42CC2SE0004 2 16363 LAST HEELS 010

fir s n

. 163 63

SUMMARY REPORT

Firesand Carbonatite Diamondiferous Study

Geological. Magnetics. Electromagnetics. Backhoe Bulk Testing

Lastheels A McMurrav Townships. Northern Ontario

by

Frederick T. Archibald, B.Sc. Geologist Novembers, 1995

42C02SE0004 2 16363 LAST HEELS 01OC

INDEX

Summary 1

Property A Location 3

Property Access 3

Topography 3

Location Plan of Claim Group (1'^1200m) 4 PLATE A

History 5

Chart 1- Gold Producers in Close Proximity to Property

Diamond Source Structural A Emplacement 8

Firesand Carbonatite Complex

Table of Lithological Units

Property Claim Description

Regional Geology

Geological 81. Structural Plan

Local Geology

Property Geology

Geological Plan

Economic Geology

Specifics of VLF Electromagnetic Survey

Results of VLF Electromagnetic Survey

Specifics of Proton Magnetometer Survey 25

Results of Proton Magnetometer Survey 26

9

10

11

12

14 PLATE C

15

17

20 PLATE K

21

22

24

Backhoe Pits and Washing Plant 28

Backhoe Location Plan 29 PLATE B

Results of Bulk Sample Concentrate Analyses 30

Conclusions 81 Recommendations 34

References 36

Cost Estimate 37

Certificate 38

Sampling Program Map A Stats- 1174419 39

Microscopic Examination Results 40

Gold Analyses 43

Daily Journal of Work 44

Claim Breakdown of Work 45

Breakdown of Costs 46

APPENDICES

Regional Structural Geology Plan Plate C

Local Geological Plan Plate E

Local Airborne Anomaly Plan Plate F

Proton Magnetics (1" to 100 meters) Plate G

VLF Electromagnetics- Dip Angles (1" to 100 meters) Plate H

VLF Electromagnetics- Field Strength (1" to 100 meters) Plate J

Photographs

Program receipts

Claim Abstracts

Claim Extensions

Firesand Carbonatite Diamondiferous Study McMurrav-Lastheels Townships. Northern Ontario

Introduction-

During the months of August and October of 1995, F.T. Archibald Consulting

Ltd. was contracted by Elliot Feder to perform work over a group of claims in the

northeastern part of McMurray Township and the northwestern part of Lastheels

Township in order to delineate potential for diamondiferous sources. The work was

performed over a group of eleven claim groups totalling some 59 claim units. A total of

S31.856.14 was spent on the claim groups.

The author has many years experience both in exploration for diamonds and in

production mining of diamonds.in Africa (Liberia), South America (Surinam and

Venezuela), and Canada (Labrador). F.T. Archibald performed a B.Sc. Thesis at

Carleton University in 1977-1978, evaluating the heavy mineral suite associated with

diamondiferous bearing kimberlites and related materials.

In the summer of 1991, diamonds were discovered in the southwest corner of

McMurray Township, and consequencial studies by Tom Morris of the Ontario

Geological Survey have confirmed that indicator minerals in the area indicate

diamondiferous sources in the area are possible.

Areas chosen for concentration of prospecting for kimberlites (diamondiferous

host rocks) were on the basis of: 1) locations in the direction of glacial flow (up-ice)

from the original find, 2) closeness of proximity to deep seated fault systems 3)

closeness to ultramafic rock swarms (including peridotites and carbonatites). The area

in which the surveys were performed satisfies all of the above criteria.

The area was geologically mapped in addition to compilation studies of

airborne electromagnetics and magnetics. Some twenty-three kilometers of VLF

electromagnetics and twenty-three kilometers of proton magnetics were carried out

over the property. Several gold showings lying within the claim area were trenched

and sampled. A series of thirteen backhoe pits were dug in selected areas; in close

proximity to major deep-seatefd faults, at the junctions between faults, and in areas of

circular magnetic (ground and airborne) features. These samples were trucked to a

portable-mobile washing plant and concentrated by sluicing methods to a concentrate

which was sent to a laboratory for heavy mineral separation and identification.

During the sluice- plant concentration process, gold flakes were observed in at

least six of the pits. One of these pits (Bulk #5), located at the northeast contact of the

Firesand Carbonatite Complex and the junction of the Firesand Creek Fault, indicated

higher than normal amounts of gold flakes and a possible source area for gold.

The proton magnetometer survey delineated a 400 meter circular conductor at

the edge of the Firesand Carbonatite Complex. This is significant and should be

further investigated by sampling and/or drilling.

On December 11th, 1995, the Ministry of Northern Development and Mines

(MNDM) announced the discovery of at least four or five parallel kimberlite dykes in

the Lagarde Hill area of McMurray-Lendrum Townships. These narrow dykes, flat and

steeply dipping, trend in a northeasterly direction and cut through the north part of

Ward Lake and through the north part of the claim group. These trends match up with a

major northeasterly trending fault which cuts the property. As well, this strike lines up

with the Firesand Carbonatite Complex. The fact that kimberlites have been

discovered in this area along with diamonds in the surficial gravels has indicated that

this area has potential for diamondiferous kimberlite pipes.

The original diamond discoveries and heavy-mineral tracings to date have

indicated that the diamonds are traceable upstream of Wawa Creek- Ward Lake which

also indicates that the property has significance as far as potential to find diamond-

bearing kimberlites in this area.

Although it is not known as yet whether the newly discovered kimberlite dykes

are diamoniferous, it is thought that these dykes could be secondary feeders from one

or more kimberlite pipes along a defined fault trend. Two promising targets could be

the Green-Emerald Lake anomaly or another circular airborne anomaly over claim

1174477.

Airborne magnetics show at least ten anomalous targets (four negative and six

positive) underlying the claim group. Another nine airborne targets are within six

hundred meters of the claim boundary. At least ten of the ninteen anomalies coincide

with fault structures; areas where it is expected to find kimberlite pipe structures.

Only six of the airborne targets have been prospected, and the rest are potential

areas which should be investigated by prospecting and bulk sampling. Significant

gold analyses in the pit operations should also be prospected.

Property SL Location-

The property is located within McMurray Township (northeast corner) and

Lastheels Township (northwest corner). The survey was performed over a contiguous

group of ten claim blocks totalling some 55 units. These claims consist of unpatented

mining claims which need in excess of 322,000.00 assessment work performed

before November 5, 1995 through January 14, 1996 for another years extension of

time. Most of this group has extensions of three months to apply the work.

The claims are located in the Wawa area of the Sault Ste. Marie Mining District

of Northern Ontario. The claims are located on the Michipicoten Harbour (1:50,000 )

NTS41N-15 sheet.

The claim group consists of a contiguous to semi-contiguous group of claims

described as follows:

1174419 (2 claims) McMurray Township

1174416 (8 claims) McMurray Township

1174421 (4 claims) McMurray Township

1110143 (4 claims) Lastheels Township

1110144 (1 claim) Lastheels Township

1174510 (5 claims) Lastheels Township

1201471 (12 claims) Lastheels Township

1201472 (12 claims) Lastheels Township

1201473 (4 claims) Lastheels Township

1174509 (3 claims) McMurray Township

1174480 (4 claims) McMurray Township

TOTAL- 59 claims (323,600 expenditures needed to extend to Nov.5,1996 to

January 14, 1997)

Additonal claim groups are also recommended to be kept as they are in line of

strike with the new kimberlite dyke discovery. These claims have been picked up on

speculation at a cost of S2500. These consist of thirteen units and are numbered as

follows:

1174413 (3 claim) restaked number

1174420 (1 claim) restaked number

1174477 (8 claims) restaked number

1174412 (1 claims) restaked number

March 8, 1996

March 8, 1996

March 8, 1996

March 8, 1996

March 8, 1995

March 8, 1995

January 14, 1996

January 14, 1996

January 14, 1996

March 8, 1996

February 9. 1995

PLATE A

f- CHABANNEL TOWNSHIP ESQUEGA TOWNSHIP

MCMURRAY TOWNSHIPLASTHEELS TOWNSHIP

SURVEY GRID

LOCATION PLAN

SURVEY GRID 8 CLAIMSSCALE

. ... _=H-_ . ^ O 400 aOO 1200 1600

The following are in good standing until March , 1996 but should be kept in

good standing due to the close proximity and significant location. A total of approximately 32400.00 is needed to keep these claims in good standing until March

3 to 21, 1997. These claims are as follows:1174530 (2 claims) McMurray Township March 3, 1996

1174531 (2 claims) Chabanel Township March 21, 1996

1174532 (2 claims) Chabanel Township March 3, 1996

Property Access-

The claim group is located some 229 kilometers northwest of Sault Ste. Marie,

Ontario.

The property can be accessed by several routes. The first is by Highway #101

east from Wawa for some 6 kilometers to the Firesand Creek Timber Access Road. The

property is located some three to four kilometers south along this gravel road to the

northern boundary. Lines 6 South to 5 North and Lines 16 South to 18 South bissect

this road. The road is presently being used year-round by a timbering operation to the

west of the claim group.

The other access is by way of the High Falls Road, south of Wawa for some five

kilometers along Highway #17, and then by gravel road to either the Surluga Road or

to another road 500 meters before the townsite of High Falls, where the Leroy Lake

trail can be accessed by ATV or skidoo vehicles to the southern portion of the property.

This trail joins up to the Firesand Timber Access Road.

