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Asacha

複成火山 · Russia · 1910m

The Asacha volcano group is seen here looking WSW from the slopes of Mutnovsky. Most of the complex was constructed during the Pleistocene, but some of a group of ten lava domes across the flanks of the complex may be early Holocene in age. During the Holocene, scoria cones and lava flows also erupted along the western and southern flanks of the Asacha complex.
The Asacha volcano group is seen here looking WSW from the slopes of Mutnovsky. Most of the complex was constructed during the Pleistocene, but some of a group of ten lava domes across the flanks of the complex may be early Holocene in age. During the Holocene, scoria cones and lava flows also erupted along the western and southern flanks of the Asacha complex. · 写真: Photo by Oleg Volynets (Institute of Volcanology, Petropavlovsk). · Wikimedia Commons
タイプ
複成火山
Russia
地域
Northwestern Pacific Volcanic Regions / Kuril Volcanic Arc
標高
1910m
座標
52.355, 157.827
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
Basalt / Picro-Basalt
地質学的概要

The Asacha group is a complex massif of Pleistocene-to-Holocene volcanoes located within a distinctly fault-bounded crustal block WSW of Mutnovsky volcano. An older Asacha shield volcano, Zheltyi stratovolcano to the east, a younger Asacha stratovolcano, and the small Tumanov lava cone (the best-preserved major cone of the group) were constructed during the late Pleistocene. Most of the ten lava domes on the flanks of the Asacha volcanoes were formed during the Pleistocene, but some may be early Holocene. Holocene basaltic cinder cones and lava flows related to regional volcanism were erupted along the western and southern flanks of the complex. A major volcano-tectonic earthquake swarm occurred near Zheltyi volcano in 1983, suggesting that the complex remains volcanically active.

Wikipedia の要約

英語版の要約

Asacha is a complex volcano located in the southern part of Kamchatka Peninsula, Russia.

Wikipedia · CC BY-SA · 記事全文を読む

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