ORGANIZATION OF TILTMEASURING OBSERVATION POINTS FOR RECORDING DEFORMATIONS OF THE EARTHʼS SURFACE AT KAMCHATKA GEODYNAMIC POLYGONS AND SOME OBSERVATION RESULTS
1 Kamchatka Branch of Geophysical Survey of the Russian Academy of Sciences
2 Vitus Bering Kamchatka State University, Petropavlovsk-Kamchatsky
3 V.I. Vyazemsky Karadag Scientific Station – Nature Reserve of the Russian Academy of Sciences – Branch of the Federal Research Center «A.O. Kovalevsky Institute of Biology
of the Southern Seas of the Russian Academy of Sciences»
Journal: Geophysical processes and biosphere
Tome: 24
Number: 2
Year: 2025
Pages: 42-66
UDK: 550.34.056
DOI: 10.21455/GPB2025.2-4
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Glukhov V.E., Makarov E.O., Boldina S.V., Israpil R.I. ORGANIZATION OF TILTMEASURING OBSERVATION POINTS FOR RECORDING DEFORMATIONS OF THE EARTHʼS SURFACE AT KAMCHATKA GEODYNAMIC POLYGONS AND SOME OBSERVATION RESULTS
// . 2025. Т. 24. № 2. С. 42-66. DOI: 10.21455/GPB2025.2-4
@article{Glukhov ORGANIZATION2025,
author = "Glukhov , V. E. and Makarov , E. O. and Boldina , S. V. and Israpil , R. I.",
title = "ORGANIZATION OF TILTMEASURING OBSERVATION POINTS FOR RECORDING DEFORMATIONS OF THE EARTHʼS SURFACE AT KAMCHATKA GEODYNAMIC POLYGONS AND SOME OBSERVATION RESULTS
",
journal = "Geophysical processes and biosphere",
year = 2025,
volume = "24",
number = "2",
pages = "42-66",
doi = "10.21455/GPB2025.2-4",
language = "English"
}
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Keywords: tiltmeter, Kamchatka, geodynamics, deformations of the Earthʼs surface, observation network, tilts, seismic camera, coseismics, seismic recorder, earthquake.
Аnnotation: A comprehensive description of geodynamic polygons where the equipment of the tiltmeasuring observation points by Kamchatka slope measuring network is installed is given. The geographical location, temperature regime, soil conditions, parameters of seismic chambers used for the organization of points, types of installed equipment, and features of power supply are given. The characteristics of the equipment used in the network data registration and transmission system are described. Due to the earthquake of 17.08.2024, Mw = 7.0, the amplitudes of coseismic changes in the inclination of the Earthʼs surface (jumps) recorded at three stations PET2, IVS2 and KRMT were obtained. After the earthquake, a bay-shaped tilt change with amplitudes of 8 and 4 μrad developed for 20 days in the E–W and N–S directions at the IVS2 station, associated with the relaxation of the geoenvironment after the earthquake.



