キフピニチ山
Kikhpinych
成層火山 · Russia · 1515m

- タイプ
- 成層火山
- 国
- Russia
- 地域
- Northwestern Pacific Volcanic Regions / Eastern Kamchatka Volcanic Arc
- 標高
- 1515m
- 座標
- 54.489, 160.251
- 最終噴火
- 1550年
- テクトニクス環境
- Subduction zone / Continental crust (> 25 km)
- 火山地形
- Composite
- 主要岩石
- Basalt / Picro-Basalt
地質学的概要
Kikhpinych, the youngest stratovolcano of the Eastern Volcanic Zone of Kamchatka, contains three summits constructed along a roughly E-W line above the eroded Pleistocene Pik volcano, NE of the Uzon caldera. Growth of the modern volcano began during the mid-Holocene about 4,800 years ago with construction of the Zapadny cone. After a long quiescence, the younger Savich cone was built about 1,400 years ago, which included strong explosive activity that destroyed part of the Zapadny and Pik cones. Numerous young lava flows mantle the flanks of Savich; it was last active about 400 years ago, when the Krab lava dome grew on its E flank. Numerous thermal fields are found throughout the complex, including two geysers (now the site of vigorous fumaroles) that were active in the summit crater of Stary Kikhpinych prior to burial by a rockfall avalanche that occurred sometime between September 1981 and July 1982.
Wikipedia の要約
英語版の要約Kikhpinych is a stratovolcano located in the eastern part of the Kamchatka Peninsula, which feeds the famous Valley of Geysers.
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噴火履歴
詳細タイムライン
- 1550年VEI ?地質学的推定1550 ~ 進行中East flank of Savich (Krab cone)
- 1350年VEI 4地質学的推定1350 ~ 進行中Savich cone and north flank
- 900年 (±50年)VEI 3地質学的推定900 ~ 進行中Savich cone
- 830年 (±25年)VEI ?地質学的推定830 ~ 進行中Savich cone
- 650年VEI ?地質学的推定650 ~ 進行中Savich cone
- 550年VEI 3地質学的推定550 ~ 進行中East side of Zapadny, Savich cone
- 紀元前 2780年 (±25年)VEI 4地質学的推定BCE 2780 ~ 進行中Zapadny
- 紀元前 2850年VEI 3地質学的推定BCE 2850 ~ 進行中Zapadny
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。