|
Clark Range (Canada)
The Clark Range is a mountain range that forms part of the Continental Divide and also the boundary between the Canadian provinces of Alberta and British Columbia. A small portion of the range extends into the far northwestern section of Glacier National Park, Montana, United States. It is the easternmost of the Border Ranges subdivision of the Canadian Rockies. The range is named for Captain William Clark of the Lewis and Clark Expedition The Lewis and Clark Expedition, also known as the Corps of Discovery Expedition, was the United States expedition to cross the newly acquired western portion of the country after the Louisiana Purchase. The Corps of Discovery was a select gr .... This range includes the following mountains and peaks: References Mountain ranges of Alberta Mountain ranges of British Columbia Mountains of Glacier National Park (U.S.) Mountain ranges of Montana Ranges of the Canadian Rockies Ranges of the Rocky Mountains Elk Valley (British ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Provinces And Territories Of Canada
Within the geographical areas of Canada, the ten provinces and three territories are sub-national administrative divisions under the jurisdiction of the Canadian Constitution. In the 1867 Canadian Confederation, three provinces of British North America—New Brunswick, Nova Scotia, and the Province of Canada (which upon Confederation was divided into Ontario and Quebec)—united to form a federation, becoming a fully independent country over the next century. Over its history, Canada's international borders have changed several times as it has added territories and provinces, making it the world's second-largest country by area. The major difference between a Canadian province and a territory is that provinces receive their power and authority from the '' Constitution Act, 1867'' (formerly called the '' British North America Act, 1867''), whereas territorial governments are creatures of statute with powers delegated to them by the Parliament of Canada. The powers flowing ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Alderson
Mount Alderson is a summit located in Waterton Lakes National Park, in the Canadian Rockies of Alberta, Canada. Its nearest higher peak is Mount Custer, to the southwest. Mount Richards is situated to the southeast, and Bertha Peak is to the immediate northeast. History Mount Alderson was named for Edwin Alderson, Sir Edwin Alfred Hervey Alderson, a senior British Army officer who served in several campaigns of the late nineteenth and early twentieth centuries, ultimately in command of the Canadian Corps in World War I. The mountain's name was officially adopted in 1943 by the Geographical Names Board of Canada. Geology Like other mountains in Waterton Lakes National Park, Mount Alderson is composed of sedimentary rock laid down during the Precambrian to Jurassic periods. Formed in shallow seas, this sedimentary rock was pushed east and over the top of younger Cretaceous period rock during the Laramide orogeny. Climate Based on the Köppen climate classification, Mount Ald ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountains Of Glacier National Park (U
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountain Ranges Of British Columbia
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit A summit is a point on a surface that is higher in elevation than all points immediately adjacent to it. The topography, topographic terms acme, apex, peak (mountain peak), and zenith are synonymous. The term (mountain top) is generally used ... area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are Monadnock, isolated summits, but most occur in mountain ranges. Mountain formation, Mountains are formed through Tectonic plate, tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through Slump (geology), slumping and other forms of mass wa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountain Ranges Of Alberta
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Font Mountain
Font Mountain is located on the border of Alberta and British Columbia on the Continental Divide. See also *List of peaks on the Alberta–British Columbia border *Mountains of British Columbia British Columbia is the westernmost province of Canada, bordered by the Pacific Ocean. With an area of it is Canada's third-largest province. The province is almost four times the size of the United Kingdom and larger than every United States ... References External links * Two-thousanders of Alberta Two-thousanders of British Columbia Canadian Rockies Kootenay Land District {{BritishColumbia-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Richards
Mount Richards is a 2,377-meter-elevation (7,799-foot) mountain summit located in Waterton Lakes National Park, in the Canadian Rockies of Alberta, Canada. It is situated just north of the Canada–United States border, with the south footing of the mountain at Boundary Creek just within Glacier National Park of the United States. Its nearest higher peak is Mount Alderson, to the northwest. Bertha Lake and Bertha Peak are situated immediately to the north. History Mount Richards was named in honor of Admiral Sir George Henry Richards (1820–1896), Hydrographer of the Navy who was the Second Commissioner of the British Boundary Commission which delineated the border from the Pacific to the Rockies. It has also been called Sleeping Indian Mountain. The mountain's toponym was officially adopted in 1943 by the Geographical Names Board of Canada. Geology Like other mountains in Waterton Lakes National Park, Mount Richards is composed of sedimentary rock laid down during the Preca ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Packhorse Peak
