Rammert
The Rammert is a forested hill range, up to , in the Keuper Uplands of central Baden-Württemberg, which belongs to the natural region major unit of Schönbuch and Glemswald in the Swabian Keuper-Lias Land. It continues the Schönbuch to the south(west) and is separated from it by the Tübingen Bay (''Tübinger Stufenrandbucht'') at the Neckar near Tübingen.Emil Meynen, Josef Schmithüsen: ''Handbuch der naturräumlichen Gliederung Deutschlands.'' Bundesanstalt für Landeskunde, Remagen/Bad Godesberg, 1953–1962 (9 issues in 8 books, updated (1960) 1:1,000,000 map with major units).Friedrich Huttenlocher: ''Geographische Landesaufnahme: Die naturräumlichen Einheiten auf Blatt 178 Sigmaringen.'' Bundesanstalt für Landeskunde, Bad Godesberg 1959. â†Online map(pdf, 6.1 MB)The Rammert is unit number 104.11, the Bay is 104.10. The majority of the ridge lies in the county of Tübingen, with small elements in the county of Zollernalbkreis. Geography The Rammert extends for 18  ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Keuper Uplands
The Keuper Uplands (german: Keuperbergland or, more rarely ''Keuperwaldberge'') are part of the South German Scarplands and cover an area of about 3,200 square kilometres. The following regions belong to the Keuper Uplands (from southwest to northeast): the Kleiner Heuberg, Rammert, Schönbuch, Glemswald, Stromberg and Heuchelberg, Schurwald and Welzheim Forest, Swabian-Franconian Forest, Franconian Heights, Steigerwald and Hassberge. The southwesternmost Keuper escarpment in the area of the Baar does not have its own name because of its small size. Natural region divisions The Keuper Uplands are divided into three natural region major unit groups which, in turn, are subdivided into major units, shown underneath in each case with three-figure index numbers (units of which only small areas lie on keuper are in italics) and ridges that are orographically separated from one another (basins and ridges on the perimeters have been omitted):Various authors: ''Geographische Landesau ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Bodelshausen
Bodelshausen is a municipality in the district of Tübingen in the German state of Baden-Württemberg. Geography Geographical Area Bodelshausen is situated southern of the Rammert forest near the town of Hechingen. Neighboring municipalities and towns Rottenburg am Neckar, Ofterdingen, Mössingen, Hechingen ¹ and Hirrlingen History The oldest historical documents date back to 1100. Politics Mayor The mayor is elected for 8 years. Mayor Bernd-Dieter Esslinger's term ended in 2006. Since 2006, Uwe Ganzenmüller holds the office. * 1982 – 2006: Bernd-Dieter Esslinger * since 2006: Uwe Ganzenmüller Sister municipalities * Soltvadkert, Hungary ''(1996)'' Bodelshausen maintains friendly relationships with: * Hohburg, Saxony * Market town Rum, Austria Sons and daughters of the town * Johannes Nill (1825–1894), Founder of private Zoo in Stuttgart * Ernst von Wittich (1835–1922), General superintendent of the city of Tübingen * Jakob Nill ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Swabian Keuper-Lias Land
The Swabian Keuper-Lias Plains (german: Schwäbisches Keuper-Lias-Land) is a major natural region in southwest Germany and includes the southwesternmost part of the Keuper Uplands, which is bordered immediately to the north by the Swabian Jura. Natural regions The Swabian Keuper lands are divided into three natural regional groups and their 3-figure major units which are given 3-figure numbers: Map of the major natural regional groups with a list of the main units (German) * 10 (=D58) Swabian Keuper-Lias Plains ** 100 Foreland of the western Swabian Jura (''Vorland der mittleren Schwäbischen Alb'') ** 101 Foreland of the central Swabian Jura (''Vorland der mittleren Schwäbischen Alb'') ** 102 Foreland of the eastern Swabian Jura (''Vorland der östlichen ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Swabian Keuper-Lias Plains
The Swabian Keuper-Lias Plains (german: Schwäbisches Keuper-Lias-Land) is a major natural region in southwest Germany and includes the southwesternmost part of the Keuper Uplands, which is bordered immediately to the north by the Swabian Jura. Natural regions The Swabian Keuper lands are divided into three natural regional groups and their 3-figure major units which are given 3-figure numbers: Map of the major natural regional groups with a list of the main units (German) * 10 (=D58) Swabian Keuper-Lias Plains ** 100 Foreland of the western Swabian Jura (''Vorland der mittleren Schwäbischen Alb'') ** 101 Foreland of the central Swabian Jura (''Vorland der mittleren Schwäbischen Alb'') ** 102 Foreland of the eastern Swabian Jura (''Vorland der östlichen ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Steinlach
The Steinlach is a river with a length of in Baden-Württemberg, Germany. It is a tributary to the Neckar. It has its source in the ''Eckenbachgraben'', a gap in the Swabian Alb mountain range. The source is on the territory of the town of Mössingen, on an elevation of above sea level. The Steinlach flows into a northerly direction. After taking up several streams outside of Mössingen, it flows through Ofterdingen, Nehren and Dußlingen to Tübingen, where it discharges into the Neckar. Geography History The Steinlach has its source east of Mössinger District Talheim and west of Ruchberges at about 710 meters above sea Level in a northeastern side valley of the ''Eckenbachgraben'', a gorge between five and ten meters deep below the Traufkante of the Swabian Alb. The source outlet of the somewhat longer left upper reaches from the Eckenbachgraben shifts with the karst water level of the Swabian Alb. The sources of both branches are just still located in the municipal ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Hirrlingen
