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Albis Tunnel
The Albis is a chain of hills in the Canton of Zürich, Switzerland, stretching for some 19 km from Sihlbrugg in the south to Waldegg near Zürich in the north. The chain forms, among others, the border between the Affoltern and Horgen districts. The best known point is Uetliberg at 870 m, overlooking the city of Zürich. Other points of interest include the Albishorn (909m.) the Bürglen (also known as Bürglenstutz, the highest peak, 914.6m.), the Schnabelburg, an observation tower, the Albis Pass, the small town of Buechenegg, and the extensive woods (known as the Sihlwald forest) on both sides of the river Sihl. The Sihl Valley borders the Albis chain on its entire east side. On the west side, the Albis is bordered by various streams (including the Reppisch) and one lake, the Türlersee. The chain is mostly wooded, but also has extensive fields, often reaching to the summit, some cultivated, some used as pastures for cows or sheep. Being very near Zürich, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Glärnisch
The Glärnisch is a mountain massif of the Schwyz Alps, overlooking the valley of the Linth in the Swiss canton of Glarus. It consists of several summits, of which the highest, ''Bächistock'', is 2,915 metres above sea level. Until 2013, the highest point was considered to be an unnamed point with a summit cross at 2,914 metres (until 2013: 2'915 metres). The other main summits are ''Vrenelisgärtli'' ("Verena's Little Garden" at 2,904 metres) and the ''Ruchen'' (2,901 metres). The massif of the Glärnisch consists of two ridges of either side of the glacier named ''Glärnischfirn'', culminating at the Ruchen to the west, rising more than 2,000 metres above the Klöntalersee, and at the Bächistock to the southwest. The Vrenelisgärtli is the closest peak to Schwanden. The Glärnischfirn (also known as the Glärnischgletscher, the "Glarnisch Glacier") is about one mile long and about one-half mile wide at between 1.5 and 2.0 miles above sea level. The surrounding peaks are ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Luftseilbahn Adliswil-Felsenegg
The Adliswil-Felsenegg cable car (LAF; german: Luftseilbahn Adliswil-Felsenegg or ) is a cable car in the canton of Zürich in Switzerland. The lower station is located in Adliswil in the Sihl Valley, whilst the upper station is located on the Felsenegg hill on the Albis ridge near the Felsenegg-Girstel TV-tower. The upper station at Felsenegg forms one end of a panoramic walk to the Uetliberg mountain, whilst the lower station is some from Adliswil railway station. The cable car is owned by the Luftseilbahn Adliswil-Felsenegg AG and is operated by the Sihltal Zürich Uetliberg Bahn (SZU), the railway company which links both Adliswil and the Uetliberg to the city of Zürich. History The cable car was built by the Swiss company Von Roll, opening on 30 December 1954. The line reused the former two cabins of the "Landi-Schwebebahn", built to connect the two sites of the . In 1960, these cabins were replaced by new cabins with a capacity of 30 passengers, constructed by SIG Neuha ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Käferberg
Käferberg (el. ) and Waidberg (el. ) are the summits of a wooded mountain respectively chain of hills overlooking the inner city of Zürich, Zürichsee, Albis chain and Uetliberg, as well as the Limmat Valley and the Zürcher Unterland in Switzerland. Geography Käferberg (Swiss German: ''Chäferberg'' meaning ''mountain of beetles'') and Waidberg (mountain of meadows) are the peaks of a longish mountain in the north of the Limmat Valley. It is located in the Zürich districts of Höngg, Wipkingen and Affoltern, between ''Bucheggplatz'' and ETH-Hönggerberg, known as ''Science City'', and the western ''Hönggerberg'' heading on the northern border of the Limmat valley to Würenlos. In the east, Käferberg is bordered by a small mountain pass between Bucheggplatz () and ''Milchbuck'' () at Zürichberg, leading from the city of Zürich to the Glatt valley. In the north, the region is bordered by the Glatt, and Furt valleys. Its highest point (''Waidberg'') is about a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sihltal
