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...

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Bibliographic Details
Published in:Journal of Glaciology
Main Authors: Kehrl, Laura M, Hawley, Robert L, Powell, Ross D, Brigham-Grette, Julie
Format: Text
Language:unknown
Published: Dartmouth Digital Commons 2011
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