apr l (j - ontario

41N13NE0ei4 2 .12369 P ILOT HARBOUR 010

APR l (J

ALOTTA RESOURCES INC.

REPORT ON 1988 EXPLORATION PROGRAM

ALOTTA-IN-BETWEEN PROPERTY

DAVID LAKES AREA, NORTHWESTERN ONTARIO

January 15, 1989Sault Ste. Marie, Ontario

Frank Pezzutto, M.Se. Geologist, Tundra Gold Mines

41N13NE0014 2 .18389 P ILOT HARBOUR 010C

TABLE OF CONTENTS

List of Figures... . , .. . .. . .. . . . . .. .. . . . . ... . .. . . .. .. .. . . .. . .3

List of Maps Enclosed With Report (in pocket)...............3

Ch. l Summary and Conclusions..,..... .... . .. .. .. . ....... .... .. .. . .4

Ch. 2 Introduction.................. . .. . .. . . . , . . . . . . . . . . . . . . , . . . . . 5

Ch. 3 Property....................... . .... . . . , . . . . . . . . . . . . . . . . . . . .6

Ch. 4 Location and Access.........................................9

Ch. 5 Topography and Vegetation............. . . . . . . . . . . . . . . , . . . . . . .9

Ch. 6 Climate............. . . , ...... . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .10

Ch. 7 Power......................................................11

Ch. 8 Water......................................................11

Ch. 9 Ancillary Services.................., .. . .. . . . . . . .. . . . . . .. .. 11

Ch. 10 Property History...........................................12

Ch. 11 Regional Geology.................,.........................13

Ch. 12 Property Geology...........................................1412.1 Mafic to intermediate volcanics............ .... . . . . . 1412.2 Intermediate to felsic volcanics.............. . ..... 1612.3 Metasediments.......................................1712.4 Basic-ultramafle intrusives.........................1712.5 Felsic intrusives.......................... .. .. ... . . 1812.6 Batholithic rocks.................................. . 1812.7 Late mafic intrusive rocks-diabase.........,..... ...1912.8 Pleistocene deposits................................ 19

Ch. 13 Structural Geology.........................................1913.1 Foliation....................................... . ...1913.2 Minor folds.........................................2013.3 Faults and lineaments...............................20

Ch. 14 Metamorphism...............................................21

Ch. 15 1988 Program...............................................2115.1 Line cutting........................................2115.2 Geochemistry (soils)................................2215.3 Prospecting.........................................2215.4 Trenching...............,...........................2215.5 Geologic mapping...,....................,...........23

Ch. 16 Mineralization............... .. . . . . . .. . . .. . . . ., . . . . . . . . .. . .2316.1 Laura Sulphide Zone.................................2316.2 Alotta Quartz Vein..................................2316.3 Kelemen Vein........................................24

Ch. 17 General Recommendations,...............................,...25

Ch. 18 Certificate of Qualifications..............................26

Ch. 19 References..................,............................,.27

Ch. 20 Personnel..................................................28

LIST OF FIGURES

Figure l Location map of the Alotta-In-Between property..............7

Figure 2 Map showing the distribution of the individual claims in the Alotta-In-Between claim block.............. ... . . .. .. ... . . .. .8

LIST OF MAPS ENCLOSED WITH REPORT (IN POCKET)

Map l Map showing line cutting results.

Map 2 Soil geochemical results for gold.

Map 3 Soil geochemical results for copper.

Map 4 Soil geochemical results for lead.

Map 5 Soil geochemical results for zinc.

Map 6 Soil geochemical results for arsenic.

Map 7 Geology map of the Alotta-In-Between property.

Chapter 1: SUMMARY AND CONCLUSIONS

The 33 claim Alotta-In-Between property, located approximately 65

km west of Wawa, Ontario, underwent a reconnaissance exploration

program during the summer and fall of 1988. The program consisted of

line cutting, prospecting, trenching, soil geochemistry {'B horizon')

and mapping.

The Alotta-In-Between property is situated along the narrow

southern limb of the Mishibishu Lake greenstone belt. The geology of

the property consists of a sliver of foliated metavolcanics and coeval

mafic intrusives bordered to the north and south by granitic

batholiths.

Mafic to intermediate metavolcanics are situated along an E-W

trending belt which parallels the baseline. Most of the said

metavolcanic units are fine grained, foliated or massive flows, but

porphyritic mafic units are also common. There is often a subtle

gradation from mafic porphyries to medium grained metadiorite and

gabbro. These units are likely intrusive or hypabyssal in origin.

Mafic tuffs were observed but only locally. They were recognized by

colour banding and intense foliation.

Intermediate to felsic metavolcanics are subordinate in volume and

exposure to their mafic counterparts. Porphyritic and fine grained

flows are the two common varieties. An E-W trending tuff-agglomerate

unit is situated along the north-central part of the property near

Sjogren Lake.

Medium-to coarse-grained diorite, mafic diorite and gabbro

comprises a 400 to 700' wide E-W trending belt north of the baseline.

This polyphase unit likely represents mafic intrusives associated with

mafic volcanism.

Spherical felsic intrusives of limited size are present on the

Alotta-In-Between property. The felsic intrusives are chiefly

granodiorite and are restricted to discrete phases in the granite

batholiths. The granite batholiths are volumetrically the most

abundant rock type on the property. The polyphase batholiths consist

of quartz monzonite, trondhjemite, hybrid granite phases and gneiss.

All rock types are intruded by late olivine-diabase dykes.

