Key Characteristics of the Ecological and Geodynamic Conditions in Southern Karakalpak Ustyurt of Uzbekistan

This article addresses a pressing issue—the study of ecological and geodynamic conditions in the southern part of the Uzbekistan Republic of Karakalpakstan Ustyurt plateau. The article synthesizes and systematizes the findings from both archival and personal research on the current state of ecological and geodynamic conditions. A schematic map of ecological–geodynamic conditions has been developed to assess the manifestation of various processes and their impact on the region’s flora and fauna, as well as on engineering and geological conditions relevant to mineral development and human economic activities. The overarching methodology involves system analysis and mapping of the natural-geological environment and geodynamically active zones. The primary criteria for evaluation include the state of the landscape, soil-grounds, and soil-forming rocks. The ecosystem serves as a nutrient base for plants and a fodder base for livestock development. In the Karakalpak Ustyurt, precipitation distribution is uneven, with annual precipitation ranging from 200–220 mm in the central and northern parts to 120–140 mm in the southern part. The Karakalpak Ustyurt presents morphological challenges related to the study of the nature of the relief, surface runoff, and the composition, state, and properties of the soil massif, including its ecological and geodynamic indicators. This study aims to provide a comprehensive understanding of the region’s ecological dynamics, contributing to sustainable development and conservation efforts. Thus, the conducted studies have revealed geodynamic processes associated with both natural geological phenomena and human engineering or economic activities. In principle, ecological geodynamics and engineering geodynamics rely on the same geological information to assess the manifestation of these processes