The Gebra Slide: a submarine slide on the Trinity Peninsula Margin, Antarctica
نویسندگان
چکیده
منابع مشابه
Origin of continental margin morphology: Submarine-slide or downslope current-controlled bedforms, a rock magnetic approach
Morphological features observed in both swath bathymetry and seismic reflection data are not unique, which introduces uncertainty as to their origin. The origin of features observed in the Humboldt Slide has generated much controversy because the same features have been interpreted as a submarine failure deposit versus current-controlled sediment waves. It is important to resolve this controver...
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A 4000-km-' area of submarine slump and slide deposits along the west flank of Mauna Loa volcano has been mapped with GLORIA side-scan sonar images, seismic reflection profiles, and new bathymetry. The youngest deposits are two debris avalanche lobes that travelled from their breakaway area near the present shoreline as much as 100 km into the Hawaiian Deep at water depths of 4800 m. The two lo...
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ژورنال
عنوان ژورنال: Marine Geology
سال: 2003
ISSN: 0025-3227
DOI: 10.1016/s0025-3227(02)00664-3