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Leine Uplands
The Leine Uplands (german: Leinebergland, ) is a region in Germany's Central Uplands which forms a part of the Lower Saxon Hills and lies along the River Leine between Göttingen and Hanover. It borders on the Weser Uplands in the west, the Innerste Uplands in the northeast, the Harz in the east and Untereichsfeld in the southeast. Geography The Leine Uplands, which merge into the Weser Uplands to the east and the Harz to the west, are not a clearly defined landscape in terms of being a natural region but are nevertheless relatively easily delineated. Their extent from south to north is determined by the river that lends them their name and their extent from east to west by high ridges. From north to south the uplands can be broadly divided into a southern half around the wide trough of the River Leine's middle course and a northern half by the lower reaches of the same river. Landscapes either side of the Leine trough The River Leine flows from Friedland via Göttingen an ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Leinebergland
The Leine Uplands (german: Leinebergland, ) is a region in Germany's Central Uplands which forms a part of the Lower Saxon Hills and lies along the River Leine between Göttingen and Hanover. It borders on the Weser Uplands in the west, the Innerste Uplands in the northeast, the Harz in the east and Untereichsfeld in the southeast. Geography The Leine Uplands, which merge into the Weser Uplands to the east and the Harz to the west, are not a clearly defined landscape in terms of being a natural region but are nevertheless relatively easily delineated. Their extent from south to north is determined by the river that lends them their name and their extent from east to west by high ridges. From north to south the uplands can be broadly divided into a southern half around the wide trough of the River Leine's middle course and a northern half by the lower reaches of the same river. Landscapes either side of the Leine trough The River Leine flows from Friedland via Göttingen an ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bunter Sandstone
The Buntsandstein (German for ''coloured'' or ''colourful sandstone'') or Bunter sandstone is a lithostratigraphic and allostratigraphic unit (a sequence of rock strata) in the subsurface of large parts of west and central Europe. The Buntsandstein predominantly consists of sandstone layers of the Lower Triassic series and is one of three characteristic Triassic units, together with the Muschelkalk and Keuper that form the Germanic Trias Supergroup. The Buntsandstein is similar in age, facies and lithology with the Bunter of the British Isles. It is normally lying on top of the Permian Zechstein and below the Muschelkalk. In the past the name Buntsandstein was in Europe also used in a chronostratigraphic sense, as a subdivision of the Triassic system. Among reasons to abandon this use was the discovery that its base lies actually in the latest Permian. Origin The Buntsandstein was deposited in the Germanic Basin, a large sedimentary basin that was the successor of the smal ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Vogler (mountain Range)
The Vogler is a range of hills, up to 460.4 m high, in the Weser Uplands in southern Lower Saxony (Germany). Together with the Solling, the Vogler forms the Solling-Vogler Nature Park which lies a couple of kilometres further south. Geography The Vogler is located in the district of Holzminden between the hills of the Ith to the north, the Hils to the northeast, the Homburg Forest to the east, the Amtsberge to the southeast, the Solling to the south and the Burgberg to the south-southwest. It also lies in the triangle formed by the towns of Bevern, Bodenwerder and Eschershausen. The River Weser flows by the Vogler to the west heading north to the North Sea. To the north the Lenne, a western tributary of the Weser runs past in a northwesterly direction. The Vogler drops steeply to the Weser through a height of 220 m. Nestling in its northern foothills is the village of Heinrichshagen, where Henry the Fowler was supposed to have trapped birds. Geology The unde ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Solling Foreland
The Solling () is a range of hills up to high in the Weser Uplands in the German state of Lower Saxony, whose extreme southerly foothills extend into Hesse and North Rhine-Westphalia. Inside Lower Saxony it is the second largest range of hills and the third highest after the Harz (Wurmberg; 971 m) and the Kaufungen Forest (Haferberg; 581 m). The Solling is a cultural landscape consisting mainly of spruce and beech forests. Oak also grows in some areas. The Solling forest is home of a number of animals and birds, for example red deer or chaffinch. They can best be observed in the ''Neuhaus wildlife park''. Together with the smaller and lower Vogler range and the little Burgberg to the north, the Solling is part of the Solling-Vogler Nature Park. Hills The main hills in the Solling include the following (heights given in m above Normalnull): * Große Blöße (527.8 m) * Großer Ahrensberg (524.9 m) * Moosberg (513.0 m) – with Hochsolling observation tower * Vog ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hube (ridge)
The Hube is a ridge, up to , in the Leine Uplands and district of Northeim, in the German state of Lower Saxony. Geography The densely wooded Hube lies immediately northeast of the town of Einbeck, with its pretty, timber-framed houses, west of the River Leine and north of the Ilme valley. Although the ridge, which measures some 8.5 x 5.5 kilometres, is west of the Leine it is counted as part of the southwestern Harz Foreland in Germany's official natural regional classification. The highest elevation on the Hube is the Fuchshöhlenberg with its transmission mast at 346.2 m. About 150 metres southeast of the tower is the highest point of the actual summit. On the northern edge of the Greene Forest, the northern part of the Hube, are the ruins of Greene Castle above the town of Greene with good views from the castle tower. In the southern part of the Hube, 570 metres north of the Altendorfer Berg and between Einbeck and Negenborn stands the Emperor Fred ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Einbeck
