Internal Geometry and Evolution of Moulins, Storglaciären, Sweden
Abstract The initial conditions needed for formation of moulins are crevasses and a supply of melt water. Water pouring into a crevasse may fill it until it overflows at the lowest point, which is normally near the margin. However, as the crevasse deepens, it intersects englacial channels through wh...
Published in: | Journal of Glaciology |
---|---|
Main Author: | |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Cambridge University Press (CUP)
1988
|
Subjects: | |
Online Access: | http://dx.doi.org/10.1017/s0022143000032305 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000032305 |