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Taganga Phyllite
Taganga is a traditional fishing village and corregimiento of Santa Marta, located on the Caribbean coast of Colombia at about 10 minutes or north of Santa Marta. Both Santa Marta and Taganga were founded by Rodrigo de Bastidas on July 29, 1525, making them two of the oldest remaining colonial settlements in present-day Colombia. The touristic town and backpacker hub is famous for its sunsets, diving and access to the Tayrona National Natural Park. Bohemian and richly decorated Taganga is full of hostels and forms part of the South American Gringo Trail. In the months of July and August the village is visited by many Israelis who finished their military draft period. Etymology The source of the name Taganga is uncertain; it is either derived from the Taganga people inhabiting the area before the Spanish conquest, from the words ''ta'' and ''gunmy''; "Snake mountain range" or from the Tairona words ''ta'' and ''ganga''; "Entrance of the sea". 2015 Etymology, draughts and park ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Corregimiento
''Corregimiento'' (; ca, Corregiment, ) is a Spanish term used for country subdivisions for royal administrative purposes, ensuring districts were under crown control as opposed to local elites. A ''corregimiento'' was usually headed by a ''corregidor''. Historical corregimientos ''Corregimientos'' were found historically in the Kingdom of Castile, the Kingdom of Aragon, and the Spanish West Indies. Castile In Old Castile ''corregimientos'' existed since the 13th century and were the administrative divisions of the ''Junta General de las Siete Merindades de Castilla Vieja''. After the Nueva Planta decrees under the rule of Philip V—the first Bourbon king of Spain, the ''corregidor'' was replaced by an intendant. ''Corregimientos'' in Castile existed until 1835, the year in which the municipal administration was reorganized under Queen Isabel II. Crown of Aragon In the territories of Aragon, Catalonia, and the Land of Valencia formerly under the ancient Crown of Aragon, th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Spanish Conquest Of The Muisca
The Spanish conquest of the Muisca took place from 1537 to 1540. The Muisca were the inhabitants of the central Andean highlands of Colombia before the arrival of the Spanish conquistadors. They were organised in a loose confederation of different rulers; the '' psihipqua'' of Muyquytá, with his headquarters in Funza, the ''hoa'' of Hunza, the '' iraca'' of the sacred City of the Sun Sugamuxi, the Tundama of Tundama, and several other independent ''caciques''. The most important rulers at the time of the conquest were ''psihipqua'' Tisquesusa, ''hoa'' Eucaneme, ''iraca'' Sugamuxi and Tundama in the northernmost portion of their territories. The Muisca were organised in small communities of circular enclosures (''ca'' in their language Muysccubbun; literally "language of the people"), with a central square where the '' bohío'' of the ''cacique'' was located. They were called "Salt People" because of their extraction of salt in various locations throughout their ter ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Phyllite
Phyllite ( ) is a type of foliated metamorphic rock created from slate that is further metamorphosed so that very fine grained white mica achieves a preferred orientation.Stephen Marshak ''Essentials of Geology'', 3rd ed. It is primarily composed of quartz, sericite mica, and chlorite. Phyllite has fine-grained mica flakes, whereas slate has extremely fine mica flakes, and schist has large mica flakes, all mica flakes of which have achieved a preferred orientation. Among foliated metamorphic rocks, it represents a gradation in the degree of metamorphism between slate and schist. The minute crystals of graphite, sericite, or chlorite, or the translucent fine-grained white mica, impart a silky, sometimes golden sheen to the surfaces of cleavage, called "phyllitic luster". The word comes from the Greek ''phyllon'', meaning "leaf". The protolith (or parent rock) for phyllite is shale or pelite, or slate, which in turn came from a shale protolith. Its constituent platy mine ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Metamorphic Rock
Metamorphic rocks arise from the transformation of existing rock to new types of rock in a process called metamorphism. The original rock ( protolith) is subjected to temperatures greater than and, often, elevated pressure of or more, causing profound physical or chemical changes. During this process, the rock remains mostly in the solid state, but gradually recrystallizes to a new texture or mineral composition. The protolith may be an igneous, sedimentary, or existing metamorphic rock. Metamorphic rocks make up a large part of the Earth's crust and form 12% of the Earth's land surface. They are classified by their protolith, their chemical and mineral makeup, and their texture. They may be formed simply by being deeply buried beneath the Earth's surface, where they are subject to high temperatures and the great pressure of the rock layers above. They can also form from tectonic processes such as continental collisions, which cause horizontal pressure, friction, and di ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rock Types
In geology, rock (or stone) is any naturally occurring solid mass or aggregate of minerals or mineraloid matter. It is categorized by the minerals included, its Chemical compound, chemical composition, and the way in which it is formed. Rocks form the Earth's outer solid layer, the Earth's crust, crust, and most of its interior, except for the liquid Earth's outer core, outer core and pockets of magma in the asthenosphere. The study of rocks involves multiple subdisciplines of geology, including petrology and mineralogy. It may be limited to rocks found on Earth, or it may include planetary geology that studies the rocks of other celestial objects. Rocks are usually grouped into three main groups: igneous rocks, sedimentary rocks and metamorphic rocks. Igneous rocks are formed when magma cools in the Earth's crust, or lava cools on the ground surface or the seabed. Sedimentary rocks are formed by diagenesis and lithification of sediments, which in turn are formed by the weathe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
South American Plate
