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Longitudinal Valley
A longitudinal valley is an elongated valley found between two almost-parallel mountain chains in geologically young fold mountains, such as the Alps, Carpathians, Andes, or the highlands of Central Asia. They are often occupied and shaped by a subsequent stream.Whittow, John (1984). ''Dictionary of Physical Geography''. London: Penguin, p. 318. {{ISBN, 0-14-051094-X. The term is frequently used if a mountain range also has prominent transverse valleys, where rivers cut through the mountain chains in so-called water gaps. Description Many longitudinal valleys follow the strike of the rock strata or significant geological fault lines. These are formed in conjunction with the tectonic movements during mountain building, which in turn are due to plate tectonic processes. The faults are structures that reach deep into the lower part of the Earth's crust, which is already in place before the actual mountain building phase and is later reactivated. The Periadriatic Seam in the Alps is ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Vue Du Val-de-Travers Depuis La Route Du Château (Môtiers, Le 24
Vue or VUE may refer to: Places * Vue, Loire-Atlantique, a commune in France * The Vue, a skyscraper in Charlotte, North Carolina Arts, entertainment and media * Vue (band), a rock and roll band from San Francisco, California * Vue Cinemas, a cinema company in the United Kingdom * ''Vue Weekly'', an alternative newspaper in Edmonton, Canada * PlayStation Vue, a former American streaming service from Sony Television stations * KVUE (Texas), KVUE, the ABC TV affiliate for Austin, Texas, US * WVUE (Wilmington, Delaware), a defunct TV station in Wilmington, Delaware, US * WVUE-DT, the Fox TV affiliate for New Orleans, Louisiana, US Brands and enterprises * Pearson VUE, an electronic testing company * Saturn Vue, a sport utility vehicle * Vue International, a multinational cinema holding company based in the UK * Vue Pack, single-serve coffee system by Keurig *Vue.ai, A Madstreetden brand based in the USA Science and technology * Villitis of unknown etiology, a placental injury Soft ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Earth's Crust
Earth's crust is Earth's thin outer shell of rock, referring to less than 1% of Earth's radius and volume. It is the top component of the lithosphere, a division of Earth's layers that includes the crust and the upper part of the mantle. The lithosphere is broken into tectonic plates whose motion allows heat to escape from the interior of the Earth into space. The crust lies on top of the mantle, a configuration that is stable because the upper mantle is made of peridotite and is therefore significantly denser than the crust. The boundary between the crust and mantle is conventionally placed at the Mohorovičić discontinuity, a boundary defined by a contrast in seismic velocity. The temperature of the crust increases with depth, reaching values typically in the range from about to at the boundary with the underlying mantle. The temperature increases by as much as for every kilometer locally in the upper part of the crust Composition File:Elemental abundances.svg, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mur (river)
The Mur () or Mura (; ; ; Prekmurje Slovene: ''Müra''Novak, Vilko. 2006. ''Slovar stare knjižne prekmurščine''. Ljubljana: ZRC SAZU, pp. 262, 269. or ''Möra'') is a river in Central Europe rising in the Hohe Tauern national park of the Central Eastern Alps in Austria with its source being above sea level. It is a tributary of the Drava and subsequently the Danube. The Mur's total length is around . About 326 km are within the interior of Austria; 95 km flow in and around Slovenia (67 km along the borders with Austria and Croatia, 28 km inside Slovenia), and the rest forms the border between Croatia and Hungary. The largest city on the river is Graz, Austria. Its drainage basin covers an area of . Tributaries of the Mur include the Mürz, the Sulm, the Ščavnica, the Ledava and the Trnava. Etymology The river was attested as ''Maura'' in AD 799, ''Muora'' in 890, ''Mura'' in 1259, ''Mvr'' and ''Mver'' in 1310, and ''Muer'' in 1354. The name is p ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Austria
