2 223 49

CAMECO GOLD INC.

REPORT ON THE FALL 2000 DIAMOND DRILL PROGRAM

BRISTOL AND BRISTOL NORTH PROPERTIES, BRISTOL TOWNSHIP

ONTARIO, NTS 42A/06

2. 22349CAMECO GOLD INC.

"Report on the Fall 2000 Diamond Drilling Program"

BRISTOL AND BRISTOL NORTH PROPERTIESBristol Township, Ontario

NTS 42A/06

Copy - Ontario Government

October, 2001 M. Koziol District Geologist

42A06NW2030 2.22349 BRISTOL Q10

SUMMARY 2 . 22349

Cameco Gold Inc. completed three diamond drill holes for a total of 741 m between November 15 and December 7, 2000, on the Bristol and Bristol North projects, both in the Bristol Township, Porcupine Mining Camp, District of Cochrane. The properties are located approximately 10 km west of Timmins, Ontario and together cover 1,952 ha (106 claims).

The purpose of the program was to test the mafic volcanic-sedimentary contact north of the Bristol Porphyry and to test IP anomalies in the northwest corner of the property. The drilling identifies geological potential in areas of bleaching and veining within mafic flows (holes BRSOO-03 and 04) and in "grey zones" within mafic flows similar to Hoyle Pond (BRSOO-03). Gold assays however, are disappointing, returning a best assay of 170 ppb Au from the altered mafic flows near the top of BRSOO-03 and 96 ppb Au from a grey zone in the same hole.

One diamond drill hole is recommended to test a weak IP anomaly to the northeast of BRSOO-03 to determine if there is potential for Hoyle Pond style of mineralization.

Cameco Gold Inc. Bristol and Bristol North Projects Report on the Fall 2000 Diamond Drilling Program

2 9 9 S 4 Q . *w (O O Tt U

SUMMARY

TABLE OF CONTENTS

Page

1.0 INTRODUCTIONl. l Property, Location, Access and Topography l1.2 Claim Ownership and Land Status l1.3 Previous Work 4

2.0 GEOLOGY2. l Regional Geology 52.2 Local Geology 52.3 Property Geology and Gold Mineralization 6

3.0 CAMECO GOLD EXPLORATION DRILLING3.1 Purpose Description of the Fall, 2000 Drilling Program 83.2 Drill Hole Descriptions and Results 10

4.0 CONCLUSIONS 11

5.0 RECOMMENDATIONS 12

6.0 REFERENCES 12

7.0 CERTIFICATES OF QUALIFICATION 14

LIST OF FIGURESFigure l Property Location Map 2 Figure 2 Claim Map 3 Figure 3 Fall, 2000 Diamond Drill Hole Locations 7

LIST OF TABLESTable l Claims Upon Which Work Was Completed 9 Table 2 Drilling Statistics 9

LIST OF MAPSMap l Vertical Geological Cross Section, L27+OOE, Hole BRSOO-03 in pocket Map 2 Vertical Geological Cross Section, L40+OOE, Hole BRSOO-04 and 05

LIST OF APPENDICESAppendix l Detailed Diamond Drill logs - Fall 2000 Drill Program Appendix 2 Gold Assay and ICP Certificates for all Analyses

Cameco Gold Inc. Bristol and Bristol North Projects Report on the Fall 2000 Diamond Drilling Program

2 223491.0 INTRODUCTION

This report describes the Fall 2000, 741 m diamond drilling program that was completed by Cameco on its Bristol and Bristol North projects, located in the Bristol Township, Ontario.

1.1 Property, Location, Access and Topography

The Bristol property is located in the centre and along the eastern boundary of Bristol Township, in the District of Cochrane, Ontario (Fig. 1). The Bristol North project is made up of four contiguous claims and adjoins the north boundary of the Bristol property. Highway 101 bisects the property and provides ready access from the City of Timmins, located 10 km to the east. Access north of highway 101 is provided by the Malette access road which trends in a NNW direction. Access south of the highway is through Gagnon's autowrecking yard. A NW grid (Az. 150 degrees) provides immediate controlled access points to the north and south of highway 101.

The topography is relatively flat and covered by black spruce with local alders growing near meandering creeks and rivers. Locally edges of certain creeks exhibit steep banks due to erosion. The entire property is covered by a 20 to 25 m thick veneer of overburden which consists of sand and clay. Recent cutting and replanting has occurred to the immediate south and north of the highway. A portion of the Tembec lumber operations (formerly Malette) is located south of Highway 101 near the Bristol/Ogden Twp. boundary, in Ogden Twp.

The narrow, locally meandering Bristol Creek, travels across the entire width of the property in a NE direction south of and parallel to highway 101. A subparallel unnamed creek, is located approximately one kilometre to the south of the Bristol Creek. Both creeks join the north trending Mattagami River, located along the western margin of Ogden Twp.

1.2 Claim Ownership and Land Status

The Bristol and Bristol North project together consist of a contiguous block of 106 unpatented mining claims, located in Bristol Township, except for eleven that are located in Ogden Township. The one hundred and two claims that make up the Bristol project are under option from Placer Dome Inc. and Cameco is working towards earning a I0007o interest in these. The four claims that make up the Bristol North project are owned lOO'Vo by Cameco. The mining rights cover a total area of 1,952 hectares. All of the claims are registered to Cameco Corporation of Saskatoon, Saskatchewan, but work on these is being carried out by Cameco Gold Inc, a wholly owned subsidiary of Cameco Corp. All of the claims are in good standing to March 2002 and most have excess assessment credits to maintain the property beyond 2002. A list of claims covering the work reported in this report is provided in Table l and the claims that make up the two projects are illustrated in Figure 2.

Cameco Gold Inc. Bristol and Bristol North Projects Report on the Fall 2000 Diamond Drilling Program

ONTARIO QUEBEC

BRISTOL

USA

Timmins

Kirkland Lake. ' Val-d'Or

100 200 300 400 500km

g 22349

Bristol A Bristol North Projects

DISPOSITION MAP

1000 1500 2000 2500mi i i i i i i i i i i i i i i i i i

Dwg. No.: BRI00004Compiled: Mike KozidDrafted: CJoyton Ourbin

Scale 1:35000 Geo. Ret.: NAD 27 - UTM Zone 17

NTS Rei.: 42 A/5,6

2. 22349

1.3 Previous Work

The general geology of the Bristol Twp. area was first mapped for the Ontario government by Hawley (1927) and subsequently re-mapped by Ferguson (1957).

Placer Dome report that the Hoyle Mining Company Limited drilled a 1,195' hole in 1945, in the SW corner of the property (Cole, 1986). Records of this drilling were not located but Placer Dome reported the presence of feldspar porphyry and felsic volcanics in this hole.

Geophysical Surveys Inc. completed an airborne geophysical survey for Tegalder Resources Inc., in December, 1980. This combined EM and magnetic survey was completed over most of the property.

Texasgulf Canada Limited completed a combined airborne EM and magnetic survey over a number of townships west of Timmins in May, 1981 (Gasteiger, 1981). This survey covered the NW corner of the property. Flight lines were orientated north-south with one-eight (1/8) mile line spacing. Texasgulf Canada subsequently drilled seven overburden holes in what is now the Bristol North project in late 1981 (see Fig. 3), to test airborne conductors marking the north sediment/mafic volcanic contact.

Placer Dome Inc. [formerly Dome Exploration (Canada) Limited] acquired the property in 1984. Placer cut a north-south grid with 100 m spaced lines and 25 m station pickets over the entire property. Placer mapped the property in the fall of 1984, however only two trenches with mafic volcanics were located in the NE corner of the former Placer Dome Bristol Property.

Placer completed an HLEM and magnetic survey in 1984 and a VLF survey was completed over the southern half of the property in 1985. Placer completed 14 km of I.P. in 1987 and an additional 7.5 km of I.P. in 1988.

Placer completed three separate drill campaigns on the property. In the fall of 1985, holes 246-1 through 246-22 were completed (4,917 m). In the spring and fall of 1987, holes 246-23 through 246-50 were completed (7,453 m). In 1988, holes 246-51 through 246-81 (7,773 m) were completed. A cumulate total of 81 holes and 20,143 m was drilled on the property over a period of four years. All of this drilling was targeting mineralization above the 300 m elevation.

Teck Corporation Limited optioned the property from Placer Dome in 1994-1995, and completed S412,370 worth of work. This work consisted of new line cutting (orientated SE at 150 Az.), real section I.P. over a selected portion of the property and 4 diamond drill holes (1,625 m).

Cameco optioned the property in the fall of 1998. Compilation work and the selective relogging of historic core was completed during 1999. A magnetic and I.P./Resistivity survey (pole- dipole) was completed over the NE corner of the property in the winter of 2000. In May, 2000, Cameco completed a 1,006 m diamond drilling program testing the gold bearing porphyry discovered by Placer. The drilling included two new holes and the deepening of two holes

Cameco Gold Inc. Bristol and Bristol North Projects Report on the Fall 2000 Diamond Drilling Program

drilled by Placer in the 1980's Coad et al., 2000). Elevated gold was detected in all four holes.

2.0 GEOLOGY

2.1 Regional Geology

The Bristol property is located on the west margin of the world class Porcupine Gold Camp (PGC) in the southwestern portion of the 2.7 Ga Abitibi Belt (Figure 2). Gold deposits in the Abitibi Belt tend to cluster in camps, of which the PGC has been by far the most productive (61 million oz. gold) to date. The deposits in the Timmins area have been mined to depths greater than 2,000 m. These centres of gold-bearing magmatic and hydrothermal activity are spatially located near regional fault structures such as the Destor-Porcupine fault and the Cadillac Larder fault.

Orebodies in the PGC are typified by single or multiple quartz-carbonate veins with or without albite, tourmaline, sericite, fuchsite, pyrite and other sulphides, and native gold hosted in variably altered wallrock of intrusive, extrusive or sedimentary origin. Gold can occur both in the veins and the immediate wallrock. The most significant gold deposits are spatially associated with quartz feldspar porphyry stocks and dikes and with albitite dikes/sills or "syenites", both of which intruded folded Archean supracrustal rocks. The supracrustal rocks, felsic intrusions and gold mineralization were affected by metamorphism and penetrative deformation and folding during the Kenoran Orogeny.

2.2 Local Geology

All bedrock in the Timmins area is of Archean age except the Proterozoic diabase dikes. Four groups of Keewatin volcanic rocks, with less abundant intercalated sedimentary rocks, are present in the area. These are the Deloro and Tisdale Groups (Dunbar, 1948), the Krist Formation (Ferguson, 1957) and the Porcupine Group (Pyke, 1982). The Deloro Group underlies the Tisdale Group and consists of a calc-alkaline group of volcanics which forms the core of the Shaw Dome located south of the Destor-Porcupine fault. The Tisdale Group of volcanics have been age dated between 2710 and 2702 Ma. They are predominantly iron-rich with a general trend to iron enrichment stratigraphically upwards. Intercalated komatiitic and magnesium-rich tholeiitic flows in the lower portion of the group give way to magnesium-rich flows intercalated with lesser iron-rich tholeiitic flows in the middle of the group, and finally to iron tholeiites at the top of the group (Pyke, 1982). The group is divided into four formations: the Northern, Central, Vipond and Gold Centre formations. Importantly, over 750Xo of the gold produced to date in the PGC was mined from orebodies in Tisdale Group rocks.

Krist Formation felsic volcaniclastic and Porcupine Group sedimentary rocks unconformably overlie the Tisdale Group (Buffam, 1948; Brisbin, 1997) and occupy synclines in Tisdale and Deloro Twps. Calc-alkaline, bedded, heterolithic, quartz and feldspar phyric intermediate to felsic volcaniclastic rocks characterize the Krist Formation. Interbedded wackes, including

Cameco Gold Inc. Bristol and Bristol North Projects Report on the Fall 2000 Diamond Drilling Program

turbidites and argillites conformably overlie the Krist and are included in the Porcupine Group of sediments (Pyke, 1982). Sediments located further away from the Porcupine syncline have been included in the Whitney Formation, Hoyle Assemblage and recently the Porcupine Assemblage (Ayersetal, 1999).

The youngest Archean supracrustal rocks in the Timmins area belong to the Timiskaming Group. These sediments consist of polymictic conglomerates, wackes and argillites and unconformably overlie the folded Keewatin Tisdale Group, Krist Formation and Porcupine Group volcanic and sedimentary rocks. A maximum depositional age of 2679 +I- 3 Ma has been recorded for these sediments. Importantly, l^/o of gold mined in the PGC has been hosted by Timiskaming Group rocks, making them the second most important host of gold in the camp.

2.3 Property Geology and Gold Mineralization

The property geology is marked by an east trending package of sediments which are bounded to the north by mafic volcanics and intruded in the central part of the property by variably altered quartz feldspar porphyry. Recent age dating suggests that the mafic volcanic rocks on the north side of the property belong to the Tisdale Group (Ayers et al., 1999). The sediments locally contain appreciable percentages of quartz grains. The mafic volcanic/sediment contact is marked by graphitic argillite and interpreted to dip north based on limited drill hole information. The property is intruded by numerous north trending diabase dikes of variable width. Over the central and south parts of the property, stratigraphic facing is to the south based upon graded bedding and flame structures in the sediments.

Structurally, the property is marked by an east trending series of steep north dipping faults or shears which impart a moderate to strong foliation to all rock types except the diabase dikes. These strong shear zones are best developed in the quartz feldspar porphyries which are locally strongly altered by sericite, chlorite and hematite (and possibly K-feldspar(?)) alteration and silicification. Albite phenocrysts are less common in these areas of intense alteration.

Gold values are spatially associated with disseminated fine to coarse grained subhedral pyrite which locally forms crude bands in the strongly foliated quartz porphyry. These chloritized bands of pyrite and minor chalcopyrite may be cored by quartz-carbonate veins which have been subsequently boudinaged. Visible gold has been recognized occurring as free grains in chlorite and/or quartz-carbonate veins or as inclusions in pyrite or chalcopyrite. However, not all pyrite is associated with gold mineralization.

Variably coloured anhydrite occurs locally as a late in-filling of quartz-carbonate (iron carbonate) veins that occur as tensional and strike-type veins. Black tourmaline can occur within the quartz- carbonate veins or as minute black-green needles within the matrix areas of altered sediments and porphyries.

Cameco Gold Inc. Bristol and Bristol North Projects Report on the Fall 2000 Diamond Drilling Program

lNorth \

O 100 200 300 400 500m i i i i i i

Scale 1:15000r135 81-f

^ Water hen Lake

13966 4 a\

\ \ \

i 985657 \9856

0-03N

983615 9S'56I6\

BR-1Legend

I.P. AnomalyI.P. Anomaly Trend

BRS0003 cameco Fall 2000 Diamond Drill Hole

j"*-* Old Diamond Drill Hole W-1J9 old Overburden Drill Hole

Cameco

Bristol A Bristol North Projects

FALL 2000DIAMOND DRILL HOLE

LOCATIONSCompiled: Mfce KozM Dwg. No.: BR100003Drafted: Ctayton Durbfci Date: 01/10/16

Figure 3Scale: 1:15.000 Geo. Bat.: NAD 27 - UTM Zone 17NTS Rat.: 42 AA6 Source:

3.0 DIAMOND DRILLING

3.1 Purpose and Description of the Fall, 2000 Drilling Program

The purpose of the three hole (BRSOO-03 to 05), 741 m diamond drilling program was to test the mafic volcanic-sedimentary contact north of the Bristol Porphyry and to test IP anomalies in the northwest corner of the property. The program was carried between November 15 and December 7, 2000. The drilling was performed by Bradley Brothers of Timmins.

The drilling was supervised in the field by Paul Coad, Project Geologist and Jacques Samson, Geologist, both residents of Timmins. Drill cores were logged in detail by Mr. Samson. All of the drill cores processed at a coreshack facility behind the Bradley Brothers shop in Timmins. The NQ-size cores were then sampled by Louis Perron of Val d'Or. Sampling procedures involved the splitting of core with a diamond saw. Half the core was shipped to Bondar Clegg in Timmins for assay preparation and then to Chimitec in Val d'Or for assaying. The remaining half core is being kept as a permanent record. All samples were prepared with standard crushing and grinding. Gold assays were obtained using fire assay procedures on a 30 gram sub-sample with AA (atomic absorption) finish. A 34 element ICP scan was also completed on each of the samples. A total of 371 samples were analyzed.

The detailed geological logs are contained in Appendix A and the assay certificates form Appendix B. The drill cor"e from this program is being temporarily stored at the Bradley yard. The drill hole locations are illustrated in Figure 3 and geological cross sections are appended in the back pocket.

Cameco Gold Inc. Bristol and Bristol North Projects Report on the Fall 2000 Diamond Drilling Program

TABLE l

Claims Upon Which Work Was Completed

Claim #

985625

1226640

Hole#

BRSOO-03

BRSOO-04 fc BRSOO-05

TABLE 2

Drilling Statistics

Hole#

BRSOO-03

BRSOO-04

BRSOO-05

Collar

L2700E+1500N

L40+OOE, 28+50N

L-40+OOE, 31+75N

Azimuth

150

330

150

Dip

-50

-47

-50

Final Depth

368m

119m

254m

# of Samples Analysed

177

30

124

Cameco Gold Inc. Bristol and Bristol North Projects Report on the Fall 2000 Diamond Drilling Program

10

3.2 Drill Hole Descriptions and Results

Hole BRSOO-03, located at L2700E 4- l SOON, Azimuth 150, dip at -50, was drilled on the northern part of the Bristol project (Placer Dome option, please see Figure 3 and Map 1). The hole was drilled to test the projected mafic volcanic stratigraphy in contact with the sediment package to the south and specifically test the IP anomaly BR-1 outlined by the 2000 ground geophysical survey. This hole was targeting an Owl Creek-Hoyle Pond type of gold-model.

BRSOO-03 collared into altered mafic volcanic (moderate to strong ankerite-sericite alteration with variable quartz veining and trace sulphides) at 34 m. These are locally pillowed, amygdaloidal, variolitic and magnetic. The strongly altered mafic volcanics returned weakly anomalous gold near the top of the hole, up to 170 ppb Au71.5m at 35.5m.

IP anomaly BR-1 is marked by intervals, starting at 275.9m, of graphitic-argillite intercalated with mafic volcanics which have been darkened by diffuse carbon/graphite. This alteration compares to the grey zones present at Hoyle Pond. Variable but generally minor quartz veining with l to 3 07o pyrite, l to 3 07o pyrrhotite and trace arsenopyrite content are present in these grey zones. Graded bedding in a short interval of carbonaceous quartz-wacke, within the darkened mafic volcanics, indicates facing down hole to the south.

At 307.3 m the hole intersected greywacke sediments. Local short quartz veins are present within the greywacke package. These veins carry l-W/o fine grained pyrite as fractures within the glassy quartz veins and/or along vein margins. Fine grained tourmaline is present with the pyrite. Aphanitic patches of tourmaline also occur in the quartz veins. Minor fine to medium grained subhedral arsenopyrite occurs in the altered wallrock of the quartz veins and locally within the quartz. Flame structures in the greywacke indicate facing up the hole to the north in this area of the stratigraphy. Graded bedding, located further down the hole suggests tops to the south. It is possible that a synformal-like fold axis may be located close to the mafic volcanic/sediment contact area and that further south the greywacke package is dominated by a south facing sequence. The hole ends at 368m in greywacke.

The mixed interval of graphite/black argillite and altered mafic volcanics returned generally low gold values (tens of ppb), up to a maximum of 96 ppb/l.Om at 281m.

Hole BRSOO-04, located at L40+OOE, 28+50N, Azimuth at 330, dip at -47, was drilled on the Bristol North project to test the very weak IP anomaly BR-2 and the stronger BR-4 (please see Figure 3 and Map2). The hole was terminated at 119 m in diabase due to poor core angles and the fact that the hole was being drilled down dip. Based on core angles, the stratigraphy is dipping north at approximately 75 degrees and not south as initially interpreted from ground magnetics. The upper portion of the hole from 42 m (depth of overburden) to 115m, intersected pillowed mafic volcanics with variable barren vein structures. Three separate narrow quartz veins with crack-seal textures (filled with black tourmaline and local trace to minor disseminated pyrite) were intersected in unaltered pillowed mafic volcanic near the top of the hole. Two of these veins are associated with thin mud/gouge slips.

Cameco Gold Inc. Bristol and Bristol North Projects Report on the Fall 2000 Diamond Drilling Program

11

No significant gold values were obtained in this hole. A best value of 25 ppb Au was obtained from 58.5m to 60.0m, associated with minor pyrite.

Hole BRSOO-05, located at L-40+OOE, 31+75N, Azimuth at 150, dip at -50, was drilled on the Bristol North project to test IP anomaly BR-4 (please see Figure 3 and Map2). The hole collared into variably altered amygdaloidal mafic volcanics at 31.0 m, marked by an interval of strong albitization and silicification from 32.7 to 36. l. This interval is marked with 2-3 "/o quartz- calcite-chlorite veins with associated disseminated pyrite in both the rock matrix and the veins. The out-contact of this area of alteration is marked by fault gouge and brecciation from 45.3 to 46.4. Fault slips exhibit an average angle to core axis of 15 degrees. Thin mud/gouge slips occur down the hole further in amygdaloidal mafic volcanics from 46.4 to 49.0. The best gold value obtained from the above altered sections is 10 ppb Au.

The interval from 49.0 to 170.7, is dominated by variably silicified amygdaloidal mafic volcanic. However, some of the silicified sections could represent intermediate to felsic tuff as evidenced by the presence of local minute quartz eyes. A short interval from 146 to 149.0, is marked by weakly anomalous gold values ranging from 6 ppb Au/1.6 m to 67 ppb Au/ 0.4 m respectively.

Felsic tuff and massive rhyolite were intersected between 163.0 - 168.5 m and 170.7 - 187.7 m. These intervals are moderately sericitized and epidotized and cut by up to 207o quartz veinlets with associated disseminated pyrite in the veins and the immediate wallrock. The highest gold value obtained was 10 ppb Au/1.2 m at 185.0. These felsic intervals correspond with a resistivity high picked up in the 2000 EP survey.

The remainder of the hole to 254.0 (EOH), is dominated by massive to weakly amygdaloidal mafic volcanic of high Fe-tholeiitic affinity. Local white quartz veins are present, however they are devoid of mineralization and associated significant alteration. The highest gold value obtained was 13 ppb Au/1.4 m at 195.1. Diabase dikes are present from 191.2 to 192.1 and 224.9 to 225.1.

4.0 CONCLUSIONS

Three holes totalling 741m of diamond drilling were completed during the Fall, 2000 program. Target modelling indicates potential in areas of bleaching and veining within mafic volcanic flows (holes BRSOO-03 and 04) as well as the "grey zones" within mafic flows (BRSOO-03) similar to Hoyle Pond. Because the grey zones are graphitic, they can be traced with IP survey methods. Gold assays however are disappointing, returning a best value of 170 ppb Au from the altered mafic flows near the top of hole 03 and 96 ppb Au from a grey zone, also in hole 03.

Cameco Gold Inc. Bristol and Bristol North Projects Report on the Fall 2000 Diamond Drilling Program

12

5.0 RECOMMENDATIONS

No additional drilling is recommended to follow up the results obtained from this program. One drill hole is recommended to test a weak EP anomaly located near L42+00, 19+OON to test for "grey zone" style of mineralization.

6.0 REFERENCES

Ayers, J.A., Trowell, N.F., Amelin, Y., and Corfu, F., (1999), Project Unit 95-24. Geological compilation of the Abitibi Greenstone Belt in Ontario: Toward a revised stratigraphy based on compilation and new geochronology results. In Summary of Field Work and Other Activities 1998, Ontario Geological Survey Miscellaneous Paper 169, p. 14 to 24.

Brisbin, D.I. (1997), Geological setting of gold deposits in the Porcupine Mining Camp, Timmins, Ontario. Unpublished Ph.D. thesis, Queen's University, Kingston, 523 p.

Buffam, B. S.W. (1948), Moneta Porcupine Mine. In Structural Geology of Canadian OreDeposits Volume 1. Canadian Institute of Mining and Metallurgy, Montreal, p. 457-464.

Coad, P., and McCracken, T., (2000), Cameco Gold Inc., Report on the 2000 Diamond DrillWork Program, Bristol Property (Placer Dome Option), Bristol Township, Ontario, NTS 42A/06, unpublished company report.

Cole, B. (1986), Dome Exploration (Canada) Limited, Report on Diamond Drilling, Project 246, Bristol Township, unpublished company report.

Cole, B. (1988), Placer Dome Inc., Diamond Drilling Report, 1987, Project 246, Bristol Twp., unpublished company report.

Cole, B. (1988), Placer Dome Inc., Diamond Drilling Report, 1988, Project 246, Bristol Twp., unpublished company report.

Dunbar, W.R. (1948), Structural relations of the Porcupine ore deposits. In Structural Geology of Canadian Ore Deposits, Volume 1; Canadian Institute of Mining and Metallurgy, Montreal, p. 442-456.

Ferguson, S. A. (1957), Geology of Bristol Township, District of Cochrane, Ontario, ODM Annual Report, Vol. LXV1, Pt. 7.

Gasteiger, W. (1981), Geophysical Reports on Airborne EM and Mag Survey by Texasgulf Canada Limited, Assessment Reports no. 2.4323 and 2.3888, Ministry of Northern Development and Mines.

Cameco Gold Inc. Bristol and Bristol North Projects Report on the Fall 2000 Diamond Drilling Program

13

Hawley, I.E. (1927), Geology of Ogden, Bristol, and Carscallen Townships, District of Cochrane, Ontario, ODM Annual Report, Vol. XXXV, Pt. 6, p. 1-36.

Houle, M. Y. (1995), Quarterly Report, Placer Dome Option, Bristol Twp., Project 16320, unpublished company report.

Pyke, D.R. (1982), Geology of the Timmins area, District of Cochrane. Ontario Geological Survey, Report 219, 141 p., Map 2455.

Tegalder Resources Inc. (1980), Geophysical Report on Airborne Survey, Assessment Report no. 2.3752, Ontario Ministry of Northern Development and Mines.

Texasgulf Canada Ltd.(1981), Overburden Drilling Report, Assessment Report no. 2. .5041, Ontario Northern Development and Mines.

Cameco Gold Inc. Bristol and Bristol North Projects Report on the Fall 2000 Diamond Drilling Program

14

7.0 CERTIFICATES OF QUALIFICATIONS

I, Marian (Mike) Koziol, residing at 137 Cranbrook Crescent, Ontario, P3E 2N4, do here by certify that:

I am currently employed by Cameco Gold Inc. of 1349 Kelly Lake Road, Sudbury, Ontario, P3E 5P5;

I attended McGill University at Montreal, Quebec and earned a Bachelor of Science degree in Geological Sciences in 1978;

I have been continuously employed in my profession since graduation.

I am a member in good standing with the Association of Professional Engineers and Geoscientists of Saskatchewan and the Association of Professional Engineers of Ontario.

I have been directly involved in a supervisory role with this project since inception in 1999.

Signed in Sudbury, Ontario, this 29th day of October, 2001

M. Koziol ' District Geologist Eastern Canada District

Cameco Gold Inc. Bristol and Bristol North Projects Report on the Fall 2000 Diamond Drilling Program

2 2234

APPENDIX l

Detailed Diamond Drill Logs - Fall 2000 Drill Program

Cameco Gold Inc. Bristol and Bristol North Projects Report on the Fall 2000 Diamond Drilling Program

2. 22349Summary Geology Composite Interval

Camecom -~BmKBM

Cameco Gold Inc.Summary Log Sheet

Hole: BRSOO-03

Project: Bristol

UTM East: 464049

Grid East: 2700

UTM base: NAD27

Claim #: 985625

Township: Bristol

Start Date: 4/12/20

UTM North: 5363944

Grid North: 1500

Local Grid : Teck

Elevation: 297

Core Size: NQ

Completion Date: 9/12/20

Logged By: J. Samson

Drilled By: Bradley Bros. Ltd.

Length: 365

Core Storage: Dome Mine core storage area

Down Hole: ezShot Casing in Hole: NoCsg

Hole making water: No # of Au Samples: 177

Purpose: Test mafic vole/sediment contact andcorresponding IP-anomaly BR1.

Downhole Survey

spth m)

.0

0.0

8.0

9.0

0.0

4.0

Corrected Azimuth

148.7

150.6

151.4

152.5

151.3

151.

Dip

-48.4

-46.9

-45.8

-45.1

-44.7

-43.1

Mag Reading

5782 5772

5779

5783

5797

5773

From (m)

Hole Rock Sample

To (m) Sample* lithology

-50

-100

~

-150

-

200

-

-250

^-

-

-300

-

-

-

-350

"f"

•9'

.p.-

•9' 0 . '

jsLiv .

-'

v

vV

",

v

V

-'V

V

V

V

'^

v

v

V

V

v*

V

v

V

T

~

~

"T-

Overburden

mafic volcanics

argillite

greywacke

j

Diamond Drill Log Sheet

Project: Bristol Z . 22349

CarjJSSS Hole: BRSOO-03 ~~^

Depth (m)

2-:

4 -E

-;

5-E

6-E

7 1

8-E

9-E

^

10-:

11-E

12 1

13 -E

14 -E

^15-E

16-E

17 -r

'H19-:

;

Lithology

: .C?'.'

3 '. :

i'.'X?'- 1

|v

^ '. .p. 1

o --s '.-p- 1

^j ".-P-'^ ~-

i?' 1

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V

j '-

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V- 1-C5 -'

^'

"p'.'

Z'

-.p.

"V-

^f-

From (m)

0.0

To (m)

34.0

Lith code

OB

lithology

Overburden

text. Comments

Alteration

Chl

CvW

Ser

w

Silic

ow

Epi

C-**

Hem

OW

Carb

CM*

other

Accessory Min.

o/o Py

in?

Cpy

CMCO

'/oQz

ooT-CN

Struct.

Struc < tea

Assay

From (m)

To (m) Sam. # Au ppb Au

i li

Page: 1 of 19

Diamond Drill Log Sheet

\ Project: Bristol

Cameco H0ie: BRSOO-OS

i0)Q

--

21 i-E

22^

:23-:

24-E

25 -|

26

27-;

28-;

29 - Z

30 -E

-

31 -r

32 -E-

33-;-E

^

35 -r

x~

37-

38 -j

39-

Lithology

0 .'-.P,'o.'

-f?. 1

-.p'.'

P-'

-i?.'

^"f:

~V-

V-'

Vif 1.'

"^

-P-'

V--J .-p.

?; p-

f; P-'

~-*~,

v

V

^

x/

^-

f

From (m)

0.0

34.0

38.3

To (m)

34.0

38.3

41.7

Lith code

OB

i

1

lithology

Overburden

mafic volcanics

mafic volcanics

text. Comments

, very fine grained ^O.Smm), Massive flow. ...Strongly altered, light green,bleached by carbonate, sericite, and weaksilicification. Moderately foliated, locally displaying brecciation, healed by veining. Greyish to white quartz-calcite stringers and veinlets, 5 to r*. 1mm to tlOcm, at all angles tocore axis, irregular, disrupted, infilling fractures, locally vuggy. Trace of chlorite and tourmaline within some veins. Weakly blocky core, with Fa-oxide staining locally.

1, very fine grained (td 5mm), Massive \ mow. ...Altered, moderately sheared, \/brecciated, with *15'*felsic-lcoking ' pseudoclasts which probably represent \ dislocated quartz veins. Rock is greenish grey, bleached, fine-grained, speckled by carbonate and remnant feldspars. Quartz veining as previously described, decreasing in intensity, only present from 38.3 to 38.6m, decreasing to a trace downhole. Weak to moderately foliatedand brecciated.

Alteration

Chl

ow~

Ser

cvw-

Silic

CNN"

[

Epi

(NW'

Hem

CNW*

Carb

CVN-

other

Accessory Min.

"/o Py

o

"/o

Cpy

CNICO

o/o QZ

ooTV*

O.IIKO.SmmdPY, 01"*dCp. 7.* 0.1 to 10cm gwvnQZ,

O.I^O.SmmdPY, 2.* 0.1 to 1cm gwvnQZ,

Struct.

Struc

*H

sfol!

<tca

56

70

Assay

From (m)

34.0

35.5

37.0

38.3

To (m)

355

37.0

38.3

39.9

Sam. #

326

327

328

329

Au ppb

-5

170

8

-5

Au

) S C

J

Page: 2 of 19

Diamond Drill Log Sheet

Project: Bristol

CagJggS Hole . BRSOO-03

Depth (m)

i

141-

42-.

--

43-

44-5

45 H;

46-

47^

48-1

494

50-

51 -i

52 J

-

53-

54^

55 ~-

56^

57^

58-

59 -.

Lithology

v

V

V

V

V

V

y

IS

V

\s

v

-v

v

V

\s

\s

/ \s

V

From (m)

383

41.7

42.5

46.2

49.8

52.8

To (m)

41,7

42.5

46.2

49.8

52.8

67.0

Lith code

i

i

i

i

i

i

lithology

mafic volcanics ,/

mafic volcanics

mafic volcanics

mafic volcanics

mafic volcanics

mafic volcanics

text. Comments

, very fine grained ^O.Smm), Massive I flow. ..Altered, moderately sheared,

brecciated, with *15* felsic-looking pseudoclasts which probably represent dislocated quartz veins. Rock is greenish grey, bleached, fine-grained, speckled by carbonate and remnant feldspars. Quartz veining as j [previously described, decreasing in intensity, only present from 38.3 to 38.6m, decreasing to a trace downhole. Weak to moderately foliated land brecciated. l., very fine grained (*0.5mm), Massive j flow. ...Same as from 38.3 to 41 ,7m, but moderately blocky, locally strongly stained by f Fe-oxide; Core Is locally pitted, vuggy, "rotten", j, very fine grained M).5mm), Massive flow. ...Fault zone. Moderate to strongly fractured, pitted, locally ground, with perhaps 1016 lost core. Host rock Is medium green, moderately foliated mafic rock, almost gabbroic, with trace of fine leucoxene. Subtle lapilli-size clasts(?) indicate weak brecciation. Chloritic fracture infilling. Trace of irregular 1 guartz-calcite stringers, locally vuggy. 1

, very fine grained (cO.Smm), Massive amygdaloidal flow. ...Same as from 42.5 to 46.3m, medium-green to light-green, weakly fractured, and with trace of quartz-calcite amygdules, O.Scm. Trace of quartz veinlets, up to 1cm wide, mostly subparallel to the weak to moderate foliation.

, very fine grained (cO.Smm), Massive flow. ...Fault Zone. Medium-green to rusty brown. Strongly brecciated, fractured to ground core, locally pitted, vuggy, with local Fe-oxide, essentially "rotten" rock.

, very fine grained ^O.Smm), Massive pillowed flow. ...Bleached, massive to pillowed. Very fine grained, light greyish-green, almost argillaceous, but with subtle possible pillow rims (chloritoid) near 64.0m. Less than 1 V) fine feldspar phenocryst locally visible, mainly from 60 to 65m, up to 2mm in dia.. Bleached by weak to moderate sericite and chlorite. Moderately foliated, with slaty cleavage locally developped. Quartz-calcite*;-epidote veinlets and stringers at various angles, mostly parallel to foliation. Pyrite is disseminated to wispy, along foliation planes.

Alteration

Chl

(NW

Ser

c*r

'

Silic

0*1-

Epi

e*r

Hem

CNW

Carb

CNW

other

Accessory Win.

"/o Py

o0-

"/o

Cpy

CVJCO

"/o QZ

00 *-CM

O.llt'cO.SmmdPY. , 2.* 0.1 to 1cm 1 \gwvnQZ. 1

O.I'K^O.SmmdPY, I.* 0.1 to 2cm

^gwvnQZ,

O.IWO.SmmdPY, 1.160.1 to 5cm gwvnQZ,

0.11K0.5mmdPY,

0.5160.1mnKx <1mmdPY,

0.516 0.1 mm< x JlmmdPY. 3.16 0.1 to 2cm wvnQZ,

Struct.

Struc

sfoii

sfoH

sfoii

<tca

62

67

75

Assay

From (m)

47.0

48.5

52.8

54.0

55.5

57.0

58.5

To (m)

485

49.8

54.0

55.5

57.0

58.5

60.0

Sam. #

330

331

332

333

334

335

336

Au ppb

ti

-5

-5

-5

-5

-5

-5

-5

Au

j ||

Page: 3 of 19

Diamond Drill Log Sheet

Project: Bristol

SjJJJJSSS Hole: BRSOO-03

tQ.

Q

;

61-

62--

~-

63--

64^

65-;

66 --

68-i

69^

70^

7, j

72 -{

73^

~

74-^

75 H

76 -i

77 -̂

78 ~i

79 J

Lithology

f

V

V

V

V

V

'"

V

V

V

' v

v

yv

^

'-

From (m)

52.8

67.0

77.5

To (m)

67.0

77.5

85.5

Lith code

1

i

i

lithology

mafic j\volcanics /

mafic volcanics

mafic volcanics

text. Comments

, very fine grained ( sO.Smm), Massive pillowedflow. ...Bleached, massive to pillowed. Very fine grained, light greyish-green, j almost argillaceous, but with subtle possible 1 pillow rims (chloritjzed) near 64.0m. Less than 1 1fe fine feldspar phenocryst locally visible, mainly from 60 to 65m, up to 2mm India.. Bleached by weak to moderate sericite and chlorite.Moderately foliated, with slaty cleavage locally developped. Quartz-calcitet;-epidote veinletsand stringers at various angles, mostly parallel to foliation. Pyrite is disseminated to wispy, alongFoliation planes. f

, very fine grained ^O.Smm), Massive pillowedflow. ...Massive to pillowed.transitional from upper unit, predominantly massive, medium-green, with trace of subtle chloriUzed pillow rims. Locally speckled by anhedral calcite, up to 2Qtli locally. Foliationweakly developped to nearly absent. Irregular tensional fractures infilled by chlorite common,2*)b. Quartz-calcite stnngers at various angles.2*.

/, very fine grained (*:0.5mm). Massive \ amygdaloidal flow. ...Very fine grained, light greyish-green to green, moderately foliated, weakly folded, sheared, with 1 to S1* amygdular-like features of quartz-calcite, up to 1cm, some of which probably resulted from the dislocation of veins. Locally weakly banded(various shades of grey to green), over 0.5 to 20cm intervals, due to bleaching by carbonate and silica, mainly in proximity to veins. |

Alteration

Chl

CvW

Ser

CVW

Silic

CM*

Epi

CMf

Hem

o*w

Carb

OW"

other

Accessory Win.

"XoPy

otOi-

o/o

Cpy

CNCO

"/oQz

ooT-CN

0 5^ 0 1mnK xi'elmmdPY, S.% \0.1to2cmwvnQZ. ;

0.5* -:0.5mm dPY, 2^ 0.1 0.5cm

2.0* tO.Smiti bPY, 0.116dCp,2.'X)0.1 to 2cm gwvnQZ,

1 .0* -:0.5mm wPY,O.HtwCp, 2.* 0.1 to 2cm gwvnQZ,

Struct.

Struc

sfoll

^ca

61

Assay

From (m)

76.0

77.5

78.6

To (m)

77.5

78.6

800

Sam. #

337

338

339

Au ppb

-5

7

-5

Au

i i^- S r

Page: 4 of 19

Diamond Drill Log Sheet

Project: Bristol

CagJgCO Ho|e . BRsoo-03

1Q. V Q

81--

~

82-:

83H-z

B4-.

85 H

86^

87^

88-^

89 H.Z

90-

191^

92-

93-

-i

94^.

i

96^

--

98-

-QQ

Lithology

^

r^'-

v

^

v

V

v

v

-V

**'

^

v

v

^

V

V

From (m)

77.5

85.5

92.0

92.9

To (m)

85.5

92.0

92.9

1000

Lith code

i

1

10c

1

lithology

\volcanics X

mafic volcanics

quartZ'tourm; line vein

mafic volcanics

text. Comments

. verv fine arained (VO.Smm). Massivel amygdaloidal flow. ...Very fine | grained, light greyish-green to green, moderately

foliated, weakly folded, sheared, with 1 to 516amygdular-llke features of quartz-catcite, up to

1 1cm, some of which probably resulted from thedislocation of veins. Locally weakly banded (various shades of grey to green), over 0.5 to 20cm intervals, due to bleaching by carbonate and silica, mainly in proximity to veins.

