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Map showing geological formations related to the Canadian Cascade Arc. The Chilcotin Group, also called the Chilcotin Plateau Basalts, is a large area of basaltic lava that forms a volcanic plateau running parallel with the Garibaldi Volcanic Belt in south-central British Columbia, Canada.
The geology of British Columbia is a function of its location on the leading edge of the North American continent. The mountainous physiography and the diversity of the different types and ages of rock hint at the complex geology , which is still undergoing revision despite a century of exploration and mapping.
Superficial deposits (or surficial deposits [1]) refer to geological deposits typically of Quaternary age (less than 2.6 million years old) for the Earth. These geologically recent unconsolidated sediments may include stream channel and floodplain deposits, beach sands, talus gravels and glacial drift and moraine .
Lone Butte is located 13 km (8 mi) southeast of 100 Mile House and is immediately north of the recreational lake-community of Green Lake.The vertical structure of Lone Butte forms a prominent monument that rises more than 50 m (160 ft) above the surrounding lowlands of the Cariboo Plateau.
The Kitimat Ranges, rising behind Kitimat, British Columbia. The Kitimat Ranges lie between the Nass River and Portland Inlet in the north [2] and the Bella Coola River and Burke Channel on the south, and are bounded on their east by the Hazelton Mountains and include the mountainous islands of the North Coastal Archipelago, as well as King Island, which lies between Dean Channel and the ...
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