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Sihlbühl
The Lindenhof (''"Tilia, linden yard"'') is a moraine hill and public square in the historic center of Zurich, Switzerland. It is the site of the Switzerland in the Roman era, Roman and Carolingian era Kaiserpfalz around which the city has historically grown. The hilltop area—including its prehistoric, Roman, and medieval remains—is listed as a Swiss inventory of cultural property of national and regional significance, Swiss heritage site of national significance. Topography Lindenhof (its northern part is called ''Sihlbühl'') dominates the Lindenhof (quarter), Lindenhof quarter in Altstadt (Zurich), district 1 (Altstadt), the historical center of Zurich's Altstadt. To the north, it bordered by Uraniastrasse and the Waisenhaus Zürich, Waisenhaus and to the south, it ends near St. Peter, Zurich, St. Peter church. To the west, the hill is bordered by Bahnhofstrasse, and in the east, it ends at the Limmat and the Schipfe quarter. Lindenhof sits atop the remains of a glacier ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Schipfe
Schipfe is a residential district in Zurich, Switzerland, located on the eastern slope of the Lindenhof, one of the oldest parts of the Helvetii Oppidum Zurich-Lindenhof, by the river Limmat. Historians and the '' Weinplatz'' suggest that the district was part of the former civilian harbour of the Celtic-Roman ''Turicum''. Location Schipfe belongs to the historic area on the left hand shore of the Limmat, located on the west side of the Lindenhof-Sihlbühl hill downstream from the ancient bridges Münsterbrücke and Rathausbrücke, Zurich between the present Limmatquai and the prehistoric Lindenhof hill. History The Lindenhof was the site of the Helvetii ''Oppidum'' and the first century BC Roman settlement (15 BC), with traces of a hypocaustum excavated between Weinplatz and Münsterhof. It was then the historical core of modern Zurich. This is the oldest area of the city, with settlements dating to the pre-Roman La Tène culture, and fortified as ''oppidum'' with a s ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Waisenhaus Zürich
The Waisenhaus (), or Amthaus I, is the last remaining building of the Oetenbach nunnery in Zurich, Switzerland, and today houses the city police department. Location The ''Waisenhaus'' building is situated at Bahnhofquai 3 near Bahnhofbrücke and Zürich Hauptbahnhof. Built outside of the historical core of the medieval town of Zurich, previously the Celtic-Roman ''Turicum'', the former ''Zucht- und Waisenhaus'' ("penitentiary and orphanage") is the last remaining structure of the Oetenbach nunnery at the ''Lindenhof-Silhlbühl'' hill on the western shore of the Limmat river. History After the Reformation in Zurich, the city government took over the monastic buildings for new uses. To manage the income of the former convent, the former administration building was held as ''Oetenbacheramt'' housing the former wine cellar. In 1601 the building was extensively remodeled and equipped with stepped gables, and as police barracks, in 1872 the remains of wall paintings were ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Glacier
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 ever ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bauschänzli
Bauschänzli is an artificial island, town square, and public park in Zürich, Switzerland. Bauschänzli (diminutive of "construction entrenchment") is one of the last remains of the Baroque fortifications of Zürich which began in 1642. The neighboring Schanzengraben (moat) and the Old Botanical Garden, Zürich, Old Botanical Garden are part of these remains. Since 1907, the island has been used as a restaurant, although it is officially a public square and park. Geography Bauschänzli is situated in the historical ''Alpenquai'' district on the artificial island. It is on the western shore of Limmat, off Bürkliplatz at the ''Stadthausquai'' road and opposite Bellevueplatz. A tiny public park can be found here. Points of interests In addition to the Quaianlagen (Zürich), Seeuferanlage and its neighboring Utoquai, Uto and General-Guisan-Quai, General Guisan quays, the Arboretum Zürich, Zürich Arboretum and the Voliere Zürich, Zürich Aviary are nearby. The aviary houses ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sechseläutenplatz
