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ASSESSMENT REPORT

DEC 1*2009-Gold Commissioner's Office

VANCOUVER, B.C.

:K SAMPLING AND PROSPECTING

ON THE

GREENHORN PROPERTY

TENURE 551876 514980

NTS 82K/031 Slocan mining division 50 21'N LATITUDE

117 52'W LONGITUDE

OWNERS

BRUCE DOYLE NELSON B.C.

GRANT DOYLE NAKUSP B.C.

Author

Bruce Doyle Prospector

December 10, 2009

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Text Box

BC Geological Survey Assessment Report 31243

Table of contents

1.0 Summary 1

2.0 Introduction 2

2.1 Property Description and Location

2.2 Accessibility, Climate, Infrastructure and Physiography

2.3 Property History 2

2.4 2009 Work Program

3.0 Geological Setting 5

3.1 Regional Geology

3.2 Property Geology

4.0 Mineralization 7

4.1 Dunn Road Showing

4.2 Dunn South Showing

5.0 Results 7

6.0 Conclusions & Recommendations 7

7.0 Disbursements 8

8.0 Statement of Qualifications 9

9.0 References 10

List of Tables

Table 1 Greenhorn Property Mineral claim 2

List of Figures

Figure 1 Property Location Map 3

Figure 2 Claim Location Map 4

Figure 3 Regional Geology Map 6

Figure 4 Sample Location Map 8

Figure 5 Prospecting Location Map 13 Appendices

Appendix 1 Analytical Method 11

Appendix 2 Rock Sample Descriptions 12

Appendix 3 Geochemical Analysis 14

1.0 Summary

The Greenhorn copper property is located twelve kilometers north of Nakusp B.C. on the east side of the Arrow Lakes. The property is accessed from highway 23 north of Nakusp and several logging roads in Dunn, Turner creek areas. Prospecting and rock sampling took place by Grant and Bruce Doyle between August 3 and August 16, 2009.

The Greenhorn property lies immediately west of the Kuskanax Batholith within a northwest-trending belt of metamorphic meta volcanic and amphibolite rocks overlain to the west by siltstone, limestone. Mineralized areas consists of chalcopyrite, magnetite, pyrrhotite in a epidote-amphibole-biotie foliated metamorphic mafic volcanic rock. Mineralization along the volcanic, sediment contact consist of quartz,-sericite-pyrrhotite horizon with porphyroblasts of garnet or shene with traces of chalcopyrite. This horizone is thought to be exhalative. Assays have returned over 5% copper from Dunn creek and up to 3.14% copper from Dunn road while the Dunn south showing has returned up to .8% copper.

The 2009 prospecting program was initiated to discover new mineralized zones between the Dunn road showing and the Dunn south showing. Most of the showings so far have been exposed in road cuts or deep creek draws such as the on Dunn creek. Weathering of exposed outcrops have removed most signs of copper mineralization. Soil geochemical anomalies will need to trenched and blasted to expose new sulfide showings. No new sulfide showings were discovered in the 2009 program but several samples were collected from previously know copper occurrences.

2.0 Introduction

This report describes the results and conclusions from work carried out on the Greenhorn copper property during the 2009 field program. The purpose of the work was to rediscover old workings or discover new copper showings between the Dunn road showing on the north end of the property and the Dunn south showing near Turner creek.

2.1 Location and Access

The Greenhorn property is located along the east shore of the upper Arrow Lakes about 12 kilometers from the town of Nakusp B.C. on map sheet 082k/31 in the Slocan mining division.

Access to the property is via highway 23 north to the Dunn creek forestry road which provides access to the north end of the property and the Turner creek forestry road which gives access the southern portion of the property. Both roads can be traversed with 2 wheel drive vehicles during the early spring to late fall field seasons.

Table 1

GREENHORN PROPERTY MINERAL CLAIMS Claim Name Tenure No Area (Ha) Expiry Date Map Number Green horn south

514622 268.20 July 16 2010 082k/31

Horn 551876 247.46 August 25 2011 082k/31 514980 247.54 July 4 2010 082k/31

2.2 Physiography and Vegetation

The mineral claims are located on the west facing slopes of mount Abriel on the west side of the Selkirk mountains. Elevations on the property range from 441m to 1420 meters. The property is cut by a deep creek draw at Dunn Creek.

The property lies within the interior rain belt and vegetation consists of mature hemlock, cedar, white pine, balsam spruce and moss covering the ground. Devils club can be found the creek draws.

2.3 History

There is very little documented work done in the area of the Greenhorn property. The first reports of exploration are written in the 1902 report of the Ministry of Mines which states on the Ophir Group, situated at Cape Horn, on the east side of the Upper Arrow lake Messrs, Maxwell and Glendinning have built a cabin and intend to work on the property all winter. The width of the vein is 40 feet and assays run 16% copper and $2 gold per ton. In the 1904 ministry mines report a large low grade showing of copper assaying 8% copper and $2 gold per ton on the Cornwall Group.

In 1967 the Copper Horn Mining company staked 83 two post claims and performed trenching, rock

LOCATION MAP

GREENHORN PROPERTY

O l T W M GEOLOGICAL. CONSULTANTS LIMITED

1

Greenhorn Property Claim Location Map

A-4-4-̂ 1

This map is a user generated static output from an Internet mapping site and is for general reference only. Data layers that appear on this map may or may not be accurate, current, otherwise reliable. THIS MAP IS NOT TO BE USED FOR NAVIGATION.

'vF!X^C*1

Legend □ Indian Reserves □ National Parks r-1 Conservancy Areas

□ Parks MTO Grid (MTO)

Blocked by MEM Other Mineral Tenure (current)

r~1 Mineral Claim n Mineral Lease

Mineral Reserves (current)

r—I Placer Claim Designation —, Placer Lease Designation —j No Staking Reserve f—] Conditional Reserve —| Release Required Reserve I—| Surface Restriction I—| Recreation Area □ Others r—. Survey Parcels

□ BCGS Grid Contours (1:250K)

Contour • Index Contour ■ Intermediate Areaof Exclusion Areaof Indefinite Contours Transportation - Points (TRIM)

, Helipad

Transportation - Lines (TRIM)

Airfield Airport Airstrip

# Scale: 1:50,000

floors 2.

sampling and geophysical surveys in the Dunn and Cape Horn Creek areas. None of this information is available. In 1967 Cold Lake resources explored fro uranium on there RBI claim and carried out prospecting, mapping, soil sampling, scintillometer and magnetometer surveys. Soil sampling outlined up to 405ppm copper in the western portion of there claims.

In 1990 Art Pigott and Lawrence Hascarl located copper mineralization on the Dunn Creek forestry while building logging roads for Pope & Talbot. Samples of copper mineralized rock assayed up to 3.14% copper and 18. lOppm silver. A small soil grid was established near the present day Dunn road showing. The soil geochem outlined a strong copper anomaly open to the north and south but no follow up work was ever carried out.

