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Hochrhein
The High Rhine (german: Hochrhein) is the name used for the part of the Rhine that flows westbound from Lake Constance to Basel. The High Rhine begins at the outflow of the Rhine from the Untersee in Stein am Rhein and turns into the Upper Rhine in Basel. In contrast to the Alpine Rhine and Upper Rhine, the High Rhine flows mostly to the west. The section is marked by Rhine-kilometers 0 to 165, measurements beginning at the outflow of the Obersee at the Old Rhine Bridge in Constance. It is the first of four sections (High Rhine, Upper Rhine, Middle Rhine, Lower Rhine) of the Rhine between Lake Constance and the North Sea. In the western part, the Rhine marks the border between Germany and Switzerland, while in the eastern part, Switzerland owns areas north of the Rhine and surrounds the popular German holiday resort of Büsingen am Hochrhein. The term ''High Rhine'' was introduced by scientists in the 19th century. Above all geologists tried to differentiate the High Rhine ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Büsingen Am Hochrhein
Büsingen am Hochrhein (, "Büsingen on the Upper Rhine"; Alemannic: ''Büesinge am Hochrhi''), commonly known as Büsingen, is a German municipality () in the south of Baden-Württemberg and an enclave entirely surrounded by the Swiss cantons of Schaffhausen, Zürich and Thurgau. It has a population of about 1,450 inhabitants. Since the early 19th century, the village has been separated from the rest of Germany by a narrow strip of land (at its narrowest, about wide) containing the Swiss village of Dörflingen. The distance to this enclave is approximately 5 km (3.1 mi) from the town of Schaffhausen and 3 km (1.8 mi) from Dörflingen, the nearest village. Politically Büsingen is part of Germany, forming part of the district of Konstanz, but economically it forms part of the Swiss customs union, along with the principality of Liechtenstein and up until 2019, albeit unofficially, the Italian village of Campione d'Italia. [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hochrhein Bei Rheinau
The High Rhine (german: Hochrhein) is the name used for the part of the Rhine that flows westbound from Lake Constance to Basel. The High Rhine begins at the outflow of the Rhine from the Untersee in Stein am Rhein and turns into the Upper Rhine in Basel. In contrast to the Alpine Rhine and Upper Rhine, the High Rhine flows mostly to the west. The section is marked by Rhine-kilometers 0 to 165, measurements beginning at the outflow of the Obersee at the Old Rhine Bridge in Constance. It is the first of four sections (High Rhine, Upper Rhine, Middle Rhine, Lower Rhine) of the Rhine between Lake Constance and the North Sea. In the western part, the Rhine marks the border between Germany and Switzerland, while in the eastern part, Switzerland owns areas north of the Rhine and surrounds the popular German holiday resort of Büsingen am Hochrhein. The term ''High Rhine'' was introduced by scientists in the 19th century. Above all geologists tried to differentiate the High Rhine () ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rhine
), Surselva, Graubünden, Switzerland , source1_coordinates= , source1_elevation = , source2 = Rein Posteriur/Hinterrhein , source2_location = Paradies Glacier, Graubünden, Switzerland , source2_coordinates= , source2_elevation = , source_confluence = Reichenau , source_confluence_location = Tamins, Graubünden, Switzerland , source_confluence_coordinates= , source_confluence_elevation = , mouth = North Sea , mouth_location = Netherlands , mouth_coordinates = , mouth_elevation = , progression = , river_system = , basin_size = , tributaries_left = , tributaries_right = , custom_label = , custom_data = , extra = The Rhine ; french: Rhin ; nl, Rijn ; wa, Rén ; li, Rien; rm, label= Sursilvan, Rein, rm, label= Sutsilvan and Surmiran, Ragn, rm, label=Rumantsch Grischun, Vallader and Puter, Rain; it, Reno ; gsw, Rhi(n), inclu ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Diessenhofen
Diessenhofen is a village and a municipality in Frauenfeld District in the canton of Thurgau in Switzerland. The village is situated on the south shore of the High Rhine just opposite the German town of Gailingen am Hochrhein. History Diessenhofen is first mentioned in 757 as ''Deozincova''. In 2000, the village of Willisdorf was incorporated into the municipality. The earliest traces of a settlement are Stone and Bronze Age scattered objects found in the shallow valleys of the district and on the banks of the Rhine. A hoard of coins from the Roman era (251-270), and the remains of three towers of the Danube-Iller-Rhein limes (4th century) show Roman settlements in the area. The reference in a deed of the Abbey of St. Gall from 757 mention an Alamanni village, which was probably on the plateau south of the church. In 1178 Count Hartmann III of Kyburg, raised the village to town and probably appointed a Ministerialis (unfree knights in the service of a feudal overlord) family as t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Schaffhausen
Schaffhausen (; gsw, Schafuuse; french: Schaffhouse; it, Sciaffusa; rm, Schaffusa; en, Shaffhouse) is a list of towns in Switzerland, town with historic roots, a municipalities of Switzerland, municipality in northern Switzerland, and the capital of the canton of Schaffhausen, canton of the same name; it has an estimated population of 36,000 It is located right next to the shore of the High Rhine; it is one of four Swiss towns located on the northern side of the Rhine, along with , the historic , and . The old town has many fine Renaissance era buildings decorated with exterior frescos and sculpture, as well as the old canton fortress, the ''Munot''. Schaffhausen is also a railway junction of Swiss and German rail networks. One of the lines connects the town with the nearby Rhine Falls in , Europe's largest waterfall, a tourist attraction. The official language of Schaffhausen is (the Swiss variety of Standard) Swiss Standard German, German, but the main spoken language ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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] |