Sihl Valley (German: ''Sihltal'') is a river valley and belongs to the Zimmerberg-Sihltal region located in the district of Horgen in the canton of Zurich, Switzerland. Commonly ''Sihltal'' is used as the name of the Lower Sihl Valley, i.e. the area in the southwest of the city of Zürich. Geography In common The area alongside Lake Zürich had been formed as the left moraine of the Ice Age glacier, the bed of which is now the Lake Zürich and the valley of the Sihl. Sihl valley is extensively wooded, but also cultivated and heavily populated in its lower parts. The Sihl () is the name of a long river located in the cantons of Schwyz (SZ) and Zürich (ZH). The valley compromises parts of the districts of Einsiedeln (SZ) (upper Sihl valley), Horgen (ZH) and Zürich. The region of the valley comprises about . Upper Sihl Valley Sihl rises at ''Drusberg'' near Hoch-Ybrig in the canton of Schwyz, passes the long Sihlsee near Einsiedeln, ''Sunnegg'' near Biberbrugg and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wollishofen
Wollishofen is a neighbourhood in Zürich's district 2 (Zürich), 2nd district. It was formerly a municipality of its own, having been incorporated into Zürich in 1893. The neighbourhood has a population of 15,592 distributed on an area of 5.75 km2. Geography Located between the Sihl, Sihl river and Lake Zurich, it forms the southern boundary of the city on the left bank of the lake. The lake occupies 28.5% (1.64 km2) of the total area of the district. To the south, Wollishofen borders the municipalities of Adliswil and Kilchberg, Zürich, Kilchberg. Werkbundsiedlung Neubühl A New Objectivity (architecture), New Objectivity estate constructed 1930-1932. Architects: Max Haefeli, Alfred Roth (Architekt), Alfred Roth, Emil Roth, Carl Hubacher, Rudolf Steiger, Werner Max Moser and Paul Artaria Transport Wollishofen is located on the A3 motorway (Switzerland), A3 motorway, and on tram route Zürich tram route 7, 7 of the Verkehrsbetriebe Zürich. Zürich Wollishofen ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Leimbach (Zürich)
Leimbach () is a quarter in the district 2 in Zürich. It is located in the lower Sihl Valley (''Sihltal''). It was formerly a municipality of its own, having been incorporated into Zürich in 1893. The quarter has a population of 5,185 as of December 31, 2008 and is distributed on an area of . Transportation Zürich Leimbach railway station is a stop of the Zürich S-Bahn on the line S4. It is a 10-minute ride from Zürich Hauptbahnhof. Gallery File:Felsenegg - Leimbach - Zürich - Käferberg IMG 3237.JPG, Leimbach, lower Sihl valley, inner city of Zürich and Käferberg (to the left) in the background, as seen from Felsenegg File:Zürich-Leimbach-Sihltal - Käferberg IMG 2374.JPG, Leimbach and lower Sihltal as seen from the Waidberg File:Albis Langnau.JPG, Langnau am Albis, Adliswil, Leimbach and Lake Zürich, as seen from the Albis hills (Hochwacht) File:Zürich - Fallätsche IMG 0202.JPG, Wollishofen Wollishofen is a neighbourhood in Zürich's district 2 (Zürich), ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Schnabelburg Castle
Schnabelburg Castle (german: Schnabelburg) was a small castle erected in 1150 by the lords of Eschenbach (Switzerland, near Lucerne) on the Albis chain South-west of Zurich, Switzerland, overlooking the nearby Schnabellücken pass. In 1309 the Schnabelburg was destroyed by the Habsburgs, in revenge for the participation of Walter von Eschenbach in the murder of Albert I of Germany. All that is left today is low ruins, reachable in about 30 minutes on foot from the Albis Pass Albis Pass (el. ) is a mountain pass in the Albis range in the canton of Zurich in Switzerland. It connects Langnau am Albis with the small village of Türlen on the Türlersee and, further on, Aeugst am Albis, Hausen am Albis, Mettmenstetten and .... Castles in the canton of Zürich {{Zurich-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Baldern Castle
Baldern Castle (german: italic=yes, Burg Baldern or ''Burgstelle Baldern'') is a former castle in the municipality of Stallikon and the canton of Zürich in Switzerland. The remains of the castle comprise a set of earthworks, situated on the Albis ridge at some above sea level and about south of the summit of Uetliberg. The earthworks are obscured by the site's woodland nature. A legend recorded ca. 1510 suggests that the castle was built by Ludwig the German, the first king of East Francia, in the 9th century, but there is no strong evidence for this. The castle is known to have been owned by the Counts of Lenzburg in the 12th century. There have been no significant archeological investigations of the site, and the date and reason it was abandoned is unknown. The site of the castle lies about walk north of the upper station of the Adliswil-Felsenegg cable car at Felsenegg. The panoramic footpath from Uetliberg to Felsenegg passes through the old castle site. Gallery File: ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Uetliberg Castle
