S3B14NE0026 53BI4SE00a0 RANDALL LAKE 010

REPORT

ON

GEOLOGICAL MAPPING, LITHOGEOCHEMICAL SAMPLING,

SOIL SAMPLING, AND PROSPECTING

AGUTUA ARM PROPERTY

DISTRICT OF KENORA, PATRICIA MINING DIVISION

NORTHWESTERN ONTARIO

FOR

MOSS RESOURCES LTD.

tN 1 .1 1986

UHDS SECTION

November, 1985 Jon W. North iB.Sc.

TABLE OF CONTENTS

PageS3BHNE0028 53B14SE0e2C! RANDALL LAKE 010C ——^"~

1.0 SUMMARY....................................... l

DRAWING NO. 1: GENERAL LOCATION MAP............ 3

2.0 INTRODUCTION................... . . . . . . . . . . . . . . 4

DRAWING NO. 2:PROPERTY LOCATION MAP........... 5

3.0 PROPERTY DESCRIPTION............... . . . . . . . . . . . 6

DRAWING NO. 3: CLAIM SKETCH........... . . . . . . . . . 7

4.0 LOCATION, ACCESS, SERVICES.................... 8

5 . O PREVIOUS WORK . . . . . . . . . . . . . . . . . . . .-. . . . . . . . . . . . . 9

6.O PHYSIOGRAPHY AND VEGETATION....... . . . . . . , . . . . . 10

7.0 REGIONAL GEOLOGY.................. ............ 11

8.0 PROPERTY GEOLOGY. . . . . . . . . . . . . . ... . . . . . . . , . . . . . . 13

8.1 GENERAL DESCRIPTION...................... 13

8.2 VOLCANICS................................ - 13

8.3 SEDIMENTS................................ 14

8.4 INTRUSIVES............................... 14

8.5 METAMORPHISM............................. 15

8.6 STRUCTURE................................ 15

DRAWING NO. 4: SOIL GEOCHEMISTRY PROFILE...... 16

9.0 GEOCHEMICAL SAMPLING................... . ...... 17

9.1 LITHOGEOCHEMICAL SAMPLING................ 17

9.2 SOIL SAMPLING............... . . . . . . . . . . . . . 17

DRAWING NO. 5: TRENCHES A-K................... 18

9.3 PROSPECTING AND TRENCHING................ 19

10.0 ECONOMIC MINERALIZATION....................... 19

10.1 AGUTUA ARM SHOWING: TRENCHES A-K........ 19

DRAWING NO. 6:TRENCHES L AND M.......... 22

10.2 TRENCHES L AND M........................ 23

10.3 NORTH CARIBOU RIVER SILVER-ZINC-LEAD

OCCURRENCE........................... . . . 24

11.0 SUMMARY OF GEOPHYSICS......................... 25

12.0 CONCLUSIONS................................... 25

13.0 RECOMMENDATIONS............................... 27

13.1 PHASE I................................ 27

13.2 PHASE II..... .... . ... . .................. 27

14.0 ESTIMATED COST OF RECOMMENDED EXPLORATION

PROGRAM................................ . . . . . . . 28

14.1 PHASE I................................ 28

14.2 PHASE II........ . . . ..................... 28

15.0 REFERENCES.................................... 29 i

APPENDICES ;

A: Certificate of Qualification..............(back of report)

B: Technical Data Statement.................. " " "

C: Rock Sample Descriptions and Assays....... " " "

D: Rock and Soil Sample Analytical

Certificates.............................. " "

Drawing No. 7 Property Geology............ (map pocket) .

1.0 SUMMARY

The Agutua Arm property of Moss Resources Ltd. is under

lain principally by an east-west trending sequence of felsic

to intermediate pyroclastics and volcanoclastics. This

sequence is intercalated with minor mafic flows and intruded

by felsic to intermediate quartz-feldspar porphyry sills and

dykes. The rocks dip to the south between 20 0 and 40 0 .

Precious and base-metal mineralization occurs in two

localities on the property; the Agutua Arm gold-silver-copper

showing, and the North Caribou River silver-zinc-lead showing.

Mineralization is associated with east-west zones of shearing

and carbonate alteration which dip steeply south at the Agutua

Arm showing, and steeply north at the North Caribou River

showing.

At the Agutua Arm showing,previous surface trenching has

exposed a carbonatized shear zone three and three-quarter feet

wide along a strike length of 90 feet. Within this zone en

echelon quartz-arsu^opyrite veins carry gold-silver-copper

values. Sampling of the trenches resulted in assays up to

0.67 ounces per ton gold, and 0.71 ounces per ton silver.

Results of earlier sampling reported higher values, up to

1.92 ounces per ton gold over one Loot, and 18.80 ounces per

ton silver over 4.0 feet.

The North Caribou River showing was not located during

the present program due to unusually high water levels. This

showing was discovered by Ontario Geological Survey geologists

in 1984, and has been described as a 13 cm wide carbonatized

shear zone with silver values up to 2.9 ounces per ton. The

mineralogy, alteration and general trend of these mineralized

zones are similar to the North Caribou River fault structure,

two miles to the south.

Fifteen east-west trending VLF-EM conductors have been

delineated on the property, and are considered to have excellent

potential for shear controlled sulphide-gold-silver-copper-

lead-zinc deposits.

A two-phase exploration program is recommended. Phase I

should consist of an I.P. survey to determine which of the EM

conductors are caused by sulphide bearing shear zones, and

humus sampling to detect other bedrock zones of gold-silver mineralization. Phase II should consist of diamond drilling.

The estimated cost of these programs is $26,340 and |122,500

for a total cost of SU8,840.

- 3 -

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fllV THUNDER ^ ^ 8*^

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K.DLAKE

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MOSS RESOURCES LTD.

AGUTUA ARM PROPERTY Patricia M.D., Ontario

LOCATION MAP

SCALE: l :!00miDWG. No: l

BY: H.H./R.T.MDATE: NOV, 1985

- 4 -

2.0 INTRODUCTION

The following report describes the results of a comprehensive

geological exploration program consisting of geological mapping,

at a scale of l inch to AGO feet, lithogeochemical sampling,

soil sampling, trenching, and prospecting on the Agutua Arm

property of Moss Resources Ltd. The property is located in

the North Caribou-Opapimiskan-Neawagank Lakes greenstone belt

in Northwestern Ontario (page 3).

The present program was carried out in August, 1985, by

Geocanex Ltd., of Toronto, subsequent to magnetic and VLF-EM

surveys which were carried out in February and March, 1985,

also by Geocanex Ltd.

All work was carried out on a cut picket line grid with

an east-west trending baseline and perpendicular cross lines

at 400-foot intervals.

The program was carried out from August 6th to August

28th, 1985.

The personnel involved in the program were:

Jon North Geologist/Party Chief Windsor, Ontario

Rob Higginson Geologist Barrie, Ontario

Brian Huston Field Assistant Pickle Lake, Ontario

Ken Wright Field Assistant Scarborough, Ontario

Grab samples of all'quartz veins and mineralized volcanics

were collected during the mapping and prospecting programs.

- 5 -900 30'

53 0 OO' MOSS RESOURCES LTD

VAN HORNE GOLD EXPLORATION INC.

NORTH CARIBOU-OPAPIMISKAN- NEAWAGANK LAKES

GREENSTONE BELTREGIONAL GEOLOGY

AND MINERALOCCURRENCES

? 6 v - H H X R T M 0*'E O ct 1 935 SCALE l - 4miGEOCANEX LTD

TORONTO. CANADA

AGUATUAARMPROPERTY

Mefavolconics

Mefosediments Staked ground

Moss Resources Ltd.

Van Horne Gold Exploration Inc

Granitic intrusive Metamorphic rocks

MUSSELWHITE DEPOSITSIron formation

Synclinal Fold axis

DOME-INCO-ESSO- L.ACANA3,000,000 tons O l/oz/ton Au

Gold occurrences

(T) Musselwhite deposit

(2) Teal prospectAgutua Arm prospect

4) Centre Lake prospect5) Eyapomikoma Lake Mo, F prospect

6) Opapimiskan Lake prospect7) N eawagank Lake prospect

8) Liberf Lake prospect9} Sage Lake prospect

, QCj) Stanley Lake prospect;:(fi) Seeseep "Lake prospect

- n i 2 "—— —-i^——j— — —L^'"T

- 6 -

In 1967, Pyrotex Mining and Exploration trenched a high

grade gold-copper-silver showing located on claim No. Pa 720082.

During the present program these trenches were cleaned out and

extended, chip sampled and mapped in detail. One north-south line was run over the trenches, and humus and '3' horizon

soil samples were collected and analyzed for orientation

purposes. A mineralized shear zone was discovered on the base

line near line 28 west. Two trenches were put in over the

zone, chip sampled and mapped. Prospecting was carried out over all geophysical anomalies.

