About: List of scheduled monuments in Sedgemoor

An Entity of Type: place, from Named Graph: http://dbpedia.org, within Data Space: dbpedia.org

Sedgemoor is a low-lying area of land in Somerset, England. It lies close to sea level south of the Polden Hills, forming a large part of the Somerset Levels and Moors, a wetland area between the Mendips and the Blackdown Hills. The Neolithic people exploited the reed swamps for their natural resources and started to construct wooden trackways, including the world's oldest known timber trackway, the Post Track, dating to the 3800s BC. The Levels were the location of the Iron Age Glastonbury Lake Village as well as two lake villages at Meare Lake. Several settlements and hill forts were built on the natural "islands" of slightly raised land, including Brent Knoll and Glastonbury. In the Roman period sea salt was extracted and a string of settlements were set up along the Polden Hills.

thumbnail
Property Value
dbo:abstract
  • Sedgemoor is a low-lying area of land in Somerset, England. It lies close to sea level south of the Polden Hills, forming a large part of the Somerset Levels and Moors, a wetland area between the Mendips and the Blackdown Hills. The Neolithic people exploited the reed swamps for their natural resources and started to construct wooden trackways, including the world's oldest known timber trackway, the Post Track, dating to the 3800s BC. The Levels were the location of the Iron Age Glastonbury Lake Village as well as two lake villages at Meare Lake. Several settlements and hill forts were built on the natural "islands" of slightly raised land, including Brent Knoll and Glastonbury. In the Roman period sea salt was extracted and a string of settlements were set up along the Polden Hills. A scheduled monument is a nationally important archaeological site or monument which is given legal protection by being placed on a list (or "schedule") by the Secretary of State for Culture, Media and Sport; English Heritage takes the leading role in identifying such sites. The legislation governing this is the Ancient Monuments and Archaeological Areas Act 1979. The term "monument" can apply to the whole range of archaeological sites, and they are not always visible above ground. Such sites have to have been deliberately constructed by human activity. They range from prehistoric standing stones and burial sites, through Roman remains and medieval structures such as castles and monasteries, to later structures such as industrial sites and buildings constructed for the World Wars or the Cold War. There are 79 scheduled monuments in Sedgemoor. The oldest are Neolithic, Bronze Age or Iron Age including hill forts, bowl barrows and occupied caves including several in Cheddar Gorge. Cannington Camp (which is also known as Cynwit Castle) dates from the Bronze Age, while Brent Knoll Camp between the Somerset Levels and Brean Down is Iron Age (although there are some Bronze Age artefacts) and it was reused in the Roman period. The Romano-British period is represented with several sites. Medieval sites include several motte-and-bailey castles and church or village crosses. Industrial development, particularly in Bridgwater, are represented by brick and tile kilns and a telescopic railway bridge. The most recent monuments are World War II bunkers and bombing decoys on Black Down. The monuments are listed below using the titles given in the English Heritage data sheets. (en)
dbo:thumbnail
dbo:wikiPageID
  • 43644918 (xsd:integer)
dbo:wikiPageLength
  • 92219 (xsd:nonNegativeInteger)
dbo:wikiPageRevisionID
  • 1076742423 (xsd:integer)
dbo:wikiPageWikiLink
dbp:commonscat
  • Cheddar Palace (en)
  • Cheddar Market Cross (en)
  • Telescopic Bridge, Bridgwater (en)
  • Chandos Glass Cone (en)
dbp:completed
  • , Anglo-Saxon and Norman (en)