Hirrlingen is a municipality in the district of Tübingen in Baden-Württemberg in Germany. Hirrlingen is located about 15 kilometers southwest from Tübingen Tübingen (, , Swabian: ''Dibenga'') is a traditional university city in central Baden-Württemberg, Germany. It is situated south of the state capital, Stuttgart, and developed on both sides of the Neckar and Ammer rivers. about one in thr .... References Municipalities in Baden-Württemberg Tübingen (district) {{Tübingen-geo-stub ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Katzenbach (Neckar)
Katzenbach (in its upper course: ''Beurenbach'') is a river of Baden-Württemberg, Germany. It flows into the Neckar in Bad Niedernau. See also *List of rivers of Baden-Württemberg A list of rivers of Baden-Württemberg, Germany: A * Aal * Aalbach *Aalenbach * Ablach * Ach *Acher *Adelbach *Aich *Aid * Aischbach, tributary of the Kinzig * Aischbach, tributary of the Körsch * Aitrach, tributary of the Danube * Aitrach, tri ... References Rivers of Baden-Württemberg Rivers of Germany {{BadenWürttemberg-river-stub ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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South German Scarplands
The South German Scarplands is a geological and geomorphological natural region or landscape in Switzerland and the south German states of Bavaria and Baden-Württemberg. The landscape is characterised by escarpments. It is variously referred to in the German literature as the: * ' (Southwest German Scarplands) * ' (Southwest German Scarp Landscape) * ' (Swabian-Franconian Scarpland(scape)) * ' (South German Scarpland(scape)) Location and short description The South German Scarplands run (from north(-northeast) to south(-southwest)) more or less between the southern Rhön, the Spessart, the Odenwald and the Black Forest in the west, the Franconian Jura in the east, the Swabian Jura to the southeast and the northeastern foothills of the Jura to the south. The wooded west and northwest-facing scarps drop sharply towards the Rhine Rift Valley and the Rhine-Main Plain, whilst the dip slopes fall comparatively gradually towards the (north-)east into the depressions beyond which ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Swabian Jura
The Swabian Jura (german: Schwäbische Alb , more rarely ), sometimes also named Swabian Alps in English, is a mountain range in Baden-Württemberg, Germany, extending from southwest to northeast and in width. It is named after the region of Swabia. The Swabian Jura occupies the region bounded by the Danube in the southeast and the upper Neckar in the northwest. In the southwest it rises to the higher mountains of the Black Forest. The highest mountain of the region is the Lemberg (). The area's profile resembles a high plateau, which slowly falls away to the southeast. The northwestern edge is a steep escarpment (called the Albtrauf or Albanstieg, rising up , covered with forests), while the top is flat or gently rolling. In economic and cultural terms, the Swabian Jura includes regions just around the mountain range. It is a popular recreation area. Geology The geology of the Swabian Jura is mostly limestone, which formed the seabed during the Jurassic period. The sea r ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Outlier (geology)
An inlier is an area of older rock (geology), rocks surrounded by younger rocks. Inliers are typically formed by the erosion of overlying younger rocks to reveal a limited outcrop, exposure of the older underlying rocks. Fault (geology), Faulting or fold (geology), folding may also contribute to the observed outcrop pattern. A classic example from Great Britain is that of the inlier of folded Ordovician and Silurian rocks at Horton in Ribblesdale in North Yorkshire which are surrounded by the younger flat-lying Carboniferous Limestone. The location has long been visited by geology students and experts. Another example from South Wales is the Usk Inlier in Monmouthshire where Silurian age rocks are upfolded amidst Old Red Sandstone rocks of Devonian age. A similar outcrop pattern which results from movement on a thrust fault followed by erosion may be termed a window (geology), window. Conversely an outlier is an area of younger rock surrounded by older rocks. An outlier is typical ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Black Jurassic
The Black Jurassic or Black Jura (german: Schwarzer Jura) in earth history refers to the lowest of the three lithostratigraphic units of the South German Jurassic, the latter being understood not as a geographical, but a geological term in the sense of a lithostratigraphic super group. Formerly and even occasionally today in the popular scientific literature, this term is equated to the chronostratigraphic series of the Lower Jurassic. This is however not quite correct, because the Black Jura does not exactly coincide with the chronostratigraphic boundaries of the Lower Jurassic. In addition, the term ''lias'', which was formerly frequently used (and sometimes is today) as a synonym, should no longer be used in connexion with the South German Jurassic. Instead, the term ''lias'', or ''North German Lias'', should be reserved for the roughly equivalent lithostratigraphic unit in the North German Jurassic. The deposition of the Black Jurassic took place about 199 to 175 million years a ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |