Casterley Camp
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Casterley Camp
Casterley Camp is the site of an Iron Age univallate hillfort in Wiltshire, England, about southwest of the village of Upavon. The site comprises a large Iron Age/Romano-British enclosure, possibly non-defensive in function, and incomplete. It was partially excavated in the 19th century. Three apparently related enclosures are identified within the site of Casterley Camp. Stock control and religious functions have been attributed to the enclosures. There is also an Iron Age/Romano-British trackway on the west side of the site, with traces of earth banks on both sides. The site is a scheduled monument. There are public footpaths and bridleways to the north and west of the site. Since 1898, land immediately west and south has been part of the Salisbury Plain firing ranges. The site of a smaller Iron Age hill fort, Chisenbury Camp, lies on the other side of the River Avon valley, about to the east. References See also *List of hill forts in England See also *List of hi ...
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Wiltshire
Wiltshire (; abbreviated Wilts) is a historic and ceremonial county in South West England with an area of . It is landlocked and borders the counties of Dorset to the southwest, Somerset to the west, Hampshire to the southeast, Gloucestershire to the north, Oxfordshire to the northeast and Berkshire to the east. The county town was originally Wilton, after which the county is named, but Wiltshire Council is now based in the county town of Trowbridge. Within the county's boundary are two unitary authority areas, Wiltshire and Swindon, governed respectively by Wiltshire Council and Swindon Borough Council. Wiltshire is characterised by its high downland and wide valleys. Salisbury Plain is noted for being the location of the Stonehenge and Avebury stone circles (which together are a UNESCO Cultural and World Heritage site) and other ancient landmarks, and as a training area for the British Army. The city of Salisbury is notable for its medieval cathedral. Swindon is the ...
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Iron Age
The Iron Age is the final epoch of the three-age division of the prehistory and protohistory of humanity. It was preceded by the Stone Age (Paleolithic, Mesolithic, Neolithic) and the Bronze Age (Chalcolithic). The concept has been mostly applied to Iron Age Europe and the Ancient Near East, but also, by analogy, to other parts of the Old World. The duration of the Iron Age varies depending on the region under consideration. It is defined by archaeological convention. The "Iron Age" begins locally when the production of iron or steel has advanced to the point where iron tools and weapons replace their bronze equivalents in common use. In the Ancient Near East, this transition took place in the wake of the Bronze Age collapse, in the 12th century BC. The technology soon spread throughout the Mediterranean Basin region and to South Asia (Iron Age in India) between the 12th and 11th century BC. Its further spread to Central Asia, Eastern Europe, and Central Europe is somewhat dela ...
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Univallate Hillfort
A hillfort is a type of earthwork used as a fortified refuge or defended settlement, located to exploit a rise in elevation for defensive advantage. They are typically European and of the Bronze Age or Iron Age. Some were used in the post-Roman period. The fortification usually follows the contours of a hill and consists of one or more lines of earthworks, with stockades or defensive walls, and external ditches. Hillforts developed in the Late Bronze and Early Iron Age, roughly the start of the first millennium BC, and were used in many Celtic areas of central and western Europe until the Roman conquest. Nomenclature The spellings "hill fort", "hill-fort" and "hillfort" are all used in the archaeological literature. The ''Monument Type Thesaurus'' published by the Forum on Information Standards in Heritage lists ''hillfort'' as the preferred term. They all refer to an elevated site with one or more ramparts made of earth, stone and/or wood, with an external ditch. Many ...
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Upavon
Upavon is a rural village and civil parish in the county of Wiltshire, England. As its name suggests, it is on the upper portion of the River Avon which runs from north to south through the village. It is on the north edge of Salisbury Plain about south of Pewsey, southeast of the market town of Devizes, and north of the cathedral city of Salisbury. The A345 and A342 roads run through the village. History Occupation of the area dates back to the Iron Age and Romano-British settlement at Casterley Camp, approximately southwest of the current village, and to the southeast was the small Iron Age settlement of Chisenbury Camp. The first mention of Upavon is in the 1086 Domesday Book as ''Oppavrene''; although no population was recorded, it can be estimated that the village supported some 200 to 250 people. The village prospered during the 12th and 13th centuries and started to develop features that are recognisable today. A large Norman church replaced the previous Saxon o ...
