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OMNR-OGS 1984

Ministry of Hon - Alan w- pope., . , MinisterNatural , K D 01

John R. Sloan Resources Deputy Minister

Ontario

ONTARIO GEOLOGICAL SURVEY

Open File Report 5521

The Gold Potential of the Huntsville-Parry Sound Area

of Ontario

by

D.J. Villard, R. Keevil and A. Hogg

1984

Parts of this publication may be quoted if credit is given. It is recommended that reference to this report be made in the following form:

Villard, D.J., Keevil, R. and Hogg, A.

1984: The Gold Potential of the Huntsville-Parry Sound Area of Ontario, Ontario Geological Survey Open File Report 5521, 58p., 39 figures and 2 maps in back pocket.

Ontario Geological Survey

OPEN FILE REPORT

Open file reports are made available to the public subject to the following conditions:

This report is unedited. Discrepancies may occur for which the Ontario Geological Survey does not assume liability. Recommendations and statements of opinion expressed are those of the author or authors and are not to be construed as statements of government policy.

Open file copies may be read at the following locations:

Mines LibraryOntario Ministry of Natural Resources8th Floor, 77 Grenville Street, Toronto

The office of the Regional or Resident Geologist in whose district the area covered by this report is located.

Handwritten notes and sketches may be made from this report. Check with the Library or Region al or Resident Geologist's office as to whether there is a copy of this report that may be borrowed. The Library or Regional or Resident Geologist's office will also give you information on copying ar rangements. A copy of this report is available for Inter-Library Loan.

This report is on file in the Regional or Resident Geologists' office(s) located at:

Brendale Square Box 9000Huntsville, Ontario POA 1KO

The right to reproduce this report is reserved by the Ontario Ministry of Natural Resources. Permission for other reproductions must be obtained in writing from the Director, Ontario Geological Survey.

V. G. Milne, Director Ontario Geological Survey

111

Foreword

The gold potential of the Central Gneiss Belt (Grenville Province) within the Ministry of Natural Resources' Algonquin Region is unknown. A flurry of activity occurred in the late 1800's and early 1900's, resulting in a producer (the McGown Mine) near Parry Sound. There has been little exploration for gold since then, due mainly to the complex deformation and high metamorphic grade of the rocks in the area.

This report summarizes the results of the first stage of a project to evaluate the gold potential of the Central Gneiss Belt within the Algonquin Region. Initial results indicate the presence of gold and it is hoped that subsequent reports will provide a better understanding of the gold potential of the area.

This publication should be of interest to the minerals industry, particularly the prospectors who are attempting to explore for gold in the study area.

V. G. MilneDirectorOntario Geological Survey

V

Table of Contents

Page

Abstract . . . . . . . . . . . . . . . . . . . . . . . . . . . . l

Introduction . . . . . . . . . . . . . . . . . . . . . . . . . . l

Acknowledgements . . . . . . . . . . . . . . . . . . . . . . . . l

Geology . . . . . . . . . . . . . . . . . . . . . . . . . . . . 2

Exploration Activity . . . . . . . . . . . . . . . . . . . . . . 2

Project Description . . . . . . . . . . . . . . . . . . . . . . 3

Results . . . . . . . . . . . . . . . . . . . . . . . . . . . . 4

Conclusions . . . . . . . . . . . . . . . . . . . . . . . . . . 5

Appendix I - Reported gold occurrences that were visited . . . . 6

Appendix II - Outcrops visited on other projects where sampleswere collected and analyzed for gold . . . . . . . 46

Appendix III - Reported occurrences (Satterly, 1942) that havenot been visited . . . . . . . . . . . . . . . . 54

Appendix IV - Reported occurrences (reference unknown) that havenot been visited . . . . . . . . . . . . . . . . . 55

References . . . . . . . . . . . . . . . . . . . . . . . . . . . 56

Vi l

The Gold Potential of the Huntsville-Parry Sound Area of Ontario

by l l l D.J. Villard, R. Keevil, and A. Hogg

ABSTRACT

The Central Gneiss Belt of the Grenville Province has never been adequately evaluated for its gold potential. A flurry of activity took place in the period from 1890 to 1910, but since then there has only been minor exploration.

The gold project currently being conducted by the Resident Geologist in Huntsville was initiated in 1981 to evaluate an area bounded by Georgian Bay, Algonquin Park, North Bay, and Gravenhurst with the intent to locate, map and sample reported gold occurrences within this area. To date 39 have been located; and a few indicate the presence of gold. This report presents preliminary results.

INTRODUCTION

In the fall of 1981 MNR, Huntsville began to determine the gold potential of the Central Gneiss Belt (Grenville Province) within the Algonquin Region. The area has had many drawbacks in its appeal to the gold explorationist. Among these are: minimal past exploration, an extremely complex geology and few geological maps. Recent improvement in the geological data base came with the mapping by A. Davidson of the Geological Survey of Canada.

The potential for gold in the area was thought to be low, mainly because of the high grade of metamorphism. However, the McGown Mine near Parry Sound shows that gold does occur in these rocks. Coleman (1900) reported values of gold up to 0.25 oz./ton from underground and free gold was beaten into finger rings. Recently there has been a reported association of gold with graphite deposits in the area.

The two main objectives: firstly, a rapid evaluation of reported gold occurrences in the Central Gneiss Belt which lie in the Algonquin Region. Results of this form this report. The second objective is to target areas within the Central Gneiss Belt that have a greater potential for gold.

ACKNOWLEDGEMENTS

The authors would like to express sincere thanks to the many people who contributed toward this report, in particular the following individuals: W. Sinclair, J. Rowan, R. Bice, R. Ennest, R. Whitehouse, R. Fraser, J. Rhiness, R. McGowan, K. Jensen, R. Stead and B. Montgomery. Many of these are local people, without whose help many of the occurrences would not have been located.

l Geologists, Ontario Ministry of Natural Resources, ResidentGeologist's Office, Huntsville.

This report is published by permission of V.G. Milne, Director Ontario Geological Survey.Manuscript approved for publication by C.R. Kustra, Liaison Geologist, Ontario Geological Survey, September 20, 1984.

- 2 -

GEOLOGY

Up until 1980, the knowledge of the Central Gneiss Belt of the Grenville geological Province lying west of Algonquin Park was extremely limited. Only Lount Township had been mapped in detail (Satterly, 1956). In 1980, A. Davidson of the Geological Survey of Canada undertook reconnaissance mapping east from Georgian Bay (Davidson and Morgan, 1981). S. Limbers of the Royal Ontario Museum has mapped in the North Bay area, in Renfrew County and is currently working in the Huntsville area. The area ... "has been considered by many to be, for the most part, an intractable 'sea of gneiss 1 , monotonous and at fairly uniform high metamorphic grade, of far less rewarding prospect for study, and certainly of little economic interest". (Davidson and Morgan, 1981). Preliminary results of Davidson's field work can best be summed up by the abstract of his 1982 paper. "Continuing field work in southwestern Grenville Province between the Grenville Front Tectonic Zone and the Central Metasedimentary Belt has revealed a network of continuous zones of various kinds of tectonite, along which predominantly northwest-directed movement has taken place. Tectonite zones outline domains and subdomains of distinctive character, and tend to truncate lithology, structure and metamorphism on one side. Domains with relatively high pressure granulite facies metamorphism, and eclogite-like rocks and sapphirine-bearing assemblages in tectonic inclusions suggest that tectonism occurred at deep crustal level. Sense of movement indicates emplacement of allochthonous crustal segments by northwest-directed ductile shear and thrusting, with maximum displacement along the tectonite zones. Such a mechanism is compatible with a Himalaya-type model for development of a thickened crust, and has implications concerning equation of rocks and orogenic events on opposing sides of the Grenville Front Tectonic Zone". (Davidson et al, 1982).

The complex geology of the Central Gneiss Belt makes it difficult to explore for gold.

EXPLORATION ACTIVITY

Past work resulted in numerous pits throughout the area. Around the turn of the century the most interesting deposit was the McGown Mine near Parry Sound. "The existence of mineral in the district of Parry Sound was first noted in 1894, when a farmer named McGown discovered traces of free gold on his land situated about two miles out of town. Sufficient quantities of this precious metal were secured to enable a local jeweller to hammer a few souvenir finger rings, and the owner of the property felt justified in forming a company to exploit for gold". (The Canadian Mining Review, 1900).

Coleman (1894) stated that: "the gold occurs as small nuggets and scales in vitreous quartz associated with copper sulphides, chalcocite or copper glance, bornite or peacock ore, a little copper pyrites, and their decomposition products, oxides of iron and malachite ... the gold may be found in quartz, in the sulphides, and between the two. An assay of the bornite gave $4 per ton of gold". Although the author has obtained gold values of up to 0.15 oz. per ton, the highest reported values were 0.25. oz per ton (Coleman 1899) obtained from the inclined shaft. Coleman (1899) also reports silver values of about 1.0 oz. per ton .

- 3 -

Many of the remaining occurrences had little work performed on them. Generally one or two pits or trenches were dug on a property that showed some potential for gold, indicated by rusty rocks, quartz veining or the presence of sulphides.

