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Odenwald
The Odenwald () is a low mountain range in the German states of Hesse, Bavaria and Baden-Württemberg. Location The Odenwald is located between the Upper Rhine Plain with the Bergstraße and the ''Hessisches Ried'' (the northeastern section of the Rhine rift) to the west, the Main and the Bauland (a mostly unwooded area with good soils) to the east, the Hanau-Seligenstadt Basin – a subbasin of the Upper Rhine Rift Valley in the Rhine-Main Lowlands – to the north and the Kraichgau to the south. The part south of the Neckar valley is sometimes called the ''Kleiner Odenwald'' ("Little Odenwald"). The northern and western Odenwald belong to southern Hesse, with the south stretching into Baden. In the northeast, a small part lies in Lower Franconia in Bavaria. Geology The Odenwald, along with other parts of the Central German Uplands, belongs to the Variscan, which more than 300 million years ago in the Carboniferous period ran through great parts of Europe. The cause ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kleiner Odenwald
The Kleiner Odenwald (“Little Odenwald”) is the southern part of the central German hill range, the Odenwald, and is up to .{{GeoQuelle, DE, BFN-Karten It is also part of the natural region of Sandstein-Odenwald in the north of the state of Baden-Württemberg. Lying east-southeast of Heidelberg and south of the River Neckar, which separates the Kleiner Odenwald from the rest of the Odenwald, its landscape is shaped by the underlying sandstone that also dominates the northern Odenwald. Geography Location The Kleiner Odenwald lies in the counties of Rhein-Neckar and Neckar-Odenwald and on the territory of the city of Heidelberg. It is bounded in the north by the Neckar and the settlements of Neckargemünd and Eberbach, in the east by the Neckar and e.g. by Obrigheim, in the south by Reichartshausen, Waibstadt and Eschelbronn and in the west by Wiesloch, Leimen and Heidelberg on the River Neckar. Municipalities in the area are: Lobbach, Bammental, Gaiberg, Wiesen ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Neckar
The Neckar () is a river in Germany, mainly flowing through the southwestern state of Baden-Württemberg, with a short section through Hesse. The Neckar is a major right tributary of the Rhine. Rising in the Schwarzwald-Baar-Kreis near Schwenningen in the ''Schwenninger Moos'' conservation area at a height of above sea level, it passes through Rottweil, Rottenburg am Neckar, Kilchberg, Tübingen, Wernau, Nürtingen, Plochingen, Esslingen, Stuttgart, Ludwigsburg, Marbach, Heilbronn and Heidelberg, before discharging on average of water into the Rhine at Mannheim, at above sea level, making the Neckar its 4th largest tributary, and the 10th largest river in Germany. Since 1968, the Neckar has been navigable for cargo ships via 27 locks for about upstream from Mannheim to the river port of Plochingen, at the confluence with the Fils. From Plochingen to Stuttgart, the Neckar valley is densely populated and heavily industrialised, with several well-known companies. Between ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bauland
The Bauland is a Gäu landscape in the northeast of the German state of Baden-Württemberg. It is a natural region within the Neckar and Tauber Gäu Plateaus (major unit 12) in the South German Scarplands. Location The Bauland is a Gäu landscape in the northeast of the German state of Baden-Württemberg. It is a natural region within the Neckar and Tauber Gäu Plateaus (major unit 12) in the South German Scarplands. It lies between the Odenwald forest and the Tauber, Jagst and Neckar rivers within the counties of Main-Tauber-Kreis and Neckar-Odenwald-Kreis. It also reaches into Hohenlohekreis and the county of Heilbronn. The Bauland is no. 128 in the classification system of the '' Handbook of Natural Region Divisions of Germany''. Etymology The name ''Bauland'' goes back to the word ''Ponland'' which meant a "strip of land in which beans are cultivated" (from the Middle High German ''pône''). The Bauland is colloquially known as Baden Siberia (''Badisch Sibirien' ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hesse
Hesse (, , ) or Hessia (, ; german: Hessen ), officially the State of Hessen (german: links=no, Land Hessen), is a States of Germany, state in Germany. Its capital city is Wiesbaden, and the largest urban area is Frankfurt. Two other major historic cities are Darmstadt and Kassel. With an area of 21,114.73 square kilometers and a population of just over six million, it ranks seventh and fifth, respectively, among the sixteen German states. Frankfurt Rhine-Main, Germany's second-largest metropolitan area (after Rhine-Ruhr), is mainly located in Hesse. As a cultural region, Hesse also includes the area known as Rhenish Hesse (Rheinhessen) in the neighbouring state of Rhineland-Palatinate. Name The German name '':wikt:Hessen#German, Hessen'', like the names of other German regions (''Schwaben'' "Swabia", ''Franken'' "Franconia", ''Bayern'' "Bavaria", ''Sachsen'' "Saxony"), derives from the dative plural form of the name of the inhabitants or German tribes, eponymous tribe, the Hes ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Baden-Württemberg
Baden-Württemberg (; ), commonly shortened to BW or BaWü, is a German state () in Southwest Germany, east of the Rhine, which forms the southern part of Germany's western border with France. With more than 11.07 million inhabitants across a total area of nearly , it is the third-largest German state by both area (behind Bavaria and Lower Saxony) and population (behind North Rhine-Westphalia and Bavaria). As a federated state, Baden-Württemberg is a partly-sovereign parliamentary republic. The largest city in Baden-Württemberg is the state capital of Stuttgart, followed by Mannheim and Karlsruhe. Other major cities are Freiburg im Breisgau, Heidelberg, Heilbronn, Pforzheim, Reutlingen, Tübingen, and Ulm. What is now Baden-Württemberg was formerly the historical territories of Baden, Prussian Hohenzollern, and Württemberg. Baden-Württemberg became a state of West Germany in April 1952 by the merger of Württemberg-Baden, South Baden, and Württemberg-Hohenzollern. The ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Katzenbuckel
