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31M05NW2004 2.19192 FIRSTBROOK 010

REPORT ON THE 1997

DIAMOND DRILLING PROGRAM

ON THE

FIRSTBROOK PROPERTY, FIRSTBROOK AND BARR TOWNSHIPS

DISTRICT OF TIMISKAMING

ONTARIO

FOR

SILVER CENTURY EXPLORATION LTD. SUITE 2302, 401 BAY ST.

P.O. BOX 102TORONTO, ONTARIO

M5H 2Y2

NTS31M/5 PETER C. HUBACHECK, LORNE D. BURDEN,

P.Geol. APEGGA F.G.A.C.

MAY 1998

W.A. HUBACHECK CONSULTANTS LIMITEDSUITE 807, 365 BAY STREET

TORONTO, ONTARIOM5H 2V1

Summary

The 3,600 hectare Firstbrook Property is wholly owned by Silver Century Exploration Ltd. The property is located approximately 15 kilometres due west of Haileybury in the western portion of Firstbrook Township and the eastern portion of Barr Township in the Province of Ontario. The property is underlain by proterozoic metasedimentary rocks of the Huronian Supergroup.

In early 1994, Sudbury Contact Mines Ltd., a sister company to Silver Century Exploration Ltd., completed a large DIGHEM v airborne geophysical survey over a number of areas in the north Lake Timiskaming region. The object of the airborne survey was to identify potential kimberlite targets for diamond exploration. In addition to identifying kimberlite targets, the survey also outlined a large champagne glass shaped, deeply rooted magnetic high feature in the western portion of Firstbrook Township. The feature was acquired by Silver Century Explorations Ltd. for a more detailed study. A number of mineral deposit models were considered to possibly occur within this target area; including, Cu-Ni-PGE deposits associated with mafic intrusive complexes, polymetallic massive sulphide deposits associated with the Archean basement, and Olympic Dam type Cu-U hematitic breccias.

Since acquiring the property, Silver Century has completed gravity, magnetic, controlled source audiofrequency magnetotelluric, and seismic surveys over portions of the property. Furthermore, four deep vertical bore holes have been drilled.

This report reviews the project to date, and makes recommendations that no further work be conducted on this property at this time.

W A. HUBACHECK CONSULTANTS LIMITED

31M05NW2004 2.19192 FIRSTBROOK 010C

TABLE OF CONTENTS

Summary

Table of Contents

List of Figures

List of Tables

List of Sections

Introduction

Location and Access

Property Status

Topography and Vegetation

Geology

Exploration History and Previous Work

Current Exploration

Diamond Drill Hole FBW-01

Discussion and Recommendations

References

Statement of Qualifications

Appendix A : Diamond Drill Logs

2

3

4

4

4

5

5

5

6

8

8

9

11

12

14

15

17


LIST OF TABLES

TABLE 1 Firstbrook Project Claim Status 6

LIST OF FIGURES

FIGURE 1 Property Location Map with DDH Site 7

LIST OF SECTIONS

SECTION 1 Section FB-96-01, FB-96-01A, and FBW-01 Pocket


Introduction

This report reviews the results of a multi-phase geophysical exploration program and three subsequent diamond drill three holes totalling 2,377.09 metres conducted under the supervision of W.A. Hubacheck Consultants Limited on behalf of Silver Century Explorations Ltd. on the Firstbrook Property located in Firstbrook and Barr Townships, north-eastern Ontario. Furthermore a more detailed summary of a fourth deep wedged 455 metre drill hole is presented.

Location and Access

The property is located approximately 15 kilometres due west of the Town of Haileybury in the west central portion of Firstbrook Township and the east central portion of Barr Township, in the Province of Ontario (Figure 1). The irregularly shaped westerly trending property is approximately nine kilometres long, and four kilometres wide. The property may be accessed by travelling westerly from its intersection with Highway 11 on Highway 558, locally known as the Mowat Landing road for approximately ten kilometres. Highway 558 cuts through the northern third of the property (Figure 2).

Haileybury is situated on the north western shore of Lake Timiskaming, and is one of the three communities which make up the Tri-town area. The three towns making up the Tri-town area are New Liskeard, Haileybury, and Cobalt. These three communities form a district commercial centre for the agricultural region known as the Little Abitibi Clay Belt.

Highway 11, the northern route of the Trans-Canada Highway, passes just to the west of the Tri-town area. The Ontario Northland Railway maintains a rail line which passes through the Tri-Towns. Daily turbo-prop air service to Toronto is available from North Bay located approximately 150 kilometres south of the Tri-towns.

Property Status

The wholly owned property consists of a contiguous group of 8 unpatented mining claims, containing 108 units, and comprising approximately 1,870 hectares. Details are as follows:


TABLE 1 Firstbrook Project Claim Status

CLAIM NUMBER

1198682

1198683

1198684

1202666

1202667

1202668

1202669

1202671

1202674

1211458

1211459

1211460

1211461

1211462

1211463

1211464

1211465

1211466

1211467

1211468

1211469

1211470

DATE RECORDED

17/10/94

17/10/94

17/10/94

09/01/95

09/01/95

09/01/95

09/01/95

09/01/95

09/01/95

31/10/95

31/10/95

31/10/95

31/10/95

31/10/95

31/10/95

31/10/95

31/10/95

31/10/95

31/10/95

31/10/95

31/10/95

10/11/95

NUMBER OF UNITS

4

16

4

16

16

16

8

16

4

1

12

16

16

12

16

16

4

6

16

1

8

16

TOWNSHIP

Firstbrook

Firstbrook

Firstbrook

Firstbrook

Firstbrook

Firstbrook

Firstbrook

Firstbrook

Firstbrook

Barr

Barr

Barr

Barr

Barr

Firstbrook

Firstbrook

Firstbrook

Firstbrook

Firstbrook

Firstbrook

Firstbrook

Firstbrook

NOTE: BOLD CLAIM NUMBERS IN GOOD STANDING IN JANUARY, 1998

Topography and Vegetation

The topography of the area can be characterised as being relatively low and flat lying with a very gentle relief. Generally, for the most part, low lying, swampy wetland areas are separated by gentle north-south trending ridges.

The western and southern portions of the project area have been subjected to forest fire and logging. Recently these areas have been replanted. The northern and eastern portions of the project area are dominated by poplar and birch forests.


HUDSON

Kilometres

Firstbrook Claims

PN351

FIRSTBROOKPROPERTY LOCATION

MAP WITH DDH SITE

l l l l l

HWy 558

Drill Access Post #1

-r -iTrail

Property Location Plan with DDH Site

Figure 1

Claim No. 1202668

Scale of inset 1:5 000

Drill Site FB-96-01(FBW-01)

Geology

The project area lies entirely within the Cobalt Embayment of the Southern Structural Province of the Canadian Shield (Card et al, 1972). Middle Precambrian Huronian metasedimentary rocks of the Cobalt Group unconformably overlie Early Precambrian metavolcanic and metasedimentary rocks (Johns, 1985).

A large Nipissing Diabase sill intrudes both the Middle and Early Precambrian rocks of the area. Johns (1985), believes this sill to be one long continuous body with an approximate thickness of 300m.

The Lorrain Formation, and the Firstbrook Member of the Gowganda Formation of the Cobalt Group metasediments are exposed in the project area. The overlying Lorrain Formation consists of arkose, quartz arenite, and wackes. The Firstbrook Member consists of grey, black and red laminated siltstones, mudstones and wackes. These Huronian Supergroup rocks are generally flat lying to very gently dipping. Folding is perceived to be supratenuous and a reflection of the underlying Early Precambrian topography (Johns, 1985).

A 1.6 kilometre wide, grabben like feature identified in Johns (1985) mapping trends north-easterly from the Montreal River Fault across the central portion of the Firstbrook property.

Exploration History and Previous Work

The Geological Survey of Canada completed an airborne magnetic geophysical survey over the area between June 1959 and October 1960. This survey delineated a large scale triangular-shaped anomaly between Red Pine Point on the Montreal River and the western shore of Moose Lake. A gravity map of the area shows no gravity anomaly anomaly coincident with this magnetic anomaly (Gupta and Wadge 1980). The depth to the anomaly as calculated by Gupta is 1392 metres. In 1979, Firstbrook and parts of the adjoining townships were mapped by Glen Johns of the Ontario Geological Survey at a scale of 1:15,840 or one inch to 1/4 mile (Johns, 1985). There is no other reported work by government agencies.

Mineral exploration of the area commenced immediately following the discovery of rich silver deposits approximately 15 kilometres to the south east at Cobalt, Ontario in 1903. Although Johns (1985) reports seeing many undocumented pits and trenches throughout Firstbrook and surrounding areas, most of the reported work within the area occurs along the southern and eastern boundary of Firstbrook Township, and along the extreme western boundary of Barr Township where the Nipissing Diabase Sill comes in contact with Huronian metasedimentary rocks. For the most part, the lands along the southern and eastern boundary of Firstbrook Township consist of patented or leased mining claims; the lands along the extreme western boundary of Barr Township are currently staked.

In the extreme north east corner of Firstbrook Township, in Lot 13, Con. VI a pit is located in a diabase dyke which contains cobalt values. Immediately to the south east in Lot 1, Con. V in Buck Township, McKinnon Mines Limited sunk a 152 foot shaft in


1907, more recently, Colebucke Mines Limited completed a geological and magnetic survey in 1948 and 1949. In 1963, Norite Exploration Limited completed a magnetic and geological survey, and some diamond drilling.

Further to the south along the township boundary, in Lot 1, Con. 2 Buck Township occurs the Dotsee Mine. The assessment file literature reports that the shaft has a depth of 210 feet with lateral workings on four levels. Only limited production of cobalt ore is reported. Agnico-Eagle Mines Limited reports drilling some surface holes in 1966 and 1979.

In Lots 4 and 5, Con. 1 in Firstbrook Township, Harmon Oil and Minerals Limited reports drilling eight bore holes in 1952. In one hole disseminated cobaltite was reported over a very narrow interval. More recently, Sapphire Petroleums Limited completed a geological survey over the this area in 1957.

In 1971, Copperfields Mining Corporation and Pickle Crow Mines Limited completed geological and geophysical surveys over Lots 7 and 8 in Con. 1 of Firstbrook Township. A felsic metavolcanic package of rocks in contact with both the Nipissing Diabase and Huronian metasedimentary rocks are reported to occur at this location.

On the west boundary of Barr Township, along the west shoreline of the Lady Evelyn River occur a number of old silver exploration workings including adits driven into the Nipissing Diabase. These historical silver workings are currently staked.

On the actual Firstbrook Property, only one recorded report of work exists which consists of a geological mapping program conducted in 1990 by Gino Chitaroni of Cobalt, Ontario.