The time breakdown in man-days for the work performed

is as follows:

Mapping 41 1/2 man-days

Chip Sampling/Trenching 37 man-days

Prospecting 13 man-days

Soil Sampling 2_______man-days

Total 93 1/2 man-da.ys

A geological map of the property is included at the back of

this report (Map 1). Geologic/sample sketches of the trenches are included with the text. All rocks and soil sample descrip tions and assays are included in the Appendix.

3.0 PROPERTY DESCRIPTION

The Agutua Arm property consists of 27 contiguous unpatented mining claims recorded on Ministry of Natural Resources Randall

Lake (M-2544) and Keeyask Lake (M-2684) claim sheets (page

(* Weagamow Loke

(Agutua Arm)

MOSS RESOURCES LTD.

AGUTUA ARM PROPERTY

Patricia M. D., Ontario

CLAIM SKETCHBY: H.H.XR.T'M. DATE; NOV. 19

GEOCANEX LTD TOPONTO,

- 8 -

laim details are as follows:

Claim Nos.No. of Claims Recording Date Work Filed

Pa 720075-089 incl. 15

823397-408 incl. 12

March 5, 1985

Jan. 14, 1985

60 days

60 days

The claims are wholly owned by Moss Resources Ltd., 804-

34 King Street East, Toronto, Ontario M5C 1E5.

4.0 LOCATION, ACCESS, SERVICES

The property is located in Northwestern Ontario (Lat.52 0 53'N, Long. 91 0 li 1 W), approximately 100 miles north-northwest

of Pickle Lake, and 170 miles northeast of Red Lake. The claim group straddles the south shore of the Agutua Arm of

Weagamow (Round) Lake. The Weagamow Lake - Agutua Arm - North

Caribou River system is the main travel route for Native trappers and fishermen from the Weagamow Indian Reserve (No. 87), which is approximately nine miles northwest of the property.

Access to the property can be made by float-or ski-equiped

aircraft from Pickle Lake, Red Lake or Weagamow Lake, or via

boat from the Weagamow settlement

Highway 808, an all-weather gravel road from Pickle Lake,

ends at Windigo Lake, approximately 25 miles south-southwest

of the property. A winter road to Weagamow runs within five

miles of the property between January and April. Groceries, building materials and general mining supplies may be obtained

in Pickle Lake. Groceries and limited building materials may

be obtained from Weagamow.

- 9 -

5.O PREVIOUS WORK

The following is a chronological account of previous work

on the property.

1938 - Jack Satterly (Satterly, 1939), mapped the property

area at a scale of l inch to l mile during a reconnaisance

survey for the Ontario Department of Mines.

1959 - An airborne magnetometer survey covering the

property was flown in the area by the ODM-GSC at a scale of

l inch to l mile (ODM-GSC, Map 909G, Weagamow Lake, 1960).

1967 - Pyrotex Mining and Exploration discoverd gold-

copper-silver mineralization in quartz veins and sheared

volcanics on the south shore of Agutua Arm, and drilled four

holes totalling 940 feet. Several quartz veins up to 0.3

metres wide were sampled in trenches. The best assays from

trenching are listed below.

Au (oz/ton) Ag (oz/ton) Cu ( "L ) Length (m)

2.54 3.68 1.35 0.3

1.92 18.80 2.50 1.2

No assays were reported from the drilling.

1979 - Thurston et al (1979) mapped the area on reconn

aisance level for the Ontario Geological Survey.

1984 - In March, 428226 Ontario Ltd. staked 15 claims

covering the Agutua Arm gold-silver-copper showing.

- 10 -

1984 - In April, Moss Resources Ltd. acquired j.5 c laim

group from 428226 Ontario Ltd.

1984 - Summer mapping program by the OGS at a scale

of l inch to 0.5 mile discovered silver-zinc-lead mineralization

at the mouth of the North Caribou River in Agutua Arm.

1985 - In January, Moss Resources Ltd. staked an additional

12 tie-on claims to the original 15 claim group to cover the

North Caribou River , .Iver-zinc-lead occurrence.

1985 - In February and March,Geocanex Ltd. carried out

linecutting, and magnetic and VLF-EM surveys on the 27 claim Agutua Arm property for Moss Resources Ltd. Fifteen east-west

trending VLF-EM conductors were delineated.

1985 - In August, Moss Resources Ltd. carried out the

present geological exploration program.

6.0 PHYSIOGRAPHY AND VEGETATION

Forty to fifty percent of the property is covered by

waters of the Agutua Arm-North Caribou River sys^.am. A set of rapids, five to ten feet high, at the mouth of the North

Caribou River near line 60 west, 2800 south, empties the

westerly flowing river into Agutua Arm. The main land portion

of the property forms a penninsula trending east-west across the property, and is 3,700 feet wide at the east end.

Outcrop is exposed on 3 to 570 of the property, and usually occurs as isolated domes protruding through thick glacial cover of sand and boulders. Most of the property

- 11 -

is covered by tall pine, spruce and hardwood forest on well-

drained glacial overburden. Ten to fifteen percent of the*

property is covered by muskeg. In 1985, the water level of

the lakes and rivers in the area was unusually high, and

many islands and shoreline outcrops were submerged. The North

Caribou River silver-zinc-lead occurrence described by Bartlett

et al (1985) was under about five feet of water.

7.0 REGIONAL GEOLOGY

The Agutua Arm property is located in the southwest

portion of the North Caribou-Opapimiskan-Neawagank Lakes greenstone belt. Due to the relative remoteness of the area,

the belt has not been extensively worked by mining and ex ploration companies . Most of the available geological inform

ation on the area is from government funded geological/geophysica^ surveys. The Ontario Geological Survey is currently involved

in the second year of a three-year geological/geophysical

survey of the area, manned by staff from the Precambrian Geology, Engineering and Terrain Geology, and Mineral Deposits Sections .

The belt forms part of the Sachigo Subprovince which is

composed of several small irregularly-shaped sequences of

supracrustal rocks. The rocks in this subprovince are avolutionarily distinct and probably older than the rocks in

the Uchi and Wabigoon Subprovinces to the south (Bartlett

et al, 1985). The belt forms an arcuate, horn-shaped assemblage

of metavolcanic and metasedimentary rocks which have been

synclinally folded about an axis, approximately coincident

with Eyapimikama Lake (Satterly, 194"1.). The syncline is

- 12 -

rimmed by mafic volcanics on the north anri -outh, and filled

with trough, cross-stratified epiclastic P icumulations in

the axial portion. Two fairly continuous bands of iron form

ation and chemical sediments mark the contact between the

volcanics and sediments, (Bartlett et al, 1985). Regional geological maps indicate that the belt is bounded by paragneiss

and migmatized rocks in the north, and felsic intrusives in

he west and south (Map 2292, Big Trout Lake - North Caribou Lake).

The entire belt extends from Weagamow Lake in the north

west to Opapimiskan Lake in the southeast. South of

Opapimiskan Lake the belt bifurcates into two major lobes, one lobe extending south through Libert Lake, the other through

the Forester and Newagank Lakes areas.

Geological mapping by the O.G.S. in 1985 at a scale

of l inch to 1/2 mile, indicates that the property area is

underlain by east-west trending felsic to intermediate pyro

clastic rocks with intercalated mafic flows. The sequence

dips shallowly to the south. This sequence of rocks is the

only large felsic to intermediate pyroclastic center documented

in the belt thus far. The rocks in the property area are

underlain by felsic intrusive rocks to the west, and abut

unconformably against the north-south trending stratigraphy of the Keeyask Lake metasedimentary-metavolcanic complex, two

miles east of the property.

- 13 -

8.0 PROPERTY GEOLOGY

G.l GENERAL DESCRIPTION

The property is underlain principally by an east-

west striking sequence of felsic and intermediate pyroclastics

and volcanoclastics (Map 1). The rocks dip to the south

between 19 0 and 81 0 but more commonly around 20-40 0 . Light

green to buff weathering intermediate flows, tuffs, lapilli

tuffs, and coarse fragmental rocks with minor agglomerate,

dominate the sequence. Massive, concordant lenses of fine to

medium-grained mafic volcanics are interbedded with the

pyroclastics, and constitute approximately ID-15% of the

section. Locally lenses of rhyloite porphyry and chert are

also present, but in very minor amounts. Quartz-feldspar

porphyry sills and dyke rocks of approximately tonalitic

composition intrude all of the volcanics, but were observed

in a few outcrops only.

