The response of the water table in coast
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G Kocurek; N.I Robinson; J.M Sharp Jr.
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Article
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2001
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Elsevier Science
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English
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The water table in some aeolian systems is a control on the type and rate of accumulation, and defines the depth to which deflation will occur in the formation of regional bounding surfaces. At the basinal scale over time, the elevation of the water table may be a function of climate, tectonism, and