Current Exploration

In late January and early February 1994, a DIGHEM v multi-coil, multi-frequency electromagnetic, a high sensitivity cesium magnetic, and a four channel very low frequency, VLF survey was flown over the project area on behalf of Sudbury Contact Mines Ltd., a sister company to Silver Century Exploration Ltd.. A large champagne glass shaped, very strong, deeply rooted magnetic anomaly was outlined in Firstbrook and Barr Townships. This feature was subsequently acquired between January and November of 1995 by Silver Century Mines Ltd..

In late July and early August of 1995, JVX Ltd., cut a 21.6 kilometre grid over a portion of the property, and completed total field magnetic and gravity surveys. Modelling of the gravity data suggests that the strong magnetic feature outlined in the airborne survey is contained within a basin like feature within which the Archean basement is estimated to be as deep as 3,000 metres. The basin trend is roughly conformable to the grabben structure outlined on Johns (1985) map. Modelling of the magnetic data suggests that the Nipissing Diabase Sill is the likely magnetic source and it is estimated to be at a depth of between 600 to 1200 metres. Furthermore, it was suggested that both the magnetic source, and the depth to the Archean basement were shallowest under line 5600W, and deepest under line 1600W.

In late August through early September 1995, Quantec Consulting Inc., conducted a Controlled Source Audio-frequency Magnetotelluric (CSAMT) resistivity survey over approximately 10.8 kilometres of grid line on the Firstbrook property. Quantec did not


10

complete any interpretation on the data provided. However, on the pseudo-sections provided it is obvious that strong vertical features occur between O and 400S on Line 0+00, between 800S and 1000S on Line 1600W, and between O to 800S, and 1600S to 1800S on Line 5600W. Furthermore, these features are conformable to the structural features identified in the interpretative gravity and magnetic survey report by JVX Ltd..

On December 6, 1995, 240 metres north west of station 2200S on Line 5600W (1950S, 5800W), on Mining Claim 1202664, located in Barr Township, Silver Century Explorations commenced drilling hole FB-95-01. This hole was positioned to test for the source of the strong magnetic feature outlined in the DIGHEM v airborne survey. The hole collared in Cobalt Group metasedimentary rocks at a depth of 3 metres, and remained in these to a depth of 1024.89 metres. The hole was lost at 1024.89 metres when the drill rods sheared off. Approximately 1,000 of drill rods, and the core barrel were lost down the hole.

In the fall of 1996, Silver Century Explorations commissioned Control Geophysics of London, Ontario to complete a seismic reflection survey along both the base line (HWY 558) and line 5600W. Roth (1996) of Stratagex Ltd., completed an evaluation of the data and integrated it with the results of the other surveys. He concluded that strong seismic reflectors located at depth between 1400 to 1600 metres. A further refinement of this estimate was made by Hubacheck and Roth using a seismic velocity of 5600 m/s measured from core yielding a depth of 1,344 metres to the top of the first planar reflector, possibly the Nipissing Sill contact. Furthermore, Roth (1996) indicates in his reinterpretation of the magnetic data that the depth of the principle magnetic source would be between 1700 to 1900 metres, approximately 200 metres below the strong seismic reflectors attributable to the sill. In addition, he suggests that the magnetic source would have high magnetic susceptibilities consistent with a rock containing 5 to 8 07o magnetite by volume.

On November 7, 1996, at approximately 200S, 400W, Silver Century Explorations commenced drilling hole FB-96-01. This hole was positioned to test the strong seismic reflector with the exceptional acoustical contrast which Roth (1996) suggests may be caused by a sulphide layer within the Nipissing Diabase. The hole collared in Cobalt Group metasedimentary rocks at a depth of 34 metres, and remained in these rocks to a depth of 1270.80 metres. An aphanitic to fine grained chill margin phase of Nipissing Diabase was cut from 1270.8 to 1287.7, and from 1287.7 to 1319.2 a varied textured phase of Nipissing Diabase cross cut by near vertical aphanitic ultramafic dykes were intersected. Extremely blocky and broken ground was encountered between 1300 to 1303 metres and the NQ rod string became wedged, a BQ string was advanced past the blockage to 1319.2 metres. Caving problems developed and after several unsuccessful cementing attempts, a bi-pass wedge set at 1275 metres, and hole FB-96-01 A commenced. Blocky broken ground was again encountered at 1300 to 1303 metres, and the wire line broke at 1303 metres leaving the BQ reaming shell and core barrel at 1303 metres. The contractor was unable to tap the tools and a decision to blast the rods free was made. After blasting, all the BQ, NQ, and HQ strings were removed from a depth of 1150 metres to surface.

Roth (1997), completed an interpretative report on the CSAMT survey in January 1997. He indicates that the strong conductive features identified on the pseudo-sections appear to extend to great depth, and are possibly near vertical faults or shear zones. Furthermore, he indicates that the CSAMT survey failed penetrate Huronian

W A. HUBACHECK CONSULTANTS LIMITED 10

11

metasedimentary rocks and detect the depth to the Archean basement. Finally, he concluded that no large body of conductive sulphides is likely present beneath or in close proximity to any of the surveyed lines at depths within the effective exploration range of the CSAMT survey, which he estimates to be approximately 700m.

On September 28, 1997, Boart Longyear of North Bay, Ontario mobilised a large Longyear 56 type drill onto the Firstbrook Property. Drill was set up on hole FB-96-01, and the bore hole was reconditioned and reamed out to HQ width to a depth of 1150 metres. A wedge was set at 1147 metres, and a fourth hole, FBW-01 commenced drilling at an angle of at -86.50 bearing of N230 E.

Diamond Drill Hole FBW-01

Drill hole FBW-01, a wedge off of drill hole FB-96-01, collared at a depth of approximately 852 metres below sea level. This hole was positioned to drill test both the strong seismic reflector with the exceptional acoustical contrast which Roth (1996) suspects may be caused by a sulphide layer within the Nipissing Diabase, and the source of the strong magnetic feature located 200 metres below the seismic reflector. Complete drill logs, drill hole cross sections and analytical certificates are appended to this report.

Hole FBW-01 collared at a down hole depth of 1147m in Cobalt Group mudstones, siltstones, and sandstones which are possibly part of the Coleman Member of the Gowganda Formation. At a depth of 1240.50m the unit develops a weak but pervasive potassic alteration, and maintains this to 1,272.81m, the weighted average of the magnetic susceptibilities of this unit are calculated to be 2.42 x 10"3 SI. The chill margin gabbro phase of the Nipissing Diabase was intersected at 1,272.81m, the weighted average of the magnetic susceptibilities of this unit are calculated to be 0.63 x 10"3 SI. At 1276.00m, a varied textured hornblende gabbro phase of the Nipissing Diabase was intersected, the weighted average of the magnetic susceptibilities of this unit are calculated to be 1.32 x 10"3 SI, and the bore hole continued to cut through this unit to a depth of 1,320.97m. A homeblende gabbro phase of the Nipissing Diabase was intersected between 1,320.97 to 1399.91m, and the weighted average of the magnetic susceptibilities of this unit are calculated to be 5.09 x 10"3 SI. The hole continued within a hornblende gabbro phase from 1,399.91 to 1,413.45m, however this unit exhibited local weak igneous gravitational layering and the weighted average magnetic susceptibility decreased to 0.81 x 10"3 SI. A distinct gabbroic phase of the Nipissing Diabase with weakly developed gravitational igneous layering was intersected between 1,413.45 to 1,457.61m, and the weighted average of the magnetic susceptibilities of the unit are calculated to be 4.23 x 10"3 SI. A third unit of hornblende gabbro was intersected between 1457.61 to 1,485.62m which has a weighted average magnetic susceptibility of 4.16 x 10"3 SI. Finally, a gabbro to gabbronorite phase of the Nipissing Diabase was intersected between 1,485.62 to 1,511.80m, and this phase has a weighted average magnetic susceptibility of 9.11 x 10"3 SI, however the basal 14.8 metres containing 5- 807o disseminated magnetite has a higher weighted average magnetic susceptibility of 11.38 x 10"3 SI. The lower contact of the Nipissing Diabase occurring at a down hole depth of 1511.80m, and in the immediate contact area the rocks are blocky and broken up by narrow irregular to near vertical ultramafic aphanitic dykes with magnetic susceptibilities on the order of 45 to 85 x 10"3 SI. Cobalt Group metasediments possibly of the Coleman Member of the Gowganda Formation were intersected between 1,511.80 to 1,602.00m.


12

These metasediments generally have a variable magnetic susceptibility of between 0.50 to 5.0 x 10"3 SI, however, from 1525.00 to 1536.50m the metasediments had a distinctly higher magnetic susceptibility of 14.6 to 24.2 x 10"3 SI. The hole was terminated at 1602.00m in Cobalt Group metasediments.

Discussion and Recommendations

Diamond drill holes FB-95-01, FB-96-01, and FB-96-01A all failed to penetrate to a sufficient depth to adequately test the geophysical targets identified in the magnetic, gravity, and seismic surveys. However, drill hole FBW-01 did manage to test and resolve the magnetic and seismic targets, as well as provide a complete section through the Firstbrook lobe of the Nipissing Diabase sill, although drill hole FBW-01 failed to intersect any significant mineralisation or test the Archean basement.

Roth (1996) using the seismic data estimated the depth to the Nipissing Daibase Sill to be between 1400 to 1600 metres; Webster and Ruygrok (1995) suggested that the Nipissing Diabase Sill was the primary source of the magnetic anomaly and estimated with magnetic modelling that its depth would be approximately 1200 metres in the east. Drill holes FB-96-01, FB-96-01 A, and FBW-01 all confirm that the depth to the Nipissing Sill at station 200S, 400W is approximately 1270 metres which is within a 607o of the original estimate of 1344 metres using a seismic velocity of 5600 m/s.

In his review of the seismic data Roth (1996) suggests that exceptional seismic reflectors with particularly strong acoustical contrast located below the principle reflector may be caused by a sulphide layer contained within the sill. Drill hole FBW-01 penetrated the entire thickness of the Nipissing Sill and failed to intersect any massive or semi-massive layers of sulphides or oxides. Furthermore, it was observed that only subtle changes in the rock composition occur throughout the sill. It is assumed that the strong reflectors located beneath the principle reflector which represents the sill contact are echo waves or bounce back waves caused by the significant change in rock composition between the Huronian sediments and the Nipissing Diabase.

Roth (1996), also estimated that the principle magnetic source of the large magnetic anomaly would be located approximately 200 metres below the strong seismic reflectors at a depth of 1700 to 1900 metres. Furthermore, he indicates that the magnetic source would have a high magnetic susceptibility consistent with a rock containing between 5- 80Xo magnetite by volume. In drill hole FBW-01, at a depth of approximately 1500 metres, approximately 200 metres below the top of the sill and the principle reflector, a 15 metre thick interval of gabbronorrite containing S-8% disseminated magnetite, with a significantly higher magnetic susceptibility than the containing rocks was intersected. These results both confirms Webster and Ruygrok (1995) suggested source for the magnetic anomaly, and Roth's (1996) location for the magnetic anomaly. 11 should also be noted that Gupta's estimate of 1.392 metres to the top of a magnetite rich differentiate of a Nipissing-Type intrusion was remarkably accurate.(Johns, 1980,p.32).

