Abstract
A detailed bathymetric survey of the crest and axial valley of the Gorda Rise, between 41°10' to 41° 29'N and 127°15' to 127°36'W, has revealed several pronounced continuous benches. The most prominent benches are at depths of 2400 and 2800 m. The regional bathymetry is consistent with a block-faulting origin for the topography of the Gorda Rise.
Recommended Citation
Heinrichs, Donald F.. 1970. "More bathymetric evidence for block faulting on the Gorda Rise." Journal of Marine Research 28, (3). https://elischolar.library.yale.edu/journal_of_marine_research/1191
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