Palaeolithic Implements from Kirmington, Lincolnshire, and their relation to the 100-foot raised beach of Late Pleistocene Times

1931 ◽  
Vol 11 (3) ◽  
pp. 262-272 ◽  
Author(s):  
J. P. T. Burchell
Keyword(s):  
Late Pleistocene ◽  
Late Glacial ◽  
Upper Palaeolithic ◽  
Similar Nature ◽  
East Anglia ◽  
North West ◽  
North East ◽  
Boulder Clay

Last year I described before the Society a series of flint implements of Upper Palaeolithic (Upper Mousterian-Aurignacian) facies discovered by me in Yorkshire at the base of, and passing up into, a deposit considered by Lamplugh to resemble a weathered Boulder clay and classed by him as of Late Glacial Age. The geological aspects of these archaeological finds I have dealt with fully in a paper read subsequently to the Prehistoric Society of East Anglia. Both papers, however, were complementary to one read by J.Reid Moir on archaeological discoveries of a similar nature made by him in north-west Norfolk in the Brown Boulder clay. With the objects of obtaining confirmation of Lamplugh's geological opinion and of bridging the gap between north-west Norfolk and Yorkshire, I decided to investigate the glacial sequence in north-east Lincolnshire, choosing Kirmington as a centre.

The Presidential Address for 1931: Early Neanthropic Man and his Relation to the Ice Age

1932 ◽  
Vol 6 (4) ◽  
pp. 253-303 ◽  
Author(s):  
J. P. T. Burchell
Keyword(s):  
Presidential Address ◽  
Ice Age ◽  
General Interest ◽  
Upper Palaeolithic ◽  
Early Neolithic ◽  
Glacial Deposits ◽  
East Anglia ◽  
North East ◽  
Boulder Clay

In order to prepare an address calculated to be of general interest to my fellow archæologists, it is essential that it be composed of a variety of ingredients. Now, it so happens that the results I have been obtaining during the course of my investigations in the last few years not only embrace a large number of culture phases, but, when arranged in proper sequence, they form a consecutive narrative. Furthermore, the greater part of the researches I have undertaken relates to those periods in British prehistory concerning which we know least. I refer to the so-called ‘Upper Palæolithic’ and ‘Early Neolithic’ times.It is not my intention to deal in this paper with those inter-glacial and cultural phases which antedate the formation of the Lower Purple Boulder Clay of Yorkshire and Lincolnshire and the Lower Chalky Boulder Clay of East Anglia, though I would mention I have recently discovered in the glacial deposits of north-east Ireland specimens similar to those which have been found beneath the Cromer Forest Bed of Norfolk and in the Sub-Crag Detritus Bed of Norfolk and Suffolk. These specimens will be fully described and illustrated in our “Proceedings” at a later date.

CLIMATE@COA project: Climate and human adaptation during the Last Glacial Period in the Côa Valley region (Portugal)

2021 ◽  
Author(s):  
Luca Dimuccio ◽  
Thierry Aubry ◽  
Lúcio Cunha ◽  
Nelson Rodrigues
Keyword(s):  
Late Pleistocene ◽  
Interdisciplinary Approach ◽  
Evolutionary Model ◽  
Depositional Environments ◽  
Glacial Period ◽  
Upper Palaeolithic ◽  
Last Glacial Period ◽  
Last Glacial ◽  
North East ◽  
The Last Glacial

