The morphostructures of the mountainous part basin river Bystrica Nadvirnianska in Ukrainian Carpathians

In the article author characterized the morphostructures of the mountainous part basin river Bystrica Nadvirnianska which are located in the north-eastern slopes of the Ukrainian Carpathians. For the first time, it was presented a large-scale map of the morphostructures of the river basin which was...

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Main Authors: Vitaliy F. Brusak, Taras V. Klapchuk
Format: Article
Language:Belarusian
Published: Belarusian State University 2017-10-01
Series:Журнал Белорусского государственного университета: География, геология
Subjects:
Online Access:https://journals.bsu.by/index.php/geography/article/view/989
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author Vitaliy F. Brusak
Taras V. Klapchuk
author_facet Vitaliy F. Brusak
Taras V. Klapchuk
author_sort Vitaliy F. Brusak
collection DOAJ
description In the article author characterized the morphostructures of the mountainous part basin river Bystrica Nadvirnianska which are located in the north-eastern slopes of the Ukrainian Carpathians. For the first time, it was presented a large-scale map of the morphostructures of the river basin which was created by the means of GIS, also it was made data base of a tectonic and geological structure, morphological and morphometric characteristics of the relief. The studies confirmed the validity of existing medium-scale schemes of morphostructures in the region and significantly refined the boundaries of morphostructures of different orders, using the means of GIS. In the territory of research identified 2 morphostructures of the first order: Skybovi and Vododilno-Verkhovynski Carpathians, which are confined to areas of major tectonic zones – Skybova cover and area of Krosno. In their boundaries allocated 7 morphostructures of the second order, confined to smaller tectonic units. In Skybova Carpathians there are the individual skyb, Beregova, Orivska, Skolivska, Parashka and Zelemyanka. In Vododilno-Verkhovynski Carpathians morphostructures of the second order which correspond of two tectonic subdivisions: Yasinya-Putyla lowland and Serednovystne horstopodibne raising Pryvododilni (Internal) Gorgan. Within the morphostructures of the second order, 11 morphostructures of the third and 8 morphostructures of the fourth order are identified, their geological structure, morphology and morphometry are characterized.
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spelling doaj.art-ed2311c00c4b41f88f04741504e5132b2022-12-22T01:08:02ZbelBelarusian State UniversityЖурнал Белорусского государственного университета: География, геология2521-67402617-39722017-10-012134142989The morphostructures of the mountainous part basin river Bystrica Nadvirnianska in Ukrainian CarpathiansVitaliy F. Brusak0Taras V. Klapchuk1Ivan Franko National University of Lviv, P. Doroshenka Street, 41, 79000, Lviv, UkraineIvan Franko National University of Lviv, P. Doroshenka Street, 41, 79000, Lviv, UkraineIn the article author characterized the morphostructures of the mountainous part basin river Bystrica Nadvirnianska which are located in the north-eastern slopes of the Ukrainian Carpathians. For the first time, it was presented a large-scale map of the morphostructures of the river basin which was created by the means of GIS, also it was made data base of a tectonic and geological structure, morphological and morphometric characteristics of the relief. The studies confirmed the validity of existing medium-scale schemes of morphostructures in the region and significantly refined the boundaries of morphostructures of different orders, using the means of GIS. In the territory of research identified 2 morphostructures of the first order: Skybovi and Vododilno-Verkhovynski Carpathians, which are confined to areas of major tectonic zones – Skybova cover and area of Krosno. In their boundaries allocated 7 morphostructures of the second order, confined to smaller tectonic units. In Skybova Carpathians there are the individual skyb, Beregova, Orivska, Skolivska, Parashka and Zelemyanka. In Vododilno-Verkhovynski Carpathians morphostructures of the second order which correspond of two tectonic subdivisions: Yasinya-Putyla lowland and Serednovystne horstopodibne raising Pryvododilni (Internal) Gorgan. Within the morphostructures of the second order, 11 morphostructures of the third and 8 morphostructures of the fourth order are identified, their geological structure, morphology and morphometry are characterized.https://journals.bsu.by/index.php/geography/article/view/989ukrainian carpathiansvododilno-verkhovynski carpathiansskybovi gorganymorphostructuresrelieftectonic zonebasin river bystrica nadvirnianskagis
spellingShingle Vitaliy F. Brusak
Taras V. Klapchuk
The morphostructures of the mountainous part basin river Bystrica Nadvirnianska in Ukrainian Carpathians
Журнал Белорусского государственного университета: География, геология
ukrainian carpathians
vododilno-verkhovynski carpathians
skybovi gorgany
morphostructures
relief
tectonic zone
basin river bystrica nadvirnianska
gis
title The morphostructures of the mountainous part basin river Bystrica Nadvirnianska in Ukrainian Carpathians
title_full The morphostructures of the mountainous part basin river Bystrica Nadvirnianska in Ukrainian Carpathians
title_fullStr The morphostructures of the mountainous part basin river Bystrica Nadvirnianska in Ukrainian Carpathians
title_full_unstemmed The morphostructures of the mountainous part basin river Bystrica Nadvirnianska in Ukrainian Carpathians
title_short The morphostructures of the mountainous part basin river Bystrica Nadvirnianska in Ukrainian Carpathians
title_sort morphostructures of the mountainous part basin river bystrica nadvirnianska in ukrainian carpathians
topic ukrainian carpathians
vododilno-verkhovynski carpathians
skybovi gorgany
morphostructures
relief
tectonic zone
basin river bystrica nadvirnianska
gis
url https://journals.bsu.by/index.php/geography/article/view/989
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AT vitaliyfbrusak morphostructuresofthemountainouspartbasinriverbystricanadvirnianskainukrainiancarpathians
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