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Dietikon - Marmoriweiher IMG 6131
Dietikon is the fifth biggest city of the canton of Zürich in Switzerland, after Zürich, Winterthur, Uster and Dübendorf. It is the capital of the same-named district of Dietikon and part of the Zürich metropolitan area. Geography The industrial city Dietikon is situated at an elevation of at the confluence of the Reppisch and the Limmat, located in the Limmat Valley (German: ''Limmattal''), along the railway line from Zürich to Baden. Here and in the neighboring region, Spreitenbach, is also the large Limmattal rail freight marshalling yard. Dietikon has an area of . Of this area, 17.2% is used for agricultural purposes, while 27% is forested. Of the rest of the land, 49.1% is settled (buildings or roads) and the remainder (6.7%) is non-productive (rivers, glaciers or mountains). housing and buildings made up 33.8% of the total area, while transportation infrastructure made up the rest (15.3%). Of the total unproductive area, water (streams and lakes) made u ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dietikon (district)
Dietikon District is a district of the Switzerland, Swiss canton of Zürich. The capital of the district of Dietikon is the city of Dietikon, located in the Limmat Valley (German: ''Limmattal''). Dietikon District was created in 1989 by splitting the former Zürich District into three parts. The western part became the Dietikon District, the eastern part became the Zürich (district), district (respectively city) of Zürich and the Municipalities of Switzerland, municipality of Zollikon (located east of Zürich) was integrated into the Meilen District. See also *Municipalities of the canton of Zürich References {{Canton Zurich Districts of the canton of Zürich ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dübendorf
Dübendorf is a municipality in the district of Uster in the canton of Zürich in Switzerland. It is a suburb of Zürich in Switzerland with a population of about 30,000 (2021). It is the fourth largest city in the canton, after Zürich, Winterthur, and Uster. History Dübendorf is first mentioned in 946 as ''Tuobilindorf''. On the northeastern side of the Adlisberg the ruins of the ''Dübelstein'' castle are situated; from 1487 to 1489 the home of Hans Waldmann, former mayor of the city of Zürich. Geography Dübendorf has an area of . Of this area, 37.6% is used for agricultural purposes, while 19.5% is forested. Of the rest of the land, 41.9% is settled (buildings or roads) and the remainder (1%) is non-productive (rivers, glaciers or mountains). housing and buildings made up 29.6% of the total area, while transportation infrastructure made up the rest (12.3%). Of the total unproductive area, water (streams and lakes) made up 1% of the area. The city is situated ro ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Glanzenberg Railway Station
Glanzenberg is a railway station in Switzerland, situated in the city of Dietikon. The station is located on the Zürich–Baden railway, Zurich to Olten main line and is a stop of the Zurich S-Bahn served by line S11 (ZVV), S11 and S12 (ZVV), S12. References Railway stations in the canton of Zürich Swiss Federal Railways stations Dietikon {{switzerland-railstation-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dietikon Railway Station
Dietikon railway station is a railway station in Switzerland, situated in the canton of Zürich and the city of Dietikon. The station is located on the Swiss Federal Railway's Zürich to Olten main line and is also the terminus of the metre gauge Bremgarten–Dietikon railway (BD). The station is served by Zürich S-Bahn lines S11, S12, S19, and S42; by some long distance trains on the main line; and by S-Bahn line S17 on the BD. History The first station on the site was built by the Swiss Northern Railway in 1847, as part of their pioneering line from Zürich to Baden, and hence was one of the first railway stations in Switzerland. The original station building was constructed on the northern side of the railway line and still exists, albeit now used as a rail enthusiasts' club. The original station was replaced in the 1860s by a new building on the southern, city centre, side of the line. This in turn was replaced in the 1970s by the current large station building ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
A3 Motorway (Switzerland)
The A3 is a motorway in northeast Switzerland, running diagonally from France toward the southeast border, and passing by Zürich on the way. The total length of the A3 motorway spans roughly , but parts of the road share sections of the A1 and A2 motorways. The A3 belongs to the Swiss motorway network. It starts at the border in Basel, where it connects to French motorway A35. From the Wiese Motorway Fork, the route is shared with the A2. At Augst, the motorway splits, with the A2 branching off and the A3 continuing past Rheinfelden and Frick. After the Bözberg tunnel is the Birrfeld Motorway Fork, near Birmenstorf. Here, the A1 and A3 share the same route as far as Motorway Interchange Limmattal, where the A3 goes towards Urdorf and the Uetliberg Tunnel which was opened on May 4, 2009. After Zürich the motorway weaves through the hills of the south-east bank of Lake Zürich. It continues along the Walensee (Walen Lake), and on to Mels where it ends at a junction w ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dietikon - Marmoriweiher IMG 6131
Dietikon is the fifth biggest city of the canton of Zürich in Switzerland, after Zürich, Winterthur, Uster and Dübendorf. It is the capital of the same-named district of Dietikon and part of the Zürich metropolitan area. Geography The industrial city Dietikon is situated at an elevation of at the confluence of the Reppisch and the Limmat, located in the Limmat Valley (German: ''Limmattal''), along the railway line from Zürich to Baden. Here and in the neighboring region, Spreitenbach, is also the large Limmattal rail freight marshalling yard. Dietikon has an area of . Of this area, 17.2% is used for agricultural purposes, while 27% is forested. Of the rest of the land, 49.1% is settled (buildings or roads) and the remainder (6.7%) is non-productive (rivers, glaciers or mountains). housing and buildings made up 33.8% of the total area, while transportation infrastructure made up the rest (15.3%). Of the total unproductive area, water (streams and lakes) made u ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
