New insights into the formation of submarine glacial landforms from high-resolution Autonomous Underwater Vehicle data ...

Autonomous Underwater Vehicles (AUVs) deployed close to the seafloor can acquire high-resolution geophysical data about the topography and shallow stratigraphy of the seabed, yet have had limited application within the fields of glacial geomorphology and ice sheet reconstruction. Here, we present mu...

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Bibliographic Details
Main Authors: Batchelor, CL, Montelli, A, Ottesen, D, Evans, J, Dowdeswell, EK, Christie, FDW, Dowdeswell, JA
Format: Article in Journal/Newspaper
Language:English
Published: Elsevier BV 2020
Subjects:
Autonomous Underwater Vehicles
Glacial landforms
Grounding-zone wedge
Iceberg ploughmarks
Corrugation ridges
Antarctic Peninsula
Antarctic
Antarc*
Ice Sheet
Iceberg*
Online Access:https://dx.doi.org/10.17863/cam.58295
https://www.repository.cam.ac.uk/handle/1810/311199
Description
Summary:Autonomous Underwater Vehicles (AUVs) deployed close to the seafloor can acquire high-resolution geophysical data about the topography and shallow stratigraphy of the seabed, yet have had limited application within the fields of glacial geomorphology and ice sheet reconstruction. Here, we present multibeam echo-sounding, side-scan sonar, sub-bottom profiler and High-Resolution Synthetic Aperture Sonar (HISAS) data acquired during three AUV dives on the northeast Antarctic Peninsula continental shelf. These data enable glacial landforms, including mega-scale glacial lineations (MSGLs), grounding-zone wedges (GZWs) and iceberg ploughmarks, to be imaged at a horizontal resolution of a few tens of centimetres, allowing for the identification of subtle morphological features. We map tidal ridges that are interpreted as having been formed 1) along the ice-sheet grounding line by the squeezing up of soft seafloor sediments by vertical motion of the grounding line during tidal cycles, and 2) by the tidally driven ...

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