, very fine grained ^0 5mm), Massive flow. ...Moderate to stronglyfoliated, bleached to light greyish-green,speckled by over 5016 anhedral calcite and dolomite (doesn't stain) locally, ^-1mm in dia. A trace of lapilli-size ghostly grey pseudoclasts(?), preferentially altered, probably resulted fromdeformation; Others probably represent shearedquartz-calcite stringers. Pyrite is disseminated towispy, very fine, 0.5*.

/...Massive bull-white to greyish and \

tourmaline. Vein has irregular margins, oriented at about 50 degrees tea. Wallrock slivers are

' sulphides noted. 1

, very fine grained ^O.Smm), Amygdaloidalpillowed flow. ...Yellowish-green.bleached, amygdu!ar(7), similar to interval from 85.5 to 92.0m. Unit is bleached by weak tomoderate carbonate, sericite, and silicaalteration, pervasive to patchy. Foliation Ismoderate. Possible quartz-carbonate amygdulesup to 0.5cm are observed near 98.0m. Locally brecciated, possibly as a result of deformation, or may represent remnant primary texture. Possible pillow rims locally observed.Semi-translucent quartzW-calcite stringers arepresent, 2*, at various angles, but mostly parallelto the foliation, dislocated. Trace of finedisseminated biotite(?) locally (ie. 98.7m). Pyrite occurs as very disseminations, to euhedralcubes up to 2mm. trace to 1 * locally, Q.5%overall.

Alteration

Chl

csw

Ser

C*W"

Silic

CM*

Epi

OW"

Hem

ow

Carb

CM*

other

Accessory Win.

"/o Py

01OT-

o/o

Cpy

CNJCO

"/oQz

ooT-r\i1.0*t0.5mmwPY.

i 0.1 16 wCp, 2.* 0.1 . \to 2cm flwvnQZ, 1

0.5%-eO.lmmwPY, wCp, 2.* 0.1 to 2cm gwvnQZ,

100.16 90cm wvnQZ,

0.516 cO.Smm dPY. 0.116 dCp, 2.* 0.1 to 2cm gwvnQZ,

Struct.

Struc

sfon

sfon

sfoM

< tea

72

69

63

Assay

From (m)

80.0

81.5

83.0

84.5

85.5

87.0

88.3

89.5

92.0

92.9

940

95.5

97.0

98.5

To (m)

81.5

83.0

84.5

85.5

87.0

88.3

89.5

91.0

92.9

94.0

95.5

97.0

98.5

100.0

Sam. #

340

341

342

343

344

345

346

347

348

349

350

351

352

353

354

Au ppb

-5

8

-5

9

9

-5

-5

10

7

6

8

9

7

9

-5

Au

' &1- S r-

Page: 5 of 19

Diamond Drill Log Sheet

Project: Bristol

Cara^ Hole: BRSOO-03

iQ.

Q

:

E101-

102-1

1103-

-5

104-^

105 -i

106-

r

107 -.

108-

109^

110^-

111 -^

112-]

-

113-^

114-^

115-r

i116 -

-.

117-!

118-;

119 r

Lithology

K

i

'l

vv " V

v.

v

V

v

v

v

v

v

v

v

v

v

'~

N'

V

From (m)

100.0

107.7

109.5

110.2

To (m)

107.7

109.5

110.2

127.0

Lith code

1

i

i

i

lithology

volcanics

mafic volcanics

mafic volcanics

mafic volcanics

text. Comments

. very fine grained (O.Smm), Massiveflow. ...Possibly a mafic dyke.Upper contact sharp at 68 degrees tea , weakly chilled over 1m, grey, bleached. Lower apparentcontact shows increase to moderate foliation over 20cm, at 43 degrees tea. Overall fairlyhomogenous, greyish-green, speckled by anhedral carbonate (calcite), up to 2516 locally, generally ^ mm. Non to weakly foliated.

/, very fine grained ^0 5mm), Massive \/flow. ...Bleached, medium 1greyish-green, similar to previous unit, possibly \ a dyke, but possible upper contact defined bysudden increase in foliation and bleaching near 100.7m, at 30 degrees tea. Generally finegrained, but variably speckled by anhedral carbonate (calcite) up to 2mm, over 50* locally, mainly within intervals of strongest foliation. Foliation varies from weak to moderate,accompanied by local weak brecciation where

i fragments are hlghlighed by selective bleaching \ (carbonate and epidote**saussurite). Overall, ;

Alteration

cm

CsW"

i ^interval probably represents altered margin to f j I nuartz vein, located below. 1 1

, very fine grained ^O.Smm), Massive fll flow. ...Same host rock between, 107.7 lto 1 08.5m. but light green, bleached by Irregularbull-white quartz veining, with black amorphous tourmaline along fractures (including biotite?) and calcite along the margins. Trace of'disseminated pyrite is contained within the veins]

, very fine grained ^O.Smm), Massiveflow. ..As previously describedabove, between 107.7 and 109.5. Massive,medium-green, mostly fine-grained, locally weakly foliated. Quartz-calcite4Y-epidote-iV-chlorite veining, 1-2*16, at all angles, barren. From 1 23.8 to 1 24.2m,1516 quartz-epidote-calcite-anhydrite(?) veiningand quartz-calcite-tourmaline veining, at allangles, with trace of fine disseminated pyrite.

Ser

OW

Silic Epi

CM*

Hem

CM*

Carb

CM*;

other

Accessory Min.

"/o Py

o

Cpy

CSKO

"/o QZ

ooT-CS

0.116^.5mmdPY,0.5160.1toO.Scm wvnQZ,

0.1*-:0.5mmdPY, 0.1 16 0.1 to 0.5cm gwvnQZ,

0.116 cO.SmmdPY, SO.,% 1 to 6cm wvnQZ

0.1*t0.5mmdPY, 2.* 0.1 to 1cm gwvnQZ,

Struct.

Struc

cont

sfoM

cont

sfoM

<tca

68

59

30

61

Assay

From (m)

100.0

108.0

109.5

110.2

To (m)

101.5

109.5

110.2

111.5

Sam. #

3S5

356

357

358

Au ppb

-5

-5

-5

-5

Au

, si- S *-

Page: 6 of 19

Diamond Drill Log Sheet

Project: Bristol

Cameco H0ie: BRSOO-OS

1Q. (DQ

Z

121 41

122 J

123^-E

124-E

^

125-^

126^

127

128-

-

129^

1304

131-^

132-^

J

133-

134 -E

135^

136^

M-^-

138 I

139-^

:

Lithology

x

^V

fV

V

v

s/

V

~Vv

V

"~'v

V

^

V

y

V

V

V

s,

"

s/

From (m)

110.2

127.0

To (m)

127.0

140.1

Lith code

i

i

lithology

mafic\volcanics 7

mafic volcanics

text. Comments

. very fine drained KO.Smm). Massive

Alteration

Chl

CM*

l flow." " ...As previously described l l above, between 107.7 and 109.5. Massive, l

medium-green, mostly fine-grained, locally ali weaklv foliated. II

Qjartz-calcitet;-epidote*;-chlorite veining, 1-2^,1 at all angles, barren. From 123.8 to 124.2m. 15* quartz-epidote-calcite-anhydrite(?) veining and quartz-calcite-tourmaline veining, at all jangles, with trace of fine disseminated pyrite. 1

, very fine grained (eO 5mm|, Massive pillowedflow. ...Transitional into a unitwhich is generally finer-grained, medium-green, with definite flow textures (le. patchy chilled and bleached textures), with poorly developed pillow rims and possible flow brecciation from 1 34 to 1 36m. Weakly feldspar glomeroporphyritic from 131 to 132.5m (116, up to 1cm in dia.). Weak brecciation and fracture Infilling by chlorite. Possible biotite in association with aquartz-calcite band near 137.1m.

Ser Silic

ow

Epi

(NW

Hem

f^W

Carb

C'W

other

Accessory Min.

"/o Py

0tfv*-

"/o

Cpy

CNCO

"XoQz

ooT-CN0 1 % <0 5mm dPY

1 2^*0.1 to 1cm \flwvnQZ, 1

D.5% *0.5mm wPY,

,

L'% 0.1 to 0.5cmgwvnQZ,

Struct.

Struc

sfoll

sfon

<tca

56

72

Assay

From (m)

123.0

123.8

124.2

125.0

1265

128.0

129.2

139.0

To(m)

1238

1242

1250

126.5

128.0

1292

130.5

140.1

Sam. #

359

360

361

362

363

364

365

366

Au ppb

-5

-5

-5

-5

-5

-5

-5

14

Au

j 8Jj- 8 i-

Page: 7 of 19

Diamond Drill Log Sheet

Project: Bristol

CanjeCO Hole: BRSOO-03

tQ.VQ

T

141^

142 -:-E

143^

144^

145-

~

146 -;—

147^

148 -:

149^

|150-^

i

151 ~-

~152-

J-

153-~

154H.z

155 -E

156 -;

157-

-

158-^

159H

Lithology

V

, v

s/

v

v

v

V

v

V

^

v

^2

IH-r :

-

n.Z Z

^-Z

^-Z~-

^..r

fi~^-T

^

-rr-rTi i-z~ ~

Jr-^

.^-r-^-z~^-z

:fl^J3

From (m)

140.1

140.8

146.0

148.4

150.5

To (m)

140. 1 140.8

146.0

148.4

150.5

1760

Lith code

1

i

n

n

lithology

mafic \volcanics /' .mafic \volcanics 1

mafic volcanics

mafic volcanics

volcanic schist

maficvolcanicschist

text. Comments

Alteration

cm

c-w-, very fine grained ^O.smm), Massive pillowed ~~ 1 . flow. ...Transitional into a unit 1 l

| which is generally finer-grained, medium-green, 1 J ' | with definite flow textures (ie. patchy chilled 1B and bleached textures), with poorly developed l [j pillow rims and possible flow brecciation from 1341

to 136m. Weakly feldspar glomeroporphyritic I from 131 to 132.5m (1*. up to 1cm in dia.). 1Weak brecciation and fracture Infilling by

mchlorite. Possible biolite in association with aIfauartz-calcite band near 137.1m. Hl, aphanitic ^0.1 mm) ...Magnetic flow ( margin. Upper contact transitional. Moderate tostrongly magnetic interval, dark grrey, weakly foliated, with -silt, quartz-calcite amygdular-like features. Contains T-2% irregular (quartz -calcite stringers and quartz -calcite-epidote stringers,at all angles, weakly disrupted. A similarmagnetic band also occurs between 139.6 tofi 39.7m.

t ...Gaboroic flow/dyke, medium-green. Upperl contact diffuse, moderately sheared, at 57

degrees tea. Very weakly to weakly foliated, but Iminor veins locally showweak folding. l iduartz-calcite-epidote veinlets, l 1*, irregular, at j(various anales. 1, fine grained (*2mm). Massive flow. ...Foliated margin to gabbroic unit above.Transitional zone, medium-green, accompanied

\ by gradual change in foliation intensity from l \weak to strong going downhole. ;

, very fine grained (O.5mm) ...Tuffaceous mafic schist. Strongly altered anddeformed mafic rock. No defined contacts,

speckled by carbonate (dolomite-calcite), within a.chlorite-carbonate-sencrte groundmass, 1

\essentially a schist. Minor veining, sheared to JVoided. \

, aphanitic ^0.1mm), Tuffaceous....Iron-rich mafic tuffaceous sediment/ Alteredamgdular volcanic. Contact transitional,arbitrarily selected. Overall homogenous,medium greyish-green, with very subtle banding locally develloped. Appears weak to moderately foliated due to very-fine grain size, but slatycleavage well develloped locally; Rock isactually schistose (chlorite-sericite-carbonate schist, with very minor quartz(?) grains, le.160.5m). Quartz-calcite amygdular-like featuresare locally observed, and may representdislocated veinlets, as some of the stringers doindicate boudinage and partial dislocations. Very fine disseminated magnetite (ie. 156m) and tourmaline (ie. 1 75m) is noted within the matrix.Quartz-calcite veinlets(SK), and trace of greyishquartz veinlets, at ali angles, mainly parallel tofoliation, sheared, folded, disrupted, containoccasional tourmaline and pyrite trace. Pyrite is fine disseminated to locally wispy, trace to Q.5%.

Ser

C\W

Silic

OW"

j

Epi

CM*

Hem

CvW

Carb

rvt

other

Accessory Min.

0XoPy

0

Cpy j0/0 Qz

CNCOopt-OI

J.% 0.1 to 0.5cm 1

0.1**0.5mmdPY,

0.1*-:0.5mmdPY, 2.* 0.1 to 1cmgwvnQZ,

0.5* TO.Smm dPY,5.* 0.1 to 3cmwvnQZ,

Struct.

Struc

-sfoH-

sfon

sfon

< tea

68

59

65

Assay

From (m)

139.0 140.1

140.8

147.0

148.4

1490

155.5

157.0

158.5

To (m)

140.1 140.8

142.0

148.4

149.0

150.4

157.0

158.5

160.0

Sam. #

-388

367

368

369

370

371

372

373

374

Au ppb

h* -5

-5

-5

-5

-5

-5

7

-5

Au

, S|- S r-

Page: 8 of 19

Diamond Drill Log Sheet

Project: Bristol

Cameco H0ie: BRSOO-OS"E,tQ. D O

r--

161-

162 -E

163-1

1644

1654--

166-

2

1674

168^

169^

170^

171 4

172 4

173^

1744

1754

176-

177 -E^

178 4

1794---

Lithology

-z-r~r~r

n-z:

fi^-Z~^

TL-:

J^^

-U

zf Z-JT-ZT

^-

^

O

i^3

O

li

^E

li

i1

vv

^-

""^

v

^

From (m)

150.5

176.0

To (m)

J 76.0

187.0

Lith code

i*

i

lithology

mafic\ volcanic 1Whist 1

mafic volcanics

text. Comments

, aphanitic ^0.1mm), Tuffaceous.

Alteration

Chl

c*r

...Iron-rich mafic tuffaceous sediment/Altered lamgdular volcanic. Contact transitional, larbitrarily selected. Overall homogenous, lmedium greyish-green, with very subtle banding j locally developed. Appears weak to moderately ] foliated due to very-fine grain size, but slaty cleavage well develloped locally; Rock isactually schistose (chlorite-sericite-carbonate schist, with very minor quartz(?) grains, ie. 160.5m). Quartz-calcite amygduTar-like featuresare locally observed, and may representdislocated veinlets, as some of the stringers doindicate boudinage and partial dislocations. Veryfine disseminated magnetite (ie. 1 56m) and tourmaline (ie. 1 75m) is noted within the matrix.Quartz-calcrte veinlets(5")fc), and trace of greyish quartz veinlets, at all angles, mainly parallel tofoliation, sheared, folded, disrupted, contain[occasional tourmaline and pyrite trace. Pyrite isline disseminated to locally wispy, trace to 0.5%-i

, very fine grained ( cO.Smm), Massive pillowed flow. ...Massive to pillowed.Arbitrary contact, very gradual transition into a fine-grained massive mafic volcanic flow, lightto medium green, with similar alteration asabove, perhaps less chloritic, and weakly foliated. Eptdotked pillow rims, with crackled fracturing and chlontJc pillow interstices, and hyaloclastite textures observed between 1 85 to187m. Quartz-calcite veinlets are very irregular, disrupted, and ^'X, greyish andtranslucent quartz veins are also noted. Pyriteoccurs as disseminations and occasional wisps.

Ser

CM*

Silic

CM*

Epi

CVW

Hem Carb

C\W

other

Accessory Win.

"/oPy

0

0Xo

Cpy

rvKO

'/oQz

00*-CH

D.5% O.Smm dPY,vS.%0.1 to 3cm\wvnQZ. 1

:1mmdPY, 3* 0.1 to4cmwvnQZ,

Struct.

St rue

sfon

< tea

64

Assay

From (m)

164.0

165.5

179.0

To (m)

165.5

167.0

Sam.#

375

376

377

Au ppb

5

-5

-5

Au

i li

Page: 9 of 19

Diamond Drill Log Sheet

Project: Bristol

^2J2S2 Hole: BRSOO-03

tIDQ

:

181-:

182-^

183-:

184-

185-1^

186^

187-

188 -?^

189-;1!

190H

191 -~

192^

193-2-

194 -E

195 J

196^-

197-i-

198^

199 J

Lithology

f

~"~v

V

V

V

v

v

s/

^v

v

\s

\f

s

V

s/

V

From (m)

176.0

187.0

191.0

To (m)

487.0

191.0

2160

Lith code

i

1

i

lithology

mafic\volcanics X

mafic volcanics

mafic volcanics

text. Comments

, very fine grained (-:0.5mm), Massive pillowednow. ...Massive to pillowed.Arbitrary contact, very gradual transition into a fine-grained massive mafic volcanic flow, light

Alteration

Chl

C*W"

:o medium green, with similar alteration as labove, perhaps less chloritic, and weakly foliated. Epidotized pillow rims, with crackledtacturing and chloritic pillow interstices, and hyaloclastite textures observed between 1 85 to187m Quartz-calcite veinlets are very irregular, disrupted, and ^*to greyish andtranslucent quartz veins are also noted. Pyrite Dccurs as disseminations and occasional wisps, f

fine grained ^2mm), Massive flow...Transitional with upper unit. Relatively

coarse-grained, gabbroic, medium-green, with fine disseminated white leucoxene, and speckledby anhedral carbonate.

aphanitic ^0.1mm), Amygdaloidal pillowedlow. ..Altered, greenish-grey,argillaceous texture locally, but overall quitelomogenous and with no apparent beds. ^ossiDle very fine amygdules locally observed, along with a trace of subtle chloritic possible )illow servages. Moderately foliated, with poorly developed slaty cleavage in places. Weakly cherty near 203.9m. White quartz-calcitestringers and veinlets and greyish quartz-calcite veining are both found, stretched to weakly folded and boudinaged. Weak bleaching (carb.) along margins to some of the veins. Trace ofourmaline occurs within the groundmass, oftennear veinlets. Pyrite occurs as finedisseminations within the veins, or as occasionalwisps within the groundmass. Chalcopyrite traceoccurs within the quartz-calcite veinlets'ie.208m). Pyrrhotite occurs as wisps and blebs,trace.

Ser

c^

Silic

CNM-

Epi

O^t"

Hem

CNW

Carb

o*w

other

Accessory Min.

"/o Py

olOi-

"/o

Cpy

O-JCO

KQz

ooT-CMO.lltO.lmmcx

\t1mmdPY, a.% 1\0.1 to 4cm wvnQZ, 1

0.5'*0.1mnKx OmmdPY, D.5% 0.1 to 2cm wvnQZ,

0.5**0.5mmwPY,0.1*vnCp, S.%0.1 to 5cm gwvnQZ, O.IWbPO,

Struct.

St rue

sfon

sfon

c tea

72

55

Assay

From (m)

1800

181.5

183.0

184.5

194.0

1955

To (m)

181.5

183.0

184.5

186.0

195.5

197.0

Sam. #

378

379

380

381

382

383

Au ppb

-5

-5

6

-5

-5

-5

Au

i 8J:- in T-

Paqe: 10 of 19

Diamond Drill Log Sheet

Project: Bristol

CgragCO Hole: BRSOO-03

tQ. (UQ

:

201^

202 -k

203 -l

204^-

J

j

206 -1

207 -E

208 -:--

209 ̂

210 -;

211 -i

H;

212 -:i

214^

215-{

216-

217^

218-

219-i

Lithology

v

^

^V

"V

'-

V

v

v

v

v

^~

^

-:-

v^

From (m)

191.0

2160

218.0

To (m)

216.0

2180

226.8

Lith code

i

i

i

lithology

mafic \volcanics '

mafic volcanics

mafic volcanics

text. Comments

Alteration

Chl

CNW*

, aphanitic (*0.1mm), Amygdaloidal pillowed flow. ...Altered, greenish-grey,argillaceous texture locally, but overall quite homogenous and with no apparent beds. 1 Possible very fine amygdules locally observed, lalong with a trace of subtle chloritic possible \ pillow selvages. Moderately foliated, with poorly developed slaty cleavage in places. Weakly cherty near 203.9m. White quartz-calcitestringers and veinlets and greyish quartz-calcite veining are both found, stretched to weaktyfolded and boudinaged. Weak bleaching (carb.) along margins to some of the veins. Trace oftourmaline occurs within the groundmass, often jnear veinlets. Pyrite occurs as finedisseminations within the veins, or as occasionalwisps within the groundmass. Chalcopyrite traca 'occurs within the quartz-calcite veinletsvie.208m). Pyrrhotite occurs as wisps and blebs J

, aphanitic (O.1 mm), Amygdaloidal pillowed flow. ..Altered fault zone. Same as previous unit, medium greenish-grey, but core is blocky, and includes a gouged zone between 217.6 to 217.7m.

/, aphanitic ^0.1 mm), Massive pillowed \ flow. ...Altered, greenish-grey, as \previously described above, overall argillaceous, homogenous, with possible remnant pillowselvages (chloritic). Locally speckled by fine carbonate. Moderately foliated, sheared, nearly gouged along discrete planes often accompanied by sheared quartz quartz-caldte-chlorite-sericite veinlets (ie 223m).

Ser

c^w

Sific

ow

Epi

ow

Hem

C\W

Carb

0*f

other

Accessory Min.

"XoPy

oIOT1

Cpy

CNOO

'/oQz

ooT-TM

D.5% ^.5mm wPY, 0.1'*vnCp,5.'*0.1

\to 5cm gwvnQZ, l W.I'itbPO. 1

O.II^O.ImmdPY,5.*0.1to5cmgwvnQZ, 0.1 li bPO,

0.1%<0.1mmdPY, 3.*0.1to1cm

0.1%'cO.lmmdPY, 3*0.1 to 1cm gwvnQZ,

Struct.

Struc

sfon

sfoM

< tea

64

56

Assay

From (m)

205.0

206.5

208.0

209.5

211.0

212.0

To (m)

206.5

208.0

209.5

211.0

2120

213.5

Sam. #

384

385

386

387

388

389

Au ppb

-5

-5

-5

-5

-5

7

Au

e |t-

Page: 11 of 19

Diamond Drill Log Sheet

Project: Bristol

O-SiS^ Hole: BRSOO-03

"E"

1Q

^-E

221 -E

222^:

223 -E

224 H

225-;-E

226^

227-

228-~

229 -E.r:

230 -.-E

231 -E

232-

\

233^

234 -E

235 J

236-;--

237 -i

1238^

239 -E

1

Lithology

/~

f

f

s

V

V

" v

v

~V' V

V' v

v

V

V

v

V

v*

V

V

v

v

fv'-

From (m)

218.0

226.8

To (m)

226.8

242.5

Lith code

i

i

lithology

maficvvolcanics j

mafic volcanics

text. Comments

, aphanitic (0. 1mm), Massive pillowedflow. ..Altered, greenish-grey, as previously described above, overall argillaceous.homogenous, with possible remnant pillow

i selvages (chloritic). Locally speckled by fine carbonate. Moderately foliated, sheared, nearly gouged along discrete planes often accompanied by sheared quartzIquanz-calcite-chlorite-sericite velnlets tie. 223m),

, very fine grained (O.5mm) ...Graphitic and Brecciated Mafic volcanic andSediments/Grey Alteration Zone. Interval is medium to dark grey, and appears to consist of a mixed zone of sheared mane volcanic,argillites, and minor greywackes. Shearing ismoderate to strong, with angular brecciation ofthe host rock (lapiTli-size fragments)'due to strong deformation. The pseudoclasts are yellowish green and preferentially sericrtized, to lighter grey and preferentially carbonatized. The matrix is strongly carbonation, mainly comprised of graphite and calcite. Weak pervasive silicification is observed locally. Core is moderately blocky, locally gouged. Weak folding, with fold closure observed near 238.6m.White quartz-calcite stringers and bands, and greyish quartz-dolomite/ankeritef?) stringers are observed, 316, sheared, disrupted, locally weakly folded. Pyrite, 1-316, occurs mainly as wisps, seams, and minor stringers, mostly parallel to theschistossity. Pyrrhotite D.5%, as wisps andoccasional bands (ie. 240.5m).

Alteration

cm

CM*

,

1

Ser

CNW"

"1

1

Silic

CM*

j

Epi

eg*

Hem

CM*

Carb

CM*

1

other

Accessory Min.

"/o Py

UO?

"/o

Cpy

CMCO

"/oQz

oc0.1%'tO.lmmdPY,

iS.% 0.1 to 1cm . \flWvnQZ. f

'0.53K0.1nvn s wPY, S.% 0.1 to 2cm gwvnQZ, Q.5%

xbaPO.

2.0* ^.1 mm wPY, 3.16 0.1 to 2cm gwvnQZ, 0 516 baPO,

Struct.

Struc

shr

sfoHshr

shux

fault

shr

shr

< tea

45

5620

59

58

25

Assay

From (m)

225.5

226.8

227.7

229.0

2305

2320

233.5

235.0

236.0

2370

238.5

To (m)

226.8

227.7

229.0

2305

2320

233.5

235.0

236.0

237.0

2385

240.0

Sam. #

390

391

392

393

394

395

396

397

398

399

400

Au ppb

-s

6

8

6

-5

•5

6

-5

9

13

13

Au

, ||- S T-

Page: 12 of 19

Diamond Drill Log Sheet

Project: Bristol

Q-imeCO Hole: BRSOO-03

f

lo

I2

241^-~

242-

243^

244^-

245 -E-~

246-:

247J

248 -^-z

249 "j

250 ~ E

251 -S

252 -E-

253 -l

254

255-^

256 -jJ

E257 ~-

^

258^

259 1

1

Lithology

x v

sv

'~

^-v

sv

v

v^

v

s**

v

sV

sv

V

v

V

v

v

^

V

v

V

V1

V

V

V

x/

v'

From (m)

226.8,

2425

2500

To (m)

242.5

250.0

2730

Lith code

i

i

i

lithology

maficVolcanics t

mafic volcanics

mafic volcanics

text. Comments

, very fine grained (*0.5mm)...Graphitic and Brecciated Mafic volcanic andSediments/Grey Alteration Zone. Interval Is medium to dark grey, and appears to consist of la mixed zone of sheared mafic volcanic, 1argillites, and minor greywackes. Shearing is fmoderate to strong, with angular brecciation of the host rock (lapilli-size fragments)' due to strong deformation. The pseudoclasts are L yellowish green and preferentially sensitized, to fighter grey and preferentially carbonatized. The matrix Is strongly carbonation, mainlycomprised of graphite and calcite. Weakwrvasive silicification is observed locally. Cores moderately blocky, locally gouged. Weakbiding, with fold closure observed near 238.6m.White quartz-calcite stringers and bands, and greyish quartz-dolomite/ankeriteffl stringers areobserved, 3*, sheared, disrupted, locally weaklyFolded. Pyrite, 1-3*, occurs mainly as wisps,seams, and minor stringers, mostly parallel to theschistosity. Pyrrhotite 0.5*, as wisps and occasional bands (le. 240.5m)., aphanitic MJ.1 mm). Massive flow....Moderately sheared mafic volcanic,medium-green, with local weak brecciation asobserved above still visible, with minor angularpseudoclasts within a chloritic matrix. Finespecks of carbonate scattered throughout (calcite),fine leucoxene, and disseminated magnetitelocally. White quartz-calcite stringers andgreyish quartz stringers also present, sheared todislocated, at all angles, perhaps 1 -2*. Pyrrhotite as fine wisps and seams, parallel to the shistossity, 0.5*. Trace of disseminated.brownish sphalerite (le. 249.1 m).

, very fine grained (^O.Srnrn), Variolitic pillowedflow. ...Massive to pillowed,medium-green. Transitional from previous unitabove. Relatively more homogenous, with subtlepossible pillow rims (chloritic), and bleached (epidote) patches accompanied by hyaloclastitetextures (le. 259.1 m). Trace of fine varioles(?) near 255.1 m. Trace of narrow brownish bands* 1 cm wide, appear to contain very finedisseminated biotite and magnetite from 258 to 266m (ie.260.5m, 261m),; The brownish bands are centered on chloritic bands (pillow rims?), and are followed on the outer margins by carbonate. Epidotized bands (up to 10cm) withwispy fracture filling pyrrhotite occur near 255.3 and 259.3m, in association with greyish quartzstringers and veinlets. Trace of chalcopyritewithin the veins (ie.258m), or in assoc. wrth postringers. Overall, 0.5* pyrrhotite, 3* locally.Fine leucoxene locally visible. Rock appearsweakly foliated but is locally sheared/brecciated,fracture infilling by chlorite, and boudinaged to stretched veins of quartz-calcrte-epidote

Alteration

Chl

CsW

-1

Ser

C*W

Silic

CXW

Epi

ow

Hem

CvM-

Carb

ow

other

Accessory Min.

"/o Py

o

"/o

Cpy

CMPO

"/o QZ

ooT-CN

2.0* eO.lmm, wPY, 3.* 0.1 to\2crngwvnOZ, 0.5* ;

3.* 0.1 to 2cm gwvnQZ, 0.5* baPO

01* ^ 1mmwPY, 1 .* 0.1 to 1cm gwvnQZ, 05*fPO, trace* dSP,

0.1*t0.1mmwPY, 0.1*vnCp,2.*0.1 to 7cm gwvnQZ, 05* fpo,

Struct.

Struc

shux

shux

-sfoM-

ctca

45

57

70

Assay

From (m)

240.0

241.5

242.5

244.0

2455

247.0

2485

250.0

251.5

253.0

254.5

2560

257.5

2590

259.5

To (m)

241.5

242.5

244.0

245.5

2470

248.5

250.0

251.5

2530

2545

256.0

257.5

259.0

2595

261.0

Sam. #

401

402

403

404

405

406

407

408

409

410

411

412

413

414

415

Au ppb

5

-5

-5

8

6

-5

-5

-5

8

-5

-5

-5

-5

-5

20

Au

, SJ:- S *-

Paqe: 13 of 19

Diamond Drill Log Sheet

Project: Bristol

SlSSSS Hole: BRSOO-03

gtQ. VQ

:,ir

261-

262 -.-.

263-

-

264^-

265-^

266-

267 -i^

268-

269 :r

270--

271 --

272-

273 --

274 -..

275-5

277-

278^;^

279^

z

Lithology

V

'-

v

v

v

v

v

v

V

v

v

V

N*-

V

V

yv

V

V.

'-

V'-

v

NX

From (m)

2500

2730

2762

279.4

To (m)

273.0

275.9

279.4

280.0

Lith code

i

i

5ae

1

Saba

lithology

mafic .volcanics 7

mafic volcanics

mafic volcanics

greywacke

text. Comments

, very fine grained ^0 5mm), Variolitic pillowedflow. ...Massive to pillowed,medium-green. Transitional from previous unitabove. Relatively more homogenous, with subtlepossible pillow rims (chloritic), and bleached (epidote) patches accompanied by hyaloclastite textures (ie. 259.1m). Trace of fine variolesf?)

Alteration

Chl

c^W"

j near 255.1 m. Trace of narrow brownish bands [l^cm wide, appear to contain very fine

l disseminated biotite and magnetite from 258 to II266m (ie.260.5m, 261 m),; The brownish bands are centered on chloritic bands (pillow rims?).and are followed on the outer margins bycarbonate. Epidotized bands (up to 10cm) withwispy fracture filling pyrrhotite occur near 255.3and 259.3m, in association with greyish quartzstringers and veinlets. Trace of chalcopyrite within the veins (ie.258m), or in assoc. with postringers. Overall, 0.516 pyrrhotite, 316 locallyFine leucoxene locally visible. Rock appearsweakly foliated but is locally sheared/brecciated,fracture infilling by chlorite, and boudinaged to {stretched veins of quartz-calcite-epidote. l

, aphanitic K0.1 mm) ...WeaklyGraphitic. Same as previously described above,medium greyish-green, weak to moderatelyfoliated, with local brecciation, but generally more greyish due to weak pervasive graphite, and disseminations of very fine magnetite. White

j to greyish quartz-calcite stringers and bands, at j lall angles, sheared. Pyrrhotite-chalcopyriteseams, 0.516, and trace pyrite. Notably, first

l occurence of 2X10mm arsenopyrite seams is j noted along margin to a vein near 275.2.

...Graphite/Graphitic Argillite. Strongly sheared.black to dark grey, schistose, strongly fractured to ground. Wispy pyrrhotite, 216.

j , aphanitic (eo 1 mm) ...Sheared l volcanic, dark greenish-grey, moderate to weakly graphitic going downhole. Similar to Interval

| above the previous graphite horizon. Moderate | 1 sheared, brecciated, with oseudoclasts 1

preferentially carbonatized (grey, calcitic). 1 Pyrrhotite stringers, seams and wisps, often l associated with very fine chalcopyrite and minor pyrite. Overall, 216 pyrrhotite, D.5% pyrite and trace chalcopyrite. No arsenopyrite noted. White to grey quartz-calcite stringers and veinlets,sheared, 216.j, vary fine grained ^O.Smm) ...Upper contact sharp at 73 degrees tea. Fine quartz-greywacke, dark grey, with approx. 5016

j fragments, strongly stretched, lapilli-size,f mostly black and argillaceous, others greyish

u and probably derived from carbonatized mafic volcanic. Strongly magnetic, due to presence of

316 pyrrhotite(?-relatively light colored), and ^possibly very fine disseminated magnetite!?). | !

Ser

c*w~

Silic

CNW

Epi

C^t1

Hem

c-w

Carb

CNW

li

other

Accessory Min.

"/o Py

o

Cpy

CMCO

"/o QZ

ooT-C\

0.116 O.lmmwPY,0.1 ttvnCp, 2.16 0.1

\to 7cm gwvnQZ, j(0.516 fDO. ;

,

0.116 cO.lmmwPY, 0.116 wCp, 2.16 0.1 to 1cm gwvnQZ, 0.516 tpo, trace* fAS,

1 .tt 0.1 to 0.3cm xxflwvnQZ. 2.16fDO. y

0.1 16 wCp, 2. 16 0.1 to 1cm gwvnQZ, 2.16 fpo.

316fPO,

Struct.

Struc

sfoM

shr

shux

shux

e tea

74

66

71

60

70

73

Assay

From (m)

259.5

261.0

262.5

2640

265.5

267.0

268.5

2700

271.5

273.0

274.5

275.9

276.2

277.5

278.5

2794

To (m)

261.0

262.5

264.0

265.5

267.0

268.5

270.0

271.5

273,0

2745

275.9

277.5

278.5

279.4

280.0

Sam. #

415

416

417

418

419

420

421

422

423

424

425

427

428

429

430

Au ppb

20

-5

-5

20

34

-5

-5

-5

-5

-5

7

46

19

12

12

19

Au

, a|- S T-

Page: 14 of 19

Diamond Drill Log Sheet

Project: Bristol

Carc*E2 Hole: BRSOO-03

Depth (m)

281 -j

282 -E

283 -9

284^-

285 -;

286^

z

287^

288-

289^

290^

291^

292-

293^

294 -r

295 4

296-:

297 -i

298-^

293^

Lithology

-r

yv

VX

\f

V

\s

*s

•*f

V

V

V

s/

V

V

v

V

V

From (m)

2800

283.5

284.5

2865

Oft7 7

288.0

To (m)

283.5

284.5

286.5

287.7

288.0

301.4

Lith code

Sae

Saba

Sae

1

Sae

1

lithology

argillite

greywacke

argillite

mafic volcanics

argillite

mafic volcanics

text. Comments

, aphanitic ^0.1 mm) ...Graphitic argillite, black, fairly homogenous, with subtle banding. Strongly graphitic, strongly sheared, weak to moderately fractured. Contains 1 -2"*, greyish quartz-calcite stringers and veinlets, boudinaged. Pyrite, 2-316, occurs as nodules up to 1 ,25cm within the matrix and also within the greyish veinlets. tt also occurs as fine wisps to large euhedral crystals (recrystallized), up to 0.5cm. Interval does not appear to be magnetic, and pyrrhotite was not observed., very fine grained ^O.Smm) ...Quartz wacke, medium to dark grey. Well sorted, with perhaps 5016 dark grey quartz grains, contained within a carbonatious matrix (calcite, graphite). Sorting indicates fining downhole. Minor black graphitic fragments are present, strongly stretched. Pyrite occurs mainly as fine disseminations, but also as minor blebs j land wisps. Overall 3* pyrite. Non-magnetic, l.aphanitic ^0.1 mm) ...Graphitic argillite, black to dark grey. As previously described from 280 to 284m. Includes a 20cm wide wacke bed from 285.9 to 286.1 m, interbedded with narrow argillite laminations. Apparent bedding parallel to schistosity and slaty cleavage at 74 degrees tea. Nodular to j blebby pyrite, and pyrite wisps and euhedral recrystalrized cubes up to 1 1 cm occurs both Within the veins and within the host rock. 3-416. 1, very fine grained (td. 5mm) ...Altered, medium grey volcanic. Strongly 1

l sheared mafic volcanic, brecciated, with J lapilli-size pseudoclasts. Speckled by fine carbonate, possibly dolomite, anhedral to wispy, pard grey graphitic bands and stringers locally. Pyrrhotite stringers, wisps, and blebs, mostly

^parallel to schistosity, 3-4* locally, 216. Pyritel St, wispy to stringers. 1.aphanitic (O.1 mm) ...Graphitic argillite, black to dark grey. Strongly sheared, brecciated, with pseudoclasts possibly derived from rip-apart sea. beds or mafic Inclusions. (Contains 216 nodular to wispy pyrrhotite, and p.5% wispy to disseminated pyrite. Arsenopyrite seams arid blebs, within the matrix, crystalline up to 1mm in dia.,0.25% overall. l, very fine grained (^0 5mm), Variolitic pillowed flow. ..Altered pillowed and variolitic volcanic. Medium greyish-green, weak to moderately sheared, weakly brecciated locally. Incipient varioles, 1-2mm, and trace of quartz-carbonate amydules (le. 298.1m) are best developped from 296 to 299 m. Poorly defined chloritic pillow rims are observed locally. Quartz-caicite (and trace ankerite?) stringers and veins, 0.1 to 3cm wide, at all angles, generally sheared, are locally associated with greyish quartz. Pyrite wisps, seams and stringers, within the host rock and locally within the veins, 1 16 locally, 0.516 overall. Pyrrhotite stringers and wisps, 0.2516. Rock is moderately magnetic locally, and probably contains very fine magnetite (ie. 290.4m).

Alteration

Chl

C*f

t

j

Ser

ow

Silic

CM*

Epi

c~w

Hem

c~w

Carb

CNW

r

other

Accessory Min.

07oPy

IOr-

r

0Xo

Cpy

C\KO

"/oQz

ooT-C\|

3.016 *0.5mn bPY, 2.* 0.1 to 1cm gwvnQZ,

3.0* cO.Smm dPY, 1.* 0.1 to 0.2cm gwvnQZ,

3.016 O.Smm bPY, 2.* 0.1 to 2cm gwvnQZ,

1 .0* -:0.5mm wPY, 1.161cm awviiOZ, 2.^ bPO. 0.516 *:0.5mm ^^" wPY, 1.160.1cm

\gwvnQZ, 2.16 bpo, l 10.216 fas. 1

O.SttcO.lmin wPY, 3.16 0.1 to 3cm gwvnQZ. 0.216 fpo.

1.016 co. 1mm stPY, 3.16 0.1 to 3cm gwvnQZ. 0.216 fpo.

Struct.

