The Oriental origin of the wheeled vehicle has long been recognized. It seems to have originated in Sumer, in the Uruk period, in the first half of the fourth millennium B.C.

A rich collection of material, including isolated wheels and other remains of wheeled vehicles, models and pictures representing vehicles, show that wagons and carts had spread to Italy, Eastern and Central Europe, and the south Scandinavian countries by the middle of the second millennium B.C. Although the presence of wheeled vehicles has been claimed in Spain as early as the ‘copper age’ the first datable evidence for them is given there by the Solana de Cabanas stele and other west Spanish stelae that probably belong to the end of the second and the first millennium B.C.

The data for this paper were obtained in the course of a journey round Scandinavia made during the summer of 1947 with the aid of a Leverhulme Research Grant. Most of the evidence is housed in the Tromsö Museum, the Statens Historiska Museum, Stockholm, and the National Museum at Helsingfors, and I am thankful to the authorities of these for ready access to their great collections and for help in many ways. A certain amount of the material from the northern provinces of Norway is contained in the Universitetets Oldsaksamling at Oslo and, since at the time of my visit the stone age collection was still in store from the war, I was not able to examine it in detail and have relied upon the works of Nicolaissen and Gjessing, supplemented by information obtained by correspondence. In the case of the material housed in the small but important collections at Umeå and Skellefteå, which I was unable to visit, I have relied upon articles by Dr Gustaf Hallström, whose knowledge of Norrland antiquities is unrivalled. While it is certain that a number of finds have escaped me, the evidence summarised in the Appendix can at least be taken as a minimum statement of what has already been discovered in territories, which owing to their remoteness, vast size—Norrland contains approximately four-sevenths of the whole of Sweden—and scanty population are still, so far as the Swedish and Finnish regions are concerned, comparatively unexplored archaeologically, when judged by the standards prevailing in other parts of Scandinavia.

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.

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.

In approaching the subject of the patination of flint implements, I am profoundly impressed with the very great difficulties of the subject; so much so indeed that I feel that some initial apology is called for. It requires some courage, nay, one may say temerity, to attack a series of problems that bristle with difficulties of a most formidable kind, about which nothing is known; and for a solution of which chemical and physical knowledge of a very high order, backed up by the aid of full laboratory equipment, is required. All this is wanting in my own case; but on the other hand I have a large first-hand acquaintance with the flints in question; for many years I have devoted much attention to the conditions in which patination is found, jand to its manifold varieties—it has been my constant endeavour to co-ordinate given patinations with other factors more or less ascertainable in connection with the flints. In this way I think I have arrived at conclusions which, though by ao means complete in themselves, may at any rate serve as points of departure or of support in the further investigations which are urgently required. I propose to divide my paper into three sections—(1) General considerations bearing on the study of patina, (2) The conditions under which patina is produced, (3) The changes in flint associated with the production of patina.

The type of flint implement which we are investigating here was first distinguished by the late Sir John Evans in his Ancient Stone Implements of Great Britain as long ago as 1872. Out of a total of 52 specimens noted in this paper, 12 were mentioned by Evans in his 2nd edition, 12 have been published elsewhere, and 28 are here recorded for the first time. Outlines of 50 and a photograph of another are given in Figs. 1-3,7 and 8.

They consist of long narrow blades carefully flaked over both faces, which are of roughly equal convexity, to produce two cutting edges. In plan the tip and the butt are usually defined by the more tapering character of the former, while the general outline is asymmetric. The type as thus defined is quite distinct from any other, though it differs only by its asymmetry from certain leaf-shaped blades flaked over both faces. There is, however, a further characteristic, namely a varying extent and degree of concavity of one cutting edge, which further defines our type and marks it off still more from other flint forms. We mention in this paper two examples showing asymmetry of form (Nos. 28 and 29), but lacking any degree of concavity in either cutting-edge, as they may be related to the true sickle form.

In giving an account of the humanly-fashioned flints found during the excavations at High Lodge, it is proposed to deal with those discovered in exposing section A, and to proceed to describe the specimens recovered in the other diggings, which will be dealt with in their alphabetical order.

Section A. A small twisted, ovate palæolithic implement, flatter on one face than on the other, and referable, it seems, to Late Acheulean times, was found associated with the thin seam of gravel occurring under the turf at section A. This specimen, which exhibits only small signs of abrasion, is of a yellowish colour, except where areas of hardness in the flint have resisted the agent of discolouration. These areas are either of a dark coffee shade, or coloured a light brown. The specimen measures in greatest length ins.; in greatest width 2 ins.; and greatest thickness ins.

