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Assessment Report

Diamond Drilling

on the

Clear Creek Mineral Property

Skeena Mining Division

16575 QuickEast Rd. Telkwa, BC, VOJ 2x2

February 19,2005

TABLE OF CONTENTS

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Summary ........................................................................................................... 1

Terms of Reference and Disclaimer .................................................................. 1

Location. Access and Physiography .................................................................. 1

Claim Ownership ............................................................................................... 2

Exploration History ............................................................................................ 2

Geology ............................................................................................................. 2 6.1 Regional Geology ....................................................................................... 2 6.2 Property Geology ........................................................................................ 3

2004 Diamond Drilling Program ......................................................................... 3

....................................................................................................... 4

Interpretation and Recommendations ................................................................ 5

REFERENCES ............................................................................................................. 7

AUTHOR’S STATEMENT ............................................................................................. 8

FIGURES, TABLES and APPENDICES ......................................................................... ii

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FIGURES, TABLES and APPENDICES

List of Figures

Figure 1 -Clear Creek Property - Location Map

Figure 2 - Clear Creek Property - Claim Map

Figure 3 -Clear Creek Property - Regional Geology Map

Figure 4 -Clear Creek Property - Drill Hole Location Map

List of Tables

Table 1 - Claim Status

Table 2 - Diamond Drill Hole Summary

Table 3 -Statement of Expenditures

List of Appendices

Appendix I - Drill Hole Logs

Appendix II - ALS Chemex Analytical Technique

Appendix 111 - ALS Chemex Assay Certificate

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Summary

The Clear Creek mineral property is located in the Cedar River valley north of Kitsumkalum Lake, 50 kilometres north of Terrace in northwest British Columbia. The property consists of three contiguous mineral claims totaling 51 units, mvering 1275 hectares. The claims are 100% owned by Harold Hendrickson.

The property is near the southern margin of the Middle Jurassic Bowser Lake Group sedimentary basin which overlaps Stikine Terrane and is less than 10 kilometres from the Coast plutonic complex.

Exploration on the property in 2004 consisted of 66.4 meters of AQTK diamond drilling in three holes. The work was completed between November 2 and November 14,2005 under permit MX-1637 and annual approval number SM1-2004- 0101717-1014 as issued by the Ministry of Energy and Mines in Smithers. Total cost for the work was $23,983.33.

Twenty-four split core samples were submitted for 34 element ICP analysis and for gold by tire assay with atomic absorption finish.

Very localized anomalous Mo values were encountered. Hole CCO4-03 returned 0.024 ppm Au, 787 ppm Cu, 306 ppm Mo; and 150 ppm W over a 0.7 meter interval from 6.0 to 6.7 meters.

Terms of Reference and Disclaimer

In-Depth Geological Services was contracted by Harold Hendrickson to log the drill core from the 2004 drilling program, to select samples for analysis and to write this assessment report. While the author has visited the property several times in the past three years to evaluate the various showings, he did not design, implement or supervise the 2004 drilling program.

Location, Access and Physiography

The Clear Creek mineral property is located on Mapsheet 1031.096 at Lat. 54O57’33”N. and Long. 128°5009”W in northwest British Columbia (Figure 1) on the east side of the Cedar River valley, 50 kilometres north of Terrace.

The property is on the western flank of the Nass Ranges at the eastem edge of a broad glacial valley at an elevation of about 500 meters. Outcrop exposure is good along numerous logging roads and in some deeply incised drainages. Vegetation consists of old growth conifer forest and numerous grassy, elevated swamps.

Access to the property from Terrace is via the Nass River Road which runs along the east side of Kitsumkalum Lake. Local logging roads provide good access to all three claims.

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. . , . . .

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Figure 1 - Property Location

4.0 Claim Ownership

Tenure No. Tenure Owner FMC Mapsheet Current Expiry Units Name Date

404226 409074 414106

5.0 Exploration History

CAT #I 11 1608 1031096 2005.07.28 15 LUCKY 11 1608 1031096 2005.03.23 20 A.B.C. 111608 I031096 2005.09.15 16

The area was previously explored as the Big Joe claims (Minfile 1031 023). Molybdenum mineralization was discovered in 1966 during construction of logging roads and the Big Joe claims were optioned from E.R. Anderson and 1. Remillong by Silver Standard Mines Ltd. (Burmeister, 1966). Silver Standard filed a molybdenum soil survey for claim assessment and the following year dug eight bulldozer trenches totalling 2500 metres in length. In 1971, the Big Joe claims were acquired by ASARCO but there is no record of work, nor of subsequent exploration activity, until 1998 when prospector Paul Wadsworth discovered a high grade gold-tungsten vein about 125 meters up the road from the molybdenum showing.

From 1998 to 2003, Harold Hendrickson explored the surrounding area by prospecting and VLF. During that time he discovered a high grade gold-silver showing (Hendrickson Vein) on the Lucky claim about 2600 meters east of the Wadsworth Vein.

