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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] |
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 of the Canadian Cordillera, which is the northern segment of the North American Cordillera, the expansive system of interconnected mountain ranges between the Interior Plains and the Pacific Coast that runs northwest–southeast from central Alaska to the Isthmus of Tehuantepec in Mexico. Canada officially defines the Rocky Mountains system as the mountain chains east of the Rocky Mountain Trench extending from the Liard River valley in northern British Columbia to the Albuquerque Basin in New Mexico, not including the Mackenzie, Richardson and British Mountains/Brooks Range in Yukon and Alaska (which are all included as the "Arctic Rockies" in the United States' definition of the Rocky Mountains system). The Canadian Rockies, bein ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mary Schäffer Warren
Mary Schäffer Warren (1861–1939) was an American-Canadian naturalist, illustrator, photographer, and writer. She was known for her experiences in the Canadian Rockies in the early 20th century. Biography Warren was born Mary Townsend Sharples in 1861 in West Chester, Pennsylvania. She studied flower painting with George Cochran Lambdin. In 1889 Sharples embarked on her first visit to the Canadian Rockies, accompanied by her fellow art student, Mary Vaux. In 1890 she married Dr. Charles Schäffer, an amateur botanist, whom she had met the previous year at Glacier House, the Canadian Pacific Railway's hotel in the Selkirk Mountains. The couple would spend summers and autumns traveling in the Canadian Rockies. Their winters were spent in Philadelphia. Charles Schäffer died in 1903, as did Mary's father and mother. In 1904, Schäffer returned to the Canadian Rockies with her friend Mary "Mollie" Adams determined to complete a botanical guide that her husband had started. To co ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geology Of The Rocky Mountains
The geology of the Rocky Mountains is that of a discontinuous series of mountain ranges with distinct geological origins. Collectively these make up the Rocky Mountains, a mountain system that stretches from Northern British Columbia through central New Mexico and which is part of the great mountain system known as the North American Cordillera. The rocky cores of the mountain ranges are, in most places, formed of pieces of continental crust that are over one billion years old. In the south, an older mountain range was formed 300 million years ago, then eroded away. The rocks of that older range were reformed into the Rocky Mountains. The Rocky Mountains took shape during an intense period of plate tectonic activity that resulted in much of the rugged landscape of the western North America. The Laramide orogeny, about 80–55 million years ago, was the last of the three episodes and was responsible for raising the Rocky Mountains. Subsequent erosion by glaciers has created the ... [...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 Of Canada
Most mountain peaks of Canada lie in the west, specifically in British Columbia, Alberta, and the Yukon. Mountains can be found all over British Columbia while those in Alberta are mainly situated on the eastern side of the Canadian Rockies. The Saint Elias Mountains in the Yukon hold some of country's highest mountains, including the highest, Mount Logan at . Alberta ;Highest peaks Mts. Columbia & King Edward.jpg, Mount Columbia & King Edward in background The Twins - South and North (l-r).jpg, The Twins massif - South Twin and North Twin (l-r) Mount Assiniboine massif.jpg, Mount Assiniboine seen from above Lake Magog Columbia Icefields - panoramio (1).jpg, Snow Dome seen from Icefields Parkway British Columbia Mount Assiniboine.jpg, Mount Assiniboine Mount Robson South.jpg, Mount Robson, highest in Canadian Rockies Garibaldi black tusk.jpg, The Black Tusk Snow Dome+Dome Glacier.jpg, Snow Dome and Dome Glacier Mount Mackenzie from Mount Revelstoke NP.jpg, Mou ... [...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] |
Stanley Waters
Lieutenant-general Stanley Charles Waters (June 14, 1920 – September 25, 1991) was Canada's first senator to be appointed to his Senate seat following a non-binding provincial Senate election. Early life Born in Winnipeg and educated at Strathcona High School and the University of Alberta, Waters commissioned into the 14th Army Tank Battalion (The Calgary Regiment (Tank)) in 1941. He was then posted to the First Special Service Force. In 1943, using scaling ropes, Waters led his unit up the sheer cliffs of Monte la Difensa to attack German defences. In February 1944 he landed at Anzio and, due to Allied losses, temporarily took command of a battalion. After the war, he rose steadily through the ranks, and ended his career as a lieutenant-general and Commander of Mobile Command (1973–75). In 1975, he joined Mannix Organization at Calgary, becoming president of Loram Group, a subsidiary of the parent company. He was a co-founder of the Bowfort Group of Companies, which en ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
1st Canadian Parachute Battalion
The 1st Canadian Parachute Battalion was an Airborne forces, airborne infantry battalion of the Canadian Army formed in July 1942 during the World War II, Second World War; it served in Western Front (World War II)#1944–45: The Second Front, North West Europe, Invasion of Normandy, Landing in Normandy during Operation Tonga, in conjunction with the Normandy landings, D-Day landings of 6 June 1944 and in the airborne assault crossing of the Rhine, River Rhine, Operation Varsity, in March 1945. After the end of hostilities in Europe, the battalion was returned to Canada where it was disbanded on 30 September 1945. By the end of the war the battalion had gained a remarkable reputation: they never failed to complete a mission, and they never gave up an objective once taken. They are the only Canadians to participate in the Battle of the Bulge and had advanced deeper than any other Canadian unit into enemy territory.Horn, Bernd. ''Bastard Sons, and Examination of Canada's Airborne Expe ... [...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] |
Stoney Language
Stoney—also called Nakota, Nakoda, Isga, and formerly Alberta Assiniboine—is a member of the Dakota subgroup of the Mississippi Valley grouping of the Siouan languages. The Dakotan languages constitute a dialect continuum consisting of Santee-Sisseton (Dakota), Yankton-Yanktonai (Dakota), Teton (Lakota), Assiniboine, and Stoney. Stoney is the most linguistically divergent of the Dakotan dialects and has been described as “on the verge of becoming a separate language”. The Stoneys are the only Siouan people that live entirely in Canada, and the Stoney language is spoken by five groups in Alberta. No official language survey has been undertaken for every community where Stoney is spoken, but the language may be spoken by as many as a few thousand people, primarily at the Morley community. Relationship to Assiniboine Stoney’s closest linguistic relative is Assiniboine. The two have often been confused with each other due to their close historical and linguistic relationsh ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
