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Giant iceberg plow marks at more than 1 km water depth offshore West Greenland
Authors:A Kuijpers  F Dalhoff  P Hümbs  A Zotova
Institution:a Geological Survey of Denmark and Greenland (GEUS), Øster Voldgade 10, DK 1350 Copenhagen K, Denmark
b NUNAOIL A/S, Tuapannguit 38, P.O. Box 579, 3900 Nuuk, Greenland
c Innomar Technology GmbH, Schutower Ringstrasse 4, 18069 Rostock, Germany
d Leibniz-Institut für Meereswissenschaften IFM-GEOMAR, Wischhofstrasse 1-3, 24148 Kiel, Germany
e UNESCO-MSU Centre for Marine Geology and Geophysics, Faculty of Geology, Moscow State University, Vorobjevy Gory, 119899 Moscow, Russia
Abstract:During a recent (2006) cruise of RV ‘Dana’ high resolution side-scan sonar and sub-bottom profiling was carried out on selected shelf and slope transects offshore Disko Bugt, central West Greenland. Available commercial seismic data from the margin indicate here irregular seabed morphology with erosional features locally extending down to c. 1100 m water depth. The newly acquired side-scan sonar data reveal the presence of giant iceberg plow marks extending (sub)parallel to the slope between about 800 and 1085 m water depth. The height difference between bottom of the scours and rim crest is up to 40 m. The largest plow marks are about 750 m wide. To date no observed modern icebergs including those from Antarctica have drafts in excess of c. 500 m. Taking into account maximum glacial sea level lowering of c. 120 m, the paleo-iceberg keel depth was at least 950 m. Due to the presence of the relatively shallow (< 700 m) sill of Davis Strait to the south, calving of these paleo-icebergs is thought to have occurred from an ice margin in the Baffin Bay region (Jakobshavn Isbræ paleo-ice stream?). The depth of occurrence (> 1000 m) and dimensions of the plow marks are concluded to be exceptional, and comparable to glacial scouring features reported from the Arctic Ocean.
Keywords:Baffin Bay  West Greenland margin  Jakobshavn Isbræ    side-scan sonar  iceberg plow marks
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