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Darling Peak
Darling Peak is a mountain summit located in British Columbia, Canada. Description Darling Peak is set within Garibaldi Provincial Park and is part of the Garibaldi Ranges of the Coast Mountains. It is situated along the western edge of the Mamquam Icefield, north of Vancouver and northwest of line parent Mamquam Mountain. Precipitation runoff from the peak drains to Skookum Creek, thence Mamquam River. Topographic relief is significant as the summit rises over 900 meters (2,953 feet) above Skookum Creek in four kilometers (2.5 miles). Etymology The landform was named by the Garibaldi Park Board (circa 1928) after Basil S. Darling (1885–1962), a pioneering climber in the area. He was born in Toronto; went to Vancouver in 1908; relocated to Toronto in 1916; and retired to Victoria in 1926. Basil Darling is credited with the first ascents of Cathedral Mountain (1908), Sky Pilot Mountain (1910), Mount Tantalus (1911), Atwell Peak (1911), Serratus Mountain (19 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mamquam Mountain
Mamquam Mountain is a mountain in the Pacific Ranges of the Coast Mountains in southwestern British Columbia, Canada, located southeast of Eanastick Meadows and east of Brackendale. It represents the highest summit of the Mamquam Icefield and lies at the southern end of Garibaldi Provincial Park. Mamquam Mountain was named on September 2, 1930 in association with the Mamquam River. Climate Based on the Köppen climate classification, Mamquam 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. The months July ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sky Pilot Mountain (British Columbia)
Sky Pilot Mountain is a mountain in British Columbia in Canada. The mountain, and Sky Pilot Rock near Desolation Sound are named for the United Church's mission boat Sky Pilot. Climate Based on the Köppen climate classification, Sky Pilot 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 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. The months July through September offer the most favorable weather for climbi ... [...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] |
Köppen Climate Classification
The Köppen climate classification is one of the most widely used climate classification systems. It was first published by German-Russian climatologist Wladimir Köppen (1846–1940) in 1884, with several later modifications by Köppen, notably in 1918 and 1936. Later, the climatologist Rudolf Geiger (1894–1981) introduced some changes to the classification system, which is thus sometimes called the Köppen–Geiger climate classification system. The Köppen climate classification divides climates into five main climate groups, with each group being divided based on seasonal precipitation and temperature patterns. 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'' indi ... [...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] |
The Red Tusk
The Red Tusk is a mountain in the Tantalus Range of the Pacific Ranges in southwestern British Columbia, Canada, located southeast of Mount Tantalus and west of Cheekye. The Red Tusk gets its name from the reddish metamorphic rock Metamorphic rocks arise from the transformation of existing rock to new types of rock in a process called metamorphism. The original rock (protolith) is subjected to temperatures greater than and, often, elevated pressure of or more, causin ... that forms the mountain. It has a similar appearance to the smaller, but more famous Black Tusk in the Garibaldi Ranges further east. References The Red Tuskin the Canadian Mountain Encyclopedia. * Two-thousanders of British Columbia Pacific Ranges New Westminster Land District {{BritishColumbia-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lydia Mountain
Lydia Mountain is a summit located in the Tantalus Range, in Tantalus Provincial Park, in southwestern British Columbia, Canada. It is situated northwest of Squamish, and south-southeast of Mount Tantalus, which is the highest peak in the Tantalus Range. The nearest higher neighbor is ''The Red Tusk'', to the west, and Mount Niobe lies to the east-southeast. Lake Lovely Water lies below the eastern slope of the peak and precipitation runoff from the peak drains east to the Squamish River, and west to the Clowhom River via Red Tusk Creek. Topographic relief is significant as Lydia Mountain rises 1,400 meters (4,600 feet) above Red Tusk Creek in approximately three kilometers (two miles). The mountain's name was officially adopted on June 6, 1957, by the Geographical Names Board of Canada. The mountain was named for mythic Lydia, of which Tantalus was a primordial ruler in Greek mythology. Several peaks in the Tantalus Range are named in association with Tant ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Alpha Mountain
Alpha Mountain is a summit located in the Tantalus Range, in Tantalus Provincial Park, in southwestern British Columbia, Canada. It is situated northwest of Squamish, and southeast of Mount Tantalus, which is the highest peak in the Tantalus Range. Its nearest higher peak is Serratus Mountain, to the west. The Serratus Glacier lies to the west of Alpha, unnamed glaciers lie on the northern and eastern slopes, and Lake Lovely Water lies below the south slope. Precipitation runoff from the peak drains into tributaries of the Squamish River. History The first ascent of the mountain was made in 1914 by Basil Darling and Alan Morkill via the southwest ridge. These two named the peak shortly after they made the ascent, alluding to Alpha, which is the first letter of the Greek alphabet, because the peak is the first (southeast) summit of the Alpha-Serratus-Tantalus-Zenith Ridge, and also because of its form. The mountain's toponym was officially adopted on June 6, 1957, by the Geogr ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Golden Ears (peaks)
Golden Ears is the name of the double summit that lies north of Maple Ridge, British Columbia and is visible from most of the western Lower Mainland. The mountain is in Golden Ears Provincial Park, and was originally referred to as ''Golden Eyries'', possibly for golden eagles that were observed near the summit. There is confusion about the name, because of the twin summits the peak exhibits. Many people believe that the mountain is named because it looks like ears which become golden in the sunset light. Naming The area encompassing ''Golden Ears'', Edge Peak and Blanshard Peak (Blanshard Needle) was originally called ''The Golden Eyries'', and the name was corrupted to ''Golden Ears''. The similarity of the peak of the double summit to cat ears led people to believe that this mountain had the name ''Golden Ears''. In the 1930s or 1940s the government of the day renamed the entire area to ''Mount Blanshard'', and gave Edge Peak its name, named the southernmost summit Bla ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
