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Sülze Saltworks
The Sülze Saltworks (german: Saline Sülze) was a 'saline', or saltworks, on the Lüneburg Heath in Germany which was worked for centuries, from the High Middle Ages to 1862. It had a considerable impact on the history of the village of Sülze and other heath villages in the area. History The saline is first mentioned in the records in 1381 and, from that time on, salt was extracted from brine in Sülze. The development of Sülze's salt spring was strongly encouraged by the dukes of the Principality of Lüneburg who wanted to create a counterbalance to the town of Lüneburg, which had largely succeeded in maintaining its independence from territorial lords as a result of the salt trade. This intent was never realised, however, because a glance at the quantities of salt produced demonstrates the overwhelming supremacy of the Lüneburg Saltworks. Whilst an average of 110,000 t of salt was extracted annually in Lüneburg, Sülze generated no more than 4,000 t. In addition ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Saltworks
A saltern is an area or installation for making salt. Salterns include modern salt-making works (saltworks), as well as hypersaline waters that usually contain high concentrations of halophilic microorganisms, primarily haloarchaea but also other halophiles including algae and bacteria. Salterns usually begin with seawater as the initial source of brine but may also use natural saltwater springs and streams. The water is evaporated, usually over a series of ponds, to the point where sodium chloride and other salts precipitate out of the saturated brine, allowing pure salts to be harvested. Where complete evaporation in this fashion was not routinely achievable due to weather, salt was produced from the concentrated brine by boiling the brine. Background Earliest examples of pans used in the solution mining of salt date back to prehistoric times and the pans were made of ceramics known as briquetage. Later examples were made from lead and then iron. The change from lead to iron c ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Salt Evaporation Pond
A salt evaporation pond is a shallow artificial salt pan designed to extract salts from sea water or other brines. The Salt pans are shallow and large of size because it will be easier for sunlight to travel and reach the sea water. Natural salt pans are geological formations that are also created by water evaporating and leaving behind salts. Some salt evaporation ponds are only slightly modified from their natural version, such as the ponds on Great Inagua in the Bahamas, or the ponds in Jasiira, a few kilometres south of Mogadishu, where seawater is trapped and left to evaporate in the sun. The seawater or brine is fed into large ponds and water is drawn out through natural evaporation which allows the salt to be subsequently harvested. The ponds also provide a productive resting and feeding ground for many species of waterbirds, which may include endangered species. The ponds are commonly separated by levees. Salt evaporation ponds may also be called salterns, salt works or ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Örtze
Örtze () is a river of Lower Saxony, Germany. The Örtze rises north of Munster in the ''Große Heide'' (in the ''Raubkammer'' federal forest) and, after , joins the Aller southeast of Winsen. Source and course The Örtze valley is an old glacial valley. It was formed during the Saale glaciation about 230,000 to 130,000 years ago by the drainage of meltwater from the ice sheet which cut deep into the plateaus of the southern Lüneburg Heath. The upper Örtze has incised its own, much smaller valley into the sandur beds and the roughly wide, flat glacial valley floor. The source region of the Örtze and its several source bogs lie on the terrain of the Munster North Training Area. In order to remove suspended solids and sediments which are washed away during heavy rains from the tank training areas with their sparse covering of vegetation, four successive lakes – the so-called ''Munoseen'' – have been created on the Örtze, and, on the ''Ilster'', the main hea ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Diesten
Diesten is a village subordinated to the Lower Saxon town of Bergen in the northern part of Celle district on the Lüneburg Heath in northern Germany. It lies 20 km north of Celle on ''Kreisstraße'' K 240 and has 264 inhabitants. History Diesten was first mentioned in the records in 1235 under the name ''Dedesten''. It has always had a rural character and, even today, has retained its original village layout. The hamlets of Huxahl, 1 km north of Diesten, and Lindhorst 2 km to the west, are administratively part of Diesten. In Lindhorst there is an old oak, protected by law, that was mentioned in a document as long ago as the 15th century. Based on that it is at least 700 years old. Politics Following the Lower Saxony district and administrative reform of 1973, the Diesten has been part of the borough of Bergen Bergen (), historically Bjørgvin, is a city and municipality in Vestland county on the west coast of Norway. , its population is roughly 285 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Altensalzkoth
Altensalzkoth is a village in the Lower Saxon town of Bergen in north Germany. It belongs to the parish of Eversen in the district of Celle on the Lüneburg Heath. It lies 13 km north of Celle on the ''Landesstraße'' L 240 and currently has 65 inhabitants. History The history of Altensalzkoth is closely bound to the saltworks in Sülze. When the moors in the vicinity of Sülze were exhausted, the boiling sites were moved initially to the Bornrieth Moor from 1673 to 1678. In 1719 the first discussions took place about moving the boiling sites again, because the Bornrieth Moor was also being exhausted. To achieve this the existing pipes to the moor from Lindhorst along the Örtze, were moved eastwards past Eversen to the ''Scheuer Bruch'', south of Sülze, in the newly established village of Altensalzkoth. The survey staff charged with organising the move described this new site on their maps as ''Alte Salz kath'', from which the present name of the village was later de ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bornrieth Moor