How much gold was actually returned is virtually unknown. Verbal records report men were able to make wages from the gold they took out of the ground, but written records are almost non-existent. Only a detailed evaluation of these occurrences will determine if there is gold associated with these old workings. This study lists minor gold from several occurrences, but most showed no gold. The "nugget effect" combined with the few samples analyzed would make it easy to miss gold present.

PROJECT DESCRIPTION

The initial objective of the gold project was to conduct a preliminary examination of all the reported gold occurrences within the Central Gneiss Belt of the Algonquin Region of the Ministry of Natural Resources. The initial identification of many of these reported occurrences came from the existing literature, but many were realized from conversations with the local people (both prospectors and non-prospectors). Once identified, an occurrence was located in the field (a difficult task at times, as several were not found) , briefly mapped and sampled. A summary of those occurrences that were located is presented in Appendix I. Appendix II lists those locations from other projects that had gold analyses. Appendices III and IV lists those occurrences that have not been searched for to date.

It is hoped that by publishing details on the location of many of these gold occurrences, prospectors will be able to go out and carry out a more thorough evaluation. It is also intended, as part of this project, to carry out a more detailed evaluation of some of the occurrences already visited.

The second objective of this project was to outline either general or specific areas in the Central Gneiss Belt of the Algonquin Region where there might be some possibility 'of detecting gold. Part of this objective has already been achieved through the results presented in this report, but it is hoped that when this project is completed, we will have a better understanding of the gold potential of the study area. As a means of meeting this objective, several things will be carried out, as summarized below:

- Several of the occurrences already visited will be re-examined in more detail.

- Several of the known graphite deposits will be studied in detail to determine if there is any association of gold with the graphite. The graphite deposit in Laurier Township was initially examined for its gold potential, as indicated by the numerous pits sunk in the rusty gneisses.

- Several of the rivers in the area will be panned for gold to confirm or disprove the rumours that gold is being detected.

- 4 -

Selected geological units will be briefly examined to determine their potential for hosting gold mineralization. An example might be the meta-arkoses northwest of Parry Sound.

Sulphide deposits in the vicinity of identified structural breaks will be checked for their possible gold association.

RESULTS

Thirty-nine reported gold occurrences have been located to date. For each of these, the location, access and geology has been briefly described, as well as, several samples collected for analysis. An initial examination of the analytical results would seem to indicate that most of these occurrences have little, if any, potential for gold. This may be the case, but one should remember that gold is a difficult element to detect, particularly when only 2 or 3 samples were analyzed from each occurrence.

The initial exploration on these occurrences may have been as a result of the detection of visible gold and it would be easy to miss this in a couple of samples. Many of these occurrences will be re-evaluated in the next stage of the project, but it is hoped that at least the re-locating of many of these occurrences will stimulate the prospectors to go out and take a look.

As previously mentioned, most of the Central Gneiss Belt of the Algonquin Region is not mapped in any detail, making it extremely difficult to place the detailed geology of these occurrences in a regional context. Most of the reported occurrences that were visited are of two types:

(1) Disseminated sulphides (mainly pyrite, with minor phrrhotite and chalcopyrite in places) in a mafic gneiss. Rusty zones and minor quartz veining are sometimes apparent.

(2) Concordant and discordant pegmatite dikes and stringers, with or without concentrations of quartz, in mafic and felsic gneisses.

Most of the occurrences sampled had non-detectable gold values, but several had values of 10 parts per billion or greater. Excluding the McGown which is well known for its gold, there are at least two occurrences, GS-3 and GS-12, with reported values somewhat higher than the others.

- 5 -

GS-3 A value of 390 ppb shows that gold is present and additional sampling required. Mineralization consists of pyrite and chalcopyrite in a series of gneisses containing rusty carbonate layers.

GS-12 Although 80 ppb is not a high value, it is anomalous and the occurrence is interesting. Mineralization consists of pyrite, phrrhotite and chalcopyrite in a mafic gneiss cut by small pegmatite stringers.

Although the results presented in Appendix II have not been discussed here, one should note that there are several occurrences that have anomalous gold values which may warrant further investigation.

CONCLUSIONS

This study, a compilation of many of the gold occurrences reported in the literature, will enable prospectors to conduct additional evaluation of these occurrences.

Although it was not intended to arrive at any conclusions at this preliminary stage of the project, there would appear to be potential for gold in the Central Gneiss Belt of the Huntsville-Parry Sound area.

Appendix I

Reported gold occurrences that were visited

GS l

Location: Haliburton County, Livingstone Township Lot l Concession VII NTS: 31E/7 UTM: Zone 17 5025800N 674900E

Access: The workings are located 200 to 300 metres north of the northeast arm of Fletcher Lake between Bloody Lake and Poorhouse Lake. Access is gained by following a hydro line from a gate located at the end of a cottage road on the east side of Fletcher Lake. Follow the hydro line north for approximately 250 metres to where the line turns 90 degrees towards the west. The pits are located on a ridge trending northeast from this corner, the nearest being 10 metres from the corner.

History: Jack Cunningham of Dorset reported that values of $10./ton gold were obtained in 1890.

Geology and Mineralization:

Sample No.

The country rock consists of a flatlying medium grained hornblende, biotite gneiss. A quartz-rich zoned pegmatite strikes 255 degrees and dips steeply to the north. The pits have been sunk in this pegmatite. Pyrite and magnetite occur in the feldspathic parts of the pegmatite.

Description Cu Pb Zn Ag Au As Sb PPM PPM PPM PPM PPB PPM PPM

81-RK-l Pegmatite, py, mag81-RK-2 Gneiss81-RK-3 Quartz81-RK-4 Pegmatite, mag, py81-RK-5 Quartz, py81-RK-6 Gneiss/Pegmatite

contact81-RK-7 Quartz81-RK-8 Quartz81-RK-9 Pegmatite81-RK-10 Quartz

44106

4384

4010328

258

567795

30

NDNDNDNDNDND

NDNDNDNDNDND

NDNDNDNDNDND

NDNDNDNDNDND

22674

217

146

204

295

NDNDNDND

NDNDNDND

NDNDNDND

NDNDNDND

V"x ISOS

ISO

GS 2

Location: Territorial District of Parry Sound, Spence Township Lot 9 Concession XII NTS: 31E/12 UTM: Zone 17 5048900N 604700E

Access: The workings are located 250 metres west of where Ahraic Creek crosses the Spence-Oranmore Road, 2.5 kilometers northwest of Spence.

Geology andMineralization: The country rock is a hornblende-biotite gneiss with

minor granitized areas. Sulphide mineralization is restricted to pyrite stringers and layers.

Sample No.

81-RK-14

81-RK-15

Description

Hornblende gneiss,PYHornblende gneissPY

Cu Pb Zn Ag Au As SbPPM PPM PPM PPM PPB PPM PPM

65 5 36 0.4 MD ND ND

61 5 40 0.4 ND ND ND

100

GS 3

Location; Territorial District of Parry Sound, Spence Township Lot 28 Concession XI NTS: 31E/12 UTM: Zone 17 5045200N 597700E

Access; The trench is located on the east shore of a pond located 1.5 kilometres north-northeast of Plumtre Lake.

Geology andMineralization; The rocks in the area consist of a series of steeply

dipping gneisses ranging from amphibolitic to quartzo- feldspathic. Rusty carbonate layers with 5 - 1(H sulphides and 2(H magnetite occur within the gneisses in a l metre thick zone. The sulphides are mainly pyrite with some chalcopyrite.

Sample No. Description Cu Pb Zn Ag Au As Sb PPM PPM PPM PPM PPB PPM PPM

81-RK-67 Hornblendegneiss, q,PY* cp

81-RK-68 Hornblendegneiss, mag, py

81-RK-69 Gneiss, q 81-RK-70 Gneiss, mag,

PY* cp 81-RK-71 Quartz and gneiss

3500

7200 MD

48014400

394

58 1.4 100

75 3.7 310

ND 30 ND ND ND ND 122 3.1 390 4

ND 43 ND 10

ND

ND

ND ND

ND

10GS 4

Location: Territorial District of Parry Sound, Ryerson Township Lot 30 Concession V NTS: 31E/12 UTM: Zone 17 5043700N 612700E

Access: The deposit is located 2 kilometres southwest of Starrat, 200 metres north of the intersection of the Bourdeau-Harrison Lake Road and the road leading west from Starrat.

History; Workings consist of 2 trenches, four pits and l water filled shaft.

Geology and Mineralization

Sample No.

Sparse outcropping exposes impure calcitic marble with bands of hornblende gneiss. The marble contains minor amounts of disseminated graphite, diopside and quartz. The only sulphides detected were disseminated pyrite and pyrrhotite..