In 1997 Bruce and Grant Doyle Staked several claims covering the Dunn Creek area and in the spring optioned the property to Phelps Dodge copper company. In the summer and fall soil geochemistry,. mapping, geophysical surveys and limited drilling was carried out.

In 1999 BGM Diversified Energy of Vancouver B.C Optioned the Green horn property and hired Crest Geological Consultants to map, prospect, and sample the Greenhorn property. Reinterpretation of the I.P and Mag-VLF data was completed by S J V Geophysics. Four targets were outlined for drilling several with massive sulfide signatures.

In 2005 Zappa Resources optioned the Greenhorn property and carried out trenching north of the present day property exposing copper mineralization.. The property was held till 2007 then returned to the Doyles.

2.4 2009 Work Program

From August 03 2009 to August 16 2009 prospecting and rock sampling were carried out on tenures 551876 and 514980 with emphasis on discovering new copper showings.

3.0 Geological Setting

3.1 Regional Geology

The Upper Arrow Lake area lies within the Omineca structural belt of the Canadian Cordillera. Mapping by Read and Wheeler, 1976 shows Paleozoic and Mesozoic metamorphosed sedimentary and volcanic rocks intruded by the Kuskanax Batholith and associated sills and dykes. The oldest rocks are exposed at the northern and southern ends of Upper Arrow Lake and consist upper Mississippian (Milford Group) oceanic sediments and minor basalt. Paleozoic to Mesozoic aged rocks consisting of the Kaslo Groups rims much of the Kuskanax Batholith. The Kaslo Group consists of met volcanic rocks (amphibolite) with minor interbedded pelitic and marble units and capped by a thick sequence of met volcanic rocks. The Kaslo and Slocan Groups underlie the property on the western side of the Kuskanax Batholith.

Stratified rocks west of the Kuskanax Batholith are complexly folded and faulted along a predominatly northwesterly trend Intensity of deformation increases westward away from the batholith and toward a series of gneissic domes located west of the north end of Upper Arrow Lake. On the west side of the lake, stratified rocks are in fault contact with Monashee Complex rocks.

The nearest significant metal occurrence is the Big Ledge Zn-Pb deposit located some 15km to the northwest on Standfast Creek. The Big Ledge deposit is hosted in an east-west trending succession of rusty weathering schist and gneiss, calcareous quartzite, cal silicate, marble and locally amphibolite. The mineralized horizon is in the core of a tight, overturned antiform to the north. Mineralization consists of sphalerite, pyrite, pyrrhotite, marcasite and minor chalcopyrite occurring over a distance of some 10 kilometers.Indicated ore reserves for the Big Ledge are 6,5 million tonnes grading 6% combined lead and

ROCKY MOUNTAIN

THRUST AND

FOLD BELT

Sco/e in Kilometres 7 7.9

LEGEND MESOZOIC/PALEOZOIC Intrusive Rocks

PALEOZOIC/MESOZOIC Lordeou Gp. and Bodsnot Em. PALEOZOIC/MESOZOIC Kaslo Gp. and S/ocan Gp.

LOWER CAMBRIAN HomUl and GOG Groups

HADRYNIAN Horsethiel Creek Group

PRECAMBRIAN/PALEOZOIC MetomorplHc Rocks

PRECAMBRIAN/PALEOZOIC Mantling Gneiss

APHEBIAN(?) Core Gneiss

A Cu-Zn Occurrence

wk Zn-Pb Occurrence

082L070X Uinfile Listing(Base Metal)

Geology oiler Gibson and Hoy. 1985

GREENHORN PROPERTY

REGIONAL GEOLOGY

Figure J O0"»»<£ GEOLOGICAL. OOMSUL.TAMTS LIMITED

zinc.

3.2 Property Geology

The Greenhorn property lies on the east side of Upper Arrow Lake just west of the Kuskanax Batholith. The eastern portion of the claims is underlain by moderately east dipping met volcanic rocks and amphibolite believed part of the Permian to Triassic aged Kaslo Group and the western part by Triassic aged met sedimentary rocks believed part of the Slocan Group. It is also possible that these rocks belong to similar aged rocks of the Lardeau Group. The eastern portion of the is underlain by metavolcanics which include Meta-basalt, Meta-andesite, Meta- tuffaceous grit unit, Meta-basaltic tuff and Meta-lapilli tuff unit.

The met sedimentary rock is exposed throughout the western part of the claims and consists of calcareous graphitic siltstone and argillite and outcrops of marble.

4.0 Mineralization

4.1 Dunn Road Showing

The Dunn Road showing is situated at 0437727mE 5579219mN and consists of chalcopyrite, pyrite, pyrrhotite, magnetite in a Epidote-amphibole-biotite metamorphic rock.

4.2 Dunn South Showing

The Dunn South showing is located at 0438117mE 5575445 mN along a new logging road. Mineralization consists of chalcopyrite, pyrite and magnetite in a foliated sheared Meta-basaltic lapilli tuff.

5.0 Results

There were no new copper outcrops discovered during the limited sampling and prospecting program at the Greenhorn property. Several grab samples were collected from a small road cut on the Dunn road logging road returning 6858ppm, 7218ppm copper and 3.9pp 3.2ppm silver. To the south of Dunn creek a .8m chip was taken in the ditch of a logging road returning 6148ppm copper and 3.2ppm silver.

6.0 Conclusions and Recommendations

The Greenhorn property hosts many copper showings mainly in new road cuts. Previous soil geochemistry outlined liner copper anomaly stretching over 2 kilometer in length. It is doubtful that further prospecting along undisturbed ground will produce any further targets. The previous copper soil anomalies should be trenched and the bedrock blasted to expose fresh rock. Sampling should include channel samples where coppper mineralization is uncovered. Drilling should be conducted on previously outlined geochemical, geophysical anomalies. It is believed the Greenhorn property could host a economic copper deposit possibly a metamorphosed VMS.

7.0 Disbursements

Disbursements August 3,4, 16 Bruce Doyle 3 Days @ $325.00 per day Grant Doyle 1 Day @ $325.00 per day

$975.00 $325.00

4 days 4x4 rental @ $75.00 per day $300.00

Truck fuel $74.50

Assays $25.50

Report Writing and Drafting $975.00

Shipping $24.00

Total $2699.00

8.0 Statement of Qualifications

L Brace Doyle of Nelson, British Columbia hereby certify that:

I am a professional prospector and have been involved with mineral exploration since 1982.

I have successfully completed the advanced prospecting coarse at Mecashi Lake on Vancouver Island in 1990.

I have been employed by Junior and Senior mining companies in British Columbia.

