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Elbe Urstromtal
The Elbe Urstromtal (german: Elbe-Urstromtal) refers to the present-day valley of the Elbe over a length of around between the German town of Genthin, Saxony-Anhalt, and the Elbe's mouth into the North Sea near Cuxhaven, Lower Saxony. The ''urstromtal'', or glacial meltwater valley, emerged at the height of the Weichselian glaciation. History The Elbe Urstromtal probably emerged between the coldest period of the Weichselian glaciation, about 22,000 to 18,000 years ago, and the end of the glaciation in North Germany about 14,500 years ago. At that time the glacier was melting and the waters attempted to find their way to the lowest lying points. The Elbe Urstromtal collected the meltwaters and carried them to the North Sea, which then lay up to 120 meters below its present level. The then coastline was about further north. The Elbe Urstromtal also collected the meltwaters of the three ''urstromtäler'', the Glogau-Baruth Urstromtal, Warsaw-Berlin Urstromtal and Thorn- Ebers ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Giant Mountains
The Giant Mountains, Krkonoše or Karkonosze (Czech: , Polish: , german: Riesengebirge) are a mountain range located in the north of the Czech Republic and the south-west of Poland, part of the Sudetes mountain system (part of the Bohemian Massif). The Czech-Polish border, which divides the historic regions of Bohemia and Silesia, runs along the main ridge. The highest peak, Sněžka ( pl, Śnieżka, german: Schneekoppe), is the Czech Republic's highest point with an elevation of . On both sides of the border, large areas of the mountains are designated national parks (the Krkonoše National Park in the Czech Republic and the Karkonosze National Park in Poland), and these together constitute a cross-border biosphere reserve under the UNESCO Man and the Biosphere Programme. The source of the River Elbe is within the Giant Mountains. The range has a number of major ski resorts, and is a popular destination for tourists engaging in downhill and cross-country skiing, hiking, cycling a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Valleys Of Saxony
A valley is an elongated low area often running between hills or mountains, which will typically contain a river or stream running from one end to the other. Most valleys are formed by erosion of the land surface by rivers or streams over a very long period. Some valleys are formed through erosion by glacial ice. These glaciers may remain present in valleys in high mountains or polar areas. At lower latitudes and altitudes, these glacially formed valleys may have been created or enlarged during ice ages but now are ice-free and occupied by streams or rivers. In desert areas, valleys may be entirely dry or carry a watercourse only rarely. In areas of limestone bedrock, dry valleys may also result from drainage now taking place underground rather than at the surface. Rift valleys arise principally from earth movements, rather than erosion. Many different types of valleys are described by geographers, using terms that may be global in use or else applied only locally. For ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Landforms Of Brandenburg
A landform is a natural or anthropogenic land feature on the solid surface of the Earth or other planetary body. Landforms together make up a given terrain, and their arrangement in the landscape is known as topography. Landforms include hills, mountains, canyons, and valleys, as well as shoreline features such as bays, peninsulas, and seas, including submerged features such as mid-ocean ridges, volcanoes, and the great ocean basins. Physical characteristics Landforms are categorized by characteristic physical attributes such as elevation, slope, orientation, stratification, rock exposure and soil type. Gross physical features or landforms include intuitive elements such as berms, mounds, hills, ridges, cliffs, valleys, rivers, peninsulas, volcanoes, and numerous other structural and size-scaled (e.g. ponds vs. lakes, hills vs. mountains) elements including various kinds of inland and oceanic waterbodies and sub-surface features. Mountains, hills, plateaux, and plains are the fou ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Landforms Of Hamburg
A landform is a natural or anthropogenic land feature on the solid surface of the Earth or other planetary body. Landforms together make up a given terrain, and their arrangement in the landscape is known as topography. Landforms include hills, mountains, canyons, and valleys, as well as shoreline features such as bays, peninsulas, and seas, including submerged features such as mid-ocean ridges, volcanoes, and the great ocean basins. Physical characteristics Landforms are categorized by characteristic physical attributes such as elevation, slope, orientation, Stratum, stratification, rock exposure and soil type. Gross physical features or landforms include intuitive elements such as berms, mounds, hills, ridges, cliffs, valleys, rivers, peninsulas, volcanoes, and numerous other structural and size-scaled (e.g. ponds vs. lakes, hills vs. mountains) elements including various kinds of inland and oceanic Waterbody, waterbodies and sub-surface features. Mountains, hills, Plateau, plat ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Landforms Of Schleswig-Holstein
A landform is a natural or anthropogenic land feature on the solid surface of the Earth or other planetary body. Landforms together make up a given terrain, and their arrangement in the landscape is known as topography. Landforms include hills, mountains, canyons, and valleys, as well as shoreline features such as bays, peninsulas, and seas, including submerged features such as mid-ocean ridges, volcanoes, and the great ocean basins. Physical characteristics Landforms are categorized by characteristic physical attributes such as elevation, slope, orientation, stratification, rock exposure and soil type. Gross physical features or landforms include intuitive elements such as berms, mounds, hills, ridges, cliffs, valleys, rivers, peninsulas, volcanoes, and numerous other structural and size-scaled (e.g. ponds vs. lakes, hills vs. mountains) elements including various kinds of inland and oceanic waterbodies and sub-surface features. Mountains, hills, plateaux, and plains are the fou ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Urstromtal
