Chasm Provincial Park
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Chasm Provincial Park
Chasm Provincial Park is a provincial park in British Columbia, Canada, located near the town of Clinton. Expanded to in 1995, the park was originally created in 1940 to preserve and promote a feature known as the Painted Chasm, or simply The Chasm, a gorge created from melting glacial waters eroding a lava plateau over a 10 million year span called the Chilcotin Group. The walls of the Chasm contain tones of red, brown yellow, and purple and are an average of in height. The Chasm is approximately wide and long, and lies adjacent to the route of the Cariboo Road, which lines the northern apex of the Chasm alongside the Canadian National Railway line. In addition to the park upland areas of ponderosa pine, marshes and lakes are included in the park's boundaries. Wildlife Wildlife found in the park includes bighorn sheep, moose, mule deer, black bear, coyote, small mammals, songbirds and birds of prey. Images File:Chasm Provincial Park trees and flood basalts.jpg, Mult ...
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Clinton, British Columbia
Clinton is a village in British Columbia, Canada, located approximately northwest of Cache Creek and 30 km south of 70 Mile House. It is considered by some to straddle the southern edge of the Cariboo country of British Columbia, although others consider Ashcroft-Cache Creek, Lillooet, Savona, Kamloops and even Lytton and Spences Bridge to be in the Cariboo. Clinton, however, does sit immediately below the southern edge of the Cariboo Plateau. Clinton has a number of attractions including horse-back riding, big game viewing, hiking, fishing and other outdoor activities. Every May, Clinton is home to the Annual Ball held on the Victoria Day weekend, where many people dress as the first settlers did. The Annual Ball kicks off the Village's Heritage week with the parade and the May rodeo and dance ending Heritage week. The Clinton Annual Ball is one of British Columbia's oldest continual events having first been held in 1867 and was a highlight of the social calendar in the ...
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Canadian National Railway
The Canadian National Railway Company (french: Compagnie des chemins de fer nationaux du Canada) is a Canadian Class I freight railway headquartered in Montreal, Quebec, which serves Canada and the Midwestern and Southern United States. CN is Canada's largest railway, in terms of both revenue and the physical size of its rail network, spanning Canada from the Atlantic coast in Nova Scotia to the Pacific coast in British Columbia across approximately of track. In the late 20th century, CN gained extensive capacity in the United States by taking over such railroads as the Illinois Central. CN is a public company with 22,600 employees, and it has a market cap of approximately CA$90 billion. CN was government-owned, having been a Canadian Crown corporation from its founding in 1919 until being privatized in 1995. , Bill Gates is the largest single shareholder of CN stock, owning a 14.2% interest through Cascade Investment and his own Bill and Melinda Gates Foundation. Fr ...
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Bonaparte Country
Bonaparte Provincial Park is an 11,811 hectare provincial park in British Columbia, Canada. It is located within the Bonaparte Plateau. History The park was established April 30, 1996 under the Kamloops Land and Resource Management Plan (LRMP) through the Environment and Land Use Act. First nations use of the land is not well known. More recently it had been used as a ranchland by settlers and for fly in tourism. Prior to the development of the park a moratoria had been placed on timber harvesting in the area in 1974. Geology The park has many small hills formed by lava flow. This has led to the over 50 small interconnected lakes located within the park. Geography The park is located 55 kilometers northwest of Kamloops. Motorized vehicle access is most easily obtained via Jamieson Creek Road. Park Boundaries The Southern boundary of the park is formed by the Hiakwah-Shelley Lake chain. To the east are tree farm license lands. To the north and west are Provin ...
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Landforms Of The Cariboo
A landform is a natural or anthropogenic land feature on the solid surface of the Earth or other planetary body. Landforms together make up a given terrain, and their arrangement in the landscape is known as topography. Landforms include hills, mountains, canyons, and valleys, as well as shoreline features such as bays, peninsulas, and seas, including submerged features such as mid-ocean ridges, volcanoes, and the great ocean basins. Physical characteristics Landforms are categorized by characteristic physical attributes such as elevation, slope, orientation, Stratum, stratification, rock exposure and soil type. Gross physical features or landforms include intuitive elements such as berms, mounds, hills, ridges, cliffs, valleys, rivers, peninsulas, volcanoes, and numerous other structural and size-scaled (e.g. ponds vs. lakes, hills vs. mountains) elements including various kinds of inland and oceanic Waterbody, waterbodies and sub-surface features. Mountains, hills, Plateau, plat ...
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Geography Of The Cariboo
Geography (from Greek: , ''geographia''. Combination of Greek words ‘Geo’ (The Earth) and ‘Graphien’ (to describe), literally "earth description") is a field of science devoted to the study of the lands, features, inhabitants, and phenomena of Earth. The first recorded use of the word γεωγραφία was as a title of a book by Greek scholar Eratosthenes (276–194 BC). Geography is an all-encompassing discipline that seeks an understanding of Earth and its human and natural complexities—not merely where objects are, but also how they have changed and come to be. While geography is specific to Earth, many concepts can be applied more broadly to other celestial bodies in the field of planetary science. One such concept, the first law of geography, proposed by Waldo Tobler, is "everything is related to everything else, but near things are more related than distant things." Geography has been called "the world discipline" and "the bridge between the human and ...
