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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Format: | Report |
Language: | English |
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National Institute of Polar Research
1979
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Online Access: | https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=1033 http://id.nii.ac.jp/1291/00001033/ https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=1033&item_no=1&attribute_id=18&file_no=1 |