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Thompson Country
Thompson Country, also referred to as The Thompson and sometimes as the Thompson Valley and historically known as the Couteau Country or Couteau District, is a historic geographic region of the Southern Interior of British Columbia, more or less defined by the basin of the Thompson River. This is a tributary of the Fraser; the major city in the area is Kamloops. Origin and usage The term originated among Scots and English in the days of the fur trade, who described Thompson Country as lying between New Caledonia to the north and the Columbia District or Oregon Country to the south. Prior to their dominance, French traders referred to this as ''Couteau nifeCountry'' or ''Couteau District''. The Thompson nomenclature is still used today, although not as an official designation. It is often used combination forms, such as the Thompson-Okanagan or Thompson-Nicola Regional District. Weather forecasts and tourism information refer to the area as Thompson-Shuswap. Although strict ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Thompson Canyon
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 is home to several varieties of Pacific salmon and trout. The area's geological history was heavily influenced by glaciation, and the several large glacial lakes have filled the river valley over the last 12,000 years. Archaeological evidence shows human habitation in the watershed dating back at least 8,300 years. The Thompson was named by Fraser River explorer, Simon Fraser, in honour of his friend, Columbia Basin explorer David Thompson. Recreational use of the river includes whitewater rafting and angling. Geography South Thompson River The South Thompson originates at the outlet of Little Shuswap Lake at the town of Chase and flows approximately southwest through a wide valley to Kamloops where it joins the North Thompson. H ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Adams Lake
Adams Lake is a large, deep, coldwater lake in British Columbia, Canada; its average depth ranks 6th in the world. The southern end of the lake is approximately north of the town of Chase in the Shuswap Country region of British Columbia. The lake's upper reaches lie in the northern Monashee Mountains, while its lower end penetrates the Shuswap Highland. The lake supports Chinook, Sockeye and Coho salmon, Kokanee, mountain whitefish and rainbow trout. Geography The lake is long and between and wide. The surface elevation is above sea level. The lake is very deep; with a mean depth of and maximum depth of it is the second deepest lake in British Columbia (next to Quesnel Lake, which has a maximum depth of ) and 6th deepest lake in the world by mean depth. Water flows into the lake though many tributaries (most notably the Upper Adams River, , and Bush Creek). The water drains from the lake as the Lower Adams River which is home to a very large and famous s ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lillooet, British Columbia
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 about northeast of Pemberton, northwest of Lytton, and west of Kamloops. First Nations A main population centre of the Stʼatʼimc (Lillooet Nation), who comprise just over 50 per cent of the Lillooet area residents, it is one of the southernmost communities in North America where indigenous people form the majority. First Nations communities assert the land is traditional territory, having been continuously inhabited for thousands of years. The confluence of several main streams with the Fraser attracted large seasonal and permanent indigenous populations. Situated in the Lower Fountain, the Bridge River Rapids (Sat' or Setl), which blocked migrating salmon, has remained a popular fishing and fish drying site for centuries. Keatley ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kamloops Lake
Kamloops Lake in British Columbia, Canada is situated on the Thompson River just west of Kamloops. The lake is 1.6 km wide, 29 km long, and up to 152 m deep. In prehistoric time, the lake was much longer, perhaps 20x, with adjacent silt cliffs defining ancient lake bottoms 100 meters higher than present water levels. At the outlet near Savona, a large tumbled rock, gravel moraine indicates the toe of a glacier once melted away here. The community of Savona, British Columbia, Savona is located at the west end of the lake, near the Thompson River outlet. The city of Kamloops is located a few miles east of the head of the lake, at the confluence of the North Thompson River, North and South Thompson Rivers. The name, Kamloops, derives from a local Indigenous word, Tk’emlúps, meaning a meeting of waters. The lake is bounded on all sides by steep hillsides, with level areas found only near creek deltas and around the inlet. On these hills, fresh, green grass feeds h ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Savona, British Columbia
