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파리나코타산

Parinacota

성층화산 · Chile-Bolivia · 6336m

Glacier-clad Volcán Parinacota rises to the NE above Laguna Chungará near the Chile-Bolivia border.  The lake was formed when collapse of Parinacota about 8000 years ago produced a 6 cu km debris avalanche that traveled 22 km to the west and blocked drainages.  Subsequent eruptions constructed the 6348-m-high symmetrical stratovolcano, which towers above late-Pleistocene andesitic-to-rhyolitic lava domes and flows in the middle ground.
Glacier-clad Volcán Parinacota rises to the NE above Laguna Chungará near the Chile-Bolivia border. The lake was formed when collapse of Parinacota about 8000 years ago produced a 6 cu km debris avalanche that traveled 22 km to the west and blocked drainages. Subsequent eruptions constructed the 6348-m-high symmetrical stratovolcano, which towers above late-Pleistocene andesitic-to-rhyolitic lava domes and flows in the middle ground. · 사진: Photo by Lee Siebert, 2004 (Smithsonian Institution). · Wikimedia Commons
화산 유형
성층화산
국가
Chile-Bolivia
지역
남아메리카 / Central Andean Volcanic Arc
해발
6336m
좌표
-18.166, -69.142
마지막 분화
290년
판구조 환경
Subduction zone / Continental crust (> 25 km)
화산 지형
Composite
주요 암석
Andesite / Basaltic Andesite
지질학적 요약

The symmetrical Volcán Parinacota is the southernmost and youngest of a pair of volcanoes forming the Nevados de Payachata group along the Chile-Bolivia border. The dominantly Pleistocene Pomerape volcano towers above a low saddle to the NE. Collapse of Parinacota about 8,000 years ago produced a 6 km3 debris avalanche that traveled 22 km W and blocked drainages, forming Lake Chungará. Holocene eruptive activity has subsequently reconstructed the stratovolcano, which contains a pristine, 300-m-wide summit crater and youthful lava flows on the W flanks. Although no historical eruptions are known, Helium surface-exposure dates have been obtained for eruptions during the past two thousand years both from the main cone and the Ajata group of satellite cones and lava flows on the S and SW flanks.

Wikipedia 요약

영어 요약

Parinacota, Parina Quta or Parinaquta is a dormant stratovolcano on the border of Bolivia and Chile. Together with Pomerape it forms the Nevados de Payachata volcanic chain. Part of the Central Volcanic Zone of the Andes, its summit reaches an elevation of 6,380 metres (20,930 ft) above sea level. The symmetrical cone is capped by a summit crater with widths of 1 kilometre (0.62 mi) or 1,000 metres (3,300 ft). Farther down on the southern slopes lie three parasitic centres known as the Ajata cones. These cones have generated lava flows. The volcano overlies a platform formed by lava domes and andesitic lava flows.

Wikipedia · CC BY-SA · 전체 기사 보기

분화 이력

요약 (VEI 시계열)
막대를 클릭하면 개별 분화가 표시됩니다
7950 BCE~7675 BCE · 1건 · 최고 VEI ?6027 BCE~5753 BCE · 1건 · 최고 VEI ?4379 BCE~4105 BCE · 1건 · 최고 VEI ?1358 BCE~1083 BCE · 1건 · 최고 VEI ?15~290 · 2건 · 최고 VEI 47950 BCE6027 BCE3830 BCE1907 BCE15

상세 타임라인

  1. 290년 (±300년)VEI 4지질학적 추정
    290 ~ 진행 중
    Parinacota 3 edifice
  2. 90년 (±50년)VEI ?지질학적 추정
    90 ~ 진행 중
    South flank (upper Volcanes de Ajata)
  3. 기원전 1100년 (±500년)VEI ?지질학적 추정
    BCE 1100 ~ 진행 중
    South flank (lower Volcanes de Ajata)
  4. 기원전 4320년 (±1200년)VEI ?지질학적 추정
    BCE 4320 ~ 진행 중
    South flank (lower Volcanes de Ajata)
  5. 기원전 5840년 (±50년)VEI ?지질학적 추정
    BCE 5840 ~ 진행 중
  6. 기원전 7950년VEI ?지질학적 추정
    BCE 7950 ~ 진행 중
    Ajata

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