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  2. Lagoon - Wikipedia

    en.wikipedia.org/wiki/Lagoon

    A lagoon is a shallow body of water separated from a larger body of water by a narrow landform, such as reefs, barrier islands, barrier peninsulas, or isthmuses. Lagoons are commonly divided into coastal lagoons (or barrier lagoons) and atoll lagoons. They have also been identified as occurring on mixed-sand and gravel coastlines.

  3. Land of the lost: Hidden lagoon network found with living ...

    www.aol.com/land-lost-hidden-lagoon-network...

    Stromatolites also tend to grow in alkaline conditions, but the Puna de Atacama’s system of lagoons are acidic. The stromatolites found today are almost all carbonate rocks (made of limestone ...

  4. Arcadia Formation - Wikipedia

    en.wikipedia.org/wiki/Arcadia_Formation

    The Tampa Member is located in DeSoto, Hardee, Hillsborough, Manatee, Pinellas, and Sarasota counties, and the northern portion of Charlotte County. It consists of carbonate sediments deposited in the Early Miocene Hillsborough Lagoon System and the Tampa Reef Track and Tampa Archipelago, which bordered the lagoon system.

  5. Coral reef - Wikipedia

    en.wikipedia.org/wiki/Coral_reef

    Formation takes considerably longer than for a fringing reef, thus barrier reefs are much rarer. The best known and largest example of a barrier reef is the Australian Great Barrier Reef . [ 42 ] [ 47 ] Other major examples are the Mesoamerican Barrier Reef System and the New Caledonian Barrier Reef . [ 47 ]

  6. Carbonate platform - Wikipedia

    en.wikipedia.org/wiki/Carbonate_platform

    An example of carbonate mud sedimentation in the internal part of the Florida Bay lagoon. The presence of young mangroves is important to entrap the carbonate mud. The internal lagoon, as the name suggests, is the part of platform behind the reef. It is characterised by shallow and calm waters, and so it is a low-energy sedimentary environment.

  7. Fringing reef - Wikipedia

    en.wikipedia.org/wiki/Fringing_reef

    Reefs can develop when an offshore reef grows to sea level, forming a barrier. When the crest grows faster than the flat, a lagoon forms. The lagoon then fills with inshore sediments. Offshore reefs can form their barrier using storms to move coral and other debris inwards. The recurring storms continually reshape the seaward side of such reefs.

  8. The Structure and Distribution of Coral Reefs - Wikipedia

    en.wikipedia.org/wiki/The_Structure_and...

    Canton Island typifies the isolated coral atolls dotting the Pacific Ocean. The Structure and Distribution of Coral Reefs, Being the first part of the geology of the voyage of the Beagle, under the command of Capt. Fitzroy, R.N. during the years 1832 to 1836, was published in 1842 as Charles Darwin's first monograph, and set out his theory of the formation of coral reefs and atolls.

  9. Alvarado Lagoon System - Wikipedia

    en.wikipedia.org/wiki/Alvarado_Lagoon_System

    The Alvarado Lagoon System is a large estuary and wetland complex in Veracruz state of eastern Mexico. It is located on the southern Gulf Coastal Plain , where the Papaloapan and Blanco rivers meet the Gulf of Mexico .