Description Cu PPM

Pb ZnPPM PPM

Ag PPM

Au PPB

AJS PPM

SbPPM

81-RK-9 Quartz and gneiss,

py, po81-RX-10 Quartz and gneiss 81-RK-ll Quartz and gneiss 81-RK-12 Gneiss and marble 81-RK-13 Gneiss

22

5192349

14 0.2

6107

51314

0.4 0.3 0.4

14 101 0.4

ND

ND ND ND ND

ND

ND ND ND

ND

ND ND

NDND ND

GS-5

Location:

Access:

11

Territorial District of Parry Sound, Monteith TownshipLot 8 Concession XINTS: 31E/5UTM: Zone 17 5035200N 610600E

The two pits are located 0.8 and 1.0 kilometres north of Bear Lake. The pits can be reached by driving north on the first gravel road west of the Bear Lake Church on Highway #518. The first pit is 20 metres north of the intersection of this road with an abandoned railroad bed. The second pit is 200 metres north of this intersection.

Geology and Mineralization The country rock is a hornblende-biotite gneiss with

quartzo-feldspathic banding. A mixture of impure marble and pegmatite occurs within the gneisses. Pyrite and chalcopyrite, with minor pyrrhotite and magnetite, occurs within the gneisses near the contact with the marble.

Sample No,

81-RK-20 81-RK-21

81-RK-22

81-RK-23

81-RK-24

Description

Rusty pegmatiteRusty gneiss, py, cp,po, magFelsic gneiss/hornblende gneisscontactMarble/gneiss contact,PY, cpPegmatite


5 6 30 0.3 MD ND ND760 9 19 0.4 5 ND ND

265 23 20 0.2 ND ND

915 17 24 0.4 10 ND ND

7 19 ND 5 ND l

# S IB

GS 612

Location: Territorial District of Parry Sound, Monteith TownshipLot 11 Concession XNTS: 31E/5UTM: Zone 17 5034100N 609800E

Access: The pit is located 400 metres southwest of the Junction ofHighway #518 and West Bear Lake Road. It is 30 to 40 metres west of the road at the northwest end of a flooded beaver pond.


Sample No.

The country rock is a biotite-hornblende-garnet gneiss with pegmatite stringers, both concordant and discordant to the foliation. Disseminated pyrite, chalcopyrite and pyrrhotite are present in both the gneiss and the pegmatite.

Description Cu Pb 2n Ag Au As Sb PPM PPM PPM PPM PPB PPM PPM

81-RK-54

81-RK-55 81-RK-56 81-RK-57

Gneiss/pegmatitecontact, py, po,graphiteRusty gneiss, qGneiss, S-10% pyPegmatite,S-10% py

100 86 ND ND ND

520 8 150 0.8312 44 620 0.5660 120 640 1.2

10 ND 10

ND 2

ND

ND

ND NDND

GS 713

Location: Territorial District of Parry Sound, Monteith TownshipLot 15 Concession VIIINTS: 31E/5UTM: Zone 17 5031500N 608700E

Access; The pit is located 1.2 kilometres southeast of where theSequin River crosses Highway #518. Drive south from Highway #518 along West Bear Lake Road for 3.0 kilometres and turn west on a hunt camp trail, just past a gravel pit. Follow road to the end (1.5 kilometers). The pits are approximately 100 metres northeast of the hunt camp.


Sample No.

81-RK-4

81-RK-5

81-RK-6 81-RK-7

81-RK-7

Bedrock in the vicinity of the pit is limited. Information pertaining to the geology was obtained from dump material. The country rock is a quartz-biotite gneiss that has been sheared and intruded by a pegmatite. Disseminated cp., py. and po. occurs disseminated throughout the rock.

Description

Rusty gneiss,py, po, cpPegmatite,20* sulphidesRusty sheer,, pyPegmatite/gneisscontactPegmatite/gneisscontact

Cu Pb Zn Ag Au As S b PPM PPM PPM PPM PPB PPM PPM

370 22 65 0.3

310 10 11 0.4

175 5 5 0,3196 10 34 0.2

33

ND ND ND

ND 2 2

ND 3 NDND ND 3

35 0.4 ND ND ND

B

c V^n x* fi7

H*-^ a

O l* 0 Jo

GS 8

14

Location; Territorial District of Parry Sound, Monteith Township.Lot 17 Concession IXNTS: 31E/5UTM: Zone 17 5031800N 607700E

Access: The pit is mapped as being 4 kilometres southwest of Bear Lake and 0.5 kilometres southwest of where Highway #518 crosses the Sequin River.

History: Satterly (1942) reports a pit at the edge of the SequinRiver. Road Construction has probably resulted in the pit being filled in.

Geology andMineralization: The country rock is a biotite-hornblende gneiss,

crosscut by numerous small pegmatite dikes. Pyrite is found in both the gneiss and the pegmatite.

Sample No Description Cu PPM

Pb PPM

Zn PPM

Ag PPM

AU

PPB

AS

PPM

SbPPM

81-RK-51 81-RK-52 81-RK-53

Quartz Gneiss, py Pegmatite, py

98 296 ND47 2

6568

ND ND ND

ND ND ND

ND ND ND

ND ND ND

So

15

GS 9

Location: Territorial District of Parry Sound, Gurd Township Lot 10 Concession XIX NTS: 31L/4 UTM: Zone 17 5103200N 605500E

Access: Proceed on a good gravel road for 3 kilometres from thehamlet of Hotham. At this point the road deteriorates to a tractor trail. Proceed for l kilometre to the local height of land and you should find the pit 10 metres east of the trail on a north-facing slope.

History; Satterly reported this pit in 1942 (Satterly, 1942).Approximately 5 tonnes of material have been removed from the pit.


Sample No.

A medium grained gneiss with both felsic and mafic layers is cut by a 30 centimetre wide diabase dike. Magnetite is present in the diabase and disseminated pyrite is found in both the diabase and the gneiss.

Description Cu Pb Zn Ag Au PPM PPM PPM PPM PPB

As Sb PPM PPM

81-RK-29 Rusty felsic 106gneiss

81-RK-30 Diabase, mag 119 81-RK-31 Diabase, mag 86 81-RK-32 Diabase/Pegmatite 30

contact, py

35

6679

ND

MDND

1010

ND ND

NDND

50 0.2 ND ND

NDND ND

ZOO

GS 10

16

Location: Territorial District of Parry Sound, Nipissing TownshipLot 28 Concession XNTS: 31L/4UTM: Zone 17 5103700N 608900E

Access; The workings are located about 10 meters from Reserve Creek, 400 meters upstream from Duncan Lake. They can be reached by a trail leading off from a road that goes to Hotham.

History: W.T. King Jr. had put down a number of pits on Reserve Creek before 1942 (Satterly, 1942). A heavy cable and a dredge are rusting nearby.

Geology and Mineralization: Two parallel diabase dikes cut a granitic, pegmatite in

the main pit. The pegmatite is medium to coarse grained, with carbonate filled fracture zones in places. No sulphide mineralization was observed.

Description Cu PPM

Pb PPM

ZnPPM

AgPPM

AU

PPBAS PPM

Sb

PPM

81-RK-33 Pegmatite/diabasecontact

81-RK-34 Pegmatite 81-RK-35 Diabase 81-RK-36 Diabase

16 79 ND

56 12 9 ND160 6 128 " ND218 5 40 ND

5 ND

5 ND5 ND5 ND

ND

ND ND ND

N

GS-11

17

Location: Territorial District of Parry Sound, Lount TownshipLot 27 Concession INTS: 31E/13UTM: Zone 17 5067000N 605000E

Access: The workings are located approximately 2 kilometres west ofthe Old Nipissing Road on a cottage road that goes to Lake of Many Islands.


Sample No.

The country rock is a calcitic marble containing zenoliths of amphibolite gneiss. The marble is cut by numerous quartzo-feldspathic dikes. Minor pyrite is disseminated throughout the gneiss and graphite is disseminated throughout the marble.

Description Cu PPM

Pb Zn PPM PPM

Ag PPM

Au PPB

As Sb PPM PPM

81-RK-61 Quartzo-feldspathic 20 NDdikes

81-RK-62 Marble, py 24 ND 81-RK-63 Marble/gneiss contact 72 ND

1314

ND

ND ND

ND

ND ND

ND

ND 5

ND

ND ND

(00

18

GS 12

Location: Territorial District of Parry Sound, Lount Township Lot 13 Concession V NTS: 31E/13 UTM: Zone 17 5073000N 608800E

Access: The pit is located about 100 metres north of the Deer Lake Road directly across from what is presently Ralph's Farm Equipment.


81-RK-64

81-RK-65

81-RK-66

83-29-1 83-29-2 83-29-3 83-29-4 83-29-5

The country rock is an amphibolite gneiss with pegmatite stringers and blebs. Sulphide mineralization includes pyrite, chalcopyrite, pentlandite and pyrrhotite, disseminated throughout the rock.

