The Stratigraphical Framework for the Palaeogene Successions of the London Basin, UK

Total Page:16

File Type:pdf, Size:1020Kb

The Stratigraphical Framework for the Palaeogene Successions of the London Basin, UK The stratigraphical framework for the Palaeogene successions of the London Basin, UK Open Report OR/12/004 BRITISH GEOLOGICAL SURVEY OPEN REPORT OR/12/004 The National Grid and other Ordnance Survey data are used The stratigraphical framework for with the permission of the Controller of Her Majesty’s Stationery Office. the Palaeogene successions of the Licence No: 100017897/2012. London Basin, UK Key words Stratigraphy; Palaeogene; southern England; London Basin; Montrose Group; Lambeth Group; Thames Group; D T Aldiss Bracklesham Group. Front cover Borehole core from Borehole 404T, Jubilee Line Extension, showing pedogenically altered clays of the Lower Mottled Clay of the Reading Formation and glauconitic sands of the Upnor Formation. The white bands are calcrete, which form hard bands in this part of the Lambeth Group (Section 3.2.2.2 of this report) BGS image P581688 Bibliographical reference ALDISS, D T. 2012. The stratigraphical framework for the Palaeogene successions of the London Basin, UK. British Geological Survey Open Report, OR/12/004. 94pp. Copyright in materials derived from the British Geological Survey’s work is owned by the Natural Environment Research Council (NERC) and/or the authority that commissioned the work. You may not copy or adapt this publication without first obtaining permission. Contact the BGS Intellectual Property Rights Section, British Geological Survey, Keyworth, e-mail [email protected]. You may quote extracts of a reasonable length without prior permission, provided a full acknowledgement is given of the source of the extract. Maps and diagrams in this book use topography based on Ordnance Survey mapping. © NERC 2012. All rights reserved Keyworth, Nottingham British Geological Survey 2012 BRITISH GEOLOGICAL SURVEY The full range of our publications is available from BGS shops at British Geological Survey offices Nottingham, Edinburgh, London and Cardiff (Welsh publications only) see contact details below or shop online at www.geologyshop.com BGS Central Enquiries Desk Tel 0115 936 3143 Fax 0115 936 3276 The London Information Office also maintains a reference collection of BGS publications, including maps, for consultation. email [email protected] We publish an annual catalogue of our maps and other publications; this catalogue is available online or from any of the Kingsley Dunham Centre, Keyworth, Nottingham NG12 5GG BGS shops. Tel 0115 936 3241 Fax 0115 936 3488 email [email protected] The British Geological Survey carries out the geological survey of Great Britain and Northern Ireland (the latter as an agency service for the government of Northern Ireland), and of the Murchison House, West Mains Road, Edinburgh EH9 3LA surrounding continental shelf, as well as basic research projects. Tel 0131 667 1000 Fax 0131 668 2683 It also undertakes programmes of technical aid in geology in email [email protected] developing countries. The British Geological Survey is a component body of the Natural Natural History Museum, Cromwell Road, London SW7 5BD Environment Research Council. Tel 020 7589 4090 Fax 020 7584 8270 Tel 020 7942 5344/45 email [email protected] Columbus House, Greenmeadow Springs, Tongwynlais, Cardiff CF15 7NE Tel 029 2052 1962 Fax 029 2052 1963 Maclean Building, Crowmarsh Gifford, Wallingford OX10 8BB Tel 01491 838800 Fax 01491 692345 Geological Survey of Northern Ireland, Colby House, Stranmillis Court, Belfast BT9 5BF Tel 028 9038 8462 Fax 028 9038 8461 www.bgs.ac.uk/gsni/ Parent Body Natural Environment Research Council, Polaris House, North Star Avenue, Swindon SN2 1EU Tel 01793 411500 Fax 01793 411501 www.nerc.ac.uk Website www.bgs.ac.uk Shop online at www.geologyshop.com OR/12/004; Version 1.0 Last modified: 2012/03/08 12:58 Foreword This report provides a summary of the lithostratigraphical scheme proposed by the British Geological Survey (BGS) Stratigraphical Framework Committee (SFC) that aims to describe and rationalise group, formation and member nomenclature for the Palaeogene of the London Basin, southern England. This framework report provides detailed descriptions for units occurring in the onshore area of the London Basin and adjacent parts of East Anglia. Existing names are used wherever appropriate, although where unit names have not previously existed or are unsatisfactory, the report proposes revisions. Acknowledgements The author would like to thank current and former BGS colleagues for helpful discussion and suggestions, in particular R A Ellison, D C Entwisle, P M Hopson, C N Waters and I T Williamson, who advised on parts of this document and who created many of the Lexicon entries on which it draws. Outside BGS, Dr Jackie Skipper, Dr Chris King, D P Page and T Newman are thanked for helpful comments and discussions, and for the provision of documentation, some unpublished. The report was reviewed within BGS by David Entwisle and Richard Ellison, who contributed significantly to its accuracy. The author has benefited from the sight of various unpublished documents, including an incomplete draft description of the Upper Palaeogene of the London Basin, dated 1998, by Richard Ellison, Ian Williamson and Chris King; a provisional stratigraphical framework for the Palaeogene and Neogene rocks of the onshore areas of the Hampshire Basin, the London Basin and East Anglia, dated July 2003, by Robert Knox and Chris King; and advanced drafts of parts of a Geological Society of London (GSL) Special Report on the stratigraphy of the British Palaeogene and Neogene by Chris King. Many details have been drawn