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Volcán Apoyeque

Apoyeque

Caldera · Nicaragua · 518 m

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. · Foto: Photo by Jaime Incer, 1981. · Wikimedia Commons
Tipo
Caldera
Paese
Nicaragua
Regione
Middle America-Caribbean Volcanic Regions / Central America Volcanic Arc
Altitudine
518 m
Coordinate
12.242, -86.342
Ultima eruzione
-50
Contesto tettonico
Subduction zone / Continental crust (> 25 km)
Forma vulcanica
Caldera
Roccia principale
Dacite
Sintesi geologica

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.

Sintesi da Wikipedia

Riassunto in inglese

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 · Leggi l'articolo completo

Storia delle eruzioni

Riepilogo (VEI nel tempo)
Fai clic su una barra per vedere le singole eruzioni
4160 BCE~3964 BCE · 1 eruzioni · VEI max. 52594 BCE~2399 BCE · 1 eruzioni · VEI max. 51224 BCE~1029 BCE · 1 eruzioni · VEI max. 4246 BCE~50 BCE · 1 eruzioni · VEI max. 64160 BCE3181 BCE2203 BCE1224 BCE246 BCE

Cronologia dettagliata

  1. 50 a.C. (±100 anni)VEI 6Stima geologica
    BCE 50 – In corso
    Apoyeque
  2. 1050 a.C. (±1000 anni)VEI 4Stima geologica
    BCE 1050 – In corso
  3. 2550 a.C. (±1500 anni)VEI 5Stima geologica
    BCE 2550 – In corso
    W Chiltepe Peninsula
  4. 4160 a.C. (±30 anni)VEI 5Stima geologica
    BCE 4160 – In corso
    Laguna Xiloá

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