Bezymianny (Russian: Безымянный Bezymyannyyi, meaning unnamed) is an active stratovolcano in Kamchatka, Russia. Bezymianny volcano had been considered extinct until 1955. Activity started in 1955, culminating in a dramatic eruption on 30 March 1956.[2][3] This eruption, similar to that of Mount St. Helens in 1980, produced a large horseshoe-shaped crater that was formed by collapse of the summit and an associated lateral blast. Subsequent episodic but ongoing lava dome growth, accompanied by intermittent explosive activity and pyroclastic flows, has largely filled the 1956 crater. The most recent eruption of lava flows occurred in February 2013.[4] An explosive eruption on 20 December 2017 released an ash plume rising to a height of 15 kilometres (49,000 ft) above sea level, which drifted for 320 kilometres (200 mi) NE.[5] The volcano erupted similarly on 28 May 2022, again spewing an ash plume over 15 kilometres (49,000 ft) high.[6]
Bezymianny | |
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Highest point | |
Elevation | 3,020 m (9,910 ft)[1] |
Coordinates | 55°58′42″N 160°35′12″E[1] |
Naming | |
Native name | Безымянный (Russian) |
English translation | Nameless |
Geography | |
Bezymianny Kamchatka, Russia | |
Parent range | Eastern Range |
Geology | |
Age of rock | 4700 years old |
Mountain type | Stratovolcano |
Volcanic field | Kliuchevskoya Volcanic Group |
Last eruption | 2022 |
The modern Bezymianny volcano, much smaller than its massive neighbors Kamen and Kliuchevskoi, was formed about 4700 years ago over a late-Pleistocene lava-dome complex and an ancestral volcano that was built between about 11,000–7000 years ago. There have been three periods of intensified activity in the past 3000 years.
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