Английская Википедия:Ampato

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Шаблон:Good article Шаблон:Short description Шаблон:Infobox mountain Ampato (possibly from Quechua hamp'atu or from Aymara jamp'atu, both meaning "frog") is a dormant Шаблон:Convert stratovolcano in the Andes of southern Peru. It lies about Шаблон:Convert northwest of Arequipa and is part of a north-south chain that includes the volcanoes Hualca Hualca and Sabancaya, the last of which has been historically active.

Ampato consists of three volcanic cones, which lie on top of an older eroded volcanic edifice. They were formed sequentially by extrusion of lava flows, but Ampato has also had explosive eruptions which have deposited ash, lapilli and pumice in the surrounding landscape. One young lava flow has been dated to 17,000 ± 6,000 years before present, but a summit lava dome is even younger, and Holocene ash layers in surrounding peat bogs may testify to the occurrence of recent eruptions.

The present-day volcano is covered by an ice cap, and during the last glacial maximum glaciers advanced to low altitudes. In 1995, an Inca mummy known as Mummy Juanita was discovered on Ampato by Johan Reinhard; it had been offered as a human sacrifice more than six hundred years earlier on the mountain.

Geography and geomorphology

Ampato lies south of the Colca Canyon and at the southern end of a chain of volcanoes formed by Hualca Hualca and Sabancaya,Шаблон:Sfn the last of which has been historically active.Шаблон:Sfn Clockwise from northeast the towns of Colihuiri, Cajamarcana, Sallalli, Japo, Baylillas, Corinta and Collpa surround the volcano;Шаблон:Sfn the city of Arequipa lies Шаблон:Convert to the southeast.Шаблон:Sfn

Ampato is part of the Central Volcanic Zone of the Andes,Шаблон:Sfn which in Peru manifests itself as several dozen Pleistocene volcanoes, some of which erupted in historical time including El Misti, Huaynaputina, Sabancaya and Ubinas. The largest historical eruption of the Andes took place at Huaynaputina.Шаблон:Sfn Other volcanoes in the Peruvian Central Volcanic Zone are Sara Sara, Solimana, Coropuna, Andagua volcanic field-Huambo volcanic field, Chachani, Ticsani, Tutupaca, Yucamane, Purupuruni and Casiri.Шаблон:Sfn

Файл:Ampato.JPG

Ampato seen from west

The volcano Ampato consists of three individual steep-sided cones which rise from a gentle glacially eroded foot. These three cones are lined up in southwest-northeast direction and the highest one reaches an elevation of Шаблон:ConvertШаблон:Sfn or Шаблон:Convert.Шаблон:Sfn Ampato is one of the highest volcanoes in the Central Volcanic ZoneШаблон:Sfn and the 35th highest summit in the Andes.Шаблон:Sfn The volume of the edifice is about Шаблон:Convert, it covers an area of about Шаблон:Convert.Шаблон:Sfn

The summit of the volcano is covered with an ice cap,Шаблон:Sfn and the edifice is incised by cirques and glacial valleys.Шаблон:Sfn The volcano is surrounded by three sets of moraines, the lowermost one at Шаблон:Convert elevation has been attributed to the last glacial maximum between 25,000-17,000 years ago, the middle one between Шаблон:Convert to a late readvance at the Pleistocene-Holocene epoch boundary and the higher ones above Шаблон:Convert to Holocene advances.Шаблон:Sfn

Geology

Off the western coast of South America, the Nazca Plate subducts beneath the South America PlateШаблон:Sfn at a rate of Шаблон:Convert.Шаблон:Sfn This subduction process is responsible for volcanism of the Central Volcanic Zone (CVZ)Шаблон:SfnШаблон:Sfn in Peru, Bolivia and Chile.Шаблон:Sfn The CVZ is one of the four volcanic belts in the Andean Volcanic Belt; the others are the Northern Volcanic Zone, the Southern Volcanic Zone and the Austral Volcanic Zone.Шаблон:Sfn The subduction started during the Jurassic period after the opening of the southern Atlantic Ocean, which triggered the onset of subduction of the Nazca Plate.Шаблон:Sfn

