bluuebunny/crossref_metadata_2025_split huggingface dataset:
The Mesvinian Industry of Clacton-on-Sea, Essex
Authors: Warren S. Hazzledine 
Published: October 2013

The flint flakes from the Elephas antiquus bed of Clacton-on-Sea have been known for many years, and were collected by the Rev. J. W. Kenworthy. I obtained a large series between the years 1911 and 1916, but their affinities remained an enigma to me until they were examined by the Abbé N. Breuil, who denned them as Mesvinian. When once it had been suggested, one realized that this determination was obviously correct, and it has since been confirmed by several continental authorities who are intimately acquainted with the Mesvinian of Belgium.Stratigraphy. Remnants of the High Terrace with Chellian implements occur in the district (at Frinton, Weeley, etc.) at levels of 70 to 85 feet O.D. These contain much Lower Greensand chert from the Wealden area, and I think they must be referred to the main river of the Thames basin.The Clacton bed is the silting-up of a tributary channel which cuts across the High Terrace, and of which the base lies below the present level of low tide.
The Discovery of an Early Palæolithic Implement in Yorkshire
Authors: Collins E. R. , Moir J. Reid 
Published: October 2013

The writer of this article was lucky enough to find last August a large ovate implement of the Early Palæolithic period in Yorkshire, after many years of careful searching; he is indebted to Mr. E. T. Lingwood for the drawings of the same, for which help he offers his grateful thanks.The site of this find is Upper Nidderdale, just within the boundary of the West Riding. At the far end of the dale, and some six and a half miles from its source, the river Nidd, which up to this point has run due East, makes a bend, practically a. right angle, to the South.Some three hundred yards below this point an interesting geological phenomenon occurs in the shape of a triangular fault with its apex to the South, which has thrust up the Carboniferous Limestone on both sides of the valley.Through this the river, with the help of the glaciers, has cut its way.This strip of limestone is about half a mile long and below this the river continues its course for some distance through the Millstone Grit series, Nidderdale being, from a geological point of view, a Millstone Grit dale.
Eoliths found “in situ” at South Ash, Kent
Authors: Crawshay de Barri 
Published: October 2013

This Paper is the outcome of a very long standing hope of proving the existence of “Eoliths” “in situ,” under the surface position where in 1866, Benjamin Harrison first found what he thought must be the very rude earliest forms of humanly worked flints, which in the “nineties” became known as “Eoliths.”He felt pretty sure of his own opinion but no one to whom he showed his finds was at that time bold enough to accept them; this discouraged but did not deter him; for though he put them away to “Suspense Account.” he always had them in his mind and at all opportunities tried to advance his belief and convert others for many years with but very little success indeed; till 1884 when Mr. H. Walker agreed with him that they were human artefacts. In April, 1887, I became acquainted with Harrison; he lectured particularly on the “Rudes” doubtless hoping to find a tyro whom he hoped to educate to be a supporter.He took me to South Ash and his other “Red Spreads” on which we found many specimens.
Percy Sladen Memorial Fund Excavations. Grimes' Graves, Norfolk, 1924
Authors: Armstrong A. Leslie 
Published: October 2013

The excavations described in the Preliminary Report were, through the generosity of the Trustees of the Percy Sladen Memorial Fund, and with the co-operation of Dr. R. V. Favell, resumed in 1924 and further efforts made to discover evidence of the earliest mining activities at Grimes' Graves. Summarised briefly the work of 1923 had already established the following facts:—(1) The existence on the southern slope of the valley, north of the Graves, of primitive flint mines roughly circular in shape and sunk to the Floor-stone, at that point 12 feet 6 inches deep.(2) That the two pits examined were devoid of galleries, the shafts being belled out at the base to obtain as much flint as possible.(3) That Hand Picks of a form not hitherto recognised and formed of the long bones of animals, had been used for excavation purposes assisted by wedges and choppers of flint.(4) That Deer-antler picks, or fragments of deer antler were entirely absent.(5) That access had been gained to the pits by rude staircases cut in the shaft walls.(6) The nature of the valley deposits was established by a series of sections and the almost complete erosion there of the Floor-stone, by glacial agencies, proved.(7) The limits within which Floor-stone exists in situ on the south side of the valley was defined and an outcrop of contorted Floor-stone discovered.
Further Excavations upon the Engraving Floor (Floor 85), Grimes' Graves
Authors: Armstrong A. Leslie 
Published: October 2013

