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Wolfsberg (Calenberg Land)
The Wolfsberg is a spur of the Süllberg, , in the Calenberg Land near Springe in the Hanover Region. Location The Wolfsberg lies just under 1 kilometre north-northeast of the Süllberg which lies east of the Deister ridge in Germany's Central Uplands. It rises around 13 kilometres south-southwest of the centre of Hanover in the borough of Springe and municipality of Wennigsen, whose boundary runs over the northwestern flank of the hill. The village of Lüdersen which belongs to Springe lies on the Wolfsberg, the parish to the west belongs to Holtensen. Geology and conservation The Wolfsberg was formed in the Jurassic period. On its eastern side there are sandstone quarries with beds of Deister sandstone, which were exhausted in the 19th century. Since 1968 the Wolfsberg has been on the far side of the limit of building for protected area H-22 in the Hanover Region (this is currently being reviewed. According to political decisions the Wolfsberg element ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Süllberg (Calenberg Land)
The Süllberg is a ridge, up to , in the Calenberg Land near Springe in Hanover Region in the German state of Lower Saxony. Location The Süllberg and its foothills, the Vörier Berg in the north, and the Wolfsberg in the northeast, lies a few kilometres east of the Deister in Germany's Central Uplands. It rises around 14 kilometres south-southwest of the city of Hanover on the territory of Springe and the municipality of Wennigsen, whose boundary runs over the triple-summit hill. A number of villages lie on the slopes of the ridge or at it feet. These are the Springe villages of Bennigsen to the south-southeast and Lüdersen to the east as well as the villages of Holtensen to the north-northwest and Bredenbeck to the west where the hills transition to the Deister. The Bundesstraße 217 federal road runs about one kilometre west of the Süllberg from north to south. Geology The hill was formed during the Jurassic period. Walking There are various hiking ... [...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] |
Late Middle Ages
The Late Middle Ages or Late Medieval Period was the Periodization, period of European history lasting from AD 1300 to 1500. The Late Middle Ages followed the High Middle Ages and preceded the onset of the early modern period (and in much of Europe, the Renaissance). Around 1300, centuries of prosperity and growth in Europe came to a halt. A series of famines and Plague (disease), plagues, including the Great Famine of 1315–1317 and the Black Death, reduced the population to around half of what it had been before the calamities. Along with depopulation came social unrest and endemic warfare. France and England experienced serious peasant uprisings, such as the Jacquerie and the Peasants' Revolt, as well as over a century of intermittent conflict, the Hundred Years' War. To add to the many problems of the period, the unity of the Catholic Church was temporarily shattered by the Western Schism. Collectively, those events are sometimes called the Crisis of the Late Middle Ages. D ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Deserted Village
An abandoned village is a village that has, for some reason, been deserted. In many countries, and throughout history, thousands of villages have been deserted for a variety of causes. Abandonment of villages is often related to epidemic, famine, war, climate change, economic depressions, environmental destruction, or deliberate clearances. Armenia and Azerbaijan Hundreds of villages in Nagorno-Karabakh were deserted following the First Nagorno-Karabakh War. Between 1988 and 1993, 400,000 ethnic Azeris, and Kurds fled the area and nearly 200 villages in Armenia itself populated by Azeris and Kurds were abandoned by 1991. Likewise nearly 300,000 Armenians fled from Azerbaijan between 1988 and 1993, including 50 villages populated by Armenians in Northern Nagorno Karabakh that were abandoned. Some of the Armenian settlements and churches outside Armenia and the Nagorno-Karabakh Republic have either been destroyed or damaged including those in Nakhichevan. Australia In Aust ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ihme