Local Resources-

Power is available from power lines some five kilometers southeast of the

property. Good access is available from all-year roads; from Highway #101 some three

to four kilometers to the north and the High Falls Road some five kilometers to the

south. Water is available from Firesand Creek which bissects the central section of the

group in a southwesterly direction. Manpower is readily available from Wawa which

has an experienced labour force from at least five gold mines which have closed down

within the past few years.

Topography-

The central portions of the property are generally flat and coveredby glacial till

overburden. The northwestern and southwestern sections are covered with slightly

undulating relief and minimal overburden. The eastern sections of the property have

high relief with steep ridges averaging ten to twenty-five meters in height.

Most of the central and western sections of the property have recently been

timbered (within the past fifteen years). The areas on top of the cliffs (east of the

Firesand Creek) on the eastern portions have not been timbered for many years due to

access problems.

Tree cover in the lower flat lying areas consist of spruce ranging from 4 to 12

inches in diameter. In the higher areas the tree coverage consists of mainly birch and

spruce ranging from 8 inches to 24 inches in diameter. Tree cover is sparse and

spread out; and it appears that the pine have been timbered-out. Over 1174510, there

has been a recent planting of jackpine which have been inadvertently been burned-

over and replanted with black spruce (1993).

History-

It has been reported that a gold-bearing vein averaging 31.0 ounces per ton

was discovered on the north boundary of the Booth claims 3292 and 3293 in the

1920's. This showing strikes onto claim 1174419.

In 1936, J.H.Teare discovered 3 gold-bearing veins associated with northwest

trending iron formation, on the east side of Leroy Lake. One vein, some 457 meters in

length, assayed between 0.264 and 0.334 ounces Au per ton. Another assayed 0.197

ounces Au per ton. These veins are in line of strike with the southwest section of

1174416.

In 1961. Algoma Steel Corporation Limited summarized results of a low-grade

niobium mineralization within the Firesand Carbonatite Complex.

In 1962, the Algoma Central Railway completed an airborne magnetometer and

electromagnetic survey over the area.

In 1972, Algoma Steel Corporation drilled the outer rim of the Firesand

Carbonatite Complex to delineate calcite content for use in the sinter plant in Wawa

without success. At least three to four holes were drilled under claims 1110143 and

1110144. Between 1951 and 1972, some 4433 meters was drilled over the

carbonatite complex in some 39 drill holes.

In 1975, the Ontario Department of Mines under RT. Rupert completed a

geological mapping over the area.

Also in 1975, Kenting Earth Sciences finished an airborne survey over the area.

In 1976, International Minerals and Chemical Corp. drilled some 114 meters in

three holes to delineate the potential for apatite mineralization within the carbonatite

complex.

In 1979, AMAX Minerals Exp. explored gold showings in the area, and

discovered the Valenti showing of north-south iron formation with gold values. This

showing is in line of strike with claim 1174416 and is some 3.5 kilometers south of the

claim group.

In 1981 and 1982, R.P.Sage of the Ontario Department of Mines mapped the'

areas of McMurray and Lastheels Townships.

In 1983, R.D. Henderson completed manual stripping and trenching, and

geological surveys over the southeast portion of the property.

In 1986, Caviar Resources Limited worked on the Reed Lake claims to the

southwest side of the property, uncovering values as high as 0.49 ounces Au per ton

from felsic metavolcanics paralleling a gabbro-diabase dyke. At the same showing

some three tons of ore was milled in 1909 (Sears, S.M., 1986). In 1987, Citadel

Gold Mines performed a geological reconnaissance of the west portion of the claim

group.In 1988, P.P. Sage of the Ontario Geological Survey ( MNDM ) studied and

reported on the Firesand River Carbonatite Complex.In 1991, G.C. Clement Jr. collected samples from the Dead Creek area of the

Michipicoten River and the Wawa Creek area on the southwest side of McMurray

Township. Of some sixty possible diamonds, two of them approximately 1.13 and 1.05

carats were confirmed as diamonds by the Royal Ontario Museum. One of these was

considered 1/2 of an octahedron, and was probably cracked in half during transport.

In the fall of 1993, Tom Morris of the Ontario Geological Survey, bulk sampled

the Dead Creek and Wawa Creek areas, and confirmed that chrome pyrope garnets

(G 10) and diopside minerals were present. In the summer of 1994, Morris confirmed

that diamond indicator minerals were widerspread and in the areas northeast and east

of the original discovery; indicating that the original discovery was not just glaciated

material but in fact from the Wawa area.

In the fall of 1995, Currie Rose Resources discovered four kimberlite dykes on

Lagarde Hill; along the boundary of McMurray and Lendrum Townships. These

became visible due to a washout caused by a busted beaver dam along Coleman

Creek.

In the same time, MNDM located another kimberlite dyke to the west of the

Curry Rose Resources discovery, called the Nichols Dyke, which is in line of strike with

the initial discovery and is possibly part of the same system. This dyke has been

diagnosed as harzburgite xenolith ultramafic type.

These discoveries initiated a staking rush over these townships and townships

in line of strike with the kimberlite dykes.

Chart 1

Gold Producers Located in Close Proximitv to Feder Property

Name Rock Type Years Mined Tons Mined Oz. Au Mined

Golden Reed granite (mafic volc.cont) 1907-1908

Cooper Mine mafic volc.(porph.cont)

Grace-Darwin mafric volc(granite dyke) 1902-1937

Parkhill mafic volcanics

Minto sheared granite-diorite

S.B.Smith tuff(porph.cont)

Hillside tuff-basalt(porph.cont)

Deep Lake mafic vole.

Stanley mafic volc.(granite cont)

Surluga mafic-porphyry cont.

(148,245 tons @ 0.30 Au per toi

Jubilee sheared granodiorite

Mariposa mafic volc.(granite dyke) Van Sickle granodior(S tuff)

Citadel sheared granodiorite

1907-1908

1898-1939

1902-1937

1929-1938

1929-1942

1935-1936

1934-1935

1936-1938

1936

1968-1989

remaining)

1929-1930

1904

1936

i ORO. -man

3.0

4.889

45,528

125,778

184,600

9,228

200

2,790

1,963

90,155

2,462

9.0

9,228

6.0

1.303

17,586

54,301

37,678

1,536

224

1,633

84

8,019

421.8

16.9

1,712

e; nnn

Diamond Source Structure and Emplacement-

Diamonds are located within kimberlite host rocks and possible lamproite sources. Ultramafic rocks such as peridotites and eclog'rtes fit similar descriptions as

kimberi'ites.Diamonds are found in garnet-bearing harzgurgite and lherzolite peridotitic

rock (Gurney, 1989). Although orthopyroxene rich pyroxenrtes and dunrtes are

possible ultramafic source rocks which could contain diamonds; with minus 40*fc and plus nint/fc olivine contents respectively.

Diamonds are thought to have formed before the emplacement of the kimberlite bodies, and during rapid magma transit to the surface xenoliths of wallrock containing the diamonds are picked up and transported.

It is thought that diamonds are formed at depths between 150 to 200 kilometers (peridotitic) and depths greater than 300 kilometers (eclogite) (Gurney, 1989). tt is also thought that during tectonic plate collision, carbon (calcitic limestone) or carbonate- bearing rocks rifted under the upper plates and gave rise to diamond- formation within the Upper Mantle. This is why Carbonatite complexes are important in exploration for diamonds. Many of the diamond-bearing pipes in the world are located in close proximity to Carbonatite complexes; which are associated with deep-seated fault structures.

Kimberlite occurs as cone- pipe structures (Kimberly Mine in South Africa), sill structures (Lesotho Mines), and as dyke structures (Sierra Leone). These rocks consist of forty to ninty percent olivine rich ultramafics with heavy mineral suites consiting of pyrope garnet, ilmenite, spinel, corundum, zircon, rutile, and chromite. Lamproites occur with the same mineralogy but occur as flat-lying bodies rather than "cone" shaped bodies.

Most kimberlite pipes range in size from 5 to 30 hectares and occur in clusters ranging from 6 to 40 pipes in one area (Gurney, 1991). Most pipes are oval shaped and are associated with deep-seated fault structures. Less than 5*^ of kimberiites are diamondiferous; and less than SW* of the diamondiferous pipes are of gem quality ' (Chris Jennings . 1994).

Firesand Carbonatite Complex-

The survey has been based around the Firesand Carbonatite Complex due to

the fact that carbonatite complexes; especially calcitic bearing units, are important

structures which have been found to be located in close proximity to kimberlite

complexes. Studies of the airborne magnetics and electromagnetics indicate that the

Firesand Carbonatite Complex underlies portions of claims 1174509, 1174510, and

1110143.

The Firesand Carbonatite Complex lies within the Michipicoten Greenstone Belt

of the Wawa Subprovince and immediately north of the Kapuskasing Subprovince of

the Canadian Shield. This complex is controlled by a series of deep-seated faults

within the Kapuskasing Subprovince; namely the Wawa-Kapuskasing Fault to the

north and the Firesand Creek Fault to the east. These two faults are the most deep-

seated faults in the area, and are bissected by a series of ultramafic complexes

(peridotites and pyroxenites) in the area; and can therefore be host for other deep-

seated complexes such as kimberlites or lamproites.

The carbonatite is elongate in a northeasterly direction and is cut-off on the east

side by the Firesand Creek Fault. It has an outer rim of silicocarbonatite (calcitic) with

an inner core of dolomitic carbonatite (Parsons, 1961).

