Seven Million Years of Glaciation in Greenland

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 gla...

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Bibliographic Details
Main Authors: Larsen, H. C., Saunders, A. D., Clift, P. D., Beget, J., Wei, W., Spezzaferri, S., Ali, J., Cambray, H., Demant, A., Fitton, G., Fram, M. S., Fukuma, K., Gieskes, J., Holmes, Mary Anne, Hunt, J., Lacasse, C., Larsen, L. M., Lykke-Andersen, H., Meltser, A., Morrison, M. L., Nemoto, N., Okay, N., Saito, S., Sinton, C., Stax, R., Vallier, T. L., Vandamme, D., Werner, R.
Format: Text
Language:unknown
Published: DigitalCommons@University of Nebraska - Lincoln 1994
Subjects:
Earth Sciences
Greenland
North Atlantic
Online Access:https://digitalcommons.unl.edu/geosciencefacpub/55
https://digitalcommons.unl.edu/context/geosciencefacpub/article/1054/viewcontent/Holmes_SCIENCE_1994_Seven_million_years__DC_VERSION.pdf
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Summary: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.

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