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El Salvador · Estratovolcán

Cordillera de Apaneca-Ilamatepec

Apaneca Range

Tipo
Estratovolcán
Altitud
2028 m
Última erupción
Desconocido
Cordillera de Apaneca-Ilamatepec
Foto: Lee Siebert, Smithsonian Institution · Public domain · Wikimedia Commons
Tipo
Estratovolcán
País
El Salvador
Región
América Central y Caribe / Central America Volcanic Arc
Altitud
2028 m
Coordenadas
13.872, -89.742
Última erupción
Desconocido
Contexto tectónico
Zona de subducción / Corteza continental (> 25 km)
Forma volcánica
Compuesto
Roca principal
Basalto / Picrobasalto
Resumen geológico

The Apaneca Range (also known as the Cuyanausul Range) consists of a group of basaltic-to-andesitic Pleistocene and Holocene stratovolcanoes in western El Salvador between the Santa Ana complex and the Guatemala border. The Pleistocene dacitic-rhyolitic Concepción de Ataco caldera (5 x 3.5 km) lies at the W end of the complex, along with post-caldera late-Pleistocene to Holocene andesitic-dacitic lava domes. The post-caldera cones of Cerro el Aguila (the highest peak of the complex) and Cerro los Naranjos at the E end of the chain were mapped as Holocene by Weber and Weisemann (1978). Young craters on the basaltic Cerro Laguna Verde stratovolcano may also have been active during the Holocene. Numerous fumarole fields are located on the N flank of the range, and the Ahuachapán geothermal field has been producing since 1975. Several small hydrothermal explosions have occurred in historical time, including one in October 1990 at the Agua Shuca thermal area in which 26 people were killed.

Resumen de Wikipedia

Resumen en inglés

Cordillera de Apaneca is a volcanic mountain range in western El Salvador. It consists mainly of volcanoes. Ilamatepec volcano, one of the most active in the region, is a part of this range.

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Historial de erupciones

Glosario

Línea de tiempo detallada

No hay registros de erupciones disponibles.

Volcanes cercanos

Enlaces externos

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