The Firesand Carbonatite is dated at 1008 to 1087 Ma for the complex (Gittins

et al, 1967).

There is a fenetic halo around the complex as indicated by the airborne

magnetics and the actual contact area of the complex. There is also a radiating pattern

of carbonatite and lamprophyre dykes around it.

Table of Lithologic Units

Cenozoic

Recent- stream till

Pleistocene- glacial till

unconformity

Late Precambrian (Proterozoic)

Firesand Carbonatite- dolomitic core rocks

gradational contact

Firesand Carbonatite- silicocarbonatite rim rocks

intrusive contact

Diabase Dykes

Early Precambrian (Archean)

Felsic Intrusives- feldspar porphyry b quartz-feldspar porphyry

intrusive contact

Intermediate Metavolcanics- tuff flows

Mafic Metavolcanics- basalt flows

Property Claim Description-

The claim group on which the survey was done is located within the northwest

part od Lastheels Township and the northeast part of McMurray Township. The claim

numbers, (together with number of units and anniversary dates) are as follows:

Lastheels Township

1110143 (4 units, March 8, 1996)

1110144 (1 unit, March 8, 1996)

1174480 (4 units, February 9, 1996)

1174509 (3 units, March 8, 1996)

1174510 (5 units, March 8, 1996)

1201471 (12 units, January 14, 1996)

1201472 (12 units, January 14, 1996)

1201473 (4 units, January 14, 1996)

McMurray Township-

1174416 (8 units, March 8, 1996)

1174419 (2 units, March 8, 1996)

These claims are contiguous as shown by the claims maps, and are unpatented

mining claims. The claims surround the southern and eastern portions of the Firesand

Carbonatite Complex, and parts of the complex underlie claims 1110143 and

1174509.

Regional Geology-

The region was last mapped in 1981 and 1982 by P.P. Sage of the Ontario

Department of Mines (Preliminary Map # 2439 and 2441). Traverses in the area were

done at approximately 1/2 mile intervals but in some cases 1/4 mile intervals.

The area is underlain by felsic metavolcanics (mainly lapilli tuffs) and mafic

metavolcanics (andesites & basalts) which are located within the southern limb of the

Michipicoten Greenstone Belt. This belt occurs within the Wawa Subprovince of the

Superior Province of the Canadian Shield. There are four metavolcanic and

metasediment rock types recognised within the Michipicoten Greenstone Belt (R.P.

Sage, 1994). The belt is comprised of several sequences of Archean felsic to mafic

metavolcanics with interbedded clastic metasediments and chemical metasediments

(iron formation). The mafic and felsic metavolcanic units are of Archean age. These

units have been intruded by numerous stocks of granitic rocks and mafic to ultramafic

rocks. Northwesterly trending diabase cut all of the other units.

The Kapuskasing Structural Zone lies between Lake Superior to the Hudson

Bay Lowlands. The two major deep-seated faults are the northeasterly trending

Firesand Creek Fault and the Wawa Lake Fault -Kapuskasing Fault trending in an

east-west direction. The Wawa Lake Fault consists of fractured crustal material that

may host kimberlitic rock formations (T.Morris, 1994). The Firesand Creek Fault is

offset and hosts several peridotite, carbonatite, and ultramafic complexes. Proterozoic

lamprophyre dykes formed from alkalic magma emplacement extending from the

Wawa Lake Fault-Kapuskasing Fault (P.P. Sage, 1994). It is along these zones that

there have been several recent diamond discoveries; such as the high-grade pipe at

Attawatiskap. The Firesand Creek Fault lies at the contact between the overlying felsic volcanics, and the underlying mafic volcanics.

Structural faults and rocks with strong or negative magnetic responses were

plotted using 1981 vintage airborne and airphotos in combination (OGS series

810006-810034; 1:20,000). In 1994 and 1995 field reconnaissance of the surrounding

area using this datauncovered several plutons of peridotite, pyroxenite, and gabbro1.

The peridotite and carbonatite structures are favoured for diamond emplacement; and

most of these units are associated with the two major fault systems as mentioned

above.

Most of the overburden coverage was deposited by Late Wisconsinian

glaciation with an ice direction at 165 degrees to 263 degrees (T.Morris, 1994).

Diamond discoveries have been located in the southwest corner of McMurray

Township and 1993 to 1994 studies by T. Morris of the MNDM-ODM have indicated

heavy mineral dispersment (diamondiferous assemblage) increasing up-ice in the

direction of Deep Lake and also in the Michipicoten River system draining from the

Firesand complex. The property lies within this area of dispersion. Also it is believed

that Monopros did a complex study of both the Coleman Creek area and the Dog Lake

area during 1993 and 1994; both areas drain from the Firesand complex and the

Wawa Lake-Kapuskasing complex respectively.

PLATE Q

Eaquagg Twsp.Lostheals " Twsp.

FELSIC NTRWS(VE ROCKS -

MAFIC METAVOLCAIfcCS - bcwtt

FELSIC METAVOLCAMCS - tuff

CLASTIC METASEDJMENTS

CHEMICAL METASEDMENTS ULTRAMAFIC NTRUSIVE

FELSIC NTRUSJVE - porphyry

CAR80NATTTE

MAFIC ttfTKUSJVE - (floba**

contact

fault / shear

^.-v vvx-vfc

GEOLOGICAL PLAN 8

STRUCTURAL GEOLOGY

^ \ ^ ~ ^ N ̂ \2 -•** \ \ \ \ \ ^^J \

i- N*V4 \ .Vv^ \

Local Geology-

In 1980 and 1981, R.P. Sage of the OGS mapped the area lithologies

surrounding the immediate vicinity of the property. In 1988 Sage studied and reported

on the Firesand Carbonatite Complex which covers the property in-part.

A general reconnaissance was done over the surrounding area; especially

around the Firesand Creek Fault and the Wawa-Kapuskasing Fault. The general trend

of the area is in a northeast-southwest direction; although in the southern sections of

McMurray Township north-south to southeasterly is the preferred direction. The area is

generally underlain by mafic metavolcanic rocks (pillowed basalts), felsic

metavolcanics (tuffs), and felsic intrusives (granite and porphyry). There are also

several areas of ultramafic intrusives consisting of gabbro, pyroxenite, and peridotite;

most of which are located along the Firesand Fault or in swarms around the

carbonatite complex.. The Firesand Carbonatite, some 2.5 kilometers X 5.0 kilometers

in diameter, is located close to the convergance of the Firesand Fault (west side) and

the Kapuskasing Fault (south side).

The central portions of the survey grid are covered by Recent and Pleistocene

glacial sand and gravel to a thickness of over thirty meters in sections. Sampling of this

material by backhoe indicated rounded cobbles (5 to 20 centimeters in diameter)

generally consisting of granitic rock, mafic volcanics, felsic volcanics, and carbonatite.

In areas where bedrock was encountered, a clay layer (light brown to light grey) was

observed for a few meters, mixed with coarse boulders, lying immediately above the

bedrock.

The ODM preliminary maps show the local geological trend to be in a

northeasterly direction when in fact the geological trend underlying the claim group is

north -south. To the north and northeast of the claim group the prominant direction is

northeasterly, and to the south and southwest of the property the prominent direction is

southeasterly. There appears to be a transition of directional trend in the central

section of the property; possibly affected by the carboantite complex which is one of

the oldest units in the area (R.P. Sage, 1988).

Geological reconnaissance of the areas surrounding the survey grid have

shown several airborne magnetic circular structures (highs and lows). Many of these

have not previously been mapped or have been incorrectly mapped. There are

several gabbro intrusive swarms located between Deep Lake to Leroy Lake (along the

south side of Reed Lake); some of which include ultramafic fragmental complexes. A

pyroxenite complex is located on the east side of the claim block, and two peridotite

bodies are located to the northeast of the claim group. Stidies of the airborne

geophysics and air-photos indicate that the peridotite complexes are controlled by

both the Firesand Creek Fault and the Kapuskasing-Wawa Lake Fault. There is

another circular structure underlying the Twin Lakes (northeast side of the Firesand

Carbonatite within Lastheels Township) which is a primary target for diamond

exploration.

Property Geology-

A detailed geological mapping of claims: 1174510, 1201471, 1201472,

1110143, 1110144, and 1174416 was undertaken. A grid consisting of some twenty-

three kilometers with lines spaced at one-hundred meters apart. The base line

consists of approximately three kilometers in length going through the central portions

of the claims ina northeast direction which is parallel to the regional geological trend

for the area.

The central part of the group is covered by thick glacial overburden material.

Processing and concentrating this overburden in the north sections of the claim group

(1174510 and 1201471) uncovered gold concentrations within the gravels. One pit

inparticular gavre rise to approximately 24 specks of gold per cubic yard in the upper

materials which is significant.

Most of the property, especially the eastern portions and southwestern portions,

have intercalated horizons of mafic and felsic metavolcanic flow units. Close to the

Firesand Fault there are coarse-grained flow units; some of which are possibly

ultramafic gabbro intrusive units. At least six diabase dyke units cut these other units in

a northwesterly direction.

In the northeasterly section of the claim group is a unit of pyroxenite (ultramafic

intrusive) complex which appears to be fault controlled. It occurs within claim 1201471.

In the southwest corner of claim 1174510 and the western portions of 1110143

are the northeast and southeast contacts respectively of the Firesand Carbonatite

Complex. These portions of the carbonatite are silicocarbonate rich. Most of the

carbonatite is overlain by glacial till however prospecting of the outer boundaries

uncovered bedrock in-place.

