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Gold/Mining/Energy : Gold and Silver Juniors, Mid-tiers and Producers

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To: LoneClone who wrote (44668)	7/12/2007 6:20:17 PM
From: E. Charters	Read Replies (1) of 78416

I have determined it is in the Overlap terrane, between the Quesnel terrane and just west of a post accretionary area and it is near or in a tertiary basin. It is in the Similkameen Okanagan region and the Kamloops administrative district. It is in the Similkameen Mining Division. It is part of the Merritt Mining region. It has Spences Bridge Group, Princeton Group, and Nicola group volcanics and sediments, which are Triassic, Cretaceous, and Eocene in age. Most volcanics are andesitic in composition. There are granodioritic rocks and dioritics to the south, as well as some granites, and some basalts. Faults and contacts run thru Princeton and around it to the North East. Some contacts to the north and south run North West. The area appears to be a regional broad tension fracture indicating a fault block is being rotated clockwise by dextral southeast movement. It is in a broad valley area with fingers extending along watersheds into the Tulameen coal measure area, along the Tulameen River and into the Okangan river. It is in the 092H map area. Relief is low for the Cordillera, between less than 1000 to 3000 ft ASL.

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