from the latter report, especially of inferred environment and age of deposition. However, sections of the latest draft of the GSL Report was received on 30 August 2011, just as work on this BGS report was drawing to a close. This late draft of the GSL Report was subject to review and so liable to be altered further before publication. The present BGS report therefore does not take full account of this latest version of the GSL Report, especially in respect of the proposed formal naming of subdivisions in the Woolwich and Reading formations. Production of this report was funded by the Standards and Best Practice Project (formerly the Geoscientific Standards and Nomenclature Project). This report has been compiled on behalf of the BGS Stratigraphy Committee, and reflects a degree of pragmatism and compromise. It is believed to provide a workable scheme within which any new data and subdivision can be accommodated. If users of this document discover inconsistencies or factual errors in the specifications given for the various lithostratigraphical units, they are encouraged to notify The Chairman, BGS Stratigraphy Committee, British Geological Survey, Keyworth, Nottingham, NG12 5GG (email [email protected]). i OR/12/004; Version 1.0 Last modified: 2012/03/08 12:58 Contents Foreword ......................................................................................................................................... i Acknowledgements ......................................................................................................................... i Contents .......................................................................................................................................... ii 1 Introduction ............................................................................................................................ 1 1.1 Scope of the report .......................................................................................................... 1 1.2 Comparison with the Geological Society of London Special Report on the Tertiary .... 1 1.3 Palaeogeography and depositional basins ...................................................................... 2 1.4 Stratigraphical frameworks ............................................................................................. 3 1.4.1 Chronostratigraphy ...................................................................................................... 4 1.4.2 Biostratigraphy ............................................................................................................ 4 1.4.3 Magnetostratigraphy .................................................................................................... 4 1.4.4 Stable-isotope stratigraphy .......................................................................................... 4 1.4.5 Radiometric dating ...................................................................................................... 5 1.4.6 Tephrostratigraphy ...................................................................................................... 5 1.4.7 Cyclic stratigraphy ...................................................................................................... 5 1.4.8 Sequence stratigraphy ................................................................................................. 5 1.5 The BGS Lexicon of Named Rock Units ....................................................................... 5 1.6 Conventions .................................................................................................................... 6 2 An introduction to the Palaeogene Groups of southern England and some terminological conventions ........................................................................................................... 7 2.1 Palaeogene Groups in southern England ........................................................................ 7 2.2 ‘Lower London Tertiaries’ ............................................................................................
Recommended publications
  • Geology of London, UK
    Proceedings of the Geologists’ Association 123 (2012) 22–45 Contents lists available at ScienceDirect Proceedings of the Geologists’ Association jo urnal homepage: www.elsevier.com/locate/pgeola Review paper Geology of London, UK a, b,c d e c Katherine R. Royse *, Mike de Freitas , William G. Burgess , John Cosgrove , Richard C. Ghail , f g h i j k Phil Gibbard , Chris King , Ursula Lawrence , Rory N. Mortimore , Hugh Owen , Jackie Skipper a British Geological Survey, Keyworth, Nottingham NG12 5GG, UK b First Steps Ltd, Unit 17 Hurlingham Studios, London SW6 3PA, UK c Department of Civil and Environmental Engineering, Imperial College London, London SW7 2AZ, UK d Department of Earth Sciences, University College London, WC1E 6BT, UK e Department of Earth Science and Engineering, Imperial College London, London SW7 2AZ, UK f Cambridge Quaternary, Department of Geography, University of Cambridge, CB2 3EN, UK g 16A Park Road, Bridport, Dorset, UK h Crossrail Ltd. 25 Canada Square, Canary Wharf, London E14 5LQ, UK i University of Brighton & ChalkRock Ltd, 32 Prince Edwards Road, Lewes BN7 1BE, UK j Department of Palaeontology, The Natural History Museum, Cromwell Road, London SW7 5BD, UK k Geotechnical Consulting Group (GCG), 52A Cromwell Road, London SW7 5BE, UK A R T I C L E I N F O A B S T R A C T Article history: The population of London is around 7 million. The infrastructure to support this makes London one of the Received 25 February 2011 most intensively investigated areas of upper crust. However construction work in London continues to Received in revised form 5 July 2011 reveal the presence of unexpected ground conditions.