I have been self employed as a professional prospector since 1990.

Respectfully Submitted,

Bruce Doyle Nelson, B.C. 10 December, 2009

9.0 References

EMPRAR 1903-page 150

Ferguson, Delbert W ;(1991) Geochemical Report on the Cape Horn Copper prospect. BC Ministry of Energy and Mines Assessment Report # 21289, 32 pages.

Jagodits, Francis L, (1998) Report on Ground Magnetics, VLF-EM & Induced Polarization /Resistivity Surveys on the GreenHorn property. BC Ministry of Energy and Mines Assessment Report #25447, 28 pages.

Leitch, Craig H.A. (1997) Unpublished Petroraphic Report 2 pages.

McLeod, Jawes W. (1979) Geophysical and Geocemical Survey RB#1 Claim. BC Ministry of Energy Assessment Report #07789, 32 pages

Payne, Craig W. (2000) Geophsical and Geological Report on the Greenhorn Property., BC Ministry of Energy Assessment Report #26162,74 pages

Appendix 1

Analytical Procedures:

Rock smpales were dried and crushed to -10 mesh using jaw and roll crushers. A 250 gram sub sample was pulverized to approximately -140 mesh with a ring pulverizer.

Multi-Element ICP

Sample splits of 0.5 grms are leached in hot 95c Aque Regia solution. The samples are analyzed on a Jarrell ash ICP unit.

Appendix 2

Rock Sample Locations and Discriptions

All sample locations on the Greenhorn property were recorded using a Garman 60csx GPS for accuracy. Sample locations were marked with blue or orange flagging tape with the sample number written on the flagging tape with perminate felt pen.

Sample 626345 was a grab sample from road cut material that was excavated back in 1990 located at 0437727mE 5579219mN. This sample is best described as a foliated mafic volcanic rock containing 15-20% actinolite 25% epidote, 12% biotite with chalcopyrite cutting across the fabric as well as parallel to the fabric. This sample returned 7218ppm Cu and 3.9ppm Ag

Sample 626346 was a .8m chip from the ditch of a new logging road. The location of the showing is 04381117mE 5575445mN. This sample is described as a sheared, foliated met basaltic- lapilli tuff. Mineralization was 10% disseminated chalcopyrite 3% magnetite and 20% pyrite.

Sample 626346 was taken at 0437727mE 5579219 the same location as sample number 626345. This sample contained 20% pyrite and 10% chalcopyrite in a schistose mafic volcanic.This sample was also a grab from old road road cut material.

r

Appendix 3

Geochemical Analysis

AcmeLabs 1020 Cordova St. East Vancouver BC V6A 4A3 Canada Phone (604) 253-3158 Fax (604) 253-1716

CERTIFICATE OF ANALYSIS

Acme Analytical Laboratories (Vancouver) Ltd.

www.acmelab.com

Client: Doyle, Bruce 1424 Crease Ave Nelson BC V1L 1A2 Canada

Submitted By: Bruce Doyle

Receiving Lab: Canada-Vancouver

Received: September 30, 2009

Report Date: October 22, 2009

Page: i o f 2

VAN09004569.1 CLIENT JOB INFORMATION

Project: None Given

Shipment ID:

P.O. Number Number of Samples: 20

SAMPLE DISPOSAL

SAMPLE PREPARATION AND ANALYTICAL PROCEDURES

Method Code R200-250 1D Group 1T 1F06

Number of Samples

19 4 10 5

Code Description

Crush, split and pulverize 250 g rock to 200 mesh 1:1:1 Aqua Regia digestion ICP-ES analysis 4 Acid digestion Ultratrace ICP-MS analysis

1:1:1 Aqua Regia digestion Ultratrace ICP-MS analysis

Test Report Lab Wgt(g) Status

VAN 0.5 Completed VAN 0.25 Completed VAN 30 Completed VAN

DISP-PLP Dispose of Pulp After 90 days

DISP-RJT Dispose of Reject After 90 days ADDITIONAL COMMENTS

Acme does not accept responsibility for samples left at the laboratory after 90 days without prior written instructions for sample storage or return.

Invoice To:

CC:

Doyle, Bruce 1424 Crease Ave Nelson BCV1L1A2 Canada

This report supersedes all previous preliminary and final reports with this file number dated prior to the date on this certificate. Signature indicates final approval; preliminary reports are unsigned and should be used for reference only. All results are considered the confidential property of the client. Acme assumes the liabilities for actual cost of analysis only. "*" asterisk indicates that an analytical result could not be provided due to unusually high levels of interference from other elements.

http://www.acmelab.com

1 1 } ] 1




Client:

Project:

Report Date:

Doyle, Bruce 1424 Crease Ave Nelson BC V1L 1A2 Canada

None Given October 22, 2009

www.acmelab.com Page: 2 of 2 Part 1

VAN09004569.1 Method Analyte

Unit MDL

WGHT 1D Wgt Mo

kg ppm 0.01 1

1D Cu

ppm 1

1D Pb

ppm 3

1D Zn

1

1D Ag

0.3

1D Ni

ppm 1

ID Co

ppm 1

1D Mn

ppm 2

1D Fe %

0.01

1D As

ppm 2

1D U

ppm 8

1D Au

ppm 2

1D Th

ppm 2

1D Sr

ppm 1

1D Cd

ppm 0.5

1D Sb

ppm 3

1D Bi

ppm 3

1D V

ppm 1

1D Ca %

0.01 626332 Rock 1.39 N.A.

L.N.R. L.N.R. 1.20 N.A. 0^98 N A 1.04 N A 0.81 4 1.11 N.A. 1.62 N A

N.A. L.N.R.

N.A. N.A. N A 169

N.A. N.A. N.A. N A N A N.A. N.A.

7218 6148 6858 N.A. N.A. N A N.A.

N.A. L.N.R.

N.A. N.A. N A

18 N A NA. N A NA. N.A. N A N.A.

<3 <3 <3

N.A. NA. NA. N A

N A L.N.R.

N A N A N A

48 N A NA. N A NA. NA. N A N A

69 81 45

NA. N.A. N A N A

N A L.N.R.

N.A. N A NA. <0.3 N A NA. N.A. NA. NA. N A N.A. 4.5 3.2 3.9

N A N.A. N A N.A.

N.A. L.N.R.

N.A. N A NA.

11 NA. N A N A N A N A

N A L.N.R.

N A L.N.R.

N A LN~R.

N A N A N A 2.51 N A N A N A N A N A N A N A 3.58 4.10 2.71 N A N A N A N A

N.A. LH.R.

N A N.A. N.A.

