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Zimmerberg II Base Tunnel
Zimmerberg (el. ) is a mountain and a region located in the district of Horgen in the canton of Zurich, Switzerland. Its name bases on the Old High German word ''zimbar'' in the meaning of lumber. Geography Zimmerberg mountain is located some in the southeast of the city of Zürich, between Langnau am Albis in the Sihl Valley (German: ''Sihltal'') and Rüschlikon and Horgen on the Lake Zurich, overlooking Sihl valley, the Albis hills, Lake Zurich and Pfannenstiel. Points of interest include Hüttnersee and, on the neighbouring Albis chain, ''Albishorn'' (), ''Bürglen'' mountain (), the observation tower near Schnabelburg, the Albis Pass, Felsenegg and the extensive woods known as Sihlwald. Sihl river borders Zimmerberg on its southern side, on the northeastern side it is bordered by the Lake Zürich. The area is wooded, but also has extensive fields, some cultivated. Being near the city Zurich, the area is a known recreation area. The area alongside Lake Zürich had ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountain
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited Summit (topography), summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are Monadnock, isolated summits, but most occur in mountain ranges. Mountain formation, Mountains are formed through Tectonic plate, tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through Slump (geology), slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce Alpine climate, colder climates than at sea level at similar latitude. These colder climates strongly affect the Montane ecosystems, ecosys ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sihl
The Sihl is a Swiss river that rises near the Druesberg mountain in the canton of Schwyz, and eventually flows into the Limmat in the centre of the city of Zürich. It has a length of , including the Sihlsee reservoir, through which the river flows. Water is abstracted from the river at the Sihlsee, leading to decreased downstream water flows and a consequent reduction in water quality. The river flows through, or along the border of, the cantons of Schwyz, Zürich and Zug. The main settlements of the Sihl Valley are all in the canton of Zürich, and include the towns of Langnau am Albis and Adliswil, along with a south-western segment of the city of Zürich. Above Langnau am Albis, some from the confluence with the Limmat, there are no major settlements alongside the river, and only a few small villages. Whilst the town of Einsiedeln is situated close to the Sihlsee, it is actually in the valley of a tributary river, the Alp. Etymology The first written reference to the name d ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Richterswil
Richterswil (Swiss German: ''Richtischwiil'' ) is a municipality in the district of Horgen in the canton of Zürich in Switzerland. History Richterswil is first mentioned in 1265 as ''Richtliswile''. During the 17th Century, a series of peasant revolts broke out across Switzerland. One of these revolts, the 1645/46 ''Wädenswiler Steueraufstand'' (Wädenswil tax revolt), occurred around Lake Zürich and involved the village of Richterswil. The Richterswiler Weibel Rudolf Goldschmid was one of the leaders of the revolt who was executed in Zürich following the failure of the revolt. During the first Villmergen war (1656) Richterswil was invaded by an army from Schwyz. During the second Villmergen war, the newly built fortifications above the city, prevented another invasion. Under the French established Helvetic Republic Richterswil was part of the District of Horgen, and had a higher tax rate than surrounding villages. As part of this higher tax, during the War of the Sec ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Plateau
In geology and physical geography, a plateau (; ; ), also called a high plain or a tableland, is an area of a highland consisting of flat terrain that is raised sharply above the surrounding area on at least one side. Often one or more sides have deep hills or escarpments. Plateaus can be formed by a number of processes, including upwelling of volcanic magma, extrusion of lava, and erosion by water and glaciers. Plateaus are classified according to their surrounding environment as intermontane, piedmont, or continental. A few plateaus may have a small flat top while others have wide ones. Formation Plateaus can be formed by a number of processes, including upwelling of volcanic magma, extrusion of lava, Plate tectonics movements and erosion by water and glaciers. Volcanic Volcanic plateaus are produced by volcanic activity. The Columbia Plateau in the north-western United States is an example. They may be formed by upwelling of volcanic magma or extrusion of lava. The un ... [...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] |
Moraine
A moraine is any accumulation of unconsolidated debris (regolith and rock), sometimes referred to as glacial till, that occurs in both currently and formerly glaciated regions, and that has been previously carried along by a glacier or ice sheet. It may consist of partly rounded particles ranging in size from boulders (in which case it is often referred to as boulder clay) down to gravel and sand, in a groundmass of finely-divided clayey material sometimes called glacial flour. Lateral moraines are those formed at the side of the ice flow, and terminal moraines were formed at the foot, marking the maximum advance of the glacier. Other types of moraine include ground moraines (till-covered areas forming sheets on flat or irregular topography) and medial moraines (moraines formed where two glaciers meet). Etymology The word ''moraine'' is borrowed from French , which in turn is derived from the Savoyard Italian ("mound of earth"). ''Morena'' in this case was derived from Provenà ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sihlwald
The Sihlwald is a forest and nature reserve in the Sihl Valley of the Swiss canton of Zürich. It is a rare example of a large-scale and original forest, situated on the eastern slopes of the Albis hills to the west side of the Sihl river. Although the forest is owned by the city of Zürich, it is situated outside the city boundary, within the municipality of Horgen and several adjoining municipalities. The Sihlwald now forms part of the Zürich Wilderness Park. The city of Zürich received the Sihl forest, or Sihlwald, as a gift in 1309 from the Hapsburgers and again in 1524 through the dissolution of the Fraumünster convent. Over the following centuries, the forest provided Zürich with timber and firewood. From 1876 on, there was even a forest railway which facilitated the work in the forest. However, the trees have not been felled since the 1990s; this is due to the actions of forest director Andreas Speich, in order to preserve the forest's unique composition. On August ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Felsenegg
Felsenegg (el. ) is a vantage point in the canton of Zürich in Switzerland. Geography Felsenegg is located some to the southwest of the city of Zürich on the Albis chain, between the municipalities of Stallikon and Adliswil. The hilltop station of Luftseilbahn Adliswil-Felsenegg (LAF for short or commonly called ''Felseneggbahn'') aerial tramway is situated on Felsenegg. The Albis area is one of the most important recreation areas of greater Zürich. The area is mostly wooded, but also has extensive fields, often reaching to the summit, some cultivated, some used as pastures for cows or sheep. Points of interest Being close to the city of Zürich, the area is heavily visited. Felsenegg includes a restaurant located at the summit overlooking the Sihl Valley and Lake Zürich to the east, and Reppisch valley, Türlersee and the so-called Säuliamt (District of Affoltern) to the west. Well maintained hiking trails from Uetliberg and Uetlibergbahn mountain station to the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 Rifferswil. Other nearby passes across the same chain are Buechenegg to the north, and Schnabellücken, which is undeveloped except for a hiking trail, to the south. The eastern ramp and crest of the pass is in the municipality of Langnau, with the western ramp in Hausen. The pass is first mentioned in 1492, when the Zurich Council made a decision on road maintenance. In past times it was regarded as an important route between Zurich and central Switzerland. In 1713, Zurich military authorities are recorded as regarding transport over the Albis Pass as being simpler and cheaper than going via Birmensdorf or Horgen. However the construction of the railway from Thalwil to Zug and later roads rendered the pass less important. The road ov ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Schnabelburg
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] |
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