Approx 6,000 acres. ARIS reports 3725, 3940, 14749 Located in Southeast British Columbia, situated near the headwaters of Albert Creek, between Justice Glacier and Primrose Icefield 36km E of Revelstoke and south of Canyon Hotsprings. The property is host to a potentially enormous deposit of tungsten with skarn areas over 6000 acres and complimentary values in Mo/Co/Zn. Possible values in Au and Ag hosted by polymetallic quartz veins. Tungsten Valley covers 5 minfile documented occurrences: 082N036 Tungsten Prospect: The Ice occurrence area is underlain by a highly siliceous and complexly interlayered sequence of Lower Cambrian and younger Lardeau Group metasediments consisting of quartzites, quartz biotite schists, quartz muscovite schists, biotite schists and minor thin lenses of impure siliceous marble. Early and/or mid-Cretaceous intrusive stocks are poorly exposed on the eastern and western extremities of the occurrence area. Mineralization occurs in the form of low-grade scheelite and minor wolframite on fracture planes primarily hosted in quartzite. The scheelite occurs as coarse platy masses up to 1.2cm in diameter and is extremely friable and is relatively abundant on fractures striking north and dipping approximately 30° W. Scheelite-bearing fractures, on average, are approximately 0.3 to 0.6m apart. Night lamping has outlined a scheelite-bearing zone in quartzite that is approximately 4.5-12.1m wide extending 426m in a north-south direction. Seven rock grab samples assayed from 0.03-0.64% WO3 and averaged 0.2% WO3. 082N037 Tungsten Molybdenum Showing 082N038 Tungsten Zinc Showing 082N039 Tungsten Showing 082N040 Tungsten Copper Molybdenum Showing. Latitude 51°02' Longitude 117°45' $250,000 + 2% NSR JV or option

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