Mining Consultant Placer & Hardrock

Mining Consultant Placer & Hardrock

1

JAMES LEWIS

Mining Consultant – Placer & Hardrock

P.O. BOX1780, R.R. 1

CLEARWATER, B.C. VOE 1NO

CANADA

Telephone: 1-250-674-2420 Fax: 1-250-674-2424

e-mail:

August 19th 2008.

LETTER REPORT

GEOLOGICAL EVALUATION OF ALROY AND CROW CLAIMS

Resource Audit of Alroy Silica Deposit, Crescent Spur, British Columbia, Canada

ALSO

Resource Audit Crow Silica Deposit, Longworth, (Station on the CN Rail Lin e between Crescent Spur, B.C. and Prince George, B.C.) British Columbia, Canada (CN Rail Line ends at port of Prince Rupert, B.C. Canada)

1.ALROY SILICA DEPOSIT

The Deposit is located approximately 100 miles east of Prince George, B.C. It consists of 166 Claim Units each 1640 ft. x 1640 ft. in size. It is accessed via paved Provincial Highway 16 (road from Prince George, B.C.) turning north to Loos Road approximately .07 miles then onto property from the Main Gate, approximately 1.9 miles to main exposure of Silica consisting of a Ridge about 1500 feet in length, approximately 200 feet in width and about 80 ft. in height.

Samples taken by Dan Hora, B.C. Provincial Geologist in 1996, assayed from 97.39% to 98.75% Silica. The Silica Deposit dips from 47 to 88 degrees to the south-west. Some minor Iron Oxide staining (on surface) and secondary Quartz veining was noted.

Drilling and Assaying performed in 2008 produced the following Assays:

Alroy 120 ft. to 50 ft94.53% Silica

Alroy 151 ft to 85 ft.95.00% Silica

Alroy 211 ft to 59 ft.97.99% Silica

Alroy 260 ft to 100 ft.97.60% Silica

Alroy 2111 ft to 155 ft.96.28% Silica

Alroy 2156 t ft o 212 ft.96.86% Silica

This Silica Deposit is covered in the area by a thin veneer of overburden from a few inches to a few feet. The Deposit is continuous over an area of approximately 7.5 miles in length by approximately 1½ miles in width.

SUMMARY

This Deposit contains millions of tons of Silica. Example: One unit 1640 ft. x 1640 ft. would contain 11.2 million tons to a depth of 50 feet of Silica in place. A tonnage factor of 12 ft³/ton is assumed in this estimate.

Recent Core Drilling in 2008 has proven that this Deposit is significantly deeper than 50 ft. Reserves of approximately 18,592,000,000 tons of Quartz Silica are estimated in the Alroy Deposit.

The Alroy Silica Deposit (which consists of the Alroy, SDF and Mary Claims) is considered World Class in size and purity. It is located approximately 3 miles from the Canadian National (CN) Rail Main Line (north/south to the Port of Prince Rupert, B.C. The Claims are currently held by CARD JM Resources Inc. and are the subject of an Agreement between CARD JM Resources Inc. and AAFFG.

2.CROW CLAIMS

This Deposit is located at Longworth B.C. approximately 60 miles east of Prince George and is accessed by CN Rail adjoining Claims and accessed by an all-weather road from Highway 16 or from Prince George, B.C. The Claims are currently held by CARD JM Resources Inc. and are the subject of an Agreement between CARD JM Resources Inc. and AAFFG.

Drilling in 2008 on the Crow Claims produced the following Assay:

`Crow30 ft. to 130 ft.97.90% Silica

Crow140 ft. to 230 ft.98.11% Silica

Crow240 ft. to 330 ft.98.83% Silica

As noted on the Assays, this Deposit contains very low Iron ratios, example: 0.03% and 0.04% Iron.

The reserves on the 38 blocks of Crow Claims were staked by the Author on behalf of AAFFG and paid for by AAFFG on May 29, 2007. Samples were

taken personally by the Author and assayed at EcoTech Laboratory in Kamloops, B.C. on 31st July, 2007 and showed 99.69% Silica. Iron content is very low.

Assays of the Crow Claims (Longworth property) taken by the B.C. Government Geologist in 1965 (Mines and Petroleum Resources Report 1965, Page 274) states the following (in part):

This Silica Deposit consists of a thick Band of White Quartzite that extends from a Forestry Fire Tower at 5,835 ft. elevation on the mountaintop north-westward down across the face of the Mountain to about 3,700 ft. elevation. The Silica (Quartzite) Band forms a prominent line of bare bluffs across the mountainside. The Quartzite band ranges from 300 to 800 feet thick and can be traced across the mountain for more than 2 miles. The CN Rail Siding at Longworth is at the 2,200 ft. elevation……… ….

Samples taken by the B.C. Government Geologist show

99.02 Silica

99.60 Silica

99.68 Silica

The Author accessed this property by Helicopter on several occasions in 2007 and from the air the Deposit is far more massive than indicated in the 1965 B.C. Government Report. The Crow Claims contain 38 individual blocks of Claims consisting of 53,000 acres, over 800 individual units at 1640 ft. x 1640 ft. Each unit at 500 ft. of depth could produce 112 millions tons. It is estimated that overall the Crow Claims could produce 69,600,000,000 tons of Quartz Silica. This estimate has been taken at 500 ft. of depth while the B.C. Government Reports show a depth of 800 ft. The B.C. Government Min-File states 400 meters (approximately 1300 ft.) depth.

I feel that my estimate is very conservative. I feel that it is also realistic. Further drilling will more than confirm the above estimate.

It is respectfully submitted that the Crow Claims are considered a World Class Deposit in size and purity and contain one of the largest Deposits of High purity Silica known in the world today.

I am including in this Report the following reference materials:

a)Copy of page 274 of the Mines and Petroleum Resources Report for 1965 entitled “Silica – Longworth, B.C.”

b)Copy of B.C.Government Ministry of Mines MinFile Summary Report on Crow Claims at Longworth, B.C. Deposit Type: Silica Sandstone.

c)Copy of Whole Rock Certificate of Analysis AK2007-869 from EcoTech Laboratory Ltd. The sample was taken by the Author in July 2007 on behalf of AAFFG.

The Longworth Silica Deposit also contains Gold Deposits as indicated by the Geological Map produced by the B.C. Government and staked by the author for AAFFG. A copy of the Ministry of Mines Map showing the Gold deposits on the Crow claims is also enclosed.

Respectfully submitted:


James W. Lewis