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Devil's Dyke, Cambridgeshire
Devil's Dyke or Devil's Ditch is a linear earthen barrier, thought to be of Anglo-Saxon origin, in eastern Cambridgeshire and Suffolk. It runs for in an almost straight line from Reach to Woodditton, with a ditch and bank system facing southwestwards, blocking the open chalkland between the marshy fens to the north and the formerly wooded hills to the south. It is a Scheduled Monument, a biological Site of Special Scientific Interest and a Special Area of Conservation. Description The name ''Devil's Ditch'' or ''Dyke'' is a post- medieval one. In medieval times it was simply called the ''dic'' ("the ditch"), or ''le Micheldyche'' or ''magnum fossatum'' ("great ditch"). Devil's Dyke is over long and is the largest of a series of ancient dykes in Cambridgeshire. In some places the bank measures high and across. The highest point along the Devil's Dyke is at Gallows Hill, where it measures from the bottom of the ditch to the top of the earth wall. Since the 19th centu ...
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Anglo-Saxon
The Anglo-Saxons were a cultural group who inhabited England in the Early Middle Ages. They traced their origins to settlers who came to Britain from mainland Europe in the 5th century. However, the ethnogenesis of the Anglo-Saxons happened within Britain, and the identity was not merely imported. Anglo-Saxon identity arose from interaction between incoming groups from several Germanic tribes, both amongst themselves, and with indigenous Britons. Many of the natives, over time, adopted Anglo-Saxon culture and language and were assimilated. The Anglo-Saxons established the concept, and the Kingdom, of England, and though the modern English language owes somewhat less than 26% of its words to their language, this includes the vast majority of words used in everyday speech. Historically, the Anglo-Saxon period denotes the period in Britain between about 450 and 1066, after their initial settlement and up until the Norman Conquest. Higham, Nicholas J., and Martin J. Ryan. ''The A ...
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Roman Britain
Roman Britain was the period in classical antiquity when large parts of the island of Great Britain were under occupation by the Roman Empire. The occupation lasted from AD 43 to AD 410. During that time, the territory conquered was raised to the status of a Roman province. Julius Caesar invaded Britain in 55 and 54 BC as part of his Gallic Wars. According to Caesar, the Britons had been overrun or culturally assimilated by other Celtic tribes during the British Iron Age and had been aiding Caesar's enemies. He received tribute, installed the friendly king Mandubracius over the Trinovantes, and returned to Gaul. Planned invasions under Augustus were called off in 34, 27, and 25 BC. In 40 AD, Caligula assembled 200,000 men at the Channel on the continent, only to have them gather seashells ('' musculi'') according to Suetonius, perhaps as a symbolic gesture to proclaim Caligula's victory over the sea. Three years later, Claudius directed f ...
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Brent Ditch
Brent Ditch is generally assumed to be an Anglo-Saxon earthwork in Southern Cambridgeshire, England, built around the 6th and 7th Centuries . However most of its structure has been lost over time. The site is scheduled as an ancient monument by Historic England. 2 km (~1mile) in length it runs from Pampisford Hall in the North-West to Abington in the South-East. For most of its length it is wooded and it is on private land and so difficult to access. It was built as a defensive structure to control the flow of trade along ancient routes. In modern times it is bisected by the routes of the old and new A11. It is from the old single carriageway road (grid reference TL514474) that the structure is best viewed as a low ditch in a wooded area besides the road. The earth works at this point are 2 to 3 m high. The dyke is one of the smaller earthworks of several in south Cambridgeshire designed to control movement along the ancient Roman roads. The others are Devil's Dyke, Flea ...
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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 ...
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Flores Historiarum
The ''Flores Historiarum'' (Flowers of History) is the name of two different (though related) Latin chronicles by medieval English historians that were created in the 13th century, associated originally with the Abbey of St Albans. Wendover's ''Flores Historiarum'' The first ''Flores Historiarum'' was created by St Albans writer, Roger of Wendover, who carried his chronology from the Creation up to 1235, the year before his death. Roger claims in his preface to have selected "from the books of catholic writers worthy of credit, just as flowers of various colours are gathered from various fields." Hence he also called his work ''Flores Historiarum''. However, like most chronicles, it is now valued not so much for what was culled from previous writers, as for its full and lively narrative of contemporary events from 1215 to 1235, including the signing of Magna Carta by King John at Runnymede. The book has survived in one thirteenth-century manuscript in the Bodleian Library (Dou ...
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Abbo Of Fleury
Abbo or Abbon of Fleury ( la, Abbo Floriacensis;  – 13 November 1004), also known as Saint Abbo or Abbon, was a monk and abbot of Fleury Abbey in present-day Saint-Benoît-sur-Loire near Orléans, France. Life Abbo was born near Orléans and brought up in the Benedictine abbey of Fleury. He was educated at Paris and Reims, devoting himself to philosophy, mathematics, and astronomy. He spent two years (985-987) in England, mostly in the newly founded monastery of Ramsey in Huntingdonshire, assisting Archbishop Oswald of York in restoring the monastic system. He was also abbot and director of the school of this newly founded monastery from 986 to 987. Abbo returned to Fleury in 988, where he was selected as its abbot after Abbot Oilbold's death. Another monk who had secured the support of the King and the Bishop of Orléans contested the choice and the matter assumed national importance. Gerbert of Aurillac later Pope Sylvester II, settled the matter in Abbo's favor. T ...
