RPT ON EXPL PROGRAM FOR GARNET/SILLIMANITE…

31F03NW0004 OP91-335 ASHBY LAKE 010

Report On

ID

ASHBY, LAKE, TUDOR AND GLAMORGAN TOWNSHIPS

This Is An O.P.A.P. funded Project (O.P.A.P. Number OP91-335)

RalpTrV. Stewart, B. Se., P. Geo l December 21,1991

31F03NWOOO4 OP91-335 ASHBY LAKE 01 OC

TABLE OF CONTbNlj

SUMMARY........................ . .. . . . . . . ....... . .. ... .. . 1

RUBY GARNET PROPERTY(Ashby Twp.)........................2,3

PARKHURST LAKE GARNET/SILLIMANITE PROPERTY (Ashby Twp)..4,5

MILLBRIOGE AREA (TUDOR-LAKE Twps).......................5,6

GOODERHAM AREA (GLAMORGAN Twp)..........................7

LOCATION AND ACCESS.....................................8

Appendix A -DAILY FIELD WORK SHEETSSee Section IV of foregoing Government Form for a summary by dates (May 21,

1991 to November 23, 1991) A1 to A45

APPENDIX B Thin Section Reports...By Glenn R. Brown B1 to B31

APPENDIX C Multielement Assay Analysis Parkhurst Lake Property

Index Page 1 (Sample List A Locations)..... 1Index Page 2 (Description Of Samples)...... 2Results By Chemex Labs Ltd *X-Ray Assay Laboratories CI to C5

APPENDIX D INDEX PAGES (Expense Account) 1,2

Receipts For Project DI to D35

DRAWINGS (IN POCKET OF REPORT)

Drawing Drawing .Title

S 91-15 Geological Plan Ruby Garnet Property (North Sheet)S 91-16 Ruby Garnet Contour Plan (X Garnets-Surface Mapping)S 91-18 Geological Plan Ruby Garnet Property (South Sheet)S 91-19 Geological Plan Parkhurst Lake Property (West Sheet)S 91-20 Geological Plan Parkhurst Lake Property (East Sheet)S 91-21 Geological Plan Gooderham Area (Glamorgan Twp.)S 91-22 Geological Plan Mi 11 bridge Area (Lake/Tudor Twp)

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Thls report describes the results of field mapolng and prospecting, carried out In the exploration and evaluation of garnet in the RUBY MINE AREA, and garnet/sillimanite, plus base/precious metals in the PARKHURST LAKE AREA, both in Ashby Twp.

In the MILLBRIDGE and GOODERHAM AREAS, exploration Mas carried out principally for wollastonite, but other commodities (talc, tremolite, A marble) were also examined.

RUBY GARNET AREA: Geological mapping has defined an extensive garnet enriched zone, at least O.SMiles (1.4KH) in strike length, and with widths from 50 to 200 feet. It 1s estimated that at least 1.8 million tons of ore, containing +30X garnets, exist from surface to a vertical depth of 100 feet. In the vicinity of an old quarry, a garnet enriched zone containing 30X to +50X garnet, has a strike length of some 500 feet, and a width of 50 feet. In addition to the garnet potential, there is also the possibility of extracting sillimanite from specific portions of the garnet enriched zones. More test work is required to determine the feasibility of mining this commodity.

PARKHURST LAKE AREA: Prospecting in the eastern part of this property in 1991, failed to locate the HANAH GARNET PROSPECT, as reported in OGS Mineral Deposits Circular 22 page 38. It is probable that the reported location of this prospect may be in error. Prospecting in the western portion of the property for garnet and sillimanite, did not locate additional reserves of these minerals. In the southwestern section of the property, a number of grab samples selected from "sulphide gossaned" zones in quartz gneiss, yielded anomalous assay values in gold (120 ppb), zinc (484 ppm), nickel (723 ppm) and copper (544 ppm). Further work is required to evaluate the significance of these silicified zones.

MILLBRIDGE AREA: Prospecting for wollastonite along the traverses shown on drawing S 91- 22, failed to define any significant amount of this mineral. One thin section sample (S 91-25) indicated the presence of minor amounts of this mineral, which points to the possibility of locating additional occurrences along the southern side of the gabbro. Along the western side of the Tudor gabbro, a number of occurrences of tremolite and talc were noted in a white carbonate bearing rock. Further work here may be warranted.

QOODERHAM AREA: Traverses completed In this area failed to locate any wollastonite mineralization, however two areas with skarn type garnet occurrences were identified. These two occurrences warrant a limited amount of field mapping to more accurately outline the size of the zone. A limited amount of testing to determine garnet hardness and processing characteristics is also warranted.

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. y

The 1991 mapping and prospecting work was a continuation of the geological mapping completed under 1990 O.P.A.P. grant- OP 90-190. The 1990 work was carried out over claims 1091941, 1094219 ft -20, and 1095197. The 1991 surveys were completed over the four claims 1150442 to 1150445 Inclusive (Dwg. S 91-15), and a limited prospecting program south of the above four claims (Dwg. S 91-18). The current survey involved the establishment of baseline 5, which was used as mapping control for the survey.Stations were established every 150 feet, along this baseline. The traverse lines shown on Drawing S 91-15, were run at right angles to this baseline, using the tape and compass method of mapping control.

The current work defined the geology and garnet enriched zones encompassing the old Ruby Quarry, and successfully traced these zones south and north of the quarry, as shown on drawing S 91-15. The limited survey completed south of the sheet (see dwg. S 91- 18), was also successful in further extending garnet bearing gneiss and paragneiss rocks a distance of some 2000 feet.

In addition to garnet, the presence of sillimanite was observed in a number of locations, especially where folding or shearing of the fine grained garnet gneiss was more intense.

GEOLOGICAL DESCRIPTION

As shown on drawing S 91-15, garnet enriched zones in gneiss and paragneiss extend in a general north-south direction, for a strike direction of some 4500 feet (1.4 KM). The rock types evaluated under this survey are designated as follows:

8A Pink Leucocratic Granite or Biotite Granite Gneiss 2a Quartz Mica Gneiss (Biotite, Quartz, Muscovite,

Plagioclase) 2pX2q- (2p-Garnet Gneiss/Paragneiss w/Trace to 10X Garnet)

(2q-Quartzitic Gneiss w/ Trace to 10X Garnet) 2peX2qe-Similar to 2p72q above but with 10* to +30X Garnet. 2pm Garnet/Muscovite Gneiss w/ 0-1OX Garnets 2pem Similar to 2pm, but w/ 10X to -i- 30X Garnet

A total of seven thin sections were cut from a number of representative rock types. A description of these is detailed in Appendix B (Pages B 18 to B 31). In general, the garnet enriched zone appears to mirror the strike and dip of the enclosing rocks. North of approximately 6+00 S (at the baseline), the

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gneissosity dips steeply to the northwest. South of this point, all dips appear to be more gentle but In an east to northeasterly direction. The old Ruby Pit is located some 500 feet north of this "change in dip direction".

ECONOMIC POTENTIAL

The geological mapping also Involved an evaluation and determination of the visual X of garnets in the rock outcrops examined. In order to calculate potential ore reserve tons and value, a separate map was prepared (Drawing S 91-16) .

Ore reserves are based on surface geological mapping and a visual evaluation of all outcrops shown on drawing S 91-15. The resulting contour map, Dwg. S 91-12, (showing the interpreted outline of +10X, 20X and +30X garnet rich areas) was used to calculate the following ore reserve figures.

