DD RPT 41 CUNNINGHAM - Ontario...DIAMOND DRILL CORE LOG Sheet No. -OF. Project No. 206 Hole No. TOW-91- T Surface DIP AT COLLAR-45' BEARING - 090" Test Depth 60m Dip-44.5" Magnetic

41010NE9109 41 CUNNINGHAM 010

DIAMOND DRILUNG

TWP/AREA Cunningham Twp REPORT NO. 4 1

WORK PERFORMED FOR: Grand America Minerals Ltd.

RECORDED HOLDER- SAME AÂBOVE : OTHER[ J

CLAIM NO. HOLE NO. FOOTAGE

1030189

1030188

1030182

1030181

P1030183/ 1030182

P1030180

P1030184/ P1030183

P1030182

P1030183

P1030179/ P1030180

TOW-91-1

TOW-91-2

TOW-91-3

TOW-91-4

TOW-91-5

TOW-91 -5X

TOW-91-6

TOW-91-7

TOW-91-8

TOW-91-9

221m

218m

209m

149m

197m

317m

197m

182m

290m

200m

Nov 91

Nov391

Nov 91

Nov 91

Nov 91

Sept 92

Dec 91

Dec 91

Dec 91

Dec 91

(D

d)

d)

d)

d )

d)

(D

(1)

d)

(1)

NOTES:

1. Report of work #W9360.00052

FILED June 16/93

4Aa0iai^ j

l 1030102 j

LOCATION MAP

Scale

Q WORK DONE ON

WORK RECORDED ON

OUTLINE OF CONTIGUOUS

CLAIM GROUP

LATITUDE - 12+50S

DEPARTURE

ELEVATION .

0+55W

NORANDA EXPLORATION COMPANY LIMITED

DIAMOND DRILL CORE LOGSheet No. -OF.

Project No. 206 Hole No. TOW-91- T

Surface

DIP AT COLLAR-45'

BEARING -090"

Test Depth

60m

Dip

-44.5"

Magnetic Bearing

Corrected Bearing Properly Tower

120m -44'

TOTAL DEPTH 221 .Om CORE SIZE BQ

180m -45"NTS..

CORE STORAGE Aunor Mjnesite - Timmins

REMARKS ———-^———--—---————-----———--——^——

410/10 TWP Cunningham claim No 1030189

Nov. 18/91 ^m[....^ Nov. 20/91

Contractor

Logged by -

Bradley Bros. Timmins

R, Pressacco

Depth Si Lithology Description (colour, grain size, texture, structure, etc.) Alteration Mineralization Remarks

0.0-7.0

7.0-23.58

FELSIC AGGLOMERATE -FLOW ( 7)

Casing. All casing recovered on termination of hole.

Interval consists of typical felsic agglo merate 7-14.10m and a plagioclase-quartz porphyritic rhyolite 19.38-23.58. Agglo merate is composed of more of less aphanitic light grey rhyolite fragments which are matiix- supported in a fine-grained chlorite-dominated matrix. Chlorite is a medium grass-green ir colour, and the contacts between rhyolite fragments and matrix are diffuse, l-3% anhedral garnets are disseminated throughout the matrix and are up to 2-3mm in size. Crude banding apparent on a Local scale.

The rhyolite (19.38-23.58) is medium grey in colour, very hard and non-magnetic. 10-] 5*! anhedral to euhedral plagioclase phenocrystE are matrix-supported. 1-3t anhedral quartz phenocrysts are disseminated throughout. Trace calcite-filled hairline fractures.

14.10-19.38 Sedimentary interval containing moderately to well bedded chert-magnetite- argillite. Generally chert-magnetite dominzted and chlorite-bearing to 15.5m, then changing to argillite-greywacke to 19.38. Load casts observed at 18.86 suggest stratigraphic tops are downhole.

l-3% disseminated Py-(Po) throughout interval.

l-3t disseminated St stringer pyrite. Pyrite stringers typic have bi-lateral silica alteration haloes up t 10mm into wallrocks.

Semi-massive, weakly bedded Po-Py 14.10-14.

lly

52.


DIAMOND DRILL CORE LOG Project No. .

Property

2Q6

Sheet No.

Hole No. -

-OF.

TOW-9l-i

Depth ft Lithology Description (colour, grain size, texture, structure, etc.) Alteration Mineralization Remarks

23.58-28.31

DIORITE DYKE

28.31-8C.08

CLASTIC SEDIMENT

Core angle: 650 tea at 18.5. Bedding.

Colour light green-grey, very hard, non magnetic. Massive very fine grained texture Occasional small patches (O.Sxlcm) of rhyolite observed. It randomly oriented quartz-calcite veinlets. Sharp, irregular upper contact.

Colour variable from medium green to black. Hard to very hard. Section is dominated by sub-equal amount of argillite and coarse greywacke. Approximately ao-25% of section composed of a mixed chert-chlorite assem blage. Chert fragments to 5-7cm are supported in a chloritic matrix. Greywacke beds are typically massive in texture and range in thickness to 1m. Overall, section is moderately well-bedded. Lower contact is somewhat gradational, with chert graduallbecoming more abundant, subjectively.

Lower contact chose i

Core Angle: 65 tea at 43.50. Bedding.

48.0-56.0 Chemical Sediment: Colour variable from light grey to dark gree i, depending on chlorite content, hardness variable, magnetism variable depending on pyrrhotite-magnetite abundance. Generally moderately bedded with alternating sections of chert and chlorite-rich material to 10-15 :m thick. Occasional interbeds of argillite- greywacke throughout, but section contains common amount of chert. Trace guartz-calcit i veinlets. Occasional interbedded magnetite.

Trace to It disseminated Po.

3-5t pyrrhotite occurs mostly as scattered patches of syngenetic sulphide, and weakly bedded. Trace to It pyrite. 31 disseminate to crudely bedded sphalerite observed in in the 46.65-47.07 interval. Sphalerite colour is red-brown to yellow-brown.

Pyrrhotite is common, (48-56) overall roughly St, and occurs as beds of smsv pyrrhotite to 7-10cm, bands of heavy disseminations to 10cm, and isolated patches oi syngenetic Po. No appa rent preference for chart or chlorite is observed, with Po occurring equally in bc th.

NORANDA EXPLORATION COMPANY UMITED

DIAMOND DRILL CORE LOG Project No.

Property —

Sheet No.

Hole No. -

-OF.

TOW-91-1

TOWERDepth 81 Lithology Description (colour, grain size, texture, structure, etc,) Alteration Mineralization fie marks

86.08-131.78

CHEMICAL SEDIMENT (CHERT)

56.75-57.56 Feldspar porphyry dyke. Colour medium grey, very hard. Abundant (30t) anhedral to subhedral plagioclase phenocryst are set in an aphanitic matrix. Sharp, but irregular contacts.

The section below 56.0 to roughly 86.0 isdominated by clastic sediments and containsrare to minor amounts of chert beds. Clastisediments are volumetrically dominated bymassive greywacke beds.80.51-80.96 Feldspar porphyry dyke. Similarto above.Core Angle: 600 tea at 81.8, bedding.

Colour variable from white to black, very hard, variably magnetic, due chiefly to pyrrhotite content. Section is dominated by weakly bedded to brecciated chert, with less than 10t interbedded chloritic material. This chloritic material may represent a chlorite-altered sediment. Chloritic bands appear to be conformable and not due to alteration. Rare amounts or argillite (weakly graphitic) are interbedded amongst the cherts (eg. 102.6m).

Core Angle: 6O0 to c.a. at 106.8m. Bedding.

Some alteration possible in chert breccia sections. An assemblage of talc(?)-silica (?)- sericite 9?) forms a a veinlet/stockwork around/defining some chert fragments. Some replacement of dark chert by a lighter silica (?) material observed.

Sulphides are common in the 56-85 interval, being roughly 7% in overall abundance. Sulphides dominated by pyrrhotite (95) with the remainder consistirg of py-cpy-sph, in that order. Sulphides occux mostly as beds, bands of heavy diss to smsv sulphides, and patches/ rods scattered through out. Chalcopyrite is relatively common, occurring in less than It abundance, and shows strong affinity to Po. Cpy occurs as diss and stringer. Trace sphalerite observed at 69.0.

Pyrrhotite is abundant, above 98.0. Overall abundance possibly lot, locally becoming smsv-msv (eg. 91.65 to 92.49). Mostly, the po occurs as stringers/veinlets/ patches around chert fragments and within larger chert sections.

HEM conductor probably due to smsv po section at 91.65-92.49.


DIAMOND DRILL CORE LOG Project No, .

Propertv206

Sheet No.

Hole No —

nr- OF e-


The talc-silica- sericite assemblage gradually decreases in intensity downhole and is virtually absent at 101.0.

Below 107.0, pyrrhotite is virtually absent, being less than l-3t in abundance. Magnetite increases in abundance and occurs as breccia matrix and rare beds.

112.60-114.96 Feldspar porphyry dyke. Colour dark grey, very hard. Characterized by abundant (35-40t) anhedral to subhedral plagioclase phenocrysts set in an aphanitic matrix. Indistinct upper and lower contacts

The cherts became more massive in texture in the 110-130m section. Weakly bedded in places with tuffaceous-looking material defining bedding planes. Occasional short sections (30-60cm) of chert breccia. Occasional bands of chloritic material are present and give the appearance of being interbedded with the cherts. Several load casts observed through 123.6 indicate stratigraphic tops are towards top of hole. 11 thin (1mm) guartz-calcite fracture- fillings.

103.08-106.10 Chlorite-alteration/ enrichment. Dark green chlorite occurs as stockworks and fracture-fillings. Heaviest chlorite in a 20cm section at 105.0. lot po with traces cpy accompany chlorite alteration.

Some bands bands/beds of smsv-msv po are present, but are not very abundant. The 91.65-92.49m section is smsv-msv po. and contains it chalco pyrite with rare sphalerite observed. Section is weakly bedded to massive texture.

102.64-103.08Argillite section contains heavy disseminated to bedded sulphides (30*). Sulphides composed of po-py-sph- cpy in that order. Overall, less than It combined sph-cpy.

Pyrrhotite abundance roughly It in the 110-130m interval. Po occurring mostly as isolated grains and patches disseminated throughout the core. Trace pyrite in places Rare chalcopyrite occurrs with pyrrhotite.

NORANOA EXPLORATION COMPANY LIMITED


Property —

Sheet No.

Hole No..

.OF.

TOW-91-1

TOWKRDepth St Lithology Description (colour, grain size, texture, structure, etc.) Alteration Mineralization Remarks

131.78-135.2

FELDSPAR PORPHYRY

135.26-150.4

GABBRO

150.45-221.0

FELDSPAR PORPHYRY

Colour medium grey, very hard. Abundant (2st) anhedral to subhedral plagioclase phenocrysts 131.78-134.0, becoming very fine grained to fine grained below. 7-10t quartz veinlets (2mm) possess a bilateral bleached halo. 20cm of possible fault gouge (healed) at 134.12m.

Colour medium to dark green-grey, moderately hard, non-magnetic. Massive, fine grained porphyritic texture with lS-20% very fine anhedral to euhedral plagioclase phenocrysts set in an aphanitic chloritic matrix. 5t quartz-rich veinlets to l-3mm wide.

Similar to above. Colour medium grey, very hard. Typically contains a strongly developed massive porphyrytic texture with plagioclase, quartz, and biotite (?) phenocrysts set in an aphanitic siliceous matrix. Plagioclase phenocrysts are anhedral to euhedral, and zoning in euhedral grains is easily visible. Zoned plagioclase suggestive of subvolcanic intrusive (?). Some sections of interval ar less porphyritic. Trace to it quartz veinle

171.95-173.14 Diabase dyke. Colour dark gr to black, moderately hard, non-magnetic. Ve: fine grained to aphanitic, massive texture. It randomly oriented quartz-calcite veinlets Both upper S lower contacts are at a high angle tea.


DIAMOND DRILL CORE LOG Project No. 2 06

Property _____TOWER

Sheet No. _____fi— OF ——i.

Hole No ______T0*-91-l

Depth 81 Lithology Description (colour, grain size, texture, structure, etc.) Alteration Mineralization Remarks

221.0

Porphyry unit gradually becomes less porphyritic and finer grained down the hole, starting roughly at 195.0. Occasional sections of khaki-coloured sericitic alteration is usually accompanied by an increase in quartz-calcite veinlet abundance

END OF HOLE

LATITUDE 9+OOS

DEPARTURE 4+15W

ELEVATION ——Surface


DIAMOND DRILL CORE LOGProject No, 206 Hole No.

Sheet No. '

TOW-91-2

OF.

DIP AT COLLAR -45* BEARING 090"

Test Depth60m

Dip

-45.5"

Magnetic Bearing

Corrected Bearing Property Tower

120m -46"180m -46" NTS.. 410/10 1030188

TOTAL DEPTH 21 8 . Om CORE SIZE BQ

CORE STORAGE Aunor Mjnesite - Timmins

REMARKS ——————————————————————————————

Cunningham C)liJmNo

comp,e.ed ÔV. 23/91Date started ——

contractor Bradley Bros. - Timmins

Logged by R. Pressacco


0.0-4.0

4.0-30.21

RHYOLITE FLOW

30.21-62.40

CLASTIC SEDIMENTS (ARGILLITE/ QREYWACKES)

Casing. All casing recovered on termin ation of hole.

Colour variable from medium grey to medium green, non-magnetic, very hard. Overall, massive, very fine grained texture with some porphyritic sections spread throughout interval. Plagioclase phenocrysts rarely exceed S-7% in abundance and are anhedral to subhedral. Maximum grain size on order of 2-3mm. Where chlorite alteration increases, phenocrysts gradually decrease in size and become more rounded. Trace to It garnets(?) occur with chlorite alteration. X-3% quartz veinlets and hairline fractures. Some irregular patches/sections present (eg. 10.4-10.65m).

Colour variable from medium grey to dark green, depending on chlorite abundance, moderately hard, variably magnetic depending chiefly on pyrrhotite distributior Generally massive to weakly bedded texture, with some short sections of argillite exhibiting very well defined bedding. Unit is a mixture of greywacke, arg. S chloritic material which is likely a chl-rich sediment

Overall moderate chlorite alteration, with some stronger sections being on the order of 1.5-2.On in length. Chlorite occurs throughout interval as tiny patches interstitial to silica matrix and phenocrysts, where chlorite becomes heavier, matrix and phenocrysts disappear Chlorite alt'n becomes stronger and over wider widths down hole.

Trace to It pyrite occurs mostly as disseminated grains and small patches (5mm). Most of the pyrite occurs within approx. 6m of lower contact.

Overall sulphide abundance roughly l-3t, occurring mostly as discrete bands or beds. Some stringer and disse minated sulphides present to minor degree.



Property

206

Sheet No. ———2 OF g

Hole No TOW-ftl-02


Trace quartz-filled veinlets and hairline fractures. Magnetite is mostly absent, but one 2cm bed is observed at 31.70m.

Sulphides are dominated by pyrrhotite with some pyrite (10t) and rare chalcopyrite also present. Chalcopyrite occurs in close asso ciation with pyrrhotite

35.83-37.43 and 41.00-42.54 Diorite Dikes. Colour light to medium grey, very hard, non-magnetic. Generally massive very fine grained texture, with some sections being weakly porphyritic. Trace very fine grained disseminated pyrite in upper dike. All contacts are at a very high angle to c.a.

Core Angle: 800 to c.a. at 37.75m. Bedding.

Unit becomes more chlorite-rich through 47m to roughly 62.5m. Argillite and greywacke are virtually absent, with the interval being dominated by chloritic sediment. Chert beds begin to appear in an inter mittent fashion below 47m and can be up to 50cm thick. Some thin felsic tuffs (or sericitic alteration) are present in the 50-53 metre interval.

Pyrrhotite abundance gradually increases downhole from It at 53m to 7t at 62m. Pyrrhotite occurs mostly as thin beds (3-5cm) and as diss eminations , and stringers to a lesser degree. No chalco pyrite observed.


DIAMOND DRILL CORE LOG Project No. 2 06

Property

Sheet No. 3 OF ^^L.

Hole No TOW-91-02


62.40-64.13

MASSIVE SULPHIDES

64.13-128.32

CHEMICAL SEDIMENT (CHERT- MAGNETITE IRON FORMATION)

Section is composed of virtually massive, bedded pyrrhotite with ID-15% patchy and disseminated fine to medium grained pyrite present from 62.4-62.9 metres. Some fragments/patches of chloritic sediments account for S-7% of section. Some larger fragments contain pervasive disseminated, very fine grained po.

Trace to H chalcopyrite occurs mostly as disseminated, small patches (l-3mm), and occasionally as mm-scale beds. Diffuse upper and lower contacts.