Austria, , bar, Östareich officially the Republic of Austria, is a country in the southern part of Central Europe, lying in the Eastern Alps. It is a federation of nine states, one of which is the capital, Vienna, the most populous city and state. A landlocked country, Austria is bordered by Germany to the northwest, the Czech Republic to the north, Slovakia to the northeast, Hungary to the east, Slovenia and Italy to the south, and Switzerland and Liechtenstein to the west. The country occupies an area of and has a population of 9 million. Austria emerged from the remnants of the Eastern and Hungarian March at the end of the first millennium. Originally a margraviate of Bavaria, it developed into a duchy of the Holy Roman Empire in 1156 and was later made an archduchy in 1453. In the 16th century, Vienna began serving as the empire's administrative capital and Austria thus became the heartland of the Habsburg monarchy. After the dissolution of the H ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Salza (Enns)
The Salza (also Mariazeller Salza) is an eastern tributary of the Enns. It originates on the mountain in Lower Austria and flows South of Mariazell through the Styrian nature preserve . After , it flows into the Enns near (part of Landl). Its drainage basin is . Below the municipality of (belongs to Mariazell) is the , a weir (stone dam) used for timber rafting in 1848. Today the water of the reservoir is used to power a small electric power plant. Downstream from the reservoir, the Salza is a favorite site for kayakers. Numerous springs of small tributaries of the Salza have been captured and are used for the Viennese Viennese may refer to: * Vienna, the capital of Austria * Viennese people, List of people from Vienna * Viennese German, the German dialect spoken in Vienna * Music of Vienna, musical styles in the city * Viennese Waltz, genre of ballroom dance * V ... water supply. References External links * Rivers of Lower Austria Rivers of Styria Rivers of Austria [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Enns (river)
The Enns (, ) is a southern tributary of the river Danube, joining northward at Enns, Austria. The Enns spans , in a flat-J-shape. It flows from its source near the village Flachau, generally eastward through Radstadt, Schladming, and Liezen, then turns north near Hieflau, to flow past Weyer and Ternberg through Steyr, and further north to the Danube at Enns (''see map in References''). "Karte-Enns" (river map in German), RadTouren.at (Austria), May 2009, webpage: (236kb). Name It was known in Latin as ''Anisus'' or ''Anasus'', of uncertain origin; Anreiter et al. tried to link it to an Indo-European *''on''- and the hydronymic suffix *''-is-''. Later sources call it ''Ensa'' or ''Enisa''. Others have linked it to Upper Danubian Vasconic *''an'', "water." Another possible link is Greek ᾰ̓νῠστός (''anystos'', "useful"). The West Slavic languages have different names for the river: in Czech it is called the ''Enže''; in Slovak, the ''Enža''; and in Polish, the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Salzach
The Salzach (Austrian: saltsax ) is a river in Austria and Germany. It is in length and is a right tributary of the Inn, which eventually joins the Danube. Its drainage basin of comprises large parts of the Northern Limestone and Central Eastern Alps. 83% of its drainage basin () lies in Austria, the remainder in Germany (Bavaria). Its largest tributaries are Lammer, Berchtesgadener Ache, Saalach, Sur and Götzinger Achen. Etymology The river's name is derived from the German word ''Salz'' "salt" and '' Aach''. Until the 19th century, shipping of salt down the ''Salzach'' was an important part of the local economy. The shipping ended when the parallel Salzburg-Tyrol Railway line replaced the old transport system. Course The Salzach is the main river in the Austrian state of Salzburg. The source is located on the edge of the Kitzbühel Alps near Krimml in the western Pinzgau region. Its headstreams drain several alpine pastures at around (metres above the Adriatic), be ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Inn (river)
, image = UnterinntalWest.JPG , image_caption = Lower Inn valley from Rattenberg castle , source1_location = Swiss Alps (Lägh dal Lunghin) , source1_elevation = , source1_coordinates= , mouth_location = Danube (Passau) , mouth_elevation = , mouth_coordinates = , progression = , subdivision_type1 = Countries , subdivision_name1 = , subdivision_type2 = Cities , subdivision_name2 = , length = , discharge1_location= mouth , discharge1_avg = , basin_size = The Inn ( la, Aenus; rm, En) is a river in Switzerland, Austria and Germany. The river is long. It is a right tributary of the Danube and it is the third largest tributary of the Danube by discharge. The highest point of its drainage basin is the summit of Piz Bernina at . The Engadine, the valley of the En, is the only Swiss valley whose waters end up in the Black Sea (via the Danube). Etymology The name Inn is derived from the old Celtic words ''en'' and ''enios'', ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pleistocene
