Spences Bridge Properties

Frontispiece. View west from the Clear Range toward the Coast Mountains. 2006 Exploration Program

Spences Bridge Area (NTS 092I/05 & 092I/06 ),

Kamloops Mining Division, Southern British Columbia

for

Bitterroot Resources Ltd.,

by S.T. Flasha (B.Sc.) & C.J. Greig (M.Sc. P.Geo.)

January 26, 2007 TABLE OF CONTENTS

1.0 Summary of Field Program and Results ...... -1- 2.0 Location, Access, and Physiography...... -4- 3.0 Claims ...... -6- 4.0 Geologic Setting & Mineral Occurrences...... -6- 5.0 Stream Sediment Geochemistry ...... -9- 6.0 Soil & Rock Geochemistry ...... -16- 7.0 Recommendations...... -16-

LIST OF FIGURES & TABLES

Frontispiece. View west from the Clear Range toward the Coast Mountains. Figure 1. Location of the Spences Bridge properties, southern British Columbia...... -2- Figure 2. Location of the Spences Bridge properties, showing selected producing mines and significant mineral occurrences in southern British Columbia...... -3- Figure 3. Spences Bridge properties claim locations, Kamloops Mining Division, southern British Columbia...... -5- Figure 4. View east down the valley of Murray Creek, toward the community of Spences Bridge, southern British Columbia...... -6- Table I. Claim information, Spences Bridge properties...... -7- Figure 5. Regional geology, showing location of the Spences Bridge properties and selected producing mines and significant mineral occurrences in southern British Columbia. . -8- Figure 6. 2006 silt and moss mat sample locations, eastern claim group...... -10- Figure 7. 2006 silt and moss mat sample locations, western claim group...... -11- Figure 8. Gold geochemistry in stream sediment samples, Spences Bridge properties...... -13- Figure 9. Copper geochemistry in stream sediment samples, Spences Bridge properties. . . -14- Figure 10. Zinc geochemistry in stream sediment samples, Spences Bridge properties. . . . . -15- Figure 11. 2006 soil & rock sample locations, Spences Bridge properties...... -17-

LIST OF APPENDICES

Appendix I. Stream Sediment Sample Locations & Geochemistry Appendix II. Soil Sample Locations & Geochemistry Appendix III. Rock Sample Locations, Descriptions, & Geochemistry Appendix IV. Cost Statement Appendix V. Statement of Qualifications

-i- 2006 Exploration, Spences Bridge Properties, Bitterroot Resources Ltd., by S.T. Flasha & C.J. Greig

1.0 Summary of Field Program and Results

Fieldwork conducted in 2006 on the Spences Bridge properties of Bitterroot Resources Ltd.

consisted primarily of stream sediment geochemical sampling, with lesser rock and soil sample

collection. A total of almost three hundred silt and moss samples were collected from sixteen

drainages, with a total cost for the program of approximately $27,700. The goal of the program

was to assess the potential of the claims to host gold mineralization, such as that discovered on

the nearby Skoonka Creek property of Strongbow Explorations Inc. Bitterroot holds two

properties, which are separated by approximately 2 kilometres (figs. 1 and 2). This report

describes the work completed on both properties, as the program was executed simultaneously on

both groups of claims, and the aims of the exploration programs were the same.

On Bitterroot’s eastern claim group, Murray Creek, a major drainage which flows into the

Thompson River from the west at Spences Bridge, yielded the best gold results in the stream

sediment sampling, with a high of 1,060 ppb Au, and a supportive value of 618 ppb Au only 150

metres upstream. Unfortunately, creeks flowing from the Bitterroot claims into Murray Creek

did not yield similar promise, as results for Au were typically below trace levels. In the western

Spences Bridge claim group, very few gold anomalies are apparent, although drainages from the

Clear Range exhibit elevated Cu and Zn. Because only a very limited amount of prospecting and

soil sampling was carried-out on the property, the source of these base metals anomalies remains

a possible target. Preliminary prospecting along the Snow Hill road system suggests that

sulphides, mainly pyrrhotite and pyrite, are abundant within foliated metavolcanic rocks in that

area, but rock and soil sampling did not yield results elevated in base metals.

In general, the rest of the results of the 2006 stream sediment sampling program were

disappointing. There are several possibilities for follow-up work. Aside from sourcing the base

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Figure 1. Location of the Spences Bridge properties, southern British Columbia.

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Scale: 1:250000 Projection: UTM Zone 10 (NAD 83) E E E E E m m m m m

0 0 0 0 0

0 2.5 5 0 10 0 0 0 MerrittMerrittMerritt 0 0 0 0 0 MerrittMerrittMerritt 0 0 0 0 0 0

kilometres 8 0 2 4 6 5 6 6 6 6 Figure 2. Location of the Spences Bridge properties, showing selected producing mines and significant mineral occurrences in southern British Columbia. -3- 2006 Exploration, Spences Bridge Properties, Bitterroot Resources Ltd., by S.T. Flasha & C.J. Greig

metal anomalies in the Clear Range, the source of anomalies in Murray Creek merit more

investigation. This is particularly so if the ground north of Murray Creek becomes available. In

the meantime, a limited program of prospecting, contour soil sampling, and perhaps some in-fill

stream sediment sampling immediately south of the anomalous stretch of the creek should be

undertaken. To follow-up on the Snow Hill-Clear Range area anomalies, contour soil sampling

and prospecting should be considered, as should in-fill stream sediment sampling.

2.0 Location, Access, and Physiography

Bitterroot Resources’ Spences Bridge properties are located approximately 4 kilometres west of

Spences Bridge, a small community near the confluence of the Thompson and Nicola rivers, and

5 kilometres east of the Fraser River Valley (figs. 1 & 2). Bitterroot’s properties are readily

accessible from Spences Bridge via the Murray Creek Forest Service Road, which connects with

the Trans Canada highway in the Thompson River Valley. The property can also be accessed

from the west, via the Izman Creek Forest Service Road, which links the Murray Creek system to

Highway 12, a paved road connecting Lytton and Lillooet (figs. 2 & 3). The forest service roads

are well maintained, as logging is active in the area.

The property lies a short distance east of the Coast Mountains, but is within the interior

dry belt. The area is free of snow for the majority of the year, and is workable for at least eight

months a year. Elevation on the property ranges between 500 and 1700 metres, resulting in a

wide range of vegetation and terrain (fig. 4). Because of the lack of moisture in the summer

months, stream sampling best accomplished during the runoff period in the spring, during snow

melt.

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2 615000 mE 2006 Exploration, Spences Bridge Properties, Bitterroot Resources Ltd., by S.T. Flasha & C.J. Greig

Figure 4. View east down the valley of Murray Creek, toward the community of Spences Bridge, southern British Columbia. 3.0 Claims

Bitterroot Resources Ltd.’s Spences Bridge properties (Table I, fig.3) consist of two separate

groups of claims, twelve in total, that cover approximately 50 square kilometres. They lie within

the Kamloops Mining Division. The claims are currently in good standing, with an expiry date

of December 23, 2007.

4.0 Geologic Setting & Mineral Occurrences

According to the Ministry of Mines website, the Spences Bridge property and surrounding area

are primarily underlain by Lower Cretaceous andesitic volcanic rocks of the Spences Bridge

Group (fig. 5). The Spences Bridge Group includes andesite flows and breccias intercalated with

-6- Table I. Claim information, Spences Bridge properties. Claim Claim Expiry Number Name Number Date of Cells SB1 524318 23-Dec-2007 25 SB2 524320 23-Dec-2007 25 524321 23-Dec-2007 24 524322 23-Dec-2007 16 SB4 524323 23-Dec-2007 25 SB5 524324 23-Dec-2007 25 SB6 524325 23-Dec-2007 25 524326 23-Dec-2007 25 524327 23-Dec-2007 25 SB9 524328 23-Dec-2007 23 SB10 524329 23-Dec-2007 2 SB11 524330 23-Dec-2007 3 Total Number of Cells: 243

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serpentinite ultramafic rocks

Lower Cretaceous

undivided sedimentary rocks Intrusive Rocks

Late Cretaceous to Paleogene

Bitterroot Resources Ltd. andesitic volcanic rocks quartz monzonitic intrusive rocks

Triassic to Jurassic Upper Triassic Spences Bridge Properties granodioritic intrusive rocks Date:19/1/2007 undivided volcanic rocks 5570000 mN Regional Geology & 5570000 mN Author: Mineral Occurences Office: Permian to Triassic Permian to Triassic

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6 LLyyttttoonn 6 kilometres6 6 6 Figure 5. Regional geology, showing location of the Spences Bridge properties and selected producing mines and significant mineral occurrences in southern British Columbia. 2006 Exploration, Spences Bridge Properties, Bitterroot Resources Ltd., by S.T. Flasha & C.J. Greig

volcanic sandstone, shale, and conglomerate. The southwestern portion of the claims are

underlain primarily by intrusive rocks of presumed Permian to Triassic age; known lithologies

include diorite and amphibolite (fig. 5). No formal geologic investigations were undertaken

during the present program.

According to the records on the Ministry of Mines websites, no previous mineral

exploration work has been completed on Bitterroot’s Spences Bridge properties. The claims

were staked in response to news of a gold discovery in late 2005 on the Skoonka Creek property

of Almaden Minerals Ltd. and Strongbow Exploration Inc. (fig. 2). At the JJ occurrence on the

Skoonka Creek ground, Strongbow and Almaden intersected quartz vein-related mineralization

grading up to 20.2 g/t Au over 12.8 metres. The mineralization at JJ is hosted by moderate to

strongly altered andesite of the Spences Bridge Group (fig. 5). Bitterroot’s property lies

approximately 4 to 9 kilometres north and northeast of the Almaden-Strongbow ground (figs. 2

& 5).

5.0 Stream Sediment Geochemistry

In May 2006, a four-man crew spent ten days collecting stream sediment samples from streams

draining Bitterroot’s Spences Bridge properties. In total, sixteen creeks were sampled and 293

silt and moss samples were collected (figs. 6 & 7; Appendix I). Spacing between samples ranged

from 100 to 150 metres.

All samples were sent to ALS Chemex Labs in Vancouver, where they were analyzed for

gold and a 34 element ICP exploration package (Appendix I). Stream sediment samples were

collected from active drainages. Material collected included fresh silt, silty sand, or locally, silty

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Spences Bridge Properties Stream Sediment Sample Locations Date:10/1/2007 Eastern Claim Group

Author: silt sample Office:

Drawing: SFlasha moss mat sample E E E E E E E E m m

m Scale: 1:20000 Projection: UTM Zone 10 (NAD 83) Contour Interval: 100m m

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0 5591000 mN

CASB6T032CASB6T032 5591000 mN CASB6T031CASB6T031 CASB6T102CASB6T102 CASB6T030CASB6T030 CASB6T029CASB6T029 CASB6T028CASB6T028 CASB6T027CASB6T027 CASB6T026CASB6T026 CASB6T027CASB6T027 CASB6T025CASB6T025 CASB6T024CASB6T024 CASB6T025CASB6T025 CASB6T023CASB6T023 CASB6T022CASB6T022 5590000 mN CASB6T021CASB6T021 CASB6T020CASB6T020 CASB6T020CASB6T020CASB6T019CASB6T019 CASB6T018CASB6T018 5590000 mN CASB6T017CASB6T017

CASB6T108CASB6T108 CASB6T107CASB6T107 CASB6T107CASB6T107 CG06SBT01CG06SBT01 CASB6T109CASB6T109 SFSB6M008SFSB6M008 CASB6T1CASB6T11010 CASB6T1CASB6T11111 DNSB6T086DNSB6T086 5589000 mN DNSB6T083DNSB6T083DNSB6T085DNSB6T085 DNSB6T083DNSB6T083 DNSB6T084DNSB6T084 DNSB6T082DNSB6T082 5589000 mN DNSB6T081DNSB6T081 DNSB6T080DNSB6T080 SS DNSB6T080DNSB6T080 nnn ooo DNSB6T079DNSB6T079 ww CC DNSB6T078DNSB6T078 LLL HH LLL EEE iiilll DNSB6T077DNSB6T077 EEE lllll AA CC AA rrr RR rrreee DNSB6T076DNSB6T076 eee kkk IHSB6M003AIHSB6M003AIHSB6M003A kkk DNSB6T075DNSB6T075 IHSB6T023IHSB6T023IHSB6T023 DNSB6T074DNSB6T074 IHSB6T021IHSB6T021IHSB6T021 IHSB6T023IHSB6T023IHSB6T023 DNSB6T074DNSB6T074 5588000 mN DNSB6T073DNSB6T073 IHSB6T022IHSB6T022IHSB6T022 IHSB6T024IHSB6T024IHSB6T024 DNSB6T073DNSB6T073 DNSB6T072DNSB6T072 DNSB6T071DNSB6T071 IHSB6T025IHSB6T025IHSB6T025 DNSB6T070DNSB6T070 IHSB6T019IHSB6T019IHSB6T019 DNSB6T070DNSB6T070 5588000 mN IHSB6T026IHSB6T026IHSB6T026 DNSB6T069DNSB6T069 IHSB6M001AIHSB6M001AIHSB6M001A IHSB6T027IHSB6T027IHSB6T027 IHSB6M002AIHSB6M002AIHSB6M002A IHSB6T020IHSB6T020IHSB6T020 IHSB6T027IHSB6T027IHSB6T027 IHSB6T016IHSB6T016IHSB6T016 IHSB6T018IHSB6T018IHSB6T018 IHSB6T030IHSB6T030IHSB6T030 IHSB6T014IHSB6T014IHSB6T014 IHSB6T017IHSB6T017IHSB6T017 IHSB6T030IHSB6T030IHSB6T030 Y Y Y

Y Y Y IHSB6T031IHSB6T031IHSB6T031 Y Y Y IHSB6T012IHSB6T012IHSB6T012 IHSB6T015IHSB6T015IHSB6T015 IHSB6T028IHSB6T028IHSB6T028 IHSB6T031IHSB6T031IHSB6T031 R R R R R R R R R IHSB6T010IHSB6T010IHSB6T010 IHSB6T013IHSB6T013IHSB6T013 IHSB6T032IHSB6T032IHSB6T032 D D D D D D D D D IHSB6T01IHSB6T01IHSB6T0111 CG06SBT03CG06SBT03 IHSB6T009IHSB6T009IHSB6T009 IHSB6T01IHSB6T01IHSB6T0111 IHSB6T029IHSB6T029IHSB6T029 CG06SBT03CG06SBT03 IHSB6T005IHSB6T005IHSB6T005 IHSB6T008IHSB6T008IHSB6T008 IHSB6T005IHSB6T005IHSB6T005 IHSB6T007IHSB6T007IHSB6T007 IHSB6T003IHSB6T003IHSB6T003 IHSB6T003IHSB6T003IHSB6T003 IHSB6T006IHSB6T006IHSB6T006 IHSB6T002IHSB6T002IHSB6T002 IHSB6T004IHSB6T004IHSB6T004 5587000 mN IHSB6T001IHSB6T001IHSB6T001 eekk RRR rrree AAA CCrrr AAA NNN

GGG CG06SBT02CG06SBT02 EEE 5587000 mN EEE SFSB6T004SFSB6T004 IHSB6T034IHSB6T034IHSB6T034 SFSB6T003SFSB6T003 IHSB6T034IHSB6T034IHSB6T034 SFSB6T003SFSB6T003 SFSB6T005SFSB6T005 SFSB6M003SFSB6M003 SFSB6T008SFSB6T008 SFSB6T007SFSB6T007 SFSB6T01SFSB6T0111 nnn SFSB6T01SFSB6T0111 nnn nnn SFSB6T006SFSB6T006 aaa aaa aaa SFSB6M001SFSB6M001 SFSB6M002SFSB6M002 mmm SFSB6M001SFSB6M001 SFSB6M002SFSB6M002 mmm mmm

z z z z z z SFSB6T001SFSB6T001 CASB6T016CASB6T016 z z z SFSB6T001SFSB6T001 CASB6T016CASB6T016 YYY I I I SFSB6T001SFSB6T001 CASB6T016CASB6T016 YYY YYY I I I I I I SFSB6T012SFSB6T012 SFSB6T012SFSB6T012 SFSB6T009SFSB6T009 CASB6T001CASB6T001 RRR SFSB6T009SFSB6T009 CASB6T001CASB6T001 RRR SFSB6T013SFSB6T013 SFSB6T002SFSB6T002 CASB6T002CASB6T002 DDD DDD SFSB6T010SFSB6T010 5586000 mN SFSB6T015SFSB6T015 SFSB6T010SFSB6T010 CASB6T003CASB6T003 SFSB6T016SFSB6T016 SFSB6M004SFSB6M004 SFSB6T018SFSB6T018 CASB6T004CASB6T004 SFSB6T016SFSB6T016 SFSB6T019SFSB6T019 CASB6T004CASB6T004 SFSB6T017SFSB6T017 SFSB6T020SFSB6T020 CASB6T005CASB6T005 SFSB6T014SFSB6T014 SFSB6T017SFSB6T017 SFSB6T020SFSB6T020 CASB6T006CASB6T006 SFSB6M005SFSB6M005 SFSB6T021SFSB6T021 CASB6T007CASB6T007 CASB6T015CASB6T015 5586000 mN SFSB6M005SFSB6M005 SFSB6T022SFSB6T022 CASB6T015CASB6T015 IHSB6M001BIHSB6M001BIHSB6M001B CASB6T009CASB6T009 CASB6T008CASB6T008 CASB6T009CASB6T009 SFSB6M006SFSB6M006 CASB6T010CASB6T010 CASB6T103CASB6T103 CASB6T010CASB6T010 Bitterroot Resources Ltd. CASB6T01CASB6T0111 CASB6T014CASB6T014 CCASB6T104ASB6T104 CASB6T01CASB6T0111 CASB6T014CASB6T014 CASB6T012CASB6T012 CASB6T013CASB6T013 Spences Bridge Properties Stream Sediment Sample Locations IHSB6M002BIHSB6M002BIHSB6M002B Date:11/1/2007 Western Claim Group Author: IHSB6M003BIHSB6M003BIHSB6M003B silt sample Office: 558500

moss mat E sample E Drawing: SFlasha m

E m E E 0

E E

m Scale: 1:25000 Projection: UTM Zone 10 (NAD 83) Contour Interval: 20m 0 0

m m m m

0 5585000 mN 0 4 0 0 0 0 0 0 0 0 3 0

111 0 111777 0 0 77700 0 6 0 0 0 000 00 2 0000 0 0 250 500 1000 8 0 9 6 0 1 9 0 9 6 0

5 metres 6 5 6 Figure 7. 2006 silt and moss mat sample locations, western claim group. -11- 2006 Exploration, Spences Bridge Properties, Bitterroot Resources Ltd., by S.T. Flasha & C.J. Greig

mud using either hands or a geotul. The material collected was placed within Kraft paper sample

bags and dried before shipping to the lab.

