Monte Carlisle
Carlisle
Estratovolcán · United States · 1620 m

- Tipo
- Estratovolcán
- País
- United States
- Región
- North America Volcanic Regions / Aleutian Ridge Volcanic Arc
- Altitud
- 1620 m
- Coordenadas
- 52.894, -170.054
- Última erupción
- 1828
- Contexto tectónico
- Subduction zone / Intermediate crust (15-25 km)
- Forma volcánica
- Composite
- Roca principal
- Andesite / Basaltic Andesite
Resumen geológico
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.
Resumen de Wikipedia
El monte Carlisle es un estratovolcán en Alaska que forma parte de la isla de Carlisle, una de las islas de los Cuatro Volcanes que mide 5 km y que, a su vez, forma parte de las islas Aleutianas centrales.
Wikipedia · CC BY-SA · Leer artículo completo →
Historial de erupciones
Línea de tiempo detallada
- 1987VEI ?Estimación geológica1987-11-16 – En curso
- 1838VEI ?Estimación geológica1838 – En curso
- 1828VEI ?Observado1828 – En curso
- 1774VEI ?Observado1774-07-02 – En curso
Enlaces externos
⚠ Solo como referencia. No apto para respuesta ante emergencias.