High-resolution onshore–offshore morpho-bathymetric records of modern chalk and granitic shore platforms in NW France
Modern shore platforms developed on rocky coasts are key areas for understanding coastal erosion processes during the Holocene. This contribution offers a detailed picture of two contrasted shore-platform systems, based on new high-resolution shallow-water bathymetry, further coupled with aerial LiD...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Duperret, Anne [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2016transfer abstract |
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| Schlagwörter: |
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| Umfang: |
10 |
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| Übergeordnetes Werk: |
Enthalten in: Communication of MRSA Status Upon Transfers of LTCF Residents to an Acute Care Hospital - 2012, Paris |
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| Übergeordnetes Werk: |
volume:348 ; year:2016 ; number:6 ; pages:422-431 ; extent:10 |
| Links: |
|---|
| DOI / URN: |
10.1016/j.crte.2015.06.005 |
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| 520 | |a Modern shore platforms developed on rocky coasts are key areas for understanding coastal erosion processes during the Holocene. This contribution offers a detailed picture of two contrasted shore-platform systems, based on new high-resolution shallow-water bathymetry, further coupled with aerial LiDAR topography. Merged land-sea digital elevation models were achieved on two distinct types of rocky coasts along the eastern English Channel in France (Picardy and Upper-Normandy: PUN) and in a NE Atlantic area (SW Brittany: SWB) in NW France. About the PUN case, submarine steps, identified as paleo-shorelines, parallel the actual coastline. Coastal erosive processes appear to be continuous and regular through time, since mid-Holocene at least. In SWB, there is a discrepancy between contemporary coastline orientation and a continuous step extending from inland to offshore, identified as a paleo-shoreline. This illustrates a polyphased and inherited shore platform edification, mainly controlled by tectonic processes. | ||
| 520 | |a Modern shore platforms developed on rocky coasts are key areas for understanding coastal erosion processes during the Holocene. This contribution offers a detailed picture of two contrasted shore-platform systems, based on new high-resolution shallow-water bathymetry, further coupled with aerial LiDAR topography. Merged land-sea digital elevation models were achieved on two distinct types of rocky coasts along the eastern English Channel in France (Picardy and Upper-Normandy: PUN) and in a NE Atlantic area (SW Brittany: SWB) in NW France. About the PUN case, submarine steps, identified as paleo-shorelines, parallel the actual coastline. Coastal erosive processes appear to be continuous and regular through time, since mid-Holocene at least. In SWB, there is a discrepancy between contemporary coastline orientation and a continuous step extending from inland to offshore, identified as a paleo-shoreline. This illustrates a polyphased and inherited shore platform edification, mainly controlled by tectonic processes. | ||
| 650 | 7 | |a Shore platform |2 Elsevier | |
| 650 | 7 | |a Rocky coast |2 Elsevier | |
| 650 | 7 | |a Shoreline |2 Elsevier | |
| 650 | 7 | |a Land-sea DEM |2 Elsevier | |
| 650 | 7 | |a Bathymetry |2 Elsevier | |
| 650 | 7 | |a Holocene |2 Elsevier | |
| 650 | 7 | |a Tectonics |2 Elsevier | |
| 700 | 1 | |a Raimbault, Céline |4 oth | |
| 700 | 1 | |a Le Gall, Bernard |4 oth | |
| 700 | 1 | |a Authemayou, Christine |4 oth | |
| 700 | 1 | |a van Vliet-Lanoë, Brigitte |4 oth | |
| 700 | 1 | |a Regard, Vincent |4 oth | |
| 700 | 1 | |a Dromelet, Elsa |4 oth | |
| 700 | 1 | |a Vandycke, Sara |4 oth | |
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10.1016/j.crte.2015.06.005 doi GBVA2016007000015.pica (DE-627)ELV040028658 (ELSEVIER)S1631-0713(15)00063-2 DE-627 ger DE-627 rakwb eng 550 910 550 DE-600 910 DE-600 610 VZ 540 VZ 35.18 bkl Duperret, Anne verfasserin aut High-resolution onshore–offshore morpho-bathymetric records of modern chalk and granitic shore platforms in NW France 2016transfer abstract 10 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Modern shore platforms developed on rocky coasts are key areas for understanding coastal erosion processes during the Holocene. This contribution offers a detailed picture of two contrasted shore-platform systems, based on new high-resolution shallow-water bathymetry, further coupled with aerial LiDAR topography. Merged land-sea digital elevation models were achieved