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Titlebook: Coral Reefs of the USA; Bernhard M. Riegl,Richard E. Dodge Book 20081st edition Springer Science+Business Media B.V. 2008 Atoll.Biology.Co

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Geology of Hawaii Reefs,n plate direction is marked by a northward kink in the chain at the end of the Hawaii Ridge approximately 3,500 km from the site of active volcanism (Moore 1987). On the basis of dredged basalts, Sharp and Clague (2006) assign an age of 50 Ma to this shift from northern to northwestern plate motion,
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Biology and Ecological Functioning of Coral Reefs in the Main Hawaiian Islands,/year. Molten lava breaking through the thin rigid crust slowly creates volcanic mountains that eventually reach the surface of the ocean and emerge as islands (Macdonald et al. 1983). As the islands move off the hot spot they undergo erosion and subsidence. Eventually they are worn down and gradual
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Geology and Geomorphology of Coral Reefs in the Northwestern Hawaiian Islands,physical isolation and low levels of marine biodiversity, Hawaiian reefs feature high levels of endemism. Approximately a quarter of the species present are found nowhere else, and the Hawaiian Archipelago has approximately twice as many endemic coral species as any other area its size in the world
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US Coral Reefs in the Line and Phoenix Islands, Central Pacific Ocean: History, Geology, Oceanograppter 13, Rooney et al.; Chapter 17, Lobel and Lobel). Johnston Atoll is mentioned in this chapter because it is geologically part of the Line Islands archipelago. Wake Atoll, administered by the US..Air Force, is north of the Republic of the Marshall Islands. Midway Atoll is located at the northwest
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Geologic Setting and Geomorphology of Coral Reefs in the Mariana Islands (Guam and Commonwealth of est documentations of the Marianas. In Guam, research received a boost when the USA acquired it from Spain following the Spanish American War, and in the CNMI, when Germany bought the islands in 1899. Coral reef investigations began in 1903 when Agassiz reported about the Marianas in the course of h
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