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Crater Mountain (Alaska)
Crater Mountain is an mountain summit located in the North Cascades of Washington state. It is the 29th-highest mountain in the Pasayten Wilderness. The Jerry Glacier resides in the cirque on the upper north slopes of the mountain. The crater-like summit of the mountain is not of volcanic origin. Crater Mountain is grouped in the sub-range Hozameen Range, which also includes Hozomeen Mountain and Jack Mountain. Geology The mountain is composed mostly of Metavolcanic rock and Metasedimentary rock from the Hozameen Group. Most predominate is greenstone from the Jurassic to Permian periods. Crater Mountain is carved from greenstone of the Hozomeen Terrane, once the basaltic floor of the ancient Methow Ocean. The mountain's name probably derives from the craterlike shape of its summit, which was carved from the ancient metamorphosed basalt by modern cirque glaciers. The rugged battlements of the greenstone viewed from the highway rest above phyllite of the Little Jack ter ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Jack Mountain
Jack Mountain is the 17th highest mountain in Washington state. It is one of the 10 non-volcanic peaks in Washington State over . It towers dramatically over the south end of Ross Lake, rising above the lakeshore in only . Nohokomeen Glacier nearly fills the cirque on the upper north slopes of the mountain. History Jack Mountain was first described by surveyor Henry Custer in 1859, and was named for prospector Jack Rowley who was active on Canyon Creek. The first recorded ascent of Jack Mountain was made in 1904 by topographer E.C. Barnard. By the 1980s climbing routes had been established on most ridges, glaciers, and directions, seven in total. Most are but some involve true technical climbing. All are long routes with a great deal of vertical gain, meaning most parties take three to four days to climb the mountain. Geology Rock Types The mountain is composed mostly of Metavolcanic rock and Metasedimentary rock from the Hozameen Group. Most predominant is Greens ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
The Mountaineers (club)
The Mountaineers is an alpine club in the US state of Washington. Founded in 1906, it is organized as an outdoor recreation, education, and conservation 501(c)(3) nonprofit organisation, and is based in Seattle, Washington. The club hosts a wide range of outdoor activities, primarily alpine mountain climbing and hikes. The club also hosts classes, training courses, and social events. The club runs a publishing business, Mountaineers Books, which has several imprints. Publications include '' Mountaineering: The Freedom of the Hills''. Organization and activities The Mountaineers has 7 branches in Western Washington, 3 mountain lodges, and 2 program centers, one in Magnuson Park in Seattle, and one in Tacoma. All classes and trips are organized. History Originally a Seattle-based part of the Mazamas, a Portland based group founded in 1894, The Mountaineers formed their own branch shortly after the 1906 Mazamas Mount Baker expedition and dubbed themselves "The Mountaineers" ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountains Of Whatcom County, Washington
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountains Of Washington (state)
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Little Jack (Mountain)
Little Jack is a 6,745-foot-elevation (2,056 meter) mountain summit in the North Cascades of Washington, United States. It is located within the Pasayten Wilderness. It is situated one mile south of its namesake Jack Mountain, west of Crater Mountain, and east of Ross Lake. Like many North Cascade peaks, Little Jack is more notable for its large, steep rise above local terrain than for its absolute elevation. In the early 1900s, the Forest Service built the Little Jack Trail for the purpose of grazing pack animals on the meadows of Little Jack Mountain.Geology of the North Cascades: A Mountain Mosaic. by Rowland W. Tabor, Ralph Albert Haugerudme. The Mountainers publisher. 1999 The name "Jack" refers to Jack Rowley, a gold prospector in the area during the late 1800s, who was credited with finding gold at Ruby Creek. Climate Little Jack is located in the marine west coast climate zone of western North America. Weather fronts originating in the Pacific Ocean travel east towa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ruby Mountain (Washington)
Ruby Mountain is a prominent mountain summit located in the North Cascades Range of Washington state. It is situated in Ross Lake National Recreation Area which is part of the North Cascades National Park Complex. The Diablo Lake Overlook along the North Cascades Highway is at the foot of the mountain. The nearest higher peak is Colonial Peak, to the southwest. Precipitation runoff on the east side of the mountain drains into Ross Lake via Ruby Creek, whereas the west side of the mountain drains into Diablo Lake via Thunder Creek. Topographic relief is significant as the summit rises above Diablo Lake in approximately two miles. History Ruby Mountain is named in association with Ruby Creek. The mountain rises above the confluence of Ruby Creek and Skagit River. Local tradition holds that in 1872, settlers John Sutter, George Sanger, and John Rowley travelled up the Skagit River and reached Ruby Creek. Sutter found a ruby on the creek, thereby giving it its name. The first ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Beebe Mountain
