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Prehistoric Britain
Prehistoric Britain
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Several species of humans have intermittently occupied Great Britain for almost a million years. The earliest evidence of human occupation around 900,000 years ago is at Happisburgh on the Norfolk coast, with stone tools and footprints probably made by Homo antecessor.[1] The oldest human fossils, around 500,000 years old, are of Homo heidelbergensis at Boxgrove in Sussex.[2] Until this time Britain had been permanently connected to the Continent by a chalk ridge between South East England and northern France called the Weald–Artois Anticline, but during the Anglian Glaciation around 425,000 years ago a megaflood broke through the ridge, and Britain became an island when sea levels rose during the following Hoxnian interglacial.

Fossils of very early Neanderthals dating to around 400,000 years ago have been found at Swanscombe in Kent, and of classic Neanderthals about 225,000 years old at Pontnewydd in Wales. Britain was unoccupied by humans between 180,000 and 60,000 years ago, when Neanderthals returned. By 40,000 years ago they had become extinct and modern humans had reached Britain. But even their occupations were brief and intermittent due to a climate which swung between low temperatures with a tundra habitat and severe ice ages which made Britain uninhabitable for long periods. The last of these, the Younger Dryas, ended around 11,700 years ago, and since then Britain has been continuously occupied.

Traditionally it was claimed by academics that a post-glacial land bridge existed between Britain and Ireland; however, this conjecture began to be refuted by a consensus within the academic community starting in 1983, and since 2006 the idea of a land bridge has been disproven based upon conclusive marine geological evidence. It is now concluded that an ice bridge existed between Britain and Ireland up until 16,000 years ago, but this had melted by around 14,000 years ago.[3][4] Britain was at this time still joined to the Continent by a land bridge known as Doggerland, but due to rising sea levels this causeway of dry land would have become a series of estuaries, inlets and islands by 7000 BC,[5] and by 6200 BC, it would have become completely submerged.[6][7]

Located at the fringes of Europe, Britain received European technological and cultural developments much later than Southern Europe and the Mediterranean region did during prehistory. By around 4000 BC, the island was populated by people with a Neolithic culture. This neolithic population had significant ancestry from the earliest farming communities in Anatolia, indicating that a major migration accompanied farming. The beginning of the Bronze Age and the Bell Beaker culture was marked by an even greater population turnover, this time displacing more than 90% of Britain's neolithic ancestry in the process. This is documented by recent ancient DNA studies which demonstrate that the immigrants had large amounts of Bronze-Age Eurasian Steppe ancestry, associated with the spread of Indo-European languages and the Yamnaya culture.[8]

No written language of the pre-Roman inhabitants of Britain is known; therefore, the history, culture and way of life of pre-Roman Britain are known mainly through archaeological finds. Archaeological evidence demonstrates that ancient Britons were involved in extensive maritime trade and cultural links with the rest of Europe from the Neolithic onwards, especially by exporting tin that was in abundant supply. Although the main evidence for the period is archaeological, available genetic evidence is increasing, and views of British prehistory are evolving accordingly. Julius Caesar's first invasion of Britain in 55 BC is regarded as the start of recorded protohistory although some historical information is available from before then.[9]

Stone Age

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Palaeolithic

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Palaeolithic (Old Stone Age) Britain is the period of the earliest known occupation of Britain by humans. This huge period saw many changes in the environment, encompassing several glacial and interglacial episodes greatly affecting human settlement in the region. Providing dating for this distant period is difficult and contentious. The inhabitants of the region at this time were bands of hunter-gatherers who roamed Northern Europe following herds of animals, or who supported themselves by fishing.

Boxgrove handaxes, c. 500,000 BP, at the British Museum

First trace of human settlement at Happisburgh

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There is evidence from animal bones and flint tools found in coastal deposits near Happisburgh in Norfolk that early humans were present in Britain over 800,000 years ago.[10] The archaeological site at Happisburgh lies underneath glacial sediments from the Anglian glaciation of 450,000 years ago.[11] Paleo magnetic analysis shows that the sediments in which the stone tools were found have a reversed polarity- which means they are at least 780,000 years old.[11] Plant remains as well as the presence of extinct species of vole, mammoth, red deer, horse and elk indicate a date between 780,000 and 990,000 years old.[11] The evidence is that the early humans were there towards the end of an interglacial during that date range. There are two candidate interglacials - one between 970,000 and 935,000 years ago and the second from 865,000 and 815,000 years ago.[11] Numerous footprints dating to more than 800,000 years ago were found on the beach at Happisburgh in 2013 of a mixed group of adult males, females and children.[11] However there are no human fossils found. Homo antecessor is the most likely candidate species of ancient human as there are remains of roughly the same age at Gran Dolina at Atapuerca.[11] Homo antecessor lived before the ancestors of Neanderthals split from the ancestors of Homo sapiens 600,000 years ago.

Summer temperatures at Happisburgh were an average of 16 to 17 °C (61 to 63 °F) and average winter temperatures were slightly colder than present day temperatures, around freezing point or just below. Conditions were comparable to present-day southern Scandinavia.[11] It is not established how early humans at Happisburgh would have been able to deal with the cold winters. It is possible that they migrated southwards during the winter but the distances are large. No evidence has been found for the use of fire during that period.[11]

At this time, Britain was a peninsula of Europe, connected by a chalk ridge running across to northern France and the English Channel did not yet exist.[11] There were two main rivers in eastern Britain: the Bytham River, flowing east from the English Midlands and then across the north of East Anglia, and the River Thames, which then flowed further north than today. Early humans may have followed the Rhine and thence around the huge north-facing bay into which the Thames and Bytham also flowed.[11] Humans in Happisburgh were in a great valley downstream from the joining of the two great rivers.

Reconstructing this ancient environment has provided clues to the route first visitors took to arrive at what was then a peninsula of the Eurasian continent. Archaeologists have found a string of early sites located close to the route of a now lost watercourse named the Bytham River which indicate that it was exploited as the earliest route west into Britain.

Settlement at Pakefield

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Chronologically, the next evidence of human occupation is at Pakefield on the outskirts of Lowestoft in Suffolk 48 kilometres (30 mi) south of Happisburgh. They were in the lower Bytham river, and not the Thames which had now moved further south. Pakefield had mild winters and warm summers with average July temperatures of between 18 and 23 °C (64 and 73 °F). There were wet winters and drier summers. Animal bones found in the area include those of rhinos, hippos, extinct elephants, giant deer, hyaenas, lions, and sabre-toothed cats.[11]

Approximate route of the pre-Anglian Bytham River, on a modern topographical map

Sites such as Boxgrove in Sussex illustrate the later arrival in the archaeological record of an archaic Homo species called Homo heidelbergensis around 500,000 years ago. These early peoples made Acheulean flint tools (hand axes) and hunted the large native mammals of the period. One hypothesis is that they drove elephants, rhinoceroses and hippopotamuses over the tops of cliffs or into bogs to more easily kill them.

The extreme cold of the following Anglian Stage was previously thought to have driven humans out of Britain altogether, with the region not being occupied again until the ice receded during the succeeding Hoxnian Stage.[12] The discovery of sharp, unworn stone tools sandwiched between two Anglian sediment layers at Chequer's Wood and Old Park in Kent, however, suggests at least some human populations visited Britain during this ice age, although probably not when glaciers reached their southern limit 65 kilometres (40 mi) north of Old Park.[13] The warmer Hoxnian Stage period lasted from around 424,000 until 374,000 years ago and saw the Clactonian flint tool industry develop at sites such as Swanscombe in Kent. The period has produced a rich and widespread distribution of sites by Palaeolithic standards, although uncertainty over the relationship between the Clactonian and Acheulean industries is still unresolved.

Britain was populated only intermittently, and even during periods of occupation may have reproduced below replacement level and needed immigration from elsewhere to maintain numbers. According to Paul Pettitt and Mark White:

The British Lower Palaeolithic (and equally that of much of northern Europe) is thus a long record of abandonment and colonisation, and a very short record of residency. The sad but inevitable conclusion of this must be that Britain has little role to play in any understanding of long-term human evolution and its cultural history is largely a broken record dependent on external introductions and insular developments that ultimately lead nowhere. Britain, therefore, was an island of the living dead.[14]

This period also saw Levallois flint tools introduced, possibly by humans arriving from Africa. However, finds from Swanscombe and Botany Pit in Purfleet support Levallois technology being a European rather than African introduction. The more advanced flint technology permitted more efficient hunting and therefore made Britain a more worthwhile place to remain until the following period of cooling known as the Wolstonian Stage, 352,000–130,000 years ago. Britain first became an island about 350,000 years ago.[15]

230,000 years BP the landscape was reachable and Early Neanderthal remains discovered at the Pontnewydd Cave in Wales have been dated to 230,000 BP,[16] and are the most north westerly Neanderthal remains found anywhere in the world.

