Taubergießen
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Taubergießen
Taubergießen is a floodplain wetland on the southern Upper Rhine in the natural area Offenburg Rhine plain. Taubergießen was declared Naturschutzgebiet (Deutschland), Naturschutzgebiet (Nature Reserve) in 1979 and, with 1,697 hectares, is one of the largest protected areas in Baden-Württemberg. It has a north–south extension of more than 12 km. The largest width is about 2.5 km. Name The name ''"Taubergießen"'' derives from ''Taubergießen'', one of the numerous watercourses and branches of the nature reserve, which runs in the north of the area and drains from the right into the lower course of the Elz (Rhein), Elz river, which is closer to the Rhine. Under "pouring" is understood underground, i.e. in direct connection with the groundwater flowing parts of the stream, which come from a sufficient depression of the bottom again to the surface. These are particularly common in this area, the middle area of the southern Upper Rhine. The word "deaf" describes nutri ...
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Elz (Rhein)
The Elz is a river in Baden-Württemberg, Germany, a right tributary of the Rhine. It rises in the Black Forest, near the source of the Breg River, Breg. The Elz flows through Elzach, Waldkirch and Emmendingen before reaching the Rhine near Lahr. Its length is approx. . The lower reaches of the Elz are by-passed by the Leopold Canal (Baden-Württemberg), Leopold Canal, a flood relief canal. Course The Elz rises north of Furtwangen im Schwarzwald, Furtwangen in the area of the Brend (mountain), Brend and the Rohrhardsberg mountains (between the Furtwänglehof and the Kolmenhof) not far from the source of the Breg (river), Breg which is hydrographically the source of the Danube. In its upper reaches the Elz flows in a northerly direction, initially through a high valley with pasture land, bog and ice age glacial landforms. Then after a steep drop at the little '':File:Elzfall.jpg, Elz Falls'', it continues through a deeply incised, wooded and sparsely populated V-shaped valley. ...
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Rhinau
Rhinau (; ) is a commune in the Bas-Rhin department of Grand Est in north-eastern France. Until 1398, the village was located on the bank of the Rhine. The present village dates from the sixteenth century. At periods of low water in the Rhine, it is possible to see the old foundations of the village, as happened in 1749. After a flood in 1541, an uninhabited 58% of its territory (10 km²) happened to end up on the right bank of the Rhine, in Germany. The German part of Rhinau is a natural reserve, the Taubergießen. A ferry crosses the river, linking the two banks in France and Germany. Geography The village of Rhinau is situated on the Rhine about 30 kilometers sound of Strasbourg. It is a notable city in that it has 997 hectares of territory on the right bank of the Rhine, in Germany. These 997 hectares are thus managed under German sovereignty, but, ''de facto'' run by the commune of Rhinau. This is due to a meander of the Rhine in 1541, and was made note of in the ...
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Rheinhausen (Breisgau)
Rheinhausen () is a town in the district of Emmendingen in Baden-Württemberg in Germany. Geography Rheinhausen is located in the northern Breisgau region on the Rhine river. Along the Rhine, it includes part of the Taubergießen Nature Reserve, one of the largest nature reserves in Baden-Wuerttemberg. Neighboring communities To the west, across the Rhine river in France, is the Rhinau Island Nature Reserve, in the Schœnau commune of the Bas-Rhin department in France's Alsace region. Across the town's southern border is the village of Weisweil, to the east are the towns of Kenzingen and Herbolzheim, and to the north is the town of Rust Rust is an iron oxide, a usually reddish-brown oxide formed by the reaction of iron and oxygen in the catalytic presence of water or air moisture. Rust consists of hydrous iron(III) oxides (Fe2O3·nH2O) and iron(III) oxide-hydroxide (FeO(OH) ..., in the Ortenau district. Villages In 1972, the town of Rheinhausen was formed by comb ...
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Floodplain
A floodplain or flood plain or bottomlands is an area of land adjacent to a river. Floodplains stretch from the banks of a river channel to the base of the enclosing valley, and experience flooding during periods of high Discharge (hydrology), discharge.Goudie, A. S., 2004, ''Encyclopedia of Geomorphology'', vol. 1. Routledge, New York. The soils usually consist of clays, silts, sands, and gravels deposited during floods. Because of regular flooding, floodplains frequently have high soil fertility since nutrients are deposited with the flood waters. This can encourage farming; some important agricultural regions, such as the Nile and Mississippi Basin, Mississippi Drainage basin, river basins, heavily exploit floodplains. Agricultural and urban regions have developed near or on floodplains to take advantage of the rich soil and freshwater. However, the Flood risk, risk of inundation has led to increasing efforts to Flood control, control flooding. Formation Most floodplai ...
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Ramsar Convention
The Ramsar Convention on Wetlands of International Importance Especially as Waterfowl Habitat is an international treaty for the conservation and sustainable use of Ramsar site, Ramsar sites (wetlands). It is also known as the Convention on Wetlands. It is named after the city of Ramsar, Mazandaran, Ramsar in Iran, where the convention was signed in 1971. Every three years, representatives of the contracting parties meet as the Ramsar Convention#Conference of the Contracting Parties, Conference of the Contracting Parties (COP), the policy-making organ of the wetland conservation, convention which adopts decisions (site designations, resolutions and recommendations) to administer the work of the convention and improve the way in which the parties are able to implement its objectives. In 2022, COP15 was held in Montreal, Canada. List of wetlands of international importance The list of wetlands of international importance included 2,531 Ramsar site, Ramsar sites in Februa ...
