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Teufelsmoor
The Teufelsmoor is a region of bog and moorland north of Bremen, Germany. It forms a large part of the district of Landkreis Osterholz, Osterholz, and extends into the neighbouring districts of Landkreis Rotenburg (Wümme), Rotenburg (Gnarrenburg municipality). Geography The Depression (geology), depression is drained by the rivers Hamme (river), Hamme, Wümme and Wörpe. The Teufelsmoor extends over an area of about and is bordered in the west by the Wesermünde Geest and in the east by the Zeven Geest. The eponymous Teufelsmoor itself is an ombrotrophic raised bog that becomes a fen in the vicinity of the streams that drain it. It is one of the largest contiguous areas of bog in northwest Germany. Its largest extent is about 20 by 20 km. The oldest parts of the terrain in Grasberg have layers of peat eleven metres deep or more. In the centre of the moor is the Worpswede artists' colony, made famous by many landscape artists, which is near the sandy hill of the Weyerberg. ...
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Torfschiffswerft Schlussdorf
The Turf Shipyard () in , Lower Saxony, Germany, is a former boat builder's yard now used as an open-air museum. The yard, operating from 1850 to 1954, was specialised on barges to transport turf, that is dried peat used as fuel. In 1975 the (i.e. Schlussdorf Traditions Club) started to rescue the dilapidated shipyard buildings and reopened the site as a museum in 1977. The Turf Shipyard is about north of Worpswede's outskirts.Barbara Pannewick, „Worpswede, Heimat der Kunst“, in: ''Bremen: Entdeckerhandbuch für Stadt und Umland'', Sabine Gorsemann (ed.), (=Peter Meyer Reiseführer), Frankfurt am Main: Peter Meyer, 22005, pp. 171–177, here p. 176. . The Turf Shipyard is the only of its kind preserved in Northern Germany. As a museum it is undoubtedly in the front row of Worpswede's tourist sights.Michael Schön„Café im Torfschiffswerft-Museum: Kaffee und Kuchen sollen Besucher locken“ in: ''Wümme-Zeitung'', 11 March 2015, retrieved on 18 November ...
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Weyerberg
The Weyerberg is a sandy geest (topography), geest island, high, in the Teufelsmoor ("Devil's Bog") in Northern Germany. It is located near its main settlement of Worpswede in the district of Landkreis Osterholz, Osterholz in Lower Saxony. Its name means something like 'wooded hill'. It probably emerged at the end of the ice age, when meltwaters deposited sand around its clay core. Traces of the New Stone Age were found on and around the hill: stone tools and items of jewellery. Urn graves dating to 1100 BC were discovered on the southern slopes, the ''Hinterm Berg''. In 500 BC, the hill was abandoned as a settlement again as the climate cooled down. In 1218 Worpswede was first mentioned in the records because the eight farms there were Tithe, tithing to Osterholz Abbey. Several landmarks are located on the Weyerberg, such as the Cheese Dome House after designs by Bruno Taut, the Worpswede#Second generation of artists, Lower Saxony Stone by Bernhard Hoetger, and the Zion's Chu ...
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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 an artistic community since the end of the 19th century. History The origins of Worpswede date 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 abolished and its territory became part of ...
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Hamme (river)
The Hamme (in its upper reaches Giehler Bach) is a long river in Germany, Lower Saxony, north-east of Bremen (city), 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 (topography), geest plateau at a height of about , which is also the source of many other geest streams (such as the Drepte, Scharmbec ...
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Wesermünde Geest
The Wesermünde Geest (; Northern Low Saxon: ''Wersermünner Geest'') is the collective name for several geest ridges in the west of Cuxhaven district and Bremen's in northern Germany. The ridges are separated from one another by wetlands. These terminal moraines were formed during the Saale glaciation, are up to between above sea level (NN), and are covered by scattered woods and farmland. The wetland areas, between above sea level, are predominantly used for grazing. Location The Wesermünde is bounded to the south by the River Lesum in the northern part of Bremen, to the west by the marshes of (on the Lower Weser south of Bremerhaven) and Land Wursten (on the Outer Weser north of Bremerhaven). To the north, the Wesermünde Geest is bordered by the Land Hadeln, part of the Elbe marshes, and the Elbe estuary near Cuxhaven. Its eastern boundary is formed by the rivers Oste, as far as the town of Bremervörde, and Hamme with the great bog of the Teufelsmoor near Osterhol ...
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Landkreis Osterholz
Osterholz is a district (''Landkreis'') in Lower Saxony, Germany. It is bounded by (from the west and clockwise) the districts of Wesermarsch, Cuxhaven, Rotenburg and Verden, and by the city of Bremen. History Originally the prince-archbishops of Bremen ruled the area comprising today's district. 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. In 1807 the ephemeral Kingdom of Westphalia annexed the Duchy, before France annexed it in 1810, there comprising a part of the département Bouches-du-Weser. In 1813 the Duchy was restored to the Electorate of Hanover, which - after its upgrade to the Kingdom of Hanover in 1814 - incorporated the Duchy in a real union and the Ducal territory became part of the Stade Region, established in 1823. In 1866 the Kingdom of Hanover fell to Prussia, forming the Province of Hanover. The Prussian administration established d ...
