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Nízký Jeseník
Nízký Jeseník (, ) is a flat highland and Geomorphological division of the Czech Republic, geomorphological mesoregion of the Czech Republic. It is located in the east of the country in the Olomouc Region, Olomouc and Moravian-Silesian Region, Moravian-Silesian regions. Nízký Jeseník is the largest Czech geomorphological mesoregion, 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. 'Fraxinus, ash'. ''Jeseník'' (respectively ''Jesenný potok'') 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 inclu ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Czech Republic
The Czech Republic, also known as Czechia, and historically known as Bohemia, is a landlocked country in Central Europe. The country 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 Humid continental climate, 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 Estate of the Holy Roman Empire in 1002 and became Kingdom of Bohemia, a kingdom in 1198. Following the Battle of Mohács in 1526, all of the Lands of the Bohemian Crown were gradually integrated into the Habsburg monarchy. Nearly a hundred years later, the Protestantism, Protestant Bohemian Revolt led to the Thirty Years' War. After the Battle of White ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Upper Morava Valley
The Upper Morava Valley () is a lowland and a geomorphological mesoregion of the Czech Republic. It is located in the Olomouc and Zlín regions. Its name is derived from the Morava river that forms the axis of the territory. Geomorphology The Upper Morava Valley is a mesoregion of the Western Outer Subcarpathia within the Outer Subcarpathia. It is a trench depression, filled with Neogene and Quaternary sediments. The lowland is further subdivided into the microregions of Holešov Plateau, Prostějov Uplands, Central Moravian Floodplain and Uničov Plateau. The area is poor in peaks. It is the largest real plain in the territory of the Czech Republic, in which the inclination of the slopes consistently does not exceed 1°. The highest peak is Horka (also called Šumvaldská horka) at above sea level. Geography The territory is elongated from north to south. The maximum length is and the width is almost . The lowland has an area of and an average elevation of . The territory ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Oder
The Oder ( ; Czech and ) is a river in Central Europe. It is Poland's second-longest river and third-longest within its borders after the Vistula and its largest tributary the 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). The origin of this name is said by onomastician Jürgen Udolph to come from the Illyrian word ''*Adra'' (“water vein”). Ptolemy knew the modern Oder as the Συήβος (''Suebos''; Latin ''Suevus''), a name apparen ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Krnov
Krnov (; , or ''Krnów'') is a town in Bruntál District in the Moravian-Silesian Region of the Czech Republic. It has about 23,000 inhabitants. Administrative division Krnov consists of three municipal parts (in brackets population according to the 2021 census): *Pod Bezručovým vrchem (14,445) *Pod Cvilínem (7,099) *Krásné Loučky (573) Geography Krnov is located about northwest of Opava and northwest of Ostrava, in the historic region of Czech Silesia on the border with Poland. The town is situated at the confluence of the rivers Opava (river), Opava and Opavice. The northern part of the territory with the town proper lies in the Opawskie Mountains, Zlatohorská Highlands, the western and the southern part lie in the Nízký Jeseník range. A small part on the southeast extends into the Opava Hilly Land. The highest point is the hill Bednářský vrch at above sea level. History The first written mention of Krnov is from 1240. At the latest in 1269 and probably alrea ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ostrava
Ostrava (; ; ) is a city in the north-east of the Czech Republic and the capital of the Moravian-Silesian Region. It has about 283,000 inhabitants. It lies from the border with Poland, at the confluences of four rivers: Oder, Opava (river), Opava, Ostravice (river), Ostravice and Lučina (river), 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 (Karviná District), 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 t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Olomouc