dbp:dateListed
  • 1925-02-12 (xsd:date)
  • 1925-11-30 (xsd:date)
  • 1929-12-19 (xsd:date)
  • 1933-07-19 (xsd:date)
  • 1933-07-20 (xsd:date)
  • 1934-02-26 (xsd:date)
  • 1946-06-21 (xsd:date)
  • 1949-03-31 (xsd:date)
  • 1953-03-11 (xsd:date)
  • 1954-10-23 (xsd:date)
  • 1960-12-01 (xsd:date)
  • 1966-11-22 (xsd:date)
  • 1967-03-20 (xsd:date)
  • 1967-05-03 (xsd:date)
  • 1967-06-15 (xsd:date)
  • 1968-10-22 (xsd:date)
  • 1969-11-26 (xsd:date)
  • 1972-11-17 (xsd:date)
  • 1974-01-16 (xsd:date)
  • 1974-03-12 (xsd:date)
  • 1976-01-14 (xsd:date)
  • 1976-10-15 (xsd:date)
  • 1976-11-02 (xsd:date)
  • 1976-12-22 (xsd:date)
  • 1977-06-13 (xsd:date)
  • 1977-12-22 (xsd:date)
  • 1981-10-09 (xsd:date)
  • 1991-03-18 (xsd:date)
  • 1991-03-19 (xsd:date)
  • 1991-09-04 (xsd:date)
  • 1992-01-07 (xsd:date)
  • 1993-10-06 (xsd:date)
  • 1996-03-06 (xsd:date)
  • 1996-05-20 (xsd:date)
  • 1996-06-28 (xsd:date)
  • 1999-08-11 (xsd:date)
  • 2000-11-24 (xsd:date)
  • 2001-08-14 (xsd:date)
  • 2001-08-28 (xsd:date)
  • 2003-04-01 (xsd:date)
  • 2013-11-26 (xsd:date)
dbp:gridRef
  • ST 18414 37782 (en)
  • ST 15423 37164 (en)
  • ST 16040 38477 (en)
  • ST 19678 39614 (en)
  • ST 21578 40581 (en)
  • ST 22431 32009 (en)
  • ST 22531 37018 (en)
  • ST 23987 35193 (en)
  • ST 24570 40268 (en)
  • ST 24682 40489 (en)
  • ST 26957 37771 (en)
  • ST 28179 30581 (en)
  • ST 28790 58958 (en)
  • ST 28938 37942 (en)
  • ST 29027 33052 (en)
  • ST 29852 37396 (en)
  • ST 29997 37635 (en)
  • ST 30020 37423 (en)
  • ST 30896 41366 (en)
  • ST 31297 46794 (en)
  • ST 31929 39272 (en)
  • ST 32916 49302 (en)
  • ST 33312 29034 (en)
  • ST 33826 29095 (en)
  • ST 34124 51021 (en)
  • ST 34330 29271 (en)
  • ST 34840 36180 (en)
  • ST 35497 37162 (en)
  • ST 37036 42486 (en)
  • ST 38800 42639 (en)
  • ST 39461 44433 (en)
  • ST 39680 55004 (en)
  • ST 41022 47891 (en)
  • ST 41142 43152 (en)
  • ST 42355 40466 (en)
  • ST 42679 39790 (en)
  • ST 42768 56077 (en)
  • ST 43345 58475 (en)
  • ST 43481 52403 (en)
  • ST 43534 58685 (en)
  • ST 43656 47849 (en)
  • ST 43666 39241 (en)
  • ST 44310 45626 (en)
  • ST 45260 50294 (en)
  • ST 45319 57012 (en)
  • ST 45748 56837 (en)
  • ST 45822 55799 (en)
  • ST 45954 58022 (en)
  • ST 45999 48984 (en)
  • ST 46442 56836 (en)
  • ST 46472 55781 (en)
  • ST 46539 55021 (en)
  • ST 46585 55059 (en)
  • ST 46612 55154 (en)
  • ST 46637 53897 (en)
  • ST 46688 53886 (en)
  • ST 46714 53917 (en)
  • ST 46737 54080 (en)
  • ST 46796 53936 (en)
  • ST 46849 56376 (en)
  • ST 46852 56110 (en)
  • ST 46862 54008 (en)
  • ST 46995 56339 (en)
  • ST 47085 56283 (en)
  • ST 47248 56680 (en)
  • ST 47589 55263 (en)
  • ST 47777 56015 (en)
  • ST 47960 57110 (en)
  • ST 48427 55846 (en)
  • ST 49457 53390 (en)
  • ST1530838148 (en)
  • ST1548538136 (en)
  • ST181363 (en)
  • ST186396 (en)
  • ST226336 (en)
  • ST420401 (en)
  • ST4247849658 (en)
  • ST456531 (en)
  • ST4592153202 (en)
dbp:lat
  • 51.056800 (xsd:double)
  • 51.057400 (xsd:double)
  • 51.059300 (xsd:double)
  • 51.070000 (xsd:double)
  • 51.082100 (xsd:double)
  • 51.092400 (xsd:double)
  • 51.096100 (xsd:double)
  • 51.110900 (xsd:double)
  • 51.119700 (xsd:double)
  • 51.121200 (xsd:double)
  • 51.127200 (xsd:double)
  • 51.127500 (xsd:double)
  • 51.128500 (xsd:double)
  • 51.130000 (xsd:double)
  • 51.131500 (xsd:double)
  • 51.131800 (xsd:double)
  • 51.133500 (xsd:double)
  • 51.134500 (xsd:double)
  • 51.136200 (xsd:double)
  • 51.136300 (xsd:double)
  • 51.139400 (xsd:double)
  • 51.148600 (xsd:double)
  • 51.149400 (xsd:double)
  • 51.149600 (xsd:double)
  • 51.150100 (xsd:double)
  • 51.154500 (xsd:double)
  • 51.156700 (xsd:double)
  • 51.157000 (xsd:double)
  • 51.159000 (xsd:double)
  • 51.159200 (xsd:double)
  • 51.160500 (xsd:double)
