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Guadalupe Hill
Guadalupe Hill is a high hill located in the Eastern Hills, uphill from the centre of Bogotá, Colombia. Together with its neighbouring hill Monserrate it is one of the landmarks of Bogotá. At the top of the hill a hermitage and a high statue has been erected. The statue was elaborated by sculptor Gustavo Arcila Uribe in 1946 and is accompanied by a chapel dedicated to Our Lady of Guadalupe. Guadalupe Hill is the type locality of the Guadalupe Group, a Late Cretaceous sedimentary sequence of sandstones and shales of thick. The formation is being thrust on top of younger strata by the reverse Bogotá Fault as a result of the ongoing Andean orogeny. The hill is the source for the Manzanares and El Chuscal creeks that flow westwards onto the Bogotá savanna. Historically, Guadalupe Hill was an important sacred site for the indigenous Muisca, who inhabited the Bogotá savanna and surrounding regions before the Spanish conquest. During the colonial period, Guadalupe Hill containe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Monserrate
Monserrate (named after Catalan language, Catalan homonym mountain ''Montserrat (mountain), Montserrat'') is a mountain over high that overlooks the city center of Bogotá, the capital city of Colombia. It rises to above the sea level, where there is a church (built in the 17th century) with a shrine, devoted to ''El Señor Caído'' ("The Fallen Lord"). The Mountain, already considered sacred in pre-Columbian times when the area was inhabited by the indigenous Muisca people, Muisca, is a pilgrim destination, as well as a major tourist attraction. In addition to the church, the summit contains restaurants, cafeteria, souvenir shops and many smaller tourist facilities. Monserrate can be accessed by aerial tramway (a cable car known as the teleférico), by funicular, or by climbing, the preferred way of pilgrims. The climbing route was previously closed due to wildfires and landslides caused by a drought, but it reopened in 2017. All downtown Bogotá, south Bogotá and some sectio ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Muisca People
The Muisca (also called the Chibcha) are indigenous peoples in Colombia and were a Pre-Columbian culture of the Altiplano Cundiboyacense that formed the Muisca Confederation before the Spanish colonization of the Americas. The Muisca speak Muysccubun, a language of the Chibchan language family, also called ''Muysca'' and ''Mosca''. The first known contact with Europeans in the region was in 1537 during the Spanish conquest of New Granada. In New Spain, Spanish clerics and civil officials had a major impact on the Muisca, attempting to Christianize and incorporate them into the Spanish Empire as subjects. Postconquest Muisca culture underwent significant changes due to the establishment of the New Kingdom of Granada. Sources for the Muisca are far less abundant than for the Aztec Empire of Mesoamerica or the Inca Empire and their incorporation to the Spanish Empire during the colonial era. In the New Kingdom of Granada and into the colonial era, the Muisca became " ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Muisca Religion
Muisca religion describes the religion of the Muisca people, Muisca who inhabited the central highlands of the Colombian Andes before the Spanish conquest of the Muisca. The Muisca formed a Muisca Confederation, confederation of holy Muisca rulers, rulers and had a variety of deity, deities, temples and rituals incorporated in their culture. Supreme being of the Muisca was Chiminigagua who created light and the Earth. He was not directly honoured, yet that was done through Chía (goddess), Chía, goddess of the Moon, and her husband Sué, god of the Sun. The representation of the two main celestial bodies as husband and wife showed the complementary character of man and Women in Muisca society, woman and the sacred status of marriage.Muisca religion - Pueblos Originarios - accessed 04-05-2016 The Muisca worshipped the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Muisca Astronomy - Position Sué - Bolívar Square & Eastern Hills, Bogotá - English Version - Short