Colour variable from white to medium green to black, very hard, variably magnetic depending on magnetite-pyrrhotite abundance and distribution. Moderate to well bedded texture with bed thickness ranging from mm-scale to 50-75cm. Interval consists mostly of light grey to white and light green cherts, but contains 10-151 interbedded magnetite and 20-251 chloritic sediments. Trace randomly oriented quartz- filled veinlets to 3-5mm thick.


HEM conductor: 62.4-64.1 metres.

Sulphide mineralizatior is quite abundant in the 64-80m interval. Overall, roughly 1C^ sulphides occur mostly as district beds or bands of heavy disseminations. Trace amounts of stringer sulphide present. Sulphide mineralogy is domin ated by pyrrhotite, but l-3t pyrite as disseminated grains and patches is also present.


DIAMOND DRILL CORE LOG Project No. 206

Sheet No. 4 np 6

Hole No TOW-91-02

Property Tower

Depth fe Lithology Description (colour, grain size, texture, structure, etc.) Alteration Mineralization Remarks

Chert abundance gradually decreases below roughly 84.5m, with clastic sediments becoming the dominant rock-type. Sediments are composed mostly of greywacke and chloritic sediment with occasional short sections of argillite. Argillite sections typically contain anywhere from 3t-20t sulphides, mostly pyrrhotite. Occasional bands and irregular stockworks of a light green to khaki-coloured material (lot overal .) appear below 84.5m and seem to be an altera tion product/effect. Occasional larger quartz veins observed at 99.5 and 102.5m. It disseminated and stringer sphalerite noted in 30cm quartz vein at 102.5m.

72.86-74.63BI Semi- massive bedded sulphides. Roughly sub-equal amounts of pyrrhotite and pyrite total SO-90% of the interval, with the remainder con sisting of mostly finely laminated chert, and chloritic sediment. Sulphides are very well bedded with only minor amounts of sulphide fragments and stringers visible. No chalco pyrite or sphalerite are observed.

85.80-87.02 and 88.42-88.76miArgillite-rich intervals containing maximum 20t bedded and disseminated pyrrhotite.

Red-brown sphalerite occurrences noted at 106.64m (3mm sph stringer), 109.OS- 109. 37 (5t bedded to heavy disseminated sph.) and 110.73m (3mm thick bedding- parallel patch).

HEM conductor72.86-74.63m.



Property —

806

Sheet No.

Hole No. —

.OF.

TOW-*1-02

ToverDepth ft Lithology Description (colour, grain size, texture, structure, etc.) Alteration Mineralization Remarks

128.32-205.5(

BASALT

120.10-122.67 Quartz veined, argillite rich interval. Rather massive, black argillites are shot through with T-10% quartz stockwork and contains 3-51 disseminated, fine to very fine grained pyrite. Several narrow section of gouge and broken core are present in the 120.1-121.5m section.

122.67-125.42 Feldspar Porphyry Dike: Colo medium grey, very hard, non-magnetic. Massi porphyritic texture with lS-20% plagioclase and quartz phenocrysts set in an aphanitic, siliceous matrix. Quartz veining occurs as 5cm veins and hairline stockworks up to 31 abundance.

125.42-127.35 Heavily quartz veined argilli unit. Quartz makes up SO-90% of interval, occurring as solid sections of quartz and heavy stockworks. 7-103; disseminated pyrite present in non-veined argillite sections. Trace sphalerite observed at 128.9m.

Colour medium to dark green, moderately hard, non-magnetic. Massive to very faintly banded texture. Typically very fine grained, granular appearance, with some coarser sections displaying a weakly developed porphyritic texture. Rounded hornblende phenocrysts range to 3-5mm in size. S-7% irregularly shaped, randomly distributed calcite-rich veinlets throughout

Possible Fault zone 120.10- 127.35m.

Trace disseminated pyrite as patches to 5mm.

171.5-186.70 It red- brown to honey-colourec sphalerite-filled fractures are present at all angles to c.a.



Property

Sheet No.

Hole No. -

.Of.

TOW-91-02


205.0-218.0

OABBRO

218.0

Hornblende phenocrysts are absent below 146.5m, and overall grain size becomes very fine grained to aphanitic. Core takes on a lighter colour, becoming light to medium grey at times.

186.70-188.03 Interflow argillite and volcanic breccia. Large blocks up to 0.5m in length are separated by massive to weakly bedded, pyrite-bearing argillite. Volcanic blocks are light grey in colour.

Unit becomes pillowed, with pillow selvages and pillow breccia commonly observed below 195.35m. Pillows are on the order of 1-1.5m in thickness, and are outlined by aphanitic chloritic margins. Some finely laminated tuffaceous- looking material is associated with py-po occurrence at 195.35m.

Colour dark green, moderately hard, non-magnetic. Massive, medium grained texture with upper 1m being very fine grained and gradually coarsening down hole. Upper contact gradational and chosen subjectively. Porphyritic texture with 103;, 3-5mm sized hornblende phenocrysts set in an aphanitic, mafic matrix. l-3t thin quartz-calcite veinlets. Larger quartz vein to 15cm wide present at 213.0m. Trace to It rounded patches of glomero porphyritic plagioclase present throughout interval.

END OF HOLE

Some association with calcite-rich veinlets is noted, however, most stringers contain sphalerite only. Trace po-py veinlets also present.

15cm of 201; combined py-po (py :^po) present at 195.35 and is possibly related to pillow breccia. Rare to trace disseminated sphalerite observed at 202.00m.

LATITUDE . 3+96S

DEPARTURE

ELEVATION .

1 + 12E


DIAMOND DRILL CORE LOGSheet No. . -OF.

Project No, . 206 TOW-91-3

SurfaceTest

Depth

DIP AT COLLAR-45*

BEARING -135'

Dip

64.Om -46"

Magnetic Bearing


120.0m -47"

TOTAL DEPTH 209.0m CQRE S |ZE ____BQ209.0m -50"

CORE STORAGE-

REMARKS ———

Aunor Minesite - Timmins

NTS. ____410/10 TWP Cunningham C iaim NO 1 030182

NOV. 23/91 completed Nov. 25/91

Contractor Bradley Bros. - Timmins

Logged by R . Pressacco /\


0.0-4.0

4.0-62.80

FELSIC AGGLOMERATE

Casing. Casing left in place. Hole making water.

Colour dark green to black, soft to moderately hard, strongly magnetic for the most part. Massive to fragmental to weakly bedded texture. Interval is chiefly composed of a chaotic mixture of chert fragments and beds, magnetite beds (and fragments) and occasional rhyolitic fragment, all set in a massive chloritic/ mafic matrix. Sulphides (mostly po) present throughout section as well.

Core Angle: 60 Bedding (?).

to c.a. at 17.10m.

It thin quartz-filled hairline fractures. 5t light red-brown garnets (almandine?) observed at 5m.

Overall sulphide abundance roughly 10t, occurring mostly below llm. Sulphides can locally be semi- massive (eg. 24m) to about 30-35% abundance Sulphides dominated by pyrrhotite (951) with occassional pyrite stringer ( 5*). Pyrr hotite occurs mostly as discrete beds and bands, with occasional patches and dissemin ated grains also present. Heavier concentration of po noted at 23-25m were it is smsv-bedded.

Possible HEN conductor 23-25m.



Property

206

Sheet No. 2 nt 7

Hole No. TOW-91-03

Depth 8. Lithology Description (colour, grain size, texture, structure, etc.) Alteration Mineralization Remarks

28.75-30.56 Chert-rich interval. Section composed dominantly of bedded chert and pyrrhotite with minor amounts of chloritic material also present.


34.04-36.37 Diorite Dyke. Colour medium grey, moderately hard, non-magnetic. Massive, fine grained texture. 5% quartz calcite veinlets and stringers.

Occasional lithic tuff beds are present in the 44.0-51.5m interval. These are composed of chert-magnetite-chloritic fragments which are matrix-supported in a matrix of anhedral plagioclase phenocrysts and aphanitic material. These tuffs are interbedded with the agglomerate and contain no appreciable amounts of sulphide.

Chert fragments are the most common type, and are typically aligned parallel to bedding.

56.74-58.40 Diorite Dike. Similar to that at 34.04m.


Sulphide abundance 20* in the 28.75- 30.56m interval. Pyrrhotite is the dominant sulphide with 11 pyrite occurring as stringers and disseminated grains. Pyrrhotite is mostly bedded with minor amounts of stringers. Beds are typically l-5cm thick, but can be up to 10-15cm.



Properly —

206

Sheet No.

Hole No. -

.OF.

TOW-91-03

Tower, iDepth 8,

lithology Description (colour, grain size, texture, structure, etc.) Alteration Mineralization Remarks

Ca.80-98.00

CHERTBRECCIA WITH SULPHIDE MATRIX

98.00-127.85

MASSIVE CHERTS AND CHERT BRECCi;

Colour generally white, depending on magnetite-pyrrhotite abundance, very magnetic. Hell developed monolithic breccia texture with rounded to angular chert fragments of all sizes being grain- supported in a mixed pyrrhotite-magnetite matrix. Upper contact chosen as last appearance of agglomerate, as some inter- bedding occurs. No size sorting of the fragments or bedding is observed. Fragment size gradually increases downhole through to roughly 98m. Interstitial matrix material (magnetite-pyrrhotite) gradually decreases in abundance down to 98m, where the unit is composed mostly of a tight, grain-supported fragmental chert. Some pyrrhotite-magnetite are still present, but only amount to roughly X-3% by 98m. Lower contact is subjective and chosen ae last appearance of significant interstitial pyrrhotite.

Colour variable from white to black, very hard, weakly to moderately magnetic. Interval composed of roughly sub-equal amounts of massive cherts (or very large fragments) and chert breccia. Breccia fragments range up to 10cm in size. Magnetite abundance lQ-15%, occurring as weakly developed beds (5cm thick) interstitial matrix to chert fragments, and as "injection" veinlets in some fragments/beds.

ID-15% pyrrhotite occurs as matrix to chert fragments. Some magnetite as matrix is also present (Po 701, Mt 30%). Pyrrhotite abundance gradually decreases downhole through roughly 80m. Below 80m, po abundance drops to S-7% overall. Rare chalcopyrite stringers observed in a 10cm interval at 87.5m. Possible quartz-vein hosted.

Sulphide abundance S-5%, occurring equally as stringers, disseminated grains, and patches. Sulphide composition consists of pyrite-pyrrhotite in roughly equal proportions.



Property —

206

Sheet No.

Hole No. - TQW-91-Q3

Tow* r


Minor amounts (11) of talc-chlorite filled fractures visible in white chert fragments. 11 quartz-filled veinlets prefferentially oriented at 450 to c.a. Some chert fragments are oriented to yield a bedded appearance.


127.85-128.8

ARGILLITE

to c.a. at 105m.

The cherts become virtually massive below 119.0m. A chloritic (??) alteration is present from 121.6 to 127.85m where a light emerald green material occurs in 20-30t abundance. This "chlorite" occurs mostly as stockworks and strong replace ment of the massive cherts, creating a brecciated/fragmental texture. Minor amounts of pyrrhotite-"chlorite" stringers present in these stringers, and overall sulphide abundance is roughly 1-3t.

Colour black, very hard, non-magnetic. Weakly to moderately developed bedded Texture. 51 bedding-parallel calcite- quartz veinlets. Occasional small chert fragment present.

Core Angle: Bedding.

65 to c.a. at 128.5m.

Sulphide abundance S-5%, consisting of py-po-sph in order of abandance. All sulphides occur in beds or bands (l-5mm), and some pyrite occurs as disseminated grains. Sphalerite abundance less than It, occurring as 4-6mm scale beds (?) near lower contact.

Possible HEM conductor.


DIAMOND DRILL CORE LOGSheet No. .OF.

Project No.

Property —

206Hole No..

TOW-91-03

TonerDepth 4 Lithology Description (colour, grain size, texture, structure, etc.) Alteration Mineralization Remarks

128.a7-l68.5l Colour light grey, soft, non-magnetic.Generally massive, very fine grained

VARIOLITIC to aphanitic texture. Some brecciation, BASALT possibly pillow breccia, is present.

Variole abundance X-3%, occurring scattered throughout the unit. Varioles typically do not exceed 3-5mm in size.

128.87-131.0 and 136.07-139.1? Diorite Dykes. Colour medium grey, massive very fine grained texture.


to c.a. at 152.8m.

Varioles begin to decrease in abundance to nil below 164m to end of section. Sharp contact with lower unit.

Core Angle: Bedding.

85 to c.a. at 168.58m.

Possible incipient to weak sericitic alteration developed. A number of short bands (20-30cm) and patches take on an aphanitic, liae green or beige-yellow -flesh colour. Textural evidence observed in core suggests that these are primary in origin as several knife-sharp contacts with unaltered country rocks observed.

In places, these beige-coloured sections are seen to be composed of very tightly packed varioles with little interstitial spaces.

Trace disseminated pyrite.


DIAMOND DRILL CORE LOGSheaf No. .Of.

Project No.

Properly —

Hole No.TOW-91-03

Depth St Lithology Description (colour, grain size, texture, structure, etc.) Alteration Mineralization Remarks

168.58-174.0) Colour variable from black to white,very hard, non-magnetic. Overall massive

8OLPHXDE- texture, with some short sections displaying BEARING a weakly developed orientation (bedding?) CHERT and others a weakly developed fragmental

texture. The cherts have been fractured and shot through with roughly 7-l(tt quartz- filled fractures which are oriented at all angles to c.a. These fractures are typicall less than l-2mm in thickness, but some can be to 5mm wide.

172.30-173.54 Quartz veined and gouge section. Approximately 70t of interval contained in 2 quartz-(dolomite) veins up to 20cm wide. The gouge sections consist of angular white chert fragments welded or healed together by a black, argillaceous-looking material. Quartz veins are oriented at roughly 30 to c.a. and sulphide content is virtually nil in this section.

Overall sulphide abundance S-5% occurring mostly as hairline stringers, disseminated grains and small patches to lcm in size. Sulphide stringers have the same character as the quartz-filled frac tures/ stockwork . Cross-cutting relationships shows they were emplaced prior to the quartz. Sulphides occur as matrix to chert fragments on rare occassion. Sulphides composed of sphalerite pyrite-galera- (pyrrhotite) in roughly that order of abundance.

Sphalerite stringers, patches and matrix filling most abund ant 168.58-170.30m, with a higher grade section 169.00-169.36m Galena is most abun dant 170.30-172.30m, occurring as very fine disseminations and tiny stringers to a lesser degree.


DIAMOND DRILL CORE LOG Project No,

Property

2-O4

Sheet No.

Hole No. — TOW-91-03


174.0-209.0

GABBRO/ MASSIVE BASALT

209.00

Core Angle: 45 to c.a. at 174.On. Contact.

Colour medium grey to light green, soft, non-magnetic. Massive, fine to very fine grained texture. Approximately 5t very tiny leucoxene grains are disseminated throughout the interval. 1-3t calcite-quartz veinlets and tension gashes are spread throughout.

Unit generally becomes coarser grained down-hole. Some sections are porphyritic with 101 rounded chloritic patches (after amphibole?). Leucoxene most abundant above 184m.

Below 204.5m the unit becomes strongly porphyritic with chloritic patches, and contains 1-31 medium to coarse grained rounded patches of glomero porphyritic plagioclase.

END OF HOLE

Some galena typically associated with sphalerite in 168.58- 170.30m section.

Pyrite is most abundant above 169.00m and from 173.54-174.00m.

It disseminated fine to very fine grained pyrite occurs mostly within 2-3 metres of upper contact.

DEPARTURE

ELEVATION

DIP AT COLLAR

TOTAL DEPTH

3+25S

6+OOE

Surface

-55 BFABIWr, 180"

149.0m TOPFSI7F BQ


DIAMOND DRILL CORE LOGSheet No. Of

Test Depth

64m

Dip -56"

Magnetic Bearing

Corrected Bearing

Project No. —206———

Property Tower

Hole No

149m -5fi c

CORE STORAGE Aunor Minesjte - Timmins

REMARKS Collar of base of hill, NE of pond.

MTg 410/10___ TWP Cunningham cmm NOmiQULL

Datestarted NOV. 26/91—————- completed NOV. 27/91

Contractor Bradley Bros. - Timmins

Logged by R . Pressacco

Depth ii Lithology Description (colour, grain size, texture, structure, etc.) Alteration Mineralization Remarks

0.0-4.0

4.0-31.80

VARIOLITIC BASALT

31.80-44.20

CHERT

Casing. Casing left in place.