The Bornrieth Moor (german: Bornriethmoor) is the remains of a raised bog in the German district of Celle and belongs to the Südheide Nature Park. It has an area of . The bog, which has had most of its peat extracted, was reflooded and placed under nature conservation protection in 1988. The moor was also designated as a Special Area of Conservation. The responsible nature conservation authority is the district of Celle. The area is out-of-bounds to the public. Several cranes have turned up here again and are breeding. The otherwise rare bog myrtle (''Myrica gale'') is common here. Much of the moor is covered by the common reed ('Phragmites'). Bog asphodel (Narthecium ossifragum), cottongrass (Eriophorum) and sundews (Drosera) may also be found here. History Salt boiling Between 1673 and 1678, boiling houses were built on the edge of the moor for the Sülze Saltworks, because the bogs in the vicinity of Sülze had been exhausted. Two salt houses were constructed here, each ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Graduation Tower
A graduation tower (occasionally referred to as a thorn house) is a structure used in the production of salt which removes water from a saline solution by evaporation, increasing its concentration of mineral salts. The tower consists of a wooden wall-like frame stuffed with bundles of brushwood (typically blackthorn) which have to be changed about every 5 to 10 years as they become encrusted with mineral deposits over time. The salt water runs down the tower and partly evaporates; at the same time some minerals from the solution are left behind on the brushwood twigs. Graduation towers can be found in a number of spa towns, primarily in Germany but also Poland and Austria. The mineral-rich water droplets in the air are regarded as having beneficial health effects similar to that of breathing in sea air. A large complex of graduation towers is located in Ciechocinek and Inowrocław, Poland.Affelt, Waldemar: Wooden masterwork of saline in Ciechocinek, Poland'', in: Santiago Huer ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lüneburg Saltworks
The Lüneburg Saltworks (german: Lüneburger Saline) was a saline in the German town of Lüneburg Lüneburg (officially the ''Hanseatic City of Lüneburg'', German: ''Hansestadt Lüneburg'', , Low German ''Lümborg'', Latin ''Luneburgum'' or ''Lunaburgum'', Old High German ''Luneburc'', Old Saxon ''Hliuni'', Polabian ''Glain''), also calle ... that extracted salt. According to legend, a hunter killed a wild boar whose coat was snow-white from crystallised salt. The sow must have wallowed in a salt spring and so the first source of salt was discovered in Lüneburg about 800 years ago. Operation From the 12th century salt mining was the dominant feature of life in the town of Lüneburg. At that time, table salt was almost as valuable as gold and was measured in ''chors'' (1 ''chor'' = 554.32 kg), one ''chor'' being worth about 300 Reichsmarks. The saline was located between ''Sülzwiese'' and the hill of the Lüneburg Kalkberg, Kalkberg. Its main entrance was on ''Lambe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lüneburg Heath
Lüneburg Heath (german: Lüneburger Heide) is a large area of heath, geest, and woodland in the northeastern part of the state of Lower Saxony in northern Germany. It forms part of the hinterland for the cities of Hamburg, Hanover and Bremen and is named after the town of Lüneburg. Most of the area is a nature reserve. Northern Low Saxon is still widely spoken in the region. Lüneburg Heath has extensive areas, and the most yellow of heathland, typical of those that covered most of the North German countryside until about 1800, but which have almost completely disappeared in other areas. The heaths were formed after the Neolithic period by overgrazing of the once widespread forests on the poor sandy soils of the geest, as this slightly hilly and sandy terrain in northern Europe is called. Lüneburg Heath is therefore a historic cultural landscape. The remaining areas of heath are kept clear mainly through grazing, especially by a North German breed of moorland sheep called th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lüneburg
Lüneburg (officially the ''Hanseatic City of Lüneburg'', German: ''Hansestadt Lüneburg'', , Low German ''Lümborg'', Latin ''Luneburgum'' or ''Lunaburgum'', Old High German ''Luneburc'', Old Saxon ''Hliuni'', Polabian ''Glain''), also called Lunenburg ( ) in English, is a town in the German state of Lower Saxony. It is located about southeast of another Hanseatic city, Hamburg, and belongs to that city's wider metropolitan region. The capital of the district which bears its name, it is home to roughly 77,000 people. Lüneburg's urban area, which includes the surrounding communities of Adendorf, Bardowick, Barendorf and Reppenstedt, has a population of around 103,000. Lüneburg has been allowed to use the title " Hansestadt" (''Hanseatic Town'') in its name since 2007, in recognition of its membership in the former Hanseatic League. Lüneburg is also home to Leuphana University. History ImageSize = width:1050 height:100 PlotArea = width:1000 height:50 left:50 bottom ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Principality Of Lüneburg
The Principality of Lüneburg (later also referred to as Celle) was a territorial division of the Duchy of Brunswick-Lüneburg within the Holy Roman Empire, immediately subordinate to the emperor. It existed from 1269 until 1705 and its territory lay within the modern-day state of Lower Saxony in Germany. The principality was named after its first capital, Lüneburg (also called Lunenburg in English), which was ruled jointly by all Brunswick-Lüneburg lines until 1637. From 1378, the seat of the principality was in Celle. It lost its independence in 1705 when it was annexed by the Electorate of Brunswick-Lüneburg, but retained its vote in the Reichstag as Brunswick-Celle. Territory When the Principality of Lüneburg emerged as a result of the division of Brunswick-Lüneburg in 1269, the domain of the Lüneburg princes consisted of a large number of territorial rights in the region of Lüneburg. However, it could not be described as a unified state, because many rights were owne ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
