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As ice sheets grow, the pressure of their
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weight on the underlyingion bedrock
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becomes significant.
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Due to the different densities of ice and
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rock, a ice sheet of 3000m thickness is
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roughly equivalent to the weight of
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1000m of solid rock.
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The initial sinking would be elastic and
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immediate.
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The bedrock later respond more slowly
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and sinks half of the remaining distance
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toward the eventual equilibrium every
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3000 years.
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The total time to reach the final
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depression depth is about 15,000 years.
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