Colour light to medium green-grey, soft, non-magnetic. Variable texture from massive, very fine grained to pillowed and pillow breccia. Pillow selvages easily observed as short bands of a dark chloritic material, likely devitrified glass. Varioles are abundant, being 7-10t in abundance through the whole unit, but can be up to BO-90% in short sections. These short sections of smsv-msv varioles usually take on a fleshy or beige colour, the typical colour of the varioles. Variole can be anywhere up to 5mm in size. Trace quartz-calcite veinlets. Quartz veining increasing to S-5% abundance within 5-6m of lower contact. Core becomes more blocky fi broken within 5-6m of lower contact also. Contact not observed due to section of broken core.

Colour generally white, very hard, non magnetic. Overall massive aphanitic texture with only a small amount of interbedded chloritic sediments observed. The core is generally very broken and blocky, and is fairly rusty due to surface weathering.

Sulphides typically absent, although some pyrrhotite a-3%) is observed in a pillow selvage at 19.25.

Sulphide abundance l-3t overall, locally lS-20% over 10cm. Sulphides are composed solely of pyrite. Pyrite occurs in equal

HEM conductor:Stringer pyrite- bearing chert at 31.80-44.20.


DIAMOND DRILL CORE LOG Project No. ————244———

Property —————TOW1R

Sheet No. —————2— OF ——g-

Hole No. ——————TOW-91-4


31.80-44.20 (continued)

44.20-49.05

GABBRO

49.05-59.66

BASALT

59.66-72.80

GABBRO

Core Angle: 70 tea at 39.5. Bedding. 41.56-43.75 Possible healed fault gouge.

amounts of stringers (to 5mm thick) and disseminated fine to very fine grained euhedral crystals.

Colour dark to medium green, soft, non-magnetic. Massive, fine to medium grained texture with 20-253; rounded chlorite particles possible representing original amphibole phenocrysts. it guartz-calciteveinlets. Contact.

Core Angle: 70 tea at 49.05.

Colour dark green, soft, non-magnetic. Unit distinguished from gabbros by its' massive aphanitic to very fine grained texture. S-5% guartz-calcite veinlets.

Colour dark to medium green, soft, non magnetic. Similar to gabbro described at 44.20-49.05, except that chloritic patches are now roughly 25-301 and 1-31 leucoxene is disseminated throughout. A weakly developed glomero-porphyritic texture is apparent with faint to strong patches of plagioclase reaching lcm in size. 1-31: guartz-calcite stringers. Upper contact is indistinct and is chosen as first appearance of chloritic patches/phenocrysts. Core Angle: 3O0 tea at 72.80, Contact.



Property —————TOWER

Sheet No. _____3 OF ——3-

Hole No. ——————TOW-91-4


72.80-149.00

BASALT

149.00

Colour medium to dark green, soft, non magnetic. Massive very fine grained to aphanitic texture, with some short sections appearing to exhibit pillowed textures. 5-7 calcite-guartz veinlets are oriented at all angles tea., and many contain a pinkish to red-brown material (possible hematite or rhodochrosite).

75.67-76.23 Aphanitic Diorite Dyke. Massive texture, trace calcite-guartz veinlets. Calcite-guartz veinlets can locally reach lQ-15% abundance.

114.75-116.09 Diorite Dyke. Massive fine grained texture. Trace calcite-quartz veinlets. S-7% hematite (?) occurs as matrix in upper half of unit.

120.67-133.02 Intrusive interval. Section consists of mostly feldspar porphyry - 120.67-125.92 - and of mostly gabbro 125.92- 133.02. Feldspar porphyry is massive and contains 30-35% anhedral plagioclase set in aphanitic siliceous matrix. Porphyry matrix is hematitic - 122.88-125.92. The gabbro i massive and weakly porphyritic with 3-5% chloritic patches/phenocrysts. Some short sections (10-30cm) contain fine grained disseminated biotite. Several larger quartz calcite veins to 10-2Ocm thick are present below 137.0 and are oriented more or less parallel tea.

END OF HOLE

n

LATITUDE --

DEPARTURE

ELEVATION .

2-*- 1 7 S

2+82E


DIAMOND DRILL CORE LOGProject No. . 206

Sheet No. l OF.

Hoi. No TOW-91-5

Surface

-45" 330*

Test

60m

Dip-46"

Magnetic Bearing

Corrected Bearing

120m -46 0

TOTAL DEPTH 197.0m CORE SIZE180m -47

BO

Aunor Minesite Timmins ^ -

50m chaining error on picket line. 3E.

Tower

NTS.- 410/10P1030163 1030182- TWP. Cunningham

NOV. 28/91______ completed Nov. 30/91

Contractor Bradley i pros. - Timmins

R. Pressacco /('/A.

Depth 8c Lithology Description (colour, grain size, texture, structure, etc.) Alteration Mineralization Remarks

0.0-3.0

3.0-44.59

CHERT BRECCIA


Colour white, very hard, moderately to strongly magnetic depending on pyrrhotite- (magnetite) content. Moderately well- developed fragmental texture with large (5-7cm) rounded to sub-rounded fragments of chert being grain-supported and accounting for most of the core volume. Some longer sections of massive chert might represent larger fragments on the order to 20-4Ocm in size. Rare guartz-calcite veinlets. Fragment size is typically very small (imm-lcm) where sulphid content is heavy. A 30cm magnetite bed is present at 5.6m and weakly developed load casts and flame structures suggests stratigraphic tops are towards the top of the hole. These features are not very reliable, however.

Core Angle: 650 tea at 16.50, Pyrrhotite bed

33.23-33.97 Gabbro Dyke: Colour dark green, soft, non-magnetic. Massive aphanitic to very fine grained texture.

The chert breccia gradually becomes more massive and exhibits a less well-developed fragmental texture below roughly 42.0.

Overall sulphide abundance on the order of S-7%, being compose l chiefly of pyrrhotite (951;) and pyrite (5t) . The sulphides occur

mostly as matrix to chert fragments and as as beds, but a significant amount of stringer sulphides can be observed (253; of total). Some disseminated sulphides also present. Sulphidii content increases to 20-251 in the 13.29- 25.72m interval. A section of semi-massivu pyrrhotite-(pyrite) present 20.18-21.21. Traces of stringer sphalerite-(pyrite) (galena) observed at 6.5, 9.65, and 10.23- 10.84 meters. This latter section (10.23- 10.84) contains up to



Property TQWBR

Sheet No. _____2 nr 7

Hole No. TOW-91-5


44.54-63.84

MASSIVE CHERT

Colour white to light grey, very hard, variably magnetic, depending on pyrrhotite abundance and distribution. Massive, aphanitic texture. No fragmental textures are present in this unit.

A 20cm wide interval of strong brecciation and chlorite alt'n is present at 50.40.

Core Angle: stringer.

50 tea, at 50.40. Chlorite

It stringers which are dominated by a deep-rec brown sphalerite. Galena and pyrite in trace amounts are also preset t in this interval.

35.C3-37.52] Traces (less than It) of red- brown sphalerite stringers are present throughout this sectior Galena is also common with the sphalerite with a roughly 70-30 split (sph-gn). Stringers are typically l-2mm in size and are oriented roughly 450 tea. 10cm section at 37.23 contains S-7% sphalerite and It galena. While overall sulphide abundance remains con stant, the mineralogy changes from po-rich to py-rich down the hole.

Overall sulphide abundance roughly l-3t, occurring mostly mostly asdisseminated grains, patches 6 stringers.



Property

Sheet No. —————3 OF 7—

Hole No. _____TOW-91-5


Core Angle: 30 tea at 63.84, contact. Angular fragments of chert up to l-2cm in size aphanitic chloritic matrix.

Roughly equal proportions of of disseminated and stringer sulphides are present. Pyrite is the dominant sulphide with at most S-10% pyrrhotite present with pyrite. Overall less than It sphalerite occurs mostly as thin stringers (l-2mm thick) and tiny disseminated grains Most of the sphalerite occurs in the 46-55m section. A higher abundance of sphalerite, to st is present at 49.90-50.40. Much of the sphalerite occurs as hairline stringers right next to the chlorite stringer, decreasing gradually away from it it. l-3t stringer (and patches) sphalerite observed in the 62.60-63.84 interval. Up to it galena is present with these stringers, and



Property

Sheet No. _____4 nr 7

Hole No. —————TOW-81-5


63.84-87.20

CLASTIC SEDIMENTS (AROILLITE- QJUSYWACKE)

Colour black to dark green, variable hardness from soft to moderately hard, generally non-magnetic to weakly magnetic depending on pyrrhotite abundance and distribution. Variable textures from bedded to fragmental to some massive sections. The unit is made up of roughly subequal amounts of argillite and greywacke with occasional short sections (30-50cm) of felsic agglomerate interbedded. The greywackes are typically fine grained, and a variety of nun-sized fragments can easily be seen in these greywackes. The fragmental-textured sections are quite commo i and are composed of mostly rounded chert fragments (lcm) set in an argillaceous matri:: Some amounts of chloritic tuff and chert bed i are also interbedded in this section. In short, this unit is a heterogenous mixture o lithologies which are dominated by argillite and greywacke.

Core Angle: 40 tea at 78.10. Bedding.

they seem to be oriented 60-650 to core axis.

Sulphide abundance is roughly S-5% throughout the whole unit, consisting of mostly pyrrhotite and sphalerite, but with galena, pyrite and chalcopyrite also present. Pyrrhotite occurs throughout the section as discrete sulphide frags in the fragmental sections, ultra fine disse, bedded St asamorphous patches of ultra fine po. Sph is ubiquitous throughov t the unit, but is most abundant from 76 to roughly 82.0. Huch of this sphalerite below 76.0 occurs as thin discrete beds or as bands and amorphous patches of disseminated grains. Sphalerite typically red-brown in colour, but some lighter coloured honey sphalerite present. Some stringer



Property ————TOWER

Sheet No. —————S— OF —Z—

Hole No. ______TOW-91-5


07.20-91.96

CHERT BRECCIA (ORE FORMATION)

Colour variable from white to black, very hard, non-magnetic. Generally a well-developed brecciated/fragmental texture is present where small (l-2cm) relatively equal sized fragments of chert are grain-supported in an aphanitic, dark- coloured matrix. No obvious bedding or any orientation to the fragments is visible. This unit-looks similar to that unit described as "ore formation" in

Weakly to moderately well developed chlo- "alteration" occurs throughout mostly as fracture-fillings, but also as a few larger chlorite- filled stringers (3-5mm). Roughly 7t chlorite in this

sphalerite is present, only in small amounts. Some galena occasional] is present with sphalerite. A more or less barren section is present form 82.0-8*

86.20-87.20t S-7% combined sphalerite-gal pyrite. These sulphide occur as stringers/netv stockworks and as disseminated grains anc patches. Roughly subequal proportions of stringer and disseminated sulphides Red-brown sphalerite is by far the most comi sulphide with 11 combined galena-pyrite also present. Some stringers to 2mm wide. Minor calcite with some stringers.

Sphalerite abundance S-7%, occurring mostly below 88.27 to 91.96. Sphalerite is red-brown in colour and occurs mostly as a very finely developed network/ stockwork of thin fracture-fillings.

but

y

.70.

ena-sorks/

on



Property —

Sheet No. _____f nr 7

Hole No. ______TOW-9 l- 9

Depthg, Lithology Description (colour, grain size, texture, structure, etc.) Alteration Mineralization Remarks

91.96-197.0

VARIOLITIC BASALT

the Page-Harley 1953 drill holes (20, 21,22). A strongly developed stockwork of quartz-calcite veinlets is present from 87.20-88.27. This stockwork consists of veinlets and patches of quartz-calcite up to 2-3nun in width and roughly mostly oriented parallel tea. Approximately 15-201 of interval is composed of stockwork, and sulphide abundance noticeably decreases to X-3% in this interval. Minor amounts of quartz-calcite veinlets present in remainder of section. Upper and lower contacts are indistinct.

Colour light grey, moderately hard, non magnetic. Massive very fine grained, variolitic texture. Variole abundance is variable up to ID-15% with the varioles seldom exceeding lcm in diameter. In places, these varioles coalesce into bands of variolites and the core takes on a light beige or flesh-colour. Minor amounts of quartz-calcite veinlets throughou

91.96-96.09 Gabbro dyke. Colour medium to dark green, moderately hard, non-magnetic Massive fine to very fine-grained texture with S-7% combined chloritic and plagioclase phenocrysts l-3% quartz-calcite veinlets.

101.21-103.69 Gabbro Dyke. Similar to abov \ , but containing a few larger patches of glomerophyritic plagioclase to 3cm in size.

interval, and is a grassy-green colour.

These fractures are typically less than 1mm in thickness, but a few are up to 3-5mm thick. Some sphalerite occurs asdisseminated grains and small patches. Minor -amounts of galena-chalcopyrite and pyrite are associated with the sphalerite, accounting for 1-23; combined.



Property

999

Sheet No. _____7 OF—2

Hole No.


197.00

115.04-133.35 Gabbro Dyke. Similar to above dykes. Several bands/patches of plagioclase phenocrysts present.

Core Angle: 350 tea at 136.2. Foliation.

147.94-160.88 Gabbro Dyke. Dark green colour, massive texture. Up to 10* fine to medium grained chloritic patches probably after amphibole phenocrysts.

170.15-185.52 Gabbro Dyke. Similar to those described previously. Several patches of glomerophyritic plagioclase present.

END OF HOLE

LATITUDE ——•^

DEPARTURE

ELEVATION .

2+17S

2+82E


DIAMOND DRILL CORE LOG

SurfaceTest

Depth Dip

248.0 -49"

Magnetic Corrected Bearing Bearing

Project No.

Property —

106

Sheet No. —I———— OF .

Hole No TOW-91-5X

Tower

BEARING . 330*

BO

DIP AT COLLAR ——-45———

TOTAL DEPTH 317.00m CORE SIZE .

CORE STORAGE Au nor Mina Sit-f — Ti mining

REMARKS ^-———————————^———-———-———————--^^—

311.0 -49"NTS ——-—410110 TWP. Cunningham C(ajm No P 103018

Sept. 26/92 COmDieted Sept. 29/92

contractor Norex Diamond Drilling

\. Pressacco ALogged by .

Depth S Lithology Description (colour, grain size, texture, structure, etc.) Alteration Mineralization Remarks

197.0-247.92

VARIOLITIC BASALT

Deepening of hole TOW-91-5 from 197.0 to 317.0m.

Colour medium green-grey,moderately hard, non-magnetic. Variable textures observed in short sections from massive to brecciated to wealy foliated, although overall appearance is fairly massive. Brecciated intervals seem to be a mix of pillow breccia (??) and cherty-looking fragments to 3-5cm. Possibly weakly pillowed. Variole content roughly B-7% overall, with varioles occurring as rounded light-coloured spots to a maximum of 5-7mm.

S-5% calcite-rich quartz-carbonate veinlets occur as randomly oriented, thin, hairline veinlets.

Thin mafic dikes occur throughout the interval, maximum 10-15cm in size.

Core Angle: 400 to c.a. at 219.5m. Foliation.

Incipient sericite- carbonate (??) alter ation affects some short sections and some varioles. These sections take on a light yellow-green colour, and are up to l-2m in size.

Rare disseminated pyrite.


DIAMOND DRILL CORE LOG Project No. . 106

Sheet No.

Hole No.

—————OF ———

TOW-91-5JC

Property Tower


247.92-293.5^

MIXED CHERT AMD CZASTZC SEDIMENTS (LOWER CHERT)

241.75-247.92 Gabbro Dike. Colour Non-dark green, moderately hard,

magnetic. Massive, very fine grained granular texture. 7-10t quartz-calcite veinlets oriented more or less at a high angle to c.a. Upper contact gradational across 10cm, lower contact irregular in shape.

Colour variable from white to dark grey, very hard, variably magnetic depending on magnetite-pyrrhotite distribution. Textures variable from massive (chert- rich sections) to well bedded (argillite- rich sections). Generally core angles are at a low angle to c.a. 3-51 quartz- calcite veinlets are preferentially oriented at a high angle to c.a. Overall, section is chert-dominated with clastic sediments accounting for approximately 30t abundance, lot bedded and disseminated magnetite observed in the 247.92-255.Om interval. Magnetite beds rarely exceed lcm in thickness.

Core Angle: Core Angle: Core Angle: Core Angle:

15" to ea at 249.7m.l O0 to ea at 254.5m.25" to ea at 264.5m.150 to ea at 273.0m.

Bedding. Bedding. Bedding. Bedding.

276.3-279.36 Dioritic dyke. Colour medium green-grey, soft, non-magnetic. Massive, very fine grained granular texture. l-3t calcite veinlets.

5-7t patchy and stringer chlorite alteration/enrich ment observed beginning at 255m and continuing on and off for the remainder of the interval. Pyrrho tite is commonly associated with this chlorite and occurs mostly as small (l-5mm) patches or clusters of patches.

overall it disse minated and stringer sulphides (po 50t, py 5t). 15t quartz vein associated coarse stringer sphalerite observed at 250.8m.

