Next Reports Climatic Limits on Landscape Development in the Northwestern Himalaya Nicholas Brozovi, * Douglas W. Burbank, Andrew J. Meigs The interaction between tectonism and erosion produces rugged landscapes in actively deforming regions.
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Furthermore, changes in continental weathering and riverine contributions to the oceans may also be linked with climate, and hydrothermal inputs vary with tectonism.
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The thick lithosphere predicted by these models appears to be inconsistent with even a low level of ongoing volcanism and tectonism.
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