Skip to main content

Deformation, Earthquakes and Mechanism of Activity of Klyuchevskoy Volcano

  • Conference paper
Volcanic Seismology

Part of the book series: IAVCEI Proceedings in Volcanology ((VOLCANOLOGY,volume 3))

Abstract

Klyuchevskoy is a gigantic, approximately 7000 year old basaltic volcano 4750 m in height. In this paper, a model of its activity, feeding channels and magma chambers is presented; it was developed from observations of summit and flank eruptions, magma flow rate, vertical ground deformation and location and migration of earthquake hypocentres and theoretical calculations.

Variations in the depth, (Zo) of the effective source of magmatic pressure and of the centre of seismic energy release, (H̄E) are traced. Relations have been established between Zo, vertical deformation (Uz) and expected magma accumulation in the feeding system (ω). Volume increments in the feeding system of the volcano δV have been calculated. Correlations were found between Zo and H̄E (correlation coefficient r = 0.63), on one hand, Uz and ω(r = 0.66), and ω and δV (r = 0.62) on the other, which support the validity of the model.

From 1979 to 1987 the volume increment δV changed by a factor of 3–5, the position of its centre migrated in depth from 3 km to 15 km below sea level, whereas the lava level remained constant in the summit crater and, consequently, pressure in the feeding channel was constant as well. The maximum increase of δV occurred at a depth of 15 km before the large flank eruption of 1983.

This model predicts that the basaltic magma rises into the crust from a large system of magma chambers located in the crust-mantle transition layer. It ascends through the crust at depths of 30-0 km in a vertical channel. Here, the feeding conduit is surrounded by a plastic shell about 3 km in diameter, around which numerous earthquakes occur. Most of them occur within the column-like zone 5–7 km in diameter. Dikes and sills are common here and frequently intrude from the vertical channel, the longest dikes reaching 20 km. No large peripheral or crustal magma chambers of the volcano were detected.

This is a preview of subscription content, log in via an institution to check access.

Access this chapter

Chapter
USD 29.95
Price excludes VAT (USA)
  • Available as PDF
  • Read on any device
  • Instant download
  • Own it forever
eBook
USD 84.99
Price excludes VAT (USA)
  • Available as PDF
  • Read on any device
  • Instant download
  • Own it forever
Softcover Book
USD 109.99
Price excludes VAT (USA)
  • Compact, lightweight edition
  • Dispatched in 3 to 5 business days
  • Free shipping worldwide - see info

Tax calculation will be finalised at checkout

Purchases are for personal use only

Institutional subscriptions

Preview

Unable to display preview. Download preview PDF.

Unable to display preview. Download preview PDF.

References

  • Balesta ST (1981) Earth’s crust and magma chambers in the regions of recent volcanism. Nauka, Moscow, p 133 (in Russian).

    Google Scholar 

  • Balesta ST, Zubin MI, Kargopoltsev AA, Fedorchenko IA (1984) Deep structure of the eruption region. In: Fedotov SA (ed) The large Tolbachik fissure eruption. Nauka, Moscow, 15:514-537 (in Russian).

    Google Scholar 

  • Chester DK, Duncan AM, Guest IE, Kilburn CRJ (1985) Mount Etna. The anatomy of a volcano. Lond, p 404.

    Google Scholar 

  • Dietrich H, Derker W (1975) Finite element modeling of surface deformation associated with volcanism. J Geophys Res 80,29:4094–4102.

    Article  Google Scholar 

  • Efimov AB, Demin SS (1979) Studies of the strain-deformational state close to the magma chamber. Volcanol Seismol 1:16–27 (in Russian).

    Google Scholar 

  • Fedotov SA (1972) Energy classification of the Kuril-Kamchatka earthquakes and the problem of magnitudes. Nauka, Moscow, p 116 (in Russian).

    Google Scholar 

  • Fedotov SA (1976a) Geophysical data on the deep magma activity beneath Kamchatka and estimation of forces which cause magma rise to the volcanoes. Izv Akad Nauk SSSR Ser Geol 4:5–16 (in Russian).

    Google Scholar 

  • Fedotov SA (1976b) Geophysical data on the deep magma activity beneath island arc volcanoes and similar structures. Izv Akad Nauk SSSR Ser Geol 5:25–37 (in Russian).

    Google Scholar 

  • Fedotov SA (1976c) On basic magma rise in the earth’s crust and mechanism of fissure basaltic eruptions. Izv Akad Nauk SSSR Ser Geol 10:5–23 (in Russian).

    Google Scholar 

  • Fedotov SA (1976d) Mechanism of magma ascent and deep feeding channels of island arc volcanoes. Bull Volcanol 39,2:241–254.

    Article  Google Scholar 

  • Fedotov SA (1980) On temperatures of entering magmas, formation, dimensions and evolution of volcanic magma chambers. Volcanol Seismol 4:3–29 (in Russian).

    Google Scholar 

  • Fedotov SA (1981) Magma rates in feeding conduits of different volcanic centers. J Volcanol Geotherm Res 9:379–394.

    Article  Google Scholar 

  • Fedotov SA (1982) Temperatures of entering magma, formation and dimensions of magma chambers of volcanoes. Bull Volcanol 45,4:333–348.

    Article  Google Scholar 

  • Fedotov SA (1984) Large fissure eruptions: their theory. Mechanism of the Tolbachik eruption. In: Fedotov SA (ed) The large Tolbachik fissure eruption. Nauka, Moscow, 16:537-575 (in Russian).

