Deception Peak
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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 ...
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Castle Towers Mountain
Castle Towers Mountain is a triple summit mountain on the east side of Garibaldi Lake in southwestern British Columbia, Canada. The first ascent party from the BC Mountaineering Club named the mountain after its appearance in August 1911. Climate Based on the Köppen climate classification, the 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 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. Gallery File:Castle Towers Mountain in winter.jpg, Castle Towers Mountain in winter File:Garibaldi Lake 2.jpg, Castle Towers Mountain (left) and Mount Carr (right) viewe ...
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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 ...
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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 ...
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Pitt River
The Pitt River in British Columbia, Canada is a large tributary of the Fraser River, entering it a few miles upstream from New Westminster and about 25 km ESE of Downtown Vancouver. The river, which begins in the Garibaldi Ranges of the Coast Mountains, is in two sections above and below Pitt Lake and flows on a generally southernly course. Pitt Lake and the lower Pitt River are tidal in nature as the Fraser's mouth is only a few miles downstream from their confluence. The river was named for William Pitt the Younger. The first mention of the name, as "Pitts River", occurs in the 1827 journal kept by James McMillan of the Hudson's Bay Company. The river has an alternate name, Quoitle, which is probably equivalent to Kwantlen. East of the lower Pitt River, 20 km long, is the community of Pitt Meadows, while to its west are the cities of Coquitlam and Port Coquitlam; opposite its mouth is Surrey. Port Coquitlam and Pitt Meadows are connected by the Highway 7 bridges ...
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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 ...
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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 ...
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