Further excavations on Floor 85, at the end of July, 1922, increased the total area of this important floor, carefully dug over and examined, to 109 square yards. Previous observations have been confirmed and a further series of implements recovered, including engraved pieces of flint crust and pieces bearing incised lines, similar in character, though of minor importance, to those described in the “Proceedings,” Vol. 3, p. 434 and 548.Dr. R. V. Favell again co-operated and the work was principally concentrated upon the S., SE., and E. sides of the previous excavation.Upon the S. side Floor A was absent, Floors B and C well marked, though Floor C proved to be thin in places and towards the termination of the dig showed signs of giving out, whereas Floor B was becoming thicker. The sterile layer separating B from C, latterly became so thin that the B floor in places was resting immediately upon the red sand layer and almost indistinguishable from Floor C, except by the most careful observation.
Some Archæological Problems
Authors: Moir J. Reid 
Published: October 2013

The object of this paper is to draw attention to certain archæological problems which, at the present time, have an important bearing upon the study of prehistoric man in England.Most archæologists are familiar with the pieces of tabular flint exhibiting human flaking, of a rough and primitive kind, along one or other of their edges, which Benjamin Harrison found, many years ago, in and upon the highest portions of the plateau of Kent. It is my purpose in this note, to discuss the geological, and cultural age of these specimens, and to endeavour to show that they represent the most ancient as well as the most primitive flint implements yet discovered.Though there is very good reason to suppose that the eoliths of the Kent Plateau (the term “eolith” should be confined solely to these specimens, and to those of the same type found elsewhere), as is the case with others found in similar situations in different parts of the country, are of a great antiquity, it is nevertheless clear that, having not yet been discovered at these places, under any geologically datable deposit, the exact measure of that antiquity remains unknown.
A Late Celtic Burial and a Series of Early Iron Age Occupation Sites at Waddon, Croydon, Surrey
Authors: Row Prescott 
Published: October 2013

The old manor of Waddon is part of the Parish of Croydon and lies to the south west of the Parish Church of that town. Here at the head of the Wandle River there are many evidences of a wide spread population in prehistoric times and the fields on the lower slopes of the North Downs which steadily rise from Waddon Station towards Purley are littered with flakes and have yielded many implements.The particular site to which I draw the attention of the Society, and indicate as the Cedars Estate, is easily reached by the bridle path running westward by Waddon Mill on the banks of the river, and the section under discussion, is the north east corner of the plot marked as Brandy Bottle Hill on the six inch Ordnance Survey. A hillock of Thanet sand here rises and extends eastward over the next field, the top of which is some 140 feet above sea level and makes a vantage spot with a good look out, over the wide stretches of the level plain running north from the present course of the Wandle river, in early times no doubt a stretch of marshland. It is still called Waddon Marsh.
A Hand-axe from beneath the Norwich Crag
Authors: Moir J. Reid 
Published: October 2013

