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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.
Geologic belts of Western 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.
Geological formation Sub-units Cruiser Formation, Goodrich Formation, Hasler Formation, Gates Formation, Moosebar Formation , Shaftesbury Formation, Peace River Formation , Spirit River Formation , Bluesky Formation , Sully Formation, Sikanni Formation, Lepine Formation, Scatter Formation, Garbutt Formation, Buckinghorse Formation
Pages in category "Geologic formations of British Columbia" The following 146 pages are in this category, out of 146 total. This list may not reflect recent changes. A.
A geologic map or geological map is a special-purpose map made to show various geological features. Rock units or geologic strata are shown by color or symbols. Bedding planes and structural features such as faults , folds , are shown with strike and dip or trend and plunge symbols which give three-dimensional orientations features.
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 ...
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