The Holocene

 

Advanced Search

Journal Navigation

Journal Home

Subscriptions

Archive

Contact Us

Table of Contents

Sign In to gain access to subscriptions and/or personal tools.
This Article
Right arrow Full Text (PDF)
Right arrow References
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Right arrow Citation Map
Services
Right arrow Email this article to a friend
Right arrow Similar articles in this journal
Right arrow Alert me to new issues of the journal
Right arrow Add to Saved Citations
Right arrow Download to citation manager
Right arrow Add to My Marked Citations
Citing Articles
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Hall, B. L.
Right arrow Articles by Denton, G. H.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation
Social Bookmarking
 Add to CiteULike   Add to Connotea   Add to Del.icio.us   Add to Digg   Add to Reddit   Add to Technorati  
What's this?
The Holocene, Vol. 12, No. 5, 619-627 (2002)
DOI: 10.1191/0959683602hl572rp
© 2002 SAGE Publications

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


Add to CiteULike CiteULike   Add to Connotea Connotea   Add to Del.icio.us Del.icio.us   Add to Digg Digg   Add to Reddit Reddit   Add to Technorati Technorati    What's this?