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Mount Nasu

Nasudake

Estratovolcán · Japan · 1915 m

A line of hikers at the lower left walk along a trail below the summit of Chausudake, the active cone of the Nasudake volcanic complex. This volcano group consists of a N-S-trending cluster of cones and lava domes at the N end of the Kanto Plain. Chausudake is a young cone that formed about 16,000 years ago. Six eruptions took place in 1408-1410 CE, when the youngest summit lava dome formed; additional smaller phreatic eruptions have occurred since then.
A line of hikers at the lower left walk along a trail below the summit of Chausudake, the active cone of the Nasudake volcanic complex. This volcano group consists of a N-S-trending cluster of cones and lava domes at the N end of the Kanto Plain. Chausudake is a young cone that formed about 16,000 years ago. Six eruptions took place in 1408-1410 CE, when the youngest summit lava dome formed; additional smaller phreatic eruptions have occurred since then. · Foto: Photo by Yukio Hayakawa, 1994 (Gunma University). · Wikimedia Commons
Tipo
Estratovolcán
País
Japan
Región
Northwestern Pacific Volcanic Regions / Northeast Japan Volcanic Arc
Altitud
1915 m
Coordenadas
37.125, 139.963
Última erupción
1963
Contexto tectónico
Subduction zone / Continental crust (> 25 km)
Forma volcánica
Composite
Roca principal
Andesite / Basaltic Andesite
Resumen geológico

The Nasudake volcanic group consists of a N-S-trending cluster of stratovolcanoes and lava domes at the north end of the Kanto Plain. Volcanic activity dates back about 500,000 years. Growth of three large basaltic-to-dacitic stratovolcanoes, each lasting about 200,000 years, was followed by construction of three smaller andesitic stratovolcanoes, Asahidake, Futamatayama, and Chausudake. Activity during the last 55,000 years included the collapse of Asahidake volcano about 30-40,000 years ago, producing the massive Ofujisan debris-avalanche deposit, which covers a broad area SE of the volcano. The youngest volcano, Chausudake, began forming about 16,000 years ago. Six magmatic eruptions took place since then, the latest in 1408-1410 CE, when the Chausudake summit lava dome formed. These eruptions produced block-and-ash flows and concluded with the extrusion of lava flows. Smaller phreatic eruptions have occurred every few hundred years during the past 5,000 years.

Resumen de Wikipedia

Resumen en inglés

Mount Nasu is a group of complex volcanoes located in the northeast part of Nikkō National Park, Japan. The tallest peak is Sanbonyari Peak at a height of 1,916.9 m (6,289 ft). Mount Nasu is one of the 100 Famous Japanese Mountains.

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Historial de erupciones

Resumen (VEI en el tiempo)
Haga clic en una barra para ver erupciones individuales
8550 BCE~8200 BCE · 1 erupciones · VEI máx. 28200 BCE~7849 BCE · 1 erupciones · VEI máx. 36097 BCE~5747 BCE · 1 erupciones · VEI máx. 25747 BCE~5396 BCE · 1 erupciones · VEI máx. 34695 BCE~4345 BCE · 1 erupciones · VEI máx. 22242 BCE~1892 BCE · 1 erupciones · VEI máx. 21541 BCE~1191 BCE · 1 erupciones · VEI máx. 2840 BCE~490 BCE · 1 erupciones · VEI máx. 3490 BCE~140 BCE · 1 erupciones · VEI máx. 2211~561 · 2 erupciones · VEI máx. 31262~1613 · 4 erupciones · VEI máx. 31613~1963 · 6 erupciones · VEI máx. 18550 BCE6097 BCE3293 BCE840 BCE1613

Línea de tiempo detallada

  1. 1963VEI 1Estimación geológica
    1963-07-10 – 1963-07-11
    Chausu-dake
  2. 1963VEI 1Observado
    1963-11-20 – 1963-11-21
    Chausu-dake (west side)
  3. 1960VEI 1Observado
    1960-10-10 – En curso
    Chausu-dake (50 m north of 1953 vent)
  4. 1953VEI 1Observado
    1953-10-24 – 1953-10-29
    Chausu-dake (1881 crater)
  5. 1881VEI 1Observado
    1881-07-01 – En curso
    Chausu-dake (west and NW side of summit)
  6. 1846VEI 1Observado
    1846-08 – En curso
    Chausu-dake
  7. 1410VEI 3Observado
    1410-03-05 – En curso
    Chausu-dake
  8. 1408VEI 3Observado
    1408-02-24 – En curso
    Chausu-dake
  9. 1404VEI 3Observado
    1404-02-11 – En curso
    Chausu-dake
  10. 1397VEI 3Observado
    1397-02-17 – En curso
    Chausu-dake
  11. 330 (±200 años)VEI 2Estimación geológica
    330 – En curso
    Chausu-dake
  12. 250 (±200 años)VEI 3Estimación geológica
    250 – En curso
    Chausu-dake
  13. 250 a. C.VEI 2Estimación geológica
    BCE 250 – En curso
    Chausu-dake
  14. 700 a. C. (±200 años)VEI 3Estimación geológica
    BCE 700 – En curso
    Chausu-dake
  15. 1440 a. C. (±500 años)VEI 2Estimación geológica
    BCE 1440 – En curso
    Chausu-dake
  16. 2000 a. C. (±1450 años)VEI 2Estimación geológica
    BCE 2000 – En curso
    Chausu-dake
  17. 4350 a. C. (±950 años)VEI 2Estimación geológica
    BCE 4350 – En curso
    Chausu-dake
  18. 5550 a. C. (±500 años)VEI 3Estimación geológica
    BCE 5550 – En curso
    Chausu-dake
  19. 6050 a. C.VEI 2Estimación geológica
    BCE 6050 – En curso
    Chausu-dake
  20. 7850 a. C.VEI 3Estimación geológica
    BCE 7850 – En curso
    Chausu-dake
  21. 8550 a. C. (±1500 años)VEI 2Estimación geológica
    BCE 8550 – En curso
    Chausu-dake

Enlaces externos

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