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Lake Kussharo

Kussharo

Kaldera · Japan · 574 m

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. · Foto: Photo by Lee Siebert, 1977 (Smithsonian Institution). · Wikimedia Commons
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 Inggris

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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Riwayat letusan

Ringkasan (VEI dari waktu ke waktu)
Klik pada bar untuk melihat letusan individu
5800 BCE~5563 BCE · 1 letusan · VEI maks. ?3664 BCE~3427 BCE · 1 letusan · VEI maks. ?1765 BCE~1528 BCE · 1 letusan · VEI maks. ?371~608 · 1 letusan · VEI maks. ?608~845 · 1 letusan · VEI maks. ?1083~1320 · 1 letusan · VEI maks. ?5800 BCE4139 BCE2240 BCE579 BCE1083

Garis waktu rinci

  1. 1320 (±300 tahun)VEI ?Perkiraan geologi
    1320 – Berlangsung
    Atosanupuri
  2. 700VEI ?Perkiraan geologi
    700 – Berlangsung
    Atosanupuri
  3. 450VEI ?Perkiraan geologi
    450 – Berlangsung
    Atosanupuri
  4. 1550 SM (±2000 tahun)VEI ?Perkiraan geologi
    BCE 1550 – Berlangsung
    Atosanupuri
  5. 3550 SMVEI ?Perkiraan geologi
    BCE 3550 – Berlangsung
    Atosanupuri
  6. 5800 SM (±2250 tahun)VEI ?Perkiraan geologi
    BCE 5800 – Berlangsung
    Atosanupuri

Tautan eksternal

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