|
Palatine-Saarland Muschelkalk Region
The Palatine-Saarland Muschelkalk Region (german: Pfälzisch-Saarländische Muschelkalkgebiet) - or more accurately the Palatine-Saarland-Lorraine Muschelkalk Region (''Pfälzisch-Saarländisch-Lothringisches Muschelkalkgebiet'') - is a natural region of the third order in southwestern Rhineland-Palatinate and southern Saarland in Germany, and, on the French side of the border, in northern Lorraine and Alsace bossue. Its name is derived from the Handbook of the Natural Region Divisions of Germany, where it bears the index number 18. Within the North French Scarplands it represents the Muschelkalk stage, but also transitions locally into bunter sandstone. Its core area is divided into the Zweibrücken Westrich (Upper Bunter Sandstone overlain by Lower Muschelkalk) in the east and the Saar-Blies-Gau with the Bliesgau (Upper Muschelkalk) in the southeast. To the northwest lies the Merzig Muschelkalk Plateau near (Unterem) Saargau, which is separated however from the heartland b ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Natural Regions Of Germany
This division of Germany into major natural regions takes account primarily of geomorphological, geological, hydrological, and pedological criteria in order to divide the country into large, physical units with a common geographical basis. Political boundaries play no part in this, apart from defining the national border. In addition to a division of Germany by ''natural regions'', the federal authorities have also produced a division by so-called ''landscape areas (Landschaftsräume)'' that is based more on human utilisation of various regions and so has clearly different boundaries. Groundwork by the Federal Institute of Regional Studies (BfL) The natural region classification of Germany, as used today by the Federal Office for Nature Conservation (''Bundesamt für Naturschutz'' or BfN) and by most state institutions, is largely based on the work in producing the Handbook of Natural Region Divisions of Germany between the years 1953 to 1962. This divided the present federal t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bliesgau
The Bliesgau is a region in the state of Saarland in the south-west of Germany and borders with France. It is named after the River Blies, which is a tributary to the Saar. Blieskastel is the principal town of the district. Other towns in the area include Gersheim, Mandelbachtal and Wolfersheim. The region forms part of the larger Muschelkalk geological zone. Historically the district is first recorded in the seventh century when it formed part of the lands of the Bishopric of Metz, along with neighbouring Sankt Ingbert. It was ruled by Counts of Bliesgau. Bliesgau Biosphere Reserve The district Einöd is part of thbiosphere reserve Bliesgauwith the Pfänderbachtal in Einöd forming a core zone of 45 hectares. The region is a sanctuary for many rare animal and plant species such as the little owl, beaver, red kite, lizard orchid, and the yellow rattle. Almost half of all types of orchids that occur in Germany can be found here, on the vast, semi-dry grasslands that cover formatio ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gutland (Luxembourg)
Gutland (french: Bon Pays) is a region covering the southern and central parts of the Grand Duchy of Luxembourg. The Gutland (literally "Good Land") covers 68% of the territory of Luxembourg; to the north of Gutland lies the Oesling, which covers the remaining 32% of the Grand Duchy. To the east, the Luxembourgian Gutland adjoins the ''Bitburger Gutland'' of Germany. Gutland is not an homogeneous region, and includes five main sub-regions: the Valley of the Seven Castles, Little Switzerland, the Luxembourg plateau, the Moselle valley, and the Red Lands. Despite its variety, Gutland does have general geographic characteristics, both physical and human, that separate it from the Oesling. Unlike the sparsely populated Oesling, Gutland is relatively urbanised. Whereas the Oesling has only one town with a population larger than 2,000 people, Gutland has four cities with a population largely above 15,000 (Luxembourg City/Lëtzebuerg, Esch-sur-Alzette/Esch-Uelzecht, Differdange/D ... [...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] |
Bunter Sandstone
The Buntsandstein (German for ''coloured'' or ''colourful sandstone'') or Bunter sandstone is a lithostratigraphic and allostratigraphic unit (a sequence of rock strata) in the subsurface of large parts of west and central Europe. The Buntsandstein predominantly consists of sandstone layers of the Lower Triassic series and is one of three characteristic Triassic units, together with the Muschelkalk and Keuper that form the Germanic Trias Supergroup. The Buntsandstein is similar in age, facies and lithology with the Bunter of the British Isles. It is normally lying on top of the Permian Zechstein and below the Muschelkalk. In the past the name Buntsandstein was in Europe also used in a chronostratigraphic sense, as a subdivision of the Triassic system. Among reasons to abandon this use was the discovery that its base lies actually in the latest Permian. Origin The Buntsandstein was deposited in the Germanic Basin, a large sedimentary basin that was the successor of the smal ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Warndt
