PROBLEMS OF GEOMORPHOLOGY AND PALEOGEOGRAPHY OF THE UKRANIAN CARPATHIANS AND ADJACENT AREAS最新文献

{"title":"STEPAN RUDNITSKY'S STUDIES OF THE PODILLYA RELIEF: ITS MORPHOLOGY, GENESIS AND HISTORY OF DEVELOPMENT","authors":"Y. Kravchuk, Y. Zinko","doi":"10.30970/gpc.2019.1.2796","DOIUrl":"https://doi.org/10.30970/gpc.2019.1.2796","url":null,"abstract":"S. Rudnitsky’s research continued in Podillya; he went on studying the morphology of genesis and history of the relief of the Carpathian and pre-Carpathian Dniester basins. Many years of expeditionary research (1903-1912) resulted in the monograph “Prerequisites for Studying Morphology of the Podilsky Catchment Area of the Dniester”, which was recommended for publication at the meeting of the Mathematical & Nature Descriptive section of the Shevchenko Scientific society (NTSh) on April 17, 1912.\u0000This work provides detailed morphographic and morphometric characteristics of the Galician Podillya relief. The monograph also reports on the formation of the Dniester basin river system, geological structure, paleogeomorphology, as well as morphological & genetic problems.\u0000In studying the Podilsky Dniester Basin, S. Rudnytsky made numerous conclusions on the problems of morphological regionalization, the relief history, in particular the formation of the Dniester valley and its Podilsky tributaries, which have not lost their relevance to this day. We can distinguish the following major points among the main findings of S. Rudnitsky's research of morphogenesis and the evolution of the Podilsky Dniester basin relief: (1) Geomorphological division of the Galician Podillya with districts allocation: Roztochya, Vereshchytsky-Shchyrets lowland, Mykolayiv-Bobretskyi “horbovyna” (land surface with hills) (Pidopillya), Opilsky “horbovyna”, Podnistriya, Podillya and Gogoloro-Kremenetsk Ridge; (2) Clarification of the history of individual regions development: the erratic Scandinavian material in Roztochya is mixed (Scandinavian-Carpathian); it is deposited by fluvia-glacial flows and represented up to altitudes of 380 m; (3) In the periglacial Pleistocene period, almost all the sands of the main areas had eolian processes; (4) Confirmation of the Podillya geological division into western and eastern with five morphological bands, proposed by W. Teisseyre; (5) Justification of the morphotectonic scheme of Podillya development, connected with tectonic elevations of the Hologoro-Kremenets Ridge, which caused the current inclination of the Podolsk hills to Southeast-East; (6) Statement that the tectonic lines of Berdo-Nârul and Kovalivka-Smykivtsi characterize the Paleozoic Platform of Podillya as a typical tectonic horst; (7) Detailed description of the Dniester “rinyshcha” (alluvial deposits) with the Carpathian material present in Podniester, Opil and Podillya itself, which are present as a strip at a distance of 14-20 km from the modern Dniester river bed; (8) Based on literary sources and his own research, the scientist came to the conclusion that there is “eolian” loess in the “rinyshcha”, sands and alluvial clay; (9) It is argued that the old Nadnistryan rivers cannot be older than the planation surfaces of the Carpathians and Pre-Carpathians; (10) Formation of the Dniester valley pattern in Pliocene and Pleistocene, which determined the direction of the flows ","PeriodicalId":374629,"journal":{"name":"PROBLEMS OF GEOMORPHOLOGY AND PALEOGEOGRAPHY OF THE UKRANIAN CARPATHIANS AND ADJACENT AREAS","volume":"16 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2019-09-25","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"131093217","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"MORPHOLOGIC CLASSIFICATION OF THE BESKIDS ROCKS \u0000IN THE UKRAINIAN CARPATHIANS","authors":"G. Bayrak","doi":"10.30970/gpc.2019.1.2806","DOIUrl":"https://doi.org/10.30970/gpc.2019.1.2806","url":null,"abstract":"The article deals with morphological classification of the sandstone rocks in the Ukrainian Carpathians Beskids. By the methods of field measurements and mathematical computations the rock peaks heights, their shape, basement lengths and strata thickness have been calculated. The highest rock peaks in the Beskids amounts 32–37 m. The classification from the morphological point of view on the base of rock forms studying has been done. All rocks are divided in two classes: the rocks-outliers and the rocks-outcrops. Among the rocks-outliers 4 types are defined: spire-shaped, chain-shaped, arc-shaped and combined. Spire-shaped rocks are divided into subtypes: tower, spoke and needle. Among the chain-shaped rocks 3 subtypes