Results obtained in the program were variable. Excellent values were obtained from

Murray Creek, with values of 1,060 and 618 ppb Au (fig. 8). Other high Au values in the Murray

Creek drainage included a sample yielding 188 ppb Au kilometres downstream from the other

highs, and a sample yielding 101 ppb Au 600 metres upstream from the mouth of East Murray

Creek (fig. 8). Unfortunately, drainages on Bitterroot’s ground that flow into Murray Creek

yielded relatively poor results for gold, and so the source for gold may lie elsewhere.

The western claim group yielded very few anomalous results for gold. North Laluwissin

Creek yielded one anomalous sample, with 51 ppb Au, although no samples in the vicinity

yielded supportive values. The southwesternmost stream on the claims showed some potential,

with the five samples farthest upstream yielding anomalous results (37, 11, 11, and 25 ppb Au in

silt, and 53 ppb in moss mat samples). Copper was also anomalous in this creek, with all values

exceeding 100 ppm Cu, including moss mat samples, with a high of 361 ppm Cu (fig. 9).

Copper was consistently high upstream in drainages from the Clear Range. One stream draining

the Clear Range, Snow Hill Creek, was sampled over a length of 2.5 kilometres. It yielded 20

samples with values over 100 ppm Cu, including one yielding 635 ppm Cu (fig. 9). In contrast,

other drainages on the Spences Bridge properties averaged only 30 or 40 ppm Cu.

In general, other elements in the silt sample dataset yielded uniformly low results,

including for Ag, Pb, and As. Zinc values were low except in Snow Hill Creek, where values

ranged up to 2,150 ppm Zn, and where several supportive values yielded greater than 1,000 ppm

Zn (fig. 10).

-12- E E E E m m m m

0 0 0 0 0 0 0 0 0 0 0 0 5 5 0 kkk 0 1

kkk 0 0 eee rrreeeeee 1 6 6 6 CCrrr CC 6 5595000 mN

nnn ininin iii MM MM k sss sss uuu sss uuu e isisis rrr iii rrrrr rrraaa e www yyy r www yyy uuu lululu C lll aaa aaa LLL LLL

ttthhh yyy rrrttt aaa ooo rrr NN rrr uuu MMM

t t t t t t CC t t t CC s s s s s s rrr s s s rrreee a a a eee a a a eee a a a eee EEE kkk EEE kkk EEE

5590000 mN

5590000 mN MM MMuuu uuurrrrrraaa rrraaayyy

SSS SSSnnn CreekCreek nnnooo CreekCreek ooowww www 111 H HH 999 HHHiii 000 iililllll 000 ll l C CC CCCrrr rrreee eee kkk

CCC CCC LLL LLL EEE EEE AAA AAA RRR RRR

eeeekkk CCrrreeee PasulkoPasulko LakeLake

RRR RRR AAA AAA NNN NNN GGG GGG EEE EEE Au (ppb)

150 to 300 (1)

nnn aaa 50 to 150 (1) mmm zzz IIzIzz Bitterroot Resources Ltd. 5585000 mN 10 to 50 (1) 111555 555000000 2 to 10 (19) Spences Bridge Properties Au (ppb) 2006 Silt and Moss Mat Date:30/6/2006 Sample Geochemistry 150 to 1,100 (3) Author: Au (ppb)

Office: (silt = red; moss mat = yellow) 40 to 150 (2) Sko Drawing: SFlasha E o

E n E E k 25 to 40 (4) a Scale: 1:50000 Projection: UTM Zone 10 (NAD 83) Contour Interval: 100m m m

m m

0 10 to 25 (21) 0 0 0 0 0 0 0 0 2 to 10 (241) 0 0 0 0 0.5 1 2 5 0 0 5 0 kkk 0 eeekkk

eee 1 9 eeeeee 6 rrreee 6 CCrrr kilometres 6 5 CC Figure 8. Gold geochemistry in stream sediment samples, Spences Bridge properties. -13- E E E E m m m m

0 0 0 0 0 0 0 0 0 0 0 0 5 5 0 kkk 0 1

kkk 0 0 eee rrreeeeee 1 6 6 6 CCrrr CC 6 5595000 mN

nnn ininin iii MM MM k sss sss uuu sss uuu e isisis rrr iii rrrrr rrraaa e www yyy r www yyy uuu lululu C lll aaa aaa LLL LLL

ttthhh yyy rrrttt aaa ooo rrr NN rrr uuu MMM

t t t t t t CC t t t CC s s s s s s rrr s s s rrreee a a a eee a a a eee a a a eee EEE kkk EEE kkk EEE

5590000 mN

5590000 mN MM MMuuu uuurrrrrraaa rrraaayyy

SSS SSSnnn CreekCreek nnnooo CreekCreek ooowww www 111 H HH 999 HHHiii 000 iililllll 000 ll l C CC CCCrrr rrreee eee kkk

CCC CCC LLL LLL EEE EEE AAA AAA RRR RRR

eeeekkk CCrrreeee PasulkoPasulko LakeLake

RRR RRR AAA AAA Cu (ppm) NNN NNN GGG GGG EEE EEE 300 to 635 (1)

150 to 300 (2) 100 to 150 (2) nnn aaa mmm 40 to 100 (13) zzz IIzIzz Bitterroot Resources Ltd. 5585000 mN 30 to 40 (3) 111555 555000000 2 to 30 (1) Spences Bridge Properties Cu (ppm) 2006 Silt and Moss Mat Date:30/6/2006 Sample Geochemistry Author: Cu (ppm) 300 to 635 (5)

Office: 150 to 300 (20) Sko Drawing: SFlasha E o

E n E

E k a Scale: 1:50000 Projection: UTM Zone 10 (NAD 83) Contour Interval: 100m 100 to 150 (30) m m

m m

0 0

0 40 to 100 (94) 0 0 0 0 0 0 0 0 0 0 0.5 1 2 30 to 40 (85) 5 0 0 5 0 kkk 0 eeekkk

eee 1 9 eeeeee 2 to 30 (37) 6 rrreee 6 CCrrr kilometres 6 5 CC Figure 9. Copper geochemistry in stream sediment samples, Spences Bridge properties. -14- E E E E m m m m

0 0 0 0 0 0 0 0 0 0 0 0 5 5 0 kkk 0 1

kkk 0 0 eee rrreeeeee 1 6 6 6 CCrrr CC 6 5595000 mN

nnn ininin iii MM MM k sss sss uuu sss uuu e isisis rrr iii rrrrr rrraaa e www yyy r www yyy uuu lululu C lll aaa aaa LLL LLL

ttthhh yyy rrrttt aaa ooo rrr NN rrr uuu MMM

t t t t t t CC t t t CC s s s s s s rrr s s s rrreee a a a eee a a a eee a a a eee EEE kkk EEE kkk EEE

5590000 mN

5590000 mN MM MMuuu uuurrrrrraaa rrraaayyy

SSS SSSnnn CreekCreek nnnooo CreekCreek ooowww www 111 H HH 999 HHHiii 000 iililllll 000 ll l C CC CCCrrr rrreee eee kkk

CCC CCC LLL LLL EEE EEE AAA AAA RRR RRR

eeeekkk CCrrreeee PasulkoPasulko LakeLake

RRR RRR AAA AAA NNN NNN GGG GGG EEE EEE Zn (ppm)

100 to 500 (5)

nnn 75 to 100 (5) aaa mmm 60 to 75 (5) zzz III Bitterroot Resources Ltd. 1 to 60 (7) 5585000 mN 111555 555000000 000 Zn (ppm) Spences Bridge Properties 2006 Silt and Moss Mat Date:30/6/2006 Sample Geochemistry 1,000 to 2,150 (6) Author: Zn (ppm)

Office: 500 to 1,000 (4)

Sko Drawing: SFlasha 100 to 500 (37) E o

E n E

E k a Scale: 1:50000 Projection: UTM Zone 10 (NAD 83) Contour Interval: 100m m 75 to 100 (45) m

m m

0 0

0 60 to 75 (56) 0 0 0 0 0 0 0 0 0 0 0.5 1 2 1 to 60 (123) 5 0 0 5 0 kkk 0 eeekkk

eee 1 9 eeeeee 6 rrreee 6 CCrrr kilometres 6 5 CC Figure 10. Zinc geochemistry in stream sediment samples, Spences Bridge properties. -15- 2006 Exploration, Spences Bridge Properties, Bitterroot Resources Ltd., by S.T. Flasha & C.J. Greig

Moss mat samples were collected when no silt was available in the drainages, and in

some instances moss mat samples were collected at the same location as silt samples in order to

compare the two. In general, moss mat and silt samples from the same location consistently

yielded values within a few ppm, for all the elements analyzed.

6.0 Soil & Rock Geochemistry

Only eleven rock samples and eight soil samples were collected during the 2006 season (fig. 11;

Appendices II & III). All samples were taken from the Snow Hill Creek area, either along the

road that parallels the lower reaches of the creek, on its northeast side, or from logging roads near

the top of the hill, along the crest of the Clear Range (fig. 11). All but one of the rock samples,

which typically carried abundant pyrrhotite or pyrite, had gold values below trace, and the

anomalous sample yielded only 71 ppb Au. The same sample also had a moderately anomalous

silver value of 1.1 ppm Ag. Interestingly, these sulphide-bearing samples (both rock and

adjacent limonitic soil) did not yield copper or zinc results that would explain the elevated Cu

and Zn values in the nearby streams. The soil samples were not analyzed for Au.

7.0 Recommendations

The high gold values discovered in Murray Creek are intriguing, and should be further

investigated, particularly if the ground north of the creek comes open. For the time being, the

creek should be silt sampled at closer spacing, and contour soil sampling south of the creek

should be considered. Soil samples should be collected at 50 metre spacings, and several levels

of contouring at different elevations are recommended. This should more clearly indicate

whether the origin of the anomalous gold is from Bitterroot’s Spences Bridge properties, or from

-16- -17- F S D O A D 5 5 5 c u B r a f i 5 f a 5 5 a t t 5 i 5 h c e g w l e e o 5 : 5 5 8 i 1 9 : n 8 : i r u

5 : 1 g 8 5

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0 e 0 s 7 1 0 5 0 0 0 0 0 h 0 0 0 0 0 0 0 0 a r 0 1 0 0

6 6 6

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B k k r i d g e p r 599500 mE o p e r t i 599500 mE e s . C C C C C C C C C C C C C C C C C C G G G G G G G G G G G G G G G G G G 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 6 6 6 0 0 0 C C C C C C 6 6 6 C C C C C C 6 6 6 C C C C C C 6 6 6 6 6 6 S S S 6 6 6 S S S G G G G G G S S S G G G G G G G G G G G G S S S S S S S S S B B B B B B

B B B 600000 mE 0 0 0 0 0 0 B B B 0 0 0 0 0 0 B B B 0 0 0 0 0 0 B B B S S S S S S 6 6 6 6 6 6 S S S 6 6 6 6 6 6 6 6 6 6 6 6 S S S S S S S S S 0 0 0 S S S S S S 0 0 0 S S S S S S 0 0 0 S S S S S S 0 0 0 0 0 0 7 7 7 0 0 0 7 7 7 B B B B B B 7 7 7 B B B B B B C C C B B B B B B C C C 8 8 8 C C C 8 8 8 8 8 8 R R R R R R C C C R R R R R R C C C G G G R R R R R R C C C 600000 mE G G G G G G C C C C C C 0 0 0 0 0 0 G G G C C C 0 0 0 0 0 0 G G G 0 0 0 0 0 0 G G G 0 0 0 0 0 0 0 0 0 C C C C C C 4 5 4 5 4 5 G G G C C C 4 5 4 5 4 5 G G G 4 5 4 5 4 5 G G G 6 6 6 0 0 0 6 6 6 0 0 0 6 6 6 0 0 0 G G G G G G G G G S S S 6 6 6 0 0 0 S S S 6 6 6 0 0 0 S S S 6 6 6 0 0 0 S S S 6 6 6 0 0 0 S S S 6 6 6 B B B 0 0 0 S S S 6 6 6 B B B 0 0 0 B B B S S S 6 6 6 S S S 6 6 6 B B B S S S 6 6 6 B B B R R R B B B R R R R R R S S S S S S B B B S S S B B B R R R B B B R R R 1 1 1 R R R 1 1 1 1 1 1 B B B B B B S S S B B B S S S 0 0 0 1 1 1 S S S 0 0 0 1 1 1 0 0 0 1 1 1 S S S 1 1 1 S S S 0 0 0 1 1 1 S S S 0 0 0 1 1 1 0 0 0 6 6 6 0 0 0 6 6 6 0 0 0 6 6 6 0 0 0 C C C C C C 5 5 5 C C C 5 5 5 5 5 5 C C C C C C C C C C C C G G G C C C C C C G G G G G G

G G G G G G G G G G G G

G G G G G G 1 0 0 0

0 0 0 0 0 0 6

6 6 6 0 0 0 0 0 0 0 6 6 6 0 0 0 0 0 0 0 6 6 6 0 0 0 0 0 0 S S S 6 6 6 6 6 6 S S S 6 6 6 6 6 6 S S S 6 6 6 6 6 6 S S S S S S S S S S S S B B B 600500 mE S S S S S S B B B B B B B B B B B B B B B B B B R R R B B B B B B R R R R R R R R R R R R R R R R R R 0 0 0 R R R R R R 0 0 0 0 0 0 8 8 8 0 0 0 0 0 0 8 8 8 0 0 0 0 0 0 8 8 8 0 0 0 0 0 0 7 7 7 6 6 6

600500 mE 7 7 7 6 6 6 7 7 7 6 6 6 C C C C C C C C C C C C C C C C C C C C C C C C C C C C C C C C C C C C C C C G G G C C C C C C G G G G G G G G G G G G G G G G G G G G G G G G G G G G G G G G G G G G G G G G G G 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 6 6 6 0 0 0 0 0 0 6 6 6 0 0 0 0 0 0 6 6 6 6 6 6 6 6 6 0 0 0 0 0 0 6 6 6 6 6 6 6 6 6 6 6 6 S S S 6 6 6 6 6 6 S S S 6 6 6 6 6 6 S S S S S S S S S 6 6 6 6 6 6 S S S S S S S S S S S S S S S S S S S S S S S S B B B S S S S S S B B B B B B B B B B B B B B B B B B B B B B B B B B B B B B B B B B B B S S S B B B B B B S S S S S S S S S R R R R R R S S S R R R S S S S S S S S S S S S S S S 0 0 0 S S S S S S 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 4 4 4 0 0 0 0 0 0 4 4 4 0 0 0 0 0 0 4 4 4 3 3 3 0 0 0 0 0 0 9 9 9 3 3 3 9 9 9 3 3 3 9 9 9 2 2 2 1 1 1 2 2 2 1 1 1 2 2 2 1 1 1

601000 mE

601000 mE 5 5 5 5 5 5 5 5 8 5 8 5 8 8 8 9 8 601500 mE 8 5 9 0 7 0 0 5 0 5 0 0 0 0 0 0

0 m m

m m m

601500 mE N N N N N 2006 Exploration, Spences Bridge Properties, Bitterroot Resources Ltd., by S.T. Flasha & C.J. Greig

the north side of the creek. Prospecting should also be a priority as this area of the claims are

underlain by andesitic volcanics rocks of the Spences Bridge Group, which also host the

Almaden-Strongbow Skoonka Creek showings. Altered rocks and quartz veins would be of

obvious interest.

Further silt samples may also be collected from unsampled (or undersampled) drainages

in the Clear Range, and a contour soil sampling program should also be considered in order to

source the base metals anomalies within the boundaries of Bitterroot’s Spences Bridge

properties. The focus should remain on the Snow Hill Creek area as the copper and zinc values

are highest, and contour soil sampling should be concentrated therein.

