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Nahe River
The Nahe () is a river in Rhineland-Palatinate and Saarland, Germany, a left tributary to the Rhine. It has also given name to the wine region Nahe (wine region), Nahe situated around it. The name Nahe is derived from the Latin word ''Nava'', which is supposed to be based upon the Celtic origin for ''the wild river''. The Nahe separates the northern part of the Palatinate (region), Palatinate from the Hunsrück. It rises in the area of Nohfelden (Saarland), flowing through Rhineland-Palatinate and joining the Rhine in Bingen am Rhein, Bingen. Its length is . Towns along the Nahe include Idar-Oberstein, Kirn, Bad Kreuznach and Bingen. Hydrology The drainage basin of the river covers an area of . Due to this relatively large area compared to the river's length high floods can occur along its middle and lower course within only a few hours, however flowing off also quickly. In 1993 and 1995 in Bad Kreuznach a flow of more than was measured and more than at its mouth into th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hunsrück
The Hunsrück () is a long, triangular, pronounced mountain range, upland in Rhineland-Palatinate, Germany. It is bounded by the valleys of the Moselle (river), Moselle-Saar (north-to-west), the Nahe (south), and the Rhine (east). It is continued by the Taunus mountains, past the Rhine and by the Eifel past the Moselle. To the south of the Nahe is a lower, hilly country forming the near bulk of the Palatinate (region), Palatinate region and all of the, smaller, Saarland. Below its north-east corner is Koblenz. As the Hunsrück proceeds east it acquires north-south width and three notable gaps in its southern ridges. In this zone are dendritic drainage, multi-branch headwaters including the Simmerbach ending at Simmertal on the southern edge. This interior is therefore rarely higher than above sea level. Peaks and escarpments are principally: the Schwarzwälder Hochwald, (Black Forest) Hochwald, the Idar Forest, the Soonwald, and the Bingen Forest. The highest mountain is the Erb ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
North Palatine Uplands
The North Palatine Uplands (german: Nordpfälzer Bergland), sometimes shortened to Palatine Uplands (''Pfälzer Bergland''), is a low mountain range and landscape unit in the German state of Rhineland-Palatinate and belongs mainly to the Palatinate region. It is part of the Saar-Nahe Uplands. Geography Location The North Palatine Uplands lie – roughly stated – between St. Wendel in the state of Saarland to the west and three towns belonging to Rhineland-Palatinate: Alzey to the east, Kaiserslautern to the south and Bad Kreuznach to the north, although these towns are not actually within the region itself. The North Palatine Uplands thus links the landscapes of the Palatine Forest, Saar-Hunsrück Nature Park, Naheland and Rheinhessen. To the northwest its boundary with Naheland is not always clear. A rough guide is the heavily folded ridge north of the Glan river with a height different of as much as 300 metres in place. The North Palatine Uplands fall ma ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rotliegendes
The Rotliegend, Rotliegend Group or Rotliegendes (german: the underlying red) is a 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 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 or subsystem of the Permian). This time span corresponds roughly with the length of the Cisuralian epoch. Facies and formation In large parts of Pangaea, the last phases of the Hercynian orogeny were still ongoing during the start of the Permian. At the same time local crustal extension formed intramontane basins such as the large Permian Basin whic ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Permian
The Permian ( ) is a geologic period and System (stratigraphy), stratigraphic system which spans 47 million years from the end of the Carboniferous Period million years ago (Mya), to the beginning of the Triassic Period 251.9 Mya. It is the last period of the Paleozoic Era; the following Triassic Period belongs to the Mesozoic Era. The concept of the Permian was introduced in 1841 by geologist Sir Roderick Murchison, who named it after the Perm Governorate, region of Perm in Russia. The Permian witnessed the diversification of the two groups of amniotes, the synapsids and the Sauropsida, sauropsids (reptiles). The world at the time was dominated by the supercontinent Pangaea, which had formed due to the collision of Euramerica and Gondwana during the Carboniferous. Pangaea was surrounded by the superocean Panthalassa. The Carboniferous rainforest collapse left behind vast regions of desert within the continental interior. Amniotes, which could better cope with these drier conditi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cisuralian
The Cisuralian is the first series/epoch of the Permian. The Cisuralian was preceded by the Pennsylvanian and followed by the Guadalupian. The Cisuralian Epoch is named after the western slopes of the Ural Mountains in Russia and Kazakhstan and dates between 298.9 ± 0.15 – 272.3 ± 0.5 Mya. The Cisuralian is often synonymous with the informal terms early Permian or lower Permian. It corresponds approximately with the Wolfcampian in southwestern North America. The series saw the appearance of beetles and flies and was a relatively stable warming period of about 21 million years. Name and background The Cisuralian is the first series or epoch of the Permian. The Cisuralian was preceded by the last Pennsylvanian epoch (Gzhelian) and is followed by the Permian Guadalupian Epoch. The name "Cisuralian" was proposed in 1982, and approved by the International Subcommission on Permian Stratigraphy in 1996. The Cisuralian Epoch is named after the western slopes of the Ural Mountain ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Aerial Fg095 DSC 1422 Bingen Nahe
