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Possible iceberg-produced submarine terraces in Hambergbukta, Spitsbergen

R. Noormets, N. Kirchner, A. E. Flink and J. A. Dowdeswell
Geological Society, London, Memoirs, 46, 101-102, 30 November 2016, https://doi.org/10.1144/M46.121
R. Noormets
1Department of Arctic Geology, University Centre in Svalbard, Longyearbyen N-9171, Norway
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  • For correspondence: Riko.Noormets@unis.no
N. Kirchner
2Department of Physical Geography and Bolin Centre for Climate Research, Stockholm University, Stockholm 106 91, Sweden
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A. E. Flink
1Department of Arctic Geology, University Centre in Svalbard, Longyearbyen N-9171, Norway
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J. A. Dowdeswell
3Scott Polar Research Institute, University of Cambridge, Cambridge CB2 1ER, UK
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Submarine landforms produced by drifting icebergs are common on the sedimentary beds of the polar seas. High-resolution multibeam-bathymetric images have revealed a variety of iceberg-related landforms, ranging from 1 to 2 m high corrugation ridges (e.g. Jakobsson et al. 2011; Graham et al. 2013) to large linear to curvilinear ploughmarks several tens of kilometres long and tens of metres deep, that are often distributed chaotically on polar continental shelves (e.g. Dowdeswell et al. 2010). Extensive lateral erosion of submarine ridge-top sediments in the central Arctic Ocean has also been attributed to the impact of deep-drafted icebergs that were once much more abundant in the Arctic than they are today (Jakobsson et al. 2008).

Description

Submarine terraces with remarkably flat surfaces were observed on the crest and along the distal slope of a large terminal-moraine ridge at the mouth of the Hambergbukta (Fig. 1a, c), a fjord in southeastern Spitsbergen (Fig. 1b). The terraces were recorded at several bathymetric levels from 29–66 m in water depth with their surface areas varying from c. 0.04 km2 to >2 km2 (Fig. 1a, d).

Fig. 1.

(a) Swath-bathymetric imagery …

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Geological Society, London, Memoirs: 46 (1)
Geological Society, London, Memoirs
Volume 46
2016
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Possible iceberg-produced submarine terraces in Hambergbukta, Spitsbergen

R. Noormets, N. Kirchner, A. E. Flink and J. A. Dowdeswell
Geological Society, London, Memoirs, 46, 101-102, 30 November 2016, https://doi.org/10.1144/M46.121
R. Noormets
1Department of Arctic Geology, University Centre in Svalbard, Longyearbyen N-9171, Norway
  • Find this author on Google Scholar
  • Find this author on PubMed
  • Search for this author on this site
  • For correspondence: Riko.Noormets@unis.no
N. Kirchner
2Department of Physical Geography and Bolin Centre for Climate Research, Stockholm University, Stockholm 106 91, Sweden
  • Find this author on Google Scholar
  • Find this author on PubMed
  • Search for this author on this site
A. E. Flink
1Department of Arctic Geology, University Centre in Svalbard, Longyearbyen N-9171, Norway
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  • Find this author on PubMed
  • Search for this author on this site
J. A. Dowdeswell
3Scott Polar Research Institute, University of Cambridge, Cambridge CB2 1ER, UK
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Possible iceberg-produced submarine terraces in Hambergbukta, Spitsbergen

R. Noormets, N. Kirchner, A. E. Flink and J. A. Dowdeswell
Geological Society, London, Memoirs, 46, 101-102, 30 November 2016, https://doi.org/10.1144/M46.121
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