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Chiqllarasu
Chiqllarasu (Quechua, ''chiqlla'' green, Ancash Quechua ''rasu'' snow, ice, mountain with snow, Hispanicized spelling ''Chicllarazo'') Portugueza or PortuguesaThe American Alpine Journal, vol. 20, No. 2, 1976, p. 495: "... I climbed Chicllarazo (16,925 feet, 5167 meters) from here on June 17 via Patahuasi and its west ridge. This is the gray glacier-hung peak seen east from the pass which on modern maps has unnecessarily been called "Nevado Portuguesa ." is a mountain in the Andes of Peru, about high. It is situated in the Ayacucho Region, Cangallo Province, Paras District. Chiqllarasu lies north-east of the mountain Saywa Q'asa, between the villages Patawasi ''(Patahuasi)'' in the northwest and Kichkawasi ''(Quichcahuasi)'' in the southeast. Chiqllarasu lies on the top of the crest of the Western Cordillera. It features a wide caldera, known as the Cerro Sagollan caldera. Within the thick deposits gold and silver have been found. These are epithermal deposits with low sulfide ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Paras District
Paras District is one of six Districts of Peru, districts of the province Cangallo Province, Cangallo in Peru. Geography One of the highest mountains of the district is Chiqllarasu at . Other mountains are listed below: Ethnic groups The people in the district are mainly Indigenous peoples of the Americas, indigenous citizens of Quechua people, Quechua descent. Quechua language, Quechua is the language which the majority of the population (85.65%) learnt to speak in childhood, 14.16% of the residents started speaking using the Spanish language, Spanish language (2007 Peru Census). INEI, Peru, Censos Nacionales 2007, Frequencias: Preguntas de Población: Idioma o lengua con el que aprendió hablar (in Spanish) References {{coord, 13.5524, S, 74.6274, W, source:wikidata, display ...[...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cangallo Province
The Cangallo Province is a province located in the Ayacucho Region of Peru. It is one of the eleven that make up the region. The province has a population of 36,977 inhabitants as of census 2005. The capital of the province is the city of Cangallo. Boundaries *North: Huamanga Province *East: Vilcas Huamán Province *South: Víctor Fajardo Province *West: Huancavelica Region Geography One of the highest mountains of the province is Chiqllarasu at . Other mountains are listed below: Political division The province extends over an area of and is divided into six districts: * Cangallo ( Cangallo) * Chuschi ( Chuschi) * Los Morochucos ( Pampa Cangallo) * María Parado de Bellido (Pomabamba) * Paras ( Paras) * Totos ( Totos) Ethnic groups The people in the province are mainly indigenous citizens of Quechua descent. Quechua is the language which the majority of the population (90.14%) learnt to speak in childhood, 9.62% of the residents started speaking using the Spanish ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Saywa Q'asa
Saywa Q'asa (Quechua '' saywa'' boundary stone, landmark, ''q'asa'' mountain pass, "landmark mountain pass", Hispanicized spelling ''Sayhuaccasa'') is a mountain in the Andes of Peru, about high. It is situated in the Ayacucho Region, Cangallo Province, in the north of the Paras District. Saywa Q'asa lies south-west of the mountain Chiqllarasu, west of the mountain Saywa ''(Sayhua)'', north-east of the mountain Waranwallqa and east of the mountain Rit'ipata Ritipata (possibly from Quechua) is a mountain in the Apolobamba mountain range in the Andes of Peru. It is located in the Puno Region, Putina Province, Ananea District, as well as in the Sandia Province, Quiaca District. Ritipata is situate .... The Pampawasi River ''(Pampahuasi)'' originates near Saywa Q'asa. It flows to the south where its waters reach Pampas River near the town of Paras. References Mountains of Peru Mountains of Ayacucho Region {{Ayacucho-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Andes