An ''urstromtal'' (plural: ''Urstromtäler'') is a type of broad glacial valley, for example, in northern Central Europe, that appeared during the ice ages, or individual glacial periods of an ice age, at the edge of the Scandinavian ice sheet and was formed by meltwaters that flowed more or less parallel to the ice margin. ''Urstromtäler'' are an element of the glacial series. The term is German and means "ancient stream valley". Although often translated as "glacial valley", it should not be confused with a valley carved out by a glacier. More accurately some sources call them "meltwater valleys" or "ice-marginal valleys". Emergence and structure Important for the emergence of the ''Urstromtäler'' is the fact that the general lie of the land on the North German Plain and in Poland slopes down from south to north. Thus the ice sheet that advanced from Scandinavia flowed into a rising terrain. The meltwaters could therefore only flow for a short distance southwards over the sa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nienstedten
Nienstedten () is a quarter in the city of Hamburg, Germany. It belongs to the Altona borough on the right bank of the Elbe river. Nienstedten is home to the International Tribunal for the Law of the Sea. In 2020 the population was 7,114. Geography In 2006, according to the statistical office of Hamburg and Schleswig-Holstein, Nienstedten had a total area of 4.4 km2. The northern border of Nienstedten to the quarter Osdorf is formed by the railway tracks of the city train. In the west lies the quarter Blankenese. To the south, in the middle of river Elbe, the border to Finkenwerder, a quarter of the Hamburg-Mitte borough, is located. To the east, Nienstedten borders the quarter of Othmarschen, in the north east lies Groß Flottbek. Demographics In 2006 Nienstedten has 6,783 inhabitants. The population density was . 18.7% were children under the age of 18, and 24.4% were 65 years of age or older. 9.8% were resident aliens. 74 people were registered as unemployed and 1,4 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Othmarschen
Othmarschen () is a quarter in the Altona borough of the Hamburg in northern Germany. In 2020 the population was 16,009. History The first records on Othmarschen are from 1317. Together with Altona, Othmarschen became a part of Hamburg in 1937/1938 through the Greater Hamburg Act. Geography In 2006 according to the statistical office of Hamburg and Schleswig-Holstein, the quarter Othmarschen has a total area of 6 km2. The western quarter is Nienstedten. In the South the river Elbe is the border to Waltershof. The border in the North to the quarters Groß Flottbek and Bahrenfeld is the railway track of the city train. In the East is the quarter Ottensen. Demographics In 2006, the quarter Othmarschen had a population of 12,169 people. The population density was 2,023 people per km2. 16.7% were children under the age of 18, and 22.9% were 65 years of age or older. 11.3% were immigrants. 153 people were registered as unemployed and 2,508 were employees subject to social insu ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Boroughs And Quarters Of Hamburg
The city of Hamburg in Germany is made up of seven boroughs (German: ''Bezirke'', also known as ''districts'' or ''administrative districts'') and subdivided into 104 quarters (German: ''Stadtteile''). Most of the quarters were former independent settlements. The areal organisation is regulated by the constitution of Hamburg and several laws. The subdivision into boroughs and quarters was last modified in March 2008. Borough overview History The first official administrative divisions of Hamburg were the parishes of four churches, the St. Peter's, St. Catherine's, St. James's and St. Nicholas's Churches (or their preceding buildings). On 24 February, 1529 a compromise of 132 articles between the senate of Hamburg and the citizens (German: ''Langer Rezeß'') established a council of citizens. The twelve councilmen were called ''Oberalte'' (eldermen) and were the three oldest deacons of each parish. Each parish was given a confirmed border. 1871 In 1871 at the declaration ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geesthacht
Geesthacht () is the largest city in the District of the Duchy of Lauenburg (Herzogtum Lauenburg) in Schleswig-Holstein in Northern Germany, south-east of Hamburg on the right bank of the River Elbe. History A church was built in what is today Geesthacht around the year 800. The town was first mentioned in 1216 as ''Hachede'', then a part of the Duchy of Saxony. A change in the course of the Elbe cut the settlement into two: Geest''hacht'' and Marschacht (in today's Lower Saxony). In 1296, Geesthacht became part of the Duchy of Saxe-Lauenburg, partitioned from Saxony. Duke Eric III pawned Geesthacht - as part of the Herrschaft of Bergedorf - to the Free City of Lübeck in 1370. In 1401, Duke Eric IV retook the pawned area by force. Geesthacht was ceded as part of a condominium to the Hanseatic cities Hamburg and Lübeck by the Peace of Perleberg in 1420. In 1811, Geesthacht was annexed to the First French Empire as part of the Bouches de l'Elbe département, but the condomin ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hamburg-Bergedorf
Bergedorf () is the largest of the seven boroughs of Hamburg, Germany, named after Bergedorf quarter within this borough. In 2020 the population of the borough was 130,994. History The city of Bergedorf received town privileges in 1275, then a part of the younger Duchy of Saxony (1180–1296), which was partitioned by its four co-ruling dukes in 1296 into the branch duchies of Saxe-Lauenburg and Saxe-Wittenberg. Bergedorf then became part of the former. This was only to last until 1303, when Lauenburg's three co-ruling dukes, Albert III, Eric I, and John II partitioned their branch duchy into three smaller duchies. Eric then held Bergedorf (Vierlande) and Lauenburg and inherited the share of his childless brother Albert III, Saxe-Ratzeburg, after he was already deceased in 1308 and a retained section from Albert's widow Margaret of Brandenburg-Salzwedel on her death. However, his other brother, John II, then claimed a part, so in 1321 Eric conceded Bergedorf (with Vierlande ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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