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Dutch Creek Hoodoos
The Dutch Creek Hoodoos are located in British Columbia, Canada, and can be seen along British Columbia Highway 93/ British Columbia Highway 95 between Canal Flats and Fairmont Hot Springs, British Columbia. The Dutch Creek Hoodoos are within a 67-acre conservation area that is managed by the Natural Conservancy of British Columbia. This conservation area is joined by the Nature Trust Hoffert Property and they both act as a habitat for varying plants and animals including the American badger, Lewis's woodpecker, the Hooker's Townsendia, Eagle, and Hawk. The Dutch Creek Hoodoos can be further discovered by following the 4.6 mile trail that faces an elevation gain of 95 meters over the course of the trail. Formation The Dutch Creek Hoodoos are formed just like all other Hoodoos form. Over time as the ground shifts and moves cracks form that causes pockets to form. When rain begins to fall it is easily caught in the cracks and can often settle within those pockets. As temperatu ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hoodoo (geology)
A hoodoo (also called a tent rock, fairy chimney, or earth pyramid) is a tall, thin spire of rock formed by erosion. Hoodoos typically consist of relatively soft rock topped by harder, less easily eroded stone that protects each column from the elements. They generally form within sedimentary rock and volcanic rock formations. Hoodoos range in size from the height of an average human to heights exceeding a 10-story building. Hoodoo shapes are affected by the erosional patterns of alternating hard and softer rock layers. Minerals deposited within different rock types can cause hoodoos to have different colors throughout their height. Etymology In certain regions of western North America these rocky structures are called hoodoos. The name is derived from Hoodoo spirituality, in which certain natural forms are said to possess certain powers, but by the late 19th century, this spirituality became associated with bad luck. Prior to the English name for these geographic formations ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kootenai
The Kutenai ( ), also known as the Ktunaxa ( ; ), Ksanka ( ), Kootenay (in Canada) and Kootenai (in the United States), are an indigenous people of Canada and the United States. Kutenai bands live in southeastern British Columbia, northern Idaho, and western Montana. The Kutenai language is a language isolate, thus unrelated to the languages of neighboring peoples or any other known language. Four bands form the Ktunaxa Nation in British Columbia. The Ktunaxa Nation was historically closely associated with the Shuswap Indian Band through tribal association and intermarriage. Two federally recognized tribes represent Kutenai people in the U.S.: the Kootenai Tribe of Idaho and the Confederated Salish and Kootenai Tribes in Montana, a confederation also including Bitterroot Salish and Pend d'Oreilles bands. Kootenay Around 40 variants of the name ''Kutenai'' have been attested since 1820; two others are also in current use. ''Kootenay'' is the common spelling in British Colum ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Landforms Of British Columbia
The following list comprises the physiogeographic regions of the Canadian province of British Columbia as defined by S.S. Holland in Bulletin 48 of the Ministry of Energy, Mines and Petroleum Resources' ''Landforms of British Columbia''. Western Cordillera (Canadian Cordillera) Western System Outer Mountain Area *Saint Elias Mountains **Fairweather Range ** Duke Depression **Alsek Ranges ** Icefield Ranges *Insular Mountains **Queen Charlotte Mountains *** Skidegate Plateau *** Queen Charlotte Ranges ** Vancouver Island Mountains ***Vancouver Island Ranges *** Alberni Basin *** Estevan Lowland (aka Estevan Strandflat) Coastal Trough *Hecate Depression ** Queen Charlotte Lowland ***Argonaut Plain ** Nahwitti Lowland *** Suquash Basin **Hecate Lowland ***Milbanke Strandflat *Georgia Depression **Georgia Lowland ***Fraser Lowland **Nanaimo Lowland Coast Mountain Area *Coast Mountains **Boundary Ranges **Kitimat Ranges ** Fiord Ranges - Geophysical Survey of Canada designation for ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rock Formations Of Canada
Rock most often refers to: * Rock (geology), a naturally occurring solid aggregate of minerals or mineraloids * Rock music, a genre of popular music Rock or Rocks may also refer to: Places United Kingdom * Rock, Caerphilly, a location in Wales * Rock, Cornwall, a village in England * Rock, County Tyrone, a village in Northern Ireland * Rock, Devon, a location in England * Rock, Neath Port Talbot, a location in Wales * Rock, Northumberland, a village in England * Rock, Somerset, a location in Wales * Rock, West Sussex, a hamlet in Washington, England * Rock, Worcestershire, a village and civil parish in England United States * Rock, Kansas, an unincorporated community * Rock, Michigan, an unincorporated community * Rock, West Virginia, an unincorporated community * Rock, Rock County, Wisconsin, a town in southern Wisconsin * Rock, Wood County, Wisconsin, a town in central Wisconsin Elsewhere * Corregidor, an island in the Philippines also known as "The Rock" * Jamaica, an islan ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rocky Mountains
The Rocky Mountains, also known as the Rockies, are a major mountain range and the largest mountain system in North America. The Rocky Mountains stretch in straight-line distance from the northernmost part of western Canada, to New Mexico in the southwestern United States. Depending on differing definitions between Canada and the U.S., its northern terminus is located either in northern British Columbia's Terminal Range south of the Liard River and east of the Trench, or in the northeastern foothills of the Brooks Range/ British Mountains that face the Beaufort Sea coasts between the Canning River and the Firth River across the Alaska-Yukon border. Its southernmost point is near the Albuquerque area adjacent to the Rio Grande rift and north of the Sandia–Manzano Mountain Range. Being the easternmost portion of the North American Cordillera, the Rockies are distinct from the tectonically younger Cascade Range and Sierra Nevada, which both lie farther to its west. The ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Yellowstone Park
