Giehler Bach
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Giehler Bach
The Hamme (in its upper reaches Giehler Bach) is a long river in Germany, Lower Saxony, north-east of Bremen. Its source is north of Osterholz-Scharmbeck. It flows through the moors north-east of Bremen called Teufelsmoor, and meets the river Wümme in Ritterhude. From this junction, the river is called Lesum. The Lesum flows into the river Weser in Bremen-Vegesack. On the river Hamme there are many water-sport clubs, for example the Wassersportclub Hamme e.V. (watersports-club Hamme), the Ruder-Verein Osterholz-Scharmbeck von 1901 e.V. (Rowing Club Osterholz-Scharmbeck since 1901) and the Segel Club Hamme e.V. (Sailing Club Hamme). Course The upper reaches of the Hamme are called the ''Giehler Bach'' (Giehl Stream). The ''Giehler Bach'' originates in the heathland of the ''Lange Heide'' northeast of Osterholz-Scharmbeck, a geest plateau at a height of about , which is also the source of many other geest streams (such as the Drepte, Scharmbecker Bach, Schönebecker Aue and Wie ...
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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 between the Baltic and North seas to the north, and the Alps to the south; it covers an area of , with a population of almost 84 million within its 16 constituent states. Germany borders Denmark to the north, Poland and the Czech Republic to the east, Austria and Switzerland to the south, and France, Luxembourg, Belgium, and the Netherlands to the west. The nation's capital and most populous city is Berlin and its financial centre is Frankfurt; the largest urban area is the Ruhr. Various Germanic tribes have inhabited the northern parts of modern Germany since classical antiquity. A region named Germania was documented before AD 100. In 962, the Kingdom of Germany formed the bulk of the Holy Roman Empire. During the 16th ce ...
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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("standard zero") or (short N. N. or NN ) is an outdated official vertical datum used in Germany.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 has been replaced by (NHN).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. ...
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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 *Ulrichswasser *Unterelbe V W Z *Zellbach * Zorge By basin This list uses bullets and indents to show the rivers' hierarchy and the sequence from river mouth to source. The number of indents corresponds to the river's position in the sequence. Tributaries are shown orographically as either a left (l) or a right (r) tributary of the next waterway in the downstream direction. Elbe * Elbe (, into the North Sea) ** Medem (l) *** Emmelke ** Oste (l) (153 km) *** Aue (tributary of the Oste) (l) (14 km) *** Mehe (l) *** Bever (r) *** Twiste (r) *** Ramme (r) ** Schwinge (l) ** Lühe (l) *** Aue (tributary of the Elbe) (26 km) ** Este (l) ** Seeve (l) (40 km) ** Ilmenau (l) (107 km) *** Luhe (l) (58 km) *** Neetze ...
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Bremen
Bremen (Low German also: ''Breem'' or ''Bräm''), officially the City Municipality of Bremen (german: Stadtgemeinde Bremen, ), is the capital of the German state Free Hanseatic City of Bremen (''Freie Hansestadt Bremen''), a two-city-state consisting of the cities of Bremen and Bremerhaven. With about 570,000 inhabitants, the Hanseatic city is the 11th largest city of Germany and the second largest city in Northern Germany after Hamburg. Bremen is the largest city on the River Weser, the longest river flowing entirely in Germany, lying some upstream from its mouth into the North Sea, and is surrounded by the state of Lower Saxony. A commercial and industrial city, Bremen is, together with Oldenburg and Bremerhaven, part of the Bremen/Oldenburg Metropolitan Region, with 2.5 million people. Bremen is contiguous with the Lower Saxon towns of Delmenhorst, Stuhr, Achim, Weyhe, Schwanewede and Lilienthal. There is an exclave of Bremen in Bremerhaven, the "Citybremian Overseas Port ...
