Brühlbach (Erms, Bad Urach)
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Brühlbach (Erms, Bad Urach)
The Brühlbach is a river in Baden-Württemberg, Germany. It flows into the Erms near Bad Urach. Geography Sources The springs of the Brühlbach are located about 150 m southwest of the Urach waterfall. They are several karst springs, which emerge in a rugged limestone plateau. The water comes from the plateau around Würtingen. There, rainwater seeps through the calcareous rock layers. The carbonated water absorbs lime and collects on the water-impermeable marl layer below. Approximately 28 hours after its infiltration, the water reappears in the Brühlbach springs. The flow varies depending on weather and season from about 70 L/s up to 420 L/s. In exceptionally dry summers the springs can even dry up. Course After its source, the Brühlbach falls down the Urach waterfall. Below it is strengthened by further springs. It flows in a predominantly northern direction through the "Brühl" and - after the "Gütersteinbach" from the "Gütersteiner Wasserfall" - through ...
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Erms
The Erms () is a river of the karstified Swabian Alb range in Baden-Württemberg, Germany. It flows into the Neckar in Neckartenzlingen. On its way from the Karst spring to the next large municipality Bad Urach, a former Erms sedimented, especially during floods, no less than eight valley cataracts, where chemically precipitated travertine repeatedly drops . Geography The Ermstal valley is one of the largest valley systems that have cut into the layer of the Swabian Alb from the northwest. The nearby large waters of the river system of the Rhine lie much deeper than the Danube on the south-eastern side of the Alb, so that regressive erosion of the Rhenish waters is gradually shifting back the European watershed at the expense of the Danube basin. Due to the Neckar river, which runs here particularly close to the Alb's eaves, and the great difference in altitude between them, the Erms possessed sufficient erosive power to form one of the most striking valleys of the Alb's eav ...
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Germany
Germany, officially the Federal Republic of Germany, is a country in Central Europe. It lies between the Baltic Sea and the North Sea to the north and the Alps to the south. Its sixteen States of Germany, constituent states have a total population of over 84 million in an area of , making it the most populous member state of the European Union. It borders Denmark to the north, Poland and the Czech Republic to the east, Austria and Switzerland to the south, and France, Luxembourg, Belgium, and the Netherlands to the west. The Capital of Germany, nation's capital and List of cities in Germany by population, most populous city is Berlin and its main financial centre is Frankfurt; the largest urban area is the Ruhr. Settlement in the territory of modern Germany began in the Lower Paleolithic, with various tribes inhabiting it from the Neolithic onward, chiefly the Celts. Various Germanic peoples, Germanic tribes have inhabited the northern parts of modern Germany since classical ...
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States Of Germany
The Federal Republic of Germany is a federation and consists of sixteen partly sovereign ''states''. Of the sixteen states, thirteen are so-called area-states ('Flächenländer'); in these, below the level of the state government, there is a division into local authorities (counties and county-level cities) that have their own administration. Two states, Berlin and Hamburg, are city-states, in which there is no separation between state government and local administration. The state of Bremen (state), Bremen is a special case: the state consists of the cities of Bremen (city), Bremen, for which the state government also serves as the municipal administration, and Bremerhaven, which has its own local administration separate from the state government. It is therefore a mixture of a city-state and an area-state. Three states, Bavaria, Saxony, and Thuringia, use the appellation ("free state"); this title is merely stylistic and carries no legal or political significance (similar t ...
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Baden-Württemberg
Baden-Württemberg ( ; ), commonly shortened to BW or BaWü, is a states of Germany, German state () in Southwest Germany, east of the Rhine, which forms the southern part of Germany's western border with France. With more than 11.07 million inhabitants across a total area of nearly , it is the third-largest German state by both List of German states by area, area (behind Bavaria and Lower Saxony) and List of German states by population, population (behind North Rhine-Westphalia and Bavaria). The List of cities in Baden-Württemberg by population, largest city in Baden-Württemberg is the state capital of Stuttgart, followed by Mannheim and Karlsruhe. Other major cities are Freiburg im Breisgau, Heidelberg, Heilbronn, Konstanz, Pforzheim, Reutlingen, Tübingen, and Ulm. Modern Baden-Württemberg includes the historical territories of Baden, Prussian Province of Hohenzollern, Hohenzollern, and Württemberg. Baden-Württemberg became a state of West Germany in April 1952 through ...