Only a preliminary geologic program has been initiated on the

Alotta-In-Between property to date. A geophysical program

(magnetometer and VLF) is recommended for the property, especially

around zones of sulphide mineralization such as the Laura Sulphide

Zone. A selective IP survey could also prove useful in helping to

interpret stratigraphy and to delineate future drill targets.

Chapter 2: INTRODUCTION

A 33 claim block, sitated on the southern limb of the Mishibishu

Lake greenstone belt, was the target of a reconnaissance gold

exploration program by Alotta Resources Inc. during 1988. Work was

conducted by a geologic crew stationed at the Oneida Resources camp

adjacent to the property. Both Alotta Resources Inc. and Oneida

Resources Inc. are part of the Applegath Group of Companies.

Although no significant gold mineralization was uncovered, the

limited amount of work conducted on the property indicates the

potential for significant gold mineralization and further work is

warranted.

Chapter 3: PROPERTY

The Alotta-In-Between property is situated on the south limb of

the Mishibishu Lake greenstone belt which separates the granitic

Central and South Batholiths of the Archean Wawa Subprovince of the

Superior Province.

The Alotta-In-Between property consists of 33 claims and comprises

approximately 1320 acres (534 hectares). The claims are situated near

the western margin of the Sault Ste. Marie Mining Division and have

been recorded in the Sault Ste. Marie Mining Recorder's Office. The

claims are numbered consecutively as follows:

Claim Numbers No. of Claims Recording Date

992002 to 992034 33 1987-05-22

The Alotta-In-Between property is bordered to the east by the

Oneida Maple Lake property (90 claims), to the south by the Oneida

Floating Heart claim block (173 claims), to the west by the Villeneuve

Pilot Harbour property (34 claims), and to the north by the Tundra

Jackfish Lake property (527 claims). Figure l provides the location of

the Alotta-In-Between property; Figure 2 shows the areal distribution

of the 33 claims which comprise the Alotta-In-Between property.

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THE APPLEGATH GROUP OF COMPANIES - MISHIBISHU UKE AREA

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NEW PROPERTY ACOUSmONS BY THE APPLEGATH GROUP OF COMPANIES Villeneuve Stoney Creek 160 claims Villeneuve Ml Nash 26 claims Villeneuve Bowman Lake 250 claims Villeneuve Ninety Miner 99 claims

Q Tundra Jackfish Lake 630 claims Q Oneida Floating Heart 173 claims

TOTAL PROPERTY HOLDINGSAlotta 167 claims New Beginnings 51 claims Oneida 263 claims Tundra 604 claims Villeneuve 605 claims GRAND TOTAL

MISHIBISHU RESOURCES CARIBBEAN RESOURCES EXMAR RESOURCES

VILLENEUVE MT, NASH Wd*lmt(1.040tcm)

R l O R

Alotta — New Beginnings — Oneida — Tundra — Villeneuve

Figure 2 Map showing the distribution of the individual claims in the Alotta-In-Between claim block.

Chapter 4: LOCATION AND ACCESS

The Alotta-In-Between property is located approximately 63 km west

of Wawa, Ontario (NTS sheet 41N/13, 42C/4). Wawa is situated 227 km

north of Sault Ste. Marie by highway.

Access to the property is presently restricted to helicopter

transport from Wawa and by boat or barge from the town of Michipicoten

Harbour, 3 km southeast of Wawa. The southern claim boundary is

approximately 8 km from Lake Superior. A float plane can land on 3

large lakes on the property.

An all-weather private road (Noranda Road) is presently under

completion and will eventually link the Noranda-Central Crude Eagle

River property to Highway 17N roughly 1/3 of the way between Wawa and

White River. Upon completion, this road will be within 6 km of the

Alotta-In-Between property and will greatly facilitate the transport of

heavy equipment into the area should it be needed.

Chapter:5 TOPOGRAPHY AND VEGETATION

The centre of the Alotta-In-Between property is marked by long,

linear, E-W trending ridges and scarps with intervening steep-sided

faults. The ridges generally have moderate slopes but some steep

ridges are common, especially near the lakes and in the batholiths.

Superimposed on the E-W trending ridges is a series of NNW

trending features which may represent strike-slip faults. The best

example of these faults is represented by lithologic displacement on

opposite shores of Waving Angel Lake. The significance of these faults

will be discussed in Chapter 13 which deals with structural elements.

Low-lying areas are represented by lakes, swamps or fens. A

classic example of a fen is located SW of Sjogren Lake. The minimum

elevation on the property is 1330' along the shore of Martyn Lake; the

maximum elevation is approximately 1590' on the summit of a large

batholithic outcrop near the NW corner of the property.

Black or white spruce and balsam fir cover most of the property.

Steep hillsides support all of the previous species as well as birch.

Hilltops are generally bare but may support maple, birch,

mountain-sumac and pin-cherry. Intervening wet areas support thick

groves of alder and cedar.

Chapter 6: CLIMATE

The climatic type which typifies the Alotta-In-Between property is

the humid continental type. Summers are short but warm and humid. The

summer of 1988 was exceptionally hot and dry. Most precipitation falls

in the summertime as heavy showers and thunderstorms. Winters are long

and cold with moderate amounts of snow. Because little snow melts in

the wintertime, snow accumulation in the bush may exceed 3' and often

lingers until early May. Yearly precipitation in the area ranges from

30 to 35 inches. The mean annual Jaunary temperature is -12 to

-200 C; the mean annual July temperatur is 16 to 21O C.

Lake Superior has a moderating effect on both seasons.

Unfortunately the presence of the nearby lake often results in periods

of dense fog which disrupts air-travel for days.

