bjdeming
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The strong explosive eruption of the Bezymianny volcano began at 23:10 UTC on 23 April. The ash cloud 36x26 km in size continues to move to the north-northeast of the volcano. KVERT continues to monitor the Bezymianny volcano.
An explosive eruption of the volcano continues. The danger of ash explosions up to 15 km (49,200 ft) a.s.l. remains. Ongoing activity could affect international and low-flying aircraft.(12) Volcanic cloud height: 10000-11000 m (32800-36080 ft) AMSL Time and method of ash plume/cloud height determination: 20250423/2310Z – Himawari-9 14m15 (13) Other volcanic cloud information: Distance of ash plume/cloud of the volcano: 32 km (20 mi)
Direction of drift of ash plume/cloud of the volcano: NNE / azimuth 25 deg
Time and method of ash plume/cloud determination: 20250423/2310Z – Himawari-9 14m15
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The strong explosive eruption of the Bezymianny volcano began at 23:10 UTC on 23 April, and ended about 03:00 UTC on 24 April. The explosions sent ash up to 11 km a.s.l., and ash plume extended for about 232 km from the volcano. Ashfalls were noted at Atlasovo, Lazo, Milkovo Villages. At now, no ash explosions observed at the volcano, but a large ash cloud 110x175 km in size continues to move to the southwest of the volcano. Ash cloud was noted at 7-7,5 km a.s.l., in the distance about 320 km of the volcano at 05:10 UTC on 24 April. KVERT continues to monitor the Bezymianny volcano.
The activity of the volcano continues. Ongoing activity could affect international and low-flying air craft.
...During the precursory eruption, fine ash was ejected, and a small lava dome, Malobago, was extruded on the southeastern slopes of the present caldera outline. Other similar lava extrusion may have occurred within the caldera.
After a geologically short pause (likely within 10 years), the main caldera-forming eruption, which consisted of three distinct eruption phases, started. The first phase involved a plinian eruption, likely within the present caldera, resulting in the northward emplacement of pumiceous tephra with bulk volume of 20km3. Partial collapse of the plinian column repeatedly occurred during the early stage of the plinian phase. These formed intra-plinian flow deposits, which are generally thin, fine grained, and associated with fallout pumice layers. A strong ground shaking occurred in the Sorsogon area during the waning stage of the plinian phase, resulting in the formation of disturbed structures both at the base and in the upper horizon of the plinian deposit.
This was followed by the generation of the lower Irosin ignimbrite with associated ground layers. The final eruption was catastrophic, forming the present caldera topography and emplacing the upper Irosin ignimbrite...
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“Although we detected a volatile-rich layer, its bubble and melt contents are below the levels typically associated with imminent eruption,” Schmandt said. “Instead, it looks like the system is efficiently venting gas through cracks and channels between mineral crystals, which makes sense to me given Yellowstone’s abundant hydrothermal features emitting magmatic gases.”
Schmandt likened the system to “steady breathing” with bubbles rising and releasing through the porous rock — a natural pressure-release valve that lowers eruption risk...
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Massive lava fountains at Kilauea right now, must watch: