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Bruntál
Bruntál (; german: Freudenthal) is a town in the Moravian-Silesian Region of the Czech Republic. It has about 16,000 inhabitants. It is located in the historical region of Czech Silesia. The historic town centre is well preserved and is protected by law as an urban monument zone. Administrative parts The area of the former village of Karlovec is an administrative part of Bruntál. It forms an exclave of the municipal territory. Etymology The original German name ''Freudenthal'' means "valley of joy" and refers to the town's location in a valley. The Czech name was later created by transcribing the German name. Geography Bruntál lies about north of Olomouc and northwest of Ostrava. It is situated in the Nízký Jeseník mountain range. The town lies in a valley surrounded by several hills. The highest point is the hill Uhlířský vrch at . The Černý Creek with its tributaries, the creeks Bukový, Kobylí and Vodárenský, flows through Bruntál. The Kobylí Pond is locat ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bruntál District
Bruntál District ( cs, okres Bruntál) is a district ('' okres'') within Moravian-Silesian Region of the Czech Republic. Its capital is Bruntál, but the largest town is Krnov. Part of the district belongs to Moravia, while another part belongs to Czech Silesia. List of municipalities Andělská Hora – Bílčice – Bohušov – Brantice – Bruntál – Břidličná – Býkov-Láryšov – Čaková – Dětřichov nad Bystřicí – Dívčí Hrad – Dlouhá Stráň – Dolní Moravice – Dvorce – Heřmanovice – Hlinka – Holčovice – Horní Benešov – Horní Město – Horní Životice – Hošťálkovy – Janov – Jindřichov – Jiříkov – Karlova Studánka – Karlovice – Krasov – Krnov – Křišťanovice – Leskovec nad Moravicí – Lichnov – Liptaň – Lomnice – Ludvíkov – Malá Morávka – Malá Štáhle – Město Albrechtice – Mezina – Milotice nad Opavou – Moravskoslezský ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Moravian-Silesian Region
The Moravian-Silesian Region ( cs, Moravskoslezský kraj; pl, Kraj morawsko-śląski; sk, Moravsko-sliezsky kraj) is one of the 14 administrative regions of the Czech Republic. Before May 2001, it was called the Ostrava Region ( cs, Ostravský kraj). The region is located in the north-eastern part of its historical region of Moravia and in most of the Czech part of the historical region of Silesia. The region borders the Olomouc Region to the west and the Zlín Region to the south. It also borders two other countries – Poland (Opole and Silesian Voivodeships) to the north and Slovakia (Žilina Region) to the east. It is a highly industrialized region, its capital Ostrava was actually called the "Steel Heart of the Republic". In addition, it has several mountainous areas where the landscape is relatively preserved. Nowadays, the economy of the region benefits from its location in the Czech/Polish/Slovak borderlands. Administrative division The Moravian-Silesian Region is d ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 Jese ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Slezská Harta Reservoir
Slezská Harta Reservoir ( cs, Vodní nádrž Slezská Harta) is an artificial reservoir and a rock-fill embankment dam in the Nízký Jeseník mountain range, Moravian-Silesian Region, Czech Republic. The dam is built on the upper course of the Moravice River. With the surface area of 8.7 km², it is one of the largest reservoirs in the country. It was constructed in 1987–1997. During the construction parts of six villages were demolished and subsequently flooded. The village of Karlovec was completely flooded and ceased to exist. Today only Church of Saint John of Nepomuk and several other abandoned buildings remain at the reservoir's shore. Villages of Dlouhá Stráň, Nová Pláň, Razová, Roudno and Leskovec nad Moravicí were also partially flooded and are today located on the shore of the reservoir. The main use of the reservoir is to supply enough water in case of unfavorable conditions to the Kružberk reservoir, which supplies drinking water for the Ostrava ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Districts Of The Czech Republic
Districts of the Czech Republic are territorial units, formerly used as second-level administrative divisions of the Czech Republic. After their primary administrative function has been abolished in 2003, they still exist for the activities of specific authorities and as statistical units. Their administrative function was moved to selected municipalities. Establishment In 1960, Czechoslovakia was re-divided into districts ('' okres'', plural ''okresy'') often without regard to traditional division and local relationships. In the area of the Czech Republic, there were 75 districts; the 76th Jeseník District was split in the 1990s from Šumperk District. Three consisted only of statutory cities Brno, Ostrava and Plzeň which gained the status of districts only in 1971; Ostrava and Plzeň districts were later expanded. The capital city of Prague has a special status, being considered a municipality and region at the same time and not being a part of any district, but ten district ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Uničov
Uničov (; german: Mährisch Neustadt) is a town in Olomouc District in the Olomouc Region of the Czech Republic. It has about 11,000 inhabitants. The historic town centre is well preserved and is protected by law as an urban monument zone. Administrative parts Villages of Benkov, Brníčko, Dětřichov, Dolní Sukolom, Horní Sukolom, Nová Dědina, Renoty and Střelice are administrative parts of Uničov. Geography Uničov is located about northwest of Olomouc. It lies in the Upper Morava Valley lowland on the Oslava River. History Uničov is one of the seven royal Moravian towns. It was founded around 1213 by the Margrave Vladislaus III, the brother of King Ottokar I of Bohemia. It received Magdeburg rights in 1223 and was granted further privileges by Ottokar's successor King Wenceslaus I in 1234. The town was to become a centre of ore and precious metal mining, but the deposits were not so plentiful. The town therefore reoriented itself to trade and crafts, and in 1327 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lapilli
