The megalithic tombs of the Tramore group in County Waterford, south-eastern Ireland, are described and reconsidered. Three are confirmed as passage-tombs, but two are now identified as wedge-tombs. The passage-tombs have their best parallels not in Ireland, but in the Scilly Isles and Cornwall.

This paper attempts to resituate the Irish so-called ‘Royal’ sites within our vision of the Iron Age by challenging current understanding of their function as primarily situated in a ceremonial or ritual realm. While the evidence from these sites speaks to the complexity of their function, conceptualisation, and symbolic relevance, it is argued here that they are integral focal points of settled landscapes. Their architecture is suggested to address very specific concerns of the agrarian communities that built them and, in its very distinct change over the course of the Iron Age, to reflect broader societal developments, namely the emergence and decline of new society formations. Artefacts and ecofacts, architecture and landscape context of these sites contain a wealth of information on the activities that were taking place on and near them. It is argued that, freed from a binary ritual/profane interpretational framework, this evidence becomes readable as a record of Iron Age society and its dramatic changes over time.

FxJj43 is one of a series of Early Stone Age archaeological sites preserved in the Okote Member of the Koobi Fora Formation, in northern Kenya. It is the focus of a new research project that aims to explore the impact of time-averaging on the composition and characteristics of Early Stone Age archaeological assemblages. FxJj43 lends itself particularly well to this exercise because, unlike other sites in the Okote Member, it preserves a laterally extensive set of interlocking landforms. These include part of a sandy river channel, its southern bank, levee, and adjacent floodplain.

Chipped stone artefacts and broken-up animal bones occur in clusters of varying size and density all the way along the 200 m long strip of outcrops containing the remnants of these landforms. Small-scale excavations aimed at investigating the characteristics of archaeological assemblages preserved in different palaeotopographic settings, and in clusters of varying size and density, suggest the existence of archaeological occurrences representing different amounts of overprinting. This underscores the long-term research potential of this locality for exploring the relationship between the material remains of individual behavioural events and agglomerations of debris resulting from many, often unrelated sets of activities.

Since the studies of Vignard brought the micro-burin, the presence of which Siret had already noted at El Garcel, into fashion as an Upper Palaeolithic tool of unknown purpose, there has been much discussion of this tiny and enigmatic object.

I confess that I paid little attention to it when I visited the collection of M. Vignard in Paris 25 years ago. He showed me his micro-burins from the Sebilian and, after hearing my account of the finds at Parpalló, predicted that I should find examples among the flints from that site, which I was then in process of classifying. And, in fact, a few months later I found the first example, a very fine and characteristic one, in the third Magdalenian level. Other examples followed from similar levels, and later, when we were classifying the flint from the Solutrean levels, we discovered to our surprise that they were also present there. Since then they have continued to appear on other sites, so that it seems worth while to summarize here the data which we now possess about them.

Let us look at the situation in the deposits which I have studied.

In the cave of Parpalló they are found in appreciable numbers at two points in the typological evolution. From a depth of 5.25 m. upwards, that is during the phases which I have named Upper Solutrean and final Solutreo-gravettian, they are relatively abundant (about 50 examples).

The English Midlands (fig. 1) as a natural region, and for the purposes of environmental archaeology, form a more restricted area than that to which the term is usually applied in modern geography. Fox (1943, 68) has written of ‘… the great triangle of forest lands which form the Midlands …’ and reference to the maps in the same work shows this triangle as roughly lying between the Dee estuary at Chester, the confluence of the Severn and the Avon at Tewkesbury, and a point in the vicinity of the watershed between the Trent and the rivers of the Wash. For convenience of reference it is suggested that the approximate eastern point should be represented by the site of Belvoir Castle for here the plain has narrowed between the southern tip of the Pennines, and the uplands of Leicestershire, to the effective basin of the Trent. This river in its course below Nottingham flows through ancient forest lands, but it is no longer Midland country.

The most uniform frontier of the Midlands, as here defined, is that provided to the south and east by the great sweep of the Jurassic uplands from the Cotswolds to Lincoln Edge. To the west, the Severn and the hill country of the Welsh borderlands form a zone which provides natural communications north and south and into the Welsh massif, but which, as it were, turns its back to the east. The northern confines of the Midlands are altogether less definite, but may be said to creep round the edges of the southern Pennines from the south bank of the Mersey to the middle course of the Trent.