-18- Appendix I. Stream Sediment Sample Locations & Geochemistry 2006 Exploration, Spences Bridge Properties, Bitterroot Resources Ltd., by S.T. Flasha & C.J. Greig

Sample UTM UTM Au Ag Al As B Ba Be Bi Ca Cd Co Cr Cu Fe Ga Hg K La Mg Mn Mo Na Ni P Pb S Sb Sc Sr Ti Tl U V W Zn Number Easting Northing ppm ppm % ppmppm ppm ppm ppm% ppm ppm ppm ppm %ppm ppm %ppm% ppm ppm % ppm ppm ppm % ppm ppm ppm % ppmppmppm ppm ppm SFSB6T001 599456 5586256 <0.005 0.3 1.05 4 <10 40 <0.5 <2 0.88 <0.5 9 15 69 2.37 <10 <1 0.06 <10 0.53 804 1 0.02 9 430 3 0.02 2 3 44 0 <10 <10 56 <10 54 SFSB6T002 599631 5586322 <0.005 <0.2 1.71 5 <10 130 <0.5 <2 0.67 <0.5 10 21 82 2.51 <10 <1 0.05 <10 0.66 575 1 0.02 13 410 <2 0.02 2 4 44 0.1 <10 <10 56 <10 78 SFSB6T003 599810 5586412 <0.005 <0.2 0.98 4 <10 60 <0.5 <2 0.44 <0.5 7 13 36 2.06 <10 <1 0.05 <10 0.39 472 1 0.01 8 370 3 0.02 <2 3 27 0 <10 <10 46 <10 57 SFSB6T004 599988 5586463 <0.005 0.2 1.4 8 <10 120 <0.5 <2 0.54 <0.5 9 15 39 2.39 <10 <1 0.1 <10 0.47 779 <1 0.01 12 440 4 0.03 <2 4 37 0 <10 <10 47 <10 69 SFSB6T005 600051 5586406 <0.005 <0.2 1.39 5 <10 80 <0.5 <2 0.86 <0.5 9 15 81 2.28 <10 <1 0.05 <10 0.59 803 1 0.01 12 590 3 0.05 2 5 49 0 <10 <10 47 <10 98 SFSB6T006 600196 5586381 <0.005 <0.2 1.27 2 <10 60 <0.5 <2 0.62 <0.5 8 15 59 2.2 <10 <1 0.04 <10 0.57 604 1 0.01 11 520 3 0.04 2 4 35 0 <10 <10 48 <10 79 SFSB6T007 600131 5586402 <0.005 0.3 1.59 5 <10 110 <0.5 <2 0.96 <0.5 9 17 89 2.5 <10 <1 0.05 <10 0.66 1085 1 0.02 14 630 4 0.06 <2 5 53 0 <10 <10 49 <10 112 SFSB6T008 599919 5586411 <0.005 <0.2 1.25 4 <10 80 <0.5 <2 0.66 <0.5 8 14 60 2.34 <10 <1 0.06 <10 0.49 662 1 0.01 10 480 3 0.04 2 4 40 0 <10 <10 49 <10 79 SFSB6T009 599704 5586370 <0.005 <0.2 1.23 5 <10 90 <0.5 <2 0.8 <0.5 8 15 64 2.16 <10 <1 0.06 <10 0.49 693 1 0.01 11 540 4 0.05 <2 4 44 0 <10 <10 45 <10 81 SFSB6T010 599495 5586259 <0.005 <0.2 1 4 <10 70 <0.5 <2 0.56 <0.5 8 13 55 2.13 <10 <1 0.05 <10 0.44 562 1 0.01 8 410 2 0.03 2 3 34 0 <10 <10 48 <10 58 SFSB6T011 599315 5586249 <0.005 <0.2 1.15 7 <10 80 <0.5 <2 0.71 <0.5 9 17 76 2.8 <10 <1 0.06 <10 0.52 632 1 0.02 10 500 2 0.04 <2 4 43 0 <10 <10 68 <10 65 SFSB6T012 599212 5586223 <0.005 <0.2 1.14 4 <10 60 <0.5 <2 0.81 <0.5 9 16 83 2.41 <10 <1 0.06 <10 0.59 619 1 0.01 9 460 3 0.02 <2 4 53 0 <10 <10 57 <10 59 SFSB6T013 599101 5586220 <0.005 <0.2 1.09 6 <10 70 <0.5 <2 0.6 <0.5 8 17 64 2.63 <10 <1 0.05 <10 0.48 568 1 0.02 9 460 2 0.03 2 4 38 0 <10 <10 64 <10 57 SFSB6T014 599000 5586201 <0.005 <0.2 0.02 <2 <10 <10 <0.5 <2 0.01 <0.5 <1 <1 2 0.04 <10 <1 <0.01 <10 0.01 11 <1 <0.01 <1 10 <2 <0.01 2 <1 1 <0.01<10 <10 1 <10 <2 SFSB6T015 598902 5586187 <0.005 0.2 1.08 4 <10 70 <0.5 <2 0.62 <0.5 8 15 72 2.25 <10 <1 0.05 <10 0.5 596 1 0.02 8 440 3 0.02 <2 3 39 0 <10 <10 52 <10 55 SFSB6T016 598807 5586163 <0.005 <0.2 1.41 3 <10 90 <0.5 <2 0.81 <0.5 9 16 104 2.41 <10 <1 0.06 <10 0.59 637 1 0.02 10 500 2 0.03 2 4 49 0 <10 <10 52 <10 68 SFSB6T017 599560 5586235 <0.005 <0.2 1.12 <2 <10 100 <0.5 <2 0.82 <0.5 8 15 117 2.18 <10 <1 0.06 <10 0.45 424 1 0.02 9 320 2 0.02 <2 3 55 0 <10 <10 53 <10 52 SFSB6T018 599596 5586159 <0.005 0.3 1.42 3 <10 150 <0.5 <2 1.16 <0.5 6 12 251 1.69 <10 <1 0.07 10 0.38 532 1 0.01 11 550 6 0.05 <2 3 80 0 <10 <10 28 <10 60 SFSB6T019 599630 5586105 0.037 0.2 1.13 3 10 200 <0.5 <2 2.33 <0.5 4 9 361 1.12 <10 <1 0.08 20 0.25 945 2 0.02 12 960 9 0.1 2 2 152 0 <10 <10 19 <10 54 SFSB6T020 599649 5586054 0.011 <0.2 1.41 5 <10 140 <0.5 <2 0.97 <0.5 6 15 167 1.81 <10 <1 0.08 10 0.41 511 1 0.01 12 780 6 0.04 <2 3 69 0 <10 <10 32 <10 76 SFSB6T021 599650 5585998 0.011 0.4 1.62 5 <10 150 <0.5 <2 0.89 <0.5 8 16 164 1.96 <10 <1 0.08 10 0.45 584 1 0.02 13 660 5 0.04 <2 3 67 0 <10 <10 34 <10 85 SFSB6T022 599635 5585938 0.025 0.4 1.43 7 <10 140 <0.5 <2 0.96 <0.5 5 14 166 1.98 <10 <1 0.08 10 0.41 540 1 0.02 12 740 12 0.04 2 3 71 0 <10 <10 35 <10 88 SFSB6T023 612260 5588530 0.009 <0.2 0.13 <2 10 80 <0.5 <2 >25.0<0.5 1 4 17 0.12 <10 <1 0.02 <10 0.25 59 <1 0.04 1 560 2 <0.01 <2 <1 381 0 <10 <10 6 <10 10 SFSB6T024 612202 5588421 <0.005 <0.2 1.14 6 10 90 <0.5 <2 18.4 <0.5 6 14 32 1.4 <10 <1 0.06 <10 0.55 320 <1 0.03 9 690 5 <0.01 <2 3 247 0.1 <10 <10 35 <10 29 SFSB6T025 612167 5588322 <0.005 <0.2 1 4 10 90 <0.5 <2 19 <0.5 4 14 28 1.48 <10 <1 0.05 <10 0.52 317 <1 0.03 10 690 5 <0.01 2 3 242 0.1 <10 <10 35 <10 29 SFSB6T026 612159 5588231 0.006 <0.2 1 2 10 100 <0.5 <2 22.1 <0.5 4 10 30 1.08 <10 <1 0.05 <10 0.49 285 <1 0.03 8 680 5 <0.01 <2 2 296 0.1 <10 <10 27 <10 23 SFSB6T027 612139 5588128 <0.005 <0.2 0.32 <2 10 80 <0.5 <2 >25.0<0.5 2 5 15 0.4 <10 <1 0.03 <10 0.29 138 <1 0.03 5 640 4 <0.01 2 1 309 0 <10 <10 10 <10 13 SFSB6T028 612122 5588028 <0.005 <0.2 0.25 <2 10 80 <0.5 2 >25.0<0.5 <1 4 10 0.31 <10 <1 0.02 <10 0.25 105 <1 0.03 2 470 4 <0.01 <2 <1 329 0 <10 <10 8 <10 9 SFSB6T029 612096 5587944 <0.005 <0.2 0.59 <2 10 90 <0.5 <2 >25.0<0.5 2 8 15 0.74 <10 <1 0.03 <10 0.33 239 <1 0.03 6 560 2 <0.01 3 1 274 0 <10 <10 16 <10 18 SFSB6T030 612103 5587936 <0.005 <0.2 0.25 <2 10 80 <0.5 <2 >25.0<0.5 1 4 13 0.3 <10 <1 0.02 <10 0.28 128 <1 0.03 3 550 3 <0.01 2 1 350 0 <10 <10 8 <10 10 SFSB6T031 612338 5588608 <0.005 <0.2 2.38 6 <10 80 0.5 <2 1.88 <0.5 11 38 29 3.36 10 <1 0.08 10 0.96 506 <1 0.07 28 820 3 0.02 3 6 160 0.2 <10 <10 100 <10 60 SFSB6T032 612207 5588589 <0.005 <0.2 2.01 3 10 70 <0.5 <2 2.33 <0.5 9 29 37 2.62 10 <1 0.08 10 0.83 495 <1 0.06 24 1020 5 0.08 2 5 147 0.2 <10 <10 87 <10 51 SFSB6T033 612117 5588652 <0.005 <0.2 2.37 4 <10 70 0.5 <2 1.66 <0.5 12 38 30 3.49 10 <1 0.09 10 0.93 537 <1 0.06 28 850 5 0.03 2 6 154 0.2 <10 <10 104 <10 61 SFSB6T034 612033 5588716 0.008 <0.2 2.59 7 <10 80 0.5 <2 1.75 <0.5 12 37 31 3.43 10 <1 0.1 10 1.01 570 <1 0.06 29 940 6 0.03 2 7 165 0.2 <10 <10 95 <10 58 SFSB6T035 611930 5588792 <0.005 <0.2 1.83 3 20 50 <0.5 <2 3.74 <0.5 7 16 67 2.17 10 <1 0.11 10 0.72 638 <1 0.03 15 1050 6 0.1 <2 4 136 0.1 <10 <10 51 <10 50 SFSB6T036 611868 5588735 <0.005 <0.2 2.67 3 <10 80 0.5 <2 1.88 <0.5 13 36 33 3.47 10 <1 0.08 10 1.04 591 <1 0.07 30 830 4 0.03 2 7 169 0.2 <10 <10 95 <10 56 SFSB6T037 611751 5588791 1.06 <0.2 2.68 <2 <10 80 0.5 <2 1.62 <0.5 13 47 32 4.15 10 <1 0.1 10 1.03 601 <1 0.06 31 580 5 0.02 <2 8 152 0.3 <10 <10 122 <10 68 SFSB6T038 611605 5588835 0.618 <0.2 2.33 4 <10 70 0.5 <2 1.54 <0.5 14 60 31 5.05 10 <1 0.08 10 0.92 629 <1 0.06 31 680 7 0.01 <2 7 137 0.3 <10 <10 168 <10 79 SFSB6T039 611493 5588882 <0.005 <0.2 2.6 3 <10 80 0.5 <2 1.56 <0.5 12 37 34 3.59 10 <1 0.08 10 0.96 561 <1 0.05 30 550 5 0.01 <2 7 143 0.2 <10 <10 98 <10 58 SFSB6T040 611270 5588913 <0.005 <0.2 2.49 5 <10 80 0.5 <2 1.62 <0.5 12 47 31 3.89 10 <1 0.09 10 0.98 540 <1 0.07 31 710 3 0.02 <2 7 149 0.3 <10 <10 118 <10 62 SFSB6T041 611131 5588974 0.015 <0.2 2.74 4 <10 90 0.5 <2 1.72 <0.5 15 42 38 3.93 10 <1 0.1 10 1.06 659 <1 0.06 32 850 5 0.02 <2 8 160 0.2 <10 <10 107 <10 60 SFSB6T042 611007 5589099 <0.005 <0.2 2.59 3 <10 80 0.5 <2 1.64 <0.5 12 37 29 3.57 10 <1 0.09 10 1.05 541 <1 0.06 30 800 4 0.01 2 7 169 0.3 <10 <10 100 <10 57 SFSB6T043 610906 5589220 <0.005 <0.2 2.41 2 <10 80 0.5 <2 1.62 <0.5 12 38 32 3.61 10 <1 0.07 10 0.99 502 <1 0.07 31 750 4 0.02 2 6 165 0.3 <10 <10 108 <10 61 SFSB6T044 610777 5589287 <0.005 <0.2 2.64 <2 <10 80 0.5 <2 1.57 <0.5 12 36 28 3.42 10 <1 0.07 10 1.04 487 <1 0.07 31 610 4 0.01 2 7 164 0.2 <10 <10 95 <10 55 SFSB6T045 610659 5589351 <0.005 <0.2 2.34 <2 <10 80 <0.5 <2 1.66 <0.5 11 38 29 3.39 10 <1 0.09 10 0.97 468 <1 0.06 29 450 5 0.03 2 7 155 0.2 <10 <10 97 <10 54 CASB6T001 600241 5586349 <0.005 0.3 1.36 3 <10 80 <0.5 <2 0.73 <0.5 7 16 67 2.19 <10 <1 0.04 <10 0.63 521 1 0.02 13 610 3 0.08 3 5 45 0 10 <10 49 <10 87 CASB6T002 600304 5586302 0.02 <0.2 1.42 <2 <10 80 <0.5 <2 0.74 <0.5 9 16 74 2.19 <10 <1 0.04 <10 0.66 551 2 0.01 11 570 2 0.07 <2 5 46 0 <10 <10 50 <10 69 CASB6T003 600371 5586180 0.007 0.3 1.48 4 <10 90 <0.5 <2 0.83 <0.5 9 16 84 2.11 <10 1 0.04 <10 0.64 499 2 0.02 12 610 4 0.09 2 5 52 0 <10 <10 49 <10 71 CASB6T004 600420 5586111 0.006 0.2 1.72 7 <10 100 <0.5 <2 1.14 <0.5 10 18 117 2.3 10 <1 0.05 10 0.71 496 2 0.02 14 730 5 0.09 <2 6 59 0 <10 <10 51 <10 83 CASB6T005 600463 5586042 0.006 0.3 1.88 9 <10 110 <0.5 <2 0.74 <0.5 11 21 115 2.78 10 <1 0.05 10 0.76 758 3 0.02 17 630 5 0.05 3 6 49 0 10 <10 68 <10 84 CASB6T006 600527 5585988 0.009 0.4 1.8 9 <10 100 <0.5 <2 0.94 <0.5 10 21 228 2.25 10 1 0.05 10 0.73 550 2 0.02 16 700 7 0.08 <2 6 60 0 <10 <10 57 <10 73 CASB6T007 600599 5585936 0.007 0.3 1.72 <2 <10 150 <0.5 <2 0.91 <0.5 9 18 111 2.7 <10 1 0.05 10 0.67 588 4 0.01 14 760 5 0.09 <2 5 61 0 <10 <10 56 <10 75 CASB6T008 600654 5585889 0.007 0.4 2.24 13 <10 180 <0.5 <2 1.14 <0.5 12 22 131 3.16 10 1 0.07 10 0.73 1500 5 0.02 18 880 5 0.08 2 6 73 0 <10 <10 62 <10 88

Stream Sediment Sample Locations & Geochemistry - 1 - 2006 Exploration, Spences Bridge Properties, Bitterroot Resources Ltd., by S.T. Flasha & C.J. Greig