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Floodplains
A floodplain or flood plain or bottomlands is an area of land adjacent to a river. Floodplains stretch from the banks of a river channel to the base of the enclosing valley, and experience flooding during periods of high discharge.Goudie, A. S., 2004, ''Encyclopedia of Geomorphology'', vol. 1. Routledge, New York. The soils usually consist of clays, silts, sands, and gravels deposited during floods. Because of regular flooding, floodplains frequently have high soil fertility since nutrients are deposited with the flood waters. This can encourage farming; some important agricultural regions, such as the Nile and Mississippi river basins, heavily exploit floodplains. Agricultural and urban regions have developed near or on floodplains to take advantage of the rich soil and freshwater. However, the risk of inundation has led to increasing efforts to control flooding. Formation Most floodplains are formed by deposition on the inside of river meanders and by overbank flow ...
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Black Forest
The Black Forest ( ) is a large forested mountain range in the States of Germany, state of Baden-Württemberg in southwest Germany, bounded by the Rhine Valley to the west and south and close to the borders with France and Switzerland. It is the source of the Danube and Neckar rivers. Its highest peak is the Feldberg (Black Forest), Feldberg with an elevation of above sea level. Roughly oblong in shape, with a length of and breadth of up to , it has an area of about . Historically, the area was known for forestry and the mining of ore deposits, but tourism has now become the primary industry, accounting for around 300,000 jobs. There are Baroque fortifications in the Black Forest, several ruined military fortifications dating back to the 17th century. History In ancient times, the Black Forest was known as , after the Celtic deity, Abnoba. In Roman times (Late antiquity), it was given the name ("Marcynian Forest", from the Germanic word ''marka'', "border"). The Black ...
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Vosges
The Vosges ( , ; ; Franconian and ) is a range of medium mountains in Eastern France, near its border with Germany. Together with the Palatine Forest to the north on the German side of the border, they form a single geomorphological unit and low mountain range of around in area. It runs in a north-northeast direction from the Burgundian Gate (the Belfort– Ronchamp– Lure line) to the Börrstadt Basin (the Winnweiler– Börrstadt– Göllheim line), and forms the western boundary of the Upper Rhine Plain. The Grand Ballon is the highest peak at , followed by the Storkenkopf (), and the Hohneck ().IGN maps available oGéoportail/ref> Geography Geographically, the Vosges Mountains are wholly in France, far above the Col de Saverne separating them from the Palatinate Forest in Germany. The latter area logically continues the same Vosges geologic structure but traditionally receives this different name for historical and political reasons. From 1871 to 1918 the Vos ...
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Rift
In geology, a rift is a linear zone where the lithosphere is being pulled apart and is an example of extensional tectonics. Typical rift features are a central linear downfaulted depression, called a graben, or more commonly a half-graben with normal faulting and rift-flank uplifts mainly on one side. Where rifts remain above sea level they form a rift valley, which may be filled by water forming a rift lake. The axis of the rift area may contain volcanic rocks, and active volcanism is a part of many, but not all, active rift systems. Major rifts occur along the central axis of most mid-ocean ridges, where new oceanic crust and lithosphere is created along a divergent boundary between two tectonic plates. ''Failed rifts'' are the result of continental rifting that failed to continue to the point of break-up. Typically the transition from rifting to spreading develops at a triple junction where three converging rifts meet over a hotspot. Two of these evolve to t ...
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Upper Rhine Plain
The Upper Rhine Plain, Rhine Rift Valley or Upper Rhine Graben ( German: ''Oberrheinische Tiefebene'', ''Oberrheinisches Tiefland'' or ''Oberrheingraben'', French: ''Vallée du Rhin'') is a major rift, about and on average , between Basel in the south and the cities of Frankfurt/Wiesbaden in the north. Its southern section straddles the France–Germany border. It forms part of the European Cenozoic Rift System, which extends across Central Europe. The Upper Rhine Graben formed during the Oligocene, as a response to the evolution of the Alps to the south. It remains active to the present day. Today, the Rhine Rift Valley forms a downfaulted trough through which the river Rhine flows. Formation The Upper Rhine Plain was formed during the Early Cenozoic era, during the Late Eocene epoch. At this time, the Alpine Orogeny, the major mountain building event that was to produce the Alps, was in its early stages. The Alps were formed because the continents of Europe and Africa coll ...
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World Database On Protected Areas
The World Database on Protected Areas (WDPA) is the largest assembly of data on the world's terrestrial and marine protected areas, containing more than 260,000 protected areas as of August 2020, with records covering 245 countries and territories throughout the world. The WDPA is a joint venture between the United Nations Environment Programme World Conservation Monitoring CentreUNEP-WCMC and the International Union for Conservation of NatureIUCN World Commission on Protected AreasWCPA. Data for the WDPA is collected from international convention secretariats, governments and collaborating NGOs, but the role of custodian is allocated to the Protected Areas Programme of UNEP-WCMC, based in Cambridge, UK, who have hosted the database since its creation in 1981. The WDPA delivers invaluable information to decision-makers around the world, particularly in terms of measuring the extent and effectiveness of protected areas as an indicator for meeting global biodiversity targets. In Oc ...
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