Lake Kussharo
Kussharo
Kaldera · Japan · 574 m

- Tipe
- Kaldera
- Negara
- Japan
- Wilayah
- Northwestern Pacific Volcanic Regions / 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.
Ringkasan Wikipedia
Ringkasan InggrisLake 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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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.