    [Show full text]
  • The Effects of Shrinkage and Swelling Were First Recognised by Geotechnical Specialists Following the Dry Summer of 1947
    C:\Documents and Settings\adixon\Local Settings\Temporary Internet Files\Content.Outlook\7NFVY2G5\08-112 revised2.doc Modelling Volume Change Potential in the London Clay L. D. Jones & R. Terrington British Geological Survey, Keyworth, Nottingham. NG12 5GG UK (e-mail: [email protected]) Abstract The London Clay Formation is particularly susceptible to shrink–swell behaviour that has resulted in a long history of foundation damage due to ground movement across the outcrop. Damage has cost up to £500 million in a single year. Underlying most of the Greater London area, the London Clay Formation is of major engineering importance as it is on and within this formation that the majority of the city’s infrastructure, buildings and underground services are constructed. The Volume Change Potential of a soil is the relative change in volume to be expected with changes in soil moisture content and the subsequent shrinkage or swelling can cause major damage to structures above or below ground. Detailed statistical and spatial analyses of data across the London Clay outcrop has revealed a significant geographical trend in the volume change potential of this deposit, confirming an overall increase from west to east, but also showing subtle trends with depth. This paper describes how this analysis was carried out and shows how such assessments can yield valuable information about shrink–swell behaviour not only of the London Clay but of similar shrink– swell prone argillaceous formations elsewhere. Introduction The effects of shrinkage and swelling of clay soils, with respect to foundation and building damage, were first recognised by geotechnical specialists following the dry summer of 1947.
    [Show full text]
  • The Expertise Behind the World's Water and Wastewater Solutions
    The expertise behind the world’S water and wastewater solutionS 60 major cases from around the world Only 2,5 percent of the world’s total water supply is freshwater. Out of that 2,5 percent, 70 percent is contained in glaciers, 29 percent is held in underground aquifers, while freshwater lakes, rivers and streams make up one percent. 2| Innovation throughout the cycle of water Clean water for everyone –that’s our goal. In aworld A small number of companies are developing the of ever growing challenges, ITT delivers innovative necessary range of solutions and applications solutions throughout the cycle of water. We are the knowledge that cover the entire cycle of water use world’s largest provider of water and wastewater and reuse. ITT is at the forefront of this transition. treatment solutions. And we are a leading provider of pumps and related technologies for aindustrial, SETTING THE INDUSTRY STANDARD commercial and municipal customers. Operating in some 140 countries, we manufacture and market a comprehensive range of water and Organizations facing challenging water issues are drainage pumps, units for primary, secondary and increasingly turning to experts who have the breadth tertiary treatment, and products for treating water of capability to own and resolve such challenges. through biological, filtering and disinfection These experts employ holistic solutions that incorporate processes. We also maintain the industry’s most a range of skills encompassing both technical and extensive sales and after-sales organization, with 70 commercial innovation. sales companies operating both locally and globally. CONTENT Water Treatment......................................................................7 Wastewater Treatment ..........................................................19 Water & Wastewater Transport ..............................................31 |3 Every week an estimated 42,000 people die from diseases related to low-quality drinking water and lack of sanitation.
