Introduction to an Archaeological Research Framework for the Solent-Thames Sub-Region: Resource Assessment and Research Agenda
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English Nature Research Report
Maritime Natural Area: MIO. Whitstable to Geological Significance: Notable North Foreland (provisional) General geologicaVgeomorpholugicaIcharactcr: The Whitstable to North Foreland Maritime Natural Area has a varied coastline with relatively low-lying coast in thc cast rising to boulder clay and chalk cliffs towards the Isle of Thanet. Geological Htrtory: This coastline is characterised by the Cretaceous chalk of the Isle oTThanet bounded to the west by clays, silts and sands of the Lower ‘I’ertiary. Upper Cretaceous Santonian chalk (87-83 Ma) is exposed dipping gently to the west from Margatc to the eastern side of Herne Bay. Unconformably overlying the chalk is a sequence of Lower Tertiary scdiments which are exposed in I Ierne Bay; the Palaeocenc Thanet, Woolwicli and Oldhaven Formations overlain by the Eocene London Clay Formation. The Chalk was deposited by a shallow sea which covered much of Northwestern Europe towards the end of the Cretaceous. Sea lcvel fall was followed by the unconformabie deposition of Tertiary Palaeocene and Ikcene sedirnents. Dominantly marine in origin, these scdiments were deposited by a rising, but fluctuating sea, which covered much of Southeast England. Marine conditions were well established by the Eocene leading to the deposition ofthe i,ondon Clay Formation. Thc fossil fauna and flora from the Tertiary rocks indicates a gradually warming climate with sub-tropical conditions established by the Eocene. Subsequent uplilt (associated with the Alpine Orogeny) and resultant erosion removed much of the remaining Tertiary sediments, the next deposition occurring during the Pleistocene. Though not covercd by ice, the area was affectcd by periglacial erosion in a tundra-like environment during the last glaciation (Devensian). -
Cambridge County Geographies
CA MBRIDGE COU NTY GE OGRA P HIE S M. ra l d t . M RD M. D Ge n e E : F H . H G UI L L E A A . i or , , HA MP SHIRE CA MBRIDGE UNIV E RSIT Y P RE S S C F C L A Y M A N . , A GE R L ONDON F E TTE R L A N E E C , . 4 N E Y O R K T H E M C M I N W A L L A C O . BOMBA Y A L U TT MA CMIL L A N A N D co . L T D C C A , . MA D RA S I T H E M C M I L L N T O R O N TO A A C O . O F C A N A D A D , L T . TO KYO MA RU Z E N - K A B US H IKI- K A IS H A O A L L RIGHT S RE S E RV E D ! 6 ’ ‘ m u S “ N aN CX F r a (3 U G , t Ca mé riafige County Geog ra pbies H A M P S H I RE TE LF ORD VARLE Y l ’ H ea d M a s er P e t er S m o n d s S c h o o] W in t , y , che s t e r W it h Ma s D a ams a nd s t a t p , i g r , Illu r ions CAMBRIDGE A T THE UNI VE RSIT Y PRESS 1 9 2 2 P RE FACE THE author b eg s t o exp ress his cordial thanks t o many friends wh o have given him valuable assistance in con i n — t o V n ect o . -
Havant Borough Townscape, Landscape and Seascape Character Assessment February 2007 13
HAVANT BOROUGH TOWNSCAPE, LANDSCAPE AND SEASCAPE CHARACTER ASSESSMENT FEBRUARY 2007 13 HAVANT BOROUGH TOWNSCAPE, LANDSCAPE AND SEASCAPE CHARACTER ASSESSMENT SECTION 2: FORMATIVE INFLUENCES ON THE LANDSCAPE HAVANT BOROUGH TOWNSCAPE, LANDSCAPE AND SEASCAPE CHARACTER ASSESSMENT FEBRUARY 2007 14 FORMATIVE INFLUENCES ON THE LANDSCAPE 2.1 Introduction The patterns and distinctive features of the Havant Borough landscape are a result of the interaction of its physical structure, the nature of the vegetation, the land uses which have resulted, its built form and the continuing influence of human activity. This section draws out the most significant past and present physical and human influences that have shaped the development of Havant Borough. The meaning of technical terms which have been used in this section are set out in the Glossary at the end of the report. 2.2 Landscape, Townscape and Seascape Context Although Havant Borough is relatively small, its landscape, townscape and seascape development is very varied and complex, reflecting the pattern of the wider landscape, townscape and seascape which surround it. Topographically and geologically it sits in the lower levels (below 50mAOD) on the Hampshire Basin clays and sands which extend along the southern seaboard of Hampshire and the Solent. However, the southern part of the Borough, like its neighbour Portsmouth, is distinguished by the higher outcrop of the chalk escarpment at Portsdown Hill. Its coastal lowlands are typical of the mix of urban growth and exposed open landscapes along the Hampshire coast east of Southampton Water, but Hayling Island, in particular, is unique in its harbour and coastal setting and predominantly rural character. -
Some Aspects of the Pleistocene Succession in Areas Adjoining The
Some Aspects of the Pleistocene Succession in Areas Adjoining the English Channel thesis presented for the degree of Doctor of Philosophy in the U n iv ersity o f London hy David Henry Keen A p ril 1975 ProQuest Number: 10098275 All rights reserved INFORMATION TO ALL USERS The quality of this reproduction is dependent upon the quality of the copy submitted. In the unlikely event that the author did not send a complete manuscript and there are missing pages, these will be noted. Also, if material had to be removed, a note will indicate the deletion. uest. ProQuest 10098275 Published by ProQuest LLC(2016). Copyright of the Dissertation is held by the Author. All rights reserved. This work is protected against unauthorized copying under Title 17, United States Code. Microform Edition © ProQuest LLC. ProQuest LLC 789 East Eisenhower Parkway P.O. Box 1346 Ann Arbor, Ml 48106-1346 ii A bstract Middle and Upper Pleistocene sea level and climatic successions for the shores of the English Channel are proposed. The sequence is based on the ezamination of an area of fluvial deposition in south Hampshire and an area of marine, colluvial and aeolian deposition in the Channel Islands. Five main conclusions are proposed: I, the terrace gravels of south Hampshire are entirely of fluvial origin and were deposited by the Pleisto cene River Solent. These terraces are of end interglacial age and were formed by the large discharges associated with cooling climates, but before glacio-eustatic effects caused sea level to fall greatly from the inter- glacial level; II, the Hoxnian inter glacial sea level was around 100 ft. -
Dorset Coast Seascape Character Assessment
Landscape & DORSET COAST Seascape Character Assessment FINAL SEPTEMBER 2010 IMAGE © MARK SIMMONS, DCC September 2010 A Worton Rectory Park, Oxford OX29 4SX T +44 (0)1865 887 050 T +44 (0)1865 887 055 W www.lda-design.co.uk This document has been prepared and checked in accordance with ISO 9001:2000 © LDA Design Consulting LLP. Quality Assured to BS EN ISO 9001 : 2000 LDA Design Consulting LLP, Registered No: OC307725 17 Minster Precincts, Peterborough PE1 1XX Dorset Coast Landscape & Seascape Character Assessment ACKNOWLEDGEMENTS The Dorset Coast Landscape and Seascape Assessment has benefited from the expertise and guidance of a number of individuals and organisations. Thanks are extended to all those who contributed. PROJECT STEERING GROUp Bob Huggins – Dorset Coast Forum, Chair Ken Buchan -Coastal Policy Manager, Dorset CC Ness Smith –C-SCOPE Project Officer, Dorset CC Tony Harris –Senior Landscape Officer, Dorset CC James Feaver – Coastal and Marine GIS Officer Sandie Wilson – Portland Harbour Authority Bridget Betts – Dorset County Council Matilda Bark – Dorset County Council Jennifer Clarke – AONB Planning Officer CONSULTANTS TEAM LDA Design Consulting LLP William Wheeler Ian Houlston Sarah Singleton Lisa Jenkinson David Lock – GIS Specialist Siobhan Gibbons – Graphics specialist Royal Haskoning Randolph Velterop Paolo Pizzolla Thanks are extended to the many individuals who participated through the Dorset Coast Forum and gave us the benefit of their local knowledge and expertise. We would also like to thank Christine Tudor (Natural England) and Dave Hooley (English Heritage) for their specialist inputs. CONTENTS SECTION 1 1 INTRODUCTION 1.1. Introduction 3 1.2. Background to the Dorset Coast Landscape and Seascape Character Assessment 4 1.3. -
River Basin Management Plan South East River Basin District