The next glaciation closed in and by about 180,000 years ago Britain no longer had humans.[17] About 130,000 years ago there was an interglacial period even warmer than today, which lasted 15,000 years. There were lions, elephants hyenas and hippos as well as deer. There were no humans. Possibly humans were too sparse at that time. Until c. 60,000 years ago there is no evidence of human occupation in Britain, probably due to inhospitable cold in some periods, Britain being cut off as an island in others, and the neighbouring areas of north-west Europe being unoccupied by hominins at times when Britain was both accessible and hospitable.[18]

Robin Hood Cave Horse, from Creswell Crags, c. 10,500 BC

This period is often divided into three subperiods: the Early Upper Palaeolithic (before the main glacial period), the Middle-Upper Palaeolithic (the main glacial period) and the Late Upper Palaeolithic (after the main glacial period). There was limited Neanderthal occupation of Britain in marine isotope stage 3 between about 60,000 and 42,000 years BP. Britain had its own unique variety of late Neanderthal handaxe, the bout-coupé, so seasonal migration between Britain and the continent is unlikely, but the main occupation may have been in the now submerged area of Doggerland, with summer migrations to Britain in warmer periods.[19] La Cotte de St Brelade in Jersey is the only site in the British Isles to have produced late Neanderthal fossils.[20]

The earliest evidence for modern humans in North West Europe is a jawbone discovered in England at Kents Cavern in 1927, which was re-dated in 2011 to between 41,000 and 44,000 years old.[21][22] The most famous example from this period is the burial of the "Red Lady of Paviland" (actually now known to be a man) in modern-day coastal South Wales, which was dated in 2009 to be 33,000 years old. The distribution of finds shows that humans in this period preferred the uplands of Wales and northern and western England to the flatter areas of eastern England. Their stone tools are similar to those of the same age found in Belgium and far north-east France, and very different from those in north-west France. At a time when Britain was not an island, hunter gatherers may have followed migrating herds of reindeer from Belgium and north-east France across the giant Channel River.[23]

The climatic deterioration which culminated in the Last Glacial Maximum, between about 26,500 and 19,000–20,000 years ago,[24] drove humans out of Britain, and there is no evidence of occupation for around 18,000 years after c.33,000 years BP.[25] Sites such as Cathole Cave in Swansea County dated at 14,500 years BP,[26] Creswell Crags on the border between Derbyshire and Nottinghamshire at 12,800BP and Gough's Cave in Somerset 12,000 years BP, provide evidence suggesting that humans returned to Britain towards the end of this ice age during a warm period from 14,700 to 12,900 years ago (the Bølling-Allerød interstadial known as the Windermere Interstadial in Britain), although further extremes of cold right before the final thaw may have caused them to leave again and then return repeatedly. The environment during this ice age period would have been largely treeless tundra, eventually replaced by a gradually warmer climate, perhaps reaching 17 °C (63 °F) in summer, encouraging the expansion of birch trees as well as shrub and grasses.

Europe during the Last Glacial Maximum c. 20,000 years ago

The first distinct culture of the Upper Palaeolithic in Britain is what archaeologists call the Creswellian industry, with leaf-shaped points probably used as arrowheads. It produced more refined flint tools but also made use of bone, antler, shell, amber, animal teeth, and mammoth ivory. These were fashioned into tools but also jewellery and rods of uncertain purpose. Flint seems to have been brought into areas with limited local resources; the stone tools found in the caves of Devon, such as Kent's Cavern, seem to have been sourced from Salisbury Plain, 100 miles (160 km) east. This is interpreted as meaning that the early inhabitants of Britain were highly mobile, roaming over wide distances and carrying 'toolkits' of flint blades with them rather than heavy, unworked flint nodules, or else improvising tools extemporaneously. The possibility that groups also travelled to meet and exchange goods or sent out dedicated expeditions to source flint has also been suggested.

The dominant food species were equines (Equus ferus) and red deer (Cervus elaphus), although other mammals ranging from hares to mammoth were also hunted, including rhino and hyena. From the limited evidence available, burial seemed to involve skinning and dismembering a corpse with the bones placed in caves. This suggests a practice of excarnation and secondary burial, and possibly some form of ritual cannibalism. Artistic expression seems to have been mostly limited to engraved bone, although the cave art at Creswell Crags and Mendip caves are notable exceptions.

Between about 12,890 and 11,650 years ago Britain returned to glacial conditions during the Younger Dryas, and may have been unoccupied for periods.[27]

Mesolithic

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(c. 9,000 to 4,300 BC)

Star Carr Pendant, c. 9000 BC

The Younger Dryas was followed by the Holocene, which began around 9,700 BC,[28] and continues to the present. By 8000 BC temperatures were higher than today, and birch woodlands spread rapidly,[29] but there was a cold spell around 6,200 BC which lasted about 150 years.[30] The plains of Doggerland were thought to have finally been submerged around 6500 to 6000 BC,[31] but recent evidence suggests that the bridge may have lasted until between 5800 and 5400 BC, and possibly as late as 3800 BC.[32]

The warmer climate changed the arctic environment to one of pine, birch and alder forest; this less open landscape was less conducive to the large herds of reindeer and wild horse that had previously sustained humans. Those animals were replaced in people's diets by pig and less social animals such as elk, red deer, roe deer, wild boar and aurochs (wild cattle),[33] which would have required different hunting techniques.[34] Tools changed to incorporate barbs which could snag the flesh of an animal, making it harder for it to escape alive. Tiny microliths were developed for hafting onto harpoons and spears. Woodworking tools such as adzes appear in the archaeological record, although some flint blade types remained similar to their Palaeolithic predecessors. The dog was domesticated because of its benefits during hunting, and the wetland environments created by the warmer weather would have been a rich source of fish and game. Wheat of a variety grown in the Middle East was present on the Isle of Wight at the Bouldnor Cliff Mesolithic Village dating from about 6,000 BC.[35]

Howick house reconstruction, c. 7600 BC

It is likely that these environmental changes were accompanied by social changes. Humans spread and reached the far north of Scotland during this period.[36] Sites from the British Mesolithic include the Mendips, Star Carr in Yorkshire and Oronsay in the Inner Hebrides. Excavations at Howick in Northumberland uncovered evidence of a large circular building dating to c. 7600 BC which is interpreted as a dwelling. A further example has also been identified at Deepcar in Sheffield, and a building dating to c. 8500 BC was discovered at the Star Carr site. A group of 25 pits, aligned with a watercourse, laid out in straight lines, up to 500 metres long, has been found at Linmere, Bedfordshire.[33] The older view of Mesolithic Britons as nomadic is now being replaced with a more complex picture of seasonal occupation or, in some cases, permanent occupation. Travel distances seem to have become shorter, typically with movement between high and low ground.

In 1997, DNA analysis was carried out on a tooth of Cheddar Man, human remains dated to c. 7150 BC found in Gough's Cave at Cheddar Gorge. His mitochondrial DNA (mtDNA) belonged to Haplogroup U5. Within modern European populations, U5 is now concentrated in North-East Europe, among members of the Sami people, Finns, and Estonians. This distribution and the age of the haplogroup indicate that individuals belonging to U5 were among the first people to resettle Northern Europe, following the retreat of ice sheets from the Last Glacial Maximum, about 10,000 years ago. It has also been found in other Mesolithic remains in Germany, Lithuania, Poland, Portugal, Russia,[37] Sweden,[38] France[39] and Spain.[40] Members of U5 may have been one of the most common haplogroups in Europe, before the spread of agriculture from the Middle East.[41] Cheddar Man likely had dark-to-black skin and blue eyes.

