Javascript must be enabled to continue!
ASSESSMENT OF THE ATTRACTIVENESS OF GEOTOURISTIC AREAS OF THE UKRAINIAN CARPATHIANS’ BESKID MOUNTAINS
View through CrossRef
For the purpose of organizing geotourism trips, geological and geomorphological objects of the Beskydy of the Ukrainian Carpathians were studied. Seven geotourism areas were identified, such as: Urytskyi, Yamelnytskyi, Syniovydnenskyi, Skole, Kliucha-Kamiankyi, Bubnyskyi and Rozgirche. Each of them characterizes morphological features of geomorphological objects, composition and structure of rocks, describes certain historical and cultural events related to them. To determine the tourist attractiveness of geological and geomorphological sites, an assessment methodology was developed based on the following indicators: the number of geological sites, their maximum heights, accessibility, picturesqueness (scenic beauty), visibility (sites as a vantage point of the area), scientific, educational, historical and cultural value, tourist infrastructure, popularity and tourist attendance. The analysis revealed that the most attractive tourist area within the study area is the Urytskyi tourist district, which, due to its picturesque cliffs with high historical and cultural value, has a significant number of tourists. In second place is the Bubnyskyi geotourism area, which has the largest number of the highest and most picturesque rocks. In third place is the Skole geotourism district, which has seven geo-attractions and is best equipped with tourist infrastructure facilities. The Kliucha-Kamianka area has an above-average attractiveness, with the largest number of different types of objects within its boundaries. It is the most popular and most visited by tourists. The tourist attractiveness of the Syniovydnianskyi geotourism area is somewhat less than the previous one, but there are outcrops among the geoattractions that have a high scientific and educational value. The Yamelnytskyi district has little attractiveness, it is little known, and the tourist infrastructure is poorly developed, but there are many rocks of different morphological types. Compared to other districts, the geotourism attractiveness of the Rozhirche district is low.
The assessment of the attractiveness of the selected tourist areas showed that the highest scores were given to areas where geological and geomorphological objects are morphologically more diverse, with significant morphometric indicators, high landscape value, geological representation of the Carpathian structure, and various sedimentary and anthropogenic signs on the rock surface.
Keywords: geological and geomorphological objects; geo-tourism; geo-attraction; tourist attractiveness; Ukrainian Carpathians’ Beskid Mountains.
Ivan Franko National University of Lviv
Title: ASSESSMENT OF THE ATTRACTIVENESS OF GEOTOURISTIC AREAS OF THE UKRAINIAN CARPATHIANS’ BESKID MOUNTAINS
Description:
For the purpose of organizing geotourism trips, geological and geomorphological objects of the Beskydy of the Ukrainian Carpathians were studied.
Seven geotourism areas were identified, such as: Urytskyi, Yamelnytskyi, Syniovydnenskyi, Skole, Kliucha-Kamiankyi, Bubnyskyi and Rozgirche.
Each of them characterizes morphological features of geomorphological objects, composition and structure of rocks, describes certain historical and cultural events related to them.
To determine the tourist attractiveness of geological and geomorphological sites, an assessment methodology was developed based on the following indicators: the number of geological sites, their maximum heights, accessibility, picturesqueness (scenic beauty), visibility (sites as a vantage point of the area), scientific, educational, historical and cultural value, tourist infrastructure, popularity and tourist attendance.
The analysis revealed that the most attractive tourist area within the study area is the Urytskyi tourist district, which, due to its picturesque cliffs with high historical and cultural value, has a significant number of tourists.
In second place is the Bubnyskyi geotourism area, which has the largest number of the highest and most picturesque rocks.
In third place is the Skole geotourism district, which has seven geo-attractions and is best equipped with tourist infrastructure facilities.
The Kliucha-Kamianka area has an above-average attractiveness, with the largest number of different types of objects within its boundaries.
It is the most popular and most visited by tourists.
