ASSESSMENT REPORT TITLE PAGE AND SUMMARY

TITLE OF REPORT: Report on the Quartzite Silica Occurrences Longworth Properties, ,

TOTAL COST: $202,432.03 (NOTE: Only $68,000 of the total expended was applied)

AUTHOR(S): Mack S. Duncan, PhD; John F. Childs, PhD SIGNATURE(S): “Signed and Sealed” NOTICE OF WORK PERMIT NUMBER(S)/DATE(S): MX-11-218; May 2-16, 2008 STATEMENT OF WORK EVENT NUMBER(S)/DATE(S ): 4217805, 4218003; May 27-28, 2008

YEAR OF WORK: 2008 PROPERTY NAME: CROW CLAIM NAME(S) (on which work was done) CROW 11, TENURE 559360

COMMODITIES SOUGHT: SIO2

MINERAL INVENTORY MINFILE NUMBER(S),IF KNOWN: 093H 038 MINING DIVISION: PRINCE GEORGE-OMINECA NTS / BCGS: 093H.093 LATITUDE 53o 56’ 56" LONGITUDE -121o 25’ 50" (at centre of work) UTM Zone 10N EASTING 603010 NORTHING 5978973

OWNER(S): CARD JM RESOURCES INC. MAILING ADDRESS: BOX 582, McBRIDE, BC, V0J 2E0

OPERATOR(S) [who paid for the work]: BOARDWALK GROUP INC. MAILING ADDRESS: B103, 912 WEST 1600, ST GEORGE, UTAH, USA, 84770

REPORT KEYWORDS (lithology, age, stratigraphy, structure, alteration, mineralization, size and attitude do not use abbreviations or codes) Quartz, Quartzite, Quartz Silica

REFERENCES TO PREVIOUS ASSESSMENT WORK AND ASSESSMENT REPORT NUMBERS

REPORT on the

Quartzite Silica Occurrences

Longworth Properties,

British Columbia, Canada

Tenure number 559360, Prince George-Omineca Mining Division

Latitude 53.948889 Longitude 121.430556

NAD83 Zone 10N UTM Northing 5978973, Easting 603010

Report filed Pursuant to Assessment Recording Events No. 4217805 and 4218003

Prepared for:

Operator: Boardwalk Group Inc.

Property Owner: Card JM Resources Inc.

By

Mack S. Duncan, Ph.D, PG

and

John F. Childs, Ph.D., Registered Geologist and Qualified Person

CHILDS AND ASSOCIATES, LLC ECONOMIC GEOLOGISTS 109 Sourdough Ridge Road

Bozeman, MT 59715 U.S.A.

Telephone/fax- (406) 585-3727 Cellular phone- (406) 223-1139

E-mail: [email protected]

September 26, 2008 TABLE OF CONTENTS

TABLE OF CONTENTS...... 1

Table of Figures ...... 1

List of Tables...... 1

INTRODUCTION ...... 2

LOCATION ...... 2

PREVIOUS WORK...... 6

GENERAL GEOLOGY...... 7

CORE...... 7

PROGRAMS USED...... 11

STATEMENT OF QUALIFICATIONS ‐ DUNCAN...... 12

STATEMENT OF QUALIFICATIONS - CHILDS...... 13

Table of Figures Figure 1 Location and Access ...... 3

Figure 2 Tenure Detail...... 4

Figure 3 Known Occurrences ...... 5

Figure 4 Drill Location ...... 9

Figure 5 Drill Section ...... 10

List of Tables Table 1: Minfile 093H 038 Summary...... 6

Table 2: Assay Result Summary ...... 8

Appendix A – References Appendix B – Core Description Appendix C – Longworth Deposit Report Appendix D – Analytical Method Appendix E – Statement of Costs Appendix F – Tenure Listing

1 INTRODUCTION

Childs and Associates were engaged to evaluate drill core obtained from the Longworth quartzite (silica) deposit, Tenure Number 559360, approximately 80 kilometers east of Prince George, British Columbia.

The work was conducted in May, 2008. Access to the drill site was by helicopter. Significant snowpack covered the area.

