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Bucklige Welt
The Bucklige Welt is a region in southeast Lower Austria. It is also known as the "land of a thousand hills" (''Land der 1000 Hügel''). Geography The Bucklige Welt is a hill country area on the eastern edge of the Alps. Its height varies between 375 and . Its name, which means something like 'hilly world', is due to the very large number of hills and mountains which are known by the locals as ''Buckln''. In the southwest the Bucklige Welt is bounded by the ''Wechsel'' massif and in the west by the '' Semmering region''. To the north it descends into the ''Vienna Basin'', into which it is drained by the Pitten. To the east the ''Rosalia Mountains'' form the boundary, to the south of which the Bucklige Welt faces Oberpullendorf in the ''Central Burgenland Bay''. To the south is the ''Geschriebenstein''. There was no glaciation during the ice age in the area of the Bucklige Welt because of its low elevation. The summit of the Hochwechsel must therefore only have a slight co ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Krumbach, Lower Austria
Krumbach is a market town in southern Lower Austria, Austria. It is part of the landscape Bucklige Welt. History Archaeological artifacts from the Stone Age, the Bronze Age and the Roman times In modern historiography, ancient Rome is the Roman civilisation from the founding of the Italian city of Rome in the 8th century BC to the collapse of the Western Roman Empire in the 5th century AD. It encompasses the Roman Kingd ... have been found in the area. In 1182, Krumbach was mentioned for the first time in writing. The present castle Schloss Krumbach was erected in the 13th century. In 1394 Hans von Chrumbach, the last Lord of Krumbach, died and left the castle to his maternal uncle. In the 17th and 18th centuries, the Bubonic plague, plague and the cholera affected Krumbach. In 1854, it became a market town. In 1884, Krumbach opened a fire station. It has a post office, a school (Volksschule Krumbach), a high school (Hauptschule Krumbach) and a church. Mayor ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geschriebenstein
The Geschriebenstein (), less commonly called the Írott-kő () in English sources, is a mountain, high,''Geschriebenstein, Austria/Hungary'' at www.peakbagger.com. Retrieved 6 Jun 2017. located on the border between Austria and Hungary. It is the highest mountain of the Kőszeg Mountains, the highest point in western Hungary (Transdanubia) and highest point in the Burgenland. Its height is according to Austrian sources, whereas Hungarian references mostly mention . The highest point on the Burgenland side of the border is (). Its former Hungarian names were ''Fenyőhegy'' and ''Szálkő''. Its present name (''Írottkő'' in Hungarian, ''Geschriebenstein'' in English and German) can be translated as ''written stone'' and is assumably derived from border stones with inscriptions between the properties o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Neunkirchen District, Austria
Bezirk Neunkirchen () is a district of the state of Lower Austria in Austria. It is located at the south of the state. Municipalities * Altendorf :Parts of the village: Altendorf, Loitzmannsdorf, Schönstadl, Syhrn, Tachenberg *Aspang-Markt * Aspangberg-Sankt Peter :Parts of the village: Großes Amt, Kleines Amt, Neustift am Alpenwald, Neuwald * Breitenau * Breitenstein * Buchbach * Bürg-Vöstenhof :Parts of the village: Bürg, Vöstenhof * Edlitz * Enzenreith :Parts of the village: Enzenreith, Hart, Hilzmannsdorf, Köttlach, Thürmannsdorf, Wörth *Feistritz am Wechsel :Parts of the village: Feistritz am Wechsel, Grottendorf, Hasleiten, Hollabrunn *Gloggnitz :Parts of the town: Abfaltersbach, Aue, Berglach, Eichberg, Gloggnitz (with Furth and Gföhl), Graben, Heufeld, Saloder, Stuppach, Weißenbach * Grafenbach-Sankt Valentin :Parts of the village: Göttschach, Grafenbach, Ober-Danegg, Penk, St. Valentin-Landschach * Grimmenstein :Parts of the village: Grimmenstein, Hochegg *Grü ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Regions Of Austria
Austria is a federal republic consisting of nine federal states. The European Commission calls them provinces. Austrian federal states can pass laws that stay within the limits of the constitution, and each federal state has representatives in the main Austrian parliament. Geography The majority of the land area in the federal states of Upper Austria, Lower Austria, Vienna, and Burgenland is situated in the Danube valley and thus consists almost completely of accessible and easily arable terrain. Austria's most densely populated federal state is Vienna, the heart of what is Austria's only metropolitan area. Lower Austria ranks only fourth in population density even though it contains Vienna's suburbs; this is due to large areas of land being predominantly agricultural. The alpine federal state Tyrol, the less alpine but geographically more remote federal state Carinthia, and the non-alpine but near-exclusively agricultural federal state Burgenland are Austria's least densely pop ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountain Ranges Of The Alps
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain and climate, mountains ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bucklige Welt
The Bucklige Welt is a region in southeast Lower Austria. It is also known as the "land of a thousand hills" (''Land der 1000 Hügel''). Geography The Bucklige Welt is a hill country area on the eastern edge of the Alps. Its height varies between 375 and . Its name, which means something like 'hilly world', is due to the very large number of hills and mountains which are known by the locals as ''Buckln''. In the southwest the Bucklige Welt is bounded by the ''Wechsel'' massif and in the west by the '' Semmering region''. To the north it descends into the ''Vienna Basin'', into which it is drained by the Pitten. To the east the ''Rosalia Mountains'' form the boundary, to the south of which the Bucklige Welt faces Oberpullendorf in the ''Central Burgenland Bay''. To the south is the ''Geschriebenstein''. There was no glaciation during the ice age in the area of the Bucklige Welt because of its low elevation. The summit of the Hochwechsel must therefore only have a slight co ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geologische Bundesanstalt
