Schanzengraben is a moat and a section of the northwestern extension of the Seeuferanlage promenades that were built between 1881 and 1887 in Zurich , Switzerland. Schanzengraben is, among the adjoint Katz bastion at the Old Botanical Garden and the so-called Bauschänzli bulwark, one of the last remains of the Baroque fortifications of Zürich. The area of the moat is also an inner-city recreation area and a public park.
32-638: Schanzengraben is one of the two present effluences of the Lake Zurich , located around 250 metres (820 ft) south of the Limmat , and situated at the historical Alpenquai lake shore area, between Bürkliplatz and General-Guisan-Quai . It marks the border of the inner-city districts of Enge and City , and flows after about 1,150 metres (3,773 ft) into the Sihl , at the western side of Zürich Hauptbahnhof where Gessnerallee and Usteristrasse cross
64-512: A concession on an issue of water rights concession and a water protection legal permit for the installation of a water wheel purpose of power generation in the Schanzengraben moat. According to the application, at the weir near the indoor aquatic centre City estimated 3,000 liters/second drop a height of 75 centimetres (30 in) and could supply electricity for about 20 households. The moat system of medieval Zurich, consisting of
96-467: A house is mentioned in 1346, and in 1537 the area of the outer trench was named Sprachhüsli , meaning a public toilet. Over the decades, the time accumulating sludge was periodically dug out by day laborers or in forced labor to process. The excavation was used to fertilize the fields of the Oetenbach nunnery . Due to its former military defensive use, the moat has a widely octagonal zig-zag form, and
128-533: Is a lake in Switzerland , extending southeast of the city of Zurich . Depending on the context, Lake Zurich or Zürichsee 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 ( lit. ' Upper Lake ' ), whilst
160-830: Is a rare and spectacular event. The lake was frozen in the following Common Era / Anno Domini years (1963 was the last time): Lake Zurich's water is very clean and reaches, during summer, temperatures well beyond 20 °C (68 °F). Swimming in the public baths and beaches is very popular. The lake's water is purified and fed into Zurich's water system; it is potable. Swiss inventory of cultural property of national and regional significance The Swiss Inventory of Cultural Property of National and Regional Significance ( German : Schweizerisches Inventar der Kulturgüter von nationaler und regionaler Bedeutung ; French : Inventaire suisse des biens culturels d'importance nationale et régionale ; Italian : Inventario dei beni culturali svizzeri d'importanza nazionale e regionale )
192-837: Is a register of cultural property in Switzerland . It was established according to article 5 of the second protocol to the Hague Convention for the Protection of Cultural Property in the Event of Armed Conflict , which provides for the establishment of national registers of cultural property. The register contains both mobile and immobile items of cultural property including old towns, quarters, squares, villages, sacral buildings, houses, castles, bridges, monuments, archaeological sites and collections. Its entries are classified in two groups: those of national significance (class A) and those of regional significance (class B). The selection
224-600: Is also listed as a Class object in the Swiss inventory of cultural property of national and regional significance . In Kempraten ( Rapperswil-Jona municipality), there was a Roman vicus named Centum Prata . Another settlement was Turicum in Zurich. The main transportation nodes around the lake are Zurich and — given the presence of the Seedamm causeway — Pfäffikon and Rapperswil . Besides Quaibrücke in Zurich and
256-478: Is based on the significance of the items in the domains of history , aesthetics , art , typology , ethnography , social studies and in other scientific disciplines, as well as on their rarity value. Items of purely local significance are not included; these may be registered separately by the cantonal authorities. The register is prepared by the Federal Office of Civil Protection in cooperation with
288-678: Is the Au peninsula at the village of Au between Wädenswil and Horgen . The lake shores are well cultivated and fertile. They include nature reserves , such as Frauenwinkel or Bätzimatt . The bay of Rapperswil and reed in Nuolen are wintering areas for birds and popular sites for bird watching . To the east, separated by Zürichberg - Adlisberg , Forch , and Pfannenstiel , are two smaller lakes, Greifensee ( lit. ' Lake Greifen ' ) and Pfäffikersee ( lit. ' Lake Pfäffikon ' ). There are several minor lakes and ponds in
