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Gutenstein Alps
The Gutenstein Alps () 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 (Leitha), 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 (river), 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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lower Austria
Lower Austria ( , , abbreviated LA or NÖ) is one of the nine states of Austria, located in the northeastern corner of the country. Major cities are Amstetten, Lower Austria, Amstetten, Krems an der Donau, Wiener Neustadt and Sankt Pölten, which has been the capital city, capital of Lower Austria since 1986, replacing Vienna, which became a separate state in 1921. With a land area of and a population of 1.7 million people, Lower Austria is the largest and second-most-populous state in Austria (after Vienna). 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 river Enns (river), Enns, which flows from the west to the east. Lower Austria has an international border, long, with the Czech Republic (South Bohemian Region, South Bohemia and South Moravian Region, South Moravia) and Slovakia (Bratislava Region, Bratislava and Trnava Regions). The state has the ... [...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 M ... [...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 Lower Austria ( , , abbreviated LA or NÖ) is one of the nine states of Austria, located in the northeastern corner of the country. Major cities are Amstetten, Lower Austria, Amstetten, Krems an der Donau, Wiener Neustadt and Sankt Pölten, which .... Population See also * Burgruine Starhemberg 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 () 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 dripstones of the gui ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cretaceous
The Cretaceous ( ) is a geological period that lasted from about 143.1 to 66 mya (unit), million years ago (Mya). It is the third and final period of the Mesozoic Era (geology), Era, as well as the longest. At around 77.1 million years, it is the ninth and longest geological period of the entire Phanerozoic. The name is derived from the Latin , 'chalk', which is abundant in the latter half of the period. It is usually abbreviated K, for its German translation . The Cretaceous was a period with a relatively warm climate, resulting in high Sea level#Local and eustatic, eustatic sea levels that created numerous shallow Inland sea (geology), 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 largely ice-free, although there is some evidence of brief periods of glaciation during the cooler first half, and forests extended to the poles. Many of the dominant taxonomic gr ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Conglomerate Rock
Conglomerate () is a sedimentary rock made up of rounded gravel-sized pieces of rock surrounded by finer-grained sediments (such as sand, silt, or clay). The larger fragments within conglomerate are called clasts, while the finer sediment surrounding the clasts is called the matrix. The clasts and matrix are typically cemented by calcium carbonate, iron oxide, silica, or hardened clay. Conglomerates form when rounded gravels deposited by water or glaciers become solidified and cemented by pressure over time. 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. They are closely related to sandstones in origin, and exhibit many of the same types of sedimentary structures, such as 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 sedim ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Stratum
In geology and related fields, a stratum (: strata) is a layer of rock or sediment characterized by certain lithologic properties or attributes that distinguish it from adjacent layers from which it is separated by visible surfaces known as either '' bedding surfaces'' or ''bedding planes''.Salvador, A. ed., 1994. ''International stratigraphic guide: a guide to stratigraphic classification, terminology, and procedure. 2nd ed.'' Boulder, Colorado, The Geological Society of America, Inc., 215 pp. . Prior to the publication of the International Stratigraphic Guide, older publications have defined a stratum as being either equivalent to a single bed or composed of a number of beds; as a layer greater than 1 cm in thickness and constituting a part of a bed; or a general term that includes both ''bed'' and '' lamina''.Neuendorf, K.K.E., Mehl, Jr., J.P., and Jackson, J.A. , eds., 2005. ''Glossary of Geology'' 5th ed. Alexandria, Virginia, American Geological Institute. 779 pp. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Triassic
The Triassic ( ; sometimes symbolized 🝈) is a geologic period and system which spans 50.5 million years from the end of the Permian Period 251.902 million years ago ( Mya), to the beginning of the Jurassic Period 201.4 Mya. The Triassic is the first and shortest period of the Mesozoic Era and the seventh period of the Phanerozoic Eon. 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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dolomite (rock)
Dolomite (also known as dolomite rock, dolostone or dolomitic rock) is a sedimentary rock, sedimentary carbonate rock that contains a high percentage of the mineral Dolomite (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). One of the first geologists to distinguish dolomite from limestone was Déodat Gratet de Dolomieu, a French mineralogist and geologist after whom it is named. He recognized and described the distinct characteristics of dolomite in the late 18th century, differentiating it from limestone. Most dolomite was formed as a magnesium replacement of limestone or of Lime (mineral), 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 v ... [...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''; ) 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 town has a long tradition in the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Limestone
Limestone is a type of carbonate rock, carbonate sedimentary rock which is the main source of the material Lime (material), lime. It is composed mostly of the minerals calcite and aragonite, which are different Polymorphism (materials science), crystal forms of calcium carbonate . Limestone forms when these minerals Precipitation (chemistry), 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 (rock), dolomite, a closely related rock, which contains a high percentage of the mineral Dolomite (mine ... [...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 Gutenstein Alps. 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 Gutenstein Alps 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 Lower Austria ( , , abb ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
