|
Erkelenz
Erkelenz (, li, Erkelens ) is a town in the Rhineland in western Germany that lies southwest of Mönchengladbach on the northern edge of the Cologne Lowland, halfway between the Lower Rhine region and the Lower Meuse (river), Meuse. It is a medium-sized town (over 44,000) and the largest in the Kreis Heinsberg, district of Heinsberg in North Rhine-Westphalia. Despite the town having more than 1,000 years of history and tradition, in 2006 the eastern part of the borough was cleared to make way for the Garzweiler open pit mine, Garzweiler II brown coal pit operated by RWE, RWE Power. This is planned to be in operation until 2045. Over five thousand people from ten villages have had to be resettled as a result. Since 2010, the inhabitants of the easternmost village of Pesch (Erkelenz), Pesch have left and most have moved to the new villages of Immerath and Borschemich in the areas of Kückhoven and Erkelenz-Nord. Geography Landscape The area is characterised by the gently ro ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Jülich-Zülpich Börde
The Jülich-Zülpich Börde (german: Jülich-Zülpicher Börde) is a landscape in the Rhineland in the German state of North Rhine-Westphalia on the northern edge of the Eifel. It forms the western part of the Lower Rhine Bay, west of the Rhine, excluding the actual Cologne Lowland, from which it is separated by the ridge of the Ville. It is divided into the Jülich Börde (''Jülicher Börde'') around the town of Jülich in the north and the Zülpich Börde (''Zülpicher Börde'') around the town of Zülpich in the south, the two areas being separated from one another by the Bürge forest. Both parts are natural region major units of the Lower Rhine Bay. The Jülich-Zülpich Börde covers areas in the counties of Euskirchen, Düren, Rhein-Erft-Kreis and parts of Rhein-Sieg-Kreis, the county of Heinsberg and the borough of Aachen. The two ''börde'' regions are also referred to as the Rhenish Börde Zone (''Rheinische Bördenzone'').Jakob Baumann, Bernd Wiese: ''Der Erftkrei ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kreis Heinsberg
Heinsberg is a Kreis (district) in the west of North Rhine-Westphalia, Germany with the town of Heinsberg as its capital. Neighbouring districts are Viersen, Neuss, Düren and Aachen, the city of Mönchengladbach and the Dutch province Limburg. Geography Heinsberg is the most westerly district of Germany, reaching 5°52'E in Selfkant municipality. Geographically it covers the lowlands of the Lower Rhine Bay. Rivers * Rur is the main river, crossing the district from southeast to northwest. *Wurm flows into river Rur, in Heinsberg. * Schwalm originates near Erkelenz. * Niers rises near Kuckum. Towns and municipalities History Development of the district The area fell to Prussia in 1815, which in 1816 created the three districts Heinsberg, Erkelenz and Geilenkirchen. In 1932 the districts Heinsberg and Geilenkirchen were merged, and in 1972 Erkelenz district was merged as well. In 1975 the district reached its present size when the municipality Niederkrüchten was moved to t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Niers
The Niers (, ) is a river in Germany and The Netherlands, a right tributary of the river Maas (Meuse). Its wellspring is near Erkelenz, south of Mönchengladbach, in North Rhine-Westphalia (Germany). Course and length The Niers flows through Mönchengladbach, Viersen, Wachtendonk, Geldern and Goch before flowing into the Meuse just across the border with the Netherlands, in Gennep, Limburg (Netherlands). Its overall length is 116 km - 108 km in Germany, 8 km in the Netherlands. See also * List of rivers of North Rhine-Westphalia A list of rivers of North Rhine-Westphalia, Germany: A * Aa, left tributary of the Möhne * Aa, left tributary of the Nethe * Aa, left tributary of the Werre * Aabach, tributary of the Afte * Aabach, small river in the Ems river system * Abbabac ... * Meuse#Tributaries References External links NiersNiersverband Rivers of Limburg (Netherlands) Rivers of North Rhine-Westphalia Rivers of the Netherlands Gennep Rivers o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Garzweiler Open Pit Mine
