Quaternary Sediments in Geosites: Evidence from the Western Caucasus

Quaternary sediments in the Western Caucasus, particularly within Mountainous Adygeya, hold significant geoheritage value despite being overshadowed by more prominent pre-Quaternary features. This study highlights three distinct localities—Rufabgo Canyon, Dakh–Sakhray Confluence, and Stonesea Range—that exhibit unique colluvial, alluvial, and eluvial–deluvial sediments, respectively. These sediments, characterized by their origin, scientific importance, and accessibility, provide insights into local Quaternary sedimentation patterns. Beyond their academic utility, these geosites serve as educational tools for sedimentology training and attract tourists due to their aesthetic appeal. The findings underscore the need to integrate Quaternary features into broader geoheritage assessments, ensuring a comprehensive understanding of the region's geological diversity.

Ruban, D. A. (2023). Quaternary Sediments in Geosites: Evidence from the Western Caucasus. Heritage, 6(5), 3903–3920. https://doi.org/10.3390/heritage6050207