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Iōtō

Ioto

Caldera · Japan · 169 m

The discolored water seen here is from the September 2001 Ioto submarine eruption, with the vent marked by the yellow arrow. The island is located within a 9-km-wide submarine caldera and narrows toward its SW tip, where the Suribachiyama cone is located. Numerous phreatic eruptions and uplift over at least the past 700 years has accompanied resurgent doming of the caldera.
The discolored water seen here is from the September 2001 Ioto submarine eruption, with the vent marked by the yellow arrow. The island is located within a 9-km-wide submarine caldera and narrows toward its SW tip, where the Suribachiyama cone is located. Numerous phreatic eruptions and uplift over at least the past 700 years has accompanied resurgent doming of the caldera. · Foto: Photo by Nakahori, 2001 (Japan Meteorological Agency, published in the Bulletin of the Global Volcanism Network). · Wikimedia Commons
Tipo
Caldera
País
Japan
Región
Northwestern Pacific Volcanic Regions / Ogasawara Volcanic Arc
Altitud
169 m
Coordenadas
24.751, 141.289
Última erupción
2025
Contexto tectónico
Subduction zone / Crustal thickness unknown
Forma volcánica
Caldera
Roca principal
Trachyandesite / Basaltic Trachyandesite
Resumen geológico

Ioto, in the Volcano Islands of Japan, lies within a 9-km-wide submarine caldera. The volcano is also known as Ogasawara-Iojima to distinguish it from several other "Sulfur Island" volcanoes in Japan. The triangular, low-elevation, 8-km-long island narrows toward its SW tip and has produced trachyandesitic and trachytic rocks that are more alkalic than those of other volcanoes in this arc. The island has undergone uplift for at least the past 700 years, accompanying resurgent doming of the caldera; a shoreline landed upon by Captain Cook's surveying crew in 1779 is now 40 m above sea level. The Motoyama plateau on the NE half of the island consists of submarine tuffs overlain by coral deposits and forms the island's high point. Many fumaroles are oriented along a NE-SW zone cutting through Motoyama. Numerous recorded phreatic eruptions, many from vents on the W and NW sides of the island, have accompanied the uplift.

Resumen de Wikipedia

Iōtō o Iōjima o Iwo Tō es una isla japonesa de origen volcánico que forma parte de las islas Vulcano, localizada a aproximadamente 1200 km al sur de Tokio. Administrativamente forma parte de la subprefectura de Ogasawara en Tokio.

Wikipedia · CC BY-SA · Leer artículo completo →

Historial de erupciones

Resumen (VEI en el tiempo)
Haga clic en una barra para ver erupciones individuales
850 BCE~658 BCE · 1 erupciones · VEI máx. ?1833~2025 · 32 erupciones · VEI máx. 1850 BCE83 BCE49212581833

Línea de tiempo detallada

  1. 2025VEI 1Observado
    2025-09-01 – 2025-09-02
  2. 2023VEI 1Observado
    2023-10-18 – 2024-03-16
  3. 2022VEI 1Observado
    2022-07-11 – 2022-12-11
    Off SE coast
  4. 2021VEI 1Observado
    2021-08-12 – 2021-11-24
    Off SE coast
  5. 2020VEI 1Observado
    2020-12-28 – 2021-04-05
    Asodai Sinkhole
  6. 2018VEI 1Observado
    2018-09-08 – 2018-09-14
    Off the S coast
  7. 2016VEI 1Observado
    2016-08-31 – 2016-09-01
    Asodai Sinkhole
  8. 2015VEI 1Observado
    2015-08-07 – 2015-08-07
    Kianohana Beach (N part of the island)
  9. 2013VEI 0Observado
    2013-08-21 – 2013-08-30
    Off the NE coast
  10. 2012VEI 1Observado
    2012-02-10 – 2012-07-09
    Asodai
  11. 2012VEI 1Observado
    2012-12-01 – 2013-04-11
    Asodai
  12. 2010VEI 1Observado
    2010-06-19 – 2010-06-19
  13. 2004VEI 1Estimación geológica
    2004-06-06 – 2004-06-08
    Asodai area
  14. 2001VEI 1Observado
    2001-09-21 – 2001-10-23
    Off SE coast and Idogahama (NW coast)
  15. 1999VEI 1Observado
    1999-09-10 – 1999-09-10
    Asodai area
  16. 1994VEI 1Observado
    1994-08-22 – 1994-08-22
    NE side
  17. 1993VEI 1Estimación geológica
    1993-10-27 – 1993-11-16
    Asodai area and NE of Iwo-jima
  18. 1982VEI 1Observado
    1982-03-09 – 1982-03-10
    NW side (Idogahama beach)
  19. 1982VEI 1Observado
    1982-11-28 – 1982-12-16
    West side (Asodai)
  20. 1980VEI 1Observado
    1980-03-13 – 1980-03-13
    Kitanohara
  21. 1978VEI 1Observado
    1978-12-11 – 1978-12-11
    West side (Asodai)
  22. 1976VEI 1Observado
    1976-01-16 – En curso
    West side (Asodai)
  23. 1974VEI 0Estimación geológica
    1974-01-16 – 1974-02-02
    NW of Iwo-jima (Kaiseinishinoba)
  24. 1969VEI 1Observado
    1969-01-12 – 1969-01-21
    West side (Asodai)
  25. 1969VEI 1Observado
    1969-12-01 – 1969-12-01
  26. 1967VEI 1Observado
    1967-12-23 – 1967-12-23
    West side (Asodai)
  27. 1957VEI 1Observado
    1957-03-28 – 1957-03-28
    Chidoriga-hara
  28. 1944VEI 1Observado
    1944-12 – En curso
    North and west sides near the coast
  29. 1935VEI 1Observado
    1935 – En curso
    SW side at Chidoriga-hara
  30. 1930VEI 1Observado
    1930 – En curso
    NW side near the coast
  31. 1922VEI 1Observado
    1922-07 – En curso
    West side (Asodai)
  32. 1889VEI 1Observado
    1889-12-31 – En curso
    Chidoriga-ana
  33. 850 a. C. (±50 años)VEI ?Estimación geológica
    BCE 850 – En curso
    Motoyama

Enlaces externos

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