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Lower Rhine Heights
The Lower Rhine Heights (German: ''Niederrheinischer Höhenzug'') is a hill ridge which, with several interruptions, stretches in a broad arc through the Lower Rhine Plain from Krefeld to Nijmegen, between the valley of the Rhine in the east and that of the Niers in the west. This landform element is also called the Lower Rhine Hill Ridge. The sandhills, which in some places reach around hundred meters in height (Klever Berg (106 m)) and protrude more than sixty meters above the surrounding river terraces of the Lower Rhine, originated in the penultimate glacial period (the Saale glaciation) as terminal moraine ridges from glaciers advancing from the northeast. Two of the glacial termini formed the glacial basins of Groesbeek and Kranenburg, resulting in the distinctly recognizable typical W-shaped ridge between Nijmegen and Kleve Kleve (; traditional en, Cleves ; nl, Kleef; french: Clèves; es, Cléveris; la, Clivia; Low Rhenish: ''Kleff'') is a town in the Lower R ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Glacier
A glacier (; ) is a persistent body of dense ice that is constantly moving under its own weight. A glacier forms where the accumulation of snow exceeds its Ablation#Glaciology, ablation over many years, often Century, centuries. It acquires distinguishing features, such as Crevasse, crevasses and Serac, seracs, as it slowly flows and deforms under stresses induced by its weight. As it moves, it abrades rock and debris from its substrate to create landforms such as cirques, moraines, or fjords. Although a glacier may flow into a body of water, it forms only on land and is distinct from the much thinner sea ice and lake ice that form on the surface of bodies of water. On Earth, 99% of glacial ice is contained within vast ice sheets (also known as "continental glaciers") in the polar regions, but glaciers may be found in mountain ranges on every continent other than the Australian mainland, including Oceania's high-latitude oceanic island countries such as New Zealand. Between lati ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geography Of North Rhine-Westphalia
Geography (from Greek: , ''geographia''. Combination of Greek words ‘Geo’ (The Earth) and ‘Graphien’ (to describe), literally "earth description") is a field of science devoted to the study of the lands, features, inhabitants, and phenomena of Earth. The first recorded use of the word γεωγραφία was as a title of a book by Greek scholar Eratosthenes (276–194 BC). Geography is an all-encompassing discipline that seeks an understanding of Earth and its human and natural complexities—not merely where objects are, but also how they have changed and come to be. While geography is specific to Earth, many concepts can be applied more broadly to other celestial bodies in the field of planetary science. One such concept, the first law of geography, proposed by Waldo Tobler, is "everything is related to everything else, but near things are more related than distant things." Geography has been called "the world discipline" and "the bridge between the human and th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geography Of Gelderland
Geography (from Greek: , ''geographia''. Combination of Greek words ‘Geo’ (The Earth) and ‘Graphien’ (to describe), literally "earth description") is a field of science devoted to the study of the lands, features, inhabitants, and phenomena of Earth. The first recorded use of the word γεωγραφία was as a title of a book by Greek scholar Eratosthenes (276–194 BC). Geography is an all-encompassing discipline that seeks an understanding of Earth and its human and natural complexities—not merely where objects are, but also how they have changed and come to be. While geography is specific to Earth, many concepts can be applied more broadly to other celestial bodies in the field of planetary science. One such concept, the first law of geography, proposed by Waldo Tobler, is "everything is related to everything else, but near things are more related than distant things." Geography has been called "the world discipline" and "the bridge between the human and th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kleve
Kleve (; traditional en, Cleves ; nl, Kleef; french: Clèves; es, Cléveris; la, Clivia; Low Rhenish: ''Kleff'') is a town in the Lower Rhine region of northwestern Germany near the Dutch border and the River Rhine. From the 11th century onwards, Cleves was capital of a county and later a duchy. Today, Cleves is the capital of the district of Cleves in the German state of North Rhine-Westphalia. The city is home to one of the campuses of the Rhine-Waal University of Applied Sciences. Territory of the municipality In addition to the inner city, the territory of Kleve comprises fourteen villages and populated places: Bimmen, Brienen, Donsbrüggen, Düffelward, Griethausen, Keeken, Kellen, Materborn, Reichswalde, Rindern, Salmorth, Schenkenschanz, Warbeyen and Wardhausen. History The name ''Kleff'' probably derives from Middle Dutch ''clef'', ''clif'' 'cliff, bluff', referring to the promontory on which the Schwanenburg castle was constructed. Since the city's coat of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kranenburg, North Rhine-Westphalia
Kranenburg is a town and municipality in the district of Cleves in the state of North Rhine-Westphalia, Germany. It is located near the border with the Netherlands, south-east of Nijmegen and west of Cleves. Since 1992, Kranenburg has evolved into a commuter town for Nijmegen. The village has always focused on the Dutch city of Nijmegen, and the local language was Dutch until far into the 19th century. Towns and villages in the municipality * Kranenburg * Nütterden * Schottheide * Mehr * Frasselt * Zyfflich * Wyler * Niel * Grafwegen History Middle Ages First records show that Kranenburg was founded in the 13th century by the Baron of Kleve. The first castle was built in 1270 and the first church a few years later by Dietrichs Luf von Kleve († 1277). In 1294, the village raised to the status of town. In 1308 "The Miraculous Trinity" ( "Wundertätigen Dreifaltigkeit“) was found, establishing Kranenburg as a place of pilgrimage. According to legend, a one-le ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Groesbeek
