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31CiaSE0e85 2.1 2688 MADOC
l
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
l
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
DERRY, MICHENER, BOOTH ft WAHL
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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13
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
DERRY, MICHENER, BOOTH ft WAHL
(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
DERRY, MICHENER. BOOTH ft WAHL
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-1-
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
AW
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of
\ Q
UE
BE
C
MADO
C AR
EA
PRO
PERTIES
U.S.A
.
Peterborough
Oshaw
a
BANKER LAKE
BLOCK
JARVIS LAKE
, \
BLOCKM
adoc
HO
lf
SO
UTH
ER
N
BLO
CK
Belleville
'Toronto
scan i: 800 ooo
16 32 km
FIG
UR
E
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LOC
AT
ION
M
AP
l l l l l l l l l I l l l l l I l l l
VII cone. no.
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
-3-
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
DERRY, MICHENER, BOOTH ft WAHL
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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
DERRY, MICHENER, BOOTH ft WAHL
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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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^^rv&P^^^BS ; li l^s13fc^fe:Piii.:. - - - \"- , , SaSt:v:v.";^23?fT. . - 'Vi :::::. vt^"-3^kii^1\' - ^,. ^/*T
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
DESCRIPTION OF DEPOSITS INHARRINGTON SOUND RESOURCES
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
PRODUCTION STATISTICSAND HISTORY
- 1917: Discovery- 1918-1920: open cutmining and some shaftdevelopment work
- 1929: shaft deepened- 1940-1944: mining of
about 2,500 tonsfluorite ore
- TOTAL PRODUCTION:2,500 tons
- 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
EXPLORATION POTENTIAL/SIGNIFICANCE
- 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
00
l
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
DESCRIPTION OF DEPOSITS INHARRINGTON SOUND RESOURCES
PROPERTY AREA
BLOCKAREA
Jarvis Lake(Madoc Twp)
NAME OF MINE/PROSPECT
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
PRODUCTION STATISTICSAND HISTORY
- 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
- TOTAL PRODUCTION:1,500 tons
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
EXPLORATION POTENTIAL/SIGNIFICANCE
- 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
DESCRIPTION OF DEPOSITS INHARRINGTON SOUND RESOURCES
PROPERTY AREA
BLOCKAREA
Jarvis Lake(Madoc Twp)continued
NAME OF MINE/PROSPECT
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
PRODUCTION STATISTICSAND HISTORY
- 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
- TOTAL PRODUCTION:6,600 tons
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
EXPLORATION POTENTIAL/SIGNIFICANCE
- 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
DESCRIPTION OF DEPOSITS INHARRINGTON SOUND RESOURCES
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
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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.
DERRY. MICHENER, BOOTH ft WAHL
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
l l l l l l l l l l l l l l l l l l l
-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.).
l l l l l l l l l l l l l l l l l l l
-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
DERRY, MICHENER, BOOTH ft WAHL
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-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-
DERRY. MICHENER, BOOTH ft WAHL
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-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
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-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
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-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.
DERRY, MICHENER, BOOTH ft WAHL
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-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
DERRY. MICHENER, BOOTH ft WAHL
l l l l l l l l l l l l l l l l l l l
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
l l l l l l l l l l l l l l l l l l l
-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.