    Google Scholar 

  • Fedotov SA, Goritsky YA (1980) Thermal computation of the cylindrical feeding channels and magma discharge for central type volcanoes. Volcanol Seismol 1:3–15 (in Russian).

    Google Scholar 

  • Fedotov SA, Gorelchik VI, Stepanov W (1980) Seismological studies on the mechanism of the large Tolbachik fissure eruption, 1975–1976. Bull Volcanol 43:73–84.

    Article  Google Scholar 

  • Fedotov SA, Gorelchik VI, Zobin VM, Stepanov W, Chubarova OS, Shirokov VA (1984a) Seismological data on mechanism and development of eruption. In: Fedotov SA (ed) The large Tolbachik fissure eruption. Nauka, Moscow, 12:389-448 (in Russian).

    Google Scholar 

  • Fedotov SA, Enman VB, Nikitenko YP, Maguskin MA, Levin VE, Zharinov NA, Enman SV (1984b) Geodetic studies. In: Fedotov SA (ed) The large Tolbachik fissure eruption. Nauka, Moscow, 14:472-513 (in Russian).

    Google Scholar 

  • Fedotov SA, Gusev AA, Chernysheva GA, Shumilina LS (1985) Kamchatka seismofocal zone (geometry, location of earthquake foci and connection with volcanism). Volcanol Seismol 4:91–107 (in Russian).

    Google Scholar 

  • Fedotov SA, Khrenov AP, Zharinov NA (1987) Klyuchevskoy volcano, its activity in 1932–1986 and probable development. Volcanol Seismol 4:3–17 (in Russian).

    Google Scholar 

  • Fedotov SA, Zharinov NA, Gorelchik VI (1988) Deformations and earthquakes of the Klyuchevskoy volcano, a model of its activity. Volcanol Seismol 2:3–42 (in Russian).

    Google Scholar 

  • Gorelchik VI (1985) Seismic activity of Klyuchevskoy during preparation and development of the Predskazanny breakthrough in March–July 1983. Volcanol Seismol 1:71–87 (in Russian).

    Google Scholar 

  • Gorelchik VI, Stepanov W (1976) Seismicity in the region of the northern volcanic group in Kamchatka in 1971–1972. In: Ivanov BV, Balesta ST (eds) Deep structure, seismicity and recent activity of the Klyuchevskoy volcanic group. Nauka, Vladivostok, pp 198–218 (in Russian).

    Google Scholar 

  • Gorelchik VI, Zobin VM, Tokarev PI (1987) Seismicity of volcanoes. Volcanol Seismol 6:61–77 (in Russian).

    Google Scholar 

  • Gorelchik VI, Chubarova OS, Garbuzova VT (1988) Seismicity in the region of the northern volcanic group in Kamchatka, 1971–1983. Volcanol Seismol 1:90–100 (in Russian).

    Google Scholar 

  • Kirsanov IT, Markov IT (1979) Evolution of basalts in the process of formation of Klyuchevskoy volcano. In: Sobolev VS (ed) The problems of deep magmatism. Nauka, Moscow, pp 80–97 (in Russian).

    Google Scholar 

  • Mogi K (1958) Relation between the eruptions of various volcanoes and the deformations of the ground surface around them. Bull Earth Res Inst 36:99–134.

    Google Scholar 

  • Piyp BI (1956) Mount Klyuchevskoy and its eruptions in 1944–1945 and in the past. Proc Lab Volcanol 11:308 (in Russian).

    Google Scholar 

  • Shirokov VA (1978) Relation betwee volcanic eruptions in Kamchatka and earthquakes in the upper mantle. Bull Volcanol Stations 54:3–8 (in Russian).

    Google Scholar 

  • Tokarev PI (1970) On focal layer, seismicity and volcanism in the Kuril-Kamchatka zone. Izv Akad Nauk SSSR Ser Phys Earth 3:15–30 (in Russian).

    Google Scholar 

  • Wright TL, Helz RJ (1987) Recent advances in Hawaiian petrology and geochemistry. In: Decker RW, Wright TL, Stauffer PH (eds) Volcanism in Hawaii. US Geol Surv Prof Pap 1350, VII:625-640, Washtington.

    Google Scholar 

  • Yoder H (1972) Formation of basaltic magma. Mir, Moscow, p 238 (in Russian).

    Google Scholar 

  • Yokoyama I (1971) A model for the crustal deformation around volcanoes. J Phys Earth 19:199–207.

    Article  Google Scholar 

  • Zharinov NA, Eremeev NN (1985) Deformations of the earth’s surface at Klyuchevskoy which preceded and accompanied eruption Predskazannoe in 1983. Volcanol Seismol 1:88–97 (in Russian).

    Google Scholar 

Download references

Authors

Editor information

Editors and Affiliations

Rights and permissions

Reprints and permissions

Copyright information

© 1992 Springer-Verlag Berlin Heidelberg

About this paper

Cite this paper

Fedotov, S.A., Gorelchik, V.I., Zharinov, N.A. (1992). Deformation, Earthquakes and Mechanism of Activity of Klyuchevskoy Volcano. In: Gasparini, P., Scarpa, R., Aki, K. (eds) Volcanic Seismology. IAVCEI Proceedings in Volcanology, vol 3. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-77008-1_3

Download citation

  • DOI: https://doi.org/10.1007/978-3-642-77008-1_3

  • Publisher Name: Springer, Berlin, Heidelberg

  • Print ISBN: 978-3-642-77010-4

  • Online ISBN: 978-3-642-77008-1

  • eBook Packages: Springer Book Archive

Publish with us

Policies and ethics