Cariboo Plateau
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The Cariboo Plateau is a
volcanic plateau A volcanic plateau is a plateau produced by volcanic activity. There are two main types: lava plateaus and pyroclastic plateaus. Lava plateau Lava plateaus are formed by highly fluid basaltic lava during numerous successive eruptions thro ...
in south-central
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 ...
. It is part of the Fraser Plateau which is a northward extension of the North American Plateau. The southern limit of the plateau is the Bonaparte River although some definitions include the
Bonaparte Plateau The Bonaparte Plateau, in British Columbia, Canada, is a sub-plateau of the Thompson Plateau which extends to the Quesnel River and lies between the Cariboo Mountains on the east and the Fraser River on the west. The Thompson Plateau is itself ...
between that river and the Thompson, but it properly is a subdivision of the
Thompson Plateau The Thompson Plateau forms the southern portion of the Interior Plateau of British Columbia, Canada, lying to the west of Okanagan Lake, south of the Thompson River and east of (although never adjoining it) the Fraser River. At its most southern ...
. The portion of the Fraser Plateau west of the Fraser River is properly known as the Chilcotin Plateau but is often mistakenly considered to be part of the Cariboo Plateau, which is east of the Fraser. As a region and historical identity, the Cariboo is sometimes considered to extend to the
Thompson River The Thompson River is the largest tributary of the Fraser River, flowing through the south-central portion of British Columbia, Canada. The Thompson River has two main branches, the South Thompson River and the North Thompson River. The river ...
to the south of that, and to border on the city of
Kamloops Kamloops ( ) is a city in south-central British Columbia, Canada, at the confluence of the North Thompson River, North and South Thompson Rivers, which join to become the Thompson River in Kamloops, and east of Kamloops Lake. The city is the ad ...
at its southeastern corner and even as far as Lytton, at the confluence of the Fraser and Thompson Rivers. The town of
Lillooet Lillooet () is a district municipality in the Squamish-Lillooet region of southwestern British Columbia. The town is on the west shore of the Fraser River immediately north of the Seton River mouth. On BC Highway 99, the locality is by road abo ...
is generally considered to be in the Cariboo, while the Bridge River Country to its west was sometimes referred to as the West Cariboo, as were also the ranches along the west side of the Fraser northwards towards the Gang Ranch. Broader meanings of "the Cariboo" sometimes include the Chilcotin, west of the Fraser. The geographic region known as the Quesnel Highland, which forms a mountainous series of foothills between the plateau proper and the Cariboo Mountains, is likewise considered to be part of the Cariboo in a cultural-historical sense – not the least because it is the location of the famous Cariboo goldfields and the one-time economic capital of the Interior of British Columbia, Barkerville. The Cariboo is commonly divided into North Cariboo, Central Cariboo and South Cariboo. The commercial centre of the north is Quesnel, of the central Williams Lake and of the south 100 Mile House. The Cariboo region is generally considered to reach as far southeast as the city of
Kamloops Kamloops ( ) is a city in south-central British Columbia, Canada, at the confluence of the North Thompson River, North and South Thompson Rivers, which join to become the Thompson River in Kamloops, and east of Kamloops Lake. The city is the ad ...
and to include the Cache Creek and
Lillooet Lillooet () is a district municipality in the Squamish-Lillooet region of southwestern British Columbia. The town is on the west shore of the Fraser River immediately north of the Seton River mouth. On BC Highway 99, the locality is by road abo ...
areas in the south. The region west of the
Fraser River The Fraser River () is the longest river within British Columbia, Canada, rising at Fraser Pass near Blackrock Mountain (Canada), Blackrock Mountain in the Rocky Mountains and flowing for , into the Strait of Georgia just south of the City of V ...
north of Lillooet, the Chilcotin, is often considered to be a part of the Cariboo; the country south of it immediately west of
