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Danubian Plain (Serbia)
Danubian Plain can be a translation of: * the approximate Serbian name (, literally: "Danubian Lowland") for the Serbian part of the Pannonian Plain * the Serbian () and Hungarian (, literally: "Danubian Lowland") name for a part of the Great Alföld * the Slovak name (, literally: "Danubian Lowland") for the Slovak part of the Little Alföld, see Danubian Lowland * the Slovak name (, literally: "Danubian Flat/Plain") for a part of the , see Danubian Flat * the Bulgarian name (, literally: "Danubian Plain") and Romanian name () for a group of plains and lowlands in Romania, Bulgaria, and Serbia, see Danubian Plain and Wallachian Plain The Romanian Plain () is located in southern Romania and the easternmost tip of Serbia, where it is known as the Wallachian Plain (). It is part of the larger Eurasian Steppe. It is located in the historical region of Wallachia, and bordered by ...
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Pannonian Plain
The Pannonian Basin, with the term Carpathian Basin being sometimes preferred in Hungarian literature, is a large sedimentary basin situated in southeastern Central Europe. After the Treaty of Trianon following World War I, the geomorphological term Pannonian Plain was also used for roughly the same region, referring to the lowlands in the area occupied by the Pannonian Sea during the Pliocene Epoch, however some consider the term "Pannonian Plain" not only unhistorical but also topologically erroneous. Terminology The term Pannonian Plain refers to the lowland parts of the Pannonian Basin as well as those of some adjoining regions like Lower Austria, Moravia, and Silesia (Czech Republic and Poland). The lands adjoining the plain proper are sometimes also called ''peri-Pannonian''. In English language, the terms "Pannonian Basin" and "Carpathian Basin" may sometimes be used synonymously, although the latter holds an irredentist Hungarian connotation. The name "Pannonian" ...
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Great Alföld
The Great Hungarian Plain (also known as Alföld or Great Alföld, or ) is a plain occupying the majority of the modern territory of Hungary. It is the largest part of the wider Pannonian Plain (however, the Great Hungarian Plain was not part of the ancient Roman province Pannonia). Its territory significantly shrank due to its eastern and southern boundaries being adjusted by the new political borders created after World War I when the Treaty of Trianon was signed in 1920. Boundaries Its boundaries are the Carpathians in the north and east, the Transdanubian Mountains and the Dinaric Alps in the southwest, and approximately the Sava river in the south. Geography Plain in Hungary Its territory covers approximately of Hungary, approximately 56% of its total area of . The highest point of the plain is Hoportyó (); the lowest point is the Tisza River. The terrain ranges from flat to rolling plains. The most important Hungarian writers inspired by and associated wit ...
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Little Alföld
The Little Hungarian Plain or Little Alföld ( Hungarian: ''Kisalföld'' , Slovak: ''Malá dunajská kotlina'', German: ''Kleine Ungarische Tiefebene'') is a plain (tectonic basin) of approximately 8,000 km² in northwestern Hungary, south-western Slovakia (''Podunajská nížina'' – Danubian Lowland), and eastern Austria. It is a part of the Pannonian plain which covers most parts of Hungary. Geography Its borders are the Carpathians on the north, the Bakony- Vértes Hills in the south, the Gerecse Hills in the east, and the Leitha Mountains and the foothills of the Alps in the west. In Hungary, it includes most of Győr-Moson-Sopron and Vas counties, and the western part of Komárom-Esztergom and Veszprém. The plain is roughly cut in half by the Danube which is split up into many arms between Bratislava and Komárno, forming large islands. Its main tributaries are the Váh, the Rába, the Rábca and the Marcal rivers. Smaller microregions of the Little Alföld ...
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Danubian Lowland
::''The Serbian lowland is treated under Danubian Plain (Serbia)'' The Danubian Lowland or Danube Lowland () is the name of the part of Little Alföld (Slovak: ''Malá dunajská kotlina'') situated in Slovakia, located between the Danube, the Little Carpathians, and all other parts of the Western Carpathians. In terms of geomorphology, it forms one unit together with the Neusiedl Basin (''Neusiedler Becken'') in Austria and the Győr Basin (''Győri-medence'') in Hungary. It is an extensive tectonic depression filled with layers of Neogene Quaternary to a height of between 100 and 350 metres. It consists of the following two parts: *Danubian Hills (also translated as Danubian Upland) in the north *Danubian Flat (also translated as Danubian Plain) in the south Many urban and other settlements can be found in this primarily agricultural area. The towns Topoľčany, Nové Zámky, Komárno, Levice, Dunajská Streda, and Galanta are administrative centers. They are centers of indust ...
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Danubian Flat
The Danubian Flat (Slovak language, Slovak and Czech language, Czech: ''Podunajská rovina'', German language, German: ''Donauebene''), also translated as Danubian Plain, is the south-western, flatter, part of the Danubian Lowland in Slovakia. The border with the Danubian Hills runs approx. along the line Bratislava – Senec (Slovakia), Senec – Sereď – Nové Zámky – Patince. It has been formed by the arms of the Danube (Little Danube and others) and by the southern Váh, Nitra and Žitava (river), Žitava rivers. It is filled with huge layers of gravel from the Danube and other rivers of the area. These Danubian gravels are covered with loess and other very fertile soils. The Danube forms here a unique continental river delta, delta system of meanders and dead arms. The area between one of those arms called Little Danube and the Danube is known as the Žitný ostrov, the biggest river island in Europe. The Žitný ostrov is an area with marsh depressions, natural lakes ...
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Danubian Plain (Bulgaria)
The Danubian Plain () constitutes the northern part of Bulgaria, situated north of the Balkan Mountains and south of the Danube. Its western border is the Timok River, and to the east it borders the Black Sea. The plain has an area of . It is about long and wide. The Danubian Plain is contiguous with the Wallachian Plain (forming the Lower Danubian Plain), but its elevation is slightly higher and the relief is more hilly and rolling, featuring numerous plateaux and river valleys. The climate is markedly temperate continental with a weak Black Sea influence in the east. Precipitation is on average 450–650 mm a year. Important rivers include the Danube, the Iskar, the Yantra, the Osam, the Vit, the Rusenski Lom, the Ogosta, and the Lom. Among the major cities of the region are Rousse, Pleven, Dobrich, Shumen, Vidin, Silistra, Targovishte, Razgrad, Svishtov and Lom. Minerals The Danubian Plain contains a wide variety of minerals, such as: * Lignite (Lomski ...
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