Though the Mesolithic environment was bounteous, the rising population and the ancient Britons' success in exploiting it eventually led to local exhaustion of many natural resources. The remains of a Mesolithic elk found caught in a bog at Poulton-le-Fylde in Lancashire show that it had been wounded by hunters and escaped on three occasions, indicating hunting during the Mesolithic. A few Neolithic monuments overlie Mesolithic sites but little continuity can be demonstrated. Farming of crops and domestic animals was adopted in Britain around 4500 BC, at least partly because of the need for reliable food sources. The climate had been warming since the later Mesolithic and continued to improve, replacing the earlier pine forests with woodland.

Neolithic

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(c. 4,300 to 2,000 BC)

Stonehenge, c. 3000–2500 BC

The Neolithic was the period of domestication of plants and animals, but the arrival of a Neolithic package of farming and a sedentary lifestyle is increasingly giving way to a more complex view of the changes and continuities in practices that can be observed from the Mesolithic period onwards. For example, the development of Neolithic monumental architecture, apparently venerating the dead,[citation needed] may represent more comprehensive social and ideological changes involving new interpretations of time, ancestry, community and identity.

In any case, the Neolithic Revolution, as it is called, introduced a more settled way of life and ultimately led to societies becoming divided into differing groups of farmers, artisans and leaders. Forest clearances were undertaken to provide room for cereal cultivation and animal herds. Native cattle and pigs were reared whilst sheep and goats were later introduced from the continent, as were the wheats and barleys grown in Britain. However, only a few actual settlement sites are known in Britain, unlike the continent. Cave occupation was common at this time.

The construction of the earliest earthwork sites in Britain began during the early Neolithic (c. 4400–3300 BC) in the form of long barrows used for communal burial and the first causewayed enclosures, sites which have parallels on the continent. The former may be derived from the long house, although no long house villages have been found in Britain — only individual examples. The stone-built houses on Orkney — such as those at Skara Brae — are, however, indicators of some nucleated settlement in Britain. Evidence of growing mastery over the environment is embodied in the Sweet Track, a wooden trackway built to cross the marshes of the Somerset Levels and dated to 3807 BC. Leaf-shaped arrowheads, round-based pottery types and the beginnings of polished axe production are common indicators of the period. Evidence of the use of cow's milk comes from analysis of pottery contents found beside the Sweet Track. According to archaeological evidence from North Yorkshire, salt was being produced by evaporation of seawater around this time, enabling more effective preservation of meat.[42]

Pollen analysis shows that woodland was decreasing and grassland increasing, with a major decline of elms. The winters were typically 3 degrees colder than at present but the summers some 2.5 degrees warmer.[citation needed]

The Middle Neolithic (c. 3300–2900 BC) saw the development of cursus monuments close to earlier barrows and the growth and abandonment of causewayed enclosures, as well as the building of impressive chamber tombs such as the Maeshowe types. The earliest stone circles and individual burials also appear.

The Neolithic site of Silbury Hill in Wiltshire, southern England, c. 2400 BC. The Neolithic saw the construction of a wide variety of monuments in the landscape, many of which were megalithic in nature.

Different pottery types, such as grooved ware, appear during the later Neolithic (c. 2900–2200 BC). In addition, new enclosures called henges were built, along with stone rows and the famous sites of Stonehenge, Avebury and Silbury Hill, which building reached its peak at this time. Industrial flint mining begins, such as that at Cissbury and Grimes Graves, along with evidence of long-distance trade. Wooden tools and bowls were common, and bows were also constructed.

Changes in Neolithic culture could have been due to the mass migrations that occurred in that time. A 2017 study showed that British Neolithic farmers had formerly been genetically similar to contemporary populations in the Iberian peninsula, but from the Beaker culture period onwards, all British individuals had high proportions of Steppe ancestry and were genetically more similar to Beaker-associated people from the Lower Rhine area. The study argues that more than 90% of Britain's Neolithic gene pool was replaced with the coming of the Beaker people.[8]

Analysis of the mitochondrial DNA of modern European populations shows that over 80% are descended in the female line from European hunter-gatherers.[citation needed] Less than 20% are descended in the female line from Neolithic farmers from Anatolia and from subsequent migrations. The percentage in Britain is smaller at around 11%. Initial studies suggested that this situation is different with the paternal Y-chromosome DNA, varying from 10 to 100% across the country, being higher in the east. This was considered to show a large degree of population replacement during the Anglo-Saxon invasion and a nearly complete masking over of whatever population movement (or lack of it) went before in these two countries.[43] However, more widespread studies have suggested that there was less of a division between Western and Eastern parts of Britain with less Anglo-Saxon migration.[44] Looking from a more Europe-wide standpoint, researchers at Stanford University have found overlapping cultural and genetic evidence that supports the theory that migration was at least partially responsible for the Neolithic Revolution in Northern Europe (including Britain).[45] The science of genetic anthropology is changing very fast and a clear picture across the whole of human occupation of Britain has yet to emerge.[46]

Bronze Age

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(Around 2200 to 750 BC)

Gold cape from Mold, Wales, c. 1900 BC

This period can be sub-divided into an earlier phase (2300–1200 BC) and a later one (1200–700 BC). Beaker pottery appears in England around 2475–2315 cal. BC[47] along with flat axes and burial practices of inhumation. With the revised Stonehenge chronology, this is after the Sarsen Circle and trilithons were erected at Stonehenge. Several regions of origin have been postulated for the Beaker culture, notably the Iberian peninsula, the Netherlands and Central Europe.[48] Beaker techniques brought to Britain the skill of refining metal. At first the users made items from copper, but from around 2150 BCE smiths had discovered how to smelt bronze (which is much harder than copper) by mixing copper with a small amount of tin. With this discovery, the Bronze Age arrived in Britain. Over the next thousand years, bronze gradually replaced stone as the main material for tool and weapon making.

Britain had large, easily accessible reserves of tin in the modern areas of Cornwall and Devon and thus tin mining began. By around 1600 BC the southwest of Britain was experiencing a trade boom as British tin was exported across Europe, evidence of ports being found in Southern Devon at Bantham and Mount Batten. Copper was mined at the Great Orme in North Wales.

The Beaker people were also skilled at making ornaments from gold, silver and copper, and examples of these have been found in graves of the wealthy Wessex culture of central southern Britain.

Early Bronze Age Britons buried their dead beneath earth mounds known as barrows, often with a beaker alongside the body. Later in the period, cremation was adopted as a burial practice with cemeteries of urns containing cremated individuals appearing in the archaeological record, with deposition of metal objects such as daggers. People of this period were also largely responsible for building many famous prehistoric sites such as the later phases of Stonehenge along with Seahenge. The Bronze Age people lived in round houses and divided up the landscape. Stone rows are to be seen on, for example, Dartmoor. They ate cattle, sheep, pigs and deer as well as shellfish and birds. They carried out salt manufacture. The wetlands were a source of wildfowl and reeds. There was ritual deposition of offerings in the wetlands and in holes in the ground.

Bronze Age and Iron Age artefacts from East Anglia

There has been debate amongst archaeologists as to whether the "Beaker people" were a race of people who migrated to Britain en masse from the continent, or whether a Beaker cultural "package" of goods and behaviour (which eventually spread across most of Western Europe) diffused to Britain's existing inhabitants through trade across tribal boundaries. A 2017 study suggests a major genetic shift in late Neolithic/early Bronze Age Britain, so that more than 90% of Britain's Neolithic gene pool was replaced with the coming of a people genetically related to the Beaker people of the lower-Rhine area.[8]

There is evidence of a relatively large scale disruption of cultural patterns (see Late Bronze Age collapse) which some scholars think may indicate an invasion (or at least a migration) into Southern Great Britain c. the 12th century BC. This disruption was felt far beyond Britain, even beyond Europe, as most of the great Near Eastern empires collapsed (or experienced severe difficulties) and the Sea Peoples harried the entire Mediterranean basin around this time. Some scholars consider that the Celtic languages arrived in Britain at this time,[49][50][51] but other elements of the Celtic cultural package derive from the Hallstatt culture.[52]

