* < <../../index.htm> Main Page <../../index.htm>* * Chapter 4* The Monuments of the Early Farmers in the Landscape Knowledge of farming reached the British Isles from France and Flanders and appeared in various localities in Britain and Ireland. It suggests that individual parties of farmers from Europe set out at different times to settle here. The conventional date for the first of these events, the beginning of the British Neolithic, is c4500BCE. Many of the monuments that were the first to appear in the British version of the Western Neolithic landscape are still with us today and include causewayed enclosures, mortuary buildings/enclosures and long barrows and some were embarked upon around 3800 cal BC, some 200 years after the introduction of agriculture. This was a period of ?settling down? in which generations of people became accustomed to the new way of life and built up the resources that allowed them to construct the enduring signs of the Neolithic presence. In contrast, their farming sites, as we have seen, were far more ephemeral and have left less record. The number of causewayed enclosures (earlier called causewayed camps) (Oswald) have greatly increased in recent years due, in the main, to aerial photography. These enclosures, usually difficult to spot from the ground, show up as crop-marks from the air in grain fields as the greater depth of soil in their ditches allows the crop planted above the ditches to grow taller and ripen later than the rest of the field so, early in the summer, the lines of the ditches appear as dark marks in the lighter green of the crop. The number of known causewayed enclosures has jumped from 16 in 1970, mainly in southern England, to round about 50 today, with one at Donegore Hill in Co. Antrim in Northern Ireland. However, northern and western Britain still appear blank on a distribution map. They are so called because the enclosure is formed by a rough circle of short stretches of ditches and banks. In some cases there is more than one 'circle' as at Windmill Hill (three) and Robin Hood's Ball (two) in Wiltshire and Maiden Castle (two) in Dorset and at least one monument, Knap Hill, in Wiltshire, appears to be incomplete. They range in area from less than two hectares at Whitesheet Hill in Wiltshire to twenty-eight hectares at Crofteon in the same county. A good deal of effort has been devoted to the elucidation of these monuments but so far no satisfactory general explanation has been forthcoming and we can only point to possible explanations for specific monuments derived from excavation evidence. But it is probably safe to assume that they were meeting places. The pioneering excavation was done at Windmill Hill, part of which was examined in 1925 and it is still one of the sites that present some of the fullest evidence. Very little was found in the interior of the enclosure but the ditches turned out to be a series of conjoined pits containing a variety of materials . These included deposits of various topsoils, pottery from as far afield as the Lizard in south-west Cornwall, animal bones, charcoal and stone axeheads from Cornwall, North Wales and the Lake District. Excavations in recent years in the area around the monument have discovered smaller pits containing animal skulls and flint implements. Dating for the site runs from 3600-3300BCE. These bewildering collections of materials were clearly buried by a variety of depositees and are ritual deposits which have also been discovered in other causewayed enclosures like Crickley Hill in Gloucestershire and Hambledon Hill in Dorset where they were found in the ditches and at Etton in Cambridgeshire (Pryor), which was almost completely excavated, where there were deposits in both the ditches and in pits in the interior of the enclosure. The deposits were perhaps made as offerings to some power(s) that was/were thought to control natural phenomena like the weather, fertility of animals, crops, human diseases, running water, etc, etc, and are attempts to ensure good fortune and the favour of the deities who were in charge of these things. Ceremonial places where deposits of this sort are made are called fana and this is one explanation for some causewayed enclosures. Other explanations that have been put forward over the years are cattle-markets and central places, a term that means a place where members of a scattered community could come together. Another particular function was identified by the excavator at Hambledon Hill. Roger Mercer found the soil in the interior of the enclosure full of small pieces of human bone and in one of the ditches the lower half of a skeleton of a small boy where it had been dragged by some wild animal. Mercer identified the monument as a place of excarnation where bodies were exposed to the elements after death until the flesh had rotted away. Thereafter the remaining bones were collected up and stored in barrows that have been identified as ossuaries. Dating of these enclosures rests mainly on determinations from the southern monuments. A rough estimate for the construction of Knap Hill would be c3450BCE, for the first construction at Maiden Castle about 3800BCE, and for Hambledon Hill, c3400BCE. So round about the middle of the fourth millenium BC would be a good starting point for them and. as far as we can tell, they seem to have been falling out of use about a thousand years later. But we have so little evidence for the use of these