The Tagebau Garzweiler is a surface mine (german: Tagebau) in the German state of North Rhine-Westphalia. It is operated by RWE and used for mining lignite. The mine currently has a size of 48 km² and got its name from the village of which previously existed at this location. The community was moved to a section of Jüchen with the same name. The open-pit mine The mine is located west of Grevenbroich and exploitation is progressing towards Erkelenz. Mining was originally limited to the 66.0 km² area ''Garzweiler I'' located east of motorway A 44. Mining in the 48.0 km² ''Garzweiler II'' sector started in 2006 and it will take until around 2045 to fully exploit both sectors. The lignite is used for power generation at nearby power plants such as Neurath and Niederaußem. It is not yet known what effect the plan to phase out all coal-fired power plants in Germany by 2038 will have on the Garzweiler lignite mine system. Traffic Motorways A 44 and A 6 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cologne Lowland
The Cologne Lowland,Dickinson 1953, 35, 461–64, 466–73.Elkins 1968, 229. also called the Cologne Bay or, less commonly, the Cologne Bight (german: Kölner Bucht), is a densely populated area of Germany lying between the cities of Bonn, Aachen, and Düsseldorf/Neuss. It is situated in the southwest of the state of North Rhine-Westphalia and forms the natural southern conclusion of the Lower Rhenish lowlands and the transition to the Rhenish Massif (''Rheinische Schiefergebirge'' or "Rhenish Slate Mountains"). The Cologne Bight is surrounded by the High Fens and the Eifel to the west of the Rhine and by the uplands of Bergisches Land to the east of the Rhine. In the south and southeast the rising Rhine Massif, visible from far off by the silhouette of the Siebengebirge, surround the head of the bight at Königswinter. To the northwest the Cologne Bight opens out into the valleys of the Rhine and the Meuse, in the northeast it is bounded by the Münsterländer Kreidebecken (Müns ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Meuse
The Meuse ( , , , ; wa, Moûze ) or Maas ( , ; li, Maos or ) is a major European river, rising in France and flowing through Belgium and the Netherlands before draining into the North Sea from the Rhine–Meuse–Scheldt delta. It has a total length of . History From 1301 the upper Meuse roughly marked the western border of the Holy Roman Empire with the Kingdom of France, after Count Henry III of Bar had to receive the western part of the County of Bar (''Barrois mouvant'') as a French fief from the hands of King Philip IV. In 1408, a Burgundian army led by John the Fearless went to the aid of John III against the citizens of Liège, who were in open revolt. After the battle which saw the men from Liège defeated, John ordered the drowning in the Meuse of suspicious burghers and noblemen in Liège. The border remained stable until the annexation of the Three Bishoprics Metz, Toul and Verdun by King Henry II in 1552 and the occupation of the Duchy of Lorraine by the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rhine
), Surselva, Graubünden, Switzerland , source1_coordinates= , source1_elevation = , source2 = Rein Posteriur/Hinterrhein , source2_location = Paradies Glacier, Graubünden, Switzerland , source2_coordinates= , source2_elevation = , source_confluence = Reichenau , source_confluence_location = Tamins, Graubünden, Switzerland , source_confluence_coordinates= , source_confluence_elevation = , mouth = North Sea , mouth_location = Netherlands , mouth_coordinates = , mouth_elevation = , progression = , river_system = , basin_size = , tributaries_left = , tributaries_right = , custom_label = , custom_data = , extra = The Rhine ; french: Rhin ; nl, Rijn ; wa, Rén ; li, Rien; rm, label= Sursilvan, Rein, rm, label= Sutsilvan and Surmiran, Ragn, rm, label=Rumantsch Grischun, Vallader and Puter, Rain; it, Reno ; gsw, Rhi(n), inclu ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ice Age
An ice age is a long period of reduction in the temperature of Earth's surface and atmosphere, resulting in the presence or expansion of continental and polar ice sheets and alpine glaciers. Earth's climate alternates between ice ages and greenhouse periods, during which there are no glaciers on the planet. Earth is currently in the Quaternary glaciation. Individual pulses of cold climate within an ice age are termed ''glacial periods'' (or, alternatively, ''glacials, glaciations, glacial stages, stadials, stades'', or colloquially, ''ice ages''), and intermittent warm periods within an ice age are called '' interglacials'' or ''interstadials''. In glaciology, ''ice age'' implies the presence of extensive ice sheets in both northern and southern hemispheres. By this definition, Earth is currently in an interglacial period—the Holocene. The amount of anthropogenic greenhouse gases emitted into Earth's oceans and atmosphere is predicted to prevent the next glacial period for th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Riedel