<2 N.A. N.A. N.A. N.A. N A N A N A

<2 <2 <2

N A N A N A N A

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N A N A N A

<8 N A N A N A N A N A N A N A

<8 <8 <8

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<2 <2 <2

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N A N A

~200 N A N A N A N A N A N A N A

27 28 26

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N A N A N A <0.5 N A N A N A N A N A N A N A <0.5 0.8

<0.5 N A N A N A N A

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<3 N A N A N A N A N A NA. NA.

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NA. N A N A N A

N A N.A. NA. 626333 626334

Rock Rock Rock Rock Rock Rock

1.39 N.A. L.N.R. L.N.R.

1.20 N.A. 0^98 N A 1.04 N A 0.81 4 1.11 N.A. 1.62 N A

N.A. L.N.R.

N.A. N.A. N A 169


7218 6148 6858 N.A. N.A. N A N.A.

N.A. L.N.R.

N.A. N.A. N A


<3 <3 <3

N.A. NA. NA. N A

N A L.N.R.

N A N A N A


69 81 45

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<2 <2 <2

N A N A N A N A

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<8 <8 <8

N A N A N A N.A.

N.A. L.N.R.

N A N A N A


<2 <2 <2

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<2

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N A L.N.R. __NA.__

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27 28 26

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NA. N A N A N A

L.N.R. NA. NA. NA.

<3 N.A.

L.N.R. N.A. N.A. N.A.

80 N A

L.N.R. N.A. N A N.A. 0.97 N A

626333 626334


1.39 N.A. L.N.R. L.N.R.

1.20 N.A. 0^98 N A 1.04 N A 0.81 4 1.11 N.A. 1.62 N A

N.A. L.N.R.

N.A. N.A. N A 169


7218 6148 6858 N.A. N.A. N A N.A.

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N.A. NA. NA. N A

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69 81 45

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N.A. N A NA.


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18 N A N.A. N.A. N.A. N.A.

N A N A N A 382 N A N A N A N.A. N A N A N A 361 444 347 N A N.A. N A

N A LN~R.


N.A. LH.R.

N A N.A. N.A.


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<3 N.A.


80 N A

L.N.R. N.A. N A N.A. 0.97 N A

626335


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N.A. L.N.R.

N.A. N.A. N A 169


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N.A. NA. NA. N A

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69 81 45

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18 N A N.A. N.A. N.A. N.A.


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27 28 26

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NA. N A N A N A

L.N.R. NA. NA. NA.

<3 N.A.


80 N A

L.N.R. N.A. N A N.A. 0.97 N A

626336


1.39 N.A. L.N.R. L.N.R.

1.20 N.A. 0^98 N A 1.04 N A 0.81 4 1.11 N.A. 1.62 N A

N.A. L.N.R.

N.A. N.A. N A 169


7218 6148 6858 N.A. N.A. N A N.A.

N.A. L.N.R.

N.A. N.A. N A


<3 <3 <3

N.A. NA. NA. N A

N A L.N.R.

N A N A N A


69 81 45

NA. N.A. N A N A

N A L.N.R.


N A N.A. N A N.A.

N.A. L.N.R.

N.A. N A NA.


N.A. N A N.A.

18 N A N.A. N.A. N.A. N.A.


N A LN~R.


N.A. LH.R.

N A N.A. N.A.


<2 <2 <2

N A N A N A N A

N.A. L.N.R.

N A N A N A


<8 <8 <8

N A N A N A N.A.

N.A. L.N.R.

N A N A N A


<2 <2 <2

N.A. N A N A N.A.

N.A. L.N.R.

N A N A N A


<2

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N A L.N.R. __NA.__

N A N A


27 28 26

N A L.N.R!



NA. L.N.R.

N A N A N A


<3 <3 <3

NA. N A N A N A

L.N.R. NA. NA. NA.

<3 N.A.


80 N A

L.N.R. N.A. N A N.A. 0.97 N A

626337


1.39 N.A. L.N.R. L.N.R.

1.20 N.A. 0^98 N A 1.04 N A 0.81 4 1.11 N.A. 1.62 N A

N.A. L.N.R.

N.A. N.A. N A 169


7218 6148 6858 N.A. N.A. N A N.A.

N.A. L.N.R.

N.A. N.A. N A


<3 <3 <3

N.A. NA. NA. N A

N A L.N.R.

N A N A N A


69 81 45

NA. N.A. N A N A

N A L.N.R.


N A N.A. N A N.A.

N.A. L.N.R.

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18 N A N.A. N.A. N.A. N.A.


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N A L.N.R. __NA.__

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27 28 26

N A L.N.R!



NA. L.N.R.

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80 N A

L.N.R. N.A. N A N.A. 0.97 N A 626338


1.39 N.A. L.N.R. L.N.R.

1.20 N.A. 0^98 N A 1.04 N A 0.81 4 1.11 N.A. 1.62 N A

N.A. L.N.R.

N.A. N.A. N A 169


7218 6148 6858 N.A. N.A. N A N.A.

N.A. L.N.R.

N.A. N.A. N A


<3 <3 <3

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N A N A N A


69 81 45

NA. N.A. N A N A

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18 N A N.A. N.A. N.A. N.A.


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27 28 26

N A L.N.R!



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80 N A

L.N.R. N.A. N A N.A. 0.97 N A

626339 Rock

1.39 N.A. L.N.R. L.N.R.

1.20 N.A. 0^98 N A 1.04 N A 0.81 4 1.11 N.A. 1.62 N A

N.A. L.N.R.

N.A. N.A. N A 169


7218 6148 6858 N.A. N.A. N A N.A.

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69 81 45

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18 N A N.A. N.A. N.A. N.A.


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<2 <2 <2

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27 28 26

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0.88 N A 0.79 N.A. 2.17 N.A. 2.31 N.A. 0.94 2 0.51 2 1.74 <1 1.92 N.A. 1.57 N.A. 1.61 N.A. 1.00 N.A.

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69 81 45

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18 N A N.A. N.A. N.A. N.A.


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27 28 26

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626341 Rock Rock Rock

1.64 N.A. 0.88 N A 0.79 N.A. 2.17 N.A. 2.31 N.A. 0.94 2 0.51 2 1.74 <1 1.92 N.A. 1.57 N.A. 1.61 N.A. 1.00 N.A.

N.A. L.N.R.

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69 81 45

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18 N A N.A. N.A. N.A. N.A.


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27 28 26

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53 101 38

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626342 626343 626344

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N.A. L.N.R.

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7218 6148 6858 N.A. N.A. N A N.A.

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69 81 45

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18 N A N.A. N.A. N.A. N.A.


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27 28 26

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53 101 38

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626342 626343 626344

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7218 6148 6858 N.A. N.A. N A N.A.

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69 81 45

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27 28 26

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53 101 38

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626342 626343 626344 Rock


N.A. L.N.R.

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7218 6148 6858 N.A. N.A. N A N.A.

