KVERT reported that strong explosions at Zhupanovsky were detected at 0206 on 23 November and 1214 on 25 November. Ash plumes rose to altitudes of 7-8 km (23,000-26,200 ft) a.s.l. and drifted 350 km E on 22 November and SE during 25-27 November. Satellite images detected a thermal anomaly over the volcano on 22, 25, and 27 November; cloud cover prevented views of the volcano on the other days. The Aviation Color Code remained at Orange.

Geological Summary. The Zhupanovsky volcanic massif consists of four overlapping stratovolcanoes along a WNW-trending ridge. The elongated complex was constructed within a Pliocene-early Pleistocene caldera whose rim is exposed only on the eastern side. Three of the stratovolcanoes were built during the Pleistocene. An early Holocene stage of frequent moderate and weak eruptions from 7,000 to 5,000 years before present (BP) was followed by a period of infrequent larger eruptions that produced pyroclastic flows. The last major eruption took place about 800-900 BP. Recorded eruptions have consisted of relatively minor explosions from Priemysh, the third cone from the E about 2.5 km from the summit peak.

Source: Kamchatkan Volcanic Eruption Response Team (KVERT)