The Andes, Andes Mountains or Andean Mountains (; ) are the longest continental mountain range in the world, forming a continuous highland along the western edge of South America. The range is long, wide (widest between 18°S – 20°S latitude), and has an average height of about . The Andes extend from north to south through seven South American countries: Venezuela, Colombia, Ecuador, Peru, Bolivia, Chile, and Argentina. Along their length, the Andes are split into several ranges, separated by intermediate depressions. The Andes are the location of several high plateaus—some of which host major cities such as Quito, Bogotá, Cali, Arequipa, Medellín, Bucaramanga, Sucre, Mérida, El Alto and La Paz. The Altiplano plateau is the world's second-highest after the Tibetan plateau. These ranges are in turn grouped into three major divisions based on climate: the Tropical Andes, the Dry Andes, and the Wet Andes. The Andes Mountains are the highest m ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rio Apacheta
Rio or Río is the Portuguese, Spanish, Italian, and Maltese word for "river". When spoken on its own, the word often means Rio de Janeiro, a major city in Brazil. Rio or Río may also refer to: Geography Brazil * Rio de Janeiro * Rio do Sul, a town in the state of Santa Catarina, Brazil Mexico * Río Bec, a Mayan archaeological site in Mexico * Río Bravo, Tamaulipas, a city in Mexico United States * Rio, a location in Deerpark, New York, US * Rio, Florida, a census-designated place in Martin County, US * Rio, Georgia, an unincorporated community in Spalding County, US * Rio, Illinois, a village in Knox County, US * Rio, Virginia, a community in Albemarle County, US * Rio, West Virginia, a village in Hampshire County, US * Rio, Wisconsin, a village in Columbia County, US * El Río, Las Piedras, Puerto Rico, a barrio * Río Arriba, Añasco, Puerto Rico, a barrio * Río Arriba, Arecibo, Puerto Rico, a barrio * Río Arriba, Fajardo, Puerto Rico, a barrio * Río Arriba, Vega Baja ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
ResearchGate
ResearchGate is a European commercial social networking site for scientists and researchers to share papers, ask and answer questions, and find collaborators. According to a 2014 study by ''Nature'' and a 2016 article in ''Times Higher Education'', it is the largest academic social network in terms of active users, although other services have more registered users, and a 2015–2016 survey suggests that almost as many academics have Google Scholar profiles. While reading articles does not require registration, people who wish to become site members need to have an email address at a recognized institution or to be manually confirmed as a published researcher in order to sign up for an account. Members of the site each have a user profile and can upload research output including papers, data, chapters, negative results, patents, research proposals, methods, presentations, and software source code. Users may also follow the activities of other users and engage in discussions with th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hydrothermal
Hydrothermal circulation in its most general sense is the circulation of hot water (Ancient Greek ὕδωρ, ''water'',Liddell, H.G. & Scott, R. (1940). ''A Greek-English Lexicon. revised and augmented throughout by Sir Henry Stuart Jones. with the assistance of. Roderick McKenzie.'' Oxford: Clarendon Press. and θέρμη, ''heat'' ). Hydrothermal circulation occurs most often in the vicinity of sources of heat within the Earth's crust. In general, this occurs near volcanic activity, but can occur in the shallow to mid crust along deeply penetrating fault irregularities or in the deep crust related to the intrusion of granite, or as the result of orogeny or metamorphism. Seafloor hydrothermal circulation Hydrothermal circulation in the oceans is the passage of the water through mid-oceanic ridge systems. The term includes both the circulation of the well-known, high-temperature vent waters near the ridge crests, and the much-lower-temperature, diffuse flow of water through sedim ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Resurgent Dome
In geology, a resurgent dome is a dome formed by swelling or rising of a caldera floor due to movement in the magma chamber beneath it. Unlike a lava dome, a resurgent dome is not formed by the extrusion of highly viscous lava onto the surface, but rather by the uplift and deformation of the surface itself by magma movement underground. Resurgent domes are typically found near the center of very large open calderas such as Yellowstone Caldera or Valles Caldera, and in turn such calderas are often referred to as "resurgent-type" calderas to distinguish them from the more common (but much smaller) calderas found on shield volcanoes and stratovolcanoes. The structure that makes a resurgent dome possible is a fracture zone made up of ring faults surrounded by concentric normal faults around the outside of the rings. During initial formation of the caldera these ring faults provide vents for ash-flow eruptions and are the point at which subsidence of the cauldron block occurs. S ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tuff