The Warndt is an extensive forest area of approximately including parts of the German Saarland and the French region Grand Est west of Saarbrücken. The geology of the Warndt is composed of Buntsandstein permeated by veins of iron ore and deposits of hard coal. Today it is a popular recreational area. The area is bounded by the Saar and two of its left tributaries, the Bist in the north and the Rossel in the south. It is transected by the Lauterbach, which flows into the Rossel in Geislautern. The name ''Warndt'' first appears in a deed of donation from 999AD of the Emperor Otto III. Off-limits to the general population, the Warndt had been a lordly hunting ground since the Middle Ages. Prince Ludwig of Nassau-Saarbrücken had a hunting lodge built at Karlsbrunn in 1717 and used it frequently for large hunts, often lasting several days. In 1815 the state forestry administration moved into the estate. In the 17th century, the Warndt was a refuge for French Huguenots. Their s ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Keuper
The Keuper is a lithostratigraphic unit (a sequence of rock strata) in the subsurface of large parts of west and central Europe. The Keuper consists of dolomite, shales or claystones and evaporites that were deposited during the Middle and Late Triassic epochs (about ). The Keuper lies on top of the Muschelkalk and under the predominantly Lower Jurassic Lias or other Early Jurassic strata. The Keuper together with the Muschelkalk and the Buntsandstein form the Germanic Trias Group, a characteristic sequence of rock strata that gave the Triassic its name. "Muschelkalk (geology)", Britannica Online Encyclopedia, October 2010, webpage: EB-39 Exposure The Upper Triassic is well exposed in Swabia, Franconia, Alsace and Lorraine and Luxembourg; it extends from Basel on the east side of the Rhine into Hanover, and through England into Scotland and north-east Ireland; it appears flanking the central plateau of France and in the Pyrenees and Sardinia. The Keuper sequence is li ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Saargau
The Saargau was a Frankish Gau county (''Gaugrafschaft''). Today the name is given to the ridge between the rivers Saar and Moselle in Germany and, in the south, the region between the Saar and the French border. County of Saargau The Saargau was a Frankish gau county that is recorded as early as the 7th century and, at that time, also included that part of the Saar valley which is today in France. In the Treaty of Mersen (870 A.D.) two Saar counties are named: ''comitatus Sarachuua inferior'' (Lower Saargau) and ''comitatur Sarachuua subterior'' (Upper Saargau), of which only the Lower Saargau continued to bear the name Saargau. Landscape of Saargau The Saargau is a ridge west of the River Saar. It begins in the south near Berus, runs northwards along the French border, from the Saarland over to the neighbouring state of Rhineland-Palatinate. The northern part is bounded in the west by the Moselle and ends near Konz, where the Saar empties into the Moselle. The eas ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Zweibrücken Westrich
The Westrich Plateau (german: Westricher Hochfläche),Helmut Beeger et al.: "Die Landschaften von Rheinhessen-Pfalz − Benennung und räumliche Abgrenzung". In: ''Berichte zur deutschen Landeskunde'', Vol. 63, Part 2, Trier, 1989, pp. 327–359 also Zweibrücken Westrich (''Zweibrücker Westrich'')For example in the Handbuch der naturräumlichen Gliederung Deutschlands. or Southwest Palatine Plateau (''Südwestpfälzische Hochfläche''), is a landscape in the German state of Rhineland-Palatinate, with small areas also in the Saarland ( Saarpfalz-Kreis). Its heart is in the southwest of the Palatinate region and it is part of the historic region of Westrich. Geography Structure and boundaries The Westrich Plateau consists mainly of the Sickingen Heights in the north and the Zweibrücken Hills in the south which, morphologically, belong more to northeastern Lorraine in France). The main plateau falls away in a marked scarp slope, the Sickingen Escarpment, to the northw ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rhineland-Palatinate
Rhineland-Palatinate ( , ; german: link=no, Rheinland-Pfalz ; lb, Rheinland-Pfalz ; pfl, Rhoilond-Palz) is a western state of Germany. It covers and has about 4.05 million residents. It is the ninth largest and sixth most populous of the sixteen states. Mainz is the capital and largest city. Other cities are Ludwigshafen am Rhein, Koblenz, Trier, Kaiserslautern, Worms and Neuwied. It is bordered by North Rhine-Westphalia, Saarland, Baden-Württemberg and Hesse and by the countries France, Luxembourg and Belgium. Rhineland-Palatinate was established in 1946 after World War II, from parts of the former states of Prussia (part of its Rhineland and Nassau provinces), Hesse (Rhenish Hesse) and Bavaria (its former outlying Palatinate kreis or district), by the French military administration in Allied-occupied Germany. Rhineland-Palatinate became part of the Federal Republic of Germany in 1949 and shared the country's only border with the Saar Protectorate until the latter wa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bunter Sandstone
The Buntsandstein (German for ''coloured'' or ''colourful sandstone'') or Bunter sandstone is a lithostratigraphic and allostratigraphic unit (a sequence of rock strata) in the subsurface of large parts of west and central Europe. The Buntsandstein predominantly consists of sandstone layers of the Lower Triassic series and is one of three characteristic Triassic units, together with the Muschelkalk and Keuper that form the Germanic Trias Supergroup. The Buntsandstein is similar in age, facies and lithology with the Bunter of the British Isles. It is normally lying on top of the Permian Zechstein and below the Muschelkalk. In the past the name Buntsandstein was in Europe also used in a chronostratigraphic sense, as a subdivision of the Triassic system. Among reasons to abandon this use was the discovery that its base lies actually in the latest Permian. Origin The Buntsandstein was deposited in the Germanic Basin, a large sedimentary basin that was the successor of the smal ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