In an archaeogenetics study, Patterson et al. (2021) uncovered a migration into southern Britain during the 500-year period 1,300–800 BC.[53] The newcomers were genetically most similar to ancient individuals from Gaul, and had higher levels of EEF ancestry.[53] During 1,000–875 BC, their genetic marker swiftly spread through southern Britain,[54] making up around half the ancestry of subsequent Iron Age people in this area, but not in northern Britain.[53] The "evidence suggests that, rather than a violent invasion or a single migratory event, the genetic structure of the population changed through sustained contacts between Britain and mainland Europe over several centuries, such as the movement of traders, intermarriage, and small scale movements of family groups".[54] The authors describe this as a "plausible vector for the spread of early Celtic languages into Britain".[53] There was much less migration into Britain during the Iron Age, so it is likely that Celtic reached Britain before then.[53] The study also found that lactose tolerance rose swiftly in early Iron Age Britain, a thousand years before it became widespread in mainland Europe; suggesting milk became a very important foodstuff in Britain at this time.[53]

Iron Age

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(around 750 BC – 43 AD)

Wandsworth Shield, in the Insular version of La Tène style, 2nd century BC

In around 750 BC iron working techniques reached Britain from southern Europe. Iron was stronger and more plentiful than bronze, and its introduction marks the beginning of the Iron Age. Iron working revolutionised many aspects of life, most importantly agriculture. Iron tipped ploughs could turn soil more quickly and deeply than older wooden or bronze ones, and iron axes could clear forest land more efficiently for agriculture. There was a landscape of arable, pasture and managed woodland. There were many enclosed settlements and land ownership was important.

It is generally thought that by 500 BC most people inhabiting the British Isles were speaking Common Brythonic, on the limited evidence of place-names recorded by Pytheas of Massalia and transmitted to us second-hand, largely through Strabo. Certainly by the Roman period there is substantial place and personal name evidence which suggests that this was so; Tacitus also states in his Agricola that the British language differed little from that of the Gauls.[55] Among these people were skilled craftsmen who had begun producing intricately patterned gold jewellery, in addition to tools and weapons of both bronze and iron. It is disputed whether Iron Age Britons were "Celts", with some academics such as John Collis[56] and Simon James[57] actively opposing the idea of 'Celtic Britain', since the term was only applied at this time to a tribe in Gaul. However, place names and tribal names from the later part of the period suggest that a Celtic language was spoken.

The traveller Pytheas, whose own works are lost, was quoted by later classical authors as calling the people "Pretanoi", which is cognate with "Britanni" and is apparently Celtic in origin. The term "Celtic" continues to be used by linguists to describe the family that includes many of the ancient languages of Western Europe and modern British languages such as Welsh without controversy.[58] The dispute essentially revolves around how the word "Celtic" is defined; it is clear from the archaeological and historical record that Iron Age Britain did have much in common with Iron Age Gaul, but there were also many differences. Many leading academics, such as Barry Cunliffe, still use the term to refer to the pre-Roman inhabitants of Britain for want of a better label.

Broch of Mousa, Scotland, c. 100 BC

Iron Age Britons lived in organised tribal groups, ruled by a chieftain. As people became more numerous, wars broke out between opposing tribes. This was traditionally interpreted as the reason for the building of hill forts, although the siting of some earthworks on the sides of hills undermined their defensive value, hence "hill forts" may represent increasing communal areas or even 'elite areas'. However some hillside constructions may simply have been cow enclosures. Although the first had been built about 1500 BC, hillfort building peaked during the later Iron Age. There are around 3,300 structures that can be classed as hillforts or similar "defended enclosures" within Britain.[59] By about 350 BC many hillforts went out of use and the remaining ones were reinforced. Pytheas was quoted as writing that the Britons were renowned wheat farmers. Large farmsteads produced food in industrial quantities and Roman sources note that Britain exported hunting dogs, animal skins and slaves.

Late pre-Roman Iron Age

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Gold Celtic coins from the Farmborough Hoard

The last centuries before the Roman invasion saw an influx of Celtic-speaking refugees from Gaul (approximately modern day France and Belgium) known as the Belgae, who were displaced as the Roman Empire expanded around 50 BC. They settled along most of the coastline of southern Britain between about 200 BC and AD 43, although it is hard to estimate what proportion of the population there they formed. A Gaulish tribe known as the Parisi, who had cultural links to the continent, appeared in northeast England.

From around 175 BC, the areas of Kent, Hertfordshire and Essex developed especially advanced pottery-making skills. The tribes of southeast England became partially Romanised and were responsible for creating the first settlements (oppida) large enough to be called towns.

The last centuries before the Roman invasion saw increasing sophistication in British life. About 100 BC, iron bars began to be used as currency, while internal trade and trade with continental Europe flourished, largely due to Britain's extensive mineral reserves. Coinage was developed, based on continental types but bearing the names of local chieftains. This was used in southeast England, but not in areas such as Dumnonia in the west.

As the Roman Empire expanded northwards, Rome began to take interest in Britain. This may have been caused by an influx of refugees from Roman occupied Europe, or Britain's large mineral reserves. See Roman Britain for the history of this subsequent period.

Protohistory

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The first significant written record of Britain and its inhabitants was made by the Greek navigator Pytheas, who explored the coastal region of Britain around 325 BC. However, there may be some additional information on Britain in the Ora Maritima, a text which is now lost but which is incorporated in the writing of the later author Avienius. Julius Caesar also wrote of Britain in about 50 BC after his two military expeditions to the island in 55 and 54 BC. The failed invasion during 54 BC is thought to be an attempt to conquer at least the southeast of Britain.[60]

After some further false starts, the Roman conquest of Britain in 43 AD led to most of the island falling under Roman rule, and began the period of Roman Britain.

See also

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Notes

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Sources

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Further reading

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Prehistoric Britain refers to the span of human occupation and cultural development on the island from the earliest evidence of hominins around 900,000 years ago until the Roman invasion in AD 43, encompassing periods of intermittent settlement during Ice Ages, the transition from lifestyles to , and advancements in technology and monumental construction. The region, separated from by rising sea levels around 6500 BC to form the modern British Isles, witnessed waves of migration and environmental adaptation, with key archaeological evidence including stone tools from sites like in dating to over 850,000 years ago, attributed to early species such as . The Palaeolithic (Old Stone Age, c. 900,000–10,000 BC) and (Middle Stone Age, c. 10,000–4000 BC) eras were dominated by nomadic hunter-gatherers who exploited flint for tools like handaxes and microliths, with populations fluctuating due to glacial cycles that rendered Britain uninhabitable at times. Sites such as Boxgrove in yield fossils of from around 500,000 years ago, while Homo sapiens arrived by at least 40,000 years ago, as evidenced by a jaw fragment from Kent's Cavern in . By the Mesolithic, post-Ice Age warming supported semi-permanent camps like in , where artifacts including barbed points and wooden platforms indicate sophisticated . The (New Stone Age, c. 4000–2400 BC) marked a transformative shift with the introduction of farming from continental Europe, leading to settled communities, polished stone axes, and the construction of iconic communal monuments such as (c. 3000–2000 BC) and in . Pottery like and causewayed enclosures, such as Windmill Hill (c. 3650 BC), reflect emerging social organization and ritual practices, while genetic studies show a population replacement from earlier Neolithic farmers by incoming groups with ancestry around 2500 BC. During the Bronze Age (c. 2400–800 BC), the arrival of metalworking—first copper and then bronze alloys—facilitated tools, weapons, and ornaments, with bell barrows and roundhouses signifying increased social hierarchies and trade networks across . Significant migrations from the continent, particularly between 1300–800 BC, introduced up to 50% new ancestry in southern Britain, linked to cultural changes like the Urnfield tradition and potentially early . The (c. 800 BC–AD 43) saw the widespread adoption of iron for more efficient tools and weapons, the proliferation of hillforts like Maiden Castle in Dorset for defense and settlement, and intensified agriculture with field systems and oppida. Regional tribal societies minted coins from around 150 BC and engaged in trade with Mediterranean cultures, culminating in contacts with Julius Caesar's expeditions in 55–54 BC, setting the stage for full Roman conquest.

