Earthquakes In Serbia
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Earthquakes In Serbia
The regional geology of Serbia describes the geologic structure and history inside the borders of Serbia. Serbia is in recent geologic time a part of the Eurasian Plate, but the bedrock lithologies are witness to a diverse geologic history. In a tectonic sense, Serbia is part of an orogenic system that is composed of the Alpine, Carpathian, and Dinaride orogenic belts. Its territory can be divided into five geotectonic units of differing genesis: *Pannonian Plain, occupying the northern part of the country (Vojvodina province) *Dinaric Alps occupy western part of Central Serbia, stretching in general northwest-southeast direction * Vardar Zone is a belt east of the Dinaric alps, continuing into central North Macedonia. It consists of three parts: Srem, Jadar and Kopaonik blocks, separated by ophiolitics fractures. *Serbian-Macedonian Massif is a belt stretching in north-south direction along the Great and South Morava valleys, into western North Macedonia and northern Greece ( ...
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Serbia Mountain Ranges
Serbia (, ; Serbian: , , ), officially the Republic of Serbia ( Serbian: , , ), is a landlocked country in Southeastern and Central Europe, situated at the crossroads of the Pannonian Basin and the Balkans. It shares land borders with Hungary to the north, Romania to the northeast, Bulgaria to the southeast, North Macedonia to the south, Croatia and Bosnia and Herzegovina to the west, and Montenegro to the southwest, and claims a border with Albania through the disputed territory of Kosovo. Serbia without Kosovo has about 6.7 million inhabitants, about 8.4 million if Kosvo is included. Its capital Belgrade is also the largest city. Continuously inhabited since the Paleolithic Age, the territory of modern-day Serbia faced Slavic migrations in the 6th century, establishing several regional states in the early Middle Ages at times recognised as tributaries to the Byzantine, Frankish and Hungarian kingdoms. The Serbian Kingdom obtained recognition by the Holy See and C ...
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