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The Holocene
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Holocene history of the Wilson Piedmont Glacier along the southern Scott Coast, Antarctica

Brenda L. Hall

Institute for Quaternary and Climate Studies and Department of Geological Sciences, University of Maine, Orono, ME 04469, USA; brendah{at}maine.edu

George H. Denton

Institute for Quaternary and Climate Studies and Department of Geological Sciences, University of Maine, Orono, ME 04469, USA

Geometric and cross-cutting relationships between the Wilson Piedmont Glacier and raised beach ridges indicate that the glacier margin has undergone Holocene ‘ uctuations. During mid-Holocene time, the Wilson Piedmont Glacier retreated to a position less extensive than at present. A subsequent readvance culmi nated less than 250 years ago. Since ad 1956, the glacier and adjacent large snow ramps have retreated up to 600 m in some locations. Large snowbanks have also disappeared. Although the cross-cutting relationships and chronology indicate a late-Holocene advance at approximately the same time as the ‘Little Ice Age’ event, the magnitude and style of that advance differ from those of the classic ‘Little Ice Age’ glacier ‘ uctuations in the Northern Hemisphere.

Key Words: Antarctica • Wilson Piedmont Glacier • raised beaches • ‘Little Ice Age’ • Holocene

The Holocene, Vol. 12, No. 5, 619-627 (2002)
DOI: 10.1191/0959683602hl572rp
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