Geological and Environmental Context

Formation of the British Landscape

The geological foundation of Britain's landscape began with the , a prolonged mountain-building event spanning from the late to the mid-Devonian periods, approximately 490 to 390 million years ago. This orogeny resulted from the subduction and closure of the , leading to the collision of continental plates including , , and . Intense compression, regional , and igneous intrusions transformed sediments into high-grade rocks such as gneisses, schists, and slates, while forming northeast-trending mountain chains across what is now , , and . Subsequent erosion over hundreds of millions of years exposed granitic intrusions and shaped the rugged terrain of the , with major faults like the and delineating its structure. The Variscan Orogeny, occurring primarily in the late Carboniferous period around 320 to 300 million years ago, further influenced southern Britain's geology through the collision of Laurussia and Gondwana. This event inverted earlier sedimentary basins in southwest England and Wales, producing intense east-west folding, thrusting, and low-grade metamorphism south of the Variscan Front. In areas like south Pembrokeshire and the South Wales Coalfield, it caused up to 50% crustal shortening and complex fault systems, such as the Neath Disturbance, while preserving Devonian to Namurian strata in regions like Gower. These processes laid the groundwork for later features in southern England, though the orogeny's direct topographic imprint was modified by subsequent erosion. Cenozoic tectonic activity, driven by the distant Alpine Orogeny, induced widespread uplift and erosion that refined Britain's modern topography from the Miocene onward, approximately 23 to 2.6 million years ago. In the Pennines, this uplift elevated Carboniferous limestone and millstone grit sequences into a north-south anticlinal dome, with erosion carving deep valleys and exposing older basement rocks along the flanks; up to several thousand meters of overlying material were removed in places like Lancashire. Similarly, the Weald region experienced Palaeogene compression and doming, forming an east-west anticline where Cretaceous chalk caps the structure, flanked by eroded Lower Cretaceous and Jurassic strata in the central basin; this uplift, combined with prolonged denudation, created the characteristic inverted basin morphology. The Scottish Highlands underwent additional Miocene-Pliocene rejuvenation, enhancing their elevation through isostatic rebound and fluvial incision, building on the ancient Caledonian framework. Tectonic stability was disrupted in the Pleistocene by eustatic sea-level changes tied to glacial cycles, culminating in Britain's separation from mainland around 450,000 years ago. Rising sea levels, exacerbated by overflows from a proglacial lake in the Southern basin, catastrophically breached the Weald-Artois chalk ridge connecting to , initiating the through waterfall erosion and megaflooding. This event severed the direct land connection, though a northern persisted. , a vast low-lying plain of marshes, rivers, and hills spanning the southern , linked eastern to the and until its gradual inundation by post-glacial sea-level rise. The final submersion occurred around 8,200 years ago, accelerated by the Storegga submarine , fully isolating Britain as an .

Climatic Fluctuations and Ice Ages

The Pleistocene epoch, spanning from approximately 2.58 million to 11,700 years ago, was characterized by repeated climatic fluctuations in Britain, driven by and resulting in alternating glacial and interglacial periods that profoundly shaped the region's environment. These cycles included major ice ages that expanded the British-Irish Ice Sheet (BIIS) across much of the landmass, followed by warmer s that allowed partial recovery of vegetation and fauna. The sequence of these events is well-documented through sediment cores, pollen records, and glacial landforms, revealing a pattern of extreme cold interspersed with milder phases. One of the most significant glaciations was the Anglian Glaciation, occurring around 450,000 years ago during Marine Isotope Stage (MIS) 12, which represented the maximum extent of the BIIS and covered nearly all of Britain with ice up to 3 km thick in places. This event sculpted the landscape by eroding major valleys, such as those in the and , and depositing extensive sheets; in , it deepened fjords like Loch Broom through repeated ice advances. The glaciation lowered sea levels substantially, exposing land bridges to that facilitated later faunal migrations, though these connections were intermittent across the Pleistocene. Following the Anglian, the Hoxnian Interglacial (~400,000 years ago, MIS 11) brought a prolonged warm period with temperatures up to 2–3°C higher than present, fostering widespread forestation dominated by , , and across southern and eastern Britain. assemblages from sites like Hoxne indicate dense woodlands interspersed with open grasslands, supporting diverse including straight-tusked elephants (Palaeoloxodon antiquus) and hippopotamuses (), which thrived in the temperate wetlands and rivers. This lasted about 30,000 years, allowing soil development and recovery before the onset of subsequent cold stages. The later Pleistocene saw additional glaciations, culminating in the Devensian Glaciation (~115,000–11,700 years ago, MIS 5d to 2), the most recent major ice advance that again blanketed much of Britain under the BIIS, reaching its peak during the around 26,500–19,000 years ago. Temperatures during this period dropped dramatically, with mean annual values in southern Britain falling to -5°C or lower, as evidenced by periglacial features like cryoturbations and fossil pollen indicating tundra-steppe vegetation. Global sea levels fell by up to 120 meters during glacial maxima due to water locked in ice sheets, exposing vast coastal plains and altering Britain's connectivity to . The Devensian ended with the Bølling–Allerød warming (~14,700–12,900 years ago), but this was interrupted by the stadial (also known as the Stadial in Britain, ~12,900–11,700 years ago), a abrupt cold snap that reversed warming trends and re-expanded ice caps in and . During this millennium-long event, temperatures plummeted by 5–10°C, reverting Britain to near-glacial conditions with strong westerly winds and sparse tundra vegetation, as recorded in lake sediments and beetle faunas. The stadial concluded around 11,700 years ago, marking the transition to the epoch with a rapid shift to a temperate maritime , rising temperatures, and the establishment of forests.

Palaeolithic Period

Early Human Arrivals and Sites

The earliest evidence of human presence in Britain dates to the , with fossilized footprints discovered at on the Norfolk coast, dated to approximately 900,000 years ago. These prints, preserved in estuarine sediments, represent the oldest known hominin activity outside and indicate a small group of individuals, including adults and children, traversing a muddy riverine environment during a mild phase. Shortly after, around 700,000 years ago, stone tools unearthed at Pakefield in provide further confirmation of hominin occupation in eastern . Comprising flint flakes and cores from a coastal site, these artifacts suggest opportunistic tool-making by early humans exploiting intertidal resources during the Cromerian Complex . This discovery pushed back the timeline of human arrivals in by over 200,000 years compared to prior estimates. A significant recent find, reported in 2025, reveals hominin occupation at Fordwich Pit in spanning 712,000 to 424,000 years ago, encompassing parts of (MIS) 17 to 12. Excavations at Old Park within the site yielded in-situ hand axes and , alongside faunal remains, indicating repeated visits by hominins during both glacial and conditions along the ancient Stour. Over 330 hand axes originally recovered from the pit in the 1920s further underscore its importance as one of Britain's earliest localities. By the Middle Pleistocene, around 500,000 years ago, more substantial evidence emerges at Boxgrove in , where a and two teeth attributed to were found alongside butchered horse remains. The site's Unit 4b horizon preserves cut marks on bones from at least 20 horses, demonstrating skilled hunting and carcass processing by robust hominins in a lakeside setting during the Hoxnian Interglacial (MIS 11). This occupation reflects advanced predatory behavior in a temperate environment. Human presence in Britain during the Lower and Middle Palaeolithic was intermittent, tied to warmer when climatic conditions allowed migration from . Severe glaciations, such as the Anglian (MIS 12, ~478,000–424,000 years ago), led to complete depopulation as ice sheets advanced and sea levels rose, isolating the region. Repopulation occurred during subsequent , including limited evidence in the Ipswichian Interglacial (~125,000 years ago, MIS 5e), where sparse archaeological traces suggest transient visits amid a warmer, forested landscape, though overall occupation remained minimal compared to earlier phases.

