Submarine Topography of the Central Part of Lutzow-Holm Bay and around Ongle Islands, Antarctica

The drowned glacial trough formed when the ice sheet expanded in the past exists in the central part of Lutzow-Holm Bay. The trough extends north-south and joins the drowned glacial troughs off the Honnor Glacier and off the Telen Glacier, and also joins the Shirase Glacier probably. This trough sug...

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Bibliographic Details
Main Author: Kiichi Moriwaki
Format: Report
Language:English
Published: National Institute of Polar Research 1979
Subjects:
Online Access:https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=1033
http://id.nii.ac.jp/1291/00001033/
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