Swash, or forewash in geography, is a turbulent layer of water that washes up on the beach after an incoming wave has broken. The swash action can move beach materials up and down the beach, which res
Swash
Figure 1. Beach classification by Wright and Short (1983) showing dissipative, intermediate, and reflective beaches.
Figure 2. Swash zone and beachface morphology showing terminology and principal processes (Modified from Masselink & Hughes 2003)
Figure 3. Beach cusp morphology. Uprush diverges at the cusp horns and backwash converges in the cusp embayments. (Modified from Masselink & Hughes 2003)
Beach cusps are shoreline formations made up of various grades of sediment in an arc pattern. The horns are made up of coarser material and the embayment contains finer sediment.
Swash
…water table) and exfiltration (below the water table) take place between the swash flow and the beach groundwater table. Beachface, berm, beach step and beach cusps are the typical morphological features associated with swash motion. Infiltration (hydrology) and sediment transport by swash motion are important…
Standing Edge Wave Theory
Beach cusps in Westerly, Rhode Island