The primary Fault structure is the Firesand Creek Fault which cuts the main

portion of the claim group in a northeasterly direction. There are at least two other

major faults splaying off the Firesand Fault. At the eastern end of Line 4+00 South, the

Firesand Fault splays and also appers to cut at several angles. This area is of primary

interest for any deep-seated intrusions. Another area of primary interest is at a point

(between claims 1174510 and 1174509) where the Firesand Carbonatite Complex

adjoins up to the Firesand Creek Fault. This is also an area to observe for deep seated

intrusions. Preliminary maps show the Firesand Carbonatite crossing thre Firesand

Creek Fault but studies and ground geology show that it in fact adbuts up to the

contact with the fault and is probably also controlled by a fault splaying from the

Firesand Creek Fault to the south. Several ultramafic complexes in the area sucgh as

the pyroxenite immediately to the east of the carbonatite complex, and ultramafic

swarms south of the carbonatite complex indicate prime areas for diamond

exploration.

11 Mafic to Intermediate Metavolcanic Rocks-

these are prevalent on the east side and the north side of the claim group. They

are generally fine grained and massive to thinly laminated. They do occur interbedded

with layers of coarse grained flows. In some cases gold-bearing quartz veins occur

along the contacts between the coarse and fine grained fractions (east of Firesand

Creek @ L 9 to 13 South, and on the south part of claim 1174419). Pillow structures

are prevalent within the finer grained phases.

2)Felsic Metavolcanic Rocks-

these rocks are generally prevalent in the southwestern portions of the property,

and occur as interbedded layers up to fifteen meters in thickness. They occur as

massive flows and as feldspar crystal tuff l laminated tuff.

3)Mafic l U ltramafic Intrusive Rocks-

These occur as fine to coarse grained units; some of which are pyroxene rich

and some of which are olivine rich. It is generally dark grey to dark green in colour.

Two bodies of peridotite occur northeast of the property in the area of Sunrise Lake

and northeast of Sunrise Lake; occurring on the east side of Firesand Creek Fault and

to the north of the Kapuskasing Fault. The peridotite is generally serpentinite rich in the

outer sections. A pyroxenite body occurs on the east side of the property within claim

1201471 (east-central). A swarm of gabbro dykes and plutons occur in a northwesterly

trend (Reed Lake to Deep Lake) on the southwest side of the property. They are

generally fine to medium grained and hornblende rich. Some ultramafic fragmental^

occur on the southwest side of Reed Lake.

4) Felsic Intrusives-

These rocks generally occur as northeasterly trending dykes and occur as

quartz-feldspar and feldspar varieties. Large areas of this type cover areas to the

northeast of the claim area within Esquega Township. Granodiorite plutons are

prevalent west and southwest of the property; the largest units being the Jubilee Stck

and the Centennial Stock. These rocks have weak schistocity of 020 degrees to 040

degrees.

5) Mafic Intrusives-

these units cut all of the other units and exist as northwesterly trending and

northeasterly trending (discordant and concordant respectively). Lamprophyre Dykes,

black and biotite rich are prevalent radiating structures from the carbonatite complex.

Carbonatite-silicocarbonatite (calcitic) dykes, displaying fine grained grey to reddish

coloured layers, are also prevalent radiating from the carbonatite complex for a few

kilometers beyond the complex contact. Diabase dykes, both olivine rich and pyroxene

rich varieties, are found cutting all of the other units in a northwesterly direction. They

are from a few meters to sixty meters in width. They are generally coarse grained and

speckled appearance (feldspar and pyroxene lath mixture).

Economic Geoloav-

The area has long been known for gold and base metals potential. Chart 1

shows a list of producers within McMurray Township and surrounding the claim group.

Most of the gold occurrences have been associated with the Jubilee Fault and fault

zones splaying off the Jubilee Fault (R.Rupert, 1988). Other gold occurrences

surrounding the claim group are associated with: northwesterly and northeasterly

trending iron formation, felsic metavolcanic units, carbonate rich mafic metavolcanic

units, and contact areas of diabase or gabbro units.

Recent exploration has indicated gold, copper, lead and zinc values associated

with the Wawa Lake-Kapuskasing Fault area.

Nickel-copper-cobalt has been associated with the peridotite complexes in the

area.

Iron has been associated with several northeasterly trending metasediment

(chemical and clastic) which occur north of the property.

Diamonds and diamond-indicator minerls have been found in close proximity

and in the direction of ice-flow from the property. Primary sources for diamond

structures (kimberlites and lamproites) are located with deep-seated magmatic

structures. The Firesand Carbonateite and Sunrise peridotite are two such structures

which have been influenced by the Firesand Creek Fault and the Wawa Lake-

Kapuskasing Fault which are again the oldest and most deep-seated fault structures in

the area. All kimberlites are fault controlled and carbonatite complexes are found in

the vicinity of many of them.

Specifics of VLF Electromagnetic Survey-

The Crone V.L.F. electromagnetic unit utilizes higher than normal

electromagnetic frequencies and is capable of detecting small sulphide bodies and

disseminated sulphide deposits. It accurately isolates banded conductors and

operates through areas of high noise and interference levels.

This method is capable of deep penetration but due to the high frequency used,

its penetration is limited in areas of clay and conductive overburden. The components

of dip angle in degrees of the magnetic field component, field strength of the magnetic

component of the VLF field, and the out of phase component of the magnetic field are

measured at each station. The out of phase is only noted when readings reflect

abnormal character which signifies a strong conductor.

There are several different channels or stations available; each with a different

frequency. A channel used should be parallel to the general strike of the area. If this

cannot be determined or if two different strikes are found, then two orthogonal stations

are used to define the systems and conductors. In this case there are two orthogonal

strikes for the area; northeast being the dominant and northwest being the weaker.

The stations of Annapolis, Maryland and Seattle, Washington were used for the

survey.

The dip angle measurement measures the angle of inclination from horizontal

of the direction of the resultant V.L.F. or the amplitude of the major axis of the

pollarization ellipse. It is detected by a minimum on the field strength meter and is read

from an inclinometer with a range of plus or minus ninty degrees. A conductor is

designated by a "true" crossover pattern of the readings. The measurement is taken

from an audio null when the instrument is held in a vertical position; after turning

perpendicular to the direction of the alignment with the V.L.F. field. The V.L.F. field is

found by an audio null or minimum field strength measurement when the instrument is

held in a horizontal position. The accuracy of the dip angle measurement is plus or

minus one-half degree.

The field strength measurement defines the shape and attitude of the conductor

by the strength of the field in the horizontal plane or the amplitude of the major axis of

the polarization ellipse. It is the maximum reading obtained from the field strength

meter when the instrument is rotated in the horizontal plane; and is measured as a

percent of the normal field strength established at a base station. The field strength of

the V.L.F. stations drifts with time and must be corrected at a base station every few

hours. The field strength measurement has an accuracy of plus or minus two percent.

The out of phase component of the magnetic field, as a pecent of the normal

primary field, is sensitive to a low order of conductivity; lower than the dip angle

measurements. It is used to locate conductors of a low order of magnitude. The

reading is not recorded but the measurement pulse is recorded. It is a measurement of

the secondary field produced by a ground conductor which is in a different phase than

the primary field. This is the minimum reading of the field strength meter obtained

when measuring the dip angle. The measurement hads an accuracy of plus or minus

two percent.

The survey was carried out during October 13 through 15, 1995. Lines were

spaced at 100 meters apart and stations every 25 meters on the lines. A total of some

twenty three kilometers was traversed during the survey. The grid was run on claims

1174510, 1201471, 1174509, 1201477, 1110143, and 1174416. Stations used were

Annapolis , Maryland (21.0 Khz. frequency) and Seattle, Washington (24.1 Khz.

frequency).

The results are plotted at 1 inch to 100 meters. The dip angle readings are

scaled at 1" to 10 degrees for contouring, and the field strength contoured at

percentages of 1007o above the base station normal which is 100.

Results of V.L.F. Electromagnetic Survey-

There are four northeasterly trending electromagnetic signatures and two east-

west electromagnetic signatures over claims 1174509, 1201472, 1110143, and

1174416.There is also one northeasterly trend across claim 1174510.

Field Strength Measurements-

The field strength over most of the property has a weak signature possibly due

to a great depth of overburden in this area. On claim 1174510 there are two moderate

field strength signatures paralleling each other in a northeasterly direction. One

corresponds to the contact area between the carbonatite complex and a felsic

metavolcanic flow unit. The other (more northerly) corresponds with the central part of

the felsic metavolcanic flow unit. On claim 1174509, a weak field strength occurs on

Line 5 North at 300 West. This has been enhanced by a junk pile of old automobiles.

On Line 1 South to 3 South, a weak filed strength corresponds to a swampy area

underlying the Firesand Creek. Similarly, on Line 12 South at 100 East there is a

weak field strength corresponding with the swampy overburden underlying the

Firesand Creek. Over the rest of the grid is a base reading with no overall signature.

Dip Angle Measurements-

There are essentially five linears, all with a weak signature, which cut across the

survey grip in a northeast and east-west direction. There are some discontinuous

trends which correspond with the five major linears.

Anomaly A- is a weak northeasterly trend traced for four hundred meters across

the south central portion of claim 1174510. It corresponds with the contact between the

carbonatite complex to the south and the felsic metavolcanic unit to the north.