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Romano-British
The Romano-British culture arose in Britain under the Roman Empire following the Roman conquest in AD 43 and the creation of the province of Britannia. It arose as a fusion of the imported Roman culture with that of the indigenous Britons, a people of Celtic language and custom. Scholars such as Christopher Snyder believe that during the 5th and 6th centuries – approximately from 410 when the Roman legions withdrew, to 597 when St Augustine of Canterbury arrived – southern Britain preserved an active sub-Roman culture that survived the attacks from the Anglo-Saxons and even used a vernacular Latin when writing. Arrival of the Romans Roman troops, mainly from nearby provinces, invaded in AD 43, in what is now part of England, during the reign of Emperor Claudius. Over the next few years the province of Britannia was formed, eventually including the whole of what later became England and Wales and parts of Scotland.Kinder, H. & Hilgemann W. ''The Penguin Atlas of World ...
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Salisbury Plain Training Area
Salisbury Plain is a chalk plateau in the south western part of central southern England covering . It is part of a system of chalk downlands throughout eastern and southern England formed by the rocks of the Chalk Group and largely lies within the county of Wiltshire, but stretches into Hampshire. The plain is famous for its rich archaeology, including Stonehenge, one of England's best known landmarks. Large areas are given over to military training and thus the sparsely populated plain is the biggest remaining area of calcareous grassland in northwest Europe. Additionally the plain has arable land, and a few small areas of beech trees and coniferous woodland. Its highest point is Easton Hill. Physical geography The boundaries of Salisbury Plain have never been truly defined, and there is some difference of opinion as to its exact area. The river valleys surrounding it, and other downs and plains beyond them loosely define its boundaries. To the north the scarp of the d ...
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Chisenbury Camp
Chisenbury Camp is the site of an Iron Age univallate hillfort in Wiltshire, England. The site comprises a small circular 5-acre enclosure that was levelled in 1931. The site was partially excavated in the 19th century and there were finds of ceramics, worked stone, worked animal bone and remains of human burial; some are held by the Wiltshire Museum at Devizes. The site currently lies within the bounds of a small grass strip airfield, the former RAF Upavon, and is run through by the perimeter access road on the southern side of the field. Location The site is at , in Enford parish, about to the southeast of the village of Upavon. The larger Iron Age hill fort of Casterley Camp lies on the other side of the River Avon valley, about 2 1⁄2 miles (4 km) to the west. There are also a number of other Iron Age earthworks in the area. See also *List of hill forts in England See also *List of hill forts in Scotland *List of hill forts in Wales *Iron Age, British Iron Ag ...
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River Avon, Hampshire
The River Avon () is in the south of England, rising in Wiltshire, flowing through that county's city of Salisbury and then west Hampshire, before reaching the English Channel through Christchurch Harbour in the Bournemouth, Christchurch and Poole conurbation of Dorset. It is sometimes known as the Salisbury Avon or the Hampshire Avon to distinguish it from namesakes across Great Britain. It is one of the rivers in Britain in which the phenomenon of anchor ice has been observed. The Avon is thought to contain more species of fish than any other river in Britain. Long-farmed pastures and planted, arable fields line much of the valley; an indication of the wealth these brought to landowners is in ten large listed houses with statutorily recognised and protected parks. Many prehistoric sites and broader "landscapes" are found on either side of the river, the largest being the World Heritage Site zone of Stonehenge, Avebury and Associated Sites, followed by the Old Sarum knoll for ...
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List Of Hill Forts In England
See also *List of hill forts in Scotland *List of hill forts in Wales *Iron Age, British Iron Age, prehistory References ;Bibliography * Further reading * * * External links * A crowd-sourced project to map the hillforts of Britain and Ireland. {{DEFAULTSORT:List Of Hill Forts In England List of hill forts Iron Age sites in England Hill forts England Hill forts A hillfort is a type of earthwork used as a fortified refuge or defended settlement, located to exploit a rise in elevation for defensive advantage. They are typically European and of the Bronze Age or Iron Age. Some were used in the post-Roma ...
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Iron Age Sites In England
Iron () is a chemical element with symbol Fe (from la, ferrum) and atomic number 26. It is a metal that belongs to the first transition series and group 8 of the periodic table. It is, by mass, the most common element on Earth, right in front of oxygen (32.1% and 30.1%, respectively), forming much of Earth's outer and inner core. It is the fourth most common element in the Earth's crust. In its metallic state, iron is rare in the Earth's crust, limited mainly to deposition by meteorites. Iron ores, by contrast, are among the most abundant in the Earth's crust, although extracting usable metal from them requires kilns or furnaces capable of reaching or higher, about higher than that required to smelt copper. Humans started to master that process in Eurasia during the 2nd millennium BCE and the use of iron tools and weapons began to displace copper alloys, in some regions, only around 1200 BCE. That event is considered the transition from the Bronze Age to the Iron Age. In t ...
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