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Lago Kussharo

Kussharo

Caldera · Japan · 574 m

The 20 x 26 km Kussharo caldera, seen here from its western rim, is the largest of a cluster of calderas in NE Hokkaido. It formed around 30,000 years ago. Nakajima, a Holocene post-caldera lava dome complex, forms the large island to the left that fills much of the western half of the caldera. Atosanupuri is located near the center of the caldera, east of the lake.
The 20 x 26 km Kussharo caldera, seen here from its western rim, is the largest of a cluster of calderas in NE Hokkaido. It formed around 30,000 years ago. Nakajima, a Holocene post-caldera lava dome complex, forms the large island to the left that fills much of the western half of the caldera. Atosanupuri is located near the center of the caldera, east of the lake. · Foto: Photo by Lee Siebert, 1977 (Smithsonian Institution). · Wikimedia Commons
Tipo
Caldera
País
Japan
Región
Northwestern Pacific Volcanic Regions / Kuril Volcanic Arc
Altitud
574 m
Coordenadas
43.615, 144.427
Última erupción
1320
Contexto tectónico
Subduction zone / Continental crust (> 25 km)
Forma volcánica
Caldera
Roca principal
Dacite
Resumen geológico

The 20 x 26 km Kussharo caldera (also spelled Kutcharo or Kuccharo), is the largest of a cluster of calderas in NE Hokkaido. The caldera was formed in a series of major eruptions between about 340,000 and 30,000 years ago. Nakajima, a Holocene post-caldera dacitic-to-rhyolitic lava-dome complex, forms an island in the large lake that fills much of the western half of the caldera. The Holocene Atosanupuri stratovolcano and lava-dome complex is located near the center of the caldera, east of the crescent-shaped Lake Kutcharo. Many lava domes were formed between about 1000-10,000 years ago. No historical eruptions are known, although intense fumarolic activity occurs on and around Atosanupuri volcano and along the shores of Lake Kutcharo.

Resumen de Wikipedia

Resumen en inglés

Lake Kussharo is a caldera lake in Akan National Park, eastern Hokkaidō, Japan. As with many geographic names in Hokkaidō, the name derives from the Ainu language. It is the largest caldera lake in Japan in terms of surface area, and the sixth largest lake in Japan. It is also the largest lake in Japan to freeze over completely in winter. The name Lake Kutcharo is also sometimes used.

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Historial de erupciones

Resumen (VEI en el tiempo)
Haga clic en una barra para ver erupciones individuales
5800 BCE~5563 BCE · 1 erupciones · VEI máx. ?3664 BCE~3427 BCE · 1 erupciones · VEI máx. ?1765 BCE~1528 BCE · 1 erupciones · VEI máx. ?371~608 · 1 erupciones · VEI máx. ?608~845 · 1 erupciones · VEI máx. ?1083~1320 · 1 erupciones · VEI máx. ?5800 BCE4139 BCE2240 BCE579 BCE1083

Línea de tiempo detallada

  1. 1320 (±300 años)VEI ?Estimación geológica
    1320 – En curso
    Atosanupuri
  2. 700VEI ?Estimación geológica
    700 – En curso
    Atosanupuri
  3. 450VEI ?Estimación geológica
    450 – En curso
    Atosanupuri
  4. 1550 a. C. (±2000 años)VEI ?Estimación geológica
    BCE 1550 – En curso
    Atosanupuri
  5. 3550 a. C.VEI ?Estimación geológica
    BCE 3550 – En curso
    Atosanupuri
  6. 5800 a. C. (±2250 años)VEI ?Estimación geológica
    BCE 5800 – En curso
    Atosanupuri

Enlaces externos

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