シバヤク山
Singkut
カルデラ · Indonesia · 2181m
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- タイプ
- カルデラ
- 国
- Indonesia
- 地域
- スンダ・バンダ / Sunda Volcanic Arc
- 標高
- 2181m
- 座標
- 3.238, 98.513
- 最終噴火
- 1881年
- テクトニクス環境
- Subduction zone / Continental crust (> 25 km)
- 火山地形
- Caldera
- 主要岩石
- Andesite / Basaltic Andesite
地質学的概要
The Quaternary Singkut caldera is about 7 x 4 km with the S half of the rim topographically distinct. Post-caldera cones have filled much of the crater and the N rim, including Sibayak, Pintau, and Pratektekan. The 900-m-wide Sibayak crater is partially filled on the north by Pintau. A lava flow traveled through a gap in the western crater wall from the summit lava dome of Sibayak; the active geothermal field SE of the summit has abundant solfataras and fumaroles. Area residents record legends of eruptions. Neumann van Padang (1983) cited a report by Hoekstra of ash clouds emitted from the volcano in 1881. The town of Berastagi is within the caldera immediately SE of the younger cones.
Wikipedia の要約
英語版の要約Mount Sibayak is a stratovolcano overlooking the town of Berastagi in northern Sumatra, Indonesia. Although its last eruption was more than a century ago, geothermal activity in the form of steam vents and hot springs remains high on and around the volcano. The vents produce crystalline sulfur, which was mined on a small scale in the past. Seepage of sulfurous gases has also caused acidic discolouration of the small crater lake.
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噴火履歴
詳細タイムライン
- 1881年VEI ?観測記録1881-07-02 ~ 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。