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The term Carpathian Basin is used in Hungarian literature, while the West Slavic languages (Czech, Polish and Slovak), the Serbo-Croatian, German and Romanian languages use Pannonian Basin (in Hungarian the basin is known as Kárpát-medence, in Czech; Panonská pánev, in Polish; Panoński Basen, in Slovak; Panónska panva, in Slovenian and ...
The Pannonian Region is a large alluvial basin surrounded by the Carpathian Mountains to the north and east, the Alps to the west and the Dinaric Alps to the south. The basin was once the bed of an inland sea. It is flat, and is crossed from north to south by the Danube and Tisza rivers. The region contains all of Hungary, and around the ...
Hungary is in the Pannonian Basin in Central Europe, is surrounded by the Carpathians, Alps and Dinarides, but for the most part dominated by lowlands. Sixty-eight percent of the country is lowlands below 200 meters altitude. Hilly terrain covers 30% of the country, while mountains cover only 2%. The entire Pannonian Basin is in the Danube ...
Approximate extent of the Pannonian Sea during the Miocene Epoch; modern-day political borders and settlements superimposed for reference. Detailed map of the south-eastern part of Pannonian Sea during the Miocene Epoch. The Pannonian Sea was a shallow ancient sea, where the Pannonian Basin in Central Europe is now. During its history it lost ...
Pannonia (/ p ə ˈ n oʊ n i ə /, Latin: [panˈnɔnia]) was a province of the Roman Empire bounded on the north and east by the Danube, on the west by Noricum and upper Italy, and on the southward by Dalmatia and upper Moesia.
Bulk of the lowlands are found in the northern regions of the country, especially in Slavonia, representing a part of the Pannonian Basin. Territory with elevations of 200 to 500 metres (660 to 1,640 feet) above sea level encompasses 25.61% of Croatia's territory, and the areas between 500 and 1,000 metres (1,600 and 3,300 feet) above sea level ...
The Jurassic-Cretaceous tectonic structure was later changed by various types of the overstep complexes: the Central Carpathian Paleogene Basin, Buda Paleogene Basin, Vienna Basin (Neogene, pull-apart type), Pannonian Basin (or the Danube Basin), and the volcanic complexes: Neogene volcanics of Carpathians (or just Neovolcanis). [12]
In the 6th century BC, some splinter Scythian groups followed the earlier route of the nomads of the Chernogorovka-Novocherkassk wave, passed through the passes of the Carpathian Mountains, and settled in the Pannonian Basin, [43] [44] where some of them settled in the territory of the Agathyrsi while others moved into the Pannonian Steppe and ...