On the formation of large subglacial lakes
Autor: | E. M. Shoemaker |
---|---|
Rok vydání: | 1991 |
Předmět: | |
Zdroj: | Canadian Journal of Earth Sciences. 28:1975-1981 |
ISSN: | 1480-3313 0008-4077 |
DOI: | 10.1139/e91-179 |
Popis: | The role of subglacial water storage beneath continental ice sheets is investigated, primarily for a deformable bed. Subglacial ponding is shown to occur under most regions of warm-based ice sheets, and large subglacial lakes can become established, for example in the Hudson Bay basin. The formation of large lakes depends upon the fact that the ice-surface gradient is reduced once subglacial ponding occurs and upon the feedback between the reduced ice-surface gradient and increased subglacial ponding. Subglacial ponding likely played a large role in determining the ice-sheet topography during late deglaciation and in speeding up the deglaciation process. |
Databáze: | OpenAIRE |
Externí odkaz: |