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Land Of Hadeln
Land Hadeln is a historic landscape and former administrative district in Northern Germany with its seat in Otterndorf on the Lower Elbe, the lower reaches of the River Elbe, in the Elbe-Weser Triangle between the estuaries of the Elbe and Weser. The name goes back to a place named ''Haduloha'' in the Royal Frankish Annals, which must have been in the north of Hohe Lieth moraine range, west of presentday Cuxhaven. Enthusiastic historians of late 19th and early 20th century postulated an Old Saxon '' Gau'' (district) of that name, but there is no evidence for this theory.Hans-Ulrich Hucker: Das Problem von Herrschaft und Freiheit in den Landesgemeinden des Mittelalters im Unterweserraum (Thesis, Münster 1978), available in Staatsarchiv Bremen (n°. 538 U) und in the Library of ''Männer vom Morgenstern'' historical society in Bremerhaven In the Middle Ages, the Land Hadeln was a fairly, but not perfectly, autonomous rural community, applying Saxon Law. Nominally, it belonged ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wappen Landhadeln
A coat of arms is a heraldry, heraldic communication design, visual design on an escutcheon (heraldry), escutcheon (i.e., shield), surcoat, or tabard (the latter two being outer garments). The coat of arms on an escutcheon forms the central element of the full achievement (heraldry), heraldic achievement, which in its whole consists of a shield, supporters, a crest (heraldry), crest, and a motto. A coat of arms is traditionally unique to an individual person, family, state, organization, school or corporation. The term itself of 'coat of arms' describing in modern times just the heraldic design, originates from the description of the entire medieval chainmail 'surcoat' garment used in combat or preparation for the latter. Roll of arms, Rolls of arms are collections of many coats of arms, and since the early Modern Age centuries, they have been a source of information for public showing and tracing the membership of a nobility, noble family, and therefore its genealogy across tim ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sachsenspiegel
The (; gml, Sassen Speyghel; modern nds, Sassenspegel; all literally "Saxon Mirror") is one of the most important law books and custumals compiled during the Holy Roman Empire. Originating between 1220 and 1235 as a record of existing local traditional customary laws and rulings, it was used in places until as late as 1900. Some legal principles as captured in the book reign into recent time laws throughout Europe. It is important not only for its lasting effect on later German and Dutch law but also as an early example of written prose in a German language. The Sachsenspiegel is the first comprehensive law book not in Latin, but in Middle Low German. A Latin edition is known to have existed, but only fragmented chapters remain. History The ''Sachsenspiegel'' was one of the first prose works written in the Middle Low German language. The original title is ''Sassen Speyghel'', ''Sachsenspiegel'' being a later Standard German translation. It is believed to have been compiled ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wingst
Wingst () is a municipality in the district of Cuxhaven, in Lower Saxony, Germany. Wingst belonged to the Prince-Archbishopric of Bremen, established in 1180. In 1648 the Prince-Archbishopric was transformed into the Duchy of Bremen, which was first ruled in personal union by the Swedish Crown - interrupted by a Danish occupation (1712–1715) - and from 1715 on by the Hanoverian Crown. In 1807 the ephemeric Kingdom of Westphalia annexed the Duchy, before France annexed it in 1810. 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 Real union is a union of two or more states, which share some state institutions in contrast to personal unions; however, they are not as unified as states in a political union. It is a development from personal union and has historically be ... and the Ducal territory, including Wingst, became part of the new Stade Region, establis ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Westerberg (Lamstedt)
The Westerberg (i.e. western hill) in is a low ridge in Northern Germany in the north of the collective municipality of Börde Lamstedt in the state of Lower Saxony. It is covered with mixed forest and, like the nearby Wingst ridge, it is an end moraine from the Saale glaciation period. Together with the Wingst it forms part of the eastern boundary of Land Hadeln. The ''Georgenhöhe'' ("George's Height") is its highest elevation at . In the middle of the Westerberg woods are ''inter alia'' a megalithic grave or dolmen, the ''Steinofen'' and a "stone garden", a collection of 106 examples of glacial erratics. A nunnery that later moved to Himmelpforten was originally seated on the hill.Georg von Issendorff, ''Kloster und Amt Himmelpforten. Nach Akten und Urkunden dargestellt'', reprint of the edition by "Stader Archiv", 1911/1913, extended by Clemens Förster, Stade and Buxtehude: Krause, 1979, pp. 5seq. No ISBN. The convent owned Westerberg hill with its forest. The erratics ar ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geest (topography)
