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Dillingen, Saarland
Dillingen (also: ''Dillingen an der Saar'') (french: Dillange) is a town in the district of Saarlouis, in Saarland. It has about 20,000 inhabitants and is divided into the three districts Dillingen-city center, Pachten and Diefflen. The city is located on the edge of the Saar-Hunsrück Nature Park at the mouth of the Prims in the Saar and is located about 10 km from the French border. Dillingen is located about 60 km from Luxembourg City and Trier, 50 km from Metz and 30 km from Saarbrücken and is directly adjacent to the urban area of Saarlouis. In terms of population, it is the second largest municipality in the district of Saarlouis. The Dillinger Hütte steelworks is located here. Geography Geographical location Dillingen lies to the right of the Saar in the northern part of the Basin of Saarlouis and thus in the Saar-Nahe Basin. The Basin of Saarlouis is bounded on the northwest, north and northeast by the heights of the Buntsandstein. They belong to ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Saarlouis (district)
Saarlouis (Sarrelouis in French) is a Kreis (district) in the middle of the Saarland, Germany. Neighboring districts are Merzig-Wadern, Sankt Wendel, Neunkirchen, Saarbrücken, and the French ''département'' Moselle. History The district was part of the Holy Roman Empire of the German nation. The biggest part of the district was part of duchy of Lorraine which gradually came under French sovereignty (still as a part of the holy empire) between 1737 and 1766. Other villages were part of the county of Nassau-Saarbrücken. The territory of the city Saarlouis which was built to protect the border, came to France as part of the three Bishoprics. Other villages, which today are considered to be too small to form villages of their own were independent imperial territories. The district showed the fundamental problem of the whole empire: A strong influence of foreign rulers and micro-sized territories. After the Napoleonic wars the area went to Prussia, which in 1816 created the d ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Schwarzwälder Hochwald
The Schwarzwälder Hochwald (; literally 'Black Forest High Forest'), not to be confused with the High Black Forest, is the high south-western part of the Hunsrück in the German states of Saarland and Rhineland-Palatinate. SWRDer Schwarzwälder Hochwald/ref> The mountains are up to 816.32 m high. Geography Location The Schwarzwälder Hochwald lies within the Saar-Hunsrück Nature Park, running roughly from Mettlach in the Saarland to the Erbeskopf in Rhineland-Palatinate. It lies northwest of Losheim, Weiskirchen, Wadern and Nonnweiler in the Saarland and between Hermeskeil and Birkenfeld and between Thalfang and Idar-Oberstein in Rhineland-Palatinate. North of the Schwarzwälder Hochwald lies the Osburger Hochwald; both forested mountain ranges are known simply as the Hochwald ("High Forest"). The southeastern part of the Schwarzwälder Hochwald is called the Dollberge. To the northeast of the Schwarzwälder Hochwald is the Idar Forest. Mountains The mountains a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Carbonate
A carbonate is a salt of carbonic acid (H2CO3), characterized by the presence of the carbonate ion, a polyatomic ion with the formula . The word ''carbonate'' may also refer to a carbonate ester, an organic compound containing the carbonate group C(=O)(O–)2. The term is also used as a verb, to describe carbonation: the process of raising the concentrations of carbonate and bicarbonate ions in water to produce carbonated water and other carbonated beverageseither by the addition of carbon dioxide gas under pressure or by dissolving carbonate or bicarbonate salts into the water. In geology and mineralogy, the term "carbonate" can refer both to carbonate minerals and carbonate rock (which is made of chiefly carbonate minerals), and both are dominated by the carbonate ion, . Carbonate minerals are extremely varied and ubiquitous in chemically precipitated sedimentary rock. The most common are calcite or calcium carbonate, CaCO3, the chief constituent of limestone (as well a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Clay
Clay is a type of fine-grained natural soil material containing clay minerals (hydrous aluminium phyllosilicates, e.g. kaolin, Al2 Si2 O5( OH)4). Clays develop plasticity when wet, due to a molecular film of water surrounding the clay particles, but become hard, brittle and non–plastic upon drying or firing. Most pure clay minerals are white or light-coloured, but natural clays show a variety of colours from impurities, such as a reddish or brownish colour from small amounts of iron oxide. Clay is the oldest known ceramic material. Prehistoric humans discovered the useful properties of clay and used it for making pottery. Some of the earliest pottery shards have been dated to around 14,000 BC, and clay tablets were the first known writing medium. Clay is used in many modern industrial processes, such as paper making, cement production, and chemical filtering. Between one-half and two-thirds of the world's population live or work in buildings made with clay, often ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Grès à Voltzia
