東オングル島水汲み沢の隆起汀線の地形と周氷河地形(日本南極地域観測隊の報告)

Based on the investigation of micro-reliefs and deposits of the Mizukumi Zawa (Valley), which is a small glacial trough near Syowa Station, geomorphic evolution after recession of ice sheet was studied. The valley floor in the investigated area was divided into five raised beaches and gentle slopes...

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Bibliographic Details
Main Authors: 藤原 健蔵, Kenzo FUJIWARA
Format: Report
Language:Japanese
Published: 広島大学教養部地理学教室 1973
Subjects:
Online Access:https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=7701
http://id.nii.ac.jp/1291/00007701/
https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=7701&item_no=1&attribute_id=18&file_no=1