Sediment dynamics and geohazards offshore Uruguay and northern Argentina: first results from the multi-disciplinary Meteor-cruise M78-3
About 90% of the sediments generated by weathering and erosion on land get finally deposited at the ocean margins. The sediment distribution processes and landscape evolution on land are relatively well understood, but comparably little is known about the role and relative importance of marine sedim...
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ftoceanrep:oai:oceanrep.geomar.de:9981 2023-05-15T14:00:12+02:00 Sediment dynamics and geohazards offshore Uruguay and northern Argentina: first results from the multi-disciplinary Meteor-cruise M78-3 Krastel, Sebastian Freudenthal, Tim Hanebuth, Till Preu, Benedict Schwenck, Tilmann Strasser, Michael Violante, Roberto Wefer, Gerold Winkelmann, Daniel 2010 text https://oceanrep.geomar.de/id/eprint/9981/ https://oceanrep.geomar.de/id/eprint/9981/1/EGU2010-5562.pdf http://meetings.copernicus.org/egu2010/ en eng https://oceanrep.geomar.de/id/eprint/9981/1/EGU2010-5562.pdf Krastel, S. , Freudenthal, T., Hanebuth, T., Preu, B., Schwenck, T., Strasser, M., Violante, R., Wefer, G. and Winkelmann, D. (2010) Sediment dynamics and geohazards offshore Uruguay and northern Argentina: first results from the multi-disciplinary Meteor-cruise M78-3. [Poster] In: EGU General Assembly. , 02.05.-07.05.2010, Vienna, Austria . Conference or Workshop Item NonPeerReviewed 2010 ftoceanrep 2023-04-07T14:57:43Z About 90% of the sediments generated by weathering and erosion on land get finally deposited at the ocean margins. The sediment distribution processes and landscape evolution on land are relatively well understood, but comparably little is known about the role and relative importance of marine sediment dynamics in controlling the architectural evolution of ocean margins. Important players include hemi-pelagic settling, down-slope and current-controlled along-slope sediment transport, depositional and post-depositional sedimentary processes (e.g. consolidation and diagenesis), as well as the destabilization of sediment bodies and their erosion. Submarine landslides in this context thus may represent an important sediment transport process, but also a major geo-hazard due to the increasing number of offshore constructions as well as their potential to instantaneously displace large water masses triggering waves in densely populated coastal areas. Here we present first results from a seagoing expedition that aimed at investigating the interaction processes of sediment redistribution, partitioning, deposition and diagenesis from the coast to the deep-sea along the western South-Atlantic passive continental margin. During RV Meteor Cruise M78/3 in May-July 2009 the shelf, slope and rise offshore Argentina and Uruguay have been investigated by means of hydroacoustic and seismic mapping as well as geological sampling with conventional coring tools as well as the new MARUM seafloor drill rig (MeBo) that revealed recovery of geological strata sampled from up to 50m below seafloor. The working area is characterized by a high amount of fluvial input by the Rio de la Plata river. The continental slope is relatively wide and shows average slope gradients between 1 and 2.5 but locally higher slope gradients may occur (>5). The transition for the continental rise with low slope gradients is found in ~3000 m water depth. The working area is located in a highly dynamic oceanographic regime. Cold Antarctic water masses of the ... Conference Object Antarc* Antarctic OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel) Antarctic Argentina Uruguay |
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OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel) |
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ftoceanrep |
language |
English |
description |