In his important Presidential Address, dealing, principally, with the diggings he carried out beneath the Norwich Crag, Mr. J. E. Sainty drew attention to a remarkable flint implement (Fig. 2 of the above-mentioned paper) which was found by Mr. T. F. Newnam in the well-known pit at Whitlingham, near Norwich. After haying shewn that the specimen was derived from the pre-Crag Stone Bed, Mr. Sainty gave a careful and accurate description of this implement, and concluded by stating, “It is altogether a very convincing and highly important specimen from the point of view of dating the industry which it represents.”There are, I imagine, few archæologists who, having examined this implement, would disagree with Mr. Sainty's opinion. The specimen is, in fact, of such great significance that it was considered desirable to have it illustrated in four views, and this has now been successfully accomplished by Mr. C. O. Waterhouse, of the British Museum. Mr. Sainty has been so good as to ask me to undertake the task of further describing, and of commenting upon, this implement, and I am indebted to the Curator of the Castle Museum, Norwich, where the flint is now preserved, for loaning it to me for examination. If attention is now directed to Figs. 1, 2, 3 and 4, it will be at once realised that the specimen found by Mr. Newnam is a coarsely-flaked and massive (it weighs 2¼ lbs.) hand-axe. A further examination will show that the flaking which has shaped the implement has been produced by heavy, though skilful blows delivered by a hammerstone of considerable size and weight. It is clear, also, that the specimen was formed by means of what is known as ‘free’ flaking, in which the side from which the flakes are to be removed is not supported by pressure of the hand, or some other object. The result of the application of the above described technique is the removal of flakes inclined to be thick, and showing prominent bulbs of percussion, and of greater breadth than length.
Upper and Lower Palaeolithic Man in East Yorkshire
Authors: Burchell J. P. T. 
Published: October 2013

The most complete section of the glacial series of deposits described and illustrated in Lamplugh's classic paper entitled “On the drifts of Flamborough Head” is that which is located at Danes' Dyke.Referring to this section Lamplugh says:—“I have spent much time in exploring this section, and consider that the beds up to this horizon represent the Basement Clay, while the persistent upper band of brown Boulder-clay (3) is all that remains of the upper Clay of Sewerby, this bed and the underlying sand and gravel (3b) together taking the place of the Purple Clays of Bridlington and Holderness. Above this clay lie the Sewerby Gravels (2b), the lower part chalkless and the upper layers composed chiefly of chalk-pebbles, as noticed farther west. A few feet of loamy stuff overlies these gravels at the cliff top (2c), resembling a weathered Boulder-clay, and a little farther east (near Hartindale Gutter) a seam of Boulder-clay certainly appears in these gravels, their contemporaneity with the uppermost part of the Boulder-clay, and consequently their Glacial age, being thus fully established.”
Further Discoveries of Flint Implements in the Brown Boulder Clay of North-West Norfolk
Authors: Moir J. Reid 
Published: October 2013

Since my original paper on the flint implements found in the Brown Boulder Clay of north-west Norfolk, I have continued my researches in that region, and now wish to give some account of these, and of the further specimens which have been discovered in this most recent boulder clay of East Anglia. I would take this opportunity of thanking the Trustees of the Percy Sladen Fund for their kindness in supporting this research with a money grant, and so enabling me to continue my examination of an era of much interest and importance to prehistoric archæology. I am also very grateful to my friends, Mr. J. B. Calkin, Mr. Guy Maynard, and Mr. J. S. Fisher, for the valuable help they have given me in carrying out the investigation of the Brown Boulder Clay.As is now widely known, this deposit, so far as Norfolk is concerned, is confined to the north-western portion of that county, and many years ago was examined and reported upon by the Geological Survey in two of their memoırs. The Brown Boulder Clay occurs approximately at sea-level at Hunstanton, while at Brancaster, as reported by Mr. Clement Reid, the deposit is exposed at low water upon the foreshore, underlying the ‘submerged forest’ which he saw there. At other places, such as Holkham brickfield, and the remarkable formation (probably a terminal moraine) in Hunstanton Park, the boulder clay rests at about 50 ft, above O.D.
Tumulus on Massingham Heath Excavated August 27th, 1931
Authors: Watson A. Q. 
Published: October 2013

This tumulus was first noticed by Mr. Sainty and myself in April, 1931, whilst on an expedition in search of implements of Cissbury type, of which we had found a considerable number in this locality. In appearance it did not seem to differ very much from the numerous mounds left bv warreners digging for rabbits, and, in fact, we had examined several such mounds showing almost the same elevation above the surrounding heath; but as this contained no rabbit workings and such parts as were not covered by gorse showed a thick covering of turf, it appeared interesting, and we marked it down for further examination at the next possible opportunity.We were not able to visit the spot again till August 27th, when after a short time spent in searching for implements in the neighbouring field, we commenced digging, removing turf about five inches thick and opening a narrow trench. It was not long before we came across flakes, and threw out some 15 or 20, all showing signs of human workmanship, some with facetted bulbs of percussion, and finally a good chopper of Cissbury type.As similar flakes had been found by us in the side of an old stone pit about 120 yards distant, we were very doubtful if it could be a tumulus after all, but decided to settle the matter by excavating till undisturbed earth was reached. At a depth of about three feet a tiny fragment of charcoal was turned up, so we at once enlarged the trench to allow for more careful working.
Preliminary Notice: Types of Clactonian Implements at Swanscombe
Authors: Chandler R. H. 
Published: October 2013

