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

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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 languageEnglish (US)
Pages (from-to)119-129
Number of pages11
JournalJournal of Glaciology
Volume35
Issue number119
DOIs
StatePublished - Jan 1 1989

All Science Journal Classification (ASJC) codes

  • Earth-Surface Processes

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