Monte Carlisle
Carlisle
Stratovulcano · United States · 1620 m

- Tipo
- Stratovulcano
- Paese
- United States
- Regione
- Nord America / Aleutian Ridge Volcanic Arc
- Altitudine
- 1620 m
- Coordinate
- 52.894, -170.054
- Ultima eruzione
- 1828
- Contesto tettonico
- Subduction zone / Intermediate crust (15-25 km)
- Forma vulcanica
- Composite
- Roccia principale
- Andesite / Basaltic Andesite
Sintesi geologica
Carlisle Island is a steep-sided, conical stratovolcano across the Carlisle Pass strait from Mount Cleveland. Radar images suggest that this uninhabited, 7-km-wide island may contain two closely spaced volcanic cones (Myers, in Wood and Kienle 1990). Like nearby Herbert volcano, no geologic studies have been conducted on the volcano. Eruptions have been reported since the 18th century, but are very poorly documented. A variety of names was attached to Carlisle on early hydrographic maps, and Miller et al. (1998) noted that some 18th and 19th century eruptions reported at the closely spaced volcanoes of the "Islands of the Four Mountains" area could refer to Carlisle as well as Cleveland, Uliaga, or Kagamil volcanoes.
Sintesi da Wikipedia
Riassunto in ingleseMount Carlisle is a stratovolcano in Alaska which forms part of the 5 mile (8 km) wide Carlisle Island, one of the Islands of Four Mountains which, in turn, form part of the central Aleutian Islands.
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Storia delle eruzioni
Cronologia dettagliata
- 1987VEI ?Stima geologica1987-11-16 – In corso
- 1838VEI ?Stima geologica1838-07-02 – In corso
- 1828VEI ?Osservata1828-07-02 – In corso
- 1774VEI ?Osservata1774-07-02 – In corso
Link esterni
⚠ Solo a scopo informativo. Non adatto a situazioni di emergenza.