Anomaly B- is a weak anomalous trend traced in an east-west direction across

the north part of claim 1174510; over a distance of over 500 meters (Lines 1 North to

Lines 6 North). It corresponds with the silicocarbonatite section of the carbonatite

complex, and also parallels the north side of a magnetic "circular" high within the

carbonatite.

Anomaly C- is a weak northeasterly trending signature which is outlined

between Line 8 South and Line 6 North, and is traced for some 1400 meters across

claims 1174509 and 1110143. This trend corresponds with the southeastern contact of

the carbonatite complex with the mafic metavolcanic flow units (basalts).

Anomaly D- is a weak to moderate trend which trends in anortheasterly

direction from Line 18 South to Line 2 North. This trend corresponds with the swamp

overburden surrounding the Firesand Creek. This trend cuts across claims 1201472,

1110143, and 1174416.

Anomaly E- is a weak to moderate anomaly which trends northeasterly

between Line 2 South and Line 11 South. Located on claim 1201472, it corresponds

with part of the Firesand Fault system. This trend cuts rock units such as: diabase

dykes, porphyry dykes, and mafic metavolcanics.

The VLF electromagnetic survey has not delineated any significant conductor

trends, but has delineated at least one major fault-shear zone coinciding with the

Firesand Creek Fault.

Specifics of Proton Magnetometer Survey-

The survey was completed with the use of the Exploranium-Geometrics

"Unirnag" proton magnetometer. It has a digital readout with a sensitivity of plus or

minus ten gammas.

The accuracy of the readings is increased by averaging two or three readings;

or until the readings settle out to a normalized reading. The range selector is changed

up or down in areas where there is high magnetic noise, or until a station with a

normalized reading is found.

The "World Gamma Range" setting on the instrument was brought down to a

scale relative to the regional magnetics of the area when plotting the final resultant

readings. The instrument requires no calibration once the proper range setting is

found. The average range setting for this area is 58,000 gammas. When plotting, the

58,000 setting is set at zero. Every few hours the readings are checked at a base

station on the base line and changes are noted and calibrated at the end of the day.

Results are plotted at 250 gamma intervals; after plotting corrections for daily

and diurnal drift. Base plans are plotted at a scale of 1 inch to 100 meters. Station

readings are taken on lines spaced at 100 meters apart with stations every twenty-five

meters. The field work was completed during October 13 to October 15, 1995. A total of

approximately twenty-three kilometers was traversed during the survey. Intervals of fifty

meter lines was carried out over Emerald-Green Lake.

Results of Proton Magnetometer Survey-

At least four anomalous signatures were outlined by the survey; the most

significant over the northern portion of Emerald-Green Lake.

Trend A-

This anomaly is a weak signature trending in a northeasterly direction across

the central portions of the survey grid; and over claims 1174416, 1110143, 1201472,

and 1201471. This trend corresponds with the outer contact of the southeast section of

the Firesand Carbonatite Complex. This is probably outlining the iron-rich contact

areas of the complex.

Trend B-

This strong magnetic signature, trending in a north-south direction, traces the

bottom edge of a cliff between Line 14 South and Line 19 South; over a distance of

some five hundred meters. It corresponds with a carbonate rich coarse grained mafic

metavolcanic flow unit. It is located on claim 1174416.

Trend C-

This is a strong circular magnetic signature; somewhat oval shaped, located

between Lines 00 and Line 4 North. Located on the north side and under Emerald-

Green Lake, it is located within the boundary area of the silicocarbonatite section of

the Firesand Carbonatite Complex (southeast side).

There is significance to this structure as it is possible for a deep-seated

ultramafic complex to be pushed up through the fractured portion of the carbonatite

complex. If this unit is a diamondiferous kimberlite plug, it would be the minimum size

to be of economical interest; as it is some 400 meters round. This anomaly is a good

drilling target; to be drilled from northwest to southeast. Other similar circular features

should be looked for in close proximity to this one as kimberlite dykes always occur in

swarms and are associated with major fault systems.

Conclusions of Magnetics and VLF Electromagnetics-

The geophysics have been useful in delineating the contact areas of the

carbonatite complex. They have also been useful in delineating fault structures and

several possible diamondiferous and gold target areas.

The electomagnetics have not been of much use probably due to the thick

overburden cover in the central portions of the survey grid. However this survey has

been useful in delineating some of the major fault systems which cut the claim group.

The magnetics have been useful in delineating a circular anomalous trend

some 400 meters round; a trend which occurs on the southeast flank of the carbonatite

complex and also centred on the north side of Emerald-Green Lake. This trend lies in

an area susceptable for intrusion of an ultramafic complex. This circular or ovoid

structure becomes a prime target for kimberlite.

Backhoe Pits and Washing Plant-

Some thirteen pits were dug down to a maximum depth of 5.5 meters or until

bedrock was reached. Areas were chosen on the basis of: closeness to anomalous

area (airborne or ground geophysics) in conjunction with deep-seated fault systems. It

is a known fact that kimberlite pipes occur in close proximity to fault systems.

The pits were dug in an attempt to reach the basal gravels. Concentrates of

heavy minerals from basal materials is more accurate in locating local source areas,

whereas heavy minerals in the surficial materials can have travelled for great

distances.

Approximately two to two and a half cubic yards of material were washed from

each set-up. The material was loaded using a Caterpillar 330 backhoe, and

transported using a five-ton dump-truck to a local area for washing.

The washing plant consisted of a five-meter length of sluice boxes which were

designed from a pilot gold-alluvial processing plant. Thre author has designed alluvial

plants for production purposes for the past fifteen years, and has worked on many gold

and diamond alluvial projects.

The material from each pit was processed independently. Each pit consumed

approximately three hours to process.

The material was panned down to a concentrate which was sent to a lab for

heavy mineral separation and microscope work to detail the heavy mineral suite.

Backhoe Pits- Bulk Sampling Program - Firesand Carbonatite Project

Contents 40 to 50 percent cobble (rounded) content. Cobbles consist of granitic-felsic volcanics- mafic volcanics. Brown colour. Some mafic volcanic bedrock fragments. Some gold specks observed in sample concentrates. Some 2.5 cubic yards sluiced and concentrated October 18, 1995. Dug to 5.2 meters depth.

Contents averaging 607o cobbles (rounded and rock fragments) with coarse sand matrix , brown colour with low clay content. Dug down to bedrock. Some specks gold observed in concentrates. Some 2.5 cubic yards washed and concentrated in sluice on October 18, 1995. Dug to 4.5 and 5.0 meters depth.

Pit F-3

Contents 5007o cobbles to 5-10 cm. diameter with clay matrix. Clay light grey and ancient-looking; similar to diamondiferous clays. Bedrock at 4.0 to 4.5 meters depth. Up to ID-15% os sample mixed with bedrock fragments of mafic volcanics. Some gold specks observed Some 2.5 cubic yards washed (sluiced) and concentrated October 18, 1995.

Pit F-4

Contents 40 to 5007o cobbles; rounded granite- felsic volcanics- mafic volcanics. Cobbles up to 3 to 8 cm. diameter. Heavy black sand concentrate and 2 to 5 specks gold each pan of concentrate (total of approximately 60 in 2.5 cubic yards of material washed). Dug to depth of 5.5 meters; no bedrock encountered. Sluiced and concentrated October 18, 1995.

Contents up to 6007o cobbles averaging 2 to 10 cm. diameter. Rounded cobbles of generally felsic volcanics with minor mafic volcanics. Beige colour with low clay content. Bedrock fragments (10 to 1507o content) up to 0.2 meters diameter. Some granitic cobbles. Dug to depth of 5.0 meters. Some 2.5 cubic meters washed and concentrated on October 18, 1995. No specks gold observed.

Pit F-6

Contents 20 to 3007o cobbles; rounded and averaging 3 to 5 cm. diameter. Cobbles mainly granitic with some mafic metavolcanics.carbonatitic, and felsic volcanics. Beige colour with no clay. Dug to depth of 5.5 meters. No outcrop

encountered. Pit lies on north side of Emerald-Green Lake and over centre of magnetic ovoid "high". Some 2.5 cubic meters washed and concentrated on October 18, 1995. No specks gold observed.

Pit F-7

Contents 25-3007o cobbles; rounded and averaging 3 to 6 cm. in diameter. Majority granitic in nature. Appears to be of recent outwash. No bedrock encountered. Matrix of fine sand and clay. Pit on west side of Firesand Creek. Dug to depth of 5.5 meters. Hole caving in due to high water content. Material slumped with water. Some 2.5 cubic meters washed and concentrated on October 19, 1995. No specks gold observed.

Contents 25 to 3007o cobbles. Beige colour with some organics layers. No bedrock encountered. Cobbles mainly granitic and mafic volcanics. Pit on west side of Firesand Creek at junction of Firesand Fault and Lyre Fault. Dug to depth of 5.5 meters. Some 2.2 cubic yards washed and concentrated on October 19, 1995. No specks of gold encountered.

Pit F-9

Contents 20-2507o cobbles, average size 2-4 cm. diameter, rounded, coarse sand matrix, mainly granitic gravel, some silt-clay, west side creek draining south side carbonatite and into Firesand Creek complex. Located northwest side Megut Lake. Depth 5.5 meters. Some 2.5 cubic yards material (saturated), washed and concentrated October 19, 1995. No visible specks gold encountered.

