Summary
Researchers have identified 14 distinct landscape facies types in the Sheki–Zagatala region of Azerbaijan, highlighting significant variations in soil chemistry and biogeochemical processes across elevations from 500 to 2000 meters. The study reveals that high-altitude eluvial systems experience intense leaching, leading to nutrient depletion and accelerated desertification on carbonate-rich substrates. Conversely, subaquatic and waterlogging-prone facies exhibit hydromorphic conditions that promote organic matter accumulation, enriching soils with nitrogen, phosphorus, and potassium. This classification integrates lithological-geomorphological, hydrological, and biological factors, applying V. V. Kovalsky's biogeochemical methodology to map chemical element distribution. The findings underscore the interplay between microclimatic variations and tectonic influences in shaping landscape dynamics within this UNESCO World Heritage Site.
Citation
Mustafabeyli, H., & Gahramanov, M. (2026). Classification of Landscape Facies Types (Based on the Example of the Sheki–Zagatala Region of Azerbaijan). Bulletin of Science and Practice, 12(9), 95–108. https://doi.org/10.33619/2414-2948/130/10