10

Chapter 7: POWER

At Mishibishu Lake (15 km NE of the Alotta-In-Between property),

the Muscocho Group has recently completed a spur-transmission line from

the Ontario Hydro Electric Power Commission to their Magnacon

mine-site. In the event that the nearby Noranda-Central Crude property

undergoes development, the Muscocho spur-line will likely be extended

to power the new mine. In this event, the Alotta-In-Between property

will be in close proximety to electrical power. Great Lakes Power Ltd.

is presently building two hydroelectric dam sites on the Magpie River,

5 km west of Wawa. These projects, which will provide 43 megawatts of

power, are expected to be complete by July of 1989 and should be able

to supply the growing needs of mining companies in the area.

Chapter 8: WATER

Three large lakes and several small streams are present on the

Alotta-In-Between property. In addition, Lake Superior is less than 8

km to the south. There are sufficient water resources in the area to

support all phases of a mining operation.

Chapter 9: ANCILLARY SERVICES

Many supplies and services necessary for exploration can be

obtained from Wawa's numerous businesses. Wawa, a siderite mining town

of 5,500, is situated on the Trans-Canada Highway and is less than a

day's drive from Thunder Bay, Timmins, Sault Ste. Marie and Sudbury.

Wawa features an airport with regular flights to Thunder Bay and

11

Sault Ste, Marie. A spur-line of the Algoma Central Railway is

situated near the outskirts of town. Wawa is also in close proximity

to a large fresh-water ship facility at Michipicoten Harbour.

Chapter 10: PROPERTY HISTORY

Very little geologic work has been conducted in the area prior to

that conducted by the Applegath Group of Companies. The best source of

information on the area is the Ontario Ministy of Natural Resources

Geology of the Pukaskwa River-University River Area (Bennett and

Thurston, 1977). The report comes with a geologic map at scale

1:63,360.

Prior to 1982, no previous assessment work on the property had

been filed. It is generally believed that little exploration has been

initiated in the area due to its isolation and rugged terrane. Some

work was conducted in the area by prospectors seeking gold or iron

ore. This is evidenced by the presence of an abandoned campsite on

Martyn Lake.

In 1983, an airborne geophysical survey was done along flight

lines 200 metres apart. The work was conducted by a helicopter

equipped with a 3 frequency electromagnetic system.

12

Chapter 11: REGIONAL GEOLOGY

The Alotta-In-Between property is situated approximately 75 km

south of the important gold mines of Hemlo and 15 km southwest of the

new Muscocho-Magnacon gold property north of Mishibishu Lake. The

property is situated on a very narrow portion of the southern limb of

the Mishibishu Lake metavolcanic-metasedimentary belt which occupies

the southern Archean Wawa Subprovince. The Wawa Subprovince is

situated in the Superior Province of the Canadian Shield. The

arc-shaped Mishibishu Lake greenstone belt has an overall length of 55

km and has an average width of 12 to 18 km.

The geology of the Mishibishu Lake greenstone belt is dominated by

a sequence of mafic to intermediate volcanic rocks and related

intrusive and hypabyssal rocks. Interbedded metagreywacke, slate,

arkose and iron formation are common. Felsic to intermediate

metavolcanics, which are not as common as their mafic counterparts, are

situated in a series of E-W trending bands. Narrow NE trending bands

of conglomerate are found locally but have not been recognized on the

Alotta-In-Between property.

Three small batholiths of granite intrude the greenstone belt and

consist mainly of trondhjemite, quartz monzonite, and granodiorite.

North trending diabase dykes transect all rock types and are best

exposed along the Lake Superior Shoreline. Much of the

Alotta-In-Between property is overlain by thick Pleistocene deposits of

gravel and sand. Outcrops are generally abundant however, especially

in the batholiths.

13

Chapter 12: PROPERTY GEOLOGY

The Alotta-In-Between claim block consists dominantly of a narrow

E-W trending sliver of mafic to felsic volcanic flows, tuffs and

porphyries which parallel the baseline. The greenstone belt is

approximately 2000 to 2600' wide and separates granodiorite and related

batholithic rocks of the Central Pluton to the north from the granites,

gneisses and migmatitos of the South Pluton. The majority of

exploration on the Alotta--In-Between property was centered along the

greenstone belt and as a result, it will be the focus of the geologic

description.

METAVOLCANICS

The metavolcanics have been divided into two main groups: mafic to

intermediate and intermediate to felsic. The division between these

two was established primarily on the basis of colour. Occasionally

rock types were identified on the basis of original constituents but

this was not common because almost all the rock units have been

chloritized, silicified or metamorphosed to some degree. Therefore

there is an arbitrary division of rocks which have a large

compositional range and the two subdivisions are complexely

interrelated and distributed. This is common especially during Archean

time when bimodal volcanism was the norm.

12.1: Mafic to Intermediate Volcanics

The mafic to intermediate metavolcanics are subdivided into a

number of categories depending upon rock fabric.

14

In terms of the potential to host gold deposits, the most

important rock types found on the Alotta-In-Between property are the

mafic to intermediate flows. These units are found in a zone

approximately 2/3 of a km wide which parallels the baseline. Fresh

surfaces are green-grey to black (depending upon chemistry and chlorite

content). Weathered surfaces are light grey or light brown. The flows

are usually fine-to medium-grained; occasional flows are porphyritic.

Flows are usually foliated but massive examples are present locally.

Uncommon flow contacts are marked by subtle changes in colour,

cummulative texture at the base and by rare interflow sediments.

Pillowed basalts were not exposed on the Alotta-In-Between

property but are present on the south shore of Line Cutter Lake,

immediately east of the boundary with land held by Oneida Resources

Inc.

