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Rheinfall Seilpark 4
The Rhine Falls ( / Swiss German: , a singular noun) is a waterfall on the High Rhine in Switzerland. It is the most powerful waterfall in Europe and a popular tourist attraction. The falls are located on the border between the cantons of Schaffhausen (SH) and Zurich (ZH), between the municipalities of Neuhausen am Rheinfall (SH) and Laufen-Uhwiesen/Dachsen (ZH), ca. south of the town of Schaffhausen and close to the border with Germany. The falls 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 in 1965, and the lowest, in 1921. Geology The Rhine Falls were formed during the last ice age, approximately 14,000 to 17,000 years ago, by erosion-resistant rocks narrowing the riverbed. The first glacial advances created today's landforms approximately 500,000 years ago. Up to the end of the Wolstonian Stage, approximately 132,000 years ago, the Rhine flowed westwards ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Laufen Castle (Switzerland)
Laufen Castle () 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 Zurich 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 circular walkway wi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Neuhausen Am Rheinfall
Neuhausen am Rheinfall (sometimes abbreviated as Neuhausen a. Rhf., called Neuhausen until 1938) is a town and a municipality in the canton of Schaffhausen in Switzerland. The town is close to the Rhine Falls (), mainland Europe's largest waterfall. History Neuhausen am Rheinfall was first mentioned in 900/910 as ''Niuhusen''. In 1253 it was mentioned as ''Niuwenhusin''. Coat of arms The German blazon reads: ''In gelb über grünem Kleeblatt weisses nach rechts gekehrtes Rebmesser mit braunem Griff.'' The municipality's arms might in English heraldic language be described thus: Or in base a cloverleaf couped proper above which a billhook argent hafted proper. In 1569, Neuhausen bore arms with a gold field and a leaping silver salmon. This symbolized the importance of fishing to the municipality. Shortly thereafter, the arms appeared with different tinctures; the field was now red. With the lessening importance of fishing, the arms, too, presumably ended up being forgotten, for ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Late Jurassic
The Late Jurassic is the third Epoch (geology), epoch of the Jurassic Period, and it spans the geologic time scale, geologic time from 161.5 ± 1.0 to 143.1 ± 0.8 million years ago (Ma), which is preserved in Upper Jurassic stratum, 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 emergence of the Atlantic Ocean, which initially was relatively narrow. Life forms This epoch is well known for many famous types of d ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gravel
Gravel () is a loose aggregation of rock fragments. Gravel occurs naturally on Earth as a result of sedimentation, sedimentary and erosion, erosive geological processes; it is also produced in large quantities commercially as crushed stone. Gravel is classified by grain size, particle size range and includes size classes from granule (geology), granule- to boulder-sized fragments. In the grain size, Udden-Wentworth scale gravel is categorized into granular gravel () and pebble gravel (). ISO 14688 grades gravels as fine, medium, and coarse, with ranges for fine and for coarse. One cubic metre of gravel typically weighs about , or one cubic yard weighs about . Gravel is an important commercial product, with a number of applications. Almost half of all gravel production is used as construction aggregate, aggregate for concrete. Much of the rest is used for road construction, either in the road base or as the road surface (with or without bitumen, asphalt or other binders.) Natu ... [...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 center 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 rivers. In the east, it borders 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 B ... [...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 Last Interglacial (also called the Eemian Stage) 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. The colder last part from around 194,000 years ago is called the Penultimate Glacial Period. 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 glac ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Glacial
A glacier (; or ) is a persistent body of dense ice, a form of rock, that is constantly moving downhill under its own weight. A glacier forms where the accumulation of snow exceeds its ablation over many years, often centuries. It acquires distinguishing features, such as crevasses and seracs, as it slowly flows and deforms under stresses induced by its weight. As it moves, it abrades rock and debris from its substrate to create landforms such as cirques, moraines, or fjords. Although a glacier may flow into a body of water, it forms only on land“Glacier, N., Pronunciation.” Oxford English Dictionary, Oxford UP, June 2024, https://doi.org/10.1093/OED/7553486115. Accessed 25 Jan. 2025. and is distinct from the much thinner sea ice and lake ice that form on the surface of bodies of water. On Earth, 99% of glacial ice is contained within vast ice sheets (also known as "continental glaciers") in the polar regions, but glaciers may be found in mountain ranges on every co ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Erosion
Erosion is the action of surface processes (such as Surface runoff, water flow or wind) that removes soil, Rock (geology), rock, or dissolved material from one location on the Earth's crust#Crust, Earth's crust and then sediment transport, transports it to another location where it is deposit (geology), deposited. Erosion is distinct from weathering which involves no movement. Removal of rock or soil as clastic sediment is referred to as ''physical'' or ''mechanical'' erosion; this contrasts with ''chemical'' erosion, where soil or rock material is removed from an area by Solvation, dissolution. Eroded sediment or solutes may be transported just a few millimetres, or for thousands of kilometres. Agents of erosion include rainfall; bedrock wear in rivers; coastal erosion by the sea and Wind wave, waves; glacier, glacial Plucking (glaciation), plucking, Abrasion (geology), abrasion, and scour; areal flooding; Aeolian processes, wind abrasion; groundwater processes; and Mass wastin ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rheinfall - Neuhausen Am Rheinfall 2010-06-24 19-17-28
The Rhine Falls ( / Swiss German: , a singular noun) is a waterfall on the High Rhine in Switzerland. It is the List of waterfalls by flow rate, most powerful waterfall in Europe and a popular Tourism in Switzerland, tourist attraction. The falls are located on the border between the Cantons of Switzerland, cantons of Canton of Schaffhausen, Schaffhausen (SH) and Canton of Zurich, Zurich (ZH), between the Municipalities of Switzerland, municipalities of Neuhausen am Rheinfall (SH) and Laufen-Uhwiesen/Dachsen (ZH), ca. south of the town of Schaffhausen and close to the Germany–Switzerland border, border with Germany. The falls 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 in 1965, and the lowest, in 1921. Geology The Rhine Falls were formed during the Last glacial period, last ice age, approximately 14,000 to 17,000 years ago, by erosion-resistant rocks narrowi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