Since my paper on the Clactonian Industry at Swanscombe was read in 1929, I have obtained many more implements from Barnfield Pit (the one there described) and also a large collection from Rickson's Farm Pit.The lower gravel at Rickson's Farm Pit has yielded the same culture as the lower gravel in Barnneld Pit, and it underlies a shell-bed containing I heodoxus cantianus (Ken. and B. B. Wood.), which is succeeded by a gravel containing well finished St. Acheul hand-axes in both places. The Acheulian tools from Rickson's Farm Pit differ somewhat from those obtained in Barnfield Pit in that there are fewer of the pear-shaped, pointed implements. The usual type in the former pit is thinner, more ovate, and frequently with a pronounced ‘twist’ of the reversed S kind.
The Evolution and Distribution of the Hand-Axe in North-East Ireland
Authors: Burchell J. P. T. , Moir J. Reid 
Published: October 2013

It has long been recognised that the post-glacial (25-ft.) raised-beach of north-east Ireland contains, in addition to flint implements of Early Neolithic age and aspect, artefacts of Lower Palaeolithic forms. The presence of these early types within this beach may be accounted for as:—1. A recrudescence of earlier forms during Early Neolithic times;2. Lower Palaeolithic artefacts which have been derived from the glacial and inter-glacial drifts of the locality:3. A mixture embraced by categories 1 and 2.The evidence for the determination of this question must be sought outside the beach itself owing to the masking of the surface variations of the specimens through the deposition of a creamy-white patination and through marine attrition, though, regarding the latter, it should be mentioned that glacial striae have been observed upon certain of the implements recovered from the post-glacial (25-ft.) raised-beach at Kilroot.
The Presidential Address for 1933: The distribution of Man in East Anglia, c. 2300 B.C.—50 A.D. A Contribution to the Prehistory of the Region
Authors: Fox Cyril 
Published: October 2013

I desire first of all to express my appreciation of the honour you have done me in electing me President of the Society. Faced with the necessity of choosing a subject suitable for a Presidential Address, it occurred to me that a brief survey of the distribution of Man in East Anglia during the Neolithic, Bronze and Early Iron Ages might be appropriate. Selection of the region wherein the Society was born, and which inspired the fruitful work of its founders and their successors, is intended as a tribute of gratitude from one who has profited by the study of the many important Papers published in its Proceedings.The general principles, recognized as governing Man's distribution under uncivilized or semi-civilized conditions in Britain, may first be summarized.In the Lowland area to which East Anglia belongs soil is the chief determinant. There are two main types of soil: pervious, such as that overlying chalk, sand, gravel; impervious, as that overlying clay. The pervious soils induce an open type of country, or carry forest with relatively thin undergrowth; the rapidity with which such soils dry up after rain, the ease with which a scratch agriculture can be practised on them, their suitability for pastoral life, the ease of movement on them—all these factors render them attractive to early Man. As a group they form the Area of Primary Settlement. The impervious clay soils, on the other hand, carry forest with dense undergrowth, are difficult to clear, and when cleared difficult to cultivate with primitive tools. To the physical unsuitability of such soils for settlement there is added a second deterrent; water-laden soils under the conditions of savage life produce disease in man and beast. But when cultivation of such soils is possible they are found to yield the heaviest crops to tillage, being especially good for corn-growing. They are, then, utilized when civilization reaches a certain level, and have accordingly been grouped as the Area of Secondary Settlement.
Cardiac diagnoses, procedures, and healthcare utilisation in inpatients with Ellis–van Creveld syndrome
Authors: O’Connor Matthew J. , Tang Xinyu , Collins R. Thomas 
Published: October 2013

