Dreisesselberg (Bavarian Forest)
The Dreisesselberg (Czech: ''Třístoličník'') is a mountain in Bavaria, Germany, in the Bavarian Forest that is 1,333 metres high. Location The Dreisesselberg is located in the eastern part of Lower Bavaria in the county of Freyung-Grafenau. It rises southeast of the village of Haidmühle and northeast of the village of Neureichenau. The Czech border runs some 370 metres southeast of the summit of the Dreisesselberg. The tripoint between Germany, Austria and the Czech Republic lies not far from the summit of the Plöckenstein, about 3 kilometres southeast of the Dreisesselberg ( as the crow flies). Description At the highest point of the most heavily forested mountain of Dreisessel, called Hochstein, is a distinctive granite rock with a summit cross, from which one can enjoy the view. Approximately 450 metres due south of the Dreisesselberg's summit is the Dreisesselfels, three bizarre granite rock formations, with pillow-like shaped rocks formed by woolsack weat ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
|
Bavarian Forest
image:Zell-bayerischer-wald.jpg, The village of Zell in the Bavarian Forest The Bavarian Forest ( or ''Bayerwald'' ; ) is a wooded, low-mountain region in Bavaria, Germany, that is about 100 kilometres long. It runs along the Czech Republic, Czech border and is continued on the Czech side by the Bohemian Forest (Czech: ''Šumava''). Most of the Bavarian Forest lies within the province of Lower Bavaria, but the northern part lies within the Upper Palatinate. In the south it reaches the border with Upper Austria. Geologically and geomorphologically, the Bavarian Forest is part of the Bohemian Forest - the highest of the truncated highlands of the Bohemian Massif. The area along the Czech border has been designated as the Bavarian Forest National Park (240 km2), established in 1970 as the first national park in Germany. Another 3,008 km2 has been designated as the Bavarian Forest Nature Park, established 1967, and another 1,738 km2 as the Upper Bavarian Forest Natur ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
|
Bohemian Forest
The Bohemian Forest, known in Czech as () and in German as , is a low mountain range in Central Europe. Geographically, the mountains extend from Plzeň Region and the South Bohemian Region in the Czech Republic to Austria and Bavaria in Germany, and form the highest truncated uplands of the Bohemian Massif, up to 50 km wide. They create a natural border between the Czech Republic on one side and Austria and Germany on the other. Names and etymology For political reasons, the Czech and German sides have different names in both languages: in Czech, the Czech side is called and the Bavarian side ('Rear Bavarian Forest'), while in German, the Czech side is called ('Bohemian Forest') and the Bavarian side ('Bavarian Forest'). In Czech, is also used as a name for the entire region in Bohemia and Germany. The designation ' has been attested in the late 15th century in Antonio Bonfini's work . Folk etymology connects the name's origin with the Czech words , (literall ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
|
Mountains Of Bavaria
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]   |
|
Bavarian Forest Club
The Bavarian Forest Club (), or BWV, is a German club that promotes culture, local history and folklore, nature and landscape conservation, and walking in the Bavarian Forest. It has its head office in Zwiesel and is registered in the register of clubs and societies in the district office at Deggendorf (VR 10158). History The founder of the club was Anton Niederleuthner, senior judge in Passau. The foundation of the club in 1883 goes back to his meeting with foresters in Bodenmais. The Bavarian Forest Club was founded in Deggendorf Town Hall on 25 November 1883. The Bodenmais townsman, Bartholomäus Stölzl, was appointed as its first chairman. On 6 June 1885, Niederleuthner founded the Passau Branch, the club's first local branch. On 22 August he was elected the first president and made Passau the base of the club. He managed the club for over 20 years and founded over 40 other local branches. The club emblem used today goes back to Niederleuthner. A club magazine, ''Der Ba ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
|
Archduchy Of Austria
The Archduchy of Austria (; ) was a major Princes of the Holy Roman Empire, principality of the Holy Roman Empire and the nucleus of the Habsburg monarchy. With its capital at Vienna, the archduchy was centered at the Empire's southeastern periphery. Its present name originates from the Frankish term ''Oustrich'' – Eastern Kingdom (east of the Francia, Frankish kingdom). The archduchy developed out of the Bavarian Margraviate of Austria, elevated to the Duchy of Austria according to the 1156 ''Privilegium Minus'' by Emperor Frederick Barbarossa. The House of Habsburg came to the Austrian throne in Vienna in 1282 and in 1453 Emperor Frederick III, Holy Roman Emperor, Frederick III, also the ruler of Austria, officially adopted the archducal title. From the 15th century onward, all Holy Roman Emperors but Charles VII, Holy Roman Emperor, one were Austrian archdukes and with the acquisition of the Lands of the Bohemian Crown, Bohemian and Kingdom of Hungary (1526–1867), Hungarian ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
|
Bishopric Of Passau
The Diocese of Passau (; ) is a Latin diocese of the Catholic Church in Germany that is a suffragan of the Archdiocese of Munich and Freising."Diocese of Passau" '' Catholic-Hierarchy.org''. David M. Cheney. Retrieved February 29, 2016."Diocese of Passau" ''GCatholic.org''. Gabriel Chow. Retrieved February 29, 2016. The Prince-Bishopric of Passau was an ecclesiastical principality that existed for centuries until it was se ...
