Beach lamination: Nature and origin
January 1, 1969
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 |
|---|---|
| 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 |