One core hole was drilled to a depth of 100.6 meters (330’). Approximately 96 meters of core were recovered (315’), described and assayed.

Regional and local geology were not investigated in the field as part of this project. Previous work by others is summarized, but its accuracy is not warranted by Duncan or Childs.

The property is covered by the following topographic maps: 093H.092, 093H.093, 093H.094, 093I.002, and 093I.003. The property is within the Prince George-Omineca mining division. The project operator is Card JM Resources Inc. and the owner of the property is Mr. Milton Braaten. The work reported here was conducted on Tenure Number 559360. The report is submitted with reference to Assessment Recording Events 4217805 and 4218003.

LOCATION

The original filing cited the wrong Tenure Number for the work performed (Tenure 559342). The drill hole was actually located on Tenure 559360.

Coordinates for the drill hole are:

NAD83, Zone 10N, Northing 5978973, Easting 603010.

Large-scale and small-scale maps showing the drill hole location and location of the Tenures are included below.

2 F RA SE R

Upper

CNR Fraser McGregor To rp hy R RI iv V er ER r ive R on wr Bo

W il lo w R iv e r Purden Lake HW Y 16 PRINCE H GEORGE u n g a r y

C r e e k

Figure 1 Location & Access ACCESS: From Prince George, travel E on Hwy 16 13.7km to Giscome turnoff, turn N 15.2km, at Willow River connect with Upper Fraser Road, turn E 69.5km to claim block

ALTERNATE ACCESS: From Prince George, travel E on Hwy 16 65.1km (first FSR E of Purden Lake), turn N 23.7km to Hansard, turn E 2.7km to connect to Upper Fraser Road, turn Mapsheets 093H/13 Scale 1:250000 E 24.3km to claim block 093H/14 093I/04 NOTE: Access to drill area via helicopter only 093I/03 To rp FR hy AS R ER ive r

RI VE R

Figure 2 Tenure Detail Mapsheets 093H.092 & Topography 093H.093 093H.094 093I.002 093I.003

Scale 1:140000 Figure 3 Known Occurrences

Taken from Lane, B., MacDonald, K., McGrath, B., Robinson, N. and Simandl, G. (2004). Longworth claims are at location 093H 038

5 PREVIOUS WORK

The following summary from Government of British Columbia MINFILE Report No 093H 038, (1989) provides an excellent overview of previous work:

Table 1: Minfile 093H 038 Summary

Name LONGWORTH, NONDA QUARTZITE, SNOW, RAIN, Mining Cariboo LONG, DOLL Division

BCGS Map 093H093

Status Prospect NTS Map 093H14W

Latitude 53º 58' 48" N UTM 10 (NAD 83)

Longitude 121º 29' 30" W Northing 5982350

Easting 598914

Commodities Silica Deposit R07 : Silica sandstone Types

Tectonic Belt Foreland Terrane Ancestral North America

Capsule Geology The Longworth prospect is located about 80 kilometres east of Prince George. The claims were staked originally in 1974 and blasting, trenching and sampling has been completed on the property

The prospect is hosted by a folded sequence of sedimentary and volcanic rocks which underlie Bearspaw Ridge. They are all, or in part, Lower Silurian in age and equivalent to the Nonda Formation.

At least four northwest trending bands of quartzite have been mapped along the western flank of Bearpaw Ridge. Thicknesses reach up to about 400 metres. The main quartzite band outlines a synformal structure open to the northwest. Rare bedding observed in outcrop dips 70 to 80 degrees east. The quartzite is very pure, massive and homogeneous. It is composed of extremely well-rounded and well- sorted quartz grains, averaging 0.5 millimetre in diameter, which are cemented by silica. The quartzite is pinkish white to buff on fresh surfaces and weathers grey to white. Impurities include muscovite in cavities, limonite on microfractures, minor calcite and possible hydrocarbons. Eight chip samples collected in 1982 by the

6 Geological Survey Branch averaged 99.5 per cent silica (Open File 1987-15).

Consolidated Silver Standard Mines Ltd. evaluated the property in 1985 for the production of ferrosilicon and silicon metal. They took 42 samples of which 28 had the required chemical specifications, SiO2 was from 98.84 to 99.80 per cent and 16 samples had acceptable thermal shock results (Open File 1987-15). Details of the 1985 work conducted by Consolidated Silver Standard Mines Ltd. may be found in MINEFILE Assessment Report 14815, (1987)

GENERAL GEOLOGY

Outcrops of the Longworth quartzite deposit were not visited by the authors due to deep snow cover. We therefore depend on previously published reports summarized below.

