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Albtrauf
The term Albtrauf (Alp escarpment) refers to the northwest facing escarpment of the Swabian Alps, situated in Baden-Württemberg and Bavaria. It is the most distinctive stepped slope within the alpine region of the South German Scarplands, leading roughly from the southwest to the northeast. The Albtrauf has its geological extension in the northeast, in the stepped slopes of the Franconian Jura and in the southwest and west among the Jurassic-era stepped slopes of the Baaralb, Hegaualb, Randen, Klettgau, Aargau as well as the Table Jura stretches from the city of Basel to the Ajoie and the French Scarplands. In geology and geomorphology, however, the term “Trauf” merely describes the brink of the stepped slopes where various stepped surfaces meet (which is not developed in hipped steps). Geography Like the entirety of the Swabian Alps, the Albtrauf leads from the southwest to the northeast, approximately following the line of Donaueschingen–Lemberg–Balingen– ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Drackensteiner Hang
The Drackensteiner Hang is a mountainside in the Swabian Alps at Kirchheim unter Teck in Baden-Württemberg, Germany. Bundesautobahn 8 between Stuttgart and Ulm divides into separate northbound and southbound routes on either side of the peak. The two halves of the autobahn each traverse one tunnel and a series of two or three viaducts that were designed by Paul Bonatz and built for the Reichsautobahn; the bridges were all destroyed in World War II and had to be rebuilt, and the route in one direction was only completed in the 1950s. A project to reroute the autobahn with new tunnels and bridges has been postponed indefinitely. Route The entire segment is long. The separated sections, which are some apart at the furthest and over which the autobahn rises or descends , lie between Mühlhausen im Täle and Hohenstadt, where there is an emergency access road. North of Mühlhausen, traffic southbound from Aichelberg, where the first viaduct is located, climbs up the north-west- ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hohenzollern Castle
Hohenzollern Castle (german: Burg Hohenzollern ) is the ancestral seat of the imperial House of Hohenzollern. The third of three hilltop castles built on the site, it is located atop Mount Hohenzollern, above and south of Hechingen, on the edge of the Swabian Jura of central Baden-Württemberg, Germany. The first castle on the mountain was constructed in the early 11th century. Over the years the House of Hohenzollern split several times, but the castle remained in the Swabian branch, the dynastic seniors of the Franconian-Brandenburgian cadet branch that later acquired its own imperial throne. This castle was completely destroyed in 1423 after a ten-month siege by the free imperial cities of Swabia. The second castle, a larger and sturdier structure, was constructed from 1454 to 1461, which served as a refuge for the Catholic Swabian Hohenzollerns, including during the Thirty Years' War. By the end of the 18th century it was thought to have lost its strategic importance a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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] |
Kirchheim Unter Teck
Kirchheim unter Teck ( Swabian: ''Kircha'') is a town in Baden-Württemberg, Germany, in the district of Esslingen. It is located on the small river Lauter, a tributary of the Neckar. It is 10 km (6 miles) near the Teck castle, approximately southeast of Stuttgart. It is the fourth city in the Esslingen district, forming a district centre for the surrounding communities. Since 1 April 1956, Kirchheim unter Teck has the status of Große Kreisstadt. The city forms a ''Verwaltungsgemeinschaft'' (administrative community) with the neighbouring municipalities Dettingen and Notzingen. Kirchheim unter Teck was also, for several centuries, seat of the Oberamt (Oa.) Kirchheim. Geography Kirchheim unter Teck is located in the foothills of the central Swabian ''Alb'', north of the Albtrauf escarpment and its foothills: the Teckberg, Breitenstein and Limburg. It is situated in the Lauter valley, at the confluence of the Lindach and several tributary streams with the Lauter. T ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Balingen
Balingen (; Swabian: ''Balenga'') is a town in Baden-Württemberg, Germany, capital of the district of Zollernalbkreis. It is located near the Swabian Jura, approx. 35 km to the south of Tübingen, 35 km northeast of Villingen-Schwenningen, and 70 km south southwest of Stuttgart. It is home to the Bizerba and Ideal companies. History Balingen is first mentioned in 863. Initially a possession of the lords of Haigerloch, in 1162 it was acquired by the count of Hohenberg. In the 13th century it received the title of city from Friedrich der Erlauchte, it was largely rebuilt on the left bank of the river Eyach. In 1403 it was sold to the County of Württemberg, whose chancellor maintained a residence there until the 18th century. Balingen became part of the unified Germany in 1870. Main sights The city was destroyed by a fire in 1809, from which only the Protestant church, the castle and a few other edifices escaped. The Protestant church's construction finished ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geology
Geology () is a branch of natural science concerned with Earth and other astronomical objects, the features or rocks of which it is composed, and the processes by which they change over time. Modern geology significantly overlaps all other Earth sciences, including hydrology, and so is treated as one major aspect of integrated Earth system science and planetary science. Geology describes the structure of the Earth on and beneath its surface, and the processes that have shaped that structure. It also provides tools to determine the relative and absolute ages of rocks found in a given location, and also to describe the histories of those rocks. By combining these tools, geologists are able to chronicle the geological history of the Earth as a whole, and also to demonstrate the age of the Earth. Geology provides the primary evidence for plate tectonics, the evolutionary history of life, and the Earth's past climates. Geologists broadly study the properties and processes of E ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Teck Castle
