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Peak rates of glacial erosion, inferred from sediment yields
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of tidewater glaciers, surpass those of fluvial erosion by up
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to an order of magnitude.
They have recently come into
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question, however, because
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Biases inherent in the
approach (effect of rapid
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retreat; sediments sloughing off fjord walls)
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Essentially
nothing is known about characteristics of
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the glaciers or of the drainage basins that cause
these
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high sediment yields.
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Little is
known about whether peak erosion rates,
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found in southern Alaska, are representative of
other
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glacial-tectonic settings.
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