6.0 Geology

6.1 Regional Geology The geology shown in Figure 3 is taken from the Mapplace. The claims are near the southern margin of the Middle Jurassic Bowser Lake Group sedimentary basin which overlaps Stikine Terrane, and the claims are less than 10 kilometers from the Coast plutonic complex. The claim area is underlain by grit. greywacke and siltstone of the Bowser Lake Group (Woodsworth et at., 1985). These rocks are intruded by a granodiorite stock w h i i is typical of the granitic rocks on the eastern flank of the Coast plutonic complex that yield K-Ar age determinations between 45 and 50 million years (Carter, 1971). The property is at the north end of a 100 kilometre long Tertiary graben known as the Kitimat Trench. This prominent topographic feature is 5 to 10 kilometers wide. South of the claims. the Kitimat Trench is

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0 0.5 1 .o 1.5 2.0

kilometers -

Figure 2 - Claim Map

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CCO4-01 CCO4-02 CCO4-03

occupied by Kitsumkalum Lake and the Cedar River, and to the north it terminates against the Nass mountain range.

The geologic setting between Terrace and Alice Arm is noted for a number of porphyry molybdenum occurrences associated with small granitic stocks, and for numerous polymetallic vein deposits. The area is currently being explored for intrusion related gold deposits.

6.2 Property Geology The geology of claims is not well understood as no property scale mapping has been conducted to date. Based on outcrop exposures along the logging access roads and on interpretation of the Mapplace aeromagnetic data, however, the entire property is likely underlain by a partially unroofed granodioiite stock between five and six kilometers in diameter. The Bowser Lake Group sediments forming roof pendants are locally hornfelsed and quartz veined. Mineralization within the quartz veins consists of local bismuthinite, native gold, scheelite, galena, sphalerite, and tetrahedrite(?).

Two polymetallic quartz vein Minfik occurrences (1031 115 and 1031 222) occur along the interpreted western margin of the stock. Their locations shown on Figure 3 are extracted from MiMe and have not been verified.

(m) (m) 6,090,501 511,404 -42 079 43.9 671 A.B.C.

6,090,023 510,429 -52 017 8.8 461 A.B.C. 6,090,248 512,873 -60 250 13.7 948 Lucky

2004 Diamond Drilling Program

Three AQTK diamond drill holes were completed totalling 66.4 meters. The drilling contractor was Lowprofile Exploration of Houston, B.C. Hole CCO4-01 was collared to test a zone of intense quartz veining. Holes CCO4-02 and CCO4-03 were collared to test the Hendrickson and Wadsworth veins respectively. Drill hole collar data is summarized in Table 2 and the drill hde locations are plotted on Figure 4. It should be noted that due to the complex claim history in the area of hole CCO4-03, a legal survey would be required to determine the actual location of the claim boundaries shown in Figure 4.

Table 2 - Diamond Drill Hole Summary

Total

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1 I 66.4 I

I Hole# I UTM N I UTM E I Dip I Ar. I Depth I Elev. 1 Claim

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D-6

ldtaebas

Figure 3 - Regional Geology Map

Finure 4 - Diamond Drill Hole Locations

0 0.5 1 .o - kilometres

The core was placed in boxes and transported to Telkwa for logging and sampling. The author converted the footage blocks to metres and logged the core for lithology, structure, mineralization and alteration. The logs are attached as Appendix I of this report.

Twenty-four split core samples were taken and submitted to ALS Chemex in North Vancouver for 34 element ICP analysis plus a 30 gram Au fire assay with an AA finish. A complete description of the analytical techniques is presented in Appendix II and the assay certificate is attached as Appendix Ill.of this report. No standards or blanks were submitted with the samples.

The core is stored permanently at the residence of Russell Benzer at 4872 Kalum Lake Drive, Terrace, B.C.

8.0 Results

CCO4-01 encountered medium to dark grey, massive to locally weakly bedded or laminated siltstones of the Bowser Lake Group that are weakly biotite +/- andahsite(?) homfelsed. Two white quartz veins were intercepted from 16.8 to 17.3 meters and from 28.0 to 28.4 meters. A single montonite dyklet, 15mm wide, was observed at 25.0 meters. Mineralization consists of pyrite + quartz as weak fracture fillings and younger quartz +/- trace molybdenite and quartz +/- pyrite veins and veinlets. Pyrite content ranges from trace amounts to 4% locally. Alteration is restricted to narrow 'bleached" envelopes surrounding quartz +/- molybdenite veins and veinlets. From 41.3 to 41.4 meters, an alteration band with garnet, quartz, pyrite, and a trace of molybdenite was encountered. The interval from 21 .O to 24.0 meters returned 177 ppm Mo.

CC04-02 intersected coarse grained, equigranular quartz-monzonite from 2.4 to 9.6 meters and from 12.3 to 13.7 meters. From 9.6 to 12.3 meters the hole encountered brown, massive, biotite homfeled, Bowser Lake Group sediments. Mineralization consists of quartz +/- trace molybdenite +/- trace chalcopyrite in rare veinlets and as weak fracture fillings. Between 11 .O and 12.5 meters there were 0.3 meters of lost core and no sludge samples were collected. The interval from 9.0 to 11 .O meters returned 277 ppm Mo.

