Laguna: Perbedaan antara revisi

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Coastal lagoons are usually found on coasts with relatively small tidal ranges. They constitute approximately 13 percent of all coastlines. They generally extend parallel to the coastland, separated from the sea by barrier islands, sand and shingle bars or coral reefs. Non-reef lagoon barriers are formed by wave-action or longshore currents piling up coarser sediments off shore of the beach. Once a lagoon barrier has formed, finer sediments can settle out in the relatively quiet water behind the barrier, including sediments brought into the lagoon by rivers. Coastal lagoons typically have only constricted openings to the sea. As a result, water conditions in the lagoon can differ significantly from the open water of the sea in temperature, salinity, dissolved oxygen and sediment load.