Bezymianny
FVFE01 at 15:00 UTC, 19/05/26 from RJTD VA ADVISORY DTG: 20260519/1500Z VAAC: TOKYO VOLCANO: BEZYMIANNY 300250 PSN: N5558 E16036 AREA: RUSSIA SOURCE ELEV: 2882M AMSL ADVISORY NR: 2026/29 INFO SOURCE: HIMAWARI-9 ERUPTION DETAILS: VA CONTINUOUSLY OBS IN SATELLITE IMAGERY OBS VA DTG: 19/1420Z OBS VA CLD: SFC/FL300 N6244 E14651 - N6140 E14748 - N5919 E14841 - N5901 E14806 - N6219 E14618 MOV NW 25KT FCST VA CLD +6 HR: 19/2020Z SFC/FL300 N6416 E14600 - N6019 E14603 - N6021 E14515 - N6333 E14311 FCST VA CLD +12 HR: 20/0220Z SFC/FL300 N6452 E14702 - N6115 E14410 - N6309 E14122 - N6516 E14546 FCST VA CLD +18 HR: 20/0820Z SFC/FL300 N6518 E14902 - N6007 E14147 - N6141 E14116 - N6619 E14738 RMK: SOME PART OF VA OBSCURED BY MET CLOUD. NXT ADVISORY: 20260519/1800Z=

Bezymianny
The modern Bezymianny, much smaller than its massive neighbors Kamen and Kliuchevskoi on the Kamchatka Peninsula, was formed about 4,700 years ago over a late-Pleistocene lava-dome complex and an edifice built about 11,000-7,000 years ago. Three periods of intensified activity have occurred during the past 3,000 years. The latest period, which was preceded by a 1,000-year quiescence, began with the dramatic 1955-56 eruption. This eruption, similar to that of St. Helens in 1980, produced a large open 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.
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