Lane, et al (2004) describe the geology as ““A folded sequence of sedimentary and volcanic rocks… The quartzite is essentially correlative with the Lower Silurian equivalent to the Nonda Formation, and is fine-grained, massive and well-sorted.”

A 3-page summary of this deposit may be found within British Columbia Open File Report OF1987-15 (Foye, 1987). A copy of the relevant 3 pages is attached as Appendix 3. The quartzite is described as “very pure, massive and homogeneous. It is composed of extremely well rounded and well-sorted quartz grains averaging 0.5 millimeters in diameter which are cemented by silica.”

CORE The hole was drilled vertically to a depth of 100.5 meters (330 feet). The core drilling effort was successful in that excellent appearing quartzite was encountered. Core recovery was excellent. No significant visible impurities were noted. The core description is included as Appendix B.

Assay results from three composite samples confirm the high quality of the quartzite (see below). Analytical methods used in assaying are included as Appendix D. The very low iron content is particularly significant.

7 Table 2: Assay Result Summary

SiO2 Al2O3 Fe2O3 CaO MgO Na2O K2O Cr2O3 TiO2 MnO P2O5 SrO BaO LOI Total %%%%%%%%%%%%%%% Crow 30ft‐130ft 97.9 0.23 0.03 <0.01 0.07 0.03 0.09 0.02 0.04 <0.01 0.012 0.01 <0.01 0.11 98.54 Crow 140ft‐230ft 98.11 0.17 0.04 <0.01 0.07 0.03 0.07 0.02 0.03 <0.01 0.012 0.01 <0.01 0.1 98.67 Crow 240ft‐330ft 98.83 0.27 0.04 <0.01 0.07 0.03 0.1 0.02 0.03 <0.01 0.012 0.01 <0.01 0.11 99.52

Bit wear was an issue and drilling was very slow. Other problems resulted in much slower drilling rates as well, in particular difficulty in maintaining a dependable supply of circulation water. The water source was 7000 meters away, downhill, and there was deep snow.

The drill section included below lacks the typical lithology breaks and intercepts because there were none noted.

8 Figure 4 Drill Location Legend NAD 83 Zone 10N UTM Coordinates

DDH 5978973N, 603010E

Scale 1:20000

Figure 5 Drill Section

DRILL SECTION LONGWORTH HOLE #1

Depth in Feet 0 10 ---- 0'-5' No recovery 20 5'-25' Poor recovery, white quartzite. 30 ---- 40 25'-330' Very consistent, homogeneous white quartzite. 50 Occassional brownish blotches 1-3cm across, 60 consisdered insignificant. 70 50 degree dip at 67'. 80 90 Fine grains visible on broken surface. 100 Silica overgrowths fill pore space. 110 Drusy quartz on some fracture surfaces. 120 130 There are no partings of material other than quartzite 140 from which to measure dip of bedding. 150 160 52 degree dip at 11'. 170 180 190 200 Two dip measurements were made where there is a 210 slight variation in quartz cementation which is 220 believed to be a function of original bedding. 230 Transposition of bedding is likely. 240 250 Excellent core recovery from 25'-330'. 260 270 280 290 300 310 320 330

10 PROGRAMS USED

The programs used in the preparation of this report are as follow: Garmin MapSource GIS software, Adobe Illustrator, Google Maps, Microsoft Word, Microsoft Excel.

