The influence of alpine glaciation on the relief of tectonically active mountain belts
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
|Collections||ANU Research Publications|
|Source:||American Journal of Science|
|01_Tomkin_The_influence_of_alpine_2002.pdf||1.23 MB||Adobe PDF||Request a copy|
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