8.2 VOLCANICS

The pyroclastic sequence on the property was probably

deposited in large part,subaerially. The sequence strikes

east-west and has an on-property thickness of approximately

6,300 feet. The rocks are light green to buff on weathered

surface, and light to dark green on fresh surface. The rocks

are generally foliated but not highly fissile. When bedding

ir. the pyroclastics was observed it was usually quite thin,

from a few inches to a few feet. Textural variation on out

crop scale is often quite pronounced and ranged from well-

bedded tuff and lapilli tuff to marbled and very poorly sorted

fragmentals, breccias, and agglomerates. Fragments are

- 14 -

generally less than five inches in diameter, angular to sub angular, and usually non-scoriaceous. These rocks do not

exhibit much compositional variation, and are approximately

dacitic or rhyodacitic to andesitic. Blocky andesite, dacite,

and rhyolite porphyry are present in minor amounts throughout

the pyroclastic sequence.

Mafic volcanics are commonly found as conformable lenses

less than 300 feet thick. These rocks are dark green, fine-

to medium-grained, graphic textured, (hornblende-plagioclase) flows. Pillows were never observed, and although the rocks

resemble typical intrusives rather than flows, no crosscutting relationships were observed. Epidotization in late cross

cutting fractures, joints and shears with minor quartz

veins, and pyrite are common features in the mafic volcanics.

8.3 SEDIMENTS

An outcrop of chert was found at 27+00 west on the

baseline. This is the only known occurrence of sedimentary

rocks on the property, and the only indication that any of the rocks were deposited subaqueously.

8.4 INTRUSIVES

There are very few intrusive rocks on the property.

Felsic to intermediate quartz-feldspar porphyry sills were

noted in a few outcrops. These rocks are concordant to

slightly crosscutting, and are probably co-magmatic with the

pyroclastic, rocks.

- 15 -

A tonalite plug was found on line 24 west, at 2400

south. The outcrop contains mafic xendiths, numerous quartz stringers and veiniets, and crosscutting networks of quartz stringers with tourmaline, arsenopyrite and pyrite mineralization^

8.5 METAMORPHISM \

The rocks on the property for the most part, appear :

to be very fresh. The fragmental and volcanoclastic rocks i

are light green coloured due to the development c f chlorite j

during regional greenschist facies metamorphism.

Localized shearing and quartz-carbonate metasomatism

along east-west trending shear planes is present on the

property. These phenomena probably reflect the strong pene

trative fabric of the North Caribou River fault which is

located two miles south of the property.

8.6 STRUCTURE

The rocks on the property are relatively undeformed.

The volcanic sequence generally strikes east-west, and dips

shallowly at 20 to 40 0 south. No .najor crosscutting lineaments,

folds, or offsets in the stratigraphy were observed. Shear

zones are approximately concordant with the strike of the

volcanics, and dip steeply south at 52 0 to 82 0 , A prominent

joint system is present on virtually all outcrops. This

system trends at 200 0 to 210 0 and usually dips between 70 0

west to vertical. One plunge measurement was obtained from

a shear zone in trench M. This zone plunges east only at 62 0 .

- 17 -

9.0 GEOCHEMICAL SAMPLING

9.1 LITHOGEOCHEMICAL SAMPLING

A total of twelve grab samples was collected during

mapping and prospecting and analyzed for gold and silver.

Ninety-six chip samples were taken from trenches A through M. All of these samples were analyzed for gold and silver;

57 of the chip samples were analyzed for copper as well as

gold ana silver. Because many gold values from the chip

samples were greater than 1000 ppb, 15 samples were run again by assay to obtain results in ounces per ton. This is

necessary because the fire-assay atomic-obsorbtion techinque

does not resolve high gold values as well as the assay

technique. All rock analyses are listed in Appendix C.

9.2 SOIL SAMPLING

One line of orientation soil geochemistry was run

on the property over the Agutua Arm gold-silver-copper , showing. Eleven humus and eleven B horizon samples were

collected at ten-foot intervals across the showing. All samples

were analyzed for gold, silver and copper. The soil geo chemistry profiles are shown in Drawing 4. The purpose of this survey was to determine the effectiveness of soil geo

chemistry as a transducer for outlining auriferous bedrock

zones. Gold anomalies occur in both humus and B horizon samples.

A two-sample anomaly which peaks at 16 ppb gold, is present in humus samples approximately 10 to 20 feet down ice from

the main mineralization at the showing. A one-sample anomaly which peaks at 68 ppb gold is present in B horizon samples

- 19 -

approximately 10 feet down ice from the main mineralization at the showing. Silver and copper values in humus and B

horizon samples are sporadic. In this survey humus sampling

and gold give the best bedrock signature over the showing.

9.3 PROSPECTING AND TRENCHING

All geophysical anomalies, were prospected with

particular emphasis on VLF-EM conductors. The numerous low

amplitude magnetic anomalies on the property are probably

caused by increased magnetite contents in the volcanics. All

of the VLF-EM anomalies are covered by overburden and muskeg.

A total of 13 man-days was spent prospecting.

A total of 28 man-days was spent trenching (including

chip sampling and mapping) the Agutua Arm showing (trenches

A to K). Nine man-days were spent on trenches L and M.

10.0 ECONOMIC MINERALIZATION

10.1 AGUTUA ARM SHOWING: TRENCHES A-K

Economic grade gold-silver-copper mineralization

occurs on the south shore of Agutua Arm near line 32 west, in

an east-west trending carbonatized shear zone hosted in

intermediate to mafic volcanics (Drawing 5). Four holes totalling 940 feet were drilled along this zoi -. in 1967, by

Pyrotex Mining and Explorations. No assays were reported from

this drilling but it was reported that the mineralized zone

was intersected in three of the four holes. This mineralization

is confined mainly to en echelon carbonate-quartz-arsenopyrite

veins which were emplaced along shear planes and crosscutting

- 20 -

fissures in the volcanics. The main zone of mineralization

at this showing averages 3.75 feet wide, and is exposed along

strike for 90 feet in trenches C,D,E,F, and G. Two smaller

quartz-arsenopyrite veins are exposed in trenches C and D, approximately 10 feet north of the main zone. The shearing

which hosts the quartz veins dips approximately 70 0 to 80 0 south,

A subsidiary massive ankerite shear zone occurs 40 feet south of the main zone and is exposed along strike for 130

feet in trenches A,B,H,I,J and K. This zone is l-.5 to 2.1

feet wide but, where exposed, does not contain significant

precious metal values.

Economic gold and silver values were obtained in chip samples from the main shear zone. Gold, silver and minor

copper are concentrated in the quartz-arsenopyrite vein

systems which pinch and swell within the shear zone. Visible gold was not observed in the showing. It is probably contained

in the arsenopyrite crystal lattice.

The highest gold value was obtained from trench G; sample no , 3052 ran 0.67 ounces gold and 0.46 ounces silver per ton over 0.8 feet. A brief description of this sample,which is

representative for all of the veins in the main zone, is as

follows:

Approximate Modes

Arsenopyrite

Quartz

Ankerite Calcite

75 - 807o

15 - 207.

2 - 37,tr . - U

Chalcopyrite

Pyrite

Bornite? Tetrahedrite

tr. - .57,

tr .

tr. tr .

- 21 -

Veins occur in sinuous, narrow networks which are concordant

to the main shear zone which strikes roughly east-west and

dips 70-80 0 south. The veins and country rock weather

recessively to deep ochre brown from the alteration of iron

carbonate and sulphides. Fresh vein surfaces are arsenopyrite,

grey and mottled with a few quartz inclusions and fragments.

The cores of the veins are generally composed of massive, medium-to coarse-grained, euhedral arsenopyrite which has been

slightly brecciated by a late injection of quartz. Minor

amounts of pyrite and chalcopyrite are found interstitial to arsenopyrite. The vein selvage is composed of sugary, vuggy

buff-to brown-coloured quartz with minor fine-grained disseminated

arsenopyrite. The wall rock is highly sheared, silicified

and carbonitized mafic volcanic which is hydraulically fractured and contains fine-grained disseminated arsenopyrite

and crosscutting quartz-sulphide veinlets.

This mineralization is exposed for 90 feet along strike.

Gold and silver values are highest in samples of vein material

and range from 40 ppb to 22, 847 ppb, and 0.2 ppm to 22.2 ppm respectively. The average gold and silver content of vein

samples from the main zone is 4,214 ppb and 4.4 ppm respectively.

The gold/silver ratio in the veins is 1.15:1. Chalcopyrite

was found in quartz-arsenopyrite veins throughout the zone,

the highest copper value was 2,360 pprn (Q.2%) over 0,3 feet.

Gold, silver, and copper concentrations decrease rapidly

from the quartz-arsenopyrite veins into the wall rock.

The wall rock at the showing is mafic volcanic which

has been bleached, silicified, and carbonatized by a strong

- 22 -

ho. so

03 CSJ

Muskeg

5o

10'

LEGEND

C ! "SS'*'e^ OS

MOSS RESOURCES LTD.

