Mechanical and hydrologic basis for the rapid motion of a large tidewater glacier: 2. Interpretation
- 10 August 1994
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research
- Vol. 99 (B8), 15231-15244
- https://doi.org/10.1029/94jb00467
Abstract
No abstract availableKeywords
This publication has 24 references indexed in Scilit:
- Characteristics of the bed of the Lower Columbia Glacier, AlaskaJournal of Geophysical Research, 1993
- Glacier surge mechanism based on linked cavity configuration of the basal water conduit systemJournal of Geophysical Research, 1987
- Analysis of time series of glacier speed: Columbia Glacier, AlaskaJournal of Geophysical Research, 1987
- Columbia Glacier, Alaska: Changes in velocity 1977–1986Journal of Geophysical Research, 1987
- Fast glacier flow: Ice streams, surging, and tidewater glaciersJournal of Geophysical Research, 1987
- A sliding law for glaciers of constant viscosity in the presence of subglacial cavitationProceedings of the Royal Society of London. Series A. Mathematical and Physical Sciences, 1986
- Glacier Surge Mechanism: 1982-1983 Surge of Variegated Glacier, AlaskaScience, 1985
- TEMPERATE VALLEY GLACIERSPublished by Elsevier ,1980
- General theory of water flow at the base of a glacier or ice sheetReviews of Geophysics, 1972
- Sliding motion of glaciers: Theory and observationReviews of Geophysics, 1970