Abstract
Lakes wander when steep ice scarps retreat due to collapse and melt. Rates of wander are c.1.3m yr-1. Rates of lowering due to lake wander on Flanders Moraine (Vestfold Hills, Antarctica) are c.0.05m yr-1, which is comparable to rates from elsewhere attributed to different processes.-from Author
| Original language | English |
|---|---|
| Pages (from-to) | 338-342 |
| Number of pages | 5 |
| Journal | Journal of Glaciology |
| Volume | 29 |
| Issue number | 102 |
| Publication status | Published - 1983 |
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