Volcanic arc-associated volcanism originally occurred within the Cordillera de la Costa in the Jurassic, but later it migrated resulting in the emplacement of the Tacaza and Toquepala groups and finally the Neogene Barroso group. The present-day volcanic arc is situated in the area of the Barroso group but has a narrower extent.Шаблон:Sfn The pre-volcanic basement consists of 1.9-1.0 billion year old rocks of the "Arequipa Massif", which consists of gneiss and granulite. They are covered by the Yura Group of the Mesozoic and the Mesozoic-Paleogene Tiabaya unit; the former consists of marine sediments and the latter of volcanic sediments intruded by plutons. The Tacaza and Barroso groups are emplaced on the sediments.Шаблон:Sfn

The basement beneath Ampato is formed by sedimentary and volcanic rocks of the Western Cordillera of Peru, and the rocks are of Mesozoic to Cenozoic age. A high plateau formed by ignimbrites and lavas of Pliocene to Miocene age rises above this basement. The terrain is cut by several different fault systems; one of these, the northeastward striking Sepina fault has been seismically active in the 20th and 21st centuries and seems to have controlled the development of the Ampato and Sabancaya volcanoes.Шаблон:Sfn

Composition

Ampato has erupted different volcanic rocks at different stages, with the earliest ones generating andesite and daciteШаблон:Sfn and which define a potassium-rich suite.Шаблон:Sfn The rocks contain amphibole, biotite, iron oxide, olivine, plagioclase, pyroxene and titanium oxide.Шаблон:Sfn

The magmas derive from mantle melts, but undergo additional differentiation processes before reaching the surface.Шаблон:Sfn Processes such as fractional crystallization, magma mixing and the absorption of crustal material by developing magmas have been invoked to explain the formation of the magmas of both Ampato and Sabancaya.Шаблон:Sfn Estimating the rate of magma production at Ampato is difficult owing to the uncertainties in determining the volume of the edifice and the duration of repose times between eruptions; on average it appears to be Шаблон:Convert. This rate does not consider "spurt"-like behaviour; volcano growth in fits and spurts has been observed at many other volcanic arc volcanoes.Шаблон:Sfn The rate is about one order of magnitude less than at neighbouring Sabancaya volcano.

Vegetation

The Western Cordillera features various climate zones, such as the quechua and suni zones. The vegetation that occurs at high altitudes is dominated by pioneer plants, with wetlands constituting additional centres of biodiversity.Шаблон:Sfn

Eruptive history

Growth of Ampato and Sabancaya commenced no earlier than 800,000 years ago.Шаблон:Sfn A Шаблон:Convert thick pile of andesitic lava flows with additional scoria and which crops out on the southern, southeastern and southwestern side of the Ampato volcano is the oldest volcanic stage of this volcano, with argon-argon dating yielding ages between 400,000 - 450,000 years before present.Шаблон:Sfn Above this formation, another pile of dacitic lava flows constructed the first Ampato edifice, which was about the same size as the present-day volcano. This pile ("Moldepampa stage") is about Шаблон:Convert thick in outcrops and was emplaced between 230,000 - 200,000 years before present.Шаблон:Sfn

After a pause in volcanic activityШаблон:Sfn and an intermediary stage ("Yanajaja stage"; one date obtained on this stage is 77,000 ± 4,000 years before present) that produced andesitic-dacitic lava flows which form a Шаблон:Convert thick unit on top of eroded remnants of the older Ampato volcanics,Шаблон:Sfn the andesitic northern cone formed as the first of the three present-day cones. The southern cone developed in several different stages; a first stage generated lava flows emanating from the summit;Шаблон:Sfn dating of two such flows has produced ages of 34,000 ± 8,000 and 40,000 ± 3,000 years before present. More than Шаблон:Convert of block-and-ash flows was erupted onto the eastern and western flanks of Ampato,Шаблон:Sfn and these flows consist of one andesitic and one dacitic formation; both appear to relate to a lava dome forming stage of volcanic activity. These block-and-ash flows are themselves covered on both the eastern and the western flanks by more thick lava flows, which make up a Шаблон:Convert thick unit and again consist of one andesitic and one dacitic unit; both units appear to have been erupted during the last glacial maximum.Шаблон:Sfn