Einbeck (; Eastphalian: ''Aimbeck'') is a town in the district Northeim, in southern Lower Saxony, Germany, on the German Timber-Frame Road. History Prehistory The area of the current city of Einbeck is inhabited since prehistoric times. Various artifacts have been unearthed in the city of Einbeck itself and in the little villages and lost villages around it over the years. They date back to the Paleolithic Era. Medieval period In the Early Middle Ages a number of villages existed along the river Ilme in the middle Leine valley before Einbeck was founded. On January 1, 1158 Einbeck was first mentioned in a deed of Friedrich Barbarossa, which mentioned ''… in loco qui Einbike vocatur …''. and related to a transfer of an estate in the 11th century. Count Udo of Katlenburg owned an estate on the bank of a brook, the Krummes Wasser (crooked water). His grandson founded the stift Sankt Alexandri, that subsequently developed into an important sanctuary. On the other side of th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Limestone
Limestone ( calcium carbonate ) is a type of carbonate sedimentary rock which is the main source of the material lime. It is composed mostly of the minerals calcite and aragonite, which are different crystal forms of . Limestone forms when these minerals precipitate out of water containing dissolved calcium. This can take place through both biological and nonbiological processes, though biological processes, such as the accumulation of corals and shells in the sea, have likely been more important for the last 540 million years. Limestone often contains fossils which provide scientists with information on ancient environments and on the evolution of life. About 20% to 25% of sedimentary rock is carbonate rock, and most of this is limestone. The remaining carbonate rock is mostly dolomite, a closely related rock, which contains a high percentage of the mineral dolomite, . ''Magnesian limestone'' is an obsolete and poorly-defined term used variously for dolomite, for limes ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Jurassic
The Jurassic ( ) is a Geological period, geologic period and System (stratigraphy), stratigraphic system that spanned from the end of the Triassic Period million years ago (Mya) to the beginning of the Cretaceous Period, approximately Mya. The Jurassic constitutes the middle period of the Mesozoic, Mesozoic Era and is named after the Jura Mountains, where limestone strata from the period were first identified. The start of the Jurassic was marked by the major Triassic–Jurassic extinction event, associated with the eruption of the Central Atlantic magmatic province, Central Atlantic Magmatic Province. The beginning of the Toarcian Stage started around 183 million years ago and is marked by an extinction event associated with widespread Anoxic event, oceanic anoxia, ocean acidification, and elevated temperatures likely caused by the eruption of the Karoo-Ferrar, Karoo-Ferrar large igneous provinces. The end of the Jurassic, however, has no clear boundary with the Cretaceous and i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Southwest Harz Foreland
The Harz () is a highland area in northern Germany. It has the highest elevations for that region, and its rugged terrain extends across parts of Lower Saxony, Saxony-Anhalt, and Thuringia. The name ''Harz'' derives from the Middle High German word ''Hardt'' or ''Hart'' (hill forest). The name ''Hercynia'' derives from a Celtic name and could refer to other mountain forests, but has also been applied to the geology of the Harz. The Brocken is the highest summit in the Harz with an elevation of above sea level. The Wurmberg () is the highest peak located entirely within the state of Lower Saxony. Geography Location and extent The Harz has a length of , stretching from the town of Seesen in the northwest to Eisleben in the east, and a width of . It occupies an area of , and is divided into the Upper Harz (''Oberharz'') in the northwest, which is up to 800 m high, apart from the 1,100 m high Brocken massif, and the Lower Harz (''Unterharz'') in the east which is up to around ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Beech
Beech (''Fagus'') is a genus of deciduous trees in the family Fagaceae, native to temperate Europe, Asia, and North America. Recent classifications recognize 10 to 13 species in two distinct subgenera, ''Engleriana'' and ''Fagus''. The ''Engleriana'' subgenus is found only in East Asia, distinctive for its low branches, often made up of several major trunks with yellowish bark. The better known ''Fagus'' subgenus beeches are high-branching with tall, stout trunks and smooth silver-grey bark. The European beech (''Fagus sylvatica'') is the most commonly cultivated. Beeches are monoecious, bearing both male and female flowers on the same plant. The small flowers are unisexual, the female flowers borne in pairs, the male flowers wind-pollinating catkins. They are produced in spring shortly after the new leaves appear. The fruit of the beech tree, known as beechnuts or mast, is found in small burrs that drop from the tree in autumn. They are small, roughly triangular, and edible, w ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Abri
A rock shelter (also rockhouse, crepuscular cave, bluff shelter, or abri) is a shallow cave-like opening at the base of a bluff or cliff. In contrast to solutional caves (karst), which are often many miles long, rock shelters are almost always modest in size and extent. Formation Rock shelters form because a rock stratum such as sandstone that is resistant to erosion and weathering has formed a cliff or bluff, but a softer stratum, more subject to erosion and weathering, lies just below the resistant stratum, and thus undercuts the cliff. In arid areas, wind erosion (Aeolian erosion) can be an important factor in rockhouse formation. In most humid areas, the most important factor in rockhouse formation is frost spalling, where the softer, more porous rock underneath is pushed off, tiny pieces at a time, by frost expansion from water frozen in the pores. Erosion from moving water is seldom a significant factor. Many rock shelters are found under waterfalls. File:Rock shelt ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Northeim
Northeim (; nds, Nuurten) is a town in Lower Saxony, Germany, seat of the district of Northeim, with, in 2011, a population of 29,000. It lies on the German Half-Timbered House Road. History Northeim is first mentioned in 800 in a document recording a property transfer by a Frankish nobleman to the Abbey of Fulda. In the 10th century the surrounding region became a county, administered by the Counts of Northeim. The first of them, Siegfried is mentioned in 982. From 1061 to 1070 Count Otto II held the stem duchy of Bavaria as an Imperial fief, but lost it again because of his involvement in the Saxon plot against King Henry IV. The monastery of St. Blasius was founded around 1100. In 1252 Northeim obtained town rights, and from 1384 to 1554 it was a member of the Hanseatic League. When protestantism was introduced in 1532 all the churches were allocated to the protestants. The town became part of the Kingdom of Hanover. A part of Northeim was devastated by a fire in 1832 w ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
