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Teufelsmauer
The Teufelsmauer (''Devil's Wall'') is a rock formation made of hard sandstones of the Upper Cretaceous in the northern part of the Harz Foreland in central Germany. This wall of rock runs from Blankenburg (Harz) via Weddersleben and Rieder to Ballenstedt. The most prominent individual rocks of the Teufelsmauer have their own names. The Teufelsmauer near Weddersleben is also called the ''Adlersklippen'' ("Eagle Crags"). Many legends and myths have been woven in order to try to explain the unusual rock formation. It was placed under protection as early as 1833 and, in 1852, by the head of the district authority in order to prevent quarrying of the much sought-after sandstone. The Teufelsmauer near Weddersleben has been protected since 1935 as a nature reserve and is thus one of the oldest nature reserves in Germany. Course The band of rock that forms the Teufelsmauer outcrops at three places between Ballenstedt in the southeast and Blankenburg (Harz) in the northwest ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Teufelsmauer Silbergrasrasen
The Teufelsmauer (''Devil's Wall'') is a rock formation made of hard sandstones of the Upper Cretaceous in the northern part of the Harz Foreland in central Germany. This wall of rock runs from Blankenburg (Harz) via Weddersleben and Rieder to Ballenstedt. The most prominent individual rocks of the Teufelsmauer have their own names. The Teufelsmauer near Weddersleben is also called the ''Adlersklippen'' ("Eagle Crags"). Many legends and myths have been woven in order to try to explain the unusual rock formation. It was placed under protection as early as 1833 and, in 1852, by the head of the district authority in order to prevent quarrying of the much sought-after sandstone. The Teufelsmauer near Weddersleben has been protected since 1935 as a nature reserve and is thus one of the oldest nature reserves in Germany. Course The band of rock that forms the Teufelsmauer outcrops at three places between Ballenstedt in the southeast and Blankenburg (Harz) in the northwest, ov ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Teufelsmauer Bei Blankenburg 2
The Teufelsmauer (''Devil's Wall'') is a rock formation made of hard sandstones of the Upper Cretaceous in the northern part of the Harz Foreland in central Germany. This wall of rock runs from Blankenburg (Harz) via Weddersleben and Rieder to Ballenstedt. The most prominent individual rocks of the Teufelsmauer have their own names. The Teufelsmauer near Weddersleben is also called the ''Adlersklippen'' ("Eagle Crags"). Many legends and myths have been woven in order to try to explain the unusual rock formation. It was placed under protection as early as 1833 and, in 1852, by the head of the district authority in order to prevent quarrying of the much sought-after sandstone. The Teufelsmauer near Weddersleben has been protected since 1935 as a nature reserve and is thus one of the oldest nature reserves in Germany. Course The band of rock that forms the Teufelsmauer outcrops at three places between Ballenstedt in the southeast and Blankenburg (Harz) in the northwest, ov ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Blankenburg (Harz)
Blankenburg (Harz) is a town and health resort in the district of Harz, in Saxony-Anhalt, Germany, at the north foot of the Harz Mountains, southwest of Halberstadt. It has been in large part rebuilt since a fire in 1836, and possesses a castle, with various collections, a museum of antiquities, an old town hall and churches. There are pine-needle baths and a psychiatric hospital. Gardening is a speciality. The nearby ridge of rocks called the ''Teufelsmauer'' (Devils Wall) offers views across the plain and into the deep gorges of the Harz. Geography The town of Blankenburg (Harz) lies on the northern edge of the Harz mountains at a height of about 234 metres. It is located west of Quedlinburg, south of Halberstadt and east of Wernigerode. The stream known as the Goldbach flows through the district of Oesig northwest of the town centre. Divisions The town Blankenburg (Harz) consists of Blankenburg proper and the following ''Ortschaften'' or municipal divisions: [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hamburger Wappen
The Hamburger Wappen (" Hamburg coat of arms") is a highly unusual rock feature on the Teufelsmauer ("Devil's Wall") rock formation not far from Timmenrode in the Harz Mountains in central Germany. The appearance of this sandstone formation, with its three steep, soaring pinnacles of rock, recalls the coat of arms of the Hanseatic city of Hamburg (male), (female) en, Hamburger(s), Hamburgian(s) , timezone1 = Central (CET) , utc_offset1 = +1 , timezone1_DST = Central (CEST) , utc_offset1_DST = +2 , postal ... with its three towers. Next to it is a rock cave known as the ''Kuhstall'' ("Cow shed"). Not far from the ''Hamburger Wappen'' is control point no. 74 on the Harzer Wandernadel hiking network. Rock formations of the Harz Rock formations of Saxony-Anhalt {{SaxonyAnhalt-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Northern Harz Boundary Fault
The Northern Harz Boundary Fault (german: Harznordrandstörung or ''Harznordrandverwerfung'') is a geological fault where the Harz Block, which consists of rocks formed during the Palaeozoic Era and folded in the course of Hercynian mountain building, borders on the Subhercynian Basin or Harz Foreland. The fault is also known in English as the Harz North Rim Fault or Harznordrand Thrust (Fault).Nielsen, Ole (2008). ''Salt tectonics'' amy.opera,com Accessed on 28 Nov 2010. The northern edge of the Harz is oriented in a Hercynian (WNW-ESE) direction and runs from Neuekrug-Hahausen via Langelsheim, Goslar, Bad Harzburg, Ilsenburg, Wernigerode, Blankenburg, Thale and Gernrode to the area of Ballenstedt. The Northern Harz Boundary Fault forms the southern border of the Northeast German Basin, a part of the Central European Basin. The Subhercynian Basin, also known as the Harz Foreland, is a small sub-basin of the Northeast German Basin. This intracontinental basin that has been subs ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gegensteine
