This study presents a retrospective analysis of vertical crustal movements in the Caucasus for the period 1925–2023, based on geodetic leveling, GNSS observations, and satellite interferometry
(InSAR). Spatial–temporal patterns of surface uplift and subsidence, reflecting the development of orogenic processes in the region, were identified through mapping. It is established that the central part of the Caucasus has been characterized by stable uplift (up to 10–12 mm/year) throughout the entire period, whereas peripheral zones demonstrate subsidence of varying intensity. A comparative analysis of seismicity revealed a correlation between anomalous vertical deformations and the foci of strong earthquakes, confirming their possible role as indicators of seismic hazard. Particular attention is given to the correlation of vertical tectonic movement phases with major seismic events of the 20th–21st centuries, including earthquakes in Armenia, Dagestan, Georgia, as well as adjacent areas of Turkey and Iran. The results emphasize the need for integrated monitoring using modern geodetic and remote sensing techniques to assess seismic risk in the Caucasus.
Caucasus vertical crustal movements orogenic processes geodetic leveling GNSS InSAR seismicity seismic hazard geodynamics tectonic deformation.
| Primary Language | English |
|---|---|
| Subjects | Seismology and Seismic Exploration, Geophysics (Other) |
| Journal Section | Research Article |
| Authors | |
| Submission Date | October 8, 2025 |
| Acceptance Date | October 30, 2025 |
| Early Pub Date | December 22, 2025 |
| Publication Date | December 22, 2025 |
| Published in Issue | Year 2026 Issue: Advanced Online Publication |
The journal is intended for seismologists, geophysicists and geochemists of scientific and industrial organizations dealing with seismology, earthquake prediction, seismic zoning and earthquake-resistant construction.
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