The influence of alpine glaciation on the relief of tectonically active mountain belts
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ID: 293920
2002
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Abstract
A surface processes model incorporating large-scale fluvial processes, local hill-slope processes, and glacial erosion is used to investigate the effect of glaciation on the relief of a fast-growing, narrow orogen. The results of several simulations show that: glaciers concentrate erosion near peaks; fluvial erosion is reduced downstream of glaciers; glaciers with frozen bases can lead to an increase in relief; and the net affect of glaciation in the absence of widespread basal freezing is to reduce relief.
| Reference Key |
openalex_W2138037883
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|---|---|
| Authors | Jonathan Tomkin |
| Journal | american journal of science |
| Year | 2002 |
| DOI |
10.2475/ajs.302.3.169
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| URL | |
| Keywords | Keywords not found |
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