Description

Gneiss, mag, py,po, quartzGneiss/pegmatitecontact, py, po,quartzGneiss, mag, py,

Gneiss, pyGneiss, pyGneiss, pyGneiss, pyGneiss, py

Cu Pb Zn Ag AuPPM PPM PPM PPM PPB

760 ND 60 ND ND

1100 ND 79 ND 80

480 ND 58 ND 10

206246891

4745517

55

308

13

11247579840

0.10.30.41.10.1

151020305

As SbPPM PPM

6 ND

4 ND

(00

F.elA

rs

GS 13

Location;

Access:

History

19

Territorial District of Parry Sound, Ferrie TownshipLot 7 Concession INTS: 31E/12UTM: Zone 17 5064400N 598500E

Drive north from Highway #124 on the Old Nipissing Road for 2.5 kilometres. Turn left and follow this road for 3 kilo meters. A tractor trail heads northwest from the main road, across from a farm. Follow the trail for 6 to 7 kilometres to a second prospector's cabin. The workings are approxi mately 0.5 kilometres northeast of the cabin.

Three pits have been excavated and several diamond drill holes have been drilled in the last ten years.


Sample No.

81-RK-73

81-EJ-3

81-EJ-4

81-EJ-5

The host rock is a medium to coarse grained amphibolite gneiss with minor pegmatite veins and augens. Sulphides present as disseminations and blebs are: pyrite (to 4C^), chalcopyrite (to 5%), pyrrhotite, pentlandite and bornite.

Description

Rusty quartz, nosulphidesAmphibolitegneissAmphibolitegneissAmphibolitegneiss

Cu Pb Zn Ag Au As Sb PPM PPM PPM PPM PPB PPM PPM

96 ND 26 3.1 ND

16400 ND 66 40

12800 ND 61 0.9

1100 ND 67 0.8

8 ND

L.Co.'t'*'*

GS

20

GS 14

Location: Territorial District of Parry Sound, Strong Township Lot 20 Concession X NTS: 31E/14 UTM: Zone 17 5069600N 623900E

Access: The workings are located on a property currently owned by C.A. Boyce of Sundridge, They are 700 metres northeast of Highway #11 on the west side of Arena Road and can be reached from the Boyce house by following a trail west for 33 metres into a hardwood bush.

History: A 3 x 3 metre pit, a shallow trench and a diamond drill hole were located on the site. Satterly (1942) reported that 2 holes were drilled in 1902.


Sample No.

The country rock is a biotite-hornblende gneiss that strikes east-west and dips 60 degrees to the north. quartz vein intrudes the country rock in the trench. Visible mineralization consists of pyrite, graphite, pyrrhotite, pentlandite and sphalerite.

Description Cu Pb Zn Ag Au As SbPPM PPM PPM PPM PPB PPM PPM

81-RK-47 Gneiss, py 88 7 98 0.5 5 6 MD81-RK-48 Rusty gneiss, py 28 6 59 ND 5 13 381-RK-49 Gneiss, po, py, mag 55 9 100 0.3 5 9 MD81-RK-50 Quartz 17 6 140 ND 5 46 MD

/3 JJ l

Drill Ue

21

GS 15

Location: Territorial District of Parry Sound, Proudfoot Township Lot 3 Concession X NTS: 31E/11 UTM: Zone 17 5058800N 635200E

Access: The pits are located 300 metres west of Tea Lake between 2 circular hills approximately 2 kilometres east of Pickerel Lake. The pits were reached by foot from Island Lake by following the creek between Island and Tea Lake and then following the shore of Tea Lake southwest for 0.5 kilometres.

History; Two pits are located here. Approximately 30 tonnes of material has been removed.

Geology andMineralization; A series of hornblende, biotite and felsic gneisses

occur within the general area. Minor pegmatite dikes are found cutting the gneisses. Sulphide mineraliza tion in the form of pyrite, chalcopyrite, pyrrhotite and pentlandite, are restricted to the hornblende gneisses.

Sample No.

81-RK-43

81-RK-44

81-RK-45

81-RK-46

Description

Hornblende gneiss,PYGneiss/pegmatite contactHornblende gneiss, 5 - 10% sulphides Hornblende gneiss


24

6

180

14

4

4

3

3

21

16

12

40

ND

ND

ND

0.2

5

5

ND

5

ND

ND

ND

ND

ND

4

ND

ND

l

"t*

V

'B

109 loo

GS 16

22

Location: Territorial District of Parry Sound, Proudfoot Township Lot 6 Concession I NTS: 3E/11 UTM: Zone 17 5051500N 639300E

Access: The pit is located l kilometre east of Himbury Lake on aneasterly facing slope near the top of a northeast-southwest trending ridge. Access is gained by walking north from Highway #518 along a tractor trail.

History: About 5 tonnes of rock have been removed.


Sample No.

The country rock is a fine to medium grained grey gneiss with white and rusty quartzo-feldspathic layers and augen. Disseminated pyrite, chalcopyrite, bornite, pyrrhotite and pentlandite are found throughout the rock.


81-RK-58 81-RK-59

81-RK-60

GneissGneiss, pyrite,borniteGneiss

96 2 83 ND ND ND ND 640 ND 66 0.6 ND 3 231

560 ND 68 0.7 ND

23

GS 17

Location: Territorial District of Parry Sound, Perry Township Lot 15 Concession X NTS: 31E/11 UTM: Zone 17 5042300N 631300E

Access: The pit is located approximately 50 metres west of Highway #11, 600 metres south of the turnoff to Emsdale.

Geology andMineralization: The country rock is a biotite-hornblende gneiss with

minor amounts of quartz, plagioclase and garnet. A granitic pegmatite intrudes the gneiss in the area of the pit. No mineralization was observed.

Sample No.

81-RK-37

81-RK-28

Description

Gneiss/pegmatitecontactPegmatite

Cu* Pb Zn Ag Au As SbPPM PPM PPM PPM PPB PPM PPM

24 4 28 ND ND ND ND

18 6 29 ND 5 ND ND

A/

GS 18

24

Location: Territorial District of Parry Sound, Perry Township Lot 13 Concession X NTS: 31E/11 UTM: Zone 17 5041500N 630600E

Access: The pit is located 1.5 kilometres west-southwest of Emsdale, 120 metres south of Highway #518 and can be reached by walking along the hydro line.


Sample No.

81-RK-39 81-RK-40 81-RK-41

Bedrock consists of a massive garnetiferous amphibolite with minor quartz and pegmatite stringers throughout. Mineralization is restricted to minor amounts of disseminated pyrite.

Description Cu Pb 2n Ag PPM PPM PPM PPM

Amphibolite Amphibolite Pegmatite

29 424 616 7

342713

0.2 MD ND

Au PPB

ND

5MD

As PPM

ND ND ND

Sb

PPM

ND ND MD

N*v**"(e*tewn*

N

Der*

\

25

GS 19

Location: Territorial District of Parry Sound, Perry Township. Lot 4 Concession XII NTS: 31E/11 UTM: 5042900N 626400E

Access: The pit is located 4 kilometres west of Highway #11 onHighway #518. Access is gained from a sideroad going north from Highway #518. The pit is approximately 60 metres west of Highway #518 and 10 metres east of the sideroad.

History: The pit has been filled in since Satterly reported on the site.

Geology and Mineralization It would appear from dump material that the rock is a

mica schist with minor quartz stringers. Graphite comprises 5 to 10% of the rock. No sulphides were detected.

Sample No. Description Cu Pb Zn Ag Au As Sb PPM PPM PPM PPM PPB PPM PPM

81-RK-42 Rusty schist, quartz

68 15 ND ND

GS 20

26

Location: District Municipality of Muskoka, Chaffey Township Lot 9 Concession I NTS: 31E/6 UTM: Zone 17 5019500N 638100E

Access: The pit is located behind what is now Bennett's Industrial on Main Street West, Huntsville.

History: Gold was reported (R. Keevil, personal communication) asbeing extracted from 2 pits at this location. One pit has been destroyed during construction.


Sample No.

A series of gneisses have been recrystallized to form "sweats" of quartz, orthoclase, plagioclase, hornblende and biotite in pegmatite and associated rusty areas. Disseminated pyrite and graphite are detected in the pit.


81-RK-98 81-RK-99 81-RK-100

Felsic gneiss Rusty gneiss, py Pegmatite py

2098

135

148334

4347026

NDND

1.0

ND ND ND

ND ND4 ND5 -ND

\ o, 3i i i

27

GS 21

Location; District Municipality of Muskoka, Chaffey Township Lot 32 Concession V NTS: 31E/6 UTM: Zone 17 5027400N 645000E

Access: The workings are on west side of a large hill on the northside of a tractor trail running south from a house presently owned by Lawrence Payne. The house is 6 kilometres northeast of Highway #11B on Williamsport-Harp Lake Road.

History: There has been little work except for the visit by J. Satterly in 1942.

Geology and Mineralization: A mixture of quartzo-feldspathic garnetiferous gneiss,

hornblende gneiss and biotite gneiss are intercalated with marble throughout. The gneisses have been intruded by pegmatites. Magnetite and disseminated pyrite occur near gneiss-pegmatite contacts.