Porphyritic mafic volcanics are common on the property and are

characterized by 0.2 to 0.4 cm long plagioclase phenocrysts that are

beige in colour. Some plagioclase phenocrysts are dark green in colour

and are set in a dark green to almost black matrix of pyroxene, biotite

and chlorite. There is often a gradation from porphyritic flows to

medium grained metadiorite and metagabbro. These rocks look hypabyssal

or intrusive in origin.

Mafic to intermediate tuffs were distinguished from flows by faint

and irregular colour banding and strong foliation. The mafic to

intermediate tuffs are generally lighter in colour than flows, due to

their susceptibility to weathering. Tuffs are not laterally extensive

15

and are interbedded with flows.

Amphibolites are noted by their dark green colour and medium-to

coarse-grained and weakly foliated texture. Amphibolite was restricted

to the southern greenstone margin and occasionally featured gneissic

banding as a result of alternating layers of mafic and felsic

minerals..

12.2: Intermediate to Felsic Volcanics

Intermediate to felsic metavolcanics are subdivided into a number

of different categories depending upon the dominant rock fabric. Three

different rock types were grouped into this category. They are

subordinate in volume to mafic-intermediate volcanics. The most common

rock type under this category is intermediate porphyry. Intermediate

porphyries are characterized by 0.1 to 0.4 cm long beige or light brown

phenocrysts set in a green chlorite rich groundmass.

Felsic to intermediate flows are characterized by an aphanitic

texture, light green-grey colour on fresh surfaces and occasional small

quartz and K-spar(?) phenocrysts. All of the intermediate to felsic

flows have been chloritized and have a distinct foliation.

Probably the most interesting lithologic unit on the

Alotta-In-Between property is a felsic tuff-agglomerate located along

the south shore of a swampy lake immediately west of SJogren Lake. The

unit contains 6 to 12 cm long bombs that have been flattened parallel

to the E-W trending geologic strike. The light green bombs are set in

a beige to light green tuffaceous matrix rich in chlorite and epidote.

The agglomerate likely represents the top of an Archean bimodal

volcanic event as evidenced by mafic volcanics and associated mafic

16

intrusives to the south. The author believes that there may be

hydrothermal deposits in the area that formed with the cessation of the

felsic volcanic phase.

12.3: Metasediments

Metasediments were rarely observed in the field and were

restricted to minor interflow sediments, arkose units and small

pyrite-pyrrhotite iron formation.

Interflow sediments were observed in a few volcanic packages and

were not observed to exceed 4' in thickness. Weathered surfaces are

light grey in colour; fresh surfaces are dark grey. All interflow

sediments are fine grained and foliated.

Several small arkose units were observed near the southern granite

contact. The arkose is rather coarse grained and metamorphised.

Occasionally the arkose units have a 'gneissic' appearance and were

often initially mistaken for them.

Two pyrite-pyrrhotite rich iron formations were discovered on the

Alotta-In-Between property. The Laura Sulphide Zone is the only one of

importance and will be discussed in Chapter 16 which deals with zones

of mineralization.

12.4: Baslc-Ultramafic Intrusives

Basic intrusives (mafic diorite and especially gabbro) are

prominent lithologies on the property. A 400 to 700' wide unit of

gabbro runs E-W immediately north of the baseline and likely represents

mafic intrusives associated with mafic volcanism. The gabbro is medium

grained, slightly foliated and has a colour index of ^5*. Light

17

brown to dark green plagioclase, pyroxene and chlorite are the

constituent minerals in the gabbro.

Mafic diorite with more felsic diorite phases, is also present and

is spatially associated with the mafic intrusives. Mafic diorite is

medium-to coarse-grained with beige or light brown plagioclase as the

dominant mineral. Pyroxene, hornblende and lesser amounts of chlorite

and biotite are the chief mafic minerals. The mafic diorite usually

has a granitic texture but occasionally features a poikilitic texture.

Diorite and mafic diorite may represent a felsic facies that

differentiated from the mafic plutons.

12.5: Felsic Intrusives

Felsic intrusives, consisting mainly of small spherical bodies of

granodiorite, are restricted to discrete phases in the granite

batholiths. The granodiorite features a granitic texture with roughly

equal amounts of K-spar and plagioclase and abundant quartz.

Hornblende is the common mafic mineral although both chlorite and

biotite are common. The southern margin of the Central Batholith in

the study area is chiefly composed of slightly foliated granodiorite.

12.6: Batholithic Rocks

Granite Batholiths are volumetrically the most abundant rock type

present on the Alotta-In-Between property. The granites are polyphase

types ranging from adamellite to quartz monzonite and hornblende

trondhjemite. Numerous hybrid granite phases also occur. The majority

of the rocks have a granitic texture although rocks with a

18

gneissic texture are common and resemble Archean basement rocks. The

granite-greenstone margins are marked by the presence of migmatites and

amphibolite-grade metavolcanics and metasediments.

12.7: Late Mafic Intrusive Rocks-Diabase

Post-granite olivine-diabase dykes are common on the

Alotta-In-Between property and intrude all lithologies. The dykes

range in thickness from a few inches to 10's of feet but the usual

width is 2 to 4'. There appears to be a preferred strike direction to

the NE.

12.8: Pleistocene Deposits

The Precambrian rocks of the Alotta-In-Between property are

generally covered with thick Pleistocene deposits of sand, gravel and

clay. Thickest deposits are confined to lows, especially in the

vicinity of SJogren Lake and along the low-lying greenstone belt.

Batholithic rocks generally provide an abundance of exposure but their

potential for economic gold deposits is low.