monuments which would have taken so long to contruct with the tools that were employed at the time that one sometimes wonders whether the actual construction was the work of various groups and an important ritual in itself and that its completion and the subsequent history of the site an irrelevance as far as its originators were concerned. They were, in fact, simply making an individual statement and not an artefact for use. In this scenario, evidence found on the sites would include deposits by later people making use of a site that was well known as a place of spiritual power. Associated with causewayed enclosures and perhaps constructed by groups of people (septs or small clans) who cleared and farmed in adjacent small areas are mortuary enclosures and barrows. Professor Colin Renfrew, who has studied megalithic stalled cairns (barrows) on the island of Rousay, identifies each barrow with an adjoining territory belonging to an individual sept. The cairns not only served as places where excarnated remains (skulls and long bones) could be deposited after exposure but also as markers of the sept territories on which dwelt the people whose ancestral remains were stored within them. It may be then that the barrows in other areas performed the same function as on Rousay, so that, in the Windmill Hill area, for example, long barrows belonged to septs who later created the causewayed enclosure. Building a long barrow may have been within the capacity of the twenty or thirty people who made up an early sept but who could not have constructed a causewayed enclosure unless they co-operated with their neighbours. Latest reaearch suggests that long barrows began to be built around two hundred years after the arrival of agriculturists but few were used for for more than three to four generations. The first barrow built at Wayland?s Smithy in Oxfordshire was probably used for under a decade. There are two types of long barrow: the earthen long barrow (Ashbee) and the megalithic long barrow (Daniel). The 'long' refers to their shape, the 'earthen' to the material forming the mound and 'megalithic' to the stones used for building the chambers. It has never been a particularly useful distinction for it really only works in Wessex and not in other parts of the country. Nowadays, it is better simply to distinguish between non-megalithic (without stone chambers) and megalithic, and this is probably valid as (a) a constructional distinction and maybe (b) as a ritual distinction which is perhaps real but which we have only the haziest conception of. A typical neolithic position! Very roughly speaking, the non-megalithic (earthen) types are found in eastern Britain while the megalithic ones are found in western Britain and Ireland. But the function of all Neolithic barrows was probably the same: they were almost certainly used as a repository for human remains left behind after excarnation (exposure to denude the flesh). As, during the decay of the corpse, animals and birds carry off the smaller skeletal bits, it is usually only the long bones and the skulls that survive the process. In Europe the bodies that lay out for months on the Western Front of the First World War suffered the same process and photographs of them show the process in various stages and suggest that, depending on the time of the year, several months are necessary for the process to be completed. At Douaumont near Verdun in France a large ossuary contains the bones of thousands of the dead from both sides collected from the battlefield and stored in chambers which visitors can view. You can think of it as a modern version of a Neolithic long barrow built for the same commemorative purpose and in much the same shape. In India and elsewhere, people still excarnate their dead. In the Naples area of Italy bodies are disinterred after they have become desiccated and are then stored in communal charnel houses where they are visited each year and ceremoniously doused in perfume and rewrapped in fresh silk for the coming twelve months. In other places today the dead are paraded annually through the village and shown the changes that have taken place over the last twelve months. So the idea that the ancestors should be respected and shown consideration as though they remained as part of the community survives in a number of societies today. In Neolithic Britain, barrows seem to have been used for a limited period of time, perhaps for not much more than three to four generations which supports the idea of small communities keeping alive memories of their immediate kin and other people they respected rather than tribal ancestors. In the case of four barrows, at Ascott-under-Wychwood, Hazleton, West Kennet and Fussell?s Lodge their period of active use ended within a decade or so of 3625BC Archaeologists love to classify things and barrows are frustrating to archaeologists because they are so varied that they defy classification except in very broad (and probably rather meaningless) categories. The mounds might be long, trapezoidal, ovate, rectangular or oval while the chambers underneath can be made of wood or megaliths (large stones) and constructed in a variety of plans. Entrances can be at the sides or at the ends or in the case of the earthen long barrows entirely obliterated by the heaping up of the mound. Do these represent local deviations encapsulated within a broad tradition? Names given to categories can be geographical: Severn-Cotswold, Clyde cairns, Maes Howe tombs, Clava cairns and Camster cairns. Other names describe some specific feature of the category: Entrance graves (portal dolmens), Wedge graves, Passage graves and Court cairns. Mortuary Enclosures show up best from the air as rectangular banked and ditched enclosures. An excavated example at Yarnton near Oxford contained three inhumation and eight cremation burials. But it seems that these enclosures were usually developed into earthen long barrows and as such have been found underneath some excavated mounds. Wor Barrow in Dorset, Willerby Wold in Yorkshire, Fussell's Lodge in Wiltshire, Nutbane in Hampshire and Lower Luggy in Powys are examples of mortuary enclosures later incorporated in barrows, the last one dated by AMS to c3600-3300BCE (Gibson). Remains of what is thought to have been an excarnation platform where dead bodies were exposed (see also the enclosure at Hambledon Hill) have been discovered at Stoney Middleton in Derbyshire (English Heritage). The platform, found underneath an Early- Bronze Age round barrow (note the continuity), was surrounded by a semi-circular wall with three standing stones by the entrance. Hundreds of human teeth and bones have been found at the site together with the tiny bones of small animals such as frogs and rodents, which are thought to have been deposited at the site in the droppings of owls and other birds of prey attracted to the decaying human flesh. The excavators suggest the site was built c3000BCE and remained in use for some 1000 years. At Wor Barrow, Dorset, a palisaded exposure enclosure was later removed and the ditches filled in and covered with a mound of chalk and soil dug out of flanking ditches so converting the site into an earthen long barrow. The bones that had previously been excarnated/stored in the enclosure were placed together at the eastern end prior to the building of the mound. Willerby Wold, Wiltshire, before the heaping up of the mound, had a timber facade at one end of the enclosure, like Kilham in Yorkshire, and a crematorium area, Fussell's Lodge, also in Wiltshire, in its early stage had a timber enclosure and porch similar to Wor Barrow while Nutbane at first was a mortuary area and featured an enclosure with a timber building/elaborate porch in front of it. Radiocarbon dates for excavated earthen long barrows include: Dalladies, Fettercairn, Kincardineshire c4100 cal BCE Willerby Wold, Yorkshire c3710 cal BCE Kilham, Yorkshire c3670 cal BCE Nutbane, Hampshire c3450 cal BCE South Street, Wiltshire c3400 cal BCE Normanton, Wiltshire c3390 cal BCE (Cal = calibrated) At Wayland's Smithy in Berkshire, an earlier non-megalithic long barrow had a megalithic barrow built on top of it, demonstrating a continuation of burial practice on the same spot and the essential equivalence of the megalithic and non-megalithic monuments so we can see them as analogous strands of the same tradition of ancestor veneration. There is no need to regard this necessarily as evidence of religious or ritual practice as we would the deposits mentioned in association with the causewayed enclosures but rather as a means of proclaiming the continuity of the communal identity with the barrow as marker of the ancestral land. The early timber barrow was used between 3450 and 2400 cal BC. Then after around a hundred years or so a second but megalithic barrow was constructed and was in use until around 3350 cal BC. Two non-megalithic long barrows are unusual in that there is no sign of any bones or wooden mortuary structures underneath the mounds, only an arrangement of hundreds of upright stakes which divide the areas under the barrows into segments along both sides of a central spine. The arrangement has the same pattern as the skeleton of a fish. These barrows at Beckhampton Road and South Street, close together in Wiltshire, are usually referred to as cenotaphs for want of a better description. The megalithic (= large stone) tradition has benefited by large-scale excavations devoted as much to the mounds as to the stone structures under them. Three Severn-Cotswold types have been totally excavated in recent years at Ascott-under-Wychwood, Oxon, Gwernvale in Brecknockshire and Hazleton North in Gloucestershire. At Ascott and Hazleton, stone-walled segments under the mounds recall the stake segments in the Wiltshire earthen examples described above and at Gwernvale a wooden phase preceded the stone phase as it did at Wayland's Smithy. Excavations of megalithic barrows have demonstrated their function as a repository for human bones, almost always long bones and skulls, lying in stone chambers that are usually arranged at the end or along the sides of the passage leading into a round mound, or in compartments of a segmented gallery in a long mound, one end of which serves as the entrance to the structure. Otherwise, the gallery is reached by means of a tunnel at right-angles to the east/west alignment running into it from the side of the long mound. Severn-Cotswold types of long barrow comprises two sub-types. One is the transepted gallery grave with a gallery, one end of which forms the entrance, from which open on both sides a number of compartments, known as transepts. The best-known excavated example open to the public is West Kennet not far from Avebury in Wiltshire. The other sub-group consists of individual chambers placed on both sides of the long mound each with its separate