Sample No. Description Cu Pb Zn Ag Au As S b PPM PPM PPM PPM PPB PPM PPM

81-RK-l Pegmatite/gneiss 81-RK-2 Gneiss with py

and mag 81-RK-3 Quartz

674

10

148

25 0.251 0.3

4 0.4

ND ND

2ND

ND ND

ND ND

ND

.'sl (

S vLOO 4oo

GS 2228

Location: District Municipality of Muskoka, Chaffey Township Lot 2 Concession VII NTS: 31E/6 UTM: Zone 17 5024000N 633300E

Access: A pit is reported approximately 2 kilometres westof Ravenscliffe, Ontario and l kilometre northeast of Camp Tawingo. The ridge can be reached by walking north from Ravenscliffe Road, across the property of R. Stead, for approximately 1/2 kilometre.

History: A sulphur and/or gold mine is reported to have operated here (R. Stead, personal communication).

Geology and Mineralization A complex of felsic and mafic gneisses is intruded by

granitic pegmatite veins and stringers. Graphite and minor pyrite occurs as disseminations in some of the gneisses.

Description Cu Ag Au As Sb PPM PPM PPB PPM PPM

101

102

Biotite gneiss, graphite, quartz Gneiss, py

(5 (2

9 0.1

l? j.

V V

V \J

lOo

29

GS 23

Location: District Municipality of Muskoka, Brunel Township Lot 22 Concession XI NTS: 31E/6 UTM: Zone 17 5017800N 644800E

Access; The pit is located on the side of a north facing slope about 100 metres west of a tractor trail that runs south from Brown's road. The tractor trail is approximately 3.7 kilo metres from Brunel Road.

History: The Heastam Mining Syndicate is reported to have examined this property 30 years ago (R. Keevil, personal communica tion) . The volume of dump material suggests a fair amount of vertical development below water level.

Geology and Mineralization; The host rock for mineralization is a medium grained,

massive, rusty weathering amphibolite, that appears gneissic in places. Sulphide mineralization seems unrelated to contact or intrusive features and varies in percentages up to 50%. Sulphide minerals include pentlandite, phyrrhotite, pyrite and chalcopyrite.


81-RK-72 Mafic gneiss, 50% sulphides, pent, po. (minor PY* cp)

1920 ND 16 0.5 ND ND MD

aa.rt.t

30

GS 24

Location: District Municipality of Muskoka, Franklin Township Lot 7 Concession XI NTS: 31E/6 UTM: Zone 17 5020300N 651000E

Access: The workings are located approximately 0.5 kilometresnorth-northeast of South Portage between Peninsula Lake and Lake of Bays. The pits can be reached by walking west for 150 metres from the South Portage-North Portage Road, at a point 0.5 kilometres north of South Portage.

History: These pits were worked about 100 years ago and gold values of $10./ton were obtained (R. Ennest, personal communication). Approximately 30 tonnes was extracted.

Geology andMineralization: Medium grained massive amphibolite and amphibolite

gneiss is cut by a network of quartzose and granitic veins. Pyrite occurs disseminated throughout the rock.

Sample No.

81-RK-92

81-RK-93 81-RK-94 81-RK-95

81-RK-96 81-RK-97

Description

Rusty gneiss,quartz, pyRusty gneiss, pyRusty quartzMassive gneiss,cpRusty gneiss, pyQuartz/gneisscontact


240 10

270 914 6

3000 14

540740

1112

15

205

18

2032

MD

NDND

0.6

ND ND

ND5

ND

NDND

3 ND

ND NDND ND2 ND

ND ND

V00'

e.rs

\

31

GS 25

Location: District Municipality of Muskoka, Stephenson Township Lot 24 Concession XIII NTS: 31E/6 UTM: Zone 17 5014600N 632200E

Access: The reported showing is located 0.5 kilometres south ofSiding Lake between Lancelot Road and the CNR railroad line,


Sample No.

Alternate layers of felsic and amphibolite gneiss are cut by minor pegmatite stringers. Disseminated pyrite is found in the amphibolite gneiss in some parts of the felsic gneiss.

Description Cu Pb Zn Ag Au As S b PPM PPM PPM PPM PPB PPM PPM

81-RK-16 81-RK-17 81-RK-18 81-RK-19

GneissRusty gneiss Gneiss, py Gneiss, py

23305555

7624

43507062

0.40.30.40.2

NDNDNDND

NDNDNDND

NDNDNDND

GS 26

32

Location: District Municipality of Muskoka, Stephenson TownshipLot 26 Concession XIVNTS: 31E/6UTM: Zone 17 5016000N 632500E

Access; The pit is located on the northeast shore of Siding Lake near the Village of Martin Siding. From the old post office at Martin Siding, a trail leads part way to the pit which is about 500 metres west of Siding Lake.

History: Several tonnes of material have been removed from the pit, but no dump exists above the lake level.


Sample No.

A series of quartzo-feldspathic and hornblende gneisses strike north-south and dip to the east. The gneisses are cut by quartz-rich pegmatite stringers.

Description Cu PPM

Pb ZnPPM PPM

Ag PPM

Au PPB

AsPPM

Sb PPM

81-RK-91 Quartz 22 24 ND ND ND ND

TV) 0/4

100 100

ftxil Li W

GS 27

33

Location: District Municipality of Muskoka, Cardwell Township Lot 26 Concession IV NTS: 31E/5 UTM: Zone 17 5012300N 611400E

Access: Approximately 4 kilometres east of Rosseau on the road toAspdin, there is a road branching off to the south. Follow this road for 1.5 kilometres to a gravel pit on left. The pit is approximately 200 metres southeast of the road.

History; The pit was worked on for gold and/or copper over a period of several years, approximately 40 years ago. (R. Keevil, personal communication).


Sample No.

Biotite and hornblende gneiss are interlayered with quartz-feldspar gneiss in 30 centimetre layers. More recent pegmatitic intrusions crosscut the gneissic fabric. Mineralization occurs as disseminated pyrite in the mafic layers and as pyrite clots in the pegmatite.


81-RK-75 81-RK-76 81-RK-77 81-RK-78

Mafic gneiss Rusty pegmatite Rusty quartz, py Mafic gneiss, disseminated py

GS 28

34

Location: District Municipality of Muskoka, Cardwell Township Lot 26 Concession I NTS: 31E/4 UTM: Zone 17 5009700N 612100E

Access: The outcrop is located approximately 5 kilometres southeast of the Village of Rosseau on Highway #532. It is the first rock cut northwest of the intersection of Highway #532 and Rosseau Road 3.

History; A cliff face has been blasted to provide for the highway widening. No known exploration activity has occurred.

Geology and Mineralization The country rock is comprised of a quartz, biotite

gneiss with minor variation to an amphibolite, feldspar gneiss. A 3 to 4 metre zoned granitic pegmatite dike intrudes the gneisses with a northeast/southwest strike and vertical dip. Sulphide mineralization is restricted to the more mafic zones adjacent (pyrite) to the pegmatite.

Sample No.

81-RK-83

81-RK-84

Description

Felsic gneiss, quartz Pegmatite, quartz


66 20 300 ND 5 4 MD

134 30 275 ND 5 5 ND

35

GS 29

Location: Territorial District of Parry Sound, Humphrey Township Lot 3 Concession VI NTS: 31E/5 UTM: Zone 17 5013100N 605900E

Access: The outcrop is located on Highway #532 approximately l kilo metre north of Rosseau in a roadcut across from the Rosseau Cemetary.

Geology andMineralization: A mixture of a medium grained quartz feldspar gneiss

and a biotite hornblend gneiss are intruded by a pegmatite striking northeast-southwest. Disseminated pyrite occurs in the pegmatite.


81-RK-85 Pegmatite, py 225 25 220 0.3 ND

* i V —f* S^oJ** Do-l- A^*-*^

r

36

GS 30

Location: Territorial District of Parry Sound, Humphrey Township Lot 4 Concession II NTS: 31E/4 UTM: Zone 17 5008300N 607700E

Access: The pit is located on the "Burgess" Farm between the barn and Bellevue Bay. A tractor trail runs east from the barn, across a field and into a hardwood bush. The pit is located approximately 100 metres from the barn and 10 metres south of the trail.

History: Values (R. Whitehouse, personal communication) of $10./ton gold were reported from this pit 30 to 40 years ago.


Sample No.

The country rock is a quartz, feldspar, biotite gneiss that has been intruded by a pegmatite. Traces of pyrite were detected within the pegmatite and along the contact with the gneiss.

Description Cu Pb Zn Ag Au As Sb PPM PPM PPM PPM PPB PPM PPF.

81-RK-79

81-RK-80 81-RK-81 81-RK-82

Pegmatite/gneiss contact, 3% py Pegmatite, py Gneiss, py Pegmatite, py

64

1105023

32 100

331618

206530

ND

NDND

0.4

ND 2 ND

ND ND4 ND

24 iID

-K0

Yorfr^V

r 3*-b^a *v\cJI'l *

oo

GS 31

37

Location: Territorial District of Parry Sound, Humphrey TownshipLot 11 Concession XIINTS: 31E/5UTM: Zone 17 5016600N 601400E

Access:

History:

The pit is located 2.5 kilometres north along Turtle Lake Road, approximately 7 kilometres northwest of the Village of Rosseau. The workings are reached by following a tractor road for 50 metres (west of the Turtle Lake Road) .

The pit was worked 40 to 50 years ago. communication) .