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Raised Bog
Raised bogs, also called ombrotrophic bogs, are acidic, wet habitats that are poor in mineral salts and are home to flora and fauna that can cope with such extreme conditions. Raised bogs, unlike fens, are exclusively fed by precipitation (ombrotrophy) and from mineral salts introduced from the air. They thus represent a special type of bog, hydrologically, ecologically and in terms of their development history, in which the growth of peat mosses over centuries or millennia plays a decisive role. They also differ in character from blanket bogs which are much thinner and occur in wetter, cloudier climatic zones. Raised bogs are very threatened by peat cutting and pollution by mineral salts from the surrounding land (due to agriculture and Industrial sector, industry). The last great raised bog regions are found in western Siberia and Canada. Terminology The term ''raised bog'' derives from the fact that this type of bog rises in height over time as a result of peat formation. T ...
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Zeven Geest
The Zeven Geest (), which is part of the Stade Geest, is an area of sandy terrain in the northeast of the German state of Lower Saxony. It is named after the town of Zeven. Geography The Zeven Geest lies in the Elbe-Weser Triangle between the cities of Hamburg, Bremen and Bremerhaven. It covers the area between Sottrum, Bremervörde, Stade, Buxtehude, Tostedt, Scheeßel and Rotenburg (Wümme). It borders in the west on the Hamme-Oste Lowland and the Teufelsmoor, in the south on the Wümme Lowland and in the northwest on the Wesermünde Geest. Administrative affiliation The region of the Zeven Geest belongs administratively to the rural districts (''Landkreisen'') of Landkreis Verden, Verden, Landkreis Harburg, Harburg, Landkreis Rotenburg (Wümme), Rotenburg (Wümme) and Landkreis Stade, Stade, that were formerly part of the Regierungsbezirk Stade, Stade administrative district. Towns and villages *Apensen *Bremervörde *Buxtehude *Gnarrenburg *Gyhum *Harsefeld *Heeslingen *O ...
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Maid
A maid, housemaid, or maidservant is a female domestic worker. In the Victorian era, domestic service was the second-largest category of employment in England and Wales, after agricultural work. In developed Western nations, full-time maids are now typically only found in the wealthiest households. In other parts of the world (mainly within the continent of Asia), maids remain common in urban middle-class households. in Middle English meant an unmarried woman, especially a young one, or specifically a virgin. These meanings lived on in English until recent times (and are still familiar from literature and folk music), alongside the sense of the word as a type of servant. Description Maids perform typical domestic chores such as laundry, ironing, cleaning the house, grocery shopping, cooking, and caring for household pets. They may also take care of children, although there are more specific occupations for this, such as nanny. In some poor countries, maids take care of t ...
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Peat
Peat is an accumulation of partially Decomposition, decayed vegetation or organic matter. It is unique to natural areas called peatlands, bogs, mires, Moorland, moors, or muskegs. ''Sphagnum'' moss, also called peat moss, is one of the most common components in peat, although many other plants can contribute. The biological features of sphagnum mosses act to create a habitat aiding peat formation, a phenomenon termed 'habitat manipulation'. Soils consisting primarily of peat are known as histosols. Peat forms in wetland conditions, where flooding or stagnant water obstructs the flow of oxygen from the atmosphere, slowing the rate of decomposition. Peat properties such as organic matter content and saturated hydraulic conductivity can exhibit high spatial heterogeneity. Peatlands, particularly bogs, are the primary source of peat; although less common, other wetlands, including fens, pocosins and peat swamp forests, also deposit peat. Landscapes covered in peat are home to sp ...
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Hufe
An oxgang or bovate (; ; ; ) is an old land measurement formerly used in Scotland and England as early as the 16th century sometimes referred to as an oxgait. It averaged around 20 English acres, but was based on land fertility and cultivation, and so could be as low as 15. An oxgang is also known as a ''bovate'', from ''bovāta'', a Medieval Latinisation of the word, derived from the Latin '' bōs'', meaning "ox, bullock or cow". Oxen, through the Scottish Gaelic word ''damh'' or ''dabh'', also provided the root of the land measurement 'daugh'. Skene in ''Celtic Scotland'' says: : "in the eastern district there is a uniform system of land denomination consisting of ' dabhachs', 'ploughgates' and 'oxgangs', each 'dabhach' consisting of four 'ploughgates' and each 'ploughgate' containing eight 'oxgangs'. :"As soon as we cross the great chain of mountains Grampian Mountains] separating the North Sea, eastern from the Atlantic Ocean, western waters, we find a different system equa ...
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Burlak
A burlak ( rus, бурла́к, p=bʊrˈlak) was a river boat or barge puller in the Russian Empire. It was a seasonal occupation.Виноградовв Д. ВИстория бурлачества в России Korea Open Access Journals. 2018, vol. 28, no. 2, pp. 197–226 Burlaks as an occupation appeared in Russia at the end of 16th century and beginning of the 17th century. With the expansion of freight-hauling, the number of burlaks increased. With the proliferation of steamships, the demand in burlaks diminished and they basically disappeared by the end of the 19th century. Overview There were ''seasonal'' burlaks, who worked from spring to autumn, and ''temporary'' burlaks, who worked occasionally. Burlaks did not work in winter, when most Russian rivers were frozen over. The main areas of the burlaks' trade in the Russian Empire were the Volga river, from Moscow to Astrakhan, the White Sea route (''Belomor'e''), from Moscow to Arkhangelsk, and the Dnieper river, in Ukr ...
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