Contourites in the Galicia bank (NW Iberian Atlantic)

International Congress Deep Water Circulation: Processes and Products, 16-18 June 2010, Baiona, Pontevedra The Galicia Bank region is under the influence of different water masses (Mediterranean Outflow Water -MOW-, Labrador Sea Water –LSW-, North Atlantic Deep Water-NADW-, and Lower Deep Water –LDW...

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Main Authors: Casas, David, Iglesias, Jorge, Vázquez, Juan Tomás, Somoza, Luis, León Buendía, Ricardo F., Medialdea Cela, Teresa, Juan, Carmen, García, Marga, Ercilla, Gemma
Format: Still Image
Language:English
Published: 2010
Subjects:
Online Access:http://hdl.handle.net/10261/31304
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author Casas, David
Iglesias, Jorge
Vázquez, Juan Tomás
Somoza, Luis
León Buendía, Ricardo F.
Medialdea Cela, Teresa
Juan, Carmen
García, Marga
Ercilla, Gemma
author_facet Casas, David
Iglesias, Jorge
Vázquez, Juan Tomás
Somoza, Luis
León Buendía, Ricardo F.
Medialdea Cela, Teresa
Juan, Carmen
García, Marga
Ercilla, Gemma
author_sort Casas, David
collection Digital.CSIC (Spanish National Research Council)
description International Congress Deep Water Circulation: Processes and Products, 16-18 June 2010, Baiona, Pontevedra The Galicia Bank region is under the influence of different water masses (Mediterranean Outflow Water -MOW-, Labrador Sea Water –LSW-, North Atlantic Deep Water-NADW-, and Lower Deep Water –LDW-), and in this study we focussed in those features and deposits formed by their interaction with the seafloor. The bottom-current features and their sedimentary deposits are one of the most widespread elements in the Galicia Bank region, and they are mapped mostly in the Galicia Bank, Transitional Zone, Deep Galicia Margin and Northwestern Flank provinces. These features comprise erosive elements such as moats (a), furrows (b), and abraded surfaces (c) and depositional elements such as drifts (d) and sediment waves (e). The bottom-current features and deposits identified in the Galicia Bank region define a complex contouritic system that is fully described here for the first time. The currents erode, re-distribute and winnow the seafloor sediments of the Galicia Bank plateau, and those around the Highs and topographic irregularities of the Transitional Zone, Deep Galicia Margin, and Northwestern Flank. This system is generated by several water masses: MOW, LSW, NADW, and LDW, flowing at different depths and velocities and in different directions. Based on the current dynamics, two largely different subsystems are defined: contourites developed by a tabular water mass with a multiple current dynamics; and contourites developed by a focused/confined current MICINN projects: CONTOURIBER (CTM2008-06399-C04-04/MAR) and MONTERA (Ref: CTM-14157-C02-02/MAR) Peer reviewed
format Still Image
genre Labrador Sea
NADW
North Atlantic Deep Water
North Atlantic
genre_facet Labrador Sea
NADW
North Atlantic Deep Water
North Atlantic
id ftcsic:oai:digital.csic.es:10261/31304
institution Open Polar
language English
op_collection_id ftcsic
op_relation Deep Water Circulation: Processes and Products (2010)
http://hdl.handle.net/10261/31304
op_rights open
publishDate 2010
record_format openpolar
spelling ftcsic:oai:digital.csic.es:10261/31304 2025-03-16T15:29:56+00:00 Contourites in the Galicia bank (NW Iberian Atlantic) Casas, David Iglesias, Jorge Vázquez, Juan Tomás Somoza, Luis León Buendía, Ricardo F. Medialdea Cela, Teresa Juan, Carmen García, Marga Ercilla, Gemma 2010 http://hdl.handle.net/10261/31304 en eng Deep Water Circulation: Processes and Products (2010) http://hdl.handle.net/10261/31304 open Contourite MOW LSW NADW Galicia Ocean Bank Current Outflow póster de congreso http://purl.org/coar/resource_type/c_6670 2010 ftcsic 2025-02-18T02:04:31Z International Congress Deep Water Circulation: Processes and Products, 16-18 June 2010, Baiona, Pontevedra The Galicia Bank region is under the influence of different water masses (Mediterranean Outflow Water -MOW-, Labrador Sea Water –LSW-, North Atlantic Deep Water-NADW-, and Lower Deep Water –LDW-), and in this study we focussed in those features and deposits formed by their interaction with the seafloor. The bottom-current features and their sedimentary deposits are one of the most widespread elements in the Galicia Bank region, and they are mapped mostly in the Galicia Bank, Transitional Zone, Deep Galicia Margin and Northwestern Flank provinces. These features comprise erosive elements such as moats (a), furrows (b), and abraded surfaces (c) and depositional elements such as drifts (d) and sediment waves (e). The bottom-current features and deposits identified in the Galicia Bank region define a complex contouritic system that is fully described here for the first time. The currents erode, re-distribute and winnow the seafloor sediments of the Galicia Bank plateau, and those around the Highs and topographic irregularities of the Transitional Zone, Deep Galicia Margin, and Northwestern Flank. This system is generated by several water masses: MOW, LSW, NADW, and LDW, flowing at different depths and velocities and in different directions. Based on the current dynamics, two largely different subsystems are defined: contourites developed by a tabular water mass with a multiple current dynamics; and contourites developed by a focused/confined current MICINN projects: CONTOURIBER (CTM2008-06399-C04-04/MAR) and MONTERA (Ref: CTM-14157-C02-02/MAR) Peer reviewed Still Image Labrador Sea NADW North Atlantic Deep Water North Atlantic Digital.CSIC (Spanish National Research Council)
spellingShingle Contourite
MOW
LSW
NADW
Galicia
Ocean
Bank
Current
Outflow
Casas, David
Iglesias, Jorge
Vázquez, Juan Tomás
Somoza, Luis
León Buendía, Ricardo F.
Medialdea Cela, Teresa
Juan, Carmen
García, Marga
Ercilla, Gemma
Contourites in the Galicia bank (NW Iberian Atlantic)
title Contourites in the Galicia bank (NW Iberian Atlantic)
title_full Contourites in the Galicia bank (NW Iberian Atlantic)
title_fullStr Contourites in the Galicia bank (NW Iberian Atlantic)
title_full_unstemmed Contourites in the Galicia bank (NW Iberian Atlantic)
title_short Contourites in the Galicia bank (NW Iberian Atlantic)
title_sort contourites in the galicia bank (nw iberian atlantic)
topic Contourite
MOW
LSW
NADW
Galicia
Ocean
Bank
Current
Outflow
topic_facet Contourite
MOW
LSW
NADW
Galicia
Ocean
Bank
Current
Outflow
url http://hdl.handle.net/10261/31304