Koryaksky
Estratovolcán · Russia · 3430 m

- Tipo
- Estratovolcán
- País
- Russia
- Región
- Northwestern Pacific Volcanic Regions / Eastern Kamchatka Volcanic Arc
- Altitud
- 3430 m
- Coordenadas
- 53.321, 158.712
- Última erupción
- 2009
- Contexto tectónico
- Subduction zone / Continental crust (> 25 km)
- Forma volcánica
- Composite
- Roca principal
- Andesite / Basaltic Andesite
Resumen geológico
The large symmetrical Koryaksky stratovolcano is the most prominent landmark of the NW-trending Avachinskaya volcano group, which towers above Kamchatka's largest city, Petropavlovsk. Erosion has produced a ribbed surface on the eastern flanks of the 3430-m-high volcano; the youngest lava flows are found on the upper W flank and below SE-flank cinder cones. Extensive Holocene lava fields on the western flank were primarily fed by summit vents; those on the SW flank originated from flank vents. Lahars associated with a period of lava effusion from south- and SW-flank fissure vents about 3900-3500 years ago reached Avacha Bay. Only a few moderate explosive eruptions have occurred during historical time, but no strong explosive eruptions have been documented during the Holocene. Koryaksky's first historical eruption, in 1895, also produced a lava flow.
Resumen de Wikipedia
El Koriakski, también llamado Koriaka, Koryaksky, Koriátzkaia, Korjaka, Korjazkij, Koryaka, Koryákskaya sopka, Koriákskaya sopka, Stréloshnaia sopka o también Streloschnaja,, es un volcán de Rusia situado en el sur de la península de Kamchatka, en el krai del mismo nombre.
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Historial de erupciones
Línea de tiempo detallada
- 2008VEI 2Observado2008-12-23 – 2009-08-27Upper NW flank (3000 m)
- 1956VEI 3Observado1956-12-16 – 1957-06-16Summit and upper NW flank (3000 m)
- 1926VEI 1Observado1926-12-22 – 1926-12-22
- 1890 (±3 años)VEI 1Observado1890 – En cursoUpper SW flank
- 1550 a. C.VEI ?Estimación geológicaBCE 1550 – En cursoSouth and SW flanks
- 1950 a. C. (±300 años)VEI ?Estimación geológicaBCE 1950 – En cursoSouth and SW flanks
- 5050 a. C.VEI ?Estimación geológicaBCE 5050 – En curso
Enlaces externos
⚠ Solo como referencia. No apto para respuesta ante emergencias.