The Pleistocene ( , often referred to as the ''Ice age'') is the geological Epoch (geology), epoch that lasted from about 2,580,000 to 11,700 years ago, spanning the Earth's most recent period of repeated glaciations. Before a change was finally confirmed in 2009 by the International Union of Geological Sciences, the cutoff of the Pleistocene and the preceding Pliocene was regarded as being 1.806 million years Before Present (BP). Publications from earlier years may use either definition of the period. The end of the Pleistocene corresponds with the end of the last glacial period and also with the end of the Paleolithic age used in archaeology. The name is a combination of Ancient Greek grc, label=none, πλεῖστος, pleīstos, most and grc, label=none, καινός, kainós (latinized as ), 'new'. At the end of the preceding Pliocene, the previously isolated North and South American continents were joined by the Isthmus of Panama, causing Great American Interchang ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Glacier
A glacier (; ) is a persistent body of dense ice that is constantly moving under its own weight. A glacier forms where the accumulation of snow exceeds its Ablation#Glaciology, ablation over many years, often Century, centuries. It acquires distinguishing features, such as Crevasse, crevasses and Serac, seracs, as it slowly flows and deforms under stresses induced by its weight. As it moves, it abrades rock and debris from its substrate to create landforms such as cirques, moraines, or fjords. Although a glacier may flow into a body of water, it forms only on land and is distinct from the much thinner sea ice and lake ice that form on the surface of bodies of water. On Earth, 99% of glacial ice is contained within vast ice sheets (also known as "continental glaciers") in the polar regions, but glaciers may be found in mountain ranges on every continent other than the Australian mainland, including Oceania's high-latitude oceanic island countries such as New Zealand. Between lati ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Eastern Alps
Eastern Alps is the name given to the eastern half of the Alps, usually defined as the area east of a line from Lake Constance and the Alpine Rhine valley up to the Splügen Pass at the Alpine divide and down the Liro River to Lake Como in the south. The peaks and mountain passes are lower than the Western Alps, while the range itself is broader and less arched. Geography Overview The Eastern Alps include the eastern parts of Switzerland (mainly Graubünden), all of Liechtenstein, and most of Austria from Vorarlberg to the east, as well as parts of extreme Southern Germany (Upper Bavaria), northwestern Italy (Lombardy), northeastern Italy (Trentino-Alto Adige/Südtirol, Veneto and Friuli-Venezia Giulia) and a good portion of northern Slovenia (Upper Carniola and Lower Styria). In the south the range is bound by the Italian Padan Plain; in the north the valley of the Danube River separates it from the Bohemian Massif. The easternmost spur is formed by the Vienna Woods range, wi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Continental Crust
Continental crust is the layer of igneous, sedimentary, and metamorphic rocks that forms the geological continents and the areas of shallow seabed close to their shores, known as continental shelves. This layer is sometimes called ''sial'' because its bulk composition is richer in aluminium silicates (Al-Si) and has a lower density compared to the oceanic crust, called ''sima'' which is richer in magnesium silicate (Mg-Si) minerals. Changes in seismic wave velocities have shown that at a certain depth (the Conrad discontinuity), there is a reasonably sharp contrast between the more felsic upper continental crust and the lower continental crust, which is more mafic in character. The continental crust consists of various layers, with a bulk composition that is intermediate (SiO2 wt% = 60.6). The average density of continental crust is about , less dense than the ultramafic material that makes up the mantle, which has a density of around . Continental crust is also less dense ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
