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- W1719307911 abstract "This chapter is provides information on the geology and hydrogeology of Barbados. Barbados is the easternmost island of the Windward Islands chain in the eastern Caribbean region. Nearly 85% of the island exposes reef-associated carbonate sedimentary rocks of differing Pleistocene ages. This Pleistocene limestone cover, which is locally known as the “Coral Cap” and formally as the Coral Rock Formation, averages about 70 m thick. Barbados lies within the belt of northeast trade winds and is characterized by a humid to subhumid tropical maritime climate. The eastern, windward side of the island experiences high-energy wave action with Atlantic rollers crashing on eroding seacliffs. The island of Barbados is a relatively unique carbonate island because of its history of continual tectonic uplift. A combination of fringing-reef deposition during late Pleistocene glacioeustatic sea-level highstands and tectonic uplift has resulted in a depositional system of discrete reef tracts, the age and topographic elevation of which decrease in a stair-step fashion toward the perimeter of the island." @default.
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- W1719307911 date "2004-01-01" @default.
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- W1719307911 title "Geology and Hydrogeology of Barbados" @default.
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- W1719307911 doi "https://doi.org/10.1016/s0070-4571(04)80033-5" @default.
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