Lake Kussharo
Kussharo
Kaldera · Japan · 574 m

- Tipe
- Kaldera
- Negara
- Japan
- Wilayah
- Pasifik Barat Laut / Kuril Volcanic Arc
- Ketinggian
- 574 m
- Koordinat
- 43.615, 144.427
- Letusan terakhir
- 1320
- Kondisi tektonik
- Subduction zone / Continental crust (> 25 km)
- Bentuk lahan
- Caldera
- Batuan utama
- Dacite
Ringkasan geologi
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.
Riwayat letusan
Garis waktu rinci
- 1320 (±300 tahun)VEI ?Perkiraan geologi1320 – BerlangsungAtosanupuri
- 700VEI ?Perkiraan geologi700 – BerlangsungAtosanupuri
- 450VEI ?Perkiraan geologi450 – BerlangsungAtosanupuri
- 1550 SM (±2000 tahun)VEI ?Perkiraan geologiBCE 1550 – BerlangsungAtosanupuri
- 3550 SMVEI ?Perkiraan geologiBCE 3550 – BerlangsungAtosanupuri
- 5800 SM (±2250 tahun)VEI ?Perkiraan geologiBCE 5800 – BerlangsungAtosanupuri
Tautan eksternal
⚠ Untuk referensi saja. Bukan untuk tanggap darurat.