on two distinct types of rocky coasts along the eastern English Channel in France (Picardy and Upper-Normandy: PUN) and in a NE Atlantic area (SW Brittany: SWB) in NW France. About the PUN case, submarine steps, identified as paleo-shorelines, parallel the actual coastline. Coastal erosive processes appear to be continuous and regular through time, since mid-Holocene at least. In SWB, there is a discrepancy between contemporary coastline orientation and a continuous step extending from inland to offshore, identified as a paleo-shoreline. This illustrates a polyphased and inherited shore platform edification, mainly controlled by tectonic processes. Modern shore platforms developed on rocky coasts are key areas for understanding coastal erosion processes during the Holocene. This contribution offers a detailed picture of two contrasted shore-platform systems, based on new high-resolution shallow-water bathymetry, further coupled with aerial LiDAR topography. Merged land-sea digital elevation models were achieved on two distinct types of rocky coasts along the eastern English Channel in France (Picardy and Upper-Normandy: PUN) and in a NE Atlantic area (SW Brittany: SWB) in NW France. About the PUN case, submarine steps, identified as paleo-shorelines, parallel the actual coastline. Coastal erosive processes appear to be continuous and regular through time, since mid-Holocene at least. In SWB, there is a discrepancy between contemporary coastline orientation and a continuous step extending from inland to offshore, identified as a paleo-shoreline. This illustrates a polyphased and inherited shore platform edification, mainly controlled by tectonic processes. Shore platform Elsevier Rocky coast Elsevier Shoreline Elsevier Land-sea DEM Elsevier Bathymetry Elsevier Holocene Elsevier Tectonics Elsevier Raimbault, Céline oth Le Gall, Bernard oth Authemayou, Christine oth van Vliet-Lanoë, Brigitte oth Regard, Vincent oth Dromelet, Elsa oth Vandycke, Sara oth Enthalten in Elsevier Communication of MRSA Status Upon Transfers of LTCF Residents to an Acute Care Hospital 2012 Paris (DE-627)ELV026358905 volume:348 year:2016 number:6 pages:422-431 extent:10 https://doi.org/10.1016/j.crte.2015.06.005 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U 35.18 Kolloidchemie Grenzflächenchemie VZ AR 348 2016 6 422-431 10 045F 550 |
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10.1016/j.crte.2015.06.005 doi GBVA2016007000015.pica (DE-627)ELV040028658 (ELSEVIER)S1631-0713(15)00063-2 DE-627 ger DE-627 rakwb eng 550 910 550 DE-600 910 DE-600 610 VZ 540 VZ 35.18 bkl Duperret, Anne verfasserin aut High-resolution onshore–offshore morpho-bathymetric records of modern chalk and granitic shore platforms in NW France 2016transfer abstract 10 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Modern shore platforms developed on rocky coasts are key areas for understanding coastal erosion processes during the Holocene. This contribution offers a detailed picture of two contrasted shore-platform systems, based on new high-resolution shallow-water bathymetry, further coupled with aerial LiDAR topography. Merged land-sea digital elevation models were achieved on two distinct types of rocky coasts along the eastern English Channel in France (Picardy and Upper-Normandy: PUN) and in a NE Atlantic area (SW Brittany: SWB) in NW France. About the PUN case, submarine steps, identified as paleo-shorelines, parallel the actual coastline. Coastal erosive processes appear to be continuous and regular through time, since mid-Holocene at least. In SWB, there is a discrepancy between contemporary coastline orientation and a continuous step extending from inland to offshore, identified as a paleo-shoreline. This illustrates a polyphased and inherited shore platform edification, mainly controlled by tectonic processes. Modern shore platforms developed on rocky coasts are key areas for understanding coastal erosion processes during the Holocene. This contribution offers a detailed picture of two contrasted shore-platform systems, based on new high-resolution shallow-water bathymetry, further coupled with aerial LiDAR topography. Merged land-sea digital elevation models were achieved on two distinct types of rocky coasts along the eastern English Channel in France (Picardy and Upper-Normandy: PUN) and in a NE Atlantic area (SW Brittany: SWB) in NW France. About the PUN case, submarine steps, identified as paleo-shorelines, parallel the actual coastline. Coastal erosive processes appear to be continuous and regular through time, since mid-Holocene at least. In SWB, there is a discrepancy between contemporary coastline orientation and a