(R. Fraser, personal

Geology and Mineralization

Sample No.

No outcrop is exposed in vicinity of the pit. From blasted rock, it would appear that a zoned pegmatite has intruded a biotite gneiss. Minor pyrite occurs in the pegmatite.


81-RK-86 81-RK-87 81-RK-88 81-RK-89

QuartzPegmatite, py Contact zone, py Pegmatite

72452 14 10048 16 12825 11 58

GS-32

38

McGown Mine

Location: Territorial District of Parry Sound, Foley Township Lot 146 Concession B NTS: 41H/8 UTM: Zone 17 5021200N 578300E

Access; The workings are on the northeast side of McGowan Lake approximately 0.5 kilometres from Highway #69.

History; Gold was discovered here in 1984 with underground workcommencing in 1897. Some free gold was recovered and the property was eventually developed for its copper potential. Various companies have examined the property during the past 80 years.


Sample No,

The rocks underlying the property consist of medium grained hornblende and/or biotite hornblende gneiss. Mineralization has been described as veins with considerable wall rock alteration. The randomly occuring veins carry varying amounts of bornite and chalcocite.

Description Cu Pb Zn Ag Au As S b PPM PPM PPM PPM PPB PPM PPM

81-RK-25 Gneiss, cc, bn 20000 81-RK-26 Gneiss 6500 81-RK-27 Gneiss, cp, bn, 20000

cc81-RK-28 Gneiss/pegmatite 13600

contact

82-AH-13 Gneiss and Quartz, 870582-AH-14 Gneiss and Quartz 64882-AH-15 Gneiss and Quartz 56082-AH-16 Gneiss, bn 2000082-AH-17 Gneiss 1550

3 23 18.5 1780 ND4 38 3.1 185 ND5 22 18.4 2790 ND

34 5.1 630 ND

t-22.5 1900.3 15 i,20.5 45 i.2

- 16.3 5370 i.20.5 90 i 2

ND ND ND

ND

1. 1

t- 1

39

GS 33 NICKEL CLIFF MINE

Location: Territorial District of Parry Sound, Armour Township Lot 17 Concession VII NTS: 31E/11 UTM: Zone 17 5054000N 628800E

Access: The pit is located on the south side of a hill approximately 200 metres north of Kernick Lake. It is approximately 220 metres west of a north-south road branching off concession road VII.

History: The workings-consist of a 5 metre shaft with 7 metres of drifting. A grab sample by Satterly (1942) assayed 1.37% cu., 1.40% ni and 0.01 oz./ton gold.

Geology andMineralization: The pit exposes a fine grained amphibolite gneiss

composed of 15% quartz, 45% amphibolite, 35% pyrozene and 5% sulphides and garnet. The gneiss is cut by quartz stringers that show no single trend.

Sample No.

82-AH-l

82-AH-2

82-AH-3

Description

Mafic gneiss,rustyRusty gneiss,PY, cpRusty gneiss,py, cp fromdump.

Cu Ag Au As Sb PPM PPM PPB PPM PPM

168 0.1

576 0.1

1425 0.3

(5

10

15

(2

4.2

a

a

\X x

A

40

GS 34

Location: Territorial District of Parry Sound, Hagerman Township ~~ Lot 61 Concession A

NTS: 31E/12 UTM: Zone 17 5055600N 589500E

Access:The two pits are located north of the intersection of Highway #124 and York Street in the town of Dunchurch. The first pit is 50 metres southwest of York Street from a point on York Street 75 metres northwest of Highway #124. The second pit is approximately 400 metres from Highway #124 on the north

side of York Street.


Sample No.

Both pits expose pegmatite dikes and lenses in a biotite, feldspar gneiss. A zone of mineralization containing pyrite, pyrrhotite and chalcopyrite is exposed at the contact of the gneiss and the pegmatite


82-AH-6 82-AH-7 82-AH-8 82-AH-9 82-AH-10

Pegmatite, py, po Pegmatite, py, po Gneiss, py Gneiss, py Pegmatite, py

474852

10954

cS0.1 0.1 a

a

E3* 10

N

IS) 40

GS 35

41

Location: Territorial District of Parry Sound, Proudfoot Township Lot 6 Concession III NTS: 31E/11 UTM: Zone 17 5052900N 638700E

Access: From a cottage (presently owned by C. Meachen) at the end of the North Sand Lake Road, walk approximately 2 kilometres at a bearing of 265 degrees to the only sizeable outcrop on the east shore of Tank Lake. No workings were located.


Sample No.

The country rock is a pink biotite, feldspar, quartz gneiss with inclusions of hornblende gneiss. A number of quartz veins, up to 15 centimetres across, cut through the gneiss. No mineralization was detected.


82-AH-ll 82-AH-12

Quartz Gneiss 0.1

Kilo** efe r 5

GS 3642

Location; Territorial District of Parry Sound, Foley Township Lots 26 Concession XI NTS : 41H/8 UTM: Zone 17 5019800N 577800E

Access: From Highway #69, go west on the South Parry Road for approx imately 2 kilometres. Cross the CN tracks just north of the South Parry station. Proceed on a path (see sketch) to the CP tracks, cross the tracks and continue into the bush. The shaft is located on the northwest side of the path.

History: The shaft is reported to be 30 metres deep.

Geology and Mineralization :

Sample No.

The country rock is amphibolite gneiss with no significant mineralization present. All samples were taken from the dump.


82-AH-23 Amphibolitegneiss



82-AH-26 Hornblende gneisswith quartz

109

25

18

8

0

^0

^0

.1

.1

.1

5

^5

^5

(-2

t-2

^2

:e.rs

43

GS 37

Location: Territorial District of Parry Sound, Lount Township Lot 129 Concession B NTS: 31E/13 UTM: 5071000N 606400E

Access: The pits are located approximately 175 metres west of the Old Nipissing Road, about 100 metres north of a bush road.

Geology andMineralization: In the pit the magnetite occurs as a l metre thick flat

lying band underlain by a quartz-feldspar gneiss.Local people reported that the magnetite ran l oz. perton gold.

Sample No. Description Cu Pb Zn Ag Au PPM PPM PPM PPM PPB

83-36-1 Magnetite 83-41-1 Gneiss, 15%

disseminated mag 83-41-2 Magnetite 83-41-3 Gneiss, 5% mag 83-41-4 Magnetite

14 284

7±2 42

'-z O'A

km.

GS 3844

Location: Territorial District of Parry Sound, Laurier Township Lot 22 Concession XIII NTS: 31E/14 UTM: Zone 17 5091900N 631400E

Access; The pits are approximately 150 metres west of a gravel road that provides access to a control dam on the north side of Sausage Lake and approximately 400 metres south of the forest access road from Trout Creek.

Geology andMineralization; The country rock is a medium grey quartz-feldspar

schist with finely disseminated flake graphite throughout. The southern pit exposes a vein of "massive graphite" up to l metre wide.

Sample No.

83-37-la 83-37-lb

83-37-lc 83-37-ld 83-37-2a

83-37-2b

83-37-2C

83-37-2d

83-37-2e

83-37-2f

Description

Massive graphite Schist, disseminated graphiteMassive graphite Massive graphite Schist, disseminated graphite, py Schist, disseminated graphite, py Schist, disseminated graphite, py Schist, disseminated graphite, py Schist, disseminated graphite, py Schist, disseminated graphite, py

Cu Pb Zn Ag Au PPM PPM PPM PPM PPB

3046

242140

51

44

45

16

22

9 17516

111723

33

18

35

18

29

65 0.2

34 0.136 0.294 0.5

17 0.8

15 0.3

20 0.4

23 0.5

15 0.3

4.5 27.8545 10.03

45 21.8045 21.5045 0.97

45

tS

45

45

(5

2.87

3.45

3.12

0.95

1.12

rtj

GS 39

45

Location: Territorial District of Parry Sound, Laurier TownshipLot 22 Concession XIIINTS: 31E/14UTM: Zone 17 5091300N 631400E

Access: Proceed east from Trout Creek along a forest access road to the gravel road that goes to the control dam on the north side of Sausage Lake. Follow this road to the end and then walk east along the lake to the second cottage. The pit is located behind the cottage.

Geology andMineralization; The country rock is a light to medium grey quartz-

feldspar schist with finely disseminated graphite throughout.

Sample No. Description Au PPB

Ag PPM

83-43-1 Schist, graphite83-43-2 Schist, graphite83-43-3 Schist, graphite83-43-4 Schist, graphite83-43-5 Schist, graphite

2 ^24 ^26 ^2

46

Appendix II

Outcrop visited from other projects where samples were collected and analyzed for gold.

