Hembury
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Hembury
Hembury is a Neolithic causewayed enclosure and Iron Age hill fort near Honiton in Devon. Its history stretches from the late fifth and early fourth millennia BC to the Roman invasion. The fort is situated on a south facing promontory at the end of a 240m high ridge in the Blackdown Hills. It lies to the north of and overlooking the River Otter valley and this location was probably chosen to give good views of the surrounding countryside as well as for defensive reasons. Stages of occupation Originally a neolithic site, an Iron Age hill fort was later built on the same site. It was excavated between 1930 and 1935 by Dorothy Liddell. She identified a timber framed entrance to the causewayed enclosure and an oval arrangement of postholes in the middle which she interpreted as being a building destroyed by fire before the enclosure earthworks were built. Other evidence of neolithic occupation included pottery, flints, axes, querns and charred grain. During an excavation in ...
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Hembury Digital Terrain Model
Hembury is a Neolithic causewayed enclosure and Iron Age hill fort near Honiton in Devon. Its history stretches from the late fifth and early fourth millennia BC to the Roman invasion. The fort is situated on a south facing promontory at the end of a 240m high ridge in the Blackdown Hills. It lies to the north of and overlooking the River Otter valley and this location was probably chosen to give good views of the surrounding countryside as well as for defensive reasons. Stages of occupation Originally a neolithic site, an Iron Age hill fort was later built on the same site. It was excavated between 1930 and 1935 by Dorothy Liddell. She identified a timber framed entrance to the causewayed enclosure and an oval arrangement of postholes in the middle which she interpreted as being a building destroyed by fire before the enclosure earthworks were built. Other evidence of neolithic occupation included pottery, flints, axes, querns and charred grain. During an excavation in t ...
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Hembury Castle, Buckfast
Hembury Castle is an Iron Age hillfort about a mile north-west of the village of Buckfast on the south-eastern edge of Dartmoor in Devon, England (). The fort is about 178 metres above sea level on a promontory between the River Dart on the east and the Holy Brook, south-west. The slope down to the River Dart is very steep and is covered by Hembury Woods which is now a Site of Special Scientific Interest. The fort is said to cover about seven acres and it is surrounded by a prominent rampart and ditch. It is one of several Iron Age forts on the eastern edge of Dartmoor, others include Holne Chase Castle, Wooston Castle, Cranbrook Castle and Prestonbury Castle. Inside the fort, on the western side, is an 11th- or 12th-century motte with a surrounding narrow inner bailey. The ramparts of the earlier hillfort may have been used as the outer bailey of the castle. The entire site has legal protection as a scheduled monument. The first documentary reference to Hembury Castle is in ...
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Dorothy Liddell
Dorothy Liddell, MBE (1890–1938), an pioneering woman archaeologist and mentor to both Mary Leakey and Mary Eily de Putron. Early life Born Dorothy Mary Liddell to Emily Catherine Berry and her husband John Liddell at Benwell, England in 1890. She was one of six children born to the couple. Her father was a prosperous director of the North British and Mercantile Insurance Company and a Justice of the Peace first for Northumberland and later for Basingstoke. There were three boys and three girls in the family. The family moved several times and by 1898 were living in Prudhoe Hall. In 1904 the family moved to Sydmonton Cork near Newbury and then later in 1908 to Sherfield Manor, Basingstoke. The family were philanthropic and interested in their community where ever they lived. They were a very close knit family. Liddell was known as Dolly and Tabitha to her family. Tabitha was a character she had performed to entertain the convalescent soldiers who stayed in Sherfield Manor when ...
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Hembury Castle, Tythecott
Hembury Castle is an Iron Age Hill fort situated close to Tythecott, south of Buckland Brewer in Devon Devon ( , historically known as Devonshire , ) is a ceremonial and non-metropolitan county in South West England. The most populous settlement in Devon is the city of Plymouth, followed by Devon's county town, the city of Exeter. Devo .... The fort is situated on a promontory off the East of a large hill at some 137 Metres above Sea Level.R.R.Sellman; Aspects of Devon History, Devon Books 1985 - - Chapter 2; The Iron Age in Devon. Map Page 11 of Iron Age hill forts in Devon includes Hembury Castle. References Hill forts in Devon {{UK-archaeology-stub ...
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Blackdown Hills
The Blackdown Hills are a range of hills along the Somerset-Devon border in south-western England, which were designated an Area of Outstanding Natural Beauty (AONB) in 1991. The plateau is dominated by hard chert bands of Upper Greensand with some remnants of chalk, and is cut through by river valleys. The hills support an extensive range of wildlife leading to the designation of 16 Sites of Special Scientific Interest (SSSIs). There is evidence of human occupation since the Iron Age. Fortifications include the remains of ancient hill forts, Norman architecture, Norman motte-and-bailey castles and Second World War airfields. There are also religious buildings such as Dunkeswell Abbey and village churches. The hills are crossed by a network of minor roads with major transport routes including the M5 motorway running around the periphery. Natural region The Blackdowns form a natural region that has been designated as a national character area - No. 147 - by Natural Eng ...
