Mariana Islands, Coral Reef Geology, Figure 5 (a) Surficial geology of Guam (Modified from Gingerich [2002]). (b) Early Miocene
volcanic highs in relation to Miocene carbonates show that the latter formed primarily as ramp facies on and around the volcanic
cones (Siegrist and Randall, 1992). (c) Surficial geology of Saipan (Modified after Carruth [2003]). (d) Surficial geology of Tinian
(Modified after Doan et al. [1960] and Gingerich [2002]).
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volcanic highs in relation to Miocene carbonates show that the latter formed primarily as ramp facies on and around the volcanic
cones (Siegrist and Randall, 1992). (c) Surficial geology of Saipan (Modified after Carruth [2003]). (d) Surficial geology of Tinian
(Modified after Doan et al. [1960] and Gingerich [2002]).
MARIANA ISLANDS, CORAL REEF GEOLOGY
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