47 Sample No.: T-9-10-25-1

Location: The location is on the east side of Parry Island near Kichimashkosing Marsh. NTS: 41H/8 UTM: Zone 17 5012800N 565200E

Description of Sample Cu Pb Zn Ag Au HgPPM PPM PPM PPM Ppi PPB

Quartz *5 clO 8 ±2 300 t.20

Sample No.: T-9-8-21-1

Location; The location is on Rumbles Island south of Parry Island. NTS: 41H/1 UTM: Zone 17 5004800N 563900E

Description of Sample Cu Pb Zn Ag Au HgPPM PPM PPM PPM PPB PPB

Mafic Meta-volcanic 92 20 240 2 7 ^20

Gr Mil Ti V Zr PPM PPM PPM PPM PPM

100-1000 500-5000 500-5000 100-1000 100-1000

Sample No. : T-9-10-3-8

Location: The location is on Ellen Pearce Island near White Bay on Sans Souci Island. NTS : 41H/1 UTM: Zone 17 5002600N 568100E


Mafic Meta-volcanic (?) 76 *:10 102 L2 36

Ni V ZnPPM PPM PPM

100-1000 100-1000 100-1000

Sample No.; T-9-10-2-2

Location: The location is on the southwest shore of Ruddy Island west of Clear Lake. NTS: 41H/1 UTM: Zone 17 5006500N 572800E

Description of Sample Cu Pb Zn Ag Au HgPPM PPM PPM PPM Ppi PPB

Felsic Meta-Volcanic (?) 5 O. O 101 (.2 6 (20

Mn Zn PPM PPM

500-5000 500-5000

48

Sample No.: T-9-10-3-12

Location; The location is on the north tip of an island off the west side of Bernyk Island. NTS: 41H/1 UTM: Zone 17 5006600N 566700E


Felsic Meta-Volcanic (?) 14 ^0 190 O 3

Zr PPM

100-1000

Sample No.: T-9-10-3-11

Location: The location the north tip of Peacock Island in Waubuno Channel. NTS: 41H/1 UTM: Zone 17 5006600N 564600E

Description of Sample Cu Pb Zn Ag Au HgPPM PPM PPM PPM PPB Ppi

Gossan zone 93 33 470 L2 13 50

Mn V ZrPPM PPM PPM

100-1000 100-1000 100-1000

Sample No. T-9-10-24-6

Location: The location is on the west tip of Lent Island southeast of Parry Island. NTS: 41H/1 UTM: Zone 17 5008200N 566800E


Mafic Meta-Volcanic (?) 22 26 190 ^2 7 20

Sample No.: T-9-10-24-3

Location: The location is on the northeast tip of an island north of Bernyk Island in Spider Bay. NTS: 41H/1 UTM: Zone 17 5007200N 567900E


Felsic Meta-Volcanic (?) 16 <lO 142 c2 13

49


Location: The location is on Highway #69 near the outlet for Mill Lake, NTS: 41H/8 UTM: Zone 17 5023200N 577200E


Meta-Sediment (?) 46 ^0 150 <2 8 30

Sample No.: T-9-10-25-4

Location: The location is on Fajanmar Point on McLaren Island. NTS: 41H/8 UTM: Zone 17 5011600N 569200E


Felsic Meta-Volcanic (?) 30 UO 22 -C2 7

Sample No.: T-9-10-25-3

Location: The location is on the southwest tip of McLaren Island in 5 Mile Bay. NTS: 41H/8 UTM: Zone 17 5011800N 567300E


Meta-Volcanic (?) with desseminated 280 11 240 *2 20 20 sulphides

Sample No.; T-8-9-20-3B

Location: The pit is located at the south end of Spider Lake. NTS: 41H/1 UTM: Zone 17 5009800N 571300E


Felsic meta-volcanic (?) 14 38 450 O 4.10

50

Sample No. T-8-9-20-3C

Location: The pit is located at the south end of Spider Lake.NTS: 41H/1UTM: Zone 17 5009800N 571300E

Description of Sample Cu Pb Zn Ag Au HgPPM PPM PPM PPM PPB

Felsic meta-volcanic (?) 4180 12 6950 O 20


Location: The pit is located on the east side of Spider Lake. NTS: 41H/8 UTM: Zone 17 5011300N 573600E

Description of Sample: Cu Pb Zn Ag Au HgPPM PPM PPM PPM PPB PPB

Felsic Tuff (?) (Brecciated) 7 66 112 c3 UO /120


Location: The pit is located on the west side of Spider Lake. NTS: 41H/1 UTM: Zone 17 5010500N 571600E

Description of Sample Cu Pb Zn Ag Au HgPPM PPM PPM PPM PPi Ppi

Felsic meta-volanic (?) with 900 18 320 O ^.10 disseminated sulphides


Location: The pit is located on the west side of Spider Lake. NTS: ' 41H/1 UTM: Zone 17 5010900N 572000E

Description of Sample Cu Pb Zn Ag Au HgPPM PPM PPM PPM P?i P?i

Felsic meta-volcanic (?) with 420 10 250 c3 disseminated sulphides

51


Location: The pit is located on the west side of Spider Lake. NTS: 41H/8 UTM: Zone 17 5012100N 573100E


Felsic Meta-volcanic (?) 330 270 490 *3 /li O /20


Location: The pit is located at the south end of Spider Lake. NTS: 41H/1 UTM: Zone 17 5009900N 571500E


Felsic volcanic (?) with 4350 28 1300 O 20 ^20 disseminated sulphides


Location: The pit is located on the east side of Spider Lake. NTS: 41H/1 UTM: Zone 17 5011300N 573600E~


Felsic volcanic (?) with 6950 15 940 ^3 20 disseminated sulphides


Location; The location is on the mainland west of Clear Lake and east of Spider Bay. NTS: 41H/1 UTM: Zone 17 5006900N 572600E


Meta-volcanic (?) 11 -clO 133 2 7

52


Location; The pit is located on the west side of Spider Lake. NTS: 41H/8 UTM: Zone 17 5012100N 573100E


Felsic Meta-volcanic (?) *5 116 520 O

Sample No. : T-8-8-30-3

Location: The pit is located on the west side of Spider Lake. NTS : 41H/8 UTM: Zone 17 5012100N 573000E


Felsic Meta-volcanic (?) 56 62 76 ±3 ±10 ^25

Sample No.: T-8-9-20-3D

Location: The pit is located at the south end of Spider Lake. NTS: 41H/1 UTM: 5009800N 571300E ' .


Mafic Meta-Volcanic (?) 24 37 206 O ^10 ^.20


Location: The location is on Milton Island in the South Channel near McLaren Island. NTS: 41H/1 UTM: Zone 17 5013300N 570900E


Meta-volcanic (?) with 580 10 110 2 10 20 disseminated sulphides

53


Location: The location is on the mainland, southeast of Parry Island near Hills Bay in the South Channel. NTS: 41H/1 UTM: Zone 17 5008700N 567700E


Meta Volcanic (?) 60 11 400 2 18 20

Gr Co Mn Ti V Zn PPM PPM PPM PPM PPM PPM

100-1000 100-1000 500-5000 5000-50000 100-1000 100-1000

54

Appendix III

Reported occurrences (Satterly, 1942) that have not been visited

Township

Armour

Bethune

Chaffey Foley

Lot

28

14

24 9

Concession

IX

VIII

XIII III

Hagerman 32

LountLountLountMacharMcconkey

McMurrichMcMurrich

McMurrich

Nipissing

Nipissing

Nipissing

Nipissing

Nipissing

14124124

218

1314

18

6

20

22

25

25

IIIABVIV

XIVXIV

I

XV

I

XV

I

VII

Pringle 25

South Himsworth 24

VII

II

Comments

l pit, quartzite band in biotitegneiss, pyriteShallow pits, disseminatedpyrrhotite in gneiss cut bypegmatiteBiotite gneiss, pyl pit, hornblende gneiss cut bypegmatite, py, pol pit, garnet-hornblende gneiss,pol pit, hornblende gneiss, cpl pit, amphibolite, po, cp, pyl shaft, amphibolite, cp, pol open cut, biotite gneissl open cut, biotite gneiss cutby pegmatitel pit, quartz-rich pegmatiteSeveral pits, gabbro cut bypegmatite1 pit, hornblende gneiss cut by pegmatite, py, po2 pits, biotite schist, granitegneiss, pegmatite, py2 pits, biotite gneiss cut bypegmatite, pol pit, granite gneiss cut bypegmatitel pit, old Hewitt mine, biotitegneiss, pyl trench, Golden Eagle Mine,limestone with bands ofhornblende gneiss, pol trench, Golden Eagle Mine,limestone with bands ofhornblende, gneiss, poBiotite gneiss cut by pegmatite

55

Appendix IV

Reported occurrences (reference unknown) that have not been visited

Township Lot Concession Comments

. Butt 3 IButt 3,6,7 VIButt 7 IX, XButt 13 VI

56

References

Bell, Robert1876: Report on geological researches north of Lake Huron and east

of Lake Superior; in Geol. Surv. Canada, Report on Progress 1876-77. (Published 1878).

The Canadian Mining Review 1900

Carter, W.E.H.1903: Mines of eastern Ontario; p. 108-140 in Ontario Bur. (now

Dept.) Mines, Vol. 12.

Coleman, A.P.1894: Gold in Ontario: its associated rocks and minerals; p. 35-100

in Ontario Bur. (now Dept.) Mines, Vol. 4. 1899: Copper in Parry Sound District; p. 259-262 in Ontario Bur.

