Late Quaternary glaciation and deglaciation of the Bunger Hills, Antarctica

• Published in: Antarctic Science
• Main Authors: Adamson, Donald A., Colhoun, Eric A.
• Format: Article in Journal/Newspaper
• Language: English
• Published: Cambridge University Press (CUP) 1992
• Subjects: Geology; Ecology, Evolution, Behavior and Systematics; Oceanography; Antarctic; The Antarctic; Bunger Hills; Edisto; Edisto Ice Tongue; Antarc*; Antarctic Science; Antarctica; Ice Sheet
• Online Access: http://dx.doi.org/10.1017/s0954102092000658; https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0954102092000658

The Bunger Hills were covered by the Antarctic Ice Sheet during the last glaciation. During deglaciation the ice sheet margin collapsed into the marine inlets and the sea entered the oasis before 7.7 ka BP. Raised beaches occur widely below 8.5 m and indicate uplift at 1.4 m ka −1 during the middle and late Holocene. After the coastal inlets were formed, the Edisto Ice Tongue and Apfels Glacier still impinged on land margins in the west of the oasis. Two sets of marginal moraines were formed; the Older Edisto Moraines after 6.2 ka BP and the Younger Edisto Moraines during the last few centuries. The margins of the Antarctic Ice Sheet and Apfels Glacier in the south have maintained their present positions since at least 5.6 ka BP and probably 10 ka BP.