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Jamaica (island)
Jamaica lies 140 km (87 mi) south of Cuba and west of Haiti. At its greatest extent, Jamaica is long, and its width varies between . Jamaica has a small area of . However, Jamaica is the largest island of the Commonwealth Caribbean and the third largest of the Greater Antilles, after Cuba and Hispaniola Hispaniola (, also ) is an island between Geography of Cuba, Cuba and Geography of Puerto Rico, Puerto Rico in the Greater Antilles of the Caribbean. Hispaniola is the most populous island in the West Indies, and the second-largest by List of C .... Many small islands are located along the south coast of Jamaica, such as the Port Royal Cays. Southwest of mainland Jamaica lies Pedro Bank, an area of shallow seas, with a number of cays (low islands or reefs), extending generally east to west for over . To the southeast lies Morant Bank, with the Morant Cays, from Morant Point, the easternmost point of mainland Jamaica. Alice Shoal, southwest of the main island of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pedro Bank
Pedro Bank is a large bank of sand and coral, partially covered with seagrass, about 80 km south and south-west of Jamaica, rising steeply from a seabed of 800 m depth. History Pedro Bank was originally named 'Viper Bank', , by Spanish mariners because its shallow reefs, rocks and shoals are laid out in the shape of a gigantic serpent.Assessing Coral reefs in Jamaica Nathalie Zenny It was once a busy and treacherous shipping passage used by seafaring Europeans in the 16th and 17th centuries; archaeologists estimate there are over 300 shipwrecks on the bank. Pedro Bank was annexed by the in 1863 and added to Jamaica in 1882. Today it is known f ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rio Minho (Jamaica)
The Rio Minho is the longest river in Jamaica at . It rises close to the island's geographic centre, flows generally south-southwest and reaches the Caribbean Sea at Carlisle Bay in the central south coast, to the west of the island's southernmost point, Portland Point. The town of May Pen, Clarendon lies on the banks of the river. IUGS geological heritage site In respect of it being the 'most diverse and thickest limestone succession with abundant rudist bivalves within the Caribbean faunal province', the International Union of Geological Sciences The International Union of Geological Sciences (IUGS) is an international non-governmental organization devoted to global cooperation in the field of geology. As of 2023, it represents more than 1 million geoscientists around the world. About Fo ... (IUGS) included the 'Late Cretaceous rudist bivalves of the Caribbean Province' around the Rio Minho in its assemblage of 100 'geological heritage sites' around the world in a listin ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Black River (Jamaica)
The Black River is one of the longest rivers in Jamaica. At a length of , it was believed to be the longest until it was discovered that the Rio Minho (Jamaica), Rio Minho was 92.8 km long.Jamaica National Heritage Trust - Black River Its name refers to the darkness of the riverbed caused by thick layers of decomposing vegetation. Over 100 species of birds have been recorded in the Black River morass. A 17,769 ha area of the river basin, encompassing much of the Upper and Lower Morass, has been designated an Important Bird Area (IBA) by BirdLife International because it supports significant populations of many Jamaican bird species. Geography Sources The river's source is the Cockpit Country where it runs underground ...[...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nassau Valley
Nassau Valley is a valley in Saint Elizabeth, Jamaica. It is one of the three main valleys in Jamaica. The valley is located in Cockpit Country and averages 443 feet above sea level, with a dry sub-humid (0.5 - 0.65 p/pet) climate. Appleton Estate, a rum-producing plantation founded under chattel slavery Slavery is the ownership of a person as property, especially in regards to their labour. Slavery typically involves compulsory work, with the slave's location of work and residence dictated by the party that holds them in bondage. Enslavemen ... and still operating today, is located in the valley along the Black River. References {{reflist Geography of Saint Elizabeth Parish ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cockpit Country
Cockpit Country is an area in Trelawny and Saint Elizabeth, Saint James, Saint Ann, Manchester and the northern tip of Clarendon parishes, mostly within the west-central side, of Jamaica. The land is marked by lush, montane forests and steep-sided valleys and hollows, as deep as in places, separated by conical hills and ridges. During the 16th and 17th centuries, maroons—the escapee former slaves (and their descendants) of the island's Spanish and British-operated sugarcane plantations—used this rugged terrain to their benefit, carving out an existence on their own, away from the violent slavers and colonial powers of the lowlands. History In the late seventeenth century, the Cockpit Country was a place of refuge for Jamaican Maroons fleeing slavery. During the course of the First Maroon War, there were two Leeward Maroon communities - Cudjoe's Town (Trelawny Town) and Accompong Town. Cudjoe's Town was located in the mountains in the southern extremities of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Karst