Beebe Mountain is a mountain summit located in the Cascade Range in the U.S. state of Washington (U.S. state), Washington. It is situated on the border of North Cascades National Park. Its nearest higher neighbor is Elija Ridge, to the southwest, and McKay Ridge is set to the northeast on the opposite side of the North Cascades Highway. The mountain's name honors Frank Beebe who worked for the Forest Service and maintained a cabin near the base of the mountain in the 1920s.Beckey, Fred W. Cascade Alpine Guide, Climbing and High Routes. Seattle, WA: Mountaineers Books, 2008. Precipitation Surface runoff, runoff on the mountain drains into Ross Lake (Washington), Ross Lake via Granite Creek and Panther Creek. Climate Beebe 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 p ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
McKay Ridge
McKay Ridge is a ridge located in Whatcom County in Washington state. It is part of the Okanogan Range which is a sub-range of the North Cascades. It's situated north of the North Cascades Highway on land administered by the Okanogan–Wenatchee National Forest. The nearest higher peak is Majestic Mountain, to the northeast. Precipitation runoff from the ridge drains into Ross Lake via tributaries of the Skagit River. Climate McKay Ridge is located in the marine west coast climate zone of western North America.Beckey, Fred W. Cascade Alpine Guide, Climbing and High Routes. Seattle, WA: Mountaineers Books, 2008. 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, causing them to drop their moisture in the form of rain or snowfall onto the Cascades ( Orographic lift). As a result, the west side of the North Cascades experie ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Jackita Ridge
Jackita Ridge is a prominent ridge located in the Pasayten Wilderness, in Whatcom County of Washington state. It is part of the Hozameen Range which is a subset of the North Cascades. The highest point is called ''Jackita Peak'', and the Jackita Ridge Trail traverses below the west aspect of this summit, providing access for an off-trail scramble to the top. The nearest higher neighbor is Crater Mountain, to the southwest, Jack Mountain is set to the west, and McKay Ridge is to the south. Precipitation runoff from this ridge drains to Ross Lake via Devils Creek and Canyon Creek, which are part of the Skagit River drainage basin. The first ascent may have been made in 1926 by the United States Coast and Geodetic Survey, which placed a ''Jackita'' benchmark. Climate Jackita Ridge is located in the marine west coast climate zone of western North America.Beckey, Fred W. Cascade Alpine Guide, Climbing and High Routes. Seattle, WA: Mountaineers Books, 2008. This climate supp ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geology Of The Pacific Northwest
The geology of the Pacific Northwest includes the composition (including rock, minerals, and soils), structure, physical properties and the processes that shape the Pacific Northwest region of North America. The region is part of the Ring of Fire: the subduction of the Pacific and Farallon Plates under the North American Plate is responsible for many of the area's scenic features as well as some of its hazards, such as volcanoes, earthquakes, and landslides. The geology of the Pacific Northwest is vast and complex. Most of the region began forming about 200 million years ago as the North American Plate started to drift westward during the rifting of Pangaea. Since that date, the western edge of North America has grown westward as a succession of island arcs and assorted ocean-floor rocks have been added along the continental margin. There are at least five geologic provinces in the area: the Cascade Volcanoes, the Columbia Plateau, the North Cascades, the Coast Mountains, and th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geography Of Washington (state)
Washington is the northwesternmost state of the contiguous United States. It borders Idaho to the east, bounded mostly by the meridian running north from the confluence of the Snake River and Clearwater River (about 117°02'23" west), except for the southernmost section where the border follows the Snake River. Oregon is to the south, with the Columbia River forming the western part and the 46th parallel forming the eastern part of the Oregon–Washington border. During Washington's partition from Oregon, the original plan for the border followed the Columbia River east until the confluence with the Snake, and then would have followed the Snake River east; this was changed to keep Walla Walla's fertile farmland in Washington. To the west of Washington lies the Pacific Ocean. Its northern border lies mostly along the 49th parallel, and then via marine boundaries through the Strait of Georgia, Haro Strait, and Strait of Juan de Fuca, with the Canadian province of British Columbi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
North Cascades Highway
North is one of the four compass points or cardinal directions. It is the opposite of south and is perpendicular to east and west. ''North'' is a noun, adjective, or adverb indicating direction or geography. Etymology The word ''north'' is related to the Old High German ''nord'', both descending from the Proto-Indo-European unit *''ner-'', meaning "left; below" as north is to left when facing the rising sun. Similarly, the other cardinal directions are also related to the sun's position. The Latin word ''borealis'' comes from the Greek '' boreas'' "north wind, north", which, according to Ovid, was personified as the wind-god Boreas, the father of Calais and Zetes. ''Septentrionalis'' is from ''septentriones'', "the seven plow oxen", a name of ''Ursa Major''. The Greek ἀρκτικός (''arktikós'') is named for the same constellation, and is the source of the English word ''Arctic''. Other languages have other derivations. For example, in Lezgian, ''kefer'' can mean b ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
