Flow behaviour of a giant landslide and debris flow entering Agadir Canyon, NW Africa.

Krastel, Sebastian, Wynn, R.B., Feldens, Peter, Schürer, A., Böttner, Christoph, Stevenson, C., Cartigny, M., Hühnerbach, Veit and Unverricht, D. (2016) Flow behaviour of a giant landslide and debris flow entering Agadir Canyon, NW Africa. Submarine mass movements and their consequences. Advances in Natural and Technological Hazards Research, 41 . Springer International Publishing, Cham, pp. 145-154. ISBN 978-3-319-20978-4 DOI 10.1007/978-3-319-20979-1_14.

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Abstract

Agadir Canyon is one of the largest submarine canyons in the World, supplying giant submarine sediment gravity flows to the Agadir Basin and the wider Moroccan Turbidite System. While the Moroccan Turbidite System is extremely well investigated, almost no data from the source region, i.e. the Agadir Canyon, are available. New acoustic and sedimentological data of the Agadir Canyon area were collected during RV Maria S. Merian Cruise 32 in autumn 2013. The data show a prominent headwall area around 200 km south of the head of Agadir Canyon. The failure occurred along a pronounced weak layer in a sediment wave field. The slab-type failure rapidly disintegrated and transformed into a debris flow, which entered Agadir Canyon at 2500 m water depth. Interestingly, the debris flow did not disintegrate into a turbidity current when it entered the canyon despite a significant increase in slope angle. Instead, the material was transported as debrite for at least another 200 km down the canyon. It is unlikely that this giant debris flow significantly contributed to the deposits in the wider Moroccan Turbidite System.

Document Type: Book chapter
Research affiliation: OceanRep > The Future Ocean - Cluster of Excellence > FO-R06
Kiel University > Kiel Marine Science
OceanRep > The Future Ocean - Cluster of Excellence
Kiel University
Refereed: Yes
DOI etc.: 10.1007/978-3-319-20979-1_14
ISSN: 1878-9897
Projects: Future Ocean
Date Deposited: 30 Jan 2017 10:11
Last Modified: 06 Feb 2019 11:38
URI: http://eprints.uni-kiel.de/id/eprint/35193

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