Drill hole FBW-01 was systematically sampled and assayed through the Nipissing Diabase. Although academically interesting trends in Cr, Pd, and Pt values occur within the sill, no significant results were encountered. Therefore, in light of the source for the magnetic anomaly being resolved, and that no mineralisation of significance was found, it is recommended that no further work be conducted on this property at this time.


13

Respectively Submitted,

Peter C. Hubacheck, B.Eng., P.GEOL. W. A. Hubacheck Consultants Limited

Lome D. Burden, B.Sc., FGAC Consulting Geologist


14

References

Johns, G. W. (1985): Geology of Firstbrook and Parts of Surrounding Townships Area, District of Timiskaming; Ontario Geological Survey Report 237.

Legault, J.M. (1995): Logistical Report on Controlled Source Audiofrequency Magnetotelluric Survey over the Firstbrook Project, Firstbrook and Barr Townships, Ontario; a private report for Silver Century Explorations Limited.

Roth, J (1997): Geophysical Report, CSAMT Survey, Firstbrook and Barr Twps, East-central Ontario; a private report for Silver Century Explorations Ltd. by Stratagex Limited.

Ruygrok, G. M. and Webster, B. (1995): Interpretive Report of the Gravity and Magnetic Surveys in Firstbrook Township Based on Modelling; a private report for Silver Century Explorations Ltd. by JVX Ltd.

Smith, P. A. and Mcconnell (1994): Dighem V Survey For Sudbury Contact Mines Limited, Lake Timisksaming Area, Ontario and Quebec; a private report for Sudbury Contact Mines Limited by Dighem, A Division of CGG Canada Ltd.


15


l Peter C. Hubacheck, of the City of Mississauga, in the Province of Ontario, do hereby certify that:

1. l am a professional exploration geologist, residing at 2401 Pyramid Crescent, Mississauga, Ontario, employed by W. A. Hubacheck Consultants Ltd., 141 Adelaide St. West, Suite 1401, Toronto, Ontario.

2. l graduated from the Haileybury School Of Mines in 1974, as a Mining Technologist.

3. l hold a Bachelor of Science in Geological Engineering degree conferred by the South Dakota School of Mines and Technology in 1977.

4. l am a registered as a professional geologist with the Association of Professional Engineers, Geologists, and Geophysicists of Alberta, and the Northwest Territories.

5. l have practised as an exploration geologist since 1977, and as a consultant with W. A. Hubacheck Consultants Limited since 1983.

6. l am member of the Prospectors and Developers Association of Canada, the Quebec Prospectors Association, and the Canadian Institute of Mining and Metallurgy both national and Toronto branches.

7. On behalf of Agnico-Eagle Group of Companies, W. A. Hubacheck Consultants has from 1983 to 1998 initiated and managed several exploration programs in the Larder Lake Mining Division. In 1994 and 1997, l personally supervised and participated as chief geologist over the duration of the exploration program cited in this report.

Dated at Toronto, Ontario this 31st day of May, 1998.

Peter C. Hubacheck, B.Eng.,P.Geol.


16


l Lorne D. Burden, of the City of Peterborough, in the Province of Ontario, do hereby certify that:

1. l am a professional exploration geologist, residing at 1524 Glenforest Crescent, Peterborough, Ontario, K9K 2J2.

2. l hold a B.Se., Geology Specialist degree conferred by the University of Toronto in 1981.

3. l have practised as an exploration geologist since 1979, and as an independent consultant since 1991.

4. l am member of the Porcupine Prospectors and Developers Association, the Northern Prospectors Association, the Prospectors and Developers Association of Canada, and a Fellow of the Geological Association of Canada.

5. l have based my interpretations and recommendations in the preceding report on my professional expertise and personal knowledge of the property.

Dated at Peterborough, Ontario this 31st day of May, 1998.

Lorne D. Burden, B.Sc., F.G.A.C.


17

APPENDIX A : DIAMOND DRILL LOGS


DIAMOND DRILL LOG

COMPANY

PROPERTY

COMMENCED

COMPLETED

Silver Century

Firstbrook (51)

Sept 28/97

Nov. 13/97

OBJECTIVE

NTS

DISTRICT

32M/5

Tinuslcuning

TWP/LAT.LONG. Firstbrook Twp.

CORE SIZE

CONTRACTOR

DATE LOGGED

CLAIM

COORD.

1202668

5257055.8m N

LOGGED BY

DDK COM

586729.8M E, 245m ASL

HQ/NQ

Longyear

23- Nov 26797

Burden

.Y,

SURVEY DEPTH

1098

1114

1158

-85.0

DIP

-84

-83.5

-96.5

AZIMUTH

W.A. HUBACHECK CONSULTANTS LTDTORONTO, ONTARIO, CANAD/

HOLE NO. raW-4)l PAGE 1/18

COLLAR AZIMUTH

COLLAR DIP -86.5

ELEVATION 852m BSL

LENGTH 455 metres

INTERVAL M D Ft D

FROM

0.0

1147.0

TO

1147.0

1188.34

xREC

100

% ROD LITHOTYPE

C5I

DESCRIP"GEOLOGY: (colour, grain size, K

J V \

noNXBirc, minerals, alteration, etc)

Drill Hole FB-96-01 was reamed from 932.0 metres to 1 150m with HO rods, a

was set @ 1147.00 and drill hole FBW-01 commenced.

Cobalt Series mudstone; and siltstone*; grey aphanitic; soft; very thinly laminated

to thinly bedded; locally graded bedding evident with top direction indicated to be up

hole; bedding varies from 88* to 90* to CA; magnetic susceptibility consistently

between 0.15 to 0.35 x 100 SI; trace disseminated ultrafine euhedral pyrite; rare

granitic dropstone!; excellent RQD Si recovery.

1150.14 to 1150.22 Aplite dyke; irregular to core axis; aphanitic; buff brown in

M.S. of 1.68 x 10"' SI; CaCO, response in dykelet.

1149.7 to 1150.14 Chill Margin/Alteration Zone to aplite dyke; weak mottled

colouration and bleaching to the grey sediments; M.S. of 0.50 x 10"J SI; weak

response; contact with dyke irregular; contact with sediment along bedding plane.

1150.22 to 1150.26 Chill Margin/Alteration Zone: same as 1149.7 to 1150.14.

1152.31 to 1152.48 Chill Margin/Alteration Zone; similar to 1149.7 to 1150.14;

M.S. of 4.9 x lO-'SI.

1152.48 to 1152.61 Aplite Dyke; similar to 1150.14 to 1150.22; M.S. of 5.31 x 10 J

1152.61 to 1152.65 Chill Margin/Alteration Zone; similar to 1149.7 to 1150.14.

SAMPLE

SAMPLE NO.

FROM TO LENGTHMixIff" SI

ASSAYS

An PI*

DIAMOND DRILL LOG

COMPANY

PROPERTY

COMMENCED

COMPLETED

Silver Century

Firstbrook (51)

Sept. 28/97

Nov. 13/97

OBJECTIVE

NTS

DISTRICT

32M/5

Timiskaming

TWP/LAT.LONG. Firstbrook Twp.

CLAIM

CO-ORD.

1202668

5257055.8m N

CORE SIZE

CONTRACTOR

DATE LOGGED

LOGGED BY

HQ/NQ

Longyear

Oct 23- Nov 26/97

Lome D. Burden

DDK COM 118

SURVEY DEPTH

1098

1114

1158

-85.0

DIP

-84

-83.5

-86.5

AZIMUTH


HOLE NO. FBW-01 PAGE 1/18

COLLAR AZIMUTH

COLLAR DIP -86.5

ELEVATION 852m BSL

LENGTH 455 metres

586729.8M E. 245m ASL

INTERVALM D Ft D

FROM

0.0

1147.0

TO

1147.0

1188.34

xREC

100

X ROD LITHOTYPE

C5I

DESCRIPTIONGEOLOGY: (colour, grain size, texture, minerals, alteration, etc)

Drill Hole FB-96-01 was reamed from 932.0 metres to 1150m with HO rods, a

was set @ 1147.00 and drill hole FBW-01 commenced.

Cobalt Series mudstones and siltstones; grey aphanitic; soft; very thinly laminated

to thinly bedded; locally graded bedding evident with top direction indicated to be up

hole; bedding varies from 88 0 to 90' to CA; magnetic susceptibility consistently

between 0.15 to 0.35 x 10J SI; trace disseminated ultrafme euhedral pyrite; rare

granitic dropstone:; excellent RQD Si recovery.

1150.14 to 1150.22 Aplite dyke; irregular to core axis: aphanitic; buff brown in

M.S. of 1.68 x ID'1 SI; CaCO, response in dykelet.

1149.7 to 1150.14 Chill Margin/Alteration Zone to aplite dyke; weak mottled

colouration and bleaching to the grey sediments; M.S. of 0.50 x 10"3 SI; weak

response; contact with dyke irregular: contact with sediment along bedding plane.

1150.22 to 1150.26 Chill Margin/Alteration Zone: same as 1149.7 to 1150.14.


M.S. of 4.9 x 10 'SI.

1152.48 to 1152.61 Aplite Dyke; similar to 1150.14 to 1150.22; M.S. of 5.31 x 10'J

1152.61 to 1152.65 Chill Margin/Alteration Zone; similar to 1149.7 to 1150.14.

SAMPLE

SAMPLE NO.

FROM TO LENGTHMS. tufa

ASSAYS

AuPI*

DIAMOND DRILL LOG

COMPANY NTS CORE SIZE

PROPERTY DISTRICT CONTRACTOR

COMMENCED TWP/LAT.LONG. DATE LOGGED

COMPLETED CLAIM LOGGED BY

OBJECTIVE CO-ORD. DDH COM

SURVEY DEPTH

1218

1248

1277

1308

DIP

-84.50

-84.55

-84.25

-83.75

AZIMUTH

W.A. HUBACHECK CONSULTANTS LTD.TORONTO, ONTARIO, CANADA


COLLAR AZIMUTH

COLLAR DIP

ELEVATION

LENGTH

INTERVALM D Ft D

FROM TO

X REC

X RQD LITHOTYPE DESCRIPTION

GEOLOGY: (colour, grain size, texture, minerals, alteration, etc)

1153.30 to 1153.39 Chill Margin/Alteration Zone: similar to 1149.70 to 1150.14:

has classic mottled/spotted alteration colouration; aphanitic; ghost bedding;

M.S. of 1.46 x 10J SI.

1153.39 to 1153.53 Aplite Dyke; similar to 1150.14 to 1150.22; M.S. of 2.66 x 100

1153.53 to 1153.85 Chill Margin/Alteration Zone; similar to 1153.30 to 1 153.39.