entrance. Occasionally in this sub-group there is a false entrance at the broad, eastern end of the mound where the entrance of the transepted gallery grave would be found. An example of a 'dummy portal' is at Belas Knap in Gloucestershire that gives the impression that it is leading into a gallery The West Kennet barrow is often taken as a typical example of the 'transepted gallery grave' but the mound is much larger than most, having megalithic chambers only under the eastern end of a ninety-metre-long mound. The chambers are fronted by a small courtyard later closed off by a facade of upright large stones, one of which is said to weigh fifty tons. The small chambers open off both sides of the gallery. There are two chambers on each side with a chamber at the end of the gallery. Unusually, the structure is high enough for one to walk upright. The mound over them is much larger than is required to cover them and boldly announces their location on the top of the ridge. The first of the burials took place in the 3640s cal BC and the last some 10-30 years later. After a hundred-year gap the chambers began to be filled up with material scraped up from the surrounding area and, last of all, a thousand years later, the barrow was finally blocked off with the large stones that still seem to bar access. Not far away, Fussell?s Lodge barrow was constructed with a mound of chalk gradually piled over a period of time inside a massive timber fence. The earliest burials date to around 3700 cal BC and the final inhumations to between 3630 and 3620 cal BC when the chalk mound was completed. In the Cotswolds, Ascott-under-Wychwood and Hazleton long barrows both consist of wedge-shaped mounds over stone chambers accessed through short passages through the sides of the mounds. Excavations found the remains of 21 people in the Ascott barrow chambers and 40 at Hazleton. A Neolithic settlement under the Ascott mound is dated to the 3900s or 3720s cal BC followed by a gap of 50 years before the barrow was built in the 3730s or 3720s cal BC. The Hazleton pre-barrow settlement dates to the 3800s cal BC and the barrow on top between 3700 and 3650 cal BC, being used until around 3630 cal BC. (English Heritage). Usually, in those barrows open to the public as, for example, at Stoney Littleton south of Bath, one has to crouch inside and crawl on all-four sinto a corridor which has three 'transepts' on each side and the mound has a kerb of drystone walling around it that may be original and not added at a whim of a nineteenth-century antiquary. In contrast to West Kennet, the chanbers take up a large proportion of the length of the mound. Examination of the alignments of long barrows in the Windmill Hill/Avebury region show that they have their broad ends, where the megalithic chambers are or where the remains of the bodies were placed in the case of a non-megalithic long barrow, facing in a general easterly direction. This has prompted the suggestion that the megalithic 'suite' or mortuary enclosure underneath the earthen barrow was built to face the point on the horizon where the sun would rise on a particular day of the year. An example of the passage grave type of megalithic tomb under a circular mound is Newgrange in the valley of the Boyne in Ireland where cremation is the commonest burial rite. The chambers lie under a vast pile of mainly water-rolled pebbles that has been restored to a likeness of its original prehistoric form. Around this 200,000 tons of material, is a kerb of oblong boulders decorated with a variety of incised designs. (Irish barrows: Herity and Eogan). A cruciform chamber at the end of the entrance passage is roofed with a hexagonal vault built of corbelled blocks each weighing up to a ton. This chamber is also ornamented with incised designs. Above the entrance is a fanlight leading to a tunnel above the passage. This allows the rising sun to shine along the tunnel and play on the centre of the chamber floor each midwinter's day. A similar phenomenon has been engineered in Cairn T and Cairn U of the Loughcrew (County Meath) group, many of which are similarly decorated. Not far off, two passage graves, one a Breton type (similar to examples in Brittany), and the other similar to that at Newgrange, lie under mounds even bigger than Newgrange's. Like Newgrange, Knowth has carving on the stones of the grave and on the kerbstones surrounding the mound but the quality of the art is higher with simple, bold designs that can be appreciated at a distance. Around this spectacular monument are grouped seventeen smaller tombs each covered with a round mound. At the eastern end of the group is the Dowth tumulus, the largest of the complex, covering two megalithic structures, both decorated, although not to the same standard as Knowth and the mound has similar kerbstones, albeit decorated in a second-rate style. These great megalithic round barrows are matched but not outclassed by the similar structures in Brittany in north-western France. This art which consists of what has been described as ?motives of the mind?, copies of mental imagery generated in the brain by altered states of consciousness ? ?trances? in other words and in the opinions of some experts is related to the Neolithic conception of death which was a transition to another environment and given substance by the structure of the tomb itself. This is an attractive idea but does not help us to explain the role of the many other