<p>In Portugal, climate fluctuations of Late Pleistocene are well-known from marine record on the western Iberian continental margin, particularly of Marine Isotope Stages 4, 3 and 2, and they include various events of secular abrupt climate changes. During cooling phases the Heinrich Events (HE) occurred, corresponding to episodes of massive ice-discharges from Northern Hemisphere ice sheets. Furthermore, several climate phases with relatively warmer conditions, known as Dansgaard-Oeschger (D-O) cycles, characterized by an abrupt warming (D-O event) followed by a more gradual cooling, took place in-between HE. This pronounced climate instability that characterizes the Last Glacial Period between ca. 80-12 ka is recorded in a variety of marine and terrestrial archives worldwide. It had a recognized impact on the bioclimatic zones and, possibly, on the Neanderthal and Anatomically Modern Human (AMH) settlements of Iberia.</p><p>Based mainly on the study of geoarchaeological records preserved in caves and rock-shelters of Iberia, a correlation framework with climate shifts has been proposed to explain the observed discontinuities between sequences containing late Middle and early Upper Palaeolithic remains. Moreover, a climate driven model has been advanced to explain the chronological differences between northern and southern Pyrenean data by a later dispersion of AMH and the persistence of last Neanderthals in Southern Iberia, which were interpreted as a direct impact of HE4 (40-38 ka) in the distribution of large ungulate populations.</p><p>Despite all these data, the exact impact of HE on terrestrial systems, the evaluation of the latitudinal differentiation of their impact and time-gap, as well as the correlation between periods of relative stabilization/soil formation and the D-O events remain to be clearly established. In addition, the whole framework relating to the Middle-to-Upper Palaeolithic transition has been excessively dependent on karst archives and it should be investigated in other geomorphological settings - among these the fluvial and Iberian plateau (“Meseta”), both present in the Côa Valley region (Douro Basin, north-east of Portugal). Alluvial and colluvial deposits preserved in the Côa Valley (e.g. at the Cardina-Salto do Boi, Quinta da Barca Sul, Penascosa, Fariseu, Olga de Ervamoira sites) have demonstrated to be a valuable record of information about Late Pleistocene sedimentary processes, depositional environments, and hunter-gatherer’s behaviour at local and regional scales.</p><p>In this context, the CLIMATE@COA project (COA/CAC/0031/2019), funded by the Fundação para a Ciência e Tecnologia (FCT), proposes an integrated multi/interdisciplinary approach based on the stratigraphical, sedimentological, geochemical, geomorphological, geoarchaeological, and geochronological analyses of terrestrial record (natural and cultural) preserved in the Côa Valley and surrounding plateau areas, with the aim to develop an evolutionary model for the region and to deduce the environmental forcing factors for such evolution - namely climate and ecosystem changes. In addition, the project’s data will allow to define better the chronology of the transition between Neanderthal and AMH and to infer on land use and social organization in its environmental context.</p>

Further Discoveries of Flint Implements in the Brown Boulder Clay of North-West Norfolk

1932 ◽  
Vol 6 (4) ◽  
pp. 306-315 ◽  
Author(s):  
J. Reid Moir
Keyword(s):  
Sea Level ◽  
Geological Survey ◽  
Prehistoric Archaeology ◽  
East Anglia ◽  
North West ◽  
Terminal Moraine ◽  
The North ◽  
Boulder Clay ◽  
Western Portion ◽  
North Western

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.

Upper Palæolithic Man in East Anglia

1926 ◽  
Vol 5 (2) ◽  
pp. 232-237
Author(s):  
J. Reid Moir
Keyword(s):  
Upper Palaeolithic ◽  
East Anglia ◽  
Initial Formation ◽  
The Past ◽  
Main Valley ◽  
Southern Side ◽  
Boulder Clay ◽  
London Clay ◽  
The Town ◽  
Slight Depression

In the northern part of Ipswich, between the Henley and the Norwich Roads, is situated the brickfield of Messrs. A. Bolton & Co., Ltd., where the Eocene London Clay is excavated, and manufactured into red bricks. The brickfield lies in a small and now streamless valley which has been found to be extraordinarily rich in vestiges of the past races of East Anglia. It has been my privilege to examine and conduct excavations in this valley, for many years past, and a great deal is now known about its geological and archæological history. The valley itself, though so near to the town of Ipswich, presents on its southern side, much beauty and wildness, and is the home of many interesting and beautiful birds. It begins as a slight depression in the plateau to the east of the Henley Road, and gradually deepening, and developing a somewhat sinuous course, joins the main valley of the River Gipping about a mile to the westward. The valley is typical of many such in Suffolk, and owes its initial formation to the melting of the glacier that laid down the Upper Boulder Clay of East Anglia. The water set free during this process would naturally find its way into the main drainage valley close by, and there is evidence, in the form of the valley under consideration, that it did this with considerable rapidity.