Aguatua Arm Property

Trenches L and M

GEOCANEX LTD TORONTO. CANADA

BY: RDATE: Qc* 29.65 SCALE: l": O"DWG. No: 6

•/-a

- 23 -

alteration envelope which is centered on the main zone of the

showing. The altered volcanic does not contain significant

gold or silver concentrations unless it is crosscut by quartz-

sulphide veinlets in hydraulic rractures, or adjacent to the

main zone of mineralization where the hydrothermal metasomatism

in the volcanics is focused.

10.2 TRENCHES L AND M

Similar metasomatism and shearing to that of the

Agutua Arm showing occurs in intermediate to mafic volcanics

near line 28 west on the baseline. An east-west trending

limonitic shear zone with fine-grained disseminated arsenopyrite

and pyrite was exposed by trenching on the edge of a scarp

(Drawing 6). The shear zone dips 54 0 south. No economic

gold or silver values were obtained in chip samples from these trenches, however, significant values of 40 ppb gold, 1.4 ppm

silver and 771 ppm (.07/0 copper were obtained from a three-

foot sample of sheared volcanic with 1-370 disseminated pyrite

and TL arsenopyrite. The intensity of shearing and alteration

increases towards the southern edge of the scarp suggesting

that a stronger zone of alteration, mineralogically and structurally similar to the Agutua Arm showing, may be present

under the muskeg a.id spruce bog to the south of the scarp. A

strong VLF-EM conductor crosses line 28 west 80 feet south

of the baseline. It i s possible that this conductor represents a shear zone with sulphide mineralization which is only

partially exposed in trenches L and M.

- 24 -

10.3 NORTH CARIBOU RIVER SILVEK-ZINC-LEAD OCCURRENCE

Silver-zinc-lead mineralization was discovered in

a 13 cm wide shear zone at the mouth of the North Caribou River by an OGS mapping crew in 1984 (Bartlett et al, 1985).

This zone trends E 30 0 S and dips 67 0 to the northeast. Silver

values of 2.1 to 2.9 ounces per ton were obtained from the

shear zone which occurs with quartz-carbonate-chlorite alter ation at the contact of intermediate tuff and a mafic dyke.

This showing is probably located near line 72 west, 3600 south at the edge of a small island, however, the water

level of Agutua Arm was very high during the present program

and the showing was submerged under approximately five feet of water .

Numerous strong-to-moderate VLF-EM conductors are

present elsewhere throughout the property. These zones are roughly concordant to the stratigraphy and known zones of

shear-related mineralization on the property. The North

Caribou River fault is located approximately two miles south of the property, and is characterized by mineralogically similar alteration to the Agutua Arm gold-silver-copper showing.

The writer suggests that the penetrative foliation developed

along this fault extends northward onto the Agutua Arm property, where it is represented by the Agutua Arm and North Caribou

mineralized shear zones. Similar zones of alteration and

economic mineralization may be present and represented by the

VLF-EM conductors on the property which are not exposed in

outcrop.

- 25 -

11.0 SUMMARY OF GEOPHYSICS

VLF-EM and magnetic surveys were carried out on the

property in February and March, 1985.

The magnetic relief on the property is generally low.

In the central portion of the property a broad magnetic ridge

of 100 to 150 gammas is present. This feature p,robably

indicates increased magnetite content of the volcanics relative

to the rocks in the north and south portions of the property.

Several weak magnetic features are coincident with VLF-EM

responses, and may represent magnetic- sulphide mineralization.

Fifteen separate moderate-to-strong VLF-EM conductors

are present on the property. These generally trend east-west

and ara probably related to sulphide mineralization, which

may be controlled by shear zones in a number of cases.

12.0 CONCLUSIONS

The property is underlain by a thick sequence of felsic

to intermediate pyroclastics and volcaniclastics with inter

calated mafic volcanic flows. The rocks on the property strike

east-west and dip at shallow angles to the south.

Two important economic mineral showings occur on the

property. Gold-silver-copper mineralization occurs at the

Agutua Arm showing in quartz-arsenopyrite veins which have

been introduced into an east-west trending carbonatized, sili

cified shear zone. Mineralization is exposed for 90 feet in

trenches at this showing. Gold values of up to .67 ounces per

- 26 -

ton, and silver values of up to 22.2 ppm,occur in a strong

zone of mineralization which averages approximately three

and three-quarter feet in width.

At the North Caribou River showing, silver-zinc-lead mineralization occurs in a 13 cm wide southeast-northwest

trending silicified, carbonati?ed shear zone at the contact

of intermediate tuff and a mafic dyke. Silver values of 2.1

and 2.9 ounces per ton were obtained by an OGS mapping crew

in 1984. This mineral occurrence was under water in 1985

and could not be observed or sampled during the present program.

The showing is probably located on claim No. Pa 823406.

A mineralized shear zone, possibly flanking a large

unexposed zone of shearing, was found near l ine 2 8 west, on the baseline. This shear zone trends approximately east-west.

The presence of numerous, roughly concordant, east-west

trending shear zones on the property may reflect the penetrative structural fabric of the North Caribou River fault which is

located two miles south of the property. The alteration

mineralogy of the Agutua Arm showing is similar to that of the

North Caribou River fault.

Numerous east-west trending VLF-EM conductors are present

on the property but not exposed in outcrop. It is very likely

that some of these anomalies represent conductive sulphide

mineralization in shear zones similar in attitude and mineralogy

to the Agutua Arm showing and the North Caribou River fault.

- 27 -

13.0 RECOMMENDATIONS

A two-phase exploration program is recommended.

13.1 PHASE I

Since economic mineralization on the property is associated with sulphides in shear zones, all VLF-EM

conductors should be covered with Induced Polarization survey

to determine whether there are sulphides present in these

zones.

Orientation soil (hur.us) sampling carried out over known mineralized zones in trenches on the property indicates

that this method of sampling will detect gold-silvor mineral

ization. Humus sampling a d analyses for gold and silver

should be carried out ove the entire land portion of the

property.

13.2 PHASE II

Diamond drilling should be carried out to determine

the extent and grade of mineralization in the known showings ,

and to investigate geophysical and geochemical anomalies defined in Phase I.

It is estimated that a maximum of 3,500 feet of

drilling will be required.

- 28 -

14.0 ESTIMATED COST OF RECOMMENDED EXPLORATION PROGRAM

14.1 PHASE I

I.P. Surveys - 10 miles @$1,400/ mile $ 14,000.00

Humus Sampling - 530 samples @$15.00/ sample 7,950.00

Contingency 2QI 4 ,390.00

Total ? 26,340.00

14.2 PHASE II

Diamond drilling - 3,500 ft.

@ |35.00 all inclusive 3122,500.00

TOTAL PHASE I AND PHASE II $148,840.00

Respectfully Submitted,

Jon W. North B. Se. Geologist

- 29 -

15.0 REFERENCES

Bartlett, J.R., Breaks, F.W., DeKemp, E.A., and Shields, H.N., 1985. Precambrian Geology of Eyapimikama Lake Area (Opapimiskan Lake Project), Kenora District (Patricia Portion); Ontario Geological Survey, Map P. 2834, Geological Series - Preliminary Map. Scale 1:31680.

Hodge, H.J., 1985. Report on VLF-EM and Magnetic Surveys,Agutua Arm Property of Moss Resources Ltd. District of Kenora (Patricia Portion) Patricia Mining Division, Ontario for Moss Resources Ltd. - Horseshoe Resources Ltd. Joint Venture NTS 53B.

Ministry of Natural Resources Assessment Work Files; Unpublished Assessment Reports, Ontario Geological Survey, Sioux Lookout, Ontario.

Ministry of Natural Resources Map 2292, Big Trout Lake - North Caribou Lake Geological Compilation Series.

Ontario Department of Mines - GSC, 1960. Aeromagnetic, Map 909G, Weagamow Lake; l inch to l mile.

Satterly, J., 1939. Geology of the Windigo - North Caribou Lakes Area; Ontario Department of Mines, Vol. 48, Part 9, p. 1-32.

Thurston, P.L., Sage, R.P. and Siraguse, G.M., 1979. Geologyof the Winisk Lake Area; District of Kenora, Patricia Portion; OGS Report 193.

APPENDIX A

CERTIFICATE OF QUALIFICATION

r1 "

CERTIFICATE OF QUALIFICATION

THIS IS TO CERTIFY THAT:

1. I have been a resident of Ontario since 1965.

2. I ara a graduate of The University of Western Ontario,

London, Ontario, with an Honours B.Se. (1984) in geology.

3. I have been actively involved in the Canadian mining and

exploration industry in Ontario as a student from 1981

to 1983, and have been a contracting geologist since

May, 1984.

4. I have worked in the Pickle Lake area of Northwestern

Ontario since May, 1984.

5. This report is based on field observations made by the

author, and on a comprehensive study of all the available

Ministry of Natural Resources assessment work records,

and published geological maps and literature of importance

to the area described in this report.

