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Upper Palatine Hills
The Upper Palatine Hills (german: Oberpfälzisches Hügelland, also ''Oberpfälzisches Hügel- und Bergland'' or ''Oberpfälzer Bruchschollenland'') is a Hercynian range of rolling hills ('' Hügelland'') and valleys running from the Upper Palatine-Bavarian Forest in the (north-)east and the Franconian Jura in the (south-)west. It lies mostly within the Bavarian province of Upper Palatinate, hence the name. The range, which is oriented northwest to southeast, is about 100 kilometres long, but only between 7 and 35 kilometres wide and covers and area of 2,000 km2. The best known settlements are (from northwest to southeast) Weiden (Ostrand), Amberg and Schwandorf. Sources and external links * BfN The German Federal Agency for Nature Conservation (german: Bundesamt für Naturschutz, ''BfN'') is the German government's scientific authority with responsibility for national and international nature conservation. BfN is one of the government' ... landscape fact files: *Upper ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Upper Palatinate
The Upper Palatinate (german: Oberpfalz, , ) is one of the seven administrative districts of Bavaria, Germany, and is located in the east of Bavaria. Geography The Upper Palatinate is a landscape with low mountains and numerous ponds and lakes in its lowland regions. By contrast with other regions of Germany it is more rural in character and more sparsely settled. It borders (clockwise from the north) on Upper Franconia, the Czech Republic, Lower Bavaria, Upper Bavaria and Middle Franconia. Notable regions are: * Stiftland, former estate and territorial lordship of Waldsassen Abbey with the market town of Konnersreuth, Fockenfeld Abbey, the town of Waldsassen and about 150 other villages. * Upper Palatine Forest with deep valleys and many castles * Upper Palatine Lake District with the Steinberger See * Upper Palatine Jura, part of the Franconian Jura * Steinwald including the Teichelberg and Pechbrunn * Waldnaab/ Wondreb Depression * Bavarian Forest, together with ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Upper Franconia
Upper Franconia (german: Oberfranken) is a ''Regierungsbezirk'' (administrative 'Regierungs''region 'bezirk'' of the state of Bavaria, southern Germany. It forms part of the historically significant region of Franconia, the others being Middle Franconia and Lower Franconia, which are all now part of the German Federal State of Bayern (''Bavaria''). With more than 200 independent breweries which brew approximately 1000 different types of beer, Upper Franconia has the world's highest brewery-density per capita. A special Franconian beer route (''Fränkische Brauereistraße'') runs through many popular breweries. Geography The administrative region borders on Thuringia (''Thüringen'') to the north, Lower Franconia (''Unterfranken'') to the west, Middle Franconia (''Mittelfranken'') to the south-west, and Upper Palatinate (''Oberpfalz'') to the south-east, Saxony (''Sachsen'') to the north-east and the Czech Republic to the east. History After the founding of the Kingdom of Bava ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bavaria
Bavaria ( ; ), officially the Free State of Bavaria (german: Freistaat Bayern, link=no ), is a state in the south-east of Germany. With an area of , Bavaria is the largest German state by land area, comprising roughly a fifth of the total land area of Germany. With over 13 million inhabitants, it is second in population only to North Rhine-Westphalia, but due to its large size its population density is below the German average. Bavaria's main cities are Munich (its capital and largest city and also the third largest city in Germany), Nuremberg, and Augsburg. The history of Bavaria includes its earliest settlement by Iron Age Celtic tribes, followed by the conquests of the Roman Empire in the 1st century BC, when the territory was incorporated into the provinces of Raetia and Noricum. It became the Duchy of Bavaria (a stem duchy) in the 6th century AD following the collapse of the Western Roman Empire. It was later incorporated into the Holy Roman Empire, became an ind ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Upper Palatine-Upper Main Hills
