Transport Agency

Bolshoi Semiachik

Russian versionEnglish version
Germanic versionChinese version

54°16' N, 160°05' E, summit elevation 1739 m

Bolshoi ("Big") Semiachik massif is a group of Late Pleistocene-Holocene stratovolcanoes and extrusive domes located within a large mid-Pleistocene caldera. The most prominent edifice of the massif is Bolshoi Semiachik (or Zubchatyi) Late Pleistocene volcano. Holocene activity of the massif reduces to several extrusive domes. The massif hosts a hydrothermal system, one of the largest in Kamchatka.

One of the Holocene extrusive domes, Ivanov, was formed in Early Holocene, 8500-9000 14C years BP. The dome has no lava flow and looks like a real well-shaped dome. At first, we did not know how to date it since no cover of later ash layers could stay on its steep slopes. However, a pit dug just near the dome exposed a layer of pumiceous andesite lapilli, which lay between marker ashes KRM (7900 14C years BP) from Karymsky caldera and so called "lower yellow ash" (about 9500 14C years BP). This lapilli layer pinched out with distance from the dome and was obviously associated with its formation.

Two other Holocene domes, Ezh ("Hedgehog") and Korona ("Crown") gave rise to long lava flows and associated lahars. They were formed about 5600 14C years BP: the lowermost marker ash layer overlying lava flows and lahar deposits of both domes is AV5 (5600 14C years BP) from Avachinsky volcano, besides, pumiceous tephra of the eruption has been found in a peat section where it lies below AV5 but above a peat layer dated at 5620±50 years (Braitseva et al., 1995).

Volcanic products of the Holocene eruptions are low-potassic andesites.

Bolshoi Semiachik massif hosts several solfatara fields. Solfatara activity within these fields is manifested by jets of overheated vapour, boiling mud and water bowls, heated areas. Most of thermal fields are located in the central part of the massif, at the western slopes of Central and Bolshoi Semiachik volcanoes. The eastern part of Burliashchii thermal field hosts strong steam jets with temperatures up to 137° C. Hot springs also occur at the outer slopes of the massif, about 8 km southeast of Bolshoi Semiachik volcano. Central Semiachik thermal field hosts Chernoe ("Black") steaming lake.

Central part of the massif (elevation of about 1000 m) hosts peat bogs. They started to form about 9500 14C years BP and contain multiple ash layers from different volcanoes, including more than ten major markers (SH2 and SH3 from Shiveluch; OP from Baranii Amphitheater; KS1 and KS2 from Ksudach; AV1, AV4 and AV5 from Avachinsky, KHG from Khangar; KRM from Karymsky caldera; "lower yellow ash" from an unknown source; traces of KO ash from the Kurile Lake caldera, etc. These peat bogs provide a continuous record of volcanic impact on the territory.