expend. Days Cr." columns.

— Do not use shaded areas below.Typ.ofSurv.vUl

Claim Holder(s)

Address

^ O 6S WJL j^." J-3i*Vf

/^c.'V

Township or Area 0*7/0^

Pr ospector's Licence No.

Survey Company

Name and Address of Author (of Geo-Techmcal report)

Date of Survey (from ft to) [Total Miles of line Cut21} O S Sfh o -f- Ob **cJDay l Mo. J Yr. j Day | Mo. | Yr. |________

10 -2.0 gr. T5^c,J-ro ft gc 2Credits Requested per Each Claim in Columns at rightSpecial Provisions

For first survey:Enter 40 days. (This includes line cutting)

For each additional survey: using the same grid:

Enter 20 days (for each)

Man Days

Complete reverse side and enter total (s) here

Airborne Credits

Note: Special provisions credits do not apply to Airborne Surveys.

Geophysical

- Electromagnetic

- Magnetometer

- Radiometric

- Other

Geological

Geochemical

Geophysical

- Electromagnetic

. Magnetometer

- Radiometric

- Other

Geological

Geochemical

Electromagnetic

Magnetometer

Radiometric

Days per Claim

^oDays per

Claim

Days perClaim

Mining Claims Traversed (List in numerical sequence)

Expenditures (excludes power stripping)Type of Work Performed

Performed on Claim(s)

Calculation of Expenditure Days Creoits

Total ExpendituresTotal

Days Credits

-r- 15Instructions

Total Days Credits may ne apportioned at the claim holder's choice. Enter number of flays credits per claim selected in columns at right.

Mining ClaimPrefix Number

SOUTHE W ONTARIO-MINING* 3IV1SION

RECEIVED

•AM ^ 7.819.10.11,12,1,8^.^

i 1909

Expend. Dav* Cr.

PM,5,6

Total number of mining claims covered by this report Of work.

Date

/lRelorciea l i t Sianatui

Certification Verifying Report of Workl hereby certify that l have a personal and ultimate knowledge of the facts set forth in the Report of Work annexed hereto, having performed the work or witnessed same during and/or after its completion and the annexed report is true.

Name and Postal Address of Person Certifying

- Zc,Dale Certified Certified by (Signaturel

V

A

l 1 5

L L HI?

' v

L r

tyi^^^y^^v

\ /"S ^A ^ ?S FA/..

/

k t L LV!? i*

K /l -l -reMadoc Twp.

Thurlow Twp.31CI2S60895 2.12688 MADOC 200

Q. 5

TD^—O

CDen 1 c±3X

J.*.K

l x

OF

HUNTICOUNTY OF

,', HASTING ;SOUTHERN ONTARIO

.MINING DIVISION SCALE MNCH"40CHAINS

LEGENDPATENTED LAND CHOWN LAND SALE LEASESLOCATED LANDLICENSE OF OCCUPATIONMINING RIGHTS ONLYSURFACE RIGHTS ONLYROADS

IMPROVED ROADS

KINGS HIGHWAYSRAILWAYSPOWER LINES ''MARSH OR MUSKEGMINES '

(P)c.s.Loc'

L.O.M,R.O,S.R.O.

-CL^P K

: NOTES ;This Map Is Not To Be Used For purvey Purposes.40.V' 3 river*

'r, r6se;vu|lcm

OF ISSUE

: JUNO 6 1983-

SOUTHr.RM ONTARIO MINING DIVISION

PLAN NO.- M.106ONTAKIO

MINISTRY OF NATURAL RESOURCESSURVEYS AND MAPPING BRANCH

Grimsthorpe Twp

1040900A SO 040634

Huntingdon Twp. Hungerford Twp.31C125EW85 2.12688 MADOC

l J P VOH K .

210

d

cpjsl

UJ

LEGEND

HIGHWAY AND ROUTE No

OTHER ROADS

TRAILS

SURVEYED LINES

TOWNSHIPS. BASE LINES, ETC

LOTS. MINING CLAIMS. PARCELS. ETC

UNSURVEYED LINES

LOT LINESPARCEL BOUNDARY

MINING CLAIMSETC

RAILWAY AND RIGHT OF WAY

UTILITY LINES

NON PERENNIAL STREAM

FLOODING OR FLOODING RIGHTS

SUBDIVISION OR COMPOSITE PLAN

RESERVATIONS

ORIGINAL SHORELINE

MARSH OR MUSKEG

MINES

TRAVERSE M ONUMENT

DISPOSITION OF CROWN LANDS

SYMBOL

PATtNT SUPfACt i V \ ',:', Hu.)M TS

SLi^F ACF W'TjH ' . V N

LEASE SURF ACE fie M sNING "i^

SURTACt RlCjHTSONi V

" .MINING RIGHTS ON L Y

LICENCE Of O CCUPATION

ORDER IN COUNCIL

RESERVATION

CANCELLED

SAND S GRAVEL ............

