Titlebook: Geology of the Cayman Islands; Evolution of Complex Brian Jones Book 2022 The Editor(s) (if applicable) and The Author(s), under exclusive

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Modern Carbonate Environments,oons. Although infrequent, storms and hurricanes have a major impact on these depositional systems by moving large amounts of sediment onshore or offshore from the lagoons and open shelves. The lagoons, characterized by a diverse array of facies, typically have extensive . banks in the quieter, near

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Terra Rossa, Phosphate, and Mangrove Swamps,the late 1800s. The phosphates that remain on Little Cayman are mostly formed of hydroxylapatite with boehmite and crandallite being present locally. These deposits, formed largely of P.O., CaO, Al.O., Fe.O., and MnO, are petrographically complex with various admixtures of lithoclasts, coated grains

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Hydrogeology,mplex hydrogeology, and variable hydrological conditions. Water flow into and out of the lenses is largely controlled by the fractures in the karstic terrains that allow intrusion of seawater or saline water, enhance hydrodynamic dispersion, and define lens geometry. The porosity and permeability of

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