Fraser Plateau
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The Fraser Plateau is an intermontane plateau. It is one of the main subdivisions of the Interior Plateau located in the
Central Interior of British Columbia Central is an adjective usually referring to being in the center of some place or (mathematical) object. Central may also refer to: Directions and generalised locations * Central Africa, a region in the centre of Africa continent, also known as ...
.


Geography

The region includes the Cariboo Plateau and Chilcotin Plateau, and the adjoining
Marble Marble is a metamorphic rock consisting of carbonate minerals (most commonly calcite (CaCO3) or Dolomite (mineral), dolomite (CaMg(CO3)2) that have recrystallized under the influence of heat and pressure. It has a crystalline texture, and is ty ...
, Clear and
Camelsfoot Range The Camelsfoot Range is a sub-range of the Chilcotin Ranges subdivision of the Pacific Ranges of the Coast Mountains in British Columbia. The Fraser River forms its eastern boundary. The range is approximately 90 km at its maximum length ...
s on its southwestern edge. It is defined as lying between the Bonaparte River on its southeast, beyond which is the Bonaparte or Kamloops Plateau, part of the Thompson Plateau, and by a line formed by the Dean and West Road Rivers on its northwest (the Nechako Plateau lies to the north of the West Road). Also included in the Fraser Plateau are the Itcha and
Ilgachuz Range The Ilgachuz Range is a name given to an extinct volcano, extinct shield volcano in British Columbia, Canada. It is not a mountain range in the normal sense, because it was formed as a single volcano that has been erosion, eroded for the past 5 mi ...
s and the adjoining Rainbow Range, which adjoin the
Coast Mountains The Coast Mountains () are a major mountain range in the Pacific Coast Ranges of western North America, extending from southwestern Yukon through the Alaska Panhandle and virtually all of the British Columbia Coast, Coast of British Columbia sout ...
.


Geology

The Fraser Plateau consists of
basalt Basalt (; ) is an aphanite, aphanitic (fine-grained) extrusive igneous rock formed from the rapid cooling of low-viscosity lava rich in magnesium and iron (mafic lava) exposed at or very near the planetary surface, surface of a terrestrial ...
ic lava of the Chilcotin Group, a group of related volcanic rocks that is nearly parallel with the Fraser Plateau.Chasm and Dog Creek lithofacies, Chilcotin Group basalt, Bonaparte Lake map area, British Columbia
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See also

* Fraser Plateau and Basin complex (WWF ecoregion)


Notes


References

* *''Landforms of British Columbia'', S. Holland, BC Govt publication, 1976 Interior Plateau Central Interior of British Columbia Plateaus of British Columbia Lava plateaus Volcanism of British Columbia Back-arc volcanism Fraser River {{BritishColumbiaInterior-geo-stub