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St. Paul

成層火山 · France · 268m

A small 1.8-km-wide caldera cuts the E side of uninhabited St. Paul Island, as depicted in this plate from the SMS Gazelle expedition. The flooded caldera has 300-m-high walls on the SW side and is narrowly constrained by low spits on the NE. Geothermal areas are located along the caldera rim and along the margins of the caldera bay. The entire NE half of the volcano forming much of the island now lies beneath the sea.
A small 1.8-km-wide caldera cuts the E side of uninhabited St. Paul Island, as depicted in this plate from the SMS Gazelle expedition. The flooded caldera has 300-m-high walls on the SW side and is narrowly constrained by low spits on the NE. Geothermal areas are located along the caldera rim and along the margins of the caldera bay. The entire NE half of the volcano forming much of the island now lies beneath the sea. · 写真: Plate from the SMS Gazelle expedition (courtesy of NOAA Photo Library). · Wikimedia Commons
タイプ
成層火山
France
地域
Somalian-Antarctic Volcanic Regions / Amsterdam-St. Paul Hotspot Volcano Group
標高
268m
座標
-38.720, 77.530
最終噴火
1793年
テクトニクス環境
Rift zone / Oceanic crust (< 15 km)
火山地形
Composite
主要岩石
Basalt / Picro-Basalt
地質学的概要

The uninhabited triangular island of St. Paul is located near the axis of the East Indian Ocean Ridge, 80 km S of Amsterdam Island. It is composed of an older tuff cone surmounted by a basaltic stratovolcano with a 1.8-km-wide caldera. The entire NE half of the volcano was submerged following collapse along a NW-trending fault. This breached the central caldera, leaving an 80-m-deep bay connected to the ocean by a narrow channel. Geothermal areas are located near the caldera rim and along the margins of the caldera bay. The only recorded eruption took place in 1793 from a vent on the lower SW flank.

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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
1793~1793 · 1件 · 最大 VEI 217931793179417941794

詳細タイムライン

  1. 1793年VEI 2観測記録
    1793 ~ 進行中
    SW flank (near Cape West)

外部リンク

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