In March 1949, work was carried out at The Bull Ring, Dove Holes, Derbyshire, by members of the Oxford University Archaeological Society, as part of the general survey of ‘henge“ monuments, undertaken by Mr R. J. C. Atkinson. The site was surveyed and was found to be of the ‘double-entrance’ class of Henge Monument. No stone-holes were found, but it is known from an 18th century account that the monument once had a stone setting similar to that at Arbor Low, Derbyshire. Trenches revealed the form of the ditch and bank, but the dating evidence was confined to two fragments of pottery, one of them a rim sherd, probably related to Beaker fabric.

This article presents the evidence for the distribution of Late Minoan stone vases outside Crete. This class of evidence has not been discussed previously and as the amount of material involved is substantial, over a hundred vases, it is here set out as a contribution to the discussion of Minoan foreign connexions in the earlier part of the Late Bronze Age in the Aegean.

The vases were made in Crete in Middle Minoan III/Late Minoan I—Late Minoan III A 1, c. 1600–1400 B.C., as is shown by the contexts of parallel vases from sites in the island (see the Catalogue). Most of the exports occur in Aegean contexts of this period; for those from contexts later than c. 1400 B.C. it is most reasonable to believe that they too were exported from Crete at the time of their floruit, containing in use for a time afterwards. In any case most of them are fragments, which indicates that their time of arrival and period of use were earlier than the late date of their contexts. Moreover after c. 1400 B.C. Cretan influence abroad ceased (Desborough 1964, 166–7; cf. Furumark 1950, 263–4 for the end of Minoan contacts with Trianda and Phylakopi), nor is there evidence that stone vases were then made in the island.

The authors of these notes acknowledge the ready collaboration of the numerous excavators who have contributed information or notes concerning work carried out during the present year.

I have chosen for the subject of my address a description of the excavations carried out at Grime's Graves by Mr. A. Leslie Armstrong and myself in the autumn of 1915. The work consisted in the digging over of four new floors, a description of which will form the main part of my paper. We also re-examined the mass of material left on three of the older floors excavated in 1914, viz., 3, 4, and 13, and devoted some time to searching the field which lies to the west of the plantation, which, in spite of many years' examination, still yields quantities of new implements. I have included, too, a description of some of the implements from a zone near Botany Bay, from which, in 1914, I obtained a number of pieces. This station lies about a mile on the Brandon side of the plantation, and is probably the ploughed-over site of some pits of similar date.

Owing to the kindness of some members of the Society, viz., Messrs. W. G. Clarke, H. H. Halls, R. H. Chandler, and the Rev. H. G. O. Kendall, I have been able to figure and describe a number of fine implements which clearly belong to the same culture—found either on the field or on the surface of the Graves, and these, together with various specimens found on these spots by Mr. Armstrong and myself, are dealt with separately.

In the present state of our knowledge of the Neolithic period in England, and especially as regards its pottery, any light that can be thrown upon it is welcome, and it is on that account that I have brought before the Society a report on two discoveries of Neolithic remains: at Pangbourne, Berks., and Caversham, Oxon.

It is greatly to be regretted that owing to the circumstances of the discovery accurate observations could not be made. In May, 1928, workmen were engaged in levelling ground to make a tennis court, at “Farmhili,” Courtlands Hill, Pangbourne, and in doing so came upon, and, as is unhappily so often the case, disturbed and partly smashed a human skeleton, other animal bones, of which a few only survive, and a large bowl of coarse pottery, definitely of Neolithic type. It would seem that when found the bowl was imore or less complete, but Mr. G. W. Smith, of Reading, who visited the spot the day after the discovery, was only able to find about two-thirds of the vessel, in fragments, on the rubbish heaps of excavated material. These fragments, together with the other remains, were presented by the owner of the land, Lt.-Com. W. S. Macilwaine, R.N., to the Reading Museum, where the writer had the opportunity of examining them.

In remote times bleak and exposed sites in the east of the county of Durham were occupied by folk who made microlithic implements. On the top of Sheddon's Hill, near the Black Fell, Gateshead, these relics were fairly abundant among hundreds of pieces of flint collected; and examples have been found elsewhere in the district and on the coast.

Many of the Belgian Tardenois types are represented among these finds, the small trapezoid which has not yet been excavated on Sheddon's Hill was found on a site near by and a small round scraper on a coast site. The finding of these remains on Sheddon's Hill adds something to our information about the distribution of the Tardenois folk in Britain who probably as Capt. Buckley has suggested spread westwards from the Continent at a time when the North Sea did not exist.

