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Guard Mountain
Guard Mountain is a summit in British Columbia, Canada. Description Guard Mountain is located within Garibaldi Provincial Park on the southeast side of Garibaldi Lake, and is part of the Garibaldi Ranges of the Coast Mountains. It is situated north of Vancouver, west-southwest of Mount Carr, and southwest of Castle Towers Mountain. Precipitation runoff from the peak drains into Garibaldi Lake and topographic relief is significant as the summit rises 700 meters (2,300 feet) above the lake in one kilometer (0.6 mile). The mountain's toponym was officially adopted on October 4, 1932, by the Geographical Names Board of Canada. Climate Based on the Köppen climate classification, Guard Mountain is located in the marine west coast climate zone of western North America. Most weather fronts originate in the Pacific Ocean, and travel east toward the Coast Mountains where they are forced upward by the range (Orographic lift), causing them to drop their moisture in the f ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Panorama Ridge
Panorama Ridge is a mountain ridge in the Garibaldi Ranges of the Pacific Ranges in southwestern British Columbia, Canada. It is located on the north side of Garibaldi Lake in Garibaldi Provincial Park. Panorama Ridge was named around 1912 by William J. Gray, a Canadian geologist from Vancouver who took most of his panoramic photos on the ridge. Climate Based on the Köppen climate classification, Panorama Ridge is located in the marine west coast climate zone of western North America. Most weather fronts originate in the Pacific Ocean, and travel east toward the Coast Mountains where they are forced upward by the range (Orographic lift), causing them to drop their moisture in the form of rain or snowfall. As a result, the Coast Mountains experience high precipitation, especially during the winter months in the form of snowfall. Winter temperatures can drop below −20 °C with wind chill factors below −30 °C. See also * * Gentian Peak * Geography of British Colum ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Marine West Coast
An oceanic climate, also known as a marine climate or maritime climate, is the temperate climate sub-type in Köppen classification represented as ''Cfb'', typical of west coasts in higher middle latitudes of continents, generally featuring cool to warm summers and cool to 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 40 and 60 degrees latitude, with subpolar versions extending to 70 degrees latitude in some coastal areas. Other varieties of climates usually classified together with these include subtropical highland climates, represented as ''Cwb'' or ''Cfb'', and subpolar oceanic or cold subtropical highland climates, represented as ''Cfc'' or ''Cwc''. Subtropical highland climates occur in some mountainous parts of the subtropics or tropics, some of which have monsoon influence, while their cold variants and subpolar oceanic climates occu ... [...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 (2,3 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Glacier Pikes
Glacier Pikes is a lava dome, located in the Garibaldi Lake volcanic field, British Columbia, Canada. The dome has two rocky points at the southern end of the Sentinel Glacier Neve. It is located within Garibaldi Provincial Park and is part of the Garibaldi Ranges of the Coast Mountains. The mountain's toponym was officially adopted on May 3, 1951, by the Geographical Names Board of Canada. Climate Based on the Köppen climate classification, Glacier Pikes is located in the marine west coast climate zone of western North America. Most weather fronts originate in the Pacific Ocean, and travel east toward the Coast Mountains where they are forced upward by the range (Orographic lift), causing them to drop their moisture in the form of rain or snowfall. As a result, the Coast Mountains experience high precipitation, especially during the winter months in the form of snowfall. Winter temperatures can drop below −20 °C with wind chill factors below −30 °C. Gallery ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
The Sphinx (British Columbia)
The Sphinx is a mountain in the southernmost Coast Mountains of British Columbia, Canada. It is southeast of Garibaldi Lake. Climate Based on the Köppen climate classification, The Sphinx is located in a marine west coast climate zone of western North America. Most weather fronts originate in the Pacific Ocean, and travel east toward the Coast Mountains where they are forced upward by the range (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 cr ...), causing them to drop their moisture in the form of rain or snowfall. As a result, the Coast Mountains experience high precipitation, especially during the winter months in the form of snowfall. Temperatures can drop below −20 °C with wind chill factors below −30 °C. References The Sphinxin the Canadian ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Phyllis's Engine
Phyllis's Engine is a granite pinnacle located in British Columbia, Canada. Description Phyllis's Engine is set within Garibaldi Provincial Park and is part of the Garibaldi Ranges of the Coast Mountains. It is situated north of Vancouver, north-northwest of Mount Carr, and south of line parent Castle Towers Mountain. Precipitation runoff and glacial meltwater from the west side of the peak drains to Garibaldi Lake, and the eastern slope drains to Cheakamus Lake. Topographic relief is significant as the west aspect rises in . History The peak is named after Phyllis Dyke (Mrs. Edward Beltz), a pioneering British Columbia Mountaineering Club member who thought the arrangement of pinnacles and spires resembled a 19th-century steam locomotive, so her fellow climbers jokingly referred to the landform as "Phyllis's Engine", circa 1914.G. P. V. Akrigg, Helen B. Akrigg (1997), ''British Columbia Place Names'', UBC Press, , p. 207 The name was formally submitted by Karl Ricker in 19 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gentian Peak