The Geological Survey of Austria (, GBA) in Vienna is a subordinate agency of the Federal Ministry of Education, Science and Research and is the central point for information and advice in the field of earth sciences for the Republic of Austria. The most important product of the GBA is a range of geological maps. These appear in various scale (map), scales both as map series and as regional maps. They form the basis for responses to questions in many areas of business (waste disposal, water supply, transportation, raw materials, geothermal energy …) and also for research. The GBA is located in the district of Landstraße in Vienna. Sources * Geologische Bundesanstalt (Hrsg.): ''Die Geologische Bundesanstalt in Wien.'' Böhlau-Verlag, Wien 1999. * Hans Georg Krenmayr (Red.): ''ROCKY AUSTRIA - Eine bunte Erdgeschichte von Österreich.'' Wien 2002. * Thomas Hofmann, Hans P. Schönlaub (Hrsg.): ''Geo-Atlas Österreich. Die Vielfalt des geologischen Untergrunds.'' 1. Auflage, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Firn
__NOTOC__ Firn (; from Swiss German "last year's", cognate with ''before'') is partially compacted névé, a type of snow that has been left over from past seasons and has been recrystallized into a substance denser than névé. It is ice that is at an intermediate stage between snow and glacial ice. Firn has the appearance of wet sugar, but has a hardness that makes it extremely resistant to shovelling. Its density generally ranges from 0.35 g/cm3 to 0.9 g/cm3, and it can often be found underneath the snow that accumulates at the head of a glacier. Snowflakes are compressed under the weight of the overlying snowpack. Individual crystals near the melting point are semiliquid and slick, allowing them to glide along other crystal planes and to fill in the spaces between them, increasing the ice's density. Where the crystals touch, they bond together, squeezing the air between them to the surface or into bubbles. In the summer months, the crystal metamorphosis can occur ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Height Above Sea Level
Height above mean sea level is a measure of a location's vertical distance (height, elevation or altitude) in reference to a vertical datum based on a historic mean sea level. In geodesy, it is formalized as orthometric height. The zero level varies in different countries due to different reference points and historic measurement periods. Climate change and other forces can cause sea levels and elevations to vary over time. Uses Elevation or altitude above sea level is a standard measurement for: * Geographic locations such as towns, mountains and other landmarks. * The top of buildings and other structures. * Mining infrastructure, particularly underground. * Flying objects such as airplanes or helicopters below a Transition Altitude defined by local regulations. Units and abbreviations Elevation or altitude is generally expressed as "metres above mean sea level" in the metric system, or " feet above mean sea level" in United States customary and imperial units. Common ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cenozoic Ice Age
The Late Cenozoic Ice Age,National Academy of Sciences - The National Academies Press - Continental Glaciation through Geologic Times https://www.nap.edu/read/11798/chapter/8#80 or Antarctic Glaciation, began 34 million years ago at the Eocene-Oligocene Boundary and is ongoing. It is Earth's current ice age or icehouse period. Its beginning is marked by the formation of the Antarctic ice sheets. Six million years after the start of the Late Cenozoic Ice Age, the East Antarctic Ice Sheet had formed, and 14 million years ago it had reached its current extent. In the last three million years, glaciations have spread to the northern hemisphere. It commenced with Greenland becoming increasingly covered by an ice sheet in late Pliocene (2.9-2.58 Ma ago) During the Pleistocene Epoch (starting 2.58 Ma ago), the Quaternary glaciation developed with decreasing mean temperatures and increasing amplitudes between glacials and interglacials. During the glacial periods of the Pleistocene, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Glaciation
A glacial period (alternatively glacial or glaciation) is an interval of time (thousands of years) within an ice age that is marked by colder temperatures and glacier advances. Interglacials, on the other hand, are periods of warmer climate between glacial periods. The Last Glacial Period ended about 15,000 years ago. The Holocene is the current interglacial. A time with no glaciers on Earth is considered a greenhouse climate state. Quaternary Period Within the Quaternary, which started about 2.6 million years before present, there have been a number of glacials and interglacials. At least eight glacial cycles have occurred in the last 740,000 years alone. Changes in atmospheric and associated radiative forcing were among the primary drivers of globally cold glacial and warm interglacial climates, with changes in ocean physical circulation, biological productivity and seawater acid-base chemistry likely causing most of the recorded changes Penultimate Glacial Period The ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Oberpullendorf
Oberpullendorf (; or ; ) is a town in Burgenland, Austria. It is the administrative center of the district of Oberpullendorf (district), Oberpullendorf. Geography Oberpullendorf is a municipality in the middle of the Burgenland. It consists of two united communities: Mitterpullendorf and Oberpullendorf, and is also the capital of the same called administrative district of Oberpullendorf. It is surrounded by the communities of Stoob to the north, Großwarasdorf to the east, Frankenau-Unterpullendorf to the south, and Steinberg-Dörfl to the west. The Stooberbach crosses the municipality from north-west to the south-east. History The district of Oberpullendorf has been populated since the Neolithic age. During the early Iron Age the district was a flourishing iron industrial area. Josef Polatschek, a gardener and regional researcher, mapped several ancient iron extraction sites in the district. Oberpullendorf was firstly documented in 1225 as a Hungarian frontier guard set ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
