Morainal bank progradation and sediment accumulation in Disenchantment Bay, Alaska: Response to advancing Hubbard Glacier

Morainal banks are primary features at the margins of advancing and stable to quasi‐stable temperate tidewater glaciers, yet their roles in glacier dynamics and terminus stability are poorly defined by submarine observations. Analysis of new and archival multibeam data and Landsat images of the adva...

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Veröffentlicht in:	Journal of Geophysical Research: Earth Surface 2012-06, Vol.117 (F2), p.n/a
Hauptverfasser:	Goff, John A., Lawson, Daniel E., Willems, Bryce A., Davis, Marcy, Gulick, Sean P. S.
Format:	Artikel
Sprache:	eng
Schlagworte:	bathymetry Cryosphere Deep water Dispersal Dynamic stability Earth sciences Earth, ocean, space Exact sciences and technology Fjords Geophysics Glacial dynamics glacier advance Glaciers Gravity Gullies Hubbard Glacier Landsat Marine geology marine-terminating morainal bank Progradation Remote sensing Satellite imagery Sediment Sediment yield Sedimentation Sedimentation & deposition Sediments Stability analysis Stabilizing Surging (ship motion) Tidewater Water depth
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