Evidence for a “Little Ice Age” glacial advance within the Antarctic Peninsula – Examples from glacially-overrun raised beaches

Evidence for a “Little Ice Age” glacial advance within the Antarctic Peninsula – Examples from glacially-overrun raised beaches

Recognition of how dynamic the Antarctic ice sheets and glaciers were during the late Holocene has grown in recent years. Proxy data suggests the presence of Neoglacial advances but few moraines or glacial features from this time have been dated compared to glaciated landscapes of the Northern Hemis...

Full description

Bibliographic Details
Main Authors: Bentley, M.J (Author), DeWitt, R. (Author), Reynolds, L.C (Author), Simkins, L.M (Author), Simms, A.R (Author), Thomas, E.R (Author), Zurbuchen, J. (Author)
Format: Article
Language:English
Published: Elsevier Ltd 2021
Subjects:
Antarctic ice sheets
Antarctic Peninsula
Antarctica
Bayesian networks
Beaches
Climate change
Coast
detection method
England
Glacial advance
Glacial advances
Glacial geology
Glaciers
glacioisostasy
Greenwich
Holocene
Holocenes
Ice
Joinville Island
Last Glacial Maximum
Last Glacial-Interglacial
Late Holocene
Little Ice Age
London [England]
Marguerite Bay
Neoglacial
Northern Hemisphere
Northern Hemispheres
Sea level
Shallow marine
Southern Ocean
tidewater glacier
United Kingdom
Weddell Sea
West Antarctica
Online Access:View Fulltext in Publisher

Internet

View Fulltext in Publisher

Similar Items