The Fosse

1924 ◽  
Vol 14 (1-2) ◽  
pp. 252-256 ◽  
Author(s):  
R. G. Collingwood
Keyword(s):  
West Coast ◽  
East Coast ◽  
Nodal Point ◽  
Relative Importance ◽  
East Anglia ◽  
North West ◽  
North East ◽  
The North ◽  
Railway System ◽  
Cross Country

The main lines of communication, in any given country, alter very little from age to age. They are dictated by geography; the vicissitudes of economic and political history may affect their relative importance and alter the details of their lay-out, but nothing except the cessation of traffic can fundamentally change them. This is strikingly exemplified in the relation between the Roman roads of England and its modern railway-system. The main Roman roads are laid out with such accurate attention to geographical facts, that the railway engineers of the nineteenth century were unconsciously forced to imitate their choice of track. In both cases, London is the hub of the system, and main lines radiate to the Channel ports, the Solent, the Exe, the Bristol Channel, the north-west coast, the north-east coast, and East Anglia. In both cases, again, there are certain “cross-country” lines—one from Cheshire to the Usk, one from the Tyne to the Solway, others through the passes of the Pennines. In short, a map of main Roman roads superimposed upon one of main railway-lines shows a very close general agreement, modified by such details as the substitution of Liverpool for Chester as the chief port of the north-west, and the substitution of Reading for Silchester or Shrewsbury for Wroxeter as a nodal point.

Presumed ground-ice depressions in East Anglia

1972 ◽  
Vol 327 (1570) ◽  
pp. 329-343 ◽  
Keyword(s):  
North America ◽  
Late Glacial ◽  
Specific Form ◽  
Ground Ice ◽  
East Anglia ◽  
Boulder Clay

Shallow depressions in the western parts of East Anglia on the Chalk between the boulder clay and the Fens are described and attributed to the formation of ground ice and its subsequent thawing. We prefer to use the non-committal term , ground-ice features, rather than the name of any specific form found in Arctic North America or Soviet Asia. The more recent of these forms seem to date here, as elsewhere in Europe, from Zone III of the Late-glacial (Weichselian), while a more important phase of development took place in Zone I or an earlier Weichselian phase. It is possible that the Breckland meres also originated as groundice features.

Chalky Boulder-clay in the North-West District of London

1927 ◽  
Vol 64 (11) ◽  
pp. 501-502
Author(s):  
H. G. Mantle
Keyword(s):  
County Council ◽  
Post Office ◽  
North West ◽  
The Road ◽  
North East ◽  
The North ◽  
Boulder Clay ◽  
Slight Rise

At the commencement of the year 1925 the Post Office authorities, for the purpose of laying down telephone lines, were making a trench from the corner of Rochester Road (Camden Town) north-eastward up the Camden Road and across it into and along Murray Street in the direction of St. Paul's Road, and were laying ducts at the depth of about 10 ft. The distance from the corner of Rochester Road to a point opposite the corner of Murray Street is 160 yards, the direction north-east, with a slight rise in that direction. Previously the London County Council tramway cable ducts had been laid down to the depth of 3 ft. 6 in., but below this level the whole of the ground excavated was in an undisturbed state. The trench was 2 ft. 7 in. wide. A man-hole had been sunk at the corner of Rochester Road, another at the end of the works on the Camden Road, and a third opposite to it at the corner of Murray Street, all to a depth from the surface of more than 12 ft. In fact the Camden Road man-hole was sunk to the depth of 15 ft. 6 in., so as to enable the excavators to tunnel under the road to Murray Street in order that the stream of traffic along the Camden Road might not be disturbed.

A new volcanic province: evidence from glacial erratics in western North Greenland

2000 ◽  
pp. 35-41 ◽  
Author(s):  
Peter R. Dawes ◽  
Bjørn Thomassen ◽  
T.I. Hauge Andersson
Keyword(s):  
Volcanic Rocks ◽  
Iron Formation ◽  
Banded Iron Formation ◽  
Common Component ◽  
Volcanic Province ◽  
North West ◽  
North East ◽  
The North ◽  
Surficial Deposits ◽  
North Greenland

