42B01NE0050 2.16749 KENOGAMING 010

GEOLOGICAL REPORT

on the

ROSS AND TRIPLE L

PROPERTIES

PENHORWOOD TOWNSHIP DISTRICT OF SUDBURY

KUKATUSH AND SEWELL LAKE AREAof

NORTHERN ONTARIO

for

BAND-ORE RESOURCES LTD.

'g". 16749

June 19, 1995 By: J. Kevin Filo HBSc., P. Geo

42B01NE0050 2 16749 KENOGAMING

TABLE OF CONTENTS

INTRODUCTION...................................... . . . . . . . . . l

PROPERTY........................ . . . . . . . . . . . . . . . . . . . . . . . . . . . 2

LOCATION AND ACCESS........................... . . . ..... . . . . .3

TOPOGRAPHY. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 4

GENERAL GEOLOGY................................ . . . . . . . . . . . . 4

AREA AND PROPERTY HISTORYROSS PROSPECT HISTORY............................. . . . .8TRIPLE L PROSPECT HISTORY.............................10

PROPERTY AND ECONOMIC GEOLOGYROSS PROSPECT.........................................11TRIPLE L PROSPECT.....................................14

CONCLUSIONS AND RECOMMENDATIONS............................17ROSS PROSPECT RECOMMENDATIONS.........................18TRIPLE L PROSPECT RECOMMENDATIONS.....................18

BIBLIOGRAPHY

CERTIFICATE

01OC

Figure l : Figure 2A: Figure 2B: Figure 3 : Figure 4 : Figure 5A: Figure 5B: Figure 6 : Figure 7 :

FIGURES

General Location MapClaim Location Map for Ross Property Claim Location Map for Triple L Property Regional Geology MapPenhorwood Twp. Area Geology Map Adapted from Milne Ross Prospect Geology Map Reinterpretation Triple L Prospect Geology Map Reinterpretation Airborne Geophysics Map For Penhorwood Area Compilation Map for Penhorwood Twp. Adapted from D. Pyke

Tables

Table l Proposed Budget for Ross and Triple L Projects

Band-Ore Resources Ltd.II, IIRoss 8c TRIPLE L PROPERTIES

N

ROSS S TRIPLE "L PROPERTIES

Timmins\ .Vald'Or Quebec

Montreal

Ottawa

200 400 600

Figure 1

PROPERTY LOCATION MAP

JN15/95 PEN-F1.CDR

INTRODUCTION

In June of 1995, a request was made by Band-Ore Resources for

a field examination and report on their Ross and Triple L prospects

in Penhorwood Twp., District of Sudbury, Northern Ontario. The

purpose of this report was to review all pertinent documentation on

these prospects in order to make recommendations to further

evaluate unexplored portions of them. The data base utilized to

prepare this report was derived from various sources which included

published government geological reports, government airborne

geophysical maps, assessment file data, and my previous experience

in this area. Further, on June 15 of 1995, the author made a field

visit to the two prospects to obtain a "first hand" impression of

the limited geology exposed on these two properties.

The geographical location and regional geological setting for

the Ross and Triple L prospects are shown in the accompanying

figures. From Fig.3 it can be seen that the two subject properties

are located in an Archean Greenstone Belt, better known as the

Swayze Belt. This area has been explored intermittently for various

mineral commodities since the early 1900s; the area was

particularily active in the 1930's and has become continually more

active since 1946. This renewed exploration was likely assisted by

better accessibility. Consquently, a fairly comprehensive

historical data base comprised of government derived regional maps,

and assessment files from various public companies, and individuals

are available for the current area of interest.

Information from this data base shows that there are a number

of gold occurrences on or near the Bandor Properties, and thesel

MBand-Ore Resources LtdRoss PROPERTY

REEVES

PENHORWOOD

C Z

o o zU-l

ll 1159928

1190384 l(16 UNITS) j

j 1159929 l

1131524

1159926

1159927

i

11159921J 1159922

i

1193449 (2 UNITS)

MILES

0.5 1.0 2.0

Figure 2(a)CLAIM LOCATION MAP

Penhorwood Twp. (G-3244)

M 21/95 PEN-F2A.CDR

prospects are well located in a very favourable geological

environment for gold deposits. Of more significance perhaps, is

data from more recent work over the last decade which suggests that

geology in Penhorwood Twp., and a number of surrounding townships

distinctly resembles that found in the famous Porcupine Gold Camp.

These similarities include the same key stratigraphy, and marker

horizons, similar structure, including the Destor Porcupine Fault,

numerous porphyritic intrusives known to be spacially associated

with gold mineralization, as well as the presence of secondary

shear zones, and associated alteration patterns.

This report will show that the Band-Ore Properties in

Penhorwood Twp. are strategically located in a good geological

environment for gold with key structure, stratigraphy, alteration

and gold occurrences all similar to that found in Timmins.

Consquently, these prospects merit a substantial exploration

program to adequately explore their potential. Formal

recommendations, and an appropriate budget to carry out the

proposed work program will be presented in the following portions

of this report.

PROPERTY

The current land holdings of Band-Ore Resources in Penhorwood

Twp. consist of two specific claim blocks, the Ross Property, and

the Triple L Property. The Ross claim block is comprised of nine

contiguous claims or fifteen 40 acre units. The Triple L group is

made up of four contiguous claims made up of fifty-six (56) 40 acre

Band-Ore Resources Ltd.TRIPLE "L" PROPERTY

1201673 (16 UNITS)

1201677 (16 UNITS)

1201660 (8 UNITS)

1201676 (16 UNITS)

Figure 2(b)CLAIM LOCATION MAP

Penhorwood Twp. (G-3244)

JNP1 ( l- P HJ l JD.COH

units. The claim numbers and due dates for work for the individual

properties are tabulated below.

ROSS CLAIM No. UNITS DUE DATE TRIPLE L CLAIM No. UNITS DUE DATE

113152411599221159923115992611599271159928115992911934491190384

111111126

10/02/9510/09/9510/09/9512/02/9612/02/9612/02/9612/02/9605/16/9612/22/96

1201660120167612016771201678

08161616

01/03/9701/03/9701/03/9701/03/97

Actual claim locations in Penhorwood Twp. can be referenced in

Fig. 2A and 2B.

