Seven million years of glaciation in Greenland

H. C. Larsen, A. D. Saunders, P. D. Clift*, J. Beget, W. Wei, S. Spezzaferri, J. Ali, H. Cambray, A. Demant, G. Fitton, M. S. Fram, K. Fukuma, J. Gieskes, M. A. Holmes, J. Hunt, C. Lacasse, L. M. Larsen, H. Lykke-Andersen, A. Meltser, M. L. MorrisonN. Nemoto, N. Okay, S. Saito, C. Sinton, R. Stax, T. L. Vallier, D. Vandamme, R. Werner

*Corresponding author for this work

Research output: Contribution to journalArticlepeer-review

244 Citations (Scopus)

Abstract

Glacial till, glaciomarine diamictites, and ice-rafted detritus found in marine cores collected off the shore of southeast Greenland record multiple Late Cenozoic glaciations beginning in the Late Miocene. Distinct rock assemblages and seismic stratigraphic control correlate the diamictites with glaciation of the southeast Greenland margin. Glaciers advanced to the sea during several intervals in the Pliocene and Pleistocene. North Atlantic glaciation may have nucleated in southern Greenland rather than further north because of the high mountains and the high levels of precipitation in this region.

Original languageEnglish
Pages (from-to)952-955
Number of pages4
JournalScience
Volume264
Issue number5161
DOIs
Publication statusPublished - 1994
Externally publishedYes

Fingerprint

Dive into the research topics of 'Seven million years of glaciation in Greenland'. Together they form a unique fingerprint.

Cite this