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Dutton

成層火山 · United States · 1465m

Mount Dutton near the tip of the Alaska Peninsula is seen here from the NE. Successive lava domes overlying lava flows form the summit. Dome and flank collapse during the Holocene produced debris avalanche that traveled to the west and also reached Belkofski Bay to the south.
Mount Dutton near the tip of the Alaska Peninsula is seen here from the NE. Successive lava domes overlying lava flows form the summit. Dome and flank collapse during the Holocene produced debris avalanche that traveled to the west and also reached Belkofski Bay to the south. · 写真: Photo by Betsy Yount (Alaska Volcano Observatory, U.S. Geological Survey).
タイプ
成層火山
United States
地域
North America Volcanic Regions / Aleutian Ridge Volcanic Arc
標高
1465m
座標
55.183, -162.276
最終噴火
不明
テクトニクス環境
Subduction zone / Continental crust (> 25 km)
火山地形
Composite
主要岩石
Andesite / Basaltic Andesite
地質学的概要

The Mount Dutton volcanic center east of Cold Bay near the tip of the Alaska Peninsula consists of a glacier-covered central lava dome complex. Early andesitic lava flows and late-stage dacitic domes have been partially removed by one or more edifice collapses about 5100-6800 years ago. Debris avalanches traveled west and south, reaching Belkofski Bay. The important regional fishing center of King Cove lies less than 15 km from the volcano, and the village's airstrip is built on top of the southern avalanche deposit. A steep-sided complex of lava domes forms the summit, and young block-and-ash flow deposits extend to the east. Two small unglaciated lava domes on the NE flank 3.5 km from the summit are also of Holocene age. Major earthquake swarms near the volcano were recorded in 1984-85 and 1988.

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。