AbstractIntroductionEllis–van Creveld syndrome is a rare condition associated with a very high incidence of congenital malformations of the heart. Prior reports have suggested increased morbidity and mortality following surgery for congenital malformations of the heart in patients with Ellis–van Creveld syndrome.Materials and methodsThe Pediatric Health Information System database, an administrative database containing data from 43 free-standing paediatric hospitals in North America, was queried to search for patients with the diagnostic code for Ellis–van Creveld syndrome between 2004 and 2011. Those patients who underwent cardiac procedures were compared with those who did not with respect to measures of healthcare utilisation.ResultsA total of 138 admissions occurred in 93 patients with Ellis–van Creveld syndrome during the study period. Of these, 74% had an underlying diagnosis of congenital malformations of the heart. Half of the patients in the sample underwent a cardiac surgical or interventional catheterisation procedure. Patients who underwent a cardiac procedure had a longer hospital length of stay, higher incidence of intensive care unit admission, and higher total and per day hospital charges than patients who did not undergo cardiac surgery during admission.ConclusionsIn a large group of inpatients with Ellis–van Creveld syndrome, the prevalence of congenital malformations of the heart was similar to that reported in prior studies. Cardiac surgical and interventional procedures appear to drive a substantial portion of healthcare utilisation in these patients.
Relations between White Matter Maturation and Reaction Time in Childhood
Authors: Scantlebury Nadia , Cunningham Todd , Dockstader Colleen , Laughlin Suzanne , Gaetz William , Rockel Conrad , Dickson Jolynn , Mabbott Donald 
Published: October 2013

AbstractWhite matter matures with age and is important for the efficient transmission of neuronal signals. Consequently, white matter growth may underlie the development of cognitive processes important for learning, including the speed of information processing. To dissect the relationship between white matter structure and information processing speed, we administered a reaction time task (finger abduction in response to visual cue) to 27 typically developing, right-handed children aged 4 to 13. Magnetoencephalography and Diffusion Tensor Imaging were used to delineate white matter connections implicated in visual-motor information processing. Fractional anisotropy (FA) and radial diffusivity (RD) of the optic radiation in the left hemisphere, and FA and mean diffusivity (MD) of the optic radiation in the right hemisphere changed significantly with age. MD and RD decreased with age in the right inferior fronto-occipital fasciculus, and bilaterally in the cortico-spinal tracts. No age-related changes were evident in the inferior longitudinal fasciculus. FA of the cortico-spinal tract in the left hemisphere and MD of the inferior fronto-occipital fasciculus of the right hemisphere contributed uniquely beyond the effect of age in accounting for reaction time performance of the right hand. Our findings support the role of white matter maturation in the development of information processing speed. (JINS, 2013,19, 1–14)
How spirituality is understood and taught in New Zealand medical schools
Authors: Lambie D. , Egan R. , Walker S. , MacLeod R. 
Published: October 2013

AbstractObjectives:The objective of this research was to explore how spirituality is currently understood and taught in New Zealand Medical Schools.Methods:A mixed methods study was carried out involving interviews (n = 14) and a survey (n = 73). The first stage of the study involved recorded semi-structured interviews of people involved in curriculum development from the Dunedin School of Medicine (n = 14); which then informed a cross-sectional self-reported electronic survey (n = 73).Results:The results indicate that spirituality is regarded by many involved in medical education in New Zealand as an important part of healthcare that may be taught in medical schools, but also that there is little consensus among this group as to what the topic is about.Significance of results:These findings provide a basis for further discussion about including spirituality in medical curricula, and in particular indicate a need to develop a shared understanding of what ‘spirituality’ means and how it can be taught appropriately. As a highly secular country, these New Zealand findings are significant for medical education in other secular Western countries. Addressing spirituality with patients has been shown to positively impact a range of health outcomes, but how spirituality is taught in medical schools is still developing across the globe.