Either during or before the last glacial maximum, Ampato erupted tephra during multiple explosive eruptions which today is preserved in two units, the Baylillas and the Corinta deposits. The first consists of lapilli, pumice and scoria and individual layers form thick sequences at large distances from the volcano, but are heavily eroded and thus difficult to measure in extent. Scoria flows identified on the southwestern-southern flanks of Ampato correspond to this unit. The dacitic Corinta deposits conversely were created during one large eruptionШаблон:Sfn which also left a crater on Ampato;Шаблон:Sfn it generated stratified Шаблон:Convert thick tephra deposits which contain pumice embedded within ash-rich layers,Шаблон:Sfn and it is probably also the source of the pumice flow deposits on the south-southwestern flank. These contain dacitic pumice fragments in a matrix rich in ash and have thicknesses of more than Шаблон:Convert in the few outcrops; much of this unit was likely eroded away by glacial activity.Шаблон:Sfn

Файл:AmpatoSabancaya.jpg

Aerial view of Ampato (back) from the northeast, with the active volcano Sabancaya in front.

The central cone grew in the gap between the northern and southern edifice and consists of lava flows again of andesitic to dacitic composition. These flows are together maximally Шаблон:Convert thick and one flow has been dated to 17,000 ± 6,000 years before present. A dacitic summit lava dome is not affected by glacial erosion and appears to be the youngest eruption product of Ampato.Шаблон:Sfn

Early Holocene (11,000 - 8,000 years before present) ash layers in peat bogs around the volcano may have originated either on Ampato or on Sabancaya.Шаблон:Sfn Late Holocene tephra layers dated to 1,790 ± 110, 2,050 ± 70 and 4,500 ± 125 likewise may have been erupted from Ampato, but Sabancaya is a more likely source for these ash layers.Шаблон:Sfn

Hazards

Presently, Ampato is considered to be a dormant volcano.Шаблон:Sfn Potential hazards from future eruptions at Ampato are lahars induced by melting of the icecap and sub-Plinian eruptions, considering the history of explosive eruptions at this volcano.Шаблон:Sfn

The Peruvian geological service has published a hazard map that describes danger areas of both Ampato and Sabancaya. Hazards mapped include both the fall of ash and the formation of lahars which can advance to distances of Шаблон:Convert in the southerly valleys of Ampato. Pyroclastic fallout primarily threatens the vicinity of the volcano but large eruptions can result in fallout over large areas around the volcanic complex.

Human history

A ceremonial platform was reported at elevations of Шаблон:Convert. Ampato was the site of human sacrifice during Inca times, around 1466 the Mummy Juanita was offered for sacrifice on the mountain, along with two other girls and a boy. The sacrifice took place on a platform on the summit of the volcano and was presumably intended to calm the mountain spirits during an eruption of the neighbouring volcano Sabancaya. The mummies were discovered in 1995 by Johan Reinhard and colleagues on the summit of the mountain.Шаблон:Sfn

Such sacrifices with children being the usual subjects are known as capacocha and the discoveries of their mummies on mountains in the Andes has gained them a lot of attention. The process served to tie the Inka empire more closely together, since children to be sacrificed were selected from the entire realm and the children adorned and their names remembered after the sacrifice.Шаблон:Sfn

See also

• Ananta

References

Sources

• Шаблон:Cite journal
• Шаблон:Cite journal
• Шаблон:Cite journal
• Шаблон:Cite journal
• Шаблон:Cite journal
• Шаблон:Cite journal

Further reading

• Reinhard, Johan The Ice Maiden: Inca Mummies, Mountain Gods, and Sacred Sites in the Andes. 2005, Washington, D.C.: National Geographic Society.
• Шаблон:Cite gvp
• Шаблон:Cite book
• Шаблон:Cite book (in Spanish; also includes volcanoes of Argentina, Bolivia, and Peru)
• Шаблон:Cite book

External links

• Ampato on Summitpost
• Шаблон:Cite thesis
• Шаблон:Cite thesis