Läuferbrunnen
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Läuferbrunnen
The Läuferbrunnen (Runner Fountain) is a fountain on Läuferplatz in the Old City of Bern, Switzerland. It is a Swiss Cultural Property of National Significance and is part of the UNESCO World Heritage Site of the Old City of Bern. History It is located near the Nydegg Church on ''Nydeggstalden''. The trough was built in 1824, but the figure dates from 1545. The Runner has moved several times since its creation, and until about 1663 was known as the ''Brunnen beim unteren Tor'' (Fountain by the lower gate). Originally the ''Läuferbrunnen'' had an octagonal trough and a tall, round column. The trough was replaced with a rectangular trough before 1757 which was replaced in 1824. The round column was replaced with the current square limestone Limestone ( calcium carbonate ) is a type of carbonate sedimentary rock which is the main source of the material lime. It is composed mostly of the minerals calcite and aragonite, which are different crystal forms of . Limesto ...
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Old City Of Bern
The Old City (german: Altstadt) is the medieval city center of Bern, Switzerland. Built on a narrow hill bordered on three sides by the river Aare, its compact layout has remained essentially unchanged since its construction during the twelfth to the fifteenth century. Despite a major fire in 1405, after which much of the city was rebuilt in sandstone, and substantial construction efforts in the eighteenth century, Bern's old city has retained its medieval character. The Old City is home to Switzerland's tallest minster as well as other churches, bridges and a large collection of Renaissance fountains. In addition to many historical buildings, the seats of the Swiss federal government, federal, Canton of Bern, cantonal and municipal government are also situated in the Old City. It is a UNESCO Cultural World Heritage Site since 1983 due to the compact and generally intact medieval core and is an excellent example of incorporating the modern world into a medieval city. Numerous bu ...
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Bern
german: Berner(in)french: Bernois(e) it, bernese , neighboring_municipalities = Bremgarten bei Bern, Frauenkappelen, Ittigen, Kirchlindach, Köniz, Mühleberg, Muri bei Bern, Neuenegg, Ostermundigen, Wohlen bei Bern, Zollikofen , website = www.bern.ch Bern () or Berne; in other Swiss languages, gsw, Bärn ; frp, Bèrna ; it, Berna ; rm, Berna is the ''de facto'' capital of Switzerland, referred to as the "federal city" (in german: Bundesstadt, link=no, french: ville fédérale, link=no, it, città federale, link=no, and rm, citad federala, link=no). According to the Swiss constitution, the Swiss Confederation intentionally has no "capital", but Bern has governmental institutions such as the Federal Assembly and Federal Council. However, the Federal Supreme Court is in Lausanne, the Federal Criminal Court is in Bellinzona and the Federal Administrative Court and the Federal Patent Court are in St. Gallen, exemplifying the federal nature of the Confederation. ...
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World Heritage Site
A World Heritage Site is a landmark or area with legal protection by an international convention administered by the United Nations Educational, Scientific and Cultural Organization (UNESCO). World Heritage Sites are designated by UNESCO for having cultural, historical, scientific or other form of significance. The sites are judged to contain " cultural and natural heritage around the world considered to be of outstanding value to humanity". To be selected, a World Heritage Site must be a somehow unique landmark which is geographically and historically identifiable and has special cultural or physical significance. For example, World Heritage Sites might be ancient ruins or historical structures, buildings, cities, deserts, forests, islands, lakes, monuments, mountains, or wilderness areas. A World Heritage Site may signify a remarkable accomplishment of humanity, and serve as evidence of our intellectual history on the planet, or it might be a place of great natural beauty. A ...
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Nydeggkirche
The Reformed Nydeggkirche (from the Bernese German expression for "Lower corner") is located on the eastern edge of the Old City of Bern, in the Nydegg section. The castle Nydegg The old town is situated on a peninsula in a loop of the Aare and developed in several expansion stages. The first occurred in 1191, as an existing settlement was expanded in the area of Nydeggkirche to the Clock Tower (Zytglogge). In 1190 Duke Berchtold V von Zähringen had built the castle Nydegg. After the extinction of the House of Zähringen, it came under the control of the city and was razed in 1266-73 by the inhabitants of Bern, in order to develop the Nydegg section. It possessed four corner towers and was located about where the current choir of the church stands. The Church The original small church was built from 1341 to 1346 to replace the old fortress. It was first sanctified in March 1344, followed by a second on 23 May 1346. This early church featured a bell tower. On 12 January ...
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Nydegg
The Nydegg is a historic section in the Old City of Bern in Bern, Switzerland. The first expansion of Bern occurred as the city was founded in 1191. At the east end of the central and oldest neighbourhood, the ''Zähringerstadt'' ( Zähringer town), was the Nydegg castle near the banks of the Aare river. The houses that grew up around the castle were the start of the Nydegg section. Around 1268 Nydegg Castle was destroyed, and the city expanded into the area formerly occupied by the castle. Situated in the northeast of the Aare peninsula, the ''Nydegg'' together with the ''Mattequartier'' in the southwest constituted medieval Bern's smallest neighbourhood. Workshops and mercantile activity prevailed in this area, and medieval sources tell of numerous complaints about the ceaseless and apparently nerve-wracking noise of machinery, carts and commerce. The Matte area at the riverside features three artificial channels, through which Aare water was diverted to power three city ...
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Limestone
Limestone ( calcium carbonate ) is a type of carbonate sedimentary rock which is the main source of the material lime. It is composed mostly of the minerals calcite and aragonite, which are different crystal forms of . Limestone forms when these minerals 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, a closely related rock, which contains a high percentage of the mineral dolomite, . ''Magnesian limestone'' is an obsolete and poorly-defined term used variously for dolomite, for limes ...
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