M.S. of 0.57 x 10-' SI.

1154.34 to 1154.43 Aplite Dyke; similar to 1153.39 to 1153.53; M.S. of 3.04 xlO"3

1154.43 to 1154.49 Chill Margin/Alteration Zone; same as 1154.20 to 1154.34.

1157.92 to 1158.04 Aplite Dyke; irregular contacts; M.S. of 1.58 x l(r3 SI;

weak CaCOj response; lacks the obvious alteration halos of previous dykes however

bates are moderately elevated in M.S. to 0.78 x 10"3 SI.

1 158.83 Several small -C lcm dropstone* of granitic material with cpy rims.

1160.37 to 1160.49 Aplite Dyke; same as 1157.92 to 1158.04; M.S. of

1.98 x 10-J SI; halos of 1.79 A. 3.22 x 10"3 SI within 15cm of contacts.

1 162.25 to 1 162.43 Classic Brown sequence showing fining up the hole;

has sharp contacts outside of sequence.

SAMPLE

SAMPLE NO. FROM TO LENGTH

M S. i 10*51

ASSAYS

AnPI*

DIAMOND DRILL LOG


PROPERTY

COMMENCED

COMPLETED

OBJECTIVE

DISTRICT

TWP/LAT.LONG.

CLAIM

CO-ORD.

CONTRACTOR

DATE LOGGED

LOGGED BY

DDK COM

SURVEY DEPTH

1338

1368

1398

1428

DIP

-84.25

-84.00

-84.25

-83.75

AZIMUTH

W.A. HUBACHECK CONSULTANTS LTDTORONTO, ONTARIO, CANADA


COLLAR AZIMUTH

COLLAR DIP

ELEVATION

LENGTH

INTERVALM D Ft D

FROM

1188.34

1200.20

1229.73

TO

1200.20

1229.73

1240.50

gREG

100

100

100

xROD LITHOTYPE

C5I

C5I A 5J

C5I A 5J


Cobalt Series Mudstones A Siltstone;: similar to 1147.0 to 1188.34 however lacks

dropstone;; bedding @ 87 to 90" to CA; locally minor beds of fine sandstone; unit

is generally very thickly laminated to thinly bedded; M.S. of 0.18 to 0.35 x Ifr3 SI.

1198.0 to 1199.17 Individual siltstone bed with M.S. of 5.86 to 12.10 x 10"3 SI;

upper contact @ 88s to CA; lower contact appears scoured @ 60" to CA; soft

sed deformation ball; pillow fractures evident.

Intercalated Cobalt Series Mudstones A Siltstones A Dirty Fine Sandstones; grey

aphanitic to fine grained; mudstones tend to be varigated A very thinly to thickly

laminated; siltstones it sandstones are very thickly bedded; bedding @ 88 to 90'

to CA; thinly laminated A varigated units show dewatering flame A ball structures;

M.S. quite variable through entire unit from 0.25 to 11.4 x 100 SI: the coarser

grained beds tend to have higher M.S.; no CaCOj evident: excellent recovery A

Intercalated Coablt Series Mudstones, Siltstones A Dirty Fine Sandstones; similar to

1200.20 to 1229.73; however unit becomes blocky * wedged; fracturing along calcite

microveinlets; microveinlets have a weakly preferred orientation of 0 to 15" to CA

but generally are irregular; trace to 1 'X: disseminated pyrite along fractured planes;

SAMPLE

SAMPLE NO.

FROM TO LENGTHM.S. I Iff' SI

ASSAYS

Au H*

DIAMOND DRILL LOG





OBJECTIVE CO-ORD. DDK COM

SURVEY DEPTH

1458

1488

1518

1548

DIP

-84.00

-84.00

-84.00

-840.00

AZIMUTH



COLLAR AZIMUTH

COLLAR DIP

ELEVATION

LENGTH

INTERVALM D Ft D

FROM

1240.50

1250.00

TO

1250.00

1272.81

xREC

100

100

xROD LITHOTYPE

C5I, 5A

C5I, 5A


locally annealed fractures show displacement of 0.5 to 1.0 cm of beddine planes: drop

stones become rare in unit; bedding remains @ 87 to 90* to CA; locally the calcite

veinlets show a brecciated A vuggy matrix; M.S. from 0.25 to 0.35 x 10"3 SI; on

individual bed @ 1239.50 to 1240.50 has a M.S. of 10.9 x l(r3 SI; poor RQD.

Similar to 1229.73 to 1240.50 however M.S. increases to 0.55 to 0.65 x 10"3 SI;

weak K alteration, pervasive though some individual more sandy beds; fracturing

A. blocky nature of rx more pronounced; narrow carbonate breccia veinlet @ 1242.84

to 1243.60 A @ 1244.50 to 1245.00, these veins @ 2cm wide @ 5" to CA

locally vuggy with quartz A carbonate generally blocky A broken; poor RQD.

Intercalated Cobalt Series Mudstones, Siltstones A Sandstones; grey; aphanitic to

fine grained; mudstones tend to be varigated; very thinly laminated to thinly

laminated A show dewatering deformation ball, pillow A flame structures:

siltstones ife sandstones are thinly laminated to very thinly bedded; bedding @

87 to 90" to CA; M.S. variable from 0.31 to 18.9 x 10J SI. sandy units

tend to have a higher M.S. than mudstone beds: weak pervasive K alteration but most

obvious in sandy units; only 1252.5 to 1259.00 has poor RQD remainder of unit

SAMPLE

SAMPLE NO.

8101

8102

8103

FROM

1269.0

1270.5

1272.0

TO

1270.50

1272.00

1272.81

LENCT H

1.50

1.50

0.81

MS. f Ut' SI

1.20

2.50

4.50

ASSAYS

Au PI*

DIAMOND DRILL LOG W.A. HUBACHECK CONSULTANTS LTD.TORONTO, ONTARIO, CANADA

COMPANY NTS CORE SEE

PROPERTY

COMMENCED

COMPLETED

OBJECTIVE

DISTRICT

TWP/LAT.LONG.

CLAIM

CO-ORD.

CONTRACTOR

DATE LOGGED

LOGGED BY

DDK COM

SURVEY DEPTH

DIP AZIMUTHHOLE NO FBW-01. PAGE 5/18

COLLAR AZIMUTH

COLLAR DIP

ELEVATION

LENGTH

INTERVALM D Ft D

FROM

1272.81

1276.00

TO

1276.00

1320.97

liREC

100

100

xROD LITHOTYPE

9

9


intact: drootsones become more obvious with some larger ones up to cobble size.

1268.4 Epidotized Microveinlets(7); @ 30', 15' 4 40' to CA; green

recrystalized fiberous appearance 2-8mm in diameter.

Nipissing Diabase: (chill margin); aphanitic Si aphyric @ contact to fine grained with

depth; contact knife sharp with overlying sediments; contact @ 87" to CA;

M.S. of overlying sediments 3.45 x 10~3 SI; chill contact diabase; M.S. of 0.71

x 10~3 SI: excellent RQD A recovery; lower contact sharp but irregular; no visible

sulphides.

Nipissing Diabase; (Varied Texture); fine to coarse grained; M.S. of 0.55 to 0.65

x 10J SI; with local patches up to 20.m of 14.1 x 10~3 SI; upper contact sharp but

irregular; aphitic texture: texture varies from fine grained gabbroic to medium

grained pegmatitic; contacts between phases are gradaaonal: phases are patchy

throughout the unit; unit becomes coarser with depth to medium grained i

pegmatitic phases decrease in frequency; generally no visible sulphides.

1285.13 to 1285.30 Pegmatitic phase with silver grey mineral Z-3% possibly ilmenite.

1276.00 to 1276.25 Pegmatitic phase @ contact with chill margin contains trace cpy

SAMPLE

SAMPLE NO.

8104

8105

8106

8107

8108

8109

8110

8111

8112

8113

8114

FROM

1272.81

1274.00

1275.00

1276.00

1277.00

1278.00

1279.50

1281.00

1282.50

1284.00

1285.50

TO

1274.0

1275.0

1276.0

1277.0

1278.0

1279.5

12281.

1282.5

1284.0

1285.5

1287.0

LENGTH

1.19

1.00

1.00

1.00

1.00

1.50

1.50

1.50

1.50

1.50

1.50

M.S. i Iff1 SI

0.68

0.61

0.61

0.64

0.55

0.62

0.53

0.53

0.53

0.56

4.50

ASSAYS

Au B*

DIAMOND DRILL LOG

COMPANY NTS

PROPERTY DISTRICT

COMMENCED TWP/LAT.LONG.

COMPLETED CLAIM

OBJECTIVE CO-ORD.

W.A. HUBACHECK CONSULTANTS LTDTORONTO, ONTARIO, CANADA

CORE SIZE

CONTRACTOR

DATE LOGGED

LOGGED BY

DDH COM

SURVEY DEPTH

DIP AZIMUTH HOLE NO. FBW-01 PAGE 6/18

COLLAR AZIMUTH

COLLAR DIP

ELEVATION

LENGTH

INTERVALM D Ft D

FROM TO

l REC

XROD LITHOTYPE DESCRIPTION


b 1-2* Dvrite/DO.

1278.S1 to 1279.41 Blocky broken core, poor RQD; some blocks have talcose faces

@ 25' to CA.

1282.58 to 1282.66 Epidote veinlets @ CaCO, @ 28" to CA; 0.5 to 1.0cm in width.

1288.68 to 1289.00 Quartz Vein; coarse milky white with epidotized/sand seritize

contacts 3-5mm; contains anhedral xline masses of cpy A po < 1 %; contacts @ 25" to

1289.50 to 1290.00 Medium Grained Diabase with S-10% coarse megnetite xls (3

euhedral M.S. of 7.81 x 10J SI.

1291.00 to 1293.00 As above with M.S. up to 14.1 x 10"3 SI.

1298.85 Quartz-Carbonate Veinlet; 0.5 to lcm wide @ 25' to CA; trace pyrite fc

1299.30 Quartz-Carbonate Veinlet; as above with < 1 36 cpy 4 po.

1299.55 to 1300.12 Quartz Vein; coarse grained; milky whole; contacts @ 25*

to CA; no visible sulphides.

1300.75 to 1301.10 Fegmatoidal phase with two -C lcm wide quartz-carbonate

veinlets with 1-2* po, cpy 40* to CA.

1319.50 to 1320.75 Unit becomes wedgy/blocky.

1320.97 Lower contact gradational over 25cm, defined by M.S. from 0.70 to

13.8 x 10-3 SI.

SAMPLE

SAMPLE NO.