G. In this report I have disclosed all relevant material,

descriptive and interpretive, which is to the best of

my knowledge, necessary to gain a complete understanding

of the viability of the project and the recommendations.

DATED this 15th day of November 1985, at TORONTO, Ontario.

Jon W. North B.Se. Geologist

APPENDIX B

TECHNICAL DATA STATEMENT

Ontario

Ministry of Natural Resources

GEOPHYSICAL - GEOLOGICAL - GEOCHEMICAL TECHNICAL DATA STATEMENT

File.

TO BE ATTACHED AS AN APPENDIX TO TECHNICAL REPORTFACTS SHOWN HERE NEED NOT BE REPEATED IN REPORT

TECHNICAL REPORT MUST CONTAIN INTERPRETATION, CONCLUSIONS ETC.

•S)D

it. O

Type of Survey{s). Geological

Township or Ar^andall Lake (H-254A) Keeyask La|ce Claim noidcr(s) Moss Resources Ltd. 804-34 Kin"g

Street East Toronto, Ontario M5C 1E5

Survey Company-

Author of Report.

Geocanex Ltd.Jon W. North

Address of Author St. Gabriel Ct. Windsor , On t . Covering Dates of .Survey Aug. 16 -Aug. 28,1985 N9E 1P2

(linecutting lo office)

Total Miles of Line Cut -^-^^^^^^^^^^^^^^^.^^^^^.^^^.

SPECIAL PROVISIONS CREDITS REQUESTED

ENTER 40 days (includes line cutting) for first survey.

ENTER 20 days for each .additional survey using same grid.

Geophysical--Electromagnetic.

—Magnetometer—

— Radiometric——

-Other

DAYSper claim

Geological_L

Geochemical.

AIRBORNE CREDITS (Special provision credili do not apply to airborne lurvcyj)

Magnetometer. .Electromagnetic. Radiometric

DATE:.

(enter dayi per claim)

SIGNATURE:_Author of Report or Agent

Res. Gcol.. .Qualiiications.

Previous Surveys File No. Type Date Claim Holder

MINING CLAIMS TRAVERSEp List numerically

See attached list(prefix) (number) i

........................................................l

........................................................j

TfYI'AI r.I AIMS 27

LIST OF CLAIMS

Pa 720075

720076

720077

720078

720079

720080

720081

720082

720083

720084

720085

' 720086

720087

720038

Pa 720089

Pa 823397

823390

023399

323400

823401

823402

023403

823404

823405

323406

823407

823408

Total 27 claims

o

APPENDIX C

ROCK SAMPLE DESCRIPTIONS AND ASSAYS

ROCK SAMPLE DESCRIPTIONS AND ASSAYS

Assay Au Au Au No. Location Description oz/ton ppb ppm

3025 1100W, BLO sheared mafic vole., qtz., pid., 30 .237. py.

3026 450 W, 75N mafic vole., joints with qtz.,- 5 .1cc-epid. , 1-37. py.

3027 875 W, SOON rhyodacite flows, qtz.,-epid.- < 5 .1hem. stringers

3028 2780W, 25N sheared rhyolite, 1-37. po., 1-37. 15 .2fach., ser.

3029 3290W, 1880N qtz. stringers in docite?, tr.- -027 865 1.1

17. py. , tr.-.57. aspy.

3030 2500U, 2200S tonalite plug, lim., tr.py., 5 < .1fractured, 27. cc

3031 2400W, 2500S tonalite, qtz., tl. stringers, 15 < .1tr.-.57. aspy. lim.

3032 L64W, 2500N sheared int. vole., q.v.'s, tr.- 10 < .1.57. py. , lim.

3033 3950W, 1900N rhyolite, sheared, qtz. veins, cc, 5 < .1lim., tr.aspy., -57. py.

3034 3950W, 1900N rhyolite, sheared, qtz. veins, cc, 10 < .1lim., tr.aspy., -57. py.

3035 L12W, 2990N mafic flow, epidotized, tr.-57. py. 5 < .1

TRENCH A

Assay LengthNo. (Ft.)

3036 1.0

3037 2.6

3038 1.5

3039

3040

2.8

3.0

Au Description oz/ton

dac.-and flow, sil., cc

int. flow or tuff, sh., 2-37. cc.

ankerite zone,10- 157. carb, sheared 60-707. qtz. , sec.

as per 3037, tr.- .57. py.

dac. flow, 2-37. cc qtz. stringers

Au ppb

10

10

10

Agppm

c .1

.1

.1

.1

.1

Cu ppm

3041 3.0

3042 1.5

3043 0.2

as per 3040

as per 3040

q. v. , epid. on

10

10

5

< .1

< .1

< .1

selvage, chl. - cc stringers

TRENCH B

Assay Length Au An Ag Cu No. (Ft.) Description oz/ton ppb ppm

3044 1.8 int. flow, qtz. < 5 < .1 stringers,lim.

3045 2.0 as per 3044, < 5 < .1 sheared, cc-lim. rind. q.v.'s

3046 1.5 ank. zone as per 20 < .1 3038

3047 3.0 as per 3039 < 5 < .1

AssayNo.

3057

3058

3059

3068

3069

3070

3071

3072

3073

3074

3075

Length(Ft.)

3.0

3.0

3.0

2.3

3.0

1.0

0.5

2.2

3.0

2.8

0.7

TRENCH C

AuDescription oz/ton

dac. and flow

as above, minormafic material

dac. and flow,lira, rind

as per 3059

as per 3059, 1-57. aspy., py.,lim. rind

as per 3069 .070

q.v, , lim. , 1~37. py. , aspy. .028overall

sil. int. andflow, lim. rind.tr.-.57. py.

as per 3072

as per 3072

q.v., 15-507. .240

Au Ag Cuppb pptn ppm

215 .1

40 < .1

40 < .1

95 .2

145 < .1

1,630 .7

1,185 .5

380 .3

80 .1

120 .1

7,460 2.3

3076 1.3

3077 1.3

3078 0.3

aspy. , tr. - .57. py./cpy., tr.- .57. cc

int. and flow, tr. .57. aspy. , 2-37. cc. lim rind

q.v. ,3-57. aspy. , py.

q.v. , 3-57. aspy. 2-37. cc

65

325

505

.4 123

.2 142

.3 243

TRENCH D

Assay LengthNo. (Ft.)

3060 3.0

3061 2.85

3062 3.0

3063 1.5

3064 1.4

3065 0.95

3066 1.3

3067 2.6

3079 3.0

3080 2.1

3081 2.6

Description

bleached mafic vole. , lim. rind, massive

as per 3060, minor qtz.-carb. stringers

as per 3060, lim. rind, chl.stringers

as per 3062, silicified qtz. veinlets, chl. stringers

as per 3063, 0.07 1 q.v. with 17. py.

q. v. , 507. a spy. , 27. cc, 1-27. cpy. tr. py.

q.v./carb, zone, sheared, 3-57. aspy . 3-57. py.

bleached, shear ed , vein wallrock, 3-57. aspy. , 3-57. py.

bleached mafic vole.? tr. py. lim. rind.

as per 3079

as per 3079, minor qtz. str ingers

Au oz/ton

Au Ag Cu

.30

100

210

75

65

105

390

280

25

.1

.1

.1

.1

.1

13,410 22.2

4.4

7.4

.5 98

< 5 .4 69

5 .4 79

TRENCH E

Assay LengthNo. (Ft.)

3082 3.0

3083 3.0

3084 1.4

3085 2.5

3086 1.8

3087 1.7

3088 2.4

3089 3.0

3090 3.0

3091 grab

3092 2.8

3093 0.7

3094 1.5

AuDescription oz/ton

silicified blea ched and., qtz. stringers,cc-py. veinlets

as per 3082

as per 3082

as per 3082,15- 207. carb. , 4'-5' carb.,tr. py.,cpy.

as per 3085, .5- 17. py./aspy.

sheared and. dac. tr. -. V7. aspy. ,

tr . py . , qtz. cc- py. veilets.

q.v. , 2-37. aspy. l PY-

Au

.066

as per 3088, tet rahedrite?

q.v. contact zone, tr.py.aspy. bleached vole.

qtz. -aspy .veins with carb.

bleached and.- dac. qtz.-cc- epid. stringers

sheared vole . , triable, 1-37. aspy., qtz. stringers

bleached vole. , 1-37. aspy.

.058

.047

350

2,010

40

4,685

50

1,060

100

Ag PP"1

.1

.2

.5

.1

.2

CuPPm

22

5 < .1 32

5 < .1 26

5 .1 23

44

.9 417

1.4 106

70

50

1.5 105

79

.7 120

.8 156

TRENCH F

Assay LengthNo. (Ft.)