CCO4-03 encountered dark brown, massive, biotite homfelsed Bowser Lake Group sediments. Mineralization consists of quartz +/- trace pyrite +/- trace pyrrhotite in veinlets and as fracture fillings. The 0.7 meter interval from 6.0 to 6.7 meters was estimated to contain 7% pyrite/pyrrhotite as patches, <. 1 molybdenite as disseminations and as fracture fillings, and 0.3% chalcopyrite in veinlets with quartz. The interval graded 0.024 ppm Au, 787 ppm Cu, 306 ppm Mo; and I50 ppm W.

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9.0 Interpretation and Recommendations c

P-

The 2004 diamond drilling program failed to intersect either the Wadsworth or Hendrickson veins. In the case of CCO4-02, the Hendrickson vein may have occupied the 0.3 meters of lost core between 11.0 and 12.5 meters. Further drilling of this vein should include sludge samples. The Cu-Au-Mo-W geochemically anomalous interval from 6.0 to 6.7 meters in CCO4-03 may represent the pinched off, dowkdip extension of the Wadsworth vein.

Based on the results of limited prospecting and limited geological work to date, the Clear Creek mineral property has potential for porphyry molybdenum, high grade gold veins, and intrusive-related gold deposits. The Wadsworth vein is closely associated with a molybdenum-bearing granodiorite stock and has the characteristic Au-Ag-W-Mo-Bi-(Pb-Sb-Cu-Zn) geochemical signature of "intrusive related" gold deposits such as Pogo in Alaska'. The location of the property at the north end of Kitimat Trench, and the close association with the fault on its eastern margin, suggests that mineralized plutons and gold veins may be genetically linked with that structure. Faults and fractures related to the trench may have provided preferred solution channelways and structural traps.

The following work program is recommended: 1. The Min17.k showings on the western flank of the large magnetic anomaly

should be located and re-examined to better assess their characteristics and exploration potential.

2. The area of the trench-bounding faults and complementary northeasterly structures should be closely prospected and geologically mapped.

3. The area between the Wadsworth and Hendrickson veins should be soil sampled at 50 meter spacing on lines with 100 meter spacing.

The cost of the proposed mapping, prospecting and soil sampling is estimated to be $45,000.

No additional drilling is recommended until the prospecting, geological mapping, and soil sampling have been completed.

' Wojddc et al, 1999

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Table 3

STATEMENT OF EXPENDITURES

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I. Diamond drilling Lowptofile Exploration

2. Geochemical Analysis ALS Chemex Greyhound (courier samples to Vancouver)

3. Helicopter

4. Cypress Forest Consultants Ltd. labour (includes chainsaw, gps, and mapping) vehicles snowmobiles

5. Harold Hendrickson labour vehicle An/

6. Core logging and report

$9,387.50

$736.05 $63.72

$2.21 1.1 1

$6,049.65 1527.3O 770.00

$1,400.00 $525.00 $350.00

$963.00

TOTAL $23,983.33

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REFERENCES

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1. Bunneister, N.W. (1966): Geochemical Report on Big Joe Claim Group; B.C. Ministry of Energy and Mines, assessment report 857,3 pp.

2. Carter, N.C. (1972): Big Joe; in Geology, Exploration and Mining in British Columbia, 1971, p. 116-118.

3. Lefebure, D.V., Foumier, M.A. and Jackaman, W. (1999): Prospective Areas in British Columbia for Intrusion-related Gold-Tungsten-Bismuth Veins; 6. C. Ministry of Emgy and Mines, Open File 1999-3.

4. Wojdak, P.J., Bulmer, W. and Hanson, D.J. (1988): Geologic Setting Of The Wadsworth Vein: An Intrusive-Related Gold Discovery Near Terrace, B.C.; Exploration and Mining in British Columbia, 1999, p. 53-57

5. Woodsworth, G.J., Hill, M.L. and Van der Heyden, P. (1985): Preliminary Geologic Map of Terrace (NTS 1031 East Half) Map Area, British Columbia; Gedogical Survey of Canada, Open File 1 136.

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AUTHOR’S STATEMENT

I, Daryl J. Hanson, of 16575 Quick East Rd., Tellcwa, B.C. do hereby certify that:

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I am a graduate of the University of British Columbia (1971) and hold a B.A.Sc. degree in Geological Engineering.

1 am registered as a Professional Engineer with the Association of Professional Engineers and Geoscientists of British Columbia, Canada.

I have practiced my profession as a geologist for 32 years in British Columbia and the Yukon.

This report is based is based upon examination of the drill core from this project an8 upon two site visits to the property in 2003.

I have no financial interest, either direct or indirect, in the Clear Creek mineral property or any adjacent properties.

Dated at Telkwa, British Columbia, this 2 5 day of February, 2005.

,LLL

Daiyl J. Hanson, PTEng.

