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North Brandenburg Plateaux And Upland
The North Brandenburg Plateaux and Upland (german: Nordbrandenburgische Platten- und Hügelland) is a natural region in the northwest of Brandenburg and, to a lesser extent, the southwest of Mecklenburg-Vorpommern and northeast of Saxony-Anhalt in Germany. It is major unit group no. 77 in the natural regional divisions of Germany. The Brandenburg portion of the North Brandenburg Plateaux and Upland is largely coextensive with the natural region of Prignitz and Ruppin Land (''Prignitz und Ruppiner Land'') in the structural atlas of the state of Brandenburg. Location The North Brandenburg Plateaux and Upland is part of the North German Plain. It extends from the Elde depression in the west to the Havel in the middle of North Brandenburg. Its neighbouring natural regions are the Southwest Foreland of the Mecklenburg Lake District to the northwest, the Mecklenburg Lake District to the northeast, the Luchland to the southeast and the Elbe Depression to the southwest. Description ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Perleberg
Perleberg (; North Margravian: ''Perlberg'') is the capital of the district of Prignitz, located in the northwest of the German state of Brandenburg. The town received city rights in 1239 and today has about 12,000 inhabitants. Located in a mostly agricultural area, the town has a long history of troops (most notably Prussian) being stationed there and as an administrative center for local government. Geography Perleberg is located in the heart of the district of Prignitz, about halfway between the two largest German cities Berlin and Hamburg. It is surrounded by the municipalities Karstädt to the north-west, Gross Pankow (Prignitz) to the north-east, Plattenburg to the south-east; the '' Ämter'' Bad Wilsnack/Weisen in the south, Lenzen-Elbtalaue in the west; and the town of Wittenberge to the south-west. The Stepenitz flows from northeast to southwest through Perleberg. The town's historic center is built on an island between two arms of the river. History One of the town ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Terminal Moraine
A terminal moraine, also called end moraine, is a type of moraine that forms at the terminal (edge) of a glacier, marking its maximum advance. At this point, debris that has accumulated by plucking and abrasion, has been pushed by the front edge of the ice, is driven no further and instead is deposited in an unsorted pile of sediment. Because the glacier acts very much like a conveyor belt, the longer it stays in one place, the greater the amount of material that will be deposited. The moraine is left as the marking point of the terminal extent of the ice. Formation As a glacier moves along its path, the surrounding area is continuously eroding. Loose rock and pieces of bedrock are constantly being picked up and transported with the glacier. Fine sediment and particles are also incorporated into the glacial ice. The accumulation of these rocks and sediment together form what is called glacial till when deposited. Push moraines are formed when a glacier retreats from a previou ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kyritz Plateau
Kyritz () is a town in the Ostprignitz-Ruppin district, in Brandenburg, Germany. It is situated 28 km west of Neuruppin and 28 km southeast of Pritzwalk. The town has 9,260 inhabitants (2019). Overview The town is situated near the Kyritzer Seenkette, a chain of lakes. The town is nicknamed "Kyritz an der Knatter" (Kyritz at the Rattle). The noise of numerous water mills along a stream parallel to the river Jäglitz was the reason for this nickname. This river channel does not exist anymore. The town includes the districts Berlitt, Bork, Drewen, Gantikow, Ganz, Holzhausen, Kötzlin, Lellichow, Mechow, Rehfeld and Teetz. History The oldest document mentioning the area around Kyritz as "Chorizi" was written in 948. The region was called "Prignitz". The name is derived from the slavic word "pregynica" meaning "inaccessible woods". A castle was built here in 1148, and little by little a town developed close to the castle. In the year 1225 a Franciscan friary was establi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Prignitz (natural Region)
Prignitz () is a ''Kreis'' (district) in northwestern Brandenburg, Germany. Neighboring districts, clockwise from the north, are Ludwigslust-Parchim (in Mecklenburg-Western Pomerania), Ostprignitz-Ruppin (Brandenburg), Stendal (Saxony-Anhalt), and Lüchow-Dannenberg (Lower Saxony). Geography The term Prignitz originally meant the region north of the confluence of the Elbe and Havel rivers. This region is larger than the district. It also includes the town of Havelberg in Saxony-Anhalt and large portions of the neighbouring district of Ostprignitz-Ruppin. The Elbe river forms the southwestern border of the district. History The historical region Prignitz consisted of the following eleven districts, established in the 13th century: Wittenberge, Lenzen, Perleberg, Putlitz, Kyritz, Nitzow, Wittstock, Pritzwalk, Havelberg, Wusterhausen and Grabow. The present district of Prignitz was created in 1993 by merging the previous districts of Pritzwalk and Perleberg and a few muni ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lake Rudow
A lake is an area filled with water, localized in a basin, surrounded by land, and distinct from any river or other outlet that serves to feed or drain the lake. Lakes lie on land and are not part of the ocean, although, like the much larger oceans, they do form part of the Earth's water cycle. Lakes are distinct from lagoons, which are generally coastal parts of the ocean. Lakes are typically larger and deeper than ponds, which also lie on land, though there are no official or scientific definitions. Lakes can be contrasted with rivers or streams, which usually flow in a channel on land. Most lakes are fed and drained by rivers and streams. Natural lakes are generally found in mountainous areas, rift zones, and areas with ongoing glaciation. Other lakes are found in endorheic basins or along the courses of mature rivers, where a river channel has widened into a basin. Some parts of the world have many lakes formed by the chaotic drainage patterns left over from the last ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lake Ruppin
Ruppiner See is a lake in Ostprignitz-Ruppin, Brandenburg, Germany. At an elevation of , its surface area is . It is believed to have formed as a glacial tunnel valley. History A Slavic fortification stood at the mouth of the Rhin on the northern shore. In the 12th century, the German settlement of Ruppin (now called Altruppin) was established next to it. A few decades later, Neuruppin was established on the southwest shore. A mill was built in Altfriesack, between the Ruppiner See and the Bützsee next to the Slavic settlement of Wustrau. The latter is probably the oldest settlement on the lake. Around the lake are other villages, which mostly now belong to the municipality of Neuruppin. Wustrau and Altfriesack now form one division in the municipality of Fehrbellin. Economic and strategic importance The lake was strategically important as it was the center of the Slavic area. It was also of economic importance due to its fisheries and for transportation. The building of the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tunnel Valley
A tunnel valley is a U-shaped valley originally cut under the glacial ice near the margin of continental ice sheets such as that now covering Antarctica and formerly covering portions of all continents during past glacial ages. They can be as long as , wide, and deep. Tunnel valleys were formed by subglacial erosion by water and served as subglacial drainage pathways carrying large volumes of meltwater. Their cross-sections often exhibit steep-sided flanks similar to fjord walls. They presently appear as dry valleys, lakes, seabed depressions, and as areas filled with sediment. If they are filled with sediment, their lower layers are filled primarily with glacial, glaciofluvial or glaciolacustrine sediment, supplemented by upper layers of temperate infill. They can be found in areas formerly covered by glacial ice sheets including Africa, Asia, North America, Europe, Australia and offshore in the North Sea, the Atlantic and in waters near Antarctica. Tunnel valleys appear in t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kyritz Lake Chain
Kyritz () is a town in the Ostprignitz-Ruppin district, in Brandenburg, Germany. It is situated 28 km west of Neuruppin and 28 km southeast of Pritzwalk. The town has 9,260 inhabitants (2019). Overview The town is situated near the Kyritzer Seenkette, a chain of lakes. The town is nicknamed "Kyritz an der Knatter" (Kyritz at the Rattle). The noise of numerous water mills along a stream parallel to the river Jäglitz was the reason for this nickname. This river channel does not exist anymore. The town includes the districts Berlitt, Bork, Drewen, Gantikow, Ganz, Holzhausen, Kötzlin, Lellichow, Mechow, Rehfeld and Teetz. History The oldest document mentioning the area around Kyritz as "Chorizi" was written in 948. The region was called "Prignitz". The name is derived from the slavic word "pregynica" meaning "inaccessible woods". A castle was built here in 1148, and little by little a town developed close to the castle. In the year 1225 a Franciscan friary was establi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rhinluch
The Rhinluch is a fen landscape in the German state of Brandenburg, bisected by the river Rhin to which it owes its name. This wetland region lies north of Fehrbellin in the county of Ostprignitz-Ruppin. The upper Rhinluch covers an area of about . The suffix '' luch'' is used to describe several wet areas in the state of Brandenburg, in which, prior to the advent of modern drainage systems, water remained largely stagnant rather than flowing. The Rhinluch was formed during the last ice age and its post-glacial period. About 16,000 years ago, the Eberswald ''urstromtal'' was formed by the meltwaters of the glacial ice sheet as they drained away to the sea. Later, this broad river valley dried up as the ice sheet retreated during the late ice age. In the land that makes up the present-day Rhinluch, lakes initially formed in individual places, especially where there were dead ice kettle holes. Over the course of time, these became bogs through the natural silting up process. In a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rhin
The Rhin is a long river in Brandenburg, Germany, right tributary to the river Havel. It flows through the city Neuruppin and several lakes. A few kilometres downstream from Rhinow it flows into the Havel, about upstream from where the Havel meets the Elbe. File:Zermuetzel_bridge_Rhin.jpg, In Neuruppin-Zermützel File:Wustrau_Wustrauer_Rhin.jpg, Wustrauer Rhin in Fehrbellin Fehrbellin is a municipality in Germany, located 60 km NW of Berlin. It had 9,310 inhabitants as of 2005, but has since declined to 8,606 inhabitants in 2012. History In 1675, the Battle of Fehrbellin was fought there, in which the troops of ...-Wustrau File:Fehrbellin_Wustrauer_Rhin.jpg, Wustrauer Rhin in Fehrbellin File:Fehrbellin_Wall_bridge.jpg, Bützrhin near Fehrbellin-Wall Rivers of Brandenburg Rivers of Germany {{Brandenburg-river-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dosse (river)
The Dosse is a river in the district of Ostprignitz-Ruppin in the northwestern part of Brandenburg, Germany. It is a right tributary of the Havel in Saxony-Anhalt. The Dosse is long, with its source on the border between Mecklenburg-Vorpommern and Brandenburg, arising out of three small brooks that unite after four kilometres. It flows generally south, through Wittstock, Wusterhausen and Neustadt an der Dosse, before joining the Havel near Havelberg in Saxony-Anhalt. The total catchment area is . With the town of Wittstock on its banks, the Dosse was the site of the 1636 Battle of Wittstock between Sweden and an alliance between Imperial and Saxon troops during the Thirty Years' War. See also *List of rivers of Brandenburg *List of rivers of Saxony-Anhalt A list of rivers of Saxony-Anhalt, Germany: A * Aland * Aller * Allerbach, tributary of the Rappbode (Rappbode Auxiliary Dam) * Allerbach, tributary of the Warme Bode * Alte Elbe B * Bauerngraben * Beber *Biese * ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
