Zhupanovsky volcan

Compound volcano 2958 m / 9,705 ft

Condition actuelle: normal / en sommeil (1 sur 5)
Last update: 29 Feb 2020

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Style éruptif tipique: unspecified
Eruptions du volcan Zhupanovsky: 1959 

No recent earthquakes
HeureMag. / ProfondeurDistance/Lieu

Introduction

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 of Zhupanovsky took place about 800-900 years BP. Historical eruptions have consisted of relatively minor explosions from the third cone.
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Smithsonian / GVP volcano information


See also: Sentinel hub | Landsat 8
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