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Appendix 1 Diamond Drill Hole Logs

DIAMOND DRJLL LOG HOLE: CCO4-01

MPth (m) Description ROCK

from to CODE

0.0 0.6 Overburden (triconed- no core) O/B

0.6 16.8 SILTSTONE JBss

Company: Harold Hendrlckson

Project Clear Creek

Con bged by : Daryl J. Hanson I Start Dab. Finish Date:

STRUCT. ALT" SCALE (1-5 MAX)" MINERALIZATION ANALYSES

S1 So zS 2K 2M Sil Chl % % % % % Racov. a m p lnterval(m) Cu Mo Zn & AU I.IW *-I mq ~1 wm Py Cp Sp Po Ga Number from to ppm Ppm ppm ppm ppm

2.4 294965 0.6 3.0 44 2 73 ~ 0 . 2 ~0.005

3.0 294966 3.0 6.0 43 18 93 1.0 <0.005

I 3.0 294967 6.0 9.0 30 49 90 1.6 <0.005

GPS Northing' 6,080,501

GPS Easting' 51 1,404

GPS Elevation (m)

UTM NAD 83

1

PAGE 112

-w/ l%disseminated py and tr. moly 2.9 294980 33.0 36.0 39 26 75 <0.2 ~0 .005

-upper cnt not observed 3.0 294981 36.0 39.0 39 64 84 <0.2 4.005

-lower cnt sharp, planar Q 60 3.0 294682 39.0 42.0 45 25 91 0.4 <0.005

1.9 294983 42.0 43.9 62 21 92 0.2 <0.005

Mmuth Inclin. N o t e s

17.3 28.0 SILTSTONE JBSS

-me4 to dark grey, loc. calc., massive to loc. thinly laminated

-lot. bleached proximal to qtr+py veins

-grades locally to sandstone

-very wk biotite hornfels developed locally

I 17.3-18.0 2% py as fracture fillings I I I I I I I II I I I I I

Sheet 1 of 2

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18 0-21.0 qtz veining w/ "bleached" envelopes (t/- chl)

19 4-19 7 "spotted" as above 9 3-1 1 0 w/<l% py as fracture fillings and

2% pale pinkish beige rounded grains (garnet?)

21 0-24 0 4% py as fracture fillings, 4 % moly aswc w/ qtz vns.

21 3-21 6 pale beige, calcareous int

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1

Depth (m) Description ROCK

fnnn to CODE

17.3-28.0 mnrd

24.0-27.0 loc. dark gy andalusite spots; loc bleached envelopes;

4% pyas fracture fillings

25.0 monzonlte dyldat; 15mm

25.4 py lamination 4mm thick. parallel to SO Q 40: tr. grey sde?; tr pink

garnet? in hangingwall and footwell w/ seridte

27.0-28.0 tr. py in very wk fracture filings; very wk. qtz vns

-bxia 8 gouge w/ mlnw clay Q lower cnt.

28.0 28.4 WHITE QUARTZ VEIN QV

-w/ Mk fracture filings locally

-upper cnt broken (not observed) -lower cnt sharp, irreg; no attitude

DIAMOND DRIU LOG

S, SO 2s 2K zM Sil Chl -- - x.1 W. qutl rnprp py Cp Sp Po Ga % Number from to ppm ppm ppm ppm

I

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HOLE: CC04-02

I STRUCT. I ALT" SCALE (1-5 MAX)! MINERALIZATION I

I 1-no sdes observed I

PAGE 2t2

ANALYSES

1 1 1 1 1 1 1 1 1 1 1 1 I I I I I

41 3-41 4 gar+q+z+py+tr moly alteration band SO conformable @ 52

42 0-43 B very wk qtz+moly vns, very wk py+qtz vnslvnlts

EOH @ 43 9 METERS

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. 1

Depth (m) Bascnmon ROCK

from to CODE

0 0 2 4 OVERBURDEN (Wooned- no core) 019

2 4 9 6 QUARTZ MONZONITE EQM

Coar6e grained, equtgranular, w/7% biotite books to 4mm, very wk chl eKn

510% qtz, 10cm void @ 3 2 meters

-rare qtr vns/vntts, wk fracture fillings w/ Fe oxide

-tr disaennnatad moly

' - ~ r cnt not observed

9 3 fracture filling w/ moly+* cpy

9 6 12 3 BIOTITE HORNFELS HFb

-brown. massive. metasediment

DIAMOND DRILL LOG HOLE: CCO4-02

S, So 2' 2K 2" SII Chl % % % % 46 Recov Sample Interval(m) Cu Mo Zn AQ [ AU - w ng was* Py Cp Sp Po Ga Number from I to ppm ppm wm ppm( ppm

1 8 294984 9 0 110 57 277 132 0 2 ~ 0 0 5

2 3 294985 110 137 75 32 404 0 3 <om

__ ~ ~ ~

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-wk qtz+/- moly vns, very wk py fracture fillings

-tr cpy in fractures

11 0-1 I 3 quartzinonrontte dyke (no cnts observed)