11 STATEMENT OF QUALIFICATIONS - DUNCAN

I, Mack S. Duncan, do hereby certify that:

1. I am a consulting geologist. Mack S. Duncan 2600 Lexington Rd. Athens, Georgia, USA 30605

2. I graduated with a PhD in Geology from Indiana University, Bloomington (1976). I have a BS in Geology from the University of Georgia (1968).

3. I am a member of the Geological Society of America and the Society for Mining, Metallurgy and Exploration, Inc.. I am a Registered Professional Geologist in the State of Georgia, USA.

4. I have practiced my profession in excess of 30 years.

5. My relevant experience for the purpose of this report is:

19 years of exploration and mining experience with J. M. Huber Corporation including Exploration Geologist and Manager, Exploration and Mining.

6. I have not had prior involvement with the properties that are the subject of this Technical Report.

7. As of the date of this certificate, to the best of my knowledge, information and belief, the Technical Report contains all scientific and technical information that is required to be disclosed to make the Technical Report not misleading.

Dated September 21, 2008

“Signed” ______Mack S. Duncan

12 STATEMENT OF QUALIFICATIONS - CHILDS

I, John F. Childs, do hereby certify that:

1. I am a Member and Owner of: Childs and Associates, LLC 109 Sourdough Ridge Road Bozeman, Montana 59715

2. I graduated with a PhD in Geology from the University of California, Santa Cruz (1982). I have an MSc from the University of British Columbia (1969) and a BSc from Syracuse University (1966).

3. I am a member of the Geological Society of America, the Geological Association of Canada, the Society of Economic Geologists, and the Association of Applied Geochemists. I am a Registered Geologist in the States of Arizona, California, and Idaho and I am a Founding Registered Member of the Society for Mining, Metallurgy and Exploration, Inc.

4. I have practiced my profession in excess of 35 years

5. I have read the definition of “qualified person” set out in National Instrument 43-101 (“NI 43-101”) and certify that by reason of my education and past relevant work experience, I fulfill the requirements to be a “qualified person” for the purposes of NI 43-101. This report is based on my personal review of information generated by Dr. Mack S. Duncan who conducted the work reported here under my direction. My relevant experience for the purpose of this report is:

Vice President, Exploration, Bolero Resources Corporation; Mine Geologist, Stillwater Mining Company, Big Timber, MT; General Manager, Exploration, Pegasus Gold Corporation, Spokane, WA; Vice President, Lupine Minerals Corporation, Denver, CO; Senior Geologist, Cyprus Georesearch Company, Los Angeles, CA; and Consulting Geologist to a variety of large and small precious metals and industrial minerals mining and exploration companies.

6. I am responsible for the preparation of this report titled “Preliminary Report, Crow/Longworth Quartzite Silica Property, British Columbia, Canada” and dated September 8, 2008 related to the Crow/Longworth silica property.

7. I have not had prior involvement with the properties that are the subject of this Technical Report.

8. As of the date of this certificate, to the best of my knowledge, information and belief, the Technical Report contains all scientific and technical information that is required to be disclosed to make the Technical Report not misleading.

9. I am independent of the issuer applying all the tests in Section 1.4 of National Instrument 43-101.

Dated September 21, 2008

Signed and Sealed,

Signature of John F. Childs, Registered Professional Geologist in the State of Arizona, License No. 19192, License Expires June 30, 2011

13 APPENDIX A - References

Foye, G. (1987): Silica Occurrences in British Columbia. British Columbia Ministry of Energy and Mines Open File 1987-15. 55 pages.

Lane, B., MacDonald, K, McGrath, B., Robinson, N. and Simandl, G. (2004): The Geology of Western North America (Abridged Version); G.J. Simandl, W.J. McMillan and N.D. Robinson, Editors, 37th Annual Forum on Industrial Minerals Proceedings, Industrial Minerals with emphasis on Western North America, British Columbia Ministry of Energy and Mines, Geological Survey Branch,, Paper 2004-2, pages 15-25.

