An investigation of the deforming layer/debris-rich basal-ice continuum, illustrated from three Alaskan glaciers
Abstract Three small Alaskan glaciers with different bed conditions were studied: Exit Glacier had a thin deforming layer and produced subglacial and proglacial glaciotectonic land forms; Childs Glacier also had a thin deforming layer but the upper part was frozen to the ice; Matanuska Glacier had n...
Published in: | Journal of Glaciology |
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Format: | Article in Journal/Newspaper |
Language: | English |
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Cambridge University Press (CUP)
1995
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Online Access: | http://dx.doi.org/10.1017/s0022143000034936 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000034936 |