Water-pressure coupling of sliding and bed deformation: II. Velocity- depth profiles

R. B. Alley

doi:10.3189/002214389793701518

Water-pressure coupling of sliding and bed deformation: II. Velocity- depth profiles

R. B. Alley

Geosciences

Research output: Contribution to journal › Article › peer-review

110 Scopus citations

Abstract

Pervasive deformation usually will account for 60-100% of the basal velocity, and the strain-rate will be proportional to the basal shear stress and inversely proportional to the square or cube of the effective pressure. -from Author

Original language	English (US)
Pages (from-to)	119-129
Number of pages	11
Journal	Journal of Glaciology
Volume	35
Issue number	119
DOIs	https://doi.org/10.3189/002214389793701518
State	Published - 1989

All Science Journal Classification (ASJC) codes

Earth-Surface Processes

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title = "Water-pressure coupling of sliding and bed deformation: II. Velocity- depth profiles",

abstract = "Pervasive deformation usually will account for 60-100% of the basal velocity, and the strain-rate will be proportional to the basal shear stress and inversely proportional to the square or cube of the effective pressure. -from Author",

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year = "1989",

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AU - Alley, R. B.

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JO - Journal of Glaciology

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ER -

Water-pressure coupling of sliding and bed deformation: II. Velocity- depth profiles

Abstract

All Science Journal Classification (ASJC) codes

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