ISO* of S-7% finely disseminated sphal erite observed at 253.2m. Rare pyrite in the 247.92-260.Om interval.

270.66-276.3 1-31; sphalerite present in this interval. Sphal erite occurs as disse minated, very fine grained and small patches concentrated within darker coloured chlorite-argillite bands, possibly suggesting a bedded habit.



Properly —

10*

Sheet No.

Hole No —

-OF-

TOW-91-5X

Tower


282.84-293.57 This interval is rich in graphitic argillite. Colour black, soft non-magnetic, overall, well bedded texture with 10t intercalated greywacke and 5-7\ sulphides defining the bedding planes. Some sections have the appearance of a healed fault gouge (eg 284.5-285.5m). S-5% quartz-calcite veinlets and stock work.

Core Angle: 4O0 to ea at 286.0m.Core Angle: 55" to ea at 290.0m.Core Angle: 45" to ea at 293.1m.

Bedding. Bedding. Bedding.

283.7-284.36 Gabbroic dyke. Upper contact at high angle to c.a., lower contact nearly parallels c.a. 10cm calcite vein at upper contact.

290.83-293.08 and 293.57-295.29Intermediate dykes (??). Colour light yellow-beige, variable hardness from hard to soft, non-magnetic. Massive aphanitic texture. It quartz-carbonate veinlets. Intrusive contacts are mostly gradational over 5-10cm and difficult to pick out. Possible sericite-altered sediments/basalt.

Sphalerite colour varies from red brown to light brown to yellowish. Some stringer sphal erite present 274.5- 276.3m.

282.84-2*3.57 Overall S-7% sulphides (py 95*, po 5t) occur as narrow, well defined beds (eg 286m), moderately defined bands of heavy disseminations, occa sional patches, and nodules.

290.83-293.08, 293.57-295.291 l-3t very fine grained disseminated pyrite.

NOR AN DA EXPLORATION COMPANY LIMITED

DIAMOND DRILL CORE LOGSheet No. .OF.

Project No. . 106 Hole No. TOW-91-5X

Property Tower


293.57-317.0

BASALT

317.0

Colour medium green-grey, moderately hard, non-magnetic. Massive, very fine grained, granular texture. S-7% randomly oriented calcite-rich quartz-calcite veinlets.

Core Angle: 4O0 to ea at 309.88m. Bedding.

309.88-312.80 Black chert. Colour black, very hard, non-magnetic. Aphanitic to weakly developed bedded texture. 5-7\ quartz-calcite veinlets.

Core Angle: 55" to ea at 312.8m. Bedding.

END OF HOLE

306.66-309.*a Weak to moderate sericite alteration lends a beige to yellowish colour to the basalt. Upper contact gradational across 15- 20cm, lower contact very sharp. 5-7t calcite-rich quartz- calcite veinlets. This interval is similar in appear ance to the inter mediate dikes at 290.83-293.57m.

Trace to It disse minated pyrite in the 306.66-309.88m interval.

SOt.88-312.80 1-31 pyrite occurs as nodules and disse minated patches to 2-3cm in size. At times these patches are oriented along bedding.

0+70NLATITUDE ——

DEPARTURE 3*00"

ELEVATION ____Surface


DIAMOND DRILL CORE LOGSheet No. .Of. 10

Project No, 206 TOW-91-6

DIP AT COLLAR ~* 5—————— HFARIMK 010

Test Depth

Om

Dip

-4 S"

Magnetic Bearing


60m. -42"

TOTAL DEPTH 197. Om COHE S |ZE BQ

CORE STORAGE Aunor Mjnesite.

REMARKS Casing in hole.

120111 -44'

P1030184 410/10 TWP. Cunningham c iaim NO P 1030183

-43" Date started NOV. 29, 1991 completed Dec. 1. 1991

contractor ...Bradley Bros. logged by Keith Green


0.0-4.0

4.0-6.9

FELDSPAR-QUARTSPORPHYRY

6.9-81.0

AROXLLXTB BRECCIA/rauxcAGGLOMERATE


Light grey, siliceous, massive feldspar- quartz porphyritic dyke. Abundant l-4mm sized feldspar phenocrystals, subhedral to euhedral shaped (5-81). Lower contact sharp and at 50 to core axis. Minor quartz phenocrysts.

Light to dark green argillite breccia unit consisting of dark green chloritic to light grey matrix hosting variably sized (2-6cm) angular pale grey chert clasts. Lighter grey matrix sometimes hosts l-3mm sized chloritic chips- tuff aceous units.

16.6-20.4 Light grey, siliceous massive to possibly weakly bedded, fine grained felsic tuff. Several elongate medium grey chert or rhyolite fragments. Abundant l-3mm sized fragments of chert and rhyolite.

Local minor clasts of pyrite-pyrrhotite in matrix as well as the clasts-fragments.

Weak local pervasive sericite.



Property —

zot

Sheet No.

Hole No. —

-OF.

TOW-91-06


25.6-35.0 Section of fine grained, light grey tuff with l-5mm angular chloritic, dark green chips. See weak bedding at 50-55 to c.a. throughout.

4S.6-S2.0 Dark green, fine grained chloritic matrix dominates, hosting rare large, light grey chert clasts up to 2O-25cm size. Pyrrhotite occurs as fine beds, fracture fillings and disseminated in chloritic matrix.

52.0-60.1 Dark to medium green chloritic matrix-tuffaceous material (fine grained).

At 56.4, possible pyrrhotite defined bedding at 4S0 to c.a. Pyrrhotite beds are chaotically folded locally, but cannot see bedding in chloritic material. Small fold closure e 56.0, and 59.0 in pyrrhotite bed.

60.1-64.0 Medium to light grey-green coloured, fine grained tuffaceous matrix.

64.0-68.0 Dark green, fine grained, chloritic tuffaceous matrix, no fragments.

35.0-55.S Fine fracture fillings, patches and bedded pyrrhotite through out as 2-5t overall. Minor associated pyrite.

55.8-60.1 T-10% pyrrhotite as 1-lOcm sized beds, dissemin ated and fracture fillings with o.\ medium grained pyrite clusters and fracture fillings.

60.1-65.7 Trace pyrite-pyrrhotite.

65.7-67.2 S-8% fine disseminated, bedded and fracture filling pyrrhotite as l-3cm sized bands. Minor disseminated fracture filling pyrite.

67.2-68.0 Semi-massivi bedded pyrrhotite, 75-80*; with X-2% fracture filling and disseminated pyrite.


DIAMOND DRILL CORE LOGSheet No. -OF 10

Project No. . 206 Hole No..TOW-91-06

Property Tower

Depth 8, Lithology Description (colour, grain size, texture, structure, etc.) Alteration Mineralization Remarks

68.0-81.0 Dark green, chloritic tuffa ceous matrix with S-8% finely bedded pyrrhotite and 2-20t subangular locally elongate and banded, translucent medium grey chert fragments surrounded by pale to olive green chlorite as fuzzy outlines and interval inclusions in quartz.

68.0-68.4 1-3* fine sphalerite fracture fillings associated with several brecci ated 1-2cm wide quartz-calcite veins, li pyrite, dissemin ated and fracture filling.

68.4-74.5 Z-5% fine disseminated and bedded (plus fracture filling) pyrrhotite.

74.S-74.75 2-31 fine fracture filling sphalerite associated within 1-2cm of marginp of quartz-calcite vein and veinlets 3mm-10cm wide. Sphalerite also inclusions in vein material.

74.75-76.2 ID-12% bedded pyrrhotite.

76.2-77.2 51 bedded pyrrhotite.

77.2-77.95 Semi- massive bedded and fracture filling pyrrhotite, eo-70%.



Property

206

Sheet No. 4———— OF .

Hole No TOW-91-06


Bl.0-93.45

CHERT BRECCIA

Pale grey, brecciated massive textured chert consisting of 0.5cn-6cn sized angular chert fragments, separated by 3-101 pyrrhotite stringers 2-5mm wide (locally up to lcm) with dark green hydrothermal chlorite.

At 88.0, SO-60 to c.a. by bedded pyrrhotite. Here, bedded pyrrhotite wraps around chert fragments.

93.0-93.45 2-31; stringer sphalerite zone at contact between brecciated and weakly brecciated chert.

Chlorite stringers associated with pyrrhotite stringers.

77.95-81.0 S-5% pyrrhotite.

Overall 3-10t stringer pyrrhotite up to lcm wide. Local bedded pyrrhotite over 5-10cm in chloritic matrix. Minor disseminated pyrite.

At 81.0, 2% stringer sphalerite over 15cm at chert/tuff contact.

85.0-85.3 X-3% stringer and fracture filling sphalerite associated with 4, 5mn-lcm wide quartz- calcite veinlets.

87.8-88.1 7 01 finely bedded pyrrhotite.

91.35-91.6 1-31 sphalerite fracture fillings.

93.0-93.45 2-3t sphalerite.



10Protect No.

206Hole No

TOW-91-06Property

Depth K Lithology Description (colour, grain size, texture, structure, etc.) Alteration Mineralization Remarks

93.45-107.7

MASSIVE/ WEAKLY BRBCCIATED CHERT

107.7-109.3

raLSXc Tonr/LITHIC QREYWACKB

White to light dark grey coloured massive to weakly to moderately fractured and brecciated chert. Chert fragments are not well developed. Where fragments can be made out, they are generally -elcm sized. Unit hosts l-3t stringer sphalerite with minor chalcopyrite. Local sections over 30cm more strongly fractured with angular chert fragments.

Lower contact at 3S0 to c.a.

106.0-107.7 section.

Much darker grey coloured

Lithic greywacke unit consisting of S\, 0.5mm-5mm sized subangular light to medium grey chert fragments in a dark green- black chlorite matrix. Bedding weakly defined at 65C to c.a. Two 15cm sized medium grey chert fragments with stringer sphalerite, minor pyrite, galena, l-2i. Unit may be more of an siltstone- greywacke matrix.

93.4S-107.7 Overall i-3% combined pyrite- lesser pyrrhotite locally (decreasing downhole), X-3% stringer sphalerite with minor patches of galena and chalcopyrite. Locally 2-41; sphal erite over 10-15cm.

At 107.6, possible bedded sphalerite.

Two 15cm sized chert fragments with 1-2t spalerite, minor pyrite, galena otherwise, non- mineralized.


DIAMOND DRILL CORE LOG Project No 206

Property TO1f*r

Shot No.

Hole No. -

-OF.

TOW-91-Qg


109.3-112.7

CHERTY BRECCIA/ MASSIVE CHERT

112.7-130.6

GABBRO

130.8-144.3

MASSIVEBASALTFLOW

Medium to dark grey coloured, mixed massive and brecciated chert unit with l-2t fine stringer sphalerite. Chert breccia section, consists of poorly defined 5mm-2cm sized angular chert fragments in a light to medium green pure chlorite matrix that appears slightly different then the black argillite breccia matrix. Can see possible fold closure at 110.7m.

At 112.3, 80=45" defined by bedded chloritic and fine (20.1mm) chertfragments. to c.a.

Lower contact at 35

Medium grained, dark green coloured massive textured gabbro. Lower contact with underlying massive flow is ambiguous and gradational. This unit may possibly be a massive basalt flow.

Fine grained, dark green, massive basaltic flow. Minor quartz-calcite veinlets.

138.1-139.1 Light to medium grey, chert breccia unit with 51 fracture filling pyrite with dark green chlorite. Top contact is diffuse and looks like a gradual silicification of the basalt?? Lower contact at 0-50 to c.a.

l-2t stringer sphalerite minor pyrite, galena and chalcopyrite.

Dark green chlorite stringers with pyrite.

138.1-139.1 5 t pyrite filling fractures, minor pyrrhotite.



Property

206

Sheet No. 7____ OF .

Hole No TOW-91-06


144.3-149.2

VARIOLITIC BASALT

149.2-161.1

MIXED CHERT AMD GRAPHITI SEDIMENT

141.25-141.9 Dark grey to black, massive chert with 1-21 disseminated pyrite. Contacts sharp. Upper contact may be folded. Lower contact at 2O0 to c.a.

143.4-144.3 slight increase in grain sized noted to medium grained and texture resembles gabbro unit logged above. Possibly a gabbro dyke. Lower contact at 4o" to c.a. and truncates bedding in underlying variolitic flow (varioles).

Medium to light green, variolitic basalt with varioles, l-5mm sized, rounded to slightly oval shaped. Varioles occur in zones 2-10cm wide.

At 144.4, S0~450 to C.a. At 147.5, SO-550 to C.a.

Unit is folded with fold closures noted at 147.7m.

Lower contact sharp and at 600 to c.a.

Light grey to black, massive to weakly to moderately brecciated chert with mixed graphitic sediment. Chert locally turns black colour adjacent to more graphite rich beds.

141.25-141.9 l-2t disseminated pyrite.

2-4t fine disseminated and fracture filling pyrite, minor pyrrhotite throughout. Trace sphalerite occurs throughout chert unit.

Graphitic sediment beds are typically rubbly with minor ground core.



Project No. 206 Hole No.. TOW-91-06

Property Tower

Depth a Lithology Description (colour, grain size, texture, structure, etc.) Alteration Mineralization Remarks

Graphitic sediment contains up to 51, 2-5mm (up to lcm) size pyrite clasts, bedded pyrite, as well as minor grey chert fragments with diffuse boundaries. Unit resembles a graphitic breccia.

152.0-156.0 Dominantly black, bedded graphitic sediment, locally hard and containing several 10-20cm wide black chert sections. Very minor fracture filling sphalerite.

Finely bedded pyrite defined S0-7O0 to c.a., (i 154.5) locally to 35-4O0 to c.a. Slight folding of the unit is evident.

1SS.5-155.72 Composite milky white quartz vein with thin layers (l-2nun) of graphite).

155.72-156.0 Section of medium to light green, fine grained massive basalt; possibly as a fragment. Over 2-3cm, both contacts marked by sericite bleaching to pale green. Upper contact by quartz vein at 70 to c.a.

Lower contact at 7O0 to c.a.

156.0-157.9 Finely bedded, locally hard,

150.2-152.0 Trace disseminated chalco pyrite galena and lesser sphalerite.

black graphitic sediment, c.a. at 156.2m.

SO at 65 to


DIAMOND DRILL CORE LOG Project No. . 206

Sheet No. 9————OF JJL

Hole No. TOW-ai-06

Property ftaimr


161.1-197.0

XASBXVBBASALTFLOW

157.9-161.1 Dominantly black to dark grey weakly fractured and brecciated chert with rubby graphitic sediment beds at 157.8-158.0 158.4-158.6, 160.1-160.2 and 160.9-161.1. Graphite occurs in fractures in chert.

Lower contact marked by 20cm graphitic sediment/breccia at 60 to c.a.

Light green to grey-green coloured, fine grained, massive basaltic flow. Unit is cut by minor quartz-calcite veinlets (locally a-5%).

170.9-171.2 Quartz-calcite vein breccia with angular mafic fragments in vein matrix at 600 to c.a.

180.6-186.15 Light to cloudy grey coloured siliceous feldspar porphyritic dyke. Phenocrysts 0.5-2mm sized subhedral to locally euhedarl and dominantly feldspar with minor quartz; make up ID-20% of the rock.

Upper contact at 9O0 to c.a. Lower contact at 8O0 to c.a.

193.05-193.6 section of light green to faint buff coloured very fine grained, massive possible interflow material, slightly harder than regular flow, weakly silicified.

162.8-163.5Zone of fracturing and rubbly, broken core.

180.6-166.15 Trace fine disseminated pyrite.

193.OS-it).6Weak silicification.


DIAMOND DRILL CORE LOG10 10

Project No. . 206

Sheet No. *v OF.

HO,. No. TOW-91-06

Property Tower


197.00

193.6-197.0 Light green coloured carbonatized basalt (massive) with local partially altered fragments of buff coloured rock (silicified) as in 193.05-193.

END OF HOLE

193.6-197.0 Moder ately carbonatized.

LATITUDE _______3+OOS

DEPARTURE 2+60E

ELEVATION ___Surface


DIAMOND DRILL CORE LOG

DIP AT COLLAR -87"_____ BEARING

TOTAL DEPTH 182. Pill CORE SIZE RQ

CORE STORAGE Aiinor

Test Depth

Om

Dip

-87"

Magnetic Bearing

Corrected Bearing

Project No. .

Property —

206Sheet No. ——i——

Hole No TOW-9 T-7

-OF. 1 J

Tower

fi firn NTS,. 410/10120m -ft!.S

-ay

REMARKS Casing in hole

Date started .

Cunningham claimNo P1030182

DeC ' 1 /91 l D^- 5/91

Contractor

Logged by .