110-125 03matcm,oflostcom

12 3 13 7 QUARTZ MONZONITE

-as above 2 4 to 9 6 m: wk &I e l n of kottte

-upper cnt not observed

-very wk qtz+py vnlts

12 8 4Ocm void

EOH Q 13 7 meters

PAGE 111

EQM

1 I i

1 Cars I O Q ~ by : Dafyi J. Henson start oats: Finirh Dak

( GPSNorthing' 6,090,2el

I GPSEasUng' I 512,8731

GPS Elevation (m) 048 EOH

UTM NAD 83

1 STRUCT. I ALT" SCALE (1-5 MAXd MlNERALlZATlON I

Azimuth Indin. Nder

ANALYSES

Appendix II ALS Chemex Analytical Techniques

Assay Procedure - ME-AA46 Evaluation of Ores and High Grade Materials by Aqua Regia

Digestion - AAS

ALSChexnex Method Code

Sample Decomposition: Aqua Regia Digestion Analytical Method: Atomic Absorption Spectroscopy (AAS)

Detection Upper Units Element Symbol Limit Limit

A prepared sample (0.4 to 2.00 grams) is digested with concentrated Ntric acid for one half hour. After cooling, hydrochloric acid is added to produce aqua regia and the mixture is then digested for an additional hour and a half. An ionization suppressant is added if moiybdenum is to be measured. The resulting solution is diluted to volume (100 or 250 ml) with demineralized water, mixed and then analyzed by atomic absorption spectrometry against matrix-matched standards.

AS-AA46 Arsenic As I 0.01 30 % Bi-AA46 Cd-AA46

Bismuth Bi 0.001 30 % cadmium Cd 0.001 10 %

CO-AA46 Cobalt cu-AA46 Copper Fe"AA46 Iron

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Ag-AA46 I silver I Ag I 1 I 1500 I ppm I

co 0.01 50 % cu 0.01 50 % Fe 0.01 30 %

&-AA& I zinc I zn I 0.01 1 30 I % I

PbAA46 Mo-AA46

Lead Pb 0.01 30 % Moiybdenwn Mo 0,001 10 %

lVxTl-AA46 I Manganese Ni-AAQG I Nickel

Mn 0.01 1 50 % Ni 0.01 50 0x3

Fire b s a v Procedure - A g - G M l F & - e m F AU-GRA21& A U - G W Precious Metals Gravimetfic Analysis Methods

upper UNtS Sample Lower Element

Method

i Code Weight Reporting Limit Reporting Limit

Sample Decomposition: Fire Assay Fusion Analptical Method: Gravimetric

A g - G W l Ag-GRA22 Au-GRA21 Au-GRA22

A prepared sample is fused with a mixture of lead oxide, sodium carbonate, borax, silica and other reagents in order to produce a Iead button. The lead button mntainhg the precious metals is cupeiled to remove the lead. The reznainjng gold and silver bead is parted in dilute nitric acid, anmaled and weighed as gold. Silver, if requested, is then determined by the difference in weights.

Silver 3Ograrns 5 l0,Ooo pprn Silver 50grams 5 l0,Ooo ppm Gold 3Ograrns 0.05 lo00 ppm Gold Sograms 0.05 loo0 ppm

I-

Tungsten" Uranium Vanadium zinc

*

w 1 . 10 l0,Ooo ppm U 10 l0,Ooo ppm v 1 10,OOO P F zn 2 10,m ppm

ALS emernex A Geochemical Procedure - ME-ICP41

Trace h v e l Methods Using Conventional ICP-AES Analysis (cm'f)

A Geochemical Procedure - ME-ICP41

Trace Level Methods Using Conventional KP-AES Analysis

r Sample Decomposition: Nitric Aqua Regia Digestion AnalyticalMethod: Indudively Coupled Plasma - Atomic Emission Spech.oscopy (ICP - AES)

A prepared sample (0.50 grams) is digested with aqua regia for at least one hour in. a graphite heating block. After cooling, the resulting solution is diluted to 125 ml with demineralized water, mixed and analyzed by inductively coupled plasma- atomic emission spectrometry. The analytical results are corrected for inter-elernent spectral interkrences.

Upper Units Detection Element Symbol Limit Limit

MercUry Hg 1 I l0,Ooo ppm Molybden urn M o 1 l0,OOO ppm

Fire Assav Procedure - Au-AA23 and Au-AA24 Fire Assay Fusion, AAS Finish

ALs mema Method Code

Au-AA23 AU-AA.24

Sample Decomposition: Fire Assay Fusion M y t i c a l Method: Atomic Abs~rption Spectroscopy (AAS)

upper Lower

Limit Limi€ Reporting Reporting Units Sample

Weight Element

Gold Au 3og 0.005 10.0 Guld AU 5og 0,005 I 10.0 ppm 1

A prepared sample is fused with a mixture of lead oxide, sodium carbonate, borax, silica and other reagents as nixpired, inquarted with 6 mg of gold-free silver and that cupelled to yield a precious metal bead.

