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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
País
Nicaragua
Región
Middle America-Caribbean Volcanic Regions / Central America Volcanic Arc
Altitud
518 m
Coordenadas
12.242, -86.342
Última erupción
-50
Contexto tectónico
Subduction zone / Continental crust (> 25 km)
Forma volcánica
Caldera
Roca principal
Dacite
Resumen geológico

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.

Resumen de Wikipedia

Resumen en inglés

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 · Leer artículo completo

Historial de erupciones

Resumen (VEI en el tiempo)
Haga clic en una barra para ver erupciones individuales
4160 BCE~3964 BCE · 1 erupciones · VEI máx. 52594 BCE~2399 BCE · 1 erupciones · VEI máx. 51224 BCE~1029 BCE · 1 erupciones · VEI máx. 4246 BCE~50 BCE · 1 erupciones · VEI máx. 64160 BCE3181 BCE2203 BCE1224 BCE246 BCE

Línea de tiempo detallada

  1. 50 a. C. (±100 años)VEI 6Estimación geológica
    BCE 50 – En curso
    Apoyeque
  2. 1050 a. C. (±1000 años)VEI 4Estimación geológica
    BCE 1050 – En curso
  3. 2550 a. C. (±1500 años)VEI 5Estimación geológica
    BCE 2550 – En curso
    W Chiltepe Peninsula
  4. 4160 a. C. (±30 años)VEI 5Estimación geológica
    BCE 4160 – En curso
    Laguna Xiloá

Enlaces externos

⚠ Solo como referencia. No apto para respuesta ante emergencias.