Buck Hill (British Columbia)
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Buck Hill (British Columbia)
Buck Hill is a hill in east-central British Columbia, Canada, located north of Clearwater. It rises from the west slope of Trophy Mountain. Buck Hill is just outside the boundary of Wells Gray Provincial Park. Geology Buck Hill is a cinder cone in the Wells Gray-Clearwater volcanic field. It last erupted about 10,000 years ago during the last glaciation of the Clearwater Valley. A slurry of lava debris and water flowed away from the cone and hardened in Second and Third Canyons further down Trophy Mountain. After the eruption stopped, a glacier smoothed the sides of Buck Hill. Several craters can be found on the west side. Access Buck Hill is one of the most accessible volcanoes in the Wells Gray Park area because one can drive to its base. Access is via Trophy Mountain Road off Clearwater Valley Road (also called Wells Gray Park Road), then some old logging and mining roads to some pits where recent mining for decorative lava rock has occurred. It is not safe to climb Buck Hil ...
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Shuswap Highland
The Shuswap Highland is a plateau-like hilly area of in British Columbia, Canada. It spans the upland area between the Bonaparte and Thompson Plateaus from the area of Mahood Lake, at the southeast corner of the Cariboo Plateau, southeast towards the lower Shuswap River east of Vernon in the Okanagan. The highland is not a unified range, but a combination of small uplands broken up by the valleys of the Clearwater, North Thompson and Adams Rivers and also by the lowlands in the southwest flanking Shuswap Lake. In that area of the valley are the towns of Falkland, Westwold, and Monte Creek along Highway 97. This area also includes the Spa Hills, and the other isolated pockets of hills and mini-plateaus between the Thompson Plateau proper and Shuswap Lake. The highest point of the Highland is Matterhorn Peak in the Dunn Peak massif at 2636 meters. The Shuswap Highland is in essence a foothill (or transitional) area between the much broader interior plateaus southwest and we ...
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Wells Gray-Clearwater Volcanic Field
The Wells Gray-Clearwater volcanic field, also called the Clearwater Cone Group, is a potentially active monogenetic volcanic field in east-central British Columbia, Canada, located approximately north of Kamloops. It is situated in the Cariboo Mountains of the Columbia Mountains and on the Quesnel and Shuswap Highlands. As a monogenetic volcanic field, it is a place with numerous small basaltic volcanoes and extensive lava flows. Most of the Wells Gray-Clearwater volcanic field is encompassed within a large wilderness park called Wells Gray Provincial Park. This park was established in 1939 to protect Helmcken Falls and the unique features of the Clearwater River drainage basin, including this volcanic field. Five roads enter the park and provide views of some of the field's volcanic features. Short hikes lead to several other volcanic features, but some areas are accessible only by aircraft. Geology Pleistocene epoch Based on radiocarbon and potassium-argon dating, volcan ...
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Monogenetic Cinder Cones
Monogenetic may refer to: * Monogenetic in biology, of or pertaining to monogenesis (Mendelian inheritance) * Monogenetic volcanic field in geology, a cluster of volcanoes that only erupted once * Monogenetic theory of pidgins in linguistics, a theory about the origin of creole languages See also * Monogenous (other) * Monogenic (other) Monogenic may refer to: * Monogenic signal, in the theory of analytic signals * Monogenic disorder, disease, inheritance, or trait, a single gene disorder resulting from a single mutated gene ** Monogenic diabetes, or maturity-onset diabetes of ...
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Pleistocene Volcanoes
The Pleistocene ( , often referred to as the ''Ice age'') is the geological epoch that lasted from about 2,580,000 to 11,700 years ago, spanning the Earth's most recent period of repeated glaciations. Before a change was finally confirmed in 2009 by the International Union of Geological Sciences, the cutoff of the Pleistocene and the preceding Pliocene was regarded as being 1.806 million years Before Present (BP). Publications from earlier years may use either definition of the period. The end of the Pleistocene corresponds with the end of the last glacial period and also with the end of the Paleolithic age used in archaeology. The name is a combination of Ancient Greek grc, label=none, πλεῖστος, pleīstos, most and grc, label=none, καινός, kainós (latinized as ), 'new'. At the end of the preceding Pliocene, the previously isolated North and South American continents were joined by the Isthmus of Panama, causing a faunal interchange between the two reg ...