    [Show full text]
  • ELECTORAL REVIEW of SWALE Final Recommendations for Ward
    SHEET 2, MAP 2 Proposed ward boundaries in the north of the Isle of Sheppey THE LOCAL GOVERNMENT BOUNDARY COMMISSION FOR ENGLAND ELECTORAL REVIEW OF SWALE Final recommendations for ward boundaries in the borough of Swale August 2012 Sheet 2 of 3 This map is based upon Ordnance Survey material with the permission of Ordnance Survey on behalf of the Controller of Her Majesty's Stationery Office © Crown copyright. Unauthorised reproduction infringes Crown copyright and may lead to prosecution or civil proceedings. The Local Government Boundary Commission for England GD100049926 2012. KEY BOROUGH COUNCIL BOUNDARY PROPOSED WARD BOUNDARY PARISH BOUNDARY PROPOSED PARISH WARD BOUNDARY SHEERNESS WARD PROPOSED WARD NAME EASTCHURCH CP PARISH NAME MINSTER EAST PARISH WARD PROPOSED PARISH WARD NAME Sheerness Hole Vehicle and Passenger Garrison Point Ferry Terminal Fort COINCIDENT BOUNDARIES ARE SHOWN AS THIN COLOURED LINES SUPERIMPOSED OVER WIDER ONES. y a w d e M r e v i Boat G R AR Basin RIS ON RO AD Scale : 1cm = 0.07600 km Grid interval 1km Es pla na de Sheerness Harbour Estate EET HIGH STR Sheppey College T Trading Estate B S RI H DG AC E R E OA B IN ROAD D BAS GREAT BLUE Station TOWN HIG H S Y TR WA EE OAD AY T BR E W L Car Park IEL BR Catamaran C e m e Yacht Club t e y r S E s Steel Works T A e P R in E ALMA ST G L M I h P N E g I R u Y L I Playing Field ro SHEERNESS T o S L D R b M E Y D n A A A T O e A N e R V R O O E A u Sheerness Harbour Estate E N R Q IN O R E D d IU n E A A R a M A nt P D M R T i A T L o Sea Cadets R S P S W D T A MARINE
    [Show full text]
  • Geology of the London Basin
    Geology of the London Basin - 100 Million Years in the Making on 16 November 2018 Mr Philip Laurie first showed a geological map of London produced in 1848 by Stanford – the first of its kind. The Earth is 46,000 million years old, so much had happened before the London area made an appearance. The geological history of London started a hundred million years ago. For 60% of that time it has been under ice, causing sea levels to fall. He lives near the Ravensbourne, which rises south of the North Downs, runs through them and north to the Thames, emerging at Deptford Creek. How did it, and other rivers such as the Wandle, Darent and Medway, come to flow through the North Downs? At one time it was thought that there were faults in the chalk which gave them a way through, but this has been discounted. The Weald is now low lying, but when tectonic plate movement, mainly caused by Africa colliding with Europe, raised not only the Alps but buckled strata in northern Europe, a Wealden ridge was formed. An underlying chalk stratum buckled with high ridges at the South and North Downs and a dip under the Weald, squeezing up the soft sedimentary rocks between them to form the Ridge. Fast flowing streams from the ridge soon eroded channels in the chalk on their way to the sea. The ridge has since been eroding away (reducing river flows). They are ancient rivers. London is over a layer of cretaceous chalk about 40m down, which in turn is over gault clay.
    [Show full text]
  • Wessex and the Reign of Edmund Ii Ironside
    Chapter 16 Wessex and the Reign of Edmund ii Ironside David McDermott Edmund Ironside, the eldest surviving son of Æthelred ii (‘the Unready’), is an often overlooked political figure. This results primarily from the brevity of his reign, which lasted approximately seven months, from 23 April to 30 November 1016. It could also be said that Edmund’s legacy compares unfavourably with those of his forebears. Unlike other Anglo-Saxon Kings of England whose lon- ger reigns and periods of uninterrupted peace gave them opportunities to leg- islate, renovate the currency or reform the Church, Edmund’s brief rule was dominated by the need to quell initial domestic opposition to his rule, and prevent a determined foreign adversary seizing the throne. Edmund conduct- ed his kingship under demanding circumstances and for his resolute, indefati- gable and mostly successful resistance to Cnut, his career deserves to be dis- cussed and his successes acknowledged. Before discussing the importance of Wessex for Edmund Ironside, it is con- structive, at this stage, to clarify what is meant by ‘Wessex’. It is also fitting to use the definition of the region provided by Barbara Yorke. The core shires of Wessex may be reliably regarded as Devon, Somerset, Dorset, Wiltshire, Berk- shire and Hampshire (including the Isle of Wight).1 Following the victory of the West Saxon King Ecgbert at the battle of Ellendun (Wroughton, Wilts.) in 835, the borders of Wessex expanded, with the counties of Kent, Sussex, Surrey and Essex passing from Mercian to West Saxon control.2 Wessex was not the only region with which Edmund was associated, and nor was he the only king from the royal House of Wessex with connections to other regions.
