General Copper Gold Corp
CNSX:GGLD
General Copper Gold Corp
General Copper Gold Corp. is a gold exploration company. The company is headquartered in Vancouver, British Columbia. The company went IPO on 2000-12-11. The firm has two exploration projects, the Topley Richfield Property in British Columbia and the Clark's Brook claim in Newfoundland. The Topley Richfield Property is located in the Omineca mining division of British Columbia, approximately 60 kilometers (km) east-southeast from Smithers. The property covers approximately 2,313 hectares (ha) and is comprised of seven contiguous claims. The Clark's Brook Property is located in central Newfoundland near Northwest Gander River, approximately 25 km west of the town of Glenwood. The Clark's Brook Property consists of about 31 claim units in one license for a total of approximately 770 ha. The property is underlain by wedges of limestone breccias and calcareous siltstones that are bound to the west by younger, feldspar-rich granite, and to the east by thrust-up conglomerates, sandstone, siltstone and shales of the Gander Lake Subzone.
General Copper Gold Corp. is a gold exploration company. The company is headquartered in Vancouver, British Columbia. The company went IPO on 2000-12-11. The firm has two exploration projects, the Topley Richfield Property in British Columbia and the Clark's Brook claim in Newfoundland. The Topley Richfield Property is located in the Omineca mining division of British Columbia, approximately 60 kilometers (km) east-southeast from Smithers. The property covers approximately 2,313 hectares (ha) and is comprised of seven contiguous claims. The Clark's Brook Property is located in central Newfoundland near Northwest Gander River, approximately 25 km west of the town of Glenwood. The Clark's Brook Property consists of about 31 claim units in one license for a total of approximately 770 ha. The property is underlain by wedges of limestone breccias and calcareous siltstones that are bound to the west by younger, feldspar-rich granite, and to the east by thrust-up conglomerates, sandstone, siltstone and shales of the Gander Lake Subzone.
