Багмет, О. Б.О. Б.Багмет2026-01-072026-01-072017Багмет О. Б. Типи берегових геоморфосистем дніпровських водосховищ. Фізична географія та геоморфологія. 2017. Вип. 4 (88). С. 40-44.УДК 911.574https://ir.library.knu.ua/handle/15071834/9489Створення Дніпровського каскаду водосховищ спричинило масштабну трансформацію природного рельєфу та істотно вплинуло на хід екзогенних процесів. В умовах зростання техногенного навантаження на рельєф моніторинг та прогноз розвитку екзогенних процесів належать до числа найважливіших прикладних завдань геоморфології.The construction of the Dnipro cascade of reservoirs caused one of the largest transformations of natural relief in Ukraine. The result of which was the following: regional activation of land flooding (an area of over 1 million hectares); strengthening of erosion processes, abrasion of shores of reservoirs; the development of dangerous exogenous relief-forming processes (landslide, sinking and suffosion). An increase of the water-edge in the Dnipro river has led to a sharp and significant increase of the local base level of erosion. As a result, a new coastline with a total length of about 3,5 thousand km was formed. More than a third of which is actively damaged by denudation, especially abrasive and erosive processes, and needs protection. In this area there are more than 190 settlements where more than 600 thousand inhabitants live. Such excessive anthropogenic loading on the Dnipro basin disturbed its natural balance and greatly increased the risk of developing dangerous exogenous processes, caused the ecological state crisis of many territories. In conditions of increasing technogenic loading on the relief monitoring and forecast of the development of exogenous processes are among the most important applied objectives of geomorphology. The features of the formation of the banks of reservoirs are influenced by a number of factors, the most important of which are: geomorphological conditions (confinement to certain forms of relief, dissection of the coast, slope steepness, spectrum and intensity of manifestation of exogenous processes); the lithologic composition of the rocks involved in the structure of the shores; wave mode and level reservoir regime. The combined influence of these and other factors is determined by: the local features of the reformation of the banks, the development of complexes of exogenous processes with distinctions of their activity and formation of certain forms of relief. Depending on the characteristics of local interaction of geomorphologic-geological factors, the dominant types of coastal processing, which are determined by the interaction of coastal slopes and water masses of reservoirs, for the Dnipro cascade we distinguish the following genetic types of coastal systems: 1) abrasive-slump; 2) abrasive-talus; 3) abrasive-slump-talus; 4) abrasive-denudation; 5) abrasive slide; 6) erosive; 7) accumulative; 8) neutral; 9) protected.ukберегові геоморфосистемитрансформація берегівводосховищеабразіяпрогнозtransformation of relieftechnogenesisreservoirabrasionСтаття