Adaptations and Tool Technologies

Early human adaptations in Britain during the Lower Palaeolithic involved the development of stone tool technologies that evolved from simple flake-based tools to more sophisticated bifacial handaxes. The earliest evidence points to Mode 1 tools, resembling industries, but by approximately 500,000 years ago, bifaces became prominent, as seen in assemblages from sites like Boxgrove in , where symmetrical handaxes indicate improved skills for butchering and . These bifaces, often made from flint or chert, reflect behavioral adaptations to exploit diverse resources in a fluctuating environment. The introduction of the Levallois technique around 300,000 years ago marked a significant advancement in the Middle Palaeolithic, enabling the production of predetermined flakes for versatile tools such as scrapers and points. This prepared-core method, evident in British assemblages from sites like Baker's Hole in , allowed for efficient resource use and is closely associated with populations who occupied Britain intermittently from about 400,000 to 40,000 years ago. utilized toolkits, characterized by Levallois flakes retouched into sidescrapers and denticulates, which supported their subsistence strategies including scavenging and hunting. Evidence of controlled fire use, a key adaptation for warmth, cooking, and predator deterrence, dates to around 400,000 years ago at Beeches Pit in during the Hoxnian . Excavations revealed hearths with charred sediments, heated flint tools, and burnt bone fragments, indicating habitual fire management by early hominins, likely Neanderthals or their predecessors. Concurrently, of megafauna such as mammoths is attested by cut-marked bones and tool scatters at sites like Lynford Quarry in , where Middle Palaeolithic artifacts suggest Neanderthals targeted large herbivores for meat, hides, and , demonstrating organized group tactics. With the arrival of anatomically modern humans (Homo sapiens) around 40,000 years ago, Upper Palaeolithic adaptations in Britain emphasized specialized bone and antler tools alongside lithic industries. Key evidence includes the Paviland Cave burial in , dated to approximately 33,000 years ago, representing the earliest known human interment in Britain with red ochre and ivory points, indicating ritual practices. Britain has evidence of parietal cave art, such as engravings at in depicting animals, dated to approximately 13,000 years ago, alongside formal burials like those at in (~14,700 years ago) with processed human remains suggesting complex social behaviors. At , artifacts include bone harpoons and awls, used for fishing and sewing hides, reflecting adaptations to a periglacial landscape during the Late Glacial Maximum. These technologies highlight a shift toward more diverse strategies as modern humans navigated the challenges of recolonizing the region post-Ipswichian .

Mesolithic Period

Post-Glacial Settlement Patterns

Following the retreat of the ice sheets at the end of the stadial around 9600 BC, human populations rapidly recolonized Britain from southern refugia in , marking the onset of the period. This recolonization involved small, mobile groups exploiting newly available landscapes as forests and wetlands expanded northward. One of the earliest and most significant sites evidencing this process is in , dated to approximately 9000 cal BC, which served as a seasonal camp with substantial structures including a post-built house and an extensive lakeside platform spanning nearly 2 hectares. Recent research at has further revealed evidence of larger, more structured settlements, including feasting activities and advanced , highlighting greater social complexity in Mesolithic communities. By the 8th millennium BC, Mesolithic communities had spread northward into Scotland and westward into Wales, demonstrating adaptive settlement strategies tailored to diverse environments. In Scotland, the site of Kinloch on the Isle of Rum represents an early highland occupation, featuring stake-built shelters, hearths, and over 140,000 lithic artifacts primarily made from local bloodstone, indicating prolonged use as a base camp from the early Mesolithic onward. In Wales, coastal sites such as Nab Head in Pembrokeshire, dated to around 10,500 years ago (c. 8500 BC), highlight initial concentrations along shorelines, while inland locations emerged later as populations expanded. Regional variations are evident in the prevalence of coastal settlements in western and northern areas, driven by resource-rich marine environments, contrasted with inland wetland sites like Star Carr in the east, where lake edges supported seasonal aggregations. Overall population levels in Britain are estimated at 3,000 to 6,000 individuals, based on site densities, artifact distributions, and environmental models, reflecting a low-density, dispersed network of groups rather than large permanent communities. Accompanying this human expansion was the presence of domesticated dogs by around 9000 BC, evidenced by skeletal remains at sites like showing morphological adaptations such as reduced tooth size and altered skull proportions consistent with early processes. The dynamic settlement patterns were profoundly influenced by post-glacial sea-level rise, which progressively submerged the low-lying connecting Britain to . This culminated in Britain's isolation around 6200 BC following the catastrophic tsunami, which inundated the remaining coastal marshes and islands, severing migration routes and compelling groups to adapt to an increasingly insular geography.

Hunter-Gatherer Lifestyles and Artifacts

The hunter-gatherers of Britain led mobile lifestyles centered on exploiting diverse post-glacial environments, relying on seasonal movements to follow game and gather wild resources. Their economy was based on and , with a diet primarily comprising , various species such as and pike, and plant foods including nuts and berries. Evidence from sites like in indicates active landscape management, including of and other woods to encourage regrowth for tools and food sources, suggesting a nuanced interaction with their surroundings rather than passive exploitation. Material culture was dominated by technology, where small, geometrically shaped flint blades—typically 1-2 cm long—were hafted into composite tools for efficiency in hunting and fishing. These microliths formed barbs on arrows, spears, and harpoons, enabling precise strikes against agile prey like deer or fish in rivers and lakes. The site of Mount Sandel in , dated to around 7000 BC, exemplifies this innovation through thousands of microliths and related tools found in hut contexts, highlighting early adoption of such versatile implements across the . Settlements were often semi-permanent, particularly in resource-rich areas, featuring wooden platforms built from split timbers and stakes to elevate living spaces above damp ground. At , dated to circa 8500 BC, excavations revealed such platforms alongside ritual deposits of antlers, including 21 stag skull-caps interpreted as possible headdresses, indicating symbolic or ceremonial practices integrated into daily life. These structures supported extended stays during peak seasons, with evidence of hearths, tool-making, and . Artistic expressions in Mesolithic Britain were rare and subtle, often manifesting in portable objects that blended utility with symbolism. Such artifacts underscore a cultural capacity for aesthetic engagement amid practical survival needs.

Neolithic Period

Introduction of Farming and Migration

The introduction of farming to Britain marked a profound transformation during the early Neolithic period, beginning around 4000 BC, when migrant populations from continental Europe brought agricultural practices that fundamentally altered the island's subsistence economy and demographics. These first farmers originated from lineages tracing back to Anatolian Neolithic groups, who had spread westward across Europe, introducing a package of domesticated crops and livestock that included emmer wheat (Triticum dicoccum), barley (Hordeum vulgare), cattle (Bos taurus), and sheep (Ovis aries). Genetic analyses of early Neolithic individuals reveal that these newcomers carried approximately 90% ancestry from continental European farmers and only about 10% from indigenous Mesolithic Britons, indicating a near-complete population replacement over subsequent centuries. This migration likely occurred via sea routes from regions like northern France or the Low Countries, supplanting the hunter-gatherer lifestyles of the preceding Mesolithic period. Archaeological evidence underscores the rapid adoption of farming in southern and eastern Britain, where sites demonstrate early experimentation with crop cultivation and . For instance, causewayed enclosures such as Windmill Hill in , constructed around 3700 BC, served as communal gathering places potentially linked to the management of agricultural resources, with associated finds of remains and animal bones highlighting the integration of farming into social practices. Further north, a 2021 excavation at Street House in , uncovered evidence of industrial-scale salt production dating to 3800–3700 BC, including vessels used for evaporating , which points to sophisticated resource processing that supported communities by preserving food and enabling . The spread of farming was not uniform across Britain, with adoption occurring more slowly in and due to environmental challenges and cultural continuities with traditions. In these regions, the Neolithic transition is dated to around 3800 BC, often featuring hybrid sites that blend indigenous foraging with incoming agricultural elements. Balbridie in , , exemplifies this, where a large timber hall from circa 3800 BC yielded extensive assemblages of carbonized and grains, suggesting localized adaptation of farming practices alongside possible persistence of wild resource exploitation. This regional variation reflects a gradual integration rather than abrupt replacement in peripheral areas, shaping diverse trajectories across the archipelago.

