Detailed Bathymetry and Submarine Terraces in the Coastal Area of the Dokdo Volcano in the Ulleung Basin, the East Sea (Sea of Japan)
SCIE
SCOPUS
Cited 15 time in
WEB OF SCIENCE
Cited 18 time in
Scopus
-
Title
- Detailed Bathymetry and Submarine Terraces in the Coastal Area of the Dokdo Volcano in the Ulleung Basin, the East Sea (Sea of Japan)
-
Author(s)
- Kim, Chang Hwan; Park, Jae Woo; Lee, Myoung Hoon; Park, Chan Hong
- KIOST Author(s)
- Kim, Chang Hwan(김창환); Lee, Myoung Hoon(이명훈); Park, Chan Hong(박찬홍)
-
Alternative Author(s)
- 김창환; 이명훈; 박찬홍
-
Publication Year
- 2013
-
Abstract
- In the northeastern part of the Ulleung Back-Arc Basin, the East Sea, the Dokdo volcano anomalously emerges, rising abruptly from the sea floor (similar to 2,100 m below sea level). It is lying as a cluster of emerged small islets surmounting a larger submerged volcanic edifice. In order to investigate the detailed bathymetry and morphologic characteristics around the volcano's underwater guyot type summit, we carried out multi-beam surveys from 2006 to 2011 and analyzed the data. From the near islets to similar to 30 m depth, the flank slopes are very steep and irregular, overlain by sunken rocks, indicating partial erosion and talus formation due to waves, currents and weathering. The area from similar to 30 m to similar to 80 m depth shows gentle rises and falls, with a modest slope. Below similar to 80 m, the bathymetry gradually transitions to a relatively flat undulation with a smooth slope, extending to offshore areas. The bathymetry and the seafloor image from backscattering data show that there are small islets of the Dokdo volcano and a rocky sea bottom elongated from the islets, probably originating from residual parts of the eroded and collapsed main crater of the volcano. The seafloor images identify typical rocky bottoms, like rocky protrusions, and less sediment around the survey area, except for some areas with shallow sand sedimentary deposits. The stepped slopes of the study area are interpreted to be wave-cut submarine terraces rather than terraces from other origins, based on their relatively flat morphology and lack of sediments. The submarine terraces suggest a repetition of sea level changes (transgressions and regressions) in the Quaternary.
-
ISSN
- 0749-0208
-
URI
- https://sciwatch.kiost.ac.kr/handle/2020.kiost/3361
-
DOI
- 10.2112/SI65-089.1
-
Bibliographic Citation
- JOURNAL OF COASTAL RESEARCH, pp.523 - 528, 2013
-
Publisher
- COASTAL EDUCATION & RESEARCH FOUNDATION
-
Subject
- GREAT-BARRIER-REEF; SUBMERGED REEFS; SHELF EDGE; SEAMOUNTS
-
Keywords
- Dokdo volcano; detailed bathymetry; multi-beam survey; seafloor image; crater; submarine terraces; sea level changes
-
Type
- Article
-
Language
- English
-
Document Type
- Article; Proceedings Paper
- Files in This Item:
-
There are no files associated with this item.
Items in ScienceWatch@KIOST are protected by copyright, with all rights reserved, unless otherwise indicated.