NOTE: This article was published in a former series of GEUS Bulletin. Please use the original series name when citing this article, for example: Dawes, P. R., Thomassen, B., & Andersson, T. H. (2000). A new volcanic province: evidence from glacial erratics in western North Greenland. Geology of Greenland Survey Bulletin, 186, 35-41. https://doi.org/10.34194/ggub.v186.5213 _______________ Mapping and regional geological studies in northern Greenland were carried out during the project Kane Basin 1999 (see Dawes et al. 2000, this volume). During ore geological studies in Washington Land by one of us (B.T.), finds of erratics of banded iron formation (BIF) directed special attention to the till, glaciofluvial and fluvial sediments. This led to the discovery that in certain parts of Daugaard-Jensen Land and Washington Land volcanic rocks form a common component of the surficial deposits, with particularly colourful, red porphyries catching the eye. The presence of BIF is interesting but not altogether unexpected since BIF erratics have been reported from southern Hall Land just to the north-east (Kelly & Bennike 1992) and such rocks crop out in the Precambrian shield of North-West Greenland to the south (Fig. 1; Dawes 1991). On the other hand, the presence of volcanic erratics was unexpected and stimulated the work reported on here.

Stratigraphy, structure and geochemistry of Archaean supracrustal rocks from Oqaatsut and Naajaat Qaqqaat, north-east Disko Bugt, West Greenland

1999 ◽  
pp. 65-78
Author(s):  
Henrik Rasmussen ◽  
Lars Frimodt Pedersen
Keyword(s):  
Tectonic Setting ◽  
Trace Element Geochemistry ◽  
Element Geochemistry ◽  
West Greenland ◽  
North West ◽  
North East ◽  
Metavolcanic Rocks ◽  
Arc Setting ◽  
Area North ◽  
Back Arc

NOTE: This article was published in a former series of GEUS Bulletin. Please use the original series name when citing this article, for example: Rasmussen, H., & Frimodt Pedersen, L. (1999). Stratigraphy, structure and geochemistry of Archaean supracrustal rocks from Oqaatsut and Naajaat Qaqqaat, north-east Disko Bugt, West Greenland. Geology of Greenland Survey Bulletin, 181, 65-78. https://doi.org/10.34194/ggub.v181.5114 _______________ Two Archaean supracrustal sequences in the area north-east of Disko Bugt, c. 1950 and c. 800 m in thickness, are dominated by pelitic and semipelitic mica schists, interlayered with basic metavolcanic rocks. A polymict conglomerate occurs locally at the base of one of the sequences. One of the supracrustal sequences has undergone four phases of deformation; the other three phases. In both sequences an early phase, now represented by isoclinal folds, was followed by north-west-directed thrusting. A penetrative deformation represented by upright to steeply inclined folds is only recognised in one of the sequences. Steep, brittle N–S and NW–SE striking faults transect all rock units including late stage dolerites and lamprophyres. Investigation of major- and trace-element geochemistry based on discrimination diagrams for tectonic setting suggests that both metasediments and metavolcanic rocks were deposited in an environment similar to a modern back-arc setting.

Palaeolithic Cave Art at Creswell Crags in European Context

2007 ◽  
Keyword(s):  
Late Pleistocene ◽  
Rock Art ◽  
Ice Age ◽  
Upper Palaeolithic ◽  
Southern France ◽  
European Context ◽  
The World ◽  
Cave Art ◽  
Illustrated Book

Cave art is a subject of perennial interest among archaeologists. Until recently it was assumed that it was largely restricted to southern France and northern Iberia, although in recent years new discoveries have demonstrated that it originally had a much wider distribution. The discovery in 2003 of the UK's first examples of cave art, in two caves at Creswell Crags on the Derbyshire/Nottinghamshire border, was the most surprising illustration of this. The discoverers (the editors of the book) brought together in 2004 a number of Palaeolithic archaeologists and rock art specialists from across the world to study the Creswell art and debate its significance, and its similarities and contrasts with contemporary Late Pleistocene ("Ice Age") art on the Continent. This comprehensively illustrated book presents the Creswell art itself, the archaeology of the caves and the region, and the wider context of the Upper Palaeolithic era in Britain, as well as a number of up-to-date studies of Palaeolithic cave art in Spain, Portugal, France, and Italy which serve to contextualize the British examples.

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