Aerial may refer to: Music * ''Aerial'' (album), by Kate Bush * ''Aerials'' (song), from the album ''Toxicity'' by System of a Down Bands *Aerial (Canadian band) * Aerial (Scottish band) * Aerial (Swedish band) Performance art * Aerial silk, apparatus used in aerial acrobatics *Aerialist, an acrobat who performs in the air Recreation and sport * Aerial (dance move) *Aerial (skateboarding) *Aerial adventure park, ropes course with a recreational purpose * Aerial cartwheel (or side aerial), gymnastics move performed in acro dance and various martial arts *Aerial skiing, discipline of freestyle skiing *Front aerial, gymnastics move performed in acro dance Technology Antennas *Aerial (radio), a radio ''antenna'' or transducer that transmits or receives electromagnetic waves **Aerial (television), an over-the-air television reception antenna Mechanical *Aerial fire apparatus, for firefighting and rescue *Aerial work platform, for positioning workers Optical *Aeri ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Binger Wald
The Bingen Forest (german: Binger Wald) is part of the Hunsrück, a low mountain range in the Central Uplands of Germany. It is up to and is located in the state of Rhineland-Palatinate. Location The landscape of the Bingen Forest lies on the boundary of the counties of Mainz-Bingen (north to southeast), Bad Kreuznach (south) and Rhein-Hunsrück-Kreis (west). It is located between the northeastern end of the Hunsrück main ridge (northwest), the Rhine valley (north and northeast), behind which the Taunus rises, the Rhine Knee near Bingen (east) and the Soonwald (southwest). Flora The flora of the densely wooded Bingen Forest, about 40% of which consists of oak but otherwise is a mixed forest, covers an area of around 7,000 hectares, most of which comprises a contiguous area of woodland. History Barrows such as that southeast of Dichtelbach, castles and the present-day settlements and villages are evidence that the Bingen Forest and its surrounding area have ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Moselle
The Moselle ( , ; german: Mosel ; lb, Musel ) is a river that rises in the Vosges mountains and flows through north-eastern France and Luxembourg to western Germany. It is a left bank tributary of the Rhine, which it joins at Koblenz. A small part of Belgium is in its basin as it includes the Sauer and the Our. Its lower course "twists and turns its way between Trier and Koblenz along one of Germany's most beautiful river valleys."''Moselle: Holidays in one of Germany's most beautiful river valleys'' at www.romantic-germany.info. Retrieved 23 Jan 2016. In this section the land to the north is the Eifel which stretches into |
Saar (river)
The Saar (; french: Sarre ) is a river in northeastern France and western Germany, and a right tributary of the Moselle. It rises in the Vosges mountains on the border of Alsace and Lorraine and flows northwards into the Moselle near Trier. It has two headstreams (the ''Sarre Rouge'' and ''Sarre Blanche'', which join in Lorquin), that both start near Mont Donon, the highest peak of the northern Vosges. After (129 kilometres; 80 miles in France and on the French-German border, and 117 kilometres; 73 miles in Germany) the Saar flows into the Moselle at Konz (Rhineland-Palatinate) between Trier and the Luxembourg border. It has a catchment area of . The Saar flows through the following departments of France, states of Germany and towns: *Moselle (F): Abreschviller (Sarre Rouge), Lorquin, Sarrebourg, Fénétrange *Bas-Rhin (F): Sarre-Union *Moselle (F): Sarralbe, Sarreguemines *Saarland (D): Saarbrücken, Völklingen, Wadgassen, Bous, Saarlouis, Dillingen, Merzi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Blies
The Blies () is a right tributary of the Saar in southwestern Germany (Saarland) and northeastern France (Moselle). The Blies flows from three springs in the Hunsrück near Selbach, Germany. It is roughly 100 km long, ending in the French city of Sarreguemines. It flows through Sankt Wendel, Ottweiler, Neunkirchen, Bexbach, Homburg and Blieskastel (Blieskastel being named after the river). Its lower extent demarcates part of the Franco–German border. The section within France and on the French-German border is long. Tributaries Tributaries of the Blies are, from source to mouth: *Todbach (left) *Oster (left) * Mutterbach (right) *Erbach (left) * Lambsbach (left) * Schwarzbach (left) *Würzbach (right) *Hetschenbach (left) * Gailbach (left) * Mandelbach (right) World War II Fighting took place on the Blies during the Lorraine Campaign, fought from September to December 1944 by the Third United States Army, famously led by George S. Patton. The 35th Infantry Divisi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Prims
The Prims is a 91 km long river in western Germany, right tributary of the Saar. It rises in the Hunsrück mountains, near the village Malborn. It flows generally south through the towns Nonnweiler, Wadern and Schmelz. It flows into the Saar in Dillingen. See also *List of rivers of Saarland A list of rivers of Saarland, Germany: B * Bickenalb * Bist * Blies * Bos E * Ellbach * Erbach F * Franzenbach G * Gailbach * Glan H * Hetschenbach * Holzbach I * Ill K * Köllerbach L * Lambsbach * Leukbach * Löster M * Mandelbach *Mose ... * List of rivers of Rhineland-Palatinate External link Rivers of Saarland Rivers of Rhineland-Palatinate Rivers of the Hunsrück Rivers of Germany {{RhinelandPalatinate-river-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
