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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.
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 ...
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.
MapQuest offers online, mobile, business and developer solutions that help people discover and explore where they would like to go, how to get there and what to do along the way and at your destination.
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 .
British Columbia is customarily divided into three main regions, the Interior, the Coast and the Lower Mainland (though the last-named is technically part of the Coast). ). These are broken up by a loose and often overlapping system of cultural-geographic regions, often based on river basins but sometimes spannin
Geology of the Rocky Mountains (5 C, 47 P) S. Seismic faults of British Columbia (1 C, 2 P) Seismic zones of British Columbia (4 P) Stratigraphy of British Columbia ...