The Muisca (also called the Chibcha) are indigenous peoples in Colombia and were a Pre-Columbian culture of the Altiplano Cundiboyacense that formed the Muisca Confederation before the Spanish colonization of the Americas. The Muisca speak Muysccubun, a language of the Chibchan language family, also called ''Muysca'' and ''Mosca''. The first known contact with Europeans in the region was in 1537 during the Spanish conquest of New Granada. In New Spain, Spanish clerics and civil officials had a major impact on the Muisca, attempting to Christianize and incorporate them into the Spanish Empire as subjects. Postconquest Muisca culture underwent significant changes due to the establishment of the New Kingdom of Granada. Sources for the Muisca are far less abundant than for the Aztec Empire of Mesoamerica or the Inca Empire and their incorporation to the Spanish Empire during the colonial era. In the New Kingdom of Granada and into the colonial era, the Muisca became "the off ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Aquifer
An aquifer is an underground layer of water-bearing material, consisting of permeability (Earth sciences), permeable or fractured rock, or of unconsolidated materials (gravel, sand, or silt). Aquifers vary greatly in their characteristics. The study of water flow in aquifers and the characterization of aquifers is called ''hydrogeology''. Related concepts include aquitard, a bed (geology), bed of low permeability along an aquifer, and aquiclude (or ''aquifuge''), a solid and impermeable region underlying or overlying an aquifer, the pressure of which could lead to the formation of a confined aquifer. Aquifers can be classified as saturated versus unsaturated; aquifers versus aquitards; confined versus unconfined; isotropic versus anisotropic; porous, karst, or fractured; and transboundary aquifer. Groundwater from aquifers can be sustainably harvested by humans through the use of qanats leading to a well. This groundwater is a major source of fresh water for many regions, althoug ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Thrust Fault
A thrust fault is a break in the Earth's crust, across which older rocks are pushed above younger rocks. Thrust geometry and nomenclature Reverse faults A thrust fault is a type of reverse fault that has a dip of 45 degrees or less. If the angle of the fault plane is lower (often less than 15 degrees from the horizontal) and the displacement of the overlying block is large (often in the kilometer range) the fault is called an ''overthrust'' or ''overthrust fault''. Erosion can remove part of the overlying block, creating a ''fenster'' (or ''window'') – when the underlying block is exposed only in a relatively small area. When erosion removes most of the overlying block, leaving island-like remnants resting on the lower block, the remnants are called ''klippen'' (singular '' klippe''). Blind thrust faults If the fault plane terminates before it reaches the Earth's surface, it is called a ''blind thrust'' fault. Because of the lack of surface evidence, blind thrust fa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cacho Formation
The Cacho Formation (, E1C, Tpc, Tec) is a geological formation of the Altiplano Cundiboyacense, Eastern Ranges of the Colombian Andes. The predominantly sandstone formation with thin intercalated beds of shales dates to the Paleogene period; Middle to Late Paleocene epochs, and has a maximum thickness of . Definition The formation was first described by Hubach in 1931 and 1957 and named by Campbell in 1962 and Julivert in 1963.Montoya & Reyes, 2005, p.55Acosta & Ulloa, 2002, p.58 Description Lithologies The Cacho Formation consists of white, yellow and reddish fine to coarse cross-bedded sandstones in thick banks intercalated with reddish and grey shales. Stratigraphy and depositional environment The thick Cacho Formation overlies the Guaduas Formation and is overlain by the Bogotá Formation.Guerrero Uscátegui, 1992, p.5 The age has been estimated to be Late Paleocene, based on paleoflora studied by Thomas van der Hammen in 1957. The formation is laterally equivalen ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bogotá Formation
The Bogotá Formation (, E1-2b, Tpb, Pgb) is a geological formation of the Eastern Hills and Bogotá savanna on the Altiplano Cundiboyacense, Eastern Ranges of the Colombian Andes. The predominantly shale and siltstone formation, with sandstone beds intercalated, dates to the Paleogene period; Upper Paleocene to Lower Eocene epochs, with an age range of 61.66 to 52.5 Ma, spanning the Paleocene–Eocene Thermal Maximum. The thickness of the Bogotá Formation ranges from near Tunja to near Bogotá. Fossils of the ungulate '' Etayoa bacatensis'' have been found in the Bogotá Formation, as well as numerous reptiles, unnamed as of 2017. Etymology The formation was first described by Hettner in 1892,Acosta & Ulloa, 2002, p.59 then by Hubach in 1931, 1945 and 1957, and named in 1963 by Julivert after the Colombian capital Bogotá and its savanna.Montoya & Reyes, 2005, p.57 Description Lithologies The Bogotá Formation consists mainly of grayish-red, locally purplish, c ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Guaduas Formation