LOCATION AND ACCESS

The Ross property is located 1.5 miles south of the extreme NE

corner of Penhorwood Twp. The actual longitude and latitude for the

centre of this prospect is 82 degrees, 02 minutes W., and 48

degrees, 10 minutes N., respectively. This property is readily

accessible by road from the City of Timmins via Highway 101 W. and

the main Kenogaming Timber Rd. which cuts through the property. The

total road distance to access the property from Timmins is

approximately 50 miles.

The Triple L Property can be accessed by continuing SSW along

the main Kenogaming Timber road which accessed the Ross Property.

Approximately 6km. beyond the Ross Property the road crosses the

eastern portion of the Triple L claims. The actual longitude and

latitude of this prospect is 82 degrees, 07 min. W., and 45

degrees, 06 min. N., respectively.

a ^ '^^^j|g!^^^^^^^^^^^:liii-;- .jest 7~^^sfe^ B *. K*^-,' -Jx-i rvj-:,A5 N ^*j2U**^^.rW^[i.e .-*?c.i 1,,,^Ross ft

Triple "L Properties

:*Lir pfX^Wb^1 v? Sf^Wf ^aasauBiw jvfelCJft iP?|.- -3^^^^ip^^^.^fer-

:V:C : /M'V.Tjij . f-^j"^^^-^. W^ H'*iir^4 ; jiV' 1P VjsU^^-'*15; : ^ ,lv7. i ^a^^-iK-,' ,-' i ' M.*!"'! -i-Ci^^i-^'^.,i lAa^il^S

^jptjf^j^P^I\Tuu-tviVali.ll 5j^?vOW^T5.\.--.Vf.;'-,-'-?i*~-S^-jl

REGIONAL GEOLOGY OF NORTHERN ONTARIO

•^

LEGEND

fag COBALT GROUP CONGLOMERATE

['IS . GRANITE - GRANODIORITE

j,;.,2 GNEISSIC - TONALITE SUITE

[lo" 1 MAFIC - ULTRAMAFIC INTRUSIVES

B l COARSE CLASTIC SEDIMENTARY ROCKS

pjpi MIGMATIZED SUPRACRUSTAL ROCKS

[T^i METASEDIMENTARY ROCKS ' i E.G WACKE ARKOSE

6 FELSIC TO INTERMEDIATE I LJ METAVOLCANICS

MAFIC TO INTERMEDIATE METAVOLCANICS

E MAFIC TO ULTRAMAFIC METAVOLCANIC ROCKS

Figure 3

REGIONAL GEOLOGY OF

NORTHERN ONTATIO ADAPTED

FROMO.G.S. MAP 2545

Ontario Geological Survey 1991. Bedrock

Geology of Ontario, East-central sheet;

O.G.S Map 2543

coJormap.cOF jn 20J85

TOPOGRAPHY

The topography on both of the properties is typical of the

Canadian Shield. Recent air photographs and assessment file data

shows that the Triple L property appears to be covered by a number

of spruce bogs in the northern, western and eastern portions of the

property, while the central portion of the property appears to be

of slightly higher relief. Once again air photographs suggest this

may be a sand hill covered by pine and/or spruce. The property also

contains a series of pothole like lakes with fairly extensive

swampy areas around their perimeters. The western portion of the

property is cut by the West Branch of the Nat River. This west

portion of the property appears very swampy for about 0.5 miles

around the river. The author would expect that minimal rock

exposure is present on this prospect, perhaps in the order of 5%.

The relief, for the most part, on the Ross Prospect is

slightly higher. Prior to logging operations this area was covered

by extensive stands of jack pine existing on gently rolling hills.

Swampy areas exist around creeks and the Nat River which cut across

the property. Air photos and assessment file data show rock

exposure on this ground is fairly limited, probably less than 5%

overall.

GENERAL GEOLOGY

The Band-Ore Resources properties are located within an

Archean greenstone belt known as the Swayze Belt. It is the opinion

of a number of geologists, including this author that this belt

represents a western extension of the prolific mineral producing

4

PENHORWOOD TOWNSHIP GEOLOGY MAP

LEGEND

f 6 i DIABASE DIKE

LATE FELSIC INTRUSIVE ROCKS

MOSTLY GRANITE

EARLY FELSIC INTRUSIVE ROCKS

MOSTLY GRANITE

H

H

m

ULTRAMAFIC INTRUSIVE ROCKS

EARLY MAFIC INTRUSIVE HOCKS

DETRITAL META SEDIMENTS

FELSIC TO INTERMEDIATE META VOLCANICS

MAFIC TO INTERMEDIATE

META VOLCANICS

Figure 4

PENHORWOOD TWR, GEOLOGY MAP

SHOWING AREA GEOLOGY PROXIMAL

TO ROSS H. TRIPLE V PROPERTIES;

ADAPTED FROM O.G.S MAP 2231

Abitibi Belt located a few miles to the NW. The extent and location

of both of these belts can be best appreciated by examining the

Fig. 3; note, the the Porcupine Gold Camp centred around Timmins

exists near the western extremity of the Abitibi Belt.

A more detailed, but general picture of the regional geology

can be seen in Fig. 4 which has been adapted from O.G.S. Map 2231

by V.G. Milne. Accompanying Milne's map is Geological Report 97.

This author has utilized substantial portions of Milne's report to

give the following overview of the geology in Penhorwood Twp.

From Milne's map (Fig.4) it can be seen that the geology in

the general vicinity of the subject properties consists of a suite

of SW trending metamorphosed (greenschist facies) volcanic rocks of

Archean age. These volcanics are shown to range in composition from

mafic to felsic.

The mafic volcanics are basically andesitic or basaltic flows,

and in numerous instances, pillow structures are evident in these

mafics. Milne's report states that these sub aqueous flows probably

make up a substantial portion of the mafic volcanics in this area.

Other typical features normally found within mafic volcanics, other

than metamorphic features such as shears, are absent in the mafic

volcanics in this area.

No real mention is made of ultramafic flow units in Milne's

report or map, although there are numerous areas mapped as

ultramafic intrusives. Milne's mapping was done prior to

publications by Viljoen from S. Africa on Archean ultramafic flows,

and similar studies in Canada by Naldrett. A large number of

Milne's so called ultramafic intrusives contain what Milne calls

"chicken track" texture (unit 6c). This is currently called

spinifex texture and is usually a diagnostic feature representative

of ultramafic volcanism or komatiitic volcanics that usually

represent the basal portions of volcanic flows. Thus, many of the

sections colored in purple on Milne's map, particularily those

marked 6c represent ultramafic flow units rather than ultramafic

intrusives.

