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Geology Of 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 ( ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Serbian-Macedonian Massif
The Serbs are one of the constitutional peoples of North Macedonia ( mk, Србите во Северна Македонија, sr-Cyrl-Latn, Срби у Северној Македонији, Srbi u Severnoj Makedoniji), numbering about 24,000 inhabitants (2021 census). Historical overview Serbia became for the first time independent under Časlav ca. 930, only to fall ca. 960 under Byzantine, later under Bulgarian and then again under Byzantine rule. From the end of the 11th to the end of the 13th century, the Serbian rulers made several attempts to penetrate into the region and briefly conquered its northernmost territories. In fact the whole of today North Macedonia was taken for the first time by medieval Serbia, during the 1280s. The territory of today's North Macedonia was part of the Serbian Kingdom and Empire to the Battle of Kosovo (1389) when it was conquered by the Ottomans. The South Slavic Orthodox people now lived under a foreign, Muslim power, in whose eyes all ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Blueschist
Blueschist (), also called glaucophane schist, is a metavolcanic rock that forms by the metamorphism of basalt and rocks with similar composition at high pressures and low temperatures (), approximately corresponding to a depth of . The blue color of the rock comes from the presence of the predominant minerals glaucophane and lawsonite. Blueschists are schists typically found within orogenic belts as terranes of lithology in faulted contact with greenschist or rarely eclogite facies rocks. Petrology Blueschist, as a rock type, is defined by the presence of the minerals glaucophane + ( lawsonite or epidote ) +/- jadeite +/- albite or chlorite +/- garnet +/- muscovite in a rock of roughly basaltic composition. Blueschist often has a lepidoblastic, nematoblastic or schistose rock microstructure defined primarily by chlorite, phengitic white mica, glaucophane, and other minerals with an elongate or platy shape. Grain size is rarely coarse, as mineral growth is retarded b ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fruška Gora
Fruška gora ( sr-Cyrl, Фрушка гора; hu, Tarcal-hegység) is a mountain in Syrmia, administratively part of Serbia with a part of its western side extending into eastern Croatia. The area under Serbian administration forms the country's oldest national park. Sometimes also referred to as the ''Jewel of Serbia'', due to its largely pristine landscape and protection effort, or the ''Serbian Mount Athos'', being the home of a large number of historical Serbian Orthodox monasteries. Name In Serbian, it is known as ''Fruška gora'' (, Фрушка гора), in Hungarian as ''Tarcal'' (also ''Almus-hegy'' or ''Árpatarló''), in German as ''Frankenwald'', and in Latin as ''Alma Mons''. In Medieval Greek, it was known as ''Frangochoria''. The mountain's name originates in the old Serbian word ''"Fruzi"'' derived from the singular form ''"Frug"''; and its adjective is ''Fruški'', used for naming the Frankish people. The name of ''"Fruška Gora"'' is ''"Frankish mountai ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sava
The Sava (; , ; sr-cyr, Сава, hu, Száva) is a river in Central and Southeast Europe, a right-bank and the longest tributary of the Danube. It flows through Slovenia, Croatia and along its border with Bosnia and Herzegovina, and finally through Serbia, feeding into the Danube in its capital, Belgrade. The Sava forms the main northern limit of the Balkan Peninsula, and the southern edge of the Pannonian Plain. The Sava is long, including the Sava Dolinka headwater rising in Zelenci, Slovenia. It is the largest tributary of the Danube by volume of water, and second-largest after the Tisza in terms of catchment area () and length. It drains a significant portion of the Dinaric Alps region, through the major tributaries of Drina, Bosna, Kupa, Una, Vrbas, Lonja, Kolubara, Bosut and Krka. The Sava is one of the longest rivers in Europe and among the longest tributaries of another river. The population in the Sava River basin is estimated at 8,176,000, and is shared by ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sava Zone
