TOURIST ATTRACTIVENESS OF GEOLOGICAL AND GEOMORPHOLOGICAL OBJECTS OF PRIGORGAN PRECARPATHIAN

G. Bayrak, A. Manko
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Abstract

Geological, geological-geomorphological, geomorphological and hydrological-geomorphological tourist attractions of the Prigorgan Precarpathian are characterized. They are mostly connected with Boryslav-Pokut (Internal) deflection zone, in which due to tectonic thrusts from the Carpathians flysch formations, massive conglomerates, sandstones come to the surface. Geological attractions are unique and typical outcrops of rocks, which reveal the internal structure and history of geological development of the Earth. Unique is the Pniv section of rocks in the form of folds, which reflects the possibility of traps for the accumulation of oil and gas layers. Other sections present rocks of different ages and lithological-facies composition of the local (Carpathian) stratigraphic scale. A notable attraction is the mud volcano from village Starunia which has been awarded the status of a geological monument. Geological and geomorphological attractions include typical or unique landforms in which the section of rocks is revealed and which have cognitive value. These are the terraces of the Prut, in which the root flysch incisions are revealed; mountain tops – observation points, from which the landscape of the Prigorgan Precarpathians opens and geological outcrops are present; rocks of massive rocks – local attractions, some of which, for example, Manyavsky Blessed Stone, have religious significance. Geomorphological tourist attractions include the leveled surfaces of the Precarpathians – Krasna and Loeva, which reflect the stage of geological development of the Carpathians. Presentable geomorphological objects are powerful pre-Carpathian rivers with strata of Quaternary pebbles and manifestations of modern channel processes. Hydrological-geomorphological objects are low waterfalls, of which there are about a dozen in the region and which cut through massive sandstones, conglomerates or flysch deposits. The attractiveness of the described geological and geomorphological objects of the Prigorgan Precarpathians has been assessed. The evaluation criteria were popularity, proximity to highways, cognitive value, size, landscape. Of the 27 objects, 8 have high, 13 medium and 6 low attractiveness. The described geotourism attractions have scientific, educational, environmental and recreational significance. It is advisable to involve them in the system of tourist routes of the Carpathian region. Key words: geotourism; geological, geomorphological, hydrological, complex attractions; Prigorgan Precarpathian.
普里根山岗地质地貌对象的旅游吸引力
对普里戈尔根不稳定巴阡山脉的地质、地质地貌、地貌和水文地貌旅游景点进行了描述。它们大多与Boryslav-Pokut(内)偏转带有关,在喀尔巴阡山脉复理石组的构造逆冲作用下,大块砾岩、砂岩涌出地表。地质景点是独特而典型的岩石露头,它揭示了地球的内部结构和地质发展史。独特的是Pniv剖面的岩石褶皱形式,这反映了油气层聚集的圈闭可能性。其他剖面显示了不同时代的岩石和当地(喀尔巴阡山脉)地层尺度的岩性相组成。一个引人注目的景点是斯塔努尼亚村的泥火山,它已被授予地质纪念碑的地位。地质和地貌景点包括典型的或独特的地貌,其中露出了岩石的剖面,并具有认知价值。这些是普鲁特的梯田,在那里可以看到根理石的切口;山顶——观察点,从这里可以看到Prigorgan Precarpathians的景观和地质露头;巨大的岩石-当地的景点,其中一些,例如,马尼亚夫斯基祝福石,具有宗教意义。地貌旅游景点包括不稳定的喀尔巴阡山脉-克拉斯纳和洛耶娃的平整表面,这反映了喀尔巴阡山脉的地质发展阶段。可见的地貌对象是强大的前喀尔巴阡河,具有第四纪卵石地层和现代河道作用的表现。水文地貌学研究对象是低矮的瀑布,该地区大约有十几个这样的瀑布,它们穿过大块的砂岩、砾岩或复理岩沉积物。对所描述的普里格根无头山的地质和地貌对象的吸引力进行了评估。评价标准为知名度、临近公路、认知价值、规模、景观。在27个对象中,8个具有高吸引力,13个具有中等吸引力,6个具有低吸引力。所描述的地质旅游景点具有科学、教育、环境和娱乐意义。将他们纳入喀尔巴阡地区的旅游路线系统是明智的。关键词:地质旅游;地质、地貌、水文、复杂景点;Prigorgan Precarpathian。
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