Bradley Bros.

completed

Keith Green


0.0-2.0

2.0-e.iCHERT BRECCIA

8.1-18.7

GABBRO

Casing - hole collared in bedrock. Casing left in place.

White to medium grey, strongly brecciated chert. Rock consists of 5mm-3cm sized angular white, grey, locally black chert fragments in a matrix of 15t combined light to medium green chlorite and fine pyrrhotite (probably primary)/argillaceous material.

At 5.0m, SO-500 to c.a. At 6.5m, SO-550 to c.a.

Bedding is defined by banded chert and sulphide-chlorite matrix.

Lower contact sharp and at 150 to c.a. Fragments locally have 0.5mm light, pale green chlorite alteration rims. This is also present in matrix and may be more or less fracture filling.

Dark green medium grained massive gabbro.

Upper contact at 150 to c.a. Lower contact at 450 to c.a.

Thin (0.5mm) chlorite alteration rims around chert fragments.

S-10% fine pyrrhotite in matrix of chlorite argillaceous material. Locally l-2t pyrite filling fractures.

8.2-8.5Fractured, rubbly core.


DIAMOND DRILL CORE LOG Project No. 206Sheet No.

Hole No. -

OF —

TOW-91-7

11

Properly Tower

Depth g. Lithology Description (colour, grain size, texture, structure, etc.) Alteration Mineralization Remarks

18.7-23.0

CHERT BRECCIA/ CHLORITIC ARGILLITE

23.0-24.8

GRAPHITIC ARGILLITE

17.3-18.7 Very fine grained, dark green chilled margin of gabbro. Unit looks like massive basalt flow.

White to medium grey chert fragments in a medium green coloured chloritic argillaceous matrix. Chert fragments are angular and up to 10cm sized, but typically ^cm. Matrix comprises lS-25% of rock and consists of weakly bedded chloritic argillite with S-10% fine disseminated and bedded pyrite; locally pyrrhotite up to 15-2Ot.

21.2-23.0 Units consists of finely bedded chloritic argillite with S-10% fine bedded pyrrhotite and up to S-10% chert fragments.

At 22.6, 80=50" to C.a.

Black, finely bedded graphitic argillite with l-3t 2-5mm sized medium to dark grey chert fragments.

Bedding is consistently at 60-650 to c.a. throughout. Lower contact is gradational with more chloritic argillite containing increasing percentage of chert fragments.

Upper contact at 55-600 to c.a.

S-10% pyrrhotite, disseminated and bedded. Locally l-2t pyrite, fracture filling.

19.6-20.25 lS-20% bedded matrix pyrrho tite. At 19.7, 5mm wide chalcopyrite stringer as fracture filling.

l-3t clasts and fracture filling pyrite, minor pyrrhotite.


DIAMOND DRILL CORE LOGSheet No. .OF. 11

Project No. 206 Hole No TQW-9t-7

Property Tower


24.8-26.0

ARGILLITE

26.0-32.55

MIXED CHERT BRECCIA

Medium green, bedded fine grained argillite with lQ-15% finely bedded pyrrhotite. Matrix is typically light green coloured chlorite that has been altered. This material is the same as that which rims chert fragments between 1.6-8.1. Rock hosts 2-41, 5mm-lcm sized light grey chert fragments. Lower contact marked by increase in number of chert fragments. Bedding is consistently 50-550 to c.a.

White, light to dark grey to black chert and argillite fragments occur in a light to medium green chlorite and pyrrhotite matrix, 10-2Ot combined.

26.0-27.9 Fragments comprise 801 of unit and consist of white chert, dark grey to black banded chert. Fragments are rimmed (1mm thick) by light green chlorite. This chlorite also occurs in fractures cutting the fragments as well as forming a significant component of the matrix, along with pyrrhotite.

At 26.4, SO-550 to c.a.

27.9-32.55 Unit consists of SO-90% medium to dark grey and black chert fragments, typically 1-Scm sized in a matrix of clastic and bedded pyrrhotite and lighter green chlorite (minor dark green to black chlorite). Rims around fragments are not as obvious because most of matrix is light green chlorite.

lQ-15% bedded pyrrhotite.

lQ-15% matrix-bedded and fragmental pyrrhotite.

26.0-27.9 Light green chlorite in matrix and rimming chert fragments.

Matrix composed entirely of light green chlorite and pyrrhotite.

At 30.8, 5cm quartz vein with fracture filling 1-21; pyrrho tite. Trace chalco pyrite and possible sphalerite vein at 658 to c.a.



Sheet No.

Hole No..

.OF.

TOW-91-7

11

Property Tower


32.55-37.3

GABBRO

37.3-43.8

CHERT BRECCIA

43.8-51.0

FELDSPAR- QUARTZ PORPHYRY

At 28.6, SO-50At 30.3, SO-600 , bedded pyrrhotitewith black chlorite.

Fine to medium grained, dark green, massive gabbro. Dyke has fine grained margins between 32.55-34.7 and 36.3- 37.2. Upper contact ground core. Lower contact at 600 to c.a.

Medium to dark grey chert breccia unit, l-5cm sized chert fragments (angular) are hosted by ID-12% lighter green chlorite and pyrrhotite.

Outline of some chert fragments is fuzzy. In general, the unit does not appear as fragmental as overlying chert breccia units.

At 43.0, SO-350 to C.a.At 43.7, SO-450 , defined by bedded pyrrhotiti

Medium grey, massive, siliceous feldspar- quartz porphyritic dyke. Unit composed of 5-101, l-2mm euhedral to subhedral feldspar and quartz phenocrysts. Minor black chlorite to locally black hard quartz phenocrysts. Both contacts are broken and rubbly over 5cm. No core angles possible.

ID-12% fragmental and bedded pyrrhotite. Local trace pyrite- fracture filling.



Property —

206Sheet No.

Hole No. — TOW-91-7

Tower


51.8-60.7

BAMDBD CHERT

60.7-70.8

CHERT BRECCIA

70.8-83.45

BANDED CHERT

Medium to dark grey banded to locally brecciated chert. Dark to lighter grey chert bands alternates with black fine pyrrhotite beds (2nn-3cn wide) and medium green chloritic argillaceous sediment. Bedding is typically 45-600 to c.a. Locally brecciated texture is developed.

At 54.0, SO-450 to C.a. At 56.0, SO-500 to C.a. At 58.2, SO-500 to C.a.

Mainly white to light grey, translucent chert fragments sit in a pyrrhotite- light green chloritic matrix (combined lS-20%). Bedding is locally developed, defined by alignment of chert fragments. Fragments are subangular, 5mm-4cm size.

As for 51.8-60.7

At 71.0, SO-600 At 74.0, SO-450 At 78.2, SO-500 At 82.8, 80=55"

10-151 very fine black pyrrhotite beds (lmm-3cm wide) together with fine to medium grained fracture-filling and bedded pyrrhotite.

lQ-15% fine bedded pyrrhotite.

At 70.6, thin ( cO. sphalerite filled fracture.

65.0-69.8 X-4% fine fracture filling pyrite, overprinting pyrrhotite.


DIAMOND DRILL CORE LOG Project No. . 206Sheet No.

Hole No. -

0 OF-

TOW-91-7

11

PropertyTower


83.45-95.

CHERT BRECCIA

Dominantly light grey to darker grey to white (translucent) chert breccia with up to lQ-12% pyrrhotite associated with chlorite stringers. Chert fragments are l-4cm sized, angular.

83.45-86.1 Chert is dominantly white coloured and well brecciated.

86.1-95.6 Chert is dominantly pale grey translucent and darker grey colour. Brecciation is less intense towards the base of unit, especially below 93.5 and unit is banded weakly.

Dark green to black chlorite filling fractures associated with pyrite, pyrrho tite stringers.

@ 91.5, SO i 94.0, SO

45450 to c. a. to c. a.

83.9-84.1 Several thin (5mm) quartz- calcite veinlets associated with sphalerite possibly.

Lower contact sharp and at 4 O0 to c. a.

S-12% fine fracture filling, disseminated and possibly bedded pyrrhotite. Minor to locally 1-21 fracture filling pyrite over 10-20cm. Decreases to s-8% below 87.5.

83.45-83.9 SO-25% matrix pyrrhotite to chert fragments. Minor pyrite.

83.9-84.1 3-54; fine fracture filling, disseminated sphalerite Minor chalcopyrite and galena, li combined. 1-21 fracture filling pyrite-sphalerite appears to overprint pyrrhotite here.

84.1-84.7 1-21 fracture filling sphalerite. Trace chalcopyrite and galena. 1-21 pyrite filling fractures.


DIAMOND DRILL CORE LOG Project No. ——206———

Property ———Tower

Depth a Lithology Description (colour, grain size, texture, structure, etc.) Alteration Mineralization Remarks

95.6-119.5

VARIOLITIC BASALT

Light green-grey to dark green coloured variably altered variolitic basalt. Minor quartz-calcite veinlets throughout. Varioles are typically 3-8mm sized, rounded, with buff or grey coloured cores and occur in patches or concentrations up to 40-80cn wide (St varioles). Local sections up to 15cm wide of ^01 -t 1mm sized varioles or spherulites.

104.2-109.1 unit resembles a pillow breccia unit with l-5cm sized angular dark green fragments in a black chlorite selvage material. Minor varioles.

9 109.5, SO - 550 to c.a. defined by varioles up to lcm sized. This is generally consistent throughout unit.

118.45-119.5 Massive dark green and fine grained basalt. Lower contact at ~550 to c.a.

95.6-97.5 Pale olive green coloured pervasive moderate sericite alteration.

97.5-104.a Moderate carbonate, light grey colour.

i09.a-iia.25 Moderate carbonate, light grey colour.

Below 115.45, car bonate alteration turns rock a faint buff colour locally.

At 15.55, 10cm wide pink and translucent white quartz vein at 8o0 to c.a. causes buff green coloured bleaching of basalt over lOcm-lScm.

104.2-109.1 St pyrrhotite. Occurs in patches of fine disseminations and in dendritic growth pattern in rock.

ll*.25-lia.45 l-2t fine fracture filling sphalerite, associated with quartz-calcite stringers.

lit.45-119.5 2-4*; medium grained fracture filling and clustered, disseminated pyrite.


DIAMOND DRILL CORE LOG 206Project No. ——

Properly Tower

Sheet No. 8 OF

Hole No TOW-91-7


119.5-125.9

WEAKLYBRECCIATEDCHERT

Medium to dark grey locally massive and banded to weakly fractured and brecciated chert. Local lighter green chloritic alteration invades fragments and matrix. See several black, subrounded chert fragments, 5mm size.

6 121.3, SO @ 123.8, SO

65 to c.a. 550 to c.a.

124.4-125.9 Lighter grey to medium grey chert with weak banding defined by light and darker chert layers up to lcm wide. Lower 10cm is pale grey, soft, argillite bed with minor graphite layers. At 125.5, a 7cm wide identical argillite bed. Lower contact at 550 to c.a.

Z-5% pyrrhotite, finely bedded. 1-21 fine fracture filling pyrite

119.5-120.9 X-2% fracture filling sphalerite. Trace galena and chalcopyrite

120.9-121.1 2-3% fracture filling sphalerite. Also 7cm of light green chlorite argillite matrix with some sphalerite.

122.0-122.45 S-7% fracture filling pyrite.

122.0-122.45Broken, fractured core, quartz veins subparallel to c.a.

123.0-123.25 finely bedded pyrr hotite as 2-4cm wide beds, cut by later pyrrhotite and pyrite fracture fillings.

125.5-125.9 X-2% fracture filling sphalerite.

125.9-127.0 Core is strongly frac tured and broken throughout.


DIAMOND DRILL CORE LOGSheet No.

Project No. . 206

OF

TOW-91-7

11

Property Tower

Depth ti Lithology Description (colour, grain size, texture, structure, etc.) Alteration Mineralization Remarks

125.9-127.0

GRAPHITIC SEDIMENT

127.0-128.7

MASSIVE BASALTFLOW

128.7-136.2

FELDSPAR -QUARTZ PORPHYRITIC DYKE

136.2-163.65

MASSIVEBASALT

Black, slightly contorted fine bedded graphitic sediment. Lower contact i 550 to c.a.

Medium to light green coloured, fine grained massive, basalt. Minor quartz- calcite and black chlorite veinlets.

At 127.2, 15cm wide translucent quartz vein with black carbonaceous material and fragments of the bleached pale green basalt. At base of vein, 8cm zone of discontinuous stringers of pyrite, veins up to lcm wide at 7O0 to c.a.

Light cloudy grey, massive, siliceous feldspar-quartz porphyritic dyke. ID-15% combined lmm-4mm subhedral to euhedral feldspar quartz phenocrysts.

Upper contact at 70* to c.a. Lower contact at 75 to c.a.

Fine grained, medium to dark green, massive homogeneous basaltic flow. Lower faint grain-size changes, from very fine to fine grained. Minor quartz-calcite veinlets stringers with local trace sphalerite.

125.9-127.0 X-3% clastic and veinlets of pyrite.

127.0-128.0 1-51 fine fracture filling and disseminated pyrit*

136.2 r 160.0 Local trace sphalerite occurring as flecks in in quartz-calcite veinlets (except in porphyry dyke11). Trace fine pyrite up to l* locally as fracture filling and disseminated.



Property —

206Sheet No.

Hole No. —

10 -OF .

TOW-91-7

Tower

Depth tt Lithology Description (colour, grain size, texture, structure, etc.) Alteration Mineralization Remarks

163.65-168.6

MAFICSUBVOLCANIC INTRUSIVE/ GABBRO

143.5-149.2 Feldspar-quartz porphyritic dyke as for 128.7-136.2.

Contacts are 85-900 to c.a.

149.2-150.0 Very fine grained portion of flow. At 150.0 see slight grain size increase to fine grained.

154.75-163.65 section of very fine grained massive homogeneous basalt. See slight grain size increase gradually starting 158.9.

At 156.0-156.3, 156.6-157.1: Bleached pale green sericite-carbonate alteration halo around milky white and translucent composite quartz veins (with calcite). At 156.0, several veins 2-5cm wide.

At 156.6, quartz vein zone is 28cm wide. Lower contact sharp at 163.65 and at SO0 to c.a. Appears that this lower unit is a subvolcanic medium to fine grained intrusive. This explains why contacts are not clear.

Dark to medium green, fine to medium grained massive homogeneous gabbro dyke/ sill. Unit may be a sub-volcanic mafic intrusive. Upper contact sharp and at 550 to c.a. Lower contact appears gradational. This suggests that unit is either a subvolcanic mafic intrusive or possibly part of the finer grained massive flow.

154.75-158.9 Slight bleaching of rock to pale grey to faint buff colour due to moderate pervasive carbonate. Includes probable addition of sericite 155.9- 157.1.


DIAMOND DRILL CORE LOGSheet No. 11 11

Project No.

Property —

206 Hole No TOW-91-7

Tower


168.65-182.0

MASSIVEBASALT FLOW

182.0

Rock has distinctive spotted texture for most part consisting of chlorite and ampholite/pyroxene crystals surrounded by white feldspar and light green chlorite. This texture is less obvious towards the base of unit.

Medium green, fine grained, homogeneous massive basaltic flow. Unit is cut by minor quartz-calcite veinlets throughout.

END OF ROLE

LATITUDE ..__-.__0+17M

k

DEPARTURE —————3+25E

ELEVATION Surface


DIAMOND DRILL CORE LOGProject No. . 206 Hole No.

Sheet No. ——1 OF —UL

TOW-91-8

DIP AT COLLAR ~85015"

Test DepthOm

Dio v-85"

Magnetic Bearing

Corrected Bearing

- BEARING

TOTAL DEPTH 290.0m CORE SIZE BQ

CORE STORAGE Aunor Minesite.____

REMARKS Casing in hole.

60m -83"120m -83 0180m -82"240m -80. 5"290m -80"

Property

NTS

Tower

Cunningham C(ajmNo P1030183

Date carted - 5/91 completed Dec. 9/91

contractor Bradley Bros.

Keith GreenLogged by .


0.0-3.0

3.0-13.5

XA88IVBCHLORITICAROILLITB

13.5-23.5

TBLDSPAR- QUARTS PORPHYRITIC DYKE

23.5-26.3

LITHIC WACKE


Very fine grained, dark green, massive to locally weakly bedded pervasively chloritized, chloritic argillite.

At 3.5, 2cm grey chert fragment is present.

11.5-11.8 51 subhedral 1mm or less size quartz phenocrysts.

Medium grey, massive, siliceous, quartz-feldspar porphyritic dyke. ID-15%, 1-3 mm sized subhedral to euhedral feldspar < quartz phenocrysts Upper contact at 750 to c.a. Lower contact at 350 to c.a.

