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パナレーア島

Panarea

成層火山 · Italy · 399m

Panarea Island is the largest subaerial component of a mostly submarine volcanic complex between Lipari and Stromboli volcanoes. The last eruptions took place during the early Holocene, but hydrothermal activity has continued at fumarolic fields at several locations on the submerged platform. The water discoloration in the foreground, 2 km E of Panarea Island, near the small islands took place during November 2002.
Panarea Island is the largest subaerial component of a mostly submarine volcanic complex between Lipari and Stromboli volcanoes. The last eruptions took place during the early Holocene, but hydrothermal activity has continued at fumarolic fields at several locations on the submerged platform. The water discoloration in the foreground, 2 km E of Panarea Island, near the small islands took place during November 2002. · 写真: Photo courtesy of Istituto Nazionale di Geofisica e Vulcanologia, Sezione di Catania (INGV), 2002. · Wikimedia Commons
タイプ
成層火山
Italy
地域
European Volcanic Regions / Aeolian Volcanic Arc
標高
399m
座標
38.638, 15.064
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 mostly submerged Panarea volcanic complex lies about midway between Stromboli and Lipari in the eastern part of the Aeolian Islands. Panarea, the smallest island in the Aeolian Archipelago, lies on the western side of a shallow platform whose shelf margin is at about 130 m depth. A series of small islands breach the surface to form the Central Reefs, the rim of a crater 2 km E of Panarea, whose shallow submerged floor contains Roman ruins. The submerged Secca dei Pesci lava dome lies at the SE end of the platform, and the rhyolitic Basiluzzo lava dome rises 165 m above the surface at the NE end, along a ridge trending towards Stromboli volcano. The complex was constructed in two main stages: an initial effusive activity phase that produced lava domes, and an explosive stage. The youngest subaerial airfall-tephra deposits are dated to about 20,000 years ago; a date of less then 10,000 BP on a lava flow is uncertain. Vigorous hydrothermal activity has continued at fumarolic fields at several locations on the submerged platform; submarine hydrothermal explosions have occurred in historical time.

Wikipedia の要約

パナレーア島 (パナレーアとう、Panarea) は、エオリア諸島で2番目に小さい島であり、火山島である。最高地点はティンポーネ・デル・コルヴォの421m。バジルッツォ (Basiluzzo) 、スピナッツォラ (Spinazzola) 、リスカ・ビャンカ 、ダッティロ (Dattilo) 、ボッタロ (Bottaro) 、リスカ・ネーラ などの小島、パナレッリ (Panarelli) 岩、フォルミケ (Formiche) 岩などと共に、リーパリ島とストロンボリ島の間で小さな群島を形作っている。休暇シーズンには多くの観光客が集まる。

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