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Twin Goat Mountain
Twin Goat Mountain is a summit in British Columbia, Canada. Description Twin Goat Mountain is located east of Pemberton in the Lillooet Ranges of the Coast Mountains. Precipitation runoff from this mountain drains into tributaries of the Lillooet River. Twin Goat Mountain is more notable for its steep rise above local terrain than for its absolute elevation as topographic relief is significant with the summit rising 1,928 metres (6,325 ft) above Lillooet Lake in . The mountain's toponym was officially adopted January 23, 1979, by the 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 .... The mountain was named in association with Twin One Creek, as submitted by Karl Ricker of the Alpine Club of Canada. Climate Based on the Köppen ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cloudraker Mountain
Cloudraker Mountain is a glaciated summit in British Columbia, Canada. Description Cloudraker Mountain is located in the Lillooet Ranges of the Coast Mountains, southeast of Pemberton and east of Whistler. Precipitation runoff and glacial meltwater from this mountain drains into tributaries of the Lillooet River. Cloudraker Mountain is more notable for its steep rise above local terrain than for its absolute elevation as topographic relief is significant with the summit rising 935 metres (3,070 ft) above Tao Lake in less than and 2,185 metres (7,170 ft) above Lillooet Lake in . The mountain's toponym was officially adopted March 31, 1969, by the 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 .... The mountain's name ... [...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] |
Two-thousanders Of British Columbia
Two-thousanders are mountains that have a height of at least 2,000 metres above sea level, but less than 3,000 metres. The term is used in Alpine circles, especially in Europe (e.g. German: ''Zweitausender''). The two photographs show two typical two-thousanders in the Alps that illustrate different types of mountain. The Säuling (top) is a prominent, individual peak, whereas the Schneeberg (bottom) is an elongated limestone massif. In ranges like the Allgäu Alps, the Gesäuse or the Styrian-Lower Austrian Limestone Alps the mountain tour descriptions for mountaineers or hikers commonly include the two-thousanders, especially in areas where only a few summits exceed this level. Examples from these regions of the Eastern Alps are: * the striking Nebelhorn (2,224 m) near Oberstdorf or the Säuling (2,047 m) near Neuschwanstein, * the Admonter Reichenstein (2,251 m), Eisenerzer Reichenstein (2,165 m), Großer Pyhrgas (2,244 m) or Hochtor (2,369&n ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Duffey Peak
Duffey Peak is a mountain summit located in southwest British Columbia, Canada. Description Duffey Peak is part of the Joffre Group, which is a subset of the Lillooet Ranges of the Coast Mountains. It is situated east of Pemberton, and immediately northeast of Lillooet Lake. The nearest higher neighbor is Slalok Mountain, to the northeast and the two peaks are connected by Two Goat Ridge. Precipitation runoff from the peak drains into Joffre Creek and Twin One Creek, both of which are tributaries of the Lillooet River. Topographic relief is significant as the summit rises over 2,000 meters (6,560 feet) above Lillooet Lake in four kilometers (2.5 miles). The summit offers a panoramic view of the lake as well as Mount Matier, Mount Hartzell, Mount Spetch, Slalok Mountain, and Mount Taylor. Etymology The mountain is named in association with Duffey triangulation station. The toponym was officially adopted on January 23, 1979, by the Geographical Names Board of Canad ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pemberton Valley
The Pemberton Valley is a valley flanking the Lillooet River upstream from Lillooet Lake, including the communities of Mount Currie, Pemberton, British Columbia and the agricultural district surrounding them and flanking the river as far upstream as the Pemberton Meadows area. The term is normally used only to refer to inhabited parts of the valley, not the unsettled areas to the north of Pemberton Meadows although the official definition extends from the head of Lillooet Lake all the way up to the confluence of Meager Creek. Historically the region was part of the Lillooet Country but due to re-orientation of the area's economy and society since the opening and expansion of BC Highway 99 the area is now more considered to be part of the Sea-to-Sky Corridor The Sea-to-Sky Corridor, often referred to as the Corridor or the Sea to Sky Country, is a region in British Columbia spreading from Horseshoe Bay through Whistler to the Pemberton Valley and sometimes beyond to include ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Howard (British Columbia)
Mount Howard is a mountain summit located in the Coast Mountains of British Columbia, Canada. It is part of the Joffre Group, which is a subset of the Lillooet Ranges. Mount Howard is situated east of Pemberton and immediately southeast of Mount Matier. Precipitation runoff from the peak drains into Twin One Creek thence Lillooet Lake which is within the Lillooet River watershed. Mount Howard is more notable for its steep rise above local terrain than for its absolute elevation as topographic relief is significant with the summit rising 1,650 meters (5,413 ft) above Twin One Creek in . Etymology The mountain was named after John Howard, (1944–1978), an avid mountaineer and founder of a guide service that opened up the Joffre Group area for other climbers. He was killed in a climbing accident near the Columbia Icefield when he fell into a crevasse near the top of the Athabasca Glacier on February 23, 1978. The mountain's toponym was officially adopted June 11 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Slalok Mountain