Yellowstone National Park is an American national park located in the western United States, largely in the northwest corner of Wyoming and extending into Montana and Idaho. It was established by the 42nd U.S. Congress with the Yellowstone National Park Protection Act and signed into law by President Ulysses S. Grant on March 1, 1872. Yellowstone was the first national park in the U.S. and is also widely held to be the first national park in the world. The park is known for its wildlife and its many geothermal features, especially the Old Faithful geyser, one of its most popular. While it represents many types of biomes, the subalpine forest is the most abundant. It is part of the South Central Rockies forests ecoregion. While Native Americans have lived in the Yellowstone region for at least 11,000 years, aside from visits by mountain men during the early-to-mid-19th century, organized exploration did not begin until the late 1860s. Management and control of the park or ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Yellowhead Pass
The Yellowhead Pass is a mountain pass across the Continental Divide of the Americas in the Canadian Rockies. It is located on the provincial boundary between the Canadian provinces of Alberta and British Columbia, and lies within Jasper National Park and Mount Robson Provincial Park. Due to its modest elevation of and its gradual approaches, the pass was recommended by Sir Sandford Fleming as a route across the Rocky Mountains for the planned Canadian Pacific Railway. The proposal was rejected in favour of a more direct and southerly route, through the more difficult Kicking Horse Pass, which was opened in 1886. However, both the Grand Trunk Pacific and Canadian Northern Railways used the Yellowhead Pass for their main lines, built c. 1910–1913, and the main line of their successor, the Canadian National Railway, still follows the route. Via Rail's premier passenger train, the ''Canadian''; the Jasper – Prince Rupert train; and the Jasper section of the ''Rocky Mountai ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Columbia Lake
Columbia Lake is the primary lake at the headwaters of the Columbia River, in British Columbia, Canada. It is fed by several small tributaries. The village of Canal Flats is located at the south end of the lake. Columbia Lake is a fresh water lake located along Highway 93 and 95, between the centres of Canal Flats and Fairmont Hot Springs in British Columbia, Canada. Its average July temperature of 18 °C makes it the largest warm water lake in the East Kootenay. It has a mean depth of only , to a maximum of , with excellent water clarity as it enjoys a much smaller volume of boat traffic than its northern neighbour, Windermere Lake. The Kootenay River, a major tributary of the Columbia, passes within a few thousand feet of the south end of the lake. In freshets the Kootenay, here already a large stream, sometimes overflows into Columbia Lake, and historically the Baillie-Grohman Canal connected the two bodies of water to facilitate the navigation of steamboat A steamb ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Columbia River
The Columbia River (Upper Chinook: ' or '; Sahaptin: ''Nch’i-Wàna'' or ''Nchi wana''; Sinixt dialect'' '') is the largest river in the Pacific Northwest region of North America. The river rises in the Rocky Mountains of British Columbia, Canada. It flows northwest and then south into the U.S. state of Washington, then turns west to form most of the border between Washington and the state of Oregon before emptying into the Pacific Ocean. The river is long, and its largest tributary is the Snake River. Its drainage basin is roughly the size of France and extends into seven US states and a Canadian province. The fourth-largest river in the United States by volume, the Columbia has the greatest flow of any North American river entering the Pacific. The Columbia has the 36th greatest discharge of any river in the world. The Columbia and its tributaries have been central to the region's culture and economy for thousands of years. They have been used for transportation since a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kootenay River
The Kootenay or Kootenai river is a major river in the Northwest Plateau, in southeastern British Columbia, Canada, and northern Montana and Idaho in the United States. It is one of the uppermost major tributaries of the Columbia River, the largest North American river that empties into the Pacific Ocean. The Kootenay River runs from its headwaters in the Kootenay Ranges of the Canadian Rockies, flowing from British Columbia's East Kootenay region into northwestern Montana, then west into the northernmost Idaho Panhandle and returning to British Columbia in the West Kootenay region, where it joins the Columbia at Castlegar. The river is known as the Kootenay in Canada and by the Ktunaxa Nation, and Kootenai in the United States and by the Confederated Salish and Kootenai Tribes and Kootenai Tribe of Idaho. Fed mainly by glaciers and snow melt, the river drains a rugged, sparsely populated region of more than ; over 70 percent of the basin is in Canada. From its hi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Yawunik
''Yawunik'' is an extinct genus of Cambrian megacheiran ("Great appendage" arthropod) known from the Burgess Shale in Canada (Marble Canyon locality). The type species has been named ''Yawunik kootenayi'' after the Kootenay, both a geographic area (and National Park, where the fossil was found) and North American First Nation, also known as the Ktunaxa. Yawunik is the name of a primordial sea monster in Ktunaxa mythology. The fossil dates back to 508 million years ago. Description ''Yawunik'' had large size for megacheiran, up to long not including great appendage. It had four eyes, in the anteriormost position of the head, and lateral eyes are larger. ''Yawunik'' differs from other leanchoilid such as ''Leanchoilia ''Leanchoilia'' is an megacheiran arthropod known from Cambrian deposits of the Burgess Shale in Canada and the Chengjiang biota of China. It was about long and had long, whip-like feelers mounted on frontal arm-like appendages. Its internal o ...'' by havi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
British Columbia, Canada
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 in 184 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