BBT

OC

Ott

(DNOTE M INING RIGHTS IN P ARCtLS P ATENTED PRIOR T' *-* * ' '

1913 V ESTtLi IN O R i G i S A L P ATENTEE Bf T p- l ' w LANDS ACT RSO 1 910 C HAP 3 BO. SEC 6 3 S H',M

SCALE 1 INCH 40 CHAINS

O iDOO *000 60OO

O Mt l Rt S

1OOOi K M

JOOO 2 KM

AREAS. W ITHDRAWN FROM DISPOSITION

M.R.O. - MINING RIGHTSONLY

S R. O. - S URFACE RIGHTSONLY

M. * S . - MINING AND SURF ACE RIGHTS

OAKfipiion Order No Dale Diiposilion '

2 j 't

-00 SJRFACfc HIGM"!i Pt'St'fiVATlON A 1 ONG i Hf" SHORES OF AL l l AKTS AND RIVERS.

V 07 S"1 : P 37/12/22 MRO

SEC. i6

sec 3t.

. St f *G

W17/B8 ER 86/02/24 MRO

c Y.

DATE OF ISSUE

AU3 , o 1933

TOWNSHIP

MADOCM.N.R ADMINISTRATIVE DISTRICT

TWEEDMINING DIVISION

SOUTHERN ONTARIOLAND T ITLES/ REGISTRY DIVISION

HASTINGS

Ministry of Ministry ofNatural Northern DevelopmentResources and Mines

Ontario

Dal t MARCH 1987Nurnbat

G-1269

\|l|y

li./

\-o \

\.* \

' i t l

P

V V

V V*, v--'.'^•*^

\/\

l l l\ t y

2 r''' id t:? fh-.'t :z/ \ h' t \h. l

i4',-t•2. K:'^2

•Vf-._h^TT .-.f ; ^•.-1/-

Jî-HM-1-. -.h -'

\\ \\\

3-748523 4^748524

Jl'/ ili/.

v III x

^

* *. ' P i * t— * * ^ *. *

2

JL

O^v\

\ \\

i ** i•2.**, * *

5-998780 4.990779 TCTT7

i * ""i iP'../.'2.':-' y2 .; ; :/ ^^'

* * * ' *' ' * ^'. ' "" X . f' r :; 7

7'V

f :.tlk T

/S/O

7^hV

V

3i998779 4.998778

H ^

\, V^,. •i ^ \ '^* M 1 -

Q ^*3 V.-i" * ii *:^ !l',.^'.•: A'.'.

* i* '

3 ^.'•i 1 # y

y

\

3 i

\\1y-

3i99878

>

O CD±^D

31C13SE8005 2.I2688 MADOC 220

iRViS LAKE A, X OX \\ \ ^- {

f ~^ \ _ ..— —— - — " "^.^X \ \ l iik

"^~~~~~ -" 7 K " 7\ti:/ X sX x/ /- -^y/ ---. x ^X ^^ ' 'o /^ ' .* 3 /juii/.

j/ .X J. .... ——— ( ——— .V \^ VV^

*x^ 748527 ^//' " ^-^-'^ x/ ^ v

XX .-^ ^y /^* \1 /X * X . . ——— ... ———————— . ———————— ——————

'' ^ **/ -** \ \/ / -3 y * csx/ - * x . * Nx/ //^^ J/

/S * 'X3xx ^ - c/- ' * *'^ * -*J^ — -\ -! ———————————— -—f — - —————————————— | ————————————————

S/ ' ^ * ' * J~' ' 9^ * H/S Jf ' ' ' -' /' ')STs/ **tf*-' ^ s^"^'

s" S:' h ' 3*. -.3i /•" i i - \ -' -1 A ' ' . .\ I"-\ } 748526\\ 1 * '

\\3\ V A . ..3. 3-. ' ,,^ . A - *. '. - . v . - V- \\"-\ *-- * * "' 'A \ \ \ \ " 3 v ,-\\ \y A v R\ *A , , V \ \

