Geological evidence of Norwegian Sea Overflow pathways into the Iceland Basin

Finn Mørk, Tove Nielsen, Francisca Staines-Urias, Antoon Kuijpers

Publikation: Bidrag til bog/rapport/konferenceproceedingsKonferenceartikel i proceedings

Abstrakt

NSOW flowing through the Faroe-Shetland Channel has a complex flowing pattern into the Iceland Basin. One branch flows across the Wyville-Thomson Ridge, along the southern flanks of the Faroe, Bill Bailey and Lousy Banks before turning north along the western flank of Lousy Bank. A general increase in the Norwegian Sea
Overflow Water intensity in the area north of Bill Bailey Bank is shown, based on sediment cores.
OriginalsprogEngelsk
TitelDeep-water circulation: Processes & products. International Congress. Baiona, Pontevedra, Spain. 16, 17 & 18 June 2010
RedaktørerF. Javier Hernández-Molina, Dorrik A.V. Stow, Estefanía Llave, Michele Rebesco, Gemma Ercilla, David van Rooij, Anxo Mena, Juan T. Vázquez, Antje Voelker
ForlagSociedad Geologica de Espana
Sider127-128
Antal sider2
StatusUdgivet - 2010
BegivenhedDeep-water circulation: Processes & products. International Congress - Baiona, Spanien
Varighed: 16 jun. 201018 jun. 2010

Publikationsserier

NavnGeo-Temas
ForlagSociedad Geológica de España
Vol/bind11
ISSN (Elektronisk)1567-5172

Konference

KonferenceDeep-water circulation: Processes & products. International Congress
Land/OmrådeSpanien
ByBaiona
Periode16/06/1018/06/10

Programområde

  • Programområde 5: Natur og klima

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