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Nízký Jeseník
Nízký Jeseník (german: Niederes Gesenke, pl, Niski Jesionik) is a flat highland and geomorphological mesoregion of the Czech Republic. It is located in the east of the country in the Olomouc and Moravian-Silesian regions. Nízký Jeseník is the largest Czech geomorphological region, and is known for the former volcanic activity. Etymology According to the most probable theory, the name has its origin in the word ''jasan'', i.e. " ash". ''Jeseník'' (respectively ''Jesenný stream'') was first the name of a stream that flowed through an ash forest in a valley. The name was Germanized to ''Gesenke'' (i.e. "slope") and used as a name of a small town that was founded in the valley (but later disappeared), and then it was transferred first to the valley, and then to the whole mountain range. Later the name was changed back to Czech ''Jeseník''. Jeseníky (plural form of Jeseník) is a collective term for an area that includes the mountain ranges of Nízký Jeseník (i.e. "low Je ... [...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] |
Upper Morava Valley
Upper may refer to: * Shoe upper or ''vamp'', the part of a shoe on the top of the foot * Stimulant, drugs which induce temporary improvements in either mental or physical function or both * ''Upper'', the original film title for the 2013 found footage film ''The Upper Footage ''The Upper Footage'' (also known as ''Upper'') is a 2013 found footage film written and directed by Justin Cole. First released on January 31, 2013 to a limited run of midnight theatrical screenings at Landmark’s Sunshine Cinema in New York Cit ...'' See also {{Disambiguation ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Oder
The Oder ( , ; Czech, Lower Sorbian and ; ) is a river in Central Europe. It is Poland's second-longest river in total length and third-longest within its borders after the Vistula and Warta. The Oder rises in the Czech Republic and flows through western Poland, later forming of the border between Poland and Germany as part of the Oder–Neisse line. The river ultimately flows into the Szczecin Lagoon north of Szczecin and then into three branches (the Dziwna, Świna and Peene) that empty into the Bay of Pomerania of the Baltic Sea. Names The Oder is known by several names in different languages, but the modern ones are very similar: English and ; Czech, Polish, and , ; (); Medieval Latin: ''Od(d)era''; Renaissance Latin: ''Viadrus'' (invented in 1534). Ptolemy knew the modern Oder as the Συήβος (''Suebos''; Latin ''Suevus''), a name apparently derived from the Suebi, a Germanic people. While he also refers to an outlet in the area as the Οὐιαδούα ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Krnov
Krnov (; german: Jägerndorf, pl, Karniów or ''Krnów'') is a town in Bruntál District in the Moravian-Silesian Region of the Czech Republic. It has about 23,000 inhabitants. Administrative parts The town is made up of town parts of Pod Bezručovým vrchem and Pod Cvilínem, and of village of Krásné Loučky. Geography Krnov lies in the historical region of Upper Silesia on the border with Poland. The town is located at the confluence of the rivers Opava and Opavice. The northern part of the territory with the town proper is situated in the Zlatohorská Highlands, the western and the southern part are situated in the Nízký Jeseník mountain range. A small part on the southeast extends into the Opava Hilly Land within the Silesian Lowlands. The highest peak of the municipal territory is Bednářský vrch at . History The first written mention of Krnov is from 1240. At the latest in 1269 and probably already in 1253, Krnov was a town. In the second half of the 13th centu ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ostrava
Ostrava (; pl, Ostrawa; german: Ostrau ) is a city in the north-east of the Czech Republic, and the capital of the Moravian-Silesian Region. It has about 280,000 inhabitants. It lies from the border with Poland, at the confluences of four rivers: Oder, Opava, Ostravice and Lučina. Ostrava is the third largest city in the Czech Republic in terms of both population and area, the second largest city in the region of Moravia, and the largest city in the historical land of Czech Silesia. It straddles the border of the two historic provinces of Moravia and Silesia. The wider conurbation – which also includes the towns of Bohumín, Havířov, Karviná, Orlová, Petřvald and Rychvald – is home to about 500,000 people, making it the largest urban area in the Czech Republic apart from the capital Prague. Ostrava grew in importance due to its position at the heart of a major coalfield, becoming an important industrial engine of the Austrian empire. During the 20th centur ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Olomouc
Olomouc (, , ; german: Olmütz; pl, Ołomuniec ; la, Olomucium or ''Iuliomontium'') is a city in the Czech Republic. It has about 99,000 inhabitants, and its larger urban zone has a population of about 384,000 inhabitants (2019). Located on the Morava River, the city is the ecclesiastical metropolis and was a historical capital city of Moravia, before having been sacked by the Swedish army during the Thirty Years' War. Today, it is the administrative centre of the Olomouc Region and the sixth largest city in the Czech Republic. The historic city centre is well preserved and is protected by law as urban monument reservation. The Holy Trinity Column was listed as a UNESCO World Heritage Site in 2000 for its quintessential Baroque style and symbolic value. Administrative division Olomouc is made up of 26 administrative parts: *Olomouc *Bělidla *Černovír *Chomoutov *Chválkovice *Droždín *Hejčín *Hodolany *Holice *Klášterní Hradisko *Lazce *Lošov *Nedvězí *Nemil ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Stratovolcano