The felsic volcanics in Penhorwood Twp. are comprised of

tuffs, lapilli tuffs, and agglomerates, intermediate to felsic

flows, and probably, locally, some tuffaceous greywacke. In

Penhorwood Twp. the felsic volcanics are not as extensive as the

mafics. They are most prominent in the NE sector of the township

near its east boundary. These felsics represent the extreme western

extremity of a more extensive belt of felsics in adjoining

Kenogaming Twp. to the west. Milne describes this suite of felsics

as the Hanrahan Lake Complex.

Milne states in his report that the Hanrahan Lake Complex

forms the core of a major structural feature, namely a NW plunging

antiform fold. In Penhorwood Twp. this feature is enclosed on all

sides by mafic volcanics. A fairly continuous iron formation known

as the Nat River Iron Fm. marks the interface between the mafic

metavolcanics and the felsics of the Hanrahan Lake complex.

More recent studies by various independent geologists

including Dr. D. Pyke now suggest that the contact between the

Hanrahan Lake Complex felsics and mafics in Penhorwood is

important for a number of other reasons. Pyke's compilation-(Fig.7)

suggests this contact may represent one of the locations in

Penhorwood Twp. that the contact between the Tisdale and Deloro

volcanics is found. Also, just a short distance north of the

contact the Porcupine Destor Fault Zone is interprteted to be

present, this fault is spatially related to the gold deposits in

Timmins. In the Porcupine, the Tisdale Group volcanics which are

marked by a komatiitic ultramafic volcanic sequence are of major

economic significance, as this volcanic group is associated with

the majority of gold deposits in the Timmins area.

Milne points out in his report that there are a number of

intrusive events in Penhorwood and the surrounding townships, and

all of these have intruded the volcanic suites described above.

Milne divides these basically Archean aged intrusives into four

categories: early mafic intrusive rocks, ultramafic intrusive

rocks, early felsic intrusive rocks and late felsic intrusive

rocks.

All of the aforementioned lithologies have been intruded by

two swarms of Late Proterezoic aged diabase dykes.

Finally, all of the rock units mentioned above were covered by

a mantle of glacial debris made up of till, gravel, boulders and

sand during the Pleistocene. This glacial debris was then in turn

covered by more recent stream and swamp deposits.

AREA AND PROPERTY HISTORY

The area in and around Penhorwood Twp. has had a long history

of mineral exploration since the early 1900's. Peak periods of

7

exploration in this area occurred in the 1900's after discoveries

in the Porcupine, and again in the 1930's. After the second world

war, there was a resurgence in gold exploration in Ont. At this

time, a gold mine was discovered in Keith Twp.(Joburke Gold Mines)

adjoining Penhorwood Twp. This discovery helped spur exploration in

this area for many years to come. In the 1950's extensive

exploration was carried out in the area for other commodities as

well. These included asbestos, iron, nickel, copper and zinc.

Over the past fifteen years, there has been excellent access

developed to many areas in the NE sector of the Swayze Belt due to

logging; and consquently, ther has been a renewed interest in the

area by prospectors and mining companies. In recent months a number

of impressive new discoveries have been made. One of the more

interesting projects is the Glen Auden/Hemlo Gold Mines joint

venture in Sewell Twp. which recently announced a drill hole

intersection of 6.52 grams/tonne Au over a core lenghth of 11.9m. (N. Miner, Dec. 1994)

In the following portions of this section, an attempt will be

made to briefly summarize the past work carried out by previous

operators on the Ross and Triple L Prospects. This will be

presented on a company by company basis in chronological order

starting with the Ross Property first.

ROSS PROPERTY HISTORY:

Penko Gold Mines Ltd (1945)

This company controlled a larger block of claims near the intersection of Penhorwood, Sewell, Kenogaming and Reeves Twp. However, a portion of their block covered current claims 1193440, 1159922 and 1159923. Penko focused its exploration on a gold target some distance NE of the current Ross Prospect, but they did do a very cursory mapping job on the current claims that their block

8

covered. Also/ their geology map makes reference to a drill hole (Kl) from some previous program. This hole was drilled in the extreme SW corner of current claim 1193440. No logs or assays were avalable but the geology map shows that greywacke, chlorite schist and porphyry were intersected in this hole.

Kukatush Mining Corporation (1950*s)

In the 1950's, the Kukatush Mining Corporation examined extensive tracts of land in Keith, Penhorwood, and Kenogaming Twps. for iron deposits. A very small portion of their extensive Nat River Group extended over current claims 1159922, 1159923, 1159927, and 1193440. The data available suggests that some drilling was done on their Nat River Group, but collar location data is not available; thus the author was unable to ascertain if any of this drilling was done on the current subject claims. Most of this report dealt with their iron deposit on the Radio Hill property west of the Ross Prospect.

Karvinen and Associates/Quinterra Resc. Inc./BHP Mines (1983-1987)

Initially, a block of claims was staked by Dr. W. Karvinen in NE Penhorwood Twp. This block was approximately seventeen claims; this block covered a substantial portion of the current Ross Prospect including current claims 1159926-1159929 inclusive, and 1190384. Karvinen did some limited exploration in 1983 to evaluate his Nol gold showing (32-450 ppb Au); this work included sampling, mechanized stripping, winkie drilling and till sampling. The Nol showing proved to be a carbonate boulder. Despite this fact the environment on this property was significantly encouraging enough to option the property to Quinterra Resc. Inc.

Quinterra held the option on the prospect for approximately one year and carried out geological mapping, magnetic surveying, mechanized stripping and sampling. The data from this work is poorly plotted relative to topography, and somewhat incomplete. Apparently, this data was not filed initially. The claims lapsed and had to be restaJced; thus this data may have been donated, and not up to standard. In any event, it appears that substantial mechanized stripping and sampling was carried out on current claims 1190384, 1159929, and 1159920. Anomalous values were found in the bedrock in trenched areas. These better values from the trench sampling ranged from 200-630ppb.

Eventually, after one year Karvinen controlled his original block once again and carried out a mapping program prior to reoptioning the ground to Utah Mines.

Utah carried out extensive geophysics including induced polarization, magnetics, VLF-EM and horizontal loop EM. They then drilled four holes, one on current claim 1193084 and a second on a coincident Au and geophysical target a few hundred ft. south of the current 1159926. This hole intersected mafic volcanics, mafic shists, serecitic fushitic shists, and intrusive feldspar porphyry. No assays were published and no further work was recommended. The hole drilled a few hundred feet south of current claim 1190384

9

intersected substantial zones of pyrite mineralization in mafic tuffs and felsic intrusives. Further work on this zone was recommended but not done.

