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Geology Of Western Carpathians
The Western Carpathians are an arc-shaped mountain range, the northern branch of the Alpine- Himalayan fold and thrust system called the Alpide belt, which evolved during the Alpine orogeny. In particular, their pre-Cenozoic evolution is very similar to that of the Eastern Alps, and they constitute a transition between the Eastern Alps and the Eastern Carpathians. The geological evolution of individual parts of the chain is complex, a result of tectonic processes like folding, thrusting and the formation of sedimentary basins of various types during the Mesozoic and Cenozoic. These processes sometimes affected not only the sedimentary fill of the basins, but also, in some cases, the former basement. Many aspects of the geological structure of the Western Carpathians have not been completely studied and are subject to ongoing research and debate. The appropriate classification of a number of specific tectonic units is still not clear. Geological definition The Wes ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Basement (geology)
In geology, basement and crystalline basement are crystalline rocks lying above the mantle and beneath all other rocks and sediments. They are sometimes exposed at the surface, but often they are buried under miles of rock and sediment. The basement rocks lie below a sedimentation, sedimentary platform (geology), platform or cover, or more generally any rock below sedimentary rocks or sedimentary basins that are metamorphic rock, metamorphic or Igneous rock, igneous in origin. In the same way, the sediments or sedimentary rocks on top of the basement can be called a "cover" or "sedimentary cover". Crustal rocks are modified several times before they become basement, and these transitions alter their composition. Continental crust Basement rock is the thick foundation of ancient, and oldest, metamorphic and igneous rock that forms the Crust (geology), crust of continents, often in the form of granite. Basement rock is contrasted to overlying sedimentary rocks which are laid down ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bohemia
Bohemia ( ; cs, Čechy ; ; hsb, Čěska; szl, Czechy) is the westernmost and largest historical region of the Czech Republic. Bohemia can also refer to a wider area consisting of the historical Lands of the Bohemian Crown ruled by the Bohemian kings, including Moravia and Czech Silesia, in which case the smaller region is referred to as Bohemia proper as a means of distinction. Bohemia was a duchy of Great Moravia, later an independent principality, a kingdom in the Holy Roman Empire, and subsequently a part of the Habsburg monarchy and the Austrian Empire. After World War I and the establishment of an independent Czechoslovak state, the whole of Bohemia became a part of Czechoslovakia, defying claims of the German-speaking inhabitants that regions with German-speaking majority should be included in the Republic of German-Austria. Between 1938 and 1945, these border regions were joined to Nazi Germany as the Sudetenland. The remainder of Czech territory became the Second ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Carpathian Foredeep
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 P ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nappe
In geology, a nappe or thrust sheet is a large sheetlike body of rock (geology), rock that has been moved more than or above a thrust fault from its original position. Nappes form in compressional tectonic settings like continental collision zones or on the overriding plate in active subduction zones. Nappes form when a mass of rock is forced (or thrust fault, "thrust") over another rock mass, typically on a low angle fault plane. The resulting structure may include large-scale recumbent Fold (geology), folds, shearing along the fault plane,Twiss, Robert J. and Eldridge M. Moores, ''Structural Geology,'' W. H. Freeman, 1992, p. 236 Thrust fault#Thrust duplex, imbricate thrust stacks, Window (geology), fensters and klippes. The term stems from the French word for ''tablecloth'' in allusion to a rumpled tablecloth being pushed across a table. History Nappes or nappe belts are a major feature of the European Geology of the Alps, Alps, Dinaric Alps, Dinarides, Carpathians and S ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Thrust Front
Thrust is a reaction (physics), reaction force (physics), force described quantitatively by Newton's third law. When a system expels or acceleration, accelerates mass in one direction, the accelerated mass will cause a force of equal magnitude (vector), magnitude but opposite direction to be applied to that system. The force applied on a surface in a direction perpendicular or normal vector, normal to the surface is also called thrust. Force, and thus thrust, is measured using the International System of Units (SI) in newton (unit), newtons (symbol: N), and represents the amount needed to accelerate 1 kilogram of mass at the rate of 1 Metre per second squared, meter per second per second. In mechanical engineering, force orthogonal to the main load (such as in parallel helical gears) is referred to as statics, static thrust. Examples A fixed-wing aircraft propulsion system generates forward thrust when air is pushed in the direction opposite to flight. This can be done by dif ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Prešov
