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Pfälzerwald
The Palatinate Forest (; ), sometimes also called the Palatine Forest, is a low-mountain region in southwestern Germany, located in the Palatinate in the state of Rhineland-Palatinate. The forest is a designated nature park () covering 1,771 km2 and its highest elevation is the Kalmit (672.6 m). Together with the northern part of the adjacent Vosges Mountains in France it forms the UNESCO-designated Palatinate Forest-North Vosges Biosphere Reserve. Geography Topography The Palatinate Forest, together with the Vosges south of the French border, from which it has no morphological separation, is part of a single central upland region of about 8,000 km2 in area, that runs from the Börrstadt Basin (a line from Winnweiler via Börrstadt and Göllheim) to the Burgundian Gate (on the line Belfort–Ronchamp– Lure) and which forms the western boundary of the Upper Rhine Plain. This landscape forms, in turn, the eastern part of the very extensive eastern scarplands ...
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Palatinate Forest Nature Park
The Palatinate Forest Nature Park () lies in the south of Rhineland-Palatinate in Germany and borders on France. The nature park covers an area of and some 76% of its area is under the woods of the Palatinate Forest, the largest contiguous forest region in Germany. Together with parts of northern Alsace and Lorraine, it forms the Palatinate Forest-North Vosges Biosphere Reserve and has an impressive Bunter sandstone landscape. The park is the responsibility of the ''Naturpark Pfälzerwald e.V.'' founded on 20 July 1982. The members of the organisation are those districts and towns on whose territory the nature park is located as well as the Palatinate Regional Association and numerous sports clubs and environmental groups. Many business are involved in the work of the nature park which enables the independence of individual functional and regional interests to be guaranteed. The aim of the organisation is to develop in a coherent way the nature park and the biosphere reserve of ...
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Kalmit
The Kalmit is the highest peak in the Palatinate Forest and the second highest (after the Donnersberg) in the Palatinate region of Germany. It is and located south of the town of Neustadt an der Weinstraße. The mountain attracts many tourists thanks to the numerous footpaths leading to its summit, its mountaintop restaurant, extensive views over the Palatinate wine region and striking rock formations on its forest-clad mountainsides. Geography Location The mountain lies within the municipal forest of the wine village of Maikammer and southwest of the independent town of Neustadt an der Weinstraße. Several lower peaks are grouped around the main summit, including the Zwergberg (589.3 m) to the north, the Taubenkopf (603.8 m) to the northeast, the Kanzel (531.7 m) and the Wetterkreuzberg (400.7 m) to the southeast, the Breitenberg (545.2 m) to the south and the Hüttenberg (591.2 m) to the southwest. On the Hüttenberg ridge there is a blo ...
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Palatinate Forest-North Vosges Biosphere Reserve
The Franco- German Palatinate Forest-North Vosges Biosphere Reserve (, ) was created in 1998 as the first UNESCO trans-boundary biosphere reserve in Europe. The German part became the 12th of 16 biosphere reserves in Germany, and the French part, the 6th of 14 in France. Description The biosphere reserve is a fusion of the older Palatinate Forest Nature Park in Germany and Northern Vosges Regional Nature Park in France, covering a total area of 3018 km2, with 1785 km2 in Germany and 1277 km2 in France respectively. The population is around 335 175 , with 253 390 living in the German part of the Reserve, compared with just over 81 785 on the French side in 2018. This difference in population is not reflected in the number of communes, as there are 142 on the German side versus 111 on the French side for a total of 253 communes. Average population density, at just over 76 inhabitants per square kilometer, is fairly low for a Western European region, although it is higher on the ...
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Palatinate (region)
The Palatinate (; ; Palatine German language, Palatine German: ''Palz''), or the Rhenish Palatinate (''Rheinpfalz''), is a historical region of Germany. The Palatinate occupies most of the Southern Germany, southern quarter of the German States of Germany, federal state of Rhineland-Palatinate (''Rheinland-Pfalz''), covering an area of with about 1.4 million inhabitants. Its residents are known as Palatines (''Pfälzer''). Geography The Palatinate borders Saarland in the west, historically also comprising the state's Saarpfalz-Kreis, Saarpfalz District. In the northwest, the Hunsrück mountain range forms the border with the Rhineland region. The eastern border with Hesse and the Baden-Württemberg, Baden region runs along the Upper Rhine river, while the left bank, with Mainz and Worms, Germany, Worms as well as the Selz basin around Alzey, belong to the Rhenish Hesse region. In the south, the German-France, French border separates the Palatinate from Alsace. One-thir ...
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Landstuhl Bruch
The Landstuhl Marsh or Landstuhl Bog (, ''Westricher Moorniederung'' or ''Westpfälzische Moorniederung'') is a region in West Palatinate in the German state of Rhineland-Palatinate. According to the Handbook of the Natural Region Divisions of Germany Landstuhl Marsh, which covers an area of the 67 km²,{{GeoQuelle, DE-RP, NRT is part of the Kaiserslautern Basin and lies in the centre of it. Within the North French Scarplands the Kaiserslautern Basin is a sub-unit of the Saar-Nahe Upland and Tableland. Geography The Landstuhl Marsh lies at an elevation of 200 metres above and is a bowl around 30 kilometres long and up to 7 kilometres wide running from Waldmohr in the southwest via Bruchmühlbach-Miesau, Ramstein-Miesenbach and Landstuhl to the city of Kaiserslautern in the northeast. In the north it is bounded by the North Palatine Uplands, which climb gradually from the lowland. In the south, by contrast, the Sickingen Heights form a very clear escarpment of ...