The tourist attractiveness of the Syniovydnianskyi geotourism area is somewhat less than the previous one, but there are outcrops among the geoattractions that have a high scientific and educational value.
The Yamelnytskyi district has little attractiveness, it is little known, and the tourist infrastructure is poorly developed, but there are many rocks of different morphological types.
Compared to other districts, the geotourism attractiveness of the Rozhirche district is low.
The assessment of the attractiveness of the selected tourist areas showed that the highest scores were given to areas where geological and geomorphological objects are morphologically more diverse, with significant morphometric indicators, high landscape value, geological representation of the Carpathian structure, and various sedimentary and anthropogenic signs on the rock surface.
Keywords: geological and geomorphological objects; geo-tourism; geo-attraction; tourist attractiveness; Ukrainian Carpathians’ Beskid Mountains.
Related Results
Geological and geomorphological objects of the Ukrainian Carpathians’ Beskid Mountains and their tourist attractiveness
Geological and geomorphological objects of the Ukrainian Carpathians’ Beskid Mountains and their tourist attractiveness
The article explores the geological and geomorphological objects of the Beskidy Ukrainian Carpathians for the further creation of geo-tourist routes. Geo-tourist areas combining se...
HIGH MOUNTAINS OF THE UKRAINIAN CARPATHIANS: STATE AND PROBLEMS OF CONCEPTS AND TERMINOLOGY
HIGH MOUNTAINS OF THE UKRAINIAN CARPATHIANS: STATE AND PROBLEMS OF CONCEPTS AND TERMINOLOGY
The problems of misreading and use of the term "high mountains" in science are considered. Under the conceptual and terminological apparatus is understood the scientific language o...
SPECIFIC TRAITS OF HUNGARIAN-UKRAINIAN POETRY TRANSLATION (BASED ON YURII SHKROBYNETS’ TRANSLATIONS)
SPECIFIC TRAITS OF HUNGARIAN-UKRAINIAN POETRY TRANSLATION (BASED ON YURII SHKROBYNETS’ TRANSLATIONS)
The article addresses matters related to the peculiarities of Hungarian-Ukrainian poetic translation. It was noted that the quality, complexity and overall mastery of literary tran...
History at Ukrainian Underground University (1921–1925)
History at Ukrainian Underground University (1921–1925)
The article considers and analyzes the origin and the activity of Ukrainian Secret University (USU) in Lviv through 1919–1925 and presents its significance for the development of U...
Static and Dynamic Cues to Male Attractiveness
Static and Dynamic Cues to Male Attractiveness
Abstract Most studies on facial attractiveness have relied on attractiveness judged from photographs rather than video clips. Only a few studies combined images and video sequences...
THE ORIGIN OF THE UKRAINIAN LITERARY LANGUAGE IN THE HYPOTHESES AND CONCEPTS OF YU. O. KARPENKO
THE ORIGIN OF THE UKRAINIAN LITERARY LANGUAGE IN THE HYPOTHESES AND CONCEPTS OF YU. O. KARPENKO
The work is devoted to the memory of a prominent scientist, philologist, founder of the Odesa onomastic school, honoured worker of science and technology of Ukraine, corresponding ...
Martyrious Galyn First Ukrainian Composer of Medical Dictionary (1856-1943)
Martyrious Galyn First Ukrainian Composer of Medical Dictionary (1856-1943)
The article is devoted to the activities of the doctor of medicine, the chief surgeon of the Kiev Military Hospital, the head of natural-medical and later of the medical section of...
NON-KARSTIC SPELEOGENESIS IN SANDSTONE ROCKS OF UKRAINIAN CARPATHIANS
NON-KARSTIC SPELEOGENESIS IN SANDSTONE ROCKS OF UKRAINIAN CARPATHIANS
Due to the limited distribution of karst rocks and, accordingly, the small number of karst caves in the Ukrainian Carpathians, the caves of non-karst (pseudokarst, clastokarst) gen...

