Geological evidence of Norwegian Sea Overflow pathways into the Iceland Basin

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

Geological evidence of Norwegian Sea Overflow pathways into the Iceland Basin

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

Research output: Chapter in Book/Report/Conference proceeding › Conference article in proceedings

Abstract

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.

Original language	English
Title of host publication	Deep-water circulation: Processes & products. International Congress. Baiona, Pontevedra, Spain. 16, 17 & 18 June 2010
Editors	F. Javier Hernández-Molina, Dorrik A.V. Stow, Estefanía Llave, Michele Rebesco, Gemma Ercilla, David van Rooij, Anxo Mena, Juan T. Vázquez, Antje Voelker
Publisher	Sociedad Geologica de Espana
Pages	127-128
Number of pages	2
Publication status	Published - 2010
Event	Deep-water circulation: Processes & products. International Congress - Baiona, Spain Duration: 16 Jun 2010 → 18 Jun 2010

Publication series

Series	Geo-Temas
Volume	11

Conference

Conference	Deep-water circulation: Processes & products. International Congress
Country/Territory	Spain
City	Baiona
Period	16/06/10 → 18/06/10

Programme Area

Programme Area 5: Nature and Climate

Access to Document

https://sge.usal.es/archivos/GEO_TEMAS/Geo_temas11.pdfLicence: Unspecified

Cite this

Mørk, F., Nielsen, T., Staines-Urias, F., & Kuijpers, A. (2010). Geological evidence of Norwegian Sea Overflow pathways into the Iceland Basin. In F. J. Hernández-Molina, D. A. V. Stow, E. Llave, M. Rebesco, G. Ercilla, D. van Rooij, A. Mena, J. T. Vázquez, & A. Voelker (Eds.), Deep-water circulation: Processes & products. International Congress. Baiona, Pontevedra, Spain. 16, 17 & 18 June 2010 (pp. 127-128). Sociedad Geologica de Espana. https://sge.usal.es/archivos/GEO_TEMAS/Geo_temas11.pdf

Mørk, Finn ; Nielsen, Tove ; Staines-Urias, Francisca et al. / Geological evidence of Norwegian Sea Overflow pathways into the Iceland Basin. Deep-water circulation: Processes & products. International Congress. Baiona, Pontevedra, Spain. 16, 17 & 18 June 2010. editor / F. Javier Hernández-Molina ; Dorrik A.V. Stow ; Estefanía Llave ; Michele Rebesco ; Gemma Ercilla ; David van Rooij ; Anxo Mena ; Juan T. Vázquez ; Antje Voelker. Sociedad Geologica de Espana, 2010. pp. 127-128 (Geo-Temas, Vol. 11).

@inproceedings{c358a74fe2764c9abfa41cf4ae31d845,

title = "Geological evidence of Norwegian Sea Overflow pathways into the Iceland Basin",

abstract = "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 SeaOverflow Water intensity in the area north of Bill Bailey Bank is shown, based on sediment cores.",

author = "Finn M{\o}rk and Tove Nielsen and Francisca Staines-Urias and Antoon Kuijpers",

year = "2010",

language = "English",

series = "Geo-Temas",

publisher = "Sociedad Geologica de Espana",

pages = "127--128",

editor = "Hern{\'a}ndez-Molina, {F. Javier} and Stow, {Dorrik A.V.} and Estefan{\'i}a Llave and Michele Rebesco and Gemma Ercilla and {van Rooij}, David and Anxo Mena and V{\'a}zquez, {Juan T.} and Antje Voelker",

booktitle = "Deep-water circulation: Processes & products. International Congress. Baiona, Pontevedra, Spain. 16, 17 & 18 June 2010",

address = "Spain",

note = "Deep-water circulation: Processes & products. International Congress ; Conference date: 16-06-2010 Through 18-06-2010",

}

Mørk, F , Nielsen, T, Staines-Urias, F & Kuijpers, A 2010, Geological evidence of Norwegian Sea Overflow pathways into the Iceland Basin. in FJ Hernández-Molina, DAV Stow, E Llave, M Rebesco, G Ercilla, D van Rooij, A Mena, JT Vázquez & A Voelker (eds), Deep-water circulation: Processes & products. International Congress. Baiona, Pontevedra, Spain. 16, 17 & 18 June 2010. Sociedad Geologica de Espana, Geo-Temas, vol. 11, pp. 127-128, Deep-water circulation: Processes & products. International Congress, Baiona, Spain, 16/06/10. <https://sge.usal.es/archivos/GEO_TEMAS/Geo_temas11.pdf>

Geological evidence of Norwegian Sea Overflow pathways into the Iceland Basin. / Mørk, Finn ; Nielsen, Tove; Staines-Urias, Francisca et al.
Deep-water circulation: Processes & products. International Congress. Baiona, Pontevedra, Spain. 16, 17 & 18 June 2010. ed. / F. Javier Hernández-Molina; Dorrik A.V. Stow; Estefanía Llave; Michele Rebesco; Gemma Ercilla; David van Rooij; Anxo Mena; Juan T. Vázquez; Antje Voelker. Sociedad Geologica de Espana, 2010. p. 127-128 (Geo-Temas, Vol. 11).

Research output: Chapter in Book/Report/Conference proceeding › Conference article in proceedings

TY - GEN

T1 - Geological evidence of Norwegian Sea Overflow pathways into the Iceland Basin

AU - Mørk, Finn

AU - Nielsen, Tove

AU - Staines-Urias, Francisca

AU - Kuijpers, Antoon

PY - 2010

Y1 - 2010

N2 - 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 SeaOverflow Water intensity in the area north of Bill Bailey Bank is shown, based on sediment cores.

AB - 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 SeaOverflow Water intensity in the area north of Bill Bailey Bank is shown, based on sediment cores.

M3 - Conference article in proceedings

T3 - Geo-Temas

SP - 127

EP - 128

BT - Deep-water circulation: Processes & products. International Congress. Baiona, Pontevedra, Spain. 16, 17 & 18 June 2010

A2 - Hernández-Molina, F. Javier

A2 - Stow, Dorrik A.V.

A2 - Llave, Estefanía

A2 - Rebesco, Michele

A2 - Ercilla, Gemma

A2 - van Rooij, David

A2 - Mena, Anxo

A2 - Vázquez, Juan T.

A2 - Voelker, Antje

PB - Sociedad Geologica de Espana

T2 - Deep-water circulation: Processes & products. International Congress

Y2 - 16 June 2010 through 18 June 2010

ER -

Mørk F , Nielsen T, Staines-Urias F, Kuijpers A. Geological evidence of Norwegian Sea Overflow pathways into the Iceland Basin. In Hernández-Molina FJ, Stow DAV, Llave E, Rebesco M, Ercilla G, van Rooij D, Mena A, Vázquez JT, Voelker A, editors, Deep-water circulation: Processes & products. International Congress. Baiona, Pontevedra, Spain. 16, 17 & 18 June 2010. Sociedad Geologica de Espana. 2010. p. 127-128. (Geo-Temas, Vol. 11).

Geological evidence of Norwegian Sea Overflow pathways into the Iceland Basin

Abstract

Publication series

Conference

Programme Area

Access to Document

Fingerprint

Cite this