PitF-10-

Contents 2507o cobbles, mafic metavolcanic & granitic cobbles(rounded), ave. cobble size 3 to 6 cm. diameter, brown coloyur, some organic layer, some red-oxide layers. West side of Firesand Creek (at edge Megut Lake), Dug to 5.5 meters depth. Some 2.5 cubic yards of saturated material washed and concentrated October 20,1995. No visible specks gold encountered.

PitF-11-

Contents 20-2507o cobbles, beige colour, red oxide layers, some organic layers, cobbles to 3-6 cm. diameter 4 rounded. West side Firesand Creek on shore of Megut Lake. Saturated with water and fine silty-sand matrix. Dug to 5.5 meters depth with no bedrock encountered. Fluvial-glacial material. Washed and concentrated October 20, 1995. No visible specks gold encountered.

Pit F-12-

Contents 1507o cobbles, beige colour, coarse sand matrix, mafic rich cobbles avering 1-3 cm. diameter. Water saturated material. Pit at west side creek draining carbonatite (south side) complex into Firesand Creek complex. Dug to 5.5 meters depth and no bedrock encountered. Wsahed and concentrated October 20 and October 21, 1995.

W.C.-1-

Contents 25-3007o cobbles (rounded and sub-angular). Cobbles of granite, mafic volcanics, porphyry, felsic volcanics. Bulk sample of 300 kilos of material from 21.0 meters below high bank on river edge; at point on inner side ox-bow. High degree of black-sand concentrate. Some specks gold visible. Garnets visible. Concentrated October 17, 1995.

S.P-1-

Contents 5007o cobbles (rounded and sub-angular). Cobbles of porphyry, granite, mafic volcanics, felsic metavolcanics, peridotite. Till sample concentrate of 140 kilos from Sunrise peridotie and North Sunrise Peridotite. Some specks gold visible. Black sand concentrate coarse grained. Concentrated spring of 1995.

PLATE B

PIT l

1201473

PH 2

PIT 3

NM0IO

PIT 4' •PITS

washing plont

1201471

PITH

BACKHOE-PITTINC LOCA

• PIT

SCALE 9^=5

O 200 4OO mfrra

Conclusions A Recommendations-

A detailed exploration program consisting of geophysical and geological

surveys with follow-up gravel bulk sampling programs was carried out over the claim

group surrounding the Firesand Carbonatite complex to investigate the potential of a

deep-seated mantle source which would lead to emplacement of kimberlite rocks.

Although no sources were outlined, several significant anomalies for both gold and

diamonds were outlined by the surveys.

Although sparse kimberlite heavy-mineral suites were detected by the surveys,

some isolated heavy minerals associated with kimberlites, picroilmenites, were

isolated from two of the thirteen backhoe pits.

One of the samples , WC-1, did not indicate any kimberlite trace-elements but is

in close proximity to a surface kimberlite recently discovered in the Lagarde Mountain

area. This indicates that kimberlite indicators might be missed if they are they are

collected up-ice or in areas with thick overburden capping.

The electromagnetics have located several fault systems which kimberlites

might be associated with.

The magnetics have located a kimberlitic-type target on the southeast contact of

the Firesand Carbonatite complex which is probably covered by an overburden cap.

Kimberlite indicator minerlas were not encountered in this area possibly due to the fact

that this anomaly is at depth and does not surface. This target is of a large enough size

to be of sgnificance. It is recommended that this target be diamond drilled.

Alluvial gold values of significance were encountered in the northern section of

the claim group in the area being drained by the Firesand Creek. Indications are that

there is a source area for the gold in this area and that further investigations are

needed to find these sources.

Several gold bearing vein systems in the west side of the property were

sampled but returned low gold values (See Chart C). However, one gold-bearing vein

system on the southwest boundary, the Booth Showing, indicates that there is a

significant gold-bearing vein system which possibly carries on to the claim group. This

area should be investigated by further prospecting and sampling.

At least six airborne targets have been defined on the present group of claims,

and another four on adjoining claims which are held by the same owner. Another three

targets are located on the claim boundary areas. Sixof these anomalies , two of which

are negative magnetic anomalies, are associated with two fault structures crossing the

property. One is the Firesand Creek Fault and the other is the fault which has been

associated with the kimberlite dykes. It is suggested that these areas in specific be

prospected and in cases of overburden cover be sampled using till-sampling

techniques. All of these zones surround the Firesand Carbonatite Complex which

increases the significance of these targets.

It is recommended that S2500 be spent on picking up adjoining claims to the

northwest of the group surveyed, and that another S2400 be spent to keep another six

claims in good standing for another year. This would bring the group to a total of

approximately 79 claim units.

It is recommended that the next phase consist of geological mapping, VLF

electromagnetics, magnetics, and bulk testing of the northwesterly group of claims; in

specific the area that is cut by the Kimberlite Dyke Fault.

December 11, 1995

Toronto, Ontario FT. Archibald, B.Se. Geologist

References

Archibald, C.W. April 1991, Qualifying Report for Firesand Resources Ltd.

Archibald, FT. January 1995, Summary Report McMurray-Chabannel Twsps.(Private)

Baird, D.S., April 1937 Planet Gold Mines Limited Report (Hillside Mine)

Canadian Mines Handbook, 1994-1995.

Johnson, E.M. 1937. Report of Claim 10294 (Wawa Gold Fields North)

Joyce, C.S. July 1967 TSL Certificate of Analysis for Algoma Ore Division

Kuryliw, C.J. July 1970 Geology Plan for Pango Gold Mines Ltd.

Kuryliw, C.J. June, 1970. Magnetometer Survey for Pango Gold Mines Ltd.

Melkman, A.C. August, 1934. Wawa Goldfields Development Plan

Morris, T.F. Nov.1994 OGS OFR 5908 Results of Overburden Sampling for Kimberlite

Heavy Mineral Indicators and Gold Grains, Michipicoten River- Wawa Area

OGS MRC 13, 1971. Gold Deposits of Ontario pg. 27-35

OGS OFR 5283, 1979 Hillside Mine pg. 116-118

OGS OFR 5283, 1979. Wawa Goldfields South pg.119-120

OGS, 1981. Wawa Area Airborne Electromagnetics 8* Magnetics (81006-81034 incl.)

Ravenbeck-Sonic Soil Sampling Inc. March 1993. Report on Investigation of Existing

Abandoned Mines Within Resident Geologist district of Wawa for MNDM, Vol. 1-3

Robinson, H.S., Sept.1928 Report on Mammoth Metals Property

Reward, C. April 1964 Diamond Drilling for McMarmac Red Lake Gold Mines Ltd.

Rupert, R.J. Sept. 1973 Hillside Mine Plan

Rupert, R.J. Sept. 1988. Citadel Gold Mines Inc.-Wawa Goldfields Mine Plan 4 Report

Sage, R.P. 1988, OGS Study 47- Firesand River Carbonatite Complex, Algoma Dist.

Sage, R.P. 1982 OGS P.2439 Geology of Chabannel Township

Sage, R.P. 1982 OGS P.2439 Geology of McMurray Township

Sage, R.P. 1982 OGS P.2442 Geology of Lastheels Township

Sage, R.P. 1982 OGS P.2440 Geology of Esquega Township

Sears, S. July 1986. Geological Mapping of Reed Lake Claim Group, Caviar Res. Ltd.

Sears, S. July 1986. Geophysical Survey of Reed Lake Claim Group, Caviar Res. Ltd.

Cost Estimate PHASE 1

17 kilometers magnetics——————— S3060 17 kilometers geology——————— S306017 kilometers electromagnetics--—— S3060 assaying—————————~-——— $1500

travel/food/board/supplies -————— S2500pitting/washing plant———————— S3300

Total Costs———————— S16.480

PHASE 2diamond drilling (ten targets)

@ S20 per foot including geologist- S60.000

Total Cost of Phase 1 and Phase 2 including 1507o contingenies-- S87.952.00

Certificate

l, Frederick Thomas Archibald, of the Town of Thornhill in the Region of York of the Province of Ontario, Canada, hereby certifies the following:

1. That l am an exploration consulting geologist and geophysicist2. That l have practised my profession in Canada for the past eighteen years,3. That l have personally been on the property and managed the programs,4. That l am a geological graduate of Carleton University, Ottawa, with a degree

of B.Se. Geology (1978).5. That the following report is a product of field work done on the property6. That Elliot Feder has advanced some 322,616.93 towards expenditures7. That l was commissioned by Elliot Feder to manage the work program and

write a report on the following group of 59 claim units8. That the field work was completed prior to November of 1995.9. That proper extensions were applied for prior to submitting these reports for

assessment purposes10. That it is believed the work was submitted prior to deadlines and that

sufficient assessment was submitted to apply at least one years extention on the 59 claim units

Dated at Concord, Ontario this 23rd. day of December, 1995.

Signed:

Breakdown of Work

Contracting - geological mapping (23 km.) S4140.00Contracting- geophysics (46 km.) S8280.00Casual Labour S9655.00Heavy Equipment Rental S3940.75Equipment Rental S 750.00Supplies S 152.06Travel Expenses S1562.60Maps b Abstracts b faxing charges S 373.22Room/Board/Subsistence S1494.27Assaying charges S1508.24 TOTAL————————————-————S31.856.14

Claim Number 1201473 (4) 1174510 (5) 1201471 (12) 1110143 (4) 1201472 (12) 1174416 (8) 1174419 (2) 1110144 (1) 1174509 (3) 1174421 (4) 1174480 (4)1174530 (2)

1174531 (2)

1174532 (2)

Assessment Performed On Claim Assessment Reserve Applied1112 1600

7032 2000

3639 4800

4030 3200

7527 4800

5756 5756

853 853

684 8001223 2447——— 1600—— 1600——- 800—-- 800—— 800

TOTAL———— 31856 31856

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OCT 31 '95 02:59PM CHAUNCEY ASSAY LABSCHAUNCEY ASSAY LABORATORIES LTD.