Lillooet Lillooet () is a district municipality in the Squamish-Lillooet region of southwestern British Columbia. The town is on the west shore of the Fraser River immediately north of the Seton River mouth. On BC Highway 99, the locality is by road abo ...
is sometimes referred to as the West Cariboo. The Cariboo Plateau is made of Late
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 ...
flood basalt A flood basalt (or plateau basalt) is the result of a giant volcanic eruption or series of eruptions that covers large stretches of land or the ocean floor with basalt lava. Many flood basalts have been attributed to the onset of a hotspot (geolo ...
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 of the Chilcotin Group, a group of related
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 ...
s that is nearly parallel with the Fraser Plateau.National Resources Canada - Catalogue of Canadian volcanoes: Chilcotin Plateau basalts
Retrieved on 2008-06-26
It extends along the adjacent
Garibaldi Volcanic Belt The Garibaldi Volcanic Belt is a northwest–southeast trending volcanic chain in the Pacific Ranges of the Coast Mountains that extends from Watts Point in the south to the Ha-Iltzuk Icefield in the north. This chain of volcanoes is located in s ...
in 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 ...
. Volcanism of the Cariboo Plateau is considered to be a result of extension of the crust behind the coastal Cascadia subduction zone. The Last Chance Lake and the Goodenough Lake beside it in the
Bonaparte Plateau The Bonaparte Plateau, in British Columbia, Canada, is a sub-plateau of the Thompson Plateau which extends to the Quesnel River and lies between the Cariboo Mountains on the east and the Fraser River on the west. The Thompson Plateau is itself ...
, as well as the Probe Lake and the Deer Lake in the Cariboo Plateau, are
soda lake A soda lake or alkaline lake is a lake on the strongly base (chemistry), basic side of neutrality, typically with a pH, pH value between 9 and 12. They are characterized by high concentrations of carbonate salts, typically sodium carbonate (and ...
s. Important events in the history of the Cariboo region: * The
Cariboo Gold Rush The Cariboo Gold Rush was a gold rush in the Colony of British Columbia, which later became the Canadian province of British Columbia. The first gold discovery was made at Hills Bar in 1858, followed by more strikes in 1859 on the Horsefly Ri ...
* The building of the Cariboo Wagon Road * The Chilcotin War of 1864 '' The Cariboo Trail'' is a
1950 Events January * January 1 – The International Police Association (IPA) – the largest police organization in the world – is formed. * January 5 – 1950 Sverdlovsk plane crash, Sverdlovsk plane crash: ''Aeroflot'' Lisunov Li-2 ...
film A film, also known as a movie or motion picture, is a work of visual art that simulates experiences and otherwise communicates ideas, stories, perceptions, emotions, or atmosphere through the use of moving images that are generally, sinc ...
about the gold rush era of the 1890s in the area. The film is based on a story by John Rhodes Sturdy, screenplay by Frank Gruber, directed by Edwin L. Marin, and starring
Randolph Scott George Randolph Scott (January 23, 1898 – March 2, 1987) was an American film actor, whose Hollywood career spanned from 1928 to 1962. As a leading man for all but the first three years of his cinematic career, Scott appeared in dramas, come ...
and Gabby Hayes. Bowron Lake Provincial Park is a popular
canoe A canoe is a lightweight, narrow watercraft, water vessel, typically pointed at both ends and open on top, propelled by one or more seated or kneeling paddlers facing the direction of travel and using paddles. In British English, the term ' ...
ing destination in the Cariboo Mountains east of Quesnel. Wells Gray Park to its south is partly in the Cariboo.


See also

*
Cariboo The Cariboo is an intermontane region of British Columbia, Canada, centered on a plateau stretching from Fraser Canyon to the Cariboo Mountains. The name is a reference to the Caribou (North America), caribou that were once abundant in the reg ...
* Volcanism in Canada


References

{{Plateaus and highlands of British Columbia , state= expanded Interior Plateau Volcanism of British Columbia Lava plateaus Miocene volcanism Flood basalts Landforms of the Cariboo Plateaus of British Columbia