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List Of Andean Peaks With Known Pre-Columbian Ascents
This is an incomplete list of mountains in the Andes that are known to have had pre-Columbian ascents. It is divided into those peaks for which there is direct evidence of an ascent to the summit, and those peaks where evidence has been found only at a lower altitude on the mountain. Ascents were made for religious purposes by groups affiliated with the Inca Empire. These ascents sometimes involved the ritual child sacrifice known as ''qhapaq hucha''. Mountains with known ascents to the summit Image:Coropuna.jpg, Coropuna, main summit on the left, Kasulla on the right. Image:Alto Toroni from the west.jpg, There is a large platform on the summit of Alto Toroni. Image:Licancabur volcano summit chile ii region.jpg, View of Licancabur from near San Pedro de Atacama. Image:Antofalla-sunset.jpg, Antofalla seen from the north. Image:Chozas dobles.jpg, Two small ruined dwellings at about 6700m on Llullaillaco Llullaillaco () is a dormant stratovolcano at the border of Argentina (S ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Inca Empire
The Inca Empire (also known as the Incan Empire and the Inka Empire), called ''Tawantinsuyu'' by its subjects, (Quechua for the "Realm of the Four Parts", "four parts together" ) was the largest empire in pre-Columbian America. The administrative, political and military center of the empire was in the city of Cusco. The Inca civilization arose from the Peruvian highlands sometime in the early 13th century. The Spanish began the conquest of the Inca Empire in 1532 and by 1572, the last Inca state was fully conquered. From 1438 to 1533, the Incas incorporated a large portion of western South America, centered on the Andean Mountains, using conquest and peaceful assimilation, among other methods. At its largest, the empire joined modern-day Peru, what are now western Ecuador, western and south central Bolivia, northwest Argentina, the southwesternmost tip of Colombia and a large portion of modern-day Chile, and into a state comparable to the historical empires of Eurasia ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Copiapó (volcano)
Copiapó, also known as Azufre, is a stratovolcano located in the Atacama Region of Chile. The volcano separates the two portions in which Nevado Tres Cruces National Park is divided. In its vicinity lies Ojos del Salado. At its summit an Inca platform can be found. Dacitic volcanism occurred at this centre 11-7 million years ago and covered a surface of . The Valle Ancho fault can be traced beneath this volcano. The main cone is formed by dacites and block and ash flows that were later intruded by dacitic porphyries, associated with hydrothermal alteration. A smaller centre formed on the northern side of the main cone, as well as thick () ignimbrites in two units. A complex of lava domes lies at their southern-eastern end with more hydrothermally altered porphyric intrusions named Azufrera de Copiapo. The last activity 6-7 million years ago formed a shield overlying the lava dome complex and the San Roman dome. Obsidian from this volcanic area has been found in archeological s ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Coropuna
Coropuna is a dormant compound volcano located in the Andes mountains of southeast-central Peru. The upper reaches of Coropuna consist of several perennially snowbound conical summits, lending it the name Nevado Coropuna in Spanish. The complex extends over an area of and its highest summit reaches an altitude of above sea level. This makes the Coropuna complex the third-highest of Peru. Its thick ice cap is the most extensive in Earth's tropical zone, with several outlet glaciers stretching out to lower altitudes. Below an elevation of , there are various vegetation belts which include trees, peat bogs, grasses and also agricultural areas and pastures. The Coropuna complex consists of several stratovolcanos. These are composed chiefly of ignimbrites and lava flows on a basement formed by Middle Miocene ignimbrites and lava flows. The Coropuna complex has been active for at least five million years, with the bulk of the current cone having been formed during the Quat ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Socompa