Glen Auden ResourcesXAmerican Barrick (1987-1992)

Glen Auden currently controls an interest in a large package of land NW of the Band-Ore Ross package. At one time, the Glen Auden holdings also included current claim 1131524. Glen Auden carried out till sampling on this claim. Till sampling showed extremely anomalous gold values in the till, in the order of 7380ppb Au. Bedrock samples from associated trenching were not anomalous in gold but were anomalous in Cr and arsenic. The anomalous bedrock was an ultramafic unit. Geophysics was later carried out in this area by Glen Auden. In 1989 American Barrick drilled a hole into this target zone. The log showed most of this hole was mainly basalt intruded by a few felsic intrusives. Gold values were found to be anomalous at best.

Morin, Ross et al. (1990-1992)

The current subject block was worked by the vendors prior to optioning to Band-Ore Resources. The work by the prospectors involved stripping, blasting, trenching and sampling. Some encouraging results were obtained on current claim 1131524 where sampling turned up values ranging from 0.008 to 0.043 oz./ton Au. Work on a massive sulphide zone was initiated on current claim 1159927 but values here were low. Also, stripping and sampling work were carried out on a zinc zone. Values here were very good ranging from 240ppm to 47100ppm Zn, with the majority of the values well over lOOOOppm. A number of good silver values were also obtained with the zinc, some over 0.5 oz./ton Ag. This zinc zone is believed to be the same one documented on Karvinen's maps but there are some minor discrepancies regarding location.

Noranda (1992)

Prior to 1992, Noranda controlled what is now claim 1190384 and some claims further to the south as well. In 1992, they drilled a hole along strike of Utah Mine's hole just south of the current subject property boundary and intersected greywacke, basalts, and ultramafics at the end of the hole. No assays were published and no recommendations were filed.

TRIPLE L PROPERTY HISTORY:

Burtho Gold Mines Ltd. (1947)

This file is the only file that shows any private work being done in the immediate area of the Bandor Triple L claims. Work by Burtho Gold Mines consisted of geological mapping and prospecting; however, only a portion of the original Burtho claims covered the

10

current Triple L holdings. The western extremity of the Burtho claims covered claim 1201676. Mapping in this area shows that some of the area is covered by mafic volcanics which have been intruded by porphyritic intrusives and late diabase dykes. No mineralized zones or assays were reported from the area currently covered by the Triple L claims.

PROPERTY AND ECONOMIC GEOLOGY

Ross Prospect:

A reasonable idea of the geology existing on the Ross Property

can be obtained by reviewing a geological compilation shown in Fig.

5 and the airborne magnetics data for the property shown in Fig. 6.

This reinterpretation of the geology on the Ross Prospect was

recently completed by this author. A variety of sources were used

to develop this picture; these included property scale mapping,

ground geophysics data, drill logs, government maps, and

independent compilation data by Pyke.

From Fig.4, it can be seen that the geology on the subject

property is comprised of a suite of intercalated volcanics ranging

in composition from ultramafic to felsic. This volcanic suite has

been intruded by a large porphyritic felsic intrusive which appears

to occupy a substantial portion of the western part of the

property. These lithologic units have been cut by a series of late

diabase dykes. Data from Dr. D. Pyke (Fig.7) suggests that the

lithological units on the subject property are stratigraphic

equivalents of those found to host the numerous gold deposits in

Timmins. These two groups are the Tisdale and Deloro Groups. The

upper Tisdale Group i s the group which is associated with the vast

majority of deposits in Timmins. More specifically, there is a

11

Band-Ore Resources Ltd.Ross PROPERTY P- l A.

H l *GLEN AUDEN l BARRICK ZONE Q | ~

l

———f" Xwith intercalated

iron formation

UTAH ZONE

MILES

05 1.0 2.0

DIABASE

[71 EARLY FELSIC INTRUSIVE — (PORPHYRITIC)

[^1 ULTRAMAFIC VOLCANICS

6c CARBONATIZED ULTRAMAFICS

| 2 | FELSIC VOLCANICS

[T] MAFIC TO INTERMEDIATE VOLCANICS

x Au GOLD SHOWINGS

X Zn ZINC SHOWINGS

-- —- MINERALIZED TREND

— —— INTERPRETED FAULT

Figure 5(A)GEOLOGY INTERPRETED FROM

KARVINEN, PYKE, UTAH MINES, A O.G.S. MAP 2231JN 21/95 PEN-SACDR

distinct association between gold deposits in Timmmins and the

generally carbonatized ultramafic komatiitic volcanics making up

the lower portion of Tisdale Group.(Pyke, GR219) Further, Pyke has

projected the Destor Porcupine Fault Zone to cut across the SE

extremity of the property; this structure has a distinct spacial

association with the gold deposits in Timmins. In Timmins, all gold

deposits are within 6km. of this fault and all deposits with only

one exception are located on the N. side of the fault. (Pyke, GR219)

Also, it is the opinion of some geologists, including this a

author, that in Timmins, porpyritic intrusive bodies were one of

the keys to the deposition of gold deposits. Intrusive porphyritic

bodies such as the Pearl Lake Porphyry at the Maclntyre and

Hollinger Mines fractured the rocks and likely prepared a "plumbing

system" for mineralizing solutions.

From these last two paragraphs, it can be seen that the Ross

Property appears to have all the right features necessary to host

gold deposits similar to those found in Timmins. These once again

include, Tisdale Group stratigraphy with a carbonatized ultramafic

basal section, proximity to the Destor Porcupine Fault, and the

presence of porphyritic intrusives on the property.

Further, exploration efforts to date have shown that there are

a number of anomalous, gold occurrences ranging from a few hundred

ppb Au to 0.043 oz./ton Au on this property in this rather

favourable environment. Numerous other gold occurrences exist just

off the property, such as the one worked by Utah Mines and Noranda

just a few hundred feet south of claim 1190384.

12

Although substantial exploration efforts have been conducted

over this property in the past, they have by no means exhausted the

exploration potential of the prospect. The principal reason for

this, is that gelolgists have only been allowed to look at a small

portion of the rock on this prospect due to overburden and some

limited drilling. Exploration efforts to date basically involved

extensive geophysics and mechanized stripping and sampling where

overburden permits. Ironically, from a review of past work the most

successful technnique for finding gold on this prospect to date has

been mechanized stripping and sampling by prospecting crews.

