Rainbow Range (Chilcotin Plateau)
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The Rainbow Range, formerly gazetted as the Rainbow Mountains, is a
mountain range A mountain range or hill range is a series of mountains or hills arranged in a line and connected by high ground. A mountain system or mountain belt is a group of mountain ranges with similarity in form, structure, and alignment that have aris ...
in
British Columbia British Columbia is the westernmost Provinces and territories of Canada, province of Canada. Situated in the Pacific Northwest between the Pacific Ocean and the Rocky Mountains, the province has a diverse geography, with rugged landscapes that ...
,
Canada Canada is a country in North America. Its Provinces and territories of Canada, ten provinces and three territories extend from the Atlantic Ocean to the Pacific Ocean and northward into the Arctic Ocean, making it the world's List of coun ...
, located northwest of Anahim Lake. Located on the western edge of the
Chilcotin Plateau The Chilcotin Plateau is part of the Fraser Plateau, a major subdivision of the Interior Plateau of British Columbia. The Chilcotin Plateau is physically near-identical with the region of the same name, i.e. "the Chilcotin", which lies between ...
, the range adjoins 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 ...
Pacific Ranges The Pacific Ranges are the southernmost subdivision of the Coast Mountains portion of the Pacific Cordillera. Located entirely within British Columbia, British Columbia, Canada, they run northwest from the lower stretches of the Fraser River to B ...
to the south, and the
Kitimat Ranges The Kitimat Ranges are one of the three main subdivisions of the Coast Mountains in British Columbia, Canada, the others being the Pacific Ranges to the south and the Boundary Ranges to the north. Geography The Kitimat Ranges lie between the Na ...
to the north. In some classification systems it is considered part of the Coast Mountains. It lies north of the Bella Coola and
Atnarko River Atnarko River is a river in the Canadian province of British Columbia British Columbia is the westernmost Provinces and territories of Canada, province of Canada. Situated in the Pacific Northwest between the Pacific Ocean and the Rocky Mo ...
s and south and west of the Dean River, which curves around its north flank, and is relatively drier in climate and easier of terrain than more mountainous areas immediately west. Once called Tsitsutl, meaning "rainbow mountains" in the Ulkatcho dialect of the
Carrier language The Dakelh () or Carrier language is a Northern Athabaskan language. It is named after the Dakelh people, a First Nations people of the Central Interior of British Columbia, Canada, for whom Carrier has been a common English name derived from F ...
, that name is now the name of the range's highest peak.


Geology

The Rainbow Range is an eight-million-year-old (
Miocene The Miocene ( ) is the first epoch (geology), geological epoch of the Neogene Period and extends from about (Ma). The Miocene was named by Scottish geologist Charles Lyell; the name comes from the Greek words (', "less") and (', "new") and mea ...
) massive
peralkaline Peralkaline rocks include those igneous rocks which have a deficiency of aluminium such that sodium and potassium are in excess of that needed for feldspar. The presence of aegerine (sodium pyroxene) and riebeckite (sodium amphibole) are indicat ...
shield volcano A shield volcano is a type of volcano named for its low profile, resembling a shield lying on the ground. It is formed by the eruption of highly fluid (low viscosity) lava, which travels farther and forms thinner flows than the more viscous lava ...
in the Anahim Volcanic Belt which includes the lower but similar 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. The shield has a diameter of is now heavily eroded by
glacier A glacier (; or ) is a persistent body of dense ice, a form of rock, that is constantly moving downhill under its own weight. A glacier forms where the accumulation of snow exceeds its ablation over many years, often centuries. It acquires ...
s carving into the
volcanic rock Volcanic rocks (often shortened to volcanics in scientific contexts) are rocks formed from lava erupted from a volcano. Like all rock types, the concept of volcanic rock is artificial, and in nature volcanic rocks grade into hypabyssal and me ...
and
sand Sand is a granular material composed of finely divided mineral particles. Sand has various compositions but is usually defined by its grain size. Sand grains are smaller than gravel and coarser than silt. Sand can also refer to a textural ...
s over millions of years. The volcanism that created the shield is not well studied and is poorly understood. It is thought to be the result of the North American Plate passing over a hotspot, similar to the one feeding the
Hawaiian Islands The Hawaiian Islands () are an archipelago of eight major volcanic islands, several atolls, and numerous smaller islets in the Pacific Ocean, North Pacific Ocean, extending some from the Hawaii (island), island of Hawaii in the south to nort ...
, known as the
Anahim hotspot The Anahim hotspot is a hypothesized hotspot in the Central Interior of British Columbia, Canada. It has been proposed as the candidate source for volcanism in the Anahim Volcanic Belt, a long chain of volcanoes and other magmatic features th ...
. The only real separate volcanic peak associated with the Rainbow Range is Anahim Peak which sits on its northeast flank. Other peaks in the range are other high eroded remnants of the shield, including Beef Peak, TaiaTaeszi Peak, Mount MacKenzie and Tsitsutl Peak , which is the highest summit of the Rainbow Range. The range gets its name from the intense and varied colours of its terrains' volcanic
lava Lava is molten or partially molten rock (magma) that has been expelled from the interior of a terrestrial planet (such as Earth) or a Natural satellite, moon onto its surface. Lava may be erupted at a volcano or through a Fissure vent, fractu ...
s and sands from heavy mineralization, like the
Spectrum Range The Spectrum Range, formerly gazetted as the Spectrum Mountains and the Rainbow Mountains, is a small mountain range in Cassiar Land District of northwestern British Columbia, Canada. Located at the southern end of the Tahltan Highland, it bord ...
in the Spatsizi Plateau.


Tweedsmuir South Provincial Park

The Rainbow Range lies partly in the Tweedsmuir South Provincial Park, while to its east the Itcha and Ilgachuz Ranges form the core of the Itcha Ilgachuz Provincial Park.


See also

*
List of volcanoes in Canada List of volcanoes in Canada is an incomplete list of volcanoes found in Geography of Canada, mainland Canada, in the Islands of Canada, Canadian islands and in Canadian waters. All but two Provinces of Canada, provinces, Prince Edward Island and ...
*
Volcanism of Western Canada Volcanism of Western Canada has produced lava flows, lava plateaus, lava domes, cinder cones, stratovolcanoes, shield volcanoes, greenstone belts, submarine volcanoes, calderas, diatremes and maars, along with examples of more less common volca ...
* Rainbow Range (Rocky Mountains) *
Spectrum Range The Spectrum Range, formerly gazetted as the Spectrum Mountains and the Rainbow Mountains, is a small mountain range in Cassiar Land District of northwestern British Columbia, Canada. Located at the southern end of the Tahltan Highland, it bord ...


References


External links


Rainbow Range entry in Canadian Mountain EncyclopediaSkiing the Pacific Ring of Fire and Beyond
{{Anahim Volcanic Belt Anahim Volcanic Belt Volcanoes of British Columbia Mountain ranges of the Interior Plateau Shield volcanoes of Canada Extinct volcanoes of North America Miocene shield volcanoes Polygenetic shield volcanoes Landforms of the Chilcotin Range 3 Coast Land District Central volcanoes Neogene British Columbia