3095 3.0

3096 0.15

3097 2.6

3098 0.3

3099 1.7

3100 2.0

3301 3.0

Description

bleached vole., mafic?, tr.-.57. cpy., qtz. stringers

q.v., x-cutting, tr. py.

carb, shear zone 0.3' q.v. with tet.? 3-57. aspy. py., tr. cpy.

q.v. offsett from 3097

bleached vole., 0.4' q.v. with 2-37. aspy. , 3-57.py.

triable, limon- itic, sheared vole., 0.3' q.v. with 3-57. aspy./py.

bleached vole, contact with q.v.

Au oz/ton

.132

.100

.053

Au ppb

115

270

2,865

?.,725

1,200

50

Ag ppm

.4

Cu ppm

69

1.2 520

2.5 189

4.4 2360

2.9 508

2.8 2270

1.2 142

3302 1.3 as per 3301 25 .2 82

TRENCH G

Assay LengthNo. (Ft.)

3048 2.4

3049 0.7

3050 0.2

3051 1.3

Description

massive and flow, 2-37. cc

as per 3048, fractured, lim. rind.

q.v., ochre, 10- 257. aspy. , py., tr.-.57. cpy.

silicified and?, 1-107. aspy. ,tr. cc

Au oz/ton

49

.023

Au Ag Cuppb ppm ppm

5 .2

15

12,070

6,050

.1

5.6

1.9

3052 0.8

3053 0.7

3054 0.2

3055 O.i

q.v. 15-507. .670 aspy., massive aspy. , tr. - .57. py./cpy.

bleached int. .024 flow, 1-37. aspy. 707. qtz. , lim. rind.

bleached vole., .111 tr.-57. cpy. , 1-37. py. , aspy. q.v.'s

sheared, bleached vole. , lim. rind.

22,847 15.6

765

3,510

180

2.0

9.4

.6

3056 0.15 q.v. tr.-.57. cc 235 .9

TRENCH H

Assay Length Au Au Ag Cu No. (Ft.) Description oz/ton ppb ppm ppm

3325 3.4 chl.-ser.-qtz. 10 < .1 23 schist (bleached mafic vole.?) cc

3326 2.0 sheared carb. .050 1,)AO .2 23 zone, friable, qtz.-cc vein- lets

3327 2.8 bleached vole., 145 .2 41 5-17. aspy.

TRENCH I

Assay Length Au Au Ag Cu No. (Ft.) Description oz/ton ppb ppm ppm

3312 3.0 massive silic- < 5 .2 29 eous int. vole. -0.1' q.v.

3313 1.1 shear zone, ser.- 195 .2 30 chl. qtz. schist

3314 2.1 massive ank. < 5 .2 24 zone, 17. py., cpy.? ser. schist

3315 3.1 0.2' chl. schist, 45 .3 44 int. vole.

3316 3.0 massive It. green 5 .1 36 vole. V' q-v., 0.2' shear, 27. cpy. , 57. aspy.

TRENCH J

AssayNo.

3306

3307

3308

3309

3310

3311

Length (Ft. )

3.3

1.7

1,7

3.1

2.1

2.1

Au Description oz/ton

bleached mafic vole. , ank. , chl. stringers

sheared ank. zone ser., chl., 0,1' q.v.

ser. schist, 0.4' q. v. , ank. , +1.

massive bleached vole. , tr . py. , lim. rind.

as per 3309, tr. .57. py. , chl. stringers, v.f.g. red mineral

as per 3310, 0.2' shear, 0.21' qtz.- carb. , .57. aspy .

Au ppb

AS Cu

10

30

.1

.2

37

15

25

30

18

15

TRENCH K

AssayNo.

Length (Ft.)

Au Description oz/ton

Au Ag ppb PPm

Cu ppm

3303 2.5 siliceous int.- 5 .1 30 mafic vole., shearing, tr. sulphide

3304 2.0 ser. schist, ank- 55 .1 10 erite, sheared

3305 2.6 as per 3304 10 < .1 25 possibly sheared mafic vole.

TRENCH L

Assay Length AM Au Ag Cu No. (Ft.) Desc ciption oz/tot: ppb ppm

85-90 0 qtz., tr.- .57. py./aspy.

3328 2.5 ser.-chl.-qtz. 40 .3 71 schist qtz.-chl. sulph. veinlets

3329 3,0 sheared vo]-.., 40 1.4 771 fissile, limon- itic, 1-37. py. , 27. a spy.

3330

3331

3332

3.0

1.3

2.1

as per 3329

as per 3329

bleached mafic?

10

10

< 5

.2

.1

.2

160

56

70

TRENCH M

AssayNo.

3317

3318

3319

3320

Length(Ft.)

3.2

3.15

2.25

2.9

AuDescription oz/ton

grey chert, 17.py. , minor vole.interbeds

as per 3317, tr.py.

as per 3318

carbonatized

Au Ag Cuppb ppm ppm

< 5 .2 81

< 5 .2 53

< 5 .1 84

10 .1 62vole. , tr. aspy. cc, py.

3321 2.5 as per 3320, ma fic? tr. epid. , chl.

3322 2.0 silicic ank. zone in mafics, shear -ed tr. py. l a spy.

3323 2.2 as per 3322, buff schist

3324 2.3 as per 3323, v. limoni tic

10

10

.2

.2

.2

54

88

55

61

APPENDIX D

ASSAY CERTIFICATES

Hi i fir "l q A Comj-jij Ud.

TM Bclfts Ko*d a*), Onuno

v^^-^Tr^w^*,^ '- 1 "' ' ,*-*i

LabG*oc lemicaJ

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PROJECT: iGijDHirw t?' -i": 7j?:TT

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DE1ECTIOI! LI^IT E?IF::C*;

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SE.URKS: :: TE^S LEtS THJIH .

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REPORT: 015-3074 ( COMPLETE ) ] | REFERENCE wo;CLIENT: MISS RESOURCES SUIIUTKD UT: JOH XDKTHPROJECT: AGUTUA ARH DATE PRINTED: 3o-SEP-es, . . .. ... . .. ... . . . . . . . ..... i. .. ......

. . L .......

ORDER

1 2

3 i,

SARPLE

SOIL

mm O F LOVERELEHENT ANALYSES DETECTIOH LIBIT EXTRACTIOI flETHOD

[B Copper 11 1 PPR HC1-HH03, (1:3) Atoiic Absorption A 9 Silver H 0.1 FPB HCI-HH03, (1:3) Aloiic Absorption

. . . . - . . jAu Sold 11 I PFI AfiOA IEBIA FTreAssajiACarbohKDo'

Testyt Au Test Ueight 1 0.01 gi

TYPES Mm S IZE FRACTIOUS UMBER SAHPLE PREPARATIOHS UMBER

H —— " " -B5 ' II " URTTSTIVl -BO 11

: ( (1EAHS LESS THAH \

j

SEPORT COPIES TO: H.J. HODBE JOX NOKTH

trnnp**} Lid

Ibt Betlta Hou) On**.. Oi.ia/io Geocliemical

REPORT: 015-307i

SARPIE ElEflENT NURBER yXITS

AA L33y-00 AA L33y-lS AA L33y-2S AA L33M-3S AA L33U-4S

AAL33y-5S AAL33y-lM AAL33V-2K AA L33U'3M AA L33IHH

Cu PPB

5 12 24 10 li

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Certificafe of Analysis

[ _ J^i^j^jjl™''CLIENT: HGSS RESOURCESPROJECT: A6UTUA ARfl

SUs.lITTED BY: JON fiflRIH DATE PRINTED: 27-SEP-E5

ORDER ELEfltHT

i Au Gold -Assay

mm O FANALYSES DETECTION LlfUT EXTRACTION J1ETHOD

7 0.001 0/T

SARPLE TYPES

OTHER

H'JURER

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SIZE FRACTIOUS

-200

KURBER

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SAMPLE PREPARATIONS NUMER

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REPORT COPIES TO: H.J. HODGE JOH XORTH

INVOICE TO: H,J. HODBE

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Certificate of Analysis

REPORT; 415-2722 1 COBPLET U H REFERENCE INFO;CLIENT: BOSS RESOURCES ROJECT! AllTUUR

SU&HITTED 6T: JOH HDRTH DATE PRINTED: 2t-SEP-85

ORDER ELE/IEHTOF LOiER

ANALYSES DETECTION UdlT EXTRACTION /IETHOD

Au Gold -Assay 8 0.001 0/T 0.01 0/T

SAHPLE TYPES

OTHER

KURBER

B

SIZE FRACTIONS

-200

NUMBER

B

SAMPLE PREPARATIONS BUBBER

PULVERIZIHB 3

REMARKS: OTHER SAKPLE TTPE REFERS TO REJECT.

REPORT COPIES TO: H. J. HODtE JOHIORTH

INVOICE TO: HJ. HODGE

pu} lid.

i Ra.OHJWJ. Ontana

Phone ( T.ki 0!J 3

of ^nalysis

REPORT: U

SAflPLEXURBER

30503051305230543065

3J7030713075

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REPORT: 015-28^3 i COMPLETE ) j RTFlRTNCTlNfor~

CLIENT: KDSS RESOURCES PROJECT: AGUTUA m

ORDER

i2

ELEMENT

Cu CopperAg Silver

mm O FANALTSES

5757

LOyERDETECTION LISIT

1 PPR1 0.1 PPR

~

SUP.fllfiED i r- R . HI66!iifiOil DATE PRINTED: 17-SEP-85

EXTRACTION

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flETHOO

Atoiic AbsorptionAtonic Absorption

3 Au Bold 57 5 PPB ABUA RE6IA FA-AA e 10 31 veight————

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K',..iir,ityolNnturalFlcsources

Ontario

Report of Work(Geophysical, Geological, Geochemical and Expenditures)

The Mining Act

Imlructioiu: -- rlc;i',o lyp" nr print,— !f number of mining c!aim^ linvr-rsiMl

excopd? sp.ico on this form, aijtnch n l'5t.l Noio: — Only days credits calculate^ In th*

"Expenditures" section may iff c riierrtdIn !ho "Expend. Dnys Cr."! columns.

— Do not use shaded areas below.]Typa of Survay(i)

GeologicalClaim Holdorli)

Moss Resources Ltd.Address

JTownihlp or Arm

Randall ^b PV'oVi"ictor'TiTic" encTRa--

804-34 King Street East Toronto, Ontario M5C 1E5__|6ate o? Si/rvev Ifrom A to)

06 08 85 28 08Day Mo. l Yr.

Company

Geocanex Ltd.Nam* And Addrtu of Author {of Qto-Tachnlca! rtport)

Jon W. North 1669 St. Gabriel Ct. Windsor, Ontario N9E 1P24—

Credits Requested per Each Claim in Columns at rightSpccijl Provisions

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

For each additional survey: using the same grid:

Enter 20 days (for each)

Man Oayt

Complete reverse side and enter total(s) here

*

Airborne Credits

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

Geophysical

- Electromagnetic

- Magnetometer

- Radiometric

- Other

Geological

Geochemical

Geophyi leal

- Electromagnetic

- Magnetometer

- Radiometric

- Other

Geological

Geochemical

Electromagnetic

Magnetometer

Radiometric

Days per Claim

-

~40

Doyi per Claim

Days per Claim

Mining Claims Traveiscd (List in numerical sequence)

Expenditures (excludes power stripping)Type of Work Performed

Performed On Claim(s)

Calculation of Expenditure Days Credits

Total Expenditures

S 4- 15

Total Days Credits

s:

Instruction! Total Days Credits mey be apportioned at the claim holder^o choice. Enter number of deyi credits par claim telected/'y' In columns at right. S X

Mining C'fl'mPrefix

'•i j ;.\..V:: 5OVV

Number

See at list

E xpend. Roys Cr,

ied

.W-i-8-t-!W"

..s r/

1986

v.

'.f:'

?r

Mining Claim Prefix Number

^Expend. Cr.

1.

Total number of mining clnimt couersd by this report of work.

Recorded^olde/or AgerrjKignature)

Certification Verifying Report ofWofl?

For Office Use OnlyTotel Days Cr rtecoided

HB co r d ad

as Hecordoo Branch Oirlctor

1 hereby certify that 1 have t personal and intimate knowledge of the fact? set forth in the deport of Work annexed hereto, having performed the i|vork or witnessed same during and/or alter its completion and the annexed report is true. i

Name ond Postal Address of Person Certifying s?

H. J. Hodge fi'

804-34 King St. Easttare IB i/o),- -.r,*.^,, wi*.'^ ; i; ".'"••; T " [ '^J?jTt 'JT5'"^T , *^"V WJ

J Oite Certified Certified by

Toronto, On t. M5C 1E5J f?n. f^/^ ( -

i ; '

(Signature)/

r?^

AGUTUA ARMS PROPERTY

LIST OF CLAIMS

Pa 720075720076720077

720078

720079

720080

720081

720082

. 720083

720084720085720086720087720088

Pa 720089

Pa 823397

823390823399823400823401823402023403823404823405823406823407823408

Total 27 claims

^E'cEs'tf fejjjiJAN-6 ^6

P.I t

\F*^*Wmml

-t-'

Onlnrlo

Ministry ofNorthern Developmentand Minesu

Technical Assessment Work Credits

Fllo

c.198.6-02.02..

.___^I Mining Recorder! R eport of Work No. l

Recorded Holder

MOSS RESOURCES LTDTownihlp or Arei

RANDALL LAKE AND KEEYASK LAKE AREAS

Type of survey and number of Assessment dayi credit per claim

Geophysical

|nrlnr*d Pol*rl'*t'O" , Hayt

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

Geological . lo ,1ay,

Opochoniical , , riayi

Man days [~] Airborne L]

Special provision [X] Ground [3

[X] Credits have been reduced because ol partial coverage of clairm.

*

L~U Credits have been reduced because of corrections to work dates end figures of applicant,

Mining Claims Assessed

PA 720075 : 720077 to 089 inclusive; 823397 to 404 inclusive. 823406-07-08

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

No credit! have been allowed for the following mining claims[X] not jufficienlfy covered by the survey

PA 720076 823405

( ] insufficient technical dels filed

Linecutting credits previously granted on Report of Work #85-68.

The Mining Recorder may reduce the above credits if necessary in order that the total number o( approved assessment days recorded on each claim cjoes not exceed the maximum allowed as follows: Geophysical - 80; Gcologocal - 40; Geochemical - 40; Section 77(19)-60.

828 (85/1?)

801-34 KING ST. EAST TORONTO, ONTARIO M5C 1F.5

(416)862-9078 ^MOSS RESOURCES LTD.

January 13th, 1986

Mr. S.E. YundtDirectorLand Management BranchRoom 6643, Whitney BlockQueen's ParkToronto, OntarioM7A 1W3

RE: Geological Reports- Randall.Lake and Agutua Arm Properties

Dear Mr. Yundt,

I am enclosing two (2) copies each of Geological Reports on our Randall Lake and Agutua Arm Properties.

I hope everything is in order.

Yours very truly,

MOSS RESOURCES

i.J. Hodge, P. Eng. President

HJH/sw Encls .

RECEIVED

MINING LANDS SF.CllOfl

mn

' ~WW*•- jlfH;t :;' ' p A t? t.'. .^ Ui3. :V

\

( i Ontario^~-*

Ministry ofNorthern Development and Mines

1986 02 07 Your File: 86-5 Our File: 2.8798

Mining RecorderMinistry of Northern Development and MinesP.O. Box 309Sioux Lookout, OntarioPOV 2TO

Dear Sir:

Enclosed are two copies of a Notice of Intent with statements listing a reduced rate of assessment work credits to be allowed for a technical survey. Please forward one copy to the recorded holder of the claims and retain in? other. In approximately fifteen days from the above date, a final letter of approval of these credits will be sent to you. On receipt of the approval letter, you may then change the work entries on the claim record sheets.For further information, if required, please contact Mr. R.J. Pichette at (416) 965-4888.

Yours sincerely,

f-i

S.E. Yundt, Director Land Management Branch

Mining Lands Section Whitney Block, 6th Floor Queen's Park Toronto, Ontario H7A 1W3

.SH/mc Ends.

cc: Moss Resources Ltd Suite 80434 King Street East Toronto, Ontario M5C 1E5 Attention: H.J. Hodge

Jon W. North 1669 St. Gabriel Ct. Windsor, Ontario N9E 1P2

G.H. FergusonMining S Lands Commissioner Toronto, Ontario

•v rv w•ip:'M-i-- 'Hie*;j^! i•f4.. j;:-i' H rf. 1 :! ; i ;'i s#:•••*\w ff^m•m^fi i;:i P:

Ontario

Ministry ofNorthern Developmentand Mines

Notice of Intc-ntfor Technical Reports

1986 02 07 2.8798-86-5

An examination of your survey report indicates that th: requirements of The Ontario Mining Act have not been fully met to warrant maximum assessment work credits. This notice is merely a warning that you will not be allowed the number of assessment work days credits that you expected and also that in approximately 15 days from the above date, the mining recorder will be authorized to change the entries on the record sheets to agree with the enclosed statement. Please note that until such time as the recorder actually changes the entry on the record sheet, the status of the claim remains unchanged.

If you are of the opinion that these changes by the mining recorder will jeopardize your claims, you may during the next fifteen days apply to the Mining and Lands Commissioner for an extension of time. Abstracts should be sent with your application.

If the reduced rate of credits does not jeopardize the status of the claims then you need not seek relief from the Mining and Lands Commissioner and this Notice of Intent may be disregarded.