It is this author's opinion, that when future exploration is

carried out on this prospect a reevaluation of the stripped areas

by Quinterra, and Morin should be given priority. This could be

carried out in conjunction with remapping of the property and

further mechanized stripping and sampling. After this preliminary

phase of work is complete, it would be prudent to reexamine all

geophysical data relative to known occurrences of gold to see if

there may be any subtle features that may have been overlooked by

previous operators. Also, portions of the property that do not

appear to have been adequately covered by geophysics, possibly the

extreme eastern section of the property, may warrant further ground

geophysics. A more detailed account of the program to be carried

out on 4his prospect is presen4ed in the closing section of this

report under recommendations.

The reader should also be aware that there have been some

significant favourable changes in gold mining economics in Timmins,

13

that may or may not enhance certain exploration properties. In the

last 24 months mining operations in Timmins have significantly

expanded their milling operations, and have begun to mine higher

tonnages of low grade open pit ore. Consquently, milling costs at

operations such as Placer-Dome or Royal Oak Mines are now in the

order of six to seven dollars per ton, and mining costs are three

dollars per ton. (personal conun.) Thus, exploration prospects

within 50-60 miles of Timmins, with reasonable access roads, and

potential for even small low grade pittable gold deposists are now

of significant interest, as these types of properties could be

joint ventured with established majors.

This type of situation was out of the guestion when most of

the exploration was carried out at the Ross Prospect. Currently,

grades in the 0.05-0.07 oz./ton when found near surface over

reasonable widths would be of significant interest today. This type

of exploration target should be kept in mind when this area is

being explored in the future.

Up to this point, all discussion on the Ross Prospect has been

focused on gold. A cursory examination of the showing with

excellent zinc values noted by Morin, Ross et al. and Karvinen

should be reexamined as well to evaluate its base metal potential,

and at least ascertain if it merits further work.

Triple L Prospect:

Once again, a reasonable picture of the geology on a property

scale on and near the Triple L Prospect can be seen by reviewing

the recently completed reinterpretation in Figure 5B.

14

Band-Ore Resources Ltd.M, HTRIPLE L PROPERTY

N

[s] LATE FELSIC INTRUSIVE

[T] EARLY FELSIC INTRUSIVE— (PORPHYRITIC)

|jF] ULTRAMAFIC VOLCANICS

6b INTERPRETED FROM MAGNETIC DATA60 OUTCROP ASSISTED l NTERPRET.

[Y] FELSIC VOLCANICS

[T] MAFIC TO INTERMEDIATE VOLCANICS

Figure 5(B)GEOLOGY INTERPRETED FROM

BURTHO GOLD MINES, PYKE, A O.G.S. MAPS 2231 d 2205

JN 22/95 PEN-5B.CDR

Airborne Electromagnetic Survey Total Intensity Magnetic Survey

GEOTEM®Peak Response Symbols

ANOMALY DECAY INTERVAL CLASSIFICATION

-3p- 1 -2 Channel (393 546 microseconds;

~~®~ 3-4 Channel (705. 862 microseconds i

~^~ 5-6 Channel [1018, 1174 microseconds)

~*?~ 7-8 Channel (1330, 1487 microseconds]

-^- 9-IOCnannol ( 1643, 1799 microseconds)

-•- 11-12 Channel fiB55, 2112 microseconds)

Magnetic Contours ———————- 10 Gamma Contour bie

50 Gamma Contour bne 250 Gamme Contour bne

Apparent Conductance

Cn 4 Amplitude [ppm)

Culture ResponseAnomaly LeOer ^ Q

Mole ResponseE dearly idantif ablest OwerbLirden art not represenled on This map

Mean magnetomelet saneof aftrtude ....... 120 metresMean electromagnetic senior amtude . .40 me ires. Mean flighi line spacing . ...... . ... .. .200 meiresFfcghl lines ..... . .. .. ..... . . 250 N -—.__^ .

Figure 6AIRBORNE ELECTROMAGNETIC

SURVEY - TOTAL INTENSITYMAGNETIC SURVEY from

Ontario Geological Survey 1990.Airborne Electromagnetic and Total

Intensity Magnetic Survey, NorthSwayze - Montcalm Area.

O.G.S. Maps 81378, 81377, B31S4

Reinterpretation by the author on this prospect relied heavily on

government airborne magnetic maps, minimal assessment file data by

Burtho Gold Mines, and D. Pyke, and some government maps.

Milnes Map (Fig. 4) and Pyke ' s Compilation Map (Fig. 7), both of

which existed prior to recent airborne data show the vast majority

of the Triple L property to be covered by felsic intrusive units.

Mafic units cover a small section of the NE sector of the property,

and ultramafic to mafic volcanics appear to exist along the

southern margins of the property. From Fig. 5B it can be seen that

it is this author's contention that there are significantly more

ultramafic, and/or mafic volcanics underlying the central portion

of the Triple L claims. The principal proof to support this idea is

the recent new government airborne map (Fig.6) showing a distinct

strong magnetic trend, typical of more mafic units, that

corresponds with ultramafic and mafic exposures along the southern

extremity of the property.

Again, as in the case of the Ross Prospect, above data from

Pyke's Compilation Map (Fig.7) suggests that the portions of the

Triple L claim block are underlain by lithological units that are

stratigraphic equivalents of the Tisdale Group in Timmins. This

group is of particular significance because of the number of gold

deposits associated with the basal ultramafic sequence of the group

in the Timmins Area. From this author's interpretation in Fig. 5B

this prospective ultramafic sequence may cover a more substantial

portion of the Triple L Property than originally interpreted by

Milne or Pyke. The relationship of the geology on Triple L Prospect

15

Band-Ore Resources Ltd.