Struc

cont

shux

sfoh

shux

shux

sfol1

shux

< tea

72

72

66

74

71

75

80

Assay

From (m)

280.0

281.0

282.0

283.5

284.5

285.5

286.5

288.0

289.0

290.0

291.0

292.0

293.5

295.0

296.5

297.5

298.5

299.5

To (m)

281.0

282.0

283.5

284.5

2855

286.5

287.7

288.0

289.0

290.0

291 0

292.0

293.5

295.0

296.5

297.5

298.5

299.5

300.5

Sam. #

431

432

433

434

435

436

437

438

439

440

441

442

443

444

445

446

447

446

449

Au ppb

ci

85

96

49

11

31

19

-5

12

-5

-5

-5

5

-5

7

-5

-5

-5

-5

-5

Au

i li

Page: 15 of 19

Diamond Drill Log Sheet

Project: Bristol

Casino Hole: BRSOO-03

Depth (m)

301 -]

302-

303-^

304-

305-

306-

307^

308--

-

309-

Lithology

V

V

V

v

V

V

V

-(--1

From (m)

288.0

301.4

302.3

303.5

304.6

307.3

TO

(m)

-301.4

302.3

303.5

304.6

307.3

317.0

Lith code

1

1

5ae

1

5ae

5

lithology

mafic\volcanics X

mafic volcanics

argillite

mafic volcanics

argillite

sediment

text. Comments

, very fine grained (sO 5mm), Variolitic pillowed flow. ...Altered pillowed and variolitic volcanic. Medium greyish-green, weak to moderately sheared, weakly brecciated locally. Imt varioles, 1-2mm, and trace of

:-carbonate amydules (ie. 298.1 m) are best ipped from 296to 299 m. Poorly defined ic pillow rims are observed locally, -calcite (and trace ankerite?) stringers and 0.1 to 3cm wide, at all angles, generally id, are locally associated with greyish . Pyrite wisps, seams and stringers, within st rock and locally within the veins, i V* . Q.5% overall. Pyrrhotite stringers and Q.25%. Rock is moderately magnetic

, and probably contains very fine magnetite 0.4m)fine grained (*0.5mm) iralized mafic volcanic, medium green. As , moderately sheared, brecciated (healed orite and graphite) with 7"* white to h white quartz-calcite veining, irregular, , 3cm, sheared to folded. Pyrite wisps, ; and stringers, both within the host rock ithin the veins, 1-316. Pyrrhotite trace, and ile trace arsenopyrite. 1nitic^O.lmm) Jhite/black graphitic aqrgillite. tially pure graphite, sheared to folded, speckled by fine carbonate (dolomite?),

'ly a highly graphitic mafic volcanic th. Slaty cleavage, locally crenulated. j ately fractured, to ground from 302.7 to

Includes a 6cm wide greyish-white -calcite veinlet near 303.3m, crackled, with rite seams infilling the fractures, and trace ish sphalerite. Overall, 1 tk disseminated W pyrite.nitic^O.lmm) ..Altered fie, medium greyish-green. As previously bed, weakly silicified, weakly sheared to ated. Dark greyish quartz-calcite )rs, sheared, boudinaged. Pyrite seams isps, along margins to the veins, and within st rock. l

, aphanitic ('0. 1mm) ...Graphite and altered mafic volcanic. Over 6Qtk graphite (black), with mafic volcanic intervals still recognizable, moderately graphitic (dark grey) as well. Sheared, folded, with weak brecciation, and local offsets (1cm) cross-cutting the main schistossity, along planes nearly subparallel tea. Moderately fractured, stongly fractured to gouged from 306.4 to 306.6m. White to greyish

; quartz-calcite veins and veinlets, sheared, with graphite infilling fractures. Pyrite wisps, seams and stringers, within the host rock and veins, 2* locally, 1* overall. Trace of sphalerite within a 6cm wide veinlet near 307.2m....Interbedded greywacke and siltstone. Predominantly quartz-greywacke beds, medium-grey, interbbed with narrow dark grey and graphitic siltstone beds (10"*); Apparent bedding varies from 2mm to 70cm thick, at 66 degrees tea, parallel to slaty cleavage. Greyish to white quartz-calcite stringers ana veinlets, sheared to boudinaged, 3*. Pyrite up to 1*.

Alteration

Chl

c\w

Ser

ow

Silic

CNN-

Epi

CM*

Hem

CNW-

Carb

C\W

other

Accessory Win.

"/oPy

olOt-

o/o

Cpy

CJCO

'/oQz

ooT-CM

1.0*4.1 mm ,stPY, S/fcO.lto i \3crn gwvnQZ, Q.2% ifpo. 1

2.OTK0.1ntm sIPY, J.% 0.1 to 3cm gwvnQZ, 0.1 "X, fpo. trace?* fas,

1.OTK0.1mm wPY, e.% 0.1 to 6cm gwvnQZ, tracer dsp,

0.5*0.1 mm wPY, 2.14 0.1 to 0.5cm gwvnQZ,

10*-:0.1mrn wPY, 4. 1* 0.1 to 6cm gwvnQZ, trace1* dsp,

1.(nK0.1min wPY, S.% 0.1 to 3cm gwvnQZ,

Struct.

Struc

shux

shr

shux

shr

<tca

53

58

61

61

61

Assay

From (m)

299.5

300.5

301.4

3023

303.0

3035

304.6

305.7

3068

307.3

308.0

3095

To (m)

300.5

301.4

302.3

3030

303.5

304.6

305.7

306.8

307.3

308.0

309.5

311.0

Sam. #

449

450

451

452

453

454

455

456

457

458

459

460

Au ppb

-5

-5

-5

5

14

6

12

14

20

-5

-5

-5

Au

} ||

Diamond Drill Log Sheet

Project: Bristol

Q-UBTCO Hole: BRSOO-03

"E

1Q

~:

:-

312-

-

313-

:

;

314-

-~

315-

~

316 ~

318-

^

319-

,

i

Lithology

r "i

i i

HT -- l

1 "f

-r?

HI-*

~ 1

r~1j iL J

i -i~7* ^

j "1

--

.^—

-~

--- -.

--

From (m)

307.3

317.0

To (m)

-317,0-

329.0

Lith code

5

Saba

lithology

sediment

greywacke

text. Comments

...Interbedded greywacke and siltstone.Predominantly quartz-greywacke beds, medium-grey, interbbed with narrow dark grey and graphitic siltstone beds (10*); Apparent j

i bedding varies from 2mm to 70cm thick, at 66 degrees tea, parallel to slaty cleavage. Greyish to white quartz -calcite stringers and veinlets, sheared to boudinaaed. 3V Pyrite up to 1*. l

, very fine grained (eO 5mm) ...Same as above unit, but most predominantly medium grey greywacke, locally interbedded with minor fine wacke to siltstone (dark grey) intervals, generally ^Ocm wide. Dark grey quartz grainsover 1mm in dia. are visible in places (ie.324.5m), and minor dark grey (chloritic to graphitic?) fragments, -:1cm in dia., flattened. White to grey quartz-calcite stringers and veinlets, T-2%, all angles. Weak to moderatelyfoliated, with local slaty cleavage. Well developped flame structures near 325.6m and 328.1m suggests tops uphole. Pyrite, D.5%,occurs as fine wisps and seams, mostly paralle tothe schistossity Trace of chalcopyrite within theveins.

Alteration

Chl

c\w

Ser

C^W"

Silic

ow

Epi

c^w*

Hem

r**t

Carb

CV*

other

Accessory Win.

"/o Py

oif)T

"/o

Cpy

CNOO

"/o QZ

ooT-CV1 0% ^.1mm

\wPY, S.%0.1 to i \3crn gwvnQZ, 1

05*^.1 mmwPY, S.% 0.1 to3cm gwvnQZ,

0.5*O.1mmwPY, 0.1*vnCp,2.*0.1 to 1cm gwvnQZ,

Struct.

Struc

shux

< tea

62

Assay

From (m)

309.5

311.0

311.6

3125

314.0

315.5

317.0

318.5

To (m)

311.0

311.6

312.5

3140

315.5

317.0

318.5

320.0

Sam. #

460

461

462

463

464

465

466

467

Au ppb

-5

6

-5

-5

-5

-5

-5

5

Au

e |T-

Diamond Drill Log Sheet

Project: Bristol

Carncco Hoie . BRSOO-OS

Depth (m)

4321-

322 -E

323-

324 -

325-4

326-

327 -i

328^

329-^

330^

331-^

332-

333 i

334 -.

335^

336-

;337-

338-

339-.

Lithology

-i-

-7-

Z-ii~~T

H -t~*-i .-v--!

r ;

J... l

.j..

:r

From (m)

317.0

3290

336.0

3369

338.1

To (m)

JZaO.

336.0

3369

3381

343.5

Lith code

Saba

5

Sac

Sac

Sac

lithology

greywacke

sediment

siltstone

siltstone

siltstone

text. Comments

, very fine grained (*0.5mm) ...Same as above unit, but most predominantly medium grey greywacke, locally interbedded with minor fine wacke to siltstone (dark grey) intervals, generally -:1 Ocm wide. Dark grey quartz grains over 1 mm in dia. are visible in places (ie. 324.5m), and minor dark grey (chloritic to l graphitic?) fragments, *1cm m dia., flattened. White to grey quartz-calcite stringers and veinlets, 1 -2*. all angles. Weak to moderately foliated, with local slaty cleavage. Well developped flame structures near 325.6m and 328.1 m suggests tops uphole. Pyrite, 0 516, occurs as fine wisps ana seams, mostly parade to the schistosity Trace of chalcopyrite within the j yeins. l

, aphanitic (*0.1 mm) ...Graphitic siltstone to argillite, dark grey to black. Moderate to strongly graphitic, with slaty cleavage well developed at 65 degrees tea., sheared. Relatively fairly homogenous, weakly banded by different shades of grey, d to 30cm. Moderatery blocky core, nearly gouged from 335.5 to 336m.j, aphanitic (0. 1mm) ...Graphitic l siltstone, black to dark grey. Fairly homogenous. Pyrite wisps and disseminatins, seams, both within the host rock and within the veins. Trace of arsenopyrite within the veins.f, aphanitic (*0.1mm) ...Mineralized | graphitic siltstone, dark grey. Contains 25 to 3016 white to greyish quartz-calcite-ankerite-tourmaline veins and stringers, up to 30cm wide (from 336.9 to 337.2m), accompanied by weak bleaching along the margins (weak sericitization); Veins are |

i sheared, and contain amourphous tourmaline patches locally. Pyrite occurs as seams and stringers and blebs, mainly infilling fractures

1 within the veins (up to S1!/!) locally), and as wisps 1 within the host rock. Overall 2* pyrite. Arsenopyrite occurs as fine disseminations and as seams, both within the rock and the veins as well, about Q.25%. Trace of possible chalcopyrite.

/, aphanitic (0. 1mm) ...Relatively ~\ | homogenous graphitic siltstone, dark grey to \ : black, weakly banded by different shades of grey over 1 to 50cm. Moderately schistose, with slaty cleavage at 73 degrees tea. Weakly folded, creating "flame-like" features near 340.2m. Arsenopyrite trace observed at least down to 341 m. Pyrite wisps and seams, both within the host rock and in association with the veins, 0.516. mainly parallel to the schistossity.

Alteration

Chl

CNW

Ser

CNW

Silic

CNW

Epi

CM*

Hem C

e\*r

:arb

CNW

other

Accessory Min.

07oPy

*2

-

"/o

Cpy

(NCO

/oQz

ooT-CN

1

0.516*0.1 mm wPY. yO/ffcvnCp, 2.* 0.1 i \to IcmjpwnQZ, l

0.516*0.1 mm wPY, 1.* 0.1 to IcmgwvnQZ,

/0.5*t0.1mm \ /wPY, 12.16 0.1 to \ 4cmgwvnQZ, trace* vn AS.

/2.01* cO.lmmfPY, \ 0.1 *vnCp, 30.16 0.2 to 30cm gwvnQZ, 0.216 das.

/2.016-:0.1mmfPY, \ 0.1 *vnCp. 1.160.1 to 2cm gwvnQZ, trace1*, das,

/Q.5% *0.1mm \ wPY, t.% 0.1 to 2cm gwvnQZ, trace* das,

Struct.

Struc

shux

shux

shr

shux

< tea

70

70

70

72

Assay

From (m)

320.0

321.5

323.0

324.5

3260

3275

329.0

3305

332.0

333.5

335.0

3360

3369

338.1

3390

To (m)

321.5

323.0

324.5

326.0

327.5

329.0

3305

332.0

333.5

335.0

336.0

336.9

338.1

3390

340.0

Sam. #

468

469

470

471

472

473

474

475

476

477

478

479

480

481

482

Au ppb

-5

5

-5

5

-5

-5

-5

-5

7

5

11

13

46

8

7

Au

| ||

Page: 17 of 19

Diamond Drill Log Sheet

Project: Bristol

Cameco H0ie: BRSOO-OS

1(DO

341 -E

342-

-i

343^

344 -z

345-

346^

^

348^

-E

349-;

350 -E

351 -1

-

353-

354 -i

-j

355^

356^

~

357 -,

358 -f

359^

~\

Lithology

-~

:-

H

t" :

i '

T"!

l .

"V

-Y--

— -

--

T

.,L

-'-

-T

From (m)

3381

343.5

347.0

To (m)

3435

347.0

3650

Lith code

Sac

5

Saba

lithology

siltstone

sediment

greywacke

text. Comments

Alteration Accessory Win.

Chl

CsW"

, aphanitic ^01 mm) ...Relatively 1 homogenous graphitic siltstone, dark grey to | black, weakly banded by different shades of grey 1 H over 1 to 50cm. Moderately schistose, with slaty fl

cleavage at 73 degrees tea. Weakly folded, creating flame-like" features near 340.2m. Arsenopyrite trace observed at least down to341m. Pyrite wisps and seams, both within thehost rock and in association with the veins,D.5%. mainlv parallel to the schistossity. l

.aphanitic ("0.1 mm) ...Interbeddedgraphitic siltstone and greywacke. Apparent bedding defined by alternating shades of grey (medium to dark), over widths of *1cm to 30cm,possibly fining downhole, weakly disrupted, folded (flame-like textures, pointing uphole). Locally speckled by very fine carbonate (dolomite?). Pyrite occurs mostly asdisseminations fine seams, Q.25%.

, very fine grained ^0 5mm) ...Mostpredominantly greywacke, grey-colored, withminor siltstone beds ^5*). Locally speckled by carbonate (calcrte-doiomrte?), and by greyish quartz grains. Appears to be locally fining downhole, although this is poorly defined. Minor

freyish quartz-calcite veinlets, 0.2 to 1cm. quivalent amount of quartz-ankerite veinlete,

generally wider (1 to 6cm). Trace ofdisseminated pyrite within the host rock and within the veinlets. Trace of fine disseminatedarsenopyrite near 359.0m. Foliation weak to moderate, with local slaty cleavage.

Ser

CM*

Silic

CM*

Epi

CNW"

Hem

c*w

Carb

CNW

other '/o Py

o

'/o

Cpy

CMCO

"/o Qz

ooO.S'iKO.Imm

.wPY, 1.1*0.1 to , \2crn gwvnQZ, ; trace* das. ;

0.1*t0.5mmdPY,1 .16 0.2 to 2cm gwvnQZ,

'

0. 11^0.1 mm dPY,Q.5% 0.2 to 6cm gwvnQZ, trace1* das

Struct.

Struc

shr

shux

sfon

<tca

72

68

62

Assay

From (m)

340.0

341.0

342.0

343.5

344.8

345.7

347.0

348.3

349.0

350.5

352.0

353.0

354.5

356.0

357.5

3587

3595

To (m)

341.0

342.0

343.5

344.8

345.7

347.0

348.3

349.0

350.5

352.0

353.0

354.5

356.0

357.5

358.7

359.5

360.8

Sam. #

483

484

485

486

487

488

489

490

491

492

493

494

495

496

497

498

499

Au ppb

t

5

42

5

15

6

12

-5

-5

6

-5

5

-5

7

8

-5

-5

-5

Au

j g|- S *-

Page: 18 of 19

Diamond Drill Log Sheet

Project: Bristol

CamCCO Hole: BRSOO-03

?.cQ.djQ

- :

361 -r

362 -:

363 -1

3644

:

366 i

367-1

368--

369 -E

370 -r-~

371 T

372 4

373 -.

374 -:

375 ^

376 4

377 -I

3784

379 ~

From (m)

-i4?,Q

i

Lithology

To (m)

.mo.

Lith code

Saba

lithology

greywacke

j

-I.-

text. Comments

, vary fine grained ^O.Smm) ...Most predominantly greywacke, grey-colored, with minor siltstone beds ^S1*). Locally speckled by carbonate (calcite-dolomlte?), and by greyish quartz grains. Appears to be locally fining downhole, although this is poorly defined. Minor greyish quartz-calcite veinlets, 0.2 to 1cm. j Equivalent amount of quartz-ankerite veinlets, generally wider (1 to 6cm). Trace of (disseminated pyrite within the host rock and within the veinlets. Trace of fine disseminated arsenopyrite near 359.0m. Foliation weak to moderate, with local slaty cleavage. l

Alteration

Chl

C~4t

Ser

CN*

Silic

CvW

Epi

CSN-

Hem

c\w

Carb

c\w

other

Accessory Min.

"/o Py

olOi-

o/o

Cpy

OJM

"/o QZ

oo'-CN

OI'ft^.lmmdPY, ^O.S'itO^toScm gwvnQZ, tracelk das

Struct.

Struc < tea

64

Assay

From (m)

3595

3608

362.0

3635

To (m)

3608

3620

3635

3650

Sam. #

499

500

7651

7652

Au ppb

i i

-5 1

-5

-5

6

Au

! li

Page: 19 of 19

Summary Geology o g* Sg/t Composite Interval

Cameco

UTM East: 464501

Grid East: 4000

UTM base: NAD27

Claim*: 1226640

Township: Bristol

Start Date: 11/27/2

Logged By: J. Samson

Drilled By: Bradley B

Core Storage: Dome

Down Hole: ezShot

Cameco Gold Inc.Summary Log Sheet

tie: BRSOO-04

oject: Bristol

UTM North: 5365756

Grid North: 2850

Local Grid : Teck

Elevation: 297

Core Size: NQ

Completion Date: 11/29/2

mson

Bros. Ltd.

Length: 119

ne Mine core storage area

ot Casing in Hole: NoCsg

ir: No # of Au Samples: 30

ojection of

eyMag

Reading

5829 5801

IP-anomaly BR-2 and BR-4.

Hole Rock SampleFrom (m) To (m) Sample # lithology

-50

-

-

-100

V; 0

.p'.'

.P-'0.-

f-'

If'.'

"•9"

.P. 0

.p.-

V;•9'0 . '

.p.'

.p."V-;"P.Ci '- .C?.'

o ,-

\s

V

V

V

V

V

v

•v

•v

o

o

V

•^4 ——— J

•V

Overburden

mafic volcanics

mafic volcanic schist

mafic volcanics

mafic volcanic schist

mafic intrusive

j

L ,- . .

Diamond Drill Log Sheet

Project: BristolCameco Hoie . BRSoo-04

fiQ.

Q

^

2\"H

3 J

A-z

5--

^6 -i

7 -E

H9 i

10-1^~

11 -r

12--

13-z

";

14-f

•i

15-r

''l

^

18-^~{

1

Lithology

•f-

-.p.*-.p1 .'^'• io" '-.p.'

^•'

o '..p.'

O" '..p.'

o' ".•p-'^p'-'

.p. 1^J '-d"3 -'0 "-.p.'

s1?0 '•p.V-

-O-

Jp

-p-

-p-

From (m)

00

To (m)

42.0

Lith code

OB

lithology

Overburden

text. Comments

Alteration

Chl

CNN-

Ser

CNW

Silic

CNN-

Epi

CNKT

Hem

CNW

Carb

CNW

other

Accessory Min.

0XoPy

o

"/o

Cpy

CNKO

0XoQz

00T-CNI

Struct.

Struc <tca

Assay

From (m)

To (m) Sam. # Au ppb Au

, Si- S *-

Page: 1 of 6

Diamond Drill Log Sheet

Project: Bristol

CarcjgCO Ho|e: BRSOO-04i i

Depth (m)

2H

22-:

23 -E

24^

25-1

26--

27^

28-

29^

30 ;

31 -r

32^

33-:

34 -i

35 l

36-;

37 H

38^-i

39^

Lithology

ri p -

'•P-

|vJ;'

|;Vo'J.

fo ' o '.•P-'

o '..p.'

"V-;

-p'.'

V-'-P-'

.1?-'

•p-'

•P-'

J - .f?-'

V-'

f'sp,•f-•9 '

f'-

"f'-

V-

/;

From (m)

Jii^

To (m)

42.0

Lith code

OB

lithology

Overburden

text. Comments

Alteration

cm

fvW

Ser

CVW

Silic

OW

Epi

(M*

Hem

CVW

Carb

CV*

other

Accessory Min.

0XoPy

o

0Xo

Cpy

CNrt

'/oQz

oc

,

Struct.

Struc < tea

Assay

From (m)

To (m) Sam. # Au ppb

\

Au

i li

Page: 2 of 6

Diamond Drill Log Sheet

Project: BristolCameco H0ie . BRSoo-04

1Q

I-

41 -i

43^z^

44H^

45-;

46-;

47 -E

48^

49 4--

50-;

51 -L^

52-;-

53-;

54^

55^

-se-;

157-;

58^~-

59-

Lithology

;V;

-3 '-

v

•v-

v

•v

v

V

V'-

V

V

V

V

V

V

V1

V

^-(

v

V

V

"x

From (m)

0.0

42.0

47.7

To (m)

42.0

47.7

85.0

Lith code

OB

i

'

lithology

Overburden

mafic volcanics

mafic volcanics

text.

- feldspar phyric

- feldspar phyric

Comments

, Massive amygdaloidal flow....Relatively light green mafic rock, Mg-rich(7),or possibly bleached. Fairly massive, weaklyfoliated, with up to 35** feldspar phenocryst locally (up to 5mm, greenish-white, subhedral).Strongly amygdularlocally, chlorite-carbonateinfilled, flattened, up to 5mm long, gives rock a "gabbroic" texture. Foliation weak to moderate,at 36 degrees tea., suggesting hole is being drilled slightly down-dip. White to pinkish quatz-calcite-epidoteW-hemattte stringers and veinlets, 1 16, up to 4cm wide, at various angles, mostly parallel to foliation, occasionally containtrace disseminated pyrite.

, Amygdaloidal pillowed flow....Transitional from above unit. Generally veryfine-grained, light green and fairly hard.probably bleached by weak to moderatecarbonate and saussurite. Strongly amygdular, with up to 2516 green to dark greychlorite-calcite-quartz amygdules, up to 3-5mm in dia. Subtle pillow features, generallyexpressed by light yellowish green to dark green bands, felsic" to chloritized. Moderately foliated, very oblique tea, mainly from 25 to 35 degrees. Fine subtle greenish feldspars arelocally visible, strongly saussuritized. White quartz-calcite*^pldotew-hematite stringers and veinlets, up to 1 0cm wide, at various angles, often disrupted, scattered, 116 overall, with tracepyrite. Some veins contain minor tourmaline (ie.65m). Pyrite within host rock varies from trace to Q.5%, disseminated to minor wisps andstringers.

Alteration

Chl

CNW"

Ser

CNW"

Silic

CNW

Epi

c\w

Hem

CNW

Carb

CNW"

other

Accessory Win.

"/o Py

olOT-

o/o

Cpy

CNCO

o/o QZ

ooT-CN

0.116O.5mmdPY,1^0.1to4cmvnQz,

'

0.5* •cO.Smm stPY, 1.16

0.116*0.5mmdPY,

Struct.

Struc

sfon

fault

sfon

shrshr

sfoM

•e tea

26

25

58 98

23

Assay

From (m)

440

45.0

46.2

54.1

55.5

570

58.5

To (m)

450

46.2

47.5

55.5

57.0

58.5

60.0

Sam. #

7653

7654

7655

7656

7657

7658

7659

Au ppb

-5

7

-5

-5

-5

-5

25

Au

, st- uS r-

Page: 3 of 6

Diamond Drill Log Sheet

Project: Bristol

Carc*gCO Hole: BRSOO-04

tQ.

Q

J

61 J

62-4

63-

64^

65-.

—66-:

67 -j

68 ~i

69 4

70 4

1 71 4

724^-

73-1

74-'

75-i

76-;

774

78 4

79-:

Lithology

'~

'~

•v

V

^

V

-'v

vv

V

v

V

From (m)

47.7

To (m)

85.0

Lith code

i

lithology

mafic \volcanics x

text. Comments

- feldspar , Amygdaloidal pillowed flow. \phyric l ...Transitional from above unit. Generally very

fine-grained, light green and fairly hard, probably bleached by weak to moderate carbonate and saussurite. Strongly amygdular, with up to 25ft green to dark grey chlorite-calcite-quartz amygdules, up to 3-5mm in dta. Subtle pillow features, generally expressed by light yellowish green to dark green

l bands, "felsic" to chloritized. Moderatelyfoliated, very oblique tea, mainly from 25 to 35 degrees. Fine subtle greenish feldspars are locally visible, strongly saussurMzed. Whitequartz-calcite*Aepidote-iV-riematite stringers and veinlets, up to 1 0cm wide, at various angles, often disrupted, scattered, 1ft overall, with trace pyrite. Some veins contain minor tourmaline (le. pom). Pyrite within host rock varies from trace to Q.5%, disseminated to minor wisps andIstringers.

Alteration

Chl

ow

Ser

c\w

Silic

CM*

Epi

CSW

Hem

CNW

Carb

CNW

other

Accessory Win.

"/oPy

0lOT-

Cpy

CNCO

0Xo Qz

oo

-

i — '

T-CN

0.1*-:0.5mmdPY,\1.* t

D.5% ^.5mm dPY, S.% 3 to 4 cmcm vnQz,

.

O.I'KO.SmmdPY,2.^0.1 to 4cmwvnQZ,

Struct.

Struc

sfon

sfon

< tea

33

27

Assay

From (m)

62.7

64.2

65.5

To (m)

64.2

65.5

67.0

Sam. #

7660

7661

7662

Au ppb

-5

-5

-5

Au

\ ^- S *~

Paqe: 4 of 6

Diamond Drill Log Sheet

Project: BristolCgrncco Hoie . BRsoo-04

I81-^

-

Oif~

83^

84^-

85 -.

-I

86 -E

87-:—

88-^

of, -oy -—

90Hj

91-:

92 :

93 -E

94 -i

95-.

96^

97-:—

98^

99^J

Lithology

S(-

vv

,c

V

v

V

V

•v

v

v

V

V

v

V

— ~

JH:

g

li

^^-^-r-r^L-:

-rH

i^S-T

From (m)

47.7

85.0

92.5

To (m)

85.0

92.5

102.5

Lith code

1

i

u

lithology

mafic \volcanics 7

mafic volcanics

mafic volcanic schist

text.

- feldspar

amygdaloic al

Comments

, Amygdaloidal pillowed flow. ...Transitional from above unit. Generally very fine-grained, light green and fairly hard, probably bleachecfby weak to moderatecarbonate and saussurite. Strongly amygdular.with up to 25* green to dark grey chlorite-calcite-quarte amygdules, up to 3-5mmin dia. Subtle pillow features, generally expressed by light yellowish green to dark green bands, •felsic" to chloritlzed. Moderatelyfoliated, very oblique tea, mainly from 25 to 35degrees. Fine subtle greenish feldspars arelocally visible, strongly saussuritteed. White quartz-calciteW-epidote*Miematite stringers and Iveinlets, up to 10cm wide, at various angles,often disrupted, scattered, 1* overall, with tracepyrite. Some veins contain minor tourmaline (ie. fesm). Pyrite within host rock varies from traceto Q.5%, disseminated to minor wisps andStringers.

, Massive amygdaloidal flow....Transitional from above unit. Light tomedium-dark greenish-grey, strongly amygdular as previously described, but more strongly carbonatized by moderate pervasive carb onate (calcite), and fracture controlled quartz-calcite stringers at all angles tea, sheared, disrupted,hairthin to 2cm, perhaps 2-346, locallyaccompanied by wallrock silicification. Theamygdules appear predominantly infilled by silica, with lesser carbonate and chlorite. Pyritetrace, fine disseminated.

...Transitional from previous unit. Light to medium-dark green. Moderate to strongly schistose, with local tight folds (ie. 94.2m).Trace of remnant amygdules still locally visible. Weak to moderately chloritized, perhaps weakly sericitized, with moderate to strong pervasive calcite alteration. Quartz-calcite stringers, mainly hairthin to 2-3mm, parallel to schistosity,sheared to folded as well, Sil. Pyrite finedisseminated to wispy, both within host rock andveins. Trace of sphalerite within the veins near1 01 .25, and possible trace of arsenopyrite.

Alteration

cm

CVM-

-

Ser

CM*

Silic

CM*

Epi

Cv**

Hem

CM*

Carb

CvW

—

other

Accessory Win.

"/o Py

0UOi-

"/o

Cpy

CMCO

VoQz

ooT-tM

-

0.11K0.5mmdPY, ^2.* 0.1 to 4cm l \wvnQ2. l

0.11K0.5mmdPY. 2.* 01 to 2cm wvnQZ,

O.SHO.Imrrxx •dmmdPY, S.%0.1 to 1cm wvnQZ, dsp,

Struct.

Struc

sfon

sfoM

shux

<tca

41

37

26

Assay

From (m)

85.5

86.9

88.0

89.0

92.5

94.0

955

97.0

98.5

To (m)

86.9

88.0

89.0

90.0

94.0

95.5

970

985

100.0

Sam. #

7663

7664

7665

7666

7667

7668

7669

7670

7671

Au ppb

c(

-5

9

-5

5

-5

-5

-5

-5

-5

Au

5 si- lo T-

Page: 5 of 6

Diamond Drill Log Sheet

Project: Bristol

^UJJgJO Hole: BRSOO-04

?

Q

101 -:

102^

103H

104^

105^

106^

^ 107^

108^

4

109-^

110 Ii

111 1

112-

113-

~115-

^116-

117^

us-:—

Lithology

— -

Si

Si

V

v-:v

-i\ v̂

~~̂^̂

~ ~rH:T^^Si

-zr.

•V

•x

From (m)

925

102.5

112.5

To (m)

102.5

112.5

115.8

115.8

116.5

116.5

119.0

Lith code

n

i

i*

i

6

lithology

mafic\ volcanic ' •schist 7

mafic volcanics

maficvolcanicschist

mafic

mafic intrusive

text.

.amygdalok

Comments

...Transitional from previous unit. Light tomedium-dark green. Moderate to strongly schistose, with local tight folds (le. 94.2m).

[ Trace of remnant amygdules still locally visible. Weak to moderately chloritized, perhaps weakly j sericitized, with moderate to strong pervasive calcite alteration. Quartz-calcite stringers, mainly hairthin to 2-3mm, parallel to schistosity.

disseminated to wispy, both within host rock and veins. Trace of sphalerite within the veins near f11 01 .25, and possible trace of arsenopyrite. l

, Massive amygdaloidal flow. ...Transitional from above unit. Light green,featureless, weakly foliated, at about 35 degrees tea. Very fine quartz-carbonate amygdules still discernible. Quartz-calcite+Aepidote stringersand veinlets, 0.2 to 1cm wide, 1 It, mainly parallelto the foliation, weakly sheared.

to 102.5m. Light green, moderate to strongly shearedtfoliated, with weak local folding.Incipient vario)es(?) near 114.4m. Quartz-calcite-W-epidote stringers and veiniets.sheared, boudinaged, ID-15% from 1 13 to114m. Pyrite trace, fine disseminated to wisps. Pyrrhotite stringers from 1 14 to 1 15m, *0.51t./...Contact zone/Mafic volcanic and mafic dyke. \/ Dark green to dark grey, fine-grained, mixed \ zone of mafic volcanic to mafic dyke (diabase?), with chilled mafic dyke intrusions. Moderately sheared, with pyrite blebs, D.5%, fracture

^.controlled, often subparallel tea., massive. ...Mafic dyke/diabase dyke. Upper contact sharp but irregular, at ^0 degreestea. Dark greenish-grey, chloritic, very fine-grained to aphanitic, partly chilled. Massive, homogenous, non-foliated. Weaklyblocky core, with chloritic fractures at allangles. Trace of quartz -calcite stringers.Non-magnetic. Trace of pyrite on fracture planes.

Alteration Accessory Min.

Chl

c^W"

j.

Ser

OW

Silic

CVW

Epi

c\w

Hem

C\W"

Carb

CNW"

r

otherk Py

0L-^P'"Y^ '

"/o

Cpy

CMCO

"/o QZ

00i-C\

J

O.S'iiO.lmn'^x\*1mmdPY, 5^0.1 \to1cmwvnQZ. dsp/

•clmmdPY, 25.* 0.1 to 4cm wvnQZ, 0.1%dsp,trace?% das,

O.llt^.lmmdPY, I.* 0.1 to 1cm

8.'* 1 to '3cm wvnQZ,

1.* 0.2 to 1cmgwvnQZ,

15.14 0.1 to 5cmwvnQZ,

wPY, 2^ 0.1 to1cm wvnQZ, 0.3*bPO,

D.5% cO.Smm bPY,

0.1%<0.1mmdPY,

Struct.

Struc

sfoM

shux

sfoh

<tca

35

25

2710

Assay

From (m)

100.0

101.0

101.5

102.5

110.0

111.0

111.6

112.5

114.0

115.0

115.8

To (m)

101.0

101.5

1025

104.0

111.0

111.6

1125

114.0

115.0

115.8

116.5

Sam. #

7672

7673

7674

7675

7676

7677

7678

7679

7680

7681

7682

Au ppb

-5

-5

-5

-5

-5

-5

9

5

-5

-5

-5

Au

, g|- u5 T-1

Page: 6 of 6

Summary Geology OP" Ss/t Composite Interval

Cameco

UTM East: 464330

Grid East: 4000

UTM base: NAD27

Claim #: 1226640

Township: Bristol

Start Date: 11/30/2

Logged By: J. Samson

Drilled By: Bradley B

Core Storage: Dome

Down Hole: ezShot

Cameco Gold Inc.Summary Log Sheet

l

tie: BRSOO-05

oject: Bristol

UTM North: 5366046

Grid North: 3175

Local Grid : Teck

Elevation: 297

Core Size: NQ

Completion Date: 3/12/20

mson

Bros. Ltd.

Length: 254

ne Mine core storage area

ot Casing in Hole: NoCsg

ir: No # of Au Samples: 124

ojection of IP-anomaly

eyMag

Reading

57915777577457715769

BR2 and BR4.

Hole Rock SampleFrom (m) To (m) Sample # lithology

-50

—

— 100

-

--

---150

"

-

-

-200

-

-

-250

j?'

•9'D ,-

"f''"

"f"'

i

V

1?!V

V

s/

V

V

V

V.

V

V

V

•V

V̂

V

V

V

V

V

V

V

V

,

V

s/

' v

V

s/

•v-

'-

Overburden

mafic volcanics

fault zone

-

mafic volcanics

felsic volcanicmafic volcanics

felsic volcanic

mafic volcanics

Diamond Drill Log Sheet

Project: Bristol

Sffl™ Ho|e: BRSOO-05

O. VQ

-i1 ~

2 -i

5-j

6 ~

^

iol1 1 --

12 1

13 -

15-E

z16 5

17H

18-

19-

]

Lithology

'•9-

T.'

K

V;

j *.o '.

• L5 -'

V-'

6 . -.O-

f-'

^b. 1d . -

f

V- 1•p'

•p-

tp".o ".

V-.p.

0 -.p.

From (m)

0.0

To (m)

31.0

Lith code

OB

lithology

Overburden

text. Comments

Alteration

Chl

CNN-

Ser

CsW

Silic

C\W

Epi

o**-

Hem

ow

Carb

ow

other

Accessory Win.

"/o Py

o

"/o

Cpy

OKO

"/oQz

oo^-01

Struct.

Struc •c tea

Assay

From (m)

To (m) Sam. # Au ppb Au

J li

Page: 1 of 13

Diamond Drill Log Sheet

Project: Bristol

Carneco Hole: BRSOO-OS

1Q

^-,

21 -|

22 -:

23-;

24-EI-

25-:r

26-;—

27 H~

28-;

29^--

30^

31-

-32-

33-^

i34-;

-35-

36--

37 -E

38^

39H

^

Lithology

D .'•.f?. 1

y '. (

^ *-

T'.'

' C -•^ v0 -,

o' . i

V-'

o '.•p- 1

•p- 1

d -

D .'

v

s/

,/

-v

From (m)

TTO

31.0

31.6

32.7

36.1

To (m)

31.0

31.6

32.7

36.1

45.3

Lith code

OB

i

i

i

i

lithology

Overburden

mafic

mafic volcanics

mafic

mafic volcanics

text. Comments

...Silicified mafic volcanic? Dark greenish-grey.very siliceous/silicrfied interval, sheared, with lapilll-slze ghostly greyish to white pseudoclasts, probably as a result of deformation. Very finequartz-eye looking features probably representremnant amygdules infilled by silica. Trace ofquartz-calcite-chlorite stringers parallel tea.{...Moderate to strongly altered. Apparent upper l fcontact(?) sharp, parallel to foliation at 57degrees tea. Diffuse bands varying from darkgreen to very light grey indicate various intensity of locally moderately chloritic to locally strongly silicified and possibly albrtitized intervals, 10to 40cm wide. Moderately foliated/sheared, with^* quartzW-calcite amygdules, 1 to 15mm India.. stretched. Less than 1* orevish-white

Alteration

Chl

quartz-calcite stringers and veinlets, Irregular, jvery oblique tea. Pyrite as fine disseminations, wisps and seams, mostly within the more |

within the veins, 1 -2*. locally, less than 0.5* H overall.

L Massive amygdaloidal flow. l I. ..Extremely altered. Interval grades from light i j yellowish green to light buff, to greenish-grey \ ' beyond 33.8m. Fine silica-infilled amygdules to

large cavities up to 1cm in dia. (infilled ibyquartz-calcite), are scattered throughout, life Moderately foliated to sheared (crackle fracturescommon), with strong to extreme and pervasivealteration by silica and/or albite, accompanied by strong saussuritization (mainly sericite-epidote-carbonate) from 32.7 to 32.6m.Translucent greyish-whitequartzW-calc!te*A-chlorite stringers and veinlets,at all angles, fracture infilling, 0.2 to 2cm, 2-316. Pyrite occurs mainly as fracture infilings, locally disseminated, within host rock and within the

, Massive amygdaloidal flow. .Faultzone. Abrupt transition from previously described altered zone above (stronglybleached), to a medium-dark greyish green and fine-grained mafic volcanic unit, moderate to strongly chloritized, perhaps weakly silicified locally. One strongly silicified bands, 3cm wide, near 42m. Intervalis strongly fractured (at allangles) to ground, with no non-broken intervals over 30cm wide. Fine quartz amygdules are stilllocally discernible. Moderately foliated at 40 to 52 degrees tea. Trace of veintng and pyrite.

CM*

L-

Ser

CM*

l

J

Silic

CM*

Epi

CNJ"^

Hem

CM*

1

1

Carb

CM*

other

Accessory Min.

"/oPy

0

"/o

Cpy

CNCO

"/oQz

ooiT-fN

,

1

0.1*-:0.1mmdPY,

Q.3% ^.5mm fPY, 1.* 0.1 to 0.5cm gwvnQZ,

LOKOSmmfPY, 2. 1* 0.2 to 2cmgwvnQZ,

0.116O.1mmdPY, 0.1 H 0.1 to 0.5cm wvnQZ,

Struct.

St rue

sfon

shr

< tea

62

—35—

Assay

From (m)

31.0

31.6

32.7

33.8

35.0

36.1

37.0

38.0

39.5

To (m)

31.6

32.7

33.8

35.0

36.1

370

38.0

39.5

41.0

Sam. #

7683

7684

7685

7686

7687

7688

7689

7690

7691

Au ppb

-5

-5

-5

-5

6

-5

11

-5

-5

Au

, S^• St-

Page: 2 of 13

Diamond Drill Log Sheet

Project: Bristol

Carneco Hole: BRSOO-OS

fo. to Q

\41-

42 J

434

44 H

--45 -

46 —

474

484

50 -^

51 i

524

53^

54 —

55 4

56 ~-

574

58-1

594

Lithology

V

^

v

''

V

•w

V

V

V

V

\/

V

V

V

V

V

From (m)

36.1

45.3

45.8

46.4

49.0

To (m)

45.3

45.8

46.4

49.0

660

Lith code

i

i i

i

i

lithology

mafic\volcanics _ ,'

mafic

mafic ^volcanics _ ,

mafic volcanics

mafic volcanics

text. Comments

, Massive amygdaloidal flow. ...Fault zone. Abrupt transition from previously described altered zone above (strongly bleached), to a medium-dark greyish green and fine-grained mafic volcanic unit, moderate to strongly chloritized, perhaps weakly silicified locally. One strongly silicified bands, 3cm wide, l near 42m. Intervalis strongly fractured (at all angles) to ground, with no non-broken intervals over 30cm wide. Fine quartz amygdules are still Uocally discernible. Moderately foliated at 40 to 62 degrees tea. Trace of veining and pyrite. l

/...Gouge zone. Strongly brecciated, milled to a \ l paste, with angular remnant fragments up to \ 0.5cm still visible. Apparent shearing angles very oblique tea, mainly 1 5 degrees.

t Epidote-green to grey, strongly altered, with \ remnant quartz-calcite veinlets also visible, (

...Structural breccia to gouge zone. Similar to previous interval above, strongly brecciated, semi-consolidated, clast supported, locally gouged. Clasts are angular, strongly bleached tol light grey by pervasive silicification and probably f albitization, and are contained within a matrix of {chlorite and carbonate. l...Blocky core, moderately sheared, locally brecciated, with several chloritic slip gouge at

1 20, 44, and up to 57 degrees tea. Medium-dark l : green to light green, fine-grained, with local weak/ ^silicification and/or possible albitization. /

, Massive amygdaloidal flow. ..Altered, medium greenish-grey to light yellowish-grey, fine-grained, with 2-3*5b fine quartz amygdules (-O mm), and minor ones infilledby calcite, up to 5mm across. Weak to moderately foliated, but moderately blocky core, with occasional slip gouge at various angles up to subparallel tea. Diffuse bands are bleached, weak to moderately silicified, with yellowish color suggesting presence of weak pervasive sericitization. The alteration as a whole appears to Increase downhole, becoming more siliceous, and sericitization weak but also pervasive. Quartz-calcite veins and veinlets vary for 2mm to over 30cm in width, overall ^K, mainly sheared, parallel to foliation. Pyrite disseminated to minor seams, within host rock and veins, trace overall.

