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Lake Kussharo

Kussharo

Caldera · Japan · 574m

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. · Photo: Photo by Lee Siebert, 1977 (Smithsonian Institution). · Wikimedia Commons
Type
Caldera
Country
Japan
Region
Northwestern Pacific Volcanic Regions / Kuril Volcanic Arc
Elevation
574m
Coordinates
43.615, 144.427
Last eruption
1320
Tectonic setting
Subduction zone / Continental crust (> 25 km)
Landform
Caldera
Major rock type
Dacite
Geological summary

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.

From Wikipedia

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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Eruption history

Summary (VEI over time)
Click a bar to see individual eruptions
5800 BCE~5563 BCE · 1 eruptions · max VEI ?3664 BCE~3427 BCE · 1 eruptions · max VEI ?1765 BCE~1528 BCE · 1 eruptions · max VEI ?371~608 · 1 eruptions · max VEI ?608~845 · 1 eruptions · max VEI ?1083~1320 · 1 eruptions · max VEI ?5800 BCE4139 BCE2240 BCE579 BCE1083

Detailed timeline

  1. 1320 (±300 yrs)VEI ?Geological estimate
    1320 – Ongoing
    Atosanupuri
  2. 700VEI ?Geological estimate
    700 – Ongoing
    Atosanupuri
  3. 450VEI ?Geological estimate
    450 – Ongoing
    Atosanupuri
  4. 1550 BCE (±2000 yrs)VEI ?Geological estimate
    BCE 1550 – Ongoing
    Atosanupuri
  5. 3550 BCEVEI ?Geological estimate
    BCE 3550 – Ongoing
    Atosanupuri
  6. 5800 BCE (±2250 yrs)VEI ?Geological estimate
    BCE 5800 – Ongoing
    Atosanupuri

External links

⚠ For reference only. Not for emergency response.