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シーナリー山

Saba

成層火山 · Netherlands · 887m

Mt. Scenery, the summit lava dome of Saba volcano, is seen from the airport on the NE side of the island.  The sun-dappled slopes in the foreground are the surface of a large andesitic lava flow that descends the NE flank of the volcano and forms the Flat Point Peninsula, on which the airport was constructed.  A steep switch-backed road extends from the airport to the village of Lower Hells Gate (center).  Saba is the northernmost active volcano of the West Indies.
Mt. Scenery, the summit lava dome of Saba volcano, is seen from the airport on the NE side of the island. The sun-dappled slopes in the foreground are the surface of a large andesitic lava flow that descends the NE flank of the volcano and forms the Flat Point Peninsula, on which the airport was constructed. A steep switch-backed road extends from the airport to the village of Lower Hells Gate (center). Saba is the northernmost active volcano of the West Indies. · 写真: Photo by John Shepherd, 2000 (Seismic Research Unit, University of West Indies). · Wikimedia Commons
タイプ
成層火山
Netherlands
地域
Middle America-Caribbean Volcanic Regions / Lesser Antilles Volcanic Arc
標高
887m
座標
17.630, -63.230
最終噴火
1640年
テクトニクス環境
Subduction zone / Oceanic crust (< 15 km)
火山地形
Composite
主要岩石
Andesite / Basaltic Andesite
地質学的概要

Saba, the northernmost active volcano of the West Indies, is a 5-km-diameter island forming the upper half of a large stratovolcano that rises 1,500 m above the sea floor. Its eruptive history is characterized by the emplacement of lava domes and associated pyroclastic flows. The summit, known as Mount Scenery (or The Mountain), is a Holocene lava dome that overtops a major collapse scarp that formed about 100,000 years ago. Flank domes were constructed on the SW, SE, E, and NE sides of the island near the coast. A large andesitic lava flow entered the sea on the NE flank, forming the Flat Point Peninsula. The village of The Bottom overlies pyroclastic-surge deposits that contain European pottery fragments and were radiocarbon dated at 280 +/- 80 years before present. The village was settled in 1640 CE on grassy meadows on the volcano's flanks reflecting initial vegetation recovery following destruction of tropical rainforests by pyroclastic flows and surges. Lava dome growth may also have occurred during this SW-flank eruption.

Wikipedia の要約

シーナリー山 は、カリブ海のオランダ領サバ島にある活火山。その溶岩円頂丘は、それ自体ひとつの成層火山である同島の山頂をなす。標高は887mで、オランダ王国の最高峰。また、2010年以後サバ島がオランダ本国に所属することとなったため(それまでは自治領オランダ領アンティルの所属であった)、オランダ本国の最高峰でもある。

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噴火履歴

概要 (VEI時系列)
バーをクリックすると個別の噴火が表示されます
1640~1640 · 1件 · 最大 VEI ?16401640164116411641

詳細タイムライン

  1. 1640年VEI ?観測記録
    1640 ~ 進行中
    SW flank

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。