Sample UTM UTM Au Ag Al As B Ba Be Bi Ca Cd Co Cr Cu Fe Ga Hg K La Mg Mn Mo Na Ni P Pb S Sb Sc Sr Ti Tl U V W Zn Number Easting Northing ppm ppm % ppmppm ppm ppm ppm% ppm ppm ppm ppm %ppm ppm %ppm% ppm ppm % ppm ppm ppm % ppm ppm ppm % ppmppmppm ppm ppm CASB6T009 600719 5585826 0.007 0.5 2.48 11 <10 200 0.5 <2 1.15 <0.5 12 24 143 3.38 10 2 0.06 10 0.83 1075 2 0.02 18 970 9 0.07 <2 8 97 0 <10 <10 71 <10 90 CASB6T010 600764 5585732 0.006 <0.2 2.52 13 <10 140 <0.5 <2 0.97 <0.5 16 24 87 3.8 10 1 0.07 10 1.01 1350 2 0.02 19 900 9 0.06 <2 9 55 0 <10 <10 80 <10 120 CASB6T011 600825 5585643 0.005 <0.2 1.68 9 <10 60 <0.5 <2 0.58 <0.5 11 19 49 2.96 10 <1 0.04 <10 0.81 888 2 0.02 11 620 2 0.03 <2 6 34 0.1 <10 <10 72 <10 79 CASB6T012 600889 5585566 0.017 0.2 2.07 6 <10 270 0.5 <2 1.65 0.5 7 18 67 2.09 10 <1 0.09 10 0.53 2260 4 0.02 16 1120 13 0.09 3 4 116 0 <10 <10 45 <10 64 CASB6T013 601007 5585487 <0.005 <0.2 2.14 12 <10 120 <0.5 <2 0.99 <0.5 10 20 76 2.87 <10 <1 0.05 10 0.69 1015 1 0.02 14 980 5 0.06 <2 5 56 0 10 <10 66 <10 88 CASB6T014 600942 5585671 0.006 0.6 2.54 6 <10 300 0.7 <2 0.92 <0.5 10 27 145 2.64 10 1 0.07 10 0.68 448 1 0.02 21 510 9 0.06 <2 7 81 0 10 <10 56 <10 81 CASB6T015 600849 5585912 0.007 0.2 1.88 6 <10 290 <0.5 <2 0.85 <0.5 10 18 145 2.51 10 1 0.11 10 0.63 881 5 0.01 15 560 6 0.05 <2 6 87 0 10 <10 49 <10 71 CASB6T016 600505 5586376 0.005 0.2 1.04 <2 10 90 <0.5 <2 1.28 <0.5 7 10 74 1.86 <10 <1 0.06 <10 0.67 535 1 0.01 7 630 5 0.37 3 4 58 0 10 <10 34 <10 146 CASB6T017 599339 5590000 <0.005 <0.2 2.75 2 <10 110 0.5 <2 1.77 <0.5 13 36 41 3.03 10 <1 0.1 10 1.09 692 1 0.05 32 910 9 0.05 2 7 150 0.2 10 <10 79 <10 89 CASB6T018 599401 5590052 <0.005 <0.2 2.78 <2 <10 100 0.5 <2 1.83 <0.5 13 37 40 3.05 10 <1 0.09 10 1.12 585 1 0.05 32 790 4 0.05 <2 7 159 0.2 10 <10 81 <10 69 CASB6T019 599479 5590118 <0.005 <0.2 2.78 6 <10 100 0.5 <2 1.83 <0.5 14 37 38 3.06 10 1 0.1 10 1.12 721 1 0.05 33 830 7 0.05 <2 7 159 0.2 10 <10 84 <10 68 CASB6T020 599568 5590163 <0.005 <0.2 2.49 <2 <10 80 <0.5 <2 1.69 <0.5 13 35 27 3.03 10 <1 0.08 10 1.05 532 <1 0.05 30 770 6 0.04 <2 6 151 0.2 <10 <10 86 <10 60 CASB6T021 599679 5590203 0.008 <0.2 3 2 10 120 0.5 <2 1.55 <0.5 14 37 51 3.35 10 1 0.17 10 1.17 761 1 0.04 29 870 8 0.05 <2 8 122 0.2 10 <10 76 <10 95 CASB6T022 599738 5590283 <0.005 <0.2 3.19 <2 10 100 0.5 <2 2.04 <0.5 15 44 46 3.3 10 <1 0.11 10 1.26 639 1 0.06 39 960 5 0.08 <2 8 174 0.2 10 <10 89 <10 75 CASB6T023 599785 5590378 <0.005 0.2 2.92 <2 10 100 0.5 <2 1.98 <0.5 14 39 40 3.07 10 <1 0.11 10 1.13 644 <1 0.05 34 900 6 0.07 <2 7 175 0.2 10 <10 85 <10 66 CASB6T024 599872 5590428 <0.005 <0.2 2.87 7 <10 100 0.5 <2 1.98 <0.5 14 38 37 3.09 10 <1 0.09 10 1.14 659 1 0.06 36 820 7 0.06 <2 7 180 0.2 <10 <10 85 <10 65 CASB6T025 599954 5590482 0.006 <0.2 3.61 2 <10 130 0.7 <2 2.06 <0.5 17 44 60 3.7 10 1 0.12 10 1.38 933 1 0.06 41 960 8 0.04 <2 9 176 0.2 10 <10 92 <10 83 CASB6T026 600052 5590520 0.006 <0.2 2.94 3 10 100 0.5 <2 1.94 <0.5 14 39 43 3.15 10 <1 0.11 10 1.17 860 1 0.05 35 890 5 0.05 <2 7 170 0.2 <10 <10 88 <10 65 CASB6T027 600152 5590543 <0.005 0.3 2.79 7 10 90 0.5 <2 1.88 <0.5 13 38 39 2.96 10 <1 0.11 10 1.14 682 <1 0.05 33 930 7 0.08 <2 7 168 0.2 10 <10 86 <10 66 CASB6T028 600253 5590590 0.005 0.2 3.21 <2 <10 130 0.6 <2 1.89 <0.5 16 41 55 3.5 10 1 0.19 10 1.24 1285 1 0.05 41 1110 9 0.04 <2 9 182 0.2 <10 <10 91 <10 74 CASB6T029 600456 5590624 <0.005 <0.2 2.56 <2 <10 80 <0.5 <2 1.63 <0.5 13 34 28 2.92 10 <1 0.1 10 0.99 584 <1 0.06 30 660 4 0.02 <2 6 158 0.3 <10 <10 84 <10 63 CASB6T030 600615 5590703 <0.005 0.3 2.75 <2 <10 90 0.5 <2 1.57 <0.5 14 37 46 3.05 10 1 0.13 10 1.04 752 1 0.05 35 780 6 0.03 <2 7 141 0.2 <10 <10 81 <10 75 CASB6T031 600753 5590827 <0.005 <0.2 2.25 4 <10 80 <0.5 <2 1.54 <0.5 9 32 26 2.82 10 <1 0.09 10 0.89 567 <1 0.06 26 630 6 0.03 <2 6 146 0.3 <10 <10 84 <10 56 CASB6T032 600844 5590998 <0.005 <0.2 2.44 4 10 80 <0.5 <2 1.68 <0.5 11 32 32 2.86 10 <1 0.1 10 0.93 736 1 0.06 28 670 3 0.04 <2 6 152 0.2 10 <10 81 <10 58 CASB6T033 602040 5591935 <0.005 0.2 3.46 5 <10 110 0.6 <2 1.47 <0.5 15 42 36 4.1 10 1 0.08 10 1.01 1630 <1 0.05 37 910 6 0.02 <2 9 134 0.2 10 <10 107 <10 61 CASB6T034 601944 5591843 <0.005 0.2 2.52 6 10 90 0.5 <2 2.04 <0.5 11 34 43 3.18 10 1 0.07 10 0.83 1810 1 0.04 31 1120 6 0.08 2 6 139 0.2 <10 <10 91 <10 72 CASB6T035 601853 5591755 <0.005 <0.2 2.36 <2 10 80 <0.5 <2 1.52 <0.5 11 35 32 2.93 10 <1 0.06 10 0.81 644 1 0.05 29 670 7 0.04 2 6 127 0.2 <10 <10 85 <10 58 CASB6T036 601771 5591697 <0.005 <0.2 2.41 7 10 70 0.5 <2 2.12 <0.5 10 32 47 2.71 10 1 0.07 10 0.81 901 1 0.04 30 950 13 0.1 <2 6 134 0.2 10 <10 70 <10 103 CASB6T037 601705 5591644 <0.005 <0.2 2.53 8 10 80 0.5 <2 2 <0.5 10 36 38 2.93 10 <1 0.08 10 0.87 828 <1 0.05 29 980 7 0.08 <2 6 136 0.2 <10 <10 78 <10 51 CASB6T038 601701 5591622 <0.005 <0.2 1.96 2 20 50 0.5 <2 2.89 <0.5 8 46 52 1.97 10 1 0.08 10 0.8 944 <1 0.04 28 1140 3 0.13 <2 5 165 0.1 <10 <10 80 <10 34 CASB6T039 601607 5591593 <0.005 <0.2 2.32 <2 10 70 <0.5 <2 1.83 <0.5 10 35 30 2.73 10 <1 0.09 10 0.87 616 1 0.05 31 730 11 0.06 <2 6 138 0.2 <10 <10 81 <10 51 CASB6T040 601517 5591543 <0.005 <0.2 2.67 4 10 70 0.5 <2 1.95 <0.5 11 37 36 3.06 10 1 0.08 10 0.96 534 <1 0.05 31 820 7 0.05 <2 7 149 0.3 <10 <10 90 <10 57 CASB6T041 601429 5591467 <0.005 <0.2 4.53 2 <10 90 0.6 <2 2.42 <0.5 16 51 50 3.9 10 <1 0.12 10 1.46 616 1 0.05 50 880 8 0.01 <2 11 190 0.3 10 <10 99 <10 67 CASB6T043 605166 5594595 <0.005 0.2 0.99 7 20 40 <0.5 <2 13.9 <0.5 4 23 45 0.89 <10 1 0.05 <10 0.56 314 1 0.04 11 1260 5 0.18 <2 1 260 0.1 <10 <10 29 <10 22 CASB6T044 604993 5594583 <0.005 0.2 1.46 <2 10 50 <0.5 <2 7.96 <0.5 7 31 39 1.75 <10 <1 0.05 <10 0.78 349 <1 0.04 20 860 4 0.11 2 3 208 0.1 10 <10 55 <10 29 CASB6T045 604884 5594510 <0.005 0.2 2.19 4 10 70 <0.5 <2 3.37 <0.5 9 45 69 2.2 10 2 0.05 10 0.91 598 <1 0.05 26 930 3 0.1 <2 4 210 0.1 10 <10 61 <10 34 CASB6T046 604800 5594409 <0.005 <0.2 0.31 <2 10 20 <0.5 <2 >25.0<0.5 <1 11 30 0.24 <10 1 0.03 <10 0.33 98 <1 0.03 9 880 3 <0.01 2 <1 340 0 <10 <10 15 <10 9 CASB6T047 604719 5594326 <0.005 0.3 2.36 <2 10 80 <0.5 <2 1.63 <0.5 9 36 75 2.42 10 1 0.08 10 0.6 1300 <1 0.05 27 740 7 0.04 <2 4 110 0.2 <10 <10 61 <10 80 CASB6T048 604581 5594287 <0.005 0.4 2.97 8 10 70 0.5 <2 12.9 <0.5 10 52 57 2.37 10 1 0.1 10 1.08 511 <1 0.06 29 860 5 0.07 <2 5 247 0.1 10 <10 51 <10 47 CASB6T049 604461 5594269 <0.005 <0.2 2.84 3 10 60 <0.5 <2 3.44 <0.5 12 46 32 2.85 10 1 0.08 10 1.15 484 <1 0.07 30 750 7 0.05 <2 6 188 0.2 <10 <10 82 <10 47 CASB6T050 604358 5594289 <0.005 0.4 1.14 <2 20 60 <0.5 <2 3.91 0.5 5 26 45 1.29 <10 1 0.06 10 0.65 4140 1 0.03 19 1280 6 0.24 <2 2 172 0.1 <10 <10 39 <10 32 CASB6T052 603434 5594057 <0.005 <0.2 2.53 4 <10 120 0.5 <2 1.91 <0.5 11 43 39 3.09 10 1 0.09 10 1.05 473 <1 0.07 37 800 6 0.07 <2 6 198 0.2 <10 <10 80 <10 49 CASB6T053 603404 5594158 <0.005 <0.2 2.54 <2 <10 120 0.5 <2 1.69 <0.5 12 47 34 3.26 10 2 0.1 10 1.06 465 1 0.08 35 810 9 0.04 <2 6 207 0.2 <10 <10 88 <10 52 CASB6T054 603367 5594252 <0.005 <0.2 2.72 <2 10 130 0.5 <2 1.97 <0.5 12 43 41 3.1 10 <1 0.1 10 1.09 511 1 0.07 36 840 4 0.07 <2 7 196 0.2 10 <10 75 <10 51 CASB6T055 603343 5594358 <0.005 0.2 2.35 3 <10 120 0.5 <2 1.75 <0.5 12 48 37 3 10 <1 0.09 10 0.98 419 1 0.07 34 790 6 0.07 <2 6 186 0.2 10 <10 86 <10 50 CASB6T056 603465 5593916 <0.005 <0.2 2.31 <2 <10 110 <0.5 <2 1.73 <0.5 11 40 33 2.94 10 1 0.09 10 0.98 416 <1 0.07 34 780 5 0.05 2 6 190 0.2 10 <10 79 <10 64 CASB6T057 603440 5593810 <0.005 <0.2 2.2 2 <10 110 <0.5 <2 1.79 <0.5 10 39 35 2.86 10 <1 0.08 10 0.95 401 1 0.06 33 740 6 0.06 <2 6 179 0.2 <10 <10 77 <10 76 CASB6T058 603401 5593748 <0.005 <0.2 2.32 5 <10 110 0.5 <2 1.87 <0.5 11 38 36 2.9 10 1 0.08 10 0.99 445 <1 0.07 32 790 8 0.06 2 6 185 0.2 <10 <10 75 <10 96 CASB6T059 603356 5593680 0.011 <0.2 2.32 2 <10 110 <0.5 <2 1.63 <0.5 10 41 30 3.1 10 <1 0.09 10 1.02 434 <1 0.08 31 720 5 0.04 <2 6 194 0.2 <10 <10 85 <10 74 CASB6T060 603381 5593594 <0.005 0.3 2.37 9 <10 110 0.5 <2 1.97 <0.5 10 38 38 2.82 10 1 0.09 10 0.99 432 <1 0.07 33 840 9 0.07 <2 6 182 0.2 <10 <10 71 <10 188 CASB6T061 603469 5593541 <0.005 <0.2 2.39 5 <10 110 <0.5 <2 1.7 <0.5 11 42 34 3.06 10 <1 0.09 10 1.01 407 1 0.07 32 720 6 0.05 <2 6 180 0.2 10 <10 84 <10 81 CASB6T062 603415 5593511 <0.005 <0.2 2.27 5 <10 100 <0.5 <2 1.58 <0.5 11 40 29 2.91 10 <1 0.06 10 1.11 401 1 0.05 34 530 7 0.04 <2 5 151 0.2 <10 <10 76 <10 48 CASB6T063 603340 5593489 <0.005 0.5 2.08 4 10 100 <0.5 <2 2.31 <0.5 9 39 36 2.58 10 <1 0.06 10 1 398 <1 0.05 29 640 3 0.08 <2 5 170 0.2 <10 <10 66 <10 44

Stream Sediment Sample Locations & Geochemistry - 2 - 2006 Exploration, Spences Bridge Properties, Bitterroot Resources Ltd., by S.T. Flasha & C.J. Greig

