|
Nechako Plateau
The Nechako Plateau is the northernmost subdivision of the Interior Plateau, one of the main geographic regions of the Canadian province of British Columbia. It spans the basin of the Nechako River and its tributaries the Stuart River and Endako Rivers, and is bounded on the south by the West Road River (Blackwater River), south of which is the Chilcotin Plateau and on the north by the Nation River and the valleys of Babine and Takla Lakes, beyond which are the Omineca Mountains (N) and Skeena Mountains (NW). To the west, it abuts the various ranges of the Hazelton Mountains while on its east it is bounded by the pass between Prince George, British Columbia and the Parsnip Arm of Williston Lake, beyond which is the McGregor Plateau, which skirts the Northern Rockies. Some classification systems include the plateau area on the east bank of the Fraser River beyond the city of Prince George; this area neighbours the northernmost reaches of the Quesnel Highland and Cariboo Mountains ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
British Columbia
British Columbia (commonly abbreviated as BC) is the westernmost province of Canada, situated between the Pacific Ocean and the Rocky Mountains. It has a diverse geography, with rugged landscapes that include rocky coastlines, sandy beaches, forests, lakes, mountains, inland deserts and grassy plains, and borders the province of Alberta to the east and the Yukon and Northwest Territories to the north. With an estimated population of 5.3million as of 2022, it is Canada's third-most populous province. The capital of British Columbia is Victoria and its largest city is Vancouver. Vancouver is the third-largest metropolitan area in Canada; the 2021 census recorded 2.6million people in Metro Vancouver. The first known human inhabitants of the area settled in British Columbia at least 10,000 years ago. Such groups include the Coast Salish, Tsilhqotʼin, and Haida peoples, among many others. One of the earliest British settlements in the area was Fort Victoria, established ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Williston Lake
Williston Lake is a reservoir created by the W. A. C. Bennett Dam and is located in the Northern Interior of British Columbia, Canada. Geography The lake fills the basin of the upper Peace River, backing into the Rocky Mountain Trench which is where the Parsnip and Finlay met at Finlay Forks to form the Peace. The lake includes three reaches, the Peace Reach (formerly the Peace Canyon), and the Parsnip and Finlay Reaches, which are the lowermost basins of those rivers, and covers a total area of , being the largest lake in British Columbia and the seventh largest reservoir (by volume) in the world. The reservoir is fed by the Finlay, Omineca, Ingenika, Ospika, Parsnip, Manson, Nation and Nabesche Rivers and by Clearwater Creek, Carbon Creek, and other smaller creeks. Several provincial parks are maintained on the shore of the lake, including Muscovite Lakes Provincial Park, Butler Ridge Provincial Park, Heather-Dina Lakes Provincial Park and Ed Bird-Estella Provincial Park ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sedimentary Rock
Sedimentary rocks are types of rock that are formed by the accumulation or deposition of mineral or organic particles at Earth's surface, followed by cementation. Sedimentation is the collective name for processes that cause these particles to settle in place. The particles that form a sedimentary rock are called sediment, and may be composed of geological detritus (minerals) or biological detritus (organic matter). The geological detritus originated from weathering and erosion of existing rocks, or from the solidification of molten lava blobs erupted by volcanoes. The geological detritus is transported to the place of deposition by water, wind, ice or mass movement, which are called agents of denudation. Biological detritus was formed by bodies and parts (mainly shells) of dead aquatic organisms, as well as their fecal mass, suspended in water and slowly piling up on the floor of water bodies (marine snow). Sedimentation may also occur as dissolved minerals precipitate from ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Volcanic Rock
Volcanic rock (often shortened to volcanics in scientific contexts) is a rock formed from lava erupted from a volcano. In other words, it differs from other igneous rock by being of volcanic origin. Like all rock types, the concept of volcanic rock is artificial, and in nature volcanic rocks grade into hypabyssal and metamorphic rocks and constitute an important element of some sediments and sedimentary rocks. For these reasons, in geology, volcanics and shallow hypabyssal rocks are not always treated as distinct. In the context of Precambrian shield geology, the term "volcanic" is often applied to what are strictly metavolcanic rocks. Volcanic rocks and sediment that form from magma erupted into the air are called "volcaniclastics," and these are technically sedimentary rocks. Volcanic rocks are among the most common rock types on Earth's surface, particularly in the oceans. On land, they are very common at plate boundaries and in flood basalt provinces. It has been estimated t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 moon onto its surface. Lava may be erupted at a volcano or through a fracture in the crust, on land or underwater, usually at temperatures from . The volcanic rock resulting from subsequent cooling is also often called ''lava''. A lava flow is an outpouring of lava during an effusive eruption. (An explosive eruption, by contrast, produces a mixture of volcanic ash and other fragments called tephra, not lava flows.) The viscosity of most lava is about that of ketchup, roughly 10,000 to 100,000 times that of water. Even so, lava can flow great distances before cooling causes it to solidify, because lava exposed to air quickly develops a solid crust that insulates the remaining liquid lava, helping to keep it hot and inviscid enough to continue flowing. The word ''lava'' comes from Italian and is probably derived from the Latin word ''labes ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tweedsmuir North Provincial Park And Protected Area