Gentian Peak is a summit in British Columbia, Canada. Description Gentian Peak is located within Garibaldi Provincial Park on the northeast side of Garibaldi Lake, and is part of the Garibaldi Ranges of the Coast Mountains. It is situated north of Vancouver and west of Castle Towers Mountain. Precipitation runoff from the peak drains south into Garibaldi Lake and north into Helm and Castle Towers creeks, all of which is within the Cheakamus River watershed. Topographic relief is significant as the summit rises 720 meters (2,362 feet) above the lake in . The mountain's toponym was officially adopted on September 2, 1930, by the Geographical Names Board of Canada and refers to a rare species of Gentian flowering plant found in the vicinity. Climate Based on the Köppen climate classification, Gentian Peak is located in the marine west coast climate zone of western North America. Weather fronts originating in the Pacific Ocean travel east toward the Coast Mountains wh ... [...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. St ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Deception Peak
Deception Peak is a summit in British Columbia, Canada. Description Deception Peak is located within Garibaldi Provincial Park on the southeast side of Garibaldi Lake, and is part of the Garibaldi Ranges of the Coast Mountains. It is situated north of Vancouver, west of The Sphinx, and southeast of Guard Mountain. Precipitation runoff from the peak drains to Garibaldi Lake and topographic relief is significant as the summit rises 750 meters (2,460 feet) above the lake in two kilometers (1.2 mile). The mountain was first climbed and named by Neal Carter in 1922. The mountain's toponym was officially adopted on September 2, 1930, by the Geographical Names Board of Canada. Climate Based on the Köppen climate classification, Deception Peak is located in the marine west coast climate zone of western North America. Most weather fronts originate in the Pacific Ocean, and travel east toward the Coast Mountains where they are forced upward by the range (orographic ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Price (British Columbia)
Mount Price is a small stratovolcano in the Garibaldi Ranges of the Pacific Ranges in southwestern British Columbia, Canada. It has an elevation of and rises above the surrounding landscape on the western side of Garibaldi Lake in New Westminster Land District. The mountain contains a number of subfeatures, including Clinker Peak on its western flank, which was the source of two thick lava flows between 15,000 and 8,000 years ago that ponded against glacial ice. These lava flows are structurally unstable, having produced large volcanic landslide, landslides as recently as the 1850s. A large provincial park surrounds Mount Price and other volcanoes in its vicinity. It lies within an ecological region that surrounds much of the Pacific Ranges. Mount Price is associated with a small group of volcanoes called the Garibaldi Lake volcanic field. This forms part of the larger Garibaldi Volcanic Belt, a north−south trending volcanic zone that represents a portion of the Canadian Cas ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
The Table (British Columbia)
The Table, sometimes called Table Mountain, is a high flow-dominated andesite tuya located south of Garibaldi Lake, northeast of Cheekye and north of Mount Garibaldi, British Columbia, Canada. It rises over above the surface of Garibaldi Lake, which lies less than to the north. The Table is almost impossible to climb because sections of the volcano have collapsed, creating steep and exceptionally rotten rock walls on all sides. Geology The Table is part of the Garibaldi Lake volcanic field, a volcanic field that includes a group of nine small andesitic stratovolcanoes and basaltic andesite vents formed during the early Holocene. This in turn is part of the Garibaldi Volcanic Belt and of the Cascade Volcanic Arc that run from southwestern British Columbia to northern California caused by subduction of the Juan de Fuca Plate and Explorer Plate under the North American Plate at the Cascadia subduction zone. Canadian geologist Bill Mathews proposed in 1951 that The Table ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Garibaldi
Mount Garibaldi (, ) is a dormant stratovolcano in the Garibaldi Ranges of the Pacific Ranges in southwestern British Columbia, Canada. It has a maximum elevation of and rises above the surrounding landscape on the east side of the Cheakamus River in New Westminster Land District. In addition to the main peak, Mount Garibaldi has two named sub-peaks. Atwell Peak is a sharp, conical peak slightly higher than the more rounded peak of Dalton Dome. Both were volcanically active at different times throughout Mount Garibaldi's eruptive history. The northern and eastern flanks of Mount Garibaldi are obscured by the Garibaldi Névé, a large snowfield containing several radiating glaciers. Flowing from the steep western face of Mount Garibaldi is the Cheekye River, a tributary of the Cheakamus River. Opal Cone on the southeastern flank is a small volcanic cone from which a lengthy lava flow descends. The western face is a volcanic landslide, landslide feature that formed in a series of c ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