Socompa is a large stratovolcano at the border of Argentina and Chile with an elevation of metres. Part of the Chilean and Argentine Andean Volcanic Belt (AVB), it is part of the Central Volcanic Zone, one of the various segments of the AVB. This part of the Andean volcanic arc begins in Peru and runs first through Bolivia and Chile, and then through Argentina and Chile, and contains about 44 active volcanoes. Socompa lies close to the pass of the same name, where the Salta-Antofagasta railway crosses the border. Socompa is known for its large debris avalanche, which was formed 7,200 years ago when most of the northwestern slope collapsed and slid down, forming an extensive deposit. It was at first considered to be either a moraine or a nuee ardende deposit, until the 1980 eruption of Mount St. Helens prompted awareness of the instability of volcanic edifices and the existence of large scale collapses on them. The Socompa collapse is among the largest known with a volume of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mercedario
Cerro Mercedario is the highest peak of the Cordillera de la Ramada range and the eighth-highest mountain of the Andes. It is located 100 km to the north of Aconcagua, in the Argentine province of San Juan. It was first ascended in 1934 by Adam Karpiński and Wiktor Ostrowski, members of a Polish andinist expedition led by Konstanty Jodko-Narkiewicz.Mercedario on andesargentinos.com.ar (In Spanish) The Polish party erected a cairn on the summit. In 1968, after several attempts by some of the strongest Argentine climbers, a Japanese group led by Saburo Yoshida accomplished the first ascension of the south side. In 1971 an Austrian expedition led by Fritz Moravec and Othmar Kucera, climbed the north side. In 1972, Itali ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Aucanquilcha
Aucanquilcha is a massive stratovolcano located in the Antofagasta Region of northern Chile, just west of the border with Bolivia and within the Alto Loa National Reserve. Part of the Central Volcanic Zone of the Andes, the stratovolcano has the form of a ridge with a maximum height of . The volcano is embedded in a larger cluster of volcanoes known as the Aucanquilcha cluster. This cluster of volcanoes was formed in stages over eleven million years of activity with varying magma output, including lava domes and lava flows. Aucanquilcha volcano proper is formed from four units that erupted between 1.04–0.23 million years ago. During the ice ages, both the principal Aucanquilcha complex and the other volcanoes of the cluster were subject to glaciation, resulting in the formation of moraines and cirques. The cluster has generated lava ranging in composition from andesite to dacite, with the main volcano being exclusively of dacitic composition. Systematic variations in te ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Aconcagua
Aconcagua () is a mountain in the Principal Cordillera of the Andes mountain range, in Mendoza Province, Argentina. It is the List of highest mountains on Earth, highest mountain in the Americas, the highest outside Asia, and the highest in the Southern Hemisphere with a summit elevation of . It lies northwest of the provincial capital, the Mendoza, Argentina, city of Mendoza, about from San Juan Province, Argentina, San Juan Province, and from Argentina's border with neighbouring Chile. The mountain is one of the Seven Summits of the seven continents. Aconcagua is bounded by the ''Valle de las Vacas'' to the north and east and the ''Valle de los Horcones Inferior'' to the west and south. The mountain and its surroundings are part of the Aconcagua Provincial Park. The mountain has a number of glaciers. The largest glacier is the Ventisquero Horcones Inferior at about long, which descends from the south face to about in elevation near the Confluencia camp. Two other large g ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cerro El Toro
Cerro El Toro is a mountain in the Andes located on the border between Argentina and Chile. It has an elevation of 6,168 m above sea level. Its territory is within the Argentinean protection areas of Provincial Reserve San Guillermo. The Argentinean side is at San Juan province, commune of Iglesia. Chilean side is at the Huasco province, and commune of Alto del Carmen. First Ascents Toro was first climbed by Incas in unknown dates. A mummy was found on the Argentine slopes in 1964. The first recorded post colonization ascent was by Antonio Beorchia Nigris (Italy), Jorge Enrique Varas and Sergio Fernandez (Argentina) in 02/26/1964. Elevation It has an official height of 6160 meters. Other data from available digital elevation models: SRTM yields 6148 metres, ASTER 6122 metres and TanDEM-X 6184 metres. The height of the nearest key col is 4326 meters, leading to a topographic prominence of 1842 meters. Toro is considered a Mountain Range according to the ''Dominance System'' ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nevado Queva
