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Estados Unidos · Estratovolcán

Mount Denison

Denison

Tipo
Estratovolcán
Altitud
2287 m
Última erupción
Desconocido
Mount Denison
Foto: Judy Fierstein (Alaska Volcano Observatory / U.S. Geological Survey) · Public domain · Wikimedia Commons
Tipo
Estratovolcán
País
Estados Unidos
Región
América del Norte / Alaska Peninsula Volcanic Arc
Altitud
2287 m
Coordenadas
58.418, -154.449
Última erupción
Desconocido
Contexto tectónico
Zona de subducción / Corteza continental (> 25 km)
Forma volcánica
Compuesto
Roca principal
Andesita / Andesita basáltica
Resumen geológico

Mount Denison lies near the head of the Serpent Tongue, Hook, and Hallo glaciers NE of Snowy volcano. This poorly known section of Katmai National Park contains a line of four closely spaced and mostly ice-covered volcanic peaks. Denison lies at the SW end of this chain, which also includes Steller, Kukak, and Devils Desk volcanoes. Orientation of lava flows and a thick cross-bedded tephra deposit suggest that a vent is located near Mount Denison (Swanson, in Wood and Kienle 1990). The precise age of the most recent activity at Denison is not known.

Resumen de Wikipedia

Resumen en inglés

Mount Denison is a stratovolcano and one of the highest peaks on the Alaska Peninsula. Discovered in 1923 by Harvard professor Kirtley Fletcher Mather, the mountain was named for the geologist's alma mater, Denison University. The mountain's connection to Denison also include its first climbers: all members of the first two ascent teams as well as the group that attempted in 1977 were either students, alumni, or faculty of the university.

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