Tweedsmuir North Provincial Park and Protected Area is a provincial park in British Columbia, Canada, which along with Tweedsmuir South Provincial Park and Entiako Provincial Park were once part of Tweedsmuir Provincial Park, then B. C.'s largest park, located in the Coast Range. History Tweedsmuir gained park status in 1938 as the earliest large park established under the BC Parks protected areas system. Tweedsmuir North Provincial Park and Protected Area was re-designated a park and protected area as the latter classification allows resource extraction and other economic activities not permitted in full park designations. Entiako Provincial Park and Protected Area is located on the south flank of the Nechako River watercourse. Geography The northern portion of the park is a wilderness area. Access is possible via boat, using Ootsa and Whitesail Lakes. The Park is between Burns Lake and Houston. BC Parks provides this explanation: "To get from Chikamin Bay on Whitesail Lake to ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Telegraph Range
The Telegraph Range is a small hill-range located on the Nechako Plateau to the south of Ootsa Lake in the Cariboo Land District of the Central Interior of British Columbia, Canada. It was named by George M. Dawson to commemorate the route of the Collins Overland Telegraph Collins may refer to: People Surname Given name * Collins O. Bright (1917–?), Sierra Leonean diplomat * Collins Chabane (1960–2015), South African Minister of Public Service and Administration * Collins Cheboi (born 1987), Kenyan middle- ..., which lay along the range's northeast flank. The range is approximately 750 km2 in area. References Hills of British Columbia Mountain ranges of British Columbia Nechako Country {{BritishColumbia-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Quanchus Range
The Quanchus Range is a subrange of the Nechako Plateau in the Interior of British Columbia, Canada, located on the north end of Tweedsmuir North Provincial Park and Protected Area. It is almost completely an island after the creation of the Nechako Reservoir. Its two main summits are Michel Peak (2260m) and Tweedsmuir Peak Tweedsmuir ( gd, Sliabh Thuaidh) is a village and civil parish in Tweeddale, the Scottish Borders Council district, southeastern Scotland. Geography The village is set in a valley, with the rolling hills and burns on both sides, covering some ... (2194m). References *Quanchus Rangein the Canadian Mountain Encyclopedia Mountain ranges of British Columbia Nechako Country {{BritishColumbiaInterior-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nechako Range
The Nechako Range, 1795 km2, is a ridge-like hill-range on the Interior Plateau of the Central Interior of British Columbia, located southwest of the city of Prince George and to the east of the similar Fawnie Range. Formerly known as Nechako Mountain, the range lies between the West Road River to its south and the Euchiniko River to the north, and Knewstubb Lake to its northwest (part of the Ootsa Lake The Nechako Reservoir, sometimes called the Ootsa Lake Reservoir, is a hydroelectric reservoir in British Columbia, Canada that was formed by the Kenney Dam making a diversion of the Nechako River through a 16-km intake tunnel in the Kitimat Ranges ... reservoir). References Nechako Country Mountain ranges of the Interior Plateau {{BritishColumbiaInterior-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fawnie Range
The Fawnie Range is a small hill-range located to the south of the Ootsa Lake reservoir and to the north of the West Road River in the Nechako Plateau region of the British Columbia Interior, Central Interior of British Columbia, Canada. The northwest part of the park is within Entiako Provincial Park and includes Mount Swannell, (1821 m /5974 ft), one of the range's main summits, overlooking Natalkuz Lake (part of the Ootsa Reservoir) from the south. Other named summits include Tutial Mountain (1844 m / 6050 ft), Fawnie Dome (1733 m / 5686 ft) and Fawnie Nose (1933 m / 6342 ft), the highest summit in the range. See also *Telegraph Range *Quanchus Range *List of landforms of British Columbia References Nechako Country Interior Plateau Mountain ranges of British Columbia {{BritishColumbiaInterior-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dakelh Language
The Dakelh (ᑕᗸᒡ) 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 French explorers naming of the people. Dakelh people speak two related languages. One, Babine-Witsuwit'en is sometimes referred to as ''Northern Carrier''. The other includes what are sometimes referred to as ''Central Carrier'' and ''Southern Carrier''. Etymology of 'Carrier' The name 'Carrier' is a translation of the Sekani name 'aɣele' "people who carry things around on their backs", due to the fact that the first Europeans to learn of the Carrier, the Northwest Company explorers led by Alexander Mackenzie, first passed through the territory of the Carriers' Sekani neighbours. The received view of the origin of the Sekani name is that it refers to the distinctive Carrier mortuary practice in which a widow carried her husban ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cariboo Mountains
The Cariboo Mountains are the northernmost subrange of the Columbia Mountains, which run down into the Spokane area of the United States and include the Selkirks, Monashees and Purcells. The Cariboo Mountains are entirely within the province of British Columbia, Canada. The range is in area and about 245 km in length (southeast–northwest) and about 90 km at its widest (southwest–northeast). Physical geography East of the range is the Rocky Mountain Trench, in this region largely the path of the upper Fraser River (including the section known as the Grand Canyon of the Fraser which is not to be confused with the better-known Fraser Canyon nearer Vancouver). To the west the range verges with the Cariboo Plateau through an intermediary "foothill" area known as the Quesnel Highland. Northwestwards the range drops to the Willow River area of the Nechako Plateau, which lies around Prince George. South of the range, northeast of Clearwater a plateau-like mountainous ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
_cropped.jpg "Click for more on -> Dakelh Language")