Area Tons___* ____Tons___* Total Tons * (+30X Garnet) (20X-30X Garnet) (+20X Garnet)

1 1,220,000 780,000 2,000,000

2 210,000 520,000 730,000

3 320,000 870,000 1,190,000

4 60.000 450.000 510.OOP

Total 1.810.OOP 2.620.000 4.43O.OOO

* tons are calculated frow surface to a depth of 100 feet.

It is Interesting to note in the vicinity of the old Ruby quarry, a zone of garnet enrichment (30* to -i- 50X garnets) approximately 50 feet wide, extends along strike for a distance of some 500 feet. It would appear this would be a preferred area to establish the main quarry.

The next step in evaluating the deposit, will be to complete a limited diamond drilling program in the vicinity of the 30X-50X garnet enrichment zone. Core from this program would be processed to determine the most feasible approach of garnet extraction and evaluation, and facilitate design of a quarry.

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EAST OF 18+00 MAIN BASE LINE EXTENSION (Dwa. S 91-20) Subsequent to the acceptance of the OPAP application, an expanded prospecting proposal east of the area explored in 1990 (ie 18+00 E to 65+00 E) was submitted. In this area, prospecting and mapping, was aimed at locating and evaluating the so called Hanah Garnet Prospect (OGS Mineral Deposits Circular 22-page 38). The location of the Hanah prospect (according to Circular 22) should be between 51+00 and 66+00 East, on drawing S 91-20. Minor indications of garnets were noted, but no significant concentrations located. This information leads me to suspect the previously reported location of this prospect may be in error. At any rate, there are no garnet concentrations of economic potential in the area prospected and mapped. A few minor occurrences of sillimanite were noted (trace amounts), and the potential for concentrations of this mineral is also negligible.

WEST PART OF PROPERTY (Dwg. S 91-19)

Geological mapping in 1990, defined a zone of garnet/si llimanite concentration from approximately 10+50 East to 10+00 West. Garnet content in portions of this zone exceeds +20X , and +10X sillimanite. Part of the 1991 objective, was to further define this garnet/si l limanite zone, and prospect for other concentrations of sillimanite/garnet within the quartz-hornblende gneiss, close to the large body of leucogranite. The traverses completed in 1991 did not encounter other significant garnet/si llimanite mineralization, although the main garnet-si l limanite zone continues westward, and is probably cut off by the leucogranite body.

In the process of the 1991 geological examinations, a number of brown gossaned outcrops (in quartz/hornblende gneiss) were noted along the southern portion of Traverse 4 (Az 197 ). A grab sample of this pyrite bearing material (Ont 91-01..Page C-2) gaveanomalous values In gold, copper, zinc, and nickel. A number of additional grab samples from other gossaned outcrops were subsequently collected, and also yielded anomalous values. The assay results from eleven samples (S 90-60 to S 90-70) are presented on pages C-4 A C-5 of Appendix C..

The following table summarizes anomalous assay values obtained:

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Samnle No. Au(ppb) Cu(ppmJ Zn(ppm) Ni(ppm)

S 91-60 S 91-61 S 91-62 S 91-63 S 91-64 S 91-65 S 91-66 S 91-67 S 91-68 S 91-69 S 91-70

3569120116

171532

98.3280.0242.0332.0

544.0

96.8136.0268.0278.0484.0286.0

114.0178.0147.0262.0

723.0

Anomalous gold values appear to be associated with a diorite/granite dyke, as shown on AREA 1 SKETCH. Sulphide mineralization occurs in silicified and sheared zones, along the contact of this dyke.

Other anomalous values appear to be associated with silicified shear zones, which may or may not lie close to granitic dykes. Anomalous base and precious metal values appear to be the result of metasomatism, along the contact of the leucogranite, immediately west of the area sampled. Further study and investigation of these occurrences is warranted.

The objective of this program was to explore for wollastonite along the contacts of the Tudor gabbro. A revision to the proposed mapping was submitted on August 21, 1991, and the work completed is shown on Drawing S 91-22. The writer had difficulties completing traverses as planned, especially along the south and southwest contact of the gabbro (see Dwg. S 91-5 in program proposal). Air photos for this area are out of date, and there are numerous "no trespassing" signs on some of the main access routes. An attempt was made to locate the reported wollastonite occurrence (OGS Open File 5715), but this was not feasible without better ai r photo control.


Rock types examined in these t. ra ve TSAR are summarized as follows:

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GEOLOGICAL DESCRIPTION-Cont...

ROCK TYPES: 8a Altered Gabbro 7d~Gabbro 7e Diorite6 Granlte/Svenlte (Intrusives) 5 Limestone/Marble (UncHfferentiated) 5a Limestone (Graohitic) 5b DolomiteSe Marble (Micaceous-Phlogopite) 5f TremoHtic Marble 5k Felsic TactiteSG/g-Calc/SiUcate Skarn (w/ pyroxenes or amphiboles 5q Quartzitlc/Calc Silicate rock ( some mica)

The object of completing the traverses shown on drawing S 91-22, was to explore for wollastonite and other associated minerals, in the metasediments (metalimestones), along their contact with the Tudor gabbro.

Where rocks looked favourable for wollastonite, samples were selected for thin section analysis. A total of seven rock samples were selected and thin sections prepared (see pages BS to B17). Sample S 91-25, was the only thin section in which wollastonite was detected, but the content was very low ( < 5X). This occurrence does point to the possibility that wollastonite may exist in more abundance at other locations along the southern contact of the gabbro. A requirement for additional exploration would be better ground control (le new air photos or cut control lines).

Other minerals of possible economic interest observed during the 1991 program were talc, tremolite, and marble. Of some interest may be the possible existence of a tremolite/talc/carbonate deposit along the western gabbro contact, and within the general area defined by Traverse 3. As indicated 1n the description of sample S 91-47 and -48, the above mentioned minerals are present, but more detailed exploration would have to be completed to determine if mineral concentrations of mineable dimensions exist. In addition, very white dolomitic marble was observed along Traverse4A, and there may be some possibility of locating a quarry to extract dimension or ornamental stone here.

Two locations of grab samples of sulphide bearing "gossaned" rock (Samples S 91-26 and S 91-52) are shown on the INDEX PLAN. These were selected for multielement assay analysis. Anomalous base or precious metal values were not detected in these samples (Appendix C pages C4 A C5)

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A number of traverses were completed around the contacts of the Glamorgan Twp. gabbro, located in the southeast corner of this township (see ODM geology map 2173). The objective of these traverses was to locate showings of wollastonite, within the altered limestones, close to the gabbro body. A number of skarns were previously reported, and are shown on map 2173. These and other areas were examined for possible wollastonite and other associated mineralization.

The results of this prospecting was essentially negative, although small deposits of skarn type garnets were located along traverse 344, and traverse 6*7. Two samples (S 91-07 ft S 91-13) selected along these traverses were cut for thin section evaluation. These rock descriptions are contained in Appendix B, pages B1 to B4.

The skarns (especially those associated with sample S 91- 07) appear to warrant further investigation, as the garnet could be of some interest for use as an abrasive. These garnet bearing zones appear to be rather narrow and small in terms of hosting potential reserves. Additional prospecting and mapping should be completed to determine their dimensions more accurately.

With respect to the possibility of locating significant wollastonite mineralization in the area, no evidence of this mineral was noted in the present survey. In the opinion of Glenn Brown (page B-5) who evaluated the thin sections, it is unlikely that wollastonite occurs in the garnet bearing skarn areas.