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Malcolm Todd
Malcolm Todd (27 November 19396 June 2013) was an English archaeologist. Born in Durham, England, the son of a miner, Todd was educated in classics and classical archaeology at St David's College, Lampeter and Brasenose College, Oxford. He subsequently served as a reader and professor at the University of Nottingham and the University of Exeter respectively. During this time, Todd conducted notable excavations at sites of Roman Britain. He was later principal at Trevelyan College, Durham. Todd retired from Durham in 2000, and subsequently dedicated himself to research and writing. He was the author and editor of several works on the archaeology of Roman Britain and the Germanic peoples in the Migration Period. Early life Malcolm Todd was born in Durham, England, on 27 November 1939, the son of Wilfrid Todd and Rose Evelyn Johnson. Durham was at the time a characteristic mining and farming community, and his father was a miner. Education Todd went to grammar school in Hartlep ...
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Lug (knob)
A lug is a typically flattened protuberance, a handle or extrusion located on the side of a ceramics, jug, glass, vase, or other container. They are sometimes found on prehistoric ceramics and stone containers, such as on pots from ancient Egypt, Hembury ware, claw beakers, and boar spears. A lug may also only be shaped as a lip for suspension–(no hole). In Ancient Egypt, lugs contained a hole for suspension, with 2– or 3–lugged vessels most common. In Roman times, ''lugs'' were on some types of column-sections to aid in construction. After slung by rope into position with a crane, the lugs were then masoned off. In Japan, Iga ware vases with lugs on each side are called "ears" and are an important feature. File:Gebel el-Arak knife mp3h8791.jpg, Single suspension lug (knob), vertical hole, of the Gebel el-Arak Knife File:Egypte louvre 294.jpg, Ancient Egyptian lugged and drilled pot of marble stone (3rd millennium BCE) See also *Package handle Refere ...
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Causewayed Enclosure
A causewayed enclosure is a type of large prehistoric earthwork common to the early Neolithic in Europe. It is an enclosure marked out by ditches and banks, with a number of causeways crossing the ditches. More than 100 examples are recorded in France and 70 in England, while further sites are known in Scandinavia, Belgium, Germany, Italy, Ireland and Slovakia. The term "causewayed enclosure" is now preferred to the older term, causewayed camp, as it has been demonstrated that the sites did not necessarily serve as occupation sites. Construction Causewayed enclosures are often located on hilltop sites, encircled by one to four concentric ditches with an internal bank. Enclosures located in lowland areas are generally larger than hilltop ones. Crossing the ditches at intervals are causeways which give the monuments their names. It appears that the ditches were excavated in sections, leaving the wide causeways intact in between. They should not be confused with segmented, or ...
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Neolithic
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 th ...
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Gabbro
Gabbro () is a phaneritic (coarse-grained), mafic intrusive igneous rock formed from the slow cooling of magnesium-rich and iron-rich magma into a holocrystalline mass deep beneath the Earth's surface. Slow-cooling, coarse-grained gabbro is chemically equivalent to rapid-cooling, fine-grained basalt. Much of the Earth's oceanic crust is made of gabbro, formed at mid-ocean ridges. Gabbro is also found as plutons associated with continental volcanism. Due to its variant nature, the term ''gabbro'' may be applied loosely to a wide range of intrusive rocks, many of which are merely "gabbroic". By rough analogy, gabbro is to basalt as granite is to rhyolite. Etymology The term "gabbro" was used in the 1760s to name a set of rock types that were found in the ophiolites of the Apennine Mountains in Italy. It was named after Gabbro, a hamlet near Rosignano Marittimo in Tuscany. Then, in 1809, the German geologist Christian Leopold von Buch used the term more restrictively in his descri ...
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The Lizard
The Lizard ( kw, An Lysardh) is a peninsula in southern Cornwall, England, United Kingdom. The most southerly point of the British mainland is near Lizard Point at SW 701115; Lizard village, also known as The Lizard, is the most southerly on the British mainland, and is in the civil parish of Landewednack, the most southerly parish. The valleys of the River Helford and Loe Pool form the northern boundary, with the rest of the peninsula surrounded by sea. The area measures about . The Lizard is one of England's natural regions and has been designated as a National Character Area 157 by Natural England. The peninsula is known for its geology and for its rare plants and lies within the Cornwall Area of Outstanding Natural Beauty (AONB). The name "Lizard" is most probably a corruption of the Cornish name "Lys Ardh", meaning "high court". The Lizard's coast is particularly hazardous to shipping and the seaways round the peninsula were historically known as the "Graveyard ...
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British Isles
The British Isles are a group of islands in the North Atlantic Ocean off the north-western coast of continental Europe, consisting of the islands of Great Britain, Ireland, the Isle of Man, the Inner and Outer Hebrides, the Northern Isles, and over six thousand smaller islands."British Isles", ''Encyclopædia Britannica''. They have a total area of and a combined population of almost 72 million, and include two sovereign states, the Republic of Ireland (which covers roughly five-sixths of Ireland), and the United Kingdom of Great Britain and Northern Ireland. The Channel Islands, off the north coast of France, are normally taken to be part of the British Isles, even though they do not form part of the archipelago. The oldest rocks are 2.7 billion years old and are found in Ireland, Wales and the northwest of Scotland. During the Silurian period, the north-western regions collided with the south-east, which had been part of a separate continental landmass. The ...
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