__NOTOC__ The Uetliberg (also known as Üetliberg) is a mountain in the Swiss plateau, part of the Albis chain, rising to . The mountain offers a panoramic view of the entire city of Zürich (to the northeast of its summit) and the Lake of Zurich (to the east), and lies on the boundary between the city of Zürich and the municipalities of Stallikon and Uitikon. The summit, known as Uto Kulm, is in Stallikon. At the summit, there is the Hotel Uto Kulm, together with two towers. One of these is a look-out tower (access costs , rebuilt 1990), whilst the other is the Uetliberg TV-tower (186 m, rebuilt 1990). The summit is easily accessible by train from Zürich. Uetliberg railway station lies some from, and below, the summit of the Uetliberg. It is the terminus of the Uetliberg line, and is linked to Zürich Hauptbahnhof by S-Bahn Zürich service S10. Trains usually run every half-hour, taking 20 minutes. There are numerous walking paths leading up to the top from Albisgüetl ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Landslide
Landslides, also known as landslips, are several forms of mass wasting that may include a wide range of ground movements, such as rockfalls, deep-seated grade (slope), slope failures, mudflows, and debris flows. Landslides occur in a variety of environments, characterized by either steep or gentle slope gradients, from mountain ranges to coastal cliffs or even underwater, in which case they are called submarine landslides. Gravity is the primary driving force for a landslide to occur, but there are other factors affecting slope stability that produce specific conditions that make a slope prone to failure. In many cases, the landslide is triggered by a specific event (such as a heavy rainfall, an earthquake, a slope cut to build a road, and many others), although this is not always identifiable. Causes Landslides occur when the slope (or a portion of it) undergoes some processes that change its condition from stable to unstable. This is essentially due to a decrease in the She ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Loess
Loess (, ; from german: Löss ) is a clastic, predominantly silt-sized sediment that is formed by the accumulation of wind-blown dust. Ten percent of Earth's land area is covered by loess or similar deposits. Loess is a periglacial or aeolian (windborne) sediment, defined as an accumulation of 20% or less of clay and a balance of roughly equal parts sand and silt (with a typical grain size from 20 to 50 micrometers), often loosely cemented by calcium carbonate. It is usually homogeneous and highly porous and is traversed by vertical capillaries that permit the sediment to fracture and form vertical bluffs. Properties Loess is homogeneous, porous, friable, pale yellow or buff, slightly coherent, typically non- stratified and often calcareous. Loess grains are angular, with little polishing or rounding, and composed of crystals of quartz, feldspar, mica and other minerals. Loess can be described as a rich, dust-like soil. Loess deposits may become very thick, more than ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lake Zürich
__NOTOC__ Lake Zurich ( Swiss German/Alemannic: ''Zürisee''; German: ''Zürichsee''; rm, Lai da Turitg) is a lake in Switzerland, extending southeast of the city of Zürich. 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 Seedamm at Rapperswil, whilst the part upstream of Rapperswil may be called the ''Obersee'' or Upper Lake. Geography Lake Zurich is formed by the Linth river, which rises in the glaciers of the Glarus Alps and was diverted by the Escher canal (completed in 1811) into Lake Walen from where its waters are carried to the east end of Lake Zurich by means of the Linth canal (completed in 1816). The waters of the Lake of Zurich flow out of the lake at its north-west end ( Quaibrücke), passing through the city of Zürich; however, the outflow is then called the Limmat. The culminating point of the lake's drainage basin is the Tödi at 3,614 metres above sea level. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