  • 51.167400 (xsd:double)
  • 51.178100 (xsd:double)
  • 51.179700 (xsd:double)
  • 51.184600 (xsd:double)
  • 51.195900 (xsd:double)
  • 51.207100 (xsd:double)
  • 51.216200 (xsd:double)
  • 51.227000 (xsd:double)
  • 51.227100 (xsd:double)
  • 51.237500 (xsd:double)
  • 51.239000 (xsd:double)
  • 51.243183 (xsd:double)
  • 51.249200 (xsd:double)
  • 51.254200 (xsd:double)
  • 51.268000 (xsd:double)
  • 51.274700 (xsd:double)
  • 51.275385 (xsd:double)
  • 51.277400 (xsd:double)
  • 51.281400 (xsd:double)
  • 51.281600 (xsd:double)
  • 51.281700 (xsd:double)
  • 51.282100 (xsd:double)
  • 51.282700 (xsd:double)
  • 51.283300 (xsd:double)
  • 51.291000 (xsd:double)
  • 51.291800 (xsd:double)
  • 51.292100 (xsd:double)
  • 51.293000 (xsd:double)
  • 51.294100 (xsd:double)
  • 51.298600 (xsd:double)
  • 51.298700 (xsd:double)
  • 51.299400 (xsd:double)
  • 51.300900 (xsd:double)
  • 51.301600 (xsd:double)
  • 51.303200 (xsd:double)
  • 51.303600 (xsd:double)
  • 51.304000 (xsd:double)
  • 51.306800 (xsd:double)
  • 51.308100 (xsd:double)
  • 51.309600 (xsd:double)
  • 51.310700 (xsd:double)
  • 51.318700 (xsd:double)
  • 51.322500 (xsd:double)
  • 51.324400 (xsd:double)
  • 51.325600 (xsd:double)
dbp:location
dbp:lon
  • -3.211900 (xsd:double)
  • -3.210000 (xsd:double)
  • -3.209300 (xsd:double)
  • -3.201500 (xsd:double)
  • -3.170000 (xsd:double)
  • -3.167400 (xsd:double)
  • -3.163000 (xsd:double)
  • -3.149700 (xsd:double)
  • -3.122800 (xsd:double)
  • -3.108800 (xsd:double)
  • -3.108400 (xsd:double)
  • -3.105000 (xsd:double)
  • -3.087200 (xsd:double)
  • -3.080800 (xsd:double)
  • -3.079900 (xsd:double)
  • -3.045300 (xsd:double)
  • -3.029000 (xsd:double)
  • -3.026400 (xsd:double)
  • -3.017100 (xsd:double)
  • -3.014800 (xsd:double)
  • -3.003900 (xsd:double)
  • -3.001500 (xsd:double)
  • -2.993800 (xsd:double)
  • -2.992100 (xsd:double)
  • -2.985000 (xsd:double)
  • -2.974600 (xsd:double)
  • -2.962300 (xsd:double)
  • -2.952900 (xsd:double)
  • -2.945600 (xsd:double)
  • -2.934580 (xsd:double)
  • -2.932400 (xsd:double)
  • -2.923200 (xsd:double)
  • -2.902100 (xsd:double)
  • -2.876900 (xsd:double)
  • -2.867800 (xsd:double)
  • -2.866400 (xsd:double)
  • -2.846000 (xsd:double)
  • -2.843500 (xsd:double)
  • -2.828800 (xsd:double)
  • -2.825700 (xsd:double)
  • -2.825437 (xsd:double)
  • -2.822300 (xsd:double)
  • -2.821000 (xsd:double)
  • -2.814400 (xsd:double)
  • -2.811700 (xsd:double)
  • -2.811500 (xsd:double)
  • -2.808300 (xsd:double)
  • -2.806800 (xsd:double)
  • -2.798600 (xsd:double)
  • -2.785800 (xsd:double)
  • -2.785700 (xsd:double)
  • -2.779700 (xsd:double)
  • -2.778900 (xsd:double)
  • -2.778500 (xsd:double)
  • -2.776900 (xsd:double)
  • -2.776655 (xsd:double)
  • -2.774900 (xsd:double)
  • -2.769700 (xsd:double)
  • -2.769100 (xsd:double)
  • -2.768100 (xsd:double)
  • -2.767400 (xsd:double)
  • -2.767000 (xsd:double)
  • -2.766500 (xsd:double)
  • -2.765800 (xsd:double)
  • -2.765100 (xsd:double)
  • -2.764200 (xsd:double)
  • -2.763800 (xsd:double)
  • -2.763700 (xsd:double)
  • -2.763200 (xsd:double)
  • -2.761700 (xsd:double)
  • -2.760400 (xsd:double)
  • -2.758100 (xsd:double)
  • -2.753000 (xsd:double)
  • -2.750500 (xsd:double)
  • -2.748000 (xsd:double)
  • -2.741100 (xsd:double)
  • -2.726000 (xsd:double)
dbp:name
dbp:notes
  • 3.15576E8
  • 7200.0
  • 1.735668E12
  • 3155760.0
  • 3.9447E11
  • Possibly two round barrows or one bowl barrow on an oval mound. (en)
  • The remains of a Z Battery, a short range anti-aircraft weapon system, which launched 3-inch diameter rockets from ground-based single and multiple launchers, for air defence. Most of the battery has been removed; however the control building survives. (en)
  • The remains of Down End Castle consist of earthworks from a Motte-and-bailey castle. (en)
