Chile · Cono piroclástico
Volcán Reclus
Reclus
- Tipo
- Cono piroclástico
- Altitud
- 1403 m
- Última erupción
- 1908
- Tipo
- Cono piroclástico
- País
- Chile
- Región
- América del Sur / Austral Andean Volcanic Arc
- Altitud
- 1403 m
- Coordenadas
- -50.940, -73.580
- Última erupción
- 1908
- Contexto tectónico
- Zona de subducción / Corteza continental (> 25 km)
- Forma volcánica
- Compuesto
- Roca principal
- Dacita
Resumen geológico
Reclus, the source of several Patagonian Holocene tephra layers, was recognized to be an independent volcanic edifice in 1987. The volcano consists of a large dacitic pyroclastic cone with a crater about 1 km in diameter. As many as six tephra layers overlie a peat layer dated at 3,780 years before present. Research has also revealed evidence for eruptions in the 19th and early 20th centuries.
Resumen de Wikipedia
Resumen en inglésReclus, also written as Reclús, is a cinder cone and stratovolcano located in the Southern Patagonian Ice Field, Chile. Part of the Austral Volcanic Zone of the Andes, its summit rises 1,000 metres (3,300 ft) above sea level and is capped by a crater about 1 kilometre (0.62 mi) wide. Close to the volcano lies the Amalia Glacier, which is actively eroding Reclus.
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Historial de erupciones
4 registradasGlosarioLínea de tiempo detallada
- 1908 (±1 años)VEI 1Observado1908-07-02 – fin desconocido
- 1879VEI 2Observado1879-07-02 – fin desconocido
- 1869VEI 2Observado1869-07-02 – fin desconocido
- 1830 a. C.VEI ?Estimación geológica1830 a. C. – fin desconocido
Volcanes cercanos
Enlaces externos
⚠ Solo como referencia. No apto para respuesta ante emergencias.