The South American Plate is a major tectonic plate which includes the continent of South America as well as a sizable region of the Atlantic Ocean seabed extending eastward to the African Plate, with which it forms the southern part of the Mid-Atlantic Ridge. The easterly edge is a divergent boundary with the African Plate; the southerly edge is a complex boundary with the Antarctic Plate, the Scotia Plate, and the Sandwich Plate; the westerly edge is a convergent boundary with the subducting Nazca Plate; and the northerly edge is a boundary with the Caribbean Plate and the oceanic crust of the North American Plate. At the Chile Triple Junction, near the west coast of the Taitao– Tres Montes Peninsula, an oceanic ridge known as the Chile Rise is actively subducting under the South American Plate. Geological research suggests that the South American Plate is moving westward away from the Mid-Atlantic Ridge: "Parts of the plate boundaries consisting of alternations of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Oca-Ancón Fault System
The Oca-Ancón Fault System ( es, Falla Oca-Ancón) is a complex of geological faults located in northeastern Colombia and northwestern Venezuela near the Caribbean Sea. The fault system is of right-lateral strike-slip type and extends for an approximate length of .Paris et al., 2000, p.9Audemard et al., 1996a The Oca-Ancón Fault System is part of the diffuse boundary between the Caribbean Plate and the South American Plate.Audemard et al., 1996b The movement rate of the Oca-Ancón Fault System is estimated at each year, more than most Venezuelan faults.Audemard et al, 2006 Oca Fault segment The vertical to subvertical Oca Fault segment in the western part of the fault system has a length of , running west–east through La Guajira, Colombia. It forms the northern boundary of the Sierra Nevada de Santa Marta and cuts through the Serranía del Perijá continuing into Venezuela. The fault segment with a slip rate of per year has been active since the Late Pleistocene (~15,000 ye ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Caribbean Plate
The Caribbean Plate is a mostly oceanic tectonic plate underlying Central America and the Caribbean Sea off the north coast of South America. Roughly 3.2 million square kilometers (1.2 million square miles) in area, the Caribbean Plate borders the North American Plate, the South American Plate, the Nazca Plate and the Cocos Plate. These borders are regions of intense seismic activity, including frequent earthquakes, occasional tsunamis, and volcanic eruptions. Boundary types The northern boundary with the North American Plate is a transform or strike-slip boundary which runs from the border area of Belize, Guatemala ( Motagua Fault), and Honduras in Central America, eastward through the Cayman trough along the Swan Islands Transform Fault before joining the southern boundary of the Gonâve Microplate. East of the Mid-Cayman Rise this continues as the Walton fault zone and the Enriquillo–Plantain Garden fault zone into eastern Hispaniola. From there it continue ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Biodiversity In Colombia
The biodiversity of Colombia is the variety of indigenous organisms in the country with the second-highest biodiversity in the world, behind Brazil. As of 2021, around 63,000 species are registered in Colombia, of which 14% are endemic. The country occupies worldwide the first position in number of orchids, birds and butterflies, second position in plants, amphibians and fresh water fish, third place in species of palm trees and reptiles and globally holds the sixth position in biodiversity of mammals. The country hosts 59 nationally designated protected areas. At the establishment of the most recent addition, Bahía Portete – Kaurrele National Natural Park, Colombian president Juan Manuel Santos said "Biodiversity is to Colombia, what oil is for the Arabs". [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tairona
Tairona (or Tayrona) was a Pre-Columbian culture of Colombia, which consisted in a group of chiefdoms in the region of Sierra Nevada de Santa Marta in present-day Cesar, Magdalena and La Guajira Departments of Colombia, South America, which goes back at least to the 1st century AD and had significant demographic growth around the 11th century. The Tairona people formed one of the two principal linguistic groups of the Chibchan family, the other being the Muisca. Genetic and archaeological evidence shows a relatively dense occupation of the region by at least 200 BC. Pollen data compiled by Luisa Fernanda Herrera in 1980 shows considerable deforestation and the use of cultigens such as yuca and maize since possibly 1200 BC. However, occupation of the Colombian Caribbean coast by sedentary or semi-sedentary populations has been documented to have occurred by c. 4000 BC. Ethnohistorical data shows that initial contact with the Spanish was tolerated by the Tairona; but by ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pico Simón Bolívar
Pico Simón Bolívar is the second highest mountain in Colombia, with an estimated height of . Pico Bolívar and the neighbouring summit of Pico Cristóbal Colón are the two highest peaks in Colombia and are very nearly equal in elevation. The difference in elevation is estimated to be only one or two metres. One or other of these peaks is therefore the fifth most prominent in the world (see list of peaks by prominence). The nearest peak that is higher is Cayambe, some away. There is a permanent snowcap on this peak and on the nearby mountains. It is part of the Sierra Nevada de Santa Marta range, along with Pico Cristóbal Colón. The peak is named after Simón Bolívar. Climbing history Pico Simón Bolívar was first climbed in 1939 by W. Wood, A. Bakerwell and E. Praolini. Access to these mountains became very difficult after the early 1990s due to hostile locals, drug traffickers, and FARC guerillas. An expedition in 2015 was one of the first to climb in the range for ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pico Cristóbal Colón
Pico Cristóbal Colón is the highest mountain in Colombia, with an estimated height of . Pico Cristóbal Colón and Pico Simón Bolívar are the two highest peaks in Colombia and are equal in elevation. One or the other of these peaks is therefore the fifth most prominent in the world (see list of peaks by prominence). The nearest peak that is higher is Cayambe, some away. There is a permanent snowcap on this peak and on the nearby mountains. It is part of the Sierra Nevada de Santa Marta range, along with Pico Simón Bolívar. The peak is named after Christopher Columbus. Climbing history Colón was first climbed in 1939 by Walter Wood, Anderson Bakerwell and E. Praolini. Access to these mountains became very difficult after the early 1990s due to hostile locals, drug traffickers, and FARC guerillas. An expedition in 2015 led by John Biggar was one of the first to climb in the range for many years, and reached the summit of Pico Colón on 13 December. See also * List o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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