Surface lowering of ice-cored moraine by wandering lakes.

J. Pickard

Research output: Contribution to journalArticlepeer-review

22 Citations (Scopus)


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 languageEnglish
Pages (from-to)338-342
Number of pages5
JournalJournal of Glaciology
Issue number102
Publication statusPublished - 1983


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