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Bad Urach
Bad Urach () is a town in the district of Reutlingen, Baden-Württemberg, Germany. It is situated 14 km east of Reutlingen, at the foot of the Swabian Jura (or Swabian Alps), and is known for its spa and therapeutic bath. Neighbouring communities The following towns border Urach and are also part of the district of Reutlingen. Clockwise from the north are: Hülben, Grabenstetten, Römerstein, Gutsbezirk Münsingen, Münsingen, St. Johann and Dettingen an der Erms. Bad Urach consists of the districts Hengen (687.01 ha; 854 inhabitants, on 31 December 2005), Seeburg (220.65 ha; 302 inhabitants), Sirchingen (481.78 ha; 1031 inhabitants), Bad Urach (2,797, 89 ha; 9289 inhabitants) and Wittlingen (1362.24 ha; 1112 inhabitants). With the exception of the district Bad Urach, the neighbourhoods form simultaneously villages within the meaning of the Baden-Wuerttemberg Municipal Code. Urach includes the homestead of Güterstein. Among the districts ofHengen and Sirchingen, e ...
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Karst Springs
A karst spring or karstic spring is a spring (exsurgence, outflow of groundwater) that is part of a karst hydrological system. Description Because of their often conical or inverted bowl shape, karst springs are also known in German-speaking lands as a ''Topf'' ("pot") which is reflected in names such as Aachtopf (the source of the Radolfzeller Aach) or Blautopf (the source of the Blau river in Blaubeuren). Karst springs often have a very high yield or discharge rate, because they are often fed by underground drainage from a large catchment basin. Because the springs are usually the terminus of a cave drainage system at the place where a river cave reaches the Earth's surface, it is often possible to enter the caves from karst springs for exploration. Large karst springs are located in many parts of the world; the largest ones are believed to be in Papua New Guinea, with others located in Mediterranean countries such as Bosnia and Herzegovina, Croatia, Turkey, Slovenia, ...
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Limestone
Limestone is a type of carbonate rock, carbonate sedimentary rock which is the main source of the material Lime (material), lime. It is composed mostly of the minerals calcite and aragonite, which are different Polymorphism (materials science), crystal forms of calcium carbonate . Limestone forms when these minerals Precipitation (chemistry), precipitate out of water containing dissolved calcium. This can take place through both biological and nonbiological processes, though biological processes, such as the accumulation of corals and shells in the sea, have likely been more important for the last 540 million years. Limestone often contains fossils which provide scientists with information on ancient environments and on the evolution of life. About 20% to 25% of sedimentary rock is carbonate rock, and most of this is limestone. The remaining carbonate rock is mostly Dolomite (rock), dolomite, a closely related rock, which contains a high percentage of the mineral Dolomite (mine ...
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Marl
Marl is an earthy material rich in carbonate minerals, Clay minerals, clays, and silt. When Lithification, 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 White cliffs of Dover, 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 mineral, carbonate-rich mud or mudstone which contains variable amounts of Clay minerals, 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 freshwa ...
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List Of Rivers Of Baden-Württemberg
A list of rivers of Baden-Württemberg, Germany: A *Aal (Kocher), Aal *Aalbach (Main), Aalbach *Aalenbach *Ablach (Danube), Ablach *Ach (Blau), Ach *Acher *Adelbach *Aich (river), Aich *Aid (Würm), Aid *Aischbach (Kinzig), Aischbach, tributary of the Kinzig *Aischbach (Körsch), Aischbach, tributary of the Körsch *Aitrach (Danube), Aitrach, tributary of the Danube *Aitrach (Iller), Aitrach, tributary of the Iller *Alb (Upper Rhine), Alb, tributary of the Rhine at Eggenstein-Leopoldshafen *Alb (High Rhine), Alb, tributary of the Rhine at Albbruck *Ammer (Neckar), Ammer *Amorsbach *Andelsbach *Annenbach *Arbach (Neckar), Arbach *Argen *Aschenbach (Mühlbach), Aschenbach *Aspenbach *Avenbach B *Badische Eschach *Bära *Bellamonter Rottum *Berneck (river), Berneck *Biber (Rhine), Biber *Biberbach (Danube), Biberbach *Bibers *Black Kocher *Black Lauter *Blau (Danube), Blau *Blinde Rot *Bollenbach (Argen), Bollenbach *Bottwar *Braunsel *Breg (river), Breg *Brehmbach *Breitenbach (Ech ...
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Rivers Of Baden-Württemberg
A river is a natural stream of fresh water that flows on land or inside caves towards another body of water at a lower elevation, such as an ocean, lake, or another river. A river may run dry before reaching the end of its course if it runs out of water, or only flow during certain seasons. Rivers are regulated by the water cycle, the processes by which water moves around the Earth. Water first enters rivers through precipitation, whether from rainfall, the runoff of water down a slope, the melting of glaciers or snow, or seepage from aquifers beneath the surface of the Earth. Rivers flow in channeled watercourses and merge in confluences to form drainage basins, or catchments, areas where surface water eventually flows to a common outlet. Rivers have a great effect on the landscape around them. They may regularly overflow their banks and flood the surrounding area, spreading nutrients to the surrounding area. Sediment or alluvium carried by rivers shapes the landscape ar ...
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