megalithic tombs that were not supplied with similar megalithic art unless it was only the passage-grave builders who were privy to these visions. A group of barrows is described as a cemetery and this is the finest barrow cemetery in the British Isles. Other passage grave cemeteries exist in Ireland, as well as individual barrows, all in the north and east of the island; the earliest built in the cemetery above Sligo town, according to the latest excavators, between 5620 and 5310BCE. This dating brings into focus the question of the nomenclature of British and Irish archaeological periods. Within the present framework, the dating of this tomb places it in the Mesolithic rather than in the Neolithic period in which megalithic tombs have long held an iconic position. So, either one accepts that Mesolithic people were building such structures, both here and on the Continent where there are radiocarbon dates of late 6^th and early 5^th millennia for tombs in Brittany, Poiters and Galicia, or one must accept that the Neolithic period had its beginning around a thousand years earlier than what is usually accepted. The definition of the Neolithic period is as the era of the earliest farming in the British Isles but one is never going to be able to give a definite date for its inception simply because the evidence for the first farmers is always going to be ephemeral and a date in the middle of the 6^th millenium is as likely as one in the middle of the 5^th . It may be germane to this discussion to point out that some of the earliest dates for firm evidence of agriculture in the British Isles are from the north of Ireland (Cf. Ballynagilly etc). The two commonest types of megalithic tombs in Ireland are the courtyard cairn, which is the earlier, and the portal dolmen. The earliest courtyard cairns date from the fifth millenium BCE. Under a trapezoid or elongated mound is a segmented gallery consisting of two or more chambers that leads out of a forecourt (an area enclosed by a wall of stones) at one end of the mound which is continued round the forecourt on both sides, forming a wall, sometimes almost totally enclosing it, like the claws of a lobster. One of the best examples of a court cairn is Creevykeel in Co. Sligo with a cairn some 55m metres long. The evidence for deposition was five small pockets of cremated bone in the chambers. Three subsidary chambers were inserted into the tail of the cairn and in one of them a great deal of pottery was discovered. Portal dolmens are found in Cornwall and Wales but their greatest concentration is in Ireland. From a miniature forecourt one enters, between two tall slabs, a rectangular chamber which usually becomes narrower and lower towards the further end. The entrance is often blocked by a slab that may reach right up to the capstone (roofing-slab) that can be massive. At the Brownshill Portal Dolmen near Carlow in Leinster it weighs over a hundred tons. Grave goods are similar to those from the court cairns except that the pottery is decorated. These similarities have led Irish archaeologists to put forward the idea that the Portal Dolmen was derived from the Court Cairn. The chambers of many Portal Dolmens stand unencumbered by a cairn, suggesting that they never reached the stage of acquiring a mound. At the end of the Neolithic period the Wedge Grave appears in Ireland. Its chamber is in the form of an antechamber and gallery that narrows slightly at the inner end and is often entered by a doorway framed by tall slabs. Some examples have a double thickness wall with a narrow space between the two walls. The cairn may be roundish, oval or D-shaped and often has a retaining wall to hold the mound in shape. Inside, both inhumations and cremations have been found together with pottery, commonly of the Beaker type (see below). At Moytirra, Co. Sligo, the inhumed remains of four adults and a child were found. At Lough Gur, the chamber contained the remains of at least twelve inhumations and a cremation. Barbed-and-tanged arrowheads and thumb scrapers occur amongst the flint artifacts. In south-west Scotland cairns tend to be rectangular or wedge-shaped with the wider end built concave to form horns like the court cairns of Ireland. The gallery leads off this forecourt and is split into compartments by kerbs. Half of the burials found in the excavated chambers were cremations and half inhumations and both were accompanied by round-bottomed early neolithic bowls and flints. Dating for the earliest example is probably before 4000BCE and the monuments are known as Clyde Cairns. Bargrennan is one of a small group of passage graves in south-west Scotland and has given its name to the group. Elsewhere in Scotland the megalithic cairns are mainly variations on the themes of the passage grave and the gallery grave. In Orkney are the passage graves referred to as the Maes Howe type named after the most famous example which has a high passage leading to a spacious rectangular corbelled chamber with three rectangular cells opening from it about a metre above the floor of the main chamber. The chamber lies under a mound of about 35 metres in diameter that is surrounded by a ditch. Radiocarbon determinations from Maes Howe and from the Quanterness passage grave indicate dates for the group in the later fourth and early third millenia BCE. In north-eastern Scotland the Clava Cairns are another type of passage grave. Two sub-groups make up the