are defined: wall, bloc and slab. The rocks of combined form are divided into subtypes: 1) with defined form – those of the rocks which are similar to certain objects and 2) undefined forms (cliffs). Among the rocks-outcrops three types are defined: cliff-shaped, canyon-shaped and angular ones. The class of rocks-outliers occurs most often. Among the types the rocks-towers occur most often. They dominate in the rock formations of Urych, Yamelnytsia and Bubnyshche. Many bloc-shaped and plate-shaped rocks are located on the Kliuch Ridge, in Bubnys’ki Rocks, Yamelnytsia. There are rocks-walls of 50–60 m in Urych and Yamelnytsia. The longest rock-wall in Danylov tract near Yamelnytsia has been investigated. Its length is 150 m and height is 17 m. Some needle and spoke rocks are situated in Bubnys’ki Rocks (Odinets’ Rock, Golets’ Rock) and Urych (Hostryi Kamin’ (Sharp Stone) Rock. Unique types are very rare. For instance: Bronenosets’ Rock in Bubnys’ki Rocks (this rock has shape of sail), Sokil (Falcon) Rock in the Kliuch Ridge, mushroom-shaped rock in Yamelnytsia. There is also unique arc-rock in the Kliuch Ridge. In the class of rocks-outcrops the types of cliff and canyon occur equally. The angular-shaped rocks are rarer. The cliff-shaped rocks are situated near Sokolova Mountain, Pozhernytsia Mountain and Kniazhi (Princes) Rocks near Tyshivnytsia. Unique rocks-canyons, the effects of tectonic breaking and gravity-erosion processes, occur on the Kliuch Ridge. The worked out morphological classification of rocks can be used by ascertaining features of rock morphogenesis with education and scientific purposes as well as by assessment of safety level and protection possibilities. Morphological types of the rocks can be considered as valuable objects of geomorphologic heritage and attractions for geo-tourism. \u0000Key words: rocks; morphology type of the rock; rock shape; Beskids of Ukrainian Carpathians.","PeriodicalId":374629,"journal":{"name":"PROBLEMS OF GEOMORPHOLOGY AND PALEOGEOGRAPHY OF THE UKRANIAN CARPATHIANS AND ADJACENT AREAS","volume":"22 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2019-09-25","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"121781381","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"THE MONUMENTS OF NON-LIVING NATURE OF THE BASINS OF PRUT AND LAZESHCHYNA RIVERS IN CHORNOHORA MOUNTAIN RANGE IN UKRAINIAN CARPATHIANS","authors":"V. Brusak, D. Senychak","doi":"10.30970/gpc.2019.1.2807","DOIUrl":"https://doi.org/10.30970/gpc.2019.1.2807","url":null,"abstract":"The classification of the monuments of non-living nature of the basins of Prut and Lazeshchyna rivers in Chornohora mountain range in Ukrainian Carpathians as well as map, tables and suggestions for further alternative use of objects are presented. In the\u0000research the monuments of non-living nature are categorized such as geological, geomorphological and hydrological based on the main object of their value for protection. \u0000The classification of the geological and geomorphological monuments according to different principles such as meaningful, scientific and cognitive significance, genetic, purpose and size is developed. According to the main object of their value for protection and the genesis objects are classified into types of monuments, and by morphological expression – into species of monuments. The other methods of the research of monuments of non-living nature such as cartographic inventory and comprehensive certification are also presented.\u0000The river basins of Prut and Lazeshchyna are located on the northeast macro-slope of the Chornohora mountain range in the Ukrainian Carpathians in the area of the Carpathian Biosphere Reserve and the Carpathian National Nature Park. On the territory of the studied river basins 11 geological monuments, 23 – geomorphological monuments, 7 – hydrological and hydrogeological monuments are identified. There are also 9 sites of fir forests and 14 sites of ancient forests protected in the Carpathian Biosphere Reserve in the Lazeshchyna river basin. On the territory of the Prut river basin there are 81 sites of ancient forests and primeval forests in the area of the Carpathian National Nature Park.