Thüster Berg
The Thüster Berg is a ridge, up to , in the Lower Saxon Hills in central Germany. It is situated in the districts of Hameln-Pyrmont and Hildesheim in the federal state of Lower Saxony. Location The Thüster Berg lies within a triangle formed by the villages of Eime, Duingen and Salzhemmendorf in the western half of the Leine Uplands, which itself is in the northern part of the Lower Saxon Hills. It is about long and its highest peak is the Kanstein. It lies between Hemmendorf and Oldendorf in the north, Ahrenfeld, Deilmissen and Deinsen in the south, Marienhagen in the southeast, Weenzen and Thüste in the south, Levedagsen and the Domäne Eggersen in the west and the village of Salzhemmendorf to the northwest. North of the Thüster Berg is the Osterwald, to the east the Külf, to the southeast the Duinger Berg and to the west the Ith. The River Saale, a southwestern tributary of the Leine flows to the west and north of the ridge. Its northwestern part belongs to the Weser ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Weenzen
Weenzen is a village and a former municipality in the district of Hildesheim in Lower Saxony, Germany. Since 1 November 2016, it is part of the municipality Duingen Duingen is a village and a municipality in the district of Hildesheim, in Lower Saxony, Germany. It is situated approximately 25 km southwest of Hildesheim, and 40 km south of Hanover. Since 1 November 2016, the former municipalities .... References Hildesheim (district) Former municipalities in Lower Saxony {{Hildesheim-geo-stub ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Birch
A birch is a thin-leaved deciduous hardwood tree of the genus ''Betula'' (), in the family Betulaceae, which also includes alders, hazels, and hornbeams. It is closely related to the beech- oak family Fagaceae. The genus ''Betula'' contains 30 to 60 known taxa of which 11 are on the IUCN 2011 Red List of Threatened Species. They are a typically rather short-lived pioneer species widespread in the Northern Hemisphere, particularly in northern areas of temperate climates and in boreal climates. Description Birch species are generally small to medium-sized trees or shrubs, mostly of northern temperate and boreal climates. The simple leaves are alternate, singly or doubly serrate, feather-veined, petiolate and stipulate. They often appear in pairs, but these pairs are really borne on spur-like, two-leaved, lateral branchlets. The fruit is a small samara, although the wings may be obscure in some species. They differ from the alders (''Alnus'', another genus in the family) ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Quarries
A quarry is a type of open-pit mine in which dimension stone, rock, construction aggregate, riprap, sand, gravel, or slate is excavated from the ground. The operation of quarries is regulated in some jurisdictions to reduce their environmental impact. The word ''quarry'' can also include the underground quarrying for stone, such as Bath stone. Types of rock Types of rock extracted from quarries include: *Chalk *China clay *Cinder *Clay *Coal *Construction aggregate (sand and gravel) *Coquina *Diabase *Gabbro *Granite *Gritstone *Gypsum *Limestone *Marble *Ores *Phosphate rock *Quartz *Sandstone *Slate *Travertine Stone quarry Stone quarry is an outdated term for mining construction rocks (limestone, marble, granite, sandstone, etc.). There are open types (called quarries, or open-pit mines) and closed types ( mines and caves). For thousands of years, only hand tools had been used in quarries. In the 18th century, the use of drilling and blasting operations was ma ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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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 lime ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Bundesstraße 240
''Bundesstraße'' (German for "federal highway"), abbreviated ''B'', is the denotation for German and Austrian national highways. Germany Germany's ''Bundesstraßen'' network has a total length of about 40,000 km. German ''Bundesstraßen'' are labelled with rectangular yellow signs with black numerals, as opposed to the white-on-blue markers of the ''Autobahn'' controlled-access highways. ''Bundesstraßen'', like autobahns, are maintained by the federal agency of the Transport Ministry. In the German highway system they rank below autobahns, but above the ''Landesstraßen'' and ''Kreisstraßen'' maintained by the federal states and the districts respectively. The numbering was implemented by law in 1932 and has overall been retained up to today, except for those roads located in the former eastern territories of Germany. One distinguishing characteristic between German ''Bundesstraßen'' and ''Autobahnen'' is that there usually is a general 100 km/h (62 mph) sp ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Bundesstraße 1
