The Vestfold Hills:a window on Antarctica.

The uncertainty about the magnitude of the Vestfold glaciation during the terminal Pleistocene is stressed. Water and salt are seen as the major current geomorphological agents in the Hills. -P.J.Jarvis

Bibliographic Details
Main Author: Pickard, J.
Format: Article in Journal/Newspaper
Language:English
Published: 1986
Subjects:
Online Access:https://researchers.mq.edu.au/en/publications/5b7e1515-8ee5-442c-9ac8-df27c15fa62d
http://www.scopus.com/inward/record.url?scp=0022837633&partnerID=8YFLogxK
Description
Summary:The uncertainty about the magnitude of the Vestfold glaciation during the terminal Pleistocene is stressed. Water and salt are seen as the major current geomorphological agents in the Hills. -P.J.Jarvis