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Geest
Geest is a type of landform, slightly raised above the surrounding countryside, that occurs on the plains of Northern Germany, the Northern Netherlands and Denmark. It is a landscape of sandy and gravelly soils formed as a glacial outwash plain and now usually mantled by a heathland vegetation on the glacial deposits left behind after the last ice age during the Pleistocene epoch.Whittow, John (1984). ''Dictionary of Physical Geography''. London: Penguin, p. 214. . The term ''geest'' is a substantivisation of the Low German adjective ''güst'', which means "dry and infertile". It is an Old Drift landscape, characterised by the sandy depositions of the Ice Age. In the depressions between the raised flats are wet meadows and, where drainage is poor, bogs. Geest lands are made up of moraines and sandurs. They are almost always next to flat marshlands, the geest being higher and better protected against flood but, compared to the marsh, with poor soil for agriculture. Where the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geesthacht
Geesthacht () is the largest city in the Lauenburg (district), District of the Duchy of Lauenburg (Herzogtum Lauenburg) in Schleswig-Holstein in Northern Germany, south-east of Hamburg on the right bank of the Elbe, 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 of Saxe-Lauenburg, Eric III pawned Geesthacht - as part of the Herrschaft (territory), Herrschaft of Bergedorf - to the Free City of Lübeck in 1370. In 1401, Duke Eric IV of Saxe-Lauenburg, 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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geest (topography)
Geest is a type of landform, slightly raised above the surrounding countryside, that occurs on the plains of Northern Germany, the Northern Netherlands and Denmark. It is a landscape of sandy and gravelly soils formed as a glacial outwash plain and now usually mantled by a heathland vegetation on the glacial deposits left behind after the last ice age during the Pleistocene epoch.Whittow, John (1984). ''Dictionary of Physical Geography''. London: Penguin, p. 214. . The term ''geest'' is a substantivisation of the Low German adjective ''güst'', which means "dry and infertile". It is an Old Drift landscape, characterised by the sandy depositions of the Ice Age. In the depressions between the raised flats are wet meadows and, where drainage is poor, bogs. Geest lands are made up of moraines and sandurs. They are almost always next to flat marshlands, the geest being higher and better protected against flood but, compared to the marsh, with poor soil for agriculture. Where th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cloppenburg Geest
The Cloppenburg Geest (german: Cloppenburger Geest) is a geest region near the town of Cloppenburg in North Germany and the centre of the Saalian glaciation Upper Pleistocene terrain of the Ems-Hunte Geest region. The meltwater sands (''Schmelzwassersande'') of the advancing ice sheet covered the old terrain with outwash sands (''Vorschüttsande''). Woldstedt (1955: 159) spoke about underlying sands that, in the "Cloppenburg-Bassum Geest", belonged to the Elster glaciation. A covering of boulder clay was deposited over the outwash sands during the Saale glaciation, or more precisely the Drenthe stage. A series of meltwater valleys characterises the surface of the Cloppenburg Geest, something that was vital to the emergence of the river network. "Numerous parallel, flat channels cross the terrain and so create a landscape of parallel ridges" writes Woldstedt (1955: 158). There are two opposing theories for the formation of the rivers. Hausfeld (1983; 1984) put their emergence dow ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Burgdorf-Peine Geest
The Burgdorf-Peine Geest (german: Burgdorf-Peiner Geest) is a geest landscape, dominated by end and ground moraines, between Hanover and Brunswick in North Germany, with an area of about . Its natural borders are the Aller depression in the north, the Hildesheim Börde and, in places, the Mittelland Canal in the south the Oker valley in the east and the Hanoverian Moor Geest in the west. Today it is bordered by the cities of Hanover and Brunswick and the towns of Burgdorf, Uetze, Vechelde, Peine and Lehrte. The whole geest region with its rural settlements has a distinctly rural character, with the exception of the town of Peine. The area is crossed from east to west by the Mittelland Canal, the A 2 motorway and the B 188 federal road. This area, also called the Burgdorf-Peine Geest (or Sand) Plateaus, belongs to the Lower Saxon geest countryside, that covers large parts of the North German Plain. The surface of the Burgdorf-Peine Geest is gently rolling. It is divided i ... [...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 Vierla ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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] |
Elbe