Laufenburg (Baden)
Laufenburg is a town in Baden-Württemberg, Germany, part of the Waldshut district. It has approximately 4300 inhabitants (including 6 outskirts 8300 inhabitants). Laufenburg is separated from a Swiss city with the same name by the river Rhine. Cities in the near vicinity *Near surrounding (15 km): Lörrach, Basel, Brugg, Aarau, Zürich, Schaffhausen, St. Blasien, Todtmoos, Freiburg City administration The city of Laufenburg encompasses also Binzgen, Grunholz, Hauenstein, Hochsal, Luttingen, Rhina, Rotzel, Stadenhausen. Brief history The city was first noted in 1207. In November 1638 one side of the city was taken by Imperialist forces. The bridge across the Rhine was burned afterwards. Laufenburg was one city until about 1800 when Napoleon divided the city, ordering that the Rhine should become the border. Ever since the two cities have been separated by nationality. The city was well placed on major rapids of the Rhine, which allowed the town to collect taxes as ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sea Level
Mean sea level (MSL, often shortened to sea level) is an average surface level of one or more among Earth's coastal bodies of water from which heights such as elevation may be measured. The global MSL is a type of vertical datuma standardised geodetic datumthat is used, for example, as a chart datum in cartography and marine navigation, or, in aviation, as the standard sea level at which atmospheric pressure is measured to calibrate altitude and, consequently, aircraft flight levels. A common and relatively straightforward mean sea-level standard is instead the midpoint between a mean low and mean high tide at a particular location. Sea levels can be affected by many factors and are known to have varied greatly over geological time scales. Current sea level rise is mainly caused by human-induced climate change. When temperatures rise, Glacier, mountain glaciers and the Ice sheet, polar ice caps melt, increasing the amount of water in water bodies. Because most of human settlem ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Laufen-Uhwiesen
Laufen-Uhwiesen is a municipality in the district of Andelfingen in the canton of Zürich in Switzerland. History Laufen-Uhwiesen is first mentioned in 858 as ''ad Laufin''. In 1290 it was mentioned as ''ze Uwisan''. Geography Laufen-Uhwiesen has an area of . Of this area, 40.1% is used for agricultural purposes, while 44.4% is forested. Of the rest of the land, 11.7% is settled (buildings or roads) and the remainder (3.8%) is non-productive (rivers, glaciers or mountains). The municipality is located on the edge of the Schaffhausen Agglomeration, though it is in the canton of Zürich. It includes the village of Uhwiesen, which is located on a terrace of the Cholfirst elevation, the village of Laufen with Laufen Castle on the Rhine Falls, and the hamlet of Nohl on the right bank of the Rhine. Until 1840, it was part of the municipality of Flurlingen. Demographics Laufen-Uhwiesen has a population (as of ) of . , 9.3% of the population was made up of foreign nationals. Over t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Würm Glaciation
The Würm glaciation or Würm stage (german: Würm-Kaltzeit or ''Würm-Glazial'', colloquially often also ''Würmeiszeit'' or ''Würmzeit''; cf. ice age), usually referred to in the literature as the Würm (often spelled "Wurm"), was the last glacial period in the Alpine region. It is the youngest of the major glaciations of the region that extended beyond the Alps themselves. Like most of the other ice ages of the Pleistocene epoch, it is named after a river, in this case the Würm in Bavaria, a tributary of the Amper. The Würm ice age can be dated to about 115,000 to 11,700 years ago, but sources differ about the dates, depending on whether the long transition phases between the glacials and interglacials (warmer periods) are allocated to one or other of those periods. The average annual temperatures during the Würm ice age in the Alpine Foreland were below −3 °C (today +7 °C). That has been determined from changes in the vegetation (pollen analysis), as well a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ice Age
An ice age is a long period of reduction in the temperature of Earth's surface and atmosphere, resulting in the presence or expansion of continental and polar ice sheets and alpine glaciers. Earth's climate alternates between ice ages and greenhouse periods, during which there are no glaciers on the planet. Earth is currently in the Quaternary glaciation. Individual pulses of cold climate within an ice age are termed ''glacial periods'' (or, alternatively, ''glacials, glaciations, glacial stages, stadials, stades'', or colloquially, ''ice ages''), and intermittent warm periods within an ice age are called '' interglacials'' or ''interstadials''. In glaciology, ''ice age'' implies the presence of extensive ice sheets in both northern and southern hemispheres. By this definition, Earth is currently in an interglacial period—the Holocene. The amount of anthropogenic greenhouse gases emitted into Earth's oceans and atmosphere is predicted to prevent the next glacial period for th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