  • Brent Knoll Camp is at the summit of a high hill which dominates the low surrounding landscape of the Somerset Levels. Brent Knoll has seen human settlement since at least the Bronze Age, becoming an Iron Age Fort about 2,000 B.C., which covers an area of . It is defended by a single wall around high and by a single ditch. The Romans used its summit as a fortification. The fort has been claimed as the site of Mons Badonicus. (en)
  • Artefacts from the cave demonstrate occupation during the Palaeolithic. (en)
  • The site was used in the Iron Age and again during the Romano-British and Medieval periods. It was at the edge of an inland lake which is now dry land. (en)
  • The first part of the market cross was built in the 15th and included a central octagonal pillar. In the 16th or 17th century it was enclosed with a hexagonal arch structure. The cross head was added in 1877. (en)
  • Earthworks from a small Roman villa and associated buildings arranged around a courtyard, which were built on a previously occupied site. (en)
  • The remains of bombing decoys and anti-aircraft obstructions in the form of earth and stone mounds. They are in the same area as prehistoric round barrows. (en)
  • Earthworks from a site occupied in the Middle Ages. Pottery from the 14th century has been found at the site. (en)
  • The site of Bronze and Iron Age trackways in the peaty soil of the Somerset Levels close to the base of the Polden Hills. (en)
  • The remains of a long cross dyke over the Quantock Hills. The bank is high and has a ditch on its western side. The name Dead Woman's Ditch was thought to relate to a woman murdered in 1789, although it is now known to have earlier usage. (en)
  • Earthworks remain of a burh which was important during the reign of Alfred the Great. It was surrounded by defensive banks and connected to Athelney Abbey by a causeway across marshland of the Somerset Levels. (en)
  • The remains of walls of a 13th-century chapel which as long and wide. (en)
  • A high stone slab. (en)
  • A bowl barrow approximately in diameter. (en)
  • A pair of probable round barrows (en)
  • A platform cairn on the Quantock Hills. (en)
  • An enclosure surrounded by a bank and ditch. (en)
  • A three pipe duck decoy with an infilled pool which is by . It was built before 1673 and fell out of use by 1788. (en)
  • A cairn mound which is approximately in diameter surrounded by a bank and ditch. (en)
  • A restored churchyard cross. The octagonal base is original; however the shaft was removed as unsafe and replaced in 1962. (en)
  • The site of Bronze and Iron Age trackways in the peaty soil of the Shapwick Heath area of the Somerset Levels. (en)
  • A four pipe duck decoy with two small islands in the pool. (en)
  • Two pieces of a timber trackway which were identified when water levels fell, as the site is waterlogged or under water normally. (en)
  • Earthworks from a bank and ditch which may have marked the boundary of the Compton Bishop estate according to a 1067 charter. In the 13th century it was associated with the boundary of the Royal Forest of Mendip. (en)
  • Earthworks from a complex of buildings, including a hall and chapel, surrounded by a moat. The site is believed to have been a bishops palace demolished by John Harewell, the Bishop of Bath and Wells, in the 1380s. (en)
  • Sections of several timber trackways including the Honeygore, Honeycat and Honeybee Tracks which were constructed between 3650 and 2870 B.C. (en)
  • The cross is high and stands on a three-step base. It was moved approximately from its original 15th-century position. (en)
  • A 15th-century churchyard cross on an octagonal base. The shaft is approximately high; however the head of the cross is missing. (en)
