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Süntel Railway
The is a massif in the German Central Uplands that is up to . It forms part of the Weser Uplands in Lower Saxony southwest of Hanover and north of Hamelin. Geographical location The Süntel is the eastern extension of the Wesergebirge and runs for about 12 km from northwest to southeast. It is surrounded by the valleys of the Aue, Deister-Süntel and Weser. It is also part of the Weser Uplands Schaumburg-Hamelin Nature Park and the Calenberg Uplands. The Hohenstein hill and its immediate vicinity are a nature reserve. Geology General The southeastern part of the Süntel, including the ''Hohe Egge'', consists mainly of Wealden sandstone from the Lower Cretaceous period as well as small anthracite deposits. Its northwestern part, including the Hohenstein with its 350 m long and 50 to 60 m high crags, comprises limestone of the Upper Jurassic period, the Corallian oolith. Features The main geological features of the Süntel are: * The giant hill caves near ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hohe Egge (Süntel)
The Hohe Egge, at a good ,The survey point that shows 437.5 does not represent the actual summit; according to TK 25 the latter is over ! is the highest point on the Süntel ridge in the Calenberg Uplands in the German federal state of Lower Saxony. On its summit is the Süntel Tower. The Hohe Egge or Süntel, with its topographic prominence of 300 metres, is one of the most prominent hills and ridges in North Germany. References [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Weald
The Weald () is an area of South East England between the parallel chalk escarpments of the North and the South Downs. It crosses the counties of Hampshire, Surrey, West Sussex, East Sussex, and Kent. It has three parts, the sandstone "High Weald" in the centre, the clay "Low Weald" periphery and the Greensand Ridge, which stretches around the north and west of the Weald and includes its highest points. The Weald once was covered with forest and its name, Old English in origin, signifies "woodland". The term is still used, as scattered farms and villages sometimes refer to the Weald in their names. Etymology The name "Weald" is derived from the Old English ', meaning "forest" (cognate of German ''Wald'', but unrelated to English "wood"). This comes from a Germanic root of the same meaning, and ultimately from Indo-European. ''Weald'' is specifically a West Saxon form; '' wold'' is the Anglian form of the word. The Middle English form of the word is ''wēld'', and the mode ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Saxon
The Saxons, sometimes called the Old Saxons or Continental Saxons, were a Germanic people of early medieval "Old" Saxony () which became a Carolingian " stem duchy" in 804, in what is now northern Germany. Many of their neighbours were, like them, speakers of West Germanic dialects, including the inland Franks and Thuringians to the south, and the coastal Frisians and Angles to the north who were among the peoples who were originally referred to as "Saxons" in the context of early raiding and settlements in Roman Britain and Gaul. To their east were Obotrites and other Slavic-speaking peoples. The political history of these continental Saxons is unclear until the 8th century and the conflict between their semi-legendary hero Widukind and the Frankish emperor Charlemagne. They do not appear to have been politically united until the generations leading up to that conflict, and before then they were reportedly ruled by regional "satraps". Previous Frankish rulers of Austrasia, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Plateau
In geology and physical geography, a plateau (; ; : plateaus or plateaux), also called a high plain or a tableland, is an area of a highland consisting of flat terrain that is raised sharply above the surrounding area on at least one side. Often one or more sides have deep hills or escarpments. Plateaus can be formed by a number of processes, including upwelling of volcanic magma, extrusion of lava, and erosion by water and glaciers. Plateaus are classified according to their surrounding environment as intermontane, piedmont, or continental. A few plateaus may have a small flat top while others have wider ones. Formation Plateaus can be formed by a number of processes, including upwelling of volcanic magma, extrusion of lava, plate tectonics movements, and erosion by water and glaciers. Volcanic Volcanic plateaus are produced by volcanic activity. They may be formed by upwelling of volcanic magma or extrusion of lava. The underlining mechanism in forming p ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hessisch Oldendorf
Hessisch Oldendorf () is a town in the Hamelin-Pyrmont district, in Lower Saxony, Germany. It is situated on the river Weser, approximately northwest of Hamelin. The adjective "Hessisch" () has been used since 1905 to distinguish it from other towns named Oldendorf. Hessisch Oldendorf was part of Landgraviate of Hessen-Kassel from 1640 until 1932. Personalities * Heinrich Beerbom (1892–1980), mayor, city manager and honorary citizen of Bramsche * Wilhelm Beisner (1911–?), German SD and SS- Guide and arms dealer, agent * Otto Deppmeyer (born 1947), politician ( CDU), Member of Landtag * Richard Krentzlin (1864–1956), died in Hessisch Oldendorf, piano teacher and composer * Heinrich Krone (1895–1989), politician ( Centre Party, CDU) Member of the Reichstag, Member of the Bundestag * Ilske Laginges (–1558), the first victim of the Witch-hunt processNiedersächsisches Jahrbuch für Landesgeschichte, Band 45, Hildesheim 1973, S. 149–151. * Konrad Schlüsselburg (1 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Waterfall