continuous step extending from inland to offshore, identified as a paleo-shoreline. This illustrates a polyphased and inherited shore platform edification, mainly controlled by tectonic processes. Shore platform Elsevier Rocky coast Elsevier Shoreline Elsevier Land-sea DEM Elsevier Bathymetry Elsevier Holocene Elsevier Tectonics Elsevier Raimbault, Céline oth Le Gall, Bernard oth Authemayou, Christine oth van Vliet-Lanoë, Brigitte oth Regard, Vincent oth Dromelet, Elsa oth Vandycke, Sara oth Enthalten in Elsevier Communication of MRSA Status Upon Transfers of LTCF Residents to an Acute Care Hospital 2012 Paris (DE-627)ELV026358905 volume:348 year:2016 number:6 pages:422-431 extent:10 https://doi.org/10.1016/j.crte.2015.06.005 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U 35.18 Kolloidchemie Grenzflächenchemie VZ AR 348 2016 6 422-431 10 045F 550 |
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10.1016/j.crte.2015.06.005 doi GBVA2016007000015.pica (DE-627)ELV040028658 (ELSEVIER)S1631-0713(15)00063-2 DE-627 ger DE-627 rakwb eng 550 910 550 DE-600 910 DE-600 610 VZ 540 VZ 35.18 bkl Duperret, Anne verfasserin aut High-resolution onshore–offshore morpho-bathymetric records of modern chalk and granitic shore platforms in NW France 2016transfer abstract 10 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Modern shore platforms developed on rocky coasts are key areas for understanding coastal erosion processes during the Holocene. This contribution offers a detailed picture of two contrasted shore-platform systems, based on new high-resolution shallow-water bathymetry, further coupled with aerial LiDAR topography. Merged land-sea digital elevation models were achieved on two distinct types of rocky coasts along the eastern English Channel in France (Picardy and Upper-Normandy: PUN) and in a NE Atlantic area (SW Brittany: SWB) in NW France. About the PUN case, submarine steps, identified as paleo-shorelines, parallel the actual coastline. Coastal erosive processes appear to be continuous and regular through time, since mid-Holocene at least. In SWB, there is a discrepancy between contemporary coastline orientation and a continuous step extending from inland to offshore, identified as a paleo-shoreline. This illustrates a polyphased and inherited shore platform edification, mainly controlled by tectonic processes. Modern shore platforms developed on rocky coasts are key areas for understanding coastal erosion processes during the Holocene. This contribution offers a detailed picture of two contrasted shore-platform systems, based on new high-resolution shallow-water bathymetry, further coupled with aerial LiDAR topography. Merged land-sea digital elevation models were achieved on two distinct types of rocky coasts along the eastern English Channel in France (Picardy and Upper-Normandy: PUN) and in a NE Atlantic area (SW Brittany: SWB) in NW France. About the PUN case, submarine steps, identified as paleo-shorelines, parallel the actual coastline. Coastal erosive processes appear to be continuous and regular through time, since mid-Holocene at least. In SWB, there is a discrepancy between contemporary coastline orientation and a continuous step extending from inland to offshore, identified as a paleo-shoreline. This illustrates a polyphased and inherited shore platform edification, mainly controlled by tectonic processes. Shore platform Elsevier Rocky coast Elsevier Shoreline Elsevier Land-sea DEM Elsevier Bathymetry Elsevier Holocene Elsevier Tectonics Elsevier Raimbault, Céline oth Le Gall, Bernard oth Authemayou, Christine oth van Vliet-Lanoë, Brigitte oth Regard, Vincent oth Dromelet, Elsa oth Vandycke, Sara oth Enthalten in Elsevier Communication of MRSA Status Upon Transfers of LTCF Residents to an Acute Care Hospital 2012 Paris (DE-627)ELV026358905 volume:348 year:2016 number:6 pages:422-431 extent:10 https://doi.org/10.1016/j.crte.2015.06.005 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U 35.18 Kolloidchemie Grenzflächenchemie VZ AR 348 2016 6 422-431 10 045F 550 |