Monument Building and Ceremonial Sites

The period in Britain witnessed the emergence of monumental architecture, reflecting the societal organization of early farming communities that had transitioned to sedentary lifestyles. Long barrows, among the earliest such structures, served primarily as communal sites, accommodating the remains of multiple individuals over time. For instance, the in , constructed around 3650 BC, features five stone chambers where at least 36 individuals—men, women, and children—were interred, likely over a span of 10 to 30 years, indicating collective mortuary practices that emphasized ancestry and community identity. These earthen mounds, often trapezoidal and up to 100 meters long, represent a widespread tradition in southern and eastern , with the earliest examples dating to approximately 3800 BC, underscoring a rapid adoption of monument-building as a cultural hallmark. Henges, circular enclosures often incorporating stone or timber elements, evolved later in the Neolithic and functioned as ceremonial centers, possibly for gatherings and rituals. The bluestones, quarried from the Preseli Hills in around 3000 BC, were erected at around 2500 BC during its later phases, possibly forming an initial circle or other arrangement that set the stage for further expansions. Recent excavations suggest these bluestones originated from a dismantled at Waun Mawn in , constructed around 3000 BC, indicating the relocation of an existing monument. The nearby complex, the largest henge in Britain with a circumference of 1.3 kilometers enclosing up to 180 stones, began with timber circles—six concentric rings—preceding the stone arrangements around 2500 BC, suggesting a progression from perishable to durable materials in ritual architecture. These monuments highlight the logistical feats of Neolithic groups, mobilizing labor and resources across distances to create enduring sacred spaces. Regional variations in monument building reveal diverse influences across the , with northern traditions drawing from broader Atlantic European networks. In , chambered tombs like Maes Howe in , built around 2800 BC, exemplify the Orkney-Cromarty type, featuring a beehive-shaped and a long passage leading to a central chamber for collective burials, possibly aligned with solstice events. Irish passage tombs, such as those at the Boyne Valley complex, exerted influence on British designs through shared motifs and construction techniques, including corbelled roofs and artistic engravings, fostering cultural exchanges evident in the fourth millennium BC. Archaeological evidence points to these sites as venues for feasting and astronomical observations, integrating social, ritual, and cosmological functions without the aid of written records. Animal bones and pottery at enclosures like near indicate large-scale feasting events, involving hundreds of participants and emphasizing communal bonds. Alignments in structures such as Maes Howe toward the sunset and 's midsummer sunrise suggest deliberate orientations to celestial events, potentially marking seasonal rituals or calendars in Neolithic cosmology.

Bronze Age

Beaker Culture and Genetic Shifts

The Beaker culture arrived in Britain around 2500 BC, originating from the region in , where communities associated with the Bell Beaker complex had developed distinctive pottery and traditions. These migrants introduced bell-shaped beakers, often used in funerary contexts, along with equipment such as wristguards and arrowheads, marking a shift from communal practices to more individualized expressions of status. The rapid dissemination of these artifacts across Britain suggests a dynamic cultural exchange, with the Beaker package appearing in first and spreading northward within a few centuries. Ancient DNA analysis reveals that this migration led to a profound genetic transformation, with approximately 90% of the Neolithic population in Britain replaced by individuals carrying steppe-related ancestry from the continent by around 2000 BC. This replacement involved migrants whose genetic profiles closely resembled those of contemporary Beaker groups in the and , contributing the dominant ancestry seen in modern British populations, particularly in . This genetic shift contrasted sharply with the earlier Neolithic farmer ancestry, indicating a near-total demographic turnover. A subsequent major migration during the Middle to Late , around 1300–800 BC, introduced additional genetic changes in southern Britain. Ancient evidence shows that incoming groups, genetically similar to populations in ancient , contributed approximately 50% of the ancestry in by the [Iron Age](/page/Iron Age). This influx increased Early European Farmer-related ancestry and is associated with the rise of to around 50% frequency, enabling adult milk consumption and supporting economies—a development that occurred about a millennium earlier in Britain than in . These migrants may have played a role in spreading early . Burial practices underscore the mobility and elite status of these newcomers, exemplified by single-grave inhumations containing rich . The , discovered near and dated to circa 2300 BC, was buried with three copper knives, gold ornaments, flint arrowheads, and Beaker pottery, signifying high social standing and long-distance travel. of his teeth indicates he originated in the Alpine region of , highlighting the role of elite individuals in transmitting Beaker culture and metallurgical knowledge across . The Beaker period also marked the initial use of in Britain, sourced primarily from mines at in Ireland, where early extraction around 2400–2200 BC coincided with Beaker pottery presence. This Irish , often in the form of arsenical alloys, supplied tools and ornaments in British burials, establishing foundational metallurgical networks that integrated Britain into wider European exchange systems.

Metallurgy, Trade, and Social Changes

The transition to bronze metallurgy in Britain around 2200 BC involved the alloying of copper with tin, creating a harder and more durable material than pure copper used in the preceding Beaker period. This innovation facilitated the production of specialized tools like palstaves, flat-axe variants with side flanges for hafting, which became widespread in the Middle Bronze Age for woodworking and agriculture. By the Late Bronze Age, weaponry advanced further with the development of leaf-shaped swords, exemplified by the Ewart Park type around 800 BC, characterized by octagonal hilt plates and protective shoulders for enhanced combat utility. These metallurgical shifts, building on early copper-working precursors from the Beaker culture, underscore a growing technical sophistication driven by resource access and craftsmanship specialization. Extensive trade networks sustained bronze production, with tin sourced primarily from Cornish deposits and exchanged along routes extending to the Mediterranean by the mid-second millennium BC. from the also circulated widely, appearing in elite burials and hoards as a prestige good, indicating long-distance connections across northern Europe. The Wilburton complex, a Late metalworking tradition centered in eastern England's fenlands circa 1150–1020 BC, exemplifies these exchanges through hoards containing swords, spearheads, and razors, often incorporating imported materials and continental influences that highlight interconnected production and distribution systems. These economic developments coincided with profound social changes, including the emergence of chiefdoms marked by hierarchical settlements on defensible hilltops. Rams Hill in , a multivallate dating to circa 1000–800 BC, served as a focal point for elite activities, with of feasting, , and controlled access suggesting centralized authority over resources and labor. Concurrently, signs of increased warfare appeared in the form of deliberate deposits, such as bent and broken swords and spears ritually interred in rivers and bogs, interpreted as offerings or decommissioning after conflicts amid rising social tensions. Environmental pressures further shaped these transformations, as a climatic cooling and wetter conditions set in around 1000 BC during the Subatlantic phase, prompting adaptations in land use. On Dartmoor, this stress is evident in the construction of field systems like those at Grimspound, a Late Bronze Age settlement of 24 stone-walled huts enclosed by a perimeter wall, dating to circa 1450–700 BC, where coaxial fields indicate intensified pastoral and arable management to cope with deteriorating conditions.

Iron Age

Emergence of Iron Technology

The introduction of ironworking to Britain marked a pivotal technological shift during the Early Iron Age, beginning around the 8th to 7th centuries BC under influences from the continental of . This technology likely arrived via trade and cultural exchanges across the Channel, with early evidence of iron objects and slag appearing in by the late 8th century BC. C phase artifacts, including imported bronzes, indicate connections that facilitated the adoption of iron smelting techniques, transitioning from bronze-dominated economies. Archaeological sites provide direct evidence of early iron production, such as the substantial slag deposits at Little Woodbury in Wiltshire, dated to ca. 400–100 BC, where bowl furnaces and iron blooms suggest small-scale smelting operations using local bog iron ores. Similarly, excavations at Shooters Hill in southeast London uncovered iron smelting slag in contexts from ca. 700–400 BC, associated with simple hearth-based furnaces that produced small blooms of 4–5 pounds. In East Yorkshire's Foulness Valley, sites like Moore's Farm yielded one of Britain's largest prehistoric slag heaps (over 5,000 kg), dated to the 6th–3rd centuries BC, highlighting organized production using shaft furnaces and plano-convex furnace bottoms. These findings demonstrate that iron smelting spread from continental models, with bloomery processes involving charcoal-fueled reduction of ore in clay-lined pits or hearths. Iron tools revolutionized , with iron-tipped ard ploughs enabling deeper soil turning and clearance on heavier clays, which supported expanded cultivation and livestock management. This innovation, evident from the onward, contributed to increased food surpluses and denser rural populations in fertile lowlands, as iron axes and sickles improved efficiency over wooden or equivalents. In warfare, the adoption of iron weapons accelerated around with the arrival of La Tène stylistic influences from the Continent, introducing longer, double-edged swords designed for slashing that enhanced combat effectiveness and social status display in elite burials. Adoption of iron technology exhibited regional variations, occurring earlier in southeast England—where Hallstatt and early La Tène contacts were strongest—by the 7th century BC, while northern regions like saw later integration around the 5th–4th centuries BC, influenced by distinct local traditions and slower diffusion. In the southwest, this period coincided with the production of distinctive ware pottery, a finely decorated, quartz-tempered ceramic style from the 4th–1st centuries BC, often found at ironworking settlements and reflecting La Tène artistic motifs in everyday vessels. Early precursors to larger oppida, such as enclosed complexes at sites like The Ditches in (3rd–1st centuries BC), emerged alongside iron production, serving as hubs for crafting and exchange that foreshadowed Late urbanism.