Karst () is a topography formed from the dissolution of soluble carbonate rocks such as limestone and Dolomite (rock), dolomite. It is characterized by features like poljes above and drainage systems with sinkholes and caves underground. There is some evidence that karst may occur in more weathering-resistant rocks such as quartzite given the right conditions. Subterranean drainage may limit surface water, with few to no rivers or lakes. In regions where the dissolved bedrock is covered (perhaps by debris) or confined by one or more superimposed non-soluble rock strata, distinctive karst features may occur only at subsurface levels and can be totally missing above ground. The study of ''paleokarst'' (buried karst in the stratigraphic column) is important in petroleum geology because as much as 50% of the world's Oil and gas reserves and resource quantification, hydrocarbon reserves are hosted in carbonate rock, and much of this is found in porous karst systems. Etymology ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dry Harbour Mountains
The Dry Harbour Mountains are a range of mountains in north central Jamaica. More accurately described as a plateau than a true mountain range, they form the eastern boundary of the Cockpit Country. This is also the mountain that people used to go and pray. The Dry Harbour Mountains starts from Discovery Bay, St. Ann and covers most settlements all the way to the eastern end of the Cockpit Country. It is a mountain which abounds in limestone and bauxite. The soil type is latosol which is of red iron and aluminium oxide. The Dry Harbour Mountains is some above sea level and many areas are very cool. The area is covered in rich verdant pastures and numerous trees. In many areas the wet limestone forest is a riotous profuse of trees. Many prominent districts are part of this plateau region of Jamaica. Nine Mile, the home of Bob Marley; Alexandria; Aboukir; Clarksonville, Inverness; Tobolski; Gibraltar; Watt Town; Bethany; Murray Mountain (the marijuana centre) and McKenzie; C ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
John Crow Mountains
The John Crow Mountains are a range of mountains in eastern Jamaica. Etymology The name John Crow was first recorded in the 1820s and comes from the Jamaican name for the turkey vulture. It has been suggested that previous to this, the range was known as the "Carrion Crow Ridge", after an earlier name for the vulture."Eager for Ecclesdown Road" a www.10000birds.com Accessed 29 July 2011. Geography The mountains extend parallel with the north-east coast of the island, bounded to the west by the banks of the , and joining with the eastern e ...[...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Limestone
Limestone is a type of carbonate rock, carbonate sedimentary rock which is the main source of the material Lime (material), lime. It is composed mostly of the minerals calcite and aragonite, which are different Polymorphism (materials science), crystal forms of calcium carbonate . Limestone forms when these minerals Precipitation (chemistry), precipitate out of water containing dissolved calcium. This can take place through both biological and nonbiological processes, though biological processes, such as the accumulation of corals and shells in the sea, have likely been more important for the last 540 million years. Limestone often contains fossils which provide scientists with information on ancient environments and on the evolution of life. About 20% to 25% of sedimentary rock is carbonate rock, and most of this is limestone. The remaining carbonate rock is mostly Dolomite (rock), dolomite, a closely related rock, which contains a high percentage of the mineral Dolomite (mine ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Blue Mountains (Jamaica)
The Blue Mountains are the longest mountain range in Jamaica. They include the island's highest point, Blue Mountain Peak, at 2256 m (7402 ft). From the summit, accessible via a walking track, both the north and south coasts of the island can be seen. On a clear day, the outline of the island of Cuba, away, can also be seen. The mountain range spans four parishes: Portland, St Thomas, St Mary and St Andrew. Geography The Blue Mountains dominate the eastern third of Jamaica, while bordering the eastern parishes of Portland, Saint Thomas, Saint Mary and Saint Andrew to the south. Part of the Blue Mountains is contained in the Blue and John Crow Mountains National Park established in 1992, which is maintained by the Jamaican government. The Blue Mountains rise to their summits from the coastal plain in the space of about , thus producing one of the steepest general gradients in the world. This provides cooling relief from the sweltering heat of the city of Kin ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Exclusive Economic Zone
An exclusive economic zone (EEZ), as prescribed by the 1982 United Nations Convention on the Law of the Sea, is an area of the sea in which a sovereign state has exclusive rights regarding the exploration and use of marine natural resource, resources, including energy production from water and wind. It stretches from the outer limit of the territorial sea (22.224 kilometres or 12 nautical miles from the baseline) out 370.4 kilometres (or 200 nautical miles) from the coast of the state in question. It is also referred to as a maritime continental margin and, in colloquial usage, may include the continental shelf. The term does not include either the Territorial waters#Territorial sea, territorial sea or the continental shelf beyond the 200 nautical mile limit. The difference between the territorial sea and the exclusive economic zone is that the first confers full sovereignty over the waters, whereas the second is merely a "sovereign right" which refers to the coastal state's righ ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
