Torch River Resources Molybdenum Copper Rhenium Exploration

Mount Copeland

Mt. Copeland Past Producing High Grade Molybdenum Property

The Mount Copeland deposit lies within metamorphic rocks flanking the southern margin of Frenchman Cap Dome, 32 kilometers northwest of Revelstoke, British Columbia. The rocks have been metamorphosed and subjected to three phases of deformation. Lenses of syenite pegmatite and syenite aplite are common along the northern border of the nepheline syenite unit, and because of their concentrations of molybdenite, are the focus of economic interest. During the life of the Mount Copeland mine (1970-1974) almost all production was from these aplite-pegmatite bodies within the syenite gneisses, more specifically the Glacier zone, which was up to 3 meters thick and exposed for 121 meters along a strike length of over 1 kilometer. The object of Torch River Resources exploration efforts will be to attempt to find a repeat of the Glacier zone, which produced 163,278 tonnes grading 1.1 percent molybdenum.

Mount Copeland Technical Report

March 16, 2009

View Photos Of Mt Copeland

Photo #1 Mount Copeland Glacier Zone 1

Photo #2 Mount Copeland Glacier Zone 3

Photo #3 Mount Copeland Looking South At Old Mill Site

Photo #4 Mount Copeland

Photo #5 Mount Copeland

TSX Venture - TCR

Frankfurt - WNF

Pink Sheets - TORVF

The Mount Copeland Property featured underground production (1970-73) which produced 169,729 tonnes and recovered 2,625,073 pounds of molybdenum (0.7% recovered Mo). When the Mount Copeland Property was in production in 1970 development work indicated 163,340 tonnes of ore at a grade of 1.83% MoS2 (or 1.1 % molybdenum). The ore indicated prior to mining has been essentially extracted.