Rapid erosion beneath the Greenland ice sheet

T. Cowton, P. Nienow, I. Bartholomew, A. Sole, D. Mair

Research output: Contribution to journalArticlepeer-review

115 Citations (Scopus)


The Pleistocene ice sheets left a clear signature of erosion, but the rate at which ice sheets erode is difficult to determine from either paleolandscapes or observations of contemporary processes. Here we use two years of sediment flux data, derived from meltwaters emerging from an outlet glacier in west Greenland, to calculate an average rate of subglacial erosion across a catchment extending >50 km inland from the ice margin. Erosion in this zone occurs at 4.8 +/- 2.6 mm a(-1), a rate 1-2 orders of magnitude greater than previous estimates of erosion rate beneath the Greenland Ice Sheet. Our results suggest that where surface meltwaters are able to access the bed, the rate of erosion by ice sheets is in keeping with the rapid erosion observed at temperate alpine glaciers. During deglacial phases, when meltwater was abundant, ice sheet margins should therefore have acted as highly efficient agents of erosion.

Original languageEnglish
Pages (from-to)343-346
Number of pages4
Issue number4
Publication statusPublished - Apr 2012


Dive into the research topics of 'Rapid erosion beneath the Greenland ice sheet'. Together they form a unique fingerprint.

Cite this