8115

8116

8117

8118

8119

8120

8121

8122

8123

8124

8125

8126

8127

8128

8129

8130

8131

8132

FROM

1287.0

1288.5

1289.5

1290.0

129.15

1293.0

1294.5

1296.0

1297.5

1299.0

1300.5

1302.0

1303.5

1305.0

1306.5

1308.0

1309.5

1311.0

TO

1288.50

1289.50

1290.00

1291.50

1293.00

1294.50

1295.00

1297.50

1298.00

1300.50

^302.00

1303.50

1305.00

1306.50

1308.00

1309.50

1311.00

1312.50

LENGTH

1.50

1.00

0.50

1.50

1.50

1.50

1.50

1.50

1.50

1.50

1.50

1.50

1.50

1.50

1.50

1.50

1.50

1.50

M.S. x 10*51

0.53

0.50

7.81

1.20

14.10

0.50

0.46

0.51

0.43

0.53

0.54

0.58

0.66

0.62

0.50

0.60

0.60

0.75

ASSAYS

Au PI*







SURVEY DEPTH

DIP AZIMUTHHOLE NO. FBW-01 PAGE 7/18

COLLAR AZIMUTH

COLLAR DIP

ELEVATION

LENGTH

INTERVALM D Ft D

FROM

1320.97

TO

1353.00

i,REC

100

X RQD LITHOTYPE

9


Nipissing Diabase (Gabbro-Noritc); dark greenish grey; equigranualr medium grained;

lacks pegvarioidal phases; M.S. generally 5.95 to 16.1 x 10'-' SI with local narrow

of 0.71 to 1.30 x 100 SI; unit appears to become slightly darker with depth; aphitk

texture; @ 1327m unit starts to show preferential fracturing @ 40-45* to CA;

fracture faces are of talc tt. chlorite; fractuing appears to increase in frequency with

depth; generally no visible sulphides.

1331.06 to 1335.11 Core becomes blocky A wedged; 100* recovery but very poor

RQD; wedge faces are chloritic Si talcose; favoured. Fracture direction @

25 A SO' to CA.

1335.11 to 1341.85 Core is weakly to moderately blocky 4 wedged; 10056 recovery;

moderate RQD; same as above.

SAMPLE

SAMPLE NO.

8133

8134

8135

8136

8137

8138

8139

8140

8141

8142

8143

8144

8145

8146

8147

8148

8149

FROM

1312.55

1314.00

1315.50

1317.00

1318.50

1320.00

1320.97

1322.00

1323.00

1324.50

1326.00

1327.50

1329.00

1330.50

1332.00

1333.50

1335.00

TO

1314.00

1315.50

1317.00

1318.50

1320.00

1320.47

1322.00

1323.00

1324.50

1326.00

1327.00

1329.00

1330.50

1332.00

1333.50

1335.00

1336.50

LENGTH

1.50

1.50

1.50

1.50

1.50

0.97

1.03

1.00

1.50

1.50

1.50

1.50

1.50

1.50

1.50

1.50

1.50

M.S. s Iff' SI

0.95

1.25

0.73

0.85

1.25

14.00

3.25

15.00

12.50

0.77

1.50

14.00

10.00

6.10

6.00

0.85

ASSAYS

Au PI*

DIAMOND DRILL LOG

COMPANY

PROPERTY

COMMENCED

COMPLETED

OBJECTIVE

NTS

DISTRICT

TWP/LAT.LONG.

CLAIM

CO-ORD.

CORE SIZE

CONTRACTOR

DATE LOGGED

LOGGED BY

DDK COM

W.A. HUBACHECK CONSULTANTS LTDTORONTO, ONTARIO, CANALV

SURVEY DEPTH

DIP AZIMUTH HOLE NO. FBW-01 Page 8/18 .

COLLAR AZIMUTH

COLLAR DIP

ELEVATION

LENGTH

INTERVALM D Ft D

FROM

1353.00

TO

1399.91

%REC

100

* ROD LITHOTYPE

9


1344.80 to 1345.05 Blockv A broken core.

1351.05 to 1351.10 Blocky A broken core with talc matrix; upper contact @ 50"

to CA; lower contact @ 15' to CA.

1351.10 to 1351.16 Ultra Mafic Aplite Dyke; black aphanitic; aphyritc; 17.8 x 10 3

upper contact @ 75' to CA; lower contact @ 75 0 to CA.

1351.16 to 1352.20 Blocky Broken Core with talc matrix on block faces; upper

contact @ 75' to CA; lower contact @ 25" to CA; M.S. of 0.71 x l(r3 SI.

1352.20 to 1352.95 Ultra Mafic Aplite Dyke; black aphyric; aphanitic; contacts

@ 25* to CA; M.S. of 56.2 x l(r3 SI.

1353.00 Rods Stuck - reducing from HQ to NQ.

(75 HQ core tags used).

Nipissing Diabase (Gabbro-Norite); core reduced from BQ to NQ; dark greyish

equigranular medium grained; M.S. quite variable from 0.58 to 11.4 x 10"3 SI:

areas of blocky A broken gravel have a lower magnetic susceptibility (0.58 to

1.95 x 100 SI); areas of rare competent gravel have M.S. of 4.90 to 11.4 x 10'3 SI;

aphitic texture to minerals; no carbonate: no visible sulphides; areas of high M.S.

SAMPLE

SAMPLE NO.

8150

8151

8152

8153

8154

8155

8156

8157

8158

8159

8160

8161

8162

8163

8164

8165

8166

FROM

1336.50

1338.00

1339.50

1341.00

1342.50

1344.00

1345.50

1347.00

1348.50

1350.00

1351.00

1352.50

1353.00

1354.50

1356.00

1357.50

1359.00

TO

1338.00

1339.50

1341.00

1342.50

1344.00

1345.50

1347.00

1348.50

1350.00

1351.00

1352.50

1353.00

1354.50

1356.00

1357.50

1359.00

1360.50

LENGTH

1.50

1.50

1.50

1.50

1.50

1.50

1.50

1.50

1.50

1.00

1.50

0.50

1.50

1.50

1.50

1.50

1.50

M.S. i 10* SI

7.50

1.75

6.50

7.00

10.10

0.85

0.90

11.00

14.20

1.50

0.72

56.20

0.78

1.00

0.65

11.30

8.50

ASSAYS

AuB*

j



PROPERTY

COMMENCED

COMPLETED

OBJECTIVE

DISTRICT

TWP/LAT.LONG.

CLAIM

CO-ORD.

CONTRACTOR

DATE LOGGED

LOGGED BY

DDK COM

SURVEY DEPTH

DIP AZIMUTH HOLE NO. FBW-01 PAGE 91 18

COLLAR AZIMUTH

COLLAR DIP

ELEVATION

LENGTH

INTERVALM D Ft D

FROM TO

% SEC

( ROD LITHOTYPE DESCRIPTION


visible monetite xls of O.lmm to 5.0mm: similar to above unit although the M.S.

to be nose variable.

1353.00 to 1353.68 Blocky wedged ground associated with overlying dyke; wedges

@ 20' to CA; M.S. 0.99 x 10"' SI.

1353.68 to 1358.00 Relatively competent rock with M.S. of 0.58 to 1.33 x 10'' SI;

good RQD.

1358.00 to 1360.50 Competent rock with good RQD; M.S. of 4.68 to 11.4 x 10"' SI;

magnetite xls up to 3mm.

1360.00 to 1361.25 Competent rock with M.S. of 0.80 x 100 SI; wedgy @ 25" A

45' lo CA.

1362.49 to 1362.95 Mafic Dyke; dark grey; aphanitic to fine grained; appears to be

digesting/assimilating host rx; lower contact @ 10' to CA; upper contact @ 20* to

no carbonate in dyke material; extremely blocky with gouge; gouge rich in CaCO,

M.S. of 0.34 x 10-1 SI: no visible sulphides.

1362.95 to 1365.60 Blocky, broken A wedged; M.S. of 0.35 to 0.69 x 10"' SI.

1364.17 Quartz-Carbonate Veinlet @ 45" to CA; lcm wide with trade cpy.

1364.25 Quartz-Carbonate Veinlet @ 45' to CA; lcm wide; 2-3* cpy.

1364.41 Quartz-Carbonate Veinlet @ 30" to CA; 5mm wide; 2-3* cpy.

SAMPLE

SAMPLE NO.

8167

8168

8169

8170

8171

8172

8173

8174

8175

8176

8177

8178

8179

8180

8181

8182

8183

8184

FROM

1360.50

1362.00

1362.49

1368.60

1365.00

1366.50

1368.00

1369.50

1371.00

1372.00

1374.00

1375.50

1377.00

1378.50

1380.00

1381.50

1383.00

1384.50

TO

1362.00

1362.49

1363.60

1365.00

1366.50

1368.00

1369.50

1371.00

1372.50

1374.00

1375.50

1377.00

1378.50

1380.00

1381.50

1383.00

1384.50

1386.00

LENGTH

1.50

0.49

1.11

1.40

1.50

1.50

1.50

1.50

1.50

1.50

1.50

1.50

1.50

1.55

1.50

1.50

1.50

1.50

M.S. l HP SI

0.55

0.42

0.43

0.45

7.13

0.85

7.15

0.75

0.75

4.00

7.15

8.50

7.00

1.25

0.48

8.00

7.60

4.00

ASSAYS

Au PI*

'

|

1

1 i

i

DIAMOND DRILL LOG W.A. HUBACHECK CONSULTANTS LTDTORONTO, ONTARIO, CANALV

COMPANY NTS CORE SEE

PROPERTY

COMMENCED

COMPLETED

OBJECTIVE

DISTRICT

TWP/LAT.LONG.

CLAIM

CO-ORD.

CONTRACTOR

DATE LOGGED

LOGGED BY

DDH COM

SURVEY DEPTH DIP AZIMUTH HOLE NO. FBW-01 PAGE 10/18

COLLAR AZIMUTH

COLLAR DIP

ELEVATION

LENGTH

INTERVALM D Ft D

FROM TO

X KEC

% *QD LITHOTYPE DESCRIPTION


1365.60 to 1366.68 Relatively eood ROD with M.S. of 7.15 x 10"3 SI; disseminated

magnetite.

1366.68 to 1373.49 Moderate RQD; wedgy; wedges @ 40-45" to CA A some @

15-20' to CA with chloritic/talcose races; M.S. @ 0.58 to 1.62 x 100 SI; small patch

of 30cm @ 8.00 x 10"3 SI.

1373.49 to 1378.65 Relatively Good RQD wit honly some wedgying; M.S. @ 5.82

to 9.22 x 100 SI; areas of higher M.S. have S-10% visible magnetite patches up to

in diameter.

1378.65 to 1331.86 Wedged A blocky Gravel; wedging @ 15 to 30* to CA;

chloritic/talcose laces on wedges; M^ of 0.45 to 1.68 x 1Q-3 SI.

1381.86 to 1391.48 Competent rock with good RQD; M^ of 4.90 to 8.44 x 1Q-3

rare chlorite/talc skip faces. Q 25' to CA.

1391.48 to 1399.81 Relatively good to moderate RQD; variable M.S. of 0.88 to

5.49 x 10-' SI: generfally 3.5 x 10"3 SI.