320-694: The Gessner bridge. In fact, the moat was built outside of the historical core of the medieval town of Zürich, previously the Celtic-Roman Turicum , an area being then called Aussersihl , meaning that it was outside of the Baroque town wall at the Sihl river delta . The lake shore area also serves as a marina associated to the Hafen Enge . A narrow alley was partially built at the level of
352-706: The Limmat . The Limmat is a tributary of the Aare , which itself is a tributary of the High Rhine . The culminating point of the lake's drainage basin is the Tödi at 3,614 metres above sea level. Besides the River Linth, other tributaries are the Jona , Schmerikoner Aa , Steinenbach and Wägitaler Aa , which all flow out into Obersee , along with several creeks. The Seedamm , an artificial causeway and bridge, crosses
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#1732780666956384-523: The Old Botanical Garden and its arboretum. There is also a unique public bath just for men ( Männerbad ) that also serves as an event restaurant. That section of the moat is also used as a ground for canoeing and a 'water stadion' for canoe waterball. Probably the most natural part is situated nearby the mouth into the Sihl, where also some waterbirds and even fish found an inner-city refugium. As of December 2015, an association asked for
416-604: The cantons of Schwyz , St. Gallen and Zurich , are among the 56 Prehistoric pile dwellings around the Alps in Switzerland. These nine sites on the Lake Zurich lakeshore are Freienbach–Hurden Rosshorn , Freienbach–Hurden Seefeld , Rapperswil-Jona/Hombrechtikon–Feldbach , Rapperswil-Jona–Technikum , Erlenbach–Winkel , Meilen–Rorenhaab , Wädenswil–Vorder Au , Zurich–Enge Alpenquai , and Kleiner Hafner . Because
448-742: The Seedamm, there are no bridges across the lake. In addition, the towns of Meilen and Horgen are connected by a car ferry . Bus routes on the western shore are operated by Zimmerberg Bus . On the eastern side, the VZO provides bus services along the lake shore and to the Zürcher Oberland . VZO also operates the urban bus routes in Rapperswil and Jona . At the northern end of the lake, in Zurich, public transport consists of trams , trolleybuses and busses of VBZ . Left bank : The towns on
480-739: The Voralpen Express. This short line connects Rapperswil with Pfäffikon SZ via Hurden . The Zürichsee-Schifffahrtsgesellschaft – lit. ' the Lake Zurich Navigation Company ' – provides with its 17-passenger ships touristic services on Lake Zurich. There are a number of passenger ferry services, notably the Horgen–Meilen ferry , an auto ferry between Horgen and Meilen . The freezing of Lake Zurich, called Seegfrörni in Swiss German ,
512-535: The canton of Zurich, and Rapperswil-Jona . The latter includes the medieval town of Rapperswil , whose castle is home to the Polish museum , and the coastal villages of Kempraten , Busskirch and Bollingen . The municipalities of Rapperswil-Jona and Schmerikon , which is close to the east end of the lake, are both in the canton of St. Gallen . A little further east is the larger town of Uznach . Nine Prehistoric pile dwellings around Zürichsee , which are located in
544-619: The cantonal authorities and formally issued by the Federal Council . It was first published in 1988 and re-issued in updated form in 1995 and 2009. The 2009 revision covers only A-class objects, with the B-class objects set to be reviewed and updated at a later time. Until then, the lists of B-class objects published by the Office include the B-class objects of the 1995 inventory, the proposals for new or changed B-class objects submitted by
576-470: 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 Tuggen ( Tuggenersee ) near Tuggen . The waters of Lake Zurich flow out of the lake at its north-west end (at the level of the Quaibrücke ), passing through the city of Zurich; however, the outflow is then called
608-498: The internal (i.e. inside the town wall) Fröschengraben , the outer Sihlgraben and the intermediate town wall was first mentioned in 1258 AD as niuwer graben (new moat), and in 1293 as graben ze Woloshofen Türlin , probably meaning the moat at the Wollishofen gate. The present Schanzengraben was still in construction around 1300. On the wall gardens , probably the area between Fröschengraben, Sihlgraben and Schanzengraben,
640-626: The lake has grown in size over time, the original piles are now around 4 metres (13 ft) to 7 metres (23 ft) under the water level of 406 metres (1,332 ft). Two other sites are not far away: Greifensee–Storen/Wildsberg at the Greifensee and Wetzikon–Robenhausen at the Pfäffikersee. As well as being part of the 56 Swiss sites of the UNESCO World Heritage Site, each of these 11 prehistoric pile dwellings
672-648: The lake. At Wädenswil , the line connects to the Wädenswil–Einsiedeln railway to Einsiedeln , served by the S13 . Right bank : Towns on the eastern shore of the lower lake (also known as the Goldcoast , or Goldküste ) are connected by the Lake Zurich right bank railway line between Zürich HB and Rapperswil . This line is served by S-Bahn services S6 , S7 , S16 and S20 of Zurich S-Bahn. The Rapperswil–Ziegelbrücke railway line along
