Abstract
Up to 12 submarine landslides retain a morphological evidence as concave amphitheater-like depressions of various sizes on the middle and upper slope of the Storfjorden and Kveithola Trough-Mouth Fans (TMFs), NW Barents Sea. The largest of them show lateral scarps 35–40 m high that reach the continental shelf edge and cover an area of at least 1,120 km2. Submarine landslides are translational, with headwall and laterals scarps clearly cut into Last Glacial Maximum debris flows deposits. The largest landslides seem to be rooted at the base of a terrigenous/hemipelagic sedimentary unit inferred to be of Middle Weichselian age (Marine Isotopic Stage 3). Stratigraphic, lithological and geotechnical observations suggest that the rapid deposition of a thick sequence of fine-grained, high water content interlaminate plumites is the most important controlling factors in the generation of submarine landslides on the southern Storfjorden and Kveithola TMFs.
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References
Bryn P, Berg K, Forsberg CF, Solheim A, Kvalstad TJ (2005) Explaining the Storegga Slide. Mar Petrol Geol 22:11–19
BS-1377 (1990) British standard methods for soils for engineering purposes, Part 7, Shear strength tests (total stress). British Standards Institution, p 46
Colmenero-Hidalgo E, Rigual Hernández AS, Lucchi RG, Bárcena MA, Sierro FJ, Flores J-A, de Vernal A, Camerlenghi A (2009) Analysis of a new micropalaeontological record from the southern margin of the Svalbard Archipelago (Arctic Ocean): preliminary results and palaeoceanographic implications. Geogaceta 46:91–94
Dimakis P, Elverhøi A, Høeg K, Solheim A, Harbitz C, Laberg JS, Vorren TO, Marr J (2000) Submarine slope stability on high-latitude glaciated Svalbard–Barents Sea margin. Mar Geol 162:303–316
Elverhoi A, De Blasio FV, Butt FA, Issler D, Harbitz C, Engvik L, Solheim A, Marr J (2002) Submarine mass-wasting on glacially-influenced continental slopes: processes and dynamics. In: Dowdeswell JA, O-Cofaigh C (eds) Glacier-influenced sedimentation on high-latitude continental margins, Journal of Geological Soceity, London, Special Publication 203, pp 73–87
Hjelstuen BO, Eldholm O, Faleide JI (2007) Recurrent Pleistocene mega-failures on the SW Barrents Sea margin. Earth Planet Sci Lett 258:605–618
Knies J, Matthiessen J, Vogt C, Laberg JS, Hjelstuem BO, Smelror M, Larsen E, Andreassen K, Eidvin T, Vorrem TO (2009) The Plio-Pleistocene glaciations of the Barents Sea-Svalbard region: a new model based on revised chronostratigraphy. Quat Sci Rev 28:812–829
Laberg JS, Camerlenghi A (2008) Significance of contourites for submarine slope stability. In: Rebesco M, Camerlenghi A (eds) contourites, vol 60, Development in Sedimentology Series. Elsevier, Amsterdam, pp 537–556
Laberg JS, Vorren TO (1996) The glacier-fed fan at the mouth of Storfjorden trough, western Barren Sea: a comparative study. Geol Rundsch 85:338–349
Lee HJ (2009) Timing of occurrence of large submarine landslides on the Atlantic Ocean margin. Mar Geol 264:53–64
Lekens WAH, Sejrup HP, Haflidason H, Petersen GØ, Hjelstuen B, Knorr G (2005) Laminated sediments preceding Heinrich event 1 in the Northern North Sea and Southern Norwegian Sea: Origin, processes and regional linkage. Mar Geol 216:27–50
Leroueil S, Le Bihan JP (1996) Liquid limits and fall cones. Can Geotech J 33:793–798
Lucchi RG, Camerlenghi A, Colmenero-Hidalgo E, Sierro FJ, Bárcena MA, Flores JA, Urgeles R, Macri P, Sagnotti L, Caburlotto A (2010) Sedimentary processes on the Storfjorden trough-mouth fan during last deglaciation phase: the role of subglacial meltwater plumes on continental margin sedimentation. Geophys Res Abstr 12: EGU2010-5753-2
Mangerud J, Dokken T, Hebbeln D, Heggen B, Ingólfsson Ó, Landvik JY, Mejdahl V, Svendsen JI, Vorren TO (1998) Fluctuations of the Svalbard-Barents sea ice sheet during the last 150,000 years. Quat Sci Rev 17:11–42
Pedrosa MT, Camerlenghi A, De Mol B, Urgeles R, Rebesco M, Lucchi RG, SVAIS, EGLACOM cruises shipboard parties (2011) Seabed morphology and shallow sedimentary structure of the Storfjorden and Kveithola Trough-Mouth Fans (north west Barents Sea). Mar Geol 286:65–81
Rebesco M, Liu Y, Camerlenghi A, Winsborrow M, Laberg JS, Caburlotto A, Diviacco P, Accettella D, Sauli C, Wardell N, Tomini I (2011) Deglaciation of the Barents Sea ice sheet - a swath bathymetric and sub-bottom seismic study from the Kveithola Trough. Mar Geol 279:141–147
Rebesco M, Pedrosa MT, Camerlenghi A, Lucchi RG, Sauli C, Dem Mol B, Madrussani G, Urgeles R, Rossi G, Böhm G (2012) One Million Years of Climatic Generated Landslide Events on the Northwestern Barents Sea Continental Margin. In: Yamada Y et al (eds) Submarine mass movements and their consequences, vol. 31, Advances in natural and technological hazards research. Springer, Dordrecht, pp 747–756
Skempton AW (1954) Discussion of the structure of inorganic soils. J Soil Mech Found Div 80:263–264
Vorren TO, Laberg JS, Blaume F, Dowdeswell JA, Kenyon NH, Mienert J, Rumohr J, Werner F (1998) The Norwegian-Greenland sea continental margins: morphology and late quaternary sedimentary processes and environment. Quat Sci Rev 17:273–302
Acknowledgements
This study is supported by Spanish IPY projects SVAIS (POL2006-07390/CGL) and IPY-NICE STREAMS (CTM2009-06370-E/ANT), the Spanish project DEGLABAR (CTM2010-17386) and by OGS IPY Project EGLACOM. We acknowledge Solheim A. and Winkermann D. for revision and improvement of the manuscript. We thank ENI E&P Division for the analysis with X-ray CT scan.
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Lucchi, R.G., Pedrosa, M.T., Camerlenghi, A., Urgeles, R., De Mol, B., Rebesco, M. (2012). Recent Submarine Landslides on the Continental Slope of Storfjorden and Kveithola Trough-Mouth Fans (North West Barents Sea). In: Yamada, Y., et al. Submarine Mass Movements and Their Consequences. Advances in Natural and Technological Hazards Research, vol 31. Springer, Dordrecht. https://doi.org/10.1007/978-94-007-2162-3_65
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