The Upper Palatine-Upper Main Hills (german: Oberpfälzisch-Obermainisches Hügelland), also called the Upper Palatine-Upper Main Hills and Uplands (''Oberpfälzisch-Obermainisches Hügel- und Bergland'') form a landscape of low, rolling hills between the Franconian Jura in the southwest and (from northwest to southeast) the Franconian Forest, Fichtel Mountains and Upper Palatine Forest in the northeast. The region runs from northwest to southeast and is about 170 kilometres long, but only 7 to 35 kilometres wideE. Meynen und J. Schmithüsen: Handbuch der naturräumlichen Gliederung Deutschlands – Bundesanstalt für Landeskunde, Remagen/Bad Godesberg 1953-1962 (9 Lieferungen in 8 Büchern, aktualisierte Karte 1:1.000.000 mit Haupteinheiten 1960) and lies mainly in the Bavarian administrative provinces of Upper Franconia and Upper Palatinate; small elements, however, also lie within the Thuringian county of Sonneberg. Its best known settlements are (from northwest to southeast) S ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rotliegendes
The Rotliegend, Rotliegend Group or Rotliegendes (german: the underlying red) is a lithostratigraphic unit (a sequence of rock strata) of latest Carboniferous to Guadalupian (middle Permian) age that is found in the subsurface of large areas in western and central Europe. The Rotliegend mainly consists of sandstone layers. It is usually covered by the Zechstein and lies on top of regionally different formations of late Carboniferous age. The name Rotliegend has in the past not only been used to address the rock strata themselves, but also the time span in which they were formed (in which case the Rotliegend was considered a series or subsystem of the Permian). This time span corresponds roughly with the length of the Cisuralian epoch. Facies and formation In large parts of Pangaea, the last phases of the Hercynian orogeny were still ongoing during the start of the Permian. At the same time local crustal extension formed intramontane basins such as the large Permian Basin whic ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bunter Sandstone
The Buntsandstein (German for ''coloured'' or ''colourful sandstone'') or Bunter sandstone is a lithostratigraphic and allostratigraphic unit (a sequence of rock strata) in the subsurface of large parts of west and central Europe. The Buntsandstein predominantly consists of sandstone layers of the Lower Triassic series and is one of three characteristic Triassic units, together with the Muschelkalk and Keuper that form the Germanic Trias Supergroup. The Buntsandstein is similar in age, facies and lithology with the Bunter of the British Isles. It is normally lying on top of the Permian Zechstein and below the Muschelkalk. In the past the name Buntsandstein was in Europe also used in a chronostratigraphic sense, as a subdivision of the Triassic system. Among reasons to abandon this use was the discovery that its base lies actually in the latest Permian. Origin The Buntsandstein was deposited in the Germanic Basin, a large sedimentary basin that was the successor of the smal ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Variscan Orogeny
The Variscan or Hercynian orogeny was a geologic mountain-building event caused by Late Paleozoic continental collision between Euramerica (Laurussia) and Gondwana to form the supercontinent of Pangaea. Nomenclature The name ''Variscan'', comes from the Medieval Latin name for the district '' Variscia'', the home of a Germanic tribe, the Varisci; Eduard Suess, professor of geology at the University of Vienna, coined the term in 1880. (Variscite, a rare green mineral first discovered in the Vogtland district of Saxony in Germany, which is in the Variscan belt, has the same etymology.) ''Hercynian'', on the other hand, derives from the Hercynian Forest. Both words were descriptive terms of strike directions observed by geologists in the field, ''variscan'' for southwest to northeast, ''hercynian'' for northwest to southeast. The ''variscan'' direction reflected the direction of ancient fold belts cropping out throughout Germany and adjacent countries and the meaning shifted from d ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hügelland
''Hügelland'' is a type of landscape consisting of low rolling hills whose topography or surface structure lies between that of a lowland region (plains or river terraces) and that of a more rugged hill range or low mountain range. The term is German and has no exact equivalent in English, but is often translated as "hill country", "hilly terrain", "upland(s)" or "gently undulating" or "rolling country", or "rolling countryside". It is derived from ''Hügel'', a low hill or hillock and appears frequently as a proper name for this type of terrain. The term ''Hügelland'' is not unambiguously defined, even in German. For example, on the plains of North Germany, Poland or Hungary it may be applied to terrain with a height variation of just 50 metres, whilst in the Alpine Foreland or in the Voralpen it might refer to terrain with a height difference of at least 100–200 metres. On the other hand, some scholars prefer to define ''Hügelland'' by its height above sea level; for exa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Upper Palatine-Bavarian Forest
