Report on Zhupanovsky (Russia) — 20 May-26 May 2015
Smithsonian Institution / US Geological Survey
Weekly Volcanic Activity Report, 20 May-26 May 2015
Managing Editor: Sally Sennert.
Please cite this report as:
Global Volcanism Program, 2015. Report on Zhupanovsky (Russia) (Sennert, S, ed.). Weekly Volcanic Activity Report, 20 May-26 May 2015. Smithsonian Institution and US Geological Survey.
Zhupanovsky
Russia
53.589°N, 159.15°E; summit elev. 2899 m
All times are local (unless otherwise noted)
On 16 May KVERT reported that the explosive eruption that began at Zhupanovsky on 6 June 2014 ended at the beginning of April 2015. The last ash plume occurred on 3 April, although weak thermal anomalies continued to be detected. The Aviation Color Code was lowered to Yellow. On 20 May an ash plume drifted 470 km E.
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.
