Cile · Cono piroclastico
Reclus
- Tipo
- Cono piroclastico
- Altitudine
- 1403 m
- Ultima eruzione
- 1908
- Tipo
- Cono piroclastico
- Paese
- Cile
- Regione
- Sud America / Austral Andean Volcanic Arc
- Altitudine
- 1403 m
- Coordinate
- -50.940, -73.580
- Ultima eruzione
- 1908
- Contesto tettonico
- Zona di subduzione / Crosta continentale (> 25 km)
- Forma vulcanica
- Composito
- Roccia principale
- Dacite
Sintesi geologica
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.
Sintesi da Wikipedia
Riassunto in ingleseReclus, 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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Storia delle eruzioni
4 registrateGlossarioCronologia dettagliata
- 1908 (±1 anni)VEI 1Osservata1908-07-02 – fine sconosciuta
- 1879VEI 2Osservata1879-07-02 – fine sconosciuta
- 1869VEI 2Osservata1869-07-02 – fine sconosciuta
- 1830 a.C.VEI ?Stima geologica1830 a.C. – fine sconosciuta
Vulcani nelle vicinanze
Link esterni
⚠ Solo a scopo informativo. Non adatto a situazioni di emergenza.