Alteration

Chl

OMt

:

7

Ser

CNW

1

Silic

OW

i

Epi 1

CNW

Hem

CsW-

1

Carb

ow

other

Accessory Win.

"/oPy

o

"/o

Cpy

CMCO

"XoQz

ooT-CN

1 0^116 0.1 to 0.5cm' i WvnQZ. 1

0.116 ^.ImmdPY,

0.1 16O.1 mm dPY.

0.116 *0.1mmdPY. 0.5* 0.1 to 1cm wvnQZ,

O.itt^.lmm wPY, 0.5* 0.1 to 1cm wvnQZ,

r'0.116^.1rnmdPY, x 0.1 fcvnCp, 50.16

\30cm wvnQZ,

s! 1* 0.5 to 4cm wvnQZ,

0.1 *t0.1 mm dPY, 1.160.1 to 1cm wvnQZ,

Struct.

St rue

sfon

shr

shr

shr

shr

sfol1

< tea

45

15

n

57

0

60

Assay

From (m)

39.5

41.0

42.5

44.0

45.3

45.8

46.4

47.3

48.0

49.0

50.5

52.2

528

54.0

55.5

56.6

To (m)

41.0

42.5

44.0

45.3

45.8

46.4

47.3

48.0

49.0

50.5

52.2

528

540

55.5

56.6

58.0

Sam. #

7691

7692

7693

7694

7695

7696

7697

7698

7699

7700

7701

7702

7703

7704

7705

7706

Au ppb

-5

-5

-5

8

10

-5

-5

10

-5

-5

11

5

-5

-5

-5

-5

Au

5 ||

Page: 3 of 13

Diamond Drill Log Sheet

Project: Bristol

CameCO Hole: BRSOO-05

1(DO

Z

~

61 —

-i

62 -E^-

63^

64 -E

~

65^

-j;

67 "i~

68---

69-

—70 4

j72 -:

~

-

73^

74^

z75-

-

77 -:

78-^--

73-

":

Lithology

v

v-

V

V

V

•V

N/

V

V

liV

v

-•w

V

V

From (m)

49.0

66.0

75.3

75.6

To (m)

66.0

75.3

75.6

83.0

Lith code

i

i

6aa

1

lithology

maficA^olcanics^/

mafic volcanics

lamprophyre

mafic volcanics

text. Comments

, Massive amygdaloidal flow.

Alteration

Chl

OW

..Altered, medium greenish-grey to light yellowish-grey, fine-grained, with 2-3* fine jquartz amygdule; (*1 mm), and minor ones l

| infilledby calcite, up to 5mm across. Weak to t moderately foliated, but moderately blocky core. J]with occasional slip gouge at various angles up to subparallel tea. Diffuse bands are bleached,weak to moderately silicified, with yellowishcolor suggesting presence of weak pervasivesericitization. The alteration as a whole appears 1

amygdalok al

amygdalok al

j to Increase downhole, becoming more siliceous,and sericitization weak but also pervasive. Quartz-calcite veins and velnlets vary for 2mm toover 30cm in width, overall *216. mainly sheared, parallel to foliation. Pyritedisseminated to minor seams, within host rockland veins, trace overall. 1

, Tuffaceous. ...Siliceous Mafic(?)Volcanic/Fault Zone. Contact arbitrarilyselected. Somewhat similar to previouslyaltered mafic volcanic, but much harder, moresiliceous, medium greenish-grey. Moderatelyfoliated, very blocky core. Fine-grained, withgreyish quartz-eyes similar to siliceousamygdules further up, generally *1mm, 1 to 516 locally. Notably, white and larger quartz -calcite amygdular features are still noted (ie. 73.2m), 1-2mm, *116, flattened. Ghosty greyish clasts arelocally noted, very subtle, generally *2-3mm, may represent flattened felsic clasts, or mayrelate to deformation. Quartz-calcite stringersand veinlets are white to grey, mostly sheared,'1cm wide, 1-216. A very fine reddish-brownmineral and silica Is Infilling hairthin fracturesparallel to the foliation near 67.5m (sphalerite?trace, hematite?).

/...Contacts fractured, appear to be parallel to the \

brownish-green, fine-grained, and appears to be

chlorite. Possibly weakly silicified. Weak foliated:. Tuffaceous. ...Siliceous Mafic(?)Volcanic. As previously described interval abovethe lamprophyre dyke. Medium-greenish grey to light grey, fine grained, very siliceous, with 3-516dark grey quartz-eyes. Ghosty felsic-looking pseudoclasts, lapilli-size. are locally noted, 2-316, and may represent dislocated/dismembered veins. Weak tomoderately foliated, sheared, with microfractures,hairthin, generally very oblique tea. Overall,weakly chloritic, weak to moderately sericitized locally, perhaps weakly silicified, with weakfracture-controlled calcite.

Ser

CNW"

Silic

CNW

Epi

CvW

Hem

ow~

J

Carb

OW"

othet

Accessory Win.

"XoPy

oin-r-

o/o

Cpy

CMCO

"/o QZ

ooi-C\

0.116*0.1 mm dPY,\ 1.11 0.1 to 1cm 1 \wvnQZ, 1

0.l'l6^.1mmdPY, 1.160.1 to 1cm gwvnQZ, trace?'*5cD

0.1 16*0.1 mm dPY,

0.116 O.lmmdPY, 1.160.1 to 1cm gwvnQZ,

Struct.

Struc

sfon

sfoll

-cont-

< tea

61

43

00

Assay

From (m)

63.5

65.0

66.0

67.0

To (m)

65.0

66.0

67.0

68.5

Sam. #

7707

7708

7709

7710

Au ppb

-5

-5

-5

-5

Au

l gji- IO T"

Page: 4 of 13

Diamond Drill Log Sheet

Project: Bristol

^22S2 Hole: BRSOO-05

t(UQ

81 H--

82 -E

83-

T

84^

86 -j

L ' E

89 H-

90-^

zQ1 -~

;92-

93^-

94 -r

95-^

~

96-^

97^

98 -i

99 :

-

Lithology

r^

f *s,

"-V

^

V

-t*

1^-v

^"•l/

V

V"

V

v

V1

v1

V

V

V

V

V

From (m)

75.6

830

85.0

868

To (m)

83.0

85.0

86.8

102.5

Lith code

i

i

10

i

lithology

mafic\yolcanics 7

mafic volcanics

quartz vein

mafic volcanics

text.

.

Comments

, Tuffaceous. ...Siliceous Mafic(?)\ amygdaloid Volcanic. As previously described interval above Val /l the lamprophyre dyke. Medium-greenish grey to

light grey, fine grained, very siliceous, with 3-511dark grey quartz-eyes. Ghosty felslc-looking

1 pseudoclasts, lapilli-size, are locally noted,2-31*, and may representdislocated/dismembered veins. Weak to moderately foliated, sheared, with microfractures,hairthin, generally very oblique tea. Overall,

Mocalry, perhaps weakly silicified, with weakfracture-controlled calcite....Bleached Mafic(?) Volcanic. Transitional with previous unit, similar characteristics, but generally yellowish green and weak to moderately sericrtized and chloritized, to light

controlled chlorite alteration as well, at allangles. Alteration zone represents margin to

i underlying quartz vein. A 4-5cm wide medium greenish-grey and aphanitic dykelet Is noted near 84.2m, very oblique tea (see description at 102.5 to 103.0m)....Quartz Veining. White quartz veining, varying

i in width from 1 to 60cm, comprises 85"* of interval. Veins are irregular, with minor

l chlorite-sericite infilling fractures. Veins

amygdalok al

contain patchy to fine disseminated pyrite along the margins mostly, O.2516 overall. Host rock is same as previously described above, moderatelybleached, moderate to strongly chloritized,Weakly sericltized, yellowish-green.

, Tuffaceous. ...Siliceous Mafic(?)Volcanic. As previously described, generallymedium greyish-green, fine-grained, perhapsless siliceous-looking overall , with fine grey quartz-eyes (*:1mm) scattered throughout, 1-516 locally. Amygdular-like features are locally common, up to 1cm, infilled by quartnV-calcite, over 516 locally. Moderately foliated, with 316quartz-calcite veining, sheared, mostlydismembered, to weakly folded (le. 98.8m). Margins to veins are commonly bleached by carbonate and by weak pervasive sericitization. Pyrite trace, both within veins and host rock.

Alteration

Chl

c\w

-

Ser

C*W"

Silic

f^W

Epi

c-w

Hem

CNW

Carb

IN*

other

Accessory Min.

"/o Py

oIOT-

cpL QzCVKO

OO

h

0.116 O.lmmdPY,\1.160.1 tolcm 1 WvnQZ, 1

0.116 O.lmmdPY, 2.16 0.1 to 1cm wvnQZ,

Q.2% *0.5mm bPY, 85.16 0.2 to 60cm wvnQZ,

0.116 ^O.lmmdPY,3.16 0.1 to 2cmwvnQZ,

X0.216 O.Smm dPY, x

\wvnQZ,

0.116 O.lmmdPY,1.1601 to 1cm wvnQZ,

/0.116O.1mm \ /dPY, 3.161cm \wvnQZ,

Struct.

Struc

sfon

sfon

-sfott-

sfon

sfoti

< tea

47

69

71

62

60

Assay

From (m)

81.5

83.0

84.0

85.0

85.7

868

88.0

89.5

91.0

92.5

94.0

95.0

95.5

97.0

98.5

99.7

To (m)

83.0

84.0

85.0

85.7

86.8

88.0

89.5

91.0

92.5

94.0

95.0

95.5

970

98.5

yy. i

100.5

Sam. #

7711

7712

7713

7714

7715

7716

7717

7718

7719

7720

7721

7722

7723

7724

7726

Au ppb

7

-5

-5

-5

5

-5

40

14

-5

-5

5

124

-5

-5

-5

Au

Page: 5 of 13

Diamond Drill Log Sheet

Project: Bristol

CagjCCO Hole: BRSOO-05

gm Q

1101 -I

-

102~

103-

104 -E

105-^

106 --

107^•i

108^

1094-;

110H—

~

^ 1 1

112-^

113 ^

115^

116-

117-i-

m^-

119 —-

i

Lithology

V

''u'

'v

x-

V

v

V

v

V

v

V

V

v

V

V

V

ys/

V

v

v'~

v~

From (m)

86.8

102.5

103.0

116.0

116.9

To (m)

102.5

103.0

116.0

1169

120.4

Lith code

i

6

1

6

1

lithology

mafic\volcanics f

mafic intrusive

mafic volcanics

mafic intrusive

mafic volcanics

text. Comments

, Tuffaceous. ...Siliceous Mafic(T)

Alteration

Chl

\ amygdaloid Volcanic. As previously described, generally l \al /i medium greyish-green, fine-grained, perhaps l

n less siliceous-looking overall , with fine grey J quartz-eyes (tlmm) scattered throughout, 1-516

j locally. Amygdular-like features are locally f|common, up to 1cm, infilled by quarfrW-calcrte, over 516 locally. Moderately foliated, with 316

dismembered, to weakly folded (ie. 98.8m).

carbonate and by weak pervasive sericitization. 1 Pyrite trace, both within veins and host rock.

...Mafic Dyke. Upper contact fractured, lower1 contact sharp at 20 degrees tea. Light

amygdaloic

greenish-grey, fine-grained to aphanitic, appears chilled, fairly hard. Contains 1 16 fine dark grey anhedral mineral (0.25mm), and fine prismatic greyish to ghosty mineral (carbonate?), within an aphanitic groundmass, moderately calcitic. Appears non to very weakly foliatea, but containsfracture-controlled calcite*/- chlorite stringers.(disrupted. 1-216, at all angles., Tuffaceous. ...Siliceous Mafic(?)Volcanic. Medium greyish-green, fine-grained,as previously descnbed, but seemingly more siliceous than interval located above thepreviously described dyke. Fine quartz-eyes arelocally discernible, *1 mm, 1-516 locally. Whitecalcrte-w-silica amygdules up to 1 em are locally observed, tO 5"*, Some may represent dismembered stringers and veinlets. Ghostlylapilli-size pseudocTasts are locally visible, lighter green, felsic looking; Overall, intervalmay be comprised of a mixed zone of felsic tuffand highly altered (silicified to chlorrtized)amygdular mafic volcanic. Moderatefoliation/shearing, moderately blocky core, with1 cm offsets common along microfractures very oblique tea. Quartz-calcite stringers and veinlets, 1-216, accompanied by bleaching alongthe margins by weak to moderate sericitization.Pyrite fine disseminated to wispy, trace.

...Mafic Dyke. Upper contact sharp at 15 degreei tea, lower contact sharp but irregular, oblique tea. Medium greenish-grey, appear chilled, \ aphanitic, fairly hard. Same as previouslyobserved from 102 5 to 103.0m. Strongly

calcite-quartz stringers infill fractures as conjugate sets, at about 45 degrees tea, 216. Trace of disseminated pyrite, and one speck of

\chalcopynte observed within the stringers. f, Massive amygdaloidal flow....Amygdular mafic volcanic. Medium-green todark green, fine-grained, weak to moderatelychlontized, strongly carbonatized, perhaps locally weakly silicified. Calcite-quartz amygdules up to 1cm, 0.516. scatteredthroughout. Trace of amygdules are infilled bysilica. Foliation moderate Quartz-calcitestringers and veinlets, 116.

L

Ser

CNW

Silic

OW

Epi

tv*

Hem

c•W

Carb

cvfr

other

Accessory Min.

"/oPy

0lO*r~

"/o

Cpy

CNCO

"/oQz

ooT-tN

j 0.116 -:0.1mm\dPY, 3.161cm \wvnQZ. t

0.1%'tO.lmmdPY,0.516 0.1 to 0.5cmwvnQZ,

0.216 tO.lmmstPY,

0.1%-cO.lmmdPY, 0.1 16 dCp, 0.1 160.2cm wvnQZ,

0.116 tO.lmmdPY. 0.516 0.1 to 3cm wvnQZ,

0.116 *0.1mmdPY, 0.5160.1 to 1cm

0.1 16*0.1 mm dPY, 0.116 dCp, 2.160.1 to 0.5cm wvnQZ,

0.1 16*0.1 mm dPY, 1 16 0.1 to 0.5cm wvnQZ,

Struct.

Struc

sfoH

fault

sfoM

•:tca

69

15

54

Assay

From (m)

99.7

100.5

101.5

102.5

103.0

107.0

To (m)

100.5

101.5

102.5

103.0

104.0

Sam. #

7726

7727

7728

7729

7730

7731

Au ppb

-5

7

-5

5

6

6

Au

\ j^- u5 T-

Page: 6 of 13

Diamond Drill Log Sheet

Project: Bristol

Cameco Hoie . BRSOO-OS

Depth (m)

-

121-

122 -E

123^

125-

127^

129 -E

130^

131 -f

132^

133 -,

134~

135-

136-

137-4

138 1

139^

1

Lithology

^V

V

V

V

V

V

v

V

V

V

V

V

V

V

v

V

From (m)

A1SS

120.4

121.2

125.0

129.7

137.9

To (m)

120A

121.2

125.0

129.7

1379

1480

Lith code

i i

i

i

i

i

lithology

mafic\volcanics_V mafic volcanics

mafic volcanics

mafic volcanics

mafic volcanics

mafic volcanics

text. Comments

, Massive amygdaloidal flow. ..Amygdular mafic volcanic. Medium-green to dark green, fine-grained, weak to moderately chlontized, strongly carbonatized, perhaps j locally weakly silicified. Calcite-quartz amygdules up to 1cm, D.5%, scattered throughout. Trace of amygdules are infilled by silica. Foliation moderate Quartz-calcite j stringers and veinlets, 1 *. f, Tuffaceous. ...Siliceous Mafic(?) j Volcanic. Apparent upper contact sharp, at 65 | degrees tea. Very siliceous, with fine -:1 mm dark jrey quartz-eyes, 1-7* locally. Moderately oliated/sheared, with lapilli-size pseudoclasts(?) rf similar composition, lighter green, common, lMassive amygdaloidal flow. ..Silicified amygdular volcanic. Medium

yellowish green to dark green, locally moderately siliceous, and locally contains 1-2* fine greyish quartz-eyes(?) or amygdules. Definite l amygdules of calcite locally, up to 2-3mm. Moderately chloritic locally, moderately siliceous in other places; Very weak sericitization locally, j pervasive, but preferably In proximity to auartz-calclte veins. lMassive amygdaloidal flow. .Altered Mafic Volcanic/Quartz Veining. Light

green to epidote-green, fine-grained, with fine 3ark grey quartz-eyes, up to 5* disseminated. Minor calcite-quartz amygdules up to 1cm long, flattened. Interval is cross-cut by 7-9* bull white to locally greyish quartz veins, very irregular, at 45 to very oblique tea. Margins are locally strongly silicified/albitized, locally moderately epidotized to weakly sericitized (saussuritized). ^rite trace to 1 * locally, fine grained to 2mm l euhedral cubes, and as blebs, mainly within the l veins. Occasional wisps and stringers. t

Massive amygdaloidal flow. ..Silicified amygdular volcanic. As previously

described. Medium greyish-green, fairly siliceous to possibly albrdzed locally, very weakly sericitic, mainly in proximity to stringers and veins, but also controlled by microfractures. Ghosty chloritic "zits' common, 1-2*. ^mm, often stretched. Foliation weak, sheared. Fine quartz-eyes relatively rare, but occasinal calcite amygdules stall visible. Quartz-calcite stringers, 1*. sheared, often dismembered. Pyrite as fine disseminations to euhedral 1mm cubes, minor wisps and rare seams...Altered Mafic Volcanic/Fault and Quartz l

Veining. Medium greenish-grey, moderate to strongly sheared, strongly fractured locally, with several gouge slips at various angles, from 20 to 55 degrees tea. Moderately blocky core. Occasional calcite amygdules, and minor pinhead quartz-eyes locally developped. White quartz veins, very irregular, at various angles rom very oblique tea, to parallel to the main schistossity, vary in width from 0.2 to 4-5cm wide, often sheared, dismembered to folded. Weak to moderately siliceous and chloritic, with weak to moderate bleaching haloes (epidote and weak sericitization) centered about the veins, up to 1 m wide. Pyrite is fine disseminated to 2mm euhedral cubes (shot-gun textures), to occasional wisps and minor stringers, both within the veins and host rock, 0.2* overall.

Alteration

cm

CM*

J

Ser

CNW

Silic

r*w

Epi

OsW

Hem

CNW

Carb other

Accessory Win.

"/o Py

tf)T-

"/O

Cpy

(NCO

"/o QZ

ooT-OJ

3

0.1*t0.1mmdPY. , 1.160.1 to 0.5cm \wvnQZ. i0.1* -:0.1mm

v wPY, 1.* 0.1 to \0.4cm gwvnQZ. 1

0.2* *0.5mm wPY,

10.* 0.5 to 8cm gwvnQZ,0.2*^. 1mm stPY, Q.5% 0.1 to 0.3cm gwvnQZ,0.1**2mmdPY, 15.* 0.5 to 8cm wvnQZ,

0.2* •cO.Smm bPY, 3.* 0.2 to 1cm wvnQZ,

0.2*0.1mnKx •elmmdPY, 0.5* 0.1 to 0.3cm vnQz,

0.2* ^mm dPY, 3.* 0.2 to 5cm gwvnQZ,

Struct.

Struc

sfon

fract

sfoh

sfoM

sfon

shr

•:tca

53

25

67

67

75

20

Assay

From (m)

124.0

1250

126.0

126.9

128.0

129.0

129.7

136.8

137.9

139.0

To (m)

125.0

126.0

126.9

128.0

129.0

129.7

1310

137.9

1390

140.5

Sam. #

7732

7733

7734

7735

7736

7737

7738

7739

7740

7741

Au ppb

5

-5

-5

-5

-5

-5

-5

-5

-5

-5

Au

l ||

Page: 7 of 13

Diamond Drill Log Sheet

Project: Bristol

CameCO Hole: BRSOO-05

lD

-

141-

^

142^

r143-^

i

146-;A

1474

149^

150^

151-

152-

^153^

-

154^~

155 -z

—

157-

158-:-

159 -5

i

Lithology

f

v

v

v

V

V

V

V

'-x/

"

-V

V

V

v

V

From (m)

137.9

148.0

149.0

151.0

To (m)

148.0

149.0

151.0

163.0

Lith code

i

i

i

i

lithology

mafic\volcanics ,'

mafic volcanics

mafic volcanics

mafic volcanics

text. Comments

..Altered Mafic Volcanic/Fault and Quartz

Alteration

Chl

CvW"

Vetoing. Medium greenish-grey, moderate to l strongly sheared, strongly fractured locally, with l several gouge slips at various angles, from 20 to 155 degrees tea. Moderately blocky core. 1 Occasional calcite amygdules, and minor IIpinhead quartz-eyes locally developped, Whitequartz veins, very Irregular, at various anglesfrom very oblique tea, lo parallel to the main schistossity, vary in width from 0.2 to 4-5cmwide, often sheared, dismembered to folded.Weak to moderately siliceous and chloritic, withweak to moderate bleaching haloes (epidote and weak sericitization) centered about the veins, upto 1 m wide. Pyrite is fine disseminated to 2mmeuhedral cubes (shot-gun textures), tooccasional wisps and minor stringers, both withinHie veins and host rock, Q.2% overall. l

/...Silicified Mafic Volcanlc/Felsic Tuff. Medium \

homogenous, with very fine hardly perceptable quartz-eyes (1 *)fc), within a fine quartz-sericite matrix. Weakly sheared, with minor folding.Approx. 216, white to greyish quartz-calcrte .

Stringers, sheared to folded. 1...Altered volcanic. Same as previously described weakly to strongly silicified locally, moderately blocky core, fractured, with irregular white quartz veinmg, accompanied by weak bleaching generated by weak sericitization along

\the margins. /

...Sheared and altered volcanic. Medium-darkgreenish-grey to grey. Fine-grained, with amygdules up to 0.75cm locally, infilled bycalcite. Moderate to strongly foliated, sheared.locally schistose, with wealt folding orGranulations. Granulations locally amplified bymicrofractures and gouge-slips, at shallowangles, mainly at 20 to 25 degrees tea. Overall weak to moderately chtoritized and silicified.weak to locally strongly carbonated (calcite). White quartz-calcite stringers and veinlets, 2-314, mainly parallel to schistossity, sheared,dismembered. Weak local sericitization alongmargins to veinlets. Pyrite as euhedraldisseminations (0.5 to 5mm), and as fine wispsand occasional blebs, 2"* locally, ^.S1* overall. Pyrrhotite disseminations and occasional stringers, fQ.5% Trace of sphalerite and chalcopyrite within some veins (ie. 1 61 .6 to162.2m).

Ser

C*W"

Silic

CNW

Epi

c*w~

Hem

c\w

Carb

CNW-

other

Accessory Min.

"/o Py

olOi-

Cpy

CsICO

VoQz

oo1-CM

D.2% *2mm dPY,1 3.* 0.2 to 5cm f awvnOZ, l

0.11K0.1mmdPY, 2.H 0.1 to 1cm gwvnQZ,

O.I'i^O.lmmdPY, S.% 0.5 to 10cm wvnQZ,

Q.2% -:0.5mm dPY,2.H 0.1 to 50.1 to1cm gwvnQZ, D.2% dpo.

0.5* *5mm dPY, 4. 1* 0.1 to 2cm gwvnQZ, Q.2% dpo,

Struct.

Struc

shux

sfon

shr

sfol1

shux

shux

< tea

47

55

20

64

55

62

Assay

From (m)

139.0

140.5

142.0

143.0

144.5

1460

147.6

148.0

1490

150.0

151.0

152.5

154.0

155.5

157.0

158.0

159.0

To (m)

140.5

142.0

143.0

144.5

146.0

147.6

148.0

149.0

150.0

151.0

152.5

154.0

155.5

157.0

158.0

159.0

160.5

Sam. #

7741

7742

7743

7744

7745

7746

7747

7748

7749

7750

7751

7752

7753

7754

7755

7756

7757

Au ppb

-5

-5

-5

-5

-5

6

67

13

-5

-5

-5

-5

-5

-5

-5

-5

-5

Au

, s^- S T-

Page: 8 of 13

Diamond Drill Log Sheet

Project: Bristol

0*22^2 Hole: BRSOO-05

f(OQ

-

161 -

\

162 -j

--

163-

164-

--

~~-

165-

-

^

167 -:-.-

i168-

:

169-

---

Lithology

v

V

•v

V

V

l-V

~

From (m)

151.0

163.0

168.5

To (m)

J63,SL

168.5

170.7

Lith code

i

3

1

lithology

mafic\yolcanics—/

felsic volcank

mafic volcanics

text. Comments

...Sheared and altered volcanic. Medium-darkgreenish-grey to grey. Fine-grained, with amygdules up to 0.75cm locally, Infilled by 1 calcite. Moderate to strongly foliated, sheared, llocally schistose, with weak folding or JGranulations. Granulations locally amplified by 1 microfractures and gouge-slips, at shallowangles, mainly at 20 to 25 degrees tea. Overallweak to moderately chloritized and silicified, weak to locally strongly carbonated (calcite).White quartz-calcite stringers and veinlets, 2-3'K, mainly parallel to schistosity, sheared, dismembered. Weak local sericitization along margins to veinlets. Pyrite as euhedral disseminations (0.5 to 5mm), and as fine wisps and occasional blebs, 2* locally, 0.516 overall. Pyrrhotite disseminations andoccasional stringers, O.516. Trace of sphaleritebnd chalcopyrite within some veins (ie. 161 .6 tofl62.2m).

, Tuffaceous. ...Felsic Tuff andHighly Altered Mafic Volcanic)?). Medium greyto medium yellowish green, fine grained,generally very siliceous/sllicified. Some intevals appear to contain abundant very finequartz crystals (felsic tuff?), up to 2mm locally, to locally becoming aphanic and very felsic, but weakly brecciated. Trace of pinhead dark greyquartz-eyes. Weakly foliated, to mainly sheared, with ghostly fragments, and with microfracturesat various angles, infilled by calcite. Whitequartz veining, up to 60cm wide, with veryirregular margins, locally sheared and dismembered to weakly folded. Margins to veins are weakly to strongly sericitized locally. Pyrite disseminated cubes up to 2mm, mainly within the host rock, trace within the veins.Sphalerite trace within the veins, and onepossible seams near 168m.

..Altered volcanic, medium greenish-grey, finegrained, strongly altered, mainly moderate to strongly chloritized and carbonatized, feels greasy, with very weak sericitization near theveins. Fine spherules of carbonate (amygdules?), generally 1-3mm, up to 1016 locally (ie. 1 70.1m), 2* overall, often containfine disseminated pyrite and pyrrhotite. Weak tomoderately foliated, sheared. Pyrite and pyrrhotite, disseminated to wisps and blebs, 1 -216

Alteration

Chl

c\W"

Ser

OW

Silic

CV*

Epi

O-W

Hem

c-w

n

Carb

CvW

other

Accessory Min.

"/o Py

oIOV-

Cpy

CNO

"/o Qz

ooT-(•N

D.5% ^mm dPY.v 4.* 0.1 to 2cm \SwvnQZ. D.2% dpo. l

0.116 O.lmmdPY, 0.1*vnCp, IS.%2 to 6cm wvnQZ, Q.2% dpo, 0.116dsp,

0.516*0.1 mm fPY,2.* 0.2 to 1cmgwvnQZ, Q.2% dpo,

2.14 0.2 to 2cmgwvnQZ, 0.1 ttvnSP,

X.% 70cm wvnQZ, 0.1*vnSP,

O.HteO.SmmdPY,30.* 0.5 to 10cmgwvnQZ, 0.1* vnSP,

1 .0* ":0.5mm wPY, 1.160.2 to 2cm gwvnQZ, 1 .16dpo,

Struct.

Struc

tract

sfoM

sfoll

< tea

18

63

74

Assay

From (m)

159.0

160.5

161.6

1622

163.0

164.7

166.0

166.7

167.9

1685

169.5

To(m)

160.5

161.6

162.2

163.0

164.7

1660

166.7

167.9

168.5

169.5

170.7

Sam. #

7757

7758

7759

7760

7761

7762

7763

7764

7765

7766

7767

Au ppb

-5

-5

9

6

-5

-5

-5

-5

-5

6

-5

Au

, s|- S T-

Diamond Drill Log Sheet

Project: Bristol

CanieCO Hole: BRSOO-05

tVQ

.

1

-

:

-

172-

-~

--

-173-

---

174-

2

175

176 -

}177-

~

178 -

179-

;

Lithology

f

^

From (m)

168.5

170.7

175.0

178.3

To (m)

170.7

175.0

178.3

181.3

Lith code

1

3

3a

3

lithology

mafic\volcanics f

felsic volcanii

rhyolite

felsic volcanic

text. Comments

..Altered volcanic, medium greenish-grey, fine

Alteration

cm

CM*

grained, strongly altered, mainly moderate to j strongly chloritized and carbonatized , feels j greasy, with very weak sericitization near the |lveins. Fine spherules of carbonate II(amygdules?), generally 1 -3mm, up to 1 01* locally (ie. 1 70.1 m), 216 overall, often contain

ifine disseminated pyrite and pyrrhotite. Weak tomoderately foliated, sheared. Pyrite and l pyrrhotite, disseminated to wisps and blebs, 1-2*

, Tuffaceous. ...Felsic Tuff.

change in texture centered on a quartz vein.Medium yellowish-green, fairly homogenous,equigranular (like a well sorted wacke/arenite),fine-grained but with discernible mineralogywhich seems to consist almost entirely of darkgrey quartz grains (IS-20%), within a finer matrixof amourphous silica and sericite. Grey to white quartz veins, irregular, 0.5 to 4-5cm, areaccompanied by weak to moderate epidotizationalong the margins Pyrite trace to Q.25% locally, along margins to the the veins.

...Felsic Flow. Contacts appear transitional.Similar to above unit, medium yellowish-green, very siliceous, aphanitic, with subtle brecciation locally, ghostly, angular, suggesting flow autobrecciation. Foliation very weak, sheared,with chlorite infilling fractures locally.

.Tuffaceous. ...Felsic Tuff. Sameas previously observed between 1 70.7 to1 75.0m. Medium yellowish-green. Homogenous, fine-grained, quartz-rich, very siliceous, weakly sericitic and epidotized (saussuritjzed). Appears weakly foliated and sheared, with minor chlorite infilling fractures. White to greyish-white quanz+y-caTcite stringersand veinlets at various angles. Pyrite disseminations and occasional seams, trace to

Ser

CM*

Silic

CM*

Epi

CM*

Hem

CM*

Carb

CM*

other

Accessory Min.

"/o Py

om*-

"/oCpy

CMTO

"/o Qz

ooi-C\1 .O* ^.5mm

;wPY, 1.* 0.2 to \2cmgwvnQZ, 1.* j

0.21^0.1 mm dPY, 40.* 0.5 to 20cmgwvnQZ,

0 1 Vi ^ 1mm dPY0.5*0.110 1cm gwvnQZ,

01!K0.1mmdPY. 1 .li 0.1 to 1cm gwvnQZ,

0.1 'ft ^.1 mm wPY, 2.* 0.1 to 3cm gwvnQZ,

Struct.

Struc

sfon

<tca

75

Assay

From (m)

169.5

170.7

172.2

173.5

175.0

176.0

177.0

178.3

179.3

To (m)

170.7

172.2

173.5

175.0

176.0

177.0

178.3

179.3

180.3

Sam. #

7767

7768

7769

7770

7771

7772

7773

7774

7775

Au ppb

-5

-5

-5

-5

-S

-5

-5

-5

-5

Au

m- in t-

Diamond Drill Log Sheet

Project: Bristol

CanjeCO Hole: BRSOO-05

tQ. 0)Q

-

182-

—

183-

-

184-^

I

185

--

188-

:187-

188-

—

189-

:

:-

Lithology

s/

V

V

V

V

v

From (m)

1/8.3

181.3

187.7

To (m)

J81i

lo/./

191.2

Lith code

3

3a

1

lithology

felsic volcanh

mafic volcanics

text. Comments

l~. f uffaceous. ...Felsic Tuff. Same

Alteration

Chl

tvw

as previously observed between 170.7 to j 175.0m. Medium yellowish-green. 1 Homogenous, fine-grained, quartz-rich, very n siliceous, weakly sericitic and epldotized l(saussuritized). Appears weakly foliated and sheared, with minor chlorite infilling fractures.

[White to greyish-white quartz+A-calcite stringers and veinlets at various angles. Pyrite

...Felsic flow. Aphanitic, mediumyellowish-green, very siliceous, locally buff-colored and possibly albirJzed. Mostly autobrecciated, with angular lapilll-sizefragments, subtle but preferentially serialized, contained within a matrix of similar composition,

in proximity to veins. Pyrite fine to 1 mm euhedral disseminations, wisps and blebs, Q.2%, within host rock and within veins. Trace ofchalcopyrite, sphalerite, and possibly galena noted within a white quartz vein subparallel tea between 184.5 to 185.0m.

...Altered volcanic. Upper contact sharp but fractured, at 35 degrees tea, accompanied by strong chloritization. Medium-green to dark green, fine-grained, moderate to stronglychloritized and carbonated. Moderatelysilicified locally. Very weak sericitization locally. Foliation moderate, schistose, moderate fractured, occasionally subparallel tea. Possible remnant calcite amygdules locally, ^'to.Quartz-calcite stringers and veinlets, at various angles, mostly sheared parallel to schistosity. Pyrite as coarse euhedral disseminations nearupper ontact, up to 0.7cm in dia. and 516, to fine disseminations and wisps. Overall, trace pyrite.

Ser

C'W

Silic

OW

Epi

c*r

Hem

o*w-

Carb

CV3"

other

Accessory Min.

"XoPy

0lOt^

"/o

Cpy

CNOO

"/o Qz

ooT-CN

01* ^.1mmiwPY, 2.* 0.1 to l \3crn gwvnQZ, 1

0.2* -sO.Smm dPY,2.* 0.1 to 4cmgwvnQZ,

0.2* *0.5mm bPY, 0.1*vnCp, 30.* 20cmwvnQZ,0.1*

10.* 1 to 5cmgwvnQZ,

0.2* O.Smm dPY,2.* 0.5 to 1cmgwvnQZ,

0.1*0.1mnKx •slmmdPY, 2.* 0.2 to 1cm gwvnQZ,

Struct.

Struc

sfon

sfon

fract

< tea

75

51

30

0

Assay

From (m)

179.3

180.3

181.3

182.5

183.5

184.5

185.0

186.2

187.7

189.0

To (m)

180.3

181.3

182.5

1835

184.5

185.0

186.2

187.7

189.0

190.0

Sam. #

7775

7776

7777

7778

7779

7780

7781

7782

7783

7784

Au ppb

-5

-5

-5

-5

-5

-5

10

-5

-5

-5

Au

j s|- S r

Diamond Drill Log Sheet

Project: Bristol

CajSSSS Hole: BRSOO-05

I

o

~

191-

-j

-

192

i193

-~-

-

195-

196-

-

-~^

197-

;

198-

,

199-

:

Lithology

^v

v

VX. ,

V

li

33^f^~r~ -"^ —

.j- -jr~r

g-^-^^~^^r^

3H^-H-E

B

From (m)

187.7

191.2

192.1

195.0

To (m)

191.2

192.1

195.0

208.0

Lith code

i

6

3

tt

lithology

mafic\volcanics J

mafic intrusive

felsic voleank

volcanic schist

text. Comments

...Altered volcanic. Upper contact sharp butl fractured, at 35 degrees tea, accompanied by | strong chloritization. Medium-green to dark

green, fine-grained, moderate to strongly l chloritized and carbonaHzed. Moderately

Alteration

cm

CNHf

silicified locally. Very weak sericitization locally. Foliation moderate, schistose, moderatefractured, occasionally subparallel tea. Possible

Quartz-calcite stringers and veinlets, at various angles, mostly sheared parallel to schistosity. Pyrite as coarse euhedral disseminations near upper ontact, up to 0.7cm in dla. and 516, to fine{disseminations and wisps. Overall, trace pyrite. 1

58 degrees, lower contact at 40 degrees tea. Light grey and aphanitic (chilled, and identical 1 to previously described mafic dykes further 1

l uphole), to dark grey/black and very fine grained j to aphanitic. Calcic-feldspar glomeroporphs, i 216, up to 1 .5cm, subhedral to euhedral, lightgreen, completely saussuritized. Very weakly jmagnetic. Massive, non-foliated, but withmicrofractures infilled by calcite. Moderatepervasive calcite alteration as well. No sulphides doted. l, Tuffaceous. ..As previouslydescribed tuffaceous felsic units. Mediumyellowish-green, bleached across the upper half (epidotized) by the presence of very irregular white quartz veining. Lower half of interval is generally finer grained, more greyish, but stillvery siliceous, very hard.

, Massive amygdaloidal flow...Altered and foliated. Upper contact sharp,fractured, at 66 degrees tea. Medium to darkgreenish-grey, moderate to strongly foliated,schistose, at 61 degrees tea. White calciticamygdules throughout, 1-216, flattened/stretched. Fine grained, withdisseminated magnetite up to 0.5mm locally (ie. 205.5m). Quartz-calcite stringers mainly, minor veinlets, predominantly parallel to the schistossity. sheared, dismembered, weaklyfolded. Moderate to strongly chloritic, locallysiliceous, moderate to strongly carbonatized.locally speckled by carbonate (calcite). Pyrite fine disseminated to 1 -2mm euhedral cubes, andas fine wisps, 1-316 locally. 116 overall.

Ser

OW

Silic

c*w

Epi

o^

Hem

CM*

Carb

CNW

other

Accessory Min.

"/o Py

oUVr-

"/O

Cpy

CNCO

"/o QZ

ooT-CV

0 116 0 1mnrK x^ImmdPY, 2.* ! \0.2 to 1 cm gwvnQZ, 1

0.216 0.1 mm* x •dmmwPY, 25.16 0.2 to 20cm wvnQZ,

D.2% -:0.5mm wPY, 2.160.2to 1cm gwvnQZ,

wPY, 2.16 0.1 to ScmwvnQZ,

Struct.

Struc

shux

cont

^ca

48

-56-

15

66

Assay

From (m)

190.0

191.2

192.1

193.6

195.1

196.5

198.0

199.5

To (m)

191.2

192.1

193.6

195.1

196.5

198.0

199.5

2010

Sam. #

7785

7786

7787

7788

7789

7790

7791

7792

Au ppb

-5

-5

-5

-5

13

5

-5

5

Au

, g|- in T-

Diamond Drill Log Sheet

Project: Bristol

CagJSSS Hole: BRSOO-05

flQ

^

Z201-

-

202 -S

203~

204 -Ei-

205 -

206^

207 -i

208-

209^r-

210H

211-

212-j

213^

214^

215-;

216^

217-;I

218 -:

219-j~^

Lithology

--—:"^-^p- -Tl-Z

1— -

fi

^~z^-r

JH

f]

^i

fi3-T

"-

v

N"

V'~

V

V

v

V

V

^J

'~

V

V

V

\r

From (m)

195.0

2080

213.5

To (m)

208.0

213.5

220.8

Lith code

j* .j

i

i

lithology

mafic\ volcanic jWhist 1

mafic volcanics

mafic volcanics

text. Comments

, Massive amvodaloidal flow.