MINFILE Report No 093H 038, (1989) Government of British Columbia, Ministry of Energy, Mines and Petroleum Resources. Summary

MINFILE Assessment Report 14815, (1987) Government of British Columbia, Ministry of Energy, Mines and Petroleum Resources. Summary

APPENDIX B - CORE DESCRIPTION

LONGWORTH HOLE #1 VERTICAL HOLE DRILLED MAY, 2008 LOGGED BY MACK S. DUNCAN

DRILLING PYRITE PHYLLITE DEPTH COLOR NO TR AB NO TR AB DIP COMMENTS 5‐25 White X X Poor core recovery; appears to be excellent quality. 25‐330 White X X Very consistent, homogeneous white quartzite. Occassional brownish blotches 1‐3cm across; considered insignificant; possible iron or hydrocarbon stain. Fine grains visible on broken surface; silica overgrowths fill pore space. Drusy quartz on some fracture surfaces. There are no partings of material other than quartzite from which to measure dip of bedding. Two dip measurements were made where there is a slight variation in quartz cementation; believed to represent original bedding. Dips were 50o at 67' and 52o at 151'. Excellent core recovery from25'‐330'.

Note: NO ‐ None observed or very rare TR ‐ Trace ‐ Scattered occurrence, but noteworthy AB ‐ Abundant ‐ Obvious occurrence

APPENDIX C - LONGWORTH DEPOSIT REPORT

APPENDIX D - ANALYTICAL METHOD

Whole Rock Geochemistry – ME-XRF06

Sample Decomposition: 50% Li2B4O7 – 50% LiBO2 (WEI-GRA06) Analytical Method: X-Ray Fluorescence Spectroscopy (XRF)

A calcined or ignited sample (0.9 g) is added to 9.0g of Lithium Borate Flux (50 % - 50 % Li2B4O7 – LiBO2), mixed well and fused in an auto fluxer between 1050 - 1100°C. A flat molten glass disc is prepared from the resulting melt. This disc is then analysed by X-ray fluorescence spectrometry.

Element Symbol Units Lower Limit Upper Limit

Aluminum Oxide Al2O3 % 0.01 100 Barium Oxide BaO % 0.01 100 Calcium Oxide CaO % 0.01 100

Chromium Oxide Cr2O3 % 0.01 100

Ferric Oxide Fe2O3 % 0.01 100

Potassium Oxide K2O % 0.01 100 Magnesium Oxide MgO % 0.01 100 Manganese Oxide MnO % 0.01 100

Sodium Oxide Na2O % 0.01 100

Phosphorus Oxide P2O5 % 0.01 100

Silicon Oxide SiO2 % 0.01 100 Strontium Oxide SrO % 0.01 100

Titanium Oxide TiO2 % 0.01 100 Loss On Ignition LOI % 0.01 100 Total % 0.01 101

Note: Since samples that are high in sulphides or base metals can damage Platinum crucibles, a ME-ICP06 finish method can be selected as an alternative method.

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

Sample preparation is the most critical step in the entire laboratory operation. The purpose of preparation is to produce a homogeneous analytical sub-sample that is fully representative of the material submitted to the laboratory. The sample is logged in the tracking system, weighed, dried and finely crushed to better than 70 % passing a 2 mm (Tyler 9 mesh, US Std. No.10) screen. A split of up to 250 g is taken and pulverized to better than 85 % passing a 75 micron (Tyler 200 mesh, US Std. No. 200) screen. This method is appropriate for rock chip or drill samples.

Method Code Description Sample is logged in tracking system and a bar code label is LOG-22 attached. Fine crushing of rock chip and drill samples to better than 70 % of CRU-31 the sample passing 2 mm. SPL-21 Split sample using riffle splitter. A sample split of up to 250 g is pulverized to better than 85 % of PUL-31 the sample passing 75 microns.

Flow Chart - Sample Preparation Package – PREP-31 Standard Sample Preparation: Dry, Crush, Split and Pulverize

Receive Sample

LOG-22 Affix Bar Code and Log Sample in LIMS

WEI-21 Record received sample weight

Is sample NO If samples air-dry dry? overnight, no charge to client. If samples are Dry Sample excessively wet, the sample should be dried YES to a maximum of 120°C. (DRY-21)

QC testing of crushing CRU-31 efficiency is conducted Fine crushing of rock chip and drill samples on random samples to better than 70 % < 2 mm (CRU-QC).

