Плешакова, А. О.А. О.Плешакова2025-12-252025-12-252017Плешакова А. О. Морфоструктури центрального типу Керченського півострова. Фізична географія та геоморфологія. 2017. Вип. 2 (86). С. 67-70.УДК 551.4https://ir.library.knu.ua/handle/15071834/9028Дослідження латеральної організації будови земної поверхні, зокрема виділення морфоструктур центрального типу в межах Керченського півострова дозволило провести кореляцію з геологічною та геоморфологічною будовою, встановити зв’язок з поширенням корисних копалин та осередкків грязевого вуланізму.The article describes the lateral organization of the earth's surface, specifically, the morphostructures of the central type, of the Kerch Peninsula. It allowed a correlation between morpostructures and the geological and geomorphological structure, to establish connection with minerals and mud volcanism. In this article, I used the scientific approach to the morphostruvtures analysis created by a scientific school of the Department of Geomorphology of the Taras Shevchenko National University of Kyiv, HoD S. Bortnik. Accordingly, by the morphostructure is understood the integral characteristic of the natural object (the area of the earth's surface) - its vertical and lateral organization, due to the tectonic, geological structure, natural and human-induced evolution, geodynamic regime. During the research were allocated 3 first-order regional morphostructures of the central type and 6 second-order regional morphostructures of the central type. The morphostructures of the Kerch Peninsula are similar to its geological structure. Different southwest and north-eastern parts also differ at the morphostructural plan. The eastern submerging of the anticline of the Crimean mountainous controls the chain of second-order regional morphostructures of the central type, on the platform northeastern part of the peninsula the second-order regional morphostructure of the central type number 5 is allocated within the Kerch syncline. The local relief is relatively young, the morphostructure is not sufficiently clearly expressed in the relief. The coastline in most cases is controlled by arc lineaments: the Bat Sea Bay, the Kamysh-Burun Bay and the first-order regional morphostructures of the central type and their centers: the Feodosian and the Kazantipian Gulfs. There are numerous salty lakes confined to the coastal areas of the regional morphostructures of both orders. Scientific researches prove the connection between morphostructures and occurrence of oil and gas, iron ores, which gives grounds to consider the morphostructural research of the Kerch Peninsula very important.ukморфоструктурна картаморфоструктураморфоструктура центрального типулінеаментморфоструктурний аналізбудова морфоструктурmorphostructural mapmorphostructure central typelineamentmorphostructural analysisthe structure of morphological structuresСтаття