Slalok Mountain, originally known as Rex's Pillar, is a mountain summit located in the Coast Mountains, in Joffre Lakes Provincial Park, in southwestern British Columbia, Canada. It is the third-highest point of the Joffre Group, which is a subset of the Lillooet Ranges. It is situated east of Pemberton, and northeast of Lillooet Lake. It is northeast of Duffey Peak and the nearest higher peak is Mount Matier, to the east. Precipitation runoff from the peak drains into Joffre Creek and Twin One Creek, both tributaries of the Lillooet River. The first ascent of the mountain was made in 1963 by C. Adam, T. Anderson, and G. Richardson. The mountain's name ''Slalok'' is the traditional name for the settlement of nearby Mount Currie. The name was officially adopted on June 11, 1979, by the Geographical Names Board of Canada. The mountain and its climate supports the Matier Glacier, Stonecrop Glacier, and Tszil Glacier on the northern slopes. Climate Based on the Köppen clima ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geology Of British Columbia
The geology of British Columbia is a function of its location on the leading edge of the North American continent. The mountainous physiography and the diversity of rock types and ages hint at the complex geology, which is still undergoing revision despite a century of exploration and mapping. The country's most prominent geological features are mountain ranges, including the North American Cordillera, which stretches from Southern Mexico to Alaska. Terrane theory Terrane theory was first proposed by Jim Monger of the Geological Survey of Canada and Charlie Rouse in 1971 as an explanation for a set of fusulinid fossils found in central British Columbia. Rather than use facies changes or seaways (which were common explanations at the time), the two geologists proposed that the fossils in question had been part of an assemblage of rocks that had migrated across the Pacific Ocean to their present location. This theory was then developed by Porter Irwin and Davy Jones of the US ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geography 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 state except Alaska. It is bounded on the northwest by the U.S. state of Alaska, directly north by Yukon and the Northwest Territories, on the east by Alberta, and on the south by the U.S. states of Washington, Idaho, and Montana. Formerly part of the British Empire, the southern border of British Columbia was established by the 1846 Oregon Treaty. The province is dominated by mountain ranges, among them the Canadian Rockies but dominantly the Coast Mountains, Cassiar Mountains, and the Columbia Mountains. Most of the population is concentrated on the Pacific coast, notably in the area of Vancouver, located on the southwestern tip of the mainland, which is known as the Lower Mainland. It is the most mountainous province of Canada. Statist ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Orographic Lift
Orographic lift occurs when an air mass is forced from a low elevation to a higher elevation as it moves over rising terrain. As the air mass gains altitude it quickly cools down adiabatically, which can raise the relative humidity to 100% and create clouds and, under the right conditions, precipitation. Orographic lifting can have a number of effects, including precipitation, rain shadowing, leeward winds, and associated clouds. Precipitation Precipitation induced by orographic lift occurs in many places throughout the world. Examples include: * The Mogollon Rim in central Arizona * The western slope of the Sierra Nevada range in California * The mountains near Baja California North – specifically La Bocana to Laguna Hanson. * The windward slopes of Khasi and Jayantia Hills (see Mawsynram) in the state of Meghalaya in India. * The Western Highlands of Yemen, which receive by far the most rain in Arabia. * The Western Ghats that run along India's western coast. * The Grea ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Weather Front
A weather front is a boundary separating air masses for which several characteristics differ, such as air density, wind, temperature, and humidity. Disturbed and unstable weather due to these differences often arises along the boundary. For instance, cold fronts can bring bands of thunderstorms and cumulonimbus precipitation or be preceded by squall lines, while warm fronts are usually preceded by stratiform precipitation and fog. In summer, subtler humidity gradients are known as dry lines can trigger severe weather. Some fronts produce no precipitation and little cloudiness, although there is invariably always a wind shift. Cold fronts generally move from west to east, whereas warm fronts move poleward, although any direction is possible. Occluded fronts are a hybrid merge of the two, and stationary fronts are stalled in their motion. Cold fronts and cold occlusions move faster than warm fronts and warm occlusions because the dense air behind them can lift as well as push ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Marine West Coast
An oceanic climate, also known as a marine climate, is the humid temperate climate sub-type in Köppen classification ''Cfb'', typical of west coasts in higher middle latitudes of continents, generally featuring cool summers and mild winters (for their latitude), with a relatively narrow annual temperature range and few extremes of temperature. Oceanic climates can be found in both hemispheres generally between 45 and 63 latitude, most notably in northwestern Europe, northwestern America, as well as New Zealand. Precipitation Locations with oceanic climates tend to feature frequent cloudy conditions with precipitation, low hanging clouds, and frequent fronts and storms. Thunderstorms are normally few, since strong daytime heating and hot and cold air masses meet infrequently in the region. In most areas with an oceanic climate, precipitation comes in the form of rain for the majority of the year. However, some areas with this climate see some snowfall annually during winter. M ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