    [Show full text]
  • A CRITICAL EVALUATION of the LOWER-MIDDLE PALAEOLITHIC ARCHAEOLOGICAL RECORD of the CHALK UPLANDS of NORTHWEST EUROPE Lesley
    A CRITICAL EVALUATION OF THE LOWER-MIDDLE PALAEOLITHIC ARCHAEOLOGICAL RECORD OF THE CHALK UPLANDS OF NORTHWEST EUROPE The Chilterns, Pegsdon, Bedfordshire (photograph L. Blundell) Lesley Blundell UCL Thesis submitted for the degree of PhD September 2019 2 I, Lesley Blundell, confirm that the work presented in this thesis is my own. Where information has been derived from other sources, I confirm that this has been indicated in the thesis. Signed: 3 4 Abstract Our understanding of early human behaviour has always been and continues to be predicated on an archaeological record unevenly distributed in space and time. More than 80% of British Lower-Middle Palaeolithic findspots were discovered during the late 19th/early 20th centuries, the majority from lowland fluvial contexts. Within the British planning process and some academic research, the resultant findspot distributions are taken at face value, with insufficient consideration of possible bias resulting from variables operating on their creation. This leads to areas of landscape outside the river valleys being considered to have only limited archaeological potential. This thesis was conceived as an attempt to analyse the findspot data of the Lower-Middle Palaeolithic record of the Chalk uplands of southeast Britain and northern France within a framework complex enough to allow bias in the formation of findspot distribution patterns and artefact preservation/discovery opportunities to be identified and scrutinised more closely. Taking a dynamic, landscape = record approach, this research explores the potential influence of geomorphology, 19th/early 20th century industrialisation and antiquarian collecting on the creation of the Lower- Middle Palaeolithic record through the opportunities created for artefact preservation and release.
    [Show full text]
  • An Introduction to the Geology and Fossils of Essex
    An Introduction to the Geology and Fossils of Essex The Foundations of Essex The rocks of Essex that were formed before the Ice Age are described as the 'solid' or 'bedrock' geology. Much of the solid geology is concealed beneath unconsolidated sediments laid down during the Ice Age. These Ice Age sediments (sand, gravel etc.) are called 'superficial' or 'drift' deposits. The Oldest Rocks The geological story of Essex starts with rocks that are between 440 and 360 million years old. Dating from the Silurian and Devonian periods these rocks consist of hard, slaty shales, mudstones and sandstones and are over 300 metres below the surface. These rocks have been encountered in boreholes at many places in Essex and they represent a time in the distant past when the first animals were leaving the sea to colonise the land. Similar rocks can be seen at the surface in the Welsh Borderland. Lying on top of these ancient rocks is the Gault, a marly clay from a muddy sea that dates from the middle of the Cretaceous period. This means that, beneath Essex, there is a gap in the geological record that represents about 250 million years and includes the Triassic, Jurassic and early Cretaceous periods. After deposition of the Gault, sand spread into this sea to form a deposit called the Upper Greensand. At this time sea levels were rising leading to widespread flooding of the continents, these are the conditions under which the next rock was formed - the Chalk. The Chalk Chalk is effectively the starting point of our geological story as it is the oldest rock exposed at the surface in our county.
    [Show full text]
  • The Ice Age in North Hertfordshire
    The Ice Age in North Hertfordshire What do we mean by ‘the Ice Age’? Thinking about ‘the Ice Age’ brings up images of tundra, mammoths, Neanderthals and great sheets of ice across the landscape. This simple picture is wrong in many ways. Firstly, there have been many different ‘Ice Ages’ in the history of the earth. The most dramatic happened between 2.4 and 2.1 billion years ago, known as the Huronian Glaciation. About the same time, earth’s atmosphere suddenly became rich in oxygen, and some scientists believe that the atmospheric changes reduced the temperature so much that the whole planet became covered in ice. 1: an Arctic ice sheet (© Youino Joe, USFWS, used under a Creative Commons licence) Another global cover of ice happened 650 million years ago when the first multi-celled animals were evolving. Geologists sometimes refer to this period as the ‘Snowball Earth’ and biologists know it as the Proterozoic. Temperatures were so low that the equator was as cold as present-day Antarctica. They began to rise again as concentrations of carbon dioxide in the atmosphere rose to about 13%, 350 times greater than today. Some carbon dioxide came from volcanic eruptions, but some was excreted by microbial life, which was beginning to diversify and increase in numbers. Neither of these Ice Ages is the one that dominates the popular imagination. Both happened many millions of years before life moved on to land. There were no humans, no mammals, no dinosaurs: none of the creatures familiar from The Flintstones. The period most people think about as the ‘real’ Ice Age is the geologists’ Pleistocene era, from more than two-and-a-half million years ago to the beginning of the Holocene, almost 12,000 years ago.
