over short tome scales (thousands of years), isostatic uplift may temporarily raise mountain summits to higher elevations. However, over longer term (millions of years), continyed erosion will reduce these summits to porgressively lower elevation. As this happens does the concept of the isostatic equilibrium predict for the depth of the bae continental lithospher beneath mountains? Remember that mountains float on the mantle at the base of the continental lithosphere.
2006-08-04
05:26:02
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6 answers
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asked by
dat dude
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Science & Mathematics
➔ Earth Sciences & Geology