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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. . Etymology The term '' geest'' is a substantivisation of the Low German adjective ''güst'', which means "dry and infertile". Description 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 ... [...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] |
Amrum
Amrum (; Öömrang, ''Öömrang'' North Frisian: ''Oomram'') is one of the North Frisian Islands on the Germany, 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, Frisians, Frisian settlers arrived at Amrum and e ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Burgdorf-Peine Geest
The Burgdorf-Peine 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 into depressions like the Fuhse ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cloppenburg Geest
The Cloppenburg 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 down to large cracks in the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Elbe Urstromtal
The 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-Eberswald Urstromtal and carri ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Outwash Plain
An outwash plain, also called a sandur (plural: ''sandurs''), sandr or sandar, is a plain formed of glaciofluvial deposits due to meltwater outwash at the glacier terminus, terminus of a glacier. As it flows, the glacier grinds the underlying rock surface and carries the debris along. The meltwater at the snout of the glacier deposits its load of sediment over the outwash plain, with larger boulders being deposited near the terminal moraine, and smaller particles travelling further before being deposited. Sandurs are common in Iceland where geothermal activity accelerates the melting of ice flows and the deposition of sediment by meltwater. Formation Sandurs are found in glaciated areas, such as Svalbard, Kerguelen Islands, and Iceland. Glaciers and icecaps contain large amounts of silt and sediment, picked up as they erosion, erode the underlying rocks when they move slowly downhill, and at the snout of the glacier, meltwater can carry this sediment away from the glacier and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Elbe
The Elbe ( ; ; or ''Elv''; Upper Sorbian, Upper and , ) 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 Tributary, tributaries include the rivers Vltava, Ohře, Saale, Havel, Mulde, and Schwarze Elster. 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 nation's territory). On its southeastern edges, the Elbe river basin also comprises small parts of Austria (0.6%) and Poland (0.2%). The Elbe catchment area is inhabited by 24.4 million people; its biggest cities are Berlin, Hamburg, Prague, Dresden a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lauenburg/Elbe
Lauenburg (), or Lauenburg an der Elbe (; ), is a town in the state of Schleswig-Holstein, Germany. It is situated on the northern bank of the river Elbe, east of Hamburg. It is overall the southernmost town of Schleswig-Holstein and belongs to the district () of Herzogtum Lauenburg. History The town was founded in 1182 by Bernard of Ascania, the ancestor of the Dukes of Lauenburg. It took its name from that of the castle of ''Lowenborch'' (erected here between 1181 and 1182), deriving from ''Lave'', the Polabian-language name of the Elbe (compare modern Czech ''Labe''). Following the Napoleonic Wars, Lauenburg was ceded by Prussia to Denmark in exchange for the region of Pomerania. Saxe-Lauenburg was a duchy until 1 July 1876, when it was incorporated into the Royal Prussian Province of Schleswig-Holstein. Lauenburg served as the ducal capital until 1616, when the castle burnt down. In 1619 the capital was moved to Ratzeburg. The area of the duchy was roughly identical wit ... [...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 Vierlan ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hamburg
Hamburg (, ; ), officially the Free and Hanseatic City of Hamburg,. is the List of cities in Germany by population, second-largest city in Germany after Berlin and List of cities in the European Union by population within city limits, 7th-largest in the European Union with a population of over 1.9 million. The Hamburg Metropolitan Region has a population of over 5.1 million and is the List of EU metropolitan areas by GDP, eighth-largest metropolitan region by GDP in the European Union. At the southern tip of the Jutland Peninsula, Hamburg stands on the branching River Elbe at the head of a estuary to the North Sea, on the mouth of the Alster and Bille (Elbe), Bille. Hamburg is one of Germany's three city-states alongside Berlin and Bremen (state), Bremen, and is surrounded by Schleswig-Holstein to the north and Lower Saxony to the south. The Port of Hamburg is Germany's largest and Europe's List of busiest ports in Europe, third-largest, after Port of Rotterdam, Rotterda ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wedel
Wedel () is a town in the Pinneberg (district), district of Pinneberg, in Schleswig-Holstein, in northern Germany. It is situated on the right bank of the Elbe, approximately south of Elmshorn, and west of Hamburg. History Foundation and Middle Ages The first known mention of Wedel in a text is in a 1212 document naming the "brothers from Wedel" as witnesses. However, the mention is not definitive and it remains unclear whether a place of this name already existed elsewhere. Artifacts of pre- and early historical periods found here bear witness to early settlement at the site. The name means "bank of water", identifying a place where a body of water must be crossed, in this case the "Wedeler Aue", a small brook which formed an obstacle on an important local trade route. The first clear and definitive reference to Wedel is in documents of the Count of Schauenburg, a member of the Lower Saxony, Lower Saxon aristocracy that ruled the area well into the 17th century. The castle ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