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#1732780666956704-782: The lower part is sometimes also referred to as the Lower Lake ( unterer Zürichsee ), respectively. Lake Zurich is a glacial lake that was formed by the Rhine-Linth glacier [ de ] . 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 ( Walensee ) from where its waters are now carried to
736-592: The moat, but also crosses underneath the General-Guisan-Quai and four road bridges, namely Börsenstrasse, Stockerstrasse, Pelikanstrasse and Sihlstrasse, as well as four pedestrian bridges. In addition to the so-called Seeuferanlage and its neighboring General-Guisan-Quai , there is nearby the Arboretum and the Voliere Zürich , Other attractions include the historical Enge quarter, but mainly
768-786: The narrowest point of the lake at the level of the Hurden Peninsula , carrying a railway line and road from Rapperswil to Pfäffikon . The waterway is also crossed by the Holzbrücke Rapperswil-Hurden , a wooden pedestrian bridge. The eastern section of the lake is known as the Obersee ( lit. ' Upper Lake ' ). West of the Seedamm lie the small islands of Lützelau and Ufenau , where in 1523 Ulrich von Hutten took refuge and died. Other islands include Grosser Hafner , Saffa Island and Schönenwerd (near Richterswil ). A popular tourist destination
800-496: The northern shore of Obersee is served by St. Gallen S-Bahn services S4 , S6 and S17 , and the Voralpen Express . This line connects Rapperswil with Schmerikon on the eastern end of the lake via Blumenau . Bollingen is a ghost station since 2004. Seedamm : The Rapperswil–Pfäffikon railway line across the Seedamm and Hurden Peninsula is served by Zurich S-Bahn services S5 and S40 and
832-475: The reconstruction of the moat in a pedestrian promenade was not done until 1975, however, the construction works ended in 1984. The Schanzengraben moat is listed in the inventory of estimable gardens and grounds of local importance. It also is listed in the Swiss inventory of cultural property of national and regional significance as an object of regional relevance . Lake Zurich Lake Zurich ( German : Zürichsee ; Alemannic German : Zürisee )
864-444: The south shore) are Kilchberg , Rüschlikon , Thalwil , Oberrieden , Horgen , Au , Wädenswil and Richterswil in the canton of Zurich , and Freienbach , Pfäffikon , Hurden, Altendorf , Lachen , Nuolen and Tuggen in the canton of Schwyz . On the opposite shore, which gradually becomes the northern shore towards east, are Zollikon , Küsnacht , Erlenbach , Herrliberg , Feldmeilen , Meilen , Stäfa , and Feldbach in
896-512: The vicinity, such as Egelsee , Lützelsee or Türlersee . Zimmerberg , Etzel and Buechberg mountains lie to the west and south of the lake, respectively. Further to the east, the Speer , Chüemettler and Federispitz can be seen from the southern part of the lake. Administratively, Lake Zurich is split between the cantons of Zurich ( Horgen District ), St. Gallen ( See-Gaster ) and Schwyz ( Höfe and March districts). The lower lake, to
928-463: The west of the Seedamm, is largely in the canton of Zurich, whilst the upper lake is shared between the cantons of St. Gallen and Schwyz. The following rivers or streams flow into lower part of Lake Zurich. From the Limmat clockwise, they are: Zurich , at the north-western end of the lake, is the largest city on Lake Zurich. The least populous is Hurden . On the west shore (which gradually becomes
960-527: The western and southern shores of Lake Zurich are linked by the Lake Zurich left bank railway line, which connects Zürich HB with Ziegelbrücke . This line is served by the S2 , S8 , S24 and S25 of the Zurich S-Bahn and InterRegio (IR) trains. It is also used by EuroCity (EC), Intercity Express (ICE), Intercity (IC) and Railjet (RJX) trains but they do not call at stations along
992-523: Was built in 1864, as a logical 'counterpart' to the Frauenbad at the Stadthausquai , being the historical men's bath. During the industrialization, on the node's banks settled various factories, and so Schanzengraben degenerated over time to an unattractive factory channel. The water tower, a local landmark, was built in 1724, and still exists in its original construction. First discussed in 1952,
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1024-478: Was completed as part of the Baroque fortifications of Zurich around 1642 AD. Being once the moat outside the town wall, the bulwark "Zur Katz" was the former easterly gunnery bastion of the city fortification. In 1830 the moat was redesigned as the second effluence of Lake Zurich, then redirected to the Sihl, and therefore it 'survived' the demolition of the Baroque fortification system. Männerbad Schanzengraben
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