(now Dept.) Mines, Vol. 81900: Copper and iron regions of Ontario; p. 143-191 in Ontario

Bur. (now Dept.) Mines, Vol. 9.

Davidson, A.1982: Graphite occurrences in the -Algonquin region, Grenville

Province, Ontario; Geological Survey of Canada, Open File 870.

Davidson, A. and Morgan, W.C.1981: Preliminary notes on the geology east of Georgian Bay,

Grenville Structural Province, Ontario; in Current Research, Part A, Geological Survey of Canada, Paper 81-1A; p. 291-298.

Davidson, A., Culshaw, N.G., and Nadeau, L.1982: A tectono-metamorphic framework for part of the Grenville

Province, Parry Sound region, Ontario; in Current Research, Part A, Geological Survey of Canada, Paper 82-lA, p. 175-190.

DeKalb, C.1901: Mines of eastern Ontario; p. 113-136 in Ontario Bur. (now

Dept.) Mines, Vol. 10

Hewitt, D.F.1967: Geology and Mineral Deposits of the Parry Sound-Huntsville

Area; Ontario Dept. Mines, Geological Report 52.

Lacy, W.C.1960: Geology of the Dunchurch area, Ontario; p. 1713-1718 in Bull.

Geol. Soc. Amer., Vol. 71.

57

References (cont'd)

Lumbers, S. B.1971: Geology of the North Bay area, Districts of Nipissing and Parry

Sound; Ontario Department of Mines and Northern Affairs, Geological Report 94; 104 P. and Map 2216.

1975: Geology of the Burwash area, Districts of Nipissing, Parry Sound, and Sudbury; Ontario Division of Mines, Geological Report 116; 158 p. and Map 2271.

1976: Mattawa - Deep River area, District of Nipissing and County of Renfrew; Ontario Division of Mines, Preliminary Maps; p. 1196 and 1197, Geological Series.

1978a: Geology of the Grenville Front Tectonic Zone in Ontario; in Toronto '78, Field Trip Guidebook, ed. A.L. Currie and W.O. Mackasey; Geological Association of Canada; p. 347-361.

1978b: Southern Renfrew County; in Summary of Field Work, 1978, ed. V.G. Milne, O.L. White, R.B. Barlow, and J.A. Robertson; Ontario Geological Survey, Miscellaneous Paper 82; p. 125-127.

1980: Geology of Renfrew County, southern Ontario; Ontario Geological Survey, Open File Report 5282; 118 p. and Preliminary Maps P. 1838, . P. 2355, P. 2356, P. 2357, Geological Series.

Ontario Dept. Mines1908: Statistical Review; p. 5-52 in Ontario Bur. (now Dept.) Mines,

Vol. 17.

1909: Statistical Review; p. 5-70 in Ontario Bur. (now Dept.) Mines, Vol. 18, pt. 1.

1916: Mines of Ontario; p. 66-162 in Ontario Bur. (now Dept.) Mines, Vol. 25, pt. 1.

Parks, W.A.1900: Work in the Muskoka district, Ontario; p. 121-126 in Geol.

Surv. Canada, Summ. Rept. for 1900, pt. A. (Published 1901).

Satterly, J.1942: Mineral Occurrences in Parry Sound District; (accompanied by

Map 51A). Ontario Dept. Mines, Vol. 51 pt. 2. (Published 1943) .

1956: Geology of Lount Township; Ontario Depatment of Mines, Annual Report for 1955, V. 64, part 6, 46 p.

Schwerdtner, W.M. and Waddington, D.H.1978: Structure and lithology of Muskoka - southern Georgian Bay

region, central Ontario; in Toronto '78, Field Trips Guidebook, ed. A.L. Currie and W.O. Mackasey; Geological Association of Canada, p. 204-212.

58

References (cont'd)

Slaght, A.1895: Sixth report of the Inspector of Mines; p. 259-287 in Ontario

Bur. (now Dept.) Mines, Vol. 5.

1898: Mines of eastern Ontario; p. 85-100 in Ontario Bur. (now Dept.) Mines, Vol. 7, pt. 1.

Walker, T.L.1905: The Muskoka district, Ontario; p. 84-86 in Geol. Surv. Canada,

Summ. Kept, for 1905. (Published 1906).

1913: The Precambrian of Parry Island and vicinity; p. 98-100 in Geol. Surv. Canada, Guide Book No. 5.

31 E CANADA EDITION 2Powassan 6 mi 10 km

. North Bay

\ f

reter TO mis-map asMAP 31 E CARTF

3 78000'46000'

Reference de cette carteFDiriQK 2 MCE FDIttOWpoor usage mi mane

TEM THOUSAND METRE UNIVERSAL THANSVERSC MERCATOR emo

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Port Severn 16 mi 26km\ 30'Lindsay

Minden 8mi 13km Lachlin 4mi 8km Apslty 19 mi 31 kmTory Hill 2 mi 3 km TnryHUI 4 mi 6km

Produced by the SURVEYS AND MAPPING BRANCH. DEPARTMENT OF ENERGY, MINES AND RESOURCES. Updated from large scale maps. Information current as shown m diagram.

Etablie par la DIRECTION DES LEVES ET DE LA CARTOGRAPHIE, MINISTERE DE L'ENERGIE, DES MINES ET DES RESSOURCES. Mise a nwr d'apres des cartes a grande echetle. Renseignements a jour lets qu indiqyes auHUNTSVILLE

ONTARIOMagnetic declination 1975 varies from 9"01 westerly at centre ot west edge to 11"0?' westerly at centre o) east edge Mean annual change decreasing O l

La declinaison magnetique pour 1975 vafie de 9=01' Quest au centre de la limit* Quest a 11117 Quest au centre de la limite Est. Variation moyenne annuelle decrwssante O l'.

G Canada 1977, tcus droits receivesG Canada Copyrights Reserved 1977

Rowh:hard surface, alt weather

hard surface, all weather

loose or stabilized surface, all weather.,

loose surface, dry weather

cart track

trail, cut line or portage

Scale 1=250,000 Echelte5 10

Routes;

pav6e, toute saison

gravier agglornir*, toute saison

de gravier p*ri

de terre

senlier. percee ou portage

{QUIDISTANCE DES COURflES 100 PIEDSElevations en pied s au-dessus du niveau moyen de la nwSysleme de telerence geodesique noid-amencain. 1927

Projection transverse de MercatorFM COMPLETE REFERENCE SEE REVERSE StK

CWTOUB INTERVAL 100 FEET Elevations in Feet above Mean Sea level

North American Datum 1927 TransvtfSe Mercator Projection

Copies may be obtained trom the Canada Map Office. Ces caries sont en vente au Bureau des Cartes do Canada. Department ot Energy, Mines and Resources, Ottawa, ministere de I'Energie, des Mines et des Ressootces. Ottawa.

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or your nearest map dealer. au chti le vendeui le plus pres.

Index to adjoining Maps ot the National Topographic System

Tableau d'ass*mblage du System* national de reference cartogiaphique

HUNTSVILLE- - 31 E , -- :

EDITION 2 . .

-am***

41 H 1:250,000 CANADA EDITION 2 41 H

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Produced by the SURVEYS AND MAPPING BRANCH, DEPARTMENT OF ENERGY, MINES AND RESOURCES Updated from 1:50.000 maps. Information current as of 1974.

ftablie par la DIRECTION DES LEVES ET DE LA CARTOGRAPHY. MtNISTERE DE L'ENERGIE, DES MINES ET DES RESSOURCES Mise a |our d'apres des cartes 1:50,000. Renseignements a jour en 1974

l S kl HORT^BAYTOBERMORYONTARIO

Magnetic declination 1975 varies from 6"19' westerly at centre of west edge to 8"31' westerly at centre of east edge. Mean annual change decreasing 1.4'

La declinaison magn*tiqut pour 1975 varie de 6019' Ouest au centre de la limite Ouest a 80 31' Ouest au centre de la limite Est Variation moyerme annuelle decroissante 1.4'

Scale 1:250,000 EchelleS 10

Roads:



loose or stabilized surface, all weather........

loose surface, dry weather

cart track

trail or portage..

CONTOUR INTERVAL 100 FEET Elevations in Feet above Mean Sea Level

North American Datum 1927 Transverse Mercator Projection

EQUIOtSTANCE DES COURSES 100 PIEDSElevations en pieds au dessus du niveau moven de la merSysteme de reference geodesique nord-americain. 1927

Projection transverse de Mercator

Routes:

pavee, toutesaison.

pavee.toutesaison..

gravier agglorner*. toute sarsen.

de gravier ptriode sdche..

de terre..

senticr cai portage..

FOR COMPLETE REFERENCE SEE REVERSE SIDE Copies may be obtained from the Canada Map Office. Ces cartes sont en vente au Bureau des Cartes du Canada.Department of Energy. Mines and Resources. Ottawa. ministere de I'tnergie. des Mines et des Ressources. Ottawa,or your nearest map dealer ou erie? le vendeur le plus pres

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TOBERMORY41 H

EDITION 2

31

f "*r of gold analysis

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