Rocks examined during these traverses were generally of three types: White limestones with minor graphite flakes, metagabbro- coarse-fine grained rocks (close to the limestones), and skarn type rocks containing garnet and olivine. There was no evidence that wollastonite mineralization has occurs in the areas examined. The following tabulation describes the rocks observed along traverse lines:

8p Granite (Pegmatite)7 Syen i te/Metasyen i te4Mg Metaqabbro3 Limestone/marble3q Limestone w/ graohite3 Sk-Skarn (Qarnet-diopside-calcite rock)3s Calc-silicate Rock

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19

1. ASHBY TOWNSHIP RUBY MINE PROPERTY

kOCATION ACCESS

81/2-Lots 3 ft 4(Cons XVI) Take hwy. 28 east of Bancroft a NI/2-Lots 3 ft 4(Cons XV ) distance of 41 KM to Harwood

Lake and continue east on route 28 a distance of approximately 4KM to the Snake River. On the east side of this river, an old road turns south off highway 28, and leads to the Ruby Mine Area, a distance of approximately 1.5 KM.

2. ASHBY TOWNSHIP PARKHURST LAKE PROPERTY

S1/2- Lot 31 (Cons XV) Take hwv. 28 east of Bancroft a N1/2- Lot 31 (Cons XIV) distance of 25 KM to MeArthur N1/2- Lot 32 (Cons X1V) Mills then approximately 6.5 KM east,

where a secondary road leads south1990 Claim 1094217 of Hwy 28, a distance of1991 Claim 1150570 approximately 3.4 KM to

Parkhurst Lake and the property.

3. MILLBRIDGE AREA LAKE/TUDOR TOWNSHIPS

To reach this work area, take Route 62 north from Madoc (Hwy. 7), a distance of 24 KM to Mi 11 bridge. At the centre of Mi 11 bridge, take the old Hastings road northwest, a distance of 4 K.M.. At this point, the Tudor Gabbro Is In contact with metasedlmentary rocks (metalimestones). For further detail on the location of traverses see the Index Plan on drawing S 91-22.

4. GOODERHAM AREA GLAMORGAN TOWNSHIP

To reach this work area, take highway 28 east to route 507 (west of Wakefield), and turn north on route 507. Continue north some 55 K.M., where a secondary road leads to the areas examined. See the Index Plan on drawing S 91-21, for the location of the traverses.

Ralph V. Stewart December 21, 1991

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APPENDIX B INDEX PAGE

LIST OF SAMPLES USED FOR IHINJiECIION CUTS(1991 OPAP PROJECT)

LOCATION

G l amorgan Twp.

Lake Twp.

SAMPLE ft

ft ft

ft ft

91-07 91-13

91-47 91-48

REFERENCE PAGE No. (Appendix B)

B1 S. B2* B2 8, B4*

B5 SB7 S, B8X-

REFERENCE DRAW I NG js[ Q

S 91-21

S 91-22

REFERENCE . ND .

Line Grid)

3 6,7

33

Tudor Twp.

Ashby Twp,

91-15 91-20 91-25

ft 91-57 ft 91-58

Ruby 7A Ruby 8 ft 91-27

91-31 91-32 91-35 91-39

B9 8, B10*B1 1B12 8, B13*

B14 8, B16 8,

B18 B20 B22 B24 B26 B28 B30

B15*-

B19X B2U 823* B25* B27*

S 91-22

See IndexPlanS 91-22

S 91-15

B31*

18S @ 1+50S 21S 9 0+0 @ 3+80S 15S @ ION @

55

4E@ 2W0.5E2W@ B4.50W1W

File R SO l

GlennHBrown PhD.398 Huron Street, Toronto, Ontario,

Canada, MSS 2C6Office: 416/978 2975 Home 416/3519390 Fax: 416/978 3938

EMail: browngr9ecfJoronto.edu

THIN SECTION ANALYSIS

ROCK NAME: garnet gneiss SAMPLE NUMBER: 91 07

LOCALITY: Glamorgan, Ontario

ROCK DESCRIPTION

Gneissic, friable, garnet porphryoblasts (max. size Smm in diameter), micaceous lustre. (Note: There are discrepancies between the hand-specimen and thin-section for this sample.)

THIN SECTION DESCRIPTION

The garnets are equigranular and anhedral (no crystal faces). The contact between 1 garnet grains is infilled with a Fe-clay mineral and hematite. The garnets are free of inclu sions (see photograph, next page). Bands of small garnet crystals create a foliation in the rock. Although apparent mica flakes are observable in hand-specimen, no mica minerals were found in the thin-section.

Photograph DescriptionThe field of view shows abundant anhedral garnets (average size is 0.50 mm)

under transmitted light. The garnets are densely packed. The contacts between the grains are dark due to infilling by alteration products. Objective-4

MINERALS

garnetclino-pyroxeiieolivinequartzterrigenous clayand hematitesphene

75-807* HJ-15% 5- 109k.

ECONOMIC NOTES

File RSOI

GlennHBrown PhD.398 Huron Street, Toronto, Ontario,

Canada, MSS 2G6Office: 416/978 2975 Home: 416/3519390 Fax: 416/978 3938

EMaik biowiigrOecf.toronto.edu


ROCK NAME: garnet gneiss SAMPLE NUMBER: 91-13

LOCALITY: Glamorgan, Ontario

ROCK DESCRIPTION

Massive, with red banding, emerald green colour.


Garnets average 0.25 mm in diameter and .occur in interconnected clusters. The garnets have few microcrystalline inclusions (*z51b, sec photograph on next page). The abundance of garnets varies along gneissic bands.

Photographic DescriptionThe field of view shows interconnecting garnets under cross-polars. Garnets are isotropic(the velocity of light through the mineral is the same in all directions). Objectivc-2.5

MINERALS

garnet olivineclino-pyroxcne talc

25-50*36 lQ-20% 20-3^

ECONOMIC NOTES

Si-

/7-r

File RS02

Clenn R. Brown 1'hD.398 Huron Sire*!, Toronto, Ontario,

Canada, MSS 2C6Office: 416/978 2975 l lorne: 416/3519390 Fax: 416/978 3938

EMaik browngr0ccfJoronto.edu


ROCK NAME: Talc-calcite tremolitite SAMPLE NUMBER: 91-47

LOCALITY:

ROCK DESCRIPTION

Friable, white rock composed essentially by medium size tremolite crystals. The tremolite appears as randomly oriented, acicular crystals.


Granoblastic texture formed by small to medium size crystals of tremolite, calcite and talc. The crystals appear lo be randomly oriented in the hand sample but, in fact, a careful observation reveals that a former foliation was folded and truncated by a new one (photograph). The metamorphic paragenesis is indicative of a low grade (greenshist) metamorphic rock. The protolith is an impure limestone.

Photographic DescriptionThis section is mainly formed by tremolite (T) oriented in two different foliations. Calcite (Q and talc (t) are sobordinate. The photograph is taken under crossed nicols and at a magnification of 25X.

MINERALS

TremoliteCalciteTalc

7.V* 20*70Wo

ECONOMIC NOTES

- 7 flic KS02

Clenn R. Brown PhD.398 Huron Sired, Toronto, Ontario,

Canada, MSS 2G6Office: 416/978 2975 l lorne: 416/351 9390 Fax: 416/978 3938

EMail: browngr9ecf.toronlo.edu


ROCK NAME: Tremolite Marble SAMPLE NUMBER: 91-48

LOCALITY:

ROCK DESCRIPTION

Very flne grained white to grey marble. The grey patches arc due to tremolite and quartz concentrations. The rock shows strong solution with effervescence in cold diluted (l O'/k) HC1.


