Beach lamination: Nature and origin
A distinctive two-fold sedimentation unit characterizes lamination in the upper swash zone of beaches. Within the unit a fine and/or a heavy mineral rich layer at the base grades upward into a coarser and/or a heavy mineral poor layer at the top. This distinctive type of lamination results from grain segregation within bed flow during wave backwash.
Citation Information
Publication Year | 1969 |
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Title | Beach lamination: Nature and origin |
DOI | 10.1016/0025-3227(69)90023-1 |
Authors | H. E. Clifton |
Publication Type | Article |
Publication Subtype | Journal Article |
Series Title | Marine Geology |
Index ID | 70009765 |
Record Source | USGS Publications Warehouse |