Abstract
Deforming till and low-pressure water channels are observed to coexist subglacially, but till also is observed to creep rapidly into low-pressure sub-glacial regions. A simple model shows that these observations are not contradictory. Creep of a thin till to a low-pressure region can occur from a narrow zone only, and will lead to isolation of channels from till farther away. -Author
| Original language | English (US) |
|---|---|
| Pages (from-to) | 200-207 |
| Number of pages | 8 |
| Journal | Journal of Glaciology |
| Volume | 38 |
| Issue number | 128 |
| DOIs | |
| State | Published - 1992 |
All Science Journal Classification (ASJC) codes
- Earth-Surface Processes
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