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Göttingen Forest
The Göttingen Forest (german: Göttinger Wald) is a ridge in Germany's Central Uplands that is up to 427.5 metres high. It forms part of the Lower Saxon Hills in South Lower Saxony. Geography The Göttingen Forest, which is divided into numerous separate woods, is found in the south of the Leine Uplands, which is in turn part of the Lower Saxon Hills. It lies in the district of Göttingen east of the city of Göttingen itself, immediately south of the Nörten Forest, west of the Untereichsfeld and north of the Reinhausen Forest with its twin peaks, Die Gleichen. The Göttingen Forest, Nörten Forest and Reinhausen Forest each form part of the Göttingen-Northeim Forest. Several kilometres to the northeast is the ridge of Rotenberg and, beyond that, the Harz Mountains. Northwest of the Göttingen Forest is the Bovenden, north-northwest is Nörten-Hardenberg, to the north is Billingshausen, northeast is Ebergötzen, east is Landolfshausen, southeast is Gleichen and s ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gleichen, Lower Saxony
Gleichen is a municipality (in this case, a '' Gemeinde'') in the district of Göttingen, in Lower Saxony, Germany. Named after the two castles, Neuen-Gleichen and Alten-Gleichen on the twin peaks in the ''Gemeinde'', it is situated about 10 km southeast of Göttingen, from which the peaks are visible. Its seat is Reinhausen. Location The municipality of Gleichen is located southeast of Göttingen, west-southwest of Duderstadt and north-northwest of Heilbad Heiligenstadt. The River Garte flows through several of the villages in the municipality, as does the small Wendebach stream, which is impounded by the Wendebach Reservoir. Both streams are right, eastern tributaries of the Leine. In the center of the municipality are Die Gleichen, a pair of hills 430 m high, that rise between Appenrode, Bettenrode and Gelliehausen. Both hills were once crowned by castles, whose ruins may still be seen. The villages in the municipality may be accessed on state roads (''Landess ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mackenröder Spitze
The Mackenröder Spitze, at about , is the highest hill in the Göttingen Forest and lies on the boundary of the Göttingen, town and Landkreis Göttingen, district of Göttingen, in South Lower Saxony in Germany. Geography The heavily forested hill is located on the eastern escarpment of the Göttingen Forest, a southern part of the Leine Uplands, about 8 km east of the Göttingen town centre and just under 1 kilometre northwest of Mackenrode (Landolfshausen), Mackenrode, a village in the southwest of the municipality of Landolfshausen. From Göttingen (e.g. the borough of Herberhausen), the Mackenröder Spitze can be ascended by a hike through forest on gently sloping terrain. Coming from Mackenrode or Waake, the hill may be reached via short and steep ascents. Harzblick observation tower Just under 400 metres north of the Mackenröder Spitze and about 1.6 kilometres northwest of Mackenrode stands the ''Harzblick'' observation tower at a height of 425&n ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Klein Lengden
Klein Lengden is a village in the Gleichen in the Göttingen district of Lower Saxony, Germany, about eight to ten kilometers south-east of Göttingen. According to the 2010 census, it has about 1363 inhabitants. The village lies in the Garte valley, south of the forested hills of Lengderburg (384 meters a.s.l.) with its Lengdener Burg (castle) and Westerberg (340 meters a.s.l.) and is otherwise surrounded by farm fields. The nearest neighboring villages are Gross Lengden to the east and Diemarden to the west-south-west, each of which is about two kilometers distant. Just outside the village, on L569, the road to Benniehausen, is the Historische Spinnerei Gartetal (historical spinning works of the Garte Valley). In the late 16th century, a flour mill was erected on the site. In the middle of the following century, a paper mill was added. The Industrial Revolution led to the conversion to a spinnery for flannel and woolen yarn. History The earliest known record of the tow ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Plesse Castle
Plesse Castle is situated to the north of Göttingen in Germany, close to the village of Bovenden. History The castle was transferred in 1015 from the private estate of Meinwerk, bishop of Paderborn to the city of Paderborn. Since 1150 it is the seat of the noble lords of Plesse, who named themselves for the castle. Holy Roman emperor Henry VI traded Plesse Castle in 1192 for Desenberg Castle close to Warburg in Westphalia, but the trade was already reverted in 1195. In 1447 the lords of Plesse transferred their possession of Plesse Castle to the Landgrave Ludwig of Hesse and in return received it as a fiefdom. The explanation for it lies in the fragmentation of the dukedom of Brunswick-Göttingen. The leading noble families could not avoid being drawn into the ensuing conflicts. They therefore sought protection from a powerful liege lord. They found this protection and backup with another ruler, who was Ludwig of Hesse. In 1536 the protestant reformation was introduced to th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Holocene