A waterfall is any point in a river or stream where water flows over a vertical drop or a series of steep drops. Waterfalls also occur where meltwater drops over the edge of a tabular iceberg or ice shelf. Waterfalls can be formed in several ways, but the most common method of formation is that a river courses over a top layer of resistant bedrock before falling onto softer rock, which erodes faster, leading to an increasingly high fall. Waterfalls have been studied for their impact on species living in and around them. Humans have had a distinct relationship with waterfalls since prehistory, travelling to see them, exploring and naming them. They can present formidable barriers to navigation along rivers. Waterfalls are religious sites in many cultures. Since the 18th century, they have received increased attention as tourist destinations, sources of hydropower, andparticularly since the mid-20th centuryas subjects of research. Definition and terminology A waterfal ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dripstone Cave
Dripstone may refer to: *Hood mould or dripstone, an architectural feature for handling rain water * Dripstone, a type of speleothem (cave formation) that includes for example stalactites * Dripstone, a type of water filter A water filter removes impurities by lowering contamination of water using a fine physical barrier, a chemical process, or a biological process. Filters cleanse water to different extents, for purposes such as: providing agricultural irrigation, ... made of porous stone * Dripstone, New South Wales {{disambig ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sedimentary Rock
Sedimentary rocks are types of rock (geology), rock formed by the cementation (geology), cementation of sediments—i.e. particles made of minerals (geological detritus) or organic matter (biological detritus)—that have been accumulated or deposited at Earth's surface. Sedimentation is any process that causes these particles to settle in place. Geological detritus originates from weathering and erosion of existing rocks, or from the solidification of molten lava blobs erupted by volcanoes. The geological detritus is transported to the place of deposition by water, wind, ice or Mass wasting, mass movement, which are called agents of denudation. Biological detritus is formed by bodies and parts (mainly shells) of dead aquatic organisms, as well as their fecal mass, suspended in water and slowly piling up on the floor of water bodies (marine snow). Sedimentation may also occur when dissolved minerals precipitate from aqueous solution, water solution. The sedimentary rock cover of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Jurassic
The Jurassic ( ) is a Geological period, geologic period and System (stratigraphy), stratigraphic system that spanned from the end of the Triassic Period million years ago (Mya) to the beginning of the Cretaceous Period, approximately 143.1 Mya. The Jurassic constitutes the second and middle period of the Mesozoic, Mesozoic Era as well as the eighth period of the Phanerozoic, Phanerozoic Eon and is named after the Jura Mountains, where limestone strata from the period were first identified. The start of the Jurassic was marked by the major Triassic–Jurassic extinction event, associated with the eruption of the Central Atlantic magmatic province, Central Atlantic Magmatic Province (CAMP). The beginning of the Toarcian Age started around 183 million years ago and is marked by the Toarcian Oceanic Anoxic Event, a global episode of Anoxic event, oceanic anoxia, ocean acidification, and elevated global temperatures associated with extinctions, likely caused by the eruption of the Kar ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Limestone
Limestone is a type of carbonate rock, carbonate sedimentary rock which is the main source of the material Lime (material), lime. It is composed mostly of the minerals calcite and aragonite, which are different Polymorphism (materials science), crystal forms of calcium carbonate . Limestone forms when these minerals Precipitation (chemistry), precipitate out of water containing dissolved calcium. This can take place through both biological and nonbiological processes, though biological processes, such as the accumulation of corals and shells in the sea, have likely been more important for the last 540 million years. Limestone often contains fossils which provide scientists with information on ancient environments and on the evolution of life. About 20% to 25% of sedimentary rock is carbonate rock, and most of this is limestone. The remaining carbonate rock is mostly Dolomite (rock), dolomite, a closely related rock, which contains a high percentage of the mineral Dolomite (mine ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