The bead is digested in 0.5 ml dilute nit& acid in the microwave oven, 0.5 ml concentrated hydrochloric acid is then added and the bead is further digested in the microwave at a lower power setting. The digested solution is cooled, diluted to a totai volume of 4 ml with de-mineratiaed water, and analyzed by atomic absorption spectroscopy against rnatrix-matcki standards.

ALS ehernex

CRU-31

SPL-21

PUL-31

Sample Preparation Packaqg - PREP-31 Standard Sample Preparation: Dry, Crush, Split and Pulverize

Fine crushing of rock chip and drill samples to better than 70% of the sample passing 2 mm. Split sample using M e splitter. A sample split of up to 250 g is pulverized to better than 85% of the sample passing 75 microns.

Sample is dried and the entire sample is crushed to better than 70% passing a 2 mm (Tyler 10 mesh) screen A split of up to 250 grams is taken and pulverized to better than 85% passing a 75 micron (Tyler 200 mesh) screen.

Description

Sample is logged in tracking system and a bar code label is attached.

ALS Chamex

SampkPreparation Package - PREP41 Dry sample and dry-sieve to -180 micron

A

Sample is dried and then dry-sieved using a 180 micron (Tyler 80 mesh) screen The plus fraction is retained unless disposal is requested. This methd is appropriate for soil or sediment samples up to m e kilogram in weight.

ALS Chemex Method Code Description

I Sample is logged in tracking system and a bar code label is I LOG22 - - I

attached. Sample is dry-sieved to -180 micron and both the PIUS and minus fractions are retained. SCR-41

s

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Appendix 111 ALS Chemex Assay Certificate

1

To: CYPRESS FOREST CONSULTANTS LTD. 51 13 KEITH AVE TERRACE BC V8G 1K8

C E RTI F I CATE VA04085 1 44

5 A

~

ALS CODE DESCRIPTION

WEI-21 Received Sample Weight LOG-22 CRU-31 SPL-21 PUL-31

Sample login - Rcd wlo BarCode Fine crushing - 70% c2mm Split sample - riffle splitter Pulverize split to 85% ~ 7 5 um

ALS Chernex

- ALS CODE DESCRIPTION INSTRUMENT - ME-ICP41 34 Element Aqua Regia ICP-AES I C P-AES AU-AA23 Au 30g FA-AA finish AAS

EXCELLENCE IN ANALYTICAL CHEMISTRY ALS Canada Ltd. 212 Brwksbank Avenue North Vancouver BC V7J 2C1 Canada Phone: 604 984 0221 Fax: 604 984 0218

Page: 1 Finalized Date: 13-DEC-2004

This copy reported on 14-DEC-2004

Account: CYPFOR

Project: P.O. No.: This report is for 27 Rock samples submitted to our lab in Vancouver, BC, Canada on

The following have access to data associated with this certificate: 2-DEC-2004.

RUSSELL BENZER

To: CYPRESS FOREST CONSULTANTS LTD. ATTN: RUSSELL BENZER 51 13 KEITH AVE TERRACE BC V8G lK8

I ANALYTICAL PROCEDURES

9 This is the Final Report and supersedes any preliminary report with this certificate number. Results apply to samples as Signature: , LFjz&&y7 submitted. All pages of this report have been checked and approved for release. /

1

Method Anmlyte

Sample Description

P-294965 P-294966 P-294967 P-294968

P-294969 P-294970 P-294971 P-294972 P-294973

P-294974 P-294975 P-294976 P-294977 P-294978

P-294979 P-294980 P-294981 P-294982 P-294983

P -294984 P-294985 P-294966 P-294987 P-294988

P-294989

ALS Chemex EXCELLENCE IN ANALYTICAL CHEMISTRY ALS Canada Ltd.

212 Brooksbank Avenue North Vancouver BC V7J 2C1 Canada Phone: 604 984 0221 Fax: 604 984 0218

To: CYPRESS FOREST CONSULTANTS LTD. 51 13 KEITH AVE TERRACE BC V8G 1K8

Page: 2 - A Total # Pages: 2 (A - C)

Finalized Date; 13-DEC-2004 Account: CYPFOR

I CERTIFICATE OF ANALYSIS VA04085144 I WEI-21 Au-AA23 ME-ICP41 ME-ICP41 ME-ICP41 ME-ICP41 ME-ICP41 ME-ICP41 ME-ICP41 ME-ICP41 ME-ICP41 MEJCP41 MGICP41 ME-ICP41 MblCP41

Be Bl Ca Cd co Cr cu Fo PPm ppm ppm ppm ppm % PPm ppm ppm m m K

RecvdWt. Au Ae A1 AS B Ba kg ppm PPm %

0.2 0.01 2 10 I 0 0.5 2 0.01 0.5 I 1 1 0.01 0.02 0.005

0.20 C0.005 0.2 0.41 C 2 <I0 100 0.5 c2 0.50 c0.5 3 71 5 1.39 2.14 C0.005 <0.2 2.78 5 <I0 70 c0.5 c2 3.03 c0.5 20 106 44 4.57 2.76 C0.005 1 .o 1.74 4 <I0 70 C0.5 5 1.18 0.8 12 22 43 4.14 2.76 ~0.005 1.6 2.09 5 <I0 150 C0.5 7 1.96 c0.5 16 23 30 3.99 2.64 <00.005 co.2 2.51 <2 <I0 110 C0.5 c2 0.68 c0.5 14 26 45 4.66