The Sava (; , ; sr-cyr, Сава, hu, Száva) is a river in Central and Southeast Europe, a right-bank and the longest tributary of the Danube. It flows through Slovenia, Croatia and along its border with Bosnia and Herzegovina, and finally through Serbia, feeding into the Danube in its capital, Belgrade. The Sava forms the main northern limit of the Balkan Peninsula, and the southern edge of the Pannonian Plain. The Sava is long, including the Sava Dolinka headwater rising in Zelenci, Slovenia. It is the largest tributary of the Danube by volume of water, and second-largest after the Tisza in terms of catchment area () and length. It drains a significant portion of the Dinaric Alps region, through the major tributaries of Drina, Bosna, Kupa, Una, Vrbas, Lonja, Kolubara, Bosut and Krka. The Sava is one of the longest rivers in Europe and among the longest tributaries of another river. The population in the Sava River basin is estimated at 8,176,000, and is shared by t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bulgaria
Bulgaria (; bg, България, Bǎlgariya), officially the Republic of Bulgaria,, ) is a country in Southeast Europe. It is situated on the eastern flank of the Balkans, and is bordered by Romania to the north, Serbia and North Macedonia to the west, Greece and Turkey to the south, and the Black Sea to the east. Bulgaria covers a territory of , and is the sixteenth-largest country in Europe. Sofia is the nation's capital and largest city; other major cities are Plovdiv, Varna and Burgas. One of the earliest societies in the lands of modern-day Bulgaria was the Neolithic Karanovo culture, which dates back to 6,500 BC. In the 6th to 3rd century BC the region was a battleground for ancient Thracians, Persians, Celts and Macedonians; stability came when the Roman Empire conquered the region in AD 45. After the Roman state splintered, tribal invasions in the region resumed. Around the 6th century, these territories were settled by the early Slavs. The Bulgars, led by Asp ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Balkan Mountains
The Balkan mountain range (, , known locally also as Stara planina) is a mountain range in the eastern part of the Balkan Peninsula in Southeastern Europe. The range is conventionally taken to begin at the peak of Vrashka Chuka on the border between Bulgaria and Serbia. It then runs for about , first in a south-easterly direction along the border, then eastward across Bulgaria, forming a natural barrier between the northern and southern halves of the country, before finally reaching the Black Sea at Cape Emine. The mountains reach their highest point with Botev Peak at . In much of the central and eastern sections, the summit forms the watershed between the drainage basins of the Black Sea and the Aegean. A prominent gap in the mountains is formed by the sometimes narrow Iskar Gorge, a few miles north of the Bulgarian capital, Sofia. The karst relief determines the large number of caves, including Magura, featuring the most important and extended European post-Palaeolithic cave ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Carpathian Mountains
The Carpathian Mountains or Carpathians () are a range of mountains forming an arc across Central Europe. Roughly long, it is the third-longest European mountain range after the Urals at and the Scandinavian Mountains at . The range stretches from the far eastern Czech Republic (3%) and Austria (1%) in the northwest through Slovakia (21%), Poland (10%), Ukraine (10%), Romania (50%) to Serbia (5%) in the south. "The Carpathians" European Travel Commission, in The Official Travel Portal of Europe, Retrieved 15 November 2016 The Carpathian ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Serbian Carpathians
Serbian Carpathians ( sr, / ) is a mountain range in eastern Central Serbia, located in Central Europe. It presents an extension of proper Carpathian Mountains across the Danube, connecting them with the Balkan Mountains in the southeast. They stretch in north-south direction in eastern Serbia, east of the Great Morava valley and west of the White Timok Valley and north of the Nišava Valley. The mountains are 800–1500 m high, and dominated by karst limestone geologic features, the highest one being Rtanj Mountain (1,565 m). Definitions Under the strict definition (as defined by the Serbian Academy of Sciences and Arts and adopted by the Carpathian Convention), Serbian part of the Carpathian Mountains covers only 732 km², or less than 1% of the total Carpathian area. That part encompasses the southern bank of the Iron Gate and the area of Đerdap National Park. The extreme points of so defined Carpathian area in Serbia are Tekija in the north, in the south, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
