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Cirrus Mountain
Cirrus Mountain is a mountain summit located in the upper North Saskatchewan River valley on the shared boundary between Banff National Park and White Goat Wilderness Area, in the Canadian Rockies of Alberta, Canada. Cirrus Mountain is situated along the east side the Icefields Parkway midway between Saskatchewan Crossing and Sunwapta Pass. Topographic relief is significant as the summit rises 1,740 meters (5,708 ft) above the parkway in . The nearest higher peak is Mount Stewart, to the north-northeast. History In 1928, Morrison P. Bridgland suggested the name ''Mount Huntington'' for the mountain, but it was not adopted. However, the Huntington name endures as the name of the ''Huntington Glacier'' below the eastern aspect of the summit. The mountain was instead named Cirrus Mountain, and that toponym was officially adopted in 1935 by the Geographical Names Board of Canada. The first ascent of the mountain was accomplished in 1939 by C.B. Sissons and H.J. Sissons ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Parker Ridge
Parker Ridge is a mountain ridge located in the upper North Saskatchewan River valley in Banff National Park, in the Canadian Rockies of Alberta, Canada. Its nearest higher peak is Mount Athabasca, to the west. Parker Ridge is situated along the west side of the Icefields Parkway and southeast of Sunwapta Pass. Parker Ridge is a ski-touring destination in the winter and popular hiking destination in the summer because it is situated beside the Icefields Parkway allowing easy access, and is nearly entirely above treeline allowing good views of the surrounding mountain landscape. A trail gains of elevation from the highway to the top of the ridge. Wandering east or west along the ridge provides views of Cirrus Mountain, the north face of Mount Saskatchewan, Saskatchewan Glacier, Mount Athabasca, Hilda Peak, and Nigel Peak among others. History Parker Ridge was named for Elizabeth Parker (1856–1944), co-founder of the Alpine Club of Canada in 1906 along with Arthur Oliv ... [...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] |
Nigel Peak
Nigel Peak is a mountain summit located on the shared border of Banff National Park and Jasper National Park, in the Canadian Rockies of Alberta, Canada. Nigel has two peaks, the north summit is the highest point. The nearest higher peak is Mount Athabasca, to the south-southwest. Nigel Peak is situated immediately north of Sunwapta Pass and can be seen from the Icefields Parkway and from Athabasca Glacier. Topographic relief is significant as the summit rises 1,100 meters (3,610 feet) above the parkway in two kilometers (1.2 mile). __NOTOC__ History Nigel Vavasour was a packer who accompanied J. Norman Collie and Hugh Stutfield to the Columbia Icefield area in 1897. The mountain was named by the mountaineers during an 1898 sheep hunt with Nigel. The mountain's toponym was officially adopted March 5, 1935, by the Geographical Names Board of Canada. The first ascent of the mountain was made in 1919 by the Interprovincial Boundary Commission. Geology Like other ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Athabasca
Mount Athabasca is located in the Columbia Icefield of Jasper National Park in Canada. The mountain was named in 1898 by J. Norman Collie, who made the first ascent on August 18 of that year. Athabasca is the Cree language name for "where there are reeds", which originally referred to Lake Athabasca. Mount Athabasca is unusual, in that water flows to the Pacific Ocean from the western slope, the Arctic Ocean from the northeastern slope, and to Hudson Bay from the southeastern slope.Geography of Alberta __NOTOC__ Routes There are several climbing routes, including: * North Glacier (Normal Route) II * Silverhorn II * AA Col II * Regular North Face III 5.8 * North Ridge III 5.5 * The Hourglass 300m, III, AI3-4 One of the most prominent features of Mount Athabasca is a horned-shaped tip near the top called the "Silverhorn". The Silverhorn is one of the easier routes to the summit but requires more caution and ability than the normal route because of blue ice and falling ice fro ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Saskatchewan (Alberta)