2.18 C0.005 c0.2 2.45 2 <I0 100 C0.5 c2 0.57 c0.5 17 25 47 4.71 1.76 <0.005 0.2 2.16 2 <I0 80 1 .o c2 3.07 c0.5 17 27 27 3.18 0.46 0.007 0.3 0.30 C2 <I0 30 0.5 c2 1.70 c0.5 1 37 20 0.56 0.66 <0.005 0.2 1.73 c2 <I0 70 0.5 c2 1.42 c0.5 14 24 32 3.74 2.76 c0.005 c0.2 2.01 7 <I0 60 C0.5 c2 2.37 c0.5 14 27 30 4.09

2.98 C0.005 c0.2 2.12 4 < I0 110 c0.5 c2 2.92 c0.5 16 22 33 4.07

0.78 C0.005 c0.2 0.62 7 4 0 60 4 5 c2 1.63 ~0.5 11 13 35 4.87 0.40 c0.005 c0.2 0.36 6 <I0 30 C0.5 c2 2.86 c0.5 6 39 22 2.24 1.50 c0.005 c0.2 0.77 10 <I0 60 C0.5 c2 I .24 c0.5 17 16 37 4.68

2.78 c0.005 c0.2 1.48 9 4 0 ~ 100 C0.5 c2 1.19 c0.5 20 24 61 4.99

3.14 C0.005 c0.2 1.28 8 <I0 80 C0.5 c2 1.12 <0.5 13 24 35 4.32 2.82 C0.005 c0.2 1.98 c2 <I0 190 C0.5 c2 0.91 ~0.5 10 28 39 3.26 3.06 <0.005 c0.2 2.28 2 <I0 I10 <0.5 2 0.63 c0.5 14 29 39 4.14 3.14 <0.005 0.4 2.59 c2 <I0 180 0.6 3 1.01 <0.5 15 35 45 4.03 2.10 c0.005 0.2 2.05 c2 <I0 140 0.6 2 1.20 c0.5 13 32 52 3.51

1.64 C0.005 0.2 1.94 15 4 0 170 c0.5 4 0.56 3.1 14 34 57 3.75 2.14 c0.005 0.3 1.26 4 <I0 170 C0.5 3 0.47 10.5 7 31 75 2.66

2.06 0.006 0.2 2.40 6 <I0 190 0.5 C2 1.55 c0.5 12 40 71 3.34

1.44 <0.005 c0.2 2.59 3 <I0 160 0.5 c2 2.03 c0.5 12 38 65 3.22

0.78 0.024 1.6 2.44 60 <I0 70 I .6 2 3.35 c0.5 36 41 787 9.65

0.38 c0.005 0.7 0.19 3 <I0 10 C0.5 c2 0.10 c0.5 2 137 239 0.63

0.16 0,009 0.8 1.47 17 4 0 60 I .2 5 3.19 0.6 12 26 118 2.77

A Method Analyh Unlb

)ampie Description LOR ~

P-294964 P-294965 P-294968 P-294967 P-294968

P-294969 P-294970 P-294971 P-294972 P-294973

P-294974 P-294975 P-294976 P-294977 P-294978

P-294979 P-294980 P-294981 P-294982 P-294983

P -294984 P-294985 P-294986 P-294987 P -294988

P-294989 P-294990

ALS Chemex EXCELLENCE IN ANALYTICAL CHEMISTRY ALS Canada Lld.

212 Bmksbank Avenue North Vancouver BC V7J 2Cl Canada Phone: 604 984 0221 Fax: 604 984 0218

To: CYPRESS FOREST CONSULTANTS LTD. Page: 2 - B Total # Pages: 2 (A. C)

Finalized Date: 13-DEC-2004 Account: CYPFOR

51 13 KEITH AVE TERRACE BC V8G 1K8

I CERTIFICATE OF ANALYSIS VA04085144

ME-ICP41 ME4CP41 ME-ICP41 ME-ICP41 ME-ICP41 ME4CP41 ME-ICP41 ME-ICP41 ME-ICP41 , ME-ICP41 ME-ICP41 ME-ICP41 ME-lCP41 ME-ICP41 Me-ICp41

Na NI P Pb S Sb sc Sr Ga Ha K La Ma Mn Ma

10 I 0.01 DDm x DPm DDm DDm x DDm DDm DDD) DDm DDm % DDm x DDm

10 0.01 5 I 0.01 1 I 0 2 0.01 2 I 1

<10 < I 0.22 20 0.08 375 5 0.03 3 820 18 0.12 <2 1 39

10 < I 0.16 10 0.93 681 49 0.05 17 470 28 0.19 <2 5 112

10 < I 0.14 10 2.23 723 2 0.04 52 750 7 0.17 <2 8 183 4 0 < I 0.17 10 0.97 696 18 0.04 12 560 18 0.21 <2 6 87

10 < l 0.19 10 1.04 610 3 0.05 11 450 4 0.03 <2 9 88

10 <1 0.16 10 1 .oo 578 3 0.05 15 480 4 0.20 <2 7 50 10 < I 0.09 10 0.89 1005 8 0.03 19 930 7 0.21 <2 6 144