Medium green to light olive green coloured. Fine grained lithic wacke unit. Fragments are typically 0.5mm- 1mm angular dark green mafic, light grey chert in an bleached olive green (pale) matrix of argillaceous chlorite. Unit is unsorted and weakly bedded at 60-650 to c.a. throughout.

Weak to moderate local sericite.

Minor disseminated pyrite and pyrrho tite occurs as very fine clusters that appear to be primary as well as in stringers. Local concentrations over 2-5cm.


DIAMOND DRILL CORE LOGSheet No. -OF. 18

Project No.

Property —

206 Hole No. ——TOW-91-8

Tower

Depth fe Lithology Description (colour, grain size, texture, structure, etc.) Alteration Mineralization Remarks

aa.3-29.*XA86XVECHLORITICAROILLITB

29.9-31.9

QOARTZPORPHYRITICDYXB

24.0-24.8 Fragments 5mm-3cm size of dark grey chert and medium green mafic material make up 40-501 of rock.

Lower contact parallel to c.a. and non-planar.

Dark green, fine grained, homogeneous, massive chloritic argillite. Lower contact is brecciated and irregular with strong dark green-black chlorite stringers cutting 20-25cm into the underlying unit and up to 29.3 into the sediment. No grain size changes noted. Unit may be a fine-grained dyke.

As for 13.5-23.5.

Lower contact marked by chlorite veinlets and quartz-calcite over 3-4cm and at 35-400 to c.a.

29.3-29.9 Strongly chloritized with up to 10-15* black chlorite stringers.

29.0-30.5Strongly fractured core. Quartz- calcite lined fracture subparallel to c.a. Brittle breccia zone with fragments cut by lQ-15% black chlorite stringers.

29.9-30.5 ID-15% black chlorite stringers separate porphyry fragments.



Property —

206

Sheet No.

Hole No..

.OF.

TOW-91-8

18

Tower


31.9-42.35

XA88ZVBCHLORITICARGILLITE

Medium to dark green, very fine grained massive to commonly brecciated and conglomerate sections of massive homogeneous very fine grained sediment is separated by sections of finely brecciated argillite where subangular lm-3mm sized dark green mafic (medium) fragments are in a very fine matrix of pale green chlorite and fine dusty pyrrhotite comprising up to lS-20% of the rock locally. These sections of alter nating massive and brecciated sulphide iron-formation are from 10cm to 1.5m thick.

At 39.0, SO - 750 to C.a.

32.1-32.3 Brecciated siliceous porphyritic dyke material. Lower 10cm has 20t black chlorite stringers in brecciated porphyry fragments.

32.3-35.6 l-12cm wide (l is 1.0m wide) patches of pale green coloured, sericitic, brecciated alteration. Here 10-201, l-3mm angular chlorite and mafic fragments sit in a pale green, sericitic matrix. This alteration patches have irregular, diffuse boundaries and are separated by massive basalt.

37.7-38.0 Pale buff to grey massive siliceous felsic dyke. Several rounded quartz phenocrysts.

36.2-3*.75 lQ-20% dusty pyrrhotite as fine clots and irregular stringer and beds.

38.5-40.2 15-20t dusty pyrrhotite.

41.15-41.45ID-15% dusty bedded pyrrhotite.

32.3-35.6 Local sections l-l2cm wide of strong sericite alteration.


DIAMOND DRILL CORE LOG Project No,

Property

206

Sheet No. ____i

Hole No.

-OF, 18

TOW-91-8

Depth Di Lithology Description (colour, grain size, texture, structure, etc.) Alteration Mineralization Remarks

42.35-53.0

CHLORITIC JUMILLITE BRECCIA

53.0-56.0

MASSIVECHLORITICJUMILLITE

Medium green argillite breccia unit with 1mm-lcm sized angular chlorite-mafic fragments and rare 2mm-lcm sized subangular medium grey to light grey, translucent chert fragments in lighter green chloritic argillaceous and fine dusty clastic, disseminated bedded pyrrhotite matrix. Matrix comprises from 20-7Of of rock at 42.5, SO - 650 to c.a.

Bedding appears to be relatively consistant at 65-800 to c.a. throughout, although marked by soft sediment deformation and slumping.

At 45.0, SO - 800

lQ-20% fine dusty bedded, clastic and disseminated pyrrhotite.

At 46.5, SO 80V

48.4-49.1 More massive chloritic argillite,

49.1-50.25 Medium grey, aphanitic, siliceous massive quartz-feldspar porphyritic dykes. 51; l-5mm quartz- feldspar phenocrysts.

At 47.35, contact at 55e to c.a.At 49.10, contact at 85* to c.a.At 48.40, contact at 5O0 to c.a.

Medium green, very fine grained, massive to locally weakly bedded chloritic argillite with fine bedded pyrrhotite.

At 53.7, SO - 650

At 48.4, 15cm Of l-2t fracture filling pyrite at felsic dyke margin.

S-8% fine dusty bedded pyrrhotite. Trace It fine fracture filling pyrite.



She*! No.

Hole No. — TOW-91-fl

Property Tower


56.0-64.4

QUARTZ- FELDSPAR PORPHYRITIC DYKE

64.4-76.6

CHERT BRECCIA

At 54.6-54.9, SO z 500 to C.a. possible cross-bedding.

Here

53.55-53.95 irregular medium to lightgrey chert bands interlayered with chloriticsediment with X-2% fine disseminated pyrite

Light to medium grey, aphanitic, siliceous, quartz-feldspar porphyritic dyke. ID-15%, 1mm-3mm sized subhedral to euhedral quartz, feldspar phenocrysts. Rare orange-brown coloured K-feldspar phenocrysts. Upper contact is brecciated and intermixed with sediment.

Light translucent grey to medium-dark grey to white coloured brecciated chert fragments sit in a matrix of lS-30% pyrrhotite and lesser light to dark green chlorite with minor black, hard carbonaceous material. Chert fragments are subangular to locally subrounded and 5mm-5cm size (locally up to 15cm).

At 55.5, 10cm wide section of 2-4t fine fracture filling and disseminated sphalerite together with minor disseminated and fracture filling pyrite. Minor quartz-calcite veinlets associated. Some of the sphalerite hosted by a fractured chert clast (5cm size)

At 55.95-56.0: l-3t fine fracture filling sphalerite.

At 63.6, two discon tinuous chlorite stringers with fine sphalerite, chalco pyrite and pyrite ( clam wide).

64.4-68.8 lS-30% fine stringer and mostly bedded matrix filling pyrrhotite. Bands are 5mm-8cm wide.


DIAMOND DRILL CORE LOGSheet No. 18

Project No. 206

Property Tower

Hole No TOW-91-B


At 66.2, SO - 60 pyrrhotite).

to c.a. (bedded

68.8-76.6 Chert is less brecciated in this interval with local, more massive sections 20-50cm wide respectively below 75.2m.

76.6-aO.45

Q0ARTZ- FBLD8PAR PORPHYRITIC DYJOS

Medium grey, massive, aphanitic, siliceous quartz-feldspar porphyritic dyke. S-10% subhedral, lmm-4mm sized feldspar-quartz phenocrysts. Contacts are broken and core angles not attainable.

At 66.2, 10cm wide pyrrhotite band (bedded).

••.•-69.1S Traceto It fine fracture filling sphalerite with minor galena and pyrite. Minor pyrrhotite.

69.15-76.7 lQ-15% fine bedded and fracture filling pyrrhotite in matrix to chert fragments. Local Smm-5cm bands pyrrhotite.

73.1-76.7 2-41fine grained clusters disseminated and fracture filling pyrite, apparently overprinting fine bedded pyrrhotite.



Property —

206

Sheet No.

Hole No. -

.OF.

TOW-91-8

Tower


60.45-82.7

MASSIVE CHERT

82.7-92.3

CHLORITIC ARGILLITE

Light translucent grey to locally dark grey, massive, weakly brecciated chert.

82.35-82.7 Unit is brecciated strongly and mainly dark grey colour, with ID-15% matrix chlorite and pyrrhotite.

Lower contact at 7O0 to c.a.

Medium to locally dark green, poorly bedded chloritic argillite unit. Local 10-2Ocm wide fragments and/or irregular beds of massive medium to dark grey chert. Where developed, bedding at 60-7O0 to c.a.

85.5-87.6 Mixed conglomerate/breccia unit consisting of ID-30% Imm-lcm sized medium grey to black chert and medium green argillite fragments in a light to medium green chloritic matrix. Below 86.15, matrix is strongly altered to soft, pale buff-green colour involving intense sericite. Fragments are unaltered. This unit mav have previously been logged as felsic tuff11

6C.15-67.4 Intense buff-pale green sericite alteration.

S-5% fine fracture filling and matrix material pyrrhotite.

62.95-82.7 S-10% fin* disseminated and matrix infilling pyrrhotite.

S-8% pyrrhotite overal] occurs locally as 1-lOcm wide fine dusty disseminates and bedde( forms.

•2.1-92.35 ID-15%very fine dusty pyrrhotite in chloritic argillite matrix.

At 86.0, SO At 90.5, SO

70 to c.a. 600 to c.a.


DIAMOND DRILL CORE LOG Project No. .206

Sheet No.

Hole No. —

nr

TOW-91-8

18

PropertyTower


92.3-113.0

CHERT BRECCIA

Medium to dark grey to rarely lighter translucent grey, brecciated chert. Fragments are massive to weakly banded, angular to subangular 5mm to typically lcm-10cm sized and are hosted by a light green to dark green chlorite and fine dusty bedded to disseminated pyrrhotite (10-151 combined).

At 92.4-92.55, bed of finely brecciated/ conglomerate with l-3mm subrounded to subangular chert fragments in a black chlorite and carbonaceous matrix.

At 95.0, SO - 60-650 to c.a. (bedded pyrrhotite and fragments).

96.4-103.0 chert is locally less brecciated with section of more massive to weakly banded chert, separated by sections of more strongly brecciated chert. Matrix to fragments is lighter green chlorite and fine dusty pyrrhotite.

At 96.6, SO - 450 to c.a. (banded chert).At 103.6, SO - 60-65 pyrrhotite).

to c.a. (bedded

At 107.0, SO - fragments).

55 to c.a. (imbricated

92.30-93.25 S-7% reddish brown fracture filling sphalerite with minor galena and chalcopyrite and lesser pyrite.

•3.25-93.5 a-4% fracture filling and disseminated sphalerite with minor pyrite and galena. l-3t pyrrhoti1

93.5-9*.4 lQ-20% fine dusty pyrrhotite in matrix. Bedded, disseminated and clustered. Occurs in massive bedded lmm-5cm wide bands (irregular).

At 93.7, minor sphal erite in fracture.

96.4-113.0 S-12% fine dusty pyrrhotite in matrix to chert fragments. Occurs Ima-Scm wide, wispy irregular beds. Local pyrite filling fractures.



Property —

206Sheet No.

Hole No.

-OF.

TOW-91-8

18

Tower


113.0-118.8


110.8-121.l

MASSIVE CHERT

At 108.0, SO - 45-60 to c.a. (defined by imbricated cherts fragments 5mm-5cm size).

At 107.8, trace fracture filling sphalerite.

At 113.0, 8mm sized cluster of dissemin ated sphalerite, along with fracture filling.

Medium grey, aphanitic, massive siliceous quartz-feldspar porphyritic dyke. Feld spar-quartz, l-3mm sized subhedral phenocrysts comprise S-15% of rock, locally up to 20t. Minor reddish-brown to orange, partially altered feldspar phenocrysts.

At 113.25, 10cm fragment or piece of chert with S-10% pyrite as fracture filling. Also 1.5cm fractured nodule and clusters of pyrite. Lower contact parallel to core axis. Upper contact broken core, undeterminable.

Medium to dark grey to locally light translucent grey coloured massive, weakly fractured chert. Fractures are typically filled with fine pyrrhotite, chlorite and to a lesser extent pyrite and traces of sphalerite.

l-5i pyrrhotite filling fractures. Trace to 2t fine fracture filling pyrite.

Traces of fracture filling sphalerite locally, especially 119.5-120.2, where most pyrite occurs U-2%) -



Sheet No.

Hole No. —

10 .OF. 18

TOW-9J-8

Property Tower


121.1-126.7

QUARTZ-rZLDBPARPORPHYRY

126.7-13C.9S

CHERT BRECCIA

As for 113.0-118.6.

Portions of porphyry are altered to pale green sericite and phenocrysts of feldspar are altered to sericite, dark olive green- translucent colour. These are: 123.7-124.1 and 126.1-126.7.

Upper contact at 450 to c.a. Lower contact narked by intrusion of porphyry into fractured chert and no angle attainable.

Light to medium to locally darker grey brecciated to locally massive and weakly fractured chert. Pyrite > pyrrhotite, but both

126.7-128.5 Massive, weakly brecciated with trace fracture filling sphalerite and minor chalcopyrite, galena throughout.

At 128.8, SO - 65-700 to c. a.

133.S-133.8 Light grey, fine grained sandy, greywacke unit. Weakly bedded at 60 to c.a.

133.8-134.2 Black, hard carbonaceous chert unit with laminae of lighter grey greywacke (l-5mm wide) and fine clustered and disseminated parallel to bedding. SO - 550 to c.a.

Overall trace to 2t pyrrhotite and trace to 3% pyrite, both fractures filling and local bedded, matrix pyrrhotite. Local pyrite fractures fillings and clusters Imm-lcn wide.

126.7-128.S Trace to 1/41 fine fracture filling sphalerite, minor chalcopyrite and lesser galena associated with minor pyrite.

12*.5-129.4 40-50t fine bedded, matrix filling pyrrhotite in two 10 and 20cm wide massive beds.



Sheet No,

Hole No..

11 . OF. 16

TOW-91-8

Property Tower


136.95-141.5

CHLORITIC AROXLLITE BRECCIA

Medium green to locally green-grey coloured very fine grained chloritic argillite breccia. Minor medium grey to green chert fragments. Several up 5cm size.

140.27-141.5 Several 15cm-35cm quartz- feldspar porphyritic dykes cut the base of the unit.

Local patchy sericite.

134.2-135.1 lQ-15% very fine disseminated matrix, bedded pyrr hotite cut and over printed by fracture filling and dissemin ated pyrite, 3-51.

13S.1-13C.95 S-10% fracture filling and matrix pyrrhotite, decreasing to X-3% down hole with 1-24 pyrite.

At 135.4, minor sphalerite filling fractures.

At 139.0, possible sphalerite filling fracture. Nearby have reddish-brown material filling fracture that is quartz or impurities??

Local dusty dissemin ated matrix type pyrrhotite, over 5mm- lcm area. Overall, 2-4t pyrrhotite.


DIAMOND DRILL CORE LOGSheet No. 12 .OF. 18

Project No. Hole No TOW-91-8

Property ——— TOWG3T


141.5-145.0

QOART2- FELDBPAR PORPHYRITIC DYKE

145.0-152.7

GABBRO

152.7-1*2.5

KXSSZV2/BAKDBDCHZRT

As for 113.0-118.8.

Upper contact irregular, but -2O0 to c.a. Lower contact irregular.

Medium to dark green to locally altered (sericite) lighter olive green coloured fine grained gabbro dyke. Lower contact marked by a weak grain size decrease. Dyke is massive with local well-developed fine grained gabbroic texture, dominated by plagioclase laths in mafic mass.

Light to medium to darker grey coloured massive to locally banded, weakly fractured chert.

152.7-158.0 Lighter grey coloured chert dominantly. Banded between 159.1-157.0 with SO - 50-600 to c.a.

158.55-161.0 Alternating bands of medium to light and dark grey chert, lcm-6cm wide. Thin bed of fragmental chert breccia 158.75-159.0 with fine bedded light green chlorite argillite, pyrrhotite with black to grey subangular chert fragments -clem sized.

At 158.9, SO - 60-65 throughout unit).

to c.a., (consistent

151.1-152.7 Weak to moderate perva sive sericite and carbonate, turning rock a light olive green colour.

Trace pyrrhotite overall. Locally occurs in dusty disseminated forms, l to locally 5t pyrite. Pyrite occurs as fine fracture fillings as well as in dusty disseminated form in rock (imm- 3cm sized patches).

157.3-158.3 Very rare, trace flecks sphalerite.


DIAMOND DRILL CORE LOG Project No. 206Sheet No.

Hole No. .

13 -OF 18

TOW-91-8

Property Tower

Depth 8t Lithology Description (colour, grain size, texture, structure, etc.) Alteration Mineralization Remarks

At 160.3, SO - 45-50 to c.a.

161.0-161.4 Finely laminated, black chert graphitic sediments. Bedding consistant at 550 to c.a.

161.4-162.5 Massive medium to dark grey chert.

isa.3-ist.ss s-7% very fine disseminated and fracture filling sphalerite, locally mimics bedding. Trace galena.

