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      Water flow through temperate glaciers

      Author(s): ,
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      Journal: Reviews of Geophysics
      Publisher: American Geophysical Union (AGU)

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          Glacier surge mechanism based on linked cavity configuration of the basal water conduit system

          Barclay Kamb (1987)
          Article 0 comments Cited 230 times – based on 0 reviews     Review now
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            Sediment deformation beneath glaciers: Rheology and geological consequences

            G. Boulton, R. Hindmarsh (1987)
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              Glacier surge mechanism: 1982-1983 surge of variegated glacier, alaska.

              B Kamb, C. F. Raymond, W. D. Harrison … (1985)
              The hundredfold speedup in glacier motion in a surge of the kind the kind that took place in Variegated Glacier in 1982-1983 is caused by the buildup of high water pressure in the basal passageway system, which is made possible by a fundamental and pervasive change in the geometry and water-transport characteristics of this system. The behavior of the glacier in surge has many remarkable features, which can provide clues to a detailed theory of the surging process. The surge mechanism is akin to a proposed mechanism of overthrust faulting.
              Article 0 comments Cited 197 times – based on 0 reviews     Review now
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                Author and article information

                Journal
                Title: Reviews of Geophysics
                Abbreviated Title: Rev. Geophys.
                Publisher: American Geophysical Union (AGU)
                ISSN: 87551209
                Publication date Created: August 1998
                Publication date (Print): August 1998
                Volume: 36
                Issue: 3
                Pages: 299-328
                Article
                DOI: 10.1029/97RG03579
                SO-VID: 6a7d492f-c18b-4cc6-9a38-b2c253dfe02d
                Copyright © © 1998
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                http://doi.wiley.com/10.1002/tdm_license_1.1

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