Glacimarine Sedimentation Processes at Kronebreen and Kongsvegen, Svalbard
Tidewater glaciers deposit sediment at their terminus, thereby reducing the relative water depth. Reduced water depth can lead to increased glacier stability through decreased rates of iceberg calving, glacier thinning and submarine melting. Here we investigate sedimentation processes at the termini...
Published in: | Journal of Glaciology |
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Main Authors: | , , , |
Format: | Text |
Language: | unknown |
Published: |
Dartmouth Digital Commons
2011
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Subjects: | |
Online Access: | https://digitalcommons.dartmouth.edu/facoa/2743 https://doi.org/10.3189/002214311798043708 https://digitalcommons.dartmouth.edu/context/facoa/article/3757/viewcontent/glacimarine_sedimentation_processes_at_kronebreen_and_kongsvegen_svalbard.pdf |