<lo < I 0.08 10 0.08 255 17 0.06 2 50 19 0.14 <2 1 100 <lo < I 0.15 10 0.79 873 15 0.04 14 600 9 0.21 <2 4 67 10 < I 0.15 10 0.83 749 4 0.04 14 540 5 0.04 <2 5 90

10 1 0.14 10 0.85 966 177 0.04 14 660 5 0.05 <2 7 132 <I0 <1 0.20 10 0.99 759 5 0.04 19 890 5 0.18 <2 8 113 <I0 <1 0.16 <lo 1.02 714 2 0.04 11 370 8 0.04 <2 8 189 <lo < I 0.09 <I0 0.57 498 26 0.05 8 110 10 0.13 <2 3 147 <lo 1 0.15 <I0 0.90 715 $0 0.04 16 380 6 0.17 <2 6 127

4 0 <1 0.20 10 0.88 687 4 0.04 15 460 8 0.04 <2 7 111 10 <1 0.38 10 0.80 527 26 0.09 12 570 5 0.08 <2 6 86 10 <1 0.22 10 0.98 490 64 0.05 I 6 420 4 0.13 <2 7 53 10 <I 0.24 10 0.92 686 25 0.10 15 710 6 0.27 <2 8 80 10 1 0.18 10 0.83 666 21 0.06 13 700 3 0.18 <2 6 62

10 < I 0.55 10 0.91 466 277 0.06 13 690 6 0.56 <2 5 38 10 < I 0.27 10 0.62 427 32 0.05 5 690 36 0.28 <2 3 29

10 <1 0.60 I 0 1.44 371 70 0.19 20 720 3 0.58 <2 6 228 10 < I 0.26 10 0.99 398 306 0.11 25 1010 4 4.33 <2 5 188 10 < l 0.71 10 1.48 403 86 0.14 23 700 4 0.60 <2 7 170

0.05 110 6 0.01 7 30 3 0.08 <2 < l 6 <lo 0.93 730 21 0.03 23 950 8 1.30 6 7 136

4 0 <I 0.02 <I0 <1 0.40 10

1 1 1 I ? 1 1 - ? 7 \

ALS Chemex EXCELLENCE IN ANALYTICAL CHEMISTRY ALS Canada Ltd.

212 Brooksbank Avenue

Page: 2 - C Total # Pages: 2 (A - C)

FinallzQd Date; 13-PEG-2004

To: CYPRESS FOREST CONSULTANTS LTD. 51 13 KEITH AVE TERRACE BC V8G 1 K8

Account: CYPFOR

North Vancouver BC V7J 2Cl Canada (A s, Phone: 604 984 0221 Fax: 604 984 0218

Mothod Analyto Unlts

Sample Description LOR

P-294964 P-294965 P-294966 P-294967 P-294968

P-294969 P-294970 P-294971 P-294972 P-294973

P-294974 P-294975 P-294976 P-294977 P-294978

P-294979 P-294980 P-294981 P-294982 P-294983

P-294984 P-294985 P-294986 P-294987 P-294988

P-294989 P-294990

CERTIFICATE OF ANALYSIS VA04085144

ME-ICP41 ME-ICP41 ME-ICP41 ME-ICP41 ME-ICP41 MCICP41 TI TI U V W Zn x ppm DPm Ppm ppm cpm

0.01 10 10 1 10 2

co.01 4 0 4 0 7 4 0 44 0.01 <I0 <I0 86 4 0 73 0.01 <I0 4 0 53 <I0 93 0.02 <I0 4 0 62 <I0 90 0.04 <I0 <I0 76 <I0 93

4 0 <I0 74 <I0 88 0.02 4 0 <I0 64 <I0 82 0.06

<0.01 4 0 20 3 <I0 9 <I0 53 10 84

0.01 c10 62 <I0 88 0.01

<I0 <I0

0.02 <I0 4 0 68 <I0 104 <I0 69 4 0 100 0.02

co.01 <I0 10 16 <I0 35 co.01 <I0 <I0 50 4 0 89

0.01 4 0 4 0 55 <I0 93 0.08 4 0 4 0 62 <I0 75 0.08 <I0 <I0 81 4 0 84 0.09 -40 4 0 91 <I0 91 0 08 <I0 <I0 71 <I0 92

<0.01 <I0 <I0 <I0 40 <I0 90

0.11 <I0 4 0 77 <I0 132 0.08 <I0 4 0 49 4 0 404 0.13 -40 4 0 85 30 55 0.16 4 0 <I0 77 150 50 0.14 -40 4 0 105 10 64

0.01 <I0 4 0 4 -40 10 0.01 4 0 <I0 50 <I0 65