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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] |
Stainach
Stainach is a former municipality in the district of Liezen in the Austrian state of Styria. Since the 2015 Styria municipal structural reform The Styria municipal structural reform (German: ''Steiermärkische Gemeindestrukturreform'') was a local government reform in the Austrian state of Styria, which was made effective January 1, 2015. This reform nearly halved the number of Styrian ..., it is part of the municipality Stainach-Pürgg. Geography Stainach lies in the Enns valley. References Cities and towns in Liezen District {{Styria-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
West Slavic Languages
The West Slavic languages are a subdivision of the Slavic language group. They include Polish, Czech, Slovak, Kashubian, Upper Sorbian and Lower Sorbian. The languages have traditionally been spoken across a mostly continuous region encompassing the Czech Republic, Slovakia, Poland, the westernmost regions of Ukraine and Belarus, and a bit of eastern Lithuania. In addition, there are several language islands such as the Sorbian areas in Lusatia in Germany, and Slovak areas in Hungary and elsewhere. Classification West Slavic is usually divided into three subgroups— Czecho-Slovak, Lechitic and Sorbian—based on similarity and degree of mutual intelligibility. The groupings are as follows: Some linguists include Upper and Lower Sorbian in the Lechitic branch, but other linguists regard it as a separate branch. The reason for this is that 'the Sorbian dialects are extremely diverse, and there are virtually no linguistic features common to all Sorbian dialects which ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ennstaler Alpen
, photo=HochtorOedsteinGroup FromS HoherZinken.jpg , photo_caption=Hochtor - Ödstein Group (Gesäuse) (from right to left) as seen from Hoher Zinken in the south , country= Austria , subdivision1_type=States , subdivision1= , parent= Northern Limestone Alps , length_mi= , length_orientation= , width_mi= , width_orientation= , geology= , orogeny= , highest= Hochtor , elevation_m=2369 , coordinates= , range_coordinates= , map_image=Alps location map (Ennstaler Alpen, AVE).png , map_caption=Ennstal Alps (in red) within the Alps.The borders of the range according toAlpine Club classification of the Eastern Alps The Ennstal Alps (German ''Ennstaler Alpen''), the Alps of the Enns valley, are a mountain range of the Northern Limestone Alps System. They are located primarily in the Austrian state of Styria, and also into the state of Upper Austria. The most famous scenery in the Ennstal Alps is the Gesäuse, a valley where the Enns river cuts through the limeston ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Canyon
A canyon (from ; archaic British English spelling: ''cañon''), or gorge, is a deep cleft between escarpments or cliffs resulting from weathering and the erosive activity of a river over geologic time scales. Rivers have a natural tendency to cut through underlying surfaces, eventually wearing away rock layers as sediments are removed downstream. A river bed will gradually reach a baseline elevation, which is the same elevation as the body of water into which the river drains. The processes of weathering and erosion will form canyons when the river's headwaters and estuary are at significantly different elevations, particularly through regions where softer rock layers are intermingled with harder layers more resistant to weathering. A canyon may also refer to a rift between two mountain peaks, such as those in ranges including the Rocky Mountains, the Alps, the Himalayas or the Andes. Usually, a river or stream carves out such splits between mountains. Examples of mountain-type ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Admont
Admont is a town in the Austrian state of Styria. It is historically most notable for Admont Abbey, a monastery founded in 1074. Gesäuse National Park, in which Admont lies, is an area of outstanding beauty. The town is situated in the middle of the Ennstal Alps, in the valley of the 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, .... Geography References External links Official site Cities and towns in Liezen District {{Styria-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dachstein
Hoher Dachstein () is a strongly karstic mountain in central Austria and the second-highest mountain in the Northern Limestone Alps. It is situated at the border of Upper Austria and Styria, and is the highest point in each of those states. Parts of the massif also lie in the state of Salzburg, leading to the mountain being referred to as the ''Drei-Länder-Berg'' ("three-state mountain"). The Dachstein massif covers an area of around with dozens of peaks above 2,500 m, the highest of which are in the southern and southwestern areas. The main summit of the Hoher Dachstein is at an elevation of . Seen from the north, the Dachstein massif is dominated by glaciers with rocky summits rising beyond them. By contrast, to the south, the mountain drops almost vertically to the valley floor. Geology The geology of the Dachstein massif is dominated by the ''Dachstein-Kalk'' Formation ("Dachstein limestone"), dating from Triassic times. In common with other karstic areas, the Dachs ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 the south by Slovenia, and clockwise, from the southwest, by the Austrian states of Carinthia, Salzburg, Upper Austria, Lower Austria, and Burgenland. The state capital is Graz. Etymology The March of Styria derived its name from the original seat of its ruling Otakar dynasty: Steyr, in today's Upper Austria. In German, the area is still called "Steiermark" while in English the Latin name "Styria" is used. The ancient link between Steyr and Styria is also apparent in their nearly identical coats of arms, a white Panther on a green background. Geography * The term " Upper Styria" (german: Obersteiermark) refers to the northern and northwestern parts of the federal-state (districts Liezen, Murau, Murtal, Leoben, Bruck-Mürz ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Central Eastern Alps
The Central Eastern Alps (german: Zentralalpen or Zentrale Ostalpen), also referred to as Austrian Central Alps (german: Österreichische Zentralalpen) or just Central Alps, comprise the main chain of the Eastern Alps in Austria and the adjacent regions of Switzerland, Liechtenstein, Italy and Slovenia. South them is the Southern Limestone Alps. The term "Central Alps" is very common in the Geography of Austria as one of the seven major landscape regions of the country. "Central Eastern Alps" is usually used in connection with the Alpine Club classification of the Eastern Alps (''Alpenvereinseinteilung'', AVE). The Central Alps form the eastern part of the Alpine divide, its central chain of mountains, as well as those ranges that extend or accompany it to the north and south. The highest mountain in the Austrian Central Alps is Grossglockner at . Location The Central Alps have the highest peaks of the Eastern Alps, and are located between the Northern Limestone Alps and t ... [...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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ice Age
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 Quaternary glaciation. Individual pulses of cold climate within an ice age are termed '' glacial periods'' (or, alternatively, ''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, ''ice age'' implies the presence of extensive ice sheets in both northern and southern hemispheres. By this definition, Earth is currently in an interglacial period—the Holocene. The amount of anthropogenic greenhouse gases emitted into Earth's oceans and atmosphere is predicted to prevent the next glacial period for ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Salzburg (state)
Salzburg (, ; bar, Soizbuag, label=Austro-Bavarian) (also known as ''Salzburgerland'') is a state (''Land'') of the modern Republic of Austria. It is officially named ''Land Salzburg'' to distinguish it from its eponymous capital — the city of Salzburg. For centuries, it was an independent Prince-Bishopric of the Holy Roman Empire. Geography Location The state of Salzburg covers area of . It stretches along its main river — the Salzach – which rises in the Central Eastern Alps in the south to the Alpine foothills in the north. It is located in the north-west of Austria, close to the border with the German state of Bavaria; to the northeast lies the state of Upper Austria; to the east the state of Styria; to the south the states of Carinthia and Tyrol. With 529,085 inhabitants, it is one of the country's smaller states in terms of population. Running through the south are the main ranges of the Alpine divide (incl. the Hohe Tauern mountains) with numerous three-thousan ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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