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Wells Gray-Clearwater
Wells most commonly refers to: * Wells, Somerset, a cathedral city in Somerset, England * Well, an excavation or structure created in the ground * Wells (name) Wells may also refer to: Places Canada *Wells, British Columbia England * Wells (Priory Road) railway station was a railway station in Wells, Somerset * Wells (Tucker Street) railway station was a railway station in Wells, Somerset * Wells (UK Parliament constituency), the UK parliamentary constituency in which the city of Wells, Somerset, is located * Wells-next-the-Sea, town and port in Norfolk ** Wells-on-Sea railway station was a railway station in Wells-next-the-Sea Scotland * Wells, Roxburghshire, a Scottish feudal barony United States *Wells, California, former name of Keene, California * Wells, Indiana *Wells, Kansas *Wells, Maine *Wells, Minnesota * Wells, Mississippi *Wells, Nevada *Wells, New York, a town ** Wells (CDP), New York, a census-designated place in the town *Wells, Texas *Wells, Vermont, a New En ...
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Cinder Cones Of British Columbia
Cinder is an alternate term for scoria. Cinder or Cinders may also refer to: In computing *Cinder (programming library), a C++ programming library for visualization *Cinder, OpenStack's block storage component *Cyber Insider Threat, CINDER, a digital threat method Other uses *Ember, also called cinder * ''Cinder'' (album), by the Dirty Three *Cinder (bear), a bear rescued with burns after 2014 wildfires in Washington, United States * ''Cinders'' (1913 film), a 1913 silent film * ''Cinders'' (1920 film), a 1920 film starring Hoot Gibson * ''Cinders'' (1926 film), a 1926 British film starring Betty Balfour * ''Cinder'' (novel), a novel by Marissa Meyer ** Linh Cinder, the character from the novel and ''The Lunar Chronicles'' series *Cinder (Killer Instinct), a character in ''Killer Instinct'' * ''Cinders'' (visual novel), a 2012 visual novel adaption of Cinderella by MoaCube *Cinder toffee, a British name for honeycomb toffee *Cinder, American hard rock band formerly signed to Gef ...
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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 volcanic forms such as tuyas and subglacial mound A subglacial mound (SUGM) is a type of subglacial volcano. This type of volcano forms when lava erupts beneath a thick glacier or ice sheet. The magma forming these volcanoes was not hot enough to melt a vertical pipe right through the overlying ...s. Volcanic belts * * * * * * * * * External links Erica A. Massey: A Comparative Study of Glaciovolcanic Palagonitization of Tholeitic and Alkaline Sideromelane in Helgafell, Icland, and Wells Gray-Clearwater Volcanic Filed, BC, Canada. B.Sc., The University of British Columbia, 2014 Volcanic fields * * * See also * * * * ReferencesVolcanoes of Canada . . . . {{Manitoba-geo-stub ...
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Volcanism Of Canada
Volcanic activity is a major part of the geology of Canada and is characterized by many types of volcanic landform, including lava flows, volcanic plateaus, lava domes, cinder cones, stratovolcanoes, shield volcanoes, submarine volcanoes, calderas, diatremes, and maars, along with less common volcanic forms such as tuyas and subglacial mounds. Though Canada's volcanic history dates back to the Precambrian eon, at least 3.11 billion years ago, when its part of the North American continent began to form, volcanism continues to occur in Western and Northern Canada in modern times, where it forms part of an encircling chain of volcanoes and frequent earthquakes around the Pacific Ocean called the Pacific Ring of Fire. Because volcanoes in Western and Northern Canada are in relatively remote and sparsely populated areas and their activity is less frequent than with other volcanoes around the Pacific Ocean, Canada is commonly thought to occupy a gap in the Ring of Fire between the ...