Sample UTM UTM Au Ag Al As B Ba Be Bi Ca Cd Co Cr Cu Fe Ga Hg K La Mg Mn Mo Na Ni P Pb S Sb Sc Sr Ti Tl U V W Zn Number Easting Northing ppm ppm % ppmppm ppm ppm ppm% ppm ppm ppm ppm %ppm ppm %ppm% ppm ppm % ppm ppm ppm % ppm ppm ppm % ppmppmppm ppm ppm CASB6T064 603260 5593523 <0.005 <0.2 2.03 2 10 100 <0.5 <2 2.25 <0.5 9 39 39 2.5 10 1 0.06 10 0.95 397 <1 0.05 28 680 7 0.09 <2 5 168 0.2 10 <10 67 <10 45 CASB6T065 603178 5593572 <0.005 <0.2 2.2 <2 10 110 <0.5 <2 2.01 <0.5 10 42 34 2.76 10 <1 0.06 10 1.01 393 <1 0.06 30 670 5 0.07 <2 5 167 0.2 <10 <10 75 <10 48 CASB6T066 603099 5593581 <0.005 <0.2 1.89 3 10 80 <0.5 <2 1.93 <0.5 9 31 35 2.21 <10 <1 0.06 10 0.85 294 <1 0.04 24 630 5 0.08 <2 4 145 0.2 <10 <10 60 <10 42 CASB6T067 607059 5589664 <0.005 <0.2 2.17 6 <10 110 0.5 <2 1.4 <0.5 9 28 27 2.97 10 <1 0.09 10 0.68 536 <1 0.04 22 600 8 0.02 <2 6 181 0.2 <10 <10 76 <10 63 CASB6T068 607069 5589549 <0.005 0.2 2.24 4 <10 110 0.5 <2 1.37 <0.5 9 25 27 2.86 10 <1 0.09 10 0.68 531 <1 0.04 20 560 7 0.01 <2 6 186 0.2 <10 <10 72 <10 58 CASB6T069 607096 5589407 <0.005 0.2 2.23 2 <10 110 0.5 <2 1.49 <0.5 9 24 29 2.66 10 <1 0.09 10 0.69 499 <1 0.04 22 590 7 0.02 <2 6 176 0.2 <10 <10 64 <10 56 CASB6T070 607032 5589793 <0.005 0.2 1.8 5 10 40 <0.5 <2 1.97 <0.5 7 28 33 1.82 10 <1 0.05 10 0.65 415 <1 0.04 21 760 4 0.1 <2 4 102 0.1 <10 <10 51 <10 37 CASB6T071 606953 5589797 <0.005 <0.2 3.29 4 <10 110 0.8 <2 2.07 <0.5 15 32 45 3.69 10 <1 0.12 10 1.02 898 1 0.05 26 1000 9 0.05 <2 8 218 0.1 <10 <10 92 <10 72 CASB6T072 606897 5589769 <0.005 <0.2 2.76 3 <10 90 0.6 <2 1.53 <0.5 12 28 35 3.39 10 <1 0.08 10 0.89 740 <1 0.05 22 780 8 0.02 2 7 181 0.1 <10 <10 83 <10 66 CASB6T073 606807 5589720 0.006 0.3 1.98 6 10 50 0.5 <2 2.2 <0.5 8 31 37 2 10 <1 0.06 10 0.7 460 1 0.04 23 850 5 0.1 <2 4 114 0.1 <10 <10 57 <10 42 CASB6T074 606723 5589694 0.013 0.2 1.32 <2 10 30 <0.5 <2 2.93 <0.5 4 19 29 1.24 <10 <1 0.05 10 0.47 253 1 0.04 14 930 5 0.14 <2 3 90 0.1 <10 <10 37 <10 23 CASB6T075 606637 5589675 0.006 0.2 1.58 <2 10 30 <0.5 <2 2.61 <0.5 5 25 46 1.59 <10 <1 0.05 10 0.48 244 1 0.03 17 990 23 0.15 <2 3 90 0.1 <10 <10 41 <10 35 CASB6T076 606636 5589679 <0.005 <0.2 2.16 6 10 50 0.5 <2 2.05 <0.5 9 35 40 2.28 10 <1 0.06 10 0.76 467 1 0.05 25 740 8 0.08 <2 5 122 0.1 <10 <10 66 <10 47 CASB6T077 606797 5589665 <0.005 <0.2 3.05 2 <10 100 0.7 <2 1.9 <0.5 15 33 44 3.52 10 <1 0.1 10 1.03 850 <1 0.05 27 850 8 0.02 <2 8 202 0.1 <10 <10 91 <10 68 CASB6T078 606764 5589634 <0.005 0.2 2.93 <2 <10 100 0.7 <2 1.69 <0.5 14 36 39 4.12 10 <1 0.1 10 0.92 887 1 0.05 22 890 8 0.02 <2 8 199 0.2 <10 <10 108 <10 86 CASB6T079 606831 5589727 <0.005 <0.2 3.1 4 <10 110 0.7 <2 1.86 <0.5 15 30 40 3.64 10 <1 0.1 10 0.99 892 <1 0.05 25 840 8 0.01 <2 8 219 0.1 <10 <10 90 <10 71 CASB6T080 607167 5589913 <0.005 0.2 2.77 6 <10 100 0.7 <2 1.88 <0.5 12 28 47 3.04 10 <1 0.08 10 0.82 820 1 0.05 21 920 8 0.04 <2 7 194 0.1 <10 <10 77 <10 60 CASB6T081 607315 5589984 0.01 0.2 2.72 8 <10 90 0.6 <2 1.71 <0.5 11 28 34 3.29 10 <1 0.08 10 0.83 668 1 0.05 21 790 8 0.03 <2 7 177 0.2 <10 <10 84 <10 66 CASB6T082 610009 5587798 0.01 <0.2 0.14 7 30 10 <0.5 <2 3.72 <0.5 1 14 14 0.15 <10 <1 0.03 <10 0.28 91 6 0.06 2 830 5 1.23 2 <1 136 0 <10 10 55 <10 29 CASB6T083 610079 5587789 <0.005 <0.2 0.11 2 20 30 <0.5 <2 20.1 <0.5 <1 12 12 0.12 <10 <1 0.06 <10 0.3 1135 2 0.04 1 1660 3 <0.01 <2 <1 316 <0.01<10 <10 12 <10 7 CASB6T084 610152 5587900 0.007 <0.2 0.14 <2 20 30 <0.5 <2 >25.0<0.5 <1 13 11 0.14 <10 <1 0.03 <10 0.34 356 2 0.06 1 960 4 <0.01 2 <1 422 0 <10 <10 12 <10 10 CASB6T085 610123 5587993 <0.005 <0.2 0.19 <2 10 30 <0.5 <2 >25.0<0.5 <1 7 6 0.18 <10 <1 0.02 <10 0.33 257 <1 0.04 1 620 <2 <0.01 <2 <1 410 0 <10 <10 7 <10 6 CASB6T086 610110 5588100 <0.005 0.3 0.28 3 20 30 <0.5 <2 23 <0.5 <1 13 67 0.23 <10 <1 0.03 10 0.37 119 1 0.03 3 700 2 <0.01 3 1 366 0 <10 <10 12 <10 8 CASB6T087 610181 5588290 <0.005 <0.2 0.05 3 10 20 <0.5 <2 >25.0<0.5 <1 1 2 0.03 <10 <1 0.01 <10 0.28 84 <1 0.03 <1 340 <2 <0.01 <2 <1 427 <0.01<10 <10 4 <10 4 CASB6T088 610303 5588531 0.007 <0.2 0.47 2 20 20 <0.5 <2 17.6 <0.5 1 18 172 0.35 <10 <1 0.04 10 0.36 186 1 0.03 3 920 2 <0.01 <2 1 321 0 <10 <10 18 <10 10 CASB6T089 610376 5588660 <0.005 0.3 0.5 <2 20 30 <0.5 <2 19.3 <0.5 1 24 157 0.37 <10 <1 0.03 10 0.41 231 <1 0.04 5 1010 4 <0.01 2 1 359 0 <10 <10 14 <10 10 CASB6T090 610626 5588844 <0.005 0.4 0.16 <2 20 30 0.7 <2 16.3 0.7 <1 20 166 0.12 <10 <1 0.03 20 0.34 265 1 0.04 4 1080 2 <0.01 2 2 361 <0.01<10 <10 13 <10 6 CASB6T091 610839 5589187 <0.005 <0.2 2.29 <2 <10 80 <0.5 <2 1.85 <0.5 10 36 28 2.99 10 <1 0.08 10 0.95 431 <1 0.07 25 740 6 0.02 <2 6 161 0.2 <10 <10 91 <10 57 CASB6T092 610851 5589258 0.032 <0.2 2.41 2 <10 80 0.5 <2 1.78 <0.5 11 33 33 2.85 10 <1 0.08 10 0.96 446 <1 0.07 26 830 6 0.04 <2 6 166 0.2 <10 <10 82 <10 53 CASB6T093 612687 5588470 <0.005 <0.2 2.13 3 <10 70 <0.5 <2 2.36 <0.5 10 26 31 2.93 10 <1 0.1 10 0.97 531 <1 0.06 21 870 6 <0.01 2 6 138 0.2 <10 <10 82 <10 56 CASB6T094 612943 5588401 0.188 <0.2 2.15 <2 <10 70 <0.5 <2 1.5 <0.5 10 43 29 3.75 10 <1 0.08 10 0.92 508 <1 0.07 25 700 8 0.02 2 6 137 0.2 <10 <10 122 <10 66 CASB6T095 613133 5588400 <0.005 <0.2 2.21 3 10 70 <0.5 <2 1.91 <0.5 10 31 33 2.93 10 <1 0.1 10 0.98 508 <1 0.06 25 860 6 0.03 3 6 143 0.2 <10 <10 83 <10 56 CASB6T096 613382 5588450 <0.005 <0.2 2.13 <2 10 70 <0.5 <2 1.82 <0.5 10 34 30 2.92 10 <1 0.11 10 0.9 470 <1 0.06 24 840 5 0.05 <2 6 141 0.2 <10 <10 91 <10 54 CASB6T097 613606 5588407 <0.005 <0.2 2.18 3 <10 70 <0.5 <2 1.7 <0.5 10 32 27 2.96 10 <1 0.1 10 0.92 470 <1 0.06 25 830 5 0.03 <2 6 145 0.2 <10 <10 89 <10 55 CASB6T098 609869 5589826 <0.005 <0.2 1.69 5 <10 80 <0.5 <2 3.06 <0.5 8 28 25 3.12 10 <1 0.09 10 0.68 494 <1 0.05 15 740 6 0.05 <2 5 134 0.2 <10 <10 107 <10 69 CASB6T099 609744 5589959 0.101 <0.2 1.66 4 10 80 <0.5 <2 4.19 <0.5 7 22 27 2.32 <10 <1 0.12 10 0.69 444 <1 0.05 16 880 6 0.07 <2 5 147 0.1 <10 <10 69 <10 54 CASB6T100 609643 5590067 <0.005 <0.2 1.71 <2 <10 80 <0.5 <2 2.58 <0.5 8 24 24 2.69 10 <1 0.09 10 0.71 454 <1 0.06 17 750 7 0.05 <2 5 143 0.2 <10 <10 87 <10 61 CASB6T101 607344 5591796 <0.005 <0.2 2.44 2 <10 80 <0.5 <2 1.49 <0.5 11 43 28 3.27 10 <1 0.07 10 1 410 <1 0.08 27 560 6 0.01 <2 6 160 0.2 <10 <10 106 <10 54 CASB6T102 597077 5590877 <0.005 <0.2 2.33 5 <10 100 <0.5 <2 1.3 <0.5 12 36 38 2.99 10 <1 0.09 10 0.96 497 <1 0.06 29 530 5 0.02 2 7 147 0.2 <10 <10 80 <10 56 CASB6T103 596756 5585890 <0.005 <0.2 1.3 4 <10 70 <0.5 <2 0.76 <0.5 9 19 105 2.47 <10 <1 0.07 <10 0.62 522 2 0.02 11 570 2 0.02 <2 4 51 0 <10 <10 58 <10 62 CASB6T104 596596 5585800 <0.005 0.2 1.07 3 <10 40 <0.5 <2 0.51 <0.5 12 20 74 2.29 <10 <1 0.04 <10 0.6 391 2 0.02 11 400 4 0.01 <2 3 37 0.1 <10 <10 59 <10 43 CASB6T105 600475 5591968 <0.005 <0.2 2.5 4 <10 100 0.5 <2 1.28 <0.5 10 25 37 2.81 10 <1 0.13 10 0.68 720 <1 0.05 22 780 3 0.04 2 6 102 0.1 <10 <10 60 <10 72 CASB6T106 600862 5591337 <0.005 <0.2 2.25 2 10 120 0.5 <2 1.49 <0.5 10 26 40 2.7 10 <1 0.12 10 0.69 527 <1 0.06 23 600 5 0.03 4 6 123 0.1 <10 <10 59 <10 50 CASB6T107 598450 5589584 <0.005 0.2 2.08 4 <10 80 <0.5 <2 0.9 0.5 21 22 70 3.75 10 <1 0.07 <10 0.95 966 2 0.03 18 610 <2 0.02 <2 7 61 0.1 <10 <10 90 <10 232 CASB6T108 598570 5589549 <0.005 <0.2 1.99 3 <10 70 <0.5 <2 1.04 0.7 23 17 86 3.56 10 <1 0.06 <10 0.83 1045 3 0.02 16 620 5 0.04 2 6 53 0.1 <10 <10 85 <10 262 CASB6T109 598646 5589481 <0.005 <0.2 2.6 5 <10 100 <0.5 <2 1.17 0.7 21 16 112 3.85 10 <1 0.07 <10 1 948 2 0.03 14 410 3 0.03 2 9 70 0.1 <10 <10 91 <10 251 CASB6T110 598715 5589420 <0.005 <0.2 1.83 <2 10 70 <0.5 <2 1.22 0.5 17 19 102 3.39 10 <1 0.07 <10 0.92 797 2 0.03 17 730 4 0.08 2 6 61 0.1 <10 <10 83 <10 173 CASB6T111 598790 5589365 0.011 <0.2 1.72 3 10 60 <0.5 <2 1.44 0.8 17 14 93 3.02 10 <1 0.05 <10 0.76 718 2 0.02 13 590 2 0.08 <2 6 62 0.1 <10 <10 75 <10 196 IHSB6T001 597149 5587300 <0.005 <0.2 1.92 11 20 60 <0.5 <2 1.59 <0.5 12 28 123 3.05 <10 <1 0.08 <10 0.86 755 2 0.03 18 480 2 0.09 <2 6 65 0.1 <10 <10 74 <10 88 IHSB6T002 597238 5587370 <0.005 <0.2 1.08 13 60 60 <0.5 <2 3.43 0.7 7 16 184 1.47 <10 1 0.06 <10 0.49 1085 7 0.03 16 720 3 0.33 <2 3 111 0 <10 <10 37 <10 48 IHSB6T003 597327 5587396 0.006 0.2 1.21 19 40 50 <0.5 <2 2.75 <0.5 6 17 165 1.68 <10 1 0.09 <10 0.58 587 11 0.03 13 870 <2 0.18 <2 3 98 0 <10 <10 45 <10 49 IHSB6T004 597424 5587409 0.007 <0.2 2.59 12 10 60 <0.5 <2 1.23 <0.5 18 35 145 3.74 10 <1 0.07 <10 1.17 764 3 0.04 24 480 <2 0.05 <2 7 61 0.1 <10 <10 91 <10 80 IHSB6T005 597516 5587425 <0.005 <0.2 1.99 6 <10 70 <0.5 <2 0.85 <0.5 14 31 82 3.66 <10 1 0.05 <10 0.89 858 2 0.02 17 280 4 0.03 <2 7 48 0.1 <10 <10 93 <10 92

Stream Sediment Sample Locations & Geochemistry - 3 - 2006 Exploration, Spences Bridge Properties, Bitterroot Resources Ltd., by S.T. Flasha & C.J. Greig

Sample UTM UTM Au Ag Al As B Ba Be Bi Ca Cd Co Cr Cu Fe Ga Hg K La Mg Mn Mo Na Ni P Pb S Sb Sc Sr Ti Tl U V W Zn Number Easting Northing ppm ppm % ppmppm ppm ppm ppm% ppm ppm ppm ppm %ppm ppm %ppm% ppm ppm % ppm ppm ppm % ppm ppm ppm % ppmppmppm ppm ppm IHSB6T006 597588 5587458 <0.005 <0.2 1.91 7 <10 60 <0.5 <2 0.65 <0.5 14 32 79 3.69 10 1 0.06 <10 0.9 771 2 0.02 18 240 3 0.02 <2 7 41 0.1 <10 <10 97 <10 95 IHSB6T007 597662 5587499 0.005 <0.2 2.23 8 <10 90 <0.5 <2 1.25 0.5 13 31 104 3.63 <10 1 0.07 10 0.94 1050 2 0.02 19 380 4 0.04 <2 8 67 0.1 <10 <10 88 <10 104 IHSB6T008 597732 5587560 0.005 <0.2 2.07 8 <10 80 <0.5 <2 1.13 0.5 10 28 108 3.29 10 <1 0.08 <10 0.86 1055 2 0.02 18 490 3 0.05 <2 7 59 0.1 <10 <10 79 <10 103 IHSB6T009 597757 5587576 <0.005 <0.2 2.45 9 <10 90 <0.5 <2 1.11 0.7 12 29 129 3.49 10 <1 0.07 <10 0.9 1010 2 0.02 20 550 4 0.05 <2 8 55 0.1 <10 <10 79 <10 127 IHSB6T010 597854 5587607 0.007 <0.2 2.19 3 <10 80 <0.5 <2 1.36 0.5 11 27 143 3.29 <10 <1 0.08 10 0.84 1105 2 0.02 18 690 3 0.09 <2 7 66 0 <10 <10 78 <10 116 IHSB6T011 597951 5587623 <0.005 0.2 1.96 4 10 70 <0.5 <2 2.16 0.5 9 23 178 2.89 <10 1 0.05 10 0.78 710 4 0.02 18 530 2 0.13 <2 6 89 0 <10 <10 65 <10 95 IHSB6T012 598050 5587640 <0.005 <0.2 1.97 10 10 80 <0.5 <2 2.03 0.9 10 24 193 2.92 <10 <1 0.07 10 0.81 1125 3 0.02 18 720 3 0.13 <2 6 84 0 <10 <10 69 <10 106 IHSB6T013 598137 5587670 <0.005 0.2 2.07 6 10 90 <0.5 <2 1.66 1.1 11 27 175 3.2 10 <1 0.08 10 0.82 1315 2 0.02 20 770 4 0.11 <2 6 78 0 <10 <10 74 <10 135 IHSB6T014 598235 5587706 0.007 <0.2 2.06 4 <10 60 <0.5 <2 0.82 <0.5 12 28 123 3.72 <10 <1 0.06 <10 0.98 933 3 0.02 17 360 <2 0.03 <2 8 43 0.1 <10 <10 90 <10 110 IHSB6T015 598329 5587730 0.006 <0.2 2.27 7 <10 130 <0.5 <2 1.13 <0.5 13 27 67 3.77 <10 <1 0.07 10 0.87 1340 1 0.02 17 460 3 0.05 <2 8 78 0.1 <10 <10 84 <10 94 IHSB6T016 598424 5587767 <0.005 <0.2 2.32 5 <10 120 <0.5 <2 1.15 <0.5 12 24 70 3.61 <10 <1 0.07 10 0.85 1275 1 0.02 17 540 3 0.06 2 8 77 0 <10 <10 78 <10 92 IHSB6T017 598504 5587789 0.006 <0.2 2.67 9 <10 190 <0.5 <2 1.19 <0.5 13 27 80 3.97 10 <1 0.08 10 0.91 1610 2 0.02 17 400 6 0.03 <2 10 90 0.1 <10 <10 82 <10 107 IHSB6T018 598593 5587820 0.006 <0.2 2.48 10 <10 180 <0.5 <2 1.29 <0.5 11 24 77 3.34 10 <1 0.09 10 0.8 1680 2 0.02 17 700 4 0.06 <2 7 88 0 <10 <10 68 <10 109 IHSB6T019 598606 5587828 0.006 <0.2 2.33 3 <10 140 <0.5 <2 0.92 <0.5 14 25 59 3.74 10 <1 0.07 10 0.88 1145 2 0.02 14 370 4 0.02 <2 9 69 0.1 <10 <10 81 <10 95 IHSB6T020 598671 5587871 0.007 <0.2 2.63 7 <10 190 <0.5 <2 1.74 <0.5 11 22 97 3.26 10 <1 0.08 10 0.81 1335 1 0.02 16 800 5 0.08 <2 8 116 0 <10 <10 63 <10 104 IHSB6T021 598675 5587875 0.008 <0.2 2.51 4 <10 180 <0.5 <2 1.35 <0.5 12 23 80 3.4 10 1 0.08 10 0.83 1555 2 0.02 16 700 3 0.06 <2 7 93 0 <10 <10 70 <10 109 IHSB6T022 598752 5587915 0.006 <0.2 2 5 <10 130 <0.5 <2 1.14 <0.5 10 21 63 3.06 10 <1 0.06 10 0.74 940 1 0.01 12 530 <2 0.05 <2 6 76 0 <10 <10 68 <10 79 IHSB6T023 598852 5587941 0.005 <0.2 2.14 7 <10 170 <0.5 <2 1.34 <0.5 10 21 68 3.08 <10 <1 0.07 10 0.69 1495 1 0.01 13 600 3 0.07 <2 6 91 0 <10 <10 60 <10 92 IHSB6T024 598941 5587965 0.008 0.2 2.4 7 <10 180 <0.5 2 1.7 <0.5 10 20 92 2.68 10 1 0.08 10 0.72 1260 1 0.01 14 710 <2 0.24 <2 7 113 0 <10 <10 52 <10 102 IHSB6T025 599038 5587960 0.006 <0.2 2.41 6 <10 250 <0.5 <2 1.46 <0.5 13 22 82 3.35 10 1 0.07 10 0.74 3220 1 0.02 17 680 3 0.07 <2 7 106 0 <10 <10 62 <10 102 IHSB6T026 599122 5587925 0.01 <0.2 2.4 8 <10 230 <0.5 2 1.23 <0.5 15 21 89 3.67 <10 <1 0.06 10 0.72 2310 2 0.01 15 740 4 0.14 <2 6 85 0 <10 <10 67 <10 99 IHSB6T027 599165 5587889 0.007 0.2 2.39 6 <10 190 <0.5 <2 1.63 <0.5 10 21 85 2.99 10 <1 0.07 10 0.7 1685 1 0.02 15 670 2 0.08 <2 6 110 0 <10 <10 54 <10 96 IHSB6T028 599185 5587760 0.006 0.2 1.92 2 <10 60 <0.5 <2 0.61 <0.5 14 23 49 3.51 10 <1 0.08 <10 1.06 980 1 0.01 10 570 2 0.03 <2 6 40 0.1 <10 <10 82 <10 91 IHSB6T029 599200 5587734 0.006 0.2 1.88 8 <10 320 <0.5 <2 2.2 0.5 15 17 146 3.56 <10 1 0.05 10 0.61 7620 4 0.02 16 990 4 0.16 <2 5 143 0 <10 <10 48 <10 104 IHSB6T030 599235 5587812 0.006 0.2 3.02 11 <10 260 0.5 <2 1.69 0.5 10 23 75 3.23 10 <1 0.09 10 0.77 841 1 0.02 19 710 5 0.08 <2 8 129 0 <10 <10 63 <10 110 IHSB6T031 599308 5587770 <0.005 <0.2 2.7 8 <10 190 <0.5 <2 1.12 <0.5 11 22 66 3.3 10 <1 0.08 10 0.83 1030 1 0.02 16 670 3 0.06 <2 8 87 0 <10 <10 70 <10 111 IHSB6T032 599353 5587744 <0.005 0.3 3.15 13 <10 250 0.6 <2 1.42 0.6 11 24 109 3.42 10 1 0.08 10 0.8 1170 1 0.02 21 700 <2 0.06 <2 8 111 0 <10 <10 68 <10 123 IHSB6T033 596853 5586924 <0.005 <0.2 2.76 8 <10 80 <0.5 <2 0.9 <0.5 17 33 56 2.97 <10 <1 0.12 <10 1.29 664 1 0.05 24 220 3 <0.01 <2 6 59 0.1 <10 <10 79 <10 68 DNSB6T001 600835 5592805 0.006 0.4 2.33 2 10 70 0.7 <2 2.73 0.7 8 25 106 2.09 10 1 0.04 10 0.7 766 1 0.06 28 1740 5 0.17 3 3 93 0.1 <10 <10 62 <10 62 DNSB6T002 600694 5592805 0.006 0.3 2.32 3 10 70 0.7 <2 1.92 0.8 9 24 101 2.16 10 <1 0.04 10 0.61 713 <1 0.05 31 1410 6 0.1 2 4 61 0.1 <10 <10 57 <10 58 DNSB6T003 600607 5592796 <0.005 0.2 2.58 <2 10 110 0.7 <2 2.5 0.7 9 23 68 2.49 10 2 0.07 10 0.7 691 <1 0.05 25 1190 7 0.1 2 4 105 0.1 <10 <10 62 <10 88 DNSB6T004 600512 5592786 <0.005 0.2 2.26 <2 10 110 0.6 <2 2.47 <0.5 7 20 52 2.2 10 1 0.09 10 0.67 546 1 0.05 20 1280 8 0.12 <2 4 124 0.1 <10 <10 52 <10 66 DNSB6T005 600407 5592803 <0.005 0.2 1.76 3 10 80 0.5 <2 3.33 <0.5 7 16 55 1.68 <10 1 0.07 10 0.57 789 <1 0.04 18 1470 6 0.17 2 2 104 0.1 <10 <10 39 <10 50 DNSB6T006 600309 5592783 0.006 0.2 1.84 10 10 80 0.6 <2 2.74 <0.5 7 17 55 1.79 10 1 0.05 10 0.55 443 <1 0.04 17 1140 6 0.16 2 3 97 0.1 <10 <10 47 <10 46 DNSB6T007 600227 5592793 <0.005 0.2 1.68 <2 10 90 0.5 <2 3.34 0.5 8 17 46 1.7 <10 <1 0.05 10 0.55 2320 1 0.05 16 1400 6 0.19 2 2 102 0.1 <10 <10 45 <10 39 DNSB6T008 600138 5592791 <0.005 <0.2 1.81 <2 10 90 0.5 <2 3.22 0.6 7 17 44 1.75 <10 1 0.06 10 0.55 3150 1 0.05 18 1560 6 0.19 2 2 99 0.1 <10 <10 41 <10 35 DNSB6T009 600036 5592788 <0.005 0.3 2.07 <2 10 90 0.6 <2 3.21 0.5 7 19 43 1.95 10 1 0.06 10 0.64 685 1 0.05 19 1340 7 0.17 2 3 108 0.1 <10 <10 40 <10 37 DNSB6T010 599934 5592811 <0.005 0.3 2.01 8 10 80 0.5 <2 3.16 <0.5 7 20 45 1.77 <10 1 0.05 10 0.62 381 <1 0.05 18 1220 6 0.2 <2 3 104 0.1 <10 <10 43 <10 35 DNSB6T011 599859 5592830 <0.005 <0.2 2.1 <2 10 90 0.6 <2 3.39 0.5 7 20 46 1.97 10 1 0.07 10 0.66 693 1 0.05 21 1450 5 0.18 3 3 108 0.1 <10 <10 42 <10 36 DNSB6T012 599785 5592843 <0.005 0.2 2.66 2 <10 120 0.6 <2 2.03 <0.5 10 28 45 2.94 10 1 0.09 10 0.85 548 <1 0.06 26 670 6 0.06 2 7 124 0.1 <10 <10 62 <10 49 DNSB6T014 599651 5592910 <0.005 <0.2 2.33 4 10 110 0.6 <2 2.56 <0.5 9 23 38 2.56 10 <1 0.1 10 0.82 440 1 0.06 22 880 6 0.12 <2 6 124 0.1 <10 <10 59 <10 47 DNSB6T015 599579 5592935 <0.005 0.2 2.84 2 <10 140 0.6 <2 1.74 <0.5 13 31 36 3.34 10 <1 0.12 10 1.1 701 1 0.12 32 770 6 0.03 <2 9 201 0.2 <10 <10 88 <10 58 DNSB6T016 599501 5592969 <0.005 <0.2 2.57 <2 <10 130 0.6 <2 1.67 <0.5 12 30 35 3.16 10 1 0.12 10 1.01 611 1 0.09 30 770 7 0.04 <2 7 172 0.2 <10 <10 81 <10 56 DNSB6T017 599416 5593003 <0.005 0.2 2.58 2 10 140 0.6 <2 1.97 <0.5 10 27 40 2.99 10 <1 0.11 10 0.91 471 <1 0.06 25 750 7 0.06 <2 7 134 0.1 <10 <10 68 <10 52 DNSB6T018 599334 5593039 <0.005 <0.2 2.69 <2 <10 150 0.7 <2 1.53 <0.5 11 30 33 3.4 10 <1 0.09 10 0.94 424 1 0.06 24 480 4 0.03 2 8 128 0.1 <10 <10 81 <10 51 DNSB6T019 599253 5593079 <0.005 <0.2 2.47 <2 10 130 0.6 <2 2.25 <0.5 10 28 38 2.91 10 1 0.09 10 0.92 430 <1 0.07 24 770 8 0.07 <2 7 151 0.1 <10 <10 73 <10 47 DNSB6T020 599186 5593120 <0.005 <0.2 2.06 5 20 110 0.5 <2 2.7 <0.5 9 24 39 2.51 10 1 0.09 10 0.83 416 1 0.06 22 910 4 0.11 3 5 136 0.1 <10 <10 61 <10 42 DNSB6T021 599093 5593166 0.006 <0.2 2.44 7 10 130 0.5 <2 1.84 <0.5 10 31 37 3.12 <10 1 0.09 10 0.93 407 <1 0.07 24 750 4 0.05 2 7 146 0.2 <10 <10 78 <10 50 DNSB6T022 599028 5593255 <0.005 <0.2 2.1 <2 10 110 0.5 <2 2.7 <0.5 9 25 45 2.49 10 1 0.09 10 0.84 449 1 0.07 23 950 6 0.11 <2 6 148 0.1 <10 <10 65 <10 43 DNSB6T023 598956 5593329 0.011 <0.2 2.28 <2 10 120 0.5 <2 1.84 <0.5 10 30 32 2.96 10 1 0.09 10 0.86 427 <1 0.07 23 670 7 0.05 <2 6 146 0.2 <10 <10 78 <10 50 DNSB6T024 598865 5593364 <0.005 <0.2 2.25 2 10 120 0.5 <2 1.62 <0.5 10 30 33 2.95 10 1 0.09 10 0.87 502 <1 0.07 23 710 6 0.04 <2 6 141 0.2 <10 <10 79 <10 51 DNSB6T025 598787 5593376 0.006 <0.2 2.18 6 10 100 0.5 <2 1.98 <0.5 11 37 41 2.42 <10 1 0.09 10 0.9 384 1 0.07 28 950 6 0.12 2 6 155 0.1 <10 <10 80 <10 65 DNSB6T026 598779 5593408 0.005 0.2 2.08 <2 10 100 <0.5 <2 1.95 <0.5 11 36 40 2.35 10 1 0.09 10 0.88 379 1 0.07 29 930 5 0.12 <2 5 153 0.1 <10 <10 78 <10 65

