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Asacha

Gunung api kompleks · Russia · 1910 m

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. · Foto: Photo by Oleg Volynets (Institute of Volcanology, Petropavlovsk). · Wikimedia Commons
Tipe
Gunung api kompleks
Negara
Russia
Wilayah
Pasifik Barat Laut / Kuril Volcanic Arc
Ketinggian
1910 m
Koordinat
52.355, 157.827
Letusan terakhir
Tidak diketahui
Kondisi tektonik
Subduction zone / Continental crust (> 25 km)
Bentuk lahan
Composite
Batuan utama
Basalt / Picro-Basalt
Ringkasan geologi

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.

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