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Canyons And Gorges Of British Columbia
A canyon (from ; archaic British English spelling: ''cañon''), or gorge, is a deep cleft between escarpments or cliffs resulting from weathering and the erosive activity of a river over geologic time scales. Rivers have a natural tendency to cut through underlying surfaces, eventually wearing away rock layers as sediments are removed downstream. A river bed will gradually reach a baseline elevation, which is the same elevation as the body of water into which the river drains. The processes of weathering and erosion will form canyons when the river's headwaters and estuary are at significantly different elevations, particularly through regions where softer rock layers are intermingled with harder layers more resistant to weathering. A canyon may also refer to a rift between two mountain peaks, such as those in ranges including the Rocky Mountains, the Alps, the Himalayas or the Andes. Usually, a river or stream carves out such splits between mountains. Examples of mountain-type c ...
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Provincial Parks Of British Columbia
Provincial may refer to: Government & Administration * Provincial capitals, an administrative sub-national capital of a country * Provincial city (other) * Provincial minister (other) * Provincial Secretary, a position in Canadian government * Member of Provincial Parliament (other), a title for legislators in Ontario, Canada as well as Eastern Cape Province, South Africa. * Provincial council (other), various meanings * Sub-provincial city in the People's Republic of China Companies * The Provincial sector of British Rail, which was later renamed Regional Railways * Provincial Airlines, a Canadian airline * Provincial Insurance Company, a former insurance company in the United Kingdom Other Uses * Provincial Osorno, a football club from Chile * Provincial examinations, a school-leaving exam in British Columbia, Canada * A provincial superior of a religious order * Provincial park, the equivalent of national parks in the Canadian province ...
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Frederick Dally
Frederick Dally (July 29, 1838 – July 28, 1914) was an English Canadian portrait and landscape photographer best known for his views of the Cariboo goldfields in British Columbia. Early life and Victoria He was born on July 29, 1838, in Southwark, a district of London, England, the youngest of nine children. Educated at Christ's Hospital, London, he served an apprenticeship with a linen and woollen draper.Roy-Sole (2008), p.59. At the age of 24, Dally emigrated to Canada, arriving in Victoria on the Colony of Vancouver Island in September 1862. He opened up a dry goods store, and a few years later he sold his stock and set up a photographic gallery in June 1866.Greenhill (1965), p.55. His commissions for photography in Victoria were varied, encompassing portraits of prominent citizens, public buildings, and street scenes, and he sometimes took pictures at the request of the Colonial Office. He also documented the presence of the government and that of the Royal Navy. An acquai ...
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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 reaching the surface of the earth via a mantle plume. Flood basalt provinces such as the Deccan Traps of India are often called '' traps'', after the Swedish word ''trappa'' (meaning "staircase"), due to the characteristic stairstep geomorphology of many associated landscapes. Michael R. Rampino and Richard Stothers (1988) cited eleven distinct flood basalt episodes occurring in the past 250 million years, creating large igneous provinces, lava plateaus, and mountain ranges. However, more have been recognized such as the large Ontong Java Plateau, and the Chilcotin Group, though the latter may be linked to the Columbia River Basalt Group. Large igneous provinces have been connected to five mass extinction events, and may be associated with b ...
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Cariboo Road
The Cariboo Road (also called the Cariboo Wagon Road, the Great North Road or the Queen's Highway) was a project initiated in 1860 by the Governor of the Colony of British Columbia, James Douglas. It involved a feat of engineering stretching from Fort Yale to Barkerville, B.C. through extremely hazardous canyon territory in the Interior of British Columbia. Between the 1860s and the 1880s the Cariboo Road existed in three versions as a surveyed and constructed wagon-road route. The first Cariboo Wagon Road surveyed in 1861 and built in 1862 followed the original Hudson's Bay Company's Harrison Trail (Port Douglas) route from Lillooet to Clinton, 70 Mile House, 100 Mile House, Lac La Hache, 150 Mile House to the contract end around Soda Creek and Alexandria at the doorstep of the Cariboo Gold Fields. The second Cariboo Wagon Road (or Yale Cariboo Road) operated during the period of the fast stage-coaches and freight-wagon companies headquartered in Yale: 1865 to 1885. Fr ...
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Erosion
Erosion is the action of surface processes (such as water flow or wind) that removes soil, rock, or dissolved material from one location on the Earth's crust, and then transports it to another location where it is deposited. Erosion is distinct from weathering which involves no movement. Removal of rock or soil as clastic sediment is referred to as ''physical'' or ''mechanical'' erosion; this contrasts with ''chemical'' erosion, where soil or rock material is removed from an area by dissolution. Eroded sediment or solutes may be transported just a few millimetres, or for thousands of kilometres. Agents of erosion include rainfall; bedrock wear in rivers; coastal erosion by the sea and waves; glacial plucking, abrasion, and scour; areal flooding; wind abrasion; groundwater processes; and mass movement processes in steep landscapes like landslides and debris flows. The rates at which such processes act control how fast a surface is eroded. Typically, physical erosion procee ...
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Chilcotin Group
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. Predominantly, during Miocene and Pliocene times, a medium-sized volcanic field of overlapping vents occurred in British Columbia's Interior Plateau. The distribution is assumed to engulf up to 50,000 km2 of the Pacific Northwest, forming a medium-sized large igneous province, of volume 3300 km3.Regional stratigraphy and age of Chilcotin Group basalts, south-central British Columbia
Retrieved on 2012-09-22 Volcanism occurred as late as Oligocene time, but continues sporadically up to present. Eruptions were most vigorous 6- ...
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