|
Mount Ernest Ross
Mount Ernest Ross is a double summit mountain located in the North Saskatchewan River valley of the Canadian Rockies of Alberta, Canada. Mount Ernest Ross can be seen from the David Thompson Highway at the southern end of Abraham Lake. Precipitation runoff from the peak drains east into the lake. Mount William Booth is across the lake to the east, and Kootenay Plains and Ex Coelis Mountain are situated to the southeast. Its nearest higher peak is Elliott Peak, to the immediate north. __NOTOC__ History This mountain is named after Ernest Ross, who in 1940 was the first to drive a motorized vehicle from Rocky Mountain House to Saskatchewan Crossing, many years before a road was built. He was instrumental in promoting the construction of what has become the David Thompson Highway, and when it was completed in 1969, was honored for his efforts. The mountain's name was officially adopted in 1980 when approved by the Geographical Names Board of Canada. Geology Mount Ernest Ross is c ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Front Ranges
The Front Ranges are a group of mountain ranges in the Canadian Rockies of eastern British Columbia and western Alberta, Canada. It is lowest and the easternmost of the three main subranges of the Continental Ranges, located east of the Bull and Elk rivers and a fault line extending northwest of West Elk Pass to McGregor Pass. Subranges * Bare Range * Bighorn Range *Bosche Range *De Smet Range * Elk Range *Fairholme Range *First Range *Fisher Range * Goat Range * Greenhills Range *High Rock Range *Highwood Range *Jacques Range *Kananaskis Range *Lizard Range *Maligne Range *Miette Range *Murchison Group *Nikanassin Range *Opal Range * Palliser Range *Queen Elizabeth Ranges *Ram Range *Sawback Range * Slate Range *Taylor Range * Vermilion Range *Victoria Cross Ranges The Victoria Cross Ranges ( to ) are a set of mountain ranges in the Canadian Rockies, located to the northwest of Jasper. Of the 19 peaks contained within this range, five are named after Canadian recipients of the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ex Coelis Mountain
Ex Coelis Mountain is a mountain with five peaks located in the North Saskatchewan River valley of the Canadian Rockies of Alberta, Canada. It is situated south of Abraham Lake and just outside the eastern boundary of Banff National Park. Its nearest higher peak is Hatter Peak, to the southeast. Ex Coelis Mountain can be seen from the David Thompson Highway east of Saskatchewan Crossing. Ex Coelis Mountain is composed of sedimentary rock laid down from the Precambrian to Jurassic periods that was pushed east and over the top of younger rock during the Laramide orogeny. History In 1911, this geographic feature was originally known as Kadoona Mountain by Mary Schäffer, which is a corruption of the Stoney name ''Kedonnaha Tinda'' (Meadow of the Winds), today known as the Kootenay Plains. The mountain's name was officially adopted in 1994 by the Geographical Names Board of Canada to honour the 1st Canadian Parachute Battalion. In Latin, ''Ex Coelis'' means ''Out of the Clo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geography Of Alberta
Alberta is one of the thirteen provinces and territories of Canada. Located in Western Canada, the province has an area of and is bounded to the south by the United States state of Montana along 49° north for ; to the east at 110° west by the province of Saskatchewan for ; and at 60° north the Northwest Territories for . The southern half of the province borders British Columbia along the Continental Divide of the Americas on the peaks of the Rocky Mountains, while the northern half borders British Columbia along the 120th meridian west. Along with Saskatchewan it is one of only two landlocked provinces or territories. Terrain Alberta's landscape is marked by the impact of the Wisconsin Glaciation, about 75,000 to 11,000 years ago, when the entire future province was covered in ice. As the ice sheet receded, the landscape was changed, and large amounts of glacial till were left behind. The southern portion consists chiefly of plains that are almost entirely treeless. As ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Mountains In The Canadian Rockies
A list of highest peaks in the Canadian Rockies is shown below: References ;Notes {{reflist, group=notes *• Canadian Rockies The Canadian Rockies (french: Rocheuses canadiennes) or Canadian Rocky Mountains, comprising both the Alberta Rockies and the British Columbian Rockies, is the Canadian segment of the North American Rocky Mountains. It is the easternmost part ... Mountains, Rockies Mountains, Rockies ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Subarctic Climate
The subarctic climate (also called subpolar climate, or boreal climate) is a climate with long, cold (often very cold) winters, and short, warm to cool summers. It is found on large landmasses, often away from the moderating effects of an ocean, generally at latitudes from 50° to 70°N, poleward of the humid continental climates. Subarctic or boreal climates are the source regions for the cold air that affects temperate latitudes to the south in winter. These climates represent Köppen climate classification ''Dfc'', ''Dwc'', ''Dsc'', ''Dfd'', ''Dwd'' and ''Dsd''. Description This type of climate offers some of the most extreme seasonal temperature variations found on the planet: in winter, temperatures can drop to below and in summer, the temperature may exceed . However, the summers are short; no more than three months of the year (but at least one month) must have a 24-hour average temperature of at least to fall into this category of climate, and the coldest month should ave ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Köppen Climate Classification
The Köppen climate classification is one of the most widely used climate classification systems. It was first published by German-Russian climatologist Wladimir Köppen (1846–1940) in 1884, with several later modifications by Köppen, notably in 1918 and 1936. Later, the climatologist Rudolf Geiger (1894–1981) introduced some changes to the classification system, which is thus sometimes called the Köppen–Geiger climate classification system. The Köppen climate classification divides climates into five main climate groups, with each group being divided based on seasonal precipitation and temperature patterns. The five main groups are ''A'' (tropical), ''B'' (arid), ''C'' (temperate), ''D'' (continental), and ''E'' (polar). Each group and subgroup is represented by a letter. All climates are assigned a main group (the first letter). All climates except for those in the ''E'' group are assigned a seasonal precipitation subgroup (the second letter). For example, ''Af'' indi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Laramide Orogeny
