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Ohm Hills
The Ohm Hills (german: Ohmgebirge) are a small range of hills up to high and about 50 km² in area. They are part of the Lower Eichsfeld region and are located in the county of Eichsfeld, North Thuringia, Germany. Geography The Ohm Hills, most of which are densely wooded, whose southeastern foothills form the Bleicherode Hills, lie in the county of Eichsfeld on its boundary with Nordhausen. They are located between Weißenborn-Lüderode to the north, Bleicherode to the southeast, Worbis to the south and Teistungen to the west, and extend from the upper reaches of the River Helme in the north to the Wipper in the south. To the north and west the range is adjoined by historic landscape of the Lower Eichsfeld (''Untereichsfeld''), further south is the ridge of the Dün and to the southwest the Eichsfeld-Hainich-Werra Valley Nature Park. Natural region classification According to "Kassel map" of the natural regional classification of Germany the Ohm Hills are grouped as ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lower Eichsfeld
The Eichsfeld ( or ; English: ''Oak-field'') is a historical region in the southeast of the state of Lower Saxony (which is called "Untereichsfeld" = lower Eichsfeld) and northwest of the state of Thuringia ("Obereichsfeld" = upper Eichsfeld) in the south of the Harz mountains in Germany. Until 1803 the Eichsfeld was for centuries part of the Archbishopric of Mainz, which is the cause of its current position as a Catholic enclave in the predominantly Protestant north of Germany. Following German partition in 1945, the West German portion became Landkreis Duderstadt. A few small transfers of territory between the American and Soviet zones of occupation took place in accordance with the Wanfried Agreement. Geography Today the greatest part of the Obereichsfeld makes up the Eichsfeld (district), Landkreis (district) Eichsfeld. Other parts belong to the district Unstrut-Hainich-Kreis. The Untereichsfeld, later Landkreis Duderstadt, was merged mostly with the Landkreis of Göttingen (di ... [...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("standard zero") or (short N. N. or NN ) is an outdated official vertical datum used in Germany.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 has been replaced by (NHN).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] |
Haynrode 7 (1940) C
Haynrode is a municipality in the Eichsfeld in Thuringia Thuringia (; german: Thüringen ), officially the Free State of Thuringia ( ), is a state of central Germany, covering , the sixth smallest of the sixteen German states. It has a population of about 2.1 million. Erfurt is the capital and larg ..., Germany. References Eichsfeld (district) {{Eichsfeld-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Holungen Ohmgebirge
Holungen is a village and a former municipality in the district of Eichsfeld in Thuringia, Germany. Since 1 December 2011, it is part of the municipality Sonnenstein, of which it is an ''''. [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Eller (Rhume)
Eller is a river of Lower Saxony and Thuringia, Germany. Its source is the confluence of the Weilroder Eller and the Geroder Eller. It flows into the Rhume in Rüdershausen. See also *List of rivers of Lower Saxony All rivers in the German state of Lower Saxony flow directly or indirectly into the North Sea. A–Z A B D E F G H I J K L M N O P * Purrmühlenbach R S T * Tiefenbeek * Trillkebach * Trutenbeek * Twiste U * Uffe * Ulrich ... * List of rivers of Thuringia Rivers of Lower Saxony Rivers of Thuringia Rivers of Germany {{Thuringia-river-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Eichsfeld Basin
The Eichsfeld ( or ; English: ''Oak-field'') is a historical region in the southeast of the state of Lower Saxony (which is called "Untereichsfeld" = lower Eichsfeld) and northwest of the state of Thuringia ("Obereichsfeld" = upper Eichsfeld) in the south of the Harz mountains in Germany. Until 1803 the Eichsfeld was for centuries part of the Archbishopric of Mainz, which is the cause of its current position as a Catholic enclave in the predominantly Protestant north of Germany. Following German partition in 1945, the West German portion became Landkreis Duderstadt. A few small transfers of territory between the American and Soviet zones of occupation took place in accordance with the Wanfried Agreement. Geography Today the greatest part of the Obereichsfeld makes up the Eichsfeld (district), Landkreis (district) Eichsfeld. Other parts belong to the district Unstrut-Hainich-Kreis. The Untereichsfeld, later Landkreis Duderstadt, was merged mostly with the Landkreis of Göttingen (di ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Thuringian Basin
The Thuringian Basin (german: Thüringer Becken) is a depression in the central and northwest part of Thuringia in Germany which is crossed by several rivers, the longest of which is the Unstrut. It stretches about from north to south and around from east to west. Its height varies from about 150 to . The Basin is surrounded by a wide outer girdle of limestone (Muschelkalk) ridges (including Hainich, Dün, Hainleite, Hohe Schrecke, Schmücke, Finne), and to the southwest by the Thuringian Forest and to the southeast by sharply divided terraces (the Ilm-Saale and Ohrdruf Muschelkalk plateaus, and the Saale-Elster Bunter sandstone plateau). The Thuringian Basin belongs to the triassic period, during which horizontal beds of Bunter sandstone, Muschelkalk and Keuper were laid down. Below those lie the salt and gypsum layers of Magnesian Limestone (Zechstein). In the Cenozoic era the surrounding ridges were uplifted, whilst the Thuringian Basin sank to form a saucer-shaped depressio ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