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Lock (water Transport)
A lock is a device used for raising and lowering boats, ships and other watercraft between stretches of water of different levels on river and canal waterways. The distinguishing feature of a lock is a fixed chamber in which the water level can be varied; whereas in a caisson lock, a boat lift, or on a canal inclined plane, it is the chamber itself (usually then called a caisson) that rises and falls. Locks are used to make a river more easily navigable, or to allow a canal to cross land that is not level. Later canals used more and larger locks to allow a more direct route to be taken. Pound lock A ''pound lock'' is most commonly used on canals and rivers today. A pound lock has a chamber with gates at both ends that control the level of water in the pound. In contrast, an earlier design with a single gate was known as a flash lock. Pound locks were first used in China during the Song Dynasty (960–1279 AD), having been pioneered by the Song politician and naval en ...
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Meanders
A meander is one of a series of regular sinuous curves in the channel of a river or other watercourse. It is produced as a watercourse erodes the sediments of an outer, concave bank (cut bank) and deposits sediments on an inner, convex bank which is typically a point bar. The result of this coupled erosion and sedimentation is the formation of a sinuous course as the channel migrates back and forth across the axis of a floodplain. The zone within which a meandering stream periodically shifts its channel is known as a meander belt. It typically ranges from 15 to 18 times the width of the channel. Over time, meanders migrate downstream, sometimes in such a short time as to create civil engineering challenges for local municipalities attempting to maintain stable roads and bridges.Neuendorf, K.K.E., J.P. Mehl Jr., and J.A. Jackson, J.A., eds. (2005) ''Glossary of Geology'' (5th ed.). Alexandria, Virginia, American Geological Institute. 779 pp. Charlton, R., 2007. ''Fundamentals o ...
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Breites Wasser
The Breites Wasser is a lake in the borough of Osterholz-Scharmbeck in the German state of Lower Saxony on the terrain of the Teufelsmoor. A nature reserve of the same name lies around the lake between Worpswede and the village of Teufelsmoor. The lake is situated at the confluence of the Beek and the Hamme about 2 km downstream of Beek. The many ox-bows of the streams and small irregular ponds with boggy shores, the so-called '' Blänken'' form a wetland triangle (''feuchtes Dreieck''), which constantly changes its appearance due to the variations in water levels. Many rare birds breed in the area and there are also colonies of gulls. In autumn and spring quite a few migratory birds rest here en route to their destinations. Several years ago a large number of paths were laid out for walkers. See also * List of lakes in Germany Sources * Hans-Gerhard Kulp: ''Der Weyerberg The Weyerberg is a sandy geest island, high, in the Teufelsmoor ("Devil's Bog") in Northern German ...
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Worpswede
Worpswede (Northern Low Saxon: ''Worpsweed'') is a municipality in the Osterholz-Scharmbeck, district of Osterholz, in Lower Saxony, Germany. It is situated in the Teufelsmoor, northeast of Bremen (city), Bremen. The small town itself is located near the Weyerberg hill. It has been the home to a lively artistic community since the end of the 19th century, with over 130 artists and craftsmen working there. History Its origin goes back to the Bronze Age. The first time it was mentioned however was in 1218. Then it belonged to the Archdiocese of Bremen, Prince-Archbishopric of Bremen. In 1630 it was occupied by Sweden for a short period of time. In 1648 the Prince-Archbishopric was transformed into the Duchy of Bremen, which was first ruled in personal union by the Swedish and from 1715 on by the Hanoverian Crown. However, it took another 120 years (1750) until the colonization of the Teufelsmoor was started by Jürgen Christian Findorff by drainage of the bog. In 1823 the Duchy was ...
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Glacial Valley
U-shaped valleys, also called trough valleys or glacial troughs, are formed by the process of glaciation. They are characteristic of mountain glaciation in particular. They have a characteristic U shape in cross-section, with steep, straight sides and a flat or rounded bottom (by contrast, valleys carved by rivers tend to be V-shaped in cross-section). Glaciated valleys are formed when a glacier travels across and down a slope, carving the valley by the action of scouring. When the ice recedes or thaws, the valley remains, often littered with small boulders that were transported within the ice, called glacial till or glacial erratic. Examples of U-shaped valleys are found in mountainous regions throughout the world including the Andes, Alps, Caucasus Mountains, Himalaya, Rocky Mountains, New Zealand and the Scandinavian Mountains. They are found also in other major European mountains including the Carpathian Mountains, the Pyrenees, the Rila and Pirin mountains in Bulgaria, ...
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