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Lago Shikotsu

Shikotsu

Caldera · Japan · 1320 m

Tarumai volcano was constructed on the SE rim of the 13 x 15 km Shikotsu caldera. The summit has a small 1.5-km-wide caldera that formed during eruptions in 1667 and 1739 CE. It contains a flat-topped summit lava dome that was extruded in 1909. Two other Holocene post-caldera volcanoes occur at Shikotsu, Fuppushi (adjacent to Tarumai) and Eniwa, on the opposite side of the caldera.
Tarumai volcano was constructed on the SE rim of the 13 x 15 km Shikotsu caldera. The summit has a small 1.5-km-wide caldera that formed during eruptions in 1667 and 1739 CE. It contains a flat-topped summit lava dome that was extruded in 1909. Two other Holocene post-caldera volcanoes occur at Shikotsu, Fuppushi (adjacent to Tarumai) and Eniwa, on the opposite side of the caldera. · Foto: Photo by Ichio Moriya (Kanazawa University). · Wikimedia Commons
Tipo
Caldera
País
Japan
Región
Northwestern Pacific Volcanic Regions / Northeast Japan Volcanic Arc
Altitud
1320 m
Coordenadas
42.688, 141.380
Última erupción
1981
Contexto tectónico
Subduction zone / Continental crust (> 25 km)
Forma volcánica
Caldera
Roca principal
Andesite / Basaltic Andesite
Resumen geológico

The 13 x 15 km Shikotsu caldera, largely filled by the waters of Lake Shikotsu, was formed during one of Hokkaido's largest Quaternary eruptions about 31-34,000 years ago. The small andesitic Tarumaesan stratovolcano was then constructed on its SE rim and has been frequently active in historical time. Pyroclastic-flow deposits from Tarumaesan extend nearly to the Pacific coast. Two other Holocene post-caldera volcanoes, Fuppushidake (adjacent to Tarumaesan) and Eniwadake (on the opposite side of the caldera), occur on a line trending NW from Tarumaesan, and were constructed just inside the caldera rim. Minor eruptions took place from the summit of Eniwadake as late as the 17th century. The summit of Tarumaesan contains a small 1.5-km-wide caldera formed during two of Hokkaido's largest historical eruptions, in 1667 and 1739. Tarumaesan is now capped by a flat-topped summit lava dome that formed in 1909.

Resumen de Wikipedia

El lago Shikotsu es un lago de cráter ubicado en Chitose, Hokkaidō, Japón. Es parte del parque nacional Shikotsu-Toya.

Wikipedia · CC BY-SA · Leer artículo completo →

Historial de erupciones

Resumen (VEI en el tiempo)
Haga clic en una barra para ver erupciones individuales
6950 BCE~6652 BCE · 1 erupciones · VEI máx. 5698 BCE~401 BCE · 1 erupciones · VEI máx. 5103 BCE~195 · 2 erupciones · VEI máx. 31386~1683 · 3 erupciones · VEI máx. 51683~1981 · 36 erupciones · VEI máx. 56950 BCE4866 BCE2484 BCE401 BCE1683

Línea de tiempo detallada

  1. 1981VEI 1Observado
    1981-02-27 – 1981-02-27
    Tarumai
  2. 1978VEI 1Observado
    1978-05-14 – 1978-05-17
    Tarumai (SE foot of summit dome)
  3. 1978VEI 1Observado
    1978-12-12 – 1979-05-11
    Tarumai (SE foot of summit dome)
  4. 1954VEI 1Observado
    1954-05-02 – 1954-05-02
    Tarumai
  5. 1954VEI 1Observado
    1954-11-19 – 1955-02-14
    Tarumai
  6. 1953VEI 1Observado
    1953-09-14 – 1953-09-14
    Tarumai
  7. 1951VEI 2Observado
    1951-01-29 – 1951-01-29
    Tarumai
  8. 1951VEI 2Observado
    1951-07-28 – 1951-07-28
    Tarumai
  9. 1947VEI 1Observado
    1947-10-15 – 1947-10-15
    Tarumai
  10. 1944VEI 1Observado
    1944-07-02 – 1944-07-02
    Tarumai
  11. 1936VEI 1Observado
    1936-04-19 – 1936-04-19
    Tarumai
  12. 1936VEI 1Observado
    1936-11-15 – 1936-11-26
    Tarumai
  13. 1933VEI 2Observado
    1933-12-01 – 1933-12-14
    Tarumai (east-west summit fissure)
  14. 1931VEI 1Observado
    1931-10-11 – 1931-10-24
    Tarumai
  15. 1928VEI 2Observado
    1928-01-07 – 1928-01-07
    Tarumai
  16. 1928VEI 1Observado
    1928-09-06 – 1929-02-10
    Tarumai
  17. 1926VEI 2Observado
    1926-10-19 – 1926-10-30
    Tarumai
  18. 1923VEI 1Observado
    1923-02 – 1923-08-23
    Tarumai
  19. 1921VEI 1Observado
    1921-07-06 – 1921-07-06
    Tarumai
  20. 1920VEI 1Observado
    1920-07-17 – 1920-07-23
    Tarumai
  21. 1919VEI 2Observado
    1919-05-04 – 1919-05-04
    Tarumai
  22. 1918VEI 1Observado
    1918-06-13 – 1918-07-31
    Tarumai
  23. 1917VEI 2Observado
    1917-04-30 – 1917-05-12
    Tarumai (east-west summit fissure)
  24. 1909VEI 3Observado
    1909-01-11 – 1909-04-22
    Tarumai
  25. 1894VEI 2Observado
    1894-02-08 – 1894-02-08
    Tarumai
  26. 1894VEI 2Observado
    1894-08-17 – 1894-08-17
    Tarumai
  27. 1887VEI 2Observado
    1887-09-03 – 1887-10-08
    Tarumai
  28. 1886VEI 2Observado
    1886-04-13 – 1886-04-28
    Tarumai
  29. 1885VEI 2Observado
    1885-01-04 – 1885-03-26
    Tarumai
  30. 1883VEI 2Observado
    1883-10-07 – 1883-11-05
    Tarumai
  31. 1874VEI 3Observado
    1874-02-08 – 1874-02-16
    Tarumai
  32. 1871VEI 2Estimación geológica
    1871-12-25 – 1871-12-28
    Tarumai
  33. 1867VEI 2Observado
    1867-09-08 – En curso
    Tarumai
  34. 1804VEI 3Observado
    1804 – 1817
    Tarumai
  35. 1739VEI 5Observado
    1739-08-19 – 1739-08-31
    Tarumai
  36. 1707 (±30 años)VEI 2Estimación geológica
    1707 – En curso
    Eniwa (crater 3)
  37. 1667VEI 5Observado
    1667-09-23 – 1667-09-26
    Tarumai
  38. 1550 (±75 años)VEI 2Estimación geológica
    1550 – En curso
    Eniwa (crater 2)
  39. 1500 (±150 años)VEI 2Estimación geológica
    1500 – En curso
    Eniwa (crater 1)
  40. 50 a. C.VEI 3Estimación geológica
    BCE 50 – En curso
    Tarumai
  41. 100 a. C. (±100 años)VEI 2Estimación geológica
    BCE 100 – En curso
    Eniwa volcano (east side of summit)
  42. 550 a. C.VEI 5Estimación geológica
    BCE 550 – En curso
    Tarumai
  43. 6950 a. C.VEI 5Estimación geológica
    BCE 6950 – En curso
    Tarumai

Enlaces externos

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