Very flne grained granoblastic (granular) texture. With the exception of few acicular tremolite crystals, all minerals are xenoblastic. The equilibrium metamorphic paragen esis of tremolite + calcite * quartz is indicative of a low grade metamorphic rock (grcenshist facies). The protolith (original form, prcmclamorphism) of this metamorphic rock is a slightly impure limestone.

Photograph DescriptionThis section is mainly composed of calcite with granoblastic texture as well as a few quartz (Q) and tremolite (T) crystals. The photograph was taken under crossed nicols and at a magnification of 40X.

MINERALS

CalciteTremoliteQuartz

92% 5% 3%

ECONOMIC NOTES

Jg-8

File R SO l-9

Glenn R. Brown PhD.398 Huron Street, Toronto, Ontario,

Canada, MSS 2G6Office: 416/978 2975 Home: 416/3519390 Fax: 416/978 3938

EMaik browngr9ecfJoronto.edu


ROCK NAME: calc-silicate skarn SAMPLE NUMBER: 91-15

LOCALITY: Millbridge,Ontario (^TuDcK l 1**f)

ROCK DESCRIPTION

Massive, coarse-grained, granoblastic texture, light-green colour.


High relief, low to parallel extinction angle, biaxial mineral, light pleochroism, of minor abundance^sphene. Some feldspars.are potasic. Pyroxene has an extinction angle of ^20. Amphibole (tremolite) is present as elongate grains with a low extinction angle (200).

MINERALS

augitefeldsparsamphibolecalcitesphene

40-50*** 20-30% 15-fc <05%

ECONOMIC NOTES

5

Ns \

File RS01

Clean R. Brown PhD.398 Huron Street, Toronto, Ontario,

Canada, MSS 2C*Office: 416/978 2975 l lorne: 416/351 9390 Fax: 416/978 3938

EMaik biDwngi9ecfJoronto.edu


ROCK NAME: quartzite (amphibolite facies) SAMPLE NUMBER: 91-20

LOCALITY: Millbridgc, Ontario

ROCK DESCRIPTION

Massive, fine-grained, thin veinlets, grey colour.


Micro-crystalline quartz grains average 0.03 mm in size. Amphibole has slight pleochro ism, inclined 190 extinction and pointed terminations in cross-section, carbonate is associ ated with the amphibole.

Photograph DescriptionThe field of view shows the interlocking granoblastic quartz (images with grey-tones). Theelongate mineral near the centre of the photograph is actinolite. This image is out of focus.Objective-4

MINERALS

quartz plagioclase carbonate actinolite

05* 05* 05*

ECONOMIC NOTES

File RS01

Clenn R. Brown PhD.398 Huron Sired, Toronto, Ontario,

Canada, MSS ZG6Office: 416/978 2975 l lorne: 416/3519390 Fax: 416/978 3938

EMaik bvowngf9ecf.loronlo.edu


ROCK NAME: tremolite marble SAMPLE NUMBER: 91-25

LOCALITY: Millbridge, Ontario

ROCK DESCRIPTION

Medium-grained, aligned l cm needles of tremolite, mica flakes, grey colour.


This rock is a recrystallised carbonate of amphibolite facies. It contains aligned needles of Tine isolated wollastonite crystals (see photograph on next page). The large crystals, visible in hand specimen are tremolite (a high birefringence, low-extinction angle, and amphibole cross-section).

Photograph DescriptionThe field of view shows the habit of wollasonite mineralization in this rock. The wollasto nite needles are isolated and surrounded by calcite. The extinct lath across the image is a tremolite crystal. The equigranular mineral in the background is a carbonate. Objective -4.

MINERALS

carbonate tremolite wollastonite quartz

90*3) 05-fc <05%

ECONOMIC NOTES

File RS02


Canada, MSS 2C6Office: 416/978 2975 l lorne: 416/3519390 Fax: 416/978 3938

EMail: browngr9ecf.loronlo.edu


ROCK NAME: Ttremolite marble SAMPLE NUMBER: 91-57

LOCALITY: \ J

ROCK DESCRIPTION

Massive with a light grey colour. Very fine grained with l -2 mm acicular tremolite crystals.


Very fine-grained granoblastic texture with interlocking calcite + quartz 4- epidote * tremolite 4- titanite. Most minerals are xenoblastic. Some larger tremolite crystals form idioblastic porphyroblasts. The metamorphic paragenesis is indicative of a low grade calcisilicatic (grccnshist facies) metamorphic rock. The protolith is a siliceous limestone.

Photograph DescriptionThe section shows large tremolite (T) crystals within a very fine grained matrix of calcite (C), quartz (Q) and epidote (E). The photograph is taken under crossed nicols and at a magnification of 40X.

MINERALS

CalciteQuartzEpidoteTremoliteTitanite

529b

ECONOMIC NOTES

File RS02


Canada, MSS 2C6Office: 416/978 2975 l lorne: 416/351 9390 Fax: 416/978 3938



ROCK NAME: Cafcisilicatic rock SAMPLE NUMBER: 9 1-58

LOCALITY:

ROCK DESCRIPTION

Massive with green to grey colour. Fine grain with few sub millimetre tremolite crystals.


Mainly granoblastic texture with very fine grain size. Mostly xenoblastic minerals. Titanite and tremolite form some idioblastic crystals. The metamorphic paragenesis.is indicative of low grade metamorphism (greenshisl facies). The mineralogical association with many calcisilicate minerals and almost no carbonate is suggestive of a mciassomaiic origin in a contact aureole (skamite).

Photographic DescriptionThis section shows some large tremolite (T) crystals within a very fine grained matrix of quartz (Q), biotite (B), epidote group minerals (li) and titanite (Ti). The photograph was taken under crossed nicols and at a magnification of 40X.

MINERALS

QuartzTremoliteBiotiteClinozoiziteEpidoteTitaniteFe-Ti oxide

459b \Th

Calcite Apatite

ECONOMIC NOTES

.3-1* File RS01

Clenn R. Brown PhD.398 Huron Street, Toronto, Ontario.

Canada, MSS 2G6Office 416/978 2975 Home: 416/3519390 Fax: 416/978 3938



ROCK NAME: garnet gneiss SAMPLE NUMBER: Ruby7A

LOCALITY: Ashby, Ontario

ROCK DESCRIPTION

Schistose, fine-grained with garnet porphyroblast*, speckled dark green arid light grey colour.


Subhedral garnets are included. Sillimanite is intimately associated with biotite folia tions and muscovite. The estimate inclusion content is ^Slb of the volume of the gar nets.

Photograph DescriptionSillimanite flbres (thin, light) associated with foliated biotite (thick, dark) viewed withcross-polars. Objectivc-4

MINERALS

quartzgarnetsillimanitebiotitemuscoviteplagioclaseiron oxideszircon

50* 159k 5-10* 10* 5-10*

ECONOMIC NOTES

20

File RSOI

Clenn R. Brown PhD.398 Huron Street, Toronto, Ontario,

Canada, MSS 2C6Of fice: 416/978 2975 l lorne: 416/3519390 Fax: 416/978 3938

EMaik browngi9ecf.toronto.edu


ROCK NAME: garnet gneiss SAMPLE NUMBER: Ruby 8


ROCK DESCRIPTION

Massive, dark red-black garnets averaging S mm in size, light-green granular amphibolite rich bands, black in colour.


The large volume of subhedral fractured garnets in this rock include quartz and oxides patches. The inclusion content varies but averages around 20*Jfc of the garnet. The black colour suggest a high magnesium content (pyrope garnet).

Photograph DescriptionIsotropic (opaque under cross-polars) garnet with internal inclusions of silica (grey). Sur rounding minerals are quartz and biotite.

MINERALS

garnet DO-70%quartz lG-20%plagioclase 209kbiotite 109o

ECONOMIC NOTES

22

File RSOI


Canada, MSS 2C6Office: 416/978 2975 Home: 416/351 9390 Fax: 416/978 3938

EMaik browngr9ecf.loronto.edu


ROCK NAME: fine-grained gneiss SAMPLE NUMBER: 91-27


ROCK DESCRIPTION

Schistose, fine-grained (-ci mm), visible but small garnets, speckled with red and dark green colours.


The isolated garnet crystals are included with quartz and oxides (see photograph, next page), inclusion range from S-10% of the garnets in cross-section). Garnets are mildly fractured. Fractures are infilled with a clay mineral.

Photograph DescriptionA fractured garnet viewed under transmitted light with inclusions of silica (light) and ironoxides (black). Surrounding crystals are pyroxene (with cleavage) and quartz. Objective-4

MINERALS

garnetquartzbiotiteplagioclasediopsidezirconopaques

10**,

ECONOMIC NOTES

10

RS01


Canada, MSS 2G6Office: 416/978 2975 l lorne: 416/3519390 Fax: 416/978 3938

EMail: browngr9ecf.toronto.edu

THIN SECTION ANALYSISROCK NAME: garnet gneiss SAMPLE NUMBER: 91-31


ROCK DESCRIPTION

Gneissic, large almandine garnets averaging 7 mm in size, dark green colour.


This rock of amphibolite grade with abundant almandine garnet and foliated ^ amphibole (actinolite). The garnets (see photograph, next page) are peppered with inclu sions of quartz and oxides (approx. ID-15%). The hairline fractures are infilled with alteration products. The garnets have corroded rims, commonly mineralized with biotite.

There are isolated needles of an elongate mineral with a high birefringence, paral lel extinction, and faint pleochroism. Because of the latter attribute it is likely an amphib ole, rather than sillimanite.

Photograph DescriptionGarnet porphyroblast viewed under cross-polars with silica inclusions (light grey tones).Objective-4.0

MINERALS

amphibolealmandinequartzbiotiteplagioclaseamphiboleoxides

ECONOMIC NOTES

12

File RS01

Glenn R. Brown PhD.398 Huron Street, Toronto, Ontario.

Canada, MSS 2C6Office: 416/978 2975 l lorne: 416/351 9390 Fax: 416/978 3938

EMaik biowngiOecf.loronto.edu


ROCK NAME: gneiss SAMPLE NUMBER: 91-32


ROCK DESCRIPTION

Schistose, medium-grained, light coloured acicular sillimanite, visible almandine garnet.


Foliated mica. Garnets are sparsely included and subhedral. Sillimanite occurs as fiberous sheafs (see photograph, next page). Some silliminate grains in this section are cut normal to the long axis.

Photograph DescriptionCluster of fibrous sillimanite surrounded by quartz (equidimensional) and biotite (nearcorner of the image), viewed under cross-polars. Objective-4.

MINERALS

quartzbiotitesillimanitemuscovitegarnetoxideszircon

20* Q51b 05*6

ECONOMIC NOTES

14

File RS01


Canada, MSS 2C6Office: 416/978 2975 Home: 416/3519390 Fax: 416/978 3938

EMaiL browngr9ecfJoionto.edu


ROCK NAME: garnet gneiss SAMPLE NUMBER: 91-35


ROCK DESCRIPTION

Gneissic, rust-coloured almandine present, black colour.


Equigranular quartz, foliated by biotite and muscovite. Subhedral garnets altered along fractures. Garnets are heavily included by quartz, biotite, and iron oxides (up to 30*). Fiberous sillimanite occurs as isolated bundles (sec photograph, next page).

Photograph DescriptionBundle of sillimanite fibres viewed under cross-polars. Objective 4.0.

MINERALS

quartzgarnetbiotitemuscovitesillimanite

50* 20* 10*

ECONOMIC NOTES

16

.3-3-0 File RSOI

Clean R. Brown PhD.398 Huron Street, Toronto, Ontario,

Canada, MSS 2C6Office 416/978 2975 Home: 416/3519390 Fax: 41O97B 3938

EMaik browngrOecf.toronto.edu


ROCK NAME* garnet gneiss SAMPLE NUMBER: 91.39


ROCK DESCRIPTION

Medium-grained granoblastic texture, garnet clusters with individual crystals averaging 1mm in diameter, redish-brown colour.


Foliated biotites. Isolated garnets. Garnets average 3mm in size and contain up to 20* inclusions of quatrz and iron oxides, (see photograph, next page).

Photograph DescriptionRings of iron-oxides (opaque) and silica inclusions within garnet, surrounded by quartzand biotite, viewed in transmitted light. Objective-4.

MINERALS

garnetquartzbiotitepyroxenemuscoviteiron oxideszircon

30*30*20-30*5*01*

ECONOMIC NOTES

18

APPENDIX C—INDEX PAGE 1

(Multielement Assay Analysis Parkhurst Lake Property)

SAMPLE SAMPLEDRAWING NUMBER LOCATION*** PAGE

Chemex Labs Ltd (Certificate Sheet) C1

S 91-19 ONT 91-01 (On B.L. @ C210+70)

X-Ray Assay Labs (Certificate Sheet) C3

S 91-60 (On B.L. 9 C4 S, C 510+50S)

S 91-61 (10+50S 90+30W)

S 91-62 (10+60S 90+50W)

S 91-63 (On B.L. 912+70S)

S 91-64 (12+OOS 96+30E)

S 91-65 (12+OOS 97+80E)

S 91-66 (On B.L. 915+30S)

S 91-67 (15+OOS 94+80W)

S 91-68 (16+OOS 94+20W)

S 91-69 (17+30S 93+80W)

S 91-70 (19+OOS @ 1+OOE)

Q *** All distances referred to Az 197 Baseline.

APPENDIX C—INDEX PAGE 2

(Description Of Samples Sent For Assay)

SAMPLE NUMBER SAMPLE DESCRIPTION

S 91-60 Sample taken on face of escarpment. A highly silicified quartz/mica gneiss, with 5X disseminated pyrite and some chalcopyrite.

S 91-61 Selected sample of silicified gneiss, along the westside of a diorite-granite dyke rock. Sample contains approximately 10X disseminated pyri te/chalcooyri te.

S 91-62 Sample selected 20 feet west of 91-61. A highly silicified quartz mica gneiss. Azimuth of shearing is 075*. Disseminated pyrite/chalcopyrite.

S 91-63 Sheared, silicified quartz mica gneiss with 5X disseminated pyrite. Strike of gneissosity is 060*.

S 91-64 Very fine grained, light green coloured silicified gneiss, with very fine disseminated pyrite or pyrrhotite?

S 91-65 Schistose and gossaned "friable" gneiss, with veryfine grained disseminated pyrite/chalcopyrite.