Stream Sediment Sample Locations & Geochemistry - 4 - 2006 Exploration, Spences Bridge Properties, Bitterroot Resources Ltd., by S.T. Flasha & C.J. Greig

Sample UTM UTM Au Ag Al As B Ba Be Bi Ca Cd Co Cr Cu Fe Ga Hg K La Mg Mn Mo Na Ni P Pb S Sb Sc Sr Ti Tl U V W Zn Number Easting Northing ppm ppm % ppmppm ppm ppm ppm% ppm ppm ppm ppm %ppm ppm %ppm% ppm ppm % ppm ppm ppm % ppm ppm ppm % ppmppmppm ppm ppm DNSB6T027 598892 5593582 0.005 <0.2 2.26 <2 <10 110 <0.5 <2 1.5 <0.5 13 37 29 2.81 10 <1 0.09 10 0.98 467 <1 0.07 31 730 6 0.03 <2 6 166 0.2 <10 <10 79 <10 52 DNSB6T028 598988 5593735 0.051 <0.2 2.03 3 <10 110 <0.5 <2 1.44 <0.5 11 34 28 2.55 10 1 0.09 10 0.89 425 <1 0.07 27 720 4 0.04 2 5 163 0.2 <10 <10 76 <10 55 DNSB6T029 599063 5593923 0.006 <0.2 2.45 <2 <10 120 0.5 <2 1.54 <0.5 13 37 33 2.9 10 <1 0.16 10 1.05 531 <1 0.07 34 820 7 0.04 2 6 170 0.2 <10 <10 81 <10 53 DNSB6T030 599123 5594100 <0.005 <0.2 2.23 <2 <10 120 <0.5 <2 1.55 <0.5 12 35 31 2.64 10 <1 0.08 10 0.91 448 <1 0.08 30 670 5 0.04 <2 6 176 0.2 <10 <10 74 <10 50 DNSB6T031 599218 5594262 <0.005 0.2 2.16 <2 <10 110 <0.5 <2 1.5 <0.5 11 37 30 2.63 10 <1 0.08 10 0.93 374 <1 0.07 30 700 5 0.04 <2 6 170 0.2 <10 <10 74 <10 49 DNSB6T037 599445 5594375 <0.005 <0.2 1.66 <2 10 100 <0.5 <2 2.44 <0.5 8 28 45 1.97 <10 1 0.08 10 0.75 467 1 0.05 23 1070 6 0.13 <2 4 144 0.1 <10 <10 70 <10 75 DNSB6T038 599568 5594363 <0.005 <0.2 1.92 <2 <10 110 <0.5 <2 1.43 <0.5 10 34 32 2.6 <10 <1 0.06 10 0.9 350 1 0.05 26 650 4 0.04 <2 5 138 0.2 <10 <10 72 <10 61 DNSB6T039 599672 5594349 <0.005 0.2 1.76 6 10 100 <0.5 <2 2.13 <0.5 9 30 37 2.15 <10 1 0.06 10 0.83 318 1 0.05 24 810 5 0.1 3 4 146 0.1 <10 <10 59 <10 58 DNSB6T040 599795 5594361 <0.005 <0.2 1.93 <2 <10 120 <0.5 <2 1.4 <0.5 11 32 30 2.59 10 <1 0.07 10 0.91 416 <1 0.06 26 660 6 0.04 3 5 148 0.2 <10 <10 72 <10 70 DNSB6T041 599909 5594399 <0.005 <0.2 2.02 <2 10 120 <0.5 <2 1.62 <0.5 11 33 34 2.58 <10 <1 0.08 10 0.88 531 <1 0.06 25 720 6 0.06 3 5 152 0.2 <10 <10 73 <10 76 DNSB6T042 600013 5594446 <0.005 <0.2 1.94 <2 10 110 <0.5 <2 1.81 <0.5 11 32 35 2.43 10 <1 0.08 10 0.85 481 1 0.06 26 820 4 0.07 2 5 158 0.1 <10 <10 74 <10 84 DNSB6T043 600091 5594506 <0.005 <0.2 1.82 4 <10 110 <0.5 <2 1.77 <0.5 10 35 34 2.48 10 2 0.07 10 0.91 408 <1 0.05 25 770 5 0.08 <2 5 144 0.1 <10 <10 74 <10 58 DNSB6T044 600141 5594579 <0.005 0.3 1.52 <2 10 90 <0.5 <2 3.35 0.5 8 28 47 1.74 <10 1 0.07 10 0.75 287 1 0.04 22 1120 6 0.23 <2 3 164 0.1 <10 <10 57 <10 41 DNSB6T045 600163 5594659 <0.005 0.2 1.94 6 10 120 <0.5 <2 1.89 <0.5 11 37 45 2.45 10 <1 0.08 10 0.89 494 1 0.05 28 910 6 0.09 <2 5 146 0.1 <10 <10 69 <10 71 DNSB6T046 601418 5594107 <0.005 0.7 0.16 2 40 120 <0.5 3 3.82 <0.5 3 1 11 0.75 <10 1 0.01 <10 <0.0145000 3 0.03 3 990 5 0.7 2 <1 189 <0.01 10 20 12 <10 16 DNSB6T047 602421 5593616 0.005 <0.2 1.81 <2 10 90 <0.5 <2 3.87 <0.5 10 36 41 2.73 <10 <1 0.05 10 0.96 483 <1 0.05 26 660 5 0.05 3 5 150 0.2 <10 <10 79 <10 45 DNSB6T048 602542 5593564 <0.005 <0.2 1.54 <2 10 90 <0.5 <2 9.49 <0.5 7 26 36 1.87 <10 <1 0.05 10 0.75 318 <1 0.05 18 710 6 0.09 2 3 197 0.1 <10 <10 50 <10 34 DNSB6T049 602618 5593556 <0.005 <0.2 1.9 6 10 100 <0.5 <2 3.18 <0.5 10 32 35 2.49 10 <1 0.05 10 0.92 304 <1 0.05 24 650 4 0.09 2 4 152 0.2 <10 <10 68 <10 45 DNSB6T050 602697 5593579 <0.005 <0.2 1.74 <2 10 90 <0.5 <2 4.03 <0.5 9 31 47 2.14 10 1 0.06 10 0.82 385 <1 0.05 23 860 5 0.12 3 4 166 0.1 <10 <10 57 <10 38 DNSB6T051 602821 5593582 <0.005 <0.2 1.8 <2 10 90 <0.5 2 2.9 <0.5 10 30 42 2.2 10 1 0.05 10 0.86 332 <1 0.06 23 750 6 0.13 2 4 156 0.1 <10 <10 58 <10 40 DNSB6T052 602913 5593592 <0.005 0.2 2.04 <2 <10 100 <0.5 <2 2.07 <0.5 11 33 32 2.6 10 <1 0.07 10 0.97 357 <1 0.06 27 630 5 0.07 <2 5 156 0.2 <10 <10 72 <10 44 DNSB6T053 610146 5589618 0.006 0.4 2.33 <2 10 80 0.5 <2 2.02 <0.5 12 38 32 3.43 10 1 0.12 10 1.01 550 <1 0.06 30 980 8 0.05 <2 7 156 0.2 <10 <10 104 <10 59 DNSB6T054 610057 5589593 0.011 <0.2 2.41 4 <10 80 0.5 <2 2.06 <0.5 12 40 32 3.38 10 <1 0.09 10 1.03 546 <1 0.07 29 960 5 0.06 <2 7 163 0.2 <10 <10 104 <10 61 DNSB6T055 609904 5589650 0.006 0.2 2.43 <2 <10 80 0.5 <2 2.07 <0.5 12 43 40 3.55 10 <1 0.1 10 1.02 522 <1 0.08 30 870 17 0.05 <2 7 162 0.2 <10 <10 110 <10 74 DNSB6T056 609736 5589680 <0.005 <0.2 2.58 <2 <10 90 0.5 <2 1.97 <0.5 12 35 38 3.13 10 1 0.1 10 1.06 533 <1 0.07 29 920 8 0.06 3 7 175 0.2 <10 <10 90 <10 61 DNSB6T057 609548 5589686 0.036 0.2 2.41 <2 <10 90 <0.5 <2 2.11 <0.5 12 35 32 3.14 10 <1 0.07 10 1.03 460 <1 0.07 29 720 8 0.04 <2 6 164 0.2 <10 <10 90 <10 54 DNSB6T058 609405 5589586 <0.005 <0.2 2.49 <2 <10 90 0.5 <2 1.63 <0.5 13 40 31 3.73 10 <1 0.07 10 1.08 555 <1 0.07 30 720 6 0.02 <2 7 156 0.2 <10 <10 111 <10 63 DNSB6T059 609307 5589445 <0.005 <0.2 2.49 6 <10 90 0.5 <2 1.72 <0.5 12 36 30 3.28 10 1 0.07 10 1.04 486 <1 0.07 30 770 6 0.03 3 7 166 0.2 <10 <10 95 <10 58 DNSB6T060 609153 5589544 0.012 <0.2 2.17 <2 <10 80 <0.5 <2 1.69 <0.5 13 45 28 3.98 10 1 0.08 10 0.97 603 <1 0.06 29 890 3 0.03 <2 6 142 0.2 <10 <10 132 <10 69 DNSB6T061 609004 5589723 <0.005 <0.2 2.46 <2 <10 90 0.5 <2 1.95 <0.5 12 36 33 3.21 10 <1 0.1 10 1.02 502 1 0.07 28 840 7 0.05 <2 7 170 0.2 <10 <10 97 <10 55 DNSB6T062 608882 5589937 0.007 <0.2 2.55 5 <10 90 0.5 <2 2.03 <0.5 13 36 34 3.13 10 <1 0.09 10 1.04 480 1 0.07 29 920 7 0.06 <2 7 174 0.2 <10 <10 95 <10 58 DNSB6T063 608778 5590122 <0.005 <0.2 2.71 <2 <10 100 0.5 <2 2.05 <0.5 13 37 37 3.23 10 <1 0.09 10 1.07 555 1 0.07 31 910 6 0.05 <2 7 180 0.2 <10 <10 93 <10 60 DNSB6T064 608666 5590291 0.01 <0.2 2.37 <2 <10 80 0.5 <2 1.72 <0.5 12 39 28 3.52 10 <1 0.09 10 1.03 526 1 0.07 29 910 7 0.03 2 7 150 0.2 <10 <10 110 <10 60 DNSB6T065 608532 5590459 <0.005 0.2 2.63 2 <10 100 0.5 <2 2 <0.5 12 42 35 3.23 10 1 0.08 10 1.09 498 1 0.08 30 820 7 0.04 4 7 189 0.2 <10 <10 95 <10 55 DNSB6T066 608541 5590446 <0.005 <0.2 2.69 <2 <10 100 0.5 <2 1.96 <0.5 13 42 33 3.23 10 <1 0.08 10 1.09 468 <1 0.08 30 780 7 0.03 2 7 198 0.2 <10 <10 94 <10 57 DNSB6T067 608364 5590609 <0.005 0.2 2.77 6 <10 90 0.5 <2 1.97 <0.5 12 40 38 3.42 10 <1 0.08 10 1.1 457 <1 0.07 31 880 5 0.04 <2 7 192 0.2 <10 <10 98 <10 59 DNSB6T068 608189 5590708 0.018 <0.2 2.75 <2 <10 90 0.5 <2 2.03 <0.5 13 39 34 3.45 10 <1 0.08 10 1.11 564 <1 0.07 29 890 5 0.03 <2 7 190 0.2 <10 <10 100 <10 57 DNSB6T069 600269 5587891 0.008 0.3 1.16 5 10 70 <0.5 2 2.6 2.1 7 11 112 1.19 <10 <1 0.08 20 0.34 1440 2 0.02 14 1480 14 0.17 <2 1 91 0 <10 <10 21 <10 126 DNSB6T070 600162 5587995 0.01 0.6 2.45 5 10 100 <0.5 <2 2.14 1 15 21 96 2.71 10 <1 0.07 10 0.96 1115 1 0.02 19 1130 7 0.13 <2 5 85 0 <10 <10 52 <10 199 DNSB6T071 600045 5588059 0.008 0.4 2.46 3 <10 90 <0.5 <2 1.45 1.1 23 22 94 3.46 10 <1 0.05 10 1.28 1105 1 0.02 18 830 4 0.1 <2 7 64 0 <10 <10 73 <10 254 DNSB6T072 599907 5588074 0.007 0.4 2.56 4 <10 90 0.7 <2 1.77 4.4 40 21 140 3.22 10 <1 0.06 10 1.19 1435 <1 0.02 37 990 6 0.12 <2 7 73 0 <10 <10 64 <10 1015 DNSB6T073 599759 5588140 0.011 0.2 4.02 4 <10 90 2.2 <2 1.41 9.1 207 18 635 2.89 10 <1 0.06 10 1.04 6330 2 0.01 95 1010 4 0.11 <2 9 61 0 <10 <10 61 <10 1995 DNSB6T074 599635 5588271 0.006 0.2 4.19 5 <10 100 2.2 <2 1.14 6.3 83 17 338 3.17 10 <1 0.05 10 1.08 3690 1 0.01 77 810 6 0.08 <2 9 64 0 <10 <10 64 <10 2150 DNSB6T075 599569 5588358 <0.005 0.2 3.01 5 10 110 1.2 <2 1.89 6.3 86 15 326 2.98 10 <1 0.05 10 0.92 4410 5 0.01 57 960 5 0.12 <2 6 89 0 <10 <10 61 <10 1325 DNSB6T076 599526 5588485 0.005 0.2 3.15 3 10 120 1 <2 1.41 4.8 75 16 280 3.67 10 <1 0.06 10 1 3310 2 0.01 50 980 6 0.09 <2 8 76 0 <10 <10 81 <10 1255 DNSB6T077 599441 5588592 0.005 0.3 2.63 <2 10 100 0.9 <2 1.54 4.1 68 15 282 3.34 <10 <1 0.06 10 0.89 2620 4 <0.01 44 920 8 0.09 <2 7 82 0 <10 <10 79 <10 1015 DNSB6T078 599376 5588683 0.007 0.2 2.21 <2 10 80 0.6 <2 1.11 2.3 43 15 183 4 10 <1 0.06 <10 0.84 1795 4 <0.01 27 720 5 0.05 <2 7 68 0.1 <10 <10 119 <10 599 DNSB6T079 599321 5588776 0.014 0.2 2.17 <2 10 80 0.5 <2 1.08 2.3 42 13 163 3.74 10 <1 0.05 <10 0.85 1740 4 <0.01 25 730 4 0.05 <2 7 66 0.1 <10 <10 100 <10 569 DNSB6T080 599255 5588866 0.006 0.2 2.36 2 10 100 0.6 <2 1.51 2.2 38 15 208 3.39 10 <1 0.06 10 0.98 1925 3 0.01 28 650 7 0.05 <2 8 80 0.1 10 <10 86 <10 664 DNSB6T081 599162 5588931 0.005 <0.2 2.56 2 <10 100 0.5 <2 0.78 1.5 49 18 135 4.1 10 <1 0.06 <10 0.98 1510 3 0.01 26 480 4 0.02 <2 9 59 0.1 <10 <10 98 <10 581 DNSB6T082 599079 5589012 <0.005 <0.2 1.69 8 10 60 <0.5 <2 1.69 1.2 18 13 186 3.04 <10 <1 0.05 <10 0.72 973 3 0.03 17 830 2 0.12 <2 5 74 0 <10 <10 91 <10 222 DNSB6T083 598965 5589101 <0.005 <0.2 1.88 6 10 70 <0.5 <2 1.26 0.9 17 14 112 3.27 <10 2 0.05 <10 0.78 772 2 0.03 14 680 <2 0.1 <2 6 64 0.1 <10 <10 92 <10 260 DNSB6T084 598948 5589102 <0.005 <0.2 1.66 6 10 60 <0.5 <2 1.51 1.1 18 13 133 3.04 <10 <1 0.05 <10 0.71 837 2 0.03 14 740 <2 0.12 <2 5 67 0.1 <10 <10 86 <10 256

