Article ID Journal Published Year Pages File Type
4690603 Sedimentary Geology 2008 9 Pages PDF
Abstract
These features are consistent with (1) deposition of the sediments on or closely overlying an unconformity surface cut in basalt bedrock in the vicinity of a rocky shoreline. They are also consistent with (2) derivation of the materials from rocky shorelines or shorefaces at lower elevations and their transport up-slope by waves generated by a Category 5 hurricane or by a mega-tsunami. We prefer the first scenario, as Lanai's vertical mobility is indicated by at least ten topographically distinct shoreline-related deposits located at various elevations on or adjacent to Lanai, including six submerged terraces on its western flank.
Related Topics
Physical Sciences and Engineering Earth and Planetary Sciences Earth-Surface Processes
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