Hillforts, Tribes, and Cultural Developments

During the Late Iron Age, Britain saw the widespread construction of hillforts, with over 4,000 examples identified across Britain and , serving as major centers of settlement, defense, and social organization. These enclosures, often situated on hilltops or promontories, featured earthen ramparts and ditches, with many evolving from simpler univallate forms to more elaborate multivallate designs involving multiple concentric walls for enhanced protection. Construction began around 600 BC in southern regions, as seen at Maiden Castle in Dorset—one of the largest hillforts, spanning over 23 hectares—and continued until about 100 AD, though activity peaked around 100 BC during a phase of intensification that reflected growing social complexity and possibly inter-group tensions. Iron tools facilitated the labor-intensive earthworks, enabling deeper ditches and steeper ramparts than earlier periods. Society in Late Iron Age Britain was organized into tribal groups, such as the in the southwest, who occupied hillforts like Maiden Castle, and the in the southeast, centered around sites like . These polities exhibited hierarchical structures, inferred from the emergence of coinage around 100 BC, which bore symbols of authority and facilitated trade, suggesting the rise of elite leaders who controlled resources and alliances. Gold and silver coins, often imitating continental styles, circulated among tribes like the under rulers such as Cunobelin, indicating centralized power and economic integration. Cultural developments included distinctive art styles, exemplified by intricately decorated bronze mirrors featuring swirling motifs and geometric patterns, which appeared in the late and symbolized status among elites. Torcs, elaborate gold neck-rings with twisted wires and terminal motifs, were similarly prestigious items, worn by high-ranking individuals and deposited in hoards, reflecting a shared aesthetic influenced by continental Celtic traditions. The arrival of remains debated, with evidence pointing to introductions around 1000 BC through earlier migrations during the transition, while later Belgic groups from the arrived in the late (ca. 150–50 BC), potentially reinforcing linguistic patterns, though continuity from earlier periods is also supported. Recent genetic studies reveal strong continuity from populations into the , with autosomal DNA showing persistent ancestry profiles across Britain and minimal additional continental beyond earlier Steppe-related inputs. This stability underscores indigenous development, tempered by localized exchanges, such as minor inputs from Belgic migrations in the southeast. In northern regions like , cultural expressions diverged with the of crannogs—artificial island dwellings—and brochs—tall drystone towers—yet these forms remain underrepresented in broader narratives dominated by southern hillforts.

Protohistory

Early Written Accounts and Explorations

The earliest external written accounts of Britain emerge from Greek and Carthaginian sources during the 6th to 4th centuries BC, reflecting Mediterranean interest in the island's resources, particularly tin essential for production. Around 450 BC, the Greek historian referenced the , or "Tin Islands," as a distant archipelago supplying tin to the eastern Mediterranean, though he expressed skepticism about their existence due to reliance on unverified Phoenician reports. Earlier, circa 500 BC, the Carthaginian navigator Himilco led an expedition into the Atlantic, reaching northwestern Europe including Britain to secure tin trade routes, as preserved in later Roman accounts drawing from Punic periploi (voyage descriptions). These voyages underscore Phoenician-Carthaginian dominance in Atlantic commerce, with Britain positioned as a peripheral but valuable outpost beyond the . The most detailed early exploration came from Pytheas of Massalia, a Greek mariner and geographer, who undertook a pioneering voyage around 325 BC, sponsored by merchants seeking direct access to northern trade goods. In his lost work On the Ocean, quoted by later authors like Strabo and Pliny, Pytheas described circumnavigating Britain, which he called "Pretannike," noting its triangular shape, the inhabitants' agrarian lifestyle, and active tin mining in the southwest, particularly Cornwall, where ore was smelted and traded. He ventured further north to Thule—often identified by scholars as possibly the Shetland Islands or Orkney—portraying it as the northernmost land where the sea congealed into a slushy mass and the midnight sun prevailed during summer solstice. Pytheas' observations extended to the amber trade along the North Sea coasts, linking Britain's resources to broader European networks. Despite their influence, these accounts suffered from limited accuracy and cultural biases, as Mediterranean writers struggled to reconcile northern phenomena with familiar geographies. ' reports of perpetual daylight, binding frosts, and tidal phenomena were dismissed by contemporaries like and as fabrications, yet they shaped subsequent , inspiring Ptolemy's later maps and medieval notions of hyperborean lands. The vagueness of Himilco's periplus, filtered through Latin intermediaries like Avienus' Ora Maritima, similarly obscured precise locations, prioritizing commercial secrecy over empirical detail. Such narratives highlight the exploratory rather than ethnographic nature of these contacts, with Britain viewed primarily through the lens of extractive trade. Prehistoric Britain lacked any indigenous writing system, rendering external accounts the sole textual records of its protohistoric phase, as confirmed by archaeological evidence of purely oral-based societies. Oral traditions, however, persisted among the Celtic-speaking peoples, inferred from later medieval compilations of myths that preserve echoes of beliefs, such as heroic cycles and otherworldly voyages akin to those in Irish and Welsh lore. These unwritten narratives likely informed interactions with early explorers, though they remain inaccessible without the bridging role of post-Roman texts.

Transitions to Historical Contacts

The late Iron Age in Britain marked a period of escalating contacts with the Mediterranean world, particularly , transitioning from sporadic reconnaissance to sustained economic and political ties. In 55 and 54 BC, led two expeditions to Britain, primarily as reconnaissance missions to deter Gallic support for continental tribes and to enhance his political prestige in . These incursions, detailed in his , involved landing on the coast, engagements with local tribes such as the and Cenimagni, and brief advances inland, though no permanent Roman presence was established. Caesar described the island's inhabitants as divided between indigenous interior peoples and coastal settlers descended from Belgic migrants from , who had crossed for plunder and conquest; he noted their use of iron for tools and weapons, imported for in the form of rings, and a society structured around cattle herding with buildings resembling those in . While his primary account of druids appears in the context of Gallic society in Book VI, Caesar's interactions during the British campaigns imply similar priestly roles among the island's , influencing religious and social practices observed by his forces. Following Caesar's expeditions, trade between Britain and the Roman world intensified, fostering economic interdependence that blurred prehistoric boundaries. Archaeological evidence from sites like reveals a surge in Mediterranean imports, including amphorae, , and luxury ceramics, arriving in greater volumes from the mid-1st century BC onward. In exchange, Britain exported staples such as grain, cattle, hides, iron, and notably slaves, alongside hunting dogs and pearls, as recorded by the geographer around 20 BC–20 AD. This commerce, channeled through ports in southeast and , not only enriched tribal elites but also introduced Roman material culture, such as pottery and coin prototypes, signaling a shift toward proto-urban exchange networks. emphasized the scale of these exchanges, noting that British slaves and grain were bartered for wine and other goods, highlighting the island's integration into broader Roman economic spheres without direct . A key indicator of this cultural was the emergence of late coinage imitating Roman designs, beginning in the late (c. 120–100 BC). Southeastern tribes, particularly the and , minted silver coins that closely replicated Republican denarii, featuring laureate heads and victory motifs to project authority and legitimacy. These imitations, often uninscribed at first, evolved into gold and silver issues with Latin legends by the 20s BC, reflecting rulers' emulation of Roman imperial iconography to consolidate power amid intensifying trade. Scholarly analysis underscores how such coinage facilitated transactions in Roman-influenced markets, with over 40,000 examples recovered from hoards, demonstrating widespread adoption and ideological alignment with Mediterranean powers. This numismatic innovation bridged local traditions with foreign influences, paving the way for political deference to . By the early 1st century AD, these interactions culminated in the formation of client kingdoms that served as buffers and allies to , setting the stage for the Claudian invasion of 43 AD. Cunobelinus, ruler of the from circa 9 to 40 AD, dominated much of southeast Britain, issuing coins that blended Celtic and Roman styles and maintaining lucrative trade ties with the . His kingdom functioned de facto as a , providing grain, metals, and slaves while receiving ; the exile of his son Adminius to Emperor in 40 AD prompted Roman preparations for intervention, as noted in ' accounts. Cunobelinus' death around 40–41 AD destabilized the region, with his sons and resisting Roman overtures, yet the prior economic entanglements made full conquest inevitable under Emperor to secure these frontiers and resources.

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