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Spahats Creek
Spahats Creek Falls, also called Spahats Falls, is a waterfall on Spahats Creek within Wells Gray Provincial Park of British Columbia, Canada. Common references place the falls at around tall, but taking into account the second tier, it is closer to 75–80 meters tall. It is a popular stop for tourists and especially motorcoach tours since it is only off the busy Yellowhead Highway. Spahats Creek rises from snowmelt and springs at a pass between Raft Mountain and Trophy Mountain. It flows 15 km west before tumbling over Spahats Falls and entering the Clearwater River (British Columbia), Clearwater River. Spahats is the First Nations term for bear and the stream was long known as Bear Creek. When the first accurate topographical map of the Clearwater Valley was published in 1953, it labelled the stream as “Bear Creek” and the falls as “Spahats (Bear) Creek Falls”. By the late 1960s, “Spahats” had become an accepted alternative due to the large number of Bear cr ...
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Thompson Rivers University
Thompson Rivers University (commonly referred to as TRU) is a public teaching and research university offering undergraduate and graduate degrees and vocational training. Its main campus is in Kamloops, British Columbia, Canada, and its name comes from the two rivers which converge in Kamloops, the North Thompson and South Thompson. The university has a satellite campus in Williams Lake, BC and a distance education division called TRU-Open Learning. It also has several international partnerships through its TRU World division. TRU is accredited by the Northwest Commission on Colleges and Universities (NWCCU) at the associate, baccalaureate and master's degree levels. TRU offers 140 on-campus programs, including trades apprenticeships, vocational certificates and diplomas, bachelor's and master's degrees and law, and approximately 60 online or distance programs through the Open Learning division. History Kamloops, the largest population centre in the regions now known as th ...
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Clearwater River (British Columbia)
The Clearwater River is the largest tributary of the North Thompson River, joining it at the community of Clearwater, British Columbia. The Clearwater rises from glaciers in the Cariboo Mountains and flows in a mostly southerly direction for to the North Thompson. Its entire course, except the last , is within Wells Gray Provincial Park. Its confluence with the North Thompson is protected by North Thompson River Provincial Park. There are two large lakes on the Clearwater River. Hobson Lake is long and averages wide. Clearwater Lake is long and averages wide. The Clearwater's largest tributaries are (from source to mouth) Hobson Creek, Goat Creek, Lickskillet Creek, Azure River, Falls Creek, Murtle River, Mahood River, Hemp Creek, Grouse Creek, and Spahats Creek.Neave, Roland (2015). ''Exploring Wells Gray Park'', 6th edition. Wells Gray Tours, Kamloops, BC. . The river is popular for fly fishing, whitewater kayaking, whitewater rafting, hiking, and wildlife viewing. Hist ...
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Cinder Cone
A cinder cone (or scoria cone) is a steep conical hill of loose pyroclastic fragments, such as volcanic clinkers, volcanic ash, or scoria that has been built around a volcanic vent. The pyroclastic fragments are formed by explosive eruptions or lava fountains from a single, typically cylindrical, vent. As the gas-charged lava is blown violently into the air, it breaks into small fragments that solidify and fall as either cinders, clinkers, or scoria around the vent to form a cone that often is symmetrical; with slopes between 30 and 40°; and a nearly circular ground plan. Most cinder cones have a bowl-shaped crater at the summit. Mechanics of eruption Cinder cones range in size from tens to hundreds of meters tall and often have a bowl-shaped crater at the summit. They are composed of loose pyroclastic material (cinder or scoria), which distinguishes them from ''spatter cones'', which are composed of agglomerated volcanic bombs. The pyroclastic material making up a cinder ...
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