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 | |
| State | Published - 1989 |
All Science Journal Classification (ASJC) codes
- Earth-Surface Processes
Fingerprint
Dive into the research topics of 'Water-pressure coupling of sliding and bed deformation: II. Velocity- depth profiles'. Together they form a unique fingerprint.Cite this
- APA
- Author
- BIBTEX
- Harvard
- Standard
- RIS
- Vancouver