Prešov (, hu, Eperjes, Rusyn language, Rusyn and Ukrainian language, Ukrainian: Пряшів) is a city in Eastern Slovakia. It is the seat of administrative Prešov Region ( sk, Prešovský kraj) and Šariš, as well as the historic Sáros County of the Kingdom of Hungary. With a population of approximately 90,000 for the city, and in total about 110,000 with the metropolitan area, it is the third-largest city in Slovakia. It belongs to the Košice-Prešov agglomeration and is the natural cultural, economic, transport and administrative center of the Šariš region. It lends its name to the Eperjes-Tokaj Hill-Chain which was considered as the geographic entity on the first map of Hungary from 1528. There are many tourist attractions in Prešov such as castles, pools and the old town. Etymology The first written mention is from 1247 (). Several authors derived the name from hu, eper (strawberry). The theory was questioned in the 1940s and newer Slovak language, Slovak works sug ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Košice
Košice ( , ; german: Kaschau ; hu, Kassa ; pl, Коszyce) is the largest city in eastern Slovakia. It is situated on the river Hornád at the eastern reaches of the Slovak Ore Mountains, near the border with Hungary. With a population of approximately 230,000, Košice is the second-largest city in Slovakia, after the capital Bratislava. Being the economic and cultural centre of eastern Slovakia, Košice is the seat of the Košice Region and Košice Self-governing Region, and is home to the Slovak Constitutional Court, three universities, various dioceses, and many museums, galleries, and theatres. In 2013 Košice was the European Capital of Culture, together with Marseille, France. Košice is an important industrial centre of Slovakia, and the U.S. Steel Košice steel mill is the largest employer in the city. The town has extensive railway connections and an international airport. The city has a preserved historical centre which is the largest among Slovak towns. There are ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hornád Fault
Hornád ( Slovak, ) or Hernád ( Hungarian, ) is a river in eastern Slovakia and north-eastern Hungary. It is a tributary to the river Slaná (Sajo). The source of the Hornád is the eastern slopes of Kráľova hoľa hill, south of Šuňava. The river is 286 km long, with 178 km located in Slovakia, and the remaining 108 km in Hungary. Cities along its course are Spišská Nová Ves and Košice, both in Slovakia. It flows into the river Sajó ( Slovak Slaná) southeast of Miskolc. Along the river are a series of six separate limestone rocky cliffs and steep slopes, which collectively make up the Site of Community Importance A Site of Community Importance (SCI) is defined in the European Commission Habitats Directive (92/43/EEC) as a site which, in the biogeographical region or regions to which it belongs, contributes significantly to the maintenance or restoration at ... 'Hornádske vápence'. References Rivers of Slovakia Rivers of Hungary Spiš I ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Uzh River
The Uzh ( uk, Уж; translit. ''Uzh''; sk, Uh; hu, Ung, pl, Uż) is a river in Ukraine and Slovakia. Its name comes from the ancient west Slavic dialect word ''už'', meaning "Snake", (lat. "Serpentes"). The Uzh is a tributary of the Laborets River, a river that flows in the Tysa Lowland in Zakarpattia Oblast of western Ukraine. The river feeds numerous industries and is a source of drinking water and irrigation. It also has a hydropower station on it. Several important cities lie along its course, including Uzhhorod. It is long, of which are in Slovakia. It flows into the Laborec river near the city of Drahňov in the Michalovce District ( okres). The Ukrainian city of Uzhhorod and the semi-ruined Nevitske Castle are situated by the Uzh. The river forms part of the Slovakia–Ukraine border for about near the village of Pinkovce. Regions The Uzh is located in the Zakarpattia Oblast in Ukraine and in the districts of Michalovce and Sobrance in eastern Slovakia. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Raaba Line
Raaba, also known as Raaba bei Graz, was a village, merged into Raaba-Grambach in 2015, in the province of the Austrian state of Styria and a suburb of Graz Graz (; sl, Gradec) is the capital city of the Austrian state of Styria and second-largest city in Austria after Vienna. As of 1 January 2021, it had a population of 331,562 (294,236 of whom had principal-residence status). In 2018, the popul .... Due to its proximity to Graz an area with medium-rise office blocks has developed on the edge of Raaba. Population References Cities and towns in Graz-Umgebung District {{Styria-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Carnuntum Gate
Carnuntum ( according to Ptolemy) was a Roman legionary fortress ( la, castra legionis) and headquarters of the Pannonian fleet from 50 AD. After the 1st century, it was capital of the Pannonia Superior province. It also became a large city of 50,000 inhabitants. Its impressive remains are situated on the Danube in Lower Austria halfway between Vienna and Bratislava in the Carnuntum Archaeological Park extending over an area of 10 km2 near today's villages of Petronell-Carnuntum and Bad Deutsch-Altenburg. History Military history Carnuntum first occurs in history during the reign of Augustus (6 AD), when Tiberius made it his base of operations as a Roman fort () in the campaigns against Maroboduus (Marbod). Legio XV Significant Romanisation happened when the town was selected as the garrison of the Legio XV before 14 AD. A few years later, it became the centre of the Roman fortifications along the Danube from Vindobona (now Vienna) to Brigetio ( Ó-Szőny). Acco ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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