The beach berm is the nearly horizontal portion of a beach on the backshore formed by the deposition of sediment by receding waves; the long linear axis of the beach berm is roughly parallel to the shoreline.
A beach may have more than one berm.
|This article is written at a definitional level only. Authors wishing to expand this entry are inivited to expand the present treatment, which additions will be peer reviewed prior to publication of any expansion.|
- Physical Oceanography Index
- Paul D. Komar. Beach Processes and Sedimentation. Prentice-Hall, Inc., 1976.