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Surb Amenaprkitch
Surbtal is a river valley region in the Canton of Aargau, Switzerland. Geography The ''Surbtal'' (literally ''Surb valley'') is situated parallel to the Limmat Valley (''Limmattal'') in the Baden District, Aargau, Baden and Zurzach District, Zurzach districts of the Canton of Aargau in Switzerland. The valley is bounded by moraines of the Linth glacier; and in the east it passes over to the border of the Canton of Zürich respectively the drainage basin of the Wehn Valley (native German name: ''Wehntal''). Surbtal comprises the area of the municipalities: * Döttingen, Aargau, Döttingen * Endingen, Aargau, Endingen * Ehrendingen * Freienwil * Lengnau, Aargau, Lengnau * Schneisingen * Tegerfelden Surb The Surb is a long river in the Swiss cantons of Aargau and Zürich, where she rises on an altitude of MAMSL at the Municipalities of the canton of Zürich, municipality of Schöfflisdorf. The river drains the northern Wehntal, passing the municipalities of Ehrendingen, Leng ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Canton Of Aargau
Aargau ( ; ), more formally the Canton of Aargau (; ; ; ), is one of the 26 cantons forming the Swiss Confederation. It is composed of eleven districts and its capital is Aarau. Aargau is one of the most northerly cantons of Switzerland, by the lower course of the Aare River, which is why it is called ''Aar- gau'' ("Aare province"). It is one of the most densely populated regions of Switzerland. History Early history The area of Aargau and the surrounding areas were controlled by the Helvetians, a tribe of Celts, as far back as 200 BC. It was eventually occupied by the Romans and then by the 6th century, the Franks. The Romans built a major settlement called Vindonissa, near the present location of Brugg. Medieval Aargau The reconstructed Old High German name of Aargau is ''Argowe'', first unambiguously attested (in the spelling ''Argue'') in 795. The term described a territory only loosely equivalent to that of the modern canton, including the region between Aare ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tegerfelden
Tegerfelden is a municipality in the district of Zurzach in the canton of Aargau in Switzerland. Geography Located in the Surb river valley, Tegerfelden has an area, , of . Of this area, or 51.5% is used for agricultural purposes, while or 37.0% is forested. Of the rest of the land, or 10.0% is settled (buildings or roads), or 0.8% is either rivers or lakes.Swiss Federal Statistical Office-Land Use Statistics 2009 data accessed 25 March 2010 Of the built up area, housing and buildings made up 4.4% and transportation infrastructure made up 3.5%. Power and water infrastructure as well as other special developed areas made up 1.3% of the area Out of the forested land, all of the forested land area is covered with heavy forests. Of the agricultu ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hurden
Hurden is a village in the municipality of Freienbach in the canton of Schwyz in Switzerland. First mentioned in 1217, the name "de Hurden" was used for the peninsula and for the fish traps made of woven work, called "Hürden" or "Hurden", which were used by the locals. Geography The village of Hurden is located on a peninsula protruding from the southern shore of Lake Zürich at its narrowest point. The peninsula has its origin in the retreat of the Linth glacier at the end of the last glacial period when Lake Zürich was formed. This retreat left a moraine across the valley now occupied by Lake Zürich. The higher southern section of this moraine extends above the lake's water level and forms the peninsula, whilst the lower northern section forms a shallow section in the otherwise deep lake. Together these separate Lake Zürich into two parts, the larger lower lake to the north-west, and the smaller upper lake ( ''Obersee'') to the east. The artificial Seedamm uses a com ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Würm Glaciation
The Würm glaciation or Würm stage ( or ''Würm-Glazial'', colloquially often also ''Würmeiszeit'' or ''Würmzeit''; cf. ice age), usually referred to in the literature as the Würm (often spelled "Wurm"), was the last glacial period in the Alpine region. It is the youngest of the major glaciations of the region that extended beyond the Alps themselves. Like most of the other ice ages of the Pleistocene epoch, it is named after a river, in this case the Würm in Bavaria, a tributary of the Amper. The Würm ice age can be dated to about 115,000 to 11,700 years ago. Sources differ about the dates, depending on whether the long transition phases between the glacials and interglacials (warmer periods) are allocated to one or other of those periods. The average annual temperatures during the Würm ice age in the Alpine Foreland were below −3 °C (today +7 °C). That has been determined from changes in the vegetation ( pollen analysis), as well as differences in the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Eemian
The Last Interglacial, also known as the Eemian, was the interglacial period which began about 130,000 years ago at the end of the Penultimate Glacial Period and ended about 115,000 years ago at the beginning of the Last Glacial Period. It corresponds to Marine Isotope Stage 5e. It was the second-to-latest interglacial period of the current Ice Age, the most recent being the Holocene which extends to the present day (having followed the last glacial period). During the Last Interglacial, the proportion of in the atmosphere was about 280 parts per million. The Last Interglacial was one of the warmest periods of the last 800,000 years, with temperatures comparable to and at times warmer (by up to on average 2 degrees Celsius) than the contemporary Holocene interglacial, with the maximum sea level being up to 6 to 9 metres higher than at present, with global ice volume likely also being smaller than the Holocene interglacial. The Last Interglacial is known as the Eemian in nort ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Glacial Maximum
