Fulde (Böhme)
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Fulde (Böhme)
The Fulde is a river of Lower Saxony, Germany. It belongs to the Weser river system. It is about long and flows entirely within the territory of the borough of Walsrode (Heidekreis, Heidekreis district. It rises in a valley between two parallel end moraines formed in the Saalian glaciation, Saalian Ice Age. By far the largest source drains the Grundloses Moor ("bottomless moor"), north of Fulde (Walsrode), Fulde and emerges from the ''Kleiner See'' ("Little Lake") there. Another source appears northwest of the village of Fulde, which gave the stream its name. From there the Fulde runs through, at times, picturesque scenery between steep, grass-covered, clay banks and fish ponds south of the Walsrode town forest of ''Eckernworth'', where the Rischmannshof Heath Museum is located, crosses the centre of the town through the ''Fulde Park'' with its town hall and joins the River Böhme south of the Walsrode Abbey lake. See also *List of rivers of Lower Saxony Literature

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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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Grundloses Moor
The Grundloses Moor (literally: "Bottomless Bog") is the largest, virtually intact raised bog in the district of Heidekreis and a Naturschutzgebiet, nature reserve in Walsrode in the German state of Lower Saxony. Description The reserve has an area of and lies about 1.5 km west of the village of Ebbingen, 3.5 km north of the village of Fulde (Walsrode), Fulde and five km northwest of the town of Walsrode. In the centre of the moor is the 2.5 metre deep lake ''Grundloser See'', which is 435 metres long from north to south, and 160 metres wide in its northern part. It has an area of and lies at above mean sea level. Roughly 400 metres to the northeast lies the ''Kleiner See'' ("Little Lake") with a diameter of about 60 metres. History The moor was formed in the northeastern half of a 4-kilometre-long depression enclosed by two parallel end moraines which were deposited during the Saalian glaciation. It is drained by a ditch that acts as the upper c ...
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Rivers Of Lower Saxony
A river is a natural flowing watercourse, usually freshwater, flowing towards an ocean, sea, lake or another river. In some cases, a river flows into the ground and becomes dry at the end of its course without reaching another body of water. Small rivers can be referred to using names such as creek, brook, rivulet, and rill. There are no official definitions for the generic term river as applied to geographic features, although in some countries or communities a stream is defined by its size. Many names for small rivers are specific to geographic location; examples are "run" in some parts of the United States, "burn" in Scotland and northeast England, and "beck" in northern England. Sometimes a river is defined as being larger than a creek, but not always: the language is vague. Rivers are part of the water cycle. Water generally collects in a river from precipitation through a drainage basin from surface runoff and other sources such as groundwater recharge, springs, a ...
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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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Walsrode Abbey
Walsrode Abbey (German: ''Kloster Walsrode'') in Walsrode, Germany, is one of the historic monasteries of Benedictine nuns on the Lüneburg Heath in North Germany which are collectively known as the ''Lüneklöster''. Today it is a Lutheran women's convent that is maintained by the Hanover monastic chamber (''Klosterkammer Hannover''). History The monastery was founded in 986 by Count Wale and his wife Odelint according to a decree by King Otto III and is by far the oldest in the former Principality of Lüneburg. Its patron saint is John the Baptist. In 1482 a large part of the monastery was burned down following a lightning strike. Part of the brick walls and stained glass windows of the chapel are products of the subsequent late Gothic restoration. In 1626, during the Thirty Years War, it was plundered by Tilly's troops. During the period 1812-1815 the convent was closed and the monastery occupied by Napoleon for 3 years. Its chequered history ensured that many art treasur ...
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River Böhme
A river is a natural flowing watercourse, usually freshwater, flowing towards an ocean, sea, lake or another river. In some cases, a river flows into the ground and becomes dry at the end of its course without reaching another body of water. Small rivers can be referred to using names such as creek, brook, rivulet, and rill. There are no official definitions for the generic term river as applied to geographic features, although in some countries or communities a stream is defined by its size. Many names for small rivers are specific to geographic location; examples are "run" in some parts of the United States, "burn" in Scotland and northeast England, and "beck" in northern England. Sometimes a river is defined as being larger than a creek, but not always: the language is vague. Rivers are part of the water cycle. Water generally collects in a river from precipitation through a drainage basin from surface runoff and other sources such as groundwater recharge, springs, a ...