1398.55 Gravatatoinal layering of Intmsive(?) narrow albite rich zone lcm wide

@ 65" to CA.

SAMPLE

SAMPLE NO.

8185

8186

8187

8188

8189

8190

8191

8192

8193

8194

FROM

1386.00

1387.50

1389.00

1390.50

1392.00

1393.50

1395.00

1396.50

1398.00

1399.00

TO

1387.50

1389.00

1390.50

1392.00

1393.50

1395.00

1396.50

1398.00

1399.00

1399.91

LENGTH

1.50

1.50

1.50

1.50

1.50

1.50

1.50

1.50

1.00

0.91

M-S-i 10* SI

6.00

5.50

6.90

4.00

1.75

4.00

2.50

1,20

4.50

5.00

ASSAYS

AuPpb

DIAMOND DRILL LOG W.A. HUBACHECK CONSULTANTS LTDTORONTO, ONTARIO, CANADA


PROPERTY

COMMENCED

COMPLETED

OBJECTIVE

DISTRICT

TWP/LAT.LONG.

CLAIM

CO-ORD.

CONTRACTOR

DATE LOGGED

LOGGED BY

DDK COM

SURVEY DEPTH


COLLAR AZIMUTH

COLLAR DIP

ELEVATION

LENGTH

INTERVALM D Ft D

FROM

1399.91

TO

1413.45

xREC

100

X RQD LITHOTYPE

9


Nbissine Diabase ( ): dark erevish green: equigranular

grained; aphilic texture; no carbonate; no visible sulphides; unit lias a weak but

pervasive K alteration; white (Na?) Feldspars show a pinkish red alteration (K);

M.S. generally low @ 0.34 to 0.98 x 10'3 SI; sill patch of 30cm of up lo 4.33 x 10J

rare intrusive layering @ 65-75' to CA in areas of slightly blocky A broken A

wedged with a port to moderate RQD; favooured fracture directions @ 45 % 15"

to CA; lower contact gradational defined by M.S. meter.

1400.05 Gravatational layering?; 1 cm wide layer of Isigbtly richer albite feldspar @

65' to CA.

1405.20 Gravatational layering?; 3cm wide layer of slightly richer albite feldspar

@ 70-75* to CA.

1408.16 Quartz Veinlet; cryptaxline lcm wide 25' to CA; no visible silphkles.

1412.00 to 1412.35 Mafic Dyke; dark grey; aphanitic to fine granted; appears to be

digesting/assimilating host rx; upper contact unrecognizable; lower contact broken;

no carbonate; generally blocky A broken; M.S. of 0.36 x 10'' SI; no visible

SAMPLE

SAMPLE NO.

8195

8196

8197

8188

8199

8200

8201

8202

8203

8204

FROM

1399.91

1401.00

1402.50

1404.00

1405.50

1407.00

1408.50

1410.00

1411.00

1412.00

TO

1401.00

1402.50

1404.00

1405.50

1407.00

1408.50

1410.00

1411.00

1412.00

1413.45

LENGTH

1.09

1.50

1.50

1.50

1.50

1.50

1.50

1.00

1.00

1.45

M.S. i UT St

0.80

3.00

0.85

0.85

0.40

0.40

0.34

0.35

0.36

0.45

ASSAYS

Au W*

,



PROPERTY

COMMENCED

COMPLETED

oBrecnvE

DISTRICT

TWP/LAT.LONG.

CLAIM

CO-ORD.

CONTRACTOR

DATE LOGGED

LOGGED BY

DDH COM

SURVEY DEPTH

Off AZIMUTH HOLE NO. FBW-01 PAGE 12/18

COLLAR AZIMUTH

COLLAR DIP

ELEVATION

LENGTH

INTERVALM D Ft D

FROM

1413.45

TO

1457.67

xREC

100

X ROD LITHOTYPE

9

DESCRIPTIONGEOLOGY: (colour, grain size, tenure, minerals, alteration, etc)

Nipissine Diabase ( ): dark erev: eauieranular medium

aphitic texture; consists primarily of plagioclase; pyroxenese have a slight brownish

tint; M.S. very consistent 3.63 to 7.00 x 10"' SI; generally @ 4.5 x 10"' SI; excellent

RQD; possible igneous layering? Even l-2cm locally; rue trace pyrite.

21417.26 Possible Example of Igneous Layering; upper slightly coarser patch in

contact with lower finer patch of diabase @ 70* to CA.

1419.66 Possible Example of Igneous Layering; albite rich patch 1.5cm wide @

70* to CA.

1420.65 Same as 1420.65; @ 60* to CA.

1423.42 Same as 1419.66 @ 65" to CA.

1423.55 Same as 1417.26 @ 60* to CA.

1426.12 Same as 1417.26 @ 50" to CA.

1426.38 Same as 1417.26 @ 50' to CA.

1427.50 to 1428.15 Wedged Core with chloritk/talcose slip face @ 10* to CA.

1430.97 to 1431.03 Mafic Dyke; same as 1412.00 to 1412.35; @ 25* to CA.

1448.00 to 1448.52 Variable Texture; locally coarser grained; M.S. of 1.15 to 1.58

x 10"' SI; trace pyrite/po.

1448.52 to 1448.60 Pegmatoidal Phase; M.S. of 0.82 x 100 SI: upper contact

SAMPLE

SAMPLE NO.

8205

8206

8207

8208

8209

8210

8211

8212

8213

8214

8215

8216

8217

8218

8219

8220

8221

8222

FROM

1413.45

1414.50

1416.00

1417.50

1419.00

1420.50

1422.00

1423.50

1425.00

1426.50

1428.00

1429.50

1431.00

1432.50

1434.00

1435.50

1437.00

1438.50

TO

1414.50

1416.00

1417.50

1419.00

1420.50

1422.00

1423.50

1425.00

1426.50

1428.00

1429.50

1431.00

1432.50

1434.00

1435.50

1437.00

1438.50

1440.00

LENGTH

1.05

1.50

1.50

1.50

1.50

1.50

1.50

1.50

1.50

1.50

1.50

1.50

1.50

1.50

1.50

1.50

1.50

1.50

M.S.. 10' SI

4.50

5.00

4.50

5.24

4.25

3.25

5.00

3.25

2.25

3.50

4.75

2.50

3.20

4.25

3.20

4.50

6.00

3.81

ASSAYS

ABPI*

DIAMOND DRILL LOG

COMPANY NTS

PROPERTY DISTRICT


COMPLETED CLAIM

OBJECTIVE CO-ORD.

CORE SIZE

CONTRACTOR

DATE LOGGED

LOGGED BY

DDH COM


SURVEY DEPTH

DIP AZIMUTHHOLE NO. FBW-01 PAGE 13/18

COLLAR AZIMUTH

COLLAR DIP

ELEVATION

LENGTH

INTERVALM D Ft D

FROM TO

X REC

X ROD LITHOTYPE DESCRIPTION


diffuse lower contact sharp O 75* to CA: < 1 ft disseminated ultrafine sulphides

Po A cpy; unit appears to consist primairty of plagioclase 4 albite with some

(box 100).

1452.32 Possible example of Igneous layering; albite rich patch 5mm wide @

65' to CA.

1452.64 As above; lcm wide @ 65* to CA.

1453.49 As above; lcm wide @ 65* to CA.

1456.80 As above; 5mm wide @ 65* to CA.

SAMPLE

SAMPLE NO.

8223

8224

8225

8226

8227

8228

8229

8230

8231

8232

8233

8234

8235

8236

8237

FROM

1440.00

1441.50

1443.00

1444.50

1446.00

1447.50

1448.00

1448.52

1448.60

1449.00

1450.50

1452.00

1453.50

1455.00

1456.49

TO

1441.50

1443.00

1444.50

1446.00

1447.50

1448.00

1448.52

1448.60

1449.00

1450.50

1452.00

1453.50

1455.00

1456.49

1457.67

LENGTH

1.50

1.50

1.50

L 1.50

1.50

0.50

0.52

0.08

0.40

1.50

1.50

1.50

1.50

1.49

1.18

M.S. s Id4 SI

3.80

4.10

5.25

4.10

5.00

4.00

1.48

0.82

3.84

5.25

4.22

5.50

5.00

3.50

6.25

ASSAYS

Au Pt*

DIAMOND DRILL LOG W.A. HUBACHECK CONSULTANTS LTDTORONTO, ONTARIO, CANALV


PROPERTY

COMMENCED

COMPLETED

OBJECTIVE

DISTRICT

TWP/LAT.LONG.

CLAIM

CO-ORD.

CONTRACTOR

DATE LOGGED

LOGGED BY

DDH COM

SURVEY DEPTH


COLLAR AZIMUTH

COLLAR DIP

ELEVATION

LENGTH

INTERVALM D Ft D

FROM

1457.67

TO

1485.12

tB EC

100

X ROD LITHOTYPE

9


Ninissine Diabase C V generally dark erev: equigranular medium grained:

with an aphilic texture; consists of plagioclase b pyroxeme; unit has porphyritic

patches where phenocrysts are dark green chloritic/talc pseudomorph* of pyroxene;

pseudomorphs are up to 5mm in length A are subhedral; locally over 1 metre

pseudomorph* of phenocrysts can account for 5-W of rock; M.S. variable from

4.02 to 8.04 x 10-' SI but generally in the 4-5 x 10 ' SI; unit has trace pyrite/po

as anhedral intentilial grains; upper contact gradationally occurring at first major

occurance of phenocrysts; lower contact at last occurence of recognizable

phenocrysts.

1460.53 to 1464.20 Blocky broken * wedged ground; M.S. of 0.46 to 0.60 x l(r3 SI;

talc/chloritc slip faces <25 to CA.

1466.00 to 1466.82 Blokcy broken A. wedged ground; M.S. of 0.27-0.68 x Iff3 SI.

1466.82 to 1467.20 Sliver of a quartz-carbonate vein @ 55' to CA; trace pyrite;

entire vein not cut therefore width indeterminable; M.S. 0.37 x 10'3 SI.

1467.45 to 1468.46 Sliver of a mafic dyke; @ ^' to CA; entire dyke not cut

therefore width indeterminable; dyke dark green, aphanitic to fine grained appears to

digesting host rx; possibly a fine grained version of host rx: no CaCO3 ;

M.S. of 0.50 x 10'' SI.

SAMPLE

SAMPLE NO.

