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Trophy Mountains
Trophy Mountain (locally called Trophy Mountains or The Trophies) is a mountain in east-central British Columbia, Canada, located in the south-east region of Wells Gray Provincial Park. The Clearwater River flows to the west, Raft River to the east and Spahats Creek to the south. Trophy Mountain is part of the Shuswap Highland. There are nine summits in the group and the highest is . Battle Mountain and Table Mountain are the closest summits to the north and Raft Mountain is immediately south.. Trophy Mountain was given its name by Dan Case, a big-game hunting guide in the area. Trophy Mountain is easily accessible by road and trail. It is a popular summer tourist attraction and is especially noted for colourful alpine meadows. Numerous hiking routes are possible beyond the end of the trail at Sheila Lake. Access Trophy Mountain Road turns east off Clearwater Valley Road (also called Wells Gray Park Road) north of the Yellowhead Highway. The gravel road is steep and rough, and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Shuswap Highland
The Shuswap Highland is a plateau-like hilly area of in British Columbia, Canada. It spans the upland area between the Bonaparte and Thompson Plateaus from the area of Mahood Lake, at the southeast corner of the Cariboo Plateau, southeast towards the lower Shuswap River east of Vernon in the Okanagan. The highland is not a unified range, but a combination of small uplands broken up by the valleys of the Clearwater, North Thompson and Adams Rivers and also by the lowlands in the southwest flanking Shuswap Lake. In that area of the valley are the towns of Falkland, Westwold, and Monte Creek along Highway 97. This area also includes the Spa Hills, and the other isolated pockets of hills and mini-plateaus between the Thompson Plateau proper and Shuswap Lake. The highest point of the Highland is Matterhorn Peak in the Dunn Peak massif at 2636 meters. The Shuswap Highland is in essence a foothill (or transitional) area between the much broader interior plateaus southwest and we ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Trophy Flower Meadows
A trophy is a tangible, durable reminder of a specific achievement, and serves as a recognition or evidence of merit. Trophies are often awarded for sporting events, from youth sports to professional level athletics. In many sports medals (or, in North America, rings) are often given out either as the trophy or along with more traditional trophies. Originally the word trophy, derived from the Greek ''tropaion'', referred to arms, standards, other property, or human captives and body parts (e.g., headhunting) captured in battle. These war trophies commemorated the military victories of a state, army or individual combatant. In modern warfare trophy taking is discouraged, but this sense of the word is reflected in hunting trophies and human trophy collecting by serial killers. Etymology Trophies have marked victories since ancient times. The word ''trophy'', coined in English in 1550, was derived from the French ''trophée'' in 1513, "a prize of war", from Old French ''trophe ... [...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 (2,369&n ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Plateau Of Lakes
In geology and physical geography, a plateau (; ; ), also called a high plain or a tableland, is an area of a highland consisting of flat terrain that is raised sharply above the surrounding area on at least one side. Often one or more sides have deep hills or escarpments. Plateaus can be formed by a number of processes, including upwelling of volcanic magma, extrusion of lava, and erosion by water and glaciers. Plateaus are classified according to their surrounding environment as intermontane, piedmont, or continental. A few plateaus may have a small flat top while others have wide ones. Formation Plateaus can be formed by a number of processes, including upwelling of volcanic magma, extrusion of lava, Plate tectonics movements and erosion by water and glaciers. Volcanic Volcanic plateaus are produced by volcanic activity. The Columbia Plateau in the north-western United States is an example. They may be formed by upwelling of volcanic magma or extrusion of lava. The u ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Volcanic Crater
A volcanic crater is an approximately circular depression in the ground caused by Volcano, volcanic activity. It is typically a bowl-shaped feature containing one or more vents. During Types of volcanic eruptions, volcanic eruptions, molten magma and volcanic gases rise from an underground magma chamber, through a conduit, until they reach the crater's vent, from where the gases escape into the atmosphere and the magma is erupted as lava. A volcanic crater can be of large dimensions, and sometimes of great depth. During certain types of explosive eruptions, a volcano's magma chamber may empty enough for an area above it to subside, forming a type of larger depression known as a caldera. Geomorphology In most volcanoes, the crater is situated at the top of a mountain formed from the erupted volcanic deposits such as lava flows and tephra. Volcanoes that terminate in such a summit crater are usually of a conical form. Other volcanic craters may be found on the flanks of volcanoe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cinder Cone
A cinder cone (or scoria cone) is a steep conical hill of loose pyroclastic fragments, such as volcanic clinkers, volcanic ash, or scoria that has been built around a volcanic vent. The pyroclastic fragments are formed by explosive eruptions or lava fountains from a single, typically cylindrical, vent. As the gas-charged lava is blown violently into the air, it breaks into small fragments that solidify and fall as either cinders, clinkers, or scoria around the vent to form a cone that often is symmetrical; with slopes between 30 and 40°; and a nearly circular ground plan. Most cinder cones have a bowl-shaped crater at the summit. Mechanics of eruption Cinder cones range in size from tens to hundreds of meters tall and often have a bowl-shaped crater at the summit. They are composed of loose pyroclastic material (cinder or scoria), which distinguishes them from ''spatter cones'', which are composed of agglomerated volcanic bombs. The pyroclastic material making up a cinder ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Buck Hill (British Columbia)