REEVES TWP

TISDALEGROUP

VOLCANICS

North Splay

SEWELL TWPPENHORWOOD TWP A f.saw \ i*-'---"--""vM^- KENOGAMING TWP

Ross Property

PORCUPINEGROUP

SEDIMENTS

TISDALEGROUP

VOLCANICS

V-Wr-'TGABBRO

LMIITKVO

DELOROGROUP

VOLCANICS

TISDALEGROUP

VOLCANICS

KUKATUSH STOCK Triple "L" Property

DELOROGROUP

VOLCANICSJN 21/95 PEKJ-F7.Kif

N

DELOROGROUP

VOLCANICS

MILES

1.0 3.0

KENOGAMISSI BATHOLJTH

REGIONAL GEOLOGYFigure 7

STRATIGRAPHIC GEOLOGICAL INTERPRETATION FROMASSESSMENT FILE T3139 FOR R.S. MIDDLETON EXPLORATIONSERVICES INC. BY D.R. PYKE AND ASSOCIATES INC., ADAPTED

TO COVER THE ROSS AND TRIPLE 'L' PROPERTIES;

to the important Destor Porcupine Fault Zone is not exactly clear

in Pyke 1 s interpretation, (Fig. 7) and its location is subject to

some conjecture due to overburden and the presence of a large

intrusive body. The fault and current stratigraphy found on the

Triple L prospect may have been shifted southwards by one of the

numerous late dextral faults evident in Penhorwood Twp. It is

interesting to note that a major topographic linament stretches

from Hardiman Bay (Fig.3) in a NW direction towards the Triple L

Prospect. This linament may represent the Destor Fault Zone on the

Triple L Prospect. The projection of this linament is shown on Fig.

5B. The Triple L Prospect like the Ross Prospect above, also has

a number of feldspar porphyritic intrusives present on it as shown

on Milne's Map (Fig. 4) and in documented assessment file data from

Burtho Gold Mines.

From the preceding paragraph, it can be seen that the Triple

L Prospect similarily displays key characteristics known to be

associated with gold deposits in the Timmins area. However, this

property has had little or no exploration carried out on it and is

covered by substantial amounts of muskeg and overburden.

Consquently, this property will require extensive ground geophysics

including, ground mag and perhaps some indudced polarization (I.P.)

where warranted to help define favourable horizons, alteration

zones, structure, and/or mineralized horizons. Upon completion of

these surveys, some limited mapping may be warranted depending on

outcrop encountered. It is anticipated that exposure will be

extremely limited on this property. If any zone of mineralization

16

is exposed in outcrop, this could be targeted for stripping and

sampling where warranted. A more detailed discussion on the

recommendations for this project are presented in the closing

section of this report.

CONCLUSIONS AND RECOMMENDATIONS

Band-Ore Resources properties in Penhorwood Twp. are located

in what is known as the Swayze Greenstone Belt, this belt is

interpreted to be the western extension of the Abitibi Greenstone

Belt. The lithological units in Penhorwood Twp. are thus considered

to represent the same prolific gold bearing volcano-sedimentary

sequence found in the western Abitibi Belt in the Porcupine Gold

Camp, which has produced over 60,000/000 oz. of gold.

Penhorwood Twp., and more specifically the areas covered by

Bandor properties in Penhorwood are crosscut by a southwest

trending auriferous deformation zone. It has been interpreted that

this structure may very well represent the westerly extention of

the Porcupine Destor Fault which is spatially associated with all

of the gold mines in the Porcupine.

Also, previous exploration and government data shows there are

a number of strong alteration zones, secondary structures, and gold

mineralization on the Band-Ore Properties.

In light of the excellent environment for Porcupine style gold

mineralization on the Band-Ore ground, an exploration program to

further evaluate these prospects should be initiated as soon as

possible. Detailed recommendations for work on the specific

17

TABLE 1

BUDGET FOR ROSS AND TRIPLE L PROPERTIES

PHASE 1

Linecutting: 60 km. @ SSOO/km:

Geophysics:a) Magnetics and VLF-EM: 60km. @ SI 75 per km:b) Induced Polarization: 30km. @ S1000 per km:

Stripping, trenching, sampling, geological mapping, A prospecting:

18,000

11.00030,000

20.000

PHASE 2: Diamond Drilling

6500 feet of NQ @ S30 per foot: 195.000

Sub-total 274.000Contingency (approx. 1007o) 26.000

GRAND TOTAL (S) 300.000

NOTATION:

Phase 2 will be carried contingent that phase 1 is successful.

^^--^W#

properties have been laid out in the following section in-point

form, and appropriate budgets for these programs are shown in the

accompanying table l .

Ross Prospect Recommendations

1) Reestablish a new control grid over the entire property, and carry out a mapping program to reexamine the geology and locate all previous showings and pits. Some cursory preliminary sampling of these pits by the mapping crew is likely warranted initially, prior to a more detailed follow up later.

2) After mapping is completed, and all pits and potential new surface zones evaluated, all geophysics carried out to date should be examined again to see if there are any subtle signatures associated with known gold mineralization. If at this time further geophysical information is required, this should be done immediately.

3) Carry out a mechanized trenching and stripping program to expand known zones of surface gold mineralization and evaluate potential new areas where overburden permits. Upon completion of the stripping program all pits and trenches should be mapped and sampled in detail.

4) Diamond drilling should be considered for all targets that warrant it. Some priority should be given to targets with potential for a low grade pittable deposit.

TRIPLE L Prospect Recommendations:

1) Similarily, a control grid should be cut over the entire Triple L Prospect.

2) Preliminary geophysical surveying, namely ground magnetics, should be carried out over the entire property to define lithologies, particularly the key ultramafic horizons, and porphyritic intrusives as well as structure, and alteration. When this survey is completed, priority areas should have an induced polarization survey carried out over them to define potential zones of mineralization.

3) Once the grid has been walked by geophysical crews, mapping should be completed in areas where suffient exposure exists. If by chance surface mapping or prospecting detects any near surface mineralized zones or structures these should be stripped by mechanized means, washed and sampled.

18

4) Diamond drilling should be considered for all priority targets.

Respec^f

J.

19

BIBLIOGRAPHY

Arnott, B.1947: Private Geological Report for Burtho Gold Mines,

Penhorwood Group, on file in the Resident Geologists Files, Ministry of Northern Development and Mines, Timmins, Ontario.

Barrick1989: Private Diamond Drill Information for Barrick Resources

Glen Auden Option, on file in the Resident Geologists Files, Ministry of Northern Development and Mines, Timmins, Ontario.

Glen Auden1987: Private Geological Reports for Glen Auden Resources,

on file in the Resident Geologists Files, Ministry of Northern Development and Mines, Timmins, Ontario.

Kukatush1955: Private Geological Files for Kukatush Mining Corp, Radio

Hill Property, Keith Twp. Property, and Nat River Property, on file in the Resident Geolgists Files, Ministry of Northern Development and Mines, Timmins, Ontario.

Karvinen, W.1986: Private Geological Report for Karvinen and Assoc.,

Penhorwood Property, on file in the Resident Geologists Files, Ministry of Northern Development and Mines, Timmins, Ontario.

