Report on Zhupanovsky (Russia) — 20 August-26 August 2014
Smithsonian Institution / US Geological Survey
Weekly Volcanic Activity Report, 20 August-26 August 2014
Managing Editor: Sally Sennert.
Please cite this report as:
Global Volcanism Program, 2014. Report on Zhupanovsky (Russia) (Sennert, S, ed.). Weekly Volcanic Activity Report, 20 August-26 August 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 during 15-21 August that moderate explosive eruption continued at Zhupanovsky. Satellite data showed a thermal anomaly over the volcano on 16-17 August. On 18 and 15 August the volcano was obscured by clouds. The Tokyo VAAC reported ash plumes rose to 3-4.5 km (10,000-15,000 ft) a.s.l. and drifted S and SSE. On August 19 KVERT reported that satellite data showed ash plumes drifted 51 km S of the volcano and on August 20 that ash plumes rose to 3 km (9800 ft) a.s.l. and drifted 110 km SSE.
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.