S 91-66 As above, with 10X disseminated pyrite.

S 91-67 Schistose quartz/mica gneiss, gossaned and sheared, with 5X disseminated pyrite.

S 91-68 Gossaned silicified gneiss with 8X disseminated pyrite. Sample taken along south edge of narrow pink coloured granitic dyke.

S 91-69 Dark bluish gray coloured schistose "quartzite" 0 with 10X f i ne disseminated pyrite. Shearing at 040 azimuth.

S 91-70 Similar to above, but with shearing at 075*.

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XRALC-

X-RAY ASSAY LABORATORIESA DIVISION OF SGS SUPERVISION SERVICES INC.

1885 LESLIE STREET - DON HILLS, ONTARIO N38 3J4 - CANADA TEL: (416)4*5-5755 TELEX: 06-966947 FAX: (416)445-4152

CERTIFICATE OF AJSTAJL Y SI S

REPORT X V 5 T 3.

TO: RALPH V. STEWART244 KEEWATIN STREET SOUTH OSHAWA, ONTARIO L1H 6Z8

CUSTOMER NO.

DATE SUBMITTED 5-NOV-91

40

REF. FILE 11266-O3 Total Pages 2

13 ROCKS

AU-1AT PPB NA PPM MG PPM P PPM TI PPM CR PPM MN PPM FE PPM CO PPM NI PPM CU PPM ZN PPM MO PPM AG PPM CD PPM PB PPM PT-1AT PPB

METHOD FADCP DCP DCP DCP DCP DCP DCP DCP DCP DCP DCP DCP DCP DCP DCP DCP FADCP

DETECTION LIMIT1.

100.100.10.2.2.2.

100.1. 1.

55

1.2.

10.

*** UNLESS INSTRUCTED OTHERWISE WE WILL DISCARD PULPS 90 DAYS *** AND REJECTS 30 DAYS FROM DATE OF THIS REPORT

DATE 02-DEC-91 CERTIFIED BY Jean H.L

Hater of the SGS Group (Societe Centrale de Surveillance)

XRAL 02-DEC-91 REPORT 17571 REF.FILE 11266-03 PAGE 1 OF 2

SAMPLE AU-UT PPB MA PPM KG PPH P PPM Tl PPH CR PPM FE PPM CO PPM

S 91-52* 4S 91-60"S 91-61S 91-62S 91-63

356912011

322001630018700191003280

166001750015500541050100

6995146351060478

41604940628070301130

6414819119488

75015208835111350

73700103000816006060040400

47611067522

S 91-64S 91-65S 91 -f 6S 91-67 S 91-68

S 91-69S 91-70

i

tVI

fi

S 91-26*.

617Kl

3 2

^7

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5796120409054103760

80103350

43500

6750023400171002440041500

168003250032700

278998108012702540

1150815656

12702920353028102740

314017602530

399162186196461

195109152

89438617806332280

30801900314

5550062500234003730042000

359004500039100

706871815

212330

AU-1AT PP8 - ASSAY PERFORMED ON 30 GRAM ALIQUOT

X-RAY ASSAY LABORATORES 1885 Lesie Street Don Ms Ontario U3B 3J4 (4*4445-5755 Fax (416)445-4152 Th 06-986947Hater of the SCS Group (Societe Centrale de Surveillance)

XRAL02-DEC-91 REPORT 17571 REF.FUE 11266-03 PAGE Z Of 2

SAMPLE Nl PPN

S 91 52* 68S 91 60S 91-61S 91-62S 91-63

8499

tx 61Y 19

CU PPN

9.998.3

280.242.332.

ZN PPN

96.8168.136.268.278.

NO PPN

71116175

AC PPH

•e.5•*. 5•c.5•*.51.5

CD PPH

^•O

122

PB PPN

312227313

PT-1AT PPB

•OO•OO

10OOOO

S 91-64S 91-65'S 91-66 S 91-67 S 91-68

S 91-69S 91 -70^ S 91-26-1

4 723. 76P 15'N *

90

9867

"r 39

13.5544.63.548.388.6

64.952.938.3

484.286.47.7

114.178.

147.262.62.5

6988824

94606

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•c.5•c.5

211

•O3

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PT-1AT PPB - ASSAY PERFORNED ON 30 GRAN ALIQUOT

X-RAY ASSAY LABORATORES 1885 Lesfe Street Don Ms Ontario M3B 3J4 (416K45-5765 Fax (416)445-462 Tlx 06-986947Nnriher of the SGS Group (Socilt* G4n6rale de Surveillance)

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PATENTED LAND

CROWN LAND SALE

Limerick Twp.(M. 114)

Z4 X \23 32 21 20 19 18 17 16 15 14 13 12 I29 28 27 26

XVIII

XIV

u

(&O y IT

Madoc Twp.(M.120)

THE TOWNSHIP OF

TUDORCOUNTY OF

HASTINGS

MINING DIVISION

SCALD l- INCH'40 CHAINS LEGEND

10 C ATE D LAND 'llCINSe OF OCCUPATION

MINING RIGHTS ONLY SURFACE RIGHTS ONLY ROADSIMPROVED ROADS KING'S H o H WAYS RAILWAYS POWER LINES MARSH OR MUSKEGMINES CANCELLED TRAILS PATENTED S R O

CS©

locL O.

MRO. SRO

-- o ---

* '.J

Kc

NOTES This Mop Is Not To Be UsedFOR SURVEY PURPOSES.

Lot Anr! Concess on Lines Shown Hereon /-re Projected F'Om The Best Informations AvoiloMi. But Their True Position Is Ijot Guorunti. .J For Offic'ol Survey Purposes Consul! In'; Original Survey Plons And F'^ld Notes Of Records In The Ministr} of Natjroi fi

400' ûrface rights reservation along the shcrea of all lakes and rivers

INMIMMAIION IMAI Al'l'l Ali , ON TMI 1 , MAC MA', llf f N COMI'II l H l IK IM VAHlOIJfi SOI IMI l '. AND A( r IIIIACY IS NOI ( .IIAMAN 1 l Ml I MO 1 ,l W l 1 MINI . K i MAKI MIN INI . l l AIM ,l l' MJI l i l l )N Mil I WllM IMI MININ( ,

l i HID! H MINI'.l HY l li f J i ) 11 l M l M N D l V l l O l' Ml l i l AND MINI '. l OH AD DI l H INAI INI l iMMA! ION

IN IMI MAIN', 01 IMI l AND 1 . Md )WN Ml Ml l IN

DATE OF ISSUE

MAR - 6 1991SOUTHERN ONTARIO

MINING DIVISION

PLAN NO.-M. 156()\ l \KI()

MINISTRY OF NATURAL RESOURCESSURVEYS AND MAPPING BRANCH

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109 Ac

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98

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Marmora Tp. M. 122

220

THE TOWNSHIP OF

LAKECOUNTY OF

HASTINGSSOUTHERN ONTARIOMINING DIVISION

SCALE I-INCH*40CHAINS

LEGENDPATENTED LANDCROWN LAND SALELEASESLOCATED LANDLICENSE OF OCCUPATIONMINING RIGHTS ONLYSURFACE RIGHTS ONLY

ROADS KINO'S HIGHWAYS RAILWAYS POWER LINES MARSH OR MUSKEG MINES CANCELLED PATENT, SURFACE RIGHTS ONLY

*

NOTES [This Map Is Not To Be Used 1 ÔRÛRVE^ PURPOSES

400' surface rights reservation along the shorts of all lakes and rivers

Flooded Lands shown thus:

Lot And Concession Lines shown hereon ore projected from the best information available, but their true position is not guaranteed For official survey purposes, consult the original survey plant and fltldnotes of record in the Dtpt. of Lands a. Forests.