The Grès à Voltzia is a geologic formation in France. It preserves fossils dating back to the Triassic period. See also * List of fossiliferous stratigraphic units in France See also * Lists of fossiliferous stratigraphic units in Europe These lists of fossiliferous stratigraphic units in Europe enumerate the rock layers which preserve the fossilized remains of ancient life in Europe by the modern countries wher ... References * Triassic France Triassic System of Europe Anisian Stage {{Triassic-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Muschelkalk
The Muschelkalk (German for "shell-bearing limestone"; french: calcaire coquillier) is a sequence of sedimentary rock strata (a lithostratigraphic unit) in the geology of central and western Europe. It has a Middle Triassic (240 to 230 million years) age and forms the middle part of the tripartite Germanic Trias, that give the Triassic its name, lying above the older Buntsandstein and below the younger Keuper. The Muschelkalk (" mussel chalk") consists of a sequence of limestone and dolomite beds. In the past, the time span in which the Muschelkalk was deposited could also be called "Muschelkalk". In modern stratigraphy, however, the name only applies to the stratigraphic unit. Occurrence The name ''Muschelkalk'' was first used by German geologist Georg Christian Füchsel (1722-1773). In 1834, Friedrich August von Alberti included it into the Triassic system. The name indicates a characteristic feature of the unit, namely the frequent occurrence of lenticular banks composed o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Röt Formation
The Röt Formation or Rötton Formation (German for Röt Shale), or Upper Buntsandstein, is a geologic formation of the Buntsandstein in Germany. It preserves fossils dating back to the Middle Triassic Epoch (Anisian or Aegean or Bithynian in the regional stratigraphy).Röt Formation at .org The formation overlies the Plattenstein and Solling Formations and is overlain by the |
Triassic
The Triassic ( ) is a geologic period and system which spans 50.6 million years from the end of the Permian Period 251.902 million years ago ( Mya), to the beginning of the Jurassic Period 201.36 Mya. The Triassic is the first and shortest period of the Mesozoic Era. Both the start and end of the period are marked by major extinction events. The Triassic Period is subdivided into three epochs: Early Triassic, Middle Triassic and Late Triassic. The Triassic began in the wake of the Permian–Triassic extinction event, which left the Earth's biosphere impoverished; it was well into the middle of the Triassic before life recovered its former diversity. Three categories of organisms can be distinguished in the Triassic record: survivors from the extinction event, new groups that flourished briefly, and other new groups that went on to dominate the Mesozoic Era. Reptiles, especially archosaurs, were the chief terrestrial vertebrates during this time. A specialized subgroup of archo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rotliegend
The Rotliegend, Rotliegend Group or Rotliegendes (german: the underlying red) is a lithostratigraphy, lithostratigraphic unit (a sequence of rock strata) of latest Carboniferous to Guadalupian (middle Permian) age that is found in the subsurface of large areas in western and central Europe. The Rotliegend mainly consists of sandstone layers. It is usually covered by the Zechstein and lies on top of regionally different formation (stratigraphy), formations of late Carboniferous age. The name Rotliegend has in the past not only been used to address the rock strata themselves, but also the time span in which they were formed (in which case the Rotliegend was considered a series (stratigraphy), series or subsystem of the Permian). This time span corresponds roughly with the length of the Cisuralian Epoch (reference date), epoch. Facies and formation In large parts of Pangaea, the last tectonic phase, phases of the Hercynian orogeny were still ongoing during the start of the Permian. A ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Carboniferous
The Carboniferous ( ) is a geologic period and system of the Paleozoic that spans 60 million years from the end of the Devonian Period million years ago ( Mya), to the beginning of the Permian Period, million years ago. The name ''Carboniferous'' means "coal-bearing", from the Latin '' carbō'' ("coal") and '' ferō'' ("bear, carry"), and refers to the many coal beds formed globally during that time. The first of the modern 'system' names, it was coined by geologists William Conybeare and William Phillips in 1822, based on a study of the British rock succession. The Carboniferous is often treated in North America as two geological periods, the earlier Mississippian and the later Pennsylvanian. Terrestrial animal life was well established by the Carboniferous Period. Tetrapods (four limbed vertebrates), which had originated from lobe-finned fish during the preceding Devonian, became pentadactylous in and diversified during the Carboniferous, including early amphibian line ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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