Lapilli is a size classification of tephra, which is material that falls out of the air during a volcanic eruption or during some meteorite impacts. ''Lapilli'' (singular: ''lapillus'') is Latin for "little stones". By definition lapilli range from in diameter. A pyroclastic particle greater than 64 mm in diameter is known as a volcanic bomb when molten, or a volcanic block when solid. Pyroclastic material with particles less than 2 mm in diameter is referred to as volcanic ash. Formation Lapilli are spheroid-, teardrop-, dumbbell- or button-shaped droplets of molten or semi-molten lava ejected from a volcanic eruption that fall to earth while still at least partially molten. These granules are not accretionary, but instead the direct result of liquid rock cooling as it travels through the air. Lapilli tuffs are a very common form of volcanic rock typical of rhyolite, andesite and dacite pyroclastic eruptions, where thick layers of lapilli can be deposited during a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Volcanic Bombs
A volcanic bomb or lava bomb is a mass of partially molten rock (tephra) larger than 64 mm (2.5 inches) in diameter, formed when a volcano ejects viscous fragments of lava during an eruption. Because volcanic bombs cool after they leave the volcano, they are extrusive igneous rocks. Volcanic bombs can be thrown many kilometres from an erupting vent, and often acquire aerodynamic shapes during their flight. Bombs can be extremely large; the 1935 eruption of Mount Asama in Japan expelled bombs measuring 5–6 m (16-20 ft) in diameter up to from the vent. Volcanic bombs are a significant volcanic hazard, and can cause severe injuries and death to people in an eruption zone. One such incident occurred at Galeras volcano in Colombia in 1993; six people near the summit were killed and several seriously injured by lava bombs when the volcano erupted unexpectedly. On July 16, 2018, 23 people were injured on a tour boat near the Kilauea volcano as a result of a basketb ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Volcanic Ash
Volcanic ash consists of fragments of rock, mineral crystals, and volcanic glass, created during volcano, volcanic eruptions and measuring less than 2 mm (0.079 inches) in diameter. The term volcanic ash is also often loosely used to refer to all explosive eruption products (correctly referred to as ''tephra''), including particles larger than 2 mm. Volcanic ash is formed during explosive volcanic eruptions when dissolved gases in magma expand and escape violently into the atmosphere. The force of the gases shatters the magma and propels it into the atmosphere where it solidifies into fragments of volcanic rock and glass. Ash is also produced when magma comes into contact with water during phreatomagmatic eruptions, causing the water to explosively flash to steam leading to shattering of magma. Once in the air, ash is transported by wind up to thousands of kilometres away. Due to its wide dispersal, ash can have a number of impacts on society, including animal a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kostel Nanebevzetí P
Kostel may refer to: * Kostel, Kostel, a settlement in the Municipality of Kostel, Slovenia * Municipality of Kostel, Slovenia * Kostel, Croatia, a village near Pregrada, Croatia * Kostel, German name of the Czech town of Podivín * Kostel Pribićki, a village near Krašić, Croatia * Kostel, Bulgaria, a village in Elena Municipality Elena Municipality ( bg, Община Елена) is a municipality ('' obshtina'') in Veliko Tarnovo Province, Central-North Bulgaria, located on the northern slopes of the central Stara planina mountain in the area of the so-called Fore-Balka ... * Pietrapelosa {{geodis ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Obec
Obec (plural: ''obce'') is the Czech language, Czech and Slovak language, Slovak word for a municipality (in the Czech Republic, in Slovakia and abroad). The literal meaning of the word is "Intentional community, commune" or "community". It is the smallest administrative unit that is governed by elected representatives. Cities and towns are also municipalities. Definition Legal definition (according to the Czech code of law with similar definition in the Slovak code of law) is: ''"The municipality is a basic territorial self-governing community of citizens; it forms a territorial unit, which is defined by the boundary of the municipality."'' Every municipality is composed of one or more cadastre, cadastral areas. Every municipality is composed of one or more administrative parts, usually called town parts or villages. A municipality can have its own flag and coat of arms. Czech Republic Almost whole area of the republic is divided into municipalities, with the only exception be ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ottokar I Of Bohemia
Ottokar I ( cs, Přemysl Otakar I.; c. 1155 – 1230) was Duke of Bohemia periodically beginning in 1192, then acquired the title of King of Bohemia, first in 1198 from Philip of Swabia, later in 1203 from Otto IV of Brunswick and in 1212 (as hereditary) from Frederick II. He was one of the most eminent members of the Přemyslid dynasty. Early years Ottokar's parents were Vladislaus II, Duke of Bohemia, and Judith of Thuringia. His early years were passed amid the anarchy that prevailed everywhere in the country. After several military struggles, he was recognized as ruler of Bohemia by Holy Roman Emperor Henry VI in 1192. He was, however, soon overthrown for joining a conspiracy of German princes to bring down the Hohenstaufen dynasty. In 1197, Ottokar forced his brother, Duke Vladislaus III Henry, to abandon Bohemia to him and to content himself with Moravia. Taking advantage of the civil war in Germany between the Hohenstaufen claimant Philip of Swabia and the Welf cand ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