33 Chauncey Avenue, Toronto, Ontario, HSZ 2Z2 Tel s (4161 239-3527 FAX: C416) 239-4O12

P.I

CERTIFICATE OF ANALYSIS

RECEIVED FROM:

REPORT NO.t

DATE RECEIVED:

FRED ARCHIBALD

AR-22O

OCTOBER 24. 1995

DATE: OCTOBER 31

SAMPLES OFs CONCENTRATES

ATTENTION: FRED ARCHIBALD

SAMPLE NO

F-1F-2F-3F-4F-5F-6F-7F-8F-9F-10F-11F--12F-13WC-1

SAMPLE WEIGHT grams

153.949.6

345.1 235.284. l 100.7 237. Qisa.o175.O 301.2 147. l 101.0 498.2 55.9

MI HEAVIES 7.

15.0 7. 2.7Q 7. 3.48 7. 9.43 7. .66 7. 1.73 X

16.69 7. 4.83 7. 1.36 7. 3.43 '/. 2.39 7. 2.4Q 7. .03 7. 3.85 7.

MI HEAVIES Au micrograms

S36 205 22O 2.121 315 134 520 55763 417 144 17O6553

MI HEAVIES Cr ppm

41 174672872 1154452

1O963

1O8SO

'-' 5 19O

* Or HAD TO BE DONE FOR DIAMOND INVESTIGATION

J. van Engelen Mgr.

REPORT

ON

MICROSCOPIC EXAMINATION

OF

FOURTEEN HEAVY MINERALS CONCENTRATES OF TILL SAMPLES

Fourteen heavy minerals concentrates of screened till samples were microscopically examined to determine their mineral constituents, with emphasis on any diamond indicator minerals that might be present, and, if present, to determine the chemical compositions.of these indicator minerals utilizing the scanning electron .'microscope, and from these compositions to determine whether these indicators were derived from a potentially diamondiferous source.

The fourteen samples are numbered F-l to F-13, inclusive, and WC-1.

Sample F-l;

Approximately 8 0* of the sample is magnetite, and 15% is pink to amber coloured almandine garnet. Augite and orthopyroxene are abundant. Epidote, sphene, and diopside occur in minor amounts, particularly the diopside. Ilmenite also occurs in minor amounts, as fresh fragments that lack the alteration crust typical of picroilmenite.

Sample F-2:

Magnetite comprises approximately 55% of the sample, and pink to amber coloured almandine garnet about 4(^. The remaining 5% is comprised of several grains of black coloured augite, a few grains of diopside, and minor epidote, sphene, zircon, and orthopyroxene.

Sample F-3:

Magnetite comprises 7 0-BO* of the sample. Pink to amber coloured almandine comprises lS-20% of the sample. Several grains of ilmenite are present, however none display the crustal surface which is typical of picroilmenite. Minor epidote is present, along with several grains of diopside, zircon, and orthopyroxene. Three fragments are present of a pale blue to dark blue coloured mineral which may be topaz or apatite. Trace amounts of tarnished sulphide grains are also present.

Sample F-4;

Magnetite and ilmenite together comprise about ^ 0% of the sample. The ilmenite displays fresh surfaces rather than the crustal surfaces which would identify it as picroilmenite. Pink almandine

comprises about 2(^ of the sample, and orthopyroxene about 5%. Minor augite is present, along with minor amounts of sphene, zircon, and epidote. Trace amounts of tarnished sulphides are also present.

Sample F-5:

Magnetite comprises about 70* of the sample, and pink coloured almandine a further 25*. Minor to trace amounts of epidote, diopside, zircon, and orthopyroxene are present. One cleavage fragment of ilmenite was identified. A portion of its surface is vaguely crusty, suggesting that it may be picroilmenite.

Sample F-6:

The predominant mineral is magnetite, which comprises about 75% of r the sample. Pink coloured almandine comprises a further 20*. : Minor to trace amounts of augite, sphene, zircon, orthopyroxene, and epitote are also present.

Sample F-7:

Approximately 70* of the sample consists of magnetite and ilmenite, with the magnetite more prevalent. Pink almandine comprises about 25% of the sample. The balance consists of minor amounts of orthopyroxene, epidote, zircon, and sphene, and traces of diopside. One grain of ilmenite displays a crustal surface which vaguely resembles that of picroilmenite.

Sample F-8:

The predominant mineral is magnetite, which comprises about 75% of the sample. Pink almandine comprises a further 20*. Minor to trace amounts of orthopyroxene, augite, sphene, zircon, epidote, and diopside are also present.

Sample F-9:

Magnetite is the predominant mineral, comprising 70-75% of the sample. Pink coloured almandine comprises a further 20*. Minor to trace amounts of orthopyroxene, epidote, zircon, sphene and diopside are also present.

Sample F-10:

Magnetite comprises 70-80* of the sample, and pink almandine about 20%. Minor to trace amounts of orthopyroxene, augite, sphene, zircon, epidote, and diopside are also present.

Sample F-ll:

Magnetite comprises 70-8O* of the sample, and pink almandine about 20%. Minor to trace amounts of orthopyroxene, augite, sphene, zircon, epidote, and diopside are also present.

3.

Sample F-12;

Magnetite is the predominant mineral, comprising about 75% of the sample. Pink almandine comprises about 2 0% of the sample. Minor to trace amounts of orthopyroxene, augite, sphene, epidote, zircon, and diopside are also present.

Sample F-13:

This sample did not produce a suitable heavy minerals concentrate. It does, however, contain several grains of fresh pyrrhotite and pyrite.

Sample WC-1:

.-Magnetite is the predominant mineral, comprising about 1 0* of the sample. Pink almandine conprises a further 25%. The balance of the sample consists of minor to trace amounts of orthopyroxene, augite, sphene, zircon, epidote, and diopside.

The microscopic examination of the fourteen heavy minerals concentrates failed to identify any pyrope garnet or chrome diopside, two of the commonest diamond indicator minerals. Picroilmenite, another common indicator mineral, was identified, but only in small amounts, one grain in each of two samples - F-5 and F-7. Sphene, a common rock-forming mineral, can also be a diamond indicator mineral under certain circumstances. However, it is far less reliable than pyrope garnet, chrome diopside, or picroilmenite. Sphene is present in samples F-l, F-2, F-4, F-6, F-7, F-8, F-9, F-10, F-ll, F-12, and WC-1.

Sulphides are present in trace amounts in Samples F-3 and F-4, and as several grains of fresh pyrite and pyrrhotite in Sample F-13.

The distinct lack of any pyrope garnets and chrome diopsides, combined with the presence of only two grains of picroilmenite strongly precludes any possibility that the site of this suite of samples might represent a glacial dispersion train. Any further diamond evaluation work on these samples in not considered warranted, and therefore no microprobe analyses were undertaken.

The abnormally high Cr values have no direct correlation with the garnet (almandine) content, the diopside content, or the

magnetite content. It is unlikely that the Cr is derived from a mantle source. The high Cr values are likely due to oxides derived from mafic and/or ultramafic rocks from a crustal source.

November 10, 1995 Toronto, Ontario E. A. Gallo, B.Se., F.G.A.C.

DAILY

Daily Field Log of Work Schedule- Feder Group (Mcmurray-Lastheels Twsps)

May 5- P.C.Deslisle and F.T.Archibald study area and traverse1201473,1174510,1174480,1174812. Study air photo and magnetics. East- west traverses every 400 feet.

May 6- P.C.Delisle and F.T.Archibald study area and traverse 1201471 and overpyroxenite area-east-west traverses every 200 feet.

May 7- P.C.Delisle & F.T.Archibald study area and traverse 1201472 and 1110143 May 8- P.C.Delisle A F.T.Archibald study area and traverse 1174416 A 1174419 area August 27- F.T.Archibald layout linecutting grid over claim group: 1174416, 1110143,

1110144, 1201472, 1201471August 28- F.T Archibald prospects group 1174419, lays grid over 1174510-1201473 Sept.1- F.T.Archibald prospects 1174480,1174812,1110143. 1110144 October 12- F.T.Archibald prospects 1201472 (northwest traverses) October 13- F.T.Archibald A Bouchard prospects 1110143 (northwest traverses) October 14- F.T. Archibald A Bouchard prospects 1174416(northwest traverses October 15- F.T.Archibald A Bouchard prospects 1174419 (northwest traverses) October 16- F.T.Archibald A Bouchard prospects 1174480,1174510, 1201473 October 17- F.T.Archibald A Bouchard set up washing plant on 1201471 October 18- F.T.Archibald 4 Bouchard start backhoe digging 1174510 October 19- F.T.Archibald 4 Bouchard backhoe digging 1201471 A 1201472 October 20- F.T.Archibald A Bouchard backhoe digging and washing plant operation

claim 1174416 .1110143, 1174509 October 21- F.T.Archibald backhoe digging 1174416 and washing plant

operationOctober 22-^/1".Archibald prospect 1174419 October 25-P.C.Delisle and B.Bouchard prospect and map 1174419, sample trenches

vfi O

l- Oex.

