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Styrian-Lower Austrian Limestone Alps
The Styrian-Lower Austrian Limestone Alps (german: Steirisch-niederösterreichische Kalkalpen) are the easternmost part of the Northern Limestone Alps, running from the River Enns to the Vienna Basin. The high Alpine, limestone massifs of the Hochschwab, Veitsch, Schneealpe, Rax and Schneeberg belong to it as do the limestone prealps to the north as far as the Flysch zone. The geological conditions in the limestone mountains make this part of the Limestone Alps a valuable drinking water reservoir, from which the Vienna Water Supply (''Wiener Wasserversorgung'') draws. The geologist, Eduard Suess, pressed the Vienna city council for a water supply from this region as early as 1864. In 1873 the First Vienna Mountain Spring Pipeline (''I. Wiener Hochquellenwasserleitung'') was opened, running from the Rax-Schneeberg area. The 2nd pipeline was opened in 1910 and also drew its water from the area of the Styrian-Lower Austrian Limestone Alps, being fed from sources in the Hochschw ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Northern Limestone Alps
The Northern Limestone Alps (german: Nördliche Kalkalpen), also called the Northern Calcareous Alps, are the ranges of the Eastern Alps north of the Central Eastern Alps located in Austria and the adjacent Bavarian lands of southeastern Germany. The distinction from the latter group, where the higher peaks are located, is based on differences in geological composition. Geography If viewed on a west–east axis, the Northern Limestone Alps extend from the Rhine valley and the Bregenz Forest in Vorarlberg, Austria in the west extending along the border between the German federal-state of Bavaria and Austrian Tyrol, through Salzburg, Upper Austria, Styria and Lower Austria and finally ending at the Wienerwald at the city-limits of Vienna in the east. The highest peaks in the Northern Limestone Alps are the Parseierspitze () in the Lechtal Alps,Reynolds, Kev (2010). ''Walking in the Alps'', Cicerone, . and the Hoher Dachstein (). Other notable peaks in this range include the Zu ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geologist
A geologist is a scientist who studies the solid, liquid, and gaseous matter that constitutes Earth and other terrestrial planets, as well as the processes that shape them. Geologists usually study geology, earth science, or geophysics, although backgrounds in physics, chemistry, biology, and other sciences are also useful. Field research (field work) is an important component of geology, although many subdisciplines incorporate laboratory and digitalized work. Geologists can be classified in a larger group of scientists, called geoscientists. Geologists work in the energy and mining sectors searching for natural resources such as petroleum, natural gas, precious and base metals. They are also in the forefront of preventing and mitigating damage from natural hazards and disasters such as earthquakes, volcanoes, tsunamis and landslides. Their studies are used to warn the general public of the occurrence of these events. Geologists are also important contributors to ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Admont Abbey
Admont Abbey (german: Stift Admont) is a Benedictine monastery located on the Enns River in the town of Admont, Austria. The oldest remaining monastery in Styria, Admont Abbey contains the largest monastic library in the world as well as a long-established scientific collection. It is known for its Baroque architecture, art, and manuscripts. The abbey's location on the borders of the mountainous Gesäuse National Park (the name Admont derives from the Latin expression "ad montes", which means "at the mountains") is of unusual scenic beauty. History Dedicated to Saint Blaise, Admont Abbey was founded in 1074 by Archbishop Gebhard of Salzburg with the legacy of the late Saint Hemma of Gurk, and settled by monks from St. Peter's Abbey in Salzburg under abbot Isingrin. The second abbot, Giselbert, is said to have introduced the Cluniac reforms here. Another of the early abbots, Wolfhold, established a convent for the education of girls of noble families, and the educational t ... [...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 * ... water supply. References External links * Rivers of Lower Austria Rivers of Styria Rivers of Austria [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hochschwab
The Hochschwab in the Upper Styria Upper Styria (german: Obersteiermark), in the Austrian usage of the term, refers exclusively to the northwestern, generally mountainous and well-wooded half of the federal state of Styria. The southwestern half of the state around the capital o ... is a mountain, , and the highest summit in the eponymous mountain range. Location The summit of the Hochschwab is a flat, rock and grass-covered dome, that may easily be climbed from the Schiestlhaus () to the northeast in about half an hour via the plateau to the west (Biwakschachtel Fleischerhütte). The Schiestlhaus may be approached from Seewiesen () at the foot of the Steirischer Seeberg via the ''Seetal'' valley, the ''Untere Dullwitz'' to the Voisthaler Hut, the ''Obere Dullwitz'' and the ''Graf-Meran- Steig'', as well as from the north, from Weichselboden in the Salza valley. The showpiece of the Hochschwab is its mighty south face which has a width of almost two kilometres and rise ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wildalpen