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69 81 45

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27 28 26

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53 101 38

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N.A. N.A. N A 169


7218 6148 6858 N.A. N.A. N A N.A.

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69 81 45

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27 28 26

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53 101 38

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626346 Rock


N.A. L.N.R.

N.A. N.A. N A 169


7218 6148 6858 N.A. N.A. N A N.A.

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69 81 45

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27 28 26

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53 101 38

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626347 Rock


N.A. L.N.R.

N.A. N.A. N A 169


7218 6148 6858 N.A. N.A. N A N.A.

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69 81 45

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27 28 26

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53 101 38

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626348 Rock


N.A. L.N.R.

N.A. N.A. N A 169


7218 6148 6858 N.A. N.A. N A N.A.

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69 81 45

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53 101 38

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626349 Rock Rock


N.A. L.N.R.

N.A. N.A. N A 169


7218 6148 6858 N.A. N.A. N A N.A.

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69 81 45

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53 101 38

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0.56 0.52 N A N A N A 193732

Rock Rock


N.A. L.N.R.

N.A. N.A. N A 169


7218 6148 6858 N.A. N.A. N A N.A.

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69 81 45

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15 15 16

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53 101 38

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0.56 0.52 N A N A N A

193733 Rock


N.A. L.N.R.

N.A. N.A. N A 169


7218 6148 6858 N.A. N.A. N A N.A.

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69 81 45

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N.A. L.N.R.

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N A N A N A N A

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N A L.N.R!



NA. L.N.R.

N A N A N A


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NA. N A N A N A N A N A N.A.

This report supersedes all previous preliminary and final reports with this file number dated prior to the date on this certificate. Signature indicates final approval; preliminary reports are unsigned and should be used for reference only.





Client:

Project:

Report Date:

Doyle, Bruce 1424 Crease Ave Nelson BC V1L 1A2 Canada

None Given October 22, 2009

www.acmelab.com Page: 2 of 2 Part 2

VAN09004569.1 Method Analyte

Unit MDL

1D P %

0.001

1D La

1

1D Cr

ppm 1

1D Mg %

0.01

1D Ba

ppm 1

1D Tl %

0.01

1D B

ppm 20

1D Al %

0.01

1D Na %

0.01

1D K %

0.01

1D W

ppm 2

1D S %

0.05

1T Mo

ppm 0.05

1T Cu

ppm 0.02

1T Pb

ppm 0.02

1T Zn

ppm 0.2

1T Ag

ppb 20

1T Ni

ppm 0.1

1T Co

ppm 0.2

n Mn

ppm 2

626332 Rock N.A. L.N.R.

N.A. L.N.R.

N.A. LN.R.

" ~ N A

N A LN.R.

N A

N A L.N.R.

N A N A N A 247 N A N A N.A. N A N.A. N A N.A.

82 115 338 N A NA. N A N A

N.A. L.N.R.

N A N A N A 0.14 N A N A N.A. N.A. N.A. N A N A 0.13 0.10

N A L.N.R.

N A N A N A <20 N A N A N A N A N A

NA" N A <20

N A LN.R.

N.A. N A NA. 1.37 N A N A N A N A N A N A N A 1.68

N A L.N.R.

N A N A N A 0.07 N A N A N A N A N.A. N.A. N A 0.02

N.A. L.N.R.

N.A. NA. N A 0.66 N A N A N A N A N.A. N A N A 1.16 0.43 1.00 NA. N A N A N A

N A L.N.R.

N A N A N A

<2 N A N A NA. N A N.A. N A N.A.

4 3 5

NA. LN.R.

N A N A N.A. 0.55 N A N A N.A. N A N A N A N A 1.96 1.24 1.10

669.9 L.N.R.

0.63 1.52 NA. N A NA. N A 1.76 1.21 0.51 0.32 0.78 N A N.A. N.A.

11.57 L.N.R. 11.28 2.19 N A N A N A N A 3.04 6.57 0.23 1.39 3.05 N.A. N.A. NA.

32.09 LN.R. 36.35 16.50 N.A. N A N A N A

34.98 28.97 33.06 33.52 20.09

N.A. N.A. N A

22.72 40.10

N.A. N.A.

22.1 L.N.R.

21.9 26.2 NA. N.A. N A N A 9.1

17.2 34.9 40.8 15.8 N A N A N A 19.1 11.5 N A N A

24 LN.R.

64 <20 N A N A N A NA.

54 453

31 <20

29 N A N A N A <20 <20 N A

~ NA

0.4 LN.R.

2.3 3.4

0.4 L.N.R.

163 LN.R. 626333 Rock

N.A. L.N.R.

N.A. L.N.R.

N.A. LN.R.

" ~ N A

N A LN.R.

N A

N A L.N.R.


82 115 338 N A NA. N A N A

N.A. L.N.R.


N A L.N.R.


NA" N A <20

N A LN.R.


N A L.N.R.


N.A. L.N.R.


N A L.N.R.

N A N A N A


4 3 5

NA. LN.R.


669.9 L.N.R.

0.63 1.52 NA. N A NA. N A 1.76 1.21 0.51 0.32 0.78 N A N.A. N.A.


32.09 LN.R. 36.35 16.50 N.A. N A N A N A

34.98 28.97 33.06 33.52 20.09

N.A. N.A. N A

22.72 40.10

N.A. N.A.

22.1 L.N.R.

21.9 26.2 NA. N.A. N A N A 9.1

17.2 34.9 40.8 15.8 N A N A N A 19.1 11.5 N A N A

24 LN.R.

64 <20 N A N A N A NA.

54 453

31 <20

29 N A N A N A <20 <20 N A

~ NA

0.4 LN.R.

2.3 3.4

0.4 L.N.R.

163 LN.R.

626334 626335

Rock Rock

N.A. N.A. N.A.

0.048 N.A. N.A. N A

N.A.

N.A. LN.R.

" ~ N A

N A LN.R.

N A

N A L.N.R.


82 115 338 N A NA. N A N A

N.A. L.N.R.


N A L.N.R.


NA" N A <20

N A LN.R.


N A L.N.R.


N.A. L.N.R.


N A L.N.R.

N A N A N A


4 3 5

NA. LN.R.


669.9 L.N.R.

0.63 1.52 NA. N A NA. N A 1.76 1.21 0.51 0.32 0.78 N A N.A. N.A.


32.09 LN.R. 36.35 16.50 N.A. N A N A N A

34.98 28.97 33.06 33.52 20.09

N.A. N.A. N A

22.72 40.10

N.A. N.A.

22.1 L.N.R.

21.9 26.2 NA. N.A. N A N A 9.1

17.2 34.9 40.8 15.8 N A N A N A 19.1 11.5 N A N A

24 LN.R.

64 <20 N A N A N A NA.