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10.1016/j.crte.2015.06.005 doi GBVA2016007000015.pica (DE-627)ELV040028658 (ELSEVIER)S1631-0713(15)00063-2 DE-627 ger DE-627 rakwb eng 550 910 550 DE-600 910 DE-600 610 VZ 540 VZ 35.18 bkl Duperret, Anne verfasserin aut High-resolution onshore–offshore morpho-bathymetric records of modern chalk and granitic shore platforms in NW France 2016transfer abstract 10 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Modern shore platforms developed on rocky coasts are key areas for understanding coastal erosion processes during the Holocene. This contribution offers a detailed picture of two contrasted shore-platform systems, based on new high-resolution shallow-water bathymetry, further coupled with aerial LiDAR topography. Merged land-sea digital elevation models were achieved on two distinct types of rocky coasts along the eastern English Channel in France (Picardy and Upper-Normandy: PUN) and in a NE Atlantic area (SW Brittany: SWB) in NW France. About the PUN case, submarine steps, identified as paleo-shorelines, parallel the actual coastline. Coastal erosive processes appear to be continuous and regular through time, since mid-Holocene at least. In SWB, there is a discrepancy between contemporary coastline orientation and a continuous step extending from inland to offshore, identified as a paleo-shoreline. This illustrates a polyphased and inherited shore platform edification, mainly controlled by tectonic processes. Modern shore platforms developed on rocky coasts are key areas for understanding coastal erosion processes during the Holocene. This contribution offers a detailed picture of two contrasted shore-platform systems, based on new high-resolution shallow-water bathymetry, further coupled with aerial LiDAR topography. Merged land-sea digital elevation models were achieved on two distinct types of rocky coasts along the eastern English Channel in France (Picardy and Upper-Normandy: PUN) and in a NE Atlantic area (SW Brittany: SWB) in NW France. About the PUN case, submarine steps, identified as paleo-shorelines, parallel the actual coastline. Coastal erosive processes appear to be continuous and regular through time, since mid-Holocene at least. In SWB, there is a discrepancy between contemporary coastline orientation and a continuous step extending from inland to offshore, identified as a paleo-shoreline. This illustrates a polyphased and inherited shore platform edification, mainly controlled by tectonic processes. Shore platform Elsevier Rocky coast Elsevier Shoreline Elsevier Land-sea DEM Elsevier Bathymetry Elsevier Holocene Elsevier Tectonics Elsevier Raimbault, Céline oth Le Gall, Bernard oth Authemayou, Christine oth van Vliet-Lanoë, Brigitte oth Regard, Vincent oth Dromelet, Elsa oth Vandycke, Sara oth Enthalten in Elsevier Communication of MRSA Status Upon Transfers of LTCF Residents to an Acute Care Hospital 2012 Paris (DE-627)ELV026358905 volume:348 year:2016 number:6 pages:422-431 extent:10 https://doi.org/10.1016/j.crte.2015.06.005 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U 35.18 Kolloidchemie Grenzflächenchemie VZ AR 348 2016 6 422-431 10 045F 550 |
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10.1016/j.crte.2015.06.005 doi GBVA2016007000015.pica (DE-627)ELV040028658 (ELSEVIER)S1631-0713(15)00063-2 DE-627 ger DE-627 rakwb eng 550 910 550 DE-600 910 DE-600 610 VZ 540 VZ 35.18 bkl Duperret, Anne verfasserin aut High-resolution onshore–offshore morpho-bathymetric records of modern chalk and granitic shore platforms in NW France 2016transfer abstract 10 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Modern shore platforms developed on rocky coasts are key areas for understanding coastal erosion processes during the Holocene. This contribution offers a detailed picture of two contrasted shore-platform systems, based on new high-resolution shallow-water bathymetry, further coupled with aerial LiDAR topography. Merged land-sea digital elevation models were achieved on two distinct types of rocky coasts along the eastern English Channel in France (Picardy and Upper-Normandy: PUN) and in a NE Atlantic area (SW Brittany: SWB) in NW France. About the PUN case, submarine steps, identified as paleo-shorelines, parallel the actual coastline. Coastal erosive processes appear to be continuous and regular through time, since mid-Holocene at least. In SWB, there is a discrepancy between contemporary coastline orientation and a continuous step extending from inland to offshore, identified as a paleo-shoreline. This illustrates a polyphased and inherited shore platform edification, mainly controlled by tectonic processes. Modern shore platforms developed on rocky coasts are key areas for understanding coastal erosion processes during the Holocene. This contribution offers a detailed picture of two contrasted shore-platform systems, based on new high-resolution shallow-water bathymetry, further coupled with aerial LiDAR topography. Merged land-sea digital elevation models were achieved on two distinct types of rocky coasts along the eastern English Channel in France (Picardy and Upper-Normandy: PUN) and in a NE Atlantic area (SW Brittany: SWB) in NW France. About the PUN case, submarine steps, identified as paleo-shorelines, parallel the