EXPENDITURE

INVOICE # 95-25

F.T.Archibald Consulting Ltd. 668 Millway Ave. Unit 15 Concord, Ontario L4K 3V2

IN ACCOUNT WITH

Elliot Feder22 Snowberry Ct.King City , Ontario Re:McMurray-Lastheels Twsp. Claim ProjectJan. maps 98.67

maps 9.63 .:maps 10.12maps 1.15

May map purchase 24.71mileage 1200 X.35 420.00motel 395.77food/groceries 246.99supplies 29.46contract labour 750.00 (P.C.Delisle, geologist)X 3.75 days

F.T.Archibald contract 750.00 (3.75 days in field)washing plant rent 750.00 (Lilex Industries)- including pumps A hose

Aug. 27 hotel/food 127.0527 meals 54.3728 maps MNDM 5.65 28 gas 23.02* 28 meals 19.53 28 motel 60.48 28 gas 33.00*

Sept. 1 air flight 70.00 1 gas 32.00* 1 meals 25.75 1 meals 18.13 1 gas 31.03*

Sept. 1 mileage 1400 X .35 370.95 (less fuel)F.T.Archibald 600.00 (3 days in field-) coordination linecutting 5000.00 (B.Bouchard- 20 km. X S250)

Oct.12-21 mileage Timmins-Wawa-Toronto @ S0.35 per km.-1993 km697.55

FT. Archibald Oct. 12 to Oct.21 @ S200 per day (field)2000.00

October 12 motel 145.60 groceries 109.47 gas 22.03*

Nov.

1314

1516

1718

19

20

21

22

23

248

10

mealmealmealgasmealsuppliesgassuppliesmealmealmealmealmealmealDump truckgroceriesgasmealhelperbackhoelabourmotelmealgasgasgasgasP.C.DelisleB.BouchardMNDMMNDMmap printsMNDMMNDMGallo report

5.13 32.79 12.57 50.00* 12.82

1.37 34.01 80.22 13.88 12.57 12.57

3.98 5.85 9.49

775.00 14.40

7.00 13.61

190.00 1845.75 1320.00 67.63 3.84

25.00* 56.32* 30.80* 45.50*

200.00 165.00

15.58** 13.50** 40.15** 59.56** 94.50** 882.75**

Chauncey Lab 572.99** Chauncey Lab 52.50**

Geological Survey 23 km. 4140.00 Electromagnetic 23 km. 4140.00 Geological Surv. 23 km. 4140.00 Photocopy 33.12

TOTAL CHARGES———— S31.856.14

(15.5hr. @ S50perhr)

(Pierre Gravel)(15.0 hr. + floating charge)Barron Bouchard 8 X 165/day

* charges do not include GST on services

Jl/^LKER Drof ting 8c ftepro Producls

G.S.T. REGISTRATION NO.

R127537207

35 McCleary Court, Unit 24, Concord. Ontario L4K 3Y9 Tel.: (905) 660-9680 1-800-268-4866 Fax: (905) 660-9688

SOLD TO:

SALES ORDER NO

18631

TERMS

NET 15 DAYS

G ST. NO. CUSTOMER ORDER NO. TIME REQUIRED ^EOF

NO.OF ORIGINALS ENCLOSED

DESCRIPTION OF ORIGINALS

NO.PRINTS

OFF EACHTYPE OF PRINT REQUIRED

TOTALNO

COPIESUNIT

SO. FT.TOTAL SQ.FT.

PRICEPER

O. FOOTAMOUNT

X? 61r

SPECIAL INSTRUCTIONS

C On AccountC CashCH ChequeD C-arge Carci - V^sa M IC AMX

RECEIVED BY

OntarioMinistry of Ministere duNorthern Development Developpement du Nordand Mines et des Mines

INVOICE

DATE:

"PLEASE QUOTE INVOICE NUMBER WHEN MAKING PAYKENT"

G-S.T. No. R124668666

Mining Recorder's Office Ministry of Northern

Development and Mines 60 church Street Sault Ste. Marie, Ontario P6A 3H3 (705) 945-6925

—PRINTS

—ABSTRACTS

2. —— —FAX FEES

—PHOTOCOPIES

—REPORTS

--—GEOLOGICAL MAPS

-PRELIMINARY MAPS

\ 1L

TYPE

@ $1.00 each

Q 5 1.02 each

@ $2.04 each page

@ Si. 02 each

@ 5 each

@ S each

@ S4-40 each

6 $2.20 each

-AEROMAGNETIC MAPS

— CERTIFIED COPIES

Payment Duo Upon Receipt

Cheques Payable to U '*- of France

cOO'd

@ 5 each

6 5 each

@ 5 each

6 $4.00 each

@ 52.04 each

SUB-TOTAL: G.S.T- P.S.T.

TOTAL:

3IMVK S S 03N OXIXIK OPtl (NOKIS6 -SZ-MOO

AMOUNT

TD

Ontario

Ministry of Ministere duNorthern Development Developpement du Nordand Mines et des Mines

"PLEASE QUOTE INVOICE NUMBER WHEN MAKING PAYMENT"

INVOICE f

TO.-: ROM:

UHVL3VZ

G.S.T. No. R124668666

Mining Recorder's office Ministry of Northern

Development and Mines 60 church Street Sault Ste. Marie, Ontario P6A 3H3 (705) 945-6925

—PRINTS l

1M-——("ABSTRACTS

)4 ——|—FAX FEES

-PHOTOCOPIES

-REPORTS

——j—GEOLOGICAL MAPS

———PRELIMINARY MAPS

$1.00 each

$1.02 each

$2.04 each page

-AEROMAGNETIC MAPS

-CERTIFIED COPIES

Payment DuoUpon Receipt

Cneques Payable toM.T.'S*.^ cf F : nance

i y \j

TOO'd

i 51.02 each

e 5 each

@ 5 each

i 54.40 each

@ 52.20 each

@ 5 each

Q 5 each

e 5 each

@ S each

i $4.00 each

i 52.04 each

SUB-TOTAL: G.S.T. P.S.T.

TOTAL:

3IHVK S S 03N OMXIlv iO'cl (XOK)Sfi .?c- MOO

NOV 2 1 '95 09:3v3AM CHfiUNCEY ftSSftY LfiES P. 6

GALLO EXPLORATION SERVICES INC.

148 Allanhurst Drive Islington, Ontario M9A 4K7

Ph: 416-245-3511

r. account with Chauncey Assay Laboratories for the following rofessional services:

inocular microscopy of 14 heavy minerals concentrates of till anples (F-l to F-13, inclusive, and WC-1):

cv. 7-9 - Microscopy and identification of mineral grains

31 hours @ 525./hour ........... $ 775.00

:ov. 10 - Report Writing1/4 day @ 5200./day ........... __50.00

Sub total $ 825.00

GST 57.75

TOTAL DUE $ 882.75

November 10, 1995 E. A. Gallo, B.Se., F.G.A.C,

JH^LKER DrofHng 8cffepro Products

G ST. R

EGISTR

ATION

NO.

R127537207

35 McCleary Court, U

nit 24, C

oncord, Ontario L4K 3Y9

Tel.: (905) 660-9680 1-800-26M

866 Fax: (905) 660-9688

SOLD TO:

/T"-r-

SALES ORDER NO

15486

- LT

D.

TERMS

NE

T 15 D

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Cb NO.

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SPECIAL IN

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RIES LTD.33 C

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M8Z 222

TELEPHO

NE: (416)239-3527 - FAX.: (416) 239-4012

DUE UPON RECEIPT

GST l R123717001

Mr.

Fred A

rchibald 668 M

illway A

venue U

nit 15 i

16 C

oncord, O

ntario L4K

3V2

A 5053

Novem

ber B,

1995

PAGE DUF DAT f

Due U

pon Receipt

DESCRIPTION

14 Assays Au 14 Assays Gr 14 Heavy Mineral Separarions

(Screening And Examination Included)

Get. No:

AR-220 SAnple No:

F-1 to F-13, WC-1

ORDERED

SHIPPEDUNIT PRICE

EXTENDED PRICE

S 8.75

S 4.50

$ 25.00

$ 122.50

S 63.00

S 350.00

SUB TOTAL

GST

PST

TOTAL

535.5037.49

572.99

S 572.99

MOVING Sk HAULAGEREFUSE, BRUSH, SNOW REMOVAL

ROOF CLEANING

BOX 67, HAWK '^T. ONT. POS 1 GO

VALOIS SNOWPLOWING* Commercial (fe Residential *

BiU ValoisHawk Junction, Ontario

Phone 889-2011

Date.

X

Address-

Location rSt/L-^CwA

Invoice

157

Work Description

Elliot Feder

Kingnclty^ Ont. RT. ARCHIBALD CONSULTING LTD.668 MillwayAve. Units 15-16 Concord. Ont. L4K3V2

Tel: (905) 660-0501 Fax: (905) 660-7143

November l, 1994

Expenses incurred re: Claims 1110167 1174474 1174475 1174473 1174416-X1174471 1174471 1174472 1174470 1174421^t

^•-—1174512 1174477 1174481 1174530 1174420-V^—1174419 1174413 1174531 1174532

Map studies and preparations; field studies, etc.

map purchases 24.71mileage charge (1200 km.) 420.00motel 395.77food/groceries 246.99supplies 29.46contract labour (P.C.Deslisle) 750.00 (3.75 days)washing plant manufacture 750.00

TOTAL OWING as per contract $2615.93

sincerely,

F.T.Archibald, B . Se -Geologist

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