Stream Sediment Sample Locations & Geochemistry - 5 - 2006 Exploration, Spences Bridge Properties, Bitterroot Resources Ltd., by S.T. Flasha & C.J. Greig

MOSS MAT SAMPLES SFSB6M001 599456 5586256 <0.005 <0.2 0.82 6 10 50 <0.5 <2 9.84 <0.5 6 11 70 1.65 <10 1 0.12 <10 0.47 1160 2 <0.01 6 620 2 0.09 3 2 215 0 <10 <10 38 <10 49 SFSB6M002 600210 5586389 <0.005 0.3 1.88 2 <10 140 <0.5 <2 1.49 <0.5 10 20 124 2.87 <10 1 0.06 10 0.81 1240 2 <0.01 15 830 4 0.08 3 6 82 0 <10 <10 56 <10 137 SFSB6M003 599311 5586246 <0.005 <0.2 1.13 3 <10 80 <0.5 <2 0.74 <0.5 8 17 67 2.46 <10 <1 0.08 <10 0.52 633 1 <0.01 9 560 3 0.02 2 3 45 0 <10 <10 59 <10 65 SFSB6M004 599560 5586235 0.008 0.2 1.04 5 <10 130 <0.5 <2 1.29 <0.5 6 14 194 2.13 <10 <1 0.09 10 0.38 413 1 <0.01 9 620 4 0.04 <2 2 85 0 <10 <10 51 <10 52 SFSB6M005 599625 5586108 0.009 0.3 1.38 8 10 180 <0.5 <2 1.82 <0.5 4 11 310 1.41 <10 1 0.16 10 0.35 650 2 <0.01 11 1080 8 0.1 3 1 126 0 <10 <10 23 <10 62 SFSB6M006 599647 5585992 0.053 0.4 1.61 7 <10 170 0.5 <2 1.45 <0.5 6 15 291 1.68 <10 <1 0.1 10 0.4 565 2 <0.01 15 870 7 0.06 3 2 102 0 <10 <10 31 <10 91 SFSB6M007 609643 5590067 <0.005 <0.2 2.29 <2 <10 80 <0.5 <2 1.76 <0.5 11 37 35 2.92 10 <1 0.08 10 0.98 480 <1 0.02 28 780 4 0.02 2 6 162 0.2 <10 <10 91 <10 50 SFSB6M008 598715 5589420 0.005 <0.2 1.68 3 10 70 <0.5 <2 1.76 0.7 15 16 132 2.71 <10 1 0.09 <10 0.84 739 2 <0.01 15 930 5 0.12 2 5 76 0.1 <10 <10 68 <10 191 IHSB6M001A 598510 5587797 <0.005 <0.2 2.44 2 <10 200 <0.5 2 1.49 <0.5 11 23 81 3.43 10 <1 0.09 10 0.82 1500 2 0.02 16 670 7 0.06 <2 7 103 0 <10 <10 68 <10 108 IHSB6M002A 598517 5587781 <0.005 <0.2 2.55 9 10 200 <0.5 <2 1.82 <0.5 11 22 91 3.16 10 <1 0.11 10 0.81 1900 1 0.02 17 950 3 0.09 <2 5 120 0 <10 <10 60 <10 114 IHSB6M003A 598844 5587938 <0.005 0.3 1.81 <2 <10 120 <0.5 <2 1.16 <0.5 9 19 58 2.82 <10 1 0.08 10 0.64 1115 1 <0.01 12 710 4 0.05 2 5 74 0 <10 <10 58 <10 90 IHSB6M001B 600646 5585896 <0.005 0.2 2.63 6 10 80 0.7 <2 2.23 <0.5 12 32 43 3.2 10 <1 0.14 10 0.89 809 1 <0.01 26 1060 6 0.05 2 7 172 0.1 <10 <10 94 <10 68 IHSB6M002B 600974 5585345 <0.005 <0.2 2.82 4 <10 90 0.7 <2 2.11 <0.5 13 34 45 3.39 10 <1 0.11 10 0.96 839 1 <0.01 27 980 8 0.03 4 7 196 0.1 <10 <10 93 <10 70 IHSB6M003B 600970 5585247 <0.005 0.2 0.31 2 10 70 <0.5 <2 3.05 0.6 3 3 72 0.32 <10 1 0.11 10 0.15 1365 1 <0.01 6 1730 5 0.15 2 <1 102 <0.01<10 <10 6 <10 76 CASBM001A 601939 5591838 <0.005 <0.2 1.55 12 <10 100 <0.5 2 0.85 <0.5 9 20 75 2.95 <10 <1 0.08 10 0.67 620 2 0.02 12 720 5 0.07 <2 5 48 0 <10 <10 73 <10 75 CASBM002A 601707 5591619 <0.005 <0.2 2.5 5 10 100 0.5 <2 1.92 <0.5 13 36 43 3.04 10 1 0.11 10 0.83 1585 <1 0.04 30 1140 4 0.07 <2 6 139 0.2 <10 <10 98 <10 106 CASB6M001B 607030 5589801 <0.005 0.2 1.4 8 10 100 <0.5 <2 1.61 0.6 7 16 68 1.94 <10 1 0.13 10 0.47 1275 1 0.02 9 1300 5 0.12 <2 2 80 0 <10 <10 45 <10 90 CASB6M002B 606950 5589795 <0.005 <0.2 1.76 7 20 50 0.5 <2 3.17 <0.5 7 45 46 1.75 <10 1 0.17 10 0.77 935 1 0.06 22 1470 4 0.14 <2 4 171 0.1 <10 <10 84 <10 35 DNSB6M001 599028 5593255 0.01 <0.2 1.87 3 10 90 <0.5 <2 1.82 <0.5 8 25 29 2.61 <10 1 0.1 10 0.81 436 <1 0.02 21 840 5 0.04 4 5 138 0.1 <10 <10 75 <10 43 DNSB6M002 598793 5593379 <0.005 <0.2 1.91 16 10 90 <0.5 <2 1.83 <0.5 8 24 34 2.46 10 <1 0.12 10 0.79 445 1 0.02 20 930 3 0.05 3 5 140 0.1 <10 <10 68 <10 41 DNSB6M003 600163 5594659 <0.005 0.2 1.94 5 10 110 <0.5 <2 1.85 <0.5 9 38 43 2.36 <10 1 0.1 10 0.85 461 <1 <0.01 26 880 4 0.06 2 5 146 0.1 <10 <10 67 <10 60 DNSB6M004 610039 5589601 0.181 0.3 2.12 4 <10 60 <0.5 <2 2.03 <0.5 10 37 31 2.95 <10 <1 0.09 10 0.91 456 <1 0.02 26 870 5 0.04 2 6 153 0.2 <10 <10 96 <10 51

Stream Sediment Sample Locations & Geochemistry - 6 - Appendix II. Soil Sample Locations & Geochemistry 2006 Exploration, Spences Bridge Properties, Bitterroot Resources Ltd., by S.T. Flasha & C.J. Greig

Soil Sample Locations Geochemistry -1- Appendix III. Rock Sample Locations, Descriptions, & Geochemistry 2006 Exploration, Spences Bridge Properties, Bitterroot Resources Ltd., by S.T. Flasha & C.J. Greig

Sample UTM UTM Sample Number Easting Northing Type Description CG06SBR01 598502 5589609 float rusty-weathering quartz eye porphyry rhyolite/quartz pebble conglomerate with distinctive bluish opalescent quartz eyes and 3-5% pyrite; a widespread, if not common, lithology in borrow pit CG06SBR02 598563 5589622 float rusty-weathering quartz eye porphyry rhyolite/quartz pebble conglomerate with distinctive bluish opalescent quartz eyes and 2-3% pyrite; from side of trail CG06SBR03 598566 5589630 float rusty-weathering "dioritic" rocks with local quartz-pyrite(?) veinlets and associated limonite and hematite; from side of trail CG06SBR04 599900 5589196 grab rusty-weathering rocks with moderately abundant limonite boxwork and local quartz-pyrite "crackle" veinlets and common clay alteration "seams"; side of Snow Hill road; possibly float, but not far from being in place; same place as sample CG06SBR05 CG06SBR05 599900 5589196 grab "crackle" veined (quartz-pyrite?) sugary textured sericitic felsic rocks (high-level intrusive?); rusty-weathering, limonite on fractures; side of Snow Hill road; possibly float, but not far from being in place; same place as sample CG06SBR04 CG06SBR06 600600 5588487 float blocky float of very fine-grained "felsite," containing locally abundant (3-5%?) pyrite, locally tarnished (could possibly be minor chalcopyrite, or perhaps even a speck of visible gold??); sulphides occur in seams or fracture coatings, but also as disseminations within pale- to medium-green-grey host rocks; side of Snow Hill road; float, but not far from being in place; same place as sample CG06SBR07 CG06SBR07 600600 5588487 float moderately abundant (approximately 3%) fracture-controlled and disseminated pyrite associated with sericite-chlorite seams and veinlets in chloritized felsic intrusive(?) rocks; side of Snow Hill road; float, but not far from being in place; same place as sample CG06SBR06 CG06SBR08 600578 5588451 float very rusty-weathering boxwork-rich siliceous (calc-silicate?) rocks, locally preserving heavily disseminated pyrite and pockets rich in chlorite and sericite; middle of Snow Hill road; float, but very close to being in place CG06SBR09 600571 5588302 grab subcrop; plagioclase(?)>chlorite>pyrite-(rare vfg garnet?) calc-silicate(?) rock ("greenstone"); fine- to medium-grained; medium to dark grey-green; pyrite common, medium-grained and commonly in cubic subhedra; variably rusty-weathering CG06SBR10 600292 5588364 grab blocky-fracturing and rusty-weathering very fine-grained sugary-textured calc-silicate of felsite with fracture-controlled and veinlet pyrite-chlorite (+/- sericite); more or less same as in previous samples; appears to be steeply interlayered with "greenstone" containing abundant chlorite and common pyrite; outcropping across 5+ metres CG06SBR11 600001 5587740 grab very rusty-weathering siliceous (calc-silicate?) rocks, locally preserving heavily disseminated pyrite

Sample Au Ag Al As B Ba Be Bi Ca Cd Co Cr Cu Fe Ga Hg K La Mg Mn Mo Na Ni P Pb S Sb Sc Sr Ti Tl U V W Zn Number ppm ppm % ppm ppm ppm ppm ppm % ppmppm ppm ppm %ppm ppm % ppm % ppm ppm % ppm ppm ppm % ppm ppm ppm % ppm ppm ppmppm ppm CG06SBR01 <0.005 <0.2 0.56 <2 <10 70 <0.5 <2 0.1 <0.5 5 19 15 2.9 <10 <1 0.3 <10 0.15 103 4 0.05 3 120 <2 1.54 <2 2 8 0 <10 <10 12 <10 17 CG06SBR02 <0.005 <0.2 0.43 <2 <10 110 <0.5 <2 0.1 <0.5 1 14 7 2.3 <10 <1 0.4 <10 0.02 24 1 0.08 1 90 <2 0.88 <2 1 15 0 <10 <10 10 <10 2 CG06SBR03 <0.005 <0.2 0.53 <2 <10 150 <0.5 <2 0.3 <0.5 2 9 44 10 10 1 0.1 <10 0.03 246 6 0.08 2 490 2 0.19 <2 3 46 0.1 <10 <10 30 <10 20 CG06SBR04 <0.005 <0.2 0.83 <2 <10 20 <0.5 <2 0.3 <0.5 3 8 6 1.7 <10 <1 0.1 <10 0.13 156 2 0.11 1 110 <2 0.01 <2 3 14 0 <10 <10 7 <10 12 CG06SBR05 <0.005 <0.2 0.41 <2 <10 20 <0.5 <2 0 <0.5 <1 9 2 1.6 <10 <1 0 <10 0.09 109 1 0.13 <1 70 <2 0.01 <2 2 3 0 <10 <10 5 <10 8 CG06SBR06 <0.005 <0.2 0.76 <2 <10 30 <0.5 <2 0.1 <0.5 10 24 3 2.4 <10 <1 0.1 <10 0.62 156 1 0.1 3 370 <2 1.86 2 5 2 0 <10 <10 22 <10 16 CG06SBR07 <0.005 <0.2 2.94 <2 <10 20 <0.5 <2 0 <0.5 17 18 34 5.1 10 <1 0.1 <10 2.5 694 1 0.05 9 220 <2 1.08 <2 21 6 0 <10 <10 91 <10 148 CG06SBR08 0.071 1.1 0.73 2 <10 30 <0.5 2 0 <0.5 2 17 8 3.5 <10 <1 0.1 <10 0.65 197 1 0.07 2 90 <2 0.77 <2 5 6 0 <10 <10 50 <10 22 CG06SBR09 <0.005 <0.2 3.1 2 <10 20 <0.5 <2 0.3 <0.5 21 4 23 6.1 10 <1 0 <10 3.15 799 <1 0.05 <1 370 <2 1.76 <2 16 4 0.2 <10 <10 218 <10 71 CG06SBR10 <0.005 <0.2 0.97 <2 <10 10 <0.5 <2 0.1 <0.5 3 21 3 1.9 <10 <1 0 <10 0.97 270 4 0.11 1 210 <2 0.22 2 7 4 0 <10 <10 30 <10 41 CG06SBR11 <0.005 <0.2 2.71 <2 <10 60 <0.5 <2 0.1 <0.5 23 12 16 6.4 10 <1 0.1 <10 2.19 1420 <1 0.07 14 290 <2 1.64 <2 23 11 0.1 <10 <10 239 <10 158

Rock Sample Locations, Descriptions, & Geochemistry -1- Appendix IV. Cost Statement 2006 Exploration, Spences Bridge Properties, Bitterroot Resources Ltd., by S.T. Flasha & C.J. Greig

COST STATEMENT 2006 Spences Bridge Properties

Consulting & Professional Wage/Day Days Sub-Total GST Total Totals Project Geologist $500.00 3.5 $1,750.00 $122.50 $1,872.50 Crew Foreman $400.00 15.5 $6,200.00 $434.00 $6,634.00 Crew (3 men @ 250/day) $750.00 10 $7,500.00 $525.00 $8,025.00 $16,531.50

Field Supplies sample bags, flagging, hip chain thread $228.00 $228.00

Fuel gasoline for work truck $430.00 $430.00

Truck Rental 10 day 4x4 truck rental $776.00 $776.00

Room & Board motel (2 rooms; 9 nights) $1,096.60 food $788.40 $1,885.00

Geochemistry ALS Chemex (silt, moss, soil & rock analyses) $7,757.00 $7,757.00

Other ship samples to lab $97.00 $97.00

GRAND TOTAL $27,704.50 Appendix V. Statement of Qualifications Statements of Qualifications I, Charles James Greig, of 250 Farrell St., Penticton, British Columbia, Canada, hereby certify that:

1. I am a graduate of the University of British Columbia with a B.Comm. (1981), a B.Sc. (Geological Sciences, 1985), and an M.Sc. (Geological Sciences, 1989), and have practiced my profession continuously since graduation.