actual coastline. Coastal erosive processes appear to be continuous and regular through time, since mid-Holocene at least. In SWB, there is a discrepancy between contemporary coastline orientation and a continuous step extending from inland to offshore, identified as a paleo-shoreline. This illustrates a polyphased and inherited shore platform edification, mainly controlled by tectonic processes. Shore platform Elsevier Rocky coast Elsevier Shoreline Elsevier Land-sea DEM Elsevier Bathymetry Elsevier Holocene Elsevier Tectonics Elsevier Raimbault, Céline oth Le Gall, Bernard oth Authemayou, Christine oth van Vliet-Lanoë, Brigitte oth Regard, Vincent oth Dromelet, Elsa oth Vandycke, Sara oth Enthalten in Elsevier Communication of MRSA Status Upon Transfers of LTCF Residents to an Acute Care Hospital 2012 Paris (DE-627)ELV026358905 volume:348 year:2016 number:6 pages:422-431 extent:10 https://doi.org/10.1016/j.crte.2015.06.005 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U 35.18 Kolloidchemie Grenzflächenchemie VZ AR 348 2016 6 422-431 10 045F 550 |
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Communication of MRSA Status Upon Transfers of LTCF Residents to an Acute Care Hospital |
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High-resolution onshore–offshore morpho-bathymetric records of modern chalk and granitic shore platforms in NW France |
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Modern shore platforms developed on rocky coasts are key areas for understanding coastal erosion processes during the Holocene. This contribution offers a detailed picture of two contrasted shore-platform systems, based on new high-resolution shallow-water bathymetry, further coupled with aerial LiDAR topography. Merged land-sea digital elevation models were achieved on two distinct types of rocky coasts along the eastern English Channel in France (Picardy and Upper-Normandy: PUN) and in a NE Atlantic area (SW Brittany: SWB) in NW France. About the PUN case, submarine steps, identified as paleo-shorelines, parallel the actual coastline. Coastal erosive processes appear to be continuous and regular through time, since mid-Holocene at least. In SWB, there is a discrepancy between contemporary coastline orientation and a continuous step extending from inland to offshore, identified as a paleo-shoreline. This illustrates a polyphased and inherited shore platform edification, mainly controlled by tectonic processes. |
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Modern shore platforms developed on rocky coasts are key areas for understanding coastal erosion processes during the Holocene. This contribution offers a detailed picture of two contrasted shore-platform systems, based on new high-resolution shallow-water bathymetry, further coupled with aerial LiDAR topography. Merged land-sea digital elevation models were achieved on two distinct types of rocky coasts along the eastern English Channel in France (Picardy and Upper-Normandy: PUN) and in a NE Atlantic area (SW Brittany: SWB) in NW France. About the PUN case, submarine steps, identified as paleo-shorelines, parallel the actual coastline. Coastal erosive processes appear to be continuous and regular through time, since mid-Holocene at least. In SWB, there is a discrepancy between contemporary coastline orientation and a continuous step extending from inland to offshore, identified as a paleo-shoreline. This illustrates a polyphased and inherited shore platform edification, mainly controlled by tectonic processes. |
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Modern shore platforms developed on rocky coasts are key areas for understanding coastal erosion processes during the Holocene. This contribution offers a detailed picture of two contrasted shore-platform systems, based on new high-resolution shallow-water bathymetry, further coupled with aerial LiDAR topography. Merged land-sea digital elevation models were achieved on two distinct types of rocky coasts along the eastern English Channel in France (Picardy and Upper-Normandy: PUN) and in a NE Atlantic area (SW Brittany: SWB) in NW France. About the PUN case, submarine steps, identified as paleo-shorelines, parallel the actual coastline. Coastal erosive processes appear to be continuous and regular through time, since mid-Holocene at least. In SWB, there is a discrepancy between contemporary coastline orientation and a continuous step extending from inland to offshore, identified as a paleo-shoreline. This illustrates a polyphased and inherited shore platform edification, mainly controlled by tectonic processes. |
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