The Upper Palatine-Bavarian Forest (german: Oberpfälzisch-Bayerische Wald), (no. D63 or 40) is a natural region in Germany in the northeast of Bavaria. It mainly comprises the low mountain ranges of the Bavarian Forest and Upper Palatine Forest which are up to 1456 m high and border on the Bohemian Massif immediately inside the Czech Republic's southwestern border with Germany. Division into geographical units *40 (=D63) Upper Palatine-Bavarian Forest **400 Upper Palatine Forest - East **401 Upper Palatine Forest - West **402 Cham-Furth Depression **403 Bavarian Forest - North **404 Regen Depression **405 Bavarian Forest - South **406 Falkensteiner Vorwald **407 Lallinger Winkel **408 Passau Abteiland and Neuburg Forest **409 Wegscheid Plateau Neighbouring main unit groups are: * 39 (= D48) Thuringian-Franconian Highlands * 08 (= D61) Franconian Jura * 07 (= D62) Upper Palatine-Upper Main Hills * 06 Lower Bavarian Hills The Lower Bavarian Upland, Lower Bavarian Hill ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Franconian Jura
The Franconian Jura ( , , or ) is an upland in Franconia, Bavaria, Germany. Located between two rivers, the Danube in the south and the Main in the north, its peaks reach elevations of up to and it has an area of some 7053.8 km2. Emil Meynen, Josef Schmithüsen: ''Handbuch der naturräumlichen Gliederung Deutschlands.'' Bundesanstalt für Landeskunde, Remagen/Bad Godesberg 1953–1962 (9 editions in 8 volumes, updated map 1:1,000,000 scale with major units, 1960). Large portions of the Franconian Jura are part of the Altmühl Valley Nature Park. The scenic meanders and gorges formed by the river Altmühl draw tourists to visit the region. Geologically, the Franconian Jura is the eastern continuation of the Swabian Jura. The mountain chains are separated from each other by the impact crater of the Nördlinger Ries The Nördlinger Ries is an impact crater and large circular depression in western Bavaria and eastern Baden-Württemberg. It is located north of the Danube in ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Weiden In Der Oberpfalz
Weiden in der Oberpfalz (official name: Weiden i.d.OPf.; Northern Bavarian: ''Weidn in da Owapfalz'') is a district-free city in Bavaria, Germany. It is located east of Nuremberg and west of the Czech border. A branch of the German Army is located here. History Weiden in der Oberpfalz was first mentioned in a document in 1241 as Weiden. It is assumed that the first settlements in Weiden are dated the year 1000. Located at the intersection of two major trading routes (Goldene Strasse and Magdeburger Strasse), Weiden soon became an important trading center with a population of 2,200 in 1531. An economic boom came along in 1863 when Weiden was connected to the railroad network. Some major companies of the glass and china industry settled in Weiden and the population increased. Districts Incorporations into Weiden in der Oberpfalz *January 1, 1914, Moosbürg, district of Moosbürg, Ermersricht, Fichtenbühl, Leihstadtmühle *February 1, 1915, Tröglersricht and Zollhaus *July 1, 1 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Amberg
Amberg () is a town in Bavaria, Germany. It is located in the Upper Palatinate, roughly halfway between Regensburg and Bayreuth. In 2020, over 42,000 people lived in the town. History The town was first mentioned in 1034, at that time under the name Ammenberg. It became an important trading centre in the Middle Ages, exporting mainly iron ore and iron products. In 1269, together with Bamberg, the town became subordinate to the Wittelsbach dynasty that ruled Bavaria. In 1329 the town and the entire region fell to the Palatinate branch of the Wittelsbach family. The region adopted the name Upper Palatinate. It was no longer part of the duchy of Bavaria politically, though in geographic terms it was regarded as Bavarian and the region was part of the Bavarian circle in the organization of the Imperial Circles. In the 16th century, the rulers of Upper Palatinate turned to Protestantism. The town turned to Lutheranism. Later attempts of the ruling family to introduce the more rad ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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