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Skagit Range
The Skagit Range ( ) is a Mountain range#Sub-ranges, subrange of the Cascade Range in southwestern British Columbia, Canada and northwestern Washington (state), Washington, United States, which are known in Canada as the Canadian Cascades or, officially, the Cascade Mountains. The Skagit Range lies to the west of the Skagit River and east and north of the Chilliwack River and flanks the Upper Fraser Valley region of British Columbia's Lower Mainland. Of the three subranges of the Canadian Cascades—the Skagit, Hozameen Range, Hozameen, and Okanagan Range, Okanagan ranges—the Skagit is the most mountainous. It continues north to the Fraser River, sometimes using different local names. The Hope Mountains, and the "Anderson River Group" are separated from the main Skagit Range by distinct natural boundaries, but are otherwise similar in character. Geography According to Fred Beckey there are differences of opinion about the names and locations of the subranges of the north ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
British Columbia
British Columbia (commonly abbreviated as BC) is the westernmost province of Canada, situated between the Pacific Ocean and the Rocky Mountains. It has a diverse geography, with rugged landscapes that include rocky coastlines, sandy beaches, forests, lakes, mountains, inland deserts and grassy plains, and borders the province of Alberta to the east and the Yukon and Northwest Territories to the north. With an estimated population of 5.3million as of 2022, it is Canada's third-most populous province. The capital of British Columbia is Victoria and its largest city is Vancouver. Vancouver is the third-largest metropolitan area in Canada; the 2021 census recorded 2.6million people in Metro Vancouver. The first known human inhabitants of the area settled in British Columbia at least 10,000 years ago. Such groups include the Coast Salish, Tsilhqotʼin, and Haida peoples, among many others. One of the earliest British settlements in the area was Fort Victoria, established ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cascade Alpine Guide
Friedrich Wolfgang Beckey (14 January 1923 – 30 October 2017), known as Fred Beckey, was an American rock climber, mountaineer and book author, who in seven decades of climbing achieved hundreds of first ascents of the tallest peaks and best routes in remote corners of Alaska, the Canadian Rockies and the Pacific Northwest. Among the Fifty Classic Climbs of North America, seven were established by Beckey, often climbing with some of the best known climbers of each generation. Early years Beckey was born in 1923 near Düsseldorf, Germany to Klaus Beckey, a surgeon, and Marta Maria Beckey who was an opera singer. In 1925 economic hardships due to hyperinflation in the Weimar Republic forced his family to emigrate to the United States, settling up in Seattle, Washington. His brother, Helmut "Helmy" Beckey, was born in Seattle in 1926 and would later become Fred's frequent climbing partner. At age twelve, Fred Beckey climbed Boulder Peak in the Cascades by himself, after wandering o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Rexford
Mount Rexford is a prominent mountain summit located in the Cascade Mountains of southwestern British Columbia, Canada. It is situated north of the Canada–United States border, west of Chilliwack Lake, and east of Slesse Mountain, which is its nearest higher neighbor. Precipitation runoff from the peak drains into Nesakwatch and Centre Creeks, both tributaries of the Chilliwack River. Originally known as ''Ensawkwatch'', the mountain was named for an early settler in the area, Rexford, who had a cabin near Slesse Creek and had trap lines in the vicinity. The mountain has two subsidiary peaks known as the Nesakwatch Spires. The mountain's name was officially adopted on June 2, 1950, by the Geographical Names Board of Canada. Mount Rexford was first climbed in July 1951 by Herman Genschorek and Walt Sparling via the West Ridge. Geology Mount Rexford is composed of granitic rock related to the Chilliwack batholith, which intruded the region 26 to 29 million years ago after th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Slesse Mountain
Slesse Mountain, usually referred to as Mount Slesse, is a mountain just north of the US-Canada border, in the Cascade Mountains of British Columbia, near the town of Chilliwack. It is notable for its large, steep local relief. For example, its west face drops over to Slesse Creek in less than . It is also famous for its huge Northeast Buttress; see the climbing notes below. The name means "fang" in the Halkomelem language. Notable nearby mountains include Mount Rexford and Canadian Border Peak in British Columbia, and American Border Peak, Mount Shuksan, and Mount Baker, all in the US state of Washington. Geology Most of Mount Slesse is made up of granitic rocks related to the Chilliwack batholith, which intruded the region 26 to 29 million years ago after the major orogenic episodes in the region. This is part of the Pemberton Volcanic Belt, an eroded volcanic belt that formed as a result of subduction of the Farallon Plate starting 29 million years ago. The primary rock c ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cheam Peak
Cheam Peak or Mount Cheam (pronounced and in English, in Halqemeylem, the local indigenous language, referring to the lowland below. The Halqemeylem name for the mountain is Lhílheqey – ''Theeth-uhl-kay'' – from the word ''Lhelqey'' – "glacier" or "rehydrate", referring to the west ridge of the peak). Description Cheam's structure is pyramidal, with north, northwest, south and east faces. While the north face is the steepest, the northwest face is also sheer. A prominent spur ending in the sub peak called "Red Pyramid" or "Red Tower" () divides the two northern faces. The western ridge divides the northwest and south faces; below the gently sloping south face is the subalpine bowl of Spoon Lake. The southeast ridge ascends from the col with Lady Peak, two km to the southeast; Jones Lake is below the east face. A sharp ridge divides the east and north faces. Cheam is the farthest northerly peak of a small group of peaks known as the Cheam Range, which form a subra ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Barr