    [Show full text]
  • Sustainability Appraisal of Draft Local Plan for Lambeth February 2013
    Sustainability Appraisal of Draft Local Plan for Lambeth February 2013 SUSTAINABILITY APPRAISAL: Draft LOCAL PLAN FOR LAMBETH NON-TECHNICAL SUMMARY AND FULL REPORT February 2013 Sustainability Appraisal draft Local Plan for Lambeth February 2013 CONTENTS PAGE PAGE NO. Non-technical Summary iv – xxi 1.0 Introduction 1 Objectives and Structure of the SA Report 2 Equality Impact Assessment 3 Health and Well-being Impact 3 Habitat Regulations Assessment 3 2.0 Lambeth Local Plan 4 3.0 SA/SEA Methodology 5 Relationship to Strategic Environment Assessment 7 Consultation and Approach and Influence of SA to date 8 Assumptions and Difficulties encountered 10 Next Steps 10 4.0 Characterisation and SA Framework 11 SA Framework 14 Tensions between SA Objectives 14 5.0 Likely Significant Effects of the draft Local Plan 24 5A Draft Local Plan Objectives Appraisal 24 5B Spatial Strategy and Reasonable Alternatives 28 5C Policies Appraisal 30 5C1 Crime 34 5C2 Good Health and Reduced Health Inequalities 48 5C3 Access and Services 69 5C4 Infrastructure 82 5C5 Equalities and Diversity 97 5C6 Housing 113 5C7 Liveability and Place 130 5C8 Built and Historic Environment 151 5C9 Transport and Travel 165 5C10 Biodiversity 180 5C11 Climate Change and Energy 190 5C12 Water Resources and Flood Risk 203 5C13 Waste 214 5C14 Air Quality 224 5C15 Education and Skills 232 5C16 & 18 Local Economy and Tacking Worklessness 240 5C17 Regeneration and Efficient Use of Land 254 6.0 Summary and Conclusions 264 The Local Plan 264 Sustainability Effects 266 Conclusion 268 i Sustainability
    [Show full text]
  • Internal Migration, England and Wales: Year Ending June 2015
    Statistical bulletin Internal migration, England and Wales: Year Ending June 2015 Residential moves between local authorities and regions in England and Wales, as well as moves to or from the rest of the UK (Scotland and Northern Ireland). Contact: Release date: Next release: Nicola J White 23 June 2016 June 2017 [email protected] +44 (0)1329 444647 Notice 22 June 2017 From mid-2016 Population Estimates and Internal Migration were combined in one Statistical Bulletin. Page 1 of 16 Table of contents 1. Main points 2. Things you need to know 3. Tell us what you think 4. Moves between local authorities in England and Wales 5. Cross-border moves 6. Characteristics of movers 7. Area 8. International comparisons 9. Where can I find more information? 10. References 11. Background notes Page 2 of 16 1 . Main points There were an estimated 2.85 million residents moving between local authorities in England and Wales between July 2014 and June 2015. This is the same level shown in the previous 12-month period. There were 53,200 moves from England and Wales to Northern Ireland and Scotland, compared with 45,600 from Northern Ireland and Scotland to England and Wales. This means there was a net internal migration loss for England and Wales of 7,600 people. For the total number of internal migration moves the sex ratio is fairly neutral; in the year to June 2015, 1.4 million (48%) of moves were males and 1.5 million (52%) were females. Young adults were most likely to move, with the biggest single peak (those aged 19) reflecting moves to start higher education.
    [Show full text]
  • Treasure Houses of Southern England
    TREASURE HOUSES OF SOUTHERN ENGLAND BEHIND THE SCENES OF THE STATELY HOMES OF ENGLAND MAY 6TH - 15TH 2018 We are pleased to present the fi rst in a two-part series that delves into the tales and traditions of the English aristocracy in the 20th century. The English class system really exists nowhere else in the world, mainly because England has never had the kind of violent social revolution that has taken away the ownership of the land from the families that have ruled it since medieval times. Vast areas of the country are still owned by families that can trace their heritage back to the Norman knