Later Prehistory from the Trent to the Tyne
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Early Medieval Dykes (400 to 850 Ad)
EARLY MEDIEVAL DYKES (400 TO 850 AD) A thesis submitted to the University of Manchester for the degree of Doctor of Philosophy in the Faculty of Humanities 2015 Erik Grigg School of Arts, Languages and Cultures Contents Table of figures ................................................................................................ 3 Abstract ........................................................................................................... 6 Declaration ...................................................................................................... 7 Acknowledgments ........................................................................................... 9 1 INTRODUCTION AND METHODOLOGY ................................................. 10 1.1 The history of dyke studies ................................................................. 13 1.2 The methodology used to analyse dykes ............................................ 26 2 THE CHARACTERISTICS OF THE DYKES ............................................. 36 2.1 Identification and classification ........................................................... 37 2.2 Tables ................................................................................................. 39 2.3 Probable early-medieval dykes ........................................................... 42 2.4 Possible early-medieval dykes ........................................................... 48 2.5 Probable rebuilt prehistoric or Roman dykes ...................................... 51 2.6 Probable reused prehistoric -
Complete 230 Fellranger Tick List A
THE LAKE DISTRICT FELLS – PAGE 1 A-F CICERONE Fell name Height Volume Date completed Fell name Height Volume Date completed Allen Crags 784m/2572ft Borrowdale Brock Crags 561m/1841ft Mardale and the Far East Angletarn Pikes 567m/1860ft Mardale and the Far East Broom Fell 511m/1676ft Keswick and the North Ard Crags 581m/1906ft Buttermere Buckbarrow (Corney Fell) 549m/1801ft Coniston Armboth Fell 479m/1572ft Borrowdale Buckbarrow (Wast Water) 430m/1411ft Wasdale Arnison Crag 434m/1424ft Patterdale Calf Crag 537m/1762ft Langdale Arthur’s Pike 533m/1749ft Mardale and the Far East Carl Side 746m/2448ft Keswick and the North Bakestall 673m/2208ft Keswick and the North Carrock Fell 662m/2172ft Keswick and the North Bannerdale Crags 683m/2241ft Keswick and the North Castle Crag 290m/951ft Borrowdale Barf 468m/1535ft Keswick and the North Catbells 451m/1480ft Borrowdale Barrow 456m/1496ft Buttermere Catstycam 890m/2920ft Patterdale Base Brown 646m/2119ft Borrowdale Caudale Moor 764m/2507ft Mardale and the Far East Beda Fell 509m/1670ft Mardale and the Far East Causey Pike 637m/2090ft Buttermere Bell Crags 558m/1831ft Borrowdale Caw 529m/1736ft Coniston Binsey 447m/1467ft Keswick and the North Caw Fell 697m/2287ft Wasdale Birkhouse Moor 718m/2356ft Patterdale Clough Head 726m/2386ft Patterdale Birks 622m/2241ft Patterdale Cold Pike 701m/2300ft Langdale Black Combe 600m/1969ft Coniston Coniston Old Man 803m/2635ft Coniston Black Fell 323m/1060ft Coniston Crag Fell 523m/1716ft Wasdale Blake Fell 573m/1880ft Buttermere Crag Hill 839m/2753ft Buttermere -
Landform Studies in Mosedale, Northeastern Lake District: Opportunities for Field Investigations
Field Studies, 10, (2002) 177 - 206 LANDFORM STUDIES IN MOSEDALE, NORTHEASTERN LAKE DISTRICT: OPPORTUNITIES FOR FIELD INVESTIGATIONS RICHARD CLARK Parcey House, Hartsop, Penrith, Cumbria CA11 0NZ AND PETER WILSON School of Environmental Studies, University of Ulster at Coleraine, Cromore Road, Coleraine, Co. Londonderry BT52 1SA, Northern Ireland (e-mail: [email protected]) ABSTRACT Mosedale is part of the valley of the River Caldew in the Skiddaw upland of the northeastern Lake District. It possesses a diverse, interesting and problematic assemblage of landforms and is convenient to Blencathra Field Centre. The landforms result from glacial, periglacial, fluvial and hillslopes processes and, although some of them have been described previously, others have not. Landforms of one time and environment occur adjacent to those of another. The area is a valuable locality for the field teaching and evaluation of upland geomorphology. In this paper, something of the variety of landforms, materials and processes is outlined for each district in turn. That is followed by suggestions for further enquiry about landform development in time and place. Some questions are posed. These should not be thought of as being the only relevant ones that might be asked about the area: they are intended to help set enquiry off. Mosedale offers a challenge to students at all levels and its landforms demonstrate a complexity that is rarely presented in the textbooks. INTRODUCTION Upland areas attract research and teaching in both earth and life sciences. In part, that is for the pleasure in being there and, substantially, for relative freedom of access to such features as landforms, outcrops and habitats, especially in comparison with intensively occupied lowland areas. -
The Iron Age Tom Moore
The Iron Age Tom Moore INTRODUCfiON In the twenty years since Alan Saville's (1984) review of the Iron Age in Gloucestershire much has happened in Iron-Age archaeology, both in the region and beyond.1 Saville's paper marked an important point in Iron-Age studies in Gloucestershire and was matched by an increasing level of research both regionally and nationally. The mid 1980s saw a number of discussions of the Iron Age in the county, including those by Cunliffe (1984b) and Darvill (1987), whilst reviews were conducted for Avon (Burrow 1987) and Somerset (Cunliffe 1982). At the same time significant advances and developments in British Iron-Age studies as a whole had a direct impact on how the period was viewed in the region. Richard Hingley's (1984) examination of the Iron-Age landscapes of Oxfordshire suggested a division between more integrated unenclosed communities in the Upper Thames Valley and isolated enclosure communities on the Cotswold uplands, arguing for very different social systems in the two areas. In contrast, Barry Cunliffe' s model ( 1984a; 1991 ), based on his work at Danebury, Hampshire, suggested a hierarchical Iron-Age society centred on hillforts directly influencing how hillforts and social organisation in the Cotswolds have been understood (Darvill1987; Saville 1984). Together these studies have set the agenda for how the 1st millennium BC in the region is regarded and their influence can be felt in more recent syntheses (e.g. Clarke 1993). Since 1984, however, our perception of Iron-Age societies has been radically altered. In particular, the role of hillforts as central places at the top of a hierarchical settlement pattern has been substantially challenged (Hill 1996). -
Early Christian' Archaeology of Cumbria
Durham E-Theses A reassessment of the early Christian' archaeology of Cumbria O'Sullivan, Deirdre M. How to cite: O'Sullivan, Deirdre M. (1980) A reassessment of the early Christian' archaeology of Cumbria, Durham theses, Durham University. Available at Durham E-Theses Online: http://etheses.dur.ac.uk/7869/ Use policy The full-text may be used and/or reproduced, and given to third parties in any format or medium, without prior permission or charge, for personal research or study, educational, or not-for-prot purposes provided that: • a full bibliographic reference is made to the original source • a link is made to the metadata record in Durham E-Theses • the full-text is not changed in any way The full-text must not be sold in any format or medium without the formal permission of the copyright holders. Please consult the full Durham E-Theses policy for further details. Academic Support Oce, Durham University, University Oce, Old Elvet, Durham DH1 3HP e-mail: [email protected] Tel: +44 0191 334 6107 http://etheses.dur.ac.uk Deirdre M. O'Sullivan A reassessment of the Early Christian.' Archaeology of Cumbria ABSTRACT This thesis consists of a survey of events and materia culture in Cumbria for the period-between the withdrawal of Roman troops from Britain circa AD ^10, and the Viking settlement in Cumbria in the tenth century. An attempt has been made to view the archaeological data within the broad framework provided by environmental, historical and onomastic studies. Chapters 1-3 assess the current state of knowledge in these fields in Cumbria, and provide an introduction to the archaeological evidence, presented and discussed in Chapters ^--8, and set out in Appendices 5-10. -
Hallam Fields, Birstall, Leicestershire
An Excavation of an Iron Age Settlement at Hallam Fields, Birstall, Leicestershire The Lithics Lynden Cooper Results Some 151 worked flints were recovered from the excavation. A large proportion (83%) was from Middle Iron Age features and are likely to be residual. However the finds from two Early Bronze Age pit fills probably represent contemporary activity. Five pieces (3%) displaying bladelet technology can be regarded as Mesolithic. Two blades also may be Mesolithic. The microlith fragment has inverse basal retouch, a feature commonly seen in Honey Hill type assemblages from the Midlands (Saville 1981). These are suspected to chronologically fall between the earliest and latest Mesolithic in the Midlands (Myers 2006). Taking the remaining flints as a group they can be split into 119 flakes (83%), five pieces of shatter (3%), five cores (3%) and 15 tools (10%). The tools contain few chronologically diagnostic types. There is a possible example of an unfinished Laurel Leaf that would be of Neolithic date. A large fragment of a discoidal scraper is similar in form and flint type to Late Neolithic examples from Eye Kettleby and Rothley. There are some indications for later Bronze Age activity from the concave scrapers and the scraper with straight-edge retouch. Another scraper used an older (slightly patinated) flake support. Such recycling has been seen at other later Bronze Age sites in the area e.g. Willow Farm, Castle Donington and Cossington barrows (Cooper 2008). The technological aspects of the debitage would also fit within a broad Neolithic-Bronze Age date. The stratified flint from context (643) is remarkably fresh and sharp, further suggesting that it is contemporary. -
Settlement Hierarchy and Social Change in Southern Britain in the Iron Age
SETTLEMENT HIERARCHY AND SOCIAL CHANGE IN SOUTHERN BRITAIN IN THE IRON AGE BARRY CUNLIFFE The paper explores aspects of the social and economie development of southern Britain in the pre-Roman Iron Age. A distinct territoriality can be recognized in some areas extending over many centuries. A major distinction can be made between the Central Southern area, dominated by strongly defended hillforts, and the Eastern area where hillforts are rare. It is argued that these contrasts, which reflect differences in socio-economic structure, may have been caused by population pressures in the centre south. Contrasts with north western Europe are noted and reference is made to further changes caused by the advance of Rome. Introduction North western zone The last two decades has seen an intensification Northern zone in the study of the Iron Age in southern Britain. South western zone Until the early 1960s most excavation effort had been focussed on the chaiklands of Wessex, but Central southern zone recent programmes of fieid-wori< and excava Eastern zone tion in the South Midlands (in particuiar Oxfordshire and Northamptonshire) and in East Angiia (the Fen margin and Essex) have begun to redress the Wessex-centred balance of our discussions while at the same time emphasizing the social and economie difference between eastern England (broadly the tcrritory depen- dent upon the rivers tlowing into the southern part of the North Sea) and the central southern are which surrounds it (i.e. Wessex, the Cots- wolds and the Welsh Borderland. It is upon these two broad regions that our discussions below wil! be centred. -
Sussex Archaeological Society
GB 1850 MS Collections Sussex Archaeological Society This catalogue was digitised by The National Archives as part of the National Register of Archives digitisation project NRA 41416 The National Archives NOTE ON ACCESS Searchers should note that to secure access to any of these collections they must first make an appointment with the honorary librarian of the Sussex Archaeological Society. Sussex Archaeological Society, Barbican House, 169 High Street, Lewes BN7 1YE Tel. 01273-486290. COLLECTIONS OF WORKING PAPERS - AUTHORS Allcroft, A. Hadrian Andrews, P.B.S. Attree, F.W.T. Barton, Kenneth J. Bax, Alfred R. Biggar, Joyce T. M. Blaauw, William Henry Bleach, John Booker, T. P.L. Bothamley, Henry W. Brackenbury, K.F. Buck land, L.A. Budgen, Walter Burstow, George Philip Chandler, Allan Child, F. Cooper, William Durrant Courthope, Daphne Crook, B.M. Curwen, Eliot & E. Cecil Davenport, W.S. De Candole, H. Dell, Richard Denman, John Domes, R.L. Dunk in, Edwin H.W. Farrant, John H. * Godfrey, Walter H. Grant ham, W.W. Gray, J.V. Grlnsell, Leslie V. Gunnis, Rupert Hannah, I. Hodson, Leonard J. Holden, Eric W. Holgate, M. S. Honeywood, W. Johnston, George D. Langdon, F.G. Leeney, 0.H. Long, A. Lovegrove, H. Lower, Mark Antony MacDermott, K.H. Machell-Cox, E. , Mannington, H. Marten (Martin) family (several members) Meads, W.E. Norris, N.E.S. Pullein, Catherine Remnant, G.L. Rice, R. Garraway Ross, T. Salt, Mary C.L. Salzman, Louis F. Shaw, Frank Sheppard, V. Simmonds, C. Smith, Verena Standen family Stevens, F. Bentham Straker, E. Style, - Tebbutt, C.F. -
Character Appraisal
Main Heading Aston Tirrold & Aston Upthorpe Conservation Area Character Appraisal The conservation area character appraisal - this sets the context for the proposals contained in Part 2. Part 1 was adopted by Council in September and is included for information only. May 2005 Aston Tirrold and Aston Upthorpe Conservation Area Character Appraisal The Council first published the Aston Tirrold and Aston Upthorpe Conservation Area Character Appraisal in draft form in July 2004. Following th a period of public consultation, including a public meeting held on 12 nd August 2004, the Council approved the Character Appraisal on the 2 September 2004. Contents Introduction . .1 1 Aston Tirrold and Aston Upthorpe The history of the area . .3 Introduction . .3 Aston Tirrold . .3 Aston Upthorpe . .5 Aston Tirrold and Upthorpe from the nineteenth century . .6 2 The established character . .7 Chalk Hill . .9 Aston Street . .9 Baker Street . .12 Spring Lane . .14 The Croft . .16 Fullers Road . .16 Thorpe Street . .19 Important open spaces outside the conservation area . .21 3 Possible areas for enhancement and design guidance for new development . .22 Introduction . .22 The need for contextual design . .22 Grain of the village . .22 Appearance, materials and detailing . .22 Boundary treatments . .23 Scale . .24 Extensions to existing buildings . .24 Repairs . .24 Negative elements . .24 Services . .24 Street furniture . .25 4 South Oxfordshire Local Plan adopted by Council, April 1997 . .26 5 Summary of the conservation policies contained within the 2011 Second Deposit Draft local Plan . .28 6 Acknowledgements and bibliography . .31 ASTON TIRROLD & ASTON UPTHORPE CONSERVATION AREA CHARACTER APPRAISAL i South Oxfordshire District Council ii ASTON TIRROLD & ASTON UPTHORPE CONSERVATION AREA CHARACTER APPRAISAL South Oxfordshire District Council Part 1 Introduction 2. -
PR Box 1 Transcriptions
Pitt-Rivers papers Transcriptions Not all of the letters have been transcribed. A full listing is available here. The decision about which letters were ‘worth’ transcribing was taken by the transcriber (Alison Petch) alone based upon her research into Pitt-Rivers’ life and career and also her catalogue of the Pitt-Rivers papers and therefore reflects (to some degree) her personal bias. All notes about aspects of the letters were also prepared by the transcriber. Note that unlike the catalogue order (or the order they were kept in by Pitt-Rivers), these transcriptions are listed together in on-going communication order so that a conversation about a site or set of sites can be followed. The relevant sites are shown below as titles in bold Transcriptions and notes were prepared between November