Sechseläutenplatz (literally: ''Sechseläuten'' square) is the largest town square situated in Zurich, Switzerland. Its name derives from the '' Sechseläuten'' (the city's traditional spring holiday), which is celebrated on the square in April. Geography Sechseläutenplatz is located on the east shore of Lake Zurich, just south of the lake's outflow to the river Limmat and the Schanzengraben moat. The plaza is bounded to the south by the linked Opernhaus and Bernhardtheater buildings; to the west by the Utoquai lakeside promenade; and to the east by Theaterstrasse, across which is Stadelhoferplatz, with the Stadelhofen railway station and the terminus of the Forchbahn (FOB). To the north, Sechseläutenplatz merges into ''Bellevueplatz'', where stops for the Zurich tram lines 2, 4, 5, 8, 9, 11 and 15 are located. On November 30, 2011, the government of Zurich announced that some streets would be renamed by redesigning the public area at Sechseläutenplatz. Theaterpla ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Grosser Hafner
Grossner Hafner is one of the 111 serial sites of the UNESCO World Heritage Site '' Prehistoric pile dwellings around the Alps'', of which are 56 located in Switzerland. Geography Grosser Hafner was located on the then swamp area between the Limmat and Zürichsee around Sechseläutenplatz on a small lake island in Zürich, and as well as the other Prehistoric pile dwellings around Zürichsee set on piles to protect against occasional flooding by the Linth and Jona. The settlement is located on Lake Zurich in Enge, a locality of the municipality of Zürich. It was neighbored by the settlements Zürich–Enge Alpenquai and Kleiner Hafner on a then island in the effluence of the Limmat, within an area of about in the city of Zürich. Grosser and Kleiner Hafner comprise , and the buffer zone including the lake area comprises in all. History Internationally known is the area since 2009, as in the beginning of the construction of the underground parking facility at Sechs ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kleiner Hafner
Kleiner Hafner is one of the 111 serial sites of the UNESCO World Heritage Site '' Prehistoric pile dwellings around the Alps'', of which are 56 located in Switzerland. Geography Kleiner Hafner was located on the then swamp land between the river Limmat and Zürichsee around Sechseläutzenplatz on a small peninsula in Zürich, and as well as the other Prehistoric pile dwellings around Zürichsee set on piles to protect against occasional flooding by the rivers Linth and Jona. The settlement is located on '' Zürichsee'' lakeshore in Enge, a locality of the municipality of Zürich. It was neighbored by the settlements Zürich–Enge Alpenquai and Grosser Hafner on a then island in the effluence of the Limmat, within an area of about in the city of Zürich. The site Kleiner Hafner comprises , and the buffer zone including the lake area comprises . History The site is internationally known since 2009, when during the beginning of the construction of the underground parki ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Prehistoric Pile Dwellings Around Lake Zurich
Prehistoric pile dwellings around Lake Zurich are Stilt house, pile dwelling sites located around Lake Zurich in the Cantons of Switzerland, cantons of Canton of Schwyz, Schwyz, Canton of St. Gallen, St. Gallen and Canton of Zurich, Zurich. The article focuses on the 9 Lake Zurich sites that are among the 111 sites included in the UNESCO World Heritage Prehistoric pile dwellings around the Alps established in 2011. 56 of the 111 UNESCO World Heritage pile dwelling sites are located in Switzerland and 9 thereof are located on the Lake Zurich seashore. The article also includes one UNESCO World Heritage site at the nearby Greifensee (lake), Greifensee and one UNESCO World Heritage site at the Pfäffikersee. The 11 sites described here are only a selection, just like the 111 UNESCO World Heritage sites are only a selection of more than 900 known sites of prehistoric pile dwellings in the Alpine region. Geography The 11 prehistoric pile-dwelling (or stilt house) sites are concentr ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lake Zurich
Lake Zurich (, ; ) is a lake in Switzerland, extending southeast of the city of Zurich. Depending on the context, Lake Zurich or can be used to describe the lake as a whole, or just that part of the lake downstream of the Hurden peninsula and Seedamm causeway (between Pfäffikon and Rapperswil). In the latter case, the upstream part of the lake is called '' Obersee'' (), while the lower part is sometimes also referred to as the Lower Lake (), respectively. Geography Lake Zurich is a glacial lake that was formed by the . Its main tributary is the River Linth, which rises in the glaciers of the Glarus Alps. The Linth originally flew directly into Lake Zurich, but was later diverted by the Escher canal (completed in 1811) into Lake Walen () from where its waters are now carried to the east end of Lake Zurich (near Schmerikon) by means of the straightened Linth canal (completed in 1816). Until the early 16th century, there was another lake upstream of ''Obersee'', Lake Tug ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