Geest is a type of landform, slightly raised above the surrounding countryside, that occurs on the plains of Northern Germany, the Northern Netherlands and Denmark. It is a landscape of sandy and gravelly soils formed as a glacial outwash plain and now usually mantled by a heathland vegetation on the glacial deposits left behind after the last ice age during the Pleistocene epoch.Whittow, John (1984). ''Dictionary of Physical Geography''. London: Penguin, p. 214. . The term '' geest'' is a substantivisation of the Low German adjective ''güst'', which means "dry and infertile". It is an Old Drift landscape, characterised by the sandy depositions of the Ice Age. In the depressions between the raised flats are wet meadows and, where drainage is poor, bogs. Geest lands are made up of moraines and sandurs. They are almost always next to flat marshlands, the geest being higher and better protected against flood but, compared to the marsh, with poor soil for agriculture. Wher ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pleistocene
The Pleistocene ( , often referred to as the ''Ice age'') is the geological epoch that lasted from about 2,580,000 to 11,700 years ago, spanning the Earth's most recent period of repeated glaciations. Before a change was finally confirmed in 2009 by the International Union of Geological Sciences, the cutoff of the Pleistocene and the preceding Pliocene was regarded as being 1.806 million years Before Present (BP). Publications from earlier years may use either definition of the period. The end of the Pleistocene corresponds with the end of the last glacial period and also with the end of the Paleolithic age used in archaeology. The name is a combination of Ancient Greek grc, label=none, πλεῖστος, pleīstos, most and grc, label=none, καινός, kainós (latinized as ), 'new'. At the end of the preceding Pliocene, the previously isolated North and South American continents were joined by the Isthmus of Panama, causing a faunal interchange between the two reg ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Saale 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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Moraine
A moraine is any accumulation of unconsolidated debris ( regolith and rock), sometimes referred to as glacial till, that occurs in both currently and formerly glaciated regions, and that has been previously carried along by a glacier or ice sheet. It may consist of partly rounded particles ranging in size from boulders (in which case it is often referred to as boulder clay) down to gravel and sand, in a groundmass of finely-divided clayey material sometimes called glacial flour. Lateral moraines are those formed at the side of the ice flow, and terminal moraines were formed at the foot, marking the maximum advance of the glacier. Other types of moraine include ground moraines ( till-covered areas forming sheets on flat or irregular topography) and medial moraines (moraines formed where two glaciers meet). Etymology The word ''moraine'' is borrowed from French , which in turn is derived from the Savoyard Italian ("mound of earth"). ''Morena'' in this case was derived from Pr ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Meltwater
Meltwater is water released by the melting of snow or ice, including glacial ice, tabular icebergs and ice shelves over oceans. Meltwater is often found in the ablation zone of glaciers, where the rate of snow cover is reducing. Meltwater can be produced during volcanic eruptions, in a similar way in which the more dangerous lahars form. When meltwater pools on the surface rather than flowing, it forms melt ponds. As the weather gets colder meltwater will often re-freeze. Meltwater can collect or melt under the ice's surface. These pools of water, known as subglacial lakes can form due to geothermal heat and friction. Water source Meltwater provides drinking water for a large proportion of the world's population, as well as providing water for irrigation and hydroelectric plants. This meltwater can originate from seasonal snowfall, or from the melting of more permanent glaciers. Climate change threatens the precipitation of snow and the shrinking volume of glaciers. So ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Marsh
A marsh is a wetland that is dominated by herbaceous rather than woody plant species.Keddy, P.A. 2010. Wetland Ecology: Principles and Conservation (2nd edition). Cambridge University Press, Cambridge, UK. 497 p Marshes can often be found at the edges of lakes and streams, where they form a transition between the aquatic and terrestrial ecosystems. They are often dominated by grasses, rushes or reeds. If woody plants are present they tend to be low-growing shrubs, and the marsh is sometimes called a carr. This form of vegetation is what differentiates marshes from other types of wetland such as swamps, which are dominated by trees, and mires, which are wetlands that have accumulated deposits of acidic peat. Marshes provide habitats for many kinds of invertebrates, fish, amphibians, waterfowl and aquatic mammals. This biological productivity means that marshes contain 0.1% of global sequestered terrestrial carbon. Moreover, they have an outsized influence on climate ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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