\u0000The monuments of non-living nature can be used not only as the conservation ones but also as the places for recreation and tourism, organization of research and environmental education of the region. In addition, 2 multi-day, 1 two-day and 9 one-day geotourism routes to promote the natural resources of the studied river basins with the purpose to reduce the recreational degression of the main eco-trail “To the Goverla Mountain” are developed. \u0000Key words: monuments of non-living nature; geological sites; Chornohora mountain range; Prut river basin; Lazeshchyna river basin; geotourism route.","PeriodicalId":374629,"journal":{"name":"PROBLEMS OF GEOMORPHOLOGY AND PALEOGEOGRAPHY OF THE UKRANIAN CARPATHIANS AND ADJACENT AREAS","volume":"80 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2019-09-20","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"122314662","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"ANALYSIS OF RELIEF MORPHOLOGY OF UKRAINIAN CARPATHIANS THROUGH THE METHOD OF AUTOCOVARIOGRAMS","authors":"O. Mkrtchian","doi":"10.30970/GPC.2018.08.2026","DOIUrl":"https://doi.org/10.30970/GPC.2018.08.2026","url":null,"abstract":"","PeriodicalId":374629,"journal":{"name":"PROBLEMS OF GEOMORPHOLOGY AND PALEOGEOGRAPHY OF THE UKRANIAN CARPATHIANS AND ADJACENT AREAS","volume":"62 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2018-10-02","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"130667423","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"METHODOLOGICAL ASPECTS OF THE RESEARCH OF RECREATIONAL DEGRESSION OF MICRORELEIF OF THE TOURIST’S ROUTES","authors":"V. Brusak","doi":"10.30970/gpc.2018.08.2019","DOIUrl":"https://doi.org/10.30970/gpc.2018.08.2019","url":null,"abstract":"","PeriodicalId":374629,"journal":{"name":"PROBLEMS OF GEOMORPHOLOGY AND PALEOGEOGRAPHY OF THE UKRANIAN CARPATHIANS AND ADJACENT AREAS","volume":"1 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2018-10-02","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"130561341","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"THE QUANTITATIVE EVALUATION OF DENUDATION IN THE PODILLYA PART OF THE DNISTER RIVER BASIN (AN EXAMPLE OF KOROPETS RIVER)","authors":"I. Kovalchuk, O. Pylypovych, Y. Andreychuk","doi":"10.30970/gpc.2018.08.2015","DOIUrl":"https://doi.org/10.30970/gpc.2018.08.2015","url":null,"abstract":"","PeriodicalId":374629,"journal":{"name":"PROBLEMS OF GEOMORPHOLOGY AND PALEOGEOGRAPHY OF THE UKRANIAN CARPATHIANS AND ADJACENT AREAS","volume":"71 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2018-10-02","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"126822019","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"GEOTOURIST RESOURCES OF NATURE PROTECTION TERRITORIES IN ZAKARPATTIA REGION","authors":"L. Dubis, N. Habchak, Marek Solski","doi":"10.30970/gpc.2018.08.2029","DOIUrl":"https://doi.org/10.30970/gpc.2018.08.2029","url":null,"abstract":"","PeriodicalId":374629,"journal":{"name":"PROBLEMS OF GEOMORPHOLOGY AND PALEOGEOGRAPHY OF THE UKRANIAN CARPATHIANS AND ADJACENT AREAS","volume":"21 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2018-10-02","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"126199194","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"TRANSFORMATION OF RELIEF RECREATION TERRITORIES AND RECOMMENDED MEASURES FOR REGULATION OF NEGATIVE PROCESSES","authors":"I. Gnatyak","doi":"10.30970/gpc.2018.08.2023","DOIUrl":"https://doi.org/10.30970/gpc.2018.08.2023","url":null,"abstract":"","PeriodicalId":374629,"journal":{"name":"PROBLEMS OF GEOMORPHOLOGY AND PALEOGEOGRAPHY OF THE UKRANIAN CARPATHIANS AND ADJACENT AREAS","volume":"26 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2018-10-02","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"132409828","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"ISSUES FROM HISTORY OF THE UKRAINIAN CARPATHIAN RELIEF DEVELOPMENT","authors":"Y. Kravchuk","doi":"10.30970/gpc.2018.08.2011","DOIUrl":"https://doi.org/10.30970/gpc.2018.08.2011","url":null,"abstract":"","PeriodicalId":374629,"journal":{"name":"PROBLEMS OF GEOMORPHOLOGY AND PALEOGEOGRAPHY OF THE UKRANIAN CARPATHIANS AND ADJACENT AREAS","volume":"12 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2018-10-02","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"133176953","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"MONUMENTS OF NON-LIVING NATURE AND HISTORICAL-CULTURAL OBJEKTS OF THE REGIONAL LANDSCAPE PARK «RAVSKE ROZTOCHIA»: CONDITION OF CONSERVATION AND PROSPECT OF RECREATIONAL USE","authors":"V. Brusak, D. Krychevska, S. Blahodyr","doi":"10.30970/GPC.2018.08.2020","DOIUrl":"https://doi.org/10.30970/GPC.2018.08.2020","url":null,"abstract":"","PeriodicalId":374629,"journal":{"name":"PROBLEMS OF GEOMORPHOLOGY AND PALEOGEOGRAPHY OF THE UKRANIAN CARPATHIANS AND ADJACENT AREAS","volume":"52 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2018-10-02","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"130680604","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}