Canada One Mining Corp. completed an orientation field program on the CM1 Copper Property, a 1,054 Ha land package that was recently added to Canada One's Copper Dome Project (now totaling over 5,800 Ha). CM1 is contiguous with the Copper Dome Project, located immediately south of Hudbay Mineral's active Copper Mountain Mine near Princeton, British Columbia.

CM1 Highlights: CM1 contains geological features consistent with the distal coppery porphyry setting and has confirmed the potential for bulk copper-gold mineralization: Alteration footprint measuring at least 2.5 by 2.5 kilometers. Favorable host rocks including Nicola Group mafic volcanic rocks. Quartz-sericite-pyrite altered quartz-feldspar porphyry intrusions.

Property contains the Ox Copper Showing (disseminated chalcopyrite-magnetite). Located 4 km south of the Hudbay Mineral's producing Copper Mountain Mine (1,132 Mt @ 0.22% Cu; 0.09 g/t Au; 0.64 g/t Ag. Field Evaluation of CM1: An orientation field evaluation campaign was conducted on CM1 to examine alteration and mineralization associated with the Nicola Group volcanic rocks and younger intrusions.

A total of 26 mapping station outcrops were reviewed and together outline an alteration footprint measuring at least 2.5 x 2.5 kilometers defined by chlorite-epidote- carbonate +/- pyrite with internal zones of quartz-sericite-pyrite alteration and zones of calc-silicate skarn development. Economic Geology of CM1: CM1 is underlain by Triassic-Jurassic Nicola group basalt-andesite composition volcanic rocks which are intruded by hornblende-feldspar porphyry dikes that are interpreted to belong to the Early Jurassic Copper Mountain stock of the Copper Mountain Intrusions to the north. Recent field work has identified a large alteration footprint consisting of chlorite-epidote-carbonate-pyrite altered Nicola Group mafic fragmental volcanic rocks.

Locally, carbonate-rich sedimentary rocks internal to the Nicola Group are altered to calc-silicate skarn (garnet-pyroxene-epidote). The Property is cut by quartz feldspar porphyry dykes (diorite) which are overprinted by intense (texturally destructive) quartz-sericite-pyrite alteration and are limonitic in exposed outcrops. The Nicola Group is considered highly prospective and is host to porphyry copper-gold deposits and mines in southern British Columbia including: Copper Mountain Mine (Hudbay Minerals) immediately north of CM1; MPD Exploration/Development project north of Princeton (Kodiak Copper); New Afton active block cave mine near Kamloops (Newgold).