DESTRUCTION OF MEDIEVAL ARCHAEOLOGICAL MONUMENTS BY STRONG EARTHQUAKES IN THE SOUTHWESTERN PART OF ISSYK-KUL BASIN, TIEN SHAN
Schmidt Institute of Physics of the Earth, Russian Academy of Sciences
Journal: Problems of Engineering Seismology
Tome: 47
Number: 3
Year: 2020
Pages: 53-74
UDK: 550.34:551.794 (235.21)
DOI: 10.21455/VIS2020.3-3
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STRELNIKOV A.A.-., KORZHENKOV A.M. DESTRUCTION OF MEDIEVAL ARCHAEOLOGICAL MONUMENTS BY STRONG EARTHQUAKES IN THE SOUTHWESTERN PART OF ISSYK-KUL BASIN, TIEN SHAN // . 2020. Т. 47. № 3. С. 53-74. DOI: 10.21455/VIS2020.3-3
@article{STRELNIKOVDESTRUCTION2020,
author = "STRELNIKOV, A. A. -. and KORZHENKOV, A. M.",
title = "DESTRUCTION OF MEDIEVAL ARCHAEOLOGICAL MONUMENTS BY STRONG EARTHQUAKES IN THE SOUTHWESTERN PART OF ISSYK-KUL BASIN, TIEN SHAN",
journal = "Problems of Engineering Seismology",
year = 2020,
volume = "47",
number = "3",
pages = "53-74",
doi = "10.21455/VIS2020.3-3",
language = "English"
}
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Keywords: earthquake, seismotectonic ledges, compensation graben, archeoseismology, paleoseismology, seismic deformations, architectural and historical complex, Tien Shan, Issyk-Kul, Kyrgyzstan, Alabash-Konuroleong depression, mountains of Duvan
Аnnotation: The destruction of a major archaeological site in VII-IX clearly demonstrates the lack of seismic knowledge of the region and, as a result, the unaccounted for and underestimated seismic hazard assessment in the Alabash-Konuroleng Depression region near the southern border of the Issyk-Kul hollow on the map of the Kyrgyz Republic. The purpose of the field research work was to study the consequences of a seismic event, to identify violations of the integrity of archaeological structures, and to estimate the strength of an earthquake in a given region. To search for archaeological sites, an aerial photograph of the site along the Akterek River was carried out - from the coast to the elevation of the Duvan Mountains. As a result of field studies in the south of the Issyk-Kul Basin - in the Alabash-Konuroleng Depression, an ancient destroyed complex located on the southern slope of the Duvan mountains was discovered. It turned out that this structure, located on a seismotectonic ledge, was destroyed by it and absorbed by a seismotectonic graben. Most likely, during the period of the complex’s existence in the VII-IX centuries (?), a strong ( I