\ VA v '^ - " -'" :' - .". 3 t '^ \ \\ A \\ --\3 - . '-- | .* -- : \ J v A/\ v\ ^ \\\ *." ? o- .'. y 7 j-\ \\ \ v * ' ' - - ^ * - * * ^ V./ 1- \ v -\ \ . , - * - *. v\ \\ ^ \\ *"' V\ \v \ \ vJ. \ vV ] \\ V

\ V '."i 3 \\ A\ ** .A ;/ A- J\ V"'\\ " t**\\ \ ^ ^ x \\ , H J' i \ \ A ^. \\ 748532 II //l i\\ \i\ \ \\ 11 ///3 X 1 \ \r.A \\\ .li///; X

1 ^ V. '^*. o-^^x 3: -i \\t'' 'l 1 V \ * L i ^*\\ O-^L. ,1 ! U V "f 7\ ^ I/.M3 \\ //h ,/l * \ \ /x j: 3 ( ^\ : ^ - x\ /y r \-tJ —— -i —— —— V^ —— 'l; — J:; v... ..: \N ' l".- \

1 * i - i \. II V' ; \\ " \ l y x— 77 \

/' 748524 \1 ' *1 ijJk y V^

7" ~~~^-^-~-.^ ~ ~^^~ — — ^^/' T77^^— — ,I^ —— —— - ~~^^ Hwy #7 1 —— 1

'. ....'.--- "^^— — -~^. ~^~-î 3 - :- •..TTTr^-— ———— ,, — ^-^^^î 3 •-". . .T^^^^HZr^

i 3 "^ ^^*^*^,f ' ' x^.'^^, * l —— '^ /l -i1 \ 'v Hl\ .-,.-, Trench J-5^0 ^ 3 T,i \ '. ' *" I '- : \ \ ' \ -/ -X---1 " 3 u X n\x : '-' v- lU \\ '- 'X Q ^ \ "

I *A^ Ponton 7 r j'\\ 3 l .'V; ^ Mine ^0 fi 1. '**

y . 3 s \ - TAV'*r"* ^.ri.|l : l iv * '. B w/- i- x :

X-"..1 Trench J-4/Y'" 1. ', 7 ii \ m . \ ' /ij /-••:" /

1 y 3 //"?'" ; /xi //' - 1-' : - ; " ;' ///'.-••-' ,/ XJ * 1 * l -* 1 1 l '\ i h ' l ! i\\ - : 748528 1 ^ j! \ 4.: .. ;/ ,/i \ ^' 3 v / ; ' \\ ' i * . . * - . L ! \

V . \ . I f . -r- y l - - X 1 ———— ' ——— T—1 \ ' f ' * ^ l * 0 . , f ' \^.* ' .- 3 ;;. 3 ; ; l, : \

! \ A .* ' /' 7 X U - ,^. ..'. /7 7 ^1 \ * * f f

' \ / f f

\ --' - . / 7 , 'f1 "' ; 1- r . -* 7 - * *y: . * */ 7i ' ' ** /*' '//' '' ' /A ^J * -* 0 . . **/ i * . X i!il/. iili; 3 .^; y/- 3 ; ;A l

998780 -'} h '-f 7l : ' - *f 7

X 3 / ; ^ '7' * * ' i 'x Q -L î 7 ' : O1 - : - .*//" . -'i '1 x *.* .1 . lv*- ' .'^1 ;'J/ x . . *. , /V/** '" ' */ I ^ •ijl^ X . . 7 i */'

X '-' . -7 ' ' v-' 1i -. .y/ . . y il/t * *y * - * V ;/'** s1 /.~\ , lT 3 /^- ; .' -^ ; /X': /X;v vf..; 3.. ';

•' -/" * ' \ *' ' 'V .' " . ' .' /; -^- -^-3 - ; -' '' ' ; ..H: ''.' ''.'

^v 3;-- ;' ;' 3 '^^ * :- !••' \ .\y y !// ; - -. h 'f ' tt * 1y x i ,. - ix y . ,. i JILL A

Trench J-3 *^;\ • ; ^V' \ \\* ^ \

. P, H X^ x 995779 \ ^! 1 A \ x \l \ \ ^ , . \~^T-A ————— ———— x ————— \-A \ ^-,

\ \ A ^^ ^ 3 X^ \ V- A 3 X^ \

\ \-'-\\ - vV-.-. 3 .--}., A :'\ \V V .^ x "' ;:.' \ '. AH" \\ '..: \

V -x - ' * \ ** V \V- ^ li**.-..' N v x

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LEGEND

PALEOZOICOrdoviciaan

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PALEOZOIC Odovician

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RPT ON PHASE I EXPL PROG€¦ · Fluorite Deposits in Harrington Sound Resources Property Area...

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