54 453

31 <20

29 N A N A N A <20 <20 N A

~ NA

0.4 LN.R.

2.3 3.4

0.9 0.6

186 170

626334 626335

Rock Rock

N.A. N.A. N.A.

0.048 N.A. N.A. N A

N.A. N.A.

3 N.A. N.A. N.A. N.A. N.A. N A N A

1 2

N.A. N.A.

21 N.A. N A N.A. N.A. N.A. N.A. N A

18 16 9

N.A.

N A N A 1.44 N A N A N.A. N A N A N A N A 1.48 1.03 1.30 N A N A N A N.A.

N A L.N.R.


82 115 338 N A NA. N A N A

N.A. L.N.R.


N A L.N.R.


NA" N A <20

N A LN.R.


N A L.N.R.


N.A. L.N.R.


N A L.N.R.

N A N A N A


4 3 5

NA. LN.R.


669.9 L.N.R.

0.63 1.52 NA. N A NA. N A 1.76 1.21 0.51 0.32 0.78 N A N.A. N.A.


32.09 LN.R. 36.35 16.50 N.A. N A N A N A

34.98 28.97 33.06 33.52 20.09

N.A. N.A. N A

22.72 40.10

N.A. N.A.

22.1 L.N.R.

21.9 26.2 NA. N.A. N A N A 9.1

17.2 34.9 40.8 15.8 N A N A N A 19.1 11.5 N A N A

24 LN.R.

64 <20 N A N A N A NA.

54 453

31 <20

29 N A N A N A <20 <20 N A

~ NA

0.4 LN.R.

2.3 3.4

0.9 0.6

186 170

626336 Rock

N.A. N.A. N.A.

0.048 N.A. N.A. N A

N.A. N.A.


1 2

N.A. N.A.


18 16 9

N.A.


N A L.N.R.


82 115 338 N A NA. N A N A

N.A. L.N.R.


N A L.N.R.


NA" N A <20

N A LN.R.


N A L.N.R.


N.A. L.N.R.


N A L.N.R.

N A N A N A


4 3 5

NA. LN.R.


669.9 L.N.R.

0.63 1.52 NA. N A NA. N A 1.76 1.21 0.51 0.32 0.78 N A N.A. N.A.


32.09 LN.R. 36.35 16.50 N.A. N A N A N A

34.98 28.97 33.06 33.52 20.09

N.A. N.A. N A

22.72 40.10

N.A. N.A.

22.1 L.N.R.

21.9 26.2 NA. N.A. N A N A 9.1

17.2 34.9 40.8 15.8 N A N A N A 19.1 11.5 N A N A

24 LN.R.

64 <20 N A N A N A NA.

54 453

31 <20

29 N A N A N A <20 <20 N A

~ NA

N A N.A. N.A. N A

1.1 2.2

<0.1 0.9 1.3

N A N A N A

1.0 0.5

N A N A

N.A. NA. N.A. N A

N.A. N A N.A. N A

626337 626338

Rock

N.A. N.A. N.A.

0.048 N.A. N.A. N A

N.A. N.A.


1 2

N.A. N.A.


18 16 9

N.A.


N A L.N.R.


82 115 338 N A NA. N A N A

N.A. L.N.R.


N A L.N.R.


NA" N A <20

N A LN.R.


N A L.N.R.


N.A. L.N.R.


N A L.N.R.

N A N A N A


4 3 5

NA. LN.R.


669.9 L.N.R.

0.63 1.52 NA. N A NA. N A 1.76 1.21 0.51 0.32 0.78 N A N.A. N.A.


32.09 LN.R. 36.35 16.50 N.A. N A N A N A

34.98 28.97 33.06 33.52 20.09

N.A. N.A. N A

22.72 40.10

N.A. N.A.

22.1 L.N.R.

21.9 26.2 NA. N.A. N A N A 9.1

17.2 34.9 40.8 15.8 N A N A N A 19.1 11.5 N A N A

24 LN.R.

64 <20 N A N A N A NA.

54 453

31 <20

29 N A N A N A <20 <20 N A

~ NA

N A N.A. N.A. N A

1.1 2.2

<0.1 0.9 1.3

N A N A N A

1.0 0.5

N A N A

N.A. NA. N.A. N A

N.A. N A N.A. N A

626337 626338 Rock

Rock Rock

N.A. N.A. N.A.

0.048 N.A. N.A. N A

N.A. N.A.


1 2

N.A. N.A.


18 16 9

N.A.


N A L.N.R.


82 115 338 N A NA. N A N A

N.A. L.N.R.


N A L.N.R.


NA" N A <20

N A LN.R.


N A L.N.R.


N.A. L.N.R.


N A L.N.R.

N A N A N A


4 3 5

NA. LN.R.


669.9 L.N.R.

0.63 1.52 NA. N A NA. N A 1.76 1.21 0.51 0.32 0.78 N A N.A. N.A.


32.09 LN.R. 36.35 16.50 N.A. N A N A N A

34.98 28.97 33.06 33.52 20.09

N.A. N.A. N A

22.72 40.10

N.A. N.A.

22.1 L.N.R.

21.9 26.2 NA. N.A. N A N A 9.1

17.2 34.9 40.8 15.8 N A N A N A 19.1 11.5 N A N A

24 LN.R.

64 <20 N A N A N A NA.

54 453

31 <20

29 N A N A N A <20 <20 N A

~ NA

N A N.A. N.A. N A

1.1 2.2

<0.1 0.9 1.3

N A N A N A

1.0 0.5

N A N A

N.A. NA. N.A. N A

N.A. N A N.A. N A 626339

Rock Rock Rock

N.A. N.A. N.A.

0.048 N.A. N.A. N A

N.A. N.A.


1 2

N.A. N.A.


18 16 9

N.A.


N A L.N.R.


82 115 338 N A NA. N A N A

N.A. L.N.R.


N A L.N.R.


NA" N A <20

N A LN.R.


N A L.N.R.


N.A. L.N.R.


N A L.N.R.

N A N A N A


4 3 5

NA. LN.R.


669.9 L.N.R.

0.63 1.52 NA. N A NA. N A 1.76 1.21 0.51 0.32 0.78 N A N.A. N.A.


32.09 LN.R. 36.35 16.50 N.A. N A N A N A

34.98 28.97 33.06 33.52 20.09

N.A. N.A. N A

22.72 40.10

N.A. N.A.

22.1 L.N.R.

21.9 26.2 NA. N.A. N A N A 9.1

17.2 34.9 40.8 15.8 N A N A N A 19.1 11.5 N A N A

24 LN.R.

64 <20 N A N A N A NA.