and December 2014. Berwickshire Box 1/ B3 [On blue paper, copy letters][1] Services – Ancient Monuments A 14235 / 1882 Subject: Guardianship of Ancient Monuments in Berwickshire Drafted by CHW [or HW] Copied by F Wilson Examined by CHW [or HW] Dispatched by G.W.D. Entred L. WR 14/ Page 156 To D. M. Home Esq [2] Convenor of Berwickshire Milne Graden Coldstream. Sir, With reference to your letter of the 27th ult. relative to the guardianship of various Ancient Monuments in the County of Berwickshire, I am directed to acquaint you that no appointment has yet been made of an Inspector under the Ancient Monuments Protection Act 1882 but that any communication addressed to this office will receive attention. I am &c N.J.C. [On outside of folded paper] A.M.P.A. -
Winchester Museums Service Historic Resources Centre
GB 1869 AA2/110 Winchester Museums Service Historic Resources Centre This catalogue was digitised by The National Archives as part of the National Register of Archives digitisation project NRA 41727 The National Archives ppl-6 of the following report is a list of the archaeological sites in Hampshire which John Peere Williams-Freeman helped to excavate. There are notes, correspondence and plans relating to each site. p7 summarises Williams-Freeman's other papers held by the Winchester Museums Service. William Freeman Index of Archaeology in Hampshire. Abbots Ann, Roman Villa, Hampshire 23 SW Aldershot, Earthwork - Bats Hogsty, Hampshire 20 SE Aldershot, Iron Age Hill Fort - Ceasar's Camp, Hampshire 20 SE Alton, Underground Passage' - Theddon Grange, Hampshire 35 NW Alverstoke, Mound Cemetery etc, Hampshire 83 SW Ampfield, Misc finds, Hampshire 49 SW Ampress,Promy fort, Hampshire 80 SW Andover, Iron Age Hill Fort - Bagsbury or Balksbury, Hampshire 23 SE Andover, Skeleton, Hampshire 24 NW Andover, Dug-out canoe or trough, Hampshire 22 NE Appleshaw, Flint implement from gravel pit, Hampshire 15 SW Ashley, Ring-motte and Castle, Hampshire 40 SW Ashley, Earthwork, Roman Building etc, Hampshire 40 SW Avington, Cross-dyke and 'Ring' - Chesford Head, Hampshire 50 NE Barton Stacey, Linear Earthwork - The Andyke, Hampshire 24 SE Basing, Park Pale - Pyotts Hill, Hampshire 19 SW Basing, Motte and Bailey - Oliver's Battery, Hampshire 19 NW Bitterne (Clausentum), Roman site, Hampshire 65 NE Basing, Motte and Bailey, Hampshire 19 NW Basingstoke, Iron -
Historic Landscape Character Areas and Their Special Qualities and Features of Significance
Historic Landscape Character Areas and their special qualities and features of significance Volume 1 Third Edition March 2016 Wyvern Heritage and Landscape Consultancy Emma Rouse, Wyvern Heritage and Landscape Consultancy www.wyvernheritage.co.uk – [email protected] – 01747 870810 March 2016 – Third Edition Summary The North Wessex Downs AONB is one of the most attractive and fascinating landscapes of England and Wales. Its beauty is the result of many centuries of human influence on the countryside and the daily interaction of people with nature. The history of these outstanding landscapes is fundamental to its present‐day appearance and to the importance which society accords it. If these essential qualities are to be retained in the future, as the countryside continues to evolve, it is vital that the heritage of the AONB is understood and valued by those charged with its care and management, and is enjoyed and celebrated by local communities. The North Wessex Downs is an ancient landscape. The archaeology is immensely rich, with many of its monuments ranking among the most impressive in Europe. However, the past is etched in every facet of the landscape – in the fields and woods, tracks and lanes, villages and hamlets – and plays a major part in defining its present‐day character. Despite the importance of individual archaeological and historic sites, the complex story of the North Wessex Downs cannot be fully appreciated without a complementary awareness of the character of the wider historic landscape, its time depth and settlement evolution. This wider character can be broken down into its constituent parts.