Savona (, originally Savona's Ferry) is a small community located at the west end of Kamloops Lake, where the Thompson River exits it. It is approximately halfway between Kamloops and Cache Creek along the Trans-Canada Highway. The countryside surrounding the community is semi-arid grasslands and hills, which support cattle ranching and agriculture. It has about 2000 hours of sunshine and less than 12 inches of precipitation a year. It has a population of approximately 650. It was a stagecoach stop, the location of a ferry across the Thompson River, and later moved to take advantage of the Canadian Pacific Railway built on the south side of the river. History Savona was originally located on the north shore of Kamloops Lake, where it was the end of the stagecoach line from Cache Creek on the Cariboo Wagon Road (later improved as the Trans-Canada Highway). Originally passengers continuing on to the goldfields of the Big Bend of the Columbia River had to take the steamboat up ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cascade Range
The Cascade Range or Cascades is a major mountain range of western North America, extending from southern British Columbia through Washington and Oregon to Northern California. It includes both non-volcanic mountains, such as the North Cascades, and the notable volcanoes known as the High Cascades. The small part of the range in British Columbia is referred to as the Canadian Cascades or, locally, as the Cascade Mountains. The latter term is also sometimes used by Washington residents to refer to the Washington section of the Cascades in addition to North Cascades, the more usual U.S. term, as in North Cascades National Park. The highest peak in the range is Mount Rainier in Washington at . part of the Pacific Ocean's Ring of Fire, the ring of volcanoes and associated mountains around the Pacific Ocean. All of the eruptions in the contiguous United States over the last 200 years have been from Cascade volcanoes. The two most recent were Lassen Peak from 1914 to 1921 and a ma ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Coast Mountains
The Coast Mountains (french: La chaîne Côtière) 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 Coast of British Columbia south to the Fraser River. The mountain range's name derives from its proximity to the sea coast, and it is often referred to as the Coast Range. The range includes volcanic and non-volcanic mountains and the extensive ice fields of the Pacific and Boundary Ranges, and the northern end of the volcanic system known as the Cascade Volcanoes. The Coast Mountains are part of a larger mountain system called the Pacific Coast Ranges or the Pacific Mountain System, which includes the Cascade Range, the Insular Mountains, the Olympic Mountains, the Oregon Coast Range, the California Coast Ranges, the Saint Elias Mountains and the Chugach Mountains. The Coast Mountains are also part of the American Cordilleraa Spanish term for an extensive ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rainshadow
A rain shadow is an area of significantly reduced rainfall behind a mountainous region, on the side facing away from prevailing winds, known as its leeward side. Evaporated moisture from water bodies (such as oceans and large lakes) is carried by the prevailing onshore breezes towards the drier and hotter inland areas. When encountering elevated landforms, the moist air is driven upslope towards the peak, where it expands, cools, and its moisture condenses and starts to precipitate. If the landforms are tall and wide enough, most of the humidity will be lost to precipitation over the windward side (also known as the ''rainward'' side) before ever making it past the top. As the air descends the leeward side of the landforms, it is compressed and heated, producing foehn winds that ''absorb'' moisture downslope and cast a broad "shadow" of dry climate region behind the mountain crests. This climate typically takes the form of shrub–steppe, xeric shrublands or even desert ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 point the plateau is squeezed by the mountainous terrain of the Cascade Range abutting closer to the Okanagan Valley. Its southwestern edge abuts the Canadian Cascades portion of that extensive range, more or less following the line of the Similkameen River, its tributary the Tulameen River, and a series of passes from the area of Tulameen, British Columbia to the confluence of the Thompson River with the Nicoamen River, a few kilometres (miles) east of Lytton, British Columbia, which is in the Fraser Canyon. Its northeastern edge runs approximately from the city of Vernon, British Columbia through the valley of Monte Creek to the junction of the same name just east of the city of Kamloops. Northeast of that line is the Shuswap Highland. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 a sub-plateau of the larger Fraser Plateau. Etymology The name of the plateau comes from a chief of the Shuswap people who adopted the name Bonaparte in emulation of Napoleon Bonaparte, who for some reason was popular among the First Nations of British Columbia, apparently for his reputation as a chieftain and warrior. Geography The Bonaparte Plateau lies between the Bonaparte River on the north and west, and the Thompson River on the east and south; on its northern edge is Bonaparte Lake, the largest in the locality and at the head of the Bonaparte River, near the edge of the plateau above the Thompson. Other streams draining the plateau is the Deadman River, in fur trade times known by its French name, ''Rivière Defunté'', which ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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