Гусайлов, Володимир ІгоровичHusaylov, Volodymyr I.2026-08-142026-08-142026Гусайлов В. І. Класифікація форм антропогенного рельєфу на прикладі Малого Аджалицького лиману. Вісник Одеського національного університету. Географічні та геологічні науки. 2026. Т. 31, вип. 1(48). С. 29–40.2303-9914https://dspace.onu.edu.ua/handle/123456789/44738У статті розглядаються підходи до класифікації антропогенних форм рельєфу в прибережних умовах географічної оболонки. Проаналізовано вплив господарської діяльності на формування сучасного рельєфу прибережної зони, зокрема роль гідротехнічних споруд, транспортної інфраструктури, туризму та рекреації. Запропоновано поділити антропогенні форми рельєфу на класи та групи залежно від умов навколишнього середовища та характеру антропогенного впливу. Дослідження проведено на прикладі Малого Аджалицького лиману з використанням вітчизняних та зарубіжних наукових джерел.Problem Statement and Purpose. The article examines the classification of anthropogenic landforms formed in coastal, terrigenous, and thalassogenic environments, with a focus on the Black Sea coastal zone and the Malyi Adzhalytskyi Liman. The impact of human activities on the transformation of modern coastal relief is analyzed, with particular attention to hydraulic engineering structures, transport infrastructure, tourism, and recreation. A classification system is proposed that organizes anthropogenic landforms into classes and groups according to environmental conditions and the nature of human influence. The study is based on long-term field observations and the analysis of domestic and international scientific sources. The purpose of the study is to substantiate approaches to the classification of anthropogenic relief forms in the coastal zone of the Black Sea using the Malyi Adzhalytskyi Liman as a case study. The object of the research is the Black Sea coastline and the water area of the liman, while the subject is the functional, structural, and classification characteristics of anthropogenically transformed landforms. The study area is characterized by intensive economic development and high morphological diversity. Data and Methods. The research is based on long-term geomorphological monitoring of the Black Sea coastal zone, including instrumental field measurements and observations at stationary coastal sites. The analysis covers abrasion and accumulative relief forms at different stages of anthropogenic transformation and allows tracing natural coastal dynamics, morphogenesis during engineering construction, and subsequent transformation of technogenic structures. Results and Analysis. Anthropogenic relief forms develop in terrigenous, coastal, and thalassogenic environments under the combined influence of natural conditions and human activity. The proposed classification distinguishes elementary and complex anthropogenic landforms organized into anthropogeomorphological taxa. Five functional groups of coastal anthropogenic relief are identified: port-related, navigational, coastal protection, recreational, and residential. Hydrotechnical structures significantly transform coastal morphology and lithodynamic processes and affect hydrochemical conditions and biotic components. Anthropogenic landforms are differentiated by spatial orientation, function, size, shape, construction material, origin, interaction with natural relief, and age. Despite overlaps between groups, the classification provides a flexible framework with considerable theoretical and applied potential for coastal geomorphology, environmental assessment, and educational use.ukантропогенний рельєфантропоморфогенезузбережжяморфогенетичне різноманіттякласифікаціяприбережна зонафункціональне призначенняanthropogenic reliefcoastal zonemorphodynamicshydraulic engineeringclassificationgeomorphologyКласифікація форм антропогенного рельєфу на прикладі Малого Аджалицького лимануClassification of anthropogenic landforms : a case study of the Malyi Adzhalytskyi LimanArticlehttps://doi.org/10.18524/2303-9914.2026.1(48).363267551.35(262.5)https://orcid.org/0009-0007-0974-26832415-315X