Lake Kussharo
Kussharo
Caldera · Japan · 574m

- 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
Detailed timeline
- 1320 (±300 yrs)VEI ?Geological estimate1320 – OngoingAtosanupuri
- 700VEI ?Geological estimate700 – OngoingAtosanupuri
- 450VEI ?Geological estimate450 – OngoingAtosanupuri
- 1550 BCE (±2000 yrs)VEI ?Geological estimateBCE 1550 – OngoingAtosanupuri
- 3550 BCEVEI ?Geological estimateBCE 3550 – OngoingAtosanupuri
- 5800 BCE (±2250 yrs)VEI ?Geological estimateBCE 5800 – OngoingAtosanupuri
External links
⚠ For reference only. Not for emergency response.