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Geest (company)
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] |
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] |
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 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 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 deposit it on a broad plai ... [...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. Etymology Firs ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lauenburg/Elbe
Lauenburg (), or Lauenburg an der Elbe ( en, Lauenberg on the 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 the southernmost town of Schleswig-Holstein and belongs to the ''Kreis'' (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''). 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 with that of today's district. In medieval times Lauenburg was a waypoint on the Old Salt Rout ... [...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] |
Hamburg
(male), (female) en, Hamburger(s), Hamburgian(s) , timezone1 = Central (CET) , utc_offset1 = +1 , timezone1_DST = Central (CEST) , utc_offset1_DST = +2 , postal_code_type = Postal code(s) , postal_code = 20001–21149, 22001–22769 , area_code_type = Area code(s) , area_code = 040 , registration_plate = , blank_name_sec1 = GRP (nominal) , blank_info_sec1 = €123 billion (2019) , blank1_name_sec1 = GRP per capita , blank1_info_sec1 = €67,000 (2019) , blank1_name_sec2 = HDI (2018) , blank1_info_sec2 = 0.976 · 1st of 16 , iso_code = DE-HH , blank_name_sec2 = NUTS Region , blank_info_sec2 = DE6 , website = , footnotes ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wedel
Wedel is a town in the district of Pinneberg, in Schleswig-Holstein, 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 Saxon aristocracy that ruled the area well into the 17th century. The castle of the Schauenburgs, built in 1311 and known as ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cloppenburg
Cloppenburg (; nds, Cloppenborg; stq, Kloppenbuurich) is a town in Lower Saxony, Germany, capital of Cloppenburg District and part of Oldenburg Münsterland. It lies 38 km south-south-west of Oldenburg in the Weser-Ems region between Bremen and the Dutch border. Cloppenburg is not far from the A1, the major motorway connecting the Ruhr area to Bremen and Hamburg. Another major road is the federal highway B213 being the shortest link from the Netherlands to the A1 and thus to Bremen and Hamburg. The town had strong cultural links with St Munchins Parish in Limerick, Ireland from the 1970s to the 1990s. During this period many groups of teens/young adults from both areas visited and were hosted by families from the other area. Economy The town is a centre for the largely agricultural region of southern Oldenburg. It is the administrative centre of the district and there are many schools. However, there is also some industry in town: e.g. Lumberg, (connector systems) and ... [...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 down ... [...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 into dep ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