Chapter 13: STRUCTURAL GEOLOGY

13.1 Foliation

The general foliation trend differs between rocks of the

greenstone belt and rocks which comprise the granite batholiths. In

the metavolcanics and metasedimentary rocks, the preferred

crystallographic orientation of the phyllosilicates (chlorite, biotite

and sericite) has resulted in an E-W trending foliation with a

consistent subvertical dip to the north. Foliation appears to be

19

axial-planer and is related to isoclinal folding of the greenstone

belt. Where plutonic rocks intrude the greenstone assemblage,

foliation tends to outline the contact margin.

The batholithic rocks of the South Pluton have a foliation

trending NE or SE; steep dips are to the north or south. Some outcrops

in the South Pluton have a gneissic appearance.

Granodiorite, which marks the northern greenstone boundary, is

slightly foliated and no consistent trends were observed.

13.2: Minor Folds

No major folds were observed in the field although the author did

look at minor folds in the gneissic rocks and migmatites. The

relationship between foliation and minor S, Z, M or W folds is helpful

in indicating the position of major folds in the area but this is

difficult along the complexely deformed rocks situated at the

greenstone-batholith margin.

1.3.3: Faults and Lineaments

Numerous E-W trending lineaments are visible on the

Alotta-In-Between property from studying airphotographs. These

lineaments , which are especially visible in the

metavolcanic-metasedimentary belt, parallel the general geology of the

area and may be bedding plane faults.

Another set of lineaments is best visible along the the shore of

Waving Angel Lake and on the western shore of Martyn Lake. These NNW

trending lineaments are sinistral strike-slip faults and likely

represent the component of least stress produced during isoclinal

20

folding in the greenstone belt or during the emplacement of the

granitic batholiths. There is a 200 to 400 ' displacement of

lithologic units on opposite sides of Waving Angel Lake. These sets of

lineaments were prospected with the hope that they may provide dilatant

zones for gold mineralization but results were dissapointing

Chapter 14: METAMORPHISM

The metavolcanic-metasedimentary Mishibishu Lake greenstone belt

in the Alotta-In-Between property has been metamorphosed under the

greenschist facies condition of regional metamorphism. All lithologies

contain chlorite and quartz "sweat 1 . Common metamorphic minerals in

the greenstone assemblage include sericite, biotite and plagioclase.

Common metamorphic minerals in the batholithic rocks include K-spar as

stringers, garnet and muscovite. Along the southern

greenstone-batholith boundary, the metavolcanics and metasediments have

been locally metamorphosed to amphibolite grade. The amphibolites

contain abundant hornblende and plagioclase with accessory amounts of

epidote, chlorite, biotite and garnet.

Chapter 15: 1988 PROGRAM

15.l: Line cutting

A total of approximately 18 miles (29 km) of line was cut on the

Alotta-In-Between property during June and July of 1988. Two baselines

were established as well as the cutting of a grid with 400 foot space

lines and 100 foot station intervals. The entire 33 claim block has an

21

established grid. A map showing the location of the grid Is Included

with the report.

15.2: Geochemistry (Soils)

The entire property was soil sampled during the summer of 1988 and

sampling took place at 100' intervals along lines 400' apart. The 'B 1

horizon was analysed by Bondar-Clegg of Ottawa for gold, copper, lead,

zinc and arsenic. The samples were screened at -20 +80 mesh. A series

of geochemical gold anomalies on Line 4+OOW were investigated and led

to the discovery of the Laura Sulphide Zone. This anomaly and several

others will be discussed in Chapter 16 which deals with zones of

mineralization. All geochemical maps are included with this report.

15.3 Prospecting

Approximately 100 man-days were utilized in prospecting the

Alotta-In-Between property. The majority of prospecting was conducted

by the resident geologists stationed at the Oneida Maple Lake camp east

of the Alotta-In-Between property. Approximately 200 samples were

obtained, 5 of which assayed better than trace amounts of gold. The

best assay ran 0.05 oz. Au/ton in a one foot wide rusty quartz vein

hosted by a gneissic rock.

15.4: Trenching

Three trenches were excavated on the Alotta-In-Between property,

mainly to remove overburden which obscurred mineralized quartz veins.

Trenching took place at the Laura Sulphide Zone (Line 4+OOW, 2+50S),

the Kelemen Vein (Line 52+OOW, 28+008), and along the Alotta Quartz

Vein (Lines 44+00 to 50+OOW, 3+OOS). These zones of mineralization

22

will be discussed in the next chapter.

15.5: Geologic Mapping

The entire Alotta-In-Between property was mapped during the summer

and fall of 1988 by G. Giga, P. McEachern and the author. Mapping was

conducted along grid lines and lake shorelines for control; some

reconnaissance mapping took place with the aid of airphotographs. The

resulting geologic map is enclosed with this report,

Chapter 16: MINERALIZATION

16.1: Laura Sulphide Zone

The most noteworthy zone of mineralization on the

Alotta-In-Between property is the Laura Sulphide Zone. It is located

on Line 4+OOW, 2+50S and is best exposed along the creek bottom which

flows from Martyn Lake to Line Cutter Lake, The zone was discovered by

the author while investigating a series of geochemical anomalies at

5+OOS, 4+OOS and 2+OOS on Line 4+OOW. The Laura Sulphide Zone consists

of a 1.5 to 2' wide pyrite and pyrrhotite rich silicified tuff(?)

situated in a series of fine grained and porphyritic intermediate

flows. Outcrop exposure in the area is limited but all outcrops

contain 2 to 5^ pyrite and pyrrhotite. In addition, the area is busy

with numerous narrow (*^1') quartz veins. To date, all gold assays have

returned trace values. Nevertheless, the Laura Sulphide Zone has the

potential to host stratiform gold mineralization.