Tuff is a type of rock made of volcanic ash ejected from a vent during a volcanic eruption. Following ejection and deposition, the ash is lithified into a solid rock. Rock that contains greater than 75% ash is considered tuff, while rock containing 25% to 75% ash is described as tuffaceous (for example, ''tuffaceous sandstone''). Tuff composed of sandy volcanic material can be referred to as volcanic sandstone. Tuff is a relatively soft rock, so it has been used for construction since ancient times. Because it is common in Italy, the Romans used it often for construction. The Rapa Nui people used it to make most of the ''moai'' statues on Easter Island. Tuff can be classified as either igneous or sedimentary rock. It is usually studied in the context of igneous petrology, although it is sometimes described using sedimentological terms. Tuff is often erroneously called tufa in guidebooks and in television programmes. Volcanic ash The material that is expelled in a volcanic ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Batholith
A batholith () is a large mass of intrusive igneous rock (also called plutonic rock), larger than in area, that forms from cooled magma deep in Earth's crust. Batholiths are almost always made mostly of felsic or intermediate rock types, such as granite, quartz monzonite, or diorite (see also ''granite dome''). Formation Although they may appear uniform, batholiths are in fact structures with complex histories and compositions. They are composed of multiple masses, or ''plutons'', bodies of igneous rock of irregular dimensions (typically at least several kilometers) that can be distinguished from adjacent igneous rock by some combination of criteria including age, composition, texture, or mappable structures. Individual plutons are solidified from magma that traveled toward the surface from a zone of partial melting near the base of the Earth's crust. Traditionally, these plutons have been considered to form by ascent of relatively buoyant magma in large masses called ''p ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Erosion
Erosion is the action of surface processes (such as water flow or wind) that removes soil, rock, or dissolved material from one location on the Earth's crust, and then transports it to another location where it is deposited. Erosion is distinct from weathering which involves no movement. Removal of rock or soil as clastic sediment is referred to as ''physical'' or ''mechanical'' erosion; this contrasts with ''chemical'' erosion, where soil or rock material is removed from an area by dissolution. Eroded sediment or solutes may be transported just a few millimetres, or for thousands of kilometres. Agents of erosion include rainfall; bedrock wear in rivers; coastal erosion by the sea and waves; glacial plucking, abrasion, and scour; areal flooding; wind abrasion; groundwater processes; and mass movement processes in steep landscapes like landslides and debris flows. The rates at which such processes act control how fast a surface is eroded. Typically, physical erosion procee ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kachimayu (Ayacucho-Huancavelica)
Kachimayu (Quechua ''kachi'' salt, ''mayu'' river, "salt river", hispanicized spellings ''Cachimayo'' or ''Cachi'') is a river in Peru located in the regions Ayacucho and Huancavelica. It is an affluent of the Mantaro River.escale.minedu.gob.pe - UGEL map of the Huanta Province (1) (Ayacucho Region) showing "Río Cachimayo" and "Río Cachi" Kachimayu originates in the Huamanga Province. First it flows along the border of the provinces Angaraes and Huamanga until reaching the Huanta Huanta is a town in Central Peru, capital of the province Huanta in the region Ayacucho. History In the era of the Spanish American wars of independence, Huanta remained loyal to the Spanish mo ... Province. Then it turns to the north following the border of the provinces Angaraes and Huanta. East of Marcas the Urubamba River of the Angaraes Province joins Kachimayu. The confluence with the Mantaro River is near Tinkuy (''Tincoy)'' and Allqumach' ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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