DERRY, MICHENER, BOOTH ft WAHL
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-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
DERRY. MICHENER, BOOTH ft WAHL
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
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-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
DERRY, MICHENER. BOOTH ft WAHL
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
DERRY, MICHENER, BOOTH ft WAHL
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APPENDIX l
SOIL SAMPLE ASSAY CERTIFICATES
DERRY. MICHENER, BOOTH ft WAHL
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
JS023JS024JS025JS026JS027
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
JS135JS116JS117JS118JS119
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
JS087JS088JS089JS090JS091
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
JS138JS139JS140JS141JS142
97204
93129140
395 757465 880669 880531 705651 651
JS106JS107JS108JS109JS110
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
PROJECT: HSR103 PAGE 4
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
Geochemical Lab Report
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 Caj^ek 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•^^AA^^hM^M ^^A 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
GeochemicalLab Report
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
GeochemicalLab Report
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
444 JS-521478 JS-522521 DUPLICATE451 JS-523379 JS-524
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
478 JS-530314 JS-531409 DUPLICATE515 JS-532600 JS-533
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
Geochemical Lab Report
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
GeochemicalLab Report
PROJECT: HSR103 PAGE 1
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
SS14SS15SS16SS17SS18
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
SS23SS24SS25SS26SS27
639759
184810211582
5287
160111154
256 SS60301 SS61328 SS62307 SS63355 SS64
668 191 424531 122 362594 114 395643 160 :BO666 290 523
SS28SS29SS30SS31SS32
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
Geochemical Lab Report
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
l l l l l l l l l l l l l l l l l l l
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
l l l l l l l l l l l l l l l l l l l
APPENDIX 3
TECHNICAL DATA STATEMENT
DERRY. MICHENER, BOOTH ft WAHL
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 Hokrtrrr^Age-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-^48^2.69^e?7.4^87-?-^
^^ft't^C*tfjc^ feT-T-l,
^9 E"??6^677-^i
?-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 jy^i ^/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^^o^ 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--'.'^•*^
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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/-
J^i-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 -
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* i* '
3 ^.'•i 1 # y
y
\
3 i
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3i99878
>
O CD±^D
31C13SE8005 2.I2688 MADOC 220
iRViS LAKE A, X OX \\ \ ^- {
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"^~~~~~ -" 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 \
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Paleozoic
3 Black River limestone
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^ 2 Granite Metavolcanics
1 Massive Mafic Metavolcanics la Mafic Agglomerate
20 + 00 N SYMBOLS
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outcrop
geological contact
pit
trench
jointing, vertical
dump rock
swamp
ridge; steep, gentlehatch marks indicate downhill direction
bush road
i iHB — FR~ claim post; observed, unobserved
LEGEND
PALEOZOICOrdoviciaan
3 black River Limestone unconformity
PRECAMBRIAN Metavolcancis
1 Massive Mafic Metavolcanic
Ib Mafic Metavolcanic, amphibolitized
la Mafic Agglomerate
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Symbols
^o outcrop
geological contact
pit
3 Umbered shaft
old trench
1989 trench
— dump rock
swamp
X^^Z' bush road
LEGEND
PALEOZOIC Odovician
3 Black River Limestone Unconformity
PRECAMBRIAN Felsic P lutonic Rocks
2 Granite
2
claim post: observed, unobserved 0 50 100 150 200 250 TI
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MADOC FLOURITE-BARITE PROPERTIES
MADOC TOWNSHIP
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89-38-04
DERRY, MICHENER. BOOTH k WAHLTORONTO
MADOC 2S0
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HARRINGTON SOUND RESOURCES INC.
MADOC FIX) URITE- BARITE PROPERTIES
MADOC TOWNSHIP
SOIL SAMPLE LOCATION MAP
SOUTHKRN CLAIM BLOCK
JUI.Y/M
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31C12SE990S 2 .12688 MADOC
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MADOC FLOURITE- BARITE PROPERTIES 1
MADOC TOWNSHIP 1
DPMm rvJ. B- K.
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GEOCHEMISTRYFor ZN H* AND F
JARVIS
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89-38-05
WAHLdSfe CANADA
2.12688 MADOC 270
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- 14+OON
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7+OON
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Intervals looking symbols represent unsampled areas.
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21+OON -
20+OON -
19+OON -
18+OON -
17+OON -
16+OON -
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HARRINGTON SOUKD RESOURCES INC.
MADOC FLOURITE— BARITE PROPERTIES
MADOC TOWNSHIP
MMM W i J.KK
SOIL GEOCHEMISTRY
ZN, BA AND F SOUTHERN CLAIM BLOCK •MVME Mb
89-38-07
DERRY. MICHENER BOOTH A WAHLTOMOxrro
31C12SEW*5 2.12688 MADOC 280