Report on Zhupanovsky (Russia) — 26 November-2 December 2014
Smithsonian / US Geological Survey Weekly Volcanic Activity Report, 26 November-2 December 2014
Managing Editor: Sally Kuhn Sennert
Please cite this report as:
Global Volcanism Program, 2014. Report on Zhupanovsky (Russia). In: Sennert, S K (ed.), Weekly Volcanic Activity Report, 26 November-2 December 2014. Smithsonian Institution and US Geological Survey.
53.589°N, 159.15°E; summit elev. 2899 m
All times are local (unless otherwise noted)
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.
Geologic Background. The Zhupanovsky volcanic massif consists of four overlapping stratovolcanoes along a WNW-trending ridge. The elongated volcanic 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, the fourth is Holocene in age and was the source of all of Zhupanovsky's historical eruptions. An early Holocene stage of frequent moderate and weak eruptions from 7000 to 5000 years before present (BP) was succeeded by a period of infrequent larger eruptions that produced pyroclastic flows. The last major eruption took place about 800-900 years BP. Historical eruptions have consisted of relatively minor explosions from the third cone.