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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Aetiology and Epidemiology of Breast Cancers. The seaward margins of the marine shelves around each island are defined by the 20 m isobath, which is the edge of the drop-off into deep water. As a result, the shelves around the islands are generally no more than 500 m wide. Lagoons, formed where fringing reefs have grown from headland to head

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https://doi.org/10.1007/978-981-15-2937-5dolostones of the Cayman Formation and Pedro Castle Formation, is characterized by dark grey to black phytokarst surfaces that are reflective of various types of microbes, including bacteria, fungi, and cyanobacteria, that actively sculpted the topographically complex phytokarst surfaces. Surface ka

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Tectonic Setting of the Cayman Islands,eparated from the depths of the Cayman Trench by the Oriente Transform Fault. The Mid-Cayman Rise, which is an active spreading center, is located off the southwest corner of Grand Cayman. Grand Cayman commonly experiences earthquakes that are triggered by activity along the Oriente Transform Fault

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,Bluff Group—The Cayman Formation, unconformities with significant karstic relief. Although the Cayman Formation is at least 150 m thick, its true original thickness is unknown because of the relief on these boundaries. This formation developed during the Middle Miocene when marine sediments were deposited on an open bank in waters

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,Bluff Group—Pedro Castle Formation, Brac, and Little Cayman. Although exposed successions are generally <5 m thick, subsurface sequences on the western peninsula of Grand Cayman are up to 21.5 m thick. The formation rests unconformably on the Cayman Formation and is unconformably overlain by the Ironshore Formation. In many areas, mu

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