Wildalpen is a municipality in the district of Liezen in the Austrian state of Styria Styria (german: Steiermark ; Serbo-Croatian and sl, ; hu, Stájerország) is a state (''Bundesland'') in the southeast of Austria. With an area of , Styria is the second largest state of Austria, after Lower Austria. Styria is bordered to .... Population References Cities and towns in Liezen District {{Styria-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
First Vienna Mountain Spring Pipeline
The First Vienna Mountain Spring Pipeline (I. Wiener Hochquellenwasserleitung) is a major part of Vienna's water supply and was the first source of safe drinking water for that city. The 95 km long line was opened on 24 October 1873, after four years of construction. Today, it delivers 62 million cubic meters of water per year (53% of Vienna's total supply in 2007). The water comes from high springs in the Rax and Schneeberg areas in Southern Lower Austria and Styria. History Beginnings to 1910 The reason for its creation Vienna's water supply originally came from private wells. In the absence of a functioning sewer system, the quality of the groundwater went from bad to worse, triggering disease and epidemics. Reinforced water pipes were built, but these primarily benefitted the wealthy and large institutions. Most of the population had to rely on spouts or fountains attached to wells. The first water pipe that provided greater coverage was built in 1803-1804, brin ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Eduard Suess
Eduard Suess (; 20 August 1831 - 26 April 1914) was an Austrian geologist and an expert on the geography of the Alps. He is responsible for hypothesising two major former geographical features, the supercontinent Gondwana (proposed in 1861) and the Tethys Ocean. Biography Eduard Suess was born on 20 August 1831 in London, England, the oldest son of Adolph Heinrich Suess, a Lutheran Saxon merchant, and mother Eleonore Friederike Zdekauer. Adolph Heinrich Suess was born on 11 March 1797 in Saxony, Holy Roman Empire and died on 24 May 1862 in Vienna, Austrian Empire, German confederation; Eleonore Friederike Zdekauer was born in Prague, nowadays part of the Czech Republic, which once belonged to the Holy Roman Empire and the Austrian Empire. When Eduard Suess was born, his family relocated to Prague, and then to Vienna when he was 14. He became interested in geology at a young age. While working as an assistant at the Hofmuseum in Vienna, he published his first paper—on the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geology
Geology () is a branch of natural science concerned with Earth and other astronomical objects, the features or rocks of which it is composed, and the processes by which they change over time. Modern geology significantly overlaps all other Earth sciences, including hydrology, and so is treated as one major aspect of integrated Earth system science and planetary science. Geology describes the structure of the Earth on and beneath its surface, and the processes that have shaped that structure. It also provides tools to determine the relative and absolute ages of rocks found in a given location, and also to describe the histories of those rocks. By combining these tools, geologists are able to chronicle the geological history of the Earth as a whole, and also to demonstrate the age of the Earth. Geology provides the primary evidence for plate tectonics, the evolutionary history of life, and the Earth's past climates. Geologists broadly study the properties and processes of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Enns
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] |
Flysch
Flysch () is a sequence of sedimentary rock layers that progress from deep-water and turbidity flow deposits to shallow-water shales and sandstones. It is deposited when a deep basin forms rapidly on the continental side of a mountain building episode. Examples are found near the North American Cordillera, the Alps, the Pyrenees and the Carpathians. Sedimentological properties Flysch consists of repeated sedimentary cycles with upwards fining of the sediments. There are sometimes coarse conglomerates or breccias at the bottom of each cycle, which gradually evolve upwards into sandstone and shale/mudstone. Flysch typically consists of a sequence of shales rhythmically interbedded with thin, hard, graywacke-like sandstones. Typically the shales do not contain many fossils, while the coarser sandstones often have fractions of micas and glauconite. Tectonics In a continental collision, a subducting tectonic plate pushes on the plate above it, making the rock fold, often to t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Schneeberg (Lower Austria)
The Schneeberg, with its high summit ''Klosterwappen'', is the highest mountain of Lower Austria, and the easternmost and northernmost mountain in the Alps to exceed 2000 m. It is a distinctive limestone massif with steep slopes on three sides. The Schneeberg is one of the Northern Calcareous Alps in the borderland between Lower Austria and Styria, in the eastern part of Austria. It and the Rax (), some to the south-west, are collectively considered the Viennese Hausberge (Vienna's "local mountains"). The rich Karst plateaux have provided drinking water for Vienna, via a long pipeline, since 1873, and is claimed to be the best drinking water in the world. On clear days, Schneeberg can be readily seen from parts of Vienna, some away (as the crow flies), from Bratislava in Slovakia and even from Babí Lom above Brno 180 km away. The Schneeberg is a summit with a height of over 1500 m, which just misses the limit for an ultra-prominent peak (1500). A rack-and-pinion r ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