Ihme (in its upper course: Wennigser Mühlbach) is a river of Lower Saxony, Germany. It is a left tributary of the Leine. The Ihme is long. Its source is in the village , a district of Wennigsen. After about , the Ihme reaches the city of Hanover, where it flows into the Leine. In order to protect the city center of Hanover from flooding, much of the water of the Leine is rerouted by a ditch into the Ihme. A bridge over the Ihme is named in memory of Benno Ohnesorg. The Ihme gives its name to the village ''Ihme'', that forms together with ''Roloven'' the district of Ronnenberg. 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 *Ulrichswas ... References Rivers of Lower Saxony Federal waterways in Germany Rivers of Germany {{LowerSaxony-r ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Loess
Loess (, ; from german: Löss ) is a clastic, predominantly silt-sized sediment that is formed by the accumulation of wind-blown dust. Ten percent of Earth's land area is covered by loess or similar deposits. Loess is a periglacial or aeolian (windborne) sediment, defined as an accumulation of 20% or less of clay and a balance of roughly equal parts sand and silt (with a typical grain size from 20 to 50 micrometers), often loosely cemented by calcium carbonate. It is usually homogeneous and highly porous and is traversed by vertical capillaries that permit the sediment to fracture and form vertical bluffs. Properties Loess is homogeneous, porous, friable, pale yellow or buff, slightly coherent, typically non- stratified and often calcareous. Loess grains are angular, with little polishing or rounding, and composed of crystals of quartz, feldspar, mica and other minerals. Loess can be described as a rich, dust-like soil. Loess deposits may become very thick, more than ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Calenberg Loess Börde
The Calenberg is a hill in central Germany in the Leine depression near Pattensen in the municipality of Schulenburg. It lies 13 km west of the city of Hildesheim in south Lower Saxony on the edge of the Central Uplands. It is made from a chalk marl slab (''Kalkmergelbank''), has a height of and was formed almost 100 million years ago at the beginning of the Upper Cretaceous series in Cenomanian stage. The Calenberg became historically important as a result of the fort, stronghold and castle built as the main residence of the House of Hanover. Etymology The syllables ''Kal'', ''Kalen-'', ''Calen-'' in the word ''Calenberg'' are derived from the word ''kal'' in the Middle High German and Middle Low German languages and mean ''kahl'' i.e. "bare", "stripped", "unwooded". Name formations using ''Kal'', ''Kalen'' or ''Calen'' could refer to its geological base (''rock, stone''). The syllable ''-berg'' goes back to the Old High German word ''berg'', to the Middle High German ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Deister Sandstone
The Deister is a chain of hills in the German state of Lower Saxony, about 15 mi (25 km) southwest of the city of Hanover. It runs in a north-westerly direction from Springe in the south to Rodenberg in the north. The next in the chain of hills to the south is the Kleiner Deister ("Little Deister") from which it is separated by the flat pass of the Deister Gate. It is surrounded by Springe, Wennigsen, Barsinghausen, Bad Nenndorf, Rodenberg and Bad Münder (counter-clockwise, starting in the south). It has a total length of 21 km (14 mi), and rises in the Hofeler to a height of 395 m (1,250 ft). The highest point is the Bröhn at 405 m (1,312 ft). The chain is well-wooded and abounds in game. From the 17th century on there were several coal mines; the last were abandoned in the 1950s. Sandstone from quarries in eastern Deister was used in several important buildings all over Europe, including the opera house in Hanover and the Reichsta ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sandstone
Sandstone is a clastic sedimentary rock composed mainly of sand-sized (0.0625 to 2 mm) silicate grains. Sandstones comprise about 20–25% of all sedimentary rocks. Most sandstone is composed of quartz or feldspar (both silicates) because they are the most resistant minerals to weathering processes at the Earth's surface. Like uncemented sand, sandstone may be any color due to impurities within the minerals, but the most common colors are tan, brown, yellow, red, grey, pink, white, and black. Since sandstone beds often form highly visible cliffs and other topographic features, certain colors of sandstone have been strongly identified with certain regions. Rock formations that are primarily composed of sandstone usually allow the percolation of water and other fluids and are porous enough to store large quantities, making them valuable aquifers and petroleum reservoirs. Quartz-bearing sandstone can be changed into quartzite through metamorphism, usually related to ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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