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Brno Highlands
The Brno Highlands ( cs, Brněnská vrchovina, german: Brünner Bergland) is a mountain range in the South Moravian Region in the Czech Republic. The highlands, together with the Jevišovice Highlands threshold, form the South-Moravian part of Moldanubian Zone – southeast part of Bohemian Massif. Geography The Brno Highlands rise to the north of the Thaya between Miroslav, and the Prostějov and Litovel in the north. The highlands have an area of and an average height of . The highest peak is ''Skalky'' at ; other peaks are ''Paprč'' , ''Proklest'' , or ''Babí lom'' . To the southeast is the Dyje–Svratka Valley. To the north is the Upper Morava Valley. To the southeast is the Vyškov Gate and Dyje–Svratka Valley. Southeast border line of Brno Highlands is also main border of two large geological provinces: Extendet crust (Bohemian Massif) and Orogeny ( Carpatien) The mountain range in the south is partly fenced and contains several vineyards that constitute part ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Czech Republic
The Czech Republic, or simply Czechia, is a landlocked country in Central Europe. Historically known as Bohemia, it is bordered by Austria to the south, Germany to the west, Poland to the northeast, and Slovakia to the southeast. The Czech Republic has a hilly landscape that covers an area of with a mostly temperate continental and oceanic climate. The capital and largest city is Prague; other major cities and urban areas include Brno, Ostrava, Plzeň and Liberec. The Duchy of Bohemia was founded in the late 9th century under Great Moravia. It was formally recognized as an Imperial State of the Holy Roman Empire in 1002 and became a kingdom in 1198. Following the Battle of Mohács in 1526, the whole Crown of Bohemia was gradually integrated into the Habsburg monarchy. The Protestant Bohemian Revolt led to the Thirty Years' War. After the Battle of White Mountain, the Habsburgs consolidated their rule. With the dissolution of the Holy Empire in 1806, the Cro ... [...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] |
Macocha Gorge
The Macocha Abyss, also known as the Macocha Gorge, is a sinkhole in the Moravian Karst cave system of the Czech Republic. The sinkhole is deep, which makes it the deepest of its kind (light hole type) in Central Europe. It is a popular tourist attraction for casual visitors to the region, in addition to cavers and advanced technical divers. Location Macocha Abyss is located in the Vilémovice (Blansko District), Vilémovice municipality in the South Moravian Region, north of the city of Brno. It is part of the Punkva Caves and the Punkva River flows through it. Description The abyss is long and wide. It is deep to the surface of Dolní Lake. Below the surface of Dolní Lake are other underground spaces, so far explored to a total depth of . The dimensions of the abyss allow for its overall daylight and therefore it is classified in the "light hole" abyss category. At the beginning of the Pustý Žleb (Desolate Canyon), below the town of Sloup (Blansko District), Sloup, the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Brno
Brno ( , ; german: Brünn ) is a city in the South Moravian Region of the Czech Republic. Located at the confluence of the Svitava and Svratka rivers, Brno has about 380,000 inhabitants, making it the second-largest city in the Czech Republic after the capital, Prague, and one of the 100 largest cities of the EU. The Brno metropolitan area has almost 700,000 inhabitants. Brno is the former capital city of Moravia and the political and cultural hub of the South Moravian Region. It is the centre of the Czech judiciary, with the seats of the Constitutional Court, the Supreme Court, the Supreme Administrative Court, and the Supreme Public Prosecutor's Office, and a number of state authorities, including the Ombudsman, and the Office for the Protection of Competition. Brno is also an important centre of higher education, with 33 faculties belonging to 13 institutes of higher education and about 89,000 students. Brno Exhibition Centre is among the largest exhibition ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Boskovice
Boskovice (; german: Boskowitz) is a town in Blansko District in the South Moravian Region of the Czech Republic. It has about 12,000 inhabitants. The area of the historic town centre, Jewish quarter, château complex and castle ruin is well preserved and is protected by law as an urban monument zone. Administrative parts Villages of Bačov, Hrádkov, Mladkov and Vratíkov are administrative parts of Boskovice. Geography Boskovice is located about north of Brno. It lies on the border of the Boskovice Furrow and Drahany Highlands. The Boskovice Reservoir is largely located in the municipal territory. The reservoir lies on the river Bělá which flows through the eastern part of the town and the southern part of the territory. History Boskovice was probably founded in the 13th century as a market village. The first written mention of Boskovice is from 1222, when the lord Jimram of Boskovice was listed as a witness in a deed of the King Ottokar I of Bohemia. The Boskovice Castle ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Blansko
Blansko (; german: Blanz) is a town in the South Moravian Region of the Czech Republic. It has about 20,000 inhabitants. It lies on the Svitava River on the border of the Moravian Karst. It is mainly an industrial town. Administrative parts Villages of Češkovice, Dolní Lhota, Horní Lhota, Hořice, Klepačov, Lažánky, Obůrka, Olešná, Skalní mlýn, Těchov and Žižlavice are administrative parts of Blansko. Geography Blansko is located about north of Brno. It lies in the Drahany Highlands. The highest point is the hill Bukovec with an altitude of . It is situated in the valley of the river Svitava, the majority of the town is situated on a slope above the left bank of the Svitava. The eastern part of the municipal territory lies in the Moravian Karst Protected Landscape Area. History Blansko was originally founded as a settlement on the right bank of the Svitava, today the local part called Staré Blansko ("Old Blansko"). It was located on an important trade route fr ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Jihlava (river)
