Bliznetsy

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  • Country
  • Subregion Name
  • Primary Volcano Type
  • Last Known Eruption
  • 57.35°N
  • 161.37°E

  • 265 m
    869 ft

  • 300552
  • Latitude
  • Longitude

  • Summit
    Elevation

  • Volcano
    Number

There are no activity reports for Bliznetsy.



 Available Weekly Reports

There are no Weekly Reports available for Bliznetsy.

Summary of eruption dates and Volcanic Explosivity Indices (VEI).

Start Date Stop Date Eruption Certainty VEI Evidence Activity Area or Unit
1060 BCE ± 40 years Unknown Confirmed 1 Radiocarbon (uncorrected)

The following references are the sources used for data regarding this volcano. References are linked directly to our volcano data file. Discussion of another volcano or eruption (sometimes far from the one that is the subject of the manuscript) may produce a citation that is not at all apparent from the title. Additional discussion of data sources can be found under Volcano Data Criteria.

Babansky A D, Pevzner M M, Volynets A O, 2006. Petrology, geochemistry and geodynamics of Holocene volcanism in the Elovka River basin (North Kamchatka). All Russian Symposium "Volcanism and Geodynamics" September, 2006, Ulan-Ude, Russia, abs .

Pevzner M M, 2004b. New data on Holocene monogenetic volcanism of the northern Kamchatka: ages and space distribution. IV Internatl Biennial Workshop on Subduction Processes, Petropavlovsk-Kamchatsky, August 21-27, 2004, Abs.

Ponomareva V, Melekestsev I, Braitseva O, Churikova T, Pevzner M, Sulerzhitsky L, 2007b. Late Pleistocene-Holocene volcanism on the Kamchatka Peninsula, northwest Pacific region. In: Eichelberger J, Gordeev E, Izbekov P, Kasahara M, Lees J (eds), Volcanism and Subduction: the Kamchatka Region, {Amer Geophys Union, Geophys Monogr}, 172: 165-198.

The Bliznetsy ("Twins") lava flows occupy a low-lying area east of the Sredinny Range and north of the Eastern Volcanic Zone volcanoes. The young flows lie south of the Ozernaya River about 80 km north of historically active Shiveluch volcano. Effusion of about 0.5 cu km of lava forming the Bliznetsy flows about 3000 years ago was preceded by weak phreatomagmatic eruptions. The unusual location of this recently studied young volcanic vent lies north of the margin of the subducting Pacific Plate.