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Steinwald
The Steinwald is a mountain range up to in southern Germany and, at the same time, a nature park (''Steinwald Nature Park'') founded in 1970 with an area of in the province of Upper Palatinate, in North Bavaria. Geography Geographical location The Steinwald lies south of the Upper Franconian county town of Marktredwitz and north of Erbendorf in the district of Tirschenreuth. The Steinwald is separated from the Fichtelgebirge to the northwest by the Waldershof trough (''Waldershofer Senke'') and from the Upper Palatine Forest to the southeast by the Waldnaab-Wondreb-trough. Mountains and hills The mountains and hills in the range and in the Steinwald Nature Park include the following − in order of height in metres (m) above sea level (NN): Geology Like the Fichtelgebirge, the Steinwald consists mainly of granite. In the south and east it is surrounded by a basalt landscape of ''Kuppen'' - gentle, rounded summits - ( Kemnather Land, Nördlicher Steinwald), w ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fichtelgebirge
The Fichtel MountainsRandlesome, C. et al. (2011). ''Business Cultures in Europe'', 2nd ed., Routledge, Abingdon and New York, p. 52. . (german: Fichtelgebirge, cs, Smrčiny), form a small horseshoe-shaped mountain range in northeastern Bavaria, Germany. They extend from the valley of the Red Main River to the Czech border, a few foothills spilling over into the Czech Republic. They continue in a northeasterly direction as the Elster Mountains, and in a southeasterly direction as the Upper Palatine Forest. The Fichtel Mountains contain an important nature park, the Fichtel Mountain Nature Park, with an area of . Etymology The first person to write about the Fichtel Mountains, Matthias of Kemnath (actually Matthias Widmann, born 23 February 1429 in Kemnath) reported in 1476: ''Ein bergk, hoch, weitt, wolbekant ligt in Beiern, gnant der Fichtelberg'' ("A mountain, high, wide and well-known, lies in Bavaria, known as the Fichtelberg"). In descriptions of the border in 1499 and 15 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Platte (Steinwald)
At , the Platte is the highest mountain in the Steinwald, a forest in the Fichtel The Fichtel MountainsRandlesome, C. et al. (2011). ''Business Cultures in Europe'', 2nd ed., Routledge, Abingdon and New York, p. 52. . (german: Fichtelgebirge, cs, Smrčiny), form a small horseshoe-shaped mountain range in northeastern Bavaria ... mountain range in central Germany. The Platte is a popular walking destination, not least because of the Upper Palatinate Tower, which is located on its summit. It is climbable and offers good views of the surrounding region. The Upper Palatinate Tower The first Upper Palatinate Tower (''Oberpfalz Tower'') lasted from 1972 to 1998. The second tower was officially opened on 10 September 2000. It is of wood and steel construction and was designed by Ferdinand Lehner. It has a total height of 35 metres. The observation deck is 30 metres high and can be reached via a stairway with 150 steps. Walking Several footpaths lead to the Platte. The best- ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Upper Palatinate Tower
The Upper Palatinate Tower (german: Oberpfalzturm) is an observation tower on the high Platte mountain, the highest peak in the Steinwald and in Northern Upper Palatinate in southern Germany. The first solid observation tower was built in 1971/72 by the Steinwald Nature Park Authority from Steinwald spruce trees. Due to dilapidation it had to be demolished on 1 April 1998. The engineer, Ferdinand Lehner, from Tirschenreuth was then given the contract to design and build a new tower. On 10 September 2000 the new observation tower was opened. It is high and was made of larch plywood. The contract was let by the town of Erbendorf. The total cost of construction came to about DM 400,000 and was supported by grants from the European Union, the Free State of Bavaria, the district of Tirschenreuth and the surrounding towns and villages. From the observation platform there are views of the Fichtelgebirge, the Egerland, the Stiftland and over the Upper Palatine Forest The Uppe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Oberpfalzturm
The Upper Palatinate Tower (german: Oberpfalzturm) is an observation tower on the high Platte mountain, the highest peak in the Steinwald and in Northern Upper Palatinate in southern Germany. The first solid observation tower was built in 1971/72 by the Steinwald Nature Park Authority from Steinwald spruce trees. Due to dilapidation it had to be demolished on 1 April 1998. The engineer, Ferdinand Lehner, from Tirschenreuth was then given the contract to design and build a new tower. On 10 September 2000 the new observation tower was opened. It is high and was made of larch plywood. The contract was let by the town of Erbendorf. The total cost of construction came to about DM 400,000 and was supported by grants from the European Union, the Free State of Bavaria, the district of Tirschenreuth and the surrounding towns and villages. From the observation platform there are views of the Fichtelgebirge, the Egerland, the Stiftland and over the Upper Palatine Forest The Uppe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Upper Palatinate