assemblage. One is an annular cairn with a hole in the middle like an American doughnut. Like the doughnut, there is no break in the encircling material. In the unroofed interior, cremation burials were made. The other sub-group is a characteristic passage grave with a corbelled chamber at the end of a short passage set under a round mound. Monuments of both sub-groups are surrounded by circles of monoliths (individual standing stones). The N.E. Clava cairn has been investigated and it has been found that the final rays of the setting midwinter sun shine directly down the passage and into the chamber. These Clava tombs have recently been dated to around 2000BCE. Further north in eastern Scotland is the group known as the Camster Cairns. Chambers are galleries, entered at one end, and divided up by projecting jambs into interconnecting compartments, the whole being covered by a circular mound. In some examples, however, the gallery can be much longer, accommodating up to twelve compartments and the mound is correspondingly elongated. In these examples the chambers are entered through a short passage at the side like the Stalled Cairns on Rousay mentioned above. A final type of megalithic tomb remains to be described. This contains a short passage with no differention between the passage and the chamber covered with a round mound that is usually revetted with a kerb of stones. In south-west Cornwall, the Scilly Isles and south-eastern Ireland there is a small group of these monuments which seem to belong to the early Bronze Age. Although we have a great deal of evidence of human remains being placed in megalithic tombs in a fragmentary condition, presumably after excarnation, as in the chambers on Rousay Island, we also find examples of complete bodies being laid in them accompanied by grave goods. Instances of such have been found in the courtyard cairn at Audleystown in Co. Down. This is perhaps the earliest evidence of a development originating in the late Neolithic that begins the practice of what we might describe as ?proper burial?. It is this variety of practice that makes it so difficult to provide a coherent picture of neolithic disposal of the dead. The best we can do is to say that a great deal of it revolved around the mortuary enclosure or the megalithic chamber and it involved the storage of body parts and the cult of veneration of the ancestors. Megalithic chambers were constructed with large stones that were not artificially pre-shaped. They were, in fact, selected so that they fitted their appointed position in the structure. Weighing many tons, the largest of them were probably not transported over a great distance but needed to be manhandled on the journey and then lifted into position, an operation that would have required considerable engineering expertise and a large number of people. This last is certainly true for constructing the passage grave mounds and for positioning the largest capstones. Our problem in understanding the proceedures that centres around this last point ? the large number of people that would have been required and our perception that the Neolithic population was small and scattered. It is unlikely that this specialised building knowledge was possessed by everybody at the time and this raises the possibility of the existence of specialist megalithic builders, people whose traditional activity was the handling of large stones. If such people existed they would have had to travel from one site to another to supervise constructions and this would have needed a system of communication between communities which may not have been as isolated as is sometimes supposed. This idea is given greater weight by the evidence of the distribution of various materials: stone artifacts and pottery. These are the materials that best survive from the period but we should remember that other things could have been circulated but they were organic and therefore perishable and have not survived in the ground to provide us with the evidence. As far as we know the stone used for making tools and weapons by earlier peoples was collected from the surface but in the Neolithic period for the first time mining or quarrying of stone is apparent. Technology had taken a significant step forward with the discovery of methods of obtaining materials from a considerable depth under the ground. This was a major advance. The first mining was for flint and the basic technology remained the same for thousand of years of mining for other materials like copper, salt, iron and coal. It involved digging a pit until the required seam of material was reached and then following it in various directions for as long as it was safe to do so before backfilling the pit and digging another close by to follow the seam further. Such pits are referred to as bell-pits, a reference to the shapes of their cross-sections. Best-quality flint is found in situ lying in discrete layers under the ground. Flint from outcrops that have been weathered on the surface is not as good for flint-working and it is clear that the difference in quality was enough to make it worth while going to the trouble of digging pits many metres deep. We first know of this activity on the Continent/. The Rijckholt mines in the Netherlands, some up to fifteen metres deep, probably produced in all over 153 million axeheads/. In England the practice started in the south, in Sussex at Findon and in Wiltshire at Easton Down, during