About 90% of the sediments generated by weathering and erosion on land get finally deposited at the ocean margins. The sediment distribution processes and landscape evolution on land are relatively well understood, but comparably little is known about the role and relative importance of marine sediment dynamics in controlling the architectural evolution of ocean margins. Important players include hemi-pelagic settling, down-slope and current-controlled along-slope sediment transport, depositional and post-depositional sedimentary processes (e.g. consolidation and diagenesis), as well as the destabilization of sediment bodies and their erosion. Submarine landslides in this context thus may represent an important sediment transport process, but also a major geo-hazard due to the increasing number of offshore constructions as well as their potential to instantaneously displace large water masses triggering waves in densely populated coastal areas. Here we present first results from a seagoing expedition that aimed at investigating the interaction processes of sediment redistribution, partitioning, deposition and diagenesis from the coast to the deep-sea along the western South-Atlantic passive continental margin. During RV Meteor Cruise M78/3 in May-July 2009 the shelf, slope and rise offshore Argentina and Uruguay have been investigated by means of hydroacoustic and seismic mapping as well as geological sampling with conventional coring tools as well as the new MARUM seafloor drill rig (MeBo) that revealed recovery of geological strata sampled from up to 50m below seafloor. The working area is characterized by a high amount of fluvial input by the Rio de la Plata river. The continental slope is relatively wide and shows average slope gradients between 1 and 2.5 but locally higher slope gradients may occur (>5). The transition for the continental rise with low slope gradients is found in ~3000 m water depth. The working area is located in a highly dynamic oceanographic regime. Cold Antarctic water masses of the ... |
format |
Conference Object |
author |
Krastel, Sebastian Freudenthal, Tim Hanebuth, Till Preu, Benedict Schwenck, Tilmann Strasser, Michael Violante, Roberto Wefer, Gerold Winkelmann, Daniel |
spellingShingle |
Krastel, Sebastian Freudenthal, Tim Hanebuth, Till Preu, Benedict Schwenck, Tilmann Strasser, Michael Violante, Roberto Wefer, Gerold Winkelmann, Daniel Sediment dynamics and geohazards offshore Uruguay and northern Argentina: first results from the multi-disciplinary Meteor-cruise M78-3 |
author_facet |
Krastel, Sebastian Freudenthal, Tim Hanebuth, Till Preu, Benedict Schwenck, Tilmann Strasser, Michael Violante, Roberto Wefer, Gerold Winkelmann, Daniel |
author_sort |
Krastel, Sebastian |
title |
Sediment dynamics and geohazards offshore Uruguay and northern Argentina: first results from the multi-disciplinary Meteor-cruise M78-3 |
title_short |
Sediment dynamics and geohazards offshore Uruguay and northern Argentina: first results from the multi-disciplinary Meteor-cruise M78-3 |
title_full |
Sediment dynamics and geohazards offshore Uruguay and northern Argentina: first results from the multi-disciplinary Meteor-cruise M78-3 |
title_fullStr |
Sediment dynamics and geohazards offshore Uruguay and northern Argentina: first results from the multi-disciplinary Meteor-cruise M78-3 |
title_full_unstemmed |
Sediment dynamics and geohazards offshore Uruguay and northern Argentina: first results from the multi-disciplinary Meteor-cruise M78-3 |
title_sort |
sediment dynamics and geohazards offshore uruguay and northern argentina: first results from the multi-disciplinary meteor-cruise m78-3 |
publishDate |
2010 |
url |
https://oceanrep.geomar.de/id/eprint/9981/ https://oceanrep.geomar.de/id/eprint/9981/1/EGU2010-5562.pdf http://meetings.copernicus.org/egu2010/ |
geographic |
Antarctic Argentina Uruguay |
geographic_facet |
Antarctic Argentina Uruguay |
genre |
Antarc* Antarctic |
genre_facet |
Antarc* Antarctic |
op_relation |
https://oceanrep.geomar.de/id/eprint/9981/1/EGU2010-5562.pdf Krastel, S. , Freudenthal, T., Hanebuth, T., Preu, B., Schwenck, T., Strasser, M., Violante, R., Wefer, G. and Winkelmann, D. (2010) Sediment dynamics and geohazards offshore Uruguay and northern Argentina: first results from the multi-disciplinary Meteor-cruise M78-3. [Poster] In: EGU General Assembly. , 02.05.-07.05.2010, Vienna, Austria . |
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1766269202701746176 |