The Upper Palatinate (german: Oberpfalz, , ) is one of the seven administrative districts of Bavaria, Germany, and is located in the east of Bavaria. Geography The Upper Palatinate is a landscape with low mountains and numerous ponds and lakes in its lowland regions. By contrast with other regions of Germany it is more rural in character and more sparsely settled. It borders (clockwise from the north) on Upper Franconia, the Czech Republic, Lower Bavaria, Upper Bavaria and Middle Franconia. Notable regions are: * Stiftland, former estate and territorial lordship of Waldsassen Abbey with the market town of Konnersreuth, Fockenfeld Abbey, the town of Waldsassen and about 150 other villages. * Upper Palatine Forest with deep valleys and many castles * Upper Palatine Lake District with the Steinberger See * Upper Palatine Jura, part of the Franconian Jura * Steinwald including the Teichelberg and Pechbrunn * Waldnaab/ Wondreb Depression * Bavarian Forest, together with ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Parkstein (Basaltkegel)
The Parkstein, also called the Hoher Parkstein and Basaltkegel Hoher Parkstein is a well-known local hill and tourist destination in the Steinwald Mountains of central Germany. It lies northwest of Weiden in der Oberpfalz in the district of Neustadt a.d.Waldnaab and is one of the most popular walking and daytripper destinations in North Upper Palatinate. Around the volcanically-formed hill, which is above sea level (N.N.), is the village of the same name, Parkstein. At one time a castle (Parkstein Castle) stood on the summit. The Parkstein is famous for its impressive basalt outcrop. This basalt formation consists of pentagonal and hexagonal columns, up to one metre high, whose shafts extend into the earth to a depth of up to 30 metres. It is part of an old stream of lava that has been exposed at the surface after the softer rock above it had been weathered away over the course of millions of years. The wall of basalt measures 38 metres. Alexander von Humboldt Friedrich W ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Großer Teichelberg
Teichelberg is a mountain of Bavaria, Germany. Mining of a 45-meter thick basalt Basalt (; ) is an aphanitic (fine-grained) extrusive igneous rock formed from the rapid cooling of low-viscosity lava rich in magnesium and iron (mafic lava) exposed at or very near the surface of a rocky planet or moon. More than 90 ... layer started in 1888 References Mountains of Bavaria Mountains under 1000 metres {{Bavaria-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Normalnull
("standard zero") or (short N. N. or NN ) is an outdated official vertical datum used in Germany. Elevations using this reference system were to be marked (“meters above standard zero”). has been replaced by (NHN). History In 1878 reference heights were taken from the Amsterdam Ordnance Datum and transferred to the New Berlin Observatory in order to define the . has been defined as a level going through an imaginary point 37.000 m below . When the New Berlin Observatory was demolished in 1912 the reference point was moved east to the village of Hoppegarten (now part of the town of Müncheberg, Brandenburg, Germany Germany,, officially the Federal Republic of Germany, is a country in Central Europe. It is the second most populous country in Europe after Russia, and the most populous member state of the European Union. Germany is situated betwe ...).S. German: ''Was ist "Normal-Null"?''. In: ''Physikalische Blätter'' 1958, vol 14, issue 2, p. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ruins Of Weißenstein (Steinwald)
Ruins () are the remains of a civilization's architecture. The term refers to formerly intact structures that have fallen into a state of partial or total disrepair over time due to a variety of factors, such as lack of maintenance, deliberate destruction by humans, or uncontrollable destruction by natural phenomena. The most common root causes that yield ruins in their wake are natural disasters, armed conflict, and population decline, with many structures becoming progressively derelict over time due to long-term weathering and scavenging. There are famous ruins all over the world, with notable sites originating from ancient China, the Indus Valley and other regions of ancient India, ancient Iran, ancient Israel and Judea, ancient Iraq, ancient Greece, ancient Egypt, Roman sites throughout the Mediterranean Basin, and Incan and Mayan sites in the Americas. Ruins are of great importance to historians, archaeologists and anthropologists, whether they were once individu ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Granite
Granite () is a coarse-grained ( phaneritic) intrusive igneous rock composed mostly of quartz, alkali feldspar, and plagioclase. It forms from magma with a high content of silica and alkali metal oxides that slowly cools and solidifies underground. It is common in the continental crust of Earth, where it is found in igneous intrusions. These range in size from dikes only a few centimeters across to batholiths exposed over hundreds of square kilometers. Granite is typical of a larger family of ''granitic rocks'', or '' granitoids'', that are composed mostly of coarse-grained quartz and feldspars in varying proportions. These rocks are classified by the relative percentages of quartz, alkali feldspar, and plagioclase (the QAPF classification), with true granite representing granitic rocks rich in quartz and alkali feldspar. Most granitic rocks also contain mica or amphibole minerals, though a few (known as leucogranites) contain almost no dark minerals. Granite is near ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Armesberg
Armesberg is a mountain in Bavaria, Germany Germany,, officially the Federal Republic of Germany, is a country in Central Europe. It is the second most populous country in Europe after Russia, and the most populous member state of the European Union. Germany is situated betwe .... It stands at 731 m or 2,398 ft tall. Mountains of Bavaria {{Bavaria-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