Alteration

Chl

CM*

1 ...Altered and foliated. Upper contact sharp, ll fractured, at 66 degrees tea. Medium to dark JI greenish-grey, moderate to strongly foliated, l

schistose, at 61 degrees tea. White calcitic \amygdules throughout, T-2%, flattened/stretched. Fine grained, with , disseminated magnetite up to 0.5mm locally (re 205.5m). Quartz-calcite stnngers mainly, minor

1 1 veinlets. predominantly parallel to the lschistossity, sheared, dismembered, weakly folded. Moderate to strongly chloritic, locally siliceous, moderate to strongly carbonatized, locally speckled by carbonate (calcite). Pyrite J nne disseminated to 1-2mm euhedral cubes, and.ks fine wisps, 1-31i locally. 1* overall. i

.Massive flow. ...Transitionalcontact, arbitrarily selected. Rock is mediumgreyish-green to dark green, distinct by an overall decrease in foliation/schistossity, tomoderate, accompanied by the absence of amygdules and by the presence of abundant very fine leucoxene. Still weak to moderatelychloritic, moderately carbonatized. Quartz-calcite stringers still sheared, disrupted, irregular. Pyrite as fine wisps, and occasionalstnngers, D.3%.

, Massive amygdaloidal flow. ...Contact arbitrarily selected. Medium greyish green, very fine-grained to aphanitic. Leucoxene essentially absent. Calcitic amygdules, 0.5cm, 116. Calcite-quartz stringers sheared, dismembered. Weak to moderately chloritic.moderate to strongly carbonatized (calcite). Pyrite fine disseminated and fine wisps.occasional blebs. C.2%.

Ser

CNM-

Silic

CM*

Epi

CM*

Hem

CM*

Carb

CM*

other

Accessory Min.

"/o Py

olOi-

o/o

Cpy

CMCO

"XoQz

ooT-CM

\wPY, 2.16 0.1 to ;\6crn wvnQZ. l

.

0.3K, •cO.Smm wPY.

0.2* ^ 5mm wPY, 1.H0.1 to 0.5cm wvnQZ,

Struct.

Struc

shux

shux

shux

sfol1

sfoll

< tea

61

75

70

59

61

Assay

From (m)

199.5

201.0

202.5

204.0

205.5

207.0

208.0

2195

To (m)

201.0

2025

204.0

205.5

207.0

208.0

209.5

220.8

Sam. #

7792

7793

7794

7795

7796

7797

7798

7799

Au ppb

5

-5

•5

-5

-5

-5

-5

-5

Au

l li- 5? T-

Page: 11 of 13

Diamond Drill Log Sheet

Project: Bristol

CatngCO Hole: BRSOO-05"E

t0)D

iT

221-

222--

223-[

224-4^

225-

r226~

—

227 -E

228 -E

230 -Ej;

231 ~

^

232-:

233^

~i

235-^

236-;

237-!

238^

239 J

Lithology

^

s,

ki*

•^V

V"

x ;

V

v,

V

\x

]-

V

^

•v

v

v

v

v

^

^

V

^V

f

From (m)

213.5

220.8

221.6

222.1

77d g

225.1

To (m)

220.8

221.6

222.1

224.9

.77S 1 .

242.5

Lith code

i

i10

1

6

1

lithology

mafic\yolcanics_y

mafic volcanicsquartz vein

mafic volcanics

mafic volcanics

text. Comments

, Massive amyadaloidal flow....Contact arbitrarily selected. Medium greyish

| green, very fine-grained to aphanitic. Leucoxeneessentially absent. Calcitic amygdules, 0.5cm, 1 *. Calcrte-quartz stringers sheared, dismembered. Weak to moderately chloritic,

l moderate to strongly carbonated (calcite), j Pyrite fine disseminated and fine wisps,Iloccasional blebs, 0.2*. l| , Massive flow. ...Upper contact 1 selected due to aprupt appearance of abundant J leucoxene (5*). Moderately foliated, at 59 1 (degrees tea. Fine-grained, moderately l Ichloritjzed, strongly carbonated (calcite). j Pyrite fine disseminated to wispy, essentially a l

Alteration

Chl

CM*

'

(trace. Less than 1*auartz-calcite stringers. 1[...Quartz Vein. Massive, bull white, with sharp L

1 but irregular contacts at 48 degrees tea. Barren. 1 jII , Massive flow. ...Same as previously 1l observed immediately above the quartz vein. (1i Weakly blocky core. Moderate to weakly foliated J Less than 1* quartz-calcite-epidote stringers. J(Trace of fine disseminated pyrite |{...Mafic/Diabase Dyke. Very irregular contacts, i |tsubparallel tea. Chilled. l

.Massive flow. ...Gabbroic. Same aspreviously described above the diabase dyke. Generally very weakly foliated, massive,relatively featureless. Fine-grained, medium-green, with abundant leucoxene, anddiscernible feldspar (greenish, epidotized). Generally weakly chloritic, weakly carbonated (calcite). Minor chlorite infilling fractures. Quartz-calcite-tV-epidote*7-trace hematite, atvarious angles, *i *. Narrow epidotization along the margins of some veins, others weaklychloritic margins. Pyrite fine disseminated, to coarser euhedral cubes (2 -3mm), andoccasional wisps, blebs, and stringers, onlyobserved within the host rock. Overall trace to0.2*.

Ser

CM*

Silic

CM*

Epi

f^W

Hem

CM*

Carb

CM*

other

Accessory Min.

"/o Py

o

"/o

Cpy

CMTO

"/O QZ

00T-CN

0.2* •cO.Smm\wPY, 1.* 0.1 to y \0.5cm wvnQZ. 10.1* •cO.lmm wPY, 0.2*0.1 to

0.1*t0.1 mm dPY,

0.2*0.1mrrKx *1mmdPY, 0.1*

Struct.

Struc

sfon

< tea

-ei —

61

Assay

From (m)

219.5

220.8

221.6

222.1

To (m)

220.8

221.6

222.1

2236

Sam. #

7799

7800

7801

7802

Au ppb

i-5

-5

-5

5

Au

j a|- IO T-

Page: 12 of 13

Diamond Drill Log Sheet

Project: BristolCameco Hoie: BRSOO-OS

"E

1

241 -j;

242-^

243-

244 -i

245^^

246^

^

247 H

248-

249^--

250-1'i

25t~

2

252 -

253^

255-

256-;

257-

258;f

259 -

Lithology

V

,-;\s

V

v

V

v

v

•v

"-

V

~

V

From (m)

225.1

242.5

To (m)

242.5

254.0

Lith code

i

i

lithology

mafic\yolcanics _ /'

mafic volcanics

text. Comments

.Massive flow. ...Gabbroic. Same asj previously described above the diabase dyke.

Generally very weakly foliated, massive, relatively featureless. Fine-grained,

l! medium-areen. with abundant leucoxene, anddiscernible feldspar (greenish, epidotized). Generally weakly chloritic, weakly carbonatized (calcite). Minor chlorite infilling fractures.

j Quartz-calcite*V-epidote*Atrace hematite, at i various angles, ^ 'ft. Narrow epidotization along the margins of some veins, others weakly chloritic margins. Pyrite fine disseminated, to coarser euhedral cubes (2-3mm), and occasional wisps, blebs, and stringers, only observed within the host rock. Overall trace to D.2%.

, Massive pillowed flow. ...Uppercontact arbitrarily selected, coincident with abrupt change in grain-size and nearly absence of leucoxene following a fracture. Medium green, finer-grained, with subtle possible chloritic toepidotized pillow rims. Also possibly autobrecciated, very subtle. Weak to moderately foliated, at 62 degrees tea. Contains less than 1 *tt) quartz-calcite stringers, excluding an interval of about 5016 bull whitequartz*Acalcite veining from 246 to 248m. Pyrite fine disseminated to euhedral cubes1-3mm, and as wisps and occasional blebs.

Alteration

Chl

CN|^

-

Ser

CNW"

Silic

CNN"

Epi

CNW

Hem

CNN"

-

Carb

P"W

other

Accessory Min.

"/oPy

01OT-

"/o

Cpy

CNCO

"/o QZ

ooT-tV

— -^

0.21t0.1mnrKxi^mmdPY, 0.1* ; \0.1 to 2cm wynQZ,^

D.3% ^mm bPY, Q.5% 0.1 to 1cm

SO.% 1 to 40cm wvnQZ,

Q.5% <2mm dPY.D.3% 02 to 1cmwvnQZ,

Struct.

Struc

sfoM

sfoll

< tea

51

51

Assay

From (m)

244.5

246.0

247.0

2480

To (m)

246.0

247.0

248.0

2495

Sam. #

7803

7804

7805

7806

Au ppb

-5

-5

-5

-5

Au

, si- UJ T-

Page: 13 of 13

APPENDIX 2

Gold Assay and ICP Certificates for all Analyses

Cameco Gold Inc. Bristol and Bristol North Projects Report on the Fall 2000 Diamond Drilling Program

CHIIV1ITEC BOIMDAR CLEGG

JTiso^oeVv®J Rapport Lab Geocnimie——________Geochemical Lab Report

+

o< o

Q

U 2 :*fcOO Oi

Chimitec - Bondar Clegg, 1322-B Harricana, Val-d'Or, Quebec, J9P 3X6, Tel: (819) 825-0178, Fax: (819) 825-0256

CHIIVIITEC BOIMDAR CLEGG

Rapport Lab Geochimie Geochemical Lab Report

REPORT: TOO-57472.0 ( COMPLETE )

CLIENT: CAMECO GOLD INC.

PROJECT: BRISTOL

REFERENCE: i

SUBMITTED BY: P. COAD \ DATE RECEIVED: 01-DEC-OO DATE PRINTED: 11 -DEC-00 \

DATE APPROVED ELEMENT .,-t-

NUMBER OFAUAI VCCC

001207 1 Au30001207 2 Ag001207 3 Cu001207 4 Pb001207 5 Zn001207 6 Mo

001207 7 Ni001207 8 Co001207 9 Cd001207 10 Bi001207 11 As001207 12 Sb

001207 13 Fe001207 14 Mn001207 15 TE001207 16 Ba001207 17 Cr001207 18 V

001207 19 Sn001207 20 W001207 21 La001207 22 Al001207 23 Mg001207 24 Ca

001207 25 Na001207 26 K001207 27 Sr001207 28 Y001207 29 Ga001207 30 Li

001207 31 Nb001207 32 Se001207 33 Ta001207 34 Ti001207 35 Zr

i 001207 36 S

GoldAg -Cu -Pb -Zn -Mo -

Ni -Co -Cd -Bi -As -Sb -

Fe -Mn -Te -Ba -Cr -V -

Sn -W -La -Al -Mg -Ca -

Na -K -Sr -Y -Ga -Li -

Nb -Se -Ta -Ti -Zr -S -

IC01IC01IC01IC01IC01

IC01IC01IC01IC01IC01IC01

IC01IC01IC01IC01IC01

IC01

IC01IC01IC01IC01IC01IC01

IC01IC01IC01

IC01IC01IC01

IC01IC01IC01IC01IC01

IC01

757575757575

757575757575

757575757575

757575757575

757575757575

757575757575

LOWER DETECTION

50.2

1211

11

0.2555

0.011

10111

2020

10.010.010.01

0.010.01

1121

1510

0.0101

0.01

PPBPPMPPMPPMPPMPPM

PPMPPMPPMPPMPPMPPM

PCTPPMPPMPPMPPMPPM

PPMPPMPPMPCTPCTPCT

PCTPCTPPMPPMPPMPPM

PPMPPMPPMPCTPPMPCT

EXTRACTION

Fire Assay of 30gHCL:HN03HCL:HN03HCL:HN03HCL:HN03HCL:HN03

HCL:HN03HCL:HN03HCL:HN03HCL:HN03HCL:HN03HCL:HN03

HCL:HN03HCL:HN03HCL:HN03HCL:HN03KCL:HN03HCL:HN03

HCL:HN03HCL:HN03HCL:HN03HCL:HN03HCL:HN03HCL:HN03

HCL:HN03HCL:HN03HCL:HN03HCL:HN03HCL:HN03HCL:HN03

HCL:HN03HCL:HN03HCL:HN03HCL:HN03HCL:HN03HCL:HN03

(3(3(3(3(3

(3(3(3(3(3(3

(3(3(3(3(3(3

(3(3(3(3(3(3

(3(3(3(3(3(3

(3(3(3(3(3(3

:1):1):1):1):1)

:1):1):1):1):1):1)

:1):1):1):1):1):1)

:1):1):1):1):1):1)

:1):1):1):1):1):1)

:1):1):1):1):1):1)

METHODl SAMPLE TYPES NUMBER SIZE FRACTIONS NUMBER SAMPLE PREPARATIONS NUMBER

i DRILL CORE 75-150 75 CRUSH, SPLIT 75 i30g Fire Assay - AA PULVERIZATION 75 iINDUC.INDUC.INDUC.INDUC.INDUC.

INDUC.INDUC.INDUC.INDUC.INDUC.INDUC.

INDUC.INDUC.INDUC.INDUC.INDUC.INDUC.

INDUC.INDUC.INDUC.INDUC.INDUC.INDUC.

INDUC.INDUC.INDUC.INDUC.INDUC.INDUC.

INDUC.INDUC.INDUC.INDUC.INDUC.INDUC.

COUP.COUP.COUP.COUP.COUP.

COUP.COUP.COUP.COUP.COUP.COUP.

COUP.COUP.COUP.COUP.COUP.COUP.

COUP.COUP.COUP.COUP.COUP.COUP.

COUP.COUP.COUP.COUP.COUP.COUP.

COUP.COUP.COUP.COUP.COUP.COUP.

PLASMA OVERWEIGHT 23 :PLASMA :-PLASMA iPLASMA REPORT COPIES TO: MIKE KOZIOL INVOICE TO: MIKE KOZIOL !PLASMA i

PLASMA This report must not be reproduced except in full. The data presented in this iPLASMA report is specific to those samples identified under "Sample Nuifcer" and is ;PLASMA applicable only to the samples as received expressed on a dry basis unless iPLASMA otherwise indicated ir un^nn :

PLASMA :

PLASMA !PLASMA iPLASMA iPLASMA iPLASMA :PLASMA i

PLASMA ' iPLASMA iPLASMA iPLASMA iPLASMA iPLASMA :

PLASMA !PLASMA iPLASMA :PLASMA iPLASMA iPLASMA ;

PLASMA :PLASMA iPLASMA iPLASMA iPLASMA iPLASMA i

Chimitec - Bondar Clegg, 1322-B Harricana, Val-d'Or, Quebec, J9P 3X6, Tel: (819) 825-0178, Fax: (819) 825-0256

BONDAR CLEGG

Rapport Lab Geochimie Geochemical Lab Report~- - - -- - - •'-~ ~ -- - -- - - - -IT -- —-

CLIENT: CAMECO GOLD INC.

REPORT: TOO-57472.0 ( COMPLETE )

SAMPLE

NUMBER

326327

328

329

330

331

332333334335

336

337338

339

340

341

342

343

344

345

346

347348349

350

351352

353

354

355

ELEMENT Au50 Ag;; Cu

UNITS PPB PPH PPM

; : :HO-;: NI ;;;;cs;:; ea ;:;B|| AS sSbjPl?M PPM Pf-H PPM PPM l PPM PPM!

^ i:2

170 i. 2 1

8 M*5 s2*5 fi4 H<5 *.'2; :<5 ^.2<5 *.2

*5 *fr

*5 IS*5 *-2|-

7 ".2<5 e-; :2- ;

<5 *:,2

8 i*.?!<5 *.2

9 *iZ\9 ^2

<5 ^2

*5 ^210 ^-2

7 <.26 * 2

8 ^.2

9 <.2

7 5, 2

9 -:.2

<5 ci! 2-

^ ^2

97

96

41

94

90

l 81

l 75

83

85

83

79

78

40

32

62

117

83

104

34

34

33

35

40

6

99

95

95

80

93

84

--! 5! : ,I'll 3'.|.

!!4 : :-l; 4;.

|||

illiii'4'll

lll'Sl : : ;|: 3:|;l;|4|

ISl|:' : "4|;!-?' :::. g ;.

'-': 5|

si-:;6;l!!?!Us:||6;

; 6 : |:..5,,-.j-

:x2l

4

3:l; : -3l: -'2

yi.4

68

61

72

75

72

ITI5959

68

71

68

68

130

187

190

147119

151

156149

162164

118

19

;l 81

64

94

50

70

62

il|125

i*:l!l39

S! 127

111:104

111 138

!|*I|172

1*1:2141 240

*1 208

;!;!tii9i

ixl||l74

I|xi||l69

||*i|| 10 :Vf: : : 3:: 5l|; 8

l!:|i::; 19;xi;;; 16

r 17xxiv. 2;xis 2

:xi ; : : 2Xl: 2

d 120

: :: ;;2J 29

l 2 145

*1 147 i i 149xl 143

1148xl 141

; io' :38

!38;i4i;;i;43l

IP!4o:|42

:|;42|

||

ill;I-37:24 li!^i;

illIII:|:3|:V3l|;;

0.0.

0.

0.

llo-

3

3

4

3

2

;o.3|o.0.

lo.lo.

|o.lo.0.

;|o.l0 -

i : o.

;;o.; ; o.lo.

6

33

3

44

4

4

5

5

45

4

3110.4

3?3136

l!-?!MI46: : l43;44

l. '43 1

40

0.

0.

0.x. '0.

0.

0.0.

4

4

4

2

5

3

4

30.3

0.3

76

95104

55

DATE RECEIVED: 01-DEC-OO DATE PRINTED: 11-DEC-OO

PROJECT: BRISTOL

PAGE 1 OF 3

Fe :;;|M|i;i TE

PCT upllHpPM

Cr

PPM

55 6.93

If! 6.06 l

*| 6.86 99^x10

1x5 7.17 126^ X10Wti 7.76 """"""""

7.267.30 128310

29

6

11

28

23

6

12 010.00 2206"^0 7;

2009*10 :

8 xSJxIO.OO 1988 X10

5 x5 ^10.00 1659 x1058 x5 l 9.53 1578x10

35 x5 1.84 372vx10

lv?: Sn III La illlll Mg Illllal Na ||||| Sr |j;|| Ga i|l; Nb ||p Ta Illl;; Zr l|i;l||pH;l;ppM ^IPPM lltf!; PCT llrcrl PCT I!W||;|PPM HH|PPM iiippM pliil^PM ilpJiifiippM l;:l||l|l|

xs: 7.79 1130x1o ; 7;; 170 ;x5 ; 7.01 11(5611^10 ; l 7| 193 l

xSI 7.63 13831^10 ;!iQl:l: 2191x5 8.24 1166x10 iloB'!:; 106 :

l;iil;;| 6.22 l^lMo Ilif l; 2251

2 2!3|;3.713 |^!3.30 3 3:61 3.55

1 Pip2| 55 pp ip||! 60 I||iblHH 52 ii

328 97 ^0 ^20 278 92 x20 *20 318 105 x20 520 ; 254 595 x20 ^?0;

2 4:53 3.722 5i22 4.303 4.31 2.87

6.89:0.02 ^iOI

l 5i60J0.04 ip|

55 l 41 l

38

53l;:;: 229 | 4 11:2.57

231 92:^20 ^0 '

272 126 x20 *20

41 : 8 *20 ^0-i 40 49 ^20 ^Oi:

5157663847

3 5.11 4.396 3.91 1.21

8 4|il 1.26

10 3MI: 1 -41

5 !Jsll|l:|l .85

5^62 0.03 Iff

41 ^0 -4.Q 'i 4 2;15 2.22 41:22 0.07

47 45 x20 -?2040 66 ^0 "^20

167 67 ^0 ^0

275 17x20 ^20

5 2,26 2.30 5 4i02 2.57 3 3.35 3.54 1 0;38 0.85

3,4(S 0.09 pjp| l 69

;;3ili|| :0.05 ^p|l|i| 59

4,89 0.07 6;03l 66

1^94 0.03 0;P3 2380 x5 8.53 1273x10 116 256 68x20 2 3.02 3.90 5^67 0.07 OiOJI 58

185 x5 7.80 1328i'^10

151 xS 8.15 117^11^10

182 *5 6.12 1232x10

30 *5 7.05 :J207:X10

91 38 x20 ^0

135 57 x20 ^20|l;78 22 x20 ^0

157 58x20 xZ'O'l;

3 1:39 3.25

2 2i:i|l:3.253 0^82 2.47 2 2;i1 3.45

8,02 0.11 0.03;!;; 56

7M |0.11 ppi! 39 7:32 0.09 biP2 | 43

868

10

lias 111x10

;;22| 5 ;:;;;i7;;xio ^pti2 !Ii!3.38 |l3Mij0.03 lill 42 111 m 4 sisii

lip *21Ip 7;Illl 111 Hi!; 11 i

j.os mm 37 in

Ip 6 i;i:|;|xio mm..iil s i|i*io in!:;;;32j| 6 ||||!|^10 ^pjjjIlil 5 lliho 1111

1 39 111 67 Illl40 ill47 HI

IB! 5

SS

oil:

111!

Ill

lil!

lil!132022

:;p lill

lil i9 laei

ipxio iiaii ;;:Zl;;;;xio ipi^s <1 oifl5: ; ; ;|ll||l|x10 |||| 15 pll|i|Nio IIHI 6 IHl li;i;xio lill 4 ill!

65 lip 16 Ip 12 i|;;x10 :i||;: *:1 |j||i 81 |||! 13 III! 9 fffihlO lUll: <1 pllil 92 Illl 15 1|| 12 llf;Mo |||ll| <1 iff| 86 il|| 23 Illl 2 |H:X10 Iliill 3 Pl|1a|89 nip 14 isiisi <1 ;;;;:ii;;xio s^oits 2 fi^;i^';;;

152212

If |i 1 |i|;xio ^p|;; 3 pi;i|;;'itjf. 2 Hiils^io ipiti:;;; 3 diii;;;26 3 16 xlO .020 1 0.26

3;; <1 x5 *io *^bl; 1 0:014 I3;xio *.c

6.09:

0.16;!

x5 7.41 1073:*10 J 271 138 x20 *20 : 3 5^63:5.02 5,47;0.02 ^01:1 59 l|;5 11

Chimitec - Bondar Clegg, 1322-B Harricana, Val-d'Or, Quebec, J9P 3X6, Tel: (819) 825-0178, Fax: (819) 825-0256

CHIIV1ITEC BONDAR CLEGG

Rapport Lab Geochimie Geochemical LabJRepqrt

CLIENT: CAMECO GOLD INC.

REPORT: TOO- 57472.0 ( COMPLETE )

SAMPLE

NUMBER

356

357

358

359

360

361

362

363

364

365

366

367

368

369

370

371

372

373

374

375

376

377

378

379

380

381

382

383

384

385

ELEMENT AU50

UNITS PPB

*5

^

^

^"5

,5•tS

^<5

<5

14

^

<5

<5

<5

*5<5

7

<5

5

4<5

<5

<5

6

^

<5

<5

<5

<5

A?J Cu

PPM PPM

*.2 98

^2. 34

*,2 87

^2 89

5.2 77

12:135^2'- 92

tt 98

i. 2 92

tt. 91

<.2 68

^.2 24

<.2 56

tt: 67

5.2 77

tt ntt 78

*;2 77

^.2 73

tt 71

<.2 63

*.2 78

<.2 84

tt: 85

i. 2 79

< .2 78

f. 2 78

5.2 72

<.2 86

5.2 79

Pt*

PPM- -- :

5

3

5 x2;l*2':

li*;X2:

M.W.;

It;;: :#

2

x2:; : ;3 :y :3

1-4.

:p: l:4:

: ;V:5 : .

H,f4|; 6

4

x2

5

4l's:-5

4

3

Zn Mo

PPM PPM

73 x i

38 2

71 x1

63 ci;

59 IT

69 2

63 xi;

53 .Xi:

43 ;; ;x1:

47 ;.xi

106 :i64 1

58 1

59 xi

67 xi

69 x'i

109 x1

115 1

109 *:1

97 l

85 xi

83 xl

72 'il

74 *r72 li

69 ^1

66 i1

76 il

72 x1

75 x1

Ni

PPM

122

58

143

126

120

141

121

126

111

108

110

18

366

327

475

:195

29

26

28

106

114

143

175

175

167

179

167

192

166

177

|c|: cd nilPPM PPM PPM;

; : ;42|:0.3 "iSl:18 0.8 x5

: 44 0.3 ;4;^4 0.3 :|5"i

v*l|;o-3 'M

111!0 - 2 W.1^2: 0.3 ;;x5!;;42lx.2 ':iS::;;;37|o.2 lisli/lo.2 II

37 0.2 :x5|

14 x. 2 iS

47 0.2 ,x5|

46; 0.3 :x5;

; sf |0.4 ~JJS?

40-0.3 ml;30l:0.3 liS;l2?!0 - 2 '*5 ;; 31 0.3 : : ^5;;:34 P.3 :;isl

37:0.3 :x5;:38|o.3 ^5;:41 0.3 X5

43:0.2 x5

41 0.2 -55

41 0.3 x5

37 0.3 : : *5;

42 0.3 :"W

38 0.3 x5: -

39 0.3 '. eS.

AS mPPM PP^

67 -i!

39 x5

79 x5

11 ;;;-S20 ;;;i;

18 x*

9 -.311 ^

13 |*S9 '^

9 f*S^ ^*5 x;36 ;::*s

153 o:*;

20 x!*5 li*5 ^ l*?^ p^ xi

*5 ^

5 ^^ -c!

^5 -^I

^5 /"*!

^ ^21 x;21 :-e!

7 V

15 x1

):;; Fe

i PCT

8.05

i 3.89

i 7.60

6.58

5.69

Jl 7.52

. 6.82

; 5.16

i 3.99

i| 4.44

- 7.95

il 4.52

. 5.31

' 6.41

i 7.69

i 7.48

i; 9.19

i: 8.56

1 9 -53

i 7.78

i: 7.90

il 7.78

i 7.36

ivi 7.41

i 6.82

i 6.43

i 6.88

;; 7.9ij 7.86

5 7.81

iK TE: pf*i;ppM

1129x10

723x10

1118;x10

;ip7B;:xio i486;;^io

HLoiiiplxio6931*10

;;:;56|;;x10H!*10;: ::9l:"*ip378x10

751x10:95|;::xios*10iil(*io15|6|x10

ISpKXlO

i4d|;:;xioS*101166 xlO1061x101022^10tiirxip1126x10

1077x101P25;;<101200x101305x101253 X10

DATE RECEIVED: 01-DEC-OO DATE PRINTED: 11-DEC-OO

Ba"Si3.:16

27: :;l : 3l

W:

m Is-:

i?;:PS 1!

||'l4 : ;:vT.

;;;5':

31wl?;:

;;ii;;: IS::

II;i4|I'i;

3|: 3;

2;

3.1.5- :;'4:

12

16

Cr |y

PPM PPM

254 104

253 30

209 61

210 ; 92207 W

245 194:

209109

164 59

145 1^5;161 56

252 113111 35968 52619 M

1102 g

275 114

49 15*

51 138so ;|i|

153 |77

136 74

250 119

266 117

272 98

243 76

259 74

263 100

285 120

256 107

275 ;98

sn ||u;;ppMfi^;;

<20 x20

<20 ^0

*20 ^o^0 i2P<20 i2P

^2P *2P :

^0 ^0 :

K20 *i20 ;

K2P x?6;;

<20 ^Q:

*20 "&Q<2P x2P ;

^o ^P:;K20 x2b

^0 x20

;^o x2p:^0 :^20 :x20 i2P: *20 ^26-:

x2o x2b:

*2o M;x20 ^20:;<20 ^2Px20 x20<20 x20

<2o :*2p:x20 x2(j

t20 -520

<20 ^0

<20 ^P

La : All Mg

PPM pqf PCT

2 3^66 4.53

2 1.25 2.28

3 3.73 4.53

1 4.|4;3.682 3;2?|2.59

2 483.991 4;|i: 4.271 3^3513.19

<1 |J68|2.231 Wi2 '*66 3153 2.13

9 1.47 0.40

1 4.54 4.95

2 S.,94 5.71

2 5-i3 6.91

3 |i96 5.23

7 3^69:1.88

8 &&J '"1 .72

9 SM 2.02

63H2ll.46

63;62 1.37

4 5^00 3.65

3 5.55 4.69

2 5.52 4.65

2 4^97 4.36

1 4.49 3.92

3 5.1 1; 4. 19

3 5.48 3.96

2 4194 3.56

3 5;31 4.01

SiCai-y Na

IIS f"07\v! : : : : : ! : : : : : :v'v'v

: 5154-0.044,33|0.02

;:|;5;:9i;i;p.P3;;;|5;;27;::p.02Hplb.oi

!iill.p21:^^10.03Ii|lo.04;li85::p.P4iifflp-03|l||;;b.o4

2.45 0.08

i.830.01

;;5.5P;P.P2

li|;r-01SH!p.p2|l5l34l;p.P4!;:5i45];b.o3i:iS;|S;i:b.P3III';0 - 03

l :7'-isjb.o74;72;0.024. 62 P. 02

: 5i24 0.01; 5.47;-?. 01

5.070.01

5:97:0.03

6,62:0.02

7I2S|0.02

6.70 0.01

nil spliillppM

olosl soP^.07 45

plii! 46IS; 34111 47

**0i;l 36^sp;li; 26ill 24Illl 32

ill ̂ill 68^0|| 34^Pil 44ilPis 68

PiP2^ 82illlil *6llll 46

Oilil 46

0.06 46

01061 63

llll 58

Sc|0'i| 38

' Oil 36

I'Oil 46

^fiil; 53

*.01 1 58

pM;;; 39

**6|| 34

PPI 25

p^ei 26

Hiii.PI111:•:::Z

i:3;III

liIIIIII111ill111:18lilil111111inIIIlilHiillla:: : :"6'.',-'.'s.::|3;

I.. 2; :V5-

v.yfi1

MW

PROJECT: BRISTOL i

PAGE 2

i Ga 111

PPM ill

: 10 ! 273 IM

\ 8 W:

; ^ |i|i *2 III

i -52 li;: ^ ;||

i *2 11

i *2 lil

! * II;

; /III; 7 IIIi ^ 11: 10 148;: 9;;||

: 11 :|i:; 16 ;;il; is :;||; 16 ||j|:

\ 11 W,: 11 lil

: 1 2 W.

: 8 ;;;4i;: 2 W

52 21

1 ^ lii: 11 38: 12 s39.:: 11 Ir**! 11 38

OF 3 ;

Nb

PPM

6; i

2

5

; 3

5; 7; 3: 2; 3

; 7

2

; 2: 4; s

i 7; 11

9

; s; 4

3

7

7

5

4

4

6

8

7

6

: , : :^jj*: : : ; Tn : : . : .9V-.-:-. la

DOM DDUrfTI : : -r m

: 14x10

i^ixlO

:::6 : x10

;::^S x10

lUl^io

S^SftXlOH^iXlO

IllH0iiiiNiolilHoIINo|?if: :^iol*5;;;xio :il:ir*10

lilHo

IliHo:|i;xipII;Hoiil;Nio;1P;x10

liiHo: : : : i : .:- :;: -~

; 16 x10

15| *10

;;io|xios^r^io

'*5':*10

i5;xioi8:x10

Iw'^io; 12 *io

111 Zr l||;O/'T -'DOU ' 'Df*T' : ' :

, : . F\r |.' : :rrn :i'-f: v i Y:'

ii01 <1 Ow05

liai.1 <1 p;p5l iziRsl <1 pip?;1 :|25l <1 0l2i|

IllH <1 pl;i:i3ai; <1 01011IIHI -51 ill;lil;: -d lilllil;;; ^ i||;

lil 2 111p| 15 P|02; ;:;

SPlp: <1 0;03:

''' : : : :-:': : :':': : : ':\ : :-:-:': : :';V l',-;-'-.''-'- 1 ' 1 - 11 : : : : . : : ; : : : : x : : : : -

lill <1 i|l|IHll 4 llll;sp||l s pW;;103^1 6 plP9| i;0i: ; : ;; <1 0^:14::;.v.;:-.'/:' .l-.' :-: : : : : : : : ::: : : :';:

:i : S ::';KJ S'SffiiH

ss;0t| 4 0.14;:;;S0j:7|; <1 oifl6; ::,102 <1 P.P5;i23p| <1 (D^PSlv239 *1 P.06

.199| <1 P. 15*:.01 <1 0.08:-: : : : .;-:;:.S. V.v -S.v : ' :

;.03i: <1 6.20;;;bl6 <1 pila:

Chimitec - Bonder Clegg, 1322-B Harricana, Val-d'Or, Quebec, J9P 3X6, Tel: (819) 825-0178, Fax: (819) 825-0256

CHIIVIITEC BOIMDAR CLEGG

Rapport Lab Geochimie Geochemical Lab.Report.

CLIENT: CAMEO) GOLD INC.REPORT: TOO- 57472.0 ( COMPLETE )

SAMPLENUMBER

386387388389390

391392393394395

396 397398399400

ELEMENT Au50UNITS PPB

4*5*5

7*5

686

*5*5

6 *5

91313

i lil cu(•PKilPPM

•*l-l? :l 64

5-2:1 73*. :2il 52?v2l 83Ml 78

Si 78li?!! 75'fix 41^ll 67HI? 81

*-2il 90 *!|1 845-?l|:107*. 2 1 102*.2 146

li znPW!i;PPM

ill 74Il3l 72|l| :3|l|l 68Oil? 77III! 77

ill 71181139|: 138

| Hi 146li128|lp|l34 ill 139I1PI|185Il3|352Ilf859

:Mio:

ji

BIxi•l#11111illllzlillHillIll

liI:Si;;: tIV 2

III!

Ni W CdDDU DDU'' DDUrrn rrW.rrn

190 !||||0.3178 4b|i0.3173 39 0.3176 i 43 lo. 3182 li0 '3164 I^i0.445 |iio.832 2? 0.359 |I;38I|0.4OA :: ^WJ : fl Tw SSw;:

101 3| 0.3110 4ll!l0.3102 ;35iio.499 |36:!:!o.895 8:1-7

HI

HiII11*5;illIIIIII

PililIIIlil

iiiii*Vi5;

Il5|

As iHlPPM (^1

25 ill25 liiiefl32 li*:-34 |i II84 111!:!

165 li!1187 lls!

72 iS;:42 11128 1!!

29 lil!! 19 pSl48 |*5|l!40 |*|!!!13 III!!

Fe i|iHii! TEPCT |ilpPM

7.87 Ill^iixlO7.43 1162?|^107.11 I33|;x108.15 i^ii^io7.79 illffoO

7.36 1S||5106.39 i|i^106.53 iiSltl-elO7.02 3511115106.84 15fiJ;:510

7.05 |3fclO 7.26 il53|:5106.66 107i6;;x105.68 11^11x105.00 11111*10

DATE RECEIVED:

lil! Cr illyli; Sn :PPJJijiO PPM PJPM :PPM fi;:;:;:s: mm :S;P; :11? l|;9:;| 284 ;ip3:;;*2o *

l 7 | 256 100 *20 '*li?;|:?| 248 1^310*20 :

8 250 99:*20 xlil 187 l6|||*20 i-

ill 141 iiiiMo i-'|38i| 110 1110*20 1Illl 97 1*31*20 ?ill! 103 |*ii!!*20 -IHI 116 1111*20 f

;l||l| 121 |5i*20 \ i3Ti| 153 B7?|:;*20 jml 132 |i!|*20 l-tt 118 sS6'*20'illl 95 11:181*20 i

01-DEC-OO DATE PRINTED: 11-DEC-OO

lil La^i PPM

CPl 3

i?lp| 3^oll 3li 3III 3Hill 4ip! 14ioi aIII 7iii! ^ib|i s |p.il 6li st20| 7^o! 10

Illl! MS lIPCT! PCT

1111.98 'iJi|3.83|i:|i:||l3.084if7i2.94111113-52

l : ilii2-86Hillill-721 IHIl .34 .illil-39!l||l.44

ill1 -36 . Iliililil .42 1|p|l.30|lM|!:1.06Iii 1 0.93

Illil Na HI:|:i||| PCT lil

llllb.03 IIsi^ijb.os bso3!lf!Hb.o6 ft^fli|6;:8B|p.06 Ha?6,48 0.08 ii

liliillb.os 11||l||!p.o5 |iilillb.os |iIHIiio.08 iiii'jjjjjp.ar 11

l!J6ip.07 ?M i|3iiZ5:!ib.05 IliiSl!!p3ili!p.o4 iiif|M;|).04 |i|||;||1ili|!p.03 HI

i SrPPM

1 30l 31i 42

36i 36

j wli 67i 54li 471 46

5258

i 81i 34l 47

III:

B

liIIlilillIIIliIIIIIIiii111111III111li!lil

PROJECT: BRISTOL iPAGE 3

l Ga 111;PPM(H

l 12 11i 11 lili 11 li\ 12 lill 8 24

\ 6 ii\ 9 illl 10 IIIi 9 lii sil1 10 1111 13 iil; 12 li; 7l||7,

i 6 lii

OF 3

i NbPPM

5l 6l 5; 5l 3

22

: 2li 2l 2

i 2 i 4

3l 1

*1

|i| Ta III•*PW i PPM ;:;:PCT: :;X;: : x : :; : ; : : : :';'; : i : ; : ' :

!ii|*io HI|i|:;:*10 *ip1;x17l;:*10 *;0il:lIMo iolllkio ill III iil|!|?|*io HIi;jipjxio ppi:1111*10 iij8|ilii:;:*io i^illft |l*io Illl

l|llNio lil

:?;::li*1P WiMill*10 111|;*|!*10 ii||

II zr l!|li!i:;PPM IIH;:

l *i illli *1 lip!!;l: *1 pllli!i! *i nil

li 1 li!l 91111 12 iiiili 10 111!1 7 111

;' O 5 ::flK:: ' :

1 7 iiiii: 6 lllli 12 Isillli is iii

Chimitec - Bondar Clegg, 1322-B Harricana, Val-d'Or, Qufbec, J9P 3X6, Tel: (819) 825-0178, Fax: (819) 825-0256

CHIIX/IITEC BONDAR CLEGG

Rapport Lab Geochimie Geochemical Lab Report

+

Chimitec - Bondar Clegg, 1322-B Harricana, Val-d'Or, Quebec, J9P3X6, Tel: (819) 825-0178, Fax: (819) 825-0256

CHIIVIITEC BOIMDAR CLEGG

Rapport Lab Geochimie Geochemical Lab Report

REPORT: TOO-57473.0 ( COMPLETE ) REFERENCE:

CLIENT: CAMECO GOLD INC. PROJECT: BRISTOL

SUBMITTED BY: P.COAD DATE RECEIVED: 01-DEC-00 DATE PRINTED: 11-DEC-00

i DATE i APPROVED ELEMENT , .,*...,

NUMBER OF Aim vccc

j 001208 1 Au30i 001208 2 Agi 001208 3 Cui 001208 4 Pb: 001208 5 Znj 001208 6 Mo

i 001208 7 Nii 001208 8 Col 001208 9 Cd: 001208 10 Bi i 001208 11 Asj 001208 12 Sb

l 001208 13 Fei 001208 14 Mni 001208 15 TE\ 001208 16 Bai 001208 17 Cr\ 001208 18 V

i 001208 19 Sni 001208 20 Wi 001208 21 Lai 001208 22 Ali 001208 23 Mgi 001208 24 Ca

i 001208 25 Nai 001208 26 Ki 001208 27 Sri 001208 28 Yi 001208 29 Gai 001208 30 Li

i 001208 31 Nb: 001208 32 Sei 001208 33 Tai 001208 34 Tii 001208 35 Zri 001208 36 S

GoldAg -Cu -Pb -Zn -Mo -

Ni -Co -Cd -Bi -As - Sb -

Fe -Mn -Te -Ba -Cr -V -

Sn -W -La -Al -Mg -Ca -

Na -K -Sr -Y -Ga -Li -

Nb -Se -Ta -Ti -Zr -S -

IC01IC01IC01IC01IC01

IC01IC01IC01IC01IC01 IC01

IC01I C01IC01I C01IC01

IC01

I C01IC01IC01IC01IC01IC01

I C01IC01IC01

IC01IC01IC01

I C01IC01IC01IC01IC01

IC01

757575757575

7575757575 75

757575757575

757575757575

757575757575

757575757575

LOWER DETECTION

50.2

1211

11

0.2555

0.011

10111

2020

10.010.010.01

0.010.01

1121

1510

0.0101

0.01

PPBPPMPPMPPMPPMPPM

PPMPPMPPMPPMDMIrrn

PPM

PCTPPMPPMPPMPPMPPM

PPMPPMPPMPCTPCTPCT

PCTPCTPPMPPMPPMPPM

PPMPPMPPMPCTPPMPCT

FVTRArTTnWC A 1 f\Al*l 1UN

Fire Assay of 30gHCL:HN03HCL:HN03HCL:HN03HCL:HN03HCL:HN03

HCL:HN03HCL:HN03HCL:HN03HCL:HN03HCL:HN03 HCL:HN03

HCL:HN03HCL:HN03HCL:HN03HCL:HN03HCL:HN03HCL:HN03

HCL:HN03HCL:HN03HCL:HN03HCL:HN03HCL:HN03HCL:HN03

HCL:HN03HCL:HN03HCL:HN03HCL:HN03HCL:HN03HCL:HN03

HCL:HN03HCL:HN03HCL:HN03HCL:HN03HCL:HN03HCL:HN03

(3:(3:(3:(3:(3:

(3:(3:(3:(3:(3: (3:

(3:(3:(3:(3:(3:(3:

(3:(3:(3:(3:(3:(3:

1)1)DD1)

1)1)1)D1)1)

DDD1)1)1)

1)D1)D1)D

(3:1)(3:1)(3:(3:(3:(3:

(3:(3:(3:(3:(3:(3:

1)DDD

DDDDD1)

METHOD: SAMPLE TYPES NUMBER SIZE FRACTIONS NUMBER SAMPLE PREPARATIONS NUMBER:

; DRILL CORE 75 -150 75 CRUSH, SPLIT 75 j30g Fire Assay - AA PULVERIZATION 75 lINDUC.INDUC.INDUC.INDUC.INDUC.

