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Landform

Barrier Island

Marine and Coastal Landforms

A long, narrow island of sand running parallel to the mainland coast, separated from it by a lagoon or sound, built up by the same wave and current processes that form an ordinary sandbar but raised high enough by additional deposition and dune growth to remain permanently above the water. Barrier islands absorb much of the wave energy that would otherwise strike the mainland coast directly, and they migrate and reshape themselves with each major storm.

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Source Barrier Island Formation (Wikipedia)
Sources
Wikidata: Barrier Island
Wikidata Q21490568, class allow-list match (w-wdresolver-0926)View the Source
Barrier Island Formation (Wikipedia)
Wikimedia FoundationShaped By: Deposition and Sedimentation, Lead
Quote, Shaped By: Deposition and Sedimentation, Lead
Barrier islands are commonly formed in long, narrow systems parallel to shorelines and are shaped by waves, tides, sediment movement, and sea-level change, which cause them to shift, grow, or erode over time.
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