Abstract
Abstract Closely spaced seismic‐reflection profiles across the eastern continental margin of Korea reveal that large‐scale slope failure scars occur ubiquitously on steep slopes (gradient, >5°) in water depths greater than 400 m. The slope failure scars are well defined with irregular scour planes and sometimes coalesce to form a large escarpment (maximum area, 275 km2 ). The failed material was deposited farther downslope as slide and mass‐flow deposits. These submarine slope failures are probably due to both seismicity associated with faulting and the steep gradient of the slope.
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