INDUC.INDUC.INDUC.INDUC.INDUC. INDUC.

INDUC.INDUC.INDUC.INDUC.INDUC.INDUC.

INDUC.INDUC.INDUC.INDUC.INDUC.INDUC.

INDUC.INDUC.INDUC.INDUC.INDUC.INDUC.

INDUC.INDUC.INDUC.INDUC.INDUC.INDUC.

COUP.COUP.COUP.COUP.COUP.

COUP.COUP.COUP.COUP.COUP. COUP.

COUP.COUP.COUP.COUP.COUP.COUP.

COUP.COUP.COUP.COUP.COUP.COUP.

COUP.COUP.COUP.COUP.COUP.COUP.

COUP.COUP.COUP.COUP.COUP.COUP.

PLASMA OVERWEIGHT 23 iPLASMA iPLASMA iPLASMA REPORT COPIES TO: MIKE KOZIOL INVOICE TO: MIKE KOZIOL iPLASMA j

PLASMA This report must not be reproduced except in full. The data presented in this iPLASMA report is specific to those sanples identified under "Sample Number" and is iPLASMA applicable only to the sanples as received expressed on a dry basis unless jPLASMA otherwise indicated iPLASMA **********************in**************t***ii*****mnni*************t*************** : PLASMA i

PLASMA iPLASMA iPLASMA iPLASMA iPLASMA iPLASMA i

PLASMA ' iPLASMA iPLASMA jPLASMA iPLASMA iPLASMA :

PLASMA iPLASMA iPLASMA iPLASMA iPLASMA iPLASMA ;

PLASMA iPLASMA iPLASMA iPLASMA iPLASMA lPLASMA i

Chimitec - Bondar Clegg, 1322-B Harricana, Val-d'Or, Quebec, J9P 3X6, Tel: (819) 825-0178, Fax: (819) 825-0256

BONDARCLEGG

Rapport Lab Geochimie Geochemical Lab Report

CLIENT: CAMECO GOLD INC.

REPORT: TOO-57473.0 ( COMPLETE )

SAMPLE

NUMBER

401

402

403

404

405

406

407

408

409

410

411

412

413

414

415

416

417

418

419

420

421

422

423

424

425

426

427

428

429

430

ELEMENT AU30 Ag

UNITS PPB PPM

5 t. 2x5 *:.2

*5 <,2

8 <.26 *'2:

x5 *,2xs *;2xS x;28 x. 2

*s *.2l

*5 M:<5 x.2

x5 x .2

x5 x. 2

20 x. 2

x5 x. 2

<5 <.220 *.2"

34 x;. 2:

xs ^2

x5 x. 2

x5 x.'2l

x5 t. 2

x5 <.27 x. 2

46 x,2

19 x.2.;

12 *.212 x.2

19 x.2

i cu ;PPM F

77

60

61

52

48

53

48 ii

48

41 ;.44

46 i

51

50

65

49

48

57

57

47

52

55

50

47

45

43

123

52

41

50

58

pb; zn*M PPM

7 153

4 193

3 256

4 232

j 4 183

lil: 210

4: 199

3 231

4 193

4 ; 210

4 i 191

x2 236

3 210

x2 220

^ 218

3 210

2 274

3 264

3: 199x2i 173

; 5;i 191

5 196

5 181

6 183

7 174

8 772

8 410

7 347

8 368

9 265

Mo Ni

PPMVPPM

Hill 78: l*l| 44

1 48

xl 40

M 1 54

IHil 25

11:1:1 20

llli! 23

l:.:2li 24

llli 22

ii'^1 26

1;; '2 1- 35

x! 25

xj 26

xl 21

2 22

1 40

2 66

21 01

|ll ; 101

til 09

1 73

1: 49

xl 45

4 70

XI 109

xl 94

1 88

2 56

liii cdppi: PPM; i 370.245 iO .3

560.3

i 57 0.2

HMisio.249 x. 2

53 0.3

53 X.2

:;.:54iix.2

!5||0.2

57:0.3

54 0.3

620.2

55 0.4

53 0.2

59 0.3

l59lo.2

61 *. 2

580.3

60 0.3

62 x.2

51 l*. 2

470.2

49-0.2

31 1 .3

60 0. 4

59 0.4

51 0.4

30 0.3

:Bi;: As

PPM PPM l

11*51 13

ilxSll 21:;-x5'l 16

i:x5l: 16i:*5;i 8

lill 10i'xSl; 9

y *5li 13

::*5lii 8

ill 8 \

:;x5-: 9 :

:x5-: 8 :

/xSl 11 :

1*5-1 14

x5 6

*5l 10

1.551 12

;x5ll 17:x5i;:i 13If?! 12

:x5 8

x5 9

x5 14

*5 25

x5l 34

ixSi 13

IxSl: 96

x5 23

x5 77

x5 38

mpili;I:x5: :Ix5: :

ix5: ;

illH:"x5^-

MM:l*5l

l|ii

1*51

l*?!*3' : -

1 '' S '

'1•'•'.**5 ::: : x5 : :1&:.:x5.:

li*5

:,'X51

'i-'xs;*5

IxSiI'xS'i

:-x5

x5- : -*5''

Fe

i PCT

6.33

7.56

: 8.47

: 9.49

i 9.69

9.35

9.21

9.43

8.61

9.20

8.84

9.95

9.32;s-10.00

9.32

9.21

9.62

9.47

i^O.OO

8.65

5-10.00

9.82

9.01

9.49

4.67

5-10.00

^10. 005-10.00

7.14

iliHhi TE

PPMiiPPM

ilU1408X10I679:x101917 x10lil*10

iilixio21 19 :x 10

2323 x10

2197lix10

226i xio

2W7;X102222 x101990lxiO202aiix102lO|x10

2098 1*1020371x1019^2x102094iix102ib5 xio

21671*102089X102014x101826x101809 x10

1037 xio1695x101676x101591 xio666X10

DATE RECEIVED: 01 -DEC-00

mi(i; i: :li-i-22':1'if

;:12l

liiii;^S3i:

iiiill:34" : i

125;:

l|i

l : 42ii1162of163

176::85.::l61;i;

47- : 43:;

-83727

; 29;i19

65503931

l33;:

i; Cr :;: : :;ViIPPM PPM;

;118 i::il05 115

95 120

i: 59 137

1 31 Pi

i 39 il||;!43 110;

57 112

35 105

i 36 111;

ii 43 1161 57 113l 41 109

\ 52 1101

51 llpi

55 108

l 39 121

51 105

i 42 10154 9li

81 lObl

33 102

45 109

50 111

44 156

65 13

43 73

58 74

50 66

85 9

l sn ;i;i;i;iwi:lDM! bbii : i rrM rrW .J

ix20 xll

x2o x2o :x20 x20

x20 x20

l*20 P

ix20 liii:x20 x26

x20 x20

x20 xapl;

x20 ^2();i;i

X20 1!

x20 x20 i

x20 x2p

;x20 x26;l*20 *?6|

x20 x20i

;x20 x20

*20 x26l|

x20 x20i;x20 x2b

X20 B

x20 x20

x20 x20

x20 x20

x20 x20

*20 *20

*20 *20i

X20 x20l

*20 x20

x20 x20

La ilfif i

PPM itsTii

13 P|i

11 2i87l

7 3l:25i;6 3l62i;8 ii;

6 3)||i;6 ytfft

6 *M5 3i;iS(f

6 3l44: :5 3^706 3.525 3:895 3l44;i

5 3^385 i-425 3;41;i6 3i||;

6 3.11

6 3lAS-:

6 3:99

6 3.61

11 3.38

11 3.38

12 0.90

9 2.38

7 2;20

9 2.12

8 0.51

DATE PRINTED: 11-DEC-OO

l Mg liii

l PCT IS

:il.04lll

;;1 .37 3^;;:1-463i36lii;1.45 2l;93;i;i: 1 ' 39 11

H. si if|1 37 4 13

1.593.54i1-*93i3|iil.67 3llli4i:

I 1-62 ||i

1.86 2:751.762;69;;i.8o|M;1.492.6|1

:il.472.5|:;i.62 Mil;1.54 2,97;;i.572|7|;i

1 36 3 84

l s, li1.662:741.453.791.464:471.594:68

0-^5 4.681.384-021.2831861.473.9I2:0.72 2,24i

; Na ;||:;PCT HI

i. 04 11i- 04 io4;.03 pi:.03 ioi|i;- 03 li

;i-02 lil03 'OS*

: .03 Wi:.03 HI

i. 02 iiii;

.03 II

i. 02 |o|i:i

i. 04 Pi

.02 .36:

:-03 11!

i- 03 ai. 03 liii.02 ^08

1-03 ym02 09

i n? ||

i. 02 i07l

.03 ,05il

.03 .07

.03 .03

02 .1?!

03 illl

.03 Ml

.04 ;b?: :i. 04 iisl

Sr:PPM

: 51

38

i 37

32

33

l 41i 49

i 44i 45

i 42

41i 43i 43: 40

39

l ,40

36

i 41

: 36

36

37

35; 40

52

88

108

83

83

; 76

48

III Ga

PpttxPPM

iiii! ali li! 6

lil! *2

111: Gill *2

in *2liii *2111 *2IIII *211! *2SSSx?

I||ii x2

lliiii x2

11 x2

HI *2

liii *2

111 *2

lil *211 "2Ki-SS *2

llli ^

111 ^iiii *2lit; 3li si 11Il9: i; 17

|l6l 4ill?: 13ill?.: 13;iM: 13

: : :4ii: : 3

PROJECT: BRISTOL i

PAGE 1

IIII Nb

H|PPM

111! 3

iiizoli 8ill 8lil! 10ill 6111 8ill! 7

lil 8

ill! 6111 7

151 8

III! 7

i! 7

lH *li 7

ii 7li 8ill 6ill 6ill s i

ill! 6 il :22li 6 i12511 7 iI**! 7 :.-'2*1 11 i

:-l6i:i x1 i''lM 4

: :23l 3

.;.27: 3

liliii *1 :

OF 3

lill Ta if f:|DDU DDU OPT :rW^xrrn ^rW;:;:.

i 6 ^10 *03dllilixio l264;lHi!*10 MIllalxio ^Mjjj.lliixio liloxox'X :-:-:-:-:-:-:-:-:-:- -: : : i::: : :-:: x-;-:-:-:-:-

ilhio iHliiilixio lilllixio iilel:liixio iiiiiiIf; xio |||pll;Nio iiiilil*io iiii;in^io i/mali;xio mmiiilixio llillihio plliiiiiiiiiiixio 'iji.1! 5:1x10 WiMiixio imiliixio nilill*10 [Mii'illxlO 1168117 xio i 107 1

x5 xio .0117x10 .044;

Il7;;x10 x.pl;l;;l7: xio xlqf:;:iix5ii;xlo x:.ipii;l

Zr IIIIP IFtl

6 liJoiii1 0:96i

Xl 0,83;::

xi 0:71;*1 mi*i III!x1 |i|;i

x1 bM;i;xi ill*i illxl bi:62'i

xi 0:61;;*1 OMiii*1 Hi;

x1 Hill

*1 jSHi*! Hixi isiij';*1 111

x1 |l3p;:;

x1 1:25

*1 0:964 6|7jp5 01871:

18 2.081

10 3 S75

10 4;68

10 4.67

13 4:39i

Chimitec - Bondar Clegg, 1322-B Harricana, Val-d'Or, Quebec, J9P 3X6, Tel: (819) 825-0178, Fax: (819) 825-0256

CHIIVIITEC BOIMDAR CLEGG

Rapport Lab Geochimie Geochemical Lab^Report

CLIENT: CAMECO GOLD INC.

REPORT: TOO-57473.O { COMPLETE )

SAMPLE ELEMENT AiiJO :A||: Cu

NUMBER UNITS PPB PPM: PPM

DATE RECEIVED: 01-DEC-OO DATE PRINTED: 11-DEC-OO

PROJECT: BRISTOL

PAGE 2 OF 3

Zn vHpl Ni Ij&js Cd :|;E|i|| As i;iS|:i Fe iiiiii; : tih|:|; TE sB|| CrD DU D DU DDU D DU D DU D DU D DU DDU -: DPT : - DDU : DDU DDU DDUr rPi r rpl rrrl r rn. ; rrrl "rn. T rPl "f^ "^ l rTTT: :-" rn rrW: -T rPI

Sn iiiUis La

PPtfiPPM

MJ Mg iiSili Na

PCT ffilPCTi!|| Sr li| Ga illll Nb ;:i||i: TaPT'' DOU bl9U*'"DDU DDiii'"'DDII DDU' 'DDU\t\.y.rrn ff^-.-.rrn Ff^.-.rrn irffl'.'.tiri

l Zr i:l|?llilpPM iiiiiii:

431

432433434435

85 S;2 181 I26il254 4 101 ;|; :3

96 d.3|352 341:1518 | ^ 126 3

49 x.2 205 23:1116 II 4| 82

11 ie.;i|i;; 35 liii 162 iiil:;i2: i;i 2831 6;2|i331 I|4l!l510 ililSlilnl

36 2.4 xS 225

il 29|i1.8 x51151iisix.2 vx5: : ; 37:!:3l!i2.4 ii:lx5i:il212

iiiixSl4.004.513.29

2.324.53

76

70

76

113

72

16 OlMliO.52 1i52|.03 J2 12 0^49i: |0.56 :1.^2i:.03 i?

14 0^46:0.62 2.51!.04 vi

19 ()Mii|0.57 i1iv;52lii.04 ||

39 lip: 2 im x1

48 |l||i 3 i|i x1 71 iii! x2 III x1

73 i||| x2 ill xl

44 11 3 li! x1

iiii 2428'........

25 fif:i11 liii 26 iiiiii

436437438

439440

441

442443444445

446

447

448

449

450

451452453454455

456

457

458

459460

19 x;2l:

12 ^.2.:*5 JMx5 *|2ii

x5 *.Z;

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7 *;i|i"5 B

x5 x;if:

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x5 x.2

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x5 x.2

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14 <.2

8 x.2

12 *.2

14 <.Z20 -C; 2i

^ <.2x5 x. 2

x5 x.2

47 ii

71

49

46

43

58

47 i

49 i

37

38

52

56

98

135

101

69

118

102

127

129

121•- 42

60

54

Iff

i:iil9iiiii : i5|iii

liii

11;ii9l;i;l : 7iiii: ; '6;iii

ililill

i-- 8!'!..7i

i:?':: ; !.5'vi'6."

'l . 7 1

1 714

:::j; i'3:i

:v14:l;li'*!' :

i ; i'i6;

10" : ' : 9:'

965

202

625

188

222

224

254

273

299

199

259

234

185

117

132

90

419

464

130

457

450

573

87

87

100

ipl-i'sliiiiiiii

illlil

x1

liii.i?!;

Si1

iilT:i'l : 1liXl'i:

Mli

/4:: ": 4|

lixll :

i 2:

3

: .iv4li;: -i : '2 :

!i : 2i

2

87

29

46

16

16

18

23

32

42

26

31

5096

141

157

139

35

67

139

112

104

71

59

75

80

ill il :37H

:34i!

!l40ii

iiiii.441!

48i;5l;iiliSOlil11421!

ii'45:l;:52ii

I47l;ii:46l;|i49li

i : i44i:'10

i:'22i:

43:i: :35:

ii. 3*.:i'22-

1722

23

ii

0

1

0

i 0

0

0

0

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0

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x

x

: .c

0

0

.6

.3

.3

.3

3

.4

.3

.4

.4

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.3

.3

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.2

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.6

.7

x.2

0

0

1x 'x

x

.8

.7

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84 li!

i:ix5ji549 liixSiiii 24 Iiiiiii 20

!*|! 18xsl; 16

•xSil; 21:;:xs! 15ixSili 10

il*5i 22

:i:*5-|i: 29 IxSil 72

178

28

X5113

I:x5| 54ix5::102

x5 62

3.31

7.417.738.48

8.23

69 !i!l7ilx20 Ml. 11 d;56ii:0.57 i4?s.04 ifl: 43 li! 2 lil xl JM^O mft* 23 ||fi|

II 8 -62

1x10.00 18831:9.78

8.53

l 9.00

9.96

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li 9.70

PI 142?

iiSOji :i22ilil

41 Il.1|lx20 la|43 123 x20 x20

33 111x20 i2|i

38 1#!|x20 X20i:

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60

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98

;: : 1p:::186 122'i^20 "

6 iiiilip x1 ijijspx-io *iii:0!J|11 Ip 3 1|MO iliii16 i||! 8 i|ixlO lH

11 pifl.62 4197 .03 ml 63 l12 4^01 lil. 89 ^35 .03 fill 49 l

11 4i1:0|l2.01 ^761.04 s||| 43 ; 10 till.51 i|.2|l|l.03 lil 40 i

10 pill.86 Pi.04 li. 53 l 10 3^75? ii.64 4lOQii.OS iiiflJ: 47 9 2.58 1.37 3i76i:i.07 iOT? 57 : 6 3.5(5:1.47 11111-05 |||| 94 i

li11! m

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171216

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i|i iil! if! liiiii ii

if:11 !l|ii 16 li15 iiiiiii

6.58 1674 x10 17 116 31 x20 x2p 4 1il7 1.33 5.27;.07 ;pl 80 ||||

2.59 :l452||x10 54| ; 65 191x20 x2p| 18 O^liO.74 3.5t|.04 i;l|:iil17 ill3.36 35?|x10 37 107 1?i x20 x20i! 14 b.9||0.60 2v09l .04 ilSll 83 Illti;8.93 2306 x10 islf 129 67:x20 x20l| 4 2,36 1.85 7MJ.OS ;OSill51 |iii||l|l6.13 1090x10 37 100 K 1x20 x20 8 1.71 1.02 4.60 .04 ,14 164 Sl^

m m

5.37

3.62 496 x10

3.61 528 x10

4.61 761 xlO

4.56 500 x10

40ll 84 22 x20 x20 8 1.,2l!il.14 5v17i.04 ,15|133 116; 5 li?!

:i 130 11:x20 x20ii;

48 104

5010018 X20 *2Q;: 23 x20 x2Cii:

9 0-89 li0.84 2^67i .03 .15 | 8716 1.5211.25 1.8|ii.05 vi?! 65

16 1.65 1.63 2.88:i.04 0|ill01 19 2^051.52 l;56i.04 !l7i 72

:iii5i::| iiil

8 ;i|f4|x10 iflifJtS 8 iiiiliSiiiixlO iitl95i:: 7 ii|ii|x10 ip|:ii 7 ||x10 lil

1

x1

x1

x1

9 pi: 11 f^Oji

s iiiiiii 6 ini4 ilfill5 |ii!

2 fill3 liii7 fjfixio ill! 5 vim7 Iil||l:x10 iliflill 6 |ii||3 f ||x10 ilffi! 15 |i|il7 SiliiJiiixlO XiiOjii:: xl QiiSJiii7 :i;i18iix10 *iiiO!?ii;i xl 0|i^i| ;

ix5:ix10

x.: 01:x ^ 2.^00^x^Ol-^ 20 0*94:^:x'vOJii;i 24 ii|T:i:

^Oliil: 16 2!'29i;i

x.01 12 2.4725 1;75 i

'. 15 03?|i|i i 7 iiiiiii

16 b;85

Chimitec - Bondar Clegg, 1322-B Harricana, Val-d'Or, Quebec, J9P 3X6, Tel: (819) 825-0178, Fax: (819) 825-0256

CHIIVliTEC BONDAR CLI

Rapport Lab Geochimie GeochemicalJLatLRepQrL,

CLIENT: CAMECO GOLD INC.

REPORT: TOO- 57473.0 ( COMPLETE )

SAMPLE

NUMBER

461

462

463

464

465

466

467

468

469

470

471

472

473

474

475

ELEMENT Au30

UNITS PPB

6

^

^

*

45

x5

5^

5^K5

^*5

Ag!; Cu ;!Pb!PPH;PPM PPM

^21 44 I'!/'

ifr 46 1:18:1i, 2; 46 l!!*:

^2: : : : 53 lil;!;

M. M i:l9l:

*ll so li^2! 48 l|: It'*;.'2I 42 HO

*;2l 43 111:8:

m, 41 !;;;1|:

*.2I: 48 if

*'.2l 48 li Si

^2 47 12O 52 13

5.2 52 : 10

ZnPPM

87

87

87

90

86

121

9585

88

87

91

11084

91

87

Hoi: NiPPH PPM

:l2l 71:12I 74

2 732 83

:l:2i 72

If 77

11:21 66

1:21 62

1 63'••M M

S. 73

l/S!! 69

2 73

2 82

2: 79

li'Col Cd 111 As Hi

PPWlPPM PPMIPPM PPM

mx ;.'.'.;w.- mm 21 x. 2 l&l; 45 f : *5l

21X.2 l;SSi 34 l|*5|- ; *\XX j o -' : -*C :;: 1^ ' ' : J^C' : '': 20 x. 2 :x5: 26 x5:?23-:x.2 ; ! : !*5 : !! 24 1*5!!!m*-2 m 19 in.. •-.'••:-:- . . /:-:-:-:-:-:-: :-:-:---:-:-:-:-

lilx.2 pill 17 lil

119!!x.2 ;!!*5J 18 i:! : *S;!!

118|!x.2 |;*5I 17 1^!!:

!!!19-x.2 !:4!l 17 l^ll:!;!17!x.2 : : ! ;*5!:i: 11 jm

il21tx.2 l!*5i!i ; 13 lil!o20!:!x.2 !:!x5|.; 9 ^Si-20'^.2 !!:^;: 10 !!^1

23 x. 2 1^ 16 -tS

23 X. 2 :!!!*5; : 14 !,*5!

Fe !!|Mri; ! : ! TEPCT iPpf PPM

4 09 l 4SO x10

4.13 i 488]x104.19 5W x10

4.52 ;i59 x104.08 plxlO

4.32 l5Q5!l!x10

3.76 501 x103.52 ;!495 x10

3.79 ! 45?!x10

3.61 ; 537!!x10

4.07 llfiko3.92 515 x10

4.10 1493 x10

4.67 494 x10

4.58 1477x10

DATE

:liS:|l| Cr r:H ..rrrl

43 : : 1 A2

l sil m72 119

'^1111*:;45'!:;!122

Il!l30

4i!|138

43 122

1 46 125

liP7

i! ;46|!!l09

45* 109

50112247 134

4411128

RECEIVED: 01-DEC-OO

ll:ISi;i; Sn Isll

flip M:!:p*2o ii*221x20 <20

;:!23lx20 X&130.^20 *20!

--' --:-:v: : : : "'" : "-"-" : .-, : : ; - - -:-::-;-; -;-"-'-"-;- 1 ' - 1

-Sp :I|S;I3Q x20 *20: ::27;x20 *20!!!

I25.I520 *20-!;!'28!!x20 it20! ; !

llf20 H;!l

fco ̂!-;28|-|x20 ^20:;:1281x20 *20|!!!34:!x20 ^20

0331^20 ^O:!;

La llAt'i

PPM til

21 1*9022 2l06

21 211523 2i59

21 2M

21 2i5lH18 2i,3017 2i1318 2.34is zm

22 iii20 ZiSTl

202^4722 2.8021 2;73|

PROJECT: BRISTOL |

DATE PRINTED: 11-DEC-OO PAGE 3 OF 3 l

Mg illPCT !:!i?CT

1.35 1. 731.42 1*60

1.41 1M

1.49 11441.43 KM

1.40 H

1.32pQ1.23 1v72

1.391M

^Hi

1.39i55l1.34 1,561.38 1^55

1.57 1.30

'1-53 1,23

Na jmP01 Pi

04 IP

.05 !t9|

.04 i17!

03 11:- 04 l|l:

.03 li

.04 m.

.04 ill!;!

-04 |i14l

- 05 ||1

03 Hi

.04 HI

.03 li*;!

.03 ;i'7:|;

' 03 iililll

Sr

PPM

79

78

79

59

54

46

5856

44

44

40

4153

64

60

illffi

If:

lilIIIIIImiH11;us::li*:Hi

III11li1151III

Ga liii: NbDM1 bb*t DOUrrn rrVf,:-:rrn

6 lil <17 liii -o7 1291; <19 i34l <19 IHI "1

9 iiilil 19 m *i8 ml <19 mi <1

1

7 ill -o7 liei <19 Ijj'jl; <1

10 IIHI 19 li *

Illili Ta ilfl

11^ 111

i:i|:!:x10 j;||lilxio iii.1*51x10 *'i,'oi:::l*5i::xio tm.sUl^io iiHt

|:i^S|x10 *iii|iPl::::::*5|:|xio s;ei:H:l5lNo *;;ot:lil*10 11:lisii-cio mil...y.v.-.v -.v.v.-.v.;.i-x-x-:-:-:- -:-:v: ;.:-:':-:

llNo 1113*85*10 ilCBf;

ill*io II:i:::*5;::xio ?iOi::s^jSSxIO *i:IMs sssss: m^fi

Zr 1111:PPM :;:PCT|:

15 Ql;4813 0^2714 0,2714 0.2613 ?!|22|

12 mi15 035!14 Q*m15 01261

13 0.23

16 III

15 02ZI

13 ttiiais!14 0.24

14 ||||;

Chimitec - Bonder Clegg, 1322-B Harricana, Val-d'Or, Quebec, J9P 3X6, Tel: (819) 825-0178, Fax: (819) 825-0256

CHUVIITEC BOIMDAR CLEGG

Rapport Lab Geochimie Geochemical Lab Report

O f*

u m^cnWin——' T1 ^ W< o V) PL,

Chimitec - Bondar Clegg, 1322-B Harricana, VaWOr, Quebec, J9P 3X6, Tel: (819) 825-0178, Fax: (819) 825-0256

CHIIVIITEC BONDAR CLEGG

Rapport Lab Geochimie Geochemical Lab Report

i REPORT: TOO-57474.0 ( COMPLETE ) REFERENCE:

! CLIENT: CAMECO GOLD INC. ; PROJECT: BRISTOL

SUBMITTED BY: P.COAD DATE RECEIVED: 01-DEC-OO DATE PRINTED: 11-DEC-00

I DATE j APPROVED

i 001208 1i 001208 2i 001208 3i 001208 4i 001208 51001208 6

i 001208 7i 001208 8i 001208 9i 001208 101001208 11 i 001208 12

i 001208 13i 001208 14l 001208 15i 001208 16i 001208 17| 001208 18

i 001208 19l 001208 20i 001208 21i 001208 22i 001208 23j 001208 24

i 001208 25i 001208 26i 001208 27i 001208 28; 001208 29i 001208 30

i 001208 31i 001208 32; 001208 33i 001208 34l 001208 35i 001208 36

CI EUCUTc Lent N I

Au30AgCUPbZnMo

NiCoCdBiAs Sb

FeMnTEBaCrV

SnWLaAlMgCa

NaKSrYGaLi

NbSeTaTiZrS

GoldAg -Cu -Pb -Zn -Mo -

Ni -Co -Cd -Bi -As - Sb -

Fe -Mn -Te -Ba -Cr -V -

Sn -W -La -Al -Mg -Ca -

Na -K -Sr -Y -Ga -Li -

Nb -Se -Ta -Ti -Zr -S -

I C01IC01IC01IC01IC01

IC01IC01IC01IC01IC01 IC01

IC01IC01IC01IC01IC01

IC01

IC01IC01IC01IC01IC01IC01

IC01IC01IC01

I C01IC01I C01

IC01IC01IC01IC01IC01

IC01

NUMBER OF ANALYSES

252525252525

25252525 5T25 25

252525252525

252525252525

252525252525

252525252525

LOWERDETECTION

50.2

1211

11

0.255 5

0.011

10111

20201

0.010.010.01

0.010.01

1121

1510

0.0101

0.01

PPBPPMPPMPPMPPMPPM

PPMPPMPPMPPMPPM PPM

PCTPPMPPMPPMPPMPPM

PPMPPMPPMPCTPCTPCT

PCTPCTPPMPPMPPMPPM

PPMPPMPPMPCTPPMPCT

EXTRACTION

Fire Assay of 30gHCL:HN03HCL:HN03HCL:HN03HCL:HN03HCL:HN03

HCL:HN03HCL:HN03HCL:HN03HCL:HN03HCL:HN03 HCL:HN03

HCL:HN03HCL:HN03HCL:HN03HCL:HN03HCL:HN03HCL:HN03

HCL:HN03HCL:HN03HCL:HN03HCL:HN03HCL:HN03HCL:HN03

HCL:HN03HCL:HN03HCL:HN03HCL:HN03HCL:HN03HCL:HN03

HCL:HN03HCL:HN03HCL:HN03HCL:HN03HCL:HN03HCL:HN03

(3:1)(3:1)(3:1)(3:1)(3:1)

(3:1)(3:1)(3:1)(3:1)(3:1) (3:1)

(3:1)(3:1)(3:1)(3:1)(3:1)(3:1)

(3:1)(3:1)(3:1)(3:1)(3:1)(3:1)

(3:1)(3:1)(3:1)(3:1)(3:1)(3:1)

(3:1)(3:1)(3:1)(3:1)(3:1)(3:1)

METHODSAMPLE TYPES NUMBER SIZE FRACTIONS NUMBER SAMPLE PREPARATIONS NUMBER

i DRILL CORE 25 -150 25 CRUSH, SPLIT 25 ;30g Fire Assay - AA PULVERIZATION 25 iINDUC.INDUC.INDUC.INDUC.INDUC.

INDUC.INDUC.INDUC.INDUC.INDUC. INDUC.

INDUC.INDUC.INDUC.INDUC.INDUC.INDUC.

INDUC.INDUC.INDUC.INDUC.INDUC.INDUC.

INDUC.INDUC.INDUC.INDUC.INDUC.INDUC.

INDUC.INDUC.INDUC.INDUC.INDUC.INDUC.

COUP.COUP.COUP.COUP.COUP.

COUP.COUP.COUP.COUP.COUP.COUP.

COUP.COUP.COUP.COUP.COUP.COUP.

COUP.COUP.COUP.COUP.COUP.COUP.

COUP.COUP.COUP.COUP.COUP.COUP.

COUP.COUP.COUP.COUP.COUP.COUP.

PLASMA OVERWEIGHT 7 iPLASMA iPLASMA iPLASMA REPORT COPIES TO: MIKE KOZIOL INVOICE TO: MIKE KOZIOL iPLASMA i

PLASMA This report must not be reproduced except in full. The data presented in this iPLASMA report is specific to those samples identified under "Sample Nuifcer" and is :PLASMA applicable only to the samples as received expressed on a dry basis unless iPLASMA otherwise indicated iPLASMA *****************************t******************************n***x***********tn* ; PLASMA |

PLASMA iPLASMA jPLASMA iPLASMAPLASMA iPLASMA i

PLASMA ' iPLASMA iPLASMA iPLASMA iPLASMA iPLASMA i

PLASMA iPLASMA iPLASMA iPLASMA 'PLASMA iPLASMA i

PLASMA iPLASMA iPLASMA iPLASMA iPLASMA iPLASMA i

Chimitec - Bondar Clegg, 1322-B Harricana, Val-d'Or, Quebec, J9P 3X6, Tel: (819) 825-0178, Fax: (819) 825-0256

CHIIV1ITEC BOIMDARCLEGG

Rapport Lab Geochimie Geochemical^Lab Report,

i CLIENT: CAMEO) GOLD INC.

REPORT: TOO-57474.O ( COMPLETE )

SAMPLE

NUMBER

476

477

478

479

480

481

482

483

484

485

486

487

438

489

490

491

492

493

494

495

496

497

498

499

500

ELEMENT Au30 0*5(0 Cu

UNITS PPB PPM:PPM

l Zn :Mp::; Ni

PPM PPM! PPM

7 *.2;;; s ra!:

11 ra:13 i;?:!46 ra;

44 44616681

4 95:|4f 84 1;3 121

52 104'If 1 72 ;

13 65W: 67

5 584 614 68

;;23:1929

:o25:;;

0.4 0.50.71.8

21 .3

*5 19li;:! 32|t5 46*5 211

I;i;;3195

8 raj; 45 :||:;; 7 i;:2|! 43 s'"'

5 "ft! so !l42 pi 51 ! -

s ill 56 I;

:54.18

of; 51 0240 1.2 :M!;! 145 1:^:3.6682

117525249

57

23

0.8

1.0

0.9

1.0

15 rao 44 oof; 98 !00;3|: 68 o23;: 0.56 "Ojo: 42 12;; 64 4 71 022 0.4

12 ra 48 4 76 3: 74 23 0.4

<5 *.,2 42 3 74 3 67 22 0.7

<5 ra 40 !2; 85 3 117 030 1.2

6 rao 45 "i*;;; 91 |!:3| 68 o22o 0.9*s •c;2;! ; 40 o;i2|: as -p;; 59 l2p|! 0.6

5 rai 42 !;!;p 75 o!: : 3j; 53 lif:! 0.9

<5 ra 40 ::M 85 o:S;: 61 119; 0.77 ra 38

a ra"o

83

42 5 92"S ra!;! 39 :';!'is| 95

^ *.2 35 5 93tS ^2 41 05 96

"5 ra 43 6 88

56

59

49

47

5964

0.6

0.8

0.6

1.7

0.6

0.7

i?f! ! ; *s!:!;

63 -:5 3.6981 |*5|3.7785 "1:3.66105 !isl3.59

11113.971^51:3.91

29

26

29 x5 4.09

61 *5 3.94

140 is 5.06

76

48

78

64

45

39

39

205

56

39

S3.89

;3.46

DATE RECEIVED: 01-DEC-OO DATE PRINTED: 11-DEC-OO PAGE

PROJECT: BRISTOL

1 OF 1

cd !:!;Si| AS ;;|b;; FePPM PPM PPM Pftio PCT

fjn TE ;: Cr

:: 3.87 15021^10 ; :5p|112 47 86

i;*;: Sn |oWo: La o::::^t:o; Mg

1p|opPM PPjlPPM M! PCT

2(i ^0 "20 : 20 2.40 1 .45 28: ^0 ^2O: 21 2i5S 1 .67W "20 "c20:;: 12 2,47 1.40

Na 1||| Sr ill Ga |1|| Nb ||||PCT ifrlppM i|:!:!pF

76;52;45 li;!; 36 111:!:44 ill

3 0:351m 3 1

iiii 51 il2!! 54 l! ;:2|| 61!o^l 71 lmi 56 1IIII 87 ; I||!;ii7:;;||;; 95;

54 89

m,- 88 0:281*20|li|i03 !:l||No o;6p;;; 76 ;;;22o;*2o o;62s 97 ;:; :2i : i;*2o

mi 16 pp. 11 i||;!.o9 Ip; 84 HI Wjj- 12 2ia!;!:i.oo ^H|. 10 111 45 ;!;;!!!|i;

*2p1;! 12 2^f;:;i.o21.3|;;!:.091|| 53 ||ilil 12 IHoO.98 lpl.07 lil 48 HI

3 lil!!!: <14 IB 1*2 lip <1

4 ip 13 ill i4|!i|| 1 3 111 *1

2 iiii 2

|i|; zr li:?;;:nnuo'nQu : '.'Df*T''''DDU ^'DiTT' 1 :: rr!l: : : :rrTI X'fV.rx'rrn : ; f;vl!: : :':

;0^5jOXlO ^JPf:; 23 Oi'28; :'

siSjssxio ^iitji;; 25 0.26

lUl^io |5||!;i 33 l^lii||p*10 II:!;! 32 |i||

|!||;!ho li|| 22 ||||!;!I||x10 |i|l 22 i|i|!!!li|!^io ppi 21 j^jsiJI li|;^io |j,||| 20 0*^|i ||i;!hio Iiii 2

18 llpl.45 11*11-06 ip 40 i|l| 3is ii?li.5i :i7|!;!.05 li! 56 !!!;||| 323 2j!f;l.61 |i|;.05 IHI 62 |||;! 4

23 2.28 1.60 ii49o.07 il9o 78 : 5; 434 2;52!!:3.90 iili.07 1111299 ill 2

111 IIIill

23i|||l.57!J!o6l!.06lP!82||5l 3 !;il 2

IHfOO Illll 25 jp|;!;iS;!^io |ii||| 24 pill;;|pc10 111! 27 lipIfNo i||! 27 Iff;111*10 iiii 9 piiilil-dO ill!: 24 Hi!

23 2|13!:!;1.59 !i;*5||.07 ;i|i 84 ;I||22 Sil .43 l!p.07 lip 86 |!||191;9||1.37 :i:i44|!.061||| TO |;;|f19 lill.34 l!90!;!!.07 li! 94 HI

3 mi i iiiHio iiii 26 (pu*2 IIII K1 IIIMo |i|| 22 Hlp2 ;i2|p <1 !i|jf*io Siflli 22 diiSi;; 2 B2S!:; 1 silSIMo iiSil 20 OiZJi

^5:3.33 431 ^10 077;: 88 21 "20 ";20;; 19 1;86;^5;;3.02 48? ^10 56; 100 19 *2o S20o 17 iii6;r(5 2.93 495^10 56 126 18 ^0 -e20 16 1,62"3o3.36 443;<10 80|; 86 230*20 *Sjp:;;; 19 2-025!x5:3.57 454ox10 !:68! 92 o22v^20 "50| 19 l!950

.41 !lf :7|s.OB !Pj||

.38 2.17!':.06 S15|

.48 !i:.5i!:!:.06 liiip

.43 1;56'l.05 !;!22:|

82 HI 3111 1 1911 20

illlilIII W-.