An ice age is a long period of reduction in the temperature of Earth's surface and atmosphere, resulting in the presence or expansion of continental and polar ice sheets and alpine glaciers. Earth's climate alternates between ice ages, and greenhouse periods during which there are no glaciers on the planet. Earth is currently in the ice age called Quaternary glaciation. Individual pulses of cold climate within an ice age are termed '' glacial periods'' (''glacials, glaciations, glacial stages, stadials, stades'', or colloquially, ''ice ages''), and intermittent warm periods within an ice age are called '' interglacials'' or ''interstadials''. In glaciology, the term ''ice age'' is defined by the presence of extensive ice sheets in the northern and southern hemispheres. By this definition, the current Holocene epoch is an interglacial period of an ice age. The accumulation of anthropogenic greenhouse gases is projected to delay the next glacial period. History of research I ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Glatttal
The Glatt Valley (German: ''Glattal'' or ''Glatttal'') is a region and a river valley in the canton of Zürich in Switzerland. Geography The Glatt is a tributary to the Rhine in the Zürcher Unterland area of the canton of Zurich. It is long and flows out from the Greifensee through its river valley, discharging into the Rhine by Rheinsfelden. The Region Glatttal comprises, among other communities in the districts of Uster, Dielsdorf and Bülach, the suburban cities and municipalities of Bassersdorf, Bülach, Dietlikon, Dübendorf, Fällanden, Glattfelden, Höri, Kloten, Oberglatt, Opfikon- Glattbrugg, Rümlang, Schwerzenbach, Wallisellen and Wangen-Brüttisellen. In addition, the districts 11 and 12 (so-called ''Zürich-Nord'') of the city of Zürich, consisting of the districts of Affoltern, Oerlikon and Seebach respectively Hirzenbach, Saatlen and Schwamendingen Mitte, are geographically located in the Glattal. Economics and transport Thanks to its excellent ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hombrechtikon
Hombrechtikon is a municipality in the district of Meilen in the canton of Zürich in Switzerland. History Hombrechtikon is first mentioned in 1200 as ''Humbrechtigkon''. In 1217 it was mentioned as ''Hunbrechticon''. Geography Hombrechtikon has an area of . Of this area, 60.6% is used for agricultural purposes, while 14.9% is forested. Of the rest of the land, 18.7% is settled (buildings or roads) and the remainder (5.8%) is non-productive (rivers, glaciers or mountains). housing and buildings made up 13.9% of the total area, while transportation infrastructure made up the rest (4.8%). Of the total unproductive area, water (streams and lakes) made up 1.2% of the area. 15.8% of the total municipal area was undergoing some type of construction. The municipality is located between Lake Zurich and the Zürcher Oberland. The land is very hilly, which prevented a large, single village from forming. There at least 97 different hamlets and individual farm houses scatt ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pfannenstiel (Zürich)
Pfannenstiel (el. ) is a wooded mountain respectively a region overlooking the Lake Zürich and Zürcher Oberland in the canton of Zürich in Switzerland. Geography Pfannenstiel (Swiss German: ''Pfannenstil'' meaning '' pan handle'') is commonly used for the mountain and the region of a longish mountain area. It is located in the district of Meilen, some in the southeast of the city of Zürich, bordered by Greifensee and Zürcher Oberland in the northeast, Lake Zürich in the southwest and the area around the municipality of Hombrechtikon in the east. In the northwest, Pfannenstiel is bordered by the village of Forch and a former mountain pass () leading from Glatt valley to the Lake Zürich shore. Its highest point (''Okenshöhe'') is about 450 metres above the Lake Zürich. From southeast to northwest, Pfannenstiel is part of a chain of peaks respectively mountains: ''Guldenen'' (), ''Wassberg'' (), '' Öschbrig'' (), Adlisberg (), Zürichberg (), Käferberg-Waid ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Aare
The Aare () or Aar () is the main tributary of the High Rhine (its discharge even exceeds that of the latter at their confluence) and the longest river that both rises and ends entirely within Switzerland. Its total length from its source to its junction with the Rhine comprises about , during which distance it descends , draining an area of , almost entirely within Switzerland, and accounting for close to half the area of the country, including all of Central Switzerland. There are more than 40 hydroelectric plants along the course of the Aare. The river's name dates to at least the La Tène period, and it is attested as ''Nantaror'' "Aare valley" in the Berne zinc tablet. The name was Latinized as ''Arula''/''Arola''/''Araris''. Course The Aare rises in the great Aargletschers (Aare Glaciers) of the Bernese Alps, in the canton of Bern and west of the Grimsel Pass. The Finsteraargletscher and Lauteraargletscher come together to form the Unteraargletscher (Lower ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Unterendingen
Unterendingen is a former municipality in the district of Zurzach in the canton of Aargau in Switzerland. On 1 January 2014 the former municipality of Unterendingen merged into the municipality of Endingen.Nomenklaturen – Amtliches Gemeindeverzeichnis der Schweiz accessed 13 December 2014 Geography Before the merger, Unterendingen had a total area of . Of this area, or 53.5% is used for agricultural purposes, while or 37.9% is forested. Of the rest of the land, or 8.1% is settled (buildings or roads), or 0.3% is either rivers or lakes.[...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wehntal
Wehntal is the name of a valley region in the Canton of Zürich in Switzerland. Geography The ''Wehn'' valley (native German name: ''Wehntal'') area is situated between the Lägern and ''Egg'' mountain chain in the Dielsdorf District of the Canton of Zürich in Switzerland. To the east the valley is bounded by a moraine of the Linth glacier, respectively the lower Glatt Valley near Dielsdorf, and in the west it passes over to the border of the Canton of Aargau respectively the drainage bassin of the Surb Valley (native German name: ''Surbtal'') and the Surb, river of the same name which rises in the Wehntal. The population of the region is expanding rapidly due to its proximity to city of Zürich and its beautiful landscape. Wehntal comprises the area of the Municipalities of the canton of Zürich, municipalities: * Schöfflisdorf * Oberweningen * Schleinikon * Niederweningen * Steinmaur * Dielsdorf ZH, Dielsdorf History About 185,000 years ago, a side lobe of the Walensee/ ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
