本文へスキップ
地図に戻る
比較

グッドイナッフ島

Goodenough

火山原 · Papua New Guinea · 220m

Goodenough (center) is the roughly circular volcanic island that is the westernmost of the D'Entrecasteaux Islands in this NASA satellite image with north to the upper right. Several Holocene eruptive centers that may be only a few hundred years old are located around the margins of fault-bounded metamorphic rocks that form the central part of Goodenough Island. The youngest volcanic features, which include the Walilagi Cones, are located at the SE end of the island on the Bwaido Peninsula (lower center).
Goodenough (center) is the roughly circular volcanic island that is the westernmost of the D'Entrecasteaux Islands in this NASA satellite image with north to the upper right. Several Holocene eruptive centers that may be only a few hundred years old are located around the margins of fault-bounded metamorphic rocks that form the central part of Goodenough Island. The youngest volcanic features, which include the Walilagi Cones, are located at the SE end of the island on the Bwaido Peninsula (lower center). · 写真: NASA Space Shuttle image STS44-83-79, 1991 (http://eol.jsc.nasa.gov/). · Wikimedia Commons
タイプ
火山原
Papua New Guinea
地域
南西太平洋 / Trobriand Volcanic Province
標高
220m
座標
-9.358, 150.246
最終噴火
不明
テクトニクス環境
Subduction zone / Continental crust (> 25 km)
火山地形
Cluster
主要岩石
Andesite / Basaltic Andesite
地質学的概要

Goodenough is a roughly circular volcanic island that is the westernmost of the D'Entrecasteaux Islands off the NE tip of Papua New Guinea. Several basaltic andesite and andesitic Holocene eruptive centers are located around the margins of fault-bounded metamorphic rocks that form the central part the island. The youngest volcanic features, which include the Walilagi Cones, are located at the SE end of the island. These well-developed ash cones and blocky lava flows on the N and E flanks of the Bwaido Peninsula may have erupted within the past few hundred years.

噴火履歴

詳細タイムライン

噴火記録はありません。

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。