3 :;;24| ^ ^ 111 ^3 lil 1

*2 :023:' ; *1

liHio 1*|1ISo^lO SIO-B

1919 Oil? 22 Di??!!23 olai

Chimitec - Bondar Clegg, 1322-B Harricana, Val-d'Or, Quibec, J9P 3X6, Tel: (819) 825-0178, Fax: (819) 825-0256

CHIIVIITEC BOIMDXXR CLEGG

Rapport Lab Geochimie

Sd 9o

o}w) enl OH

Chimitec - Bondar Clegg, 1322-B Harricana, Val-d'Or, Quebec, J9P 3X6, Tel: (819) 825-0178, Fax: (819) 825-0256

CHIIVHTEC BONDAR CLI

Rapport Lab Geochimie Geochemical Lab Report

i REPORT: TOO-57478.0 ( COMPLETE ) REFERENCE:

j CLIENT: CAMECO GOLD INC. l PROJECT: BRISTOL

SUBMITTED BY: P. COAD DATE RECEIVED: 06-DEC-OO DATE PRINTED: 11-DEC-OO

i DATE i APPROVED

1 001208 1i 001208 2i 001208 3i 001208 4i 001208 5j 001208 6

i 001208 7i 001208 8i 001208 9i 001208 10: 001208 11 i 001208 12

! 001208 13; 001208 14; 001208 15i 001208 16i 001208 17j 001208 18

l 001208 19i 001208 20i 001208 21i 001208 22j 001208 23i 001208 24

i 001208 25i 001208 26i 001208 27l 001208 28i 001208 29i 001208 30

i 001208 31i 001208 32i 001208 33; 001208 34i 001208 35i 001208 36

EL

Au30AgCuPbZnMo

NiCoCdBi

Sb

FeMnTEBaCrV

SnWLaAlMgCa

NaKSrYGaLi

NbSeTaTiZrS

pup UTxncni

GoldAg -Cu -Pb -Zn -Mo -

Ni -Co -Cd -Bi -As - Sb -

Fe -Mn -Te -Ba -Cr -V -

Sn -W -La -Al -Mg -Ca -

Na -K -Sr -Y -Ga -Li -

Nb -Se -Ta -Ti -Zr -S -

IC01IC01IC01IC01I C01

IC01IC01IC01IC01I C01 IC01

IC01IC01IC01I C01IC01

IC01

IC01IC01IC01IC01I C01IC01

IC01IC01IC01

IC01IC01IC01

IC01IC01IC01IC01IC01

IC01

NUMBER OF ANALYSES

424242424242

4242424242 42

424242424242

424242424242

424242424242

424242424242

LOWER iftPTPPT T fill PYTDAPT Tnkl UPTUfTl -L/C 1 CUI ILW CAI Knl*l lUH Ft 1 nUU :

50.2

1211

11

0.255 5

0.011

10111

20201

0.010.010.01

0.010.01

1121

1510

0.0101

0.01

PPBPPMPPMPPMPPMPPM

PPMPPMPPMPPMPPM PPM

PCTPPMPPMPPMPPMPPM

PPMPPMPPMPCTPCTPCT

PCTPCTPPMPPMPPMPPM

PPMPPMPPMPCTPPMPCT

Fire Assay of 30gHCL:HN03 (3:1)HCL:HN03 (3:1)HCL:HN03 (3:1)HCL:HN03 (3:1)HCL:HN03 (3:1)

HCL:HN03 (3:1)HCL:HN03 (3:1)HCL:HN03 (3:1)HCL:HN03 (3:1)HCL:HN03 (3:1) HCL:HN03 (3:1)

HCL:HN03 (3:1)HCL:HN03 (3:1)HCL:HN03 (3:1)HCL:HN03 (3:1)HCL:HN03 (3:1)HCL:HN03 (3:1)

HCL:HN03 (3:1)HCL:HN03 (3:1)HCL:HN03 (3:1)HCL:HN03 (3:1)HCL:HN03 (3:1)HCL:HM03 (3:1)

HCL:HN03 (3:1)HCL:HN03 (3:1)HCL:HN03 (3:1)HCL:HN03 (3:1)HCL:HN03 (3:1)HCL:HN03 (3:1)

HCL:HN03 (3:1)HCL:HN03 (3:1)HCL:HN03 (3:1)HCL:HN03 (3:1)HCL:HN03 (3:1)HCL:HN03 (3:1)

30g Fire Assay - AAINDUC.INDUC.INDUC.INDUC.INDUC.

INDUC.INDUC.INDUC.INDUC.INDUC. INDUC.

INDUC.INDUC.INDUC.INDUC.INDUC.INDUC.

INDUC.INDUC.INDUC.INDUC.INDUC.INDUC.

INDUC.INDUC.INDUC.INDUC.INDUC.INDUC.

INDUC.INDUC.INDUC.INDUC.INDUC.INDUC.

COUP.COUP.COUP.COUP.COUP.

COUP.COUP.COUP.COUP.COUP. COUP.

COUP.COUP.COUP.COUP.COUP.COUP.

COUP.COUP.COUP.COUP.COUP.COUP.

COUP.COUP.COUP.COUP.COUP.COUP.

COUP.COUP.COUP.COUP.COUP.COUP.

PLASMAPLASMAPLASMAPLASMAPLASMA

PLASMAPLASMAPLASMAPLASMAPLASMA PLASMA

PLASMAPLASMAPLASMAPLASMAPLASMAPLASMA

PLASMAPLASMAPLASMAPLASMAPLASMAPLASMA

PLASMAPLASMAPLASMAPLASMAPLASMAPLASMA

PLASMAPLASMAPLASMAPLASMAPLASMAPLASMA

SAMPLE TYPES NUMBER SIZE FRACTIONS NUMBER SAMPLE PREPARATIONS NUMBER

DRILL CORE 42 -150 42 CRUSH, SPLIT 42PULVERIZATION 42

REPORT COPIES TO: MR PAUL COAD INVOICE TO: MIKE KOZIOLMIKE KOZIOL

This report must not be reproduced except in full. The data presented in thisreport is specific to those samples identified under "Sample Nuifcer" and isapplicable only to the sanples as received expressed on a dry basis unlessotherwise indicated

t******************************************************************************

1

Chimitec - Bondar Clegg, 1322-B Harricana, Val-d'Or, Quebec, J9P 3X6, Tel: (819) 825-0178, Fax: (819) 825-0256

CHIIVIITEC BOIMDAR CLEGG

Rapport Lab Geochimie Geochemical Lab Report,

SAMPLE

NUMBER

7651

7652765376547655

7656765776587659

7660

7661

7662

766376647665

7666766776687669

7670

7671

7672767376747675

767676777678

7679

7680

GO cao INC. PROJECT: BRISTOL ;57478.0 ( COMPLETE )

ELEMENT AlBO AgUNITS PPB PPM

x5 X.2?6 x''!;*:

x5 0.27 0.4

x5 0,2

x5 OjS;X5 X;2

xs xi2';;25 0:21"5 Hx5 6,3:x5 0.4x5 0.29 x.2

x5 0,3?

5 0,3x5 0.3x5 0.;4x5 8.5x5 0.3

x5 6.5;x5 0.3x5 0.5x5 0.7x5 0.3

x5 0.3x5 0.49 0.25 0.7

x5 x.2:

CuPPM

4348838395

8295

11095

: 85

76908996

: 9i

9492687062

7764587873

7178685242

Pb ZnPPH PPM

5 821-51 93

x2 103l*2! 93li;114

1x21 87;;x|:? 76

?;x'2l 90Igl 61IP00

1*21 79x2 89x2 81x2 72*2 73

x2 81x2 922 83

:x2 166

x2 104

x2 83x2 75x2 65x2 64x2 78

x2 62x2 59X2 62x2 758 209

;?Mo: NiPPM PPM

'it? 67; ;2 74xi 61xi 58

?xi?; 57

1*11 50? ;*i 1 so

1 68,;1!i1 621*1?;; ss

li; 48xi 62

1 601*11 61;*V; 57

111 59111! 581*1?; 44

1 591 56

xl 80; ; 1 69

5 60.fi?; 66

x1 75

x1 671*11 57x1 68x1 471 19

Co: CdF*M PPM

118 0.3; 20 0.344 x.2M 0.2•li*- 2

111*- 237X.254 0.2

;!45lx.2?ll0 - 3

ilkz46 0.239:0.3411x.23|?0.2

l*?!0 - 34010.429J0.43iio.4290.3

ft.230 0.3260.332 x.234 0.2

320.327: 0.232 0.323 0.245 1.1

; ;BJ;?; AS ist:PPM PPM PPM

: *5l; 26 ?x5l!?.x5l 22 ;?x5;?

•x5?; 16 ;.x5::•?x5'?: 15 ??x5?;lil 7 is::

:?il 6iB? : x5l; 9 mlis!;;; 17 i|;li* l 26 1||1*51 23 1x15?:

ixsl 8 !?x5l ;•M: 7 if!

?' : x5?? is j;*?;!x5::: 22 x5 :

1*5l 26 1*5;?

?:X5 ? 31 :?x5;?1*5';; 6 1x51;;:x5?: 8 : .?x5?:;Ixsl xs sxs;:;;: : x5i x5 : : : x5?;

VxS?; x5 ?:'*5;•'xs;?; 9 ? ;x5;1*5.1 x5 ''VS;:-:x5': ; - x5 .?x5 ; :

x5 6 x5

??x5:?: 28 •xs?: : x5l 21 ?x5 ; :

x5 26 x5x5 13 x5

x5 7 x5

DATE RECEIVED: 06-DEC-OO DATE PRINTED: 11-DEC-OO

Fe |!!!|hi| TE |B|| Cr ||y1 Sn 1?Wl La Ijitl Mg !?pcT ;;::PPM:;PPM PI*M!?PPM PPM?:PPM PPM; PPM ! per PCT :?

3.66 l|7i:!;xio :::;56;;;! 71 ?;26;;!!x2o xatil 22 ip:;i .32 ?;; 4.16 1481x10 SK*;!; 82 !;29?x20 x20: 23 2*1911.45

4.92 1145 xlO 14 ; 74 1011x20 x20 3 i.41 2.45: 4.32 10981x10 131?; 78 1911x20 ^0? 2 190/2.10 ;

5.02 |2|o?!xio ;;|i;!?; so ||||x2o ^;; 3 1^12.74 1

; 5.42 lijolxio lHi so ;;?90??x20 ^b?? 2 3B;i3:;:2.o6 i?! 5.42 I||?;!;!x10 |i| 72 I25;!?x20 Mj:: 2 ii||i2.32 ;i;; 5.58 i635lx10 ; ;?;:4l 70 !||;?x20 xjal 1 2i96:;1.75 :?; 4.29 l|flx10 :;!;||| 62 ||||x20 ||| 2 Si. 72 |! 5 ' 61 ?Bli*10 18 " 111*20 li! 2 H2 '31 1; 4.61 127HX10 111; 62 1401x20 ||| 1 |;'70;;;1.74 \-i 4.79 1234 1x10 :?17 66 ;8b;?x20 x2bl 23ip9;?1.86?i 4.73 13^11x10 1:14! 59 ??75lx20 x^)l 2 JS:|S|1 .38 I?: 4.48 i379;' : x10 1;i(Sl 59 ??7?::;x20 *^j1 2 2^11 .27 ':; 4.53 I2||!xio !;;i|; 59 l87;?;x20 Wjtt 3 2;;:55li.2i : ; '

; 4.84 ii6olxio ;;i|? 65 |ii!x2o lip;;! 2 2:s|i .44 ?;: 6.C16 I527?x10 49;:? 50 :;:^;;;x20 xZO? 52?.72ll.18;; 5.30 i5pl1?x10 15|1 66 ?:6|lx20 pi 4217711.60?

5.69 171? *10 20 114 ioi|x20 ^o!? 7 3ll8 2.266.45 1713 x10 8 128 93|x20 ^ol 6 3^18 1.98

; 5.37 1364 xio 15 203 79 x20 x2(jl 6 3.42 2.664.24 1015 1x10 47 119 48 x20 x20 ii 7 2*75 2.03

; 4.49 1l93 xio 37 142 51 x20 x201 62.521.666.82 1786 x10 15 176 97 x20 x20 6 3.58 2.635.23 1371 x10 13 199 92 x20 x20 5 3.32 2.62

3.31 880x10 22ll70 641x20 x20 1 32.321.823.40 956:X10 122161 "(SO x20 ^Os 22:271.84

! 3.69 9261x10 ;;; 24: 176 (W x20 ^0? 32,54:1.984.77 2428 ix10 24125 68 x20 x20; 3 2.43; 1.71 J

>10.00 1713 xio 4 31 115; x20 x20 5 3.83?2.09

•mctf? Na'i;;pcf?:;pcT

:l:isiil.o6;M24?;.os1:3^45;?. os;?; 5^1. os!!i!ii!:!-o4

!;!||||;.04Hf!!;;. osISiMl.OSl4loi;;.o4lA:|5i-03

;?;sl79:;.oi3160-05

i?5M;;.osi^Mi:.06

: '?4p1.06

;!Si!-o7;;;6;;'b:7;;.o5••iifiiisl.oi?:;8l'2l;;.o3I;|;,|(j;;.o3::11I.0415.67?;. 02if. 95:. 02? 8; 02?;. 035;37:.04

4.361.06l5.'88l?.0413:;45|.06'10.00l.02i-isM.02

lii!;Illlilol2lblbslbibs?Ill111;lililillil;iHIII!iililloSOllll

111illiii11:^||l!Illmipjsii0,2(50.09;;0 -'b*?;

o.b8blbl?0.08olio;olbi;

SrPPM

7868434243

2734262030

3333363534

2748738482

5546695146

4341337343

HI

Blililsl;l?l?IlllilillIII;lil111:illillsHI1;?;7.;Ill

liiili;iiillli!iipi11 si;??lo1S

111?l5l1;;6?;1ip!; :ilil

PAGE

GaPPM

^x2<2x2x2

x2x2x2x2x2

x2x2x2x2x2

x2x2x2x2x2

x2x2<2x2x2

x2x2x2x2x2

liSiniii : !iiii111!!iiwiliiill111liii;?22i;??21??

ii111IllsIlls11111illWn*171

126;;Sii?!?112?

lii1:121:;;:i|:

1 OF 2 :

; NbPPM

12666

57655 ;

j ]

54 '\

45

je

4 ;65

4 ;2355

4344 :6

III!;: Ta 11^1:

Wi:;;ppM !:::j!|;;i

IxSsxio ^;:b:i??Sij^ssxio *: ^:bl;?•:-:-:':':' -:-: "- ' ' . :-.-:-:-'-'.-'.•:-: 'f -:-: ... :-: '^f^^-'--'-

tf" II•llxio li!;|||?xio Ijiial;;||xio jjm;;;;||;;;xio |s|8||Ilixio HHl!

iHixio liillil*io ilil!; ll;xio iislilli;*io ioiilip?;;xio |tHl

iiihio liiilllNio Ilillil*10 IBi;||;;!xio !||i|iIlixio 10521;

|:|l*io lilI'SlxlO llOBl:l?7?x10 ;;098l

12 x10 i126;.;;:.9! : xio .2661

|;xio .200.;ii';xio .ITS?;??? : 6? : xio ;.:i9t;;llalxio ;;i53?;;;l8?xio ;;378i

Zr'PM

1515x1x1x1

x1•*1

xix1x1

^xix1x1xi

<11452

,67

x1*1

<1X1

<1^x1

1111?

illiBilMl6,p8?0:Mi:

111

Ilil;8*1*1b'i37?;Ilillipilil|i||lollillill;

Ilil6.24?MlilllilWii:

b^balO- 380,401;

?Sf0.060-07?0;056i:22lb^66l!

Chimitec - Bondar Clegg, 1322-B Harricana, Val-d'Or, Quebec, J9P 3X6, Tel: (819) 825-0178, Fax: (819) 825-0256

CHIIVIITEC: BOIMDAR CLEGG

Rapport Lab Geochimie Geochemical Lab Report

CLIENT: CAMECO GOLD INC. REPORT: TOO-57478.0 { COMPLETE )

SAMPLENUMBER

76817682768376847685

76867687768876897690

76917692

ELEMENT AuJOUNITS PPB

**5*5*5*5

x5

6*5

11*5

*5*5

|il| Cuf*fi;PPM

il?i 35ill T5*M *1

lil: 2

111 2

If! 3il 28li 7

&II 3lil! 't1

ill *i"S: 2;!! *1

Ilil ZnDDU : DDU m^.-i-rrrl

iiliil26iii"i! ; 129!*2l 49•111 22Iii 13III 21Illi 36III 39Si 51ill! 36

III 29ill 46

Ho NiDDU DDUrfr\. m ~.-rrn

11 42III 41

li! 2

11! 2

II! 3

il 2iii 4II! 1III 1HI 3

11 3||;i 3

i;!C6;i; CdffMiiiPPM

Isiio.s;i|i;o.3|i|*.2lil*-2|||*.2

l!*-2III*. 2li!*- 2iiii*.2iililiii*.2

lil!*-2

ill AsWiiiPPM

iili 16

S 9|iif 1 <5!:*c5!:!; K5?:*S:S *5

iiiil *sHi 15!*l! *5ill *5!|5| *5

53*11 *5iili *5

iiiilnIIIliin11ilIlliiliimininliin

i Fe ilii TEPa IfjliPPM

i 9.92 1111*10HO.OO 111*10: 5.22 ||i|*10: 2.31 :;i;8?|i;*10i 0.61 ||ii:*10

0.59 16131*10i 1.78 |l|l*10i 4.17|i||*10i 6.02 !!i!*10i 5.02 ii!i|||ii*10

i 4.16 flitMo7.27 IHIMo

DATE RECEIVED: 06-DEC-OO

|IS| CrMJKi|':'nnurrn :r*rn

iiiil 57iiiiliiiii 49illi 48mi so

III 86Biil17lli 32Ilil 32iiii 4imi 4o^4iP 34

illli11

ii Sn liiii

f™ 111

:!*20 ^28!:!

La |P|PPM IIH

5 il-

DATE PRINTED: 11 -DEC- 00

i Mg i! PCT

i2.30iS||ii*20 ^Oi;? 7 11112.13 i

li'•:'-:'-'.'-'.'f

iiiilil

ill

liliiililiip

i*2" PI^20 "fiss?;;^20 H|

:*20 -^^J:::

! :*20 S2tf!!: :*20 S^!;:

!:*20 ^Os^:*20 x20;::

i*2o mi:*20 iJSJs

43 iSS:16 0.9923 11

21 iii170^3127 ill36 Ilii45 ||i38 11137 3i01

0.41 i0.230.04;

0.05 ;i

0.07;0.28!0.50 i0.82 i

0.71 ii1.09 i

iiiililiiIlil!li!liiiiIlllliIlil!:iliiiiilliliiiIliiilliilii

! Na Ills

m lil•05 iili!.08 Ilil.OB iiiii.04 i||i;.04 OV19

-04 Hiii-04 li!•os iii•03 111!.02 IHii

: : : : :xo::xo :y:-:-:-:-:':-:-:

•os iii!•03 iiiiiii

SrPPM

3636197345

5931653513

1313

liHiinill!ilIII111illillill11!Iliiiiiili

PAGE

Ga 11PPM PPM;:

3 ii3 119 li2 iii

*2 II

^ Illi*2 11!s ii7 iili!4 III

4 114 ii

PROJECT: BRISTOL i 2 OF 2 i

NbPPM

1415*1*1*1

*1•d•el

*1*1

*1

i;i|i| Ta fillHiiippM |ii;

11*10 pi111*10 HI111*10 loifl!!!!^Sr;!*10 i*tft1! :i!i;||i*10 iii!

!siiS!!!*10 *S(Jli;!!?!*!S!!!*10 *iiSi!;iiii*io iiiiiiii|i*io ilii||i|*io il!1111*10 ||i|||;||*io IliSt III 111

: : : : : : : : :| '-:'- : . ; ... :; ox. . x:: : : : : : : : : :-:x-:':-;-;-:':

l:™!: Z :-: : : : !:: : : : : : : : : : :

i z r IIIIIPPM ;||i|

: *i B*i tMs66 0*0234 Iliii45 |I|

so iiii 41 111!i 33 Iiii 28 iipi' 20 P!*:(i2^

26 i||i20 S'iilSJS

Chimitec - Bondar Clegg, 1322-B Harricana, Val-d'Or, Quebec, J9P 3X6, Tel: (819) 825-0178, Fax: (819) 825-0256

cmivirrECBOIMDAR CLEGG

^ISO-^V^m fftjtltfia , ^ft

Vw^ Rapport Lab Geochimie Geochemical Lab Report

+

+

Q

lu

+

vo t*

Chimitec - Bondar Clegg, 1322-B Harricana, VaWOr, Quebec, J9P 3X6, Tel: (819) 825-0178, Fax: (819) 825-0256

CHIIVIITEC BOIMDAR CLEGG

Rapport Lab Geochimie Geochemical Lab Report

! REPORT: TOO-57479.0 ( COMPLETE )

j CLIENT: CAMEO) GOLD INC.

j PROJECT: BRISTOL

REFERENCE:

SUBMITTED BY: P. COAD

DATE RECEIVED: 06-DEC-OO DATE PRINTED: 14-DEC-OO

! DATEj APPROVED

; 001213 1i 001213 2i 001213 3j 001213 4i 001213 5l 001213 6

i 001213 7i 001213 8i 001213 9i 001213 10i 001213 11 i 001213 12

l 001213 13; 001213 14: 001213 15i 001213 16i 001213 17i 001213 18

i 001213 19l 001213 20i 001213 21l 001213 22i 001213 23\ 001213 24

i 001213 25i 001213 26i 001213 27; 001213 28j 001213 29: 001213 30

; 001213 31i 001213 32i 001213 33! 001213 34i 001213 35i 001213 36

PI CUPUTCLCFCN i

Au30AgCuPbZnMo

NiCoCdBiAs Sb

FeMnTEBaCrV

SnWLaAlMgCa

NaKSrYGaLi

NbSeTaTiZrS

GoldAg -Cu -Pb -Zn -Mo -

Ni -Co -Cd -Bi -As -Sb -

Fe -Mn -Te -Ba -Cr -V -

Sn -W -La -Al -Mg -Ca -

Na -K -Sr -Y -Ga -Li -

Nb -Se -Ta -Ti -Zr -S -

IC01IC01IC01IC01IC01

IC01IC01IC01IC01IC01 IC01

IC01IC01IC01IC01IC01

IC01

IC01IC01IC01IC01IC01I C01

IC01IC01IC01

IC01IC01IC01

IC01IC01IC01IC01IC01

1C01

NUMBER OF ANALYSES

424242424242

4242424242 42

424242424242

424242424242

424242424242

424242424242

LOWERDETECTION

50.2

1211

11

0.255 5

0.011

10111

20201

0.010.010.01

0.010.01

1121

1510

0.0101

0.01

PPBPPMPPMPPMPPMPPM

PPMPPMPPMPPMDDU rrn

PPM

PCTPPMPPMPPMPPMPPM

PPMPPMPPMPCTpaPCT

paPCTPPMPPMPPMPPM

PPMPPMPPMPCTPPMPCT

EXTRACTION

Fire Assay of 30gHCL:HN03HCL:HN03HCL:HN03HCL:HN03HCL:HN03

HCL:HN03HCL:HN03HCL:HN03HCL:HN03 un uun7nu. t rinuj HCL:HN03

HCL:HN03HCL:HN03HCL:HN03HCL:HN03HCL:HN03HCL:HN03

HCL:HN03HCL:HN03HCL:HN03HCL:HN03HCL:HN03HCL:HN03

HCL:HN03HCL:HN03HCL:HN03HCL:HN03HCL:HN03HCL:HN03

HCL:HN03HCL:HN03HCL:HN03HCL:HN03HCL:HN03HCL:HN03

(3:1)(3:1)(3:1)(3:1)(3:1)

(3:1)(3:1)(3:1)(3:1)(3:1) (3:1)

(3:1)(3:1)(3:1)(3:1)(3:1)(3:1)

(3:1)(3:1)(3:1)(3:1)(3:1)(3:1)

(3:1)(3:1)(3:1)(3:1)(3:1)(3:1)

(3:1)(3:1)(3:1)(3:1)(3:1)(3:1)

icTumne i nuuSAMPLE TYPES NUMBER SIZE FRACTIONS NUMBER SAMPLE PREPARATIONS NUMBER

; DRILL CORE 42 -150 42 CRUSH. SPLIT 4230g Fire Assay - AA PULVERIZATION 42INDUC.INDUC.INDUC.INDUC.INDUC.

INDUC.INDUC.INDUC.INDUC.f km ir inu\A* .INDUC.

INDUC.INDUC.INDUC.INDUC.INDUC.INDUC.

INDUC.INDUC.INDUC.INDUC.INDUC.INDUC.

INDUC.INDUC.INDUC.INDUC.INDUC.INDUC.

INDUC.INDUC.INDUC.INDUC.INDUC.INDUC.

COUP.COUP.COUP.COUP.COUP.

COUP.COUP.COUP.COUP.COUP. COUP.

COUP.COUP.COUP.COUP.COUP.COUP.

COUP.COUP.COUP.COUP.COUP.COUP.

COUP.COUP.COUP.COUP.COUP.COUP.

COUP.COUP.COUP.COUP.COUP.COUP.

PLASMAPLASMAPLASMA REPORT COPIES TO: MR PAUL COAD INVOICE TO: MIKE KOZIOLPLASMA MIKE KOZIOLPLASMA

PLASMA This report must not be reproduced except in full. The data presented in thisPLASMA report is specific to those sanples identified under "Sample Number11 and isPLASMA applicable only to the sanples as received expressed on a dry basis unlessPLASMA otherwise indicated

PLASMA

PLASMAPLASMAPLASMAPLASMAPLASMAPLASMA

PLASMAPLASMAPLASMAPLASMAPLASMAPLASMA

PLASMAPLASMAPLASMAPLASMAPLASMAPLASMA

PLASMAPLASMAPLASMAPLASMAPLASMAPLASMA

Chimitec - Bondar Clegg, 1322-B Harricana, Val-d'Or, Quebec, J9P 3X6, Tel: (819) 825-0178, Fax: (819) 825-0256

CMIIVIITEC BONDAR CLEGG C!c2Sp2\

W* Rapport Lab Geochimie Geochemical Lab Report

i CLIENT: CAMECO GOLD INC.

j REPORT: TOO-57479.0 ( COMPLETE )

SAMPLE

NUMBER

ELEMENT A030 oAg- Cu IPb Zn Itiofl Ni lCpl; Cd JBil As j^b;;

UNITS PPB PPM PPM PPM PPM PPS PPM FW|PPM PPH|PPM PPM l

DATE RECEIVED: 06-DEC-OO DATE PRINTED: 14-DEC-OO PAGE

PROJECT: BRISTOL

1 OF 2

Fe ;:;|;Mrt;;; TE ftp Cr ffflVl; SnDPT ; DDU DDU DDU DDU DPU : DDUrui x.rrPP ::*"" rrn rrn rrTlx''"

;U;l La Mg Iles! Na jjKj- Sr ||| Ga ||i;| Nb Ip! Ta llTH Zr

PCT i : PGT:;': PCT PCT;-; PPM PPHuPPM PPpf^PPM PPM: PPM -iPCTx.PPM

7693

7694

7695

7696

7697

8 -i,21 10 *.2l

5 :x2; 3 ;x2:s III! 9 li

35

87

16

13

12

88

36

*s *;2: :; 6 ;::*2l is 112:; 9

;5 0.2 xs; *s ;;*5;;: 4.93 4ip;;*io;;9 0.3 *s *s ;;:*5;;^io.oo 8751*10;l?f*.21*5| 17 l*s!| 3.18 1:3261*10lix.2 !*5j *5 P5|! 2.56 i^xlO

l*!;!;! 59 ;;i! 113H123 fi;

'1:411123 ||

; 5 *20 ^2p:: :: 38 1^90 0.66 0.29 0.03 J2ft 5 SS9 6 sJK*5 *2o ^20143 3.7? 1.06 o;29 0.03sil;; s |i|| n 111;;;;

!7:x20 *2P1 29 1.28 0.35 0*70 0.01 iff! 12 :!!i'Pl 3 |l|!|

;;4;*20 *2p;; 41 i.26 0.32 0*97:0.03 s27 18 13; 3 ; 141;

16 sill; 23 pil43 p'j(75l 35 0.06

62 ;.2 17 lall 41:1;!; -^ iiMo ip 36 mm

7698

7699

7700

7701

7702

10 *;|s 11 11|1 39 vis;;; 4 ;;:;;;6;;;*.2 ^si *s l^sl 4.73*s *i'2:;; 7 ;;;:;: 4;;;; 30 ;;;;;;;;3;;; 4 ;i;ii*.z ;;::*is;::: *s ;xisii 3.70*s *;;2| 9 i*|| 43 H|; 6 i^x.z |*5;1 *s Wi s.zs11 JM!;; 11 HI!;; 31 l|3l: s !|6:;x.2 ;;|5i *s Ifsl 3.aas *.2l 23 ;1;5:; ; 7 li;; 4 lil*.2 W& *s : : ::*5i : :; 0.97

1(^1108 1151*20 mi 13 119510.46 !i;i79|;o.03 jjjj Z3 i|i 7 ||;: *1;S9; 97; ;3;;xzo *2o;; 46 1.57 0.33 1.so 0.03 a27: 27 ;;ilt;; 7 sift; *1!;;|41 as l||l*zo 3jfe s ilji|;;P.44 I*|i:!;!o.o2 iiii 471||;!; 6 ||l;! *116|1 89 ;;1;41*20 iS|:::: 22 ;i : i75;;;0.38 2i31:l0.02 ||p 36 1|S:;; 5 ||1;;; *1

;::7JJ1227 117:;*20 ^201 37 0.66 0.11 6;77l*.01 Uli 12 |lj|| 2 1141 *1

;;:|::;;*10 |;|| 7 PJ||

l||l*10 i:i||;;: 6 ||ji|;;;;;|||xlo ||H| 5 j||^ ;|ii;*io ilfl 45""'"""""""

7703

7704

7705

7706

7707

*s i*;?:'; 10 ;:;::4:; 13 :::;;::z;; 4 ;;;.'2!*.2 '^ ̂ 1*51 1.57*5 *.2l 3 li| 13 • ; '; ; ;2 : ; 4 l;2l*.2 1*51 *5 1*51 1.62*s ^i; 31 si 10 ;l3 : ' : 4 lfx.2 ;x5l *s :x5 : :;: 1-13*5 *.2 43 82 3 1 x.2 *5 *5 *5 0.95

*5 *.2 23 63 3 1 *.2 *5 *5 *5 0.71

185::126 ;;;; 51*20 23 Pi?40 PiS

Iii 10 flfi *2 lil

4171*10 53 152 ll| 1*20 pp 29 0.6| 0.12 1.63 0.03 ;3|;i 22

300 *10 53 150 1141*20 *20 33 O.W 0.09 1.26 0.04 .33; 16

274 *10 52 89 3*20 *2P; 47 0.54 0.09 1.35 0.05 .321 14

;i:4;;:*i

*i*5 *10*5 *10

•iiill 56 ft||p

44 0:02;39 biP2

7708

7709

7710

7711

7712

*5 *,2 5 : S; 8 4 4 1 1.4 *5l *5 *5; 0.88*5 *.2l 2 l|2l 18 li?!; 3 1.2^.2 !*|!; *5 1*5'!! 1.82*s *lz;; 1 ;x2: : ; is 1*1! 3 Il2lx.2 ;;:*5: 1 *s s*!; 2.077 *.2l 11 !.5:: ; 9 slzl 3 |; : 2|*.2 ::!*5l! *s !;!|t|| 1.34

*5 *'.'2" 7 ;l::4l 7 li: 3 li|x.2 ! : *5! *5 :xSl 0.87304: :

tt 113 :: 4x20 39 6.62;;o.ii i: PI ,18 Ii3i 3114!:; *iJ.591106 l|4l*20 *2p:;; : 32 0,881:0.20 !ll36|0.05 i24|; 14 I||;; 5 ||5| *1

61 102 ; 4 *20 *20; 29 0.88 0.16 pi79 0.07 il9j 10 fiSSs 5 5:44; *1;;;;4l!| 93 H4l*20 ^20| 33 0^641:0.13 !l : i.32i!o.06 Il9:: 12 fijl 4 |l|! *1:: ::47ll34 ;.:; ; 5l*20 *2pl 33 pi57;0.10 liilllO.06 Wl 13 111;: 3 Hill *1

*iPil

400-04

Pi(i|

7713

7714

7715

7716

7717

*,2 42 15*5 *.2l 13 H51: 6

5 *;i;; 18 i-31 9*5 *.2l 8 1141 11 40 *.2; 6 4: 9

7 1121*.213' 41:5;; sIz:; 3

2 3

1*5;;*;

2.04 ;^1.11 a1.47 1

1-50 12

1.20

;47;116 ;:29l*20 35 iipSO.28 i i3p;; is mi 4 mi 2: ;272l*10 :|82l192 1^61*20 *2P1 27 P^66l0.08 ;1:,36|0.02 i|?l 16 117;: *2 1141188;*10 ; 59 193 6;*20 *20 16 0.63 0.11 0.57 0.02 ^31: 7 9; *2 isjs

!:332|*io |53!| 95 !!!;!3|*2o *zo!; ; ; 42 Pi89!;6.i7 iiiplo.os ^i 15 |i9l 31||!;299*10 56 122 4 *20 *20 34 6:67 0.12 1.25 0.06 ,25; 13 231 3 14

f^ssxio iii.pi;;;; 46 piWfj;

!*5l;!*io *lpt! 56 om-:

*5 *io *.01 54 0:02:

7718

7719

77207721

7722

14 *.2 5 5 10 2 3*5 *.2;: 3 ;l4ll 16 li;; 3*s *;2" 7 'li!!! 19 :;|2;!; 35 *.:2x 7 !1; ; :4|;; 17 li! 3

124 *vi: 11 lli;; is ;;;li:; : 3

*5

*5

*5

*5

1.31 *10 69 129 4 *20 32 0,7i0.13 1,42 0.06 .27 15 23 4 51.68 1311 xl O 56 i 97 1.84 128511*10 |42|114

1.86 2941*10 ; 50; 106

1.91 19311*10 !36ll13

:4;;;*2o *zo: 17 0,75:0.12 ;i;25;o.o6 :22l u 126 4;; 4;: *1ll;*2o -526!;;;; 31 P,73!lo.ii :lib2|o.o8 !13| u |22l 6 lyli *1:::4l*20 ^P| 37 Pv76!l0.12 1i08l0.07 lil'; 18 lz|;! 6 f|3| *1

:;4.1*20 ml 42 Pi75':::0.13 Ol42: : 0.08 W&l 6 IjjS;!; 6 ll^l *1

Chimitec - Bondar Clegg, 1322-B Harricana, Val-d'Or, Quebec, J9P 3X6, Tel: (819) 825-0178, Fax: (819) 825-0256

1*5 *1O *.01 l 59 0.03;

;*5 *10 *.01; 67 p;P3|;

*5l*10 *|P1l 68 Oi02|*5l*10 *vPt 63 Pib2

CHIIVIITEC BOIMDAR CLEGG

Rapport Lab Geochimie Geochemical Lab Report

CLIENT: REPORT:

SAMPLENUMBER

77Z37724772577267727

77287729773077317732

77337734

CAMECO GOLD INC. TOO-57479.0 ( COMPLETE

ELEMENT AlfiO Ag;UNITS PPB PPM

<5 lil^ *;2;:

*5 *i2l<5 ^1?!

7 *;;2l

<5 II;5 am6 m6 S2is sif i

11:5 li*5 11

,

CuPPM

877

108

25186

165

14

62

III Zn

HP111 10::l :2l 10:l3l 10

ilS::i 9|p; 36

111 23s:;:;?! 52ml 221*:: 91*21319

Hi 12151 9

III; Ni i;||i; cd lil AS miDDU DDU DDU DDU DDU DDU DDU: : :rWJt : : :rrn rWtorrn rrfi; rrn FITT;

li 3 !ik2 liil <5 lil-::v?: : ; 3 111SK.2 ;M;:; <5 l^Sv'i&i 3 ilit.2 1*51 <5 ;1*5;31151; 3 |lix.2 1:*5| ^ l-sSlIf;; 4 11111.2 1*5;| ^ III;;III III ' III IIIIII 9 i!;*.2 lil *s lil121; 53 135i0.2 1*51 12 1*51131 4 Us*. 2 1*51 <5 1*51

S!?-;*:; 1:1:1:*" lilsl; * li:;:!1191 4 11110.8 ;:*5J; 7 1*5:;;;

Hi 4 lih.2 IS! <5 1*51111; 3 lJlx.2 1*1! <5 1551

Fe ill; TEDPT :;::DOW' :CDMrUI x fflpfll ::rrn

1.56 13011*101.76 256:*101.85 3001x101.11 12291*101.65 lJSi3!*10

3.26 lJS||i*108.82 *677l*102.15 1391*101.73 ISStt^lO7.07 17581x10

1.45 ||i;;Nio1.08 1217^10

DATE

lil! CrS*"

ill si1671: 93lisa! 86;:;81;:;1351791103

111 99HI: 901441106154! 95t6?! 34

1481143187;:;; 88

PROJECT: BRISTOL ; RECEIVED: 06-DEC-OO DATE PRINTED: 14-DEC-OO PAGE 2 OF 2 i

III Sn |i| La lil; Mg |!|i| Na Ifi Sr ;||| Ga 1|| Nb jjji Ta |||| Zr ;|||;PPU' 'POU DDU :DDU ': ' : ftPT : ' : ' Df T :vCNnnf*: : ; DT*T Df"T: ' ::DDU ODU^'DDU DJbii( ::: DDU DDU' 'DDU '-'OPT' &DU viv^f'^rrnxrrn ?Tn;:;rrn :::.rwl;x; rLI liKLi:;::: rUI rVix.rrn fTWorrn ppll^rrn WflS^rrn ;:.ffV:l!: : :;:rMi o.rvl|.;:;:

111^20 H| 27 ii|o.15 |l|i;b.07 HI 13 Ifl 3 ||I <1 ||I|x10 111 65 1||l|i;i*20 lib;! 35 iiisjlo.is oM|o.06 igs! 10 Mii 3 lip <1 i^slxio tfmji 63 ij-iprjil!x20 IM;! 38 py,93;;;0.20 fij^l0.06 iH! 14 fj9| 3 l|;:7l <1 ^1*10 S^OIl 60 iJi|S||11^20 is! 37 o^;;;o.i2 ililo.os jjji 12 lil! 3 li; <1 ;ili*io lil 62 lil;||;;;*20 H| 35 |||o.i8 |i|lo.o4 i|: u l||| 3 ||:; *1 ||i;;;xio gil; 61 ill

UNO li 31 ili|0.40 ilio.06 111 24 li 5 i|| 2 111^10 ||i| 58 gH234|*20 iol; 13 ii|l.46 SilB.05 HI 47 liii! 11 lHi 24 ;;|i^0 ij|| 12 (tm1151^0 *20i; 27 pj8l;:0.19 1^10.07 |J|| 15 HI 6 HI "1 1*51*10 Ijm 62 0;021ll!*20 *2|l 30 i|i;::0.19 115:10.04 i|| 15 iff 3 ifl *1 !||!*10 ^|| 57 ilHlIl^O ||l 23 liiO.65 |||!0.02 || 43 f|| 5 |||| *1 !H|*10 Jl; 6 |H|:|:|:;:;:;:|:|:: V:^:^:^:^ 1:1^:^!:! ^:^;^;^;^:: iii-S:::::-:: K-i-SSi: -iw:?:-: S:?#*i :::^:S :^::::::S:^

|||*20 li! 29 p^Tllb.12 b|H;:;o.03 iHl 12 ftl 2 ||| *1 ^^10 *f|| 42 i||:;:1|;::*20 ^jjj. 38 OlTSlO.OS SjlllO.01 1*! 8 lil 2 ill tl ft*10 5i|| 55 li!

