Rhine Falls
   HOME
*



picture info

Rhine Falls
The Rhine Falls (german: Rheinfall , a singular noun) is a waterfall located in Switzerland and the List of waterfalls by flow rate, most powerful waterfall in Europe. The falls are located on the High Rhine on the border between the cantons of Canton of Schaffhausen, Schaffhausen (SH) and Canton of Zürich, Zürich (ZH), between the municipalities of Neuhausen am Rheinfall (SH) and Laufen-Uhwiesen/Dachsen (ZH), next to the town of Schaffhausen in northern Switzerland. They are wide and high. In the winter months, the average water flow is , while in the summer, the average water flow is . The highest flow ever measured was more than 1250m3/s in 1999, previous to that the record was in 1965; and the lowest, in 1921. The falls cannot be climbed by fish, except by eels that are able to worm their way up over the rocks. Geology The Rhine Falls were formed in the Last glacial period, last ice age, approximately 14,000 to 17,000 years ago, by erosion-resistant rocks narrowing the ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  




Laufen Castle (Switzerland)
Laufen Castle (german: Schloss Laufen) is a castle in the municipality of Laufen-Uhwiesen in the Swiss canton of Zurich. It is a Swiss heritage site of national significance overlooking the Rhine Falls. The first documented reference to the castle dates to the year 858 when it was the home of the Barons of Laufen. It passed through several owners until the Old Zürich War (1439–1450) when the castle was acquired by the Fulach family, from whom the city of Zurich bought the castle in 1544. Following the Helvetic Republic (1798–1803) the castle was once again in private ownership, with the city of Zurich reacquiring the castle by buying it again in 1941. The castle now serves as a tourist attraction, and contains a restaurant and a youth hostel. Between 2009 and 2010 a project was undertaken to restore and expand the facilities, including a visitors’ centre situated in the former staff quarters, an exhibition in the northern part of the castle, and a wheelchair-accessible ci ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


picture info

Swiss Alpine Club
The Swiss Alpine Club (german: Schweizer Alpen-Club, french: Club Alpin Suisse, it, Club Alpino Svizzero, rm, Club Alpin Svizzer) is the largest mountaineering club in Switzerland. It was founded in 1863 in Olten and it is now composed of 111 sections with 160,000 members (2020). These include the Association of British Members of the Swiss Alpine Club. History The Swiss Alpine Club was the first Alpine club founded in continental Europe after the foundation of the Alpine Club (1857) in London. One of the founders and the first president of the Club was Dr. Melchior Ulrich; other members were Gottlieb Samuel Studer and Dr. Simler. The inaugural meeting was held in Olten. With the increasing number of climbers, steps had to be taken to make the approach to the mountains a little less complicated and exhausting. Until mountain huts were built, there had been no choice for the climbers other than sleeping in the highest chalets or in a Bivouac shelter under some overhanging ro ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


picture info

Electricity Generation
Electricity generation is the process of generating electric power from sources of primary energy. For electric utility, utilities in the electric power industry, it is the stage prior to its Electricity delivery, delivery (Electric power transmission, transmission, Electric power distribution, distribution, etc.) to end users or its Grid energy storage, storage (using, for example, the Pumped-storage hydroelectricity, pumped-storage method). Electricity is not freely available in nature, so it must be "produced" (that is, transforming other forms of energy to electricity). Production is carried out in power stations (also called "power plants"). Electricity is most often generated at a power plant by electromechanical electric generator, generators, primarily driven by heat engines fueled by combustion or nuclear fission but also by other means such as the kinetic energy of flowing water and wind. Other energy sources include solar photovoltaics and geothermal power. There are al ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


Neuhausen - Wassermühle Am Rheinfall
Neuhausen may refer to: *Neuhausen am Rheinfall, a town in the canton of Schaffhausen, Switzerland *Neuhausen railway station, a railway station in Switzerland *Neuhausen Rheinfall railway station, a railway station in Switzerland *Neuhausen Badischer Bahnhof, a railway station in Switzerland *Neuhausen auf den Fildern, a municipality in Baden-Württemberg, Germany *Neuhausen (Enz), a municipality in Baden-Württemberg, Germany *Neuhausen ob Eck, a municipality in Baden-Württemberg, Germany *Neuhausen/Spree, a municipality in Brandenburg, Germany *Neuhausen, Saxony, a municipality in the district of Freiberg in Saxony, Germany *Neuhausen, a borough of Worms, Germany *Neuhausen, a city in East Prussia, today Guryevsk, Kaliningrad Oblast *Danish name for the SIG Sauer P210 *Vastseliina Castle See also * Neuhaus (other) * Neuhausen-Nymphenburg Neuhausen (Central Bavarian: ''Neihausn'') and Nymphenburg are boroughs of Munich, the capital of the German state of Bavaria. They h ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


picture info

Iron Ore
Iron ores are rocks and minerals from which metallic iron can be economically extracted. The ores are usually rich in iron oxides and vary in color from dark grey, bright yellow, or deep purple to rusty red. The iron is usually found in the form of magnetite (, 72.4% Fe), hematite (, 69.9% Fe), goethite (, 62.9% Fe), limonite (, 55% Fe) or siderite (, 48.2% Fe). Ores containing very high quantities of hematite or magnetite (greater than about 60% iron) are known as "natural ore" or "direct shipping ore", meaning they can be fed directly into iron-making blast furnaces. Iron ore is the raw material used to make pig iron, which is one of the main raw materials to make steel—98% of the mined iron ore is used to make steel. In 2011 the ''Financial Times'' quoted Christopher LaFemina, mining analyst at Barclays Capital, saying that iron ore is "more integral to the global economy than any other commodity, except perhaps oil". Sources Metallic iron is virtually unknown on ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


