SHORT NOTES GLACIERS AND ICE-SHEETS: MODERN PROBLEMS AND TECTONIC ASSOCIATIONS

Abstract: Glaciers, and rocks of the Earth’s crust, have a brittle zone (which breaks) above a plastic zone (which flows). The brittle zone is distinguished by crevasses (glaciers) and faults (rocks); the plastic zone by flow structures. Glaciers and ice-sheets such as Greenland and Antarctica flow...

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Bibliographic Details
Main Author: Cliff D. Ollier
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Subjects:
glaciers
creep
melting
tectonic basins
Greenland
Antarc*
Antarctica
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.638.245
http://www.galileomovement.com.au/docs/7.4.09 Oliver Glaciers 4.07.pdf
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Summary:Abstract: Glaciers, and rocks of the Earth’s crust, have a brittle zone (which breaks) above a plastic zone (which flows). The brittle zone is distinguished by crevasses (glaciers) and faults (rocks); the plastic zone by flow structures. Glaciers and ice-sheets such as Greenland and Antarctica flow essentially by creep, and are governed by laws of creep. The surface temperature has negligible effect on flow. Global warming cannot cause a “collapse ” of the ice-caps. The basins of Greenland and Antarctica are, if created by isostatic response to the load of the ice pile, a result of creep in the lower crust or mantle.

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