Origin and significance of dispersed facies basal ice: Svínafellsjökull, Iceland
Dispersed facies basal ice – massive (i.e. structureless) ice with dispersed debris aggregates – is present at the margins of many glaciers and, as a product of internal glacial processes, has the potential to provide important information about the mechanisms of glacier flow and the nature of the s...
Main Authors: | , , , |
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Format: | Other Non-Article Part of Journal/Newspaper |
Language: | unknown |
Published: |
2010
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Subjects: | |
Online Access: | https://figshare.com/articles/journal_contribution/Origin_and_significance_of_dispersed_facies_basal_ice_Sv_nafellsj_kull_Iceland/9481457 |