  • Cheddar Palace was established in the 9th century. It was a royal hunting lodge in the Anglo-Saxon and medieval periods and hosted the Witenagemot in the 10th century. Nearby are the ruins of the 14th-century St Columbanus Chapel. Roman artifacts and a burial have also been discovered. The site of the palace is now marked by concrete slabs within the grounds of The Kings of Wessex Academy. (en)
  • The remains of a kiln built in 1725 as part of a glassworks. The kiln was originally high. The remaining brickwork is between and high and up to thick. (en)
  • The retractable bridge was built in 1871 for the Bristol and Exeter Railway. It carried a railway siding over the river at the coal yard and docks in the Port of Bridgwater, but had to be movable, to allow boats to proceed upriver to the Town Bridge. The bridge was temporarily immobilised during World War II and last opened in 1953, and the traverser section was demolished in 1974. (en)
  • A 14th-century churchyard cross. The broken shaft is high. (en)
  • A Bronze Age and Iron Age hill fort. The small hill rises to above low lying land about west of the tidal estuary of the River Parrett, near the ancient port and ford at Combwich. The hill fort is roughly square in shape, with a single rampart enclosing , and the main entrance to the south-east. The north side of the hill has been destroyed by quarrying during the 19th and 20th centuries. Minor excavations were carried out in 1905, 1913 , and 1963 . Flint tools, scrapers and flakes have been found on or near the hill, indicating Mesolithic occupation. Bronze Age finds include an axe head and a knife. The area destroyed by quarrying was a late Roman and Saxon cemetery, with several hundred E-W graves, and various grave goods such as coins and pottery from the period 350-800 AD. (en)
  • The possible site of chapel which may also have been a homestead surrounded by a moat. (en)
  • A 14th-century churchyard cross. The shaft is high, with a round moulding and square cross head. (en)
  • A 14th-century churchyard cross. The shaft is high; however, the head is missing. (en)
  • Brean Down is a promontory off the coast, standing high and extending into the Bristol Channel at the eastern end of Bridgwater Bay between Weston-super-Mare and Burnham-on-Sea. Made of Carboniferous Limestone, it is a continuation of the Mendip Hills. Two further continuations are the small islands of Steep Holm and Flat Holm. The cliffs on the northern and southern flanks of Brean Down have large quantities of fossils laid down in the marine deposits about 320–350 million years ago. The site has been occupied by humans since the late Bronze Age and includes the remains of a Romano-Celtic Temple. At the seaward end is Brean Down Fort which was built in 1865 and then re-armed in the Second World War. Brean Down is now owned by the National Trust, and is rich in wildlife, history and archaeology. It is a Site of Special Scientific Interest due to both the geology and presence of nationally rare plants including the white rock-rose. It has also been scheduled as an ancient monument. (en)
  • Earthworks of uncertain date which may show the site of a settlement or field system. (en)
  • Rowberrow Camp was an Iron Age defended settlement covering and surrounded by a bank and ditch. (en)
  • A round barrow cemetery consisting of three barrows from which bones and a ceramic urn have been recovered. (en)
  • The cave includes a Palaeolithic hearth floor. Iron Age and Roman remains have also been uncovered. (en)
  • Balt Moor Wall is an earthwork situated on the Somerset Levels to the northwest of the River Tone. The site contains the remains of a section of medieval causeway, which now forms a raised embankment between and wide and up to high. The structure, which English Heritage refers to as "a rare example of medieval engineering", appears to have been built to protect the Salt Moor from the flooding of the River Tone in the Athelney-Lyng gap. (en)