Milne, V.G.1972: Geology of the Kukatush-Sewell Lake Area, District of

Sudbury; Ont. Div. Mines, GR97, 116p. Accompanied by Maps 2230, 2231, Scale lin. = 0 .5 miles.

Morin1992: Private Prospecting Reports for Morin et al.,

Ross Prospect, on file in the Resident Geologists Files, Ministry of Northern Development and Mines, Timmins, Ontario.

Noranda1992: Private Diamond Drill Log for Noranda Exploration,

Penhorwood Twp., on file in the Resident Geologists Files, Ministry of Northern Development and Mines, Timmins, Ontario.

N. Miner1994: Northern Miner Newspaper, Dec. 19, 1994.

O.D.M.1974: Chapleau-Folyet, Geological Compilation

Series, Algoma, Cochrane, and Sudbury Districts; Ontario Division of Mines, Map 2231, Scale lin =4miles.

O.G.S.1990: Airborne Electromagnetic and Total Intensity Magnetic

Survey, North Swayze-Montcalm Area, Ontario Geological Survey Maps 81377, 81378, 81384. Scale 1:20000

1991: Bedrock Geology of Ontario, east-central sheet; OntarioGeological Survey, Map 2543. Scale 1:1,000,000

Pyke, D. R.1982: Geology of the Timmins Area, District of Cochrane;

Ontario Geological Survey Report 219,141p. Accompanied by Map 2455, Scale 1:50000, 3 charts, and l Sheet Microfiche.

1987: Private Compilation Map for R. S. Middleton Exploration Services Inc., Kukatush River Area; on file in the Resident Geologists Files, Ministry of N. Development and Mines, Timmins, Ontario.

Quinterra1984: Private Geological and Geophysical Reports for

Quinterra Resources Inc. Penhorwood Twp.; on file in the Resident Geologists Files, Ministry of Northern Development and Mines, Timmins, Ontario.

Utah Mines1987: Private Geophysical and Diamond Drill Logs for Utah

Mines, Penhorwood Twp; on file in Resident Geologists Files, Ministry of Northern Development and Mines, Timmins, Ontario.

CERTIFICATE

I, J. K. Filo of 535 Bartleman of the City of Timmins, Ontario do hereby certify:

1) I have personally written this report on the Ross and Triple L Prospects for Bandor Resources Inc. and I have based the opinions contained in this report on a personal property examination, a review of all pertinent government data, and historical information available, and my own past experience in this area.

2) I further certify that I have no personal interest in these prospects or the securities of Bandor Resources Inc., nor do I expect to receive any interest in the future, other than my professional fee.

3) I hold an Honours BSc. (1980) in Geology from Laurentian University in Sudbury, Ontario. I have been practicing my profession as both a mining and exploration geologist for the past fifteen years in Canada, Mexico, and SE Asia. I have been employed by various mining companies in a variety of geological capacities prior to carrying out consulting work on my own. Some of these companies include Texasgulf Exploration Inc., Amax Exploration, Cominco (Pine Point Mines), Giant Yellowknife Mines (Pamour Div.), Nerco Con Mine, Freeport-McMoran Copper and Gold.

4) I am a professional geologist in good standing with the Association of Professional Engineers, Geologists, and Geophysicists of Alberta (Reg. No.41399), and a member in good standing of the Association of Professional Engineers and Geoscientists of B.C. (Reg. No. 18677)

33ibrfotted,•"•'^-^

J. K L Filo 'P-P ~ "

Ministry ofrthern Development

and MinesOntario

Report of Work Conducted After Recording Claim

Mining Act

Transaction Number

Personal information collected on this form is obtained under the authority of the Mining Act. This information will be used for correspondence. Questions about this collection should be directed to the Provincial Manager, Mining Lands, Ministry of Northern Development and Mines, Fourth Floor, 159 Cedar Street, Sudbury, Ontario, P3E 6A5, telephone (705) 670-7264. n

Instructions: - Please type or print and submit in duplicate.- Refer to the Mining Act and Regulation

Recorder.- A separate copy of this form must be c- Technical reports and maps must acco- A sketch, showing the claims the work

" ; ning

42B01NE0050 2 16749 KENOGAMING 900

Recorded Holder(s) Client No.

Telephone No.

Mining Division

PTownship/Area' M or G Plan No.

Dates Work Performed

From:

Work Performed (Check One Work Group Only)Work Group

Geotechnical Survey

Physical Work, Including Drilling

Rehabilitation

Other Authorized Work

Assays

Assignment from Reserve

Type

ures/o* ,c^ '^fe/txnr f SWQ^

RECEIVED

C;FP 10 1996

MINING LANDS BRANCH

Total Assessment Work Claimed on the Attached Statement of Costs

Note: 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

Ac o : 5^3

(attach a schedule If necessary)

Certification of Beneficial Interest * See Note No. 1 on reverse side

l certify that at the time the work was performed, the claims covered in this work report were recorded in the current holder's name or held under a beneficial interest by the current recorded holder.

(Signature)

Certification of Work Report\ 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 aftor its completion and annexed report is true.

ddress of Person Certifying .^

CQ^rCertifi^ By/Sipnatrfre)Telepone No. Date

fFor Office Use Only

Total Value Cr. Recorded Date Recorded

,. . ,'ate Notice for Amerfdments Sent

0241 (03/91) 'PdftCUPINE MINING DIVISION

3 3 it tr

-C^ o

^s-o

•O

Ni

c

o S.Us

^^

fst%< TJ-rs

f0 Nis'a*

oj^

S10

a

oS.

Reserve

"^**t

M

1

,-.

5 >

glff3 2.

ea~n ^ 5.^5?

IIPat

Credits you are claiming in this report may be cut back. Th order to minimize the adverse effects of such deletions, please indicate from which claims you wish to priorize the deletion of credits. Please mark (^) one of the following:

1. Cj/Credits are to be cut back starting with the claim listed last, working backwards.2. H Credits are to be cut back equally over all claims contained in this report of work.3. D Credits are to be cut back as priorized on the attached appendix.

In the event that you have not specified your choice of priority, option one will be implemented.

Note 1: Examples of beneficial interest are unrecorded transfers, option agreements, memorandum of agreements, etc., with respect to the mining claims.

Note 2 : If work has been performed on patented or leased land, please complete the following:

l certify that the recorded holder had a beneficial interest in the patented or leased land at the time the work was performed.