2. I have been employed in the geoscience industry for over 20 years, and have explored for gold and base metals in North, Central, and South America, and Africa for both senior and junior mining companies, and have several years of experience in regional-scale government geological mapping.

3. I am a member in good standing of the Association of Professional Engineers and Geoscientists of British Columbia (license #27529).

4. I am a “Qualified Person” as defined by National Instrument 43-101.

5. I am not aware of any material fact or material change with respect to the subject matter of the technical report that is not reflected in the technical report, the omission to disclose which makes the technical report misleading.

6. I own shares of Bitterroot Resources Ltd., who is the owner of the Spences Bridge Properties.

7. I am an author of the report entitled; “2006 Exploration Program, Spences Bridge Properties” dated January 2007. I worked on and supervised the work program reported on herein. I have been involved with exploration on behalf of Bitterroot Resources Ltd. since 1996.

8. I have read National Instrument 43-101 and Form 43-101F1 and the technical report has been prepared in compliance with National Instrument 43-101 and Form 43-101F1.

Dated at Penticton, British Columbia, this 26th day of January, 2007

Respectfully submitted,

“Charles James Greig” - signed

Charles James Greig, P.Geo I, Susan Teresa Flasha, of 764 Government St, Penticton, British Columbia, Canada, hereby certify that:

1. I am a graduate of the Okanagan University College with a B.Sc. (Earth & Environmental Science, 2003), and have practiced my profession continuously since graduation.

2. I have been employed in the geoscience industry for 3 years, and have explored for gold and base metals in Canada for junior mining companies.

3. I am not aware of any material fact or material change with respect to the subject matter of the technical report that is not reflected in the technical report, the omission to disclose which makes the technical report misleading.

4. I am an author of the report entitled; “2006 Exploration Program, Spences Bridge Properties” dated January 2007. I worked on the program reported on herein. I have been involved with exploration on behalf of Bitterroot Resources Ltd. since March 2004.

Dated at Penticton, British Columbia, this 26th day of January, 2007

Respectfully submitted,

“Susan Teresa Flasha” - signed

Susan Teresa Flasha, B.Sc.

Quality Control

Laboratory Registration

ALS Chemex has attained ISO 9001:2000 registration at all of our North American and Peruvian laboratories as well as the Brisbane, Australia site, with Chile and the rest of Australia actively pursuing registration. Recently, we were accredited to ISO 9001:2000 for North America. ISO 9001:2000 requires evidence of a quality management system covering all aspects of our organisation. To ensure compliance with this system regular internal audits are undertaken by staff members specially trained in auditing techniques.

In addition, ALS Chemex is currently working towards accreditation to ISO 17025, which provides specific assessment of our laboratories’ analytical competence for specific analytical techniques. In our opinion, the combination of the two ISO standards provides our clients complete assurance regarding the quality of every aspect of ALS Chemex operations. Our Brisbane laboratory has already been similarly accredited by NATA for key analytical methods.

Aside from laboratory registration, ALS Chemex has been a leader in participating in and sponsoring the Assayer Certification program in the Canadian province of British Columbia, one of the few jurisdictions that maintains a rigorous assayer registration program. We have on staff a number of Registered Assayers who have undergone extensive theoretical and practical training and passed comprehensive examinations prior to receiving their certificates.

Proficiency Testing

As part of our progress towards ISO 17025 registration ALS Chemex laboratories participate in a number of international proficiency tests, such as those managed by CANMET (Proficiency Testing Program – Minerals Analysis Laboratories) and Geostats. Both of these agencies circulate samples for analysis twice a year and evaluate the performance of participating laboratories.

Documentation

All sample preparation and analytical procedures have been assigned unique code numbers so that we always know exactly which procedure is to be followed. Each code is fully documented by written procedures that contain unique filenames and a revision number. Senior technical staff and the Quality Assurance Manager must approve any new revision. All new methods must go through a process of method validation that ensures the proposed procedure conforms to reasonable standards with respect to such critical parameters as accuracy, precision and detection limit.

Quality Assessment

Assessment Procedures

Quality Assessment is the system of activities we employ to assure our clients and ourselves that our quality control procedures are effective in providing accurate data. Part of this assessment involves a continuing evaluation of the performance of our analytical systems, primarily through statistical analysis. There are, however, other aspects to our quality assessment program: Evaluation of Routine Quality Control Data

ALS Chemex standard operating procedures require the analysis of quality control samples (reference materials, duplicates and blanks) with all sample batches. As part of the assessment of every data set, results from the control samples are evaluated to ensure they meet set standards determined by the precision and accuracy requirements of the method.

In the event that any reference material or duplicate result falls outside the established control limits, an Error Report is automatically generated. This ensures the person evaluating the sample set for data release is made aware that a problem may exist with the data set and investigation can be initiated.

All data generated from quality control samples is automatically captured and retained in a separate database used for Quality Assessment. Control charts for in- house reference materials from frequently used analytical methods are regularly generated and evaluated by senior technical staff at Quality Assurance meetings to ensure internal specifications for precision and accuracy are being met.

Quality Control Reports

Quality control data for reference materials and duplicates are routinely reported to clients so that they may monitor laboratory data independently. These reports are generated at no charge to the client and are issued together with the Certificates of Analysis. QC data summaries and customised QC reports are also available. Please contact our Quality Assurance Department to request custom QC reports.

Round Robin Exchanges

Quality Assurance staff control monthly inter-laboratory test programs covering both gold and base metal determinations to monitor the quality of data generated by our network of laboratories. The Quality Assurance group selects and circulates the samples and then evaluates the performance of each laboratory through statistical analysis.

Sample Preparation Quality Control

As part of our routine procedures, ALS Chemex uses barren wash material between sample preparation batches and, where necessary, between highly mineralised samples. This cleaning material is tested before use to ensure no contaminants are present and results are retained for reference. In addition, logs are maintained for all sample preparation activities. In the event a problem with a prep batch is identified, these logs can be used to trace the sample batch preparation and initiate appropriate action. Performing regular QC checks on prepared material monitors sample preparation quality. Laboratories are required to submit results from QC checks to the Quality Assurance department to compile and make sure standards outlined in our Service Schedule are being met.

Quality Control Procedures for Sample Preparation

QC Specifications for Crushing and Grinding

ALS Chemex has established minimum specifications for crushing and pulverization procedures. Statistics are maintained for each sample preparation workstation, permitting an assessment of all pieces of machinery. Not only does this data ensure sample preparation specifications are being met, but it also allows us to optimise the sample preparation process and helps us in the purchase of new equipment.

Sample Tracking System

ALS Chemex has developed a unique sample tracking system that is an integral part of the company’s new Laboratory Information Management System (LIMS). This system utilizes bar coding and scanning technology that provides, for the first time by any laboratory, complete chain of custody records for every stage in the sample preparation and analytical process.

Upon receipt of samples at any of the ALS Chemex worldwide locations, a bar code label is attached to the original sample bag. This label is then scanned and the weight of sample recorded together with information such as date, time, equipment used and operator name. The scanning process is repeated for each subsequent activity performed on the sample from sample preparation to analysis through to the storage or disposal of the pulp and reject material. Sample labels are also scanned at the shipping and destination locations whenever samples are transported locally or internationally between ALS Chemex facilities. The system has also been designed to accept client supplied bar coded labels that are attached to the sample bags in the field.

The benefits to our clients of this system are:

• Complete traceability of the sample through the entire laboratory process. • Sample integrity is guaranteed by scanning the sample label at every stage. • Record of every sample weight submitted to the laboratory from the field. • Full computer generated audit report available on request to complement property evaluation audits.

Contamination Control during Sample Preparation

We take many steps to minimize the risk of cross contamination between samples during the preparation process. One of the most important steps is to sort and classify samples according to matrix type and expected metal concentrations as soon as they enter the laboratory. The samples will then be routed through the laboratory in different batch streams. Physically separated areas are maintained as much as possible so that, for example, concentrates and vegetation samples would never be processed in the same area.

Once samples are classified, they are prepared using equipment that has been designated for certain matrix types and expected metal concentration ranges. Equipment is color-coded and numbered so that it is clear for which sample type it is intended to be used.

In addition, our routine operating procedures call for the use of barren wash material to clean out sample preparation equipment between batches of submitted samples, drill holes (if identified) and samples that appear to be of a substantially different type than those submitted in the same batch. However, if the client expects significant mineralisation, we recommend that they identify the samples and request a clean ‘wash’ between samples. The wash material is tested for the elements of interest prior to use in the laboratory, and on a routine basis once in use.

By the end of 2001, our Dustbox dust extraction system is installed in all of our sample preparation laboratories. The Dustbox ensures that crushing and grinding equipment is virtually completely enclosed. Our experience has shown that the fine dust, which can otherwise collect, will invariably contain trace amounts of gold and base metals. The end result is an improved dust control system which reduces the risk of sample contamination and provides a healthier workplace environment for our employees.

It is unfortunate that all grinding surfaces impart some degree of metal content to samples during pulverisation. As a result, there will always be some degree of contamination when crushing and grinding procedures are used. However, at ALS Chemex we have a great variety of grinding surfaces that vary widely in their chemical composition. We offer equipment made of hardened manganese steel, chrome steel or carbon steel as well as non-ferrous materials such as zirconia and tungsten carbide. Hence an Explorer can choose one of these options in such a way as to eliminate the possibility of contaminating a sample with an element of potential exploration significance.

Sample Preparation Procedures

Crushing

Samples that require crushing are dried at 110-120°C and then crushed with either an oscillating jaw crusher or a roll crusher. The ALS Chemex QC specification for crushed material is that >70% of the sample must pass a 2mm (10 mesh) screen.

Pulverising

A whole or split portion derived from the crushing process is pulverised using a ring mill. The size of the split is determined by the client based on the pulverising procedure that is selected. Split sizes for manganese or chrome steel rings are typically 250 g to 4 kg; however split sizes for zirconia rings are 100 g and those for tungsten carbide rings are only 75 g. Because of the relative lightness of these latter two materials, the size of the sample to be pulverized must necessarily be reduced to these weights in order to achieve the ALS Chemex QC specification for final pulverizing, namely that >85% of the sample be less than 75 microns (200 mesh).

Screening

Soil and sediment samples are typically sieved through a 180 micron ( -80 mesh) screen and the fine fraction is retained for analysis. This procedure is satisfactory for smaller (i.e. 500 g or less) samples where the exploration target is base metals. However, when gold is the exploration target, we recommend that the particle size of the minus fraction be further reduced using ring mill pulverization to > 85% - 75 microns (150 mesh) in order to obtain more reproducible gold data.

Analytical Procedures

MEICP-41

Inductively Coupled Plasma Emission Spectroscopy (ICP-AES)

In plasma emission spectroscopy, a sample solution is introduced into the core of an inductively coupled argon plasma (ICP) at a temperature of approximately 8000°C. At this temperature all elements become thermally excited and emit light at their characteristic wavelengths. This light is collected by the spectrometer and passes through a diffraction grating that serves to resolve the light into a spectrum of its constituent wavelengths. Within the spectrometer, this diffracted light is then collected by wavelength and amplified to yield an intensity measurement that can be converted to an elemental concentration by comparison with calibration standards. This measurement process is a form of atomic emission spectroscopy (AES).

Advantages of ICP-AES Spectroscopy

• Many elements (up to 70 in theory) can be determined simultaneously in a single sample analysis; the largest ICP only package offered by ALS Chemex includes 34 elements. • Instrumentation is readily amenable to automation, thus enhancing accuracy, precision and throughput. • High instrumental productivity permits very competitive pricing of analytical packages, thus giving the explorer a significant return on a relatively small expenditure. • Electronic data capture and transfer to the LIMS ensures that no manual data transcription errors occur. • ICP-AES offers a useful working range over several orders of magnitude.

Limitations of ICP-AES Spectroscopy

• Complex instrumentation requires highly skilled staff both for routine operations and for repairs and maintenance. • The emission spectra are complex and inter-element interferences are possible if the wavelength of the element of interest is very close to that of another element; for example, one of the phosphorus wavelengths suffers from both copper and aluminum interference. • As with atomic absorption spectroscopy, the sample to be analysed must be digested prior to analysis in order to dissolve the element(s) of interest. In certain ICP packages (e.g., the ALS Chemex ME-ICP41 package), a significant number of elements are only partially digested. • Rigid temperature and humidity control is required for best stability of the spectrometer.

Aqua Regia Digestion

Quantitatively dissolves base metals for the majority of geological materials, and may provide anomaly enhancement in some geological environments. Major rock forming elements and more resistive metals are only partially dissolved.

Method code ME-ICP41 34 elements by aqua-regia acid digestion and ICP-AES.

Elements and Ranges (ppm) Ag (0.2 - 100) Co (1 - 10,000) Mn (5 - 10,000) Sr* (1 - 10,000) Al* (0.01% - 15%) Cr* (1 - 10,000) Mo (1 - 10,000) Ti* (0.01% - 10%) As (2 - 10,000) Cu (1 - 10,000) Na* (0.01% - 10%) Tl* (10 - 10,000) B* (10 - 10,000) Fe (0.01% - 15%) Ni (1 - 10,000) U (10 - 10,000) Ba* (10 - 10,000) Ga* (10 - 10,000) P (10 - 10,000) V (1 - 10,000) Be* (0.5 - 100) Hg (1 - 10,000) Pb (2 - 10,000) W* (10 - 10,000) Bi (2 - 10,000) K* (0.01% - 10%) S (0.01% - 10%) Zn (2 - 10,000) Ca* (0.01% - 15%) La* (10 - 10,000) Sb (2 - 10,000) Cd (0.5 - 500) Mg* (0.01% - 15%) Sc* (1 - 10,000) For elements marked with * digestion will be incomplete for most sample matrices.

AA-23

Fire Assay-Atomic Absorption procedures for Exploration and Low to Medium Grade Ore Samples

Exploration samples (particularly soils) may require a better detection limit than that offered by the above procedures. Method codes Au-AA21 and Au-AA22, which include a fire assay collection followed by cupellation, dissolution of the precious metal prill and a pre-concentration solvent extraction step. The final determination is by flame AAS, providing a detection limit of 1 ppb. It is a more expensive technique than the conventional fire assay /AAS procedure, but for explorers looking for the best resolution of low level gold anomalies, this procedure is excellent.

In recent times, we have turned to ICPMS technology to offer trace level gold. See method codes Au-MS21 and Au-MS22. In addition to a detection limit of 1ppb, the advantage offered by this technique is the ability to determine platinum and palladium together with gold.

Many samples arriving at our laboratories have "intermediate" levels of gold; that is in the range of 3-10 g/t (0.1-0.3 oz/ton). These samples are best analyzed using FA- AAS procedures Au-AA23, Au-AA24. If samples contain higher concentrations of gold, procedures Au-AA25 or Au-AA26 would be a more appropriate technique.

Advantages of the Fire Assay Process

• A large sub-sample (10-50g or more) can be taken for analysis, helping to ensure that the analytical sub-sample is truly representative of the sample submitted to the laboratory • The fire assay fusion is considered to provide a "total" gold. • All samples are amenable to the fire assay procedure in the hands of a skilled assayer. • The fire assay procedure is universally accepted as the definitive method for the analysis of gold. • The fire assay fusion quantitatively dissolves and extracts the entire platinum metal group in addition to gold and silver.

Limitations of the Fire Assay Process

• When a gravimetric finish is used, it is essential that the separation ("parting") of silver and gold is complete. If the silver is incompletely removed, then the gold results will be artificially high and the silver results will be low. • A certain amount of silver (usually estimated to be in the range of 2%) is lost by volatilization during the cupellation process. • When an atomic absorption spectroscopy finish is selected, the upper reporting limit is set at 10 g/t (0.3 oz/ton) and samples higher than this must be re-analyzed using additional silver in the firing process and a larger dilution factor. Alternatively, gravimetric finish can be used. • Samples containing coarse gold can give erratic results making it difficult to determine the true ore grade; however, sample heterogeneity rather than the fire assay process causes this problem. • Soil samples (typically -180um(-80 mesh material)) can also give erratic results but again for the same reason • It can take many years of experience before a fire assayer has the necessary degree of skill and knowledge to flux difficult ore types. • Some ores such as chromites and tellurides can be more difficult to fuse, resulting in the need to take smaller subsamples for analysis and consequently yielding higher detection limits than normal.

Material used in this summary can be found on the ALS Chemex website: www.alschemex.com