54 453

31 <20

29 N A N A N A <20 <20 N A

~ NA

N A N.A. N.A. N A

1.1 2.2

<0.1 0.9 1.3

N A N A N A

1.0 0.5

N A N A

N.A. NA. N.A. N A

N.A. N A N.A. N A

626340

Rock Rock Rock

N.A. N.A. N.A.

0.048 N.A. N.A. N A

N.A. N.A.


1 2

N.A. N.A.


18 16 9

N.A.


N A L.N.R.


82 115 338 N A NA. N A N A

N.A. L.N.R.


N A L.N.R.


NA" N A <20

N A LN.R.


N A L.N.R.


N.A. L.N.R.


N A L.N.R.

N A N A N A


4 3 5

NA. LN.R.


669.9 L.N.R.

0.63 1.52 NA. N A NA. N A 1.76 1.21 0.51 0.32 0.78 N A N.A. N.A.


32.09 LN.R. 36.35 16.50 N.A. N A N A N A

34.98 28.97 33.06 33.52 20.09

N.A. N.A. N A

22.72 40.10

N.A. N.A.

22.1 L.N.R.

21.9 26.2 NA. N.A. N A N A 9.1

17.2 34.9 40.8 15.8 N A N A N A 19.1 11.5 N A N A

24 LN.R.

64 <20 N A N A N A NA.

54 453

31 <20

29 N A N A N A <20 <20 N A

~ NA

N A N.A. N.A. N A

1.1 2.2

<0.1 0.9 1.3

N A N A N A

1.0 0.5

N A N A

0.2 0~3

462 1038 626341 Rock N.A.

N.A. N A N.A.

0.028 0.058

N.A. N.A.


1 2

N.A. N.A.


18 16 9

N.A.


N A L.N.R.


82 115 338 N A NA. N A N A

N.A. L.N.R.


N A L.N.R.


NA" N A <20

N A LN.R.


N A L.N.R.


N.A. L.N.R.


N A L.N.R.

N A N A N A


4 3 5

NA. LN.R.


669.9 L.N.R.

0.63 1.52 NA. N A NA. N A 1.76 1.21 0.51 0.32 0.78 N A N.A. N.A.


32.09 LN.R. 36.35 16.50 N.A. N A N A N A

34.98 28.97 33.06 33.52 20.09

N.A. N.A. N A

22.72 40.10

N.A. N.A.

22.1 L.N.R.

21.9 26.2 NA. N.A. N A N A 9.1

17.2 34.9 40.8 15.8 N A N A N A 19.1 11.5 N A N A

24 LN.R.

64 <20 N A N A N A NA.

54 453

31 <20

29 N A N A N A <20 <20 N A

~ NA

N A N.A. N.A. N A

1.1 2.2

<0.1 0.9 1.3

N A N A N A

1.0 0.5

N A N A

0.2 0~3

462 1038

626342 626343

Rock Rock

N.A. N.A. N A N.A.

0.028 0.058

N.A. N.A.


1 2

N.A. N.A.


18 16 9

N.A.


N A L.N.R.


82 115 338 N A NA. N A N A

N.A. L.N.R.


N A L.N.R.


NA" N A <20

N A LN.R.


N A L.N.R.


N.A. L.N.R.


N A L.N.R.

N A N A N A


4 3 5

NA. LN.R.


669.9 L.N.R.

0.63 1.52 NA. N A NA. N A 1.76 1.21 0.51 0.32 0.78 N A N.A. N.A.


32.09 LN.R. 36.35 16.50 N.A. N A N A N A

34.98 28.97 33.06 33.52 20.09

N.A. N.A. N A

22.72 40.10

N.A. N.A.

22.1 L.N.R.

21.9 26.2 NA. N.A. N A N A 9.1

17.2 34.9 40.8 15.8 N A N A N A 19.1 11.5 N A N A

24 LN.R.

64 <20 N A N A N A NA.

54 453

31 <20

29 N A N A N A <20 <20 N A

~ NA

N A N.A. N.A. N A

1.1 2.2

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N A N A N A

1.0 0.5

N A N A

<0.2 0.5 1.1

193 235 211 626344 Rock

N.A. N.A. N A N.A.

0.028 0.058

N.A. N.A.


1 2

N.A. N.A.


18 16 9

N.A.


N A L.N.R.


82 115 338 N A NA. N A N A

N.A. L.N.R.


N A L.N.R.


NA" N A <20

N A LN.R.


N A L.N.R.


N.A. L.N.R.


N A L.N.R.

N A N A N A


4 3 5

NA. LN.R.


669.9 L.N.R.

0.63 1.52 NA. N A NA. N A 1.76 1.21 0.51 0.32 0.78 N A N.A. N.A.


32.09 LN.R. 36.35 16.50 N.A. N A N A N A

34.98 28.97 33.06 33.52 20.09

N.A. N.A. N A

22.72 40.10

N.A. N.A.

22.1 L.N.R.

21.9 26.2 NA. N.A. N A N A 9.1

17.2 34.9 40.8 15.8 N A N A N A 19.1 11.5 N A N A

24 LN.R.

64 <20 N A N A N A NA.

54 453

31 <20

29 N A N A N A <20 <20 N A

~ NA

N A N.A. N.A. N A

1.1 2.2

<0.1 0.9 1.3

N A N A N A

1.0 0.5

N A N A

<0.2 0.5 1.1

193 235 211

626345 Rock Rock

N.A. N.A. N A N.A.

0.028 0.058

N.A. N.A.


1 2

N.A. N.A.


18 16 9

N.A.


N A L.N.R.


82 115 338 N A NA. N A N A

N.A. L.N.R.


N A L.N.R.


NA" N A <20

N A LN.R.


N A L.N.R.


N.A. L.N.R.


N A L.N.R.

N A N A N A


4 3 5

NA. LN.R.


669.9 L.N.R.

0.63 1.52 NA. N A NA. N A 1.76 1.21 0.51 0.32 0.78 N A N.A. N.A.


32.09 LN.R. 36.35 16.50 N.A. N A N A N A

34.98 28.97 33.06 33.52 20.09

N.A. N.A. N A

22.72 40.10

N.A. N.A.

22.1 L.N.R.

21.9 26.2 NA. N.A. N A N A 9.1

17.2 34.9 40.8 15.8 N A N A N A 19.1 11.5 N A N A

24 LN.R.

64 <20 N A N A N A NA.

54 453

31 <20

29 N A N A N A <20 <20 N A

~ NA

N A N.A. N.A. N A

1.1 2.2

<0.1 0.9 1.3

N A N A N A

1.0 0.5

N A N A

NA. N A 626346

Rock Rock

N.A. N.A. N A N.A.

0.028 0.058

N.A. N.A.


1 2

N.A. N.A.


18 16 9

N.A.


N A L.N.R.


82 115 338 N A NA. N A N A

N.A. L.N.R.

