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Eversen (Bergen)
Eversen is a village in the town of Bergen in the northern part of Celle district on the Lüneburg Heath in the north German state of Lower Saxony. Although Eversen was mentioned for the first time in a feudal register dating from 1330, the earliest archaeological discoveries stem from the Paleolithic period. The village is on the edge of the Südheide Nature Park and was an independent municipality until it was incorporated into the borough of Bergen in 1973. It has an area of and a population of 1,270 inhabitants (2019). Geography Geographical location Eversen is located on the boundary of the Südheide Nature Park about north of the town of Celle and about southwest of Hermannsburg on the L 240 state road that runs from Celle to Hermannsburg. The village lies on a sandy island of loess in the glacial valley of the Örtze which was formed in the Weichselian Ice Age. It is responsible for administering the neighbouring hamlets of Feuerschützenbostel and Altensalzkoth ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bergen, Lower Saxony
Bergen ( Eastphalian: ''Bargen'') is a town in the north of Celle district on the Lüneburg Heath, in Lower Saxony, Germany. Administratively it acts as a municipal borough divided into 12 subordinate parishes based on the town and its surrounding villages: Becklingen, Belsen, Bergen, Bleckmar, Diesten, Dohnsen, Eversen, Hagen, Hassel, Offen, Sülze and Wardböhmen. Bergen-Belsen concentration camp was located in the area of Belsen. The town had 13,099 inhabitants according to the census conducted in December 2008. Members of the British military and their families, who were not included in the census, brought the actual population to about 17,000. These soldiers occupied a NATO base and exercise on the Bergen-Hohne Training Area just outside the town, but the base closed in summer 2015 as part of the British Army's withdrawal from Germany. The ''Sieben Steinhäuser'', a cluster of dolmens dating from the Stone Age, are located within the training area. Geography Bergen is loca ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kolk (bog)
A bog pond (german: Moorauge) is a waterbody in the middle of a raised bog, raised or kettle bog, formerly also in percolating mires (''Durchströmungsmooren''). It is also called a bog pool, bog eye, raised bog kolk, bog kolk or just kolk. Bog ponds owe their existence to the growth of the bog body and are thus of biogenic origin. Brown bog ponds are surrounded by peat and receive their water exclusively from precipitation or from the large rain storage capacity of raised bogs. Such kolks generally represent the non-evaporating excess water of a bog. The central waterbody of these bogs exhibit almost no sedimentation. The accumulation of nutrients can lead to the formation of floating mats. Their vegetation differs from that of other structures in the bog. Usually the edges of the kolk are more nutrient-rich as a result of Mineralization (biology), mineralisation processes caused by wave and wind action. Here, woody plants such as downy birch (''Betula pubescens'') and other sp ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Enfeoffed
In the Middle Ages, especially under the European feudal system, feoffment or enfeoffment was the deed by which a person was given land in exchange for a pledge of service. This mechanism was later used to avoid restrictions on the passage of title in land by a system in which a landowner would give land to one person for the use of another. The common law of estates in land grew from this concept. Etymology The word ''feoffment'' derives from the Old French or ; compare with the Late Latin . England In English law, feoffment was a transfer of land or property that gave the new holder the right to sell it as well as the right to pass it on to his heirs as an inheritance. It was total relinquishment and transfer of all rights of ownership of an estate in land from one individual to another. In feudal England a feoffment could only be made of a fee (or "fief"), which is an estate in land, that is to say an ownership of rights over land, rather than ownership of the land itself, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Enfeoffment
In the Middle Ages, especially under the European feudal system, feoffment or enfeoffment was the deed by which a person was given land in exchange for a pledge of service. This mechanism was later used to avoid restrictions on the passage of title in land by a system in which a landowner would give land to one person for the use of another. The common law of estates in land grew from this concept. Etymology The word ''feoffment'' derives from the Old French or ; compare with the Late Latin . England In English law, feoffment was a transfer of land or property that gave the new holder the right to sell it as well as the right to pass it on to his heirs as an inheritance. It was total relinquishment and transfer of all rights of ownership of an estate in land from one individual to another. In feudal England a feoffment could only be made of a fee (or "fief"), which is an estate in land, that is to say an ownership of rights over land, rather than ownership of the land itself, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Duchy Of Saxony
