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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] |
Corrie Peak
Corrie Peak is a summit in British Columbia, Canada. Description Corrie Peak is located within Garibaldi Provincial Park on the southwest side of Cheakamus Lake, and is part of the Garibaldi Ranges of the Coast Mountains. It is situated north of Vancouver and north of Castle Towers Mountain. Precipitation runoff from the peak drains north to Cheakamus Lake which is within the Cheakamus River watershed. Topographic relief is significant as the summit rises 1,430 meters (4,692 feet) above the lake in . Etymology The peak was named in 1916 by Scottish-born botanist John Davidson. In Scotland "Corrie" refers to a steep-sided hollow on a mountain, which in other parts of the world is called a cirque. The mountain's toponym was officially adopted on September 2, 1930, by the Geographical Names Board of Canada as labelled on a 1928 topographic map of Garibaldi Park. Climate Based on the Köppen climate classification, Corrie Peak is located in the marine west coast cli ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Topographic Relief
Terrain (), alternatively relief or topographical relief, is the dimension and shape of a given surface of land. In physical geography, terrain is the lay of the land. This is usually expressed in terms of the elevation, slope, and orientation of terrain features. Terrain affects surface water flow and distribution. Over a large area, it can affect weather and climate patterns. Bathymetry is the study of underwater relief, while hypsometry studies terrain relative to sea level. Importance The understanding of terrain is critical for many reasons: * The terrain of a region largely determines its suitability for human settlement: flatter alluvial plains tend to have better farming soils than steeper, rockier uplands. * In terms of environmental quality, agriculture, hydrology and other interdisciplinary sciences; understanding the terrain of an area assists the understanding of watershed boundaries, drainage characteristics, drainage systems, groundwater systems, water ... [...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] |
The Black Tusk
The Black Tusk, known as Q̓elqámtensa ti Skenknápa in the St'at'imcets (Lillooet) language and as T'ákt'akmúten tl'a Ín7inyáx̱a7en in the Sḵwx̱wú7mesh (Squamish) language, is a stratovolcano and a pinnacle of volcanic rock in Garibaldi Provincial Park of British Columbia, Canada. At above sea level, the upper spire is visible from a great distance in all directions. It is particularly noticeable from the Sea-to-Sky Highway just south of Whistler, British Columbia. Distinctive and immediately identifiable, The Black Tusk is among the best known mountains in the Garibaldi Ranges of the Coast Mountains. The volcano is part of the Garibaldi Volcanic Belt which is a segment of the Canadian Cascade Arc, but it is not within the geographic boundary of the Cascade Range. Indigenous The mountain traditionally is part of the border line between the Squamish and Lil'wat nations. To the Squamish people, this mountain is known as ''T'ákt'akmúten tl'a Ín7inyáx̱a7en'', wh ... [...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] |
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] |
Mount Carr
Mount Carr is a mountain summit located in British Columbia, Canada. Description Mount Carr is set within Garibaldi Provincial Park and is part of the Garibaldi Ranges of the Coast Mountains. It is situated north of Vancouver and south-southeast 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 summit rises 1,440 meters (4,724 feet) above Isosceles Creek in 4 kilometers (2.5 miles). History The peak is named after Frank Edward Carr (1886–1915), Vancouver post office clerk and British Columbia Mountaineering Club executive member, who served with the 7th Battalion, Canadian Expeditionary Forces, in Canada, England and France during World War I. He was killed in action April 26, 1915, in France and is commemorated at the Menin Gate Memorial to the Missing in Belgium. The toponym was of ... [...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] |
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 western slope of the Wasatch Range in Utah. Specifically the Little and Big Cottonwood Canyons. * 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 rece ... [...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 known as dry lines can trigger severe weather. Some fronts produce no precipitation and little cloudiness, although there is invariably 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 the warme ... [...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] |
Köppen Climate Classification
The Köppen climate classification divides Earth climates into five main climate groups, with each group being divided based on patterns of seasonal precipitation and temperature. 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'' indicates a tropical rainforest climate. The system assigns a temperature subgroup for all groups other than those in the ''A'' group, indicated by the third letter for climates in ''B'', ''C'', ''D'', and the second letter for climates in ''E''. Other examples include: ''Cfb'' indicating an oceanic climate with warm summers as indicated by the ending ''b.'', while ''Dwb'' indicates a semi-Monsoon continental climate, monsoonal continental climate ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