N A N A N A 0.14 N A N A N.A. N.A. N.A. N A N A 0.13 0.10 <20 1.65

L56 NA. N A N A N A

0.10 0.03 N A N A N A N A

N.A. L.N.R.


N A L.N.R.

N A N A N A


4 3 5

NA. LN.R.


669.9 L.N.R.

0.63 1.52 NA. N A NA. N A 1.76 1.21 0.51 0.32 0.78 N A N.A. N.A.


32.09 LN.R. 36.35 16.50 N.A. N A N A N A

34.98 28.97 33.06 33.52 20.09

N.A. N.A. N A

22.72 40.10

N.A. N.A.

22.1 L.N.R.

21.9 26.2 NA. N.A. N A N A 9.1

17.2 34.9 40.8 15.8 N A N A N A 19.1 11.5 N A N A

24 LN.R.

64 <20 N A N A N A NA.

54 453

31 <20

29 N A N A N A <20 <20 N A

~ NA

N A N.A. N.A. N A

1.1 2.2

<0.1 0.9 1.3

N A N A N A

1.0 0.5

N A N A

NA. N A

N A 626347 626348 626349 193732

Rock Rock Rock

0.026 N.A.

1 N.A.

N.A. N.A.


18 16 9

N.A.


N A L.N.R.


82 115 338 N A NA. N A N A

0.11 N A N A N A N A

<20 1.65 L56 NA. N A N A N A

0.10 0.03 N A N A N A N A

N.A. L.N.R.


N A L.N.R.

N A N A N A


4 3 5

NA. LN.R.


669.9 L.N.R.

0.63 1.52 NA. N A NA. N A 1.76 1.21 0.51 0.32 0.78 N A N.A. N.A.


32.09 LN.R. 36.35 16.50 N.A. N A N A N A

34.98 28.97 33.06 33.52 20.09

N.A. N.A. N A

22.72 40.10

N.A. N.A.

22.1 L.N.R.

21.9 26.2 NA. N.A. N A N A 9.1

17.2 34.9 40.8 15.8 N A N A N A 19.1 11.5 N A N A

24 LN.R.

64 <20 N A N A N A NA.

54 453

31 <20

29 N A N A N A <20 <20 N A

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N A N.A. N.A. N A

1.1 2.2

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N A N A N A

1.0 0.5

N A N A

NA. N A N A 626347

626348 626349 193732

Rock Rock Rock

0.026 N.A.

1 N.A.

N.A. N.A.


18 16 9

N.A.


N A L.N.R.


82 115 338 N A NA. N A N A


N A N A N A N A

1.65 L56 NA. N A N A N A

0.10 0.03 N A N A N A N A

N.A. L.N.R.


N.A. NA. N A N.A.

N.A. N.A. NA. N.A.

0.35 1.90 N.A. N.A.

23.29 11.01 N.A. N A

32.09 LN.R. 36.35 16.50 N.A. N A N A N A

34.98 28.97 33.06 33.52 20.09

N.A. N.A. N A

22.72 40.10

N.A. N.A.

22.1 L.N.R.

21.9 26.2 NA. N.A. N A N A 9.1

17.2 34.9 40.8 15.8 N A N A N A 19.1 11.5 N A N A

24 LN.R.

64 <20 N A N A N A NA.

54 453

31 <20

29 N A N A N A <20 <20 N A

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1.1 2.2

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N A N A N A

1.0 0.5

N A N A

0.5 252 626347 626348 626349 193732

Rock Rock Rock N.A. N.A.

N.A. N.A.

N A N A N A


N A L.N.R.


82 115 338 N A NA. N A N A


N A N A N A N A

1.65 L56 NA. N A N A N A

0.10 0.03 N A N A N A N A

N.A. L.N.R.


N.A. NA. N A N.A.

N.A. N.A. NA. N.A.

0.35 1.90 N.A. N.A.

23.29 11.01 N.A. N A

32.09 LN.R. 36.35 16.50 N.A. N A N A N A

34.98 28.97 33.06 33.52 20.09

N.A. N.A. N A

22.72 40.10

N.A. N.A.

22.1 L.N.R.

21.9 26.2 NA. N.A. N A N A 9.1

17.2 34.9 40.8 15.8 N A N A N A 19.1 11.5 N A N A

24 LN.R.

64 <20 N A N A N A NA.

54 453

31 <20

29 N A N A N A <20 <20 N A

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1.1 2.2

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N A N A N A

1.0 0.5

N A N A

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413 N A

626347 626348 626349 193732 Rock N.A.

N A

N.A. N.A. N.A.

N A N A N A


N A L.N.R.


82 115 338 N A NA. N A N A


N A N A N A N A

1.65 L56 NA. N A N A N A

0.10 0.03 N A N A N A N A

N.A. L.N.R.


N.A. NA. N A N.A.

N.A. N.A. NA. N.A.

0.35 1.90 N.A. N.A.

23.29 11.01 N.A. N A

32.09 LN.R. 36.35 16.50 N.A. N A N A N A

34.98 28.97 33.06 33.52 20.09

N.A. N.A. N A

22.72 40.10

N.A. N.A.

22.1 L.N.R.

21.9 26.2 NA. N.A. N A N A 9.1

17.2 34.9 40.8 15.8 N A N A N A 19.1 11.5 N A N A

24 LN.R.

64 <20 N A N A N A NA.

54 453

31 <20

29 N A N A N A <20 <20 N A

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1.1 2.2

<0.1 0.9 1.3

N A N A N A

1.0 0.5

N A N A

<0.2 N A

413 N A

193733 Rock N.A. N A

N.A. N.A. N.A.

N A N A N A


N A L.N.R.


82 115 338 N A NA. N A N A


N A N A N A N A

1.65 L56 NA. N A N A N A

0.10 0.03 N A N A N A N A

N.A. L.N.R.


N.A. NA. N A N.A.

N.A. N.A. NA. N.A.

0.35 1.90 N.A. N.A.

23.29 11.01 N.A. N A

32.09 LN.R. 36.35 16.50 N.A. N A N A N A

34.98 28.97 33.06 33.52 20.09

N.A. N.A. N A

22.72 40.10

N.A. N.A.

22.1 L.N.R.

21.9 26.2 NA. N.A. N A N A 9.1

17.2 34.9 40.8 15.8 N A N A N A 19.1 11.5 N A N A

24 LN.R.

64 <20 N A N A N A NA.

54 453

31 <20

29 N A N A N A <20 <20 N A

~ NA

N A N.A. N.A. N A

1.1 2.2

<0.1 0.9 1.3

N A N A N A

1.0 0.5

N A N A NA. NA.

This report supersedes all previous preliminary and final reports with this file number dated prior to the date on this certificate. Signature indicates final approval; prelminary reports are unsigned and should be used for reference only.


c*cs vv°

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