, i.hern DevelopmentMines

Ministers dupeveloppement du Nord et des mines

Statement of Costs for Assessment Credit

Etat des couts aux fins du credit devaluation

Mining Act/Loi sur les mines

Transaction No./N 0 de transt

r'personal information collected on this form is obtained under the authority of (he 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 conlenus dans la presenle formule sont recueilhs en vertu de la Loi sur les m ines et serviront a tenir a jour un registre des concessions minieres Adresser toute quesiton sur la collece de ces renseignements au chef provincial des terrains miniers, Tiinistere du Developpement du Nord et des Mines, 159, rue Cedar, 4 e etage, Sudbury (Ontario) P3E 6A5, telephone (705) 670-7264.

1. Direct Costs/Gouts directs

Type

Wages Salaires

Contractor's and Consultant's Fees Oroits de ('entrepreneur et de I'expert- consell

Supplies Used Fournitures utllisees

Equipment Rental Location de materiel

Description

Labour Main-d'oeuvreField Supervision Supervision sur le terrain

T i - 4 c0(e^O^,(^jJ. f

'PrarV.^

Type

Type

Amount Montant

ST*--

Total Direct Costs Total des couts directs

Totals Total global

'5,7^

2. Indirect Costs/Couts indirectsNote: When claiming Rehabilitation work Indirect costs are not

allowable as assessment work.Pour le remboursement des travaux de rehabilitation, les couts indirects ne sont pas admissibles en tant que travaux d'evaluation.

Type

Transportation Transport

Food and Lodging Nourriture et hebergementMobilization and Demobilization Mobilisation et demobilisation

Description

Type

Amount Montant

Sub Total of Indirect Costs Total partiel des couts indirects

Amount Allowable (not greater than 20to of Direct Costs) Montant admissible (n'excedant pas 20 H des couts directs)Total Value of Assessment Credit Valeur totale du credit Total of Direct and Allowable d'evaluation Indirect costa) (Total des couti directs

Totals Total global

et Indirect* admissible*

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 titulaire enregistre sera tenu de verifier les depenses demandees dans le present etat des couts dans les 30 jours suivant une demande a eel eflet. Si la verification n'est pas effectuee, le ministre peut rejeter tout ou une partie des travaux devaluation presentes.

Filing Discounts Remises pour depdt

1. Work filed within two years of completion is claimed at 100 07o of the above Total Value of Assessment Credit.

1. Les travaux deposes dans les deux ans suivant leur achievement sont rembourses a 100 Vo de la valeur totale susmentionnee du credit d'evaluation.

2. Work filed three, four or five years after completion is claimed at SQo/o of the above Total Value of Assessment Credit. See calculations below:

Total Value of Assessment Credit Total Assessment Claimed

x 0.50 =

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 as j/ictf ' Xrvy/t/v.r f'V^^A* . \ am authorized(Recorded Holder, Agent, Position m Company)

to make this certification

2. Les travaux deposes trois, quatre ou cinq ans apres leur achievement sont rembourses a 50 0A de la valeur totale du credit d'evaluation susmentionne. Voir les calculs ci-dessous.

Valeur totale du credit d evaluation

X

Attestation de l'etat des couts

J'atteste par la presente :que les montants indiques sontdepenses ont ete engagees pour effectuer les travaux d'evaluationsur les terrains indiques dans la formule de rapport de travail ci-joint.

Et qu'a litre de. je suis autorise(titulaira anregistri, repr^sentant. poste occupe dans la compagnie)

a faire cette attestation.

02)2 (04/91) Nota : Dans cette formule, lorsqu'il designe des personnes, le masculin est utilise au sens neutre.

Ministry o fNorthern Developmentand Mines

September 13, 1996

Gary WhiteMining Recorder60 Wilson Avenue, 1st FloorTimmins, ONP4N 2S7

Ministers du Developpement du Nord et des Mines Ontario

Geoscience Assessment Office 933 Ramsey Lake Road 6th Floor Sudbury, Ontario P3E 6B5

Telephone: Fax:

(705) (705)

670-5853 670-5863

Dear Sir or Madam: Submission Number: 2.16749

Subject: Transaction Number(s): W 9560.00508

After reviewing the Work Report(s) we have prepared this letter and the attached summary, which lists the results of our review. Requirements of the Assessment Work Regulation may not have been fully met. Please examine the summary to determine the next course of action concerning the identified Work Report(s).

NOTE: The 90 day deemed approval provision, subsection 6(7) of the Assessment Work Regulation, is no longer in effect for this submission.

PLEASE NOTE ANY REQUESTED REVISIONS MUST BE SUBMITTED IN DUPLICATE.

If the anniversary dates for the mining claims affected by this correspondence have not passed, a number of options are available. Please contact the Mining Recorder to discuss these options.

If you have any questions regarding this correspondence, please contact Bruce Gates at (705)670-5856.

Yours sincerely,

ORIGINAL SIGNED BYRon C. GashinskiSenior Manager, Mining Lands SectionMines and Minerals Division

Correspondence ID: 10206

Copy for: Assessment Library

Work Report Assessment Results

Submission Number: 2 .16749

Date Correspondence Sent: S eptember 13, 1996 Assessor: B ruce Gates

General Comment:Although this particular submission has been deemed approved the work submitted is a compilation of previously published material and previously accepted documents and would not normally be accepted for assessment credit or be deemed approved in the future.

Transaction Number

First Claim Number

W9560.00508 1201678

Section:12 Geological GEOL

Township(s) l A rea(s)

PENHORWOOD

Status

Deemed Approval

Approval Date

March 03, 1996

Correspondence to:Mining Recorder Timmins, ON

Resident Geologist Timmins, ON

Assessment Files Library Sudbury, ON

Other Recorded Holder(s) and/or Agent(s):Robert Duess KINGSTON, ONTARIO

BAND-ORE RESOURCES LTD. WILLOWDALE, ONTARIO

Page: l

Correspondence ID: 10206

10 o

o

O 2

Z 3

J W

2

III—

—

- V

33 O

5 "

n <

H f

m ~

n >

o m

a 5

("l

—J

T1 r

— ^

-*

KEIT

H

TWP.

- J

~ "J •••

HI fei

vj

SJ

I ^

l

5 7

W ^

8

-v

" ~

" ~

~ -'

J027

W3

|P.!0

2792

0.

PJ0

27V

06

KEN

OG

AMIN

G

TWP.

J3 Z

(D

0)

qw

? 2

O

b w

i i.

5