Rate of late Quaternary ice‐cap thinning on King George Island, South Shetland Islands, West Antarctica defined by cosmogenic 36 Cl surface exposure dating

Glacial landforms on the Barton and Weaver peninsulas of King George Island in the South Shetland Islands, West Antarctica were mapped and dated using terrestrial cosmogenic 36 Cl methods to provide the first quantitative terrestrial record for late Quaternary deglaciation in the South Shetland Isla...

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Bibliographic Details
Published in:Boreas
Main Authors: SEONG, YEONG BAE, OWEN, LEWIS A., LIM, HYOUN SOO, YOON, HO IL, KIM, YEADONG, LEE, YONG IL, CAFFEE, MARC W.
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2009
Subjects:
King George Island
West Antarctica
South Shetland Islands
Weaver
Barton
Antarc*
Antarctica
Ice cap
Online Access:http://dx.doi.org/10.1111/j.1502-3885.2008.00069.x
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1502-3885.2008.00069.x
https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1502-3885.2008.00069.x
Description
Summary:Glacial landforms on the Barton and Weaver peninsulas of King George Island in the South Shetland Islands, West Antarctica were mapped and dated using terrestrial cosmogenic 36 Cl methods to provide the first quantitative terrestrial record for late Quaternary deglaciation in the South Shetland Islands. 36 Cl ages on glacially eroded and striated bedrock surfaces range from 15.5±2.5 kyr to 1.0±0.7 kyr. The 36 Cl ages are younger with decreasing altitude, indicating progressive downwasting of the southwestern part of the Collins Ice Cap at a rate of ∼12 mm yr −1 since 15.5±2.5 kyr ago, supporting the previously published marine records for the timing and estimate of the rate of deglaciation in this region.

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