The Bundesstraße 1 (abbr. B1) is a German federal highway running in an east-west direction from the Dutch border near Aachen to the Polish border at Küstrin-Kietz on the Oder River. History The road developed from an ancient east-western trade route connecting the shore of the North Sea at Bruges with the area of Novgorod. A trade and military road was already mentioned in Ptolemy's ''Geography'' about 150 AD, parts of it formed the medieval Westphalian Hellweg trade route, vital for the transport of salt and crops, and the course of the Via Regia, the Ottonian "royal road" through the Holy Roman Empire from Aachen to Magdeburg. From the late 18th century onwards, parts of the route were rebuilt as a chaussee, mainly in the area between Aachen and Jülich as well as on the nearby territory of the County of Mark, promoted by the Brandenburg-Prussian administration under Heinrich Friedrich Karl vom und zum Stein. Stein also concluded an agreement to extend the road via the terr ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Weser Uplands Schaumburg-Hamelin Nature Park
The Weser Uplands-Schaumburg-Hamelin Nature Park (german: Naturpark Weserbergland Schaumburg-Hameln) lies on the northern edge of the German Central Uplands where it transitions to the North German Plain, about southwest of Hanover. The sponsor of the nature park, which was founded in 1975, is the state of Lower Saxony. The park extends along the Weser valley between Rinteln and Hamelin and includes parts of the Schaumburg Land, Calenberg, Lippe and Pyrmont Uplands from Bad Nenndorf in the north to Bad Pyrmont in the south, Bückeburg and Bad Eilsen in the west and Bad Münder and Osterwald in the east. Its highest elevation is in the Süntel hills. Location Bordered in the north by the forested ridges of the Bückeberg and the Deister, the nature park covers almost from the eastern Weser Hills, Harrl and Süntel running along both sides of the River Weser southwards to the Ith ridge, the Osterwald and the Thüster Berg, through a very varied landscape of wooded, roll ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Leine (river)
The Leine (; Old Saxon ''Lagina'') is a river in Thuringia and Lower Saxony, Germany. It is a left tributary of the Aller and the Weser and is long. The river's source is located close to the town of Leinefelde in Thuringia. About downriver, the river enters Lower Saxony and runs northwards. Important towns along its course, from upstream to downstream, are Göttingen, Einbeck, Freden, Alfeld, and Gronau, before the river enters Hanover, the largest city on its banks. Downstream some north of Hanover, near Schwarmstedt, the river joins the Aller and reaches the North Sea via the Weser. Its northern (lower) reaches are only navigable today by the smallest commercial carriers, though in the past, it served as an important pre-railway barge transport artery as far upriver as Göttingen. The river is somewhat polluted by industry, so the water is not used for drinking, but the pollution has never been severe enough to prevent fish from living in it. Like many western rivers ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Tributary
A tributary, or affluent, is a stream or river that flows into a larger stream or main stem (or parent) river or a lake. A tributary does not flow directly into a sea or ocean. Tributaries and the main stem river drain the surrounding drainage basin of its surface water and groundwater, leading the water out into an ocean. The Irtysh is a chief tributary of the Ob river and is also the longest tributary river in the world with a length of . The Madeira River is the largest tributary river by volume in the world with an average discharge of . A confluence, where two or more bodies of water meet, usually refers to the joining of tributaries. The opposite to a tributary is a distributary, a river or stream that branches off from and flows away from the main stream. PhysicalGeography.net, Michael Pidwirny ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Saale (Leine)
Saale is a river of Lower Saxony, Germany. It is a left tributary of the Leine. Its source is near the village Duingen Duingen is a village and a municipality in the district of Hildesheim, in Lower Saxony, Germany. It is situated approximately 25 km southwest of Hildesheim, and 40 km south of Hanover. Since 1 November 2016, the former municipalities .... It flows into the Leine in Elze. See also * List of rivers of Lower Saxony References Rivers of Lower Saxony Rivers of Germany {{LowerSaxony-river-stub ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |