Bottom Crevasses in the Ross Ice Shelf

Bottom crevasses were detected at many locations in the southern portion of the Ross Ice Shelf during the 1973-74 austral summer. The crevasses which extended up about 100 m from the bottom of the shelf were detected by radio-echo sounding. These linear features were mapped in some detail at the RIS...

Full description

Bibliographic Details
Published in:Journal of Glaciology
Main Author: Clough, John W.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1975
Subjects:
Online Access:http://dx.doi.org/10.1017/s0022143000034560
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000034560
Description
Summary:Bottom crevasses were detected at many locations in the southern portion of the Ross Ice Shelf during the 1973-74 austral summer. The crevasses which extended up about 100 m from the bottom of the shelf were detected by radio-echo sounding. These linear features were mapped in some detail at the RISP Camp. Wide-angle reflection velocity measurements, airborne radio-echo sounding, and other results of the R1GGS program will be included in the discussion.