15*.55-15*.CS Trace to locally 1/2* fine fracture filling sphalerite.

ISt. (5-160.25 2-44; finely disseminated and fracture filling sphalerite. Trace galena.

ICO.25-162.1C Local trace fracture filling sphalerite at 160.16, 15cm of 15-201 dusty pyrite.

At 161.4, 4cm of 1-21 disseminated sphalerit i

168.16-1*2.5 1-2* fine fracture filling sphalerite.


DIAMOND DRILL CORE LOG Project No. , 206

Sheet No.

Hole No. -

14 OF. 18

TOW-91-8

Property Tower


162.5-163.95

ORBYWACKE

Light grey, fine grained, massive to locally weakly bedded greywacke. Bedding varies between 60-75 to c.a.

10. 95-175. 3

CHERTYGRAPHITICSEDIMENTS

Black, very fine grained, hard, cherty graphitic sediments of carbonaceous chert. Fine bedding is defined by dusty pyrite bands, and clusters to disseminated. Several 30-50cm wide dark grey chert beds mixed in with sediments. Locally see contorted, slumped pyritic laminae.

At 169.6, SO - SO0 to c.a. (consistently)At 171.3, SO - 70C to c.a.At 174.5, SO - 550 to c.a.

168.45-169.0 Dark grey chert with 30-40t finely bedded pyrite 2O0 to c.a. Bedding above and below this unit is contorted.

171.2-171.6 chert beds.

Two 7cm wide dark grey

174.6-175.0 Two 10cm wide dark grey chert beds with minor pyrrhotite and abundant fine pyrite.

2-4t disseminated clusters and fracture filling pyrite, locallv mimics bedding. Also fine dusty pyrite and lmm-5mm sized pyrite crystals occur locally

Fine dusty pyrite defines bedding. Also occurs as rounded nodules up to 1.5cm diameter, fracture filling, clusters and disse minations. Overall S-7% pyrite, locally S-10%.

16*.45-169.O 30-401 fine dusty bedded and fracture filling pyrite in dark grey chert. One fleck sphalerite noted11

171.2-171.7 20-30% fine, dusty bedded and fine fracture filling pyrite. Here, two 7cm wide dark grey chert beds.



Property ———Tower

Sheet No. ————15——OF——18 .

Hole No TOW-91-B


175.3-200.0

MASSIVEBASALT

200.0-204.75

QUARTS5- FBLD8PAR PORPHYRITIC DYKE

Medium grey to green, fine grained, homogeneous massive basalt flow. Slightly finer grained (chilled?) upper contact zone 175.3-175.8. Upper contact core angle is unattainable due to missing, ground core (minor). Unit is cut by minor quartz-calcite veinlets throughout.

184.9-185.5 Black, massive to locally bedded, locally hard and cherty graphitic sediment. Clustered and minor fine pyrite, together with minor carbonate veins (calcite?) define possible bedding at 700 to c.a.

Upper contact at 750 to c.a. Lower contact at 8O0 to c.a.

Gabbro shows faint chilling (finer grained) of contacts around graphitic sediments over 20cm.

199.0-199.1 Bed of black, hard cherty graphitic sediment. Bedding at 70th to c.a.

As for 113.0-118.8.

Upper and lower contacts at 50-550 to c.a.

Moderate pervasive carbonate.

175.3-178.5 Minor to 2t fracture filling pyrite with calcite and/or chlorite as well as disseminated pyrite.


DIAMOND DRILL CORE LOG w*.Sheet No. 16 -OF. 18

U....U.. TOW-91-8

Properly Tower


204.75-210.6

OABBRO

210.C-290.0

MASSIVE BASALT

Medium green, fine to medium grained massive homogeneous gabbro. Local subangular fragments up to lcm size of finer grained mafic rock are present. Lower contact marked by abrupt grain size change and at 600 to c.a. Pervasive calcite alteration occurs in matrix of rock.

Light to medium green, very fine to fine grained, homogeneous massive. Basalt, cut by subvolcanic (feldspar) gabbro dykes and sills. Minor to St calcite and quartz-calcite veinlets throughout. Fine white to faint mauve coloured leucoxene is locally present.

210.6-213.0 Unit is weak to moderately foliated and contains 5-2 Ot foliation parallel and cross-cutting calcite and lesser quartz-calcite veinlets up to 1.5cm wide. Foliation consistent at 45e to c.a. Locally see pieces of overlying gabbro in part of the core.

217.8-223.7 Fine to locally medium grained massive gabbro dyke. Upper contact gradational and arbitrary. Lower contact sharp and marked by gradual decrease in grain size over 40-50CB. Unit is brecciated with lmm-8mm subrounded mafic fragments down to ~221.4.

Pervasive and veinlets of calcite. Local minor flecks leucoxene.

Local fine leucoxene. Trace to St calcite (lesser quartz- calcite) veinlets.

210.C-213.0 S-20% calcite veining (plus quartz-calcite)

Moderate to locally strong pervasive calcite.

Minor fracture filling pyrite.

224.6-22*.3 Local patches of very fine-dusty pyrite in basalt. Appears, at first, to be alteration.



Property

Sheet No.

Hole No. —

17 -OF. 18

TOW-91-8


238.8-239.7 Section of lighter to medium grey-green fine grained basalt with local irregular shaped, hard pale tan to green colour fragments that are brecciated and may be varioles. Also see fragments that appear to be possible chert, 2mm-2cm sized. Favour brecciated varioles for some fragments. See fabric at 60-650 to c.a. defined by brecciated possible varioles.

243.65-244.55 Medium grained gabbro dyke/sill. Lower contact marked by sharp grain size change; upper contact gradational and indistinct.

248.0-249.35 5-8*, l-2mm wide calcite veinlets define weak foliation at 450 to c.a.

249.35-249.5 Fault breccia, pale green, sericitized granulated, gritty matrix with bleached pale buff fragments and minor white to translucent quartz fragments lcm sized.

Below 251.0, basalt is darker green colour and very homogeneous.

267.4-270.5 Light grey, siliceous, quartz-feldspar porphyritic dyke. Minor orange to orange-brown altered feldspar phenocrysts. Upper contact at 45 to c.a. Lower contact non-planar. Phenocrysts l-3mm size, S-10% of rock.

At 247.8, possible trace flecks sphalerite.

249.35-249.Sstrong sericite.

249.35-249.5Sericitized, bleached fault breccia at 70C to c.a.

253.0-8*7.4 Trace to minor possible reddish brown sphalerite with quartz calcite veinlets. May actually be an impurity with vein.


DIAMOND DRILL CORE LOG Project No.206

Sheet No.

Hole No. -

18 .Of. 18

TOW-91-8

PropertyTower


290.8

271.75-274.9 As for 267.4-270.5 above. Upper contact at 45C to c.a. Lower contact at 3O0 to c.a.

267.35-288.4 Medium green, very fine grained pillowed basalt flow. Thin pillow rims are typically bleached pale green-buff, lcm wide and marked by -c 1mm sized rounded spherulites. Locally, pillow cores contain concentrations of •e 1mm pale buff spherulites. Pillow selvages range from 5mm to 4cm wide and are marked by dark green chlorite and commonly calcite (minor quartz) veinlets up to 3cm wide. Pillows range in size approximately from 2cm to 50cm diameter and possibly larger.

Upper contact sharp and at 450 to c.a. Lower contact very gradational and indistinct.

288.4-290.8 Fine grained, dark green, massive, homogeneous probable gabbro subvolcanic dyke/sill. Upper contact is gradational with overlying pillowed flow and indistinct.

END OF HOLE

In one location, was able to smudge the reddish-brown, apparently oxidized material on a fracture surface.

LATITUDE . 0+06N

DEPARTURE

ELEVATION .

4+78E


DIAMOND DRILL CORE LOGProject No. 206 Hole No.

Sheet No. ———

TOW-91-9OF.

Surface

DIP AT COLLAR -45' BEARING 010'

Test Depth

OmDip

-45"Magnetic Bearing


60m -45' NTS.. 410/10P1030179

Cunningham clajmNo P1030180

TOTAL DEPTH 200.0m CORE SIZE BQ

CORE STORAGE Atinor Mineaite-———

REMARKS _____Casing in hole.

120m -45'180m -46" ' 9/91Date .tarted

contractor Bradley Bros.

Logged by .

completed - 11/91

Keith Green


0.0-3.7

3.7-20.0

MASSIVECHLORITEJUMILLITE

20.0-C0.85

CHLORITIC JUMILLITE BRECCIA


Medium to dark green, very fine grained, massive chlorite argillite unit looks like a massive basalt for most part. Unit contains rounded to subrounded lcm- 9cm sized purplish-red quartz porphyritic clasts, l-3t down to ll.lm. Quartz phenocrysts are up to 10-151 in clasts and are subhedral shaped.

13.B-14.05 Light grey-green, carbonatized very fine grained massive mafic dyke. Sharp contacts at 650 to c.a.

i 18.1, So - 650 to c.a. 8 19.0, SO - 650 to c.a.

Medium to dark green, well bedded fragmental sediment with a fine grained chlorite- argillite and pyrrhotite matrix. Bedding is typically well defined by bedded pyrrhotite and imbricated fragments. Unit is locally massive to weakly bedded.

Minor very fine pyrrhotite in rare, Imm-lcm wide beds. Trace frac ture filling pyrite.

l*.0-20.O 30t finely bedded pyrrhotite occu :s in semi-massive beds, lcm-3Ocm wide.

18.0-18.3, 18.4-18.7Beds eo-90% pyrrhotite.

20.0-24.7 lS-20% pyrrhotite. Pyrrho tite is very fine and dusty, is finely bedded and disseminate l and occurs in irregula semi-massive to massiv beds 5mm-30cm.


DIAMOND DRILL CORE LOGSheet No .Of.

Project No. ——2Hfi——

Tower

TOW-91-9

Property


20.0-24.7 Unit is commonly brecciated to locally massive and contains irregular shaped beds of pyrrhotite 5mm-lOcm wide. Fragments are up to 1.5cm of subangular and of the same composition as host rock, but generally darker green.

24.7-60.85 Fragments of subrounded to subangular light to medium grey chert comprise -cl-3t of rock (lmm-3cm size). Locally fragments make up 50-601 of rock in 2cm-50cm bands. They are typically imbricated and together with bedded pyrrhotite, define bedding. Fragments and irregular bands of chlorite argillite typically alternate with pyrrhotite beds and lighter green chlorite matrix and bands of chert locally. Bedding generally consist at 55-650 to c.a.

Local tiny (-c 1mm) calcite veinlets rimming tiny frag ments and locally pyrrhotite.

Chert fragments have thin alteration rims of pale green sericite with possible calcite.

@ 26.5, SO@ 30.0, SO8 31.5, SO@ 33.0, SO8 38.0, SO@ 41.0, SO@ 45.0, SO

60" 600 550 500 550 60" 550

46.1-46.7 Section with no pyrrhotite.

46.7-47.55 Fine grained, dirty brown-grey coloured massive mafic diabase dyke. Contacts sharp and at 60-7O0 to c.a. Weak pyritic halos in argillite breccia over up to l.Om on both sides of dyke.

21.3-22.2 30-351; pyrrhotite.

24.35-24.6 l-2% fracture filling and clustered sphal erite. Trace galena and minor pyrite.

25.2-46.1 20-501 pyrrhotite as fine irregular semi- massive to massive beds and disseminated in rock. Beds are Imra to 10cm wide, with semi-massive beds 10cm up to 1.5m wide.

25.2-27.5 70-80%pyrrhotite.

46.1-46.7Trace pyrite.

47.6-48.6 Traceto 3% dissem pyrite.

57.4-60.85 15-25*; fine bedded pyrrhotite


DIAMOND DRILL CORE LOG 206Sheet No.

Hole No.

-"—— OF.

TOW-91-9

PropertyTower


CO.85-89.35

CHERT BRECCIA

48.6-57.4 Light to medium grey, aphanitic, siliceous quartz-feldspar porphyritic dyke. S-10%, l-3mm sized quartz and feldspar phenocrysts. Lower contact at 4S0 to c.a.

@ 58.5, SO - 55-600 to c.a.

59.65-60.85 Increase in abundance of medium grey chert fragments, locally up to 70% cher: over 10-3Ocm. Bedding consistent at 55-600 to c.a. Lower contact marked by first appearance of true chert breccia, but is gradational.

Light to medium grey, strongly brecciated chert with 5mm-5cm subangular to angular chert fragments in a matrix of pyrrhotite and chert fragments in a matrix of pyrrhotit and light green chloritic argillite (up to 2

Fragments of chert have thin ^lmm-2mm) pale green altered rims of possible sericite. This matrix is the true matrix to the chert breccia, along with the primary pyrrhotite. Rare dark grey to black finely bedded chert fragments.

63.4-64.7 Section of more massive, moderate fracture chert with S-7% fine fracture filli pyrite and local sphalerite.

40.85-64.7 lQ-20% fine bedded and clusters of pyrrho tite, up to 2cm wide.

At 81.8-62.05 1/2 - l fine fractures filling sphalerite with trace galena and i\ pyrite.

63.4-64.7 S-7% fine fracture filling pyrite

NOR AN DA EXPLORATION COMPANY LIMITED


Sheet No.

Hole No. -

.Of.

TOW-91-9

Property Tower

Depth tt Lithology Description (colour, grain size, texture, structure, etc.) Alteration Mineralization Remarks

89.35-126.3


64.7-69.25 Quartz-feldspar porphyritic dyk* as for 48.6-57.4. Top contact has lOcm of consolidated fault breccia at 8O0 to c.a. Lower contact at 650 to c.a.

75.85-76.9 Section of 30-401 bedded pyrrhotite in chloritic argillite breccia with minor chert fragments.

f 76.5, SO - 60C to c.a.i 88.0, SO - 750 to c.a. (bedded pyrrhotite)

Quartz-feldspar porphyry dyke. As for 48.6-57.4. Upper contact at 500 to c.a. Phenocrysts locally up to lS-20%. Between 108.9-120.0, - St phenocrysts. Lower contact non-planar.

63.4-64.05 Overall 1/2 - max It fracture filling sphalerite and trace galena, concent rated over 5cm at 63.4 and 20cm @ 63.85.

69.25-87.12 S-10% pyrrhotite in matrix. Trace pyrite locally.

75.8-76.9 30-40t bedded pyrrhotite.

87.15-88.2 Trace fracture filling sphalerite. 5t pyrrhotite.

88.2-89.35 Trace to It fine fracture filling sphalerite. Trace galena, pyrite. Minor pyrrhotite.

At 88.0, 10cm wide massive pyrrhotite band at 750 to c.a.

64.7-64.8Consolidated fault breccia at 800 to c.a. at chert- porphyry contact.



Sheet No. ——J OF —

Hole No TOW-91-9

Property Tower


126.3-134.9

VARIOLITIC BASALT FLOW

134.9-141.1

XAS8IVE CHBRT

Light to medium green, to locally faint buff coloured fine grained variolitic basalt flow. Varioles are typically lmm-7mm diameter, rounded and occur in concentrations over 5-10cm commonly.

126.3-129.5 Several 10-50cm wide sections of buff coloured concentrations of coalesced varioles up to lcm sized.

133.35-133.55 Part of a chert fragment with contact subparallel to c.a., cross-cut by 54, l-3mm wide quartz- calcite tension veinlets. Fragments contains fine pyrrhotite.

Light to dark grey coloured, moderately fractured, locally brecciated massive chert with fracture filling sphalerite throughout. Locally chert is weakly banded in darker grey sections.

At 135.1, weak banding, SO - 600

Minor pyrrhotite and pyrite.

133.35-133.55 S-10% fine dusty pyrrhotite in possible chert fragment. Trace pyrite.

At 132.45, minor fracture filling sphalerite.

134.9-140.0 Nil pyrrhotite. Overall 1-34 fracture filling pyrite and 1-44 fracture filling sphalerite with trace galena and rare chalcopyrite.

134.9-135.0 104 very fine dusty pyrrhotite.

135.0-135.65 1-34 fracture filling sphalerite.



Sheet No.

Hole No. —

.OF.

TOW-91-9

Property Tower


140.25-140.6 Pale green to faint buff, aphanitic siliceous, weakly porphyritic felsic dyke. Nil sulphides.

At 140.1, several irregular graphitic fractures and seams. Lower contact sharp at 600 to c.a. and marked by 10cm composite, white quartz vein (sheeted).

141.1-146.35

GRAPHITIC SEDIMENTS

Black, faintly bedded to massive and locally contorted graphitic sediments with 5mm-2cm sized clasts of clustered pyrite.

141.1-141.3 Composite, sheeted milky white quartz veins at 60* to c. a.

