Zobrazeno 1 - 10
of 14
pro vyhledávání: '"Yaroslav Kravchuk"'
Autor:
Yaroslav Kravchuk, Vitaliy Brusak
Publikováno v:
PROBLEMS OF GEOMORPHOLOGY AND PALEOGEOGRAPHY OF THE UKRANIAN CARPATHIANS AND ADJACENT AREAS. :18-36
Relief and geological structure of Hutsulshchyna and Verkhovynskyi national natural parks (NNP), located in the south-eastern part of the Ukrainian Carpathians, present four geomorphological regions of the Ukrainian Carpathians. Hutsulshchyna NNP is
Autor:
Yaroslav Kravchuk, Vasyl Chalyk
Publikováno v:
PROBLEMS OF GEOMORPHOLOGY AND PALEOGEOGRAPHY OF THE UKRANIAN CARPATHIANS AND ADJACENT AREAS. :129-137
The analysis of four stages of relief development is done, which created the corresponding complexes within the Solotvyno hollow. The main attention is paid to the morphostructural and morphosculptural features. The morphostructures of the third and
Autor:
Yaroslav Kravchuk, Vitaliy Brusak
Publikováno v:
PROBLEMS OF GEOMORPHOLOGY AND PALEOGEOGRAPHY OF THE UKRANIAN CARPATHIANS AND ADJACENT AREAS. :19-38
The relief and geological structure of Carpathian Biosphere Reserve represent the features of the geological and geomorphological structure of the four geomorphological regions of the Ukrainian Carpathians. The block mid-mountains of the Polonynsko-C
Autor:
Vitaliy Brusak, Yaroslav Kravchuk
Publikováno v:
PROBLEMS OF GEOMORPHOLOGY AND PALEOGEOGRAPHY OF THE UKRANIAN CARPATHIANS AND ADJACENT AREAS. :184-207
In the stydy an analysis of the geological structure and relief of Uzhansky, “Skolivsky Beskydy”, and “Boykivshchyna” national natural parks (NNP), located in the north-western part of the Ukrainian Carpathians, is presented. Uzhansky NNP is
Publikováno v:
PROBLEMS OF GEOMORPHOLOGY AND PALEOGEOGRAPHY OF THE UKRANIAN CARPATHIANS AND ADJACENT AREAS. :85-104
The segment has a rather complex geological structure. The Svydovets massif is characterized by a complex division of structural overthrust sheets – Dukliansky, Porkuletsky and Chornohirsky overthrusts. The northern part of the site is located in t
Publikováno v:
PROBLEMS OF GEOMORPHOLOGY AND PALEOGEOGRAPHY OF THE UKRANIAN CARPATHIANS AND ADJACENT AREAS. :3-29
This year we celebrate the 70th anniversary of the Department of Geomorphology (since 2000 – Geomorphology and Paleogeography) of the Faculty of Geography, Ivan Franko National University of Lviv, formed on the basis of the existing Lviv school of
Publikováno v:
PROBLEMS OF GEOMORPHOLOGY AND PALEOGEOGRAPHY OF THE UKRANIAN CARPATHIANS AND ADJACENT AREAS. :18-41
The promising area – attractive for recreation – is located within two large geomorphological regions, the Polonynsko-Chornohorsky Carpathians (Svydivets Massif) and the Vododilno-Verhovynsky Carpathians (Bratkivsky Ridge of the Pryvododilny Gorg
PRECARPATHIAN AND TRANSCARPATHIAN LANDFORM EVOLUTION IN THE PLIOCENE-PLEOSTOCENE AND AT EARLY STAGES
Autor:
Vasyl Chalyk, Yaroslav Kravchuk
Publikováno v:
PROBLEMS OF GEOMORPHOLOGY AND PALEOGEOGRAPHY OF THE UKRANIAN CARPATHIANS AND ADJACENT AREAS. :154-165
The Sarmatian-Pannonian and Pontian-Pliocene stages are most important in the landform evolution of the Inner Precarpathians and Solotvyn basin. Due to the intense elevations in the upper Miocene, the Precarpathian Sea was pushed to the east and nort
Autor:
Yaroslav Kravchuk, Yuriy Zinko
Publikováno v:
PROBLEMS OF GEOMORPHOLOGY AND PALEOGEOGRAPHY OF THE UKRANIAN CARPATHIANS AND ADJACENT AREAS. :3-20
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
Autor:
Yurii Zinko, Yaroslav Kravchuk
Publikováno v:
PROBLEMS OF GEOMORPHOLOGY AND PALEOGEOGRAPHY OF THE UKRANIAN CARPATHIANS AND ADJACENT AREAS. :68-83
The problem of influence of meso- and macrorelief on the spatial structure of the soil cover was studied based on the example of Lviv Region. Analysis of relief and soil correlation was considered at the level of soil catenae and spatial-structural (