Nevado Queva or Quewar is a volcano in the Andes mountain range of South America, located in the Salta Province of Argentina. Queva has a summit elevation of above sea level. Its name is alternately spelled Quehuar. There are extensive pre Columbian ruins on the summit of the mountain, which is a broad crater. It is the highest of Nevados de los Pastos Grandes and its territory is within the Argentinean protection area of Provincial Fauna Reserve Los Andes. It is located within the territory of the Argentinean province of Salta. Its slopes are within the administrative boundaries of the Argentinean city of San Antonio de los Cobres. File:Volcan Nevado de Quewar.jpg, Nevado de Quewar File:Queva_summit_ruins.jpg, Pre-Columbian ruins on the summit of Nevado Queva First Ascent Quewar was climbed by the Incas and evidence of such ascents is currently found on the summit in the form of a 80 square metre platform found for the first time in 1974 by Antonio Beorchia Nigris. The fi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pular (volcano)
Pular is a massive stratovolcano located in the Antofagasta Region of northern Chile, about 15 km west of the border with Argentina, which in this area is a straight line between the summits of Socompa volcano and ''Cerro del Rincón''. Pular, along with '' Cerro Pajonales'', forms a high volcanic ridge, which runs in a generally north-east to south-west direction for . Southward, following the same direction as the ridge, lies Socompa volcano. The ridge's crest forms a drainage divide between Salar de Atacama basin and ''Salar de Pular'' basin. This latter is a bowl-shaped basin enclosed on the east by Aracar volcano. In the Kunza language Pular means "The Eyebrow"Humberto Barrera, "Cerro Pular", ''American Alpine Journal'', 1974, p. 194. Available aAAJ Online (PDF). and the volcano was a site of Inka cultural activity. Geology and geomorphology The Andes of northern Chile are formed by a number of volcanoes, some of which reach elevation. During winter they are co ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pichu Pichu
Pichu Pichu or Picchu Picchu is an inactive eroded volcano in the Andes of Peru. It is located in the Arequipa Region, Arequipa Province, on the border of Pocsi and Tarucani districts.escale.minedu.gob.pe – UGEL map of the Arequipa Province (Arequipa Region) Pichu Pichu reaches a height of and is part of Salinas and Aguada Blanca National Reserve. Name The name possibly stems from Quechua ''pikchu'' pyramid; mountain or prominence with a broad base which ends in sharp peaks. The duplication is probably meant to imply that the mountain has multiple peaks. Location Pichu Pichu, together with Nevado Chachani and El Misti, border the city of Arequipa towards the northeast. These volcanoes are found southwest of the principal Cordillera Occidental in the region. Geography and geology Pichu Pichu is an extinct volcano with the form of a ridge which drops off steeply on its western side. The volcano features four different heavily eroded craters. It was active 6.7 million ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Paniri
Paniri (Aymara for "he who comes, visits") is a stratovolcano located in El Loa Province, Antofagasta Region, Chile, and near the border with Bolivia. To its northwest lie the twin volcanoes San Pedro and San Pablo, and to its southeast lies Cerro del León, from which it is separated by the huge '' Chao'' lava dome. The volcano features lava flows, which are well preserved on the south-southwest flanks, and a scoria cone on its summit. The volcano has three craters. Paniri also shows evidence of glacier activity on its southeastern slope. The volcano developed in several different stages with substages; the first stage formed a shield like volcano with most of its volume, the later ones formed the cone and "main edifice". One date obtained from the youngest stage is 150,000 years ago, with an uncertainty of 6,000 years. Once considered of Holocene or Pleistocene age, Paniri was later determined that to be of Pleistocene age. Paniri is part of the San Pedro-Linzor volcanic ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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