Cuevas De Taulabé
Taulabé Caves are part of a natural cave system that spreads throughout the municipality of Taulabé, in the Honduran department of Comayagua. The speleafer (a geologic formation with significant cave development) in Honduras is a limestone vault of Cenomanian age (earliest Late Cretaceous) named the Jaitique Formation (“high-TEE-kay”). It is very similar in outcrop appearance to the Atima limestone (generally consisting of thick-bedded grey micrite Micrite is a limestone constituent formed of calcareous particles ranging in diameter up to four μm formed by the recrystallization of lime mud. Flügel, Erik, ''Microfacies of Carbonate Rocks: Analysis, Interpretation and Application,'' Springe ...), but it does not achieve the thicknesses common to the Atima, probably never exceeding thickness, more commonly around 100 meters. The only partially mapped caves extends at least 921 meters. References External links * * * {{DEFAULTSORT:Cuevas de Taulabe Caves of ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Cave
A cave or cavern is a natural void in the ground, specifically a space large enough for a human to enter. Caves often form by the weathering of rock and often extend deep underground. The word ''cave'' can refer to smaller openings such as sea caves, rock shelters, and grottos, that extend a relatively short distance into the rock and they are called ''exogene'' caves. Caves which extend further underground than the opening is wide are called ''endogene'' caves. Speleology is the science of exploration and study of all aspects of caves and the cave environment. Visiting or exploring caves for recreation may be called ''caving'', ''potholing'', or ''spelunking''. Formation types The formation and development of caves is known as ''speleogenesis''; it can occur over the course of millions of years. Caves can range widely in size, and are formed by various geological processes. These may involve a combination of chemical processes, erosion by water, tectonic forces, microorgani ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Taulabé
Taulabé is a municipality in the Honduran department of Comayagua Comayagua () is a city, municipality and old capital of Honduras, located northwest of Tegucigalpa on the highway to San Pedro Sula and above sea level. The accelerated growth experienced by the city of Comayagua led the municipal authoriti .... It is a very small town that is rapidly growing. The Caves of Taulabe are in the municipality. A guided tour of 400 meters of the caves is available. The caves have been explored up to 12 km, but the exact length of the caves has yet to be determined. Municipalities of the Comayagua Department {{Honduras-geo-stub ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Honduras
Honduras, officially the Republic of Honduras, is a country in Central America. The republic of Honduras is bordered to the west by Guatemala, to the southwest by El Salvador, to the southeast by Nicaragua, to the south by the Pacific Ocean at the Gulf of Fonseca, and to the north by the Gulf of Honduras, a large inlet of the Caribbean Sea. Its capital and largest city is Tegucigalpa. Honduras was home to several important Mesoamerican cultures, most notably the Maya, before the Spanish Colonization in the sixteenth century. The Spanish introduced Catholicism and the now predominant Spanish language, along with numerous customs that have blended with the indigenous culture. Honduras became independent in 1821 and has since been a republic, although it has consistently endured much social strife and political instability, and remains one of the poorest countries in the Western Hemisphere. In 1960, the northern part of what was the Mosquito Coast was transferred from Nicara ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Departments Of Honduras
Honduras is divided into 18 departments ( Spanish: ''departamentos''). Each department is headed by a governor, who is appointed by the President of Honduras. The governor represents the executive branch in the region in addition to acting as intermediary between municipalities and various national authorities; resolves issues arising between municipalities; oversees the penitentiaries and prisons in his department; and regularly works with the various Secretaries of State that form the President's Cabinet. To be eligible for appointment as governor, the individual must a) live for five consecutive years in the department; b) be Honduran; c) be older than 18 years of age and; d) know how to read and write. Evolution of Honduras's territorial organization 1825: The constitutional congress convened in that year orders that the state be divided into seven departments: Comayagua, Santa Bárbara, Tegucigalpa, Choluteca, Yoro, Olancho, and Gracias (later renamed Lempira). 1834: An extr ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Comayagua Department
Comayagua () is one of the 18 departments ''(departamentos)'' into which Honduras is divided. The departmental capital is Comayagua. Geography The department covers a total surface area of 5,124 km² and, in 2015, had an estimated population of 511,943 people. Economy Historically, the department produced gold, copper, cinnabar, asbestos, and silver. Gems were also mined, including opal and emerald. The area was also known for "fine" cattle. Municipalities # Ajuterique # Comayagua # El Rosario # Esquías # Humuya # La Libertad # Lamaní # Las Lajas # La Trinidad # Lejamaní # Meámbar # Minas de Oro # Ojos de Agua # San Jerónimo # San José de Comayagua # San José del Potrero # San Luis # San Sebastián # Siguatepeque Siguatepeque () is a city and municipality in the Honduran department of Comayagua. The city has a population of 73,480 (2020 calculation). History Founded by the Spanish in 1689 as a religious centre for retreats and monastic training, th ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Limestone