Mount Barr is a mountain in the Skagit Range of the Cascade Mountains of southern British Columbia, Canada, located on the northeast side of Wahleach Lake and just southwest of Hope. It is a ridge highpoint with an elevation of . Mount Barr is one of several magmatic features just north of the Chilliwack batholith. It is part of a large circular igneous intrusion that was placed along the Fraser Fault 16 to 21 million years ago. The intrusion is part of the Pemberton Volcanic Belt, an eroded volcanic belt that formed as a result of subduction of the Farallon Plate The Farallon Plate was an ancient oceanic plate. It formed one of the three main plates of Panthalassa, alongside the Phoenix Plate and Izanagi Plate, which were connected by a triple junction. The Farallon Plate began subducting under the west ... starting 29 million years ago. [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hope Mountain
Hope Mountain, commonly called Mount Hope, is a prominent mountain overlooking the town of Hope, British Columbia, Canada from the south. It is the northernmost summit of the Skagit Range of the Cascade Mountains and stands above the confluence of the Coquihalla and Fraser Rivers. Hope Mountain dominates the view of southbound travellers in the lower Fraser Canyon between Yale Yale University is a private research university in New Haven, Connecticut. Established in 1701 as the Collegiate School, it is the third-oldest institution of higher education in the United States and among the most prestigious in the wor ... and Hope. References Canadian Cascades Mountains of the Lower Mainland One-thousanders of British Columbia Yale Division Yale Land District {{BritishColumbiaCoast-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Picket Range
The Picket Range is a small, extremely rugged subrange of the North Cascades in the northwestern part of the American state of Washington. It is entirely contained within North Cascades National Park. It is about long, running northwest–southeast, and lies north of the Skagit River, west of Ross Lake, and east of Mounts Baker and Shuksan. There are at least 21 peaks in the range over high. Swedish American Lage Wernstedt of the U.S. Forest Service mapped the Picket Range in the 1920s and named it for its resemblance to a picket fence (and not for George Pickett). Wernstedt was also apparently responsible for the names of the main peaks, including Mt. Challenger, Fury, Terror, and Phantom. These names first appeared on maps in 1931. There are few trails in the Picket Range, and any excursion there has a strong wilderness character. Most of the access points are characterized as steep brush thick valleys, with little open terrain. Many of the peaks are challenging rock c ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Strait Of Georgia
The Strait of Georgia (french: Détroit de Géorgie) or the Georgia Strait is an arm of the Salish Sea between Vancouver Island and the extreme southwestern mainland coast of British Columbia, Canada and the extreme northwestern mainland coast of Washington, United States. It is approximately long and varies in width from .Environmental History and Features of Puget Sound , NOAA-NWFSC Along with the and , it is a constituent part of the |
Mount Chardonnay
Mount Chardonnay is a prominent mountain summit located in the Skagit Range, which is a subset of the North Cascades in Whatcom County of Washington state. It is situated north of Granite Mountain and east of Goat Mountain in the Mount Baker Wilderness, which is managed by the Mount Baker-Snoqualmie National Forest. Its nearest higher peak is Mount Sefrit, to the southwest. Precipitation runoff from the mountain drains into Silesia Creek, a tributary of the Fraser River. Climate Mount Chardonnay is located in the marine west coast climate zone of western North America. Most weather fronts originate in the Pacific Ocean, and travel northeast toward the Cascade Mountains. As fronts approach the North Cascades, they are forced upward by the peaks of the Cascade Range (Orographic lift), causing them to drop their moisture in the form of rain or snowfall onto the Cascades. As a result, the west side of the North Cascades experiences high precipitation, especially during the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Granite Mountain (Whatcom County, Washington)
Granite Mountain is a mountain summit located in the Skagit Range, which is a subset of the North Cascades in Whatcom County of Washington state. It is situated south of Mount Chardonnay, and northwest of Hannegan Peak in the Mount Baker Wilderness, which is managed by the Mount Baker-Snoqualmie National Forest. Precipitation runoff from the mountain drains into tributaries of the Fraser River and the Nooksack River. Climate Granite Mountain is located in the marine west coast climate zone of western North America. Most weather fronts originate in the Pacific Ocean, and travel northeast toward the Cascade Mountains. As fronts approach the North Cascades, they are forced upward by the peaks of the Cascade Range (Orographic lift), causing them to drop their moisture in the form of rain or snowfall onto the Cascades. As a result, the west side of the North Cascades experiences high precipitation, especially during the winter months in the form of snowfall. Due to its temperat ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
GNIS
The Geographic Names Information System (GNIS) is a database of name and locative information about more than two million physical and cultural features throughout the United States and its territories, Antarctica, and the associated states of the Marshall Islands, Federated States of Micronesia, and Palau. It is a type of gazetteer. It was developed by the United States Geological Survey (USGS) in cooperation with the United States Board on Geographic Names (BGN) to promote the standardization of feature names. Data were collected in two phases. Although a third phase was considered, which would have handled name changes where local usages differed from maps, it was never begun. The database is part of a system that includes topographic map names and bibliographic references. The names of books and historic maps that confirm the feature or place name are cited. Variant names, alternatives to official federal names for a feature, are also recorded. Each feature receives a per ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
