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Marine-planation terraces on the shelf around Grand Cayman: a result of stepped Holocene sea-level rise
Download1995-01-01
The shelf around Grand Cayman consists of two seaward-sloping terraces separated by a mid-shelf scarp . Except along the exposed windward margin where coral growth is dominant, the upper terrace (0-10 m bal) largely consists of a barren rocky pavement traversed by erosional furrows. Exposure...
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