8 GRAVEL

UUAOHY P ERMIT

TMt INMWMAHON IHAI Al'l'l AH 1 . ON HIT. MAI' HA', (KIN r OMI'II l O l MOM VARIOUS SOUH( l '. AND A( ( UHA( Y l'. NO! (,DAMAN lllli l MO',1 WI'.MIN(. 10 MAM MIN IN(. l l AIM', '.MODI D ( ON '.DI l WllM 1HI MININC. Ml l OKI II M MINI'.IMY Ol NOM l Ml MN Ut VI l Ol' Ml Nl AND MINI :. l ( 1M AD DIIIONAI INFOMMATION ON IMI '.lATUf. 01 1MI l AND', SHOWN Ml Ml ON

DATE OF ISSUE

MAR - 6 1991SOUTHERN ONTARIO

MINING DIVISION

PLAN NO.-M. 110ONTARIO

MINISTRY OF NATURAL RESOURCESSURVEYS AND MAPPING BRANCH

0 TWP.c

c/i oo CD

CD

Oo: o

H

cr

CD ic/i or cr

o innn

Dudley Twp.Dysart Twp.Q H ^ [j 13 14 15 16 17 18 19)1201 2J 22 23 24 25 26 27 28 29 30 31 32 33 34

Galway22 23 24 25 27 28 29

Cavendish Twp.

LEGENDHIGHWAY AND ROUTF No

OTHER ROADSTRAILS —--

SURVEYED LINESTOWNSHIPS BASb LINES ETC -^LOTS MINING Pi AIMS PAHCHS H( ——

UNSURVEYED LINESLOTLINFS ———

PARCEL BOUNDARYMINING CLAIMS ETC.

RAILWAY AND RK,UT Oh WAY -i——-~ UTILITY LINtS -o——

NON PFRFNNIAl STM AM — -

FLOOOINI, C)R f l OOpiNCi RIGHTS -^^

SUBDIVISION ORfOMPOSITI PI AN """"

RESERVAI IONS *W™

ORlbiNAi SHOHt i iNf

MARSH OH MUSKKi *

MINES

TRAVERSE MONUMENT LAND ACQUISITION___________[A]

L 6 "'J.'-

DISPOSITION OF CROWN LANDS

TYPE OF DOCUMENT SYMBOL

PATENT SuHf-AC E Si MININC, HK.HTS 0

SURI ACI HK.HTS ONt Y C

MININC, MIGHTS ONl Y Q

LEASE SUM Act 8, MININC. Hid HIS B

SUHI ACI HIC.H1SONI Y B

MININC, HK.HTS ON! Y Q

LlCFNCrf Of O(.C UPAT ION T

ORDER IN COUN( H OC

RES! RVATION (J)

CANCEL ltO ®

SAND fl. ClHAVi l (*)

NOT t MININi, HI IITS IN PAHf t l S PAK-NMDPHIOH IDMAV b VtitMl IN DHli.lNAl I'ATlNMt b' iMt POBllC

LANDS Ar l H S (l 19'0 CHAP JBO Sit b3 SHUSH 1

SCALE 1 INCH 40 CHAINS

•000

AREAS WITHDRAWN FROM DISPOSITION

M.R.O. - MINING RIGHTS ONLY

8.R.O. -SURFACE RIGHTS ONLY

.* S. - MINING AND SURFACE RIGHTS

OrdwNo OM*

3CT '7l

OtapodttOfi

s a o

Fil*

RcsesvE 'OR P'.BI ic use

Q) M is R PESt R 't

'OR Pu8 1C USC

RESERVE TOR PI PUC i SE

M NR RESERVE

ste s* (4) WITHDRAWN FROM 3TAKM9

' 7 ^ J t

m 10

l 4 c S o

i, .t-6,a

SAND S GRAVEL

QUARRY PERMIT

l t II irjl c IHMAI l' )h l MAI M'l-t AH', ( i ti I HI' MAI

HA HI l N ' l IMI'II l l l 1 ((i iM VAHIi li l 1 ,( H IHI l

A l l l IIIAI r l rji l li' i r/ ' i i : i HI i

.'•loHINU lU blAM MIN ING CLAIMS SHOULD CONSULT WITH THE MINING

l MINISTRY OF NORTHERN DEVFIOI' Ml NI AND MINFS f OH A|i

INf OMMAIIf )N .lAIir, DI IHI

AMP' '.HI iwrj HI MI i m

DATE OF ISSUE

MAR 2 2 1991SOUTHERN ONTARIO

MINING DIVISION

TOWNSHIP

GLAMORGANMMR ADMINISTRATIVE DISTRICT

MINDENMINING DIVISION

SOUTHERN ONTARIOLAND TITUS/ REGISTRY DIVISION

HALIBURTON

Ministry of Ministry ofNatural Northern DevelopmentResources and Mines

34 35

Anstruther Twp.

Ontario

DiliFEBRUARY 1987

Number

G-1288

31F03NWOQ04 OP91-33B ASHBY

0\ r'

230 RES. GEO. TWEED .N.R. DIST. MINDEN

c o10I^BV

lo

H

o :o o

L- O

00GO 10•••M

l

O

•••"•-. l ap'•f. f.

AREA 2

LEGEND

joy. GARNFT Contour (Visual estimate)

'•-•\ \L K \ 20V, GARNET Contour( " " j

t30V, GARNCT Contour

Surface Elevation Contour(Approximat0

X1\AREA3

RUBY GARNET PROPERTYt ASHBY TOWNSHIP. ONTARIO)

gONTQUR. PLAN of VisualVt-Gorne ts (from surface mapping data)

Drown By - RV. Stewart

INDEX PLAN

PARKHURST

/•/t4t*fl-f C-j^lC- 4®*t""'rl

LEGEND

PINK LEUCOGRANITE

QUARTZ/MICA GNEISS ( Biotite. QuarU, Plagioclase)

L 2P ] GARNET GNEISS 7 PAR AGNEISS (Biotite, Ojuartj; Feldspar w/Trace-10% Garnets)

QUARTZITIC GNEISS

GNEISSOSITY (Direction ft Dip)

INTERPRETED GEOLOGICAL CONTACT

ROCK OUTCROPS EXAMINED

TOPOGRAPHY (Direction S, Slope)

TRAVERSE LINE

Q.V. QUARTZ VEINS

,.!!,,'! MINOR ESCARPMENT

rop61-338 ASHBY UAKEIllllllll 250

\

GEOLOGICAL PLAN PARKHURST LAKE PROPERTY

( ASHBY TWP. )

-- EAST SHEET—

Drawn By RV Stewart SCALE l" 200' DWG. S 91-20

LEG

EN

D

8 *

PIN

K

LEU

CO

GR

AN

ITE

(Bath

olith

or D

ykes)

QU

AR

TZ / M/C

A G

NE

ISS

(Biotite, Q

uartz. Plag.oclase)

2pe l

SIM

ILAR

to

2p except

10V. to 20V.