The Gegensteine are crags near the town of Ballenstedt on the northern edge of the Harz Mountains in Germany. There are two: the Großer Gegenstein and Kleiner Gegenstein ("Great Gegenstein" and "Little Gegenstein"). They are striking, free-standing rock pinnacles and outliers of the Teufelsmauer. They lie within the ''Gegensteine–Schierberg'' nature reserve. The Großer Gegenstein () can be ascended by means of ladders and steps carved out of the rock. A cross was erected on its summit in 1863 by order of the Prince of Anhalt; it was replaced in 1993. From the summit there are extensive views over the Harz Mountains and its northern foreland. Near the Kleiner Gegenstein () there used to be a site used for driver training purposes by the ''Gesellschaft für Sport und Technik The Gesellschaft für Sport und Technik (GST), lit. “Sport and Technology Association”, was one of the East German “Mass Organizations”. Officially, it was established to structure the free ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Harz Foreland
The Harz () is a highland area in northern Germany. It has the highest elevations for that region, and its rugged terrain extends across parts of Lower Saxony, Saxony-Anhalt, and Thuringia. The name ''Harz'' derives from the Middle High German word ''Hardt'' or ''Hart'' (hill forest). The name ''Hercynia'' derives from a Celtic name and could refer to other mountain forests, but has also been applied to the geology of the Harz. The Brocken is the highest summit in the Harz with an elevation of above sea level. The Wurmberg () is the highest peak located entirely within the state of Lower Saxony. Geography Location and extent The Harz has a length of , stretching from the town of Seesen in the northwest to Eisleben in the east, and a width of . It occupies an area of , and is divided into the Upper Harz (''Oberharz'') in the northwest, which is up to 800 m high, apart from the 1,100 m high Brocken massif, and the Lower Harz (''Unterharz'') in the east which is up to aroun ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Weddersleben
Weddersleben is a village and a former municipality in the district of Harz, Saxony-Anhalt, in the Harz area. Since 1 January 2009, it is part of the town Thale. The village is well known for being located adjacent to the famed natural rock formation known as the Teufelsmauer The Teufelsmauer (''Devil's Wall'') is a rock formation made of hard sandstones of the Upper Cretaceous in the northern part of the Harz Foreland in central Germany. This wall of rock runs from Blankenburg (Harz) via Weddersleben and Rieder ..., or "Devil's Wall" in English. Surrounding forest area has numerous paths for biking and hiking, making it a popular tourist destination for nature seekers. Among the many natural formations in the area, the Bode River flows by the edges of the village. Former municipalities in Saxony-Anhalt Thale {{Harz-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ballenstedt
Ballenstedt is a town in the Harz district, in the German state of Saxony-Anhalt. Geography It is situated at the northern rim of the Harz mountain range, about 10 km (6 mi) southeast of Quedlinburg. The municipal area comprises the villages of Asmusstedt, Badeborn, Opperode, Radisleben, and Rieder. Ballenstedt is a stop on the scenic Romanesque Road. History The Saxon count Esico of Ballenstedt (c. 1000–1059/60) was mentioned in a 1030 entry in the medieval chronicles of the Annalista Saxo and in a 1036 deed issued by Emperor Conrad II. He was a son of one Count Adalbert, who held the office of a ''Vogt'' of Nienburg Abbey, and Hidda, a daughter of Margrave Odo I of the Saxon Ostmark. Esico, whose sister Uta married Margrave Eckard II of Meissen is considered the progenitor of the House of Ascania. He had a collegiate church erected in Ballenstedt, dedicated to Saints Pancras and Abundius, in the presence of Emperor Henry III in 1046. Ballenstedt church was men ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Neocomian
In geology, Neocomian was a name given to the lowest stage of the Cretaceous system. It is generally considered to encompass the interval now covered by the Berriasian, Valanginian and Hauterivian, from approximately 145 to 130 Ma. It was introduced by Jules Thurmann in 1835 on account of the development of these rocks at Neuchâtel (Neocomum), Switzerland. It has been employed in more than one sense. In the type area the rocks have been divided into two sub-stages, a lower, Valanginian (from Valengin, Pierre Jean Édouard Desor, 1854) and an upper, Hauterivian (from Hauterive, Eugène Renevier, 1874); there is also another local sub-stage, the infra-Valanginian or Berriasian (from Berrias, Henri Coquand, 1876). These three sub-stages constitute the Neocomian in its restricted sense. Adolf von Koenen and other German geologists extend the use of the term to include the whole of the Lower Cretaceous up to the top of the Gault or Albian. Eugène Renevier Eugène Renevier (26 March ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Erosion
Erosion is the action of surface processes (such as water flow or wind) that removes soil, rock, or dissolved material from one location on the Earth's crust, and then transports it to another location where it is 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 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 waves; glacial plucking, abrasion, and scour; areal flooding; wind abrasion; groundwater processes; and mass movement processes in steep landscapes like landslides and debris flows. The rates at which such processes act control how fast a surface is eroded. Typically, physical erosion procee ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Muschelkalk
The Muschelkalk (German for "shell-bearing limestone"; french: calcaire coquillier) is a sequence of sedimentary rock strata (a 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 tripartite Germanic Trias, that give 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 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 stratigraphic unit. 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. The name indicates a characteristic feature of the unit, namely the frequent occurrence of lenticular banks composed o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
