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The Geology of Puerto Rico can be divided into three major geologic provinces: The Cordillera Central, the Carbonate, and the Coastal Lowlands. [1] Puerto Rico is composed of Jurassic to Eocene volcanic and plutonic rocks, which are overlain by younger Oligocene to recent carbonates and other sedimentary rocks .
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The Northern Karst Belt (Spanish: Cinturón del Carso Norteño) is a limestone karst landscape located in the northwestern region of Puerto Rico. A karst is a topographical zone formed by the dissolution of soluble porous rocks, such as limestone , with features such as mogotes , canyons , caves , sinkholes , streams and rivers , all of which ...
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Author: Pease, M.H., Jr., and Monroe, W.H. Image title: Geologic map of the San Juan quadrangle, Puerto Rico; Short title: USGS Miscellaneous Investigations Series ...
Topographic map of Puerto Rico, 1952. Puerto Rico is mostly mountainous with large coastal areas in the north and south. The main mountain range is called Cordillera Central (Central Mountain Range). The highest elevation in Puerto Rico, Cerro de Punta at 4,393 feet (1,339 m), [24] is located in this range.
Guajataca State Forest is located in the middle of the karst landscape country, particularly the Northern Karst zone of Puerto Rico. A karst is a topographical zone formed by the dissolution of soluble porous rocks, in this case limestone, with features such as mogotes, canyons, caves, sinkholes, streams and rivers, all of which are common on this region of the island.
Before the flow of the Usabón River, the area where the San Cristóbal Canyon is located was the location of a former fault line during the Late Cretaceous period. This fault line might have contributed to the inward flow of previous rivers by creating a depression next to a rise of the superficial terrestrial crust along the region which began the process of carving the gorge approximately ...
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