Lake Kussharo
Kussharo
Caldera · Japan · 574m

- Type
- Caldera
- Country
- Japan
- Region
- Northwestern Pacific / 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.
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.