8238

8239

8240

8241

8242

8243

8244

8245

8246

8247

8248

8249

8250

8251

8252

8253

8254

8255

FROM

1457.67

1458.50

1459.50

1461.00

1462.50

1464.00

1465.50

1466.50

1468.45

1468.46

1470.00

1471.50

1473.00

1474.50

1476.00

1477.50

1479.00

1480.50

TO

1458.50

1459.50

1461.00

1462.50

1464.00

1465.50

1466.50

1467.45

1468.46

1470.00

1471.50

1473.00

1474.50

1476.00

1477.50

1479.00

1480.50

1481.77

LENGTH

0.89

1.00

1.50

1.50

1.50

1.50

1.00

0.95

1.01

1.54

1.50

1.50

1.50

1.50

1.50

1.50

1.50

1.27

M.S. x WfSl

7.27

5.88

3.50

0.46

0.58

2.89

2.50

0.37

0.50

6.25

5.00

5.10

5.83

4.50

7.30

6.35

8.10

7.50

ASSAYS

AuW*

DIAMOND DRILL LOG

COMPANY NTS

PROPERTY DISTRICT


COMPLETED CLAIM

OBJECTIVE CO-ORD.

CORE SEE

CONTRACTOR

DATE LOGGED

LOGGED BY

DDH COM

W.A. HUBACHECK CONSULTANTS LTDTORONTO, ONTARIO, CANALV

SURVEY DEPTH


COLLAR AZIMUTH

COLLAR DIP

ELEVATION

LENGTH

INTERVALM D Ft D

FROM

1485.62

TO

1511.80

nREC

100

xROD LITHOTYPE

9


1475.61 to 1476.75 Blocky broken 4 wedeed ground: M.S. of 1.0 x Ifr3 SI.

1477.87 to 1478.80 Weakly wedged ground; wedging @ <20° to CA; M.S. of

6.35 x 10 3 SI.

1481.77 to 1482.08 Ultra Mafic Dyke; dark greenish grey; aphanitic; contacts sharp

but irregular; trace pyrite; M.S. of 1.23 x 10J SI; rich in CaCO3 (possibly related

to upper contact type dykes).

1484.10 to 1485.62 K-Altered b bleached; M.S. 0.45 to 0.51 x 1(H SI; albite

altering to pinkish colour St plagioclase to sertaic/sanssunite?; unit blocky.

Nipissing Diabase ( )' dark grey; fine to medium grained; but

darker i finer grained than overlying units; M.S. 7.84 to 13.1 x 10'3 SI; M.S.

generally 10.1 x 10"' SI; SK dusseminated subhedral magnetite (ilmenite) xls of l-3mm

in size; trace pyrhe/po; equigranular aphhic texture; excellent recovery; generally

moderate to good RQD.

1486.44 to 1486.85 Mafic Dyke; weak to moderate CaCO3 response; aphanitic;

@ 20* lo CA: apparent width about 2cm; black; aphanitic; M.S. of 0.9 x 100 SI.

1491.00 to 1398.75 Blokcy ground; weak to moderate RQD; local narrow patches

of low M.S. 0.26 to 1.03 x 10O SI over busted up areas.

SAMPLE

SAMPLE NO.

8256

8257

8258

8259

8260

8261

8262

8263

8264

8265

8266

8267

8268

FROM

1481.77

1482.08

1483.00

1484.10

1485.62

1487.00

1488.00

1489.50

1491.00

1492.50

1494.00

1495.55

1497.00

TO

1482.08

1483.00

1434.10

1485.62

1487.00

1488.00

1489.50

1491.00

1492.50

1494.00

1495.50

1497.00

1498.50

LENGTH

0.31

0.92

1.10

1.52

1.38

1.00

1.50

1.50

1.50

1.50

1.50

1.50

1.50

M S. xla's

1.23

1.50

4.50

0.42

6.94

8.00

10.50

4.50

9.00

5.00

0.95

5.00

9.00

ASSAYS

Au

PPe

DIAMOND DRILL LOG

COMPANY

PROPERTY

COMMENCED

COMPLETED

OBJECTIVE

NTS

DISTRICT

TWP/LAT.LONG.

CLAIM

CO-ORD.

CORE SIZE

CONTRACTOR

DATE LOGGED

LOGGED BY

DDH COM


SURVEY DEPTH


COLLAR AZIMUTH

COLLAR DIP

ELEVATION

LENGTH

INTERVALM D Ft D

FROM

1511.80

1512.38

TO

1512.38

1525.00

xREG

100

100

X ROD LITHOTYPE

6

C5I


1509.17 to 1511.80 Extremely blocky, wedged ground; M.S. of 11.2 x 10"1 SI: lower

contact knife sharp @ 45" Co CA; in contact with mafic dyke/siltstone.

Ultra Mafic Dyke with inclusions of coblat siltstone; mafic dyke grey-black;

aphanitic to very fine grained; very high M.S. of 46.1 x 100 SI; rich in CaC03; no

visible sulphides; upper contact of dyke @ 45* to CA; also inclusions of lighter

grey weakly to altered cobalt series siltstones; unit blokcy A broken.

Cobalt Series Mudstones i Siltstones; grey aphanitic to vry fine grained; very

thinly laminated; weak pervasive k-alteration; rare large dropstone: up to cobble

size; several ultramafic dykes unit generally blocky i wedgy; bedding varies from

SAMPLE

SAMPLE NO.

8269

8270

8271

8272

8273

8274

8275

8276

8277

8278

8279

8280

8281

FROM

1498.50

1500.00

1501.50

1503.00

1504.50

1506.00

1507.50

1509.00

1510.50

1511.80

1512.38

1513.70

1515.00

TO

1500.00

1501.50

1503.00

1504.50

1506.00

1507.50

1509.00

1510.50

1511.80

1512.38

1513.70

1515.00

1516.50

LENGTH

1.50

1.50

1.50

1.50

1.50

1.50

1.50

1.50

1.30

0.58

1.32

1.30

1.50

M.S., 10' SI

10.80

10.20

11.00

8.50

13.00

13.50

13.00

12.10

13.00

46.10

3.10

45.00

1.00

ASSAYS '

Au PI*

DIAMOND DRILL LOG W.A. HUBACHECK CONSULTANTS LTDTORONTO, ONTARIO, CANAD/






SURVEY DEPTH


COLLAR AZIMUTH

COLLAR DIP

ELEVATION

LENGTH

INTERVALM D Ft D

FROM

1525.00

1536.50

TO

1536.50

1555.75

xKEC

100

100

* OD LITHOTYPE

C5I

C5I


20 to 60* to CA near contact: M.S. of 0.56 to 5.8 x 100 SI: further down hole

consistently @ 85-90 ' to CA.

1513.70 to 1515.00 UltrannuTic Dyke near parallel to core axis; host by siltstone/

mudstone; blocky SL broken core; M.S. up to 86.1.

1517.70 to 1518.96 Ultramafic Dyke; aphanitic to fine grained; M.S. 86.6 x 10'3 SI;

very rich in CaCO,; upper It lower contacts @ 15" to CA; dykes intact just blocky/

wedgy along contacts.

1521.66 lo 1522.42 Granodionhic Dyke; pink medium grained; epodhized; M.S. of

0.37 x 10~3 SI; weakly foliated @ 60" to CA; up to 196 cpy; upper contact

@ 45" to CA; lower contacat @ 70* to CA.

Similar lo 1512.30 to 1525.00 however M.S. significantly higher 14.6 to 24.2 x 10J

very thickly laminated to thinly bedded; bedding @ 85-90* to CA.

Similar to above with lower M.S. of 0.29 to 3.21 x lO'3 SI; generally 0.29 to 0.39 x

SI.

SAMPLE

SAMPLE NO.

8282

8283

8284

8285

8286

FROM

1516.50

1517.50

1518.96

1520.50

1521.66

TO

1517.70

1518.96

1520.50

1521.66

1522.42

LENGTH

1.20

1.26

1.54

1.16

6.76

M.S. x Iff1 SI

2.85

86.50

1.80

1.75

0.37

ASSAYS

Au PI*

1

j

DIAMOND DRILL LOG





OBJECTIVE CO-ORD. DDH COM

SURVEY DEPTH DIP AZIMUTH


PAGE 18/18HOLE NO. FBW-01

COLLAR AZIMUTH

COLLAR DIP

ELEVATION

LENGTH

INTERVALM D Ft D

FROM

1555.75

1573.45

1590.96

1602.00

TO

1573.45

1590.96

1602.00

xREG

100

100

100

*RQO LITHOTYPE

C5I.J

C5I

C5I

E.O.H.

DESCRIPTIONGEOLOGY: (colour, grain sac, texture, minerals, alteration, etc)

Cobalt Series Siltstones A. Mudstones with narrow beds of sandstone: erev aphanitic

to very fine grained; very thinly laminated to thinly bedded; rare dropstone?; M.S.

variable from 0.39 to 39.6 x 10'3 SI; generally M.S. around 2.0 x 10"3 SI; mudstones

have low M.S.; sandstones have high M.S. with siltstones generally 2.0 x 10J SI;

bedding 85-90" to CA; trace pyrite; no CaCO,.

Cobalt Series Siltstones Si Mudstones; dark grey aphanitic to very fine grained;

very thinly laminated to very thinly bedded; bedding @ 35" to CA; M.S. of

1.27 to 4.85 x 10-' SI; generally M.S. 2.5 x 10"' SI; no CaCOj; trace pyrite;

rare dropstones.

Cobalt Series Siltstone; grey very fine grained possibly one bed; M.S. relatively

consistent between 3.0 to 4.0 x 100 SI; dropstones are extremely rare; no CaCCS;

no evidence of lamination or bedding units; no visible sulphides.

SAMPLE

SAMPLE NO.

FROM TO LENGTHM.S., W SI

ASSAYS

Al PI*

Ontario MnMryolNortfiem Developmentand Mines

Declaration of Assessment Work Performed on Mining Land

- - ' ' "'2) and 66(3), R.S.O. 1990

Transaction Number (office use)

. bOOA lAssessment Files Research Imaging

authority of subsections 65C2) and 66(3) of the Mining Act. UndeJ . This information will be used to review the assessment work anC ction should be directed to a Provincial Mining Recorder, Ministry , Sudbury, Ontario, P3E 6B5.

31M05NW2004 2.19192 FIRSTBROOK 900Instructions: - For work performed on Crown Lands before recording a claim, use form 0240.

- Please type or print in ink.

1. Recorded holder(s) (Attach a list if necessary) 2.19 192Name Silver Century Explorations Ltd.Address c/o W. A. Hubacheck Consultants Ltd.,

#807-365 Bay St., Toronto, Ontario, M5H 2V1Name

Address

2. Type of work performed: Check (/) and report on only ONE of the following g

Client Number 301001Telephone Number: 416-364-2895

Fax Number: 416-364-5384

Client Number

Telephone Number:

Fax Number:

roups for this declaration.

Geotechnical: prospecting, surveys, assays and work under section 18 (regs) X Physical: drilling stripping,

trenching and associated assaysRehabilitation

Work Type- diamond drilling

Dates Work From 28 09 Performed Day | Month

Global Positioning System Data (if available)

11997 To 13 11 1997

| Year Day | Month | Year

Township/Area Firstbrook Twp.

