Uploaded May 2020 | Updated September 2026, 1 week ago
Tidal flows produce distinctive suites of sedimentary structures related to the systematic changes in flow speed and direction. In this video, I show how changes in flow speed and direction produce herringbone cross stratification/lamination, mud drapes, mud clasts, and reactivation surfaces.
Tidal flows produce distinctive suites of sedimentary structures related to the systematic changes in flow speed and direction. In this video, I show how changes in flow speed and direction produce herringbone cross stratification/lamination, mud drapes, mud clasts, and reactivation surfaces.










