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The Geology of Jamaica is formed of rocks of Cretaceous to Neogene age. The basement consists of Cretaceous island arc and back-arc basin sequences that formed above a subduction zone. The cover is of mainly Eocene to Miocene shallow water limestones, that have been uplifted due to the presence of a restraining bend along the major strike-slip ...
Jamaica lies 140 km (87 mi) south of Cuba and 190 km (118 mi) west of Haiti. At its greatest extent, Jamaica is 235 km (146 mi) long, and its width varies between 34 and 84 km (21 and 52 mi). [1] Jamaica has a small area of 10,992 km 2 (4,244 sq mi). [1] However, Jamaica is the largest island of the Commonwealth Caribbean and the third largest ...
Jamaica ( / dʒəˈmeɪkə / ⓘ jə-MAY-kə; Jamaican Patois: Jumieka [dʒʌˈmie̯ka]) is an island country in the Caribbean Sea and the West Indies. At 10,990 square kilometres (4,240 sq mi), it is the third largest island—after Cuba and Hispaniola —of the Greater Antilles and the Caribbean. [11] Jamaica lies about 145 km (90 mi) south ...
Charles Alfred Matley. Charles Alfred Matley (1866–1947) was a British paleontologist and geologist in India, the British West Indies and Wales . Matley was educated at Birmingham University, and earned a doctorate in geology (D.Sc.) from the University of London in July 1902. [1]
James Gay Sawkins (1806–July 20, 1878) was an artist, geologist, copper miner, and illustrator. He was a member of the Geological Society of London who joined and led research during England's West Indian Geological Surveys of the islands of Trinidad and Jamaica. [1] [2] [3] He also worked in the mining industries of Jamaica, Peru, Hawaii ...
Geologic formations of Jamaica (3 C, 12 P) ... Pages in category "Geology of Jamaica" The following 8 pages are in this category, out of 8 total.
Metallogeny is the study of the genesis and regional-to-global distribution of mineral deposits, with emphasis on their relationship in space and time to regional petrologic and tectonic features of the Earth's crust . The term metallogeny (métallogénie) was created by Louis de Launay, a professor at the Ecole des Mines de Paris, in his 1913 ...
The Carlin Unconformity or Carlin Trend is a geologic feature in northeastern Nevada which represents a period of erosion or non-deposition likely associated with a collision between a tectonic crustal block called a terrane and the North American Plate. The collision occurred during the Mississippian Period, about 350 million years before present.
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