Chimitec - Bondar Clegg, 1322-B Harricana, Val-d'Or, Quebec, J9P 3X6, Tel: (819) 825-0178, Fax: (819) 825-0256

CHIIVHTEC BOIMDAR CLEGG

Rapport Lab Geochimie Geochemical Lab Report

+

+

Q < O

u HH I-H

Sim

Chimitec - Bondar Clegg, 1322-B Harricana, Val-d'Or, Quebec, J9P 3X6, Tel: (819) 825-0178, Fax: (819) 825-0256

CHIIVHTEC BONDAR CLI

Rapport Lab Geochimie Geochemical Lab Report

REPORT: TOO-57485.0 ( COMPLETE )

CLIENT: CAMECO GOLD INC. PROJECT: BRISTOL

REFERENCE:

SUBMITTED BY: P. COAD DATE RECEIVED: 06-DEC-OO DATE PRINTED: 13-DEC-OO

DATE APPROVED ELEMENT

001211 1 Au30001211 2 Ag001211 3 Cu001211 4 Pb001211 5 Zn001211 6 Mo

001211 7Ni001211 8 Co001211 9 Cd001211 10 Bi001211 11 As 001211 12 Sb

001211 13 Fe001211 14 Mn001211 15 TE001211 16 Ba001211 17 Cr001211 18 V

001211 19 Sn001211 20 W001211 21 La001211 22 Al001211 23 Mg001211 24 Ca

001211 25 Na001211 26 K001211 27 Sr001211 28 Y001211 29 Ga001211 30 Li

GoldAg -Cu -Pb -Zn -Mo -

Ni -Co -Cd -Bi -As - Sb -

Fe -Mn -Te -Ba -Cr -V -

Sn -W -La -Al -Mg -Ca -

Na -K -Sr -Y -Ga -Li -

IC01IC01IC01IC01IC01

IC01IC01IC01IC01IC01 IC01

IC01IC01IC01IC01IC01

IC01

IC01IC01IC01IC01IC01IC01

IC01IC01IC01

IC01IC01IC01

NUMBER OFANALYSES

404040404040

4040404040 40

404040404040

404040404040

404040404040

LOWERDETECTION

50.2

1211

11

0.255 5

0.011

10111

20201

0.010.010.01

0.010.01

1121

PPBPPMPPMPPMPPMPPM

PPMPPMPPMPPMPPM PPM

PCTPPMPPMPPMPPMPPM

PPMPPMPPMPCTPCTPCT

PCTPCTPPMPPMPPMPPM

FYTDArTTfJUC A 1 Knl*l lUn

Fire Assay of 30gHCL:HN03HCL:HN03HCL:HN03HCL:HN03HCL:HN03

HCL:HN03HCL:HN03Ha:HN03HCL:HH03Ha:HN03 HCL:HN03

HCL:HN03HCL:HN03HCL:HN03HCL:HN03HCL:HN03HCL:HN03

HCL:HN03HCL:HN03HCL:HN03HCL:HN03HCL:HN03HCL:HN03

HCL:HN03HCL:HN03HCL:HN03HCL:HN03HCL:HN03HCL:HN03

(3:1)(3:1)(3:1)(3:1)(3:1)

(3:1)(3:1)(3:1)(3:1)(3:1) (3:1)

(3:1)(3:1)(3:1)(3:1)(3:1)(3:1)

(3:1)(3:1)(3:1)(3:1)(3:1)(3:1)

(3:1)(3:1)(3:1)(3:1)(3:1)(3:1)

METHOD :

30g Fire Assay - AAINDUC.INDUC.INDUC.INDUC.INDUC.

INDUC.INDUC.INDUC.INDUC.INDUC. INDUC.

INDUC.INDUC.INDUC.INDUC.INDUC.INDUC.

INDUC.INDUC.INDUC.INDUC.INDUC.INDUC.

INDUC.INDUC.INDUC.INDUC.INDUC.INDUC.

COUP.COUP.COUP.COUP.COUP.

COUP.COUP.COUP.COUP.COUP. COUP.

COUP.COUP.COUP.COUP.COUP.COUP.

COUP.COUP.COUP.COUP.COUP.COUP.

COUP.coup.COUP.COUP.COUP.COUP.

PLASMAPLASMAPLASMAPLASMAPLASMA

PLASMAPLASMAPLASMAPLASMAPLASMA PLASMA

PLASMAPLASMAPLASMAPLASMAPLASMAPLASMA

PLASMAPLASMAPLASMAPLASMAPLASMAPLASMA

PLASMAPLASMAPLASMAPLASMAPLASMAPLASMA

SAMPLE TYPES NUMBER SIZE FRACTIONS NUMBER SAMPLE PREPARATIONS NUMBER

DRILL CORE 40 -150 40 CRUSH, SPLIT 40PULVERIZATION 40

REPORT COPIES TO: MR PAUL COAD INVOICE TO: MIKE KOZIOLMIKE KOZIOL

This report must not be reproduced except in full. The data presented in thisreport is specific to those samples identified under "Sample Number" and isapplicable only to the samples as received expressed on a dry basis unlessotherwise indicated

001211 31 Nb001211 32 Se001211 33 Ta001211 34 Ti001211 35 Zr001211 36 S

Nb -Se -Ta -Ti -Zr -S -

IC01IC01IC01IC01IC01

IC01

404040404040

15

100.010

10.01

PPMPPMPPMPCTPPMPCT

HCLHCLHCLHCLHCLHCL

:HN03:HN03:HN03:HN03:HN03:HN03

(3:1)(3:1)(3:1)(3:1)(3:1)(3:1)

INDUC.INDUC.INDUC.INDUC.INDUC.INDUC.

COUP.COUP.COUP.COUP.COUP.COUP.

PLASMAPLASMAPLASMAPLASMAPLASMAPLASMA

Chimitec - Bondar Clegg, 1322-B Harricana, Val-d'Or, Quebec, J9P 3X6, Tel: (819) 825-0178, Fax: (819) 825-0256

CHIIVIITEC BOIMDAR CLEGG C!2SS*\

m* Rapport Lab Geovhimie GeochemicaLLabJR.epprt

i CLIENT: CAMEO) GOLD INC.

i REPORT: TOO-57485.O ( COMPLETE )

SAMPLE ELEMENT Au30 Ago: Cu If*:; Zn i:Mo;; Ni vGqi Cd i Bi ; As ESbi; Fe iiisMri; TE

NUMBER UNITS PPB PPMiPPM ml PPM PPMiPPM PPM^PPM PPMipPM ppi: PCT lpPMl;PPM

DATE RECEIVED: 06-DEC-OO DATE PRINTED: 13-DEC-OO

PROJECT: BRISTOL

PAGE 1 OF 2

Cr ;;;:yfi; Sn PPM PPH/PPM

La IIB Mg i;i;; :ca: ;; Na .f ;jf;;; sr |;g| Ga |ip Nb;PPM PCT PCT ptl PCT PtT PPM j^JliPPM IfJliPPM l

Ta S Zr :::;; ::?S:; -PPM ifpcfiJi

77357736773777387739

4 2; 84 2ii 3 ixtiO.4

9 s;;3;;;172 il;'2l 3 i 2 0.312 'i : ::;2| 48 ;:,3il 3 lii; : 2lx.210 x2 : 19 ; 3 3 ;x|x.210 x2:; i 22 il2;i 2 i'xiliix.2

-s<5

-64160

92 i

26 0.55 .05 1.0S x.01 33 b;64iii.07 0.37 0.01

28 0.59 .06 QM 0.01 37 0:72 .12 "" : ' : '""" : ' : ""

42 ll03 .19

i.if i; 2 lil;;;; <1::'1|| 3 131 1lilli 2 liii; <1!if| 4 i||l 1ill 5 ii! 2

^Oi|:i:i 53 0,17;;4bii;iii 53 diiiai;!^01 55 0.25:: : :

liiil 49 Iflli:

7740774177427743

7744

4 *.:2; :;; 12 |i : i2:; ; 22 ^m 3 :l'i2iix.2 jjSA <5x5 42? 12 i :;:i2i 30 iff;!; 2 ilfiix.2 iixsli <5<5 5.2:; 7 ixj:;: 19 li? 2 ;xlx.2 xjji; <5<5 5i2 6 ^2 20 ; l;; 2 :xf: x.2 J-cS; ^<5 *;f; 4 i;. :?;2iii 50 1;?! 3 lixi^-2 iisi? ^

519x10 ^B 121 ; 4i;x20 ^20; 27 pi95: -15 tiS2 0.01 S4J5 ; 10 siSp 459i;:x10 48:104 l : 3x20 *2b? 28 1.15;:.24 1^40 0.03 .Si;; 6 siitli 6

i : :453ii'XlO :;::52ii; 77 il2;;^0 *20iiii 34 0.92 :iii.20 l^iio.OS :;||| -ci Ip 4

i:ii442x10 iii;^iii 96 Ijj.^O ^1 36 0.82^^.16 1ii14iii6.02 ;^| 2 |||l 3

sffy- <1

III 1

1|;;; 2 lil i

ilp 21 ppItili 22 |ijic||*ibl| 56 biOli|

m i iis;;;xio 1101130 m7745

77467747

7748

7749

4 5:.;2l;; 12 :ix2 6 42 15 4 101 67 t;?-; 4 3| 79 13 ^2;i 7 4 i 17 ^ ̂ 2 3 <2 12

12s 2 9 X5i 5.04

2 11 0.4

2 8 0.33 lx.22 x1 x.2

8 l5 2.79 1161X10 74 120

46 xSi;0.99 445;^10 i 80 112

<5 X5 1.09 :334:x10 73 89

pi;;; 62 ;i||No ^i 251^1-36 p lil; 40 HI 9 liii 2126 2M10.01 iSil 50 lip 8 pi 2

;'|: :: ^0 ^0;i; 20 1.28li.21 3.6()'i:0.01 !47fi 57 lisif 5 |l|| 2i:4;ii^o i??o| 33 o;7oi;ii.o8 i:,44iiio.oi ^491 9 siiiij'i:; 2 l|;ii 13ix20 *20 38 0,72: .09 0-72 0.03 i40ii <1 ;18 3 ^ i 1

ill! slipIbjpi 10 oi^il;xi-blii; 12 b.05j4bii|i 32 icail e^OI 46 OsOI

77507751775277537754

^ *,2; 4^ 0.2 6<5 0.2 8<5 0.4 7

61164

135

7

^ 15

30 2 416 11; 5 7 1.1

x5 4.12 1499x10

cS 5.02 2074x10

x5 5.18 2001 ;x10

103 sx^i^O X?0li 36 0,:6ll08 b;78i;i0.03 JJRfl *V Iilii 2 il|| *:1 I^SsxIO iQll 54 tijfcj:100 ii4:i:^0 ^61 30 i.il|iii.21 1.54iii;0.02 !ii?|| 6 |||| 6 !f| 2 ;^!^10 4^1; 41 61^!;72 ;;.';2ii:i^0 x2b;i:: 30 TiS9!;?.4i 2^04x0.01 '*3^;;; 29 slSI 7 ::.:ii|| 2 |^5:::xlo *.01.: i: i 30 0.05;;;

76 iii'^^O K2p:ii 27 ll79il.39 2.65i: : 0.02 i^l 45 ill 8 ll|;i 2 l^SlixlO io|| 35 ^bfrli67 ;i;l5l^0 ^oi; 16 li;: 83i' : 'i.42 3;17j;:o.01 : :35:iv 63 lil*! 8 Il9i; i : 2 IM-xlO 4oil; 31 0;32l

7755775677577758

7759

^ 0.5; 71 ;x2 55 liii 14 28X.2<5 0:4; 55 i^i 96 iiiliii; 32 ^'^.2^ O'. :3i:: 33 l2-i'114 I'illii 33 v.2^^.2<5 0.5 75 <2 143 xl| 35 44 x.2

9 0.2 28 ^2 i 76 i 21 20 16X.2

11 ;:ifl5;;6.30 2688x10 194: 59 137x20 i?0i; 56 x5 4.82 29ti4x10 :63 40 28 x20 *20;

43 x5 4.88 2031 x10 ;57 44 S28 X20 *20

32 xS 8.85 2220 xl O 53 27 72 x20 ^0

13 l.: 6'l;i;.36 5ii25i;x.01 i^44iiiil37 i';l|i 8

3 2.29 .58 S;40; x.01 L38ll41 10 14

JiNo

25 x5 2.30 1195x10 39il38 s 17x20 ^ 20 0.95 .20 2.69 0.02 .Sis 42 11 4

4

2 !x5|x10 iibi?;3 IfrxlO i.058ii

27 If!! 13 |S|pi 22 0^44

19 i:i4 22 0^05

77607761

776277637764

6 0,3 22 X2; 80 f 16 17 x.2 x5 24 x5 4.83 18261^10 45 54 19 <20 -c20; 22 1.79;i.45 4.07 <.01 ;39l 67 112 i^ 0.3 8 1^2': 66 i 3 ; 3 1:3:0.2 ii^5 ^ *:5i3.90 1202ii^10 i42 90 4x20 ^20 24 1.39;iii.26 liilSSlx.OI ii-Zp 9 i^piil<5 Oii'21 5 ;iiii:2; 8 121 3 '^ix^ Mi; <5 |*5;!;1.12 ;i282ix10 i;i.63l: 94 ^•eo *ZO 30 0.56;;.06 Oi37 : :x.01 |||!i <1 |||i

^ 4.2': i 6 x2i 5 :i 2:: 6 ;x1x.2 :x5l *5 x5 0.60 i 172x10 33li280 ; 10x20 x20; 15 Oi;27l.02 0^25 x.01 lli?! <1 |:||<5 -:.2 4 ^2 12 i 2 4 :x1x.2 x5 <5 X50.69 296X10 56iil78 ; 7x20 520;: 34 0.481.04 0.52 x.01 :;3l| <1 ill6l

12lii; liplil

.019 18 0.11

.bil:i^5::x10

i;*5.;i;xio

38 O.p9iii 48 b^2iS 23 b:pj

Chimitec - Bondar Clegg, 1322-B Harricana, Val-d'Or, Quebec, J9P 3X6, Tel: (819) 825-0178, Fax: (819) 825-0256

CHIIVIITEC BOIMDAR CLEGG

Rapport Lab Geochimie Geochemical Lab Report

CLIENT: CAHECO GOLD INC.

REPORT: TOO-57485.O ( COMPLETE )

SAMPLE NUMBER

DATE RECEIVED: 06-DEC-OO DATE PRINTED: 13-DEC-OO

PROJECT: BRISTOL

PAGE 2 OF 2

7765

7766

7767

7768

7769

7770

7771

7772

7773

7774

6 (fcS <5 Ols <5 b;3 <5 isl

2J 45 l

5 238 l

25545 ii|l72

5 li; 20

4 If 0.3 34 |3fk2 42 |fl-k2

19 19 3 i

<5 III 18 1*1;: 20 III 3 1110.3*5 If! 21 llfl 20 111 4 iipkZ<5 *;;|s 4 r*2l: 35 : ;;;;:|l;l 3 lil;*.2<5 *:i.2| 4 I;jc2|; 13 ilil 3 ;;*iil: *.2<5 HI 4 li 5 ill 3 ilx.2

*5 i||l.43 l||l*10 |f|| W |1|*20 35 1*515.40 24||;x10 ||i 57 ?|||*20 63 3^^4.49 !!|ji;|;x10 iSfifJ 46 :?2JiK:'^ <5 |*5l0.77 1I||;H10 ITS;;: 158 ||;6;;!*20 <5 11*520.40 sJSijixlO SS13130 li;ift-;i*20

<5 ;1||0.43 |; 6 |^|0.96 Ii <5 PN.83 l^ i: :;:t5;;:;0.74 I<5 |p!0.48 i

iTii 91 1111*20

||145 i I?i|l09 i

35 ^6||.08 pOjsO.01 SiJSl *1 i^|| 9 p||.26 Sipikoi |||| 86 i

*20. : : 38 0^5^4:-.03 ^*5T:^*.01 ^38^ 9 ' 42Sk 46 0^49^.02 Oii68-:X.01 ^41^ *1 ^

i||i; 46 1^1.02 ||^||*.01 |3i|| i*20l 43 OiSSp.OS 6w6^;0.01 1SS|

iii 46 Ol5|l.02 1111:0.01 lil;

;!;5i5;:^10 SiWf'S 62 tlii35;s ;:;S5;ii*10 S047s 22 iifi7:iiiliHo ii|i is ii|ij:;:jiiS:s*10 *iiOi; :5: 60 jBififti:!

11*10 lil 49 III

l 3 111 1 ii 9 Hi 3 \i 6 IHI z ii 2 111 *i ;

i;i;2|;;:; *2 ^p| *1 ^p*10 SiliPp 46 ^ till 3 i|| 2 lii*10 |i||| 58 pipm 2 nil 21111*10 iii 59 im•jStijj: Z |||| 2 |i|;;;;*10 pill 49 i|ji||| 111 *2 III 1 H*10 I|| 52 |IH

Chimitec - Bondar Clegg, 1322-B Harricana, Val-d'Or, Quebec, J9P 3X6, Tel: (819) 825-0178, Fax: (819) 825-0256

BOIMDAR CLEGG

Rapport Lab Gec^nimie Geochemical Lab Report

+

u

QJ J

ISSiSU 2 *fc OT PH

+

Chimitec - Bondar Clegg, 1322-B Harricana, Val-d'Or, Quebec, J9P 3X6, Tel: (819) 825-0178, Fax: (819) 825-0256

CMIIVIITEC BOIMDAR CLEGG

Rapport Lab Gec~nimie Geochemical Lab Report

REPORT: TOO-57486.O ( COMPLETE ) REFERENCE:

CLIENT: CAHECO GOLD INC. PROJECT: BRISTOL

SUBMITTED BY: P.COAD DATE RECEIVED: 06-DEC-OO DATE PRINTED: 14-DEC-OO

i DATE i APPROVED

l 001213i 001213i 001213i 001213i 001213i 001213

i 001213i 001213i 001213i 001213i 001213 \ 001213

! 001213i 001213j 001213i 001213i 001213i 001213

; 001213; 001213i 001213! 001213; 001213j 001213

; 001213i 001213i 001213i 001213j 001213i 001213

i 001213i 001213i 001213i 001213i 001213i 001213

123456

7891011 12

131415161718

192021222324

252627282930

313233343536

CI CUCUTNUMBER OFAUAI VOeeCLcnCN i mini- i onj

Au30AgCuPbZnMo

NiCoCdBiAs Sb

FeMnTEBaCrV

SnWLaAlMgCa

NaKSrYGaLi

NbSeTaTiZrS

GoldAg -Cu -Pb -Zn -Mo -

Ni -Co -Cd -Bi -As - Sb -

Fe -Mn -Te -Ba -Cr -V -

Sn -W -La -Al -Mg -Ca -

Na -K -Sr -Y -Ga -Li -

Nb -Se -Ta -Ti -Zr -S -

IC01IC01IC01IC01IC01

IC01IC01IC01IC01IC01 IC01

IC01IC01IC01IC01IC01

IC01

IC01I C01IC01IC01IC01IC01

IC01IC01IC01

IC01IC01IC01

IC01IC01IC01IC01IC01

IC01

323232323232

3232323232JC.32

323232323232

323232323232

323232323232

323232323232

LOWERDETECTION

50.2

1211

11

0.255 5

0.011

10111

20201

0.010.010.01

0.010.01

1121

1510

0.0101

0.01

PPBPPMPPMPPMPPMPPM

PPMPPMPPMPPMDDUrm PPM

PCTPPMPPMPPMPPMPPM

PPMPPMPPMPCTPCTPCT

PCTPCTPPMPPMPPMPPM

PPMPPMPPMPCTPPMPCT

EXTRACTION

Fire Assay of 30gHCL:HN03 (3:1)HCL:HN03 (3:1)HCL:HM03 (3:1)HCL:HN03 (3:1)HCL:HN03 (3:1)

HCL:HN03 (3:1)HCL:HN03 (3:1)HCL:HN03 (3:1)HCL:HN03 (3:1)UPI . IlkVTC /7 . 1 \nLL:HNQj (.3:1} HCL:HN03 (3:1)

HCL:HN03 (3:1)HCL:HN03 (3:1)HCL:HN03 (3:1)HCL:HN03 (3:1)HCL:HN03 (3:1)HCL:HN03 (3:1)

HCL:HN03 (3:1)HCL:HN03 (3:1)HCL:HN03 (3:1)HCL:HN03 (3:1)HCL:HN03 (3:1)HCL:HN03 (3:1)

HCL:HN03 (3:1)HCL:HN03 (3:1)HCL:HN03 (3:1)HCL:HN03 (3:1)HCL:HN03 (3:1)HCL:HN03 (3:1)

HCL:HN03 (3:1)HCL:HN03 (3:1)HCL:HN03 (3:1)HCL:HN03 (3:1)HCL:HN03 (3:1)HCL:HN03 (3:1)

METHODi SAMPLE TYPES NUMBER SIZE FRACTIONS NUMBER SAMPLE PREPARATIONS NUMBER:

\ DRILL CORE 32 -150 32 CRUSH. SPLIT 32 i30g Fire Assay - AA PULVERIZATION 32 iINDUC.INDUC.INDUC.INDUC.INDUC.

INDUC.INDUC.INDUC.INDUC.f uni IP INDUC.INDUC.

INDUC.INDUC.INDUC.INDUC.INDUC.INDUC.

INDUC.INDUC.INDUC.INDUC.INDUC.INDUC.

INDUC.INDUC.INDUC.INDUC.INDUC.INDUC.

INDUC.INDUC.INDUC.INDUC.INDUC.INDUC.

COUP.COUP.COUP.COUP.COUP.

COUP.COUP.COUP.COUP.COUP. COUP.

COUP.COUP.COUP.COUP.COUP.COUP.

COUP.COUP.COUP.COUP.COUP.COUP.

COUP.COUP.COUP.COUP.COUP.COUP.

COUP.COUP.COUP.COUP.COUP.COUP.

PLASMA iPLASMA ;PLASMA REPORT COPIES TO: MR PAUL COAD INVOICE TO: MIKE KOZIOL iPLASMA MIKE KOZIOL iPLASMA i

PLASMA This report must not be reproduced except in full. The data presented in this iPLASMA report is specific to those samples identified under "Sample Nuifcer" and is jPLASMA applicable only to the samples as received expressed on a dry basis unless iPLASMA otherwise indicated iPLASMA ****************************M************************************************** :

PLASMA i

PLASMA ;PLASMA jPLASMA iPLASMA jPLASMA iPLASMA :

PLASMA ' lPLASMA iPLASMA !PLASMA iPLASMA iPLASMA i

PLASMA iPLASMA iPLASMA :PLASMA iPLASMA lPLASMA j

PLASMA iPLASMA :PLASMA iPLASMA iPLASMA iPLASMA ;

Chimitec - Bondar Clegg, 1322-B Harricana, Val-d'Or, QueTjec, J9P 3X6, Tel: (819) 825-0178, Fax: (819) 825-0256

CHIIVIITEC BOIMDAR CLEGG

Rapport Lab Geochemical Lab Report

CLIENT: CAMECO GOLD INC.

REPORT: TOO-57486.0 ( COMPLETE )

SAMPLE

NUMBER

7775

7776

7777

7778

7779

7780

7781

7782

7783

7784

7785

7786

7787

7788

7789

7790

7791

7792

7793

7794

7795

7796

7797

7798

7799

7800

7801

7802

7803

7804

ELEMENT Au50

UNITS PPB

55

55

55

55

55

55

10

55

55

55

55

55

55

55

13

555

555

55

55

55

55

55

55

55

55

555

55

mppHl

5.2}

5 :,2: :

5.2:

X.*:

(l

w*ti5"2''

5/2!liH*l2l5; 2

5.2

''-l

5^2'

0;30^2:5.2

5.2

**l5.2:*-2'

0.3

0.2

5.2'

0.2

5.2;5.2

*.2

Cu

PPM

; s6

9

3

3

6

8

: 736

47

: 48129

10

7

67

67

75

70

48

47

42

73

71

41

30

21

6

34

33

39

Pb : zn ;;PPM PPM F

it j H iIIP! 11l/?! H ^

21; 14 ;ill 7 : '

l;|7l 13 ;;I:-*! s ;;i*l 77 .

8 202

le;;i63 ;

Ip; 66 lle: 1488 74

6 292

2 141

52 112

52/123 :'

x2 135 ::2 83

li 114 ;Hi! 96 i:

x2i8o ;*2 166

X2 58

52 91

52 16

x2 107 ;*2 87

/52 : : 95 ;

M Ni

VK PPM

/:-2! 2

14:1 4;!2| 4/'f! 4

/?! 3

lil sli! sli:-; 3W- 24

III 58

2:170

! : 2/; 55/ s;;; 4/2/ 3

2 21

.12;;; 20Izi 19

;|:3:| 21|2| 12

m 14

|3|; sl:?! 22

| :2l 30

li! so: 3 : 24

2 28

2 Hm 33:;!:2/: 41!:f2:: : is

mPPH: :

li/

Ixl!111!ill!'

li;IpI/ly

li:. :'2V:

Mw:4P!-'2; '

136

Ip

Hilid!34

133.

Ip

46:!4i-;;4i!/se-

26

I/5: 30:

is24

cd ; iiiPPM PPM

x.2 m1.0 /5s;0.2 x50.2 X5

i"' 2 li

x 2 lil

x.2 1*5;;

0.2 i|:

0.7 Is!

0-5 11

x.2 illi

0.5 i*!

0.3 ; xs:;1.1 *5

0.3 *5

; 0 4 ;i|*^2 1*5!0.5 1*1

:'0.2 /5S;

'0.5 lis!

0 9 "l!

0.6 1*5;;0 -4 *5

0 -4 1x5';:0.4 55

0.4 55

5.2 55

5.2 55

5.2 *5

0.4 : 55

;; AS ;;;:sb;;PPM PPM

i *s Ili: 55 : ;'^Si"

: *s ;::x5::; 55 ;-; : 55; ; ;

; *s oxs;;

i ^ llg!

; <5 lli;;; 55 "XJ;l 31 |*5|

^ 55 'S

l 59 IxSl

' 55 ;; : ;*5;;; *s |*:5/ : *s : ;x5-:

11 : *5

: : *5 ..xs:;: ; *5 :'X5:f

;; 55 r^s;;: 55 ;;x5: ;l *5 li:

;; *s 1*5;;; 55 i^s: : 55 : ;i:55:; : 55 1*5-;

55 55

55 55

55 ; 5555 ; 55

]; : 5 ; *5

: ; "5 /*5"

DATE RECEIVED: 06-DEC-OO DATE PRINTED: 14-DEC-OO

: Fe //Kriy TE /Bi/ Cr //V/ Sn g/W/: La l.jjtt. Mg //C^/ Na !!K;: Sr

PCT PM PPM Pp|i;PPM PPM PPM PPH PPM PCT PCT PCT PCT PCT PPM

0.63 liHxlO ;;:65|; 78 lilNo ml 35 pPp.03 bi9p!5.01 i33! 18

0.47 11)3 X10 65! 99 ! 2/520 iZpl 43 pl44!o.03 p/,74 0.01 i3S| 18

; 0.70 I28p:5l0 6b|l07 ;|;|| : |*20 5?P/ 37 0,39|o.04 0,69 0.02 .29/ 14

1.09 441*10 54 100 |l X20 520| 32 6^59 0.10 IM Ip. 01 iZSl 13

; 1.26 |3ji;*10 Isj! 95 12/520 x2p| 24 i)|li;0.11 P&.01 HI 12

ilx/Vxl; ^iv;!::;/: i:;!!:!!-;! .i./'oxiy: :H-!I' : I:| : :: : :V ^viv l:;/^:^!

1 01 314:*10 33 153 2 x20 ^20 32 0^47 0 09 0 66 : 0 02 ^20 ^ 11

~- '" U* i;:;/^";;;; xi^ox!;:- !oll'.;:;; ^^::i rfx^;'/ " /"/^i^o: " x^'ii:

0 88 ; j47 xlO 59" 79 : 1 : :^0 -cj^J : 32 0 53 0 08 0 A^ 0 02 ^3iJ 15

4.39 1*2; X10 5| ; 37 12 520 m ti 10 pBlfo.47 3J77 0.01 |4J| 87i *- 96 Sir10 il! ** ^llh0 Pi 7 IS/1 '23 IS j0 ' 01 lip; 4.66 llsINo !;3|!187 ||i*20 HI 11 3l4f;2.68 Pl!;*.01 ||||l92

9.36 22031*10 |!j|| 77 ^1*20 x20/ 9 4i22 2.14 4.02 0.07 .2|l01; 0.90 ;;i^2i!:*io /67/102 f 5|*20 520! 32 6|s2 0.09 1.23 *.oi .3i| 26; 1.04 603/xlO /72;! 85 | 2 x20 *2o:; 31 0-58 0.06 1,16 0.02 .il! 21

; 8.03 28461*10 laSl 20 45:*20 *2p 5 2;42 0.98 5.27;5.01 ,41;139

8 37 Iip5l0 Ipi 22 IllUo il : 6 I'l^l 41 I'Pp 01 lPl97

9.28 1^7 *10 36 15 154:;520 X20 5 3.99 1.61 3;9p;0.02 |li;'l82

;>10.00 3595X10 'ffi 17 174/520 *2Q 5 4.40 2.37 4;37 0.02 105/157

8.10 3JJB7 *io 64 18 58 520 520: 9 3.03 0.99 3.98 0.03 Iz|:;;i00

^10.00 3588 510 79:; 11 112/520 520: 9 4:^52/1.55 3.81 0.02 ,1l| 88

7 37 2725 *10 66 22 64/520 x20 12 2.82 0.86 3 81 0.04 vl8/ 81

yio.oo 3132 xio ;;26;! 9 i34:|52o liipl 10 4^741.77 133/0.02 ^3! SB8.69 1728x10 ; 21 ; 30 138 X20 *2o| 8 3,78 1.31 4;67 0.03 pi!; 84

; 8.19 1607 *10 /16 54 119*20 520: 9 3.84 1.53 5/77:0.02 .15 85

9.77 1542 510 4 28 155 520 *20 8 4.53 1.81 4.23 0.03 ;0i 39

8.25 1864 510 19 35 59 '520 x20 7 3.81 1.22 4.08 0.02 .19 31

1.53 289 5io 5 196 :14;520 X20 Z 0^60:0.20 0.88:0.01 .136 8

; 8.15 1671 X10 12';::: 49 ;|73|x20 520l; 7 3;94;i.35 4,17|0.02 lil! 30

^10. 00 1714/510 292! 40 1651:520 *2o! 5 4.08 2.38 2,40|l0 - 05 *5|l 47

: 7.64 1606 *10 114/ 59 10p!:520 520; 3 2.64/1.53 3;49::0.09 ill 35

Ililppilil1-23'-

l??: iillil|flil20

!l|;

li

1111-15!

1!?:|l.6l

li;||;;|;p;III-ffi;111

;1|111i'9:•M./12'-

li?lli111IP111

Ga

PPM

i*2

*2

52

52

*2

52

52

52

*2

*2

1 3

8

*2

*2

h2i; 4

9

7

l 51 8

8

8

9 : 7

11

5*2

: 6

7

3

PROJECT: BRISTOL

PAGE 1

III:(Hi::

HI;/!2:

;. |2;i.i//j';:

111:1IIIlil:in111I42-:Sii:

!- ;4:

lil

ml?l11lil

IIIlil:l22:;:l29:/24

w; /3:M|;23; ;!l4!

; Nb

PPM

51

51

2; *ii*1

l ^l *1; *1*i

M1

;; 221*1

: *1

3

i; 7

1317

4

;: 8

i 4

i; 1212

11

14

2

;; i:; 5

; is9

OF

/lilHi;a1*5;;! :*5y1:^5:

ill

li!l*?!

li;

111121:s*?!!;*5; :II:

111

Iii/li11ill: ; ;lo/::9:

17:

il!*5: ;my/7;!*5l

2

: Ta /Iff/ Zr

PPM PCt/PPM

xlO ^Olo 45

x10 *.0l! 45

*10 *.01 50

*10 *iOi; 45

X10 SP1 45

Mo 111; 39*10 *.Wt;;;; 58

:;*io i:ii| 42*10 ^020 24

l*10 111 14MO 111 32*io iisel; s;*10 *;:p|j| 53*io *.pi;; 53

;i*io ;.p46l 20

;;*io i||: is

;*io Ip3i; 12;xio jjjjjft 20r10 PM 21Mo ipssll is*10 i.051 ; 18

xio Ip4l 16

;;*io iipsi-:;; 12Mo ;:3i9l 5

ixiolii sX10 .071 2

;*io izs:;;;; 3xio ;433;;; ; 51;xio l|i*i 5i

ill/lil

ill!i, 04!.19;10

111

Pi;Hi/os;;;.60

lililliii'lii;

.14;;;

.20

'7S|

ipIII!wi.f4p|

illiiiilil||i;!

••60il'24-:

ft.02;:;

ii;45|

S'2p|

Chimitec - Bondar Clegg, 1322-B Harricana, Val-d'Or, Quebec, J9P 3X6, Tel: (819) 825-0178, Fax: (819) 825-0256

CHIIVHTEC BOIMDAR CLEGG

Rapport Lab Ge^Jiimie Geochemical Lab Report

i CLIENT: CAMEO) GOLD INC.

i REPORT: TOO-57486.0 ( COMPLETE ) DATE RECEIVED: 06-DEC-OO DATE PRINTED: 14-DEC-OO

PROJECT: BRISTOL

PAGE 2 OF 2

SAMPLE NUMBER

78057806

! 38 62 :i 14 |0.2 i!! <5 ?74 il01 ;|;|;;: 24 10.4 ;is| <5

5.90 c10 I15

35

*lf!:0.06 |||| 38 H;|6;i; 3 ||j| 8 |fMO 2'i^ls0.02 WU 32 is? 9 i?il 19 11^10

Chimitec - Bondar Clegg, 1322-B Harricana, Val-d'Or, Quebec, J9P 3X6, Tel: (819) 825-0178, Fax: (819) 825-0256

ONTMIO MINISTRY OF NORTHERN DEVELOPMENT AND MINES

Transaction No:

Recording Date:

Approval Date:

Client(s):

114820

Survey Type(s):

W0160.31022 2001-NOV-02 2001-DEC-21

Work Report Summary

Status: APPROVED

Work Done from: 2000-NOV-15

to: 2000-DEC-07

CAMECO CORPORATION/CORPORATION CAMECO

ASSAY PDRILL

Work Report Details:

Claim*

P 985616

P 985625

P 1226640

Perform

310517

329

357

,744

,907

,042

,693

Perform Applied Approve Applied Approve

310,744

317,907

329,042

357,693

30

30

50

50

SO

SO

SO

SO

Assign Assign Approve

305030

50

000

so

Reserve

510,517,529,

S57,

744

907

042

693

Reserve Approve

310,744

317,907

529,042

557,693

Due Date

2002-JUL-06

2002-JUL-06

2002-MAR-26

Status of claim is based on information currently on record.

42A06NW2030 2.22349 BRISTOL 900

2002-Jan-06 22:02 Armstrongji Page 1 of 1

Ministry ofNorthern Developmentand Mines

Date:2001-DEC-21

Ministers du Developpement du Nord et des Mines Ontario

GEOSCIENCE ASSESSMENT OFFICE 933 RAMSEY LAKE ROAD, 6th FLOOR SUDBURY, ONTARIO P3E 6B5

CAMECO CORPORATION/CORPORATION CAMEC(1349 KELLY LAKE ROADUNIT #6SUDBURY, ONTARIOP3E 5P5 CANADA

Tel: (888) 415-9845 Fax:(877)670-1555

Dear Sir or Madam

Submission Number: 2.22349 Transaction Number(s): W0160 31022

Subject: Approval of Assessment Work

We have approved your Assessment Work Submission with the above noted Transaction Number(s). The attached Work Report Summary indicates the results of the approval.

At the discretion of the Ministry, the assessment work performed on the mining lands noted in this work report may be subject to inspection and/or investigation at any time.

The revisions outlined in the Notice dated Deceber 12, 2001 have been corrected.

If you have any question regarding this correspondence, please contact LUCILLE JEROME by email at lucille.jerome@ndm.gov.on.ca or by phone at (705) 670-5858.

Yours Sincerely,

Ron GashinskiSupervisor, Geoscience Assessment Office

Cc: Resident Geologist

Cameco Corporation/Corporation Cameco (Claim Holder)Marian (Mike) Koziol (Agent)

Assessment File Library

Cameco Corporation/Corporation Cameco (Assessment Office)

Visit our website at http://www.gov.on.ca/MNDM/LANDS/mlsmnpge.htm Page: 1 Correspondence 10:16684

NCftTHlKil UbVtUh MbR(

urn iiPti

PROVINCIAL HIMttC

MINING LAND TENURE

MAP

1*'

120.11m^—ii^-—^ 1226486

j 98SB3'*^,M, 98JS34 98*633"""" : - ""

..98S739 j 985746 SV9S5747'ZI/'SP/S

j ^

1203840

, lm'- ..l---*{ 12025ZA. "S,"•"a ITr?!*!*. A-/-^"--/- - -r-i : l irm K,5-

^/"•^^^^^^g^^^nr^ ";:f;^-M I \MW67\ ,^L

\ 1193477 /fi4 ' f ft \'\

^...^^,...,._^^^Mm.^^ ,- , . , j ' ———",.-v.,,^,.. B . , .,,

General Information and Limitations

Cala/ Time of ISSUB N[iv22001

TOWNSHIP r AREA

BRISTOL

14;58h Eastern

PLAN

G-3 998

ADMINISTRATIVE DISTRICTS l DIVISIONSMining Division Porcupine

Land Titles/Registry Division COCHRANE

Ministry of Natural Resource* District TIMMINS

TOPOGRAPHIC LAND TENURE

a ,,

m

ID-cenct ut

aL -cenct ut (X ru

Qm

sD

LAND TENURE WITHDRAWALS

IMPORTANT NOTICES

LAND TENURE WITHDRAWAL DESCRIPTIONS

nl HW' iUb Jt-, i u L HW LI JvL fLKMH T Ml'j MOM/MMUM W. W

n i ran JipPiirjtTKVN r OP CPOWH L AM D UNO r R inr pnnur1 JLHM-S ncr NOTICE nUJHAY 4'.'^D LXIAVAHUN l Wl' SUl HHLUH! -s. l UK J i, l L 11,..-

IMPORTANT NOTICES

o o

oH CO H Km

iB lin Ctoi* ilw cvtin 4iwi iHitii- sod

464691E

5365431IS

G-

200

-O*

46489 IE

5365080N

250 300 350 400 450 500 550

46445.0E

464I50E

\ IP AnomalyIP Anomaly

.•...v-v-/'.,,::. .;.-.:..^.', ^ *. •'.-v':i''-'r'j'^V^-'^::^-V';, ; :^TJtTT?^.*-;'"i'/f-xi.v--';-"'"i V •'.•/•\./..::^'::v:.-^:-^V':"; :V^^.V:::\

-.:.'.; •,^.--;. •//.•x,'- .'•.•..f.,-.-'.;. ,:-,.^'r •.' v ''"-'' r- ''J Ni'"'^ ̂ -'''•-"*.1'; .'y- V,,' t- "-'

"' ','i ';'\-!'...' .'",t'';. ;*''.- .•..'".'1 -':''"v'''-.' i*

-50

-100

-150

-200

42A06NW2030 2.22349 BRISTOL 210

DRILL HOLE LEGEND

LHS Posting Au (ppb)

RHS Posting : Quartz veinlets abundance

RHS Posting : Structures

LHS Bargraph : Au (ppb)

RHS Bargraph : Quartz veinlets abundance

Drill Log : RockCode

GEOLOGICAL LEGEND

mafi:: volcanicsmafi:: volcanic schistquarlz-tourmaline veinfelsic volcanic, rhyolitemafi: intrusive, lamprophyreOverburden

Structure Legend

"^-s schistosity"^-^ shear^--c contact~-—-f foliation""--ft fault"——f, fracture Cameco

Compiled: D B , M K

Bristol Project

Vertical Geological Cross-Section, L40+OOE Oriented 150-330, Looking Southwest

BRS00'04 and 05Dwg. No.: BRI01003

Drafted: D e , c.o.o Date: QT/10/03Scale: i: 500 NTS Ret.:

Map 2Geo. Ref.: Source:

464176E

5363712N

464375E

5-363345N

50 100 150 200 250 300 350

536365QN

464150E

IP Anomaly

464050E

5363950N

-50 i--

-100

-150

-200

-250

DRILL HOLE LEGEND

LHS Posting : Au (ppb)

RHS Posting : Quartz veinlets abundance (07o)

RHS Posting : Structures

LHS Bargraph : Au (ppb)

RHS Bargraph : Quartz veinlets abundance

Drill Log : RockCode42A06NW2030 2.22349 BRISTOL 220

GEOLOGICAL LEGEND

mafic volcanics mafic volcanic schist quartz-tourmaline vein sediment, greywacke siltstonegraphitic argillite Overburden

Structure Legend

~----. schistosity~~--s/, shear ~----e contact "----f foliation ^---. fault

fracture-fr

10 20 30

2 9 O 9 4 Q A..,- ,W ^J -- -J Scale l 500

CamecoGOLD

Bristol ProjectVertical Geological Cross-Section, L27+OOE

Oriented 150-330, Looking SouthwestHole BRSOO-03

Compiled: D B . M K Dwg. No.: BRI01002Dratted: D.B . C.D.D Scale: i SOP NTS Ref.:

Date: 01/i 0/03 Geo. Ret.:-^^-^^ Source:

Map l