Limestone ( calcium carbonate ) is a type of carbonate sedimentary rock which is the main source of the material lime. It is composed mostly of the minerals calcite and aragonite, which are different crystal forms of . Limestone forms when these minerals 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, a closely related rock, which contains a high percentage of the mineral dolomite, . ''Magnesian limestone'' is an obsolete and poorly-defined term used variously for dolomite, for limes ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Cenomanian
The Cenomanian is, in the ICS' geological timescale, the oldest or earliest age of the Late Cretaceous Epoch or the lowest stage of the Upper Cretaceous Series. An age is a unit of geochronology; it is a unit of time; the stage is a unit in the stratigraphic column deposited during the corresponding age. Both age and stage bear the same name. As a unit of geologic time measure, the Cenomanian Age spans the time between 100.5 and 93.9 million years ago (Mya). In the geologic timescale, it is preceded by the Albian and is followed by the Turonian. The Upper Cenomanian starts around at 95 Mya. The Cenomanian is coeval with the Woodbinian of the regional timescale of the Gulf of Mexico and the early part of the Eaglefordian of the regional timescale of the East Coast of the United States. At the end of the Cenomanian, an anoxic event took place, called the Cenomanian-Turonian boundary event or the "Bonarelli event", that is associated with a minor extinction event for marine spec ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Late Cretaceous
The Late Cretaceous (100.5–66 Ma) is the younger of two epochs into which the Cretaceous Period is divided in the geologic time scale. Rock strata from this epoch form the Upper Cretaceous Series. The Cretaceous is named after ''creta'', the Latin word for the white limestone known as chalk. The chalk of northern France and the white cliffs of south-eastern England date from the Cretaceous Period. Climate During the Late Cretaceous, the climate was warmer than present, although throughout the period a cooling trend is evident. The tropics became restricted to equatorial regions and northern latitudes experienced markedly more seasonal climatic conditions. Geography Due to plate tectonics, the Americas were gradually moving westward, causing the Atlantic Ocean to expand. The Western Interior Seaway divided North America into eastern and western halves; Appalachia and Laramidia. India maintained a northward course towards Asia. In the Southern Hemisphere, Australia and Ant ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Atima
Atima is a municipality in the Honduran department of Santa Bárbara. In 2018 it had a population of 11,976. As of 2020 its mayor is Roger Gabriel Leiva Gonzales. In 2021, two workers were stabbed fatally in the village of Berlín. Demographics At the time of the 2013 Honduras census, Atima municipality had a population of 17,648. Of these, 88.62% were Mestizo, 7.13% Indigenous (6.96% Lenca), 3.54% White White is the lightest color and is achromatic (having no hue). It is the color of objects such as snow, chalk, and milk, and is the opposite of black. White objects fully reflect and scatter all the visible wavelengths of light. White on ... and 0.71% Black or Afro-Honduran. References Municipalities of the Santa Bárbara Department, Honduras {{Honduras-geo-stub ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Micrite
Micrite is a limestone constituent formed of calcareous particles ranging in diameter up to four μm formed by the recrystallization of lime mud. Flügel, Erik, ''Microfacies of Carbonate Rocks: Analysis, Interpretation and Application,'' Springer, pp 74-94, 2004 The term was coined in 1959 by Robert Folk for his carbonate rock classification system. Micrite is derived from MICRocrystalline calcITE. In the Folk classification micrite is a carbonate rock dominated by fine-grained calcite. Carbonate rocks that contain fine-grained calcite in addition to allochems are named ''intramicrite'', ''oomicrite'', ''biomicrite'' or ''pelmicrite'' under the Folk classification depending on the dominant allochem. Micrite is lime mud, carbonate of mud grade. Micrite as a component of carbonate rocks can occur as a matrix, as micrite envelopes around allochems or as peloids Peloids are allochems that are composed of micrite, irrespective of size, shape, or origin. The two primary types of ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Caves Of Honduras
A cave or cavern is a natural void in the ground, specifically a space large enough for a human to enter. Caves often form by the weathering of rock and often extend deep underground. The word ''cave'' can refer to smaller openings such as sea caves, rock shelters, and grottos, that extend a relatively short distance into the rock and they are called ''exogene'' caves. Caves which extend further underground than the opening is wide are called ''endogene'' caves. Speleology is the science of exploration and study of all aspects of caves and the cave environment. Visiting or exploring caves for recreation may be called ''caving'', ''potholing'', or ''spelunking''. Formation types The formation and development of caves is known as '' speleogenesis''; it can occur over the course of millions of years. Caves can range widely in size, and are formed by various geological processes. These may involve a combination of chemical processes, erosion by water, tectonic forces, microorgan ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |