Please use this identifier to cite or link to this item:
logo share SHARE BASE
Visualizar otros formatos: MARC | Dublin Core | RDF | ORE | MODS | METS | DIDL | DATACITE

Contourites in the Galicia bank (NW Iberian Atlantic)

AuthorsCasas, David CSIC ORCID ; Iglesias, Jorge CSIC; Vázquez, J. T.; Somoza, Luis; León, Ricardo; Medialdea, Teresa; Juan, Carmen CSIC ORCID ; García, Marga CSIC ORCID; Ercilla, Gemma CSIC ORCID
Issue Date2010
AbstractThe 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.
DescriptionGemma Ercilla, David Casas, Jorge Iglesias, Juan T. Vázquez, Luís Somoza, Ricardo León, Teresa Medialdea, Carmen Juan, Marga García. (2010). Contourites in the Galicia Bank region (NW Iberian Atlantic) International Congress. Deep Water Circulation: Processes and Products Baiona, Pontevedra (España) 2010-06-16 / 2010-06-18
Appears in Collections:(ICM) Comunicaciones congresos
(IGME) Comunicaciones congresos

Files in This Item:
File Description SizeFormat
Casas_et_al_2010.pdf11,61 MBAdobe PDFThumbnail
Show full item record
Review this work

Page view(s)

checked on May 17, 2022


checked on May 17, 2022

Google ScholarTM


WARNING: Items in Digital.CSIC are protected by copyright, with all rights reserved, unless otherwise indicated.