picture info

Watermill
A watermill or water mill is a mill that uses hydropower. It is a structure that uses a water wheel or water turbine to drive a mechanical process such as milling (grinding), rolling, or hammering. Such processes are needed in the production of many material goods, including flour, lumber, paper, textiles, and many metal products. These watermills may comprise gristmills, sawmills, paper mills, textile mills, hammermills, trip hammering mills, rolling mills, wire drawing mills. One major way to classify watermills is by wheel orientation (vertical or horizontal), one powered by a vertical waterwheel through a gear mechanism, and the other equipped with a horizontal waterwheel without such a mechanism. The former type can be further divided, depending on where the water hits the wheel paddles, into undershot, overshot, breastshot and pitchback (backshot or reverse shot) waterwheel mills. Another way to classify water mills is by an essential trait about their location: tide mills ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


picture info

Museum Zu Allerheiligen
Kloster Allerheiligen (All Saints abbey) is a former Benedictine monastery in the Swiss municipality of Schaffhausen in the Canton of Schaffhausen. The church ''Münster Allerheiligen'' is the oldest building in Schaffhausen, and houses also the ''Museum zu Allerheiligen''. Geography Today the convent houses the Museum zu Allerheiligen, an art museum and a natural history museum, the monastery garden, and the buildings of the former convent, including the library. The former monastery's building complex is located at the center of the historic old city of the municipality of Schaffhausen in the Canton of Schaffhausen, includes the oldest buildings that still exist in Schaffhausen. History The development of the city of Schaffhausen is closely linked to the ''Nellenburg'' noble family who became extinct around 1100 AD. Various archaeological finds and the building of the present church of St. Johann (John) date back to around 1000 AD. The Earls (German: ''Grafen'') ''von Nell ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


picture info

Lake Constance
Lake Constance (german: Bodensee, ) refers to three Body of water, bodies of water on the Rhine at the northern foot of the Alps: Upper Lake Constance (''Obersee''), Lower Lake Constance (''Untersee''), and a connecting stretch of the Rhine, called the Seerhein, Lake Rhine (''Seerhein''). These waterbodies lie within the Lake Constance Basin () in the Alpine Foreland through which the Rhine flows. The lake is situated where Germany, Switzerland, and Austria meet. Its shorelines lie in the German states of Baden-Württemberg and Bavaria, the Swiss cantons of Canton of St. Gallen, St. Gallen, Canton of Thurgau, Thurgau, and Canton of Schaffhausen, Schaffhausen, and the Austrian state of Vorarlberg. The actual location of the border Lake_Constance#International_borders, is disputed. The Alpine Rhine forms in its original course the Austro-Swiss border and flows into the lake from the south. The High Rhine flows westbound out of the lake and forms (with the exception of the Canton ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


Late Jurassic
The Late Jurassic is the third epoch of the Jurassic Period, and it spans the geologic time from 163.5 ± 1.0 to 145.0 ± 0.8 million years ago (Ma), which is preserved in Upper Jurassic strata.Owen 1987. In European lithostratigraphy, the name "Malm" indicates rocks of Late Jurassic age. In the past, ''Malm'' was also used to indicate the unit of geological time, but this usage is now discouraged to make a clear distinction between lithostratigraphic and geochronologic/chronostratigraphic units. Subdivisions The Late Jurassic is divided into three ages, which correspond with the three (faunal) stages of Upper Jurassic rock: Paleogeography During the Late Jurassic Epoch, Pangaea broke up into two supercontinents, Laurasia to the north, and Gondwana to the south. The result of this break-up was the spawning of the Atlantic Ocean. However, at this time, the Atlantic Ocean was relatively narrow. Life forms of the epoch This epoch is well known for many famous types of dinosau ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  




Klettgau
Klettgau (High Alemannic: ''Chleggau'') is a municipality in the district of Waldshut in Baden-Württemberg, Germany. It is the centre of the ''Klettgau'' historical region stretching across the Swiss border into the cantons of Aargau, Schaffhausen and Zürich. The municipal area includes the villages of Bühl, Erzingen, Geißlingen, Grießen, Rechberg, Riedern am Sand, and Weisweil. Geography Klettgau is located on the Klingengraben and Schwarzbach creeks. In the east it borders on the Swiss municipalities of Trasadingen, Wilchingen and Wasterkingen. The neighbouring German municipalities are Wutöschingen, Lauchringen, Küssaberg, and Hohentengen am Hochrhein in the west, as well as Dettighofen in the east. There is a border crossing into Switzerland on the road from Erzingen to Trasadingen. The municipal area comprises the villages of Bühl, Erzingen, Geißlingen, Grießen, Rechberg, Riedern am Sand, and Weisweil. Erzingen, Bühl and Riedern am Sand are part of the Baden w ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


Wolstonian Stage
The Wolstonian Stage is a middle Pleistocene stage of the geological history of Earth from approximately 374,000 until 130,000 years ago. It precedes the Eemian Stage in Europe and follows the Hoxnian Stage in the British Isles. It is also approximately analogous to the Warthe and Saalian stages in northern Europe; the Riss glaciation in the Alps; and the Illinoian Stage in North America. It is equivalent to Marine isotope stages (MIS) 10 through 6. MIS 10, 8 and 6 were glacial periods and 9 and 7 were interglacials. It is named after Wolston in the English county of Warwickshire. Description The Wolstonian Stage is a middle Pleistocene stage of the geological history of Earth that precedes the Ipswichian Stage (Eemian Stage in Europe) and follows the Hoxnian Stage in the British Isles. The Wolstonian Stage apparently includes three periods of glaciation. The Wolstonian Stage is temporally analogous to the Warthe Stage and Saalian Stage in northern Europe and the Riss glaci ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]