the fourth millenium BCE (Russell). But the most extensive flint-mining area is at Grimes Graves in Norfolk with 350 shafts up to 18m deep. Here, the miners sank their shafts in the upper chalk, passing through two layers of flint, the topstone and the wallstone, to reach the desired floorstone that is found in the form of large tabular chunks of black, glossy flint. This industry dates from c2500 BCE and continued for several hundred years. It has been estimated that some 28 million flint axeheads were made from the flint mined there. Axeheads were the principal product and must have been distributed over a wide area. Work on identifying the places of origin of specific flints is still in its infancy but it will be a great step forward in our understanding of the processes of trade/exchange at the time when the method has been fully established and we can map the distribution pattern of the Grimes Graves products. Quarrying was confined to the highland regions of Britain and Ireland where specific kinds of rock are to be found. Like the flint from Grimes Graves, the stone was to be made into axeheads and needed to be tough and resilient. Also, it was to be polished to ape the gl;ossy flint so required to be fine-grained enough for this to be possible. Fortunately, petrology (the study of rocks) is far enough advanced now to allow experts to pin down these stone axeheads to their places of origin. There were a large number of axe quarry or axe-factory sites but the most productive was a site in Cornwall, precise location uncertain, where greenstone was quarried. The axeheads made from this rock are the most widely distributed in England, particularly in the south, with an overwhelming preponderance around Penzance. Another quarry is at Great Langdale in the Lake District where the only intensive exploration of such a site has been done. The rock here is a fine-grained andesitic ash, formed between 400 and 350 million years ago which produces arguably the finest of all axeheads which were distributed widely throughout Britain. Graig Llwyd, near Penmaenmawr, in North Wales, produces an igneous rock, formed by volcanic action. Not far away is Mynydd Rhiw in the Lleyn peninsula where another ash formed the rock that is very different from the Langdale material. In Northern Ireland two quarry sites have been identified. One is at Tievebulliagh in Co. Antrim and the other at Rathlin Island in the same county. The rock is black and flint-like and examples of axeheads made from it are found all over Ireland and even in Britain as far afield as Kent. Stone axeheads, like some of the flint axeheads, were polished, using, one supposes, fine sand, water and a leather and were then hafted in a hole in a wooden handle, perhaps using an antler sleeve between the stone and the handle to absorb some of the vibration. Complete examples of hafted axeheads have been discovered in both Ireland, in Co. Fermanagh and at Ehenside Tarn in the English Lake District. Axeheads can often be found in almost mint condition, showing very little signs of wear and some found in this country are made of a dark-green semi-precious stone known as jadeite. They were imported from the Continent. Such axeheads were presumably not employed for common tasks like chopping wood and may have been carried as status symbols or used in some sort of ritual. But others were clearly working tools as worn examples in settlements at Goodland and Lyles Hill in Antrim and at several other habitation sites in Ireland has shown. Because of the ability of the petrologist to identify sources of a number of these axeheads, it is possible to say something about their distribution in a way that is not yet possible with the flint examples. What is surprising is the distance that they could travel. The Tievebulliagh axeheads have been found not only in Kent but also in the London area, in north-eastern Scotland and in the Western Isles. In Ireland their distribution is densest in Ulster but the spread is as far south as Co. Cork. It is difficult to believe in organised trade in the Neolithic period. For one thing the quantity of goods concerned is too small to support such an idea and there is no evidence of markets or anything of that sort nor is it likely that there was such a demand for the products so that it was worthwhile trading directly with customers over a long distance. As there was no currency at this time goods were exchanged for other goods or services and one can visualise a local system whereby small quantities of artifacts were carried round by pedlars in the zone surrounding the production source and given to customers in exchange for s night's lodging, food, clothes or other necessities of life. This would account for the concentration of finds of Tievebulliagh axeheads around the axe quarry for example. When we look at the long distance distribution, we can remark that the numbers of artifacts are very small compared to the number in the production source zone and perhaps could have reached their find-spots by being passed on from hand to hand as gifts or tribute. Petrology, of course, can be useful in identifying stones that have been used for other artifacts apart from axeheads. Querns and millstones must be made of rocks with hard mineral contents and yet they must contain a limited proportion of softer grains or crystals that wear away to maintain a rough grinding surface. At the Iron Age hillfort of Danebury in