Traces of Seismic Impacts in the Walls of the Ulugbek Madrassa (Samarkand, Uzbekistan)

This article considers the results of a macroseismic survey of one of the oldest buildings in Samarkand, the Ulugbek Madrassa, built in 1417–1420 by Ulugbek, the beloved grandson of Emir Timur. Despite the ongoing restoration work since the 1920s, the madrassaʼs building structures have retained traces of seismic impacts, in particular, the tilt of the arched complex of the southern wall to the south and the arched complex of the eastern wall to the east. Until the mid-1960s (when it was straightened), the southeastern minaret was tilted to the south-southeast. Based on these facts, we have concluded that the source of seismic oscillations responsible for the aforementioned damage was located south-southeast of Samarkand, at the western end of the Zeravshan range. Judging by the data available in the seismic catalogs, it may be an earthquake that occurred in 1817–1818, the local seismic intensity of which was Il = VIII– IX in the city.

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Publication Details

Journal
Izvestiya Atmospheric and Oceanic Physics
Published
2024-12-01
DOI
https://doi.org/10.1134/s0001433825700574
Primary Topic
Engineering and Agricultural Innovations
Type
article
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article

Traces of Seismic Impacts in the Walls of the Ulugbek Madrassa (Samarkand, Uzbekistan)

L. A. Korzhenkova, А. М. Корженков, M. M. Saidov, A. A. Nazarov et al.
Izvestiya Atmospheric and Oceanic Physics
Engineering and Agricultural Innovations
article

Traces of Seismic Impacts in the Walls of the Ulugbek Madrassa (Samarkand, Uzbekistan)

L. A. Korzhenkova, А. М. Корженков, M. M. Saidov, A. A. Nazarov, A. A. Anarbayev
article en

Abstract

This article considers the results of a macroseismic survey of one of the oldest buildings in Samarkand, the Ulugbek Madrassa, built in 1417–1420 by Ulugbek, the beloved grandson of Emir Timur. Despite the ongoing restoration work since the 1920s, the madrassaʼs building structures have retained traces of seismic impacts, in particular, the tilt of the arched complex of the southern wall to the south and the arched complex of the eastern wall to the east. Until the mid-1960s (when it was straightened), the southeastern minaret was tilted to the south-southeast. Based on these facts, we have concluded that the source of seismic oscillations responsible for the aforementioned damage was located south-southeast of Samarkand, at the western end of the Zeravshan range. Judging by the data available in the seismic catalogs, it may be an earthquake that occurred in 1817–1818, the local seismic intensity of which was Il = VIII– IX in the city.

Izvestiya Atmospheric and Oceanic PhysicsVol. 60(11)
Samarkand State University named after Sharof Rashidov (UZ), Academy of Sciences Republic of Uzbekistan (UZ), Sergeev Institute of Environmental Geoscience (RU), Samarkand Institute of Veterinary Medicine (UZ), Schmidt Institute of Physics of the Earth (RU)
Sustainable cities and communities
Openalex Percentile: Top 72%
Engineering and Agricultural Innovations
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Traces of Seismic Impacts in the Walls of the Ulugbek Madrassa (Samarkand, Uzbekistan) — L. A. Korzhenkova, А. М. Корженков, et al. · Izvestiya Atmospheric and Oceanic Physics (2024) | TGRS Research Map | TGRS