135.65-136.1 S-8% pyrrhotite.

136.1-136.951-2t sphalerite.

136.95-137.94-7t sphalerite.

137.9-138.35 Minor to trace sphalerite.

138.35-139.0 3-51 sphalerite, locally S-7% over 10-12cm. Galena little more than usually but ^*.

139.0-140.01-4t sphalerite.

140.6-141.1 2-4% fin* fracture filling pyrite.

1-31 fragments of clustered pyrite up to 2cm diameter.

141.4-142.7Most of core is rubble with -50cm of missing ground core.



Project No. . 206

ne

TOW-91-9

Property Tower


146.35-153.5

MASSIVE BASALT

141.4-142.7 Section of rubble, ground core with 50cm of missing core.

145.3-146.35 Fine grained, silty massive carbonaceous sediment with S-4% disseminated and fracture filling pyrite.

Light grey coloured, very fine to fine grained massive basalt. Minor calcite -quartz veinlets throughout. Upper

at 558

153.5-1S9.7S

GRAPHITIC SEDIMENTS

159.75-168.9

WEAKLY PILLOWED BASALT FLOW

Moderately to strongly carbonatized

contactat 7O0 to c.a.

to c.a. Lower contactUnit may be weakly

developed pillowed flow, identical to 159.75-168.95 below.

Black, massive to locally bedded, very fine grained, competent graphitic sediments with 2-5% pyrite.

0 155.8, SO - 30-400 to c.a. i 157.9, SO - 50s to c.a.

Lower contact marked by 10cm of laminated pale green to buff coloured cherty argillite with bedding at 3S0 to c.a. Lower contact is actually at 55-600 to c.a.

Light grey, very fine to fine grained very locally weakly pillowed basalt flow. In several places see incipient pillows with l-5mm wide poorly developed selvages. Lower contact sharp and at 80-85* to c.a.

145.3-146.352-4t pyrite.

Trace pyrite through.

146.35-148.0 1-31 fine disseminated and fracture filling pyrite.

2-51 pyrite in bedded, fracture filling, clast forms.

Moderate to strong carbonate.

ICO.3-160.45 2-3* fracture filling sphalerite with trace galena and l-3t pyrite.



Project No. .

Property —

206

-OF.

TOW-91-9

Tower


166.95-200.0

MASSIVEBASALT

200.0

160.45-160.7 Probable light buff to green contorted argillite.

At 161.2, incipient pillows over 15cm.

164.6-164.8 Poorly developed, brecciated pillows with 3mm-5mm wide selvages.

165.85-166.95 Fine grained, finely bedded greywacke/siltstone unit. Bedding is consistent 50-550 to c.a. Several 5mm sized flat chert fragments.

168.5-168.95 Poorly developed pillow selvages lcm wide (three are present).

Medium green, fine grained, homogeneous massive basalt, cut by l-2t calcite- quartz veinlets throughout.

171.6-174.8 Light grey quartz-feldspar porphyritic dyke. S-10% quartz-feldspar phenocrysts, 1mm-3mm sized. Upper contact at 7O0 to c.a.

END OF HOLE

At 160.68, trace sphalerite.

16S.85-1C6.95 2-4*;fine bedded pyrite.

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Ministry ofNorthern Developmentand Mines

OntarioidMlne

Report of Work Conducted After Recording Claim

Mining Act

IS.Transaction Number

Personal Information collected on this form is obtained under the authority of the Minlni this collection should be directed to the Provincial Manager, Mining Lands, Ministry Sudbury, Ontario, P3E 6AS, telephone (705) 670-7264.

41018NE9189 41 CUNNINGHAMInstructions: - Please type or print and submit in duplicate.

- Refer to the Mining Act and Regulations for requirements of filing assessment work or consult Recorder.

- A separate copy of this form must be completed for each Work Group.- Technical reports and maps must accompany this form in duplicate.- A sketch, showing the claims the work is assigned to, must accompany this form.

-tffe**

900 the Mining ,

Recorded Holders) , L(v(. / rvlire-JU Uvfe/

Client No.

AddressSdk3w.fry.-n-.,-^ po (k* li

Be*Ul3, ft) ft.x4*crfc,- - 'vij 7 rr"______-T6*nship7Area

r , |5 C.Telephone No.fort)

ning Dvision M or Q Plan No.

ates Work Performed

From: /ft l9oi W, (W/ P9, W A

Work Performed (Check One Work Group Only)

Physical Work, including Drilling

Assignment from Reserve

total Assessment Work Claimed on the Attached Statement of Costs S f Ofe, Q0'7. OONote: The Minister may reject for assessment work credit all or part of the assessment work submitted If the recorded

holder cannot verify expenditures claimed in the statement of costs within 30 days of a request for verification,

Persons and Survey Company Who Performed the Work (Give Name and Address of Author of Report)Name Address

Ut* i W 2367

Po 6os 88 , ft PoM /CO

(attach a schedule If necessary)

Certification of Beneficial Interest * See Note No. 1 on reverse sideDate RecordedMplder or Agent (Signature)1 Certify that at the time the work was performed, the claims covered In this work

report word recorded In the current holder's name or held under a beneficial Interest by the current recorded holder.

Certification of Work Reportl certify that l have a personal knowledge of the facts set forth In this Work report, having performed the work or witnessed same during and/or after Its completion and annexed report Is true.

Name and Address of Person CertifyingP?rV

Telepone No. Date

vxCertified By (Signature)

For Office Use Only

Date Notice for Amendments Sent

0241 (03/91)

Details for Kork Renort t NEONT93.00? Page

Xork Report* for Applying

ReserveClaim Number see note 2)

^ 1,030,1791-1,030,180

0 1,030,181

9 1 ,030,182

P 1,030,183

? 1,030,184

? 1,030,185

P 1,030,186

? 1,030,137

P 1,030,188

? 1,030,189

? 1,176,938

? 1,176,989

P 1,176,990

? 1,178,991

9 1,176,992

P 1,176,993

f OfClaim Units

11t11t1

111111l111i

Value of Assesment Vork Done

on this Claim2,330.00

8,505.00

3,083.00

29,854,00

30,872.00

4,409.00

11,269.00

11,585.00

Value Applied to this Claim

1,400.001,400,00

1,400.00

1,400.00

1,400.00

1,400.00

1,400.00

1,400.00

1,400.00

1,400.00

1,400,00

2,000.00

2,000.00

2,000.00

2,000.00

2,000.00

2,000,00

106,907,00 27,400,00

Values Assigned from this Claim

8,000.008,200.00

Reserve;i(ork to be Claimed at

a Future Date930.00

7,105,00

6,683.00

20,454.00

21,212,00

3,009.00

9,869.00

10,185.00

!6,200.00 79,507.00Total Number

of ClaimsTotal Value Xork

DoneTotal Value Work Applied

Total Assigned From

Total Reserve

Credits you are claiming in this report may be cut back. In order to minimize the adverse affects of such deletions, please indicate from which claims you wish to priorize the deletion of credits. Please mark (x) one of the following:1.M Credits are to be cut back starting with the claims listed last, working backwards.

2.M Credits are to be cut back equally over all claims contained in this report of work.

3.1 j Credits are to be cut back as priorized on the attatched appendix,

4.[x] Credits are to be cut back starting with the claims that have reserve credits.In the event that you have not specified your choice of priority, option one will be implemented.Note l: Examples of beneficial Interest are unrecorded transfers, option payments, memorandum of agreements, etc.,

with respect to the mining claims, Note 2: If work nas been performed on patented or leased land, please complete the following:I certify the patf

that the recorded holder H or leased land at the

had a beneficial interest in time the work was performed.

Signature Date

Ontario

Ministry ofNorthern Development

MinesCI)

6itere du Developpement du Nord et des mines

Statement of Costs for Assessment CreditIztat des coOts aux fins du credit devaluation

Mining Act/Lot sur les mines

Transaction No./N" de transaction

Personal Information collected on this form is obtained under the authority of the Mining Act. This Information will be used to maintain a record and ongoing status of the mining claim(s). Questions about this collection should be directed to the Provincial Manager, Minings Lands, Ministry of Northern Development and Mines, 4th Floor, 159 Cedar Street, Sudbury, Ontario P3E 6A5, telephone (705) 670-7264.

Les renseignements personnels contenus dans la presente formule sont recuelllis en vertu de la Lo) sur le* mines et servlront a tenlr a Jour un reglstre des concessions minleres. Adresser toute question sur la collece de ces renseignements au chef provincial des terrains mlnlers, mlnlstere du Developpement du Nord et des Mines, 159, rue Cedar, 4* etage, Sudbury (Ontario) P3E 6A5, telephone (705) 670-7264.

1. Direct Costs/Couts directs

Type

WagesSalalrea

Contractor'* and Consultant'* Fee* Droll* d* ('entrepreneur •t de ('expert- conceit

Supplle* Used Fournlture* utlll****

Equipment Rental Location de materiel

Description

Labour Maln-d'oeuvreField Supervision Supervision sur le terrain

Type

Type

Type

Amount Montant

iijrt**

tyW-OQ

Total Direct Costs Total des coOts directs

Totals Total global

lljtf'OO

fyfrtf-aO

ICl,8il-o6

2. Indirect Costs/CoQts Indirects* * Note: When claiming Rehabilitation work Indirect costs are not

allowable as assessment work. Pour le remboursement des travaux de rehabilitation, les coOts Indirects ne sont pas admlsslbles en tant que travaux devaluation.

Type

Transportation Transport

Food and Lodging Nourrtture *t heberoamentMobilization and Demoblllutlon Mobllliatlon et demoblllMtlon

Description

T(u*nv*k k^*i

CeôG^

Amount Montant

3*49-00

nnoo

Sub Total of Indirect Costs Total partlel des coOts Indirects

Amount Allowable (not greater thin 20H of Direct Costs) Montant idmltslble (n'excedant p*s 20 H d** coot* directs)Total Value of A**e*sment Credit Valeur total* du credit (Total of Direct and Allowable devaluationindlmet eattil rTatil du eeflta dlracO

Totals Total global

ittoH&oo. ' ,. ; ' ?i'.W,.*' . -

•#"i*' L,.IW: ' ;- *f*^ \ '.'. ,

i&fooi•i,-.;*'.-

**

iik,to.0t•t Mlraett idmlMlb)**

Note: The recorded holder will be required to verify expenditures claimed in this statement of costs within 30 days of a request for verification. If verification Is not made, the Minister may reject for assessment work all or part of the assessment work submitted.

Note : Le titulalre enregistrd sera tenu de verifier les depenses demandees dans le present etat des coOts dans les 30 jours suivant une demande a cet effet. SI la verification n'est pas effectuee, le ministre peut rejeter tout ou une pattle des travaux devaluation preserves.

Filing Discounts

1. Work filed within two years of completion is claimed at 100"M) of the above Total Value of Assessment Credit.

2. Work filed three, four or five years after completion Is claimed at 50Vo of the above Total Value of Assessment Credit. See calculations below:

Total Value of Assessment Credit Total Assessment Claimedx 0.50

Remises pour depot

1. Les travaux deposes dans les deux ans suivant leur achievement sont rembourses a 100 *Mi de la valeur totals susmentkmnee du credit d'evaluatton.

2. Les travaux deposes trols, quatre ou cinq ans apres leur achievement sont rembourses a 50 M) de la valeur totale du credit devaluation susmentionne. Voir les calculs cl-dessous.

Valeur totale du credit devaluationx 0,50

Evaluation totale demandde

Certification Verifying Statement of Costs

l hereby certify:that the amounts shown are as accurate as possible and these costs were Incurred while conducting assessment work on the lands shown on the accompanying Report of Work form.

that

to make this certification

0212(04/911

Attestation de l'6tat des couts

J'atteste par la presente :que les montants Indlques sont le plus exact possible et que ces depenses ont et6 engagees pour effectuer les travaux devaluation sur les terrains indiques dans la formule de rapport de travail ci-joint.

as ___AcifwT"____________ l am authorized Et qu'a titre de(llsaoH/a j Holder, Agent. P-Mitton In Company) (titulalre en

je suls autoris6(titulalre enreglstre, representant, poste occupe dans la compagnle)

faire cette attestation.

Date

Nota : Dans cette formule, lorequII ddslgne des personnes, le maseulin est utilise1 au sens neutre

OJ

\ ,

Ol

O

-OSEH

2

CD

GT O

OJroO

l CD

ARfASJ/VITHDRAVyN FR0M DISPOSITION

M.R.O. - MINING RIGHTS ONLY

S.R.O. - SURFACE^RIGHTSONLY

M.+ S. - MINING AND SURFACE RIGHTS

D**crtption Order No. Dite Disposition Fit*

CROWN RESERVE

THE INFORMATION THAT APPEARS ON THIS MAP HAS BEEN COMPILED FROM VARIOUS:SOURCES, AND ACCURACY IS NOT GUARANTEED. THOSE WISHING TO STAKE MIN ING CLAIMS SHOULD CON SULT WITH THE MINING RECORDER, MINISTRY OF NORTHERN DEVELOP MENT AND MINES, FOR AD DITIONAL INFORMATION ON THE STATUS OF THE LANDS SHOWN HEREON.

SWAYZE TWP.' |M

TICOECLIUATION

9- WEST

rf————p————l 740067 l- 740078 l 799011

* 7 f S f : m j 740066 j 7407)9 f i 'f,

— --4Ptl854*fl L l- —— — ^

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1182489(2 U N!

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642069 l .1182820 (12 UNITS)

*^ ---L--___ JJ

90034 (4 UNITS)

1189871(10 UNITS)(9 UNITS)

(18285:(9TJNITS)

1182824

BLAMEY TWP.

LEGENDIf S,

SUM .^ i t(J LINESTOWNSHIPS. BASt LiNES ETC irns M4NINC, ( l A;MS

UNSiJH w F: ^ M) l

^^^^ ^^^^Jg&^gj^

Mi\'N^ , ri AIMS t T 'RA 1 ! ,\ .'^ A\U HIGH! OP WAV

urn ' ' - t iNt sNi f, *" H^ NNiAL SlHt AM

F UM ;.-iNl.j OR F LOOOING RIGHTS

Si lil 'v'SlfJN OR COMPOSITE PLAN

M t St HV A'TiQNS

ORIGINAL SHORELiNEMARSH OR MUSKEG

MINES

TRAVERS!

r nzTim.ô-^^P^-^g^

DISPOSITION OF CROWN LANDS

TYPE OF DOCUMENT S YMBOL

PATENT. SURFACE 81 MINING RIGHTS ,. "- 0. SURF-ACE RIGHTS ONLY . 6.MINING RIGHTS ONLY , O

LEASE. SURF ACE A MINING RIGHTS BSURFACE RIGHTSONLY ".. . . v. BMINING RiGHTSONLY .. . B

LICENCE OF OCCUPATION . ,. . . . . . TORDER 'N COUNCIL . OCRESERVATION ,. (J)CANCELLED . . ' ®SAND&GRAVEL ...^ .... . ©

NOTE M INING,,RKiHTS IN P ARC, f i S PATtfs/ltO PRIOR |O M AY 6 1913 VESTED I N ORIGINAL PATENTEE B V T ME P UBLIC LANDS A CT R SO 1 970 CM A P 380. SEC 63 SU6SEC 1

i.00 1000M el res

10 O 10 20 30 40 ^0 60 70Chain*

SCO O 1000 2000 3000 *000 SOOOFeet

SCALE 1:20 000

THIS TWP. IS SUBJECT TO FOREST ACTIVITIES IN IME/93

FURTHER INFORMATION AVAILABLE ON FILE.

TWPJS-aUBJECT TO FOREST ACTIVITY IN ?998 W4. (HFCWMATION ON FILE.

TOWNSHIP

CUNNINGHAMMN R ADMINISTRATIVE DISTRICT

CHAPLEAUMINING D IVISION

PORCUPINELAND TITLES/ REGISTRY DIVISION

SUDBURYn^

Ministry of Ministry ofNatural Northern DevelopmentResources and Mines

OntarioDa " AUGUST, I986

G-1095

-OJ

olo

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X CD

C O

f*

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41010NE9109 41 CUNNINGHAM 200

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P-1030183

P-1U30180

P-1030187

P-1030182 --EOH 149m

P-1030188P-1176988 P-1176989

P-1030189

-0176990

P-11769P-1176993

PROPERTYDRILL PLAN

EXPLORATION CO. LTD.41010NE9189 41 CUNNINGHAM2TW-CP1

01/05/12

Documents

DD RPT 41 CUNNINGHAM - Ontario...DIAMOND DRILL CORE LOG Sheet No. -OF. Project No. 206 Hole No. TOW-91- T Surface DIP AT COLLAR-45' BEARING - 090" Test Depth 60m Dip-44.5" Magnetic