Olomouc (; ) is a city in the Czech Republic. It has about 103,000 inhabitants, making it the Statutory city (Czech Republic), sixth largest city in the country. It is the administrative centre of the Olomouc Region. Located on the Morava (river), Morava River, the city is the ecclesiastical metropolis and was a historical co-capital city of Moravia, before having been occupied by the Military of the Swedish Empire, Swedish army during the Thirty Years' War. The historic city centre is well preserved and is protected as Cultural monument (Czech Republic)#Monument reservations, urban monument reservation. The Holy Trinity Column in Olomouc, Holy Trinity Column was listed as a UNESCO World Heritage Site in 2000 for its quintessential Baroque architecture, Baroque style and symbolic value. Administrative division Olomouc consists of 26 municipal parts (in brackets population according to the 2021 census): *Olomouc (13,446) *Bělidla (834) *Černovír (1,010) *Chomoutov (1,070) *Ch ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Stratovolcano
A stratovolcano, also known as a composite volcano, is a typically conical volcano built up by many alternating layers (strata) of hardened lava and tephra. Unlike shield volcanoes, stratovolcanoes are characterized by a steep profile with a summit crater and explosive eruptions. Some have collapsed summit craters called calderas. The lava flowing from stratovolcanoes typically cools and solidifies 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 can travel as far as 8 km (5 mi). The term ''composite volcano'' is used because strata are usually mixed and uneven instead of neat layers. They are among the most common types of volcanoes; more than 700 stratovolcanoes have erupted lava during the Holocene Epoch (the last 11,700 years), and many ol ... [...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), as well as the current and most recent of the twelve periods of the Phanerozoic eon. 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); a proposed third epoch, the Anthropocene, was rejected in 2024 by IUGS, the governing body of the ICS. The Quaternary is typically defined by the Quaternary glaciation, 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 succ ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Proterozoic
The Proterozoic ( ) is the third of the four geologic eons of Earth's history, spanning the time interval from 2500 to 538.8 Mya, and is the longest eon of Earth's geologic time scale. It is preceded by the Archean and followed by the Phanerozoic, and is the most recent part of the Precambrian "supereon". The Proterozoic is subdivided into three geologic eras (from oldest to youngest): the Paleoproterozoic, Mesoproterozoic and Neoproterozoic. It covers the time from the appearance of free oxygen in Earth's atmosphere to just before the proliferation of complex life on the Earth during the Cambrian Explosion. The name ''Proterozoic'' combines two words of Greek origin: meaning "former, earlier", and , meaning "of life". Well-identified events of this eon were the transition to an oxygenated atmosphere during the Paleoproterozoic; the evolution of eukaryotes via symbiogenesis; several global glaciations, which produced the 300 million years-long Huronian glaciation ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Červená Hora (Nízký Jeseník)
Červená hora (meaning 'red mountain') is a mountain in the Nízký Jeseník range in the Moravian-Silesian Region of the Czech Republic. It is located in the territory of Budišov nad Budišovkou. With above sea level it is the highest hill of the Domašov Highlands, which are a part of the Nízký Jeseník, and the highest point in the Opava District. A hydrometeorological station and a station of the European Fireball Network at the same time is located here. Climate Červená hora has a humid continental climate (Köppen Köppen is a German surname. Notable people with the surname include: * Bernd Köppen (1951–2014), German pianist and composer * Carl Köppen (1833-1907), German military advisor in Meiji era Japan * Edlef Köppen (1893–1939), German author ... ''Dfb''). The annual average temperature is , the hottest month in July is , and the coldest month is in January. The annual precipitation is , of which July is the wettest with , while February is the d ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Moravia
Moravia ( ; ) is a historical region in the eastern Czech Republic, roughly encompassing its territory within the Danube River's drainage basin. It is 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 First Czechoslovak Republic, Czechoslovakia founded in 1918. In 1928 it was merged with Czech Silesia, and then dissolved in 1948 during the abolition of the land system following the 1948 Czechoslovak coup d'état, communist coup d'état. Its area of 22,623.41 km2 is home to about 3.0 million of the Czech Republic's 10.9 million inhabitants. The people are historically named Moravians, a subgroup of Czechs, the other group being calle ... [...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 popul ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