The Jihlava (german: Igel) is a river in the Moravia (Czech Republic), a right tributary of the Svratka River. It originates in the Bohemian-Moravian Highlands ''(Českomoravská vrchovina)'' upland at the elevation of 665 m and flows to the Nové Mlýny reservoirs, where it enters the Svratka River. It is 180.8 km long, and its basin area is 2,997 km2. It flows through numerous towns and villages, including Jihlávka, Horní Ves, Horní Cerekev, Batelov, Dolní Cerekev, Kostelec, Dvorce, Rantířov, Jihlava, Malý Beranov, Luka nad Jihlavou, Bítovčice, Bransouze, Číchov, Přibyslavice, Třebíč, Vladislav, Kramolín, Mohelno, Biskoupky, Ivančice, Moravské Bránice, Nové Bránice, Dolní Kounice, Pravlov, Kupařovice, Medlov, Pohořelice, Přibice, Ivaň. The Dalešice Hydro Power Plant, including the Dalešice and Mohelno Dams, are constructed on the river. The longest tributaries of the river are the Oslava, Brtnice Brtnice (; german: Pir ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Svratka (river)
The Svratka (), formerly ''Švarcava'' (german: Schwarzach) is a river in the South Moravian Region of the Czech Republic. It is long, and its basin area is . It rises in the Bohemian-Moravian Highlands, converges with the Svitava in Brno, and flows into the Dyje (''Thaya'') a near Mikulov. The river is known in the local Moravian dialect as the ''Švarcava'' (from the German German(s) may refer to: * Germany (of or related to) ** Germania (historical use) * Germans, citizens of Germany, people of German ancestry, or native speakers of the German language ** For citizens of Germany, see also German nationality law **Ge ... name of the river ''Schwarzach''). References Rivers of the Vysočina Region Rivers of the South Moravian Region Břeclav District Žďár nad Sázavou District {{CzechRepublic-river-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Svitava (river)
The Svitava (german: Zwittawa) is a river in the Pardubice and South Moravian regions of the Czech Republic. The Svitava rises near Svitavy, passes through Blansko, and flows into the Svratka in Brno. It is long, and its basin area is . Etymology The river's name referred to its clear water and was derived from ''svítat'', which meant "be clear" in Old Czech. The river is first documented in 1125 in ''Chronica Boemorum The ''Chronica Boemorum'' (Chronicle of the Czechs, or Bohemians) is the first Latin chronicle in which the history of the Czech lands has been consistently and relatively fully described. It was written in 1119–1125 by Cosmas of Prague. The ...''. References Rivers of the Pardubice Region Rivers of the South Moravian Region Blansko District Svitavy District {{CzechRepublic-river-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Flysch
Flysch () is a sequence of sedimentary rock layers that progress from deep-water and turbidity flow deposits to shallow-water shales and sandstones. It is deposited when a deep basin forms rapidly on the continental side of a mountain building episode. Examples are found near the North American Cordillera, the Alps, the Pyrenees and the Carpathians. Sedimentological properties Flysch consists of repeated sedimentary cycles with upwards fining of the sediments. There are sometimes coarse conglomerates or breccias at the bottom of each cycle, which gradually evolve upwards into sandstone and shale/mudstone. Flysch typically consists of a sequence of shales rhythmically interbedded with thin, hard, graywacke-like sandstones. Typically the shales do not contain many fossils, while the coarser sandstones often have fractions of micas and glauconite. Tectonics In a continental collision, a subducting tectonic plate pushes on the plate above it, making the rock fold, often to th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Granodiorite
Granodiorite () is a coarse-grained (phaneritic) intrusive igneous rock similar to granite, but containing more plagioclase feldspar than orthoclase feldspar. The term banatite is sometimes used informally for various rocks ranging from granite to diorite, including granodiorite. Composition According to the QAPF diagram, granodiorite has a greater than 20% quartz by volume, and between 65% and 90% of the feldspar is plagioclase. A greater amount of plagioclase would designate the rock as tonalite. Granodiorite is felsic to intermediate in composition. It is the intrusive igneous equivalent of the extrusive igneous dacite. It contains a large amount of sodium (Na) and calcium (Ca) rich plagioclase, potassium feldspar, quartz, and minor amounts of muscovite mica as the lighter colored mineral components. Biotite and amphiboles often in the form of hornblende are more abundant in granodiorite than in granite, giving it a more distinct two-toned or overall darker appearan ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Carboniferous
The Carboniferous ( ) is a geologic period and system of the Paleozoic that spans 60 million years from the end of the Devonian Period million years ago ( Mya), to the beginning of the Permian Period, million years ago. The name ''Carboniferous'' means "coal-bearing", from the Latin '' carbō'' ("coal") and '' ferō'' ("bear, carry"), and refers to the many coal beds formed globally during that time. The first of the modern 'system' names, it was coined by geologists William Conybeare and William Phillips in 1822, based on a study of the British rock succession. The Carboniferous is often treated in North America as two geological periods, the earlier Mississippian and the later Pennsylvanian. Terrestrial animal life was well established by the Carboniferous Period. Tetrapods (four limbed vertebrates), which had originated from lobe-finned fish during the preceding Devonian, became pentadactylous in and diversified during the Carboniferous, including early amphibian line ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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