The Katzenbuckel (626 metres) is an extinct volcano and the highest elevation in the Odenwald region of southeast Germany. The mountain is located eastwards of Eberbach, near the village of Waldbrunn. At the top of the Katzenbuckel is an 18-m-high lookout, built out of sandstone. If the weather is good, it is possible to see the Donnersberg (83 km away) and the surrounding secondary mountains (Taunus). When the view is exceptionally clear, it is theoretically possible to see the Kreuzberg (120 km away) in the Rhön. It translates directly into 'cat hump'. Volcanoes of Germany Mountains and hills of Baden-Württemberg {{BadenWurttemberg-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Felsenmeer Odenwald Herbst
A blockfieldWhittow, John (1984). ''Dictionary of Physical Geography''. London: Penguin, 1984, pp. 66 and 190. . (also spelt block fieldLeser, Hartmut, ed. (2005). ''Wörterbuch Allgemeine Geographie'', 13th ed., dtv, Munich, pp. 107 and 221. . ), felsenmeer, boulder field or stone field is a surface covered by boulder- or block-sized angular rocks usually associated with alpine and subpolar climates and periglaciation. Blockfields differ from screes and talus slope in that blockfields do not apparently originate from mass wastings. They are believed to be formed by frost weathering below the surface. An alternative theory that modern blockfields may have originated from chemical weathering that occurred in the Neogene when the climate was relatively warmer. Following this thought the blockfields would then have been reworked by periglacial action. Most known blockfields are located in the northern hemisphere. Examples can be found in Abisko National Park in Sweden, Snowd ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 colli ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bergstraße Route
Bergstraße or Bergstrasse can refer to: *Bergstraße Route, literally "Mountain Road", in the Odenwald of Baden-Württemberg and Hesse, Germany *Bergstraße (district), a district in Hesse, Germany *Hessische Bergstraße The Hessische Bergstraße ("Hessian Mountain Road") is a defined region (''Anbaugebiet'') for wine in Germany located in the state of Hesse among the northern and western slopes of the Odenwald mountain chain. With only of vineyards it is the ..., a Hessian winegrowing region * Badische Bergstraße, a winegrowing region in Baden-Württemberg, Germany {{disambig, geo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hanau-Seligenstadt Basin
The Hanau-Seligenstadt Basin is a subbasin of the Upper Rhine Graben southeast of Frankfurt am Main (Hesse, Bavaria, Germany). Location The Hanau-Seligenstadt Basin is located in the eastern part of the Lower Main lowlands. The river Main (river), Main crosses the basin between Aschaffenburg and Offenbach am Main. The largest cities of the area are Hanau, Seligenstadt and Dieburg. Geologic setting The Hanau-Seligenstadt Basin is a Cenozoic graben. As a subbasin of the Upper Rhine Graben it belongs to the European Cenozoic Rift System, a fracture zone crossing Europe from the North Sea to the Mediterranean. The Hanau-Seligenstadt Basin is separated from the Upper Rhine Graben to the west by a Horst (geology), horst block. The Spessart mountains form its eastern margin. To the south it is bounded by the Odenwald mountains. Towards the north the graben margins converge. The basin sediments rest on top of the Variscan Orogeny, Variscan basement and Permian to Triassic rocks. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kraichgau
The Kraichgau () is a hilly region in Baden-Württemberg, southwestern Germany. It is bordered by the Odenwald and the Neckar to the North, the Black Forest to the South, and the Upper Rhine Plain to the West. To the east, its boundary is considered to be the Stromberg and the Heuchelberg. The largest towns of the Kraichgau are Sinsheim, Eppingen, and Bretten. On the western end of the Kraichgau is the town of Bruchsal, the gateway to the Rhineland plains. Origins of the name The word "Kraich" apparently arose from the Celtic word "Creuch," meaning "mud" or "loam." The territory of a Gau (country subdivision) signifies an open area, free from woods, such as farmland or meadows. The area of Kraichgau was first mentioned in the Early Middle Ages, in the Lorsch codex, as "Creichgowe" in the year 769. In 773, it was called "Chrehgauui," in 778 "Craichgoia." By 1594, the name was closer to its modern form, being referred to as "Kreuchgau." See also *Aalkistensee Aalk ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Triassic
The Triassic ( ) is a geologic period and system which spans 50.6 million years from the end of the Permian Period 251.902 million years ago ( Mya), to the beginning of the Jurassic Period 201.36 Mya. The Triassic is the first and shortest period of the Mesozoic Era. Both the start and end of the period are marked by major extinction events. The Triassic Period is subdivided into three epochs: Early Triassic, Middle Triassic and Late Triassic. The Triassic began in the wake of the Permian–Triassic extinction event, which left the Earth's biosphere impoverished; it was well into the middle of the Triassic before life recovered its former diversity. Three categories of organisms can be distinguished in the Triassic record: survivors from the extinction event, new groups that flourished briefly, and other new groups that went on to dominate the Mesozoic Era. Reptiles, especially archosaurs, were the chief terrestrial vertebrates during this time. A specialized subgroup of archo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