BDWM BDe 8-8 Ortsdurchfahrt Dietikon
BDWM Transport was a transport company in Switzerland, that operated regional rail and bus services in the cantons of Aargau and Zürich. The company was formed in 2000 by the merger of the Bremgarten–Dietikon railway (BD) and (WM) companies. The company merged with Wynental and Suhrental Railway to form Aargau Verkehr AG (AVA). The company operates: * The Bremgarten–Dietikon railway line (line S17 of the Zürich S-Bahn) * The Wohlen–Meisterschwanden bus service * The SBB bus Zofingen / Reiden * The express bus Bremgarten / Busslingen–Zurich Enge * The Limmat Bus AG In May 2016 it was announced that the Limmattal light rail line, to be constructed in the densely populated Limmattal area to the west of Zürich, would be operated by BDWM. The line will connect Killwangen, Spreitenbach, Dietikon, Urdorf and Schlieren to Zürich-Altstetten railway station, with connection to the Bremgarten–Dietikon line at Dietikon and to Zürich tram route 2 , neighboring_municip ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Spring (hydrology)
A spring is a point of exit at which groundwater from an aquifer flows out on top of Earth's crust (pedosphere) and becomes surface water. It is a component of the hydrosphere. Springs have long been important for humans as a source of fresh water, especially in arid regions which have relatively little annual rainfall. Springs are driven out onto the surface by various natural forces, such as gravity and hydrostatic pressure. Their yield varies widely from a volumetric flow rate of nearly zero to more than for the biggest springs. Formation Springs are formed when groundwater flows onto the surface. This typically happens when the groundwater table reaches above the surface level. Springs may also be formed as a result of karst topography, aquifers, or volcanic activity. Springs also have been observed on the ocean floor, spewing hot water directly into the ocean. Springs formed as a result of karst topography create karst springs, in which ground water travels through ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Glacial Erratic
A glacial erratic is glacially deposited rock differing from the type of rock native to the area in which it rests. Erratics, which take their name from the Latin word ' ("to wander"), are carried by glacial ice, often over distances of hundreds of kilometres. Erratics can range in size from pebbles to large boulders such as Big Rock () in Alberta. Geologists identify erratics by studying the rocks surrounding the position of the erratic and the composition of the erratic itself. Erratics are significant because: *They can be transported by glaciers, and they are thereby one of a series of indicators which mark the path of prehistoric glacier movement. Their lithographic origin can be traced to the parent bedrock, allowing for confirmation of the ice flow route. *They can be transported by ice rafting. This allows quantification of the extent of glacial flooding resulting from ice dam failure which release the waters stored in proglacial lakes such as Lake Missoula. Erratics ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Limmat Valley
The Limmat Valley (German: ''Limmattal'') is a river valley and a region in the cantons of Zürich and Aargau in Switzerland. Geography The Limmat () is a long river located in the cantons of Zürich (ZH) and Aargau (AG). It is the continuation of the Linth, and is known as the Limmat from the point of effluence from Lake Zürich, in the city of Zürich, flowing in northwesterly direction to the Aare. The confluence is located northeast of the small town of Brugg (AG), shortly after the mouth of the Reuss, and shortly before the Aare joins the Rhine. The confluence of the three rivers Aare, Reuss and Limmat is known as ''Wasserschloss''. Nature In 1930 the government of the canton of Zurich set the remains of the original Limmat riverside meadows and floodplains near Dietikon (''Dietiker Altläufe'') under conservation, as well in 2005 the floodplains (''Dietiker Schachen'') near Wettingen accommodating more than 150 plant species and rare species as common kingfis ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Limmat
The Limmat is a river in Switzerland. The river commences at the outfall of Lake Zurich, in the southern part of the city of Zurich. From Zurich it flows in a northwesterly direction, after 35 km reaching the river Aare. The confluence is located north of the small town of Brugg and shortly after the mouth of the Reuss. The main towns along the Limmat Valley downstream of Zurich are Dietikon, Wettingen, and Baden. Its main tributaries are the Linth, via Lake Zurich, the Sihl, in Zurich, and the Reppisch, in Dietikon. The hydronym is first attested in the 8th century, as ''Lindimacus''. It is of Gaulish origin, from ''*lindo-'' "lake" (Welsh ''llyn'') and ''*magos'' "plain" (Welsh ''maes''), and was thus presumably in origin the name of the plain formed by the Linth. Power generation Like many Swiss rivers, the Limmat is intensively used for production of hydroelectric power: along its course of , its fall is used by no less than ten hydroelectric power stations. Th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Reppisch
The Reppisch is a river in Switzerland. It rises in the Türlersee and joins the Limmat as its tributary, near the town of Dietikon. The Reppisch flows in the Säuliamt (Affoltern district), canton of Zürich, an area featuring still partially untouched nature. Between Birmensdorf and Dietikon, the river crosses a narrow valley which is used as a target range by the Swiss army troops stationed in the infantry barracks nearby. Therefore, this valley may be closed to entry during some parts of the week. Shortly before entering Dietikon, the river underruns the Mutschellenpassstrasse and the Bremgarten-Dietikon-Bahn railway. In the spring of 1999, there were heavy floods in this area, blocking the road and the railway service for several days. Tributaries Sixty eight named streams empty into the Reppisch, of which three, namely the Wüeribach, the Rummelbach and the Lunnerenbach, are 4 or more kilometres long. In addition there are 5 tributaries that are 2 kilometres lo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
