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Guadalupe Hill
Guadalupe Hill is a high hill located in the Eastern Hills, Bogotá, 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 (geology), 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 people, Muisca, who inhabited the Bogotá savanna and surrounding regions before the Spanish ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Monserrate
Monserrate (named after Catalan homonym mountain '' Montserrat'') is a high mountain over 10,000 feet high that dominates 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, 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 sections of the north of the city are visible ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Muisca People
The Muisca (also called Chibcha) are an indigenous peoples of Colombia, indigenous people and Pre-Columbian cultures of Colombia, culture of the Altiplano Cundiboyacense, Colombia, that formed the Muisca Confederation before the Spanish conquest of the Muisca, Spanish conquest. The people spoke Muysccubun, a language of the Chibchan languages, Chibchan language family, also called ''Muysca'' and ''Mosca''. They were encountered by list of conquistadors in Colombia, conquistadors dispatched by the Spanish Empire in 1537 at the time of the Spanish conquest of the Muisca, conquest. Subgroupings of the Muisca were mostly identified by their allegiances to three great rulers: the ''zaque, hoa'', centered in Tunja, Hunza, ruling a territory roughly covering modern southern and northeastern Boyacá Department, Boyacá and southern Santander Department, Santander; the ''zipa, psihipqua'', centered in Bacatá, Muyquytá and encompassing most of modern Cundinamarca Department, Cundinama ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Muisca Religion
Muisca religion describes the religion of the Muisca who inhabited the central highlands of the Colombian Andes before the Spanish conquest of the Muisca. The Muisca formed a confederation of holy rulers and had a variety of 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 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 woman and the sacred status of marriage.Muisca religion - Pueblos Originarios - accessed 04-05-2016 The Muisca worshipped their gods at sacred sites, both natural, such as |
Muisca Astronomy - Position Sué - Bolívar Square & Eastern Hills, Bogotá - English Version - Short
The Muisca (also called Chibcha) are an indigenous people and culture of the Altiplano Cundiboyacense, Colombia, that formed the Muisca Confederation before the Spanish conquest. The people spoke Muysccubun, a language of the Chibchan language family, also called ''Muysca'' and ''Mosca''. They were encountered by conquistadors dispatched by the Spanish Empire in 1537 at the time of the conquest. Subgroupings of the Muisca were mostly identified by their allegiances to three great rulers: the ''hoa'', centered in Hunza, ruling a territory roughly covering modern southern and northeastern Boyacá and southern Santander; the '' psihipqua'', centered in Muyquytá and encompassing most of modern Cundinamarca, the western Llanos; and the ''iraca'', religious ruler of Suamox and modern northeastern Boyacá and southwestern Santander. The territory of the Muisca spanned an area of around from the north of Boyacá to the Sumapaz Páramo and from the summits to the western porti ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Aquifer
An aquifer is an underground layer of water-bearing, permeable rock, rock fractures, or unconsolidated materials ( gravel, sand, or silt). Groundwater from aquifers can be extracted using a water well. Aquifers vary greatly in their characteristics. The study of water flow in aquifers and the characterization of aquifers is called hydrogeology. Related terms include aquitard, which is a bed of low permeability along an aquifer, and aquiclude (or ''aquifuge''), which is a solid, impermeable area underlying or overlying an aquifer, the pressure of which could create a confined aquifer. The classification of aquifers is as follows: Saturated versus unsaturated; aquifers versus aquitards; confined versus unconfined; isotropic versus anisotropic; porous, karst, or fractured; transboundary aquifer. Challenges for using groundwater include: overdrafting (extracting groundwater beyond the equilibrium yield of the aquifer), groundwater-related subsidence of land, groundwater becomin ... [...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 referred to as a ''blind thrust'' fault. Because of the lack of surface evidence, blind ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cacho Formation
The Cacho Formation ( es, Formación Cacho, 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 i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bogotá Formation
The Bogotá Formation ( es, Formación Bogotá, 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-re ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Guaduas Formation
The Guaduas Formation ( es, Formación Guaduas, 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'', ' ... [...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 minerals (hydrous aluminium phyllosilicates, e.g. kaolin, Al2 Si2 O5( 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 ( laminae) less than one centimeter in thickness. This property is called '' 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 more narrow 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 into thin layers, often splintery and usually parallel to the otherwise indistinguishable bed ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sandstone
Sandstone is a clastic sedimentary rock composed mainly of sand-sized (0.0625 to 2 mm) silicate grains. Sandstones comprise about 20–25% of all sedimentary rocks. Most sandstone is composed of quartz or feldspar (both silicates) because they are the most resistant minerals to weathering processes at the Earth's surface. Like uncemented sand, sandstone may be any color due to impurities within the minerals, but the most common colors are tan, brown, yellow, red, grey, pink, white, and black. Since sandstone beds often form highly visible cliffs and other topographic features, certain colors of sandstone have been strongly identified with certain regions. Rock formations that are primarily composed of sandstone usually allow the percolation of water and other fluids and are porous enough to store large quantities, making them valuable aquifers and petroleum reservoirs. Quartz-bearing sandstone can be changed into quartzite through metamorphism, usually r ... [...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 sanctuary of the Catholic Church, dedicated to the Virgin Mary in her invocation 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 Salvador Martínez Ávila, who has the title of general and episcopal vicar of Guadalupe and abbot of the basilica. It is the most visited Marian precinct in the world, surpassed only by Saint Peter's Basilica. Although the figures cited are not uniform, annually some twenty million pilgrims visit the sanctuary, of which about nine million do so in the days around December. Every year some twenty million pilgrims visit the sanctuary, of which about nine million do so in the days around D ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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