Landform
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Image:Columbia icefield-Canada.jpg|'''[[Glacier]]''' is a perennial mass of '''[[ice]]''' which moves over land. A glacier forms in locations where the mass accumulation of '''[[snow]]''' and '''[[ice]]''' exceeds ablation over many years. Columbia Icefields, Alberta Canada | Image:Columbia icefield-Canada.jpg|'''[[Glacier]]''' is a perennial mass of '''[[ice]]''' which moves over land. A glacier forms in locations where the mass accumulation of '''[[snow]]''' and '''[[ice]]''' exceeds ablation over many years. Columbia Icefields, Alberta Canada | ||
Image:Airdrie Canada glacier erratic.jpg|'''[[Glacial erratic]]''' is a piece of rock that differs from the size and type of rock native to the area in which it rests. | Image:Airdrie Canada glacier erratic.jpg|'''[[Glacial erratic]]''' is a piece of rock that differs from the size and type of rock native to the area in which it rests. | ||
+ | Image:Glacial lake.JPG|'''[[Glacial lake]]''' is a lake with origins in a melted '''[[glacier]]'''. | ||
Image:Base gully gros morne.jpg|'''[[Gully]]''' is a '''[[landform]]''' created by running '''[[water]]''' '''[[eroding]]''' sharply into '''[[soil]]''', typically on a hillside. Gullies resemble large ditches or small '''[[valleys]]''', but are metres to tens of metres in depth and width. | Image:Base gully gros morne.jpg|'''[[Gully]]''' is a '''[[landform]]''' created by running '''[[water]]''' '''[[eroding]]''' sharply into '''[[soil]]''', typically on a hillside. Gullies resemble large ditches or small '''[[valleys]]''', but are metres to tens of metres in depth and width. | ||
Image:Stockhorn Thun Switzerland.jpg|'''[[Horn]]''' a pyramid-shaped mountain '''[[peak]]''' created by several '''[[glaciers]]''' '''[[eroding]]''' away at different sides of the same '''[[mountain]]''' | Image:Stockhorn Thun Switzerland.jpg|'''[[Horn]]''' a pyramid-shaped mountain '''[[peak]]''' created by several '''[[glaciers]]''' '''[[eroding]]''' away at different sides of the same '''[[mountain]]''' | ||
Image:Glaciers mountain terms.jpg|'''[[Glacier]]''' and '''[[Mountain]]''' terms | Image:Glaciers mountain terms.jpg|'''[[Glacier]]''' and '''[[Mountain]]''' terms | ||
</gallery> | </gallery> |
Revision as of 17:49, 4 July 2010
Gallery
Alpine permafrost (most permafrost is located in high latitudes (i.e. land in close proximity to the North and South poles)) may exist at high altitudes in much lower latitudes. |
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Cliff is a significant vertical, or near vertical, rock exposure. Cliffs are formed as erosion landforms due to the processes of erosion and weathering that produce them. Cliffs are common on coasts, in mountainous areas, escarpments and along rivers. |
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Escarpment is a steep slope or long cliff that results from erosion or faulting and separates two relatively level areas of differing elevations. |
Foothills are geographically defined as gradual increases in hilly areas at the base of a mountain range. They are a transition zone between plains and low relief hills to the adjacent topographically high mountains. |
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Glacial erratic is a piece of rock that differs from the size and type of rock native to the area in which it rests. |
Glacial lake is a lake with origins in a melted glacier. |
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