barrier island
Quick Summary
A barrier island is a long, sandy island that runs parallel to the coast. It is formed by the action of waves, currents, and winds, and it serves to protect the mainland shore from the ocean's impact. These islands are often separated from the mainland by a lagoon, which is a body of relatively shallow, quiet water.12
Barrier islands are typically composed of sand and are found on low-energy coastlines where there is an abundant supply of sediment. They can be formed by various geological processes, including the gradual rise of sea levels, the outbuilding of material by glacial outwash streams, or the development of a spit into a bay-mouth barrier. Storms and tsunamis can also significantly alter barrier islands by breaching or overtopping them.3
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