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.
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References
Balesta ST (1981) Earth’s crust and magma chambers in the regions of recent volcanism. Nauka, Moscow, p 133 (in Russian).
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).
Chester DK, Duncan AM, Guest IE, Kilburn CRJ (1985) Mount Etna. The anatomy of a volcano. Lond, p 404.
Dietrich H, Derker W (1975) Finite element modeling of surface deformation associated with volcanism. J Geophys Res 80,29:4094–4102.
Efimov AB, Demin SS (1979) Studies of the strain-deformational state close to the magma chamber. Volcanol Seismol 1:16–27 (in Russian).
Fedotov SA (1972) Energy classification of the Kuril-Kamchatka earthquakes and the problem of magnitudes. Nauka, Moscow, p 116 (in Russian).
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).
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).
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).
Fedotov SA (1976d) Mechanism of magma ascent and deep feeding channels of island arc volcanoes. Bull Volcanol 39,2:241–254.
Fedotov SA (1980) On temperatures of entering magmas, formation, dimensions and evolution of volcanic magma chambers. Volcanol Seismol 4:3–29 (in Russian).
Fedotov SA (1981) Magma rates in feeding conduits of different volcanic centers. J Volcanol Geotherm Res 9:379–394.
Fedotov SA (1982) Temperatures of entering magma, formation and dimensions of magma chambers of volcanoes. Bull Volcanol 45,4:333–348.
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).
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).
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.
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).
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).
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).
Fedotov SA, Khrenov AP, Zharinov NA (1987) Klyuchevskoy volcano, its activity in 1932–1986 and probable development. Volcanol Seismol 4:3–17 (in Russian).
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).
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).
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).
Gorelchik VI, Zobin VM, Tokarev PI (1987) Seismicity of volcanoes. Volcanol Seismol 6:61–77 (in Russian).
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).
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).
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.
Piyp BI (1956) Mount Klyuchevskoy and its eruptions in 1944–1945 and in the past. Proc Lab Volcanol 11:308 (in Russian).
Shirokov VA (1978) Relation betwee volcanic eruptions in Kamchatka and earthquakes in the upper mantle. Bull Volcanol Stations 54:3–8 (in Russian).
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).
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.
Yoder H (1972) Formation of basaltic magma. Mir, Moscow, p 238 (in Russian).
Yokoyama I (1971) A model for the crustal deformation around volcanoes. J Phys Earth 19:199–207.
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).
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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
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DOI: https://doi.org/10.1007/978-3-642-77008-1_3
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