DEEP LAKE, CAPE BARNE-ANTARCTICA1

ablation, and a 3.3 m high ice cone to tilting of ice blocks beneath a gravel cover of varying thickness. The temperature of the lake water beneath the ice is thought to be a result of solar heating and the chemical stratification to bc an indication that there has been an arid period in the immedia...

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Bibliographic Details
Main Authors: C. H. Hendy, M. J. Selby, A. T. Wilson
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Subjects:
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.581.9950
http://www.aslo.org/lo/toc/vol_17/issue_3/0356.pdf
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Summary:ablation, and a 3.3 m high ice cone to tilting of ice blocks beneath a gravel cover of varying thickness. The temperature of the lake water beneath the ice is thought to be a result of solar heating and the chemical stratification to bc an indication that there has been an arid period in the immediate past.