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Westrich Plateau
The Westrich Plateau (),Helmut Beeger et al.: "Die Landschaften von Rheinhessen-Pfalz − Benennung und räumliche Abgrenzung". In: ''Berichte zur deutschen Landeskunde'', Vol. 63, Part 2, Trier, 1989, pp. 327–359 also Zweibrücken Westrich (''Zweibrücker Westrich'')For example in the Handbuch der naturräumlichen Gliederung Deutschlands. or Southwest Palatine Plateau (''Südwestpfälzische Hochfläche''), is a List of landscapes in Rhineland-Palatinate, landscape in the German state of Rhineland-Palatinate, with small areas also in the Saarland (Saarpfalz-Kreis). Its heart is in the southwest of the Palatinate region and it is part of the historic region of Westrich (historic region), Westrich. Geography Structure and boundaries The Westrich Plateau consists mainly of the Sickingen Heights in the north and the Zweibrücken Hills in the south which, morphologically, belong more to northeastern Lorraine (region), Lorraine in France). The main plateau falls away in a mark ...
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North Palatine Uplands
The North Palatine Uplands (, ), sometimes shortened to Palatine Uplands (''Pfälzer Bergland''), is a low mountain range and landscape unit in the German state of Rhineland-Palatinate and belongs mainly to the Palatinate region. It is part of the Saar-Nahe Uplands. Geography Location The North Palatine Uplands lie – roughly stated – between St. Wendel in the state of Saarland to the west and three towns belonging to Rhineland-Palatinate: Alzey to the east, Kaiserslautern to the south and Bad Kreuznach to the north, although these towns are not actually within the region itself. The North Palatine Uplands thus links the landscapes of the Palatine Forest, Saar-Hunsrück Nature Park, Naheland and Rheinhessen. To the northwest its boundary with Naheland is not always clear. A rough guide is the heavily folded ridge north of the Glan river with a height different of as much as 300 metres in place. The North Palatine Uplands fall mainly within the districts of ...
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Upper Rhine Plain
The Upper Rhine Plain, Rhine Rift Valley or Upper Rhine Graben ( German: ''Oberrheinische Tiefebene'', ''Oberrheinisches Tiefland'' or ''Oberrheingraben'', French: ''Vallée du Rhin'') is a major rift, about and on average , between Basel in the south and the cities of Frankfurt/Wiesbaden in the north. Its southern section straddles the France–Germany border. It forms part of the European Cenozoic Rift System, which extends across Central Europe. The Upper Rhine Graben formed during the Oligocene, as a response to the evolution of the Alps to the south. It remains active to the present day. Today, the Rhine Rift Valley forms a downfaulted trough through which the river Rhine flows. Formation The Upper Rhine Plain was formed during the Early Cenozoic era, during the Late Eocene epoch. At this time, the Alpine Orogeny, the major mountain building event that was to produce the Alps, was in its early stages. The Alps were formed because the continents of Europe and Africa coll ...
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Donnersberg
The Donnersberg (; literally: "thunder mountain") is the highest peak of the Palatinate () region of Germany. The mountain lies between the towns of Rockenhausen and Kirchheimbolanden, in the Donnersbergkreis district, which is named after the mountain. The highway A63 runs along the southern edge of the Donnersberg. European walking route E8 runs across the mountain. The highest point of the Donnersberg is the rock ''Königstuhl'' ("king's seat") at 687 metres above sea level. The mountain has a diameter of about 7 kilometres and covers an area of some 2,400 hectares. The Donnersberg was formed by volcanic activity during the Permian, in the transition period between the lower and upper Rotliegend strata. The name Donnersberg is thought to refer to Donar, the Germanic god of thunder, a theory supported by the fact that the Romans dubbed the Donnersberg ''Mons Jovis'' after their god of thunder, Jupiter. According to other theories, the name of the mountain was derived fro ...
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Muschelkalk
The Muschelkalk (German for "shell-bearing limestone"; ) is a sequence of sedimentary rock, sedimentary rock strata (a lithostratigraphy, lithostratigraphic unit) in the geology of central and western Europe. It has a Middle Triassic (240 to 230 million years) age and forms the middle part of the three-part Germanic Trias (that gives the Triassic its name) lying above the older Buntsandstein and below the younger Keuper. The Muschelkalk ("mussel-chalk") consists of a sequence of limestone and Dolomite (rock), dolomite Bed (geology), beds. In the past, the time span in which the Muschelkalk was deposited could also be called "Muschelkalk". In modern stratigraphy, however, the name only applies to the layers of rock. Occurrence The name ''Muschelkalk'' was first used by German geologist Georg Christian Füchsel (1722-1773). In 1834, Friedrich August von Alberti included it into the Triassic system (stratigraphy), system. The name indicates a characteristic feature of the unit, name ...
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Kaiserslautern
Kaiserslautern (; ) is a town in southwest Germany, located in the state of Rhineland-Palatinate at the edge of the Palatinate Forest. The historic centre dates to the 9th century. It is from Paris, from Frankfurt am Main, 666 kilometers (414 miles) from Berlin, and from Luxembourg. Kaiserslautern is home to about 100,000 people. Additionally, approximately 45,000 NATO military personnel are based in the city and its surrounding district ('' Landkreis Kaiserslautern''). History and demographics Prehistoric settlement in the area of what is now Kaiserslautern has been traced to at least 800 BC. Some 2,500-year-old Celtic tombs were uncovered at Miesau, a town about west of Kaiserslautern. The recovered relics are now in the Museum for Palatinate History at Speyer. Medieval period Kaiserslautern received its name from the favourite hunting retreat of Holy Roman Emperor Frederick Barbarossa who ruled the Holy Roman Empire from 1155 until 1190. The small river Lauter made t ...
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Rotliegendes
The Rotliegend, Rotliegend Group or Rotliegendes () 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 which covered parts of present ...
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