  • The Somerset Brick and Tile Museum incorporates the last surviving 'pinnacle kiln' in Bridgwater, which dates from the 19th century. It is high and the circular base is in diameter. (en)
  • The remains of several brushwood trackways dating from the Neolithic period. (en)
  • A small cave occupied during the Iron Age. Excavation has found pottery and other artefacts from that period. (en)
  • Earthworks from a medieval settlement and surrounding fields. The platforms of several buildings survive at, or just below, ground level. (en)
  • Stowey Castle was a Norman motte-and-bailey castle, built in the 11th century, in the village of Nether Stowey on the Quantock Hills. (en)
  • A cave in Cheddar Gorge from which flint artefacts from the Late Upper Palaeolithic have been recovered. (en)
  • Earthworks including roadways and courtyards from a Roman settlement covering . Artefacts from the site have included coins and pottery. (en)
  • Earthworks from a medieval village which had a population of 40 to 45 people. (en)
  • A six pipe duck decoy on a low lying area in the valley of the River Axe. It was constructed before 1668 but redug in 1762 and fell out of use after 1813. (en)
  • Earthworks from several houses and associated fields. (en)
  • Athelney Abbey was founded by King Alfred in 888, after he stayed there before the Battle of Edington, as a religious house for monks of the Order of St. Benedict. Originally Athelney was a small island in swampland. Following the dissolution it was acquired for use as a private residence by Lord Audley who had the church demolished. With the church demolished and other buildings fallen into disrepair, nothing visible remains at the site today. The site of the Abbey is marked by King Alfred's Monument which is a Grade II listed building. (en)
  • A 13th-century churchyard cross. The shaft is high; however the head of the cross is missing. (en)
  • The remains of salt mounds used in Roman times. The largest is approximately in diameter. (en)
  • Gorsey Bigbury is an earth henge about in diameter. The nearby Longwood Barrow may be a long barrow or a misshapen round barrow. (en)
  • Plainsfield Camp is a possible Iron Age earthwork on the Quantock Hills, but may have been an animal enclosure. (en)
  • The bowl barrow next to Wilmot's pool is in diameter. The cairn, which is from the barrow, is approximately in diameter and high. (en)
  • A 15th-century churchyard cross. The shaft is high; however, the head of the cross is missing. (en)
  • A stone cross on a five step base which supports a high shaft with a lantern head. (en)
  • The remains of several prehistoric trackways in the peaty soil of the Somerset Levels. (en)
  • Gough's Cave is located in Cheddar Gorge on the Mendip Hills. The cave is deep and is long, and contains a variety of large chambers and rock formations. It contains the Cheddar Yeo, the largest underground river system in Britain. The cave contained skeletal remains of both humans and animals, all showing cut-marks and breakage consistent with de-fleshing and eating. In 1903 the remains of a human male, since named Cheddar Man, were found a short distance inside Gough's Cave. He is Britain’s oldest complete human skeleton, having been dated to approximately 7150 B.C. A Skull cup dating from 14,700 B.C. has been uncovered at the site. The first of the cave are open to the public as a show cave, and this stretch contains most of the more spectacular formations. The greater part of the cave's length is made up of the river passage, which is accessible only by cave diving. (en)
dbp:reference
  • (en)
dbp:showArchitect
  • no (en)
dbp:showImg
  • yes (en)
dbp:showListed
  • no (en)
dbp:showNotes
