散布山
Chirippusan [Chirip]
成層火山 · Japan - administered by Russia · 1587m
- タイプ
- 成層火山
- 国
- Japan - administered by Russia
- 地域
- Northwestern Pacific Volcanic Regions / Kuril Volcanic Arc
- 標高
- 1587m
- 座標
- 45.338, 147.920
- 最終噴火
- 1860年
- テクトニクス環境
- Subduction zone / Intermediate crust (15-25 km)
- 火山地形
- Composite
- 主要岩石
- Basalt / Picro-Basalt
地質学的概要
Chirippusan (also simply Chirip) volcano is on the Chirip Peninsula, which extends N into the Sea of Okhotsk from central Iturup Island. The summits of two overlapping stratovolcanoes are ~4.5 km apart along a volcanic ridge, with Kitachirippusan on the north and Minamichirippu (also called Bogdan Khmelnitskii) on the south. Lava flows from both edifices are truncated by a large 4-km-wide depression on the west side of the peninsula. Basaltic rocks dominate at both volcanoes over basaltic andesite and andesitic products. Kitachirippusan has a shallow summit crater, partially filled by a small lake, that has fed lava flows down all sides; satellitic cones are located on the northern flank. Lava flows from Minamichirippusan reach the coast on both the east and west. Only two eruptions are known, one in 1843 CE and another in 1860 CE from a vent SE of the Minamichirippusan summit.
Wikipedia の要約
要約が短いです。詳細は記事全文をご覧ください。
散布山 は択捉島にある火山。
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噴火履歴
詳細タイムライン
- 1860年VEI 1観測記録1860 ~ 進行中SE of Bogdan Khmelinitskii summit
- 1843年VEI 2観測記録1843 ~ 進行中
外部リンク
⚠ 参考情報です。緊急対応には使用しないでください。