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Gutenstein Alps
The Gutenstein Alps (german: Gutensteiner Alpen) are a mountain range in the Eastern Alps in Central Europe, and the northeasternmost part of the Northern Limestone Alps, reaching heights over 1,000 m. Topography Die Gutenstein Alps are separated in the north from the Vienna Woods by the valleys of the Gölsen and Triesting. In the east they descend to the Vienna Basin. Their boundary with the Rax-Schneeberg Group to the south is formed by the valley of the Sierningbach between Ternitz and Puchberg am Schneeberg, the saddle near the Mamauwiese and the Voisbach and Schwarza valleys. To the west, from the Seebach stream near St. Aegyd am Neuwalde, the boundary with the Türnitz Alps runs along the Unrecht Traisen and the Traisen. The highest elevations in the Gutenstein Alps are, from west to east: * Kloster-Hinteralpe (1311 m) and the Muckenkogel (1248 m) * Reisalpe (1399 m) and Hochstaff (1305 m) * Handlesberg (1370 m) near Schwarzau im Gebir ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lower Austria
Lower Austria (german: Niederösterreich; Austro-Bavarian: ''Niedaöstareich'', ''Niedaestareich'') is one of the nine states of Austria, located in the northeastern corner of the country. Since 1986, the capital of Lower Austria has been Sankt Pölten, replacing Vienna which became a separate state in 1921. With a land area of and a population of 1.685 million people, Lower Austria is the second most populous state in Austria (after Vienna). Other large cities are Amstetten, Klosterneuburg, Krems an der Donau, Stockerau and Wiener Neustadt. Geography With a land area of situated east of Upper Austria, Lower Austria is the country's largest state. Lower Austria derives its name from its downriver location on the Enns River which flows from the west to the east. Lower Austria has an international border, long, with the Czech Republic (South Bohemia and South Moravia Regions) and Slovakia (Bratislava and Trnava Regions). The state has the second longest external border of all A ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Unterberg (Lower Austria)
The Unterberg is a prominent summit, high, in the Gutenstein Alps in southern Lower Austria. It is located about 10 km south of Hainfeld and is the westernmost and highest summit of a loose chain of mountains that include the Hocheck (1,037 m) and the Kieneck (1,106 m). Its crest continues towards the southwest, albeit less high, to the Brunntaler Höhe (1,090 m) and the Leitermauern (1,025 m). In a field on the summit there is a chapel with the name of ''Maria Einsiedl''. The mountain is made of limestone rock and has a steep, wooded face to the northwest which is pierced by crags, whilst to the southeast it falls away only half as sharply. About 150 metres in height below the summit is the mountain hut of ''Unterberghaus''. It is a local winter sports centre with several ski pistes and is popular in spring for ski mountaineering. The ski lift runs up the southeastern flank to the top and may be reached from Pernitz in the Piesting valley via Mugge ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dreistetten
Markt Piesting is a municipality in the district of Wiener Neustadt-Land in the Austrian state of Lower Austria. Population See also * Burgruine Starhemberg Burgruine Starhemberg was a castle in Lower Austria, Austria. Built in the 1140s, the castle fell into ruins by the late 19th century. Burgruine Starhemberg is above sea level. History The name is derived from the original name of 'high mounta ... References Cities and towns in Wiener Neustadt-Land District Starhemberg family {{LowerAustria-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Unicorn Cave (Austria)
The Unicorn Cave (german: Einhornhöhle) in Austria is situated in the Hohe Wand Nature Park near Dreistetten in Lower Austria and may be reached on signposted hiking trails in ca. 20 minutes from Dreistetten (typical signpost illustrated). The cave was discovered in 1927 by Otto Langer senior and opened as a show cave in 1930. In 1964 the structures built by Otto Langer junior were modernised. Guided tours that take about 20 minutes are laid on from Easter to the end of September on Sundays and public holidays. Overview The guided tour leads first along an artificially-created gallery into the cave. Its natural entrance is located above the current man-made entrance and is visible from the present-day pathway. A hut has been built in front of the artificial gallery through which the gallery entrance is accessed. Inside the cave the tour leads initially down a side tunnel and then along the main corridor to the first squeeze. In the hall in front of this constriction, the largest dr ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cretaceous
The Cretaceous ( ) is a geological period that lasted from about 145 to 66 million years ago (Mya). It is the third and final period of the Mesozoic Era, as well as the longest. At around 79 million years, it is the longest geological period of the entire Phanerozoic. The name is derived from the Latin ''creta'', "chalk", which is abundant in the latter half of the period. It is usually abbreviated K, for its German translation ''Kreide''. The Cretaceous was a period with a relatively warm climate, resulting in high eustatic sea levels that created numerous shallow inland seas. These oceans and seas were populated with now- extinct marine reptiles, ammonites, and rudists, while dinosaurs continued to dominate on land. The world was ice free, and forests extended to the poles. During this time, new groups of mammals and birds appeared. During the Early Cretaceous, flowering plants appeared and began to rapidly diversify, becoming the dominant group of plants across the Earth b ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Conglomerate Rock
