The purpose of the study is to determine the prerequisites for the formation of agritourism in the Zaporozhye region, to identify the features of territorial organization and understanding of its regional uniqueness. Research methods and techniques. The study of the territorial organization of agritourism at the regional level is based on two methodological approaches: dialectical and territorial. At the analytical and synthetic stages, the methods of correlation analysis and cartographic modeling, the comparative-geographical method and the method of computer technologies were used. Results. The region has a strong tourist and resource potential for the development of agritourism - in fact, in every district of the region there are rural green estates and tourist attractions. It is proved that the maximum effect of sustainable development can be achieved only if agritourism develops not spontaneously, but within the framework of relevant programs of state, interregional and regional significance. Otherwise, local projects in the field of agritourism in the current conditions of lack of financial resources will be slowed down by uncontrolled development. The idea of the role of rural (green) tourism in the conditions of reset of national and regional recreation caused by the planetary pandemic is deepened and the laconic map of the spatial organization of rural (green) tourism of the region is offered. The practical significance of the study lies in the implementation of its results in the educational process (in teaching courses "tourism organization", "excursion activities", "rural green tourism organization") at geographical, historical faculties of higher education institutions of Ukraine) and the use of article materials in travel companies , excursion establishments and public associations of Ukraine, in strengthening public attention to modern types of recreation and features of their organization. Scientific novelty. The main trends and features of territorial location of agro-villages in accordance with the tourist and recreational potential of Zaporizhia region are highlighted, a cartographic model of spatial organization of rural (green) tourism in the region is introduced.
The area of the Pologivskiy deposit of kaolins and refractory clays is located on the border of two geological regions: the Azov crystalline massif and the Konksko-Yalynska depression. Precambrian crystalline rocks and sediments of the Cretaceous, Paleogene, Neogene, and Quaternary systems take part in the geological structure of the district. The geological structure of the district is based on the results of field exploration (23–25) and geological surveying works. Deposits of the Quaternary system are widespread in the territory and are similar to mantle on the underlying rocks. The lower border of the Quaternary system is formed at the base of the Berezanskiy climatolite in accordance with the Geological Map of Ukraine legend (the scale 1:200 000) of the 1996 Central Ukrainian series. The underlying rocks are red-brown Pliocene clays in most parts of the territory, in the rest there are rocks of crystalline basement of Cretaceous, Paleogene and Neogene systems. The thickness of the Quaternary deposits is 10–20 m. Deposits of the Novopetrivska Neogene suite are productive for the extraction of clays and kaolins, in the base of which the undivided deposits of the Upper Eocene (Kyivska suite) and Oligocene (Kharkivska suite) lie. These are coastal-marine deposits – marls, calcareous clays, siltstones, weakly cemented sandstones and glauconite quartz sands. The total thickness of the Kyivska and Kharkivska suites varies from 0,0 to 60–70 m. Clays and kaolins are characterized by almost the same mineral composition. Most of them are composed of fine-grained kaolinite, and quartz predominates among impurities. Accessory and ore minerals are represented by zircon, rutile, ilmenite and hematite. Quartz is present in clays and kaolins in the form of rolled, semirolled and unrolled grains. High-quality aluminosilicate products are obtained from the kaolins of the deposit. Pologivskiy kaolin can be used to make chamotte without the clay addition, as well as a binder. The ratio of chamotte and binder is 80–20 %. The refractories obtained in the laboratory meet the requirements of high density for Class A blast furnace bricks and other products of appropriate determination. Pologivskiy clays are recognized as suitable for the production of 100 % refractories, as well as a binder component instead of ChasovYarska clays. Products made entirely of semi-acid clay meet the requirements for semi-acid refractory products of class B. Pologivskiy kaolins and clays have long been used in refractory, machine-building, ceramic, cement and other industries.
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