Report on Zhupanovsky (Russia) — 29 October-4 November 2014
Smithsonian / US Geological Survey Weekly Volcanic Activity Report,
29 October-4 November 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, 29 October-4 November 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 the eruption at Zhupanovsky had likely finished in mid-October; satellite images last detected an explosion on 11 October and a thermal anomaly on 12 October. Volcanologists conducting an overflight on 17 October observed only gas-and-steam activity from the active crater. The Aviation Color Code was lowered to Yellow.
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.