The Laramide orogeny was a time period of mountain building in western North America, which started in the Late Cretaceous, 70 to 80 million years ago, and ended 35 to 55 million years ago. The exact duration and ages of beginning and end of the orogeny are in dispute. The Laramide orogeny occurred in a series of pulses, with quiescent phases intervening. The major feature that was created by this orogeny was deep-seated, thick-skinned deformation, with evidence of this orogeny found from Canada to northern Mexico, with the easternmost extent of the mountain-building represented by the Black Hills of South Dakota. The phenomenon is named for the Laramie Mountains of eastern Wyoming. The Laramide orogeny is sometimes confused with the Sevier orogeny, which partially overlapped in time and space. The orogeny is commonly attributed to events off the west coast of North America, where the Kula Plate, Kula and Farallon Plates were sliding under the North American plate. Most hypothes ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Jurassic
The Jurassic ( ) is a Geological period, geologic period and System (stratigraphy), stratigraphic system that spanned from the end of the Triassic Period million years ago (Mya) to the beginning of the Cretaceous Period, approximately Mya. The Jurassic constitutes the middle period of the Mesozoic, Mesozoic Era and is named after the Jura Mountains, where limestone strata from the period were first identified. The start of the Jurassic was marked by the major Triassic–Jurassic extinction event, associated with the eruption of the Central Atlantic magmatic province, Central Atlantic Magmatic Province. The beginning of the Toarcian Stage started around 183 million years ago and is marked by an extinction event associated with widespread Anoxic event, oceanic anoxia, ocean acidification, and elevated temperatures likely caused by the eruption of the Karoo-Ferrar, Karoo-Ferrar large igneous provinces. The end of the Jurassic, however, has no clear boundary with the Cretaceous and i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Precambrian
The Precambrian (or Pre-Cambrian, sometimes abbreviated pꞒ, or Cryptozoic) is the earliest part of Earth's history, set before the current Phanerozoic Eon. The Precambrian is so named because it preceded the Cambrian, the first period of the Phanerozoic Eon, which is named after Cambria, the Latinised name for Wales, where rocks from this age were first studied. The Precambrian accounts for 88% of the Earth's geologic time. The Precambrian is an informal unit of geologic time, subdivided into three eons ( Hadean, Archean, Proterozoic) of the geologic time scale. It spans from the formation of Earth about 4.6 billion years ago ( Ga) to the beginning of the Cambrian Period, about million years ago ( Ma), when hard-shelled creatures first appeared in abundance. Overview Relatively little is known about the Precambrian, despite it making up roughly seven-eighths of the Earth's history, and what is known has largely been discovered from the 1960s onwards. The Precambrian fossil ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geographical Names Board Of Canada
The Geographical Names Board of Canada (GNBC) is a national committee with a secretariat in Natural Resources Canada, part of the Government of Canada, which authorizes the names used and name changes on official federal government maps of Canada created since 1897. The board consists of 27 members, one from each of the provinces and territories, and others from departments of the Government of Canada. The board also is involved with names of areas in the Antarctic through the Antarctic Treaty. Structure The secretariat is provided by Natural Resources Canada. In addition to the provincial and territorial members are members from the following federal government departments: Aboriginal Affairs and Northern Development Canada, Canada Post Corporation, Fisheries and Oceans Canada, Elections Canada, Library and Archives Canada, Department of National Defence, Natural Resources Canada (including Geological Survey of Canada and Canada Centre for Mapping and Earth Observation), Pa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Saskatchewan River Crossing
Saskatchewan River Crossing is a locality in western Alberta, Canada. It is located within Banff National Park at the junction of Highway 93 (Icefields Parkway) and Highway 11 (David Thompson Highway). It is administered by Improvement District No. 9. It was named "The Crossing", when travellers and fur traders used this spot to cross the North Saskatchewan River on their way to British Columbia in the 19th century. Geography It lies as the confluence of the North Saskatchewan River with Howse River and Mistaya River in the Canadian Rockies and is the starting point for tours on the Columbia Icefield and other scenic hiking trails. - Icefields Parkway Drive Mount Wil ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rocky Mountain House
Rocky Mountain House is a town in west-central Alberta, Canada. It is approximately west of Red Deer at the confluence of the Clearwater and North Saskatchewan Rivers, and at the crossroads of Highway 22 (Cowboy Trail) and Highway 11 (David Thompson Highway). The surrounding Clearwater County's administration office is located in Rocky Mountain House. History The town has a long history dating to the 18th century with the presence of British and Canadian fur traders during the westward Canadian expansion. In 1799, the Hudson's Bay Company and the North West Company each established the Rocky Mountain House and Acton House fur trading posts. Trade with the local aboriginal peoples continued until 1821 when the companies merged, they continued to trade until 1875 and closed the Rocky Mountain House post. The name of the settlement however remained. The Rocky Mountain House settlement also served as a launching point for many explorers such as David Thompson, in search for ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