M or G-Plan Number:

Commodity

Total S Value of Work Claimed

NTS Reference:

Mining Division7i

Resident Geologist District ^

Office Use

AifS. /C 5

0 -f, k*

k'tk/Afid. -A^tU-

Please remember to: - obtain a work permit from the Ministry of Natural Resources as required;- provide proper notice to surface rights holders before starting work;- complete and attach a Statement of Costs, form 0212;- provide a map snowing contiguous mining lands that are linked for assigning work;- include two copies of your technical report.

3. Person or companies who prepared the technical report (Attach a list if necessary)

Name Peter C. Hubacheck, Lorne D. Burden W. A. Hubacheck Consultants Ltd.,Address #807-365 Bay Street, Toronto, Ontario, M5H 2V1Name

Address

Name

Address

Telephone Number 416-364-2895Fax Number 416-364-5384Telephone Number

Fax Number

Telephone Number

Fax Number

4. Certification by Recorded Holder or Agent

I, David W. Christie , do hereby certify that I have personal knowledge of the facts set forth in(Print Name)

completion and, to the best of my knowledge, the annexed report is true.

Signature of Recorded H

lir or,.

Agent's Address l ""c/o W. A. Hubachedk Consultants LtdSt., Toronto, Ontario, H5H 2V1

#807-365 BayTelephone Number

416-364-2895

Fax Number f

416-364-53840241 (06/97)

RECEIVEDJAN 08 ICj3 4

GEOSCIENCE ASSESSMENT OfFICE

5. Work to be recorded and distributed. Work can only be assigned to claims that are contiguous (adjoining) to the Mining land where work was performed, at the time work was performed. A nap showing the contiguous link must accompany this fora.

Mining Claim Nuabar. Or if work was done on other eligible mining land, show in this column the location number indicated on the claim map.

*g

eg

*g

1

2

3

4

5

6

7

8

9

10

11

12

13

14

15

1202668

1202671

Column Totals

Busbar of Claim Oniti. For ocher mining land, list hectares.

16

16

Value of work performed on this claim or other mining land.

S 268,105

0

S 268,105

Value of work applied to this claim.

2.

0

S 985

S 985

Value of work assigned to other mining claims.

1919

S 985

0

S 985

Bank. Value of work co be distributed at a future date

•2

S 267,120

0

S 267,120

l, David U. Christie , do hereby certify that the above work credits are eligible under(Print Pull Nane)

subsection 7 (1) of the Assessment Work Regulation 6/96 for assignment to contiguous claims or for application to the claim where the work was done.

A ySignatur zed in Writing

6. Instructions for cutting back credits that are not approved.

Some of the credits claimed in this declaration may be cut back. Please check (/) in the boxes below to show how you wish to prioritize the deletion of credits:

X 1. Credits are to be cut back from the Bank first, followed by option 2 or 3 or 4 as indicated.

CI 2. Credits are to be cut back starting with the claims listed last, working backwards; or

d 3. Credits are to be cut back equally over all claims listed in this declaration; or

Q 4. Credits are to be cut back as prioritized on the attached appendix or as follows (describe):

Note: If you have not indicated how your credits are to be deleted, credits will be cut back from the Bank first, followed by option number 2 if necessary.

For Office Use OnlyReceived Stamp

0241 (06/97)

RECEIVED (

JAN G 8 1233 *

GEOSCIENCF ASSESSMENTOfFICE

Deemed Approved Date

Date Approved

Date Notification Sent

Total Value of Credit Approved

Approved for Recording by Mining Recorder (Signature)

Ontario MMMyofNorthern Developmentand Mines

Statement of Costs for Assessment Credit

Transaction Number (office use)

OOP a y- ^

2.191f subsection 6 (1) ofthPersonal information collected on this form is obtained under the authority of subsection 6 (1) ofthe Assessment Work Regulation

6/96. Under section 8 of the Mining Act, this information is a public record. This information will be used to review the assessment work and correspond with the mining land holder. Questions about this collection should be directed to a Provincial Mining Recorder, Ministry of Northern Development and Mines, 3rd Floor, 933 Ramsey Lake Road, Sudbury, Ontario, P3E 6B5.

Work TypeUnits of work

Depending on the type of work, list the number of hours/days worked, metres of drilling, kilometres of grid line, number of samples, etc.

Geologists' Wages

Technicians' Wages

Drill Contractor -reaming: 1147m.; drilling: 455m.

Consulting Fee

Site Preparation

Surveying Costs

Associated Costs (e.g. supplies, mobilization and demobilization).

Nob/Demob Costs

Core Shack/Field Office Renta l

Core Saw Supplies

Report Preparation

Field Supplies and Expenses

Transportation Costs

Truck and Snowmobile Rental

Gas

Shipping

Food and Lodging Costs

Equipment Rental

Cost Per Unit of work

Total Value of Assessment Work

Total Cost

S

S

S

11,687.88

1,067.33

210,287.47

i 35,544.50

S

S

220.00

290.00

S

t

i

3,068.20

600.00

375.00

* 268.90

S

S

S

S

S

S

S

345.98

493.92

1,842.63

183.45

85.50

1,644.17

100.00

S 139,429.79

Calculations of Filing Discounts:

Lwork filed within two years of performance is claimed at 100X of the above Total Value of Assessment Work.2.If work is filed after two years and up to five years after performance, it can only be claimed at 502! of the Total Value ofAssessment Work. If this situation applies to your claims, use the calculation below:

x 0.50 = Total S value of worked claimed.TOTAL VALUE OF ASSESSMENT WORK Note:-work older than 5 years is not eligible for credit.-A recorded holder may be required to verify expenditures claimed in this statement of costs within 45 days of a request for verification and/or correction/clarification. If verification and/or correction/clarification is not made, the Minister may reject all or part of the assessment work submitted.

Certification verifying costs:

I, David W. Christie, do hereby certify, that the amounts shown are as accurate as may reasonably(please print full name)

be determined and the costs were incurred while conducting assessment work on the lands indicated on the accompanying Declaration of Work form as ______________ Agent___________ I am authorized to make this certification. (recorded holder, agent, or state company position with signing authority)

RECEIVED,

JAN c e r:;-:GEOSCIENCE ASSESSMENT

OFFICE___ _

/LSignat Date

0212 (06/97)

Ministry of Minlstere duNorthern Development Developpement du Nordand Mines et des Mines Ontario

Geoscience Assessment Office 933 Ramsey Lake Road

June 16, 1999 6th FloorSudbury, Ontario

SILVER CENTURY EXPLORATIONS LTD. P3E 6B5401 BAY STREET, SUITE 2302P.O. BOX 102 Telephone: (888) 415-9846TORONTO, ONTARIO Fax: (877)670-1555M5H-2Y4

Visit our website at: www.gov.on.ca/MNDM/MINES/LANDS/mlsmnpge.htm

Dear Sir or Madam: Submission Number: 2.19192

Status Subject: Transaction Number(s): W9980.00029 Approval After Notice

We have reviewed your Assessment Work submission with the above noted Transaction Number(s). The attached summary page(s) indicate the results of the review. WE RECOMMEND YOU READ THIS SUMMARY FOR THE DETAILS PERTAINING TO YOUR ASSESSMENT WORK.

If the status for a transaction is a 45 Day Notice, the summary will outline the reasons for the notice, and any steps you can take to remedy deficiencies. The 90-day deemed approval provision, subsection 6(7) of the Assessment Work Regulation, will no longer be in effect for assessment work which has received a 45 Day Notice. Allowable changes to your credit distribution can be made by contacting the Geoscience Assessment Office within this 45 Day period, otherwise assessment credit will be cut back and distributed as outlined in Section #6 of the Declaration of Assessment work form.

Please note any revisions must be submitted in DUPLICATE to the Geoscience Assessment Office, by the - response date on the summary.

If you have any questions regarding this correspondence, please contact Lucille Jerome by e-mail at [email protected] or by telephone at (705) 670-5858.

Yours sincerely,

ORIGINAL SIGNED BYBlair KiteSupervisor, Geoscience Assessment OfficeMining Lands Section

Correspondence ID: 13909

Copy for: Assessment Library

Work Report Assessment Results

Submission Number: 2.19192

Date Correspondence Sent: June 16, 1999 Assessor: Lucille Jerome

Transaction Number

W9980.00029

Section:16 Drilling PDRILL

First Claim Number

1202668

Township(s) l Area(s)

FIRSTBROOK

Status

Approval After Notice

Approval Date

May 18, 1999

The 45 days outlined in the Notice dated March 31, 1999 have passed. Assessment work credit has been approved as outlined on the attached Distribution of Assessment Work Credit sheet.

The assessment credit is being reduced by 835,544. The TOTAL VALUE of assessment credit that will be allowed, based on the information provided in this submission, is 8232,561.00.

Correspondence to:

Resident Geologist Kirkland Lake, ON

Assessment Files Library Sudbury, ON

Recorded Holder(s) and/or Agent(s):

David W. ChristieTORONTO, ONTARIO, CANADA

SILVER CENTURY EXPLORATIONS LTD. TORONTO, ONTARIO

Page: 1


Distribution of Assessment Work Credit

The following credit distribution reflects the value of assessment work performed on the mining land(s).

Date: June 16, 1999

Submission Number: 2.19192

Transaction Number: W9980.00029

Claim Number Value Of Work Performed

1202668 232,561.00

Total: S 232,561.00

Page: l


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THIS TOWNSHIP FALLS WITHIN THE TEMAGAMI COMPREHENSIVE PLANING AREA. SPECIAL WORKING CONDCriONS MAY APPLY TO EXPLORATION ACTIVITIES, FOR MORE DETAJLS PLEASE CONTACT:

DISTRICT MANAGER, NORTH BAY DISTRICT MINISTRY, NATURAL RESOURCES

NOTICE OF FORESTRY ACTIVITYTHtt TOWNSHT ; AHEA FALL* WTTMIN THE ^^.

LATCHFORD MANAGEMENT UNIT

CONTACTED AT; P.O. BOX 36

POH 2HO7O5 569 3622

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THE INFORMATION THAT APPEARS ON THI8 MAP HAS BEEN COMPILED FROM VARIOUS SOURCES. AND ACCURACY IS NOT GUARANTEED. THOSE WISHING TO STAKE UN- ING CLAIMS SHOULD CON SULT WITH THE MtNWG HECOKOea MINISTRY OF NORTHERN DEVELOP MENT AND MINES. FOR AD DITIONAL INFORMATION ON THE STATUS OF THE LANDS SHOWN HEREON.

.CIRCULATED MAY 3/68AACKIVEC JANUARY 9, l

ARCHIVED JUNE 24/97

Tfio di&r.nsilifiri of tan J, locatinn ol lot latx'C and partul boundaries onIhi^ TiK'ji r, is rurnpilfL1 tor admnuaimtvt purp-rses only.

report on the 1997 diamond drilling program for€¦ · daily turbo-prop air service to toronto is...

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