A stratovolcano, also known as a composite volcano, is a conical volcano built up by many layers (strata) of hardened lava and tephra. Unlike shield volcanoes, stratovolcanoes are characterized by a steep profile with a summit crater and periodic intervals of explosive eruptions and effusive eruptions, although some have collapsed summit craters called calderas. The lava flowing from stratovolcanoes typically cools and hardens before spreading far, due to high viscosity. The magma forming this lava is often felsic, having high-to-intermediate levels of silica (as in rhyolite, dacite, or andesite), with lesser amounts of less-viscous mafic magma. Extensive felsic lava flows are uncommon, but have travelled as far as . Stratovolcanoes are sometimes called composite volcanoes because of their composite stratified structure, built up from sequential outpourings of erupted materials. They are among the most common types of volcanoes, in contrast to the less common shield volcano ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Quaternary
The Quaternary ( ) is the current and most recent of the three periods of the Cenozoic Era in the geologic time scale of the International Commission on Stratigraphy (ICS). It follows the Neogene Period and spans from 2.58 million years ago to the present. The Quaternary Period is divided into two epochs: the Pleistocene (2.58 million years ago to 11.7 thousand years ago) and the Holocene (11.7 thousand years ago to today, although a third epoch, the Anthropocene, has been proposed but is not yet officially recognised by the ICS). The Quaternary Period is typically defined by the cyclic growth and decay of continental ice sheets related to the Milankovitch cycles and the associated climate and environmental changes that they caused. Research history In 1759 Giovanni Arduino proposed that the geological strata of northern Italy could be divided into four successive formations or "orders" ( it, quattro ordini). The term "quaternary" was introduced by Jules Desn ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Proterozoic
The Proterozoic () is a geological eon spanning the time interval from 2500 to 538.8million years ago. It is the most recent part of the Precambrian "supereon". It is also the longest eon of the Earth's geologic time scale, and it is subdivided into three geologic eras (from oldest to youngest): the Paleoproterozoic, Mesoproterozoic, and Neoproterozoic. The Proterozoic covers the time from the appearance of oxygen in Earth's atmosphere to just before the proliferation of complex life (such as trilobites or corals) on the Earth. The name ''Proterozoic'' combines two forms of ultimately Greek origin: meaning 'former, earlier', and , 'of life'. The well-identified events of this eon were the transition to an oxygenated atmosphere during the Paleoproterozoic; the evolution of eukaryotes; several glaciations, which produced the hypothesized Snowball Earth during the Cryogenian Period in the late Neoproterozoic Era; and the Ediacaran Period (635 to 538.8 Ma) which is chara ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Červená Hora (Nízký Jeseník)
Červená hora (meaning "Red Mountain") is a flat geological formation in the Nízký Jeseník mountain range in Moravia, the Czech Republic. With above sea level it is the highest formation of the Domašov Highlands, which are a part of the Nízký Jeseník, and the highest formation in the Opava District. A hydrometeorological station and a station of the European Fireball Network at the same time is located here. Climate See also * Earth-grazing meteoroid of 13 October 1990 On 13 October 1990, meteoroid EN131090, with an estimated mass of 44 kg, entered the Earth's atmosphere above Czechoslovakia and Poland and, after a few seconds, returned to space. Observations of such events are quite rare; this was the ... References Mountains and hills of the Czech Republic {{MoraviaSilesia-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Moravia
Moravia ( , also , ; cs, Morava ; german: link=yes, Mähren ; pl, Morawy ; szl, Morawa; la, Moravia) is a historical region in the east of the Czech Republic and one of three historical Czech lands, with Bohemia and Czech Silesia. The medieval and early modern Margraviate of Moravia was a crown land of the Lands of the Bohemian Crown from 1348 to 1918, an imperial state of the Holy Roman Empire from 1004 to 1806, a crown land of the Austrian Empire from 1804 to 1867, and a part of Austria-Hungary from 1867 to 1918. Moravia was one of the five lands of Czechoslovakia founded in 1918. In 1928 it was merged with Czech Silesia, and then dissolved in 1949 during the abolition of the land system following the communist coup d'état. Its area of 22,623.41 km2 is home to more than 3 million people. The people are historically named Moravians, a subgroup of Czechs, the other group being called Bohemians. Moravia also had been home of a large German-speaking popu ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Oderské Vrchy
The Oderské vrchy (in English the Oder Mountains or, less commonly, Odra Highlands) is a mountain range in the Czech Republic. It is a geomorphological microregion, part of the Nízký Jeseník mountain range within the Eastern Sudetes (part of the Sudetes). The highest peak is Fidlův kopec at a height of . In the Oderské vrchy is the source of the Oder river, the second longest river in Poland. Geography The range is located entirely in Czech territory and create a slight highland within the Eastern Sudetes mountains. To the southeast, the Oderské vrchy borders the Moravian Gate that separates it from the Western Carpathians. Otherwise they are surrounded by other smaller mountain ranges that belong to Nízký Jeseník. Large part of the mountains are part of the Libavá military training area. Though recently reduced in size, this area, except for the trails to the source of the Oder river, is not open to tourists or visitors. Population The area is very sparsely populate ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