Packhorse Peak is a summit in British Columbia, Canada. Description Packhorse Peak is a mountain located in the Clark Range of the Canadian Rockies. The remote peak is situated west of the Continental Divide and southeast of Fernie. The nearest higher neighbor is Tombstone Mountain, to the southeast. Packhorse Peak is more notable for its steep rise above local terrain than for its absolute elevation as topographic relief is significant with the summit rising over 885 meters (2,900 ft) above Cate Creek in . Precipitation runoff from Packhorse Peak drains into tributaries of the Flathead River, which is three kilometers to the west. The mountain's toponym was published in 1917 from surveys performed in 1915, and was officially adopted in 1939 by the Geographical Names Board of Canada. Geology Packhorse Peak is composed of sedimentary rock laid down during the Precambrian to Jurassic periods. Formed in shallow seas, this sedimentary rock was pushed east and ov ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Matkin
Mount Matkin is a Canadian mountain located on the border of Alberta and British Columbia on the Continental Divide. It was named after Sergeant Philip K Matkin of the Royal Canadian Air Force. See also * List of peaks on the Alberta–British Columbia border * Mountains of Alberta * Mountains of British Columbia British Columbia is the westernmost province of Canada, bordered by the Pacific Ocean. With an area of it is Canada's third-largest province. The province is almost four times the size of the United Kingdom and larger than every United States ... References External links * Matkin Matkin Canadian Rockies Kootenay Land District {{EastKootenay-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tombstone Mountain (British Columbia)
Tombstone Mountain is a double summit mountain located near the southern end of the Opal Range in Kananaskis Country of the Canadian Rockies in Alberta, Canada. Tombstone South is the lower of the two summits, and is labelled as Tombstone Mountain on some maps. It can be reached via scrambling, whereas the true north summit requires technical climbing. Tombstone Mountain is situated within Elbow-Sheep Wildland Provincial Park, and its nearest higher peak is Elpoca Mountain, to the south. History The mountain was named by Canadian surveyor George Mercer Dawson in 1884 for the pinnacles and slabs which resembled tombstones near the summit. The mountain's name was officially adopted in 1924 by the Geographical Names Board of Canada. Geology Tombstone Mountain is composed of sedimentary rock laid down during the Precambrian to Jurassic periods. Formed in shallow seas, this sedimentary rock was pushed east and over the top of younger rock during the Laramide orogeny. Tombstone Mou ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Commerce Peak
Commerce is the large-scale organized system of activities, functions, procedures and institutions directly and indirectly related to the exchange (buying and selling) of goods and services among two or more parties within local, regional, national or international economies. More specifically, commerce is not business, but rather the part of business which facilitates the movement and distribution of finished or unfinished but valuable goods and services from the producers to the end consumers on a large scale, as opposed to the sourcing of raw materials and manufacturing of those goods. Commerce is subtly different from trade as well, which is the final transaction, exchange or transfer of finished goods and services between a seller and an end consumer. Commerce not only includes trade as defined above, but also a series of transactions that happen between the producer and the seller with the help of the auxiliary services and means which facilitate such trade. These auxilia ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Langemarck Mountain
Langemark is a village in the Belgian province of West Flanders, and a subdivision of the municipality of Langemark-Poelkapelle. The village has about 5,000 inhabitants. Besides the village center, there are also three smaller hamlets on the territory, , Bikschote and Saint-Julien/Sint-Juliaan. Written as Langemarck on French, British and German maps, the village is known in military history as the scenesee trench map of the first gas attacks by the German army in the western front, which marked the beginning of the Second Battle of Ypres in April 1915. Before and during the First Battle of Ypres, the German reserve corps suffered enormous losses: over 10,000 young soldiers (some only 15 years old), led by young officers without practical experience, died without achieving any objective. On 10 November 1914, about 2,000 soldiers died during an attempted breakthrough. One day later, the German Command ( Oberste Heeresleitung) published the following communiqué: :''West ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