Mount Saskatchewan is a mountain located in the North Saskatchewan River valley of Banff National Park, in the Canadian Rockies of Alberta, Canada. J. Norman Collie named the mountain in 1898 for the nearby Saskatchewan River. One report said Collie so named it due to its possession of the headwaters of the North Saskatchewan River. Geographic Board of Canada. Place Names of Alberta (1928) Lighthouse Tower A pinnacle unofficially named Lighthouse Tower and also sometimes referred to as "Cleopatra's Needle" (elevation ), is located two kilometres from the summit on the eastern ridge of Mt. Saskatchewan. It was first climbed in 1964 by G. Boehnisch and L. Mackay. Geology Like other mountains in Banff Park, Mount Saskatchewan is composed of sedimentary rock laid down from 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. The north aspect of the peak supports an unnamed ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Wilson (Alberta)
Mount Wilson is a mountain summit located in the North Saskatchewan River valley of Banff National Park, in the Canadian Rockies of Alberta, Canada. Its nearest higher peak is Mount Cline, to the northeast. Mount Wilson is situated immediately north of the confluence of the North Saskatchewan River, Mistaya River, and Howse River near Saskatchewan Crossing, where the Icefields Parkway intersects with the David Thompson Highway.__NOTOC__ History Mount Wilson honours Tom Wilson (1859–1933) who was an early explorer in the Canadian Rockies. The mountain was named in 1898 by Norman Collie. The first ascent of the mountain was made in 1902 by James Outram and Christian Kaufmann. The mountain's name was officially adopted in 1924 by the Geographical Names Board of Canada. Geology Like other mountains in Banff Park, Mount Wilson is composed of sedimentary rock laid down from the Precambrian to Jurassic periods. Formed in shallow seas, this sedimentary rock was pushed east a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Coleman (Alberta)
Mount Coleman is a mountain summit located in the upper North Saskatchewan River valley in Banff National Park, in the Canadian Rockies of Alberta, Canada. Its nearest higher peak is Cirrus Mountain, to the north. Mount Coleman is situated along the east side the Icefields Parkway midway between Saskatchewan Crossing and Sunwapta Pass. History Mount Coleman was named in 1898 after Arthur P. Coleman (1852-1939), a Canadian geologist and among the first white men to explore the area that is now Jasper National Park. Geology Like other mountains in Banff Park, Mount Coleman is composed of sedimentary rock laid down from 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. Climate Based on the Köppen climate classification, Mount Coleman is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill f ... [...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] |
Surface Runoff
Surface runoff (also known as overland flow) is the flow of water occurring on the ground surface when excess rainwater, stormwater, meltwater, or other sources, can no longer sufficiently rapidly infiltrate in the soil. This can occur when the soil is saturated by water to its full capacity, and the rain arrives more quickly than the soil can absorb it. Surface runoff often occurs because impervious areas (such as roofs and pavement) do not allow water to soak into the ground. Furthermore, runoff can occur either through natural or man-made processes. Surface runoff is a major component of the water cycle. It is the primary agent of soil erosion by water. The land area producing runoff that drains to a common point is called a drainage basin. Runoff that occurs on the ground surface before reaching a channel can be a nonpoint source of pollution, as it can carry man-made contaminants or natural forms of pollution (such as rotting leaves). Man-made contaminants in runoff i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Weeping Wall (Alberta)
The Weeping Wall is a set of cliffs, approximately 1000 feet high, located at the western base of Cirrus Mountain alongside Highway 93 (Icefields Parkway) in northern Banff National Park in Alberta, Canada, just south of the boundary with Jasper National Park. In spring and summer, the faces of the cliffs are usually covered with a series of cascading waterfall A waterfall is a point in a river or stream where water flows over a vertical drop or a series of steep drops. Waterfalls also occur where meltwater drops over the edge of a tabular iceberg or ice shelf. Waterfalls can be formed in several wa ...s. In winter, the waterfalls freeze into towering pillars of ice and become a well-known site for ice climbing. References External links "Weeping Wall" at Canadian Rockies Ice Climbing Encyclopediawith route descriptions, degrees of difficulty, and equipment needs. Mountains of Banff National Park One-thousanders of Alberta Climbing areas of Canada Waterfall ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