Hampshire the millstones were made of a particular form of greensand that was traced to its actual quarry source in West Sussex. The aptly-named millstone grit of the Carboniferous rocks of the north Midlands and Yorkshire has provided grinding stone throughout the ages. A source much further away in the Rhineland of Germany, at Niedermendig, sent millstones to Britain from the Neolithic period onwards. This demonstrates the amount of trouble people took in selecting and obtaining the best materials at the time. The same care was taken with later materials. When metals came in, hones became very important for sharpening edged tools. Suitable stone for them was also carried over long distances. In medieval Yorkshire, a number of whetstones were found that had been quarried near Aberdeen. Petrological examination of metal slags can show what product was being made on the site and often what type of ore was being smelted. Jewellery too can be examined to suggest where the stones came from. Although petrology is a geological study, it is one that archaeologists have 'borrowed' as they have done with a number of other disciplines. In recent years a small number of defended or fortified sites have been discovered which belong to the Neolithic period. Three of the best-known are Carn Brae in Cornwall, Helman Tor in Devon and Crickley Hill in Gloucestershire. At Carn Brae a neolithic hut was found built up against a stone rampart and was associated with pottery, flints, pits and hearths. At Crickley Hill (Dixon) around 3500BCE over 1.6 hectares of the highest area of the hill were enclosed with a stone bank. Evidence of the use of antler picks was found in the shallow pits from which the stone was quarried immediately in front of the rampart. Around the inner edge of the half-metre high rampart a timber stockade was built. There appear to have been five entrances. Inside, neolithic flints and pottery were uncovered which suggested a settlement site. Later, a second bank dug from a deeper ditch and another palisade about thirty metres inside the first surrounded the same settlement. Four entrances in this new rampart matched four in the outer bank. They were framed in timber and apparently had wooden gates. Through the south-eastern entrance led a straight, fenced roadway with a rectangular wooden house standing beside it. These defences were demolished and rebuilt several times and also suffered from fire. It has been suggested that finds of arrowheads are evidence of attack. Round about 2,500BCE the last neolithic defences were built. There were three entrances with a low stone rampart and a rear palisade. One of the entrances opened onto a fenced road along which stood at least two wooden, rectangular houses. A path continuing the line of the road led to a fenced enclosure that has been interpreted as a shrine. This final neolithic settlement was apparently razed to the ground and burnt after an attack by bowmen, four hundred of whose arrowheads have been found embedded in the remains of the palisade and around the entrances. This ultimate disaster occurred some time before 2000BCE in the early Bronze Age. Neolithic leaf-shaped arrowheads occur in some numbers at other neolithic enclosure sites: at Carn Brea and Hambledon Hill in Dorset. These occurrences have been taken by archaeologists to demonstrate that serious clashes took place between rival groups at the time but we do not know whether this was tribal warfare or the result of disputes between neighbouring communities over grazing land or animals or similar local concerns. It is interesting to record that a dozen or more instances of death by leaf arrowheads have been recorded from various excavations where skeletons have been unearthed in sites of this period. The bow and arrow was clearly a seriously popular weapon, the earliest example of a bow coming from a Scottish peat-bog at Rotten Bottom dated by radio-carbon to 3040BCE. Apparently, large enclosures in the later Neolithic period were used for a variety of purposes, none of which we fully understand. There are ditched areas with no special characteristics as at Bury Hill in West Sussex which was discovered as a crop mark from the air, large rectangular areas at Dorchester in Dorset and very large timber-palisaded enclosures found and partially excavated at West Kennet near Avebury, at Hindwell, Powys, in Wales and Plasketlands in the Lake District. Like a great many neolithic monuments, these large enclosures remain an enigma. At West Kennet, its location in the special area where so many neolithic barrows and ritual features have been found may mean that it too had a ritual function. A type of monument that makes its first appearance in the Neolithic period is rock art or cup and-ring carving which is found on rocks in northern England, Scotland and Ireland. The symbols are pecked into a rock slab with a hammer-stone and are reminiscent of but by no means identical to the megalithic art on Irish tombs in the Boyne valley. Recent work has established that the earliest-known examples date from the Neolithic and the latest-known from the Early Bronze Age. A useful way of studying the rock art in Northumbria is with the web-site at http://rockart.nd.ac.uk **** ** <../../Templates/onlinetexts-index.htm>************ * Environment and Landscape ** <../cap.htm>* * * * main page <../onlinetexts-start.htm>* ** <../onlinetexts-start.htm>** * Cults and Rituals * * * *** ** *