The seafloor morphology offshore cide-sinop, southern Black Sea

N. Ocakoglu*, Y. Işcan, F. Kılıç, O. Özel

*Corresponding author for this work

Research output: Chapter in Book/Report/Conference proceedingConference contributionpeer-review

Abstract

The multi-beam echosounder data were collected in the southern Black Sea shelf between 2002 and 2008 by the Turkish Navy, Department of Navigation, Hydrography and Oceanography and studied under the research project of Scientific and Technological Research Council of Turkey (Project no. TUBİTAK-114Y057). Multi-beam ASCII data were exported to vector points. The data covers an area of 2.59 km2 and elevations range from -2 to -503 m. The multi-beam points were interpolated into DEM of pixel size 5 m, using Topo-to-Raster interface of ArcGIS software. The bottom morphology offshore Cide-Sinop shelf is quite smooth plain with an approx. 25 km wide and -100 m water depth. The continental shelf edge is around -120 m isobath. Slope angles from 0 to 1 degree at the shelf plain, increases about to 40 degrees along the shelf slope. Some landslides are mapped in this zone. The shelf plain is widely characterized by sand dunes with an average height of 10 m. These hills are separated from each other by flat plains. The hills and plains are interpreted as the sand dunes and submarine plains which probably evolved during aeolian processes. These results are thought that the shelf plain was once a terrestrial landscape.

Original languageEnglish
Title of host publication9th Congress of the Balkan Geophysical Society, BGS 2017
PublisherEuropean Association of Geoscientists and Engineers, EAGE
ISBN (Electronic)9789462822368
DOIs
Publication statusPublished - 2017
Event9th Congress of the Balkan Geophysical Society, BGS 2017 - Belek, Antalya, Turkey
Duration: 5 Nov 20179 Nov 2017

Publication series

Name9th Congress of the Balkan Geophysical Society, BGS 2017
Volume2017-November

Conference

Conference9th Congress of the Balkan Geophysical Society, BGS 2017
Country/TerritoryTurkey
CityBelek, Antalya
Period5/11/179/11/17

Bibliographical note

Publisher Copyright:
© 2017 European Association of Geoscientists and Engineers EAGE. All Rights Reserved.

Funding

This study was supported by The Scientific and Technological Research Council of Turkey, Project no. TUBITAK-ÇAYDAG-114Y057. We thank the officers and crew as well as the scientists and technicians onboard the TCG Çubuklu and TCG Çeşme of the Turkish Navy, Department of Navigation, Hydrography, and Oceanography. This study was supported by The Scientific and Technological Research Council of Turkey, Project no. TUBITAK-?AYDAG-114Y057. We thank the officers and crew as well as the scientists and technicians onboard the TCG ?ubuklu and TCG ?e?me of the Turkish Navy, Department of Navigation, Hydrography, and Oceanography.

FundersFunder number
TUBITAKAYDAG-114Y057
Turkish Navy
Florida Institute of Oceanography
Türkiye Bilimsel ve Teknolojik Araştirma KurumuTUBITAK-ÇAYDAG-114Y057

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