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Kagamil Island

Kagamil

Estratovolcán · United States · 893 m

The southern half of 5 x 10 km Kagamil Island in the NE part of the "Islands of Four Mountains" group contains two postglacial cones with small summit craters. The larger cone (center) is seen here from the SW and is located at the SE end. Hot springs and fumaroles occur near the SE coast.
The southern half of 5 x 10 km Kagamil Island in the NE part of the "Islands of Four Mountains" group contains two postglacial cones with small summit craters. The larger cone (center) is seen here from the SW and is located at the SE end. Hot springs and fumaroles occur near the SE coast. · Foto: Photo by G. Vernon Byrd, 1972 (U.S. Fish and Wildlife Service, courtesy of Alaska Volcano Observatory). · Wikimedia Commons
Tipo
Estratovolcán
País
United States
Región
North America Volcanic Regions / Aleutian Ridge Volcanic Arc
Altitud
893 m
Coordenadas
52.974, -169.720
Última erupción
1929
Contexto tectónico
Subduction zone / Intermediate crust (15-25 km)
Forma volcánica
Composite
Roca principal
No Data (checked)
Resumen geológico

Kagamil Island lies near the NE end of the Islands of the Four Mountains archipelago in the central Aleutians, between Chuginadak and Uliaga Islands. The southern half of the 5 x 10 km island contains two undissected cones of postglacial age with small summit craters. The larger cone is located at the SE end of the NNW-SSE-trending volcano. Arcuate ridges at the northern and southern ends of the island suggest a possible earlier caldera. Hot springs and fumaroles occur along a steaming beach at the SE coast. The early explorer Veniaminof (1840) indicated that Kagamil formerly "flamed and smoked," but the only eruptive report is of unspecified activity in 1929 (Coats 1950).

Historial de erupciones

Resumen (VEI en el tiempo)
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1929~1929 · 1 erupciones · VEI máx. ?19291929193019301930

Línea de tiempo detallada

  1. 1929VEI ?Observado
    1929-12 – En curso

Enlaces externos

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