The Holocene ( ) is the current geological epoch. It began approximately 11,650 cal years Before Present (), after the Last Glacial Period, which concluded with the Holocene glacial retreat. The Holocene and the preceding Pleistocene together form the Quaternary period. The Holocene has been identified with the current warm period, known as MIS 1. It is considered by some to be an interglacial period within the Pleistocene Epoch, called the Flandrian interglacial.Oxford University Press – Why Geography Matters: More Than Ever (book) – "Holocene Humanity" section https://books.google.com/books?id=7P0_sWIcBNsC The Holocene corresponds with the rapid proliferation, growth and impacts of the human species worldwide, including all of its written history, technological revolutions, development of major civilizations, and overall significant transition towards urban living in the present. The human impact on modern-era Earth and its ecosystems may be considered of global si ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pleistocene
The Pleistocene ( , often referred to as the ''Ice age'') is the geological Epoch (geology), epoch that lasted from about 2,580,000 to 11,700 years ago, spanning the Earth's most recent period of repeated glaciations. Before a change was finally confirmed in 2009 by the International Union of Geological Sciences, the cutoff of the Pleistocene and the preceding Pliocene was regarded as being 1.806 million years Before Present (BP). Publications from earlier years may use either definition of the period. The end of the Pleistocene corresponds with the end of the last glacial period and also with the end of the Paleolithic age used in archaeology. The name is a combination of Ancient Greek grc, label=none, πλεῖστος, pleīstos, most and grc, label=none, καινός, kainós (latinized as ), 'new'. At the end of the preceding Pliocene, the previously isolated North and South American continents were joined by the Isthmus of Panama, causing Great American Interchang ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Muschelkalk
The Muschelkalk (German for "shell-bearing limestone"; french: calcaire coquillier) is a sequence of sedimentary rock strata (a lithostratigraphic unit) in the geology of central and western Europe. It has a Middle Triassic (240 to 230 million years) age and forms the middle part of the tripartite Germanic Trias, that give the Triassic its name, lying above the older Buntsandstein and below the younger Keuper. The Muschelkalk (" mussel chalk") consists of a sequence of limestone and dolomite beds. In the past, the time span in which the Muschelkalk was deposited could also be called "Muschelkalk". In modern stratigraphy, however, the name only applies to the stratigraphic unit. Occurrence The name ''Muschelkalk'' was first used by German geologist Georg Christian Füchsel (1722-1773). In 1834, Friedrich August von Alberti included it into the Triassic system. The name indicates a characteristic feature of the unit, namely the frequent occurrence of lenticular banks composed o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Triassic
The Triassic ( ) is a geologic period and system which spans 50.6 million years from the end of the Permian Period 251.902 million years ago ( Mya), to the beginning of the Jurassic Period 201.36 Mya. The Triassic is the first and shortest period of the Mesozoic Era. 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 chief terrestrial vertebrates during this time. A specialized subgroup of archo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bedrock
In geology, bedrock is solid Rock (geology), rock that lies under loose material (regolith) within the crust (geology), crust of Earth or another terrestrial planet. Definition Bedrock is the solid rock that underlies looser surface material. An exposed portion of bedrock is often called an outcrop. The various kinds of broken and weathered rock material, such as soil and subsoil, that may overlie the bedrock are known as regolith. Engineering geology The surface of the bedrock beneath the soil cover (regolith) is also known as ''rockhead'' in engineering geology, and its identification by digging, drilling or geophysics, geophysical methods is an important task in most civil engineering projects. Superficial deposition (geology), deposits can be very thick, such that the bedrock lies hundreds of meters below the surface. Weathering of bedrock Exposed bedrock experiences weathering, which may be physical or chemical, and which alters the structure of the rock to leave ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bundesstraße 27
Bundesstraße 27 or B27 is a German federal road. It connects Blankenburg am Harz with Rafz in Switzerland. Route The Bundesstraße 27 crosses the following states and towns (north to south): * Saxony-Anhalt: Blankenburg am Harz * Lower Saxony: Braunlage, Göttingen * Hesse: Sontra, Bad Hersfeld, Fulda * Bavaria: Hammelburg, Würzburg * Baden-Württemberg: Tauberbischofsheim, Heilbronn, Ludwigsburg, Stuttgart, Tübingen, Rottweil, Donaueschingen, Jestetten The B27 is interrupted in two places: between Würzburg and Tauberbischofsheim, where it has been replaced by the motorways A3 and A81, and between Randen and Jestetten, where it crosses through Switzerland. The part south of Stuttgart follows the ''Schweizer Straße'' (Suisse road), a chaussee from 18th century. D ST Rübeland HVLE 285001 Sz 20080511.jpg, in the Harz mountains Stuttgart-pragsatteltunnel-2006-06-05-bigcat.jpg, interchange with B 10 in Stuttgart B27 Tübingen.jpg, in the Neckar valley See also *List ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
