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Süntel
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 nea ... [...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 In topography, prominence (also referred to as autonomous height, relative height, and shoulder drop in US English, and drop or relative height in British English) measures the height of a mountain or hill's summit relative to the lowest contou ... of 300 metres, is one of the most prominent hills and ridges in North Germany. References Hills of Lower Saxony Hameln-Pyrmont Weser Uplands {{LowerSaxony-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Weser Uplands Schaumburg-Hamelin Nature Park
The Weser Uplands-Schaumburg-Hamelin Nature Park (german: Naturpark Weserbergland Schaumburg-Hameln) lies on the northern edge of the German Central Uplands where it transitions to the North German Plain, about southwest of Hanover. The sponsor of the nature park, which was founded in 1975, is the state of Lower Saxony. The park extends along the Weser valley between Rinteln and Hamelin and includes parts of the Schaumburg Land, Calenberg, Lippe and Pyrmont Uplands from Bad Nenndorf in the north to Bad Pyrmont in the south, Bückeburg and Bad Eilsen in the west and Bad Münder and Osterwald in the east. Its highest elevation is in the Süntel hills. Location Bordered in the north by the forested ridges of the Bückeberg and the Deister, the nature park covers almost from the eastern Weser Hills, Harrl and Süntel running along both sides of the River Weser southwards to the Ith ridge, the Osterwald and the Thüster Berg, through a very varied landscape of wooded, rol ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wesergebirge
The Weser Hills (''Wesergebirge''), also known in German as the ''Weserkette'' ("Weser Chain"),"Ein anderes Bild als die Bergländer der oberen Weser bieten die ''Weserkette'', das ''Wiehengebirge'' und der ''Teutoburger Wald'', see Christian Degn, et al. (ed.) Seydlitz, 1st Part, ''das deutsche Vaterland, wir und die Welt'', 7th ed., Kiel, Hanover, 1954, p. 50 form a low hill chain, up to , in the Weser Uplands in the German states of North Rhine-Westphalia and Lower Saxony. The thickly wooded Weser ridge is one of the northern outliers of the German Central Uplands on the southern edge of the North German Plain and forms part of the TERRA.vita Nature Park in the west and Weser Uplands Schaumburg-Hameln Nature Park in the east. The Weser Hills are widely known because of Schaumburg Castle which stands on the Nesselberg (c. ) in the Schaumburg district of the town of Rinteln, and is the emblem of Schaumburg Land. Geography The Weser Hills cross the counties of Minden-Lü ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Central Uplands
The Central UplandsDickinson (1964), p.18 ff. (german: die MittelgebirgeN.B. In German die ''Mittelgebirge'' (plural) refers to the Central Uplands; das ''Mittelgebirge'' refers to a low mountain range or upland region (''Mittel'' = "medium" and ''-gebirge'' = "range").) is one of the three major natural regions of Germany. It stretches east to west across the country. To the north lies the North German Plain or Northern Lowland; to the south, the Alps and the Alpine Foreland. Formation The German Central Uplands, like the Scandinavian and British mountain ranges and the Urals, belong to the oldest mountains of Europe, even if their present-day appearance has only developed relatively recently. In the Carboniferous, i.e. about 350 million years ago, Variscan mountain ranges were formed in central Europe by the uplifting caused by tectonic plate collision. Immediately after their formation the erosion of the mountains began under the influence of exogenous processes during t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Weser Uplands
The Weser Uplands (German: ''Weserbergland'', ) is a hill region in Germany, between Hannoversch Münden and Porta Westfalica, along the river Weser. The area reaches into three states, Lower Saxony, Hesse, and North Rhine-Westphalia. Important towns of this region include Bad Karlshafen, Holzminden, Höxter, Bodenwerder, Hameln, Rinteln, and Vlotho. The tales of the Brothers Grimm are set in the Weser Uplands, and it has many renaissance buildings, exhibiting a peculiar regional style, the Weser Renaissance style. The region roughly coincides with the natural region of the Lower Saxon Hills defined by the Federal Agency for Nature Conservation (BfN). Geography In addition to the whole of the Weser Valley between Hann. Münden und Porta Westfalica, several geologically associated, but clearly separate chains of uplands, ridges and individual hills are considered part of the Weser Uplands. In its narrowest sense, the following would be included (running from north to sout ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hamelin
Hamelin ( ; german: Hameln ) is a town on the river Weser in Lower Saxony, Germany. It is the capital of the district of Hamelin-Pyrmont and has a population of roughly 57,000. Hamelin is best known for the tale of the Pied Piper of Hamelin. History Hamelin started with a monastery, which was founded as early as 851 AD. A village grew in the neighbourhood and had become a town by the 12th century. The incident with the "Pied Piper" (see below) is said to have happened in 1284 and may be based on a true event, although somewhat different from the tale. In the 15th and 16th centuries Hamelin was a minor member of the Hanseatic League. In June 1634, during the Thirty Years' War, Lothar Dietrich, Freiherr of Bönninghausen, a General with the Imperial Army, lost the Battle of Oldendorf to the Swedish General Kniphausen, after Hamelin had been besieged by the Swedish army. The era of the town's greatest prosperity began in 1664, when Hamelin became a fortified border town of t ... [...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 (1543– ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Waterfall
A waterfall is a 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 on to 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 for years, 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 waterfall is genera ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Anthracite
Anthracite, also known as hard coal, and black coal, is a hard, compact variety of coal that has a submetallic luster. It has the highest carbon content, the fewest impurities, and the highest energy density of all types of coal and is the highest ranking of coals. Anthracite is the most metamorphosed type of coal (but still represents low-grade metamorphism), in which the carbon content is between 86% and 97%. The term is applied to those varieties of coal which do not give off tarry or other hydrocarbon vapours when heated below their point of ignition. Anthracite ignites with difficulty and burns with a short, blue, and smokeless flame. Anthracite is categorized into standard grade, which is used mainly in power generation, high grade (HG) and ultra high grade (UHG), the principal uses of which are in the metallurgy sector. Anthracite accounts for about 1% of global coal reserves, and is mined in only a few countries around the world. The Coal Region of northeastern P ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
