Titlebook: Landscapes and Landforms of Slovakia; Milan Lehotsky,Martin Bolti?iar Book 2022 Springer Nature Switzerland AG 2022 Slovakian Landscapes.G

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Outline of Geology and Cenozoic Evolution of Slovakiazoic Basin system in the central and southern parts. The Western Carpathians are an integral part of the northern branch of the Carpathian arc and the whole European Alpine orogenic system, which was formed by the closure of the Tethys and Alpine Atlantic oceans during the Mesozoic and Cenozoic time

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Climate in the Past and Present in the Slovak Landscapes—The Central European Contextom the Mesozoic Era to the present. The climate for the earliest period can only be reconstructed in the broadest terms. The level of detail possible increases as we approach to the period of the instrumental observations. The regular systematic meteorological measurements began in Slovakia in the m

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The Longest and the Most Symmetrical Mountain Ridge of Slovakia—Low Tatra Mts.mately 1,240 km. and culminates in Mt. ?umbier (2,043?m a.s.l.). As a geomorphological unit of the Inner Western Carpathians, the Low Tatra belong to the Fatra–Tatra region. In terms of the geological structure, it belongs to two different units, the structure of which also conditioned their geomorp

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