Triggering mechanism and tsunamogenic potential of the Cape Fear Slide complex, U.S. Atlantic margin
Hornbach, Matthew J.
Lavier, Luc L.
Ruppel, Carolyn D.
MetadataShow full item record
Analysis of new multibeam bathymetry data and seismic Chirp data acquired over the Cape Fear Slide complex on the U.S. Atlantic margin suggests that at least 5 major submarine slides have likely occurred there within the past 30,000 years, indicating that repetitive, large-scale mass wasting and associated tsunamis may be more common in this area than previously believed. Gas hydrate deposits and associated free gas as well as salt tectonics have been implicated in previous studies as triggers for the major Cape Fear slide events. Analysis of the interaction of the gas hydrate phase boundary and the various generations of slides indicates that only the most landward slide likely intersected the phase boundary and inferred high gas pressures below it. For much of the region, we believe that displacement along a newly recognized normal fault led to upward migration of salt, oversteepening of slopes, and repeated slope failures. Using new constraints on slide morphology, we develop the first tsunami model for the Cape Fear Slide complex. Our results indicate that if the most seaward Cape Fear slide event occurred today, it could produce waves in excess of 2 m at the present-day 100 m bathymetric contour.
Author Posting. © American Geophysical Union, 2007. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Geochemistry Geophysics Geosystems 8 (2007): Q12008, doi:10.1029/2007GC001722.
Suggested CitationArticle: Hornbach, Matthew J., Lavier, Luc L., Ruppel, Carolyn D., "Triggering mechanism and tsunamogenic potential of the Cape Fear Slide complex, U.S. Atlantic margin", Geochemistry Geophysics Geosystems 8 (2007): Q12008, DOI:10.1029/2007GC001722, https://hdl.handle.net/1912/3267
Showing items related by title, author, creator and subject.
Walsh, Joseph B.; Zhu, Wenlu (American Geophysical Union, 2004-05-19)Sliding of a rough surface having a range of asperity heights is a gradual process, starting at contacts under relatively low normal shear load and spreading until the surface slides as a unit. We analyze this process ...
Temporal and spatial perspectives on the fate of anthropogenic carbon : a carbon cycle slide deck for broad audiences Khatiwala, Samar; DeVries, Timothy; Cook, Jack; McKinley, Galen A.; Carlson, Craig A.; Benway, Heather M. (Ocean Carbon & Biogeochemistry Program, 2015-12-08)This slide deck was developed to inform broader scientific, as well as general audiences about the role of the ocean in the global carbon cycle, including key sinks and sources of anthropogenic carbon and how they have ...