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Danes
Danes ( da, danskere, ) are a North Germanic ethnic group and nationality native to Denmark and a modern nation identified with the country of Denmark. This connection may be ancestral, legal, historical, or cultural. Danes generally regard themselves as a nationality and reserve the word "ethnic" for the description of recent immigrants, sometimes referred to as "new Danes". The contemporary Danish national identity is based on the idea of "Danishness", which is founded on principles formed through historical cultural connections and is typically not based on racial heritage. History Early history Denmark has been inhabited by various Germanic peoples since ancient times, including the Angles, Cimbri, Jutes, Herules, Teutones and others. The first mentions of " Danes" are recorded in the mid-6th century by historians Procopius ( el, δάνοι) and Jordanes (''danī''), who both refer to a tribe related to the Suetidi inhabiting the peninsula of Jutland, the province of ...
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Edward The Elder
Edward the Elder (17 July 924) was King of the Anglo-Saxons from 899 until his death in 924. He was the elder son of Alfred the Great and his wife Ealhswith. When Edward succeeded to the throne, he had to defeat a challenge from his cousin Æthelwold, who had a strong claim to the throne as the son of Alfred's elder brother and predecessor, Æthelred I. Alfred had succeeded Æthelred as king of Wessex in 871, and almost faced defeat against the Danish Vikings until his decisive victory at the Battle of Edington in 878. After the battle, the Vikings still ruled Northumbria, East Anglia and eastern Mercia, leaving only Wessex and western Mercia under Anglo-Saxon control. In the early 880s Æthelred, Lord of the Mercians, the ruler of western Mercia, accepted Alfred's lordship and married his daughter Æthelflæd, and around 886 Alfred adopted the new title King of the Anglo-Saxons as the ruler of all Anglo-Saxons not subject to Danish rule. Edward inherited the new title ...
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Anglo-Saxon Chronicle
The ''Anglo-Saxon Chronicle'' is a collection of annals in Old English, chronicling the history of the Anglo-Saxons. The original manuscript of the ''Chronicle'' was created late in the 9th century, probably in Wessex, during the reign of Alfred the Great (r. 871–899). Multiple copies were made of that one original and then distributed to monasteries across England, where they were independently updated. In one case, the ''Chronicle'' was still being actively updated in 1154. Nine manuscripts survive in whole or in part, though not all are of equal historical value and none of them is the original version. The oldest seems to have been started towards the end of Alfred's reign, while the most recent was written at Peterborough Abbey after a fire at that monastery in 1116. Almost all of the material in the ''Chronicle'' is in the form of annals, by year; the earliest are dated at 60 BC (the annals' date for Caesar's invasions of Britain), and historical material follows up ...
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Devil's Dyke (1853)
Devil's Dyke may refer to: * Devil's Dykes, a series of Roman fortifications between Hungary and Serbia *Devil's Dyke, Cambridgeshire, an earthen barrier in eastern Cambridgeshire *Devil's Dyke, Hertfordshire, a prehistoric defensive ditch in Hertfordshire *Devil's Dyke, Sussex Devil's Dyke is a 100 metre deep V-shaped dry valley on the South Downs in Sussex in southern England, north-west of Brighton. It is managed by the National Trust, and is also part of the Beeding Hill to Newtimber Hill Site of Special Scienti ..., a valley on the South Downs Way See also: * Deil's Dyke, earthwork in Scotland {{Disambig ...
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Radiocarbon Dating
Radiocarbon dating (also referred to as carbon dating or carbon-14 dating) is a method for determining the age of an object containing organic material by using the properties of radiocarbon, a radioactive isotope of carbon. The method was developed in the late 1940s at the University of Chicago by Willard Libby. It is based on the fact that radiocarbon () is constantly being created in the Earth's atmosphere by the interaction of cosmic rays with atmospheric nitrogen. The resulting combines with atmospheric oxygen to form radioactive carbon dioxide, which is incorporated into plants by photosynthesis; animals then acquire by eating the plants. When the animal or plant dies, it stops exchanging carbon with its environment, and thereafter the amount of it contains begins to decrease as the undergoes radioactive decay. Measuring the amount of in a sample from a dead plant or animal, such as a piece of wood or a fragment of bone, provides information that can be used to ca ...
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Fleam Dyke
Fleam Dyke is a linear earthwork between Fulbourn and Balsham in Cambridgeshire, initiated at some timepoint between AD 330 and AD 510. It is three miles long and seven metres high from ditch to bank, and its ditch faces westwards, implying invading Saxons as its architects. Later, it formed a boundary of the Anglo-Saxon administrative division of Flendish Hundred. At a prominent point, the earthwork runs beside Mutlow Hill, crowned by a 4000-year-old Bronze Age burial mound. Description The dyke is located near Cambridge, between Fulbourn and Balsham. It forms a barrier across an open chalkland ridge, bounded near Fulbourn by marshy fenland and near Balsham by 90-metre-high formerly wooded hills ("The Ambush"). It is three miles long and seven metres high from ditch to bank, and its ditch faces southwest. Most of the earthwork survives and a footpath leads along the crest of the bank (now part of the modern Harcamlow Way long distance footpath). Possible extensions to Fleam ...
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