An Atlas of Submarine Glacial Landforms: Modern, Quaternary and Ancient

Wednesday, 17 December 2014
Julian A. Dowdeswell1, Miquel Canals2, Martin Jakobsson3, Brian Jeremy Todd4, Evelyn K Dowdeswell1 and Kelly A Hogan5, (1)Scott Polar Research Institute, University of Cambridge, Cambridge, United Kingdom, (2)Universitat de Barcelona, GRC Geociencies Marines, Barcelona, Spain, (3)Stockholm University, Department of Geological Sciences, Stockholm, Sweden, (4)Geological Survey of Canada Atlantic, Dartmouth, NS, Canada, (5)NERC British Antarctic Survey, Cambridge, United Kingdom
In the past two decades there have been several advances that make the production of an atlas of submarine glacial landforms timely. First is the development of high-resolution imaging technologies; multi-beam echo-sounding or swath bathymetry that allows the detailed mapping of the sea floor at water depths of tens to thousands of metres across continental margins, and 3-D seismic methods that enable the visualisation of palaeo-continental shelves in Quaternary sediments and ancient palaeo-glacial rocks (e.g. Late Ordovician of Northern Africa). A second technological development is that of ice-breaking or ice-strengthened ships that can penetrate deep into the ice-infested waters of the Arctic and Antarctic, to deploy the multibeam systems. A third component is that of relevance – through both the recognition that the polar regions, and especially the Arctic, are particularly sensitive parts of the global environmental system and that these high-latitude margins (both modern and ancient) are likely to contain significant hydrocarbon resources. An enhanced understanding of the sediments and landforms of these fjord-shelf-slope systems is, therefore, of increasing importance to both academics and industry. We are editing an Atlas of Submarine Glacial Landforms that presents a series of individual contributions that describe, discuss and illustrate features on the high-latitude, glacier-influenced sea floor. Contributions are organised in two ways: first, by position on a continental margin – from fjords, through continental shelves to the continental slope and rise; secondly, by scale – as individual landforms and assemblages of landforms. A final section provides discussion of integrated fjord-shelf-slope systems. Over 100 contributions by scientists from many countries contain descriptions and interpretation of swath-bathymetric data from both Arctic and Antarctic margins and use 3D seismic data to investigate ancient glacial landforms. The Atlas will be published in late 2015 in the Memoir Series of the Geological Society of London.