Buck Hill is a hill in east-central British Columbia, Canada, located north of Clearwater. It rises from the west slope of Trophy Mountain. Buck Hill is just outside the boundary of Wells Gray Provincial Park. Geology Buck Hill is a cinder cone in the Wells Gray-Clearwater volcanic field. It last erupted about 10,000 years ago during the last glaciation of the Clearwater Valley. A slurry of lava debris and water flowed away from the cone and hardened in Second and Third Canyons further down Trophy Mountain. After the eruption stopped, a glacier smoothed the sides of Buck Hill. Several craters can be found on the west side. Access Buck Hill is one of the most accessible volcanoes in the Wells Gray Park area because one can drive to its base. Access is via Trophy Mountain Road off Clearwater Valley Road (also called Wells Gray Park Road), then some old logging and mining roads to some pits where recent mining for decorative lava rock has occurred. It is not safe to climb Buck Hil ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fissure Vent
A fissure vent, also known as a volcanic fissure, eruption fissure or simply a fissure, is a linear volcanic vent through which lava erupts, usually without any explosive eruption, explosive activity. The vent is often a few metres wide and may be many kilometres long. Fissure vents can cause large flood basalts which run first in lava channels and later in lava tubes. After some time, the eruption tends to become focused at one or more spatter cones. Small fissure vents may not be easily discernible from the air, but the crater rows (see Laki) or the canyons (see Eldgjá) built up by some of them are. The Dike_(geology)#Magmatic_dikes, dikes that feed fissures reach the surface from depths of a few kilometers and connect them to deeper magma chamber, magma reservoirs, often under volcanic centers. Fissures are usually found in or along rifts and rift zones, such as Iceland and the East African Rift. Fissure vents are often part of the structure of shield volcanoes. Icelan ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Intrusion
In geology, an igneous intrusion (or intrusive body or simply intrusion) is a body of intrusive igneous rock that forms by crystallization of magma slowly cooling below the surface of the Earth. Intrusions have a wide variety of forms and compositions, illustrated by examples like the Palisades Sill of New York and New Jersey; the Henry Mountains of Utah; the Bushveld Igneous Complex of South Africa; Shiprock in New Mexico; the Ardnamurchan intrusion in Scotland; and the Sierra Nevada Batholith of California. Because the solid country rock into which magma intrudes is an excellent insulator, cooling of the magma is extremely slow, and intrusive igneous rock is coarse-grained (phaneritic). Intrusive igneous rocks are classified separately from extrusive igneous rocks, generally on the basis of their mineral content. The relative amounts of quartz, alkali feldspar, plagioclase, and feldspathoid is particularly important in classifying intrusive igneous rocks. Intrusions ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Quesnel Highland
The Quesnel Highland is a geographic area in the Central Interior of the Canadian province of British Columbia. As defined by BC government geographer in ''Landforms of British Columbia'', an account and analysis of British Columbia geography that is often cited as authoritative, the Highland is a complex of upland hill and plateau areas forming and defined as being the buffer between the Cariboo Plateau and the Cariboo Mountains, as a sort of highland foothills along the eastern edge of the Interior Plateau running southeast from a certain point southeast of the city of Prince George to the Mahood Lake area at the southeast corner of the Cariboo. S. Holland, ''Landforms of British Columbia'', BC Govt, Vancouver, 1976./ref> Beyond Mahood Lake lies another separately classified area dubbed by Holland the Shuswap Highland which spans similar terrain across the North Thompson and Shuswap Lake-Adams River drainage basins, forming a similar upland-area buffer between the Thompson Plat ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Adams Lake
Adams Lake is a large, deep, coldwater lake in British Columbia, Canada; its average depth ranks 6th in the world. The southern end of the lake is approximately north of the town of Chase in the Shuswap Country region of British Columbia. The lake's upper reaches lie in the northern Monashee Mountains, while its lower end penetrates the Shuswap Highland. The lake supports Chinook, Sockeye and Coho salmon, Kokanee, mountain whitefish and rainbow trout. Geography The lake is long and between and wide. The surface elevation is above sea level. The lake is very deep; with a mean depth of and maximum depth of it is the second deepest lake in British Columbia (next to Quesnel Lake, which has a maximum depth of ) and 6th deepest lake in the world by mean depth. Water flows into the lake though many tributaries (most notably the Upper Adams River, , and Bush Creek). The water drains from the lake as the Lower Adams River which is home to a very large and famous sockeye ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Shuswap Lake
Shuswap Lake (pronounced /ˈʃuːʃwɑːp/) is a lake located in the southern interior of British Columbia, Canada that drains via the Little Shuswap River into Little Shuswap Lake. Little Shuswap Lake is the source of the South Thompson River, a branch of the Thompson River, a tributary of the Fraser River. It is at the heart of a region known as the Columbia Shuswap or "the Shuswap", noted for its recreational lakeshore communities including the city of Salmon Arm. The name "Shuswap" is derived from the Shuswap or Secwepemc First Nations people, the most northern of the Interior Salish peoples, whose territory includes the Shuswap. The Shuswap call themselves /ʃǝxwépmǝx/ in their own language, which is called /ʃǝxwepmǝxtʃín/. Geography The central interior plateau of British Columbia drained by the Fraser and Okanagan rivers is part of the Shuswap terrane in British Columbia and northern Washington state. It is dissected by numerous elongated, glacially- overdeep ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