16.2 Alotta Quartz Vein

The Alotta Quartz Vein consists of an E-W trending, 600' long

23

rusty quartz vein situated 300" south of the baseline from Line 44+20

to 50+OOW. The vein is not exposed over the entire strike length but

averages l to 4' wide where it is exposed. Some sections of the vein

have a sheeted appearance and there is an abundance of sulphides in

these sheeted quartz zones. The host rock is a series of sheared mafic

to intermediate flows and porphyries. The rusty coloured vein contains

l to 3* chalcopyrite at an exposure near Line 44+OOW; chalcopyrite

becomes less abundant westward. A 4' wide exposure at Line 48+OOW,

3+OOS, contains minor amounts of chalcopyrite, pyrite and

arsenopyrite. Several trenches were dug in order to better expose the

vein and to sample it. All assays returned trace gold values,

16.3: Kelemen Vein

The Kelemen Vein is a rusty quartz vein exposed approximately

2800' south of the baseline on Line 52+OOW. The chalcopyrite bearing

vein, which strikes ENE, is hosted by a granitic gneiss. The vein has

a width between 2 and 24" and containes l to 4* chalcopyrite. The vein

was trenched and sampled along its length but all results returned

trace amounts of gold.

24

Chapter 17: GENERAL RECOMMENDATIONS

Only a preliminary geologic program has been conducted on the

Alotta-In-Between property to date. Five whole-rock samples returned

anomalous gold assays and this indicates the potential for gold

mineralization in the area. Because only a reconnaissance prospecting,

soil geochemistry and mapping program has been completed on the

property, the author recommends geophysical surveys for the spring of

1989. Magnetometer and VLF electromagnetic surveys should be conducted

throughout the property. In addition, IP surveys should be implemented

in the vicinity of the Laura Sulphide Zone, the Alotta Quartz Vein and

along the tuff agglomerate near Sjogren Lake. These three areas appear

to have the most potential for economic gold deposits. It is possible

that follow-up work concentrated in these three areas will lead to

several drill targets.

25

Chapter 18: CERTIFICATE OF QUALIFICATIOS

I, Frank Pezzutto, of 669 Albert St. West, Sault Ste. Marie, Ontario, P6A 1C7, do hereby certify that:

1. I am a geologist employed by the Applegath Group of Companies.

2. I am a graduate of the University of Minnesota, Duluth, holding a Masters of Science degree in geology (1988).

3. I have been practicing my profession as a geologist since 1985.

4. I do not have, nor do I expect to receive aither directly orindirectly any interest in this property of Alotta Resources Ltd.

Sault Ste. Marie, Ontario Frank Pezzutto, M. Se. Geology

26

Chapter 19: REFERENCES

Bennet, G., and Thurston, P.C., 1977: Geology of the PukaskwaRiver-University River Area, Districts of Algoma and Thunder Bay, Ontario Division of Mines, GR 153, 60 p. Accompanied by maps 2332 and 2333, scale 1:63,360 or l inch to l mile.

27

Chapter 20; PERSONNEL

Frank Pezzutto Consulting Geologist 669 Albert St. West Sault Ste. Marie, Ontario P6A 1C7

George Giga Geologist 6954 Molson St. Montreal, P.Q. H2A 3K1

Peter MacEachernGeologist600 Boundary Road,Sault Ste. Marie, OntarioP6A 5C6

Martyn S. HarringtonGeological Assistant and Mechanical Engineer66 4th St.Kirkland Lake, OntarioP2N 1T1

P. Mike Harrington Jr. Geological Assistant 17 Foss Lane Kirkland Lake, Ontario P2N 1T1

Tracy Nixon Geological Assistant Sault Ste. Marie, Ontario

Gregory Wahl Geological Assistant RR 4 Gower Point Road Gibson, B.C. VON 1VO

28

WMinistry ofNorthern Developmentand Mines

oao-73Report of Work(Geophysical, Geologica Geochemical and Expen;

DC

41N13NEC8M 2.12389 PILOT HARBOUR 900

ITownship or Area

-L P±U *I.

Type of Survey(s)

Claim Holder(s) Prospector's Licence No

BSurvey Company

Name and Address of Author (of Geo Technical report)

[Date of Survey (from Si to) r*-T^0'* 1 Miles of line Cut i-S. Od ffg l /^ / * ?S; / r,

J-P-a.yJ,Mo-.J .Vr.J-pay J MoJ^r^ | f O______

Credits Requested per Each Claim in Columns at rightSpecial Provisions

For first survey:Enter 40 days. (This includes line cutting)

For each additional survey: using the same grid:

Enter 20 days (for each)

Man Days

Complete reverse side and enter total(s) here

Geophysical

- Electromagnetic

- Magnetometer

- Radiometric

- Other

Geological

Geochemical

Days per Claim

Geophysical

j - Electromagnetic i

' - Magnetometer

j- Radiornetric

- Other

j Geologicall: Geochemical

Days per Claim

imeter i

etric l

Airborne Credits !

Note: Special provisions Electromagnetic credits do not apply to Airborne Surveys. | Magnetometer

Radiometric

Days per Claim

Expenditures (excludes power stripping)Type of Work Performed

Performed on Oaim(s)

Calculation of Expenditure Days Credits

Total Expenditures

InstructionsTotal Days Credits may be apportioned at the claim holder's choice. Enter number of days credits per claim selected in columns at right.

Date Recmded Holdorp*-Agent (Signature)

/fyu-#l-r^Certification Verifying Rqffort of Work

Mining Claims Traversed (List in numerical sequence)Mining Claim

NumberExpend. Days Cr.

RECEIVECr

MINING LANDS S

t-- — -- -— —

ii

Total ri,"-.rer of mining claims cc.ered by this report o' .vork.

ICIJQN

— -—

— —

33ForJMftccUsc'On'ty

Mining Recorder

Branch elector

l hereby certify that l have a personal .nui intimate knouluiloe of the f;icts set forth in the Report ol Woik anncxud IIIMO:O. irving performed the \ or witnessed same during and/or after its completion anrt the annexed repnit is true

\'ame and Postal Address of Person Certifying

zfo/t-4-j t^ A o i --j /si .i-* . T-/,Dau- Cot tit ird

'V ' * f \' t'* *"''^ r . t '-- 4 ' J ' t ' 'i

f,789 ALOTTA RESOURCES: IN BETWEEN PROPERTY Page l

PROJ NAME TAG NO ttOF CLAIMS TOWNSHIP

INININININ.ININININININININININININININININININININININININININININ

BETWEENBETWEENBETWEENBETWEENBETWEENBETWEENBETWEENBETWEENBETWEENBETWEENBETWEENBETWEENBETWEENBETWEENBETWEENBETWEENBETWEENBETWEENBETWEENBETWEENBETWEENBETWEENBETWEENBETWEENBETWEENBETWEENBETWEENBETWEENBETWEENBETWEENBETWEENBETWEENBETWEEN

SSMSSMSSMSSMSSMSSMSSMSSMSSMSSMSSMSSMSSMSSMSSMSSMSSMSSMSSMSSMSSMSSMSSMSSMSSMSSMSSMSSMSSMSSMSSMSSMSSM

992002992003992004992005992006992007992008992009992010992011992012992013992014992015992016992017992018992019992020992021992022992023992024992025992026992027992028992029992030992031992032992033992034

1111

.111111111111iiiiiiiiiiiiiiiii

PILOTPILOTPILOTPILOTPILOTPILOTPILOTPILOTPILOTPILOTPILOTPILOTPILOTPILOTPILOTPILOTPILOTPILOTPILOTPILOTPILOTPILOTPILOTPILOTPILOTPILOTPILOTPILOTPILOTPILOTPILOTPILOTPILOT

HARBOURHARBOURHARBOURHARBOURHARBOURHARBOURHARBOURHARBOURHARBOURHARBOURHARBOURHARBOURHARBOURHARBOURHARBOURHARBOURHARBOURHARBOURHARBOURHARBOURHARBOURHARBOURHARBOURHARBOURHARBOURHARBOURHARBOURHARBOURHARBOURHARBOURHARBOURHARBOURHARBOUR

33*

2-

Ontario

m i s 1989

Ministry ofNorthern Developmentand Mines

Ministere du D6veloppement du Nord et des MinesJuly 12, 1989

Mining RecorderMinistry of Northern Development and Mines875 Queen Street EastBox 669Sault Ste. Marie, OntarioP6A 2B3

Mining Lands Section 880 Bay Street, 3rd Floor Toronto, Ontario M5S 1Z8

Telephone:(416) 965-4888

Your file: W8905-73 Our file: 2.12389

Dear Madam:

Re: Notice of Intent dated June 7, 1989 Geological and Geochemical Survey submitted on Mining Claims SSM 992002 et al in Pilot Harbour Area.

The assessment work credits, as listed with the above-mentioned Notice of Intent, have been approved as of the above date.

Please inform the recorded holder of these mining claims and so Indicate on your records.

Yours sincerely,

W.R. CowanProvincial Manager, Mining LandsMines tt Minerals Division

)AB:eb Enclosure

cc: Mr. G.H. FergusonMining and Lands Commissioner Toronto, Ontario

Alotta Resources Ltd. 188 ave Perreault Val D'or, Quebec J9P 2H5

Frank Pezzutto 669 Albert Street W. Sault Ste. Marie, Ontario PA JC7

Resident Geologist Sault Ste. Marie, Ontario

Minislry o(Northern Developmentand Minos

Technical AssessmentWork Credits

D.t.

June 7, 1989

File2.12389

Winino Recorder* Report o*

wWSt)5-073

Recorded Holder

ALOTTA RESOURCES LTD.Townihlp or Area

PILOT HARBOUR AREAT y pt of survey and number of

Assessment days credit per claim Mining Claims Assessed

GeophysicalElectromagnetic .

Magnetometer.

Radiometric _

Induced polarization .

Other . .

.days

.days

.days

.days

.days

SSM 992002 to 05 1ncl. 992007 to 21 1nc1. 992023 to 25 incl. 992027 to 34 1ncl.

Section 77 (19) See "Mining Claims Assessed" column

Geological ______40___________days

Geochemical __________________deys

Man days

Special provision

Airborne

Ground

f~l Credits have been reduced because of partial coverage of claims.

|~l Credits have been reduced because of corrections to work dates and figures of applicant.

Special credits under tection 77 (16) for the following mining claims

30 days Geological

SSM 992006 992022 992026

No credits have been allowed for the following mining claims

f") not sufficiently covered by the survey Q Insufficient technical data filed

The Mining Recorder may reduce the above credits it necessary in order that the total number of approved assessment days rtcorded on each claim does not exceed the maximum allowed as follows: Geophysical -80; Geologocal - 40; Geochemical - 40; Section 77(191-60.

628 (8 W12)

Ministry ofNorthern Developmentand Mines

Technical Assessment Work Credits

..Ontario O*te

June 7, 1989

File

2.12389Minlno Recorder* Report of

W05-073

Recorded Holder

ALOTTA RESOURCES LTD.Township or Area

PILOT HARBOUR AREAType of survey tnd number of

Assessment dayt credit per claim Mining Claims Attested

Geophysical

Electromagnetic.

Magnetometer.

Radiometric —

Induced polarization.

Other—-—————

-dayt

.days

-days

.day.

.days

SSM 992002 to 05 1ncl. 992007 to 17 1ncl. 992019 to 21 1ncl. 992023 to 34 1ncl.

Section 77 (19) See "Mining Claims Assessed" column

Geological _________________days

Geochemical _______*-2——————————days

Man days Q

Special provision gj

Airborne f"!

Ground (g

O Credits have been reduced because of partial coverage of claims.

D Credits have been reduced because of corrections to work dates and figures of applicant.

Special credits under section 77 (16) for the following mining claims

10 days geochemical

SSM 992006

l5 days Geochemlcal

SSM 992018 992022

No credits have been allowed for the following mining claims

[~1 not sufficiently covered by the survey Q Insufficient technical data filed

The Mining Recorder may reduce the above credits if necessary in order that the total number of approved assessment days recorded on e*ch claim does not exceed the maximum allowed as follows: Geophysical -80; Geologocal - 40; Geochemical. 40; Section 77(191-60.

tie (8 vi 2)

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41N13NE0014 a .12389 P ILOT HARBOUR 210

TUNDRA GOLD MINES LTD

ALOTTA RESOURCESIN BETWEEN

PROPERTY GRID MAPSHOWING 2 . 1 238^

CLAIMS

WORK BY: F PEZZUTO

DATE: NOV./88

i — — — iSCALE: l" - 500

DRN: K.B.C. MAP NO.- t of 7

l

1FT 20O IOO Q 50 100 200 300 400 500 600 FT.

^^^^^5=5 Scale l"; 500'


4IN13NE0014 2 .12389 P ILOT HARBOUR 220—————————————————————————— ———————————————————————————————————————————————————————————

WORK BY: F PEZZUTO

DATE: NOV./88

SCALE: l" - 500'

DRN: K.B.C. MAP NO; 2 of 7


2.1238?SOIL GEOCHEMISTRY

AU IN PPB

FT 20O I OO O 5O 100 200 30O 400 500 600 FT.

Seal* l" s 500'

•HN13NE8014 2 .12389 P ILOT HARBOUR 230



. 12389SOIL GEOCHEMISTRY

COPPER IN PPM.

WORK BY: F PEZZUTO SCALE: l" = 500

DATE-. NOV/88 DRN: K.B.C. MAP NO-- 3 of 7

O J B. L

FT 2OO 100 Q 50 IOO 2OO 300 4OO 5OO 6OO FT.

Scale l" - 3OO 1

41NI3NE0014 2.12389 PILOT HARBOUR

TUNDRA, GOLD MINES LTD


SOIL GEOCHEMISTRY

LEAD IN PPM

WORK BY: F PEZZUTO SCALE: l" -- 500'

DATE: NOV/88 DRN: K. BC. MAP NO; 4 of 7

a

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ALOTTA RESOURCESIN BETWKfg -a n O O

SOIL GEOCHEMISTRY

ZINC IN PPM

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SCALE: l" : 500'

DRN: K.BC. MAP NO.- 5 Of 7

FT 20O IOO Q 50 100 200 3OO 4OO 500 6OO FT.^^5555^——Scale l" s 500'

4IN13NE0014 2 .12389 P ILOT HARBOUR 260


ALOTTA RESOURCESIN BETWEEN ^ ^ x~2.l23b

SOIL GEOCHEMISTRY

ARSENIC IN P.PM.

WORK BY: F PE2ZUTO

DATE: NOV/88

SCALE: l" - 500'

DRN: K. ac. MAP NO.- 6 of 7

4IMI3NE0314 2 .123B9 P ILOT HARBOUR

LEGENDKEWATIN VOLCANICS

DORE SERIES SEDIMENTS

DIABASE

BATHOLITHIC ROCKS o) GRANITES S GNEISS

b) MIGMAT1TES

FELSIC INTRUSIVES o ) PORPHYRITIC DIORITE

b) GRANODIORITEc) SYENITE

d) MAFIC DIORITE

BASIC; ULTRAMAFIC INTRUSIVESa) GABBRO, DIORITEb) PERIDOTITE, KIMBERLITE,

LAMPROPHYRE

POLYMICTIC CONGLOMERITE

SEDIMENTS a) GREYWACKE, SLATEb) SLATE ARGILLITEc) IRON FORMATIONd) ARKOSE

FELSIC-INTERMEDIATE VOLCANICSa) FLOWSb) PORPHYRITICc) TUFF-AGGLOMERATE tchl. rich ft occasionally mafic)

d) RHYODACITE

INTERMEDIATE MAFIC VOLCANICS

a) MASSIVE FLOWS, ASH TUFFb) PILLOWEDc) AMPHIBOLITE (mafic metadronite)(O SCHISTOSEel CARBONIT1ZED f) SILICIFIED

FT 200 IOO Q 50 100 200 30O 400 500 600 FT.^^^^Z^^ Scale l" - 500'

TUNDRA GOLD MINES LTD,


GEOLOGY2. 1 23

WORK BY: F PEZZUTO

DATE: NOV/88

SCALE: l - 5OO

DRN: K.BC. MAP NO; 7 of 7

apr l (j - ontario

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