Conglomerate () is a clastic sedimentary rock that is composed of a substantial fraction of rounded to subangular gravel-size clasts. A conglomerate typically contains a matrix of finer-grained sediments, such as sand, silt, or clay, which fills the interstices between the clasts. The clasts and matrix are typically cemented by calcium carbonate, iron oxide, silica, or hardened clay. Conglomerates form by the consolidation and lithification of gravel. They can be found in sedimentary rock sequences of all ages but probably make up less than 1 percent by weight of all sedimentary rocks. In terms of origin and depositional mechanisms, they are closely related to sandstones and exhibit many of the same types of sedimentary structures, e.g., tabular and trough cross-bedding and graded bedding.Boggs, S. (2006) ''Principles of Sedimentology and Stratigraphy.'', 2nd ed. Prentice Hall, New York. 662 pp. Friedman, G.M. (2003) ''Classification of sediments and sedimentary rocks.'' In Ger ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Layering
Layering has evolved as a common means of vegetative propagation of numerous species in natural environments. Layering is also utilized by horticulturists to propagate desirable plants. Natural layering typically occurs when a branch touches the ground, whereupon it produces adventitious roots. At a later stage the connection with the parent plant is severed and a new plant is produced as a result. The horticultural layering process typically involves wounding the target region to expose the inner stem and optionally applying rooting compounds. In ground layering or simple layering, the stem is bent down and the target region is buried in the soil. This is done in plant nurseries in imitation of natural layering by many plants such as brambles which bow over and touch the tip on the ground, at which point it grows roots and, when separated, can continue as a separate plant. In either case, the rooting process may take from several weeks to a year. Layering is more complicate ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Triassic
The Triassic ( ) is a geologic period and system which spans 50.6 million years from the end of the Permian Period 251.902 million years ago ( Mya), to the beginning of the Jurassic Period 201.36 Mya. The Triassic is the first and shortest period of the Mesozoic Era. Both the start and end of the period are marked by major extinction events. The Triassic Period is subdivided into three epochs: Early Triassic, Middle Triassic and Late Triassic. The Triassic began in the wake of the Permian–Triassic extinction event, which left the Earth's biosphere impoverished; it was well into the middle of the Triassic before life recovered its former diversity. Three categories of organisms can be distinguished in the Triassic record: survivors from the extinction event, new groups that flourished briefly, and other new groups that went on to dominate the Mesozoic Era. Reptiles, especially archosaurs, were the chief terrestrial vertebrates during this time. A specialized subgroup of archo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dolomite (rock)
Dolomite (also known as dolomite rock, dolostone or dolomitic rock) is a sedimentary carbonate rock that contains a high percentage of the mineral dolomite, CaMg(CO3)2. It occurs widely, often in association with limestone and evaporites, though it is less abundant than limestone and rare in Cenozoic rock beds (beds less than about 66 million years in age). The first geologist to distinguish dolomite rock from limestone was Belsazar Hacquet in 1778. Most dolomite was formed as a magnesium replacement of limestone or of lime mud before lithification. The geological process of conversion of calcite to dolomite is known as dolomitization and any intermediate product is known as dolomitic limestone. The "dolomite problem" refers to the vast worldwide depositions of dolomite in the past geologic record in contrast to the limited amounts of dolomite formed in modern times. Recent research has revealed sulfate-reducing bacteria living in anoxic conditions precipitate dolomite which ind ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gutenstein Limestone
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Gutenstein may mean: *A district of the city of Sigmaringen: Gutenstein (Sigmaringen) *A municipality in Lower Austria: Gutenstein, Austria *The German name for the Slovenian town of Ravne na Koroškem Ravne na Koroškem (; until 1952: ''Guštanj''; german: Gutenstein in Kärnten) is a town in northern Slovenia. It is the seat of the Municipality of Ravne na Koroškem, and the largest town and the capital of Slovenia's Carinthia region. The tow ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Limestone
Limestone ( calcium carbonate ) is a type of carbonate sedimentary rock which is the main source of the material lime. It is composed mostly of the minerals calcite and aragonite, which are different crystal forms of . Limestone forms when these minerals precipitate out of water containing dissolved calcium. This can take place through both biological and nonbiological processes, though biological processes, such as the accumulation of corals and shells in the sea, have likely been more important for the last 540 million years. Limestone often contains fossils which provide scientists with information on ancient environments and on the evolution of life. About 20% to 25% of sedimentary rock is carbonate rock, and most of this is limestone. The remaining carbonate rock is mostly dolomite, a closely related rock, which contains a high percentage of the mineral dolomite, . ''Magnesian limestone'' is an obsolete and poorly-defined term used variously for dolomite, for limes ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Piesting
The Piesting is a river in southern Lower Austria. A left tributary of the Fischa, its drainage basin is . The sources of the Piesting are the Kalte Gang, the , and the Längapiesting, which begin south of the Schneeberg. These rivers meet in Gutenstein in the Vienna Woods. From there the Piesting flows east through Markt Piesting and Wöllersdorf and into the Viennese Basin. The tributary Myrabach discharges at Pernitz into the Piesting. Between the () in the north and the () in the south, the Piesting breaks through the , a rocky ravine, and flows further eastwards through Markt Piesting and Wöllersdorf into the Vienna Basin. Near Gramatneusiedl the Piesting discharges into the Fischa. The valley west of the (the thermal line at the Vienna Basin) in the Vienna Woods is known as the Piesting Valley. See also * Markt Piesting Markt Piesting is a municipality in the district of Wiener Neustadt-Land in the Austrian state of Lower Austria. Population See also * Burgr ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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