River Basin Management Plan South East River Basin District Annex C: Actions to deliver objectives Contents C.1 Introduction 3 C.2 Actions we can all take 9 C.3 Agriculture and rural land management 11 C.4 Angling and conservation 40 C.5 Central government 57 C.6 Environment Agency 124 C.7 Industry, manufacturing and other business 208 C.8 Local Government 231 C.9 Mining and quarrying 258 C.10 Navigation 264 C.11 Urban and transport 272 C.12 Water industry 290 Environment Agency River Basin Management Plan South East River Basin District Annex C: Actions to deliver objectives 2 December 2009 C.1 Introduction This annex sets out tables of the actions (the programmes of measures) that are proposed for each sector. Actions are the on the ground activities that will be implemented to manage the pressures on the water environment and achieve the objectives of this plan. Further information relating to these actions and how they have been developed is given in: • Annex B Objectives for waters in the South East River Basin District This gives information on the current status and environmental objectives that have been set and when it is planned to achieve • Annex D Protected area objectives (including programmes for Natura 2000) This gives details of the location of protected areas, the monitoring networks for these, the environmental objectives and additional information on programmes of work for Natura 2000 sites • Annex E Actions appraisal This gives information about how we have set the water body objectives for this plan and how we have selected the actions • Annex F Mechanisms for action This sets out the mechanisms - that is, the policy, legal, financial and voluntary arrangements - that allow actions to be put in place Environment Agency River Basin Management Plan South East River Basin District Annex C: Actions to deliver objectives 3 December 2009 Tables of actions The actions are set out in tables for each sector. -
ARCHAEOLOGICAL STRATEGY Hampshire Archaeological Strategy
HAMPSHIRE ARCHAEOLOGICAL STRATEGY Hampshire Archaeological Strategy CHAPTER ONE. INTRODUCTION BACKGROUND TO STRATEGY Government advice in the National Planning Policy Framework identifies the historic environment as a Core Planning Principle1 and as one aspect of sustainable development2. As such the impact of development proposals on archaeological remains is a material consideration within the planning system. Substantial harm or loss of nationally significant archaeological sites should be wholly exceptional3 The case for preservation needs to be supported by an understanding of the archaeological implications of this course. Conversely, where development results in intervention the objectives of the intervention have to be described. These decisions need to be made within an archaeological framework that has wide support and reflects broad issues, and which is based on the available data. PURPOSE AND ROLE OF THIS FRAMEWORK To harmonise curatorial and academic objectives. - Assist in the identification of sites meriting preservation in situ, balancing preservation of the most important sites with the need for a developing understanding of the resource and for the evolution of archaeological study. -Ensuring that the ‘consumption’ of the various elements of the archaeological resource does not result in any of those elements dropping below the ‘minimum viable academic sample’, without that fact being overtly recognised within that decision. -Ensure academic, curatorial and local archaeologists have access to common data, in particular that development control gathered data is available to, and can influence, wider public research interests. -Where a site is not otherwise threatened, consider whether research aims can be met by re-investigating the existing data -Where excavation is required to review whether the scale of excavation is appropriate to the objective. -
5I the HISTORY of the DRAINAGE of the HAMPSHIRE BASIN And
»5i THE HISTORY OF THE DRAINAGE OF THE HAMPSHIRE BASIN and the Relation of Prehistoric Man to that History. BY REGINALD W. HOOLEY, F.'G.S. In endeavouring to trace the history of the drainage of the Hampshire Basin, we soon discover that the present physical features reveal few signs of its beginning. In view of the present insignificance of the rivers and the comparative insufficiency of their watersheds, the work, which they, aided by subseriaJ agencies, have accomplished in the excavation of their valleys is stupendous. Their wide, open valleys, the terraces of gravel on their flanks, the sheets of gravel on the plains bordering their valleys are conclusive evidence that the conditions now obtaining are totally inadequate to explain the observed phenomena ; these can only be deciphered by an acquaintance with the geology of the district. Great earth movements resulting in elevation and subsidence, and the formation of water-partings, the origin of the superficial deposits and raised sea-beaches, the effects of marine and subaerial denudation, changes of climate and the immense period during which the forces of nature have been at work— all have to be taken into consideration. The strata drained by the rivers of the Hampshire Basin belong to the Secondary and Tertiary formations. After the deposition of the Tertiary strata, in the Miocene Period, a profound upheaval began, raising the South East of England above the sea and puckering the strata into a .series of folds with their long axes running approximately North West and South East, with one great fold, the Wealden anticline, over-topping, and far greater in extent than the others. -
Selsey Bill to Portland Bill
HR Wallingford A MACROREVIEW OF THE COASTLINE OF ENGLANDAND WALES Volume 5. The South Coast. Selsey Bill to Portland Bill J Welsby and J M Motyka Report SR I72 January 1989 Atldrcss:Hydraulics Research Ltd, wallingford,oxforcl-shirc oX10 88A, uniredKingdom. Telcphone:0491 35381 Intemational +4449r 35381relex: 848552HRswALc. Facsirnile:0491 32233International + 44 49r 32233 Registeredin EnglandNo. 1622174 This report describes work carried out by Hydraulics Research in a review of the coastline of England and Wales. It has been funded by the Ministry of Agriculture, Fisheries and Food under contract number CSA 1033, the nominated officer being Mr Allison. At the ti-rne of reporting the Hydraulics Research nominated project officer was Dr S W Huntington. ltre report is published on behalf of the Ministry of Agriculture, Fisheries and Food, but any opinion oqpressed within it are those of the authors onIy, and are not necessarily those of the Ministry who sponsored the research. @ Crown copyright 1989 Published by permission of the Controller of Her Majesty's Stationery Office. ABSTRACT This report rev ews the coastline between Selsey BilL and Portland Bill on the south coast of England. In it are described the various natural and man-madeproc es which affect the behaviour of this partlcular stretch of Britainrs shore ine. The report includes a descri.ption of the maJor eoastal defencee, areag of erosion and accretion and various other aspects of beach:- development. retches of coastline whlch for coastal engineering purposes can be treated independent or semi-dependent cells are also ldentified. Ttris is the flf report of a series, which Hydraulics Researchare carrying out for the try of Agriculture, Fisherles and Food. -
•S-R-Og.Tfcmfor D on Sea 0 12 3 4 5 Hms 'X
Proc. Hants. Field Club Archaeol. Soc. 36, 1980, 15-24. 15 THE ENVIRONMENT OF DEPOSITION OF THE SOUTH HAMPSHIRE PLATEAU GRAVELS By DAVID H. KEEN INTRODUCTION 1975) also agree on a non-aeolian origin for this deposit. The Plateau Gravels of the New Forest and Fossiliferous Pleistocene deposits are known Bournemouth form a conspicuous feature of only from one site in the area. This is Stone the superficial geology of southern England. Point (SZ 158984) where West and Sparks Considerable discussion has continued about (1960) and Brown, Gilbertson, Green and the origin of these gravels since their first com Keen (1975) describe peats and silt with prehensive description in the mid-nineteenth brackish mollusca and a pollen spectrum of century (Codrington 1870). Ipswichian zone lib age. Three depositional environments have been THE GRAVELS postulated for the gravels: a fluvial environ The gravels of South Hampshire are ment (White 1917); a marine environment arranged as a series of terraces. Below 40 m (Codrington 1870; Everard 1954); and a O.D. these terraces are only moderately dis glacio-fluvial environment (Kellaway, Redding, sected. Above this height the gravel spreads Shepard-Thorn, Destombes 1975). Addition are separated into eroded remnants. The ally, Palmer and Cooke (1923) and J. F. N. general arrangement of the terraces can be Green (1946) suggested that both fluvial and seen in Everard (1954, Fig. 1) and Green marine action were responsible for the depo (1940, PI. 5). No general agreement on the sition of the gravels and the cutting of the heights of the major terrace stages can be benches on which they rest.