The excavations which, with the flint implements and other relics discovered, it is the purpose of this paper to describe, commenced towards the end of February, 1919, and continued until July, 1920. The money to pay for the wages of the excavator, Baxter, was most generously supplied by the Trustees of the Percy Sladen Memorial Fund, and I wish to record my thanks for their invaluable help.

I have to acknowledge also, with gratitude the assistance given me in my researches by Sir Ray Lankester, K.C.B., F.R.S., Sir Arthur Keith, F.R.S., Mr. W. Whitaker, F.R.S., Professor J. E. Marr, F.R.S., Dr. Smith Woodard, F.R.S., Dr. Charles Andrews, F.R.S., Mr. Reginald Smith, and the owners of the various properties upon which the diggings were conducted.

The drawings which illustrate this paper are reproduced from work executed by Mr. E. T. Lingwood, to whom the science of prehistoric archæology is greatly indebted for his continued and invaluable help in the matter of illustrations.

I am exhibiting a number of flakes and implements, which appear to be of Le Moustier date, from Acton on the Taplow Terrace, and West Drayton and Iver on the Boyn Hill Terrace.

The Acton specimens are from the immediate vicinity of the working floor discovered by the late Mr. Allen Brown some forty years ago. During recent excavations in Creffield Road, I picked out of the brick-earth, thrown up from a depth of 4 to 6½ feet, seventy humanly struck flints. Forty-six are unpatinated, fresh-looking and unabraded, twenty have a bluey-white patination, amongst which are several with slightly dulled edges, and four are light-ochreous. The freshness of the cortex on several of the unpatinated flints suggests that some of the raw material was derived directly from the chalk. The majority are simple flakes and spalls. The remainder consists of eighteen small Levallois flakes, varying in size from 2 by 1½ to 3½ by 2¼ inches, one small tortoise core, a small flattish core with flaking on one face at right angles to that on the other, a flint pebble which has been used as a hammerstone, one small point and two exceptional pieces. One of these is a fairly typical graver (bee de flûte) with bluey-white patination (Fig. 1); the other may be described as a busked graver, it is made from a thickish external flake and is unpatinated (Fig. 2). A few of the flakes shew slight signs of use.

Hackpen Hill, 888-ft., is the highest ridge of the Marlborough Downs properly so called, and has already been described in my paper on the Palæoliths found on its summit. The southern hills, overlooking the Pewsey Valley, rise to 965-ft. The top of the hill, hough narrow, is flat, and bears pockets of Tertiary remains, the ub-soil being of a clayey nature almost throughout.

Until recently, five large fields were tilled, and seventeen years ago a sixth was still under the plough. The space covered by these was 1½ miles in length; and on an average, about ⅓ mile in width, two of the fields stretching a little way down the dip slope of the hill.

It is admitted by all workers in prehistory that the human implements which are found upon the surface do not all belong to the Neolithic period, although, until recently, they have always been called Neolithic. It therefore seems better to define them clearly as a Surface Series, without prejudice to their date.

Beyond this point of general agreement, differences of opinion are strongly marked. Some workers would boldly place the majority of the Surface Series in the Later Palæolithic period, or “Cave Age,” while others are unable to accept this view.

It must be admitted that we have very little knowledge of remains belonging to a strictly-defined Neolithic period. We know that “Neolithic” implements continued to be extensively used during the Early Bronze Age, and even in later times.

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.

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).

This report describes a group of distinctive earthworks in the north-east of the North York Moors (fig. 1) that, prior to investigation by the RCHME, had been categorised as double pit-alignments. The earthworks consist of two or three pairs of pits, with the spoil from the pits spread into parallel enclosing banks. The orientation of the segments is fairly consistent along an axis north-west to south-east; in each case there seems to be a tangential alignment on burial mounds, putatively Bronze Age in date, which may give a clue as to their age and function.

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.

Perforated plates of fired clay have long been recognised as a component of Late Bronze Age material culture in south-eastern England, but recent developer-funded excavations have produced a wealth of new evidence. These artefacts, showing a considerable degree of standardisation, are now known from more than 70 sites, which show a markedly riverine and estuarine distribution along the lower Thames. Their function is still uncertain, but it is suggested that they were parts of ovens for baking bread, a new technology for food preparation in the later Bronze Age. Some of the largest assemblages of such plates are found at strongly defended sites, and it is further suggested that the baking and consumption of bread was particularly associated with such sites of social authority. The estuarine distribution is discussed in this paper, and it presents further evidence for the regionally distinctive nature of food consumption in later prehistory.