Riedel is a German surname. Notable people with the surname include: * August Riedel (Johann Friedrich Ludwig Heinrich August Riedel) (1799–1883), German painter *Bruce Riedel (born c. 1953), U.S. foreign policy analyst and author *Eberhard Riedel (born 1938), German former alpine skier * Georg Riedel (Altstadt Kantor) (1676-1738), German composer *Georg Riedel (Swedish jazz musician) (born 1934), Czech-born Swedish musician * Hermann Riedel (1847–1913), German composer *Klaus Riedel (1907-1944), German engineer *Lars Riedel (born 1967), German discus thrower *Ludwig Riedel (1790-1861), German botanist *Oliver Riedel (born 1971), German musician * Ryszard Riedel (1956-1994), Polish blues singer and author of many songs of group Dzem *Walter Riedel (1902-1968), German engineer * Antje Göhler (born ''Riedel'', 1967), German chess master and writer See also *Riedel's thyroiditis, a disease *Riedel (glass manufacturer) Riedel ( ) Crystal is a glassware manufacturer based i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sand
Sand is a granular material composed of finely divided mineral particles. Sand has various compositions but is defined by its grain size. Sand grains are smaller than gravel and coarser than silt. Sand can also refer to a textural class of soil or soil type; i.e., a soil containing more than 85 percent sand-sized particles by mass. The composition of sand varies, depending on the local rock sources and conditions, but the most common constituent of sand in inland continental settings and non-tropical coastal settings is silica (silicon dioxide, or SiO2), usually in the form of quartz. Calcium carbonate is the second most common type of sand, for example, aragonite, which has mostly been created, over the past 500million years, by various forms of life, like coral and shellfish. For example, it is the primary form of sand apparent in areas where reefs have dominated the ecosystem for millions of years like the Caribbean. Somewhat more rarely, sand may be composed of calciu ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gravel
Gravel is a loose aggregation of rock fragments. Gravel occurs naturally throughout the world as a result of sedimentary and erosive geologic processes; it is also produced in large quantities commercially as crushed stone. Gravel is classified by particle size range and includes size classes from granule- to boulder-sized fragments. In the Udden-Wentworth scale gravel is categorized into granular gravel () and pebble gravel (). ISO 14688 grades gravels as fine, medium, and coarse, with ranges 2–6.3 mm to 20–63 mm. One cubic metre of gravel typically weighs about 1,800 kg (or a cubic yard weighs about 3,000 lb). Gravel is an important commercial product, with a number of applications. Almost half of all gravel production is used as aggregate for concrete. Much of the rest is used for road construction, either in the road base or as the road surface (with or without asphalt or other binders.) Naturally occurring porous gravel deposits have a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Marl
Marl is an earthy material rich in carbonate minerals, clays, and silt. When hardened into rock, this becomes marlstone. It is formed in marine or freshwater environments, often through the activities of algae. Marl makes up the lower part of the cliffs of Dover, and the Channel Tunnel follows these marl layers between France and the United Kingdom. Marl is also a common sediment in post-glacial lakes, such as the marl ponds of the northeastern United States. Marl has been used as a soil conditioner and neutralizing agent for acid soil and in the manufacture of cement. Description Marl or marlstone is a carbonate-rich mud or mudstone which contains variable amounts of clays and silt. The term was originally loosely applied to a variety of materials, most of which occur as loose, earthy deposits consisting chiefly of an intimate mixture of clay and calcium carbonate, formed under freshwater conditions. These typically contain 35–65% clay and 65–35% carbonate. The te ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
.jpg "Click for more on -> Meuse")