Groesbeek () is a town and former municipality in the province of Gelderland, the Netherlands. In January 2015 the former municipality merged with Millingen aan de Rijn and Ubbergen. The larger area was known as Groesbeek until January 2016, when its name was changed to Berg en Dal. Description Groesbeek is named after a small stream called the Groesbeek (''beek'' being Dutch for "stream" or "brook"), which no longer exists in its original form. Hills and forests surround the town, and because of this, Groesbeek was isolated in the past, with a close community and a strong dialect. Geography Groesbeek and Kranenburg are situated on the banks of the Groesbeek, a small stream in the Groesbeek valley, a large valley between the Nijmeegse heuvelrug and Reichswald. The Groesbeek valley was carved out by glaciers during the Saale glacial, marking the southernmost expansion of ice-age glaciers in the Netherlands. The hills surrounding the valley in which Groesbeek lies are technicall ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Glacier Terminus
A glacier terminus, toe, or snout, is the end of a glacier at any given point in time. Although glaciers seem motionless to the observer, in reality glaciers are in endless motion and the glacier terminus is always either advancing or retreating. The location of the terminus is often directly related to glacier mass balance, which is based on the amount of snowfall which occurs in the accumulation zone of a glacier, as compared to the amount that is melted in the ablation zone. The position of a glacier terminus is also impacted by localized or regional temperature change over time. Tracking Tracking the change in location of a glacier terminus is a method of monitoring a glacier's movement. The end of the glacier terminus is measured from a fixed position in neighboring bedrock periodically over time. The difference in location of a glacier terminus as measured from this fixed position at different time intervals provides a record of the glacier's change. A similar way of trac ... [...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] |
Lower Rhine Plain
The Lower Rhine Plain (German: ''Niederrheinisches Tiefland'') is one of the natural regions of Germany and lies on either side of the Rhine north of the city of Düsseldorf. Geography The Lower Rhine Plain is bordered in the south by the Lower Rhine Bay and Cologne Lowland, in the southeast by the Bergisches Land, to the east and northeast by the Westphalian Basin and in the west by the Netherlands. The Lower Rhine Plain is an extensively terraced landscape. The otherwise level terraces are interrupted by various features like the V-shaped valleys, flood plains, old river courses or the terminal moraine ridges of the Lower Rhine Heights. The height of the terrain is under 100m above NN almost everywhere. Geology The Lower Rhine Plain is the northern half of the geological structure known as the Lower Rhine Bay (''Niederrheinische Bucht''). Its geology was probably a result of deposition in the last 30 million years, which has given rise to sediments and layers of sedimen ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Saale Glaciation
The Saale glaciation or Saale Glaciation, sometimes referred to as the Saalian glaciation, Saale cold period (german: Saale-Kaltzeit), Saale complex (''Saale-Komplex'') or Saale glacial stage (''Saale-Glazial'', colloquially also the ''Saale-Eiszeit'' or ''Saale-Zeit''), covers the middle of the three large glaciations in Northern Europe and the northern parts of Eastern, Central and Western Europe by the Scandinavian Inland Ice Sheet between the older Elster glaciation and the younger Weichselian glaciation, also called the Last Glacial Period. Age and definitions It succeeded the Holstein interglacial and was followed by the Eemian interglacial. The Saale complex is currently estimated, depending on the source, as existing from around 300,000 to 130,000 years ago or 347,000 to 128,000 years ago (duration: around 219,000 years), roughly contemporaneous with the glaciation of the Riss Glacial in the Alpine region. The actual "ice age" includes only part of the Saale glaciation ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lower Rhine
The Lower Rhine (german: Niederrhein; kilometres 660 to 1,033 of the river Rhine) flows from Bonn, Germany, to the North Sea at Hook of Holland, Netherlands (including the Nederrijn or "Nether Rhine" within the Rhine–Meuse–Scheldt delta); alternatively, ''Lower Rhine'' may refer to the part upstream of Pannerdens Kop, excluding the Nederrijn. Almost immediately after entering the Netherlands, the Rhine splits into numerous branches. The main branch is called the Waal which flows from Nijmegen to meet the Meuse; after which it is called Merwede. Near Rotterdam the river is known as Nieuwe Maas, and becomes the Nieuwe Waterweg flowing into the North Sea at Hook of Holland. The downstream Lower Rhine is a low lying land. Up to the beginning of industrialization roughly one fifth of the land area could only be used as pasture: an endless meadow, which could not be farmed because of flooding and a high ground-water level. However, the remaining soils of the Lower Rhine were alwa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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