The sample reject is saved or dumped SPL-21 pending client Keep Reject Split sample using riffle instructions. Prolonged Reject splitter storage (> 45 days) of rejects will be charged to the client.

QC testing of PUL-31 pulverizing efficiency is Up to 250 g sample split is pulverized to conducted on random better than 85 % < 75 microns samples (PUL-QC).

Lab splits are required when analyses must Retain be performed at a pulp for location different than analysis where samples received.

APPENDIX E – STATEMENT OF COSTS

Item Payable Invoice Cost

Drilling Geotech Drilling Services Ltd. 3787 $120,270.35

Mob/Demob/ Heli Support Yellowhead Helicopters Ltd. various $ 71,000.00

Geological Childs and Associates LLP 08-1 $ 5,159.93

Geo Mob/Demob Return flight Georgia, USA $ 650.00

Report Childs and Associates LLP 08-2 $ 5,000.00 Accurate Mining Services 08-09-30 $ 351.75

Total 2008 Costs $202,432.03

Total Person Days = 62.5*

*Does not include standby time

NOTE: Only $68,000 of the total expended was applied to these assessment reporting events APPENDIX F – TENURE LISTING

Tenure No Claim Name Owner Good To Date Are a 559341 CROW 1 145798 (100%) 2009/may/28 476.023 559342 CROW 2 145798 (100%) 2009/may/28 476.044 559343 CROW 3 145798 (100%) 2009/may/28 476.047 559344 CROW 4 145798 (100%) 2009/may/28 475.966 559350 CROW 5 145798 (100%) 2009/may/28 456.838 559351 CROW 6 145798 (100%) 2009/may/28 114.204 559352 CROW 7 145798 (100%) 2009/may/28 476.021 559356 CROW 8 145798 (100%) 2009/may/28 190.34 559357 CROW 9 145798 (100%) 2009/may/28 475.678 559358 CROW 10 145798 (100%) 2009/may/28 475.68 559360 CROW 11 145798 (100%) 2009/may/28 475.704 559361 CROW 12 145798 (100%) 2009/may/28 475.707 559364 CROW 13 145798 (100%) 2009/may/28 475.722 559367 CROW 14 145798 (100%) 2009/may/28 475.746 559368 CROW 15 145798 (100%) 2009/may/28 475.478 559372 CROW 16 145798 (100%) 2009/may/28 475.223 559379 CROW 17 145798 (100%) 2009/may/28 475.5 559381 CROW 18 145798 (100%) 2009/may/28 475.242 559382 CROW 19 145798 (100%) 2009/may/28 456.602 559383 CROW 20 145798 (100%) 2009/may/28 456.314 559385 CROW 21 145798 (100%) 2009/may/28 456.0 559416 CROW 22 145798 (100%) 2009/may/29 474.97 559417 CROW 23 145798 (100%) 2009/may/29 474.956 559419 CROW 24 145798 (100%) 2009/may/29 474.994 559420 CROW 25 145798 (100%) 2009/may/29 475.015 559421 CROW 26 145798 (100%) 2009/may/29 474.762 559429 CROW 28 145798 (100%) 2009/may/29 474.771 559430 CROW 29 145798 (100%) 2009/may/29 474.833 559431 CROW 30 145798 (100%) 2009/may/29 455.601 559432 CROW 31 145798 (100%) 2009/may/29 475.025 559433 CROW 32 145798 (100%) 2009/may/29 475.289 559435 CROW 33 145798 (100%) 2009/may/29 475.282 559437 CROW 34 145798 (100%) 2009/may/29 475.264 559438 CROW 35 145798 (100%) 2009/may/28 475.523 559446 CROW 36 145798 (100%) 2009/may/29 475.069 559450 CROW 37 145798 (100%) 2009/may/28 171.176 559643 CROW 38 145798 (100%) 2009/may/28 114.147 566881 CROW 27 145798 (100%) 2009/may/28 474.739