Teck Castle (german: Burg Teck) was a ducal castle in the kingdom of Württemberg, immediately to the north of the Swabian Jura and south of the town of Kirchheim unter Teck (now in the district of Esslingen). The castle took its name from the Teckberg ridge, 2,544 feet high, which it crowned. It was destroyed in the German Peasants' War (1525). The site's current buildings were constructed during the 19th and 20th centuries on the ruins of the original castle. Buildings In 1889, an observation tower (called the ''Teckturm'') with a refuge shelter was built and inaugurated on 1 September 1889. A hall was built in 1933 near the tower, called Mörike Hall (''Mörikehalle''). Since 6 June 1941, the buildings have been owned by the Schwäbischer Albverein. From 1954 to 1955, the ''Mörikehalle'' became a restaurant with sleeping rooms. On 9 November 1999, the area surrounding the site was designated a protected area (''Naturschutzgebiet''). Teck family In 1863, the title "Prince o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hohenneuffen Castle
Hohenneuffen Castle is a large ruined castle in the northern foothills of the Swabian Alb, above the town of Neuffen in the district of Esslingen in Baden-Württemberg. Location The medieval castle is situated on a large late Jurassic rock on the edge of the Swabian Alb at an elevation of 743 m (2437 ft) in a strategically advantageous location on the slopes of the mountain range. History There is evidence for a pre-historic, Iron Age settlement on Hohenneuffen. It functioned as an outpost for the oppidum at '' Heidengraben'' during the late La Tène period in the first century BCE. The pre-Germanic name ''Neuffen'' is derived from the proto-Celtic adjective ', meaning holy or sacred, implying that the mountain had a religious rather than a military function 2000 years ago. The castle was built between 1100 and 1120 by Mangold von Sulmetingen who later changed his name to include the element ''von Neuffen''. The first documentary evidence dates from 1198. At ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Inliers And Outliers (geology)
An inlier is an area of older rocks surrounded by younger rocks. Inliers are typically formed by the erosion of overlying younger rocks to reveal a limited exposure of the older underlying rocks. Faulting or 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. Conversely an outlier is an area of younger rock surrounded by older rocks. An outlier is typically formed when sufficient erosion of surrounding rocks has taken place to s ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Eroded
Erosion is the action of surface processes (such as Surface runoff, water flow or wind) that removes soil, Rock (geology), rock, or dissolved material from one location on the Earth's crust#Crust, Earth's crust, and then sediment transport, transports it to another location where it is deposit (geology), deposited. Erosion is distinct from weathering which involves no movement. Removal of rock or soil as clastic sediment is referred to as ''physical'' or ''mechanical'' erosion; this contrasts with ''chemical'' erosion, where soil or rock material is removed from an area by Solvation, dissolution. Eroded sediment or solutes may be transported just a few millimetres, or for thousands of kilometres. Agents of erosion include rainfall; bedrock wear in rivers; coastal erosion by the sea and Wind wave, waves; glacier, glacial Plucking (glaciation), plucking, Abrasion (geology), abrasion, and scour; areal flooding; Aeolian processes, wind abrasion; groundwater processes; and Mass wasti ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gingen An Der Fils
Gingen an der Fils is a municipality in the district of Göppingen in Baden-Württemberg, Germany. Geography The municipality (''Gemeinde'') of Gingen an der Fils is found in the district of Göppingen, in Baden-Württemberg, one of the 16 States of the Federal Republic of Germany. Gingen is physically located in the valley of the Fils, up to the hills of the , in the of the Swabian Jura. Elevation above sea level in the municipal area ranges from a high of Normalnull (NN) to a low of NN. Gingen an der Fils includes the hamlet of Grünenberg as well as the ghost town Marrbach. Geological demographics Source: History Some time between 1382 and 1396, Gingen was sold by the County of Helfenstein to the Free Imperial City of Ulm, whose bailiff resided in the town until 1750. Gingen became a possession of the Electorate of Bavaria in 1802, but was ceded in 1810 to the Kingdom of Württemberg. Gingen was assigned to . In 1845, the town was connected to the growing network ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Reutlingen
Reutlingen (; Swabian: ''Reitlenga'') is a city in Baden-Württemberg, Germany. It is the capital of the eponymous district of Reutlingen. As of June 2018, it has a population of 115,818. Reutlingen has a university of applied sciences, which was founded in 1855, originally as a weavers' school. Today, Reutlingen is home to an established textile industry and also houses machinery, leather goods and steel manufacturing facilities. It has the narrowest street in the world, Spreuerhofstraße (width 31 cm). Geography Reutlingen is located about south of the State capital of Baden-Württemberg, Stuttgart. It lies in the Southwest corner of Germany, right next to the Swabian Jura, and that is why it is often called ''The gateway to the Swabian Jura'' (german: link=no, Das Tor zur Schwäbischen Alb). The Echaz river, a tributary of the Neckar, flows through the city centre. Along with the old university town of Tübingen (about to the west), Reutlingen is the centre of th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