The Elbe (; cs, Labe ; nds, Ilv or ''Elv''; Upper and dsb, Łobjo) is one of the major rivers of Central Europe. It rises in the Giant Mountains of the northern Czech Republic before traversing much of Bohemia (western half of the Czech Republic), then Germany and flowing into the North Sea at Cuxhaven, northwest of Hamburg. Its total length is . The Elbe's major tributaries include the rivers Vltava, Saale, Havel, Mulde, Schwarze Elster, and Ohře. The Elbe river basin, comprising the Elbe and its tributaries, has a catchment area of , the twelfth largest in Europe. The basin spans four countries, however it lies almost entirely just in two of them, Germany (65.5%) and the Czech Republic (33.7%, covering about two thirds of the state's territory). Marginally, the basin stretches also to Austria (0.6%) and Poland (0.2%). The Elbe catchment area is inhabited by 24.4 million people, the biggest cities within are Berlin, Hamburg, Prague, Dresden and Leipzig. Etymo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hamburg
Hamburg (, ; nds, label=Hamburg German, Low Saxon, Hamborg ), officially the Free and Hanseatic City of Hamburg (german: Freie und Hansestadt Hamburg; nds, label=Low Saxon, Friee un Hansestadt Hamborg),. is the List of cities in Germany by population, second-largest city in Germany after Berlin, as well as the overall List of cities in the European Union by population within city limits, 7th largest city and largest non-capital city in the European Union with a population of over 1.85 million. Hamburg's urban area has a population of around 2.5 million and is part of the Hamburg Metropolitan Region, which has a population of over 5.1 million people in total. The city lies on the River Elbe and two of its tributaries, the River Alster and the Bille (Elbe), River Bille. One of Germany's 16 States of Germany, federated states, Hamburg is surrounded by Schleswig-Holstein to the north and Lower Saxony to the south. The official name reflects History of Hamburg, Hamburg's history ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Low German
: : : : : (70,000) (30,000) (8,000) , familycolor = Indo-European , fam2 = Germanic , fam3 = West Germanic , fam4 = North Sea Germanic , ancestor = Old Saxon , ancestor2 = Middle Low German , dia1 = West Low German , dia2 = East Low German , iso2 = nds , iso3 = nds , iso3comment = (Dutch varieties and Westphalian have separate codes) , lingua = 52-ACB , map = Nds Spraakrebeet na1945.svg , mapcaption = Present day Low German language area in Europe. , glotto = lowg1239 , glottoname = Low German , notice = IPA Low German or Low Saxon (in the language itself: , and other names; german: Plattdeutsch, ) is a West Germanic language variety spoken mainly in Northern Germany and the northeastern part of the Netherlands. The dialect of Plautdietsch is also spoken in the Russian Mennonite diaspora wor ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dörpling Hohe Geest
Dörpling, a municipality in the district of Dithmarschen in Schleswig-Holstein, Germany, was first mentioned in a document in 1320. Located 17 km north-east of Heide and 4 km east of Tellingstedt upon Eider, it has blurred boundaries with Pahlen. The ancient water mill - destroyed at the end of the 19th century - is said to have inspired a tale of writer Klaus Groth Klaus Groth (24 April 1819 – 1 June 1899) was a Low German poet. Biography Groth was born in Heide, in Ditmarschen, the western part of the Duchy of Holstein. He was the oldest son of Hartwig Groth, a miller, and his wife Anna Christina. H .... References {{DEFAULTSORT:Dorpling Dithmarschen ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cliff
In geography and geology, a cliff is an area of rock which has a general angle defined by the vertical, or nearly vertical. Cliffs are formed by the processes of weathering and erosion, with the effect of gravity. Cliffs are common on coasts, in mountainous areas, escarpments and along rivers. Cliffs are usually composed of rock that is resistant to weathering and erosion. The sedimentary rocks that are most likely to form cliffs include sandstone, limestone, chalk, and dolomite. Igneous rocks such as granite and basalt also often form cliffs. An escarpment (or scarp) is a type of cliff formed by the movement of a geologic fault, a landslide, or sometimes by rock slides or falling rocks which change the differential erosion of the rock layers. Most cliffs have some form of scree slope at their base. In arid areas or under high cliffs, they are generally exposed jumbles of fallen rock. In areas of higher moisture, a soil slope may obscure the talus. Many cliffs als ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Amrum
Amrum (; ''Öömrang'' North Frisian: ''Oomram'') is one of the North Frisian Islands on the German North Sea coast, south of Sylt and west of Föhr. It is part of the Nordfriesland district in the federal state of Schleswig-Holstein and has approximately 2,300 inhabitants. The island is made up of a sandy core of geestland and features an extended beach all along its west coast, facing the open North Sea. The east coast borders to mudflats of the Wadden Sea. Sand dunes are a characteristic part of Amrum's landscape, resulting in a vegetation that is largely made up of heath and shrubs. The island's only forest was planted in 1948. Amrum is a refuge for many species of birds and a number of marine mammals including the grey seal and harbour porpoise. Settlements on Amrum have been traced back to the Neolithic period when the area was still a part of the mainland of the Jutland peninsula. During the Middle Ages, Frisian settlers arrived at Amrum and engaged in salt making and se ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
