Alpine permafrost

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[[Image:Permafrost-extent-in-the-northern-hemisphere.jpg|thumb|300px|'''[[Permafrost]]''' or permafrost soil is '''[[soil]]''' at or below the '''[[freezing point]]''' of '''[[water]]''' ('''0 °C or 32 °F''') for two or more '''[[years]]'''.]] [[Image:Permafrost-extent-in-the-northern-hemisphere.jpg|thumb|300px|'''[[Permafrost]]''' or permafrost soil is '''[[soil]]''' at or below the '''[[freezing point]]''' of '''[[water]]''' ('''0 °C or 32 °F''') for two or more '''[[years]]'''.]]
-Also see;+ 
 +== Also see; ==
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*'''[[Water Cycle]]''' *'''[[Water Cycle]]'''
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-----+== Reference ==
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* See Wikipedia ''Permafrost'' [http://en.wikipedia.org/wiki/Permafrost] * See Wikipedia ''Permafrost'' [http://en.wikipedia.org/wiki/Permafrost]

Revision as of 15:39, 22 July 2010

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.

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.
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.
Permafrost or permafrost soil is soil at or below the freezing point of water (0 °C or 32 °F) for two or more years.
Permafrost or permafrost soil is soil at or below the freezing point of water (0 °C or 32 °F) for two or more years.


Also see;


Reference

  • See Wikipedia Permafrost [1]

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