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Rischmannshof Heath Museum
The Rischmannshof Heath Museum (German: ''Heidemuseum Rischmannshof'') is an open-air museum in Walsrode, Germany. History Rischmannshof was opened in 1912 as one of the first open-air museums in Germany. The museum consists of a rural farmyard with outbuildings and other exhibits. The heart of the site is a thatched, timber-framed hall house (''Fachhallenhaus'') built as a two-post farmhouse dating to 1798. This originally stood in Hartem near Fallingbostel and was reconstructed in Walsrode. In addition the site has the house of a hireling (''Heuerling'' or ''Häusling'') originally from Fulde and about the same age, as well as a type of apiary, known locally as a ''Bienenzaun''. A ''Treppenspeicher'' storage barn from Oberndorfmark dates back to 1669. Not until some time later was the site enhanced with a bakehouse from the year 1752 and a timber-framed barn with a workshop from 1842. There is a branch of the museum in the old village school in Klein Eilstorf which itsel ...
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Fulde (Walsrode)
Fulde may refer to: *Fulde (Böhme), a river of Lower Saxony, Germany, tributary of the Böhme People with the surname *Gordian Fulde (born 1948), Australian emergency medicine specialist *Peter Fulde Peter Fulde (born 6 April 1936 in Breslau, now Wroclaw) is a physicist working in condensed matter theory and quantum chemistry. Fulde received a PhD degree at the University of Maryland in 1963. After spending more than one year as a postdo ... (born 1936), a physicist working in condensed matter theory and quantum chemistry {{disambiguation, surname German-language surnames German toponymic surnames ...
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Saalian Glaciation
The Saale glaciation or Saale Glaciation, sometimes referred to as the Saalian glaciation, Saale cold period (german: Saale-Kaltzeit), Saale complex (''Saale-Komplex'') or Saale glacial stage (''Saale-Glazial'', colloquially also the ''Saale-Eiszeit'' or ''Saale-Zeit''), covers the middle of the three large glaciations in Northern Europe and the northern parts of Eastern, Central and Western Europe by the Scandinavian Inland Ice Sheet between the older Elster glaciation and the younger Weichselian glaciation, also called the Last Glacial Period. Age and definitions It succeeded the Holstein interglacial and was followed by the Eemian interglacial. The Saale complex is currently estimated, depending on the source, as existing from around 300,000 to 130,000 years ago or 347,000 to 128,000 years ago (duration: around 219,000 years), roughly contemporaneous with the glaciation of the Riss Glacial in the Alpine region. The actual "ice age" includes only part of the Saale glaciation ...
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End Moraine
A terminal moraine, also called end moraine, is a type of moraine that forms at the terminal (edge) of a glacier, marking its maximum advance. At this point, debris that has accumulated by plucking and abrasion, has been pushed by the front edge of the ice, is driven no further and instead is deposited in an unsorted pile of sediment. Because the glacier acts very much like a conveyor belt, the longer it stays in one place, the greater the amount of material that will be deposited. The moraine is left as the marking point of the terminal extent of the ice. Formation As a glacier moves along its path, the surrounding area is continuously eroding. Loose rock and pieces of bedrock are constantly being picked up and transported with the glacier. Fine sediment and particles are also incorporated into the glacial ice. The accumulation of these rocks and sediment together form what is called glacial till when deposited. Push moraines are formed when a glacier retreats from a previou ...
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Weser
The Weser () is a river of Lower Saxony in north-west Germany. It begins at Hannoversch Münden through the confluence of the Werra and Fulda. It passes through the Hanseatic city of Bremen. Its mouth is further north against the ports of Bremerhaven and Nordenham. The latter is on the Butjadingen Peninsula. It then merges into the North Sea via two highly saline, estuarine mouths. It connects to the canal network running east-west across the North German Plain. The river, when combined with the Werra (a dialectal form of "Weser"), is long and thus, the longest river entirely situated within Germany (the Main, however, is the longest if the Weser and Werra are not combined). The Weser itself is long. The Werra rises in Thuringia, the German state south of the main projection (tongue) of Lower Saxony. Etymology "Weser" and "Werra" are the same words in different dialects. The difference reflects the old linguistic border between Central and Low German, passing through H ...
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