If your survey was submitted and assessed under the "Special Provision-Performance and Coverage" method and you are of the opinion that a re-appraisal under the "Man-days," method would result in the approval of a greater number of days credit per claim, you may, within the said fifteen day period, submit assessment work breakdowns listing the employees names, addresses and the dates and hours they worked. The new work breakdowns should be submitted directly to the Land Management Branch, Toronto. The report will be re-assessed and a new statement of credits based on actual days worked ^ill be issued.

.ii;- !- mrnf'';;;,:---^Iii

March 4, 1986 Your File: 86-5 Our File: 2.8798

Mining RecorderMinistry of Northern Davelopwant and MinesP.O. Box 309Sioux Lookout, OntarioPOV 2TO

Dear Sir:

RE: Notice of Intent dated February 7, 19fl6 Geological Survey on Mining Claims PA 720075, et al, 1n the Randall Lake and Keeyask Lake Areas

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,

J.C. Smith, Supervisor Mining Lands Section

Whitney Block, 6th Floor Queen's Park Toronto, Ontf/Mo M7A 1H3

Telephone: (416) 965-4888

SH/mccc: Moss Resources Ltd

Suit* 80434 King Street EastToronto, OntarioM5C 1E5Attention: H.J. Hodge

Resident Geologist Sioux Lookout, Ontario

Oon W. North 1669 St. Gabriel Ct. Windsor, Ontario N9E 1P2

Mr. G.H. FergusonMining A Lands CommissionerToronto, Ontario

End.

'MM'!-''gmk

LEGEND

QUATERNARY

30 N

20N

ION

B.L.00-90

ooCD CD

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5:srCM

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AGUTUA ARM

2a

BL.2IS

30 S

405

PINE AND HARDWOOD

GLACIAL OVERBURDEN

720076 -__

l___130,30^.___ i___^\. i-)*. V ^ ~- -~

Hardwood foresl Agutua Arm Cu-Au-Ag showing,Trenches A-Karea enlarged onDwg. No. 5 )

glacial overburden

720 .083

DEADFALL ON HUMMOCKY OVERBURDEN

., - 'q.v.epidt —^t

720 -- 089 :*

, DEADFALL ON OVERBURDEN

720

086 '3028 po,.fu

sh.py.q.v.

2o epid.py ::.--r-^ sK 4 -

Trenches L a see Dwg. No. 6

3c,3d,4b Ai

**zr--J*—r399D E A D FA L L

ON GLACIAL

OVERBURDEN

DEADFALL '

OVERBURDEN..-l-:-3c,3d,5b.....

3031 qtz tl.aspy

HARDWOODGLACIAL OVERBURDEN

PROBABLE SUBMERGEDLOCATION OF

THE N.CARIBOU •RIVER Ag-Zn-Pb ~

OCCURRENCE

-—— — -~ ,;;.v2a

NORTH CARIBOU RIVER

500t^

53B14NEW28 53et4SEM28 RANDALL LAKE

1000 t

1500 t -

2000 i - t T

ddhqvSh9" sil ser ccpypo a spycpy ga spa l bn9f"mt litn tl mo

Stream, lake, bog deposits Glacial, glociofluvial lacustrine sediments

LATE PRECAMBRIAN (Keeweenawan?)

Ma Diabase

EARLY PRECAMBRIAN

Intermediate and Felsic Intrusives!0a Granite pegmatitelOb AplitelOc Granitel Od Syenite10* Quartz monzonitelOf GranodioritelOg TrondjemitelOh Quartz diorite(Oj Diorite10k Unsubdivided gneiss10 l Granite gneiss

Mafic Intrusives9a Unsubdivided9b Gabbro9c Leucogabbro9d Plagioclase-phyric gabbro9e Peridotite9f Pyroxenite

Iron Formation8a Oxide facies8b Carbonale facies8c Silicate facies6d Sulphide facies

Chemical Metasediments 7a Chert 7b Calcitic marble 7c Dolomitic marble

Clastic Metasediments6a Clast supported conglomerate6b Matrix supported conglomerate6c Oligomictic conglomerate6d Polymictic conglomerate6e Sandstone , Unsubdivided6f Wacke6g Arenite6h Mudstone, argilliteSj Feldspathic wacke6k Feldspathic arenite61 Quartz arenite6m Schistose rock i omphibole,± biotite,

± garnet, ± chlorite of probablesedimentary origin

Felsic and Intermediate Subvolcanic Rocks5a Unsubdivided5b Quartz-feldspar porphyry5c Quartz porphyry5d Feldspar porphyry

Felsic Metavolcanics

4o Massive fine-medium grained flow4b Pyroclastic breccia , tuff breccia

j 4c Tuff, lapilli tuff

Intermediate Metavolcanics3o Massive fine-medium groined flow 3b Flow breccia3c Pyroclastic breccia, tuff breccia 3d Tuff , lapilli tuff

Mafic Metavolcanics2a Massive fine-medium groined flow2b Amygdaloidal flow2c Variolitic flow2d Pillowed flow, pillow breccia2e Flow breccia2f Medium-coarse grained flow centres2g Plagioclase-phyric flow2h Amphibolite2t Co-magmatic sills, dikes2j Pyroclastic breccia, tuff breccia2k Tuff, lapilli tuff21 Chorite ± amphibole schist

Ultramafic Metavolcanicsla Massive fine-medium grained flow Ib Spinifex textured flow le Talc-carbonate i magnetite ± amphibole

± s erpentine ± chlorite schist

SVI1BOL5 l ABBREVIATIONS

xxxxxxXx

diamond drill holequartz veinshearinggneisssil icificationsericitizationcarbonatizedpyritepyrrhotitearsenopyritechalcopyritenalenasphaleritebornitegraphitemagnetitelimonitetourmalinemolybdenite

beaver damscarpwatercreek with flow direction, intermittentwet groundclaim post, claim l inetownship line

trenchdiamond drill holebedding strike, dip, top directionfoliation strike, dipgneissosity strike, dippillowed flow, top directiongeologic contact, inferredqeoloqic contact inferred fron geophysics

fault, inferredslope, steep slope pointing downhill

bush road, winter road

MOSS RESOURCES LTD -- TORONTO

AGUTUA ARM PROPERTYNORTH CARIBOU LAKE AREA Patricia Mining Division, Ontario

GEOLOGY

GEOCANE.X LTDTORONTO. CANADA

BY:DATE: NOV. 1965SCALE: l":400'DWG. No:

- 16 -

68ppb

E E SQ. g- Q.Q. d Q.

oC*

30 -i 3 .0 T 30 n

25 -

20-

15 -

10-

5-

O J

2.5 -

2.0-

1.5-

1.0 -

0.5 -

O J

25 -

20-

Gold, Silver, Copper in Humus

6 EQ. Q. Q.^ -

o30 -, 3,0 i

25 H 25 -

20 -

15 -

10 -

5 -

O J

2.0-

.5 -

1.0 - l

0.5 -

O J

30 i

25 -

20 -

15 -

10 -

5 -

O J

Gold, Silver, Copper in B Horizon Soils

5 N 4N 3N 2N 00 IS fe 3S 43 5S

Main shear zone with quartz-arsenopyrite veins

Subsidiary ankerite zone

ICE DIRECTION

5N 4N 3N 2N 00 2S \

3S—i—

4S 55

Main shear zone withquartz-arsenopyrite veins

^ Subsidiary ankerite zone

ICE DIRECTION

MOSS RESOURCES LTD.

Aguatua Arm Property

Aguatua Arm Au-Ag-CuShowing Orientation Soil

Geochemistry Profile

QEOCANEX LTD TORONTO. CANADA

BY; R T. M.DATE; AUG 1985SCALE: l :lOft.DWG. No: 4

PART

Aguatua Arm of Weagamow Lake

332? n-r o-i l tiJlltS, /fit, ' l t) IStf, to 'f ' , J!

Sheared ankerite zone

Silica-carbonate alteration zone ishearing ± quartz stringers

V'5 Quartz vein ± carbonotized volcanic

Geologic contact , inferred

Foliation , dip indicated

Joint , dip indicated

3641 1 /f .,, . , Chip sample , classified os such ' number, Au ppb , Ag ppm , Cu ppm

- iw r*i f ) M G rab sample

i ..J— c Soil sample station, showing - ' v^ ""Au in B Horizon (ppb)

--— ---™Au in humus (ppb)

*~-t~—*' S carp

Outcrop, trench

- - T. L. 18 t 27 N

Main Shear Zone

f Subsidiary Ankerite Zone

Trench ATrench K

2 + 5'

53B14NEM28 53814SEM20 RANDALL LAKE aio l

MOSS RESOURCES LTD.

Aguatua Arm Property

Trenches A-K

QEOCANEX LTD TORONTO. CANADA

BY: R T. M DATE: Aug. 36. 85SCALE: T i IQft. DWG. No: /3