[...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
|
Geotope
A geotope is the geological component of the abiotic matrix present in an ecotope. Example geotopes might be an exposed outcrop of rocks, an erratic boulder, a grotto or ravine, a cave, an old stone wall marking a property boundary, and so forth. It is a loanword from German ''( Geotop)'' in the study of ecology and might be the model for many other similar words coined by analogy. As the prototype, it has enjoyed wider currency than many of the other words modelled on it, including physiotope, with which it is used synonymously. But the geotope is properly the rocks and not the whole lay of the land (which would be the physiotope). For usage in the context of geoheritage, like e.g. in Friedrich Wiedenbein's contributions (see below) and in the German discussion on geoheritage, the more adequate term (and translation from the German) is geosite. See also * Ecological land classification Ecological classification or ecological typology is the classification of land or water i ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
|
Bavarian Department Of The Environment
Bavarian is the adjective form of the German state of Bavaria, and refers to people of ancestry from Bavaria. Bavarian may also refer to: * Bavarii, a Germanic tribe * Bavarians, a nation and ethnographic group of Germans * Bavarian, Iran, a village in Fars Province * Bavarian language, a West Germanic language See also * * Bavaria (other) Bavaria may refer to: Places Germany * Bavaria, one of the 16 federal states of Germany * Duchy of Bavaria (–1805) * Electorate of Bavaria (1623–1805) * Kingdom of Bavaria (1805–1918) * Bavarian Soviet Republic (1919), a short-lived communi ... {{disambiguation Language and nationality disambiguation pages ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
|
Grossglockner
The Großglockner ( ), or just Glockner, is, at 3,798 metres above the Adriatic (12,461 ft), the highest mountain in Austria and highest mountain in the Alps east of the Brenner Pass. It is part of the larger Glockner Group of the Hohe Tauern range, situated along the main ridge of the Central Eastern Alps and the Alpine divide. The Pasterze, Austria's most extended glacier, lies on the Grossglockner's eastern slope. The characteristic pyramid-shaped peak actually consists of two pinnacles, the ''Großglockner'' and the Kleinglockner (, from German: ''groß'' 'big', ''klein'' 'small'), separated by the ''Glocknerscharte'' col. Etymology The name ''Glocknerer'' is first documented in a 1561 map designed by the Viennese cartographer Wolfgang Lazius. The denotation ''Glogger'' is mentioned in a 1583 description of the Tyrolean Kals legal district, then referring to the whole ridge south of the Alpine main chain. In the 1760s, the ''Atlas Tyrolensis'' listed a ''Glo ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
|
Glacial Lake
A glacial lake is a body of water with origins from glacier activity. They are formed when a glacier erodes the land and then melts, filling the depression created by the glacier. Formation Near the end of the last glacial period, roughly 10,000 years ago, glaciers began to retreat. A retreating glacier often left behind large deposits of ice in hollows between drumlins or hills. As the ice age ended, these melted to create lakes. These lakes are often surrounded by drumlins, along with other evidence of the glacier such as moraines, eskers and erosional features such as glacial striations, striations and chatter marks. These lakes are clearly visible in aerial photos of landforms in regions that were glaciated during the last ice age. The formation and characteristics of glacial lakes vary between location and can be classified into glacial erosion lake, ice-blocked lake, moraine-dammed lake, other glacial lake, supraglacial lake, and subglacial lake. Glacial lakes and chan ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |