This form provides that any Party may propose that geoscience operations be conducted on the Contract Area lands. The Party wishing to conduct geoscience operations shall furnish the other Parties with an information notice which generally describes the proposed geoscience operation.
Puerto Rico Geoscience Operations on the Contract Area
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US-OG-705
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From Puerto Rico and the Lesser Antilles Semiprecious stones such as carnelian, turquoise, amethyst, serpentine, nephrite, and jadeitite occur naturally on certain islands of the Antilles and in parts of the mainland and were exchanged either as a raw material or as finished objects.
Puerto Rico, the closest land area, has a central longitudinal core of Cretaceous and early Tertiary volcanic rocks, some serpentinite of undetermined age, and numerous small intrusions.
Punta Ventana, which translates to ?Window Point,? was a stone arch shaped like a round window located in Guayanilla along the southern coast. The rock formation was one of the island's most iconic treasures and major tourist attractions.
The main bathymetric features of this area include: the Lesser Antilles volcanic arc; the old inactive volcanic arc of the Greater Antilles (Virgin Islands, Puerto Rico, and Hispaniola); the Muertos Trough; and the Puerto Rico Trench formed at the plate boundary zone between the Caribbean and obliquely subducting North ...
Puerto Rico consists of volcanic, volcaniclastic, and sedimentary rocks of Late Jurassic to Early Tertiary age, which were intruded by felsic plutonic rocks during the Late Cretaceous and Early Tertiary, and are overlain by slightly tilted Oligocene and younger sedimentary rocks and sediments (Briggs and Akers, 1965).
The Geology of Puerto Rico "can be divided into three major geologic provinces: The Cordillera Central, the Carbonate, and the Coastal Lowlands." 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.