In this paper I shall endeavour to outline the progress which has been made recently in archaeological studies in the prehistoric periods in Wales. In the last number of the Proceedings (1931, 383–4), I contributed at the request of the Secretary a number of notes on this subject, taking as my starting point the publication of Dr. R. E. M. Wheeler's book, Prehistoric and Roman Wales, in 1925. In the present instance I propose to give a more detailed, as well as a more general account, demonstrating how recent research and discoveries have advanced our knowledge, clarifying the position in relation both to Wales herself and to the connexions of Wales with other external influences.

The publication of Prehistoric and Roman Wales in 1925 may truly be said to mark the end of one era and the beginning of a new. Drawing together the scattered threads of what had been done before, Wheeler has given them meaning and set forth the results of many years of unorganised, frequently ill-considered, work in tangible form. In so doing, he has exposed the gaps in our knowledge and suggested, specifically or by implication, a policy in the form of a series of problems the elucidation of which will lead ultimately to a more complete picture of the early cultures of Wales, and hence of Britain as a whole. Wheeler's survey therefore forms a natural and admirable jumping-off place, and the subject will be treated in the following pages in its natural chronological sequence.

During the great drought in 1929 there came to light at Gouthwaite Reservoir in Nidderdale three sites of Upper Palaeolithic industry. In that summer the level of the water became so low that the reservoir was less than half full, thus affording an opportunity for field work. The Pleistocene deposit exposed consists of a stiff yellow clay covered with sand and gravel along the banks of the reservoir, washed out by the action of the water in rough weather, from the lateral moraines. This clay is exposed in many places when the water has fallen 4 ft. below ordinary level, and it is on this horizon that Upper Palaeolithic man apparently lived. A complete geological section across the valley in this part does not exist, but sections of trial holes were made when the construction of the dam at Gouthwaite was being undertaken and for the copies of these sections I am indebted to Mr. E. Tillotson of Leeds University. The dam is actually built at the upper end of the last, and best preserved, terminal moraine in the valley. From the section it appears that the yellow clay stretches right across the valley, forming the uppermost stratum of the terminal moraine. This being so, and if this was the horizon on which the inhabitants lived, then the terminal moraine must have been cut through by the river action, otherwise the horizon on which the Upper Palaeolithic implements are found would have been under water and not habitable.

In the following study, the region dealt with is bounded on the north by the Thames, and on the west by the Avebury and Stonehenge areas. It consists therefore of Wiltshire, Hampshire, Berkshire, Surrey, Sussex and Kent, and a small portion of Dorset. The area contains about five thousand barrows, or ancient burial-mounds, about seven-eighths of which I have seen; it is believed therefore that the following details are fairly complete.

Not only is Grimes' Graves an essentially East Anglian site, but it is also one of the most interesting, and most perplexing, prehistoric sites of Britain, presenting many controversial problems which only persistent research and careful observation will solve.

Recent work upon the site has marked a distinct advance in this direction, notably by the fortunate discovery in 1920 of Floor 85 with its definite stratification, and evidences of successive occupation during at least five widely separated intervals of time. With Dr. R. V. Favell as a co-worker, excavations were resumed upon this floor in August, 1921, and continued for six days. An additional 40 square yards was carefully and systematically explored down to the level of the boulder clay, resulting in the recovery of a further series of important flint implements and examples of engraving. Owing to the favourable nature of the site with its stratified chipping and occupation levels, each sealed and separated by sterile layers of humus, and closely compacted chalk debris, it has thrown important light upon some of the problems of the Grimes' Graves industry, and should enable not only certain definite conclusions to be arrived at, but materially assist in the ultimate classification of the various cultural forms of the implements from the Graves generally.

The pygmy and small implements shown to-night from Cornwall were found on the landward slope of Trevose Head, near Padstow, on the north coast of the county. The sea end of this promontory rises to some 200 feet, and thence the ground inclines rapidly back to the mainland, the connecting neck being not more than half a mile wide. At the narrowest part the rain-water, constantly filtering through the adjacent peat, wastes down the hard bedrock of slate, comes out as a small spring, which, in the course of ages, has cut a channel of a hundred yards in length to the cliff edge. At the springhead stands a cairn of a massive block of white quartz, obviously of great age, but whether coeval with the prehistoric settlpment it would be impossible to say. This cairn or beacon would be seen from a long way over the adjacent bay, and might have served to guide seafarers of any age to the fresh-water supply. Here, amongst the faint traces of trenching and hut circles, the small implements, and chips made in their manufacture, all of snow-white patina, were lying about in great profusion.