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Rehburg Hills
The Rehburg Hills (german: Rehburger Berge) are a hill range, up to , in the districts of Nienburg and Schaumburg in Lower Saxony, Germany. Origin of the name The Rehburg Hills and their foothills give the impression of being several small neighbouring hills. The little village of Bad Rehburg was a well-known spa and bathing resort in the 18th and 19th centuries. As a result, they have been referred to for centuries as the ''Rehburger Berge'' or Rehburg Hills. Geography Geographical location The Rehburg Hills occupy the southern part of the district of Nienburg and northern part of the district of Schaumburg on the southwestern edge of the Steinhuder Meer Nature Park. They lie between Rehburg-Loccum (to the northwest), Hagenburg (to the east) and Sachsenhagen (to the south) and run close by the village of Bad Rehburg that gives them their name. The latter, like the settlements of Loccum, Rehburg, Münchehagen in the west and Winzlar in the east belong to the borough ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lower Saxony
Lower Saxony (german: Niedersachsen ; nds, Neddersassen; stq, Läichsaksen) is a German state (') in northwestern Germany. It is the second-largest state by land area, with , and fourth-largest in population (8 million in 2021) among the 16 ' federated as the Federal Republic of Germany. In rural areas, Northern Low Saxon and Saterland Frisian are still spoken, albeit in declining numbers. Lower Saxony borders on (from north and clockwise) the North Sea, the states of Schleswig-Holstein, Hamburg, , Brandenburg, Saxony-Anhalt, Thuringia, Hesse and North Rhine-Westphalia, and the Netherlands. Furthermore, the state of Bremen forms two enclaves within Lower Saxony, one being the city of Bremen, the other its seaport, Bremerhaven (which is a semi-enclave, as it has a coastline). Lower Saxony thus borders more neighbours than any other single '. The state's largest cities are state capital Hanover, Braunschweig (Brunswick), Lüneburg, Osnabrück, Oldenburg, Hildesheim, Salzgitt ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lake Steinhude
Lake Steinhude, german: Steinhuder Meer, , is a lake in Lower Saxony, Germany located northwest of Hanover. Named after the nearby village of Steinhude, it has an area of about , making it the largest lake of northwestern Germany. At the same time, Lake Steinhude is very shallow, with an average depth of only and a maximum depth of less than . It lies within a region known as the Hanoverian Moor Geest. Geology It is part of the glacial landscape formed after the recession of the glaciers of the latest Ice Age, the Weichselian glaciation. There are two theories regarding how the lake of Steinhude was formed. One of them says that glaciers gouged out the hole and meltwater filled it. The other theory states that an ice storm formed the hole and as the groundwater rose, the lake was created. In its middle there is a small artificial island carrying an 18th-century fortification, the ''Wilhelmstein''. Today the lake is the heart of a nature reserve, the Steinhuder Meer Nature Par ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lower Cretaceous
Lower may refer to: *Lower (surname) *Lower Township, New Jersey *Lower Receiver (firearms) *Lower Wick Lower Wick is a small hamlet located in the county of Gloucestershire, England. It is situated about five miles south west of Dursley, eighteen miles southwest of Gloucester and fifteen miles northeast of Bristol. Lower Wick is within the civil ... Gloucestershire, England See also * Nizhny {{Disambiguation ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sandstone
Sandstone is a clastic sedimentary rock composed mainly of sand-sized (0.0625 to 2 mm) silicate grains. Sandstones comprise about 20–25% of all sedimentary rocks. Most sandstone is composed of quartz or feldspar (both silicates) because they are the most resistant minerals to weathering processes at the Earth's surface. Like uncemented sand, sandstone may be any color due to impurities within the minerals, but the most common colors are tan, brown, yellow, red, grey, pink, white, and black. Since sandstone beds often form highly visible cliffs and other topographic features, certain colors of sandstone have been strongly identified with certain regions. Rock formations that are primarily composed of sandstone usually allow the percolation of water and other fluids and are porous enough to store large quantities, making them valuable aquifers and petroleum reservoirs. Quartz-bearing sandstone can be changed into quartzite through metamorphism, usually related to ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Upper Jurassic
The Late Jurassic is the third epoch of the Jurassic Period, and it spans the geologic time from 163.5 ± 1.0 to 145.0 ± 0.8 million years ago (Ma), which is preserved in Upper Jurassic strata.Owen 1987. In European lithostratigraphy, the name "Malm" indicates rocks of Late Jurassic age. In the past, ''Malm'' was also used to indicate the unit of geological time, but this usage is now discouraged to make a clear distinction between lithostratigraphic and geochronologic/chronostratigraphic units. Subdivisions The Late Jurassic is divided into three ages, which correspond with the three (faunal) stages of Upper Jurassic rock: Paleogeography During the Late Jurassic Epoch, Pangaea broke up into two supercontinents, Laurasia to the north, and Gondwana to the south. The result of this break-up was the spawning of the Atlantic Ocean. However, at this time, the Atlantic Ocean was relatively narrow. Life forms of the epoch This epoch is well known for many famous types of dinosaurs, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountain Pass
A mountain pass is a navigable route through a mountain range or over a ridge. Since many of the world's mountain ranges have presented formidable barriers to travel, passes have played a key role in trade, war, and both Human migration, human and animal migration throughout history. At lower elevations it may be called a hill pass. A mountain pass is typically formed between two volcanic peaks or created by erosion from water or wind. Overview Mountain passes make use of a gap (landform), gap, saddle (landform), saddle, col or notch (landform), notch. A topographic saddle is analogous to the mathematical concept of a saddle surface, with a saddle point marking the highest point between two valleys and the lowest point along a ridge. On a topographic map, passes are characterized by contour lines with an hourglass shape, which indicates a low spot between two higher points. In the high mountains, a difference of between the summit and the mountain is defined as a mountain pas ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wiehen Hills
The Wiehen Hills (german: Wiehengebirge, , also locally, just ''Wiehen'') are a hill range in North Rhine-Westphalia and Lower Saxony in Germany. The hills run from west to east like a long finger away from the main upland area of the Lower Saxon Hills, beginning at the Weser River near Minden and terminating in the vicinity of Osnabrück. It is the northernmost of the German Central Upland ranges extending into the Northern Lowlands. Their highest hill is the Heidbrink near Lübbecke with an altitude of . Location The Wiehen Hills lie within the districts of Landkreis Osnabrück, Osnabrück, Kreis Minden-Lübbecke, Minden-Lübbecke and Kreis Herford, Herford. Their northern section runs in an east-west direction roughly from the territory of Bramsche (northwest of Osnabrück) via Ostercappeln, Bad Essen, Preußisch Oldendorf and Rödinghausen, Lübbecke, Hüllhorst and Bad Oeynhausen as far as the towns of Minden and Porta Westfalica on the Porta Westfalica (gorge), Porta We ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Stemweder Berg
The Stemweder Berg (also known as the Stemmer Berge)Because it has several rounded summits, it should really be called the ''Stemweder Berge'' i.e. "Stemwede Hills". is a ridge above sea levelHeight according tDeutsche Grundkarte auf geoserver.nrw.de/ref> on the border of North Rhine-Westphalia and Lower Saxony in Germany. It is the northernmost and smallest of Germany's Central Uplands ranges. Like the adjacent municipality of Stemwede, the ridge gets its name from the medieval Free County (''Freigrafschaft'') of Stemwede. Location The Stemweder Berg lies on the southern rim of the North German Plain. Relief Amongst the elevations on the Stemweder Berg are the following − sorted by height in metres above Normalnull (NN): Abbreviations: Lower Saxony = LS, North Rhine-Westphalia = NRW * Kollwesshöh (181.4 m), NRW * Scharfer Berg (180.1 m), NRW * Schlichter Brink (ca. 170 m), NRW * Rauher Berg (167.8 m), NRW * Wegmannsberg (160.5 m), NRW ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bückeberg
The Bückeberg (; also the Bückeberge) is a small hill range, up to high, in the Calenberg Uplands between the Harrl and the Deister in central Germany, and is often considered part of the Weser Uplands. It lies in the district of Schaumburg, and stretches for some from west to east from Bückeburg and the village of Bad Eilsen towards Bad Nenndorf. Topography The ridge runs from southwest to northeast for about at heights of to about . It only has a few summits, like the Bückeberg (or ''Diebische Ecke'') (ca. ), east of the track junction on the ''Eulenburg'' Way, and the ''Großer Karl'' () near Reinsdorf. Here its course swings north and ends with the foothills of ''Münchhausener Berg'' and ''Heisterberg'' near Beckedorf. The gentle northern dip slope descends into the North German Plain, whilst the steeper southern scarp slope drops into the Aue valley, through which the A 2 autobahn runs. The Heeßer Berge in the west is a nature reserve. The ridge is c ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Deister
The Deister is a chain of hills in the German state of Lower Saxony, about 15 mi (25 km) southwest of the city of Hanover. It runs in a north-westerly direction from Springe in the south to Rodenberg in the north. The next in the chain of hills to the south is the Kleiner Deister ("Little Deister") from which it is separated by the flat pass of the Deister Gate. It is surrounded by Springe, Wennigsen, Barsinghausen, Bad Nenndorf, Rodenberg and Bad Münder (counter-clockwise, starting in the south). It has a total length of 21 km (14 mi), and rises in the Hofeler to a height of 395 m (1,250 ft). The highest point is the Bröhn at 405 m (1,312 ft). The chain is well-wooded and abounds in game. From the 17th century on there were several coal mines; the last were abandoned in the 1950s. Sandstone from quarries in eastern Deister was used in several important buildings all over Europe, including the opera house in Hanover and the Reichstag i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wilhelm Tower
Wilhelm may refer to: People and fictional characters * William Charles John Pitcher, costume designer known professionally as "Wilhelm" * Wilhelm (name), a list of people and fictional characters with the given name or surname Other uses * Mount Wilhelm Mount Wilhelm (german: Wilhelmsberg) is the highest mountain in Papua New Guinea at . It is part of the Bismarck Range and the peak is the point where three provinces, Chimbu, Jiwaka and Madang, meet. The peak is also known as ''Enduwa Kombuglu' ..., the highest mountain in Papua New Guinea * Wilhelm Archipelago, Antarctica * Wilhelm (crater), a lunar crater See also * Wilhelm scream, a stock sound effect * SS ''Kaiser Wilhelm II'', or USS ''Agamemnon'', a German steam ship * Wilhelmus, the Dutch national anthem {{Disambiguation ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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