Garnet

SIM

ILAR

to

2 p excepttlO

V. S

illimanite

and tlO

V. G

arnet

GN

EIS

SO

SIT

Y

(Dire

ctio

n i

Dip)

INT

ER

PR

ET

ED

G

EO

LOG

ICA

L C

ON

TAC

T

INT

ER

PR

ET

ED

FA

ULT

RO

CK

OU

TCR

OPS

EX

AM

INE

DPAR

KHU

RST

LAK

SLO

PIN

G

TOP

OG

RA

PH

Y

(Direction

81 S

lope)

CLA

IM

BO

UN

DA

RY

GA

RN

ET

B

EA

RIN

G

SA

MP

LE

AN

OM

ALO

US

S

AM

PLE

(Gold)

u\

AN

OM

ALO

US

S

AM

PLE

(C

ooper)

AN

OM

ALO

US

S

AM

PLE

( N

ickel

AN

OM

ALO

US

SA

MP

LE (2

mc)

t .

. , - -

ES

CA

RP

ME

NT

'99:

1990 8,

1991

Mcpptrg

Areas

**Lrfi'frS

7\ '

\ \

CLA

IM115057

l/ \ \

S^

'UjA

RN

ET/

^ \N

siLL

IMA

fflTE

\ \V.

ZO

Nff

lOY L}—

— (*4

t

3-OOE ,

^J*

L--J

*? i^

z. '

—i-

i# :??7 ^ ;v.

-- ^ i ' i \-; -V. -i

: ,;

^ \*-

LEGEND

ITiH. PINK LEUCOCRATIC GRANITE or BIOTITE GRANrTE GNEISS

J QUARTZ MICA GNEISS! BIOT l T E. QUARTZ. MUSCOVITE PLAGIOCLASE)

O1^CM

2pm

[Tp GARNET GNEISS/PA RAGNEISS ( Trace-10V. Garnet) Uq QUARTZITIC GNEISS w/ Trace -10 V. Garnet

SIMILIAR TO 2pX2q (Above) but with 10V.-30V. Garnet

GARNET X MUSCOVITE GNEISS wX 0-10V.Garnets

l ? P ern J SIMILAR TO 2pm Above but w/ 10V.-30V. Garnet

GNEISSOSITY (Direction ^ Dip)

(S) Sillimanite

STRIKE t DIP OF TOPOGRAPHY

INTERPRETED GARNET ENRICHMENT ZONES

GEOLOGICAL PLAN RUBY GARNET PROPERTY

(ASHBY TWP. ONTARIO)

— SOUTH SHEET—

Drawn By RV Stewart SCALE'.1*200 Dwg-. S 9H8

LEGENDNDEX PLAN

60 J PINK LEUCOCRATIC GRANITEgr BIOTITE GR AN l TE GNEISS

QUARTZ MICA GNEISS(BIOTI TE, QUARTZ, MUSCOVITE, PLAGIOCLASE)RUBY PROPERTY

Two2fM3ARNET GNEISS/PARAGNEISS { Trace-10% Garnet)

I2q QUARTZITIC GNEISS w/ Trace-lOV, Garnet

SIMILIAR TO 2pX2q(Above) but with 10*-30V. Garnet

GARNET/ MUSCOVITE GNEISS w/ O H (ft Garnets

SIMILIAR TO 2pm Above but w/ 10^-3OV. Garnet

*H Hemitite (hemitization)

(L) (S) (L) Garnet size 1/16-1/2". (S) Garnet size 1/16-1/8

GNEISSOSITY (Direction 8, Dip)

INTERPRETED GEOLOGICAL CONTACT (Garnet Enriched Zone)

OUTCROP w/ T2Q*/. Garnet

OLD ROAD

O O B ROKEN ROCK PILE

STRIKE li DIP OF TOPOGRAPHY

BASELINE w/ PICKETS SPACED ON 150 CENTRES

SAMPLE PROCESSED

ROCK SAMPLE SELECTEDM991 )

mrniri Jtoi-iBtriQ1 ~31991 Mapping Dwg S 91-15

"i - v r ^^\ x

li i H . i i l i l l i l l H li*

C ^•J -9*OON

,'VT v2/ l/i.

O.

Claim 1094220^^L? ~" ~ *"v Claim

T fX-• a ^ ** ^ l

'A,- f \"M \\\

^ ,Tf/.^fi

GEOLOGICAL PLAN FT PROPFRTY

(ASHBY TOWNSHIP. ONTARIO)

-NORTH SHEET- SHOWING 1990 fc 1991 MAPPING DATA

Drawn By : R.V Stewart' SCALS '.1-200 Dwg S 91-15

NDEX PI AN^"^^^^"^^^"^^*^^^^™"^^Sl^^m^^^3^^S^^Ê^^S^î

( Scale; r'^1/2 Mile)

X

TRAVERSE 1 '

l

-s

TRAVERSE 2

TRAVERSE 5 N

N

TRAVERSE AA

NTRAVERSE 4 B

\

TRAVERSE 3

\\\

\

"~2S

!20S

l S 'i'

' 3 0S

N

LEGEND*

j ALTERED GABBRO ( Dykes/Sills )

j 7d ) GABBRO

L 7* l DIORITE

GRANi'E/SYENITE (Intrusive Rocks)

L g [ LIMESTONE/MARBLE (Un differentiated)

? *5a j LIMESTONE (Graphitic )

[ 5 b j DOLOMITE

M APBLE ( Miccceous/Phloqopi t e )

TREMOLITIC MARBLE

SK [ FELSfC TACTITE

( 5 6/9 l CALC X SILICATE SK ARN ( w/ Pyroxenes end/orAmphiboles )

Qjartzitic CA LC l S I LI CATE ROCK w/or w.out Mica

TRAVERSE LINE

rNEiSSOS(TYXSCHlS T OSlTY / L INEATION

1-12 SAMPLE LOCATION

SMALL OUTCROP

ESCARPMENT

TOPOGRAPHICAL D'RECTION AND SLOPE

CRAG FOLDING

py-s PYR.TE v S ULPHIDES

CllARTZ VEINS

Tc- TALC Y

" OLTCROP AREA EXAMINED

31FQ3MW00040P91-335 ASHBY LAKE 290

GEOLOGICAL PLAN —— MILLBRIDGE AREA—

l LAKE and TUDOR TWPS.)

SHOWING GEOLOGICAL TRAVERSE LINES

Drawn By: RV Stewart SCALE: 1=200 Dwg S 91-22

LOCATION PLAN

TRAVERSE 1TRAVERSE 3 8,

Glamorgan Twp

* Az 270'

NDEX PLAN(SCALE MILE)

— APPROXIMATE SCALE—

Mlapprox4

TRAVERSE 2 TRAVERSE

L 8P l ORANITE ( Pegmatite)

7 l SYENITE/ Meta-Syemte

[ META-GABBRO

LIMESTONE / M ARBLE

j LIMESTONE (W/Oraphite and/or Mica)

Sh J SKARN ( Gannet-Diopsi de-Calcite Rock)TRAVERSE 6*7f 3s i Calc-Silicate Rock

Gneissosity/ Schistosity (Direction 4 Dtp)

TOPOGRAPHY (Direction ft Slope)

XS91-2 ROCK SAMPLE COLLECTED

OLD TRENCHES

TRAVERSE (w/ Direction

OUTCROPS EXAMINED

TRAVERSE 1A

GEOLOGICAL PLAN GOODERHAM AREA

(GLAMORGAN TWP)

SHOWING GEOLOGICAL TRAVERSE UNES

Drown By: RV Stewart SCALE :iV200' l Dwq-S 91-21 J**.S9t l *

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