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Volcán Apoyeque

Apoyeque

칼데라 · Nicaragua · 518m

Apoyeque stratovolcano forms the large Chiltepe Peninsula in central Lake Managua.  A 2.8-km wide, 500-m-deep caldera truncates the volcano's summit, below and to the left of the airplane wing.  Laguna de Jiloa, the large lake in the foreground, lies immediately SE of Apoyeque.  The age of the latest eruption of Apoyeque is not known, but human footprints underlie pumice deposits thought to originate from Apoyeque volcano or a nearby vent beneath Lake Managua.  Momotombo volcano is visible in the distance to the NW across Lake Managua.
Apoyeque stratovolcano forms the large Chiltepe Peninsula in central Lake Managua. A 2.8-km wide, 500-m-deep caldera truncates the volcano's summit, below and to the left of the airplane wing. Laguna de Jiloa, the large lake in the foreground, lies immediately SE of Apoyeque. The age of the latest eruption of Apoyeque is not known, but human footprints underlie pumice deposits thought to originate from Apoyeque volcano or a nearby vent beneath Lake Managua. Momotombo volcano is visible in the distance to the NW across Lake Managua. · 사진: Photo by Jaime Incer, 1981. · Wikimedia Commons
화산 유형
칼데라
국가
Nicaragua
지역
Middle America-Caribbean Volcanic Regions / Central America Volcanic Arc
해발
518m
좌표
12.242, -86.342
마지막 분화
-50년
판구조 환경
Subduction zone / Continental crust (> 25 km)
화산 지형
Caldera
주요 암석
Dacite
지질학적 요약

The Apoyeque volcanic complex occupies the broad Chiltepe Peninsula, which extends into south-central Lake Managua. The peninsula is part of the Chiltepe pyroclastic shield volcano, one of three large ignimbrite shields on the Nicaraguan volcanic front. A 2.8-km wide, 400-m-deep, lake-filled caldera whose floor lies near sea level truncates the low Apoyeque edifice, which rises only about 500 m above the lake shore. The caldera was the source of a thick deposit of dacitic pumice that covers the surrounding area. The 2.5 x 3 km lake-filled Xiloá (Jiloá) maar is located immediately SE of Apoyeque. The Talpetatl lava dome was constructed between Laguna Xiloá and Lake Managua. Pumiceous pyroclastic flows from Laguna Xiloá were erupted about 6,100 years ago and overlie deposits of comparable age from the Masaya Plinian eruption.

Wikipedia 요약

영어 요약

Apoyeque is a pyroclastic shield, located in the Chiltepe Peninsula Natural Reserve in Nicaragua. It has a 2.8-km wide, 400-m-deep, lake-filled caldera.

Wikipedia · CC BY-SA · 전체 기사 보기

분화 이력

요약 (VEI 시계열)
막대를 클릭하면 개별 분화가 표시됩니다
4160 BCE~3964 BCE · 1건 · 최고 VEI 52594 BCE~2399 BCE · 1건 · 최고 VEI 51224 BCE~1029 BCE · 1건 · 최고 VEI 4246 BCE~50 BCE · 1건 · 최고 VEI 64160 BCE3181 BCE2203 BCE1224 BCE246 BCE

상세 타임라인

  1. 기원전 50년 (±100년)VEI 6지질학적 추정
    BCE 50 ~ 진행 중
    Apoyeque
  2. 기원전 1050년 (±1000년)VEI 4지질학적 추정
    BCE 1050 ~ 진행 중
  3. 기원전 2550년 (±1500년)VEI 5지질학적 추정
    BCE 2550 ~ 진행 중
    W Chiltepe Peninsula
  4. 기원전 4160년 (±30년)VEI 5지질학적 추정
    BCE 4160 ~ 진행 중
    Laguna Xiloá

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