The Guaduas Formation (, K2P1G, K2E1G, KPgg, KTg, TKg, Ktg) is a geological formation of the Middle Magdalena Basin and the Altiplano Cundiboyacense, Eastern Ranges of the Colombian Andes. The predominantly shale with coalbed formation dates to the Late Cretaceous and Paleogene periods; Maastrichtian-Paleocene epochs, and has a maximum thickness of . Fossils of '' Coussapoa camargoi'', '' Ficus andrewsi'', '' Berhamniphyllum sp.'' and '' Archaeopaliurus boyacensis'' have been found in coalbeds in Zipaquirá and Tasco, Boyacá. Etymology The formation was first described by Hettner in 1894 and named in 1931 by Hubach after Guaduas, Cundinamarca, former northern territory of the Panche.Montoya & Reyes, 2005, p.51 Description Lithologies The Guaduas Formation consists mainly of shales with intercalated sandstone beds. The formation contains coalbeds that are widely explored in the area. Fossil remains of '' Coussapoa camargoi'', '' Ficus andrewsi'', '' Berhamniphyllum sp. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Shale
Shale is a fine-grained, clastic sedimentary rock formed from mud that is a mix of flakes of Clay mineral, clay minerals (hydrous aluminium phyllosilicates, e.g., Kaolinite, kaolin, aluminium, Al2Silicon, Si2Oxygen, O5(hydroxide, OH)4) and tiny fragments (silt-sized particles) of other minerals, especially quartz and calcite.Blatt, Harvey and Robert J. Tracy (1996) ''Petrology: Igneous, Sedimentary and Metamorphic'', 2nd ed., Freeman, pp. 281–292 Shale is characterized by its tendency to split into thin layers (Lamination (geology), laminae) less than one centimeter in thickness. This property is called ''Fissility (geology), fissility''. Shale is the most common sedimentary rock. The term ''shale'' is sometimes applied more broadly, as essentially a synonym for mudrock, rather than in the narrower sense of clay-rich fissile mudrock. Texture Shale typically exhibits varying degrees of fissility. Because of the parallel orientation of clay mineral flakes in shale, it breaks in ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sandstone
Sandstone is a Clastic rock#Sedimentary clastic rocks, clastic sedimentary rock composed mainly of grain size, sand-sized (0.0625 to 2 mm) silicate mineral, silicate grains, Cementation (geology), cemented together by another mineral. Sandstones comprise about 20–25% of all sedimentary rocks. Most sandstone is composed of quartz or feldspar, because they are the most resistant minerals to the weathering processes at the Earth's surface. Like uncemented sand, sandstone may be imparted any color by impurities within the minerals, but the most common colors are tan, brown, yellow, red, grey, pink, white, and black. Because sandstone beds can form highly visible cliffs and other topography, topographic features, certain colors of sandstone have become strongly identified with certain regions, such as the red rock deserts of Arches National Park and other areas of the Southwestern United States, American Southwest. Rock formations composed of sandstone usually allow the p ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Basilica Of Our Lady Of Guadalupe
The Basilica of Santa María de Guadalupe, officially called Insigne y Nacional Basílica de Santa María de Guadalupe (in English: Basilica of Our Lady of Guadalupe) is a basilica of the Catholic Church, dedicated to the Virgin Mary in her invocation of Our Lady of Guadalupe, located at the foot of the Hill of Tepeyac in the Gustavo A. Madero borough of Mexico City. It belongs to the Primate Archdiocese of Mexico through the Guadalupana Vicariate, which since November 4, 2018, is in the care of Monsignor Efraín Hernández Díaz, who has the title of general and episcopal vicar of Guadalupe and abbot of the basilica. Every year some twenty million pilgrims visit the sanctuary, of which about nine million do so in the days around December 12, the day on which Our Lady of Guadalupe is celebrated. Annually, the Basilica of Santa María de Guadalupe has at least twice as many visitors as the best-known Marian shrines. History The church known as the Old Basilica of Guadal ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
