Beach

A beach is the zone of unconsolidated material that extends from the low water line to where there is an abrupt change in physiographic form or vegetation (e.g. dune scarp, seawall, etc). Beaches occur wherever there is mobile sediment along the shore, in the region between extreme low and extreme high water.

 

Important concepts

 

Beach sediment

Composition:
Beaches are composed of whatever sediment is available.
  • siliciclastic sand -Common where sediment source is fluvial
  • volcanic debris (black and green olivine-bearing sands) Iceland and Hawaii
  • gravel (shingle) - New England, England and glaciated coasts where till and rocky headlands are the principle sediment source
  • Shelly carbonate debris - Florida beaches and sandy beach on Mt. Desert in Maine.
  • Minerals precipitated directly for seawater (hydrogenous)- oolitic and glaconitic sands
  • Wood (Dri Kai)
  • beer cans, trash and sewage outfall

 


 Sediment sources

Composition of beaches in New England


Types of beaches

 

The is no single, all-incompassing classification of beaches. The list given below is a simple descriptive classification.