Properties

Northwest Copper

The Northwest Copper area covers a mineralized area of at least eight square kilometers. Geophysical surveys have defined a large magnetic anomaly in the area. Several copper-silver-gold showings occur within this anomaly. A leached cap associated with argillic hydrothermal alteration, structurally-controlled mineralization and altered hornblende-porphyry dykes is further evidence of the porphyry copper-gold potential of the area.

Charlie and Hub

Disseminated and veinlet copper and molybdenum occur at lower elevations along the Tchaikazan River and copper-bearing veins occur at higher elevations. This prospect has the potential to host two styles of mineralization: copper-molybdenum mineralization (Hub) and mesothermal to epithermal gold-silver-copper veins (Charlie). Mineralized targets are partially outlined by copper and molybdenum soil geochemical anomalies and by an arcuate IP Chargeability anomaly.

Magic Twin Area

The Magic Twin area comprises two claim blocks covering mesothermal to epithermal precious-metals veins. Arsenic-bearing veins located in Twin Creek and the quartz veins carrying copper-gold mineralization on the ridge crest to the west demonstrate this potential. The Twin Creek vein system has unexplored potential for vein extensions beneath the drift-covered valley adjacent to a major fault and intrusive contact.

Fortune

The Fortune property covers 10,138 hectares and remains largely unexplored. It covers part of the Tchaikazan fault which is thought to be a controlling structure and conduit for mineralization.

Spokane

Three showings, Spokane, Ice and Syndicate, occur within the Spokane target area. The mineralization is characterized by pyrite, pyrrhotite and chalcopyrite, which occur in veins associated with silification, sericite, and clay alteration. High copper, silver and gold assays have been reported from the area.

Battlement

The Battlement area includes the former Taylor-Windfall gold mine ("MINFILE 092O 028). This prospect is hosted by volcanic and sedimentary rocks and volcanic breccias. The area was previously explored in the mid-1980's for epithermal gold mineralization. A two square-kilometre area contains silicified and argillically altered volcanics associated with plutonic rocks, large-scale high-angle faults, and gold-bearing veins. Veins in the area contain up to 0.9 oz/ton gold and greater than 3.5 oz/ton silver.