  • yes (en)
dbp:showRef
  • yes (en)
dbp:showWikidata
  • no (en)
dbp:type
dbp:uid
  • 1002958 (xsd:integer)
  • 1003028 (xsd:integer)
  • 1006133 (xsd:integer)
  • 1006134 (xsd:integer)
  • 1006135 (xsd:integer)
  • 1006136 (xsd:integer)
  • 1006137 (xsd:integer)
  • 1006148 (xsd:integer)
  • 1006166 (xsd:integer)
  • 1006221 (xsd:integer)
  • 1006222 (xsd:integer)
  • 1006223 (xsd:integer)
  • 1006225 (xsd:integer)
  • 1007669 (xsd:integer)
  • 1007670 (xsd:integer)
  • 1008211 (xsd:integer)
  • 1008248 (xsd:integer)
  • 1008254 (xsd:integer)
  • 1008806 (xsd:integer)
  • 1010715 (xsd:integer)
  • 1010753 (xsd:integer)
  • 1010800 (xsd:integer)
  • 1010906 (xsd:integer)
  • 1010921 (xsd:integer)
  • 1010922 (xsd:integer)
  • 1011125 (xsd:integer)
  • 1011533 (xsd:integer)
  • 1011584 (xsd:integer)
  • 1011914 (xsd:integer)
  • 1011915 (xsd:integer)
  • 1011916 (xsd:integer)
  • 1011925 (xsd:integer)
  • 1011926 (xsd:integer)
  • 1012064 (xsd:integer)
  • 1012311 (xsd:integer)
  • 1012592 (xsd:integer)
  • 1012593 (xsd:integer)
  • 1012594 (xsd:integer)
  • 1014430 (xsd:integer)
  • 1014431 (xsd:integer)
  • 1014433 (xsd:integer)
  • 1014437 (xsd:integer)
  • 1014438 (xsd:integer)
  • 1014439 (xsd:integer)
  • 1014444 (xsd:integer)
  • 1014445 (xsd:integer)
  • 1014452 (xsd:integer)
  • 1014712 (xsd:integer)
  • 1014858 (xsd:integer)
  • 1014872 (xsd:integer)
  • 1015450 (xsd:integer)
  • 1015451 (xsd:integer)
  • 1015452 (xsd:integer)
  • 1015453 (xsd:integer)
  • 1015454 (xsd:integer)
  • 1015455 (xsd:integer)
  • 1015456 (xsd:integer)
  • 1015457 (xsd:integer)
  • 1015458 (xsd:integer)
  • 1015495 (xsd:integer)
  • 1015499 (xsd:integer)
  • 1015815 (xsd:integer)
  • 1017290 (xsd:integer)
  • 1018952 (xsd:integer)
  • 1019033 (xsd:integer)
  • 1019099 (xsd:integer)
  • 1019100 (xsd:integer)
  • 1019291 (xsd:integer)
  • 1019421 (xsd:integer)
  • 1019801 (xsd:integer)
  • 1019899 (xsd:integer)
  • 1019900 (xsd:integer)
  • 1020016 (xsd:integer)
  • 1020438 (xsd:integer)
  • 1020624 (xsd:integer)
  • 1020994 (xsd:integer)
  • 1020995 (xsd:integer)
  • 1417361 (xsd:integer)
  • 1417363 (xsd:integer)
dbp:uploadDesc
  • Market Cross (en)
  • Roadside Cross At Ngr St 4248 4966 (en)
dbp:wikiPageUsesTemplate
dbp:wikidata
  • Q17003189 (en)
  • Q2736549 (en)
  • Q3403788 (en)
  • Q4274798 (en)
  • Q4813330 (en)
  • Q4961445 (en)
  • Q5032713 (en)
  • Q5302812 (en)
  • Q7200749 (en)
  • Q7376177 (en)
  • Q7559824 (en)
  • Q7620710 (en)
dcterms:subject
gold:hypernym
rdf:type
rdfs:comment
  • Sedgemoor is a low-lying area of land in Somerset, England. It lies close to sea level south of the Polden Hills, forming a large part of the Somerset Levels and Moors, a wetland area between the Mendips and the Blackdown Hills. The Neolithic people exploited the reed swamps for their natural resources and started to construct wooden trackways, including the world's oldest known timber trackway, the Post Track, dating to the 3800s BC. The Levels were the location of the Iron Age Glastonbury Lake Village as well as two lake villages at Meare Lake. Several settlements and hill forts were built on the natural "islands" of slightly raised land, including Brent Knoll and Glastonbury. In the Roman period sea salt was extracted and a string of settlements were set up along the Polden Hills. (en)
rdfs:label
  • List of scheduled monuments in Sedgemoor (en)
owl:sameAs
prov:wasDerivedFrom
foaf:depiction
foaf:isPrimaryTopicOf
is dbo:wikiPageRedirects of
is dbo:wikiPageWikiLink of
is foaf:primaryTopic of
Powered by OpenLink Virtuoso    This material is Open Knowledge     W3C Semantic Web Technology     This material is Open Knowledge    Valid XHTML + RDFa
This content was extracted from Wikipedia and is licensed under the Creative Commons Attribution-ShareAlike 3.0 Unported License