Sea Ice Thrust Structures

Unusual thrust structures in thin sea ice sheets were observed in Labrador and Greenland. These structures are the result of thin ice sheets being forced into each other by a combination of wind and waves. When thicker pack ice is subjected to these same forces pressure ridges result.

Bibliographic Details
Main Authors: Weeks, W. F., Anderson, D. L.
Format: Article in Journal/Newspaper
Language:unknown
Published: International Glaciological Society 1958
Subjects:
Online Access:https://authors.library.caltech.edu/45123/
https://authors.library.caltech.edu/45123/1/Anderson_1958p173.pdf
https://resolver.caltech.edu/CaltechAUTHORS:20140422-155026235
Description
Summary:Unusual thrust structures in thin sea ice sheets were observed in Labrador and Greenland. These structures are the result of thin ice sheets being forced into each other by a combination of wind and waves. When thicker pack ice is subjected to these same forces pressure ridges result.