The Shortliff Lake Property located in western Nova Scotia is primarily a base-metal (Copper, Zinc,Silver), fault related skarn target. Recent IP surveys (2007-2008) have identified a laterally extensive (minimum 3 km) chargeability anomaly (approximately 250 meters depth) up-ice of previously discovered sulphide bearing, hematitic and siliceous sediment breccia float that occur over the same distance (approximately 3 km). Boulders contained 0.5 - 29% Copper, 0.13% lead and up to 5 oz/ton silver. Similar rock types were intersected in a few shallow drill holes by Shell (1980) in wide alteration zones (9 -- 22 meters thick) of argillic limestones of the Lower Devonian, Torbrook Formation near the contact aureole of the South Mountain granite. The area is underlain by highly favourable geology for mineralization including, limestone host rocks, major fault systems and nearby metal-generating granitiod intrusions.
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