The Duchy of Saxony ( nds, Hartogdom Sassen, german: Herzogtum Sachsen) was originally the area settled by the Saxons in the late Early Middle Ages, when they were subdued by Charlemagne during the Saxon Wars from 772 and incorporated into the Carolingian Empire (Francia) by 804. Upon the 843 Treaty of Verdun, Saxony was one of the five German stem duchies of East Francia; Duke Henry the Fowler was elected German king in 919. Upon the deposition of the Welf duke Henry the Lion in 1180, the ducal title fell to the House of Ascania, while numerous territories split from Saxony, such as the Principality of Anhalt in 1218 and the Welf Duchy of Brunswick-Lüneburg in 1235. In 1296 the remaining lands were divided between the Ascanian dukes of Saxe-Lauenburg and Saxe-Wittenberg, the latter obtaining the title of Electors of Saxony by the Golden Bull of 1356. Geography The Saxon stem duchy covered the greater part of present-day Northern Germany, including the modern German states ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
New Stone Age
The Neolithic period, or New Stone Age, is an Old World archaeological period and the final division of the Stone Age. It saw the Neolithic Revolution, a wide-ranging set of developments that appear to have arisen independently in several parts of the world. This "Neolithic package" included the introduction of farming, domestication of animals, and change from a hunter-gatherer lifestyle to one of settlement. It began about 12,000 years ago when farming appeared in the Epipalaeolithic Near East, and later in other parts of the world. The Neolithic lasted in the Near East until the transitional period of the Chalcolithic (Copper Age) from about 6,500 years ago (4500 BC), marked by the development of metallurgy, leading up to the Bronze Age and Iron Age. In other places the Neolithic followed the Mesolithic (Middle Stone Age) and then lasted until later. In Ancient Egypt, the Neolithic lasted until the Protodynastic period, 3150 BC.Karin Sowada and Peter Grave. Egypt in the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sand Dunes
A dune is a landform composed of wind- or water-driven sand. It typically takes the form of a mound, ridge, or hill. An area with dunes is called a dune system or a dune complex. A large dune complex is called a dune field, while broad, flat regions covered with wind-swept sand or dunes with little or no vegetation are called ''ergs'' or ''sand seas''. Dunes occur in different shapes and sizes, but most kinds of dunes are longer on the stoss (upflow) side, where the sand is pushed up the dune, and have a shorter ''slip face'' in the lee side. The valley or trough between dunes is called a ''dune slack''. Dunes are most common in desert environments, where the lack of moisture hinders the growth of vegetation that would otherwise interfere with the development of dunes. However, sand deposits are not restricted to deserts, and dunes are also found along sea shores, along streams in semiarid climates, in areas of glacial outwash, and in other areas where poorly cemented san ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Middle Stone Age
The Middle Stone Age (or MSA) was a period of African prehistory between the Early Stone Age and the Late Stone Age. It is generally considered to have begun around 280,000 years ago and ended around 50–25,000 years ago. The beginnings of particular MSA stone tools have their origins as far back as 550–500,000 years ago and as such some researchers consider this to be the beginnings of the MSA. The MSA is often mistakenly understood to be synonymous with the Middle Paleolithic of Europe, especially due to their roughly contemporaneous time span, however, the Middle Paleolithic of Europe represents an entirely different hominin population, ''Homo neanderthalensis'', than the MSA of Africa, which did not have Neanderthal populations. Additionally, current archaeological research in Africa has yielded much evidence to suggest that modern human behavior and cognition was beginning to develop much earlier in Africa during the MSA than it was in Europe during the Middle Paleoli ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Flint
Flint, occasionally flintstone, is a sedimentary cryptocrystalline form of the mineral quartz, categorized as the variety of chert that occurs in chalk or marly limestone. Flint was widely used historically to make stone tools and start fires. It occurs chiefly as nodules and masses in sedimentary rocks, such as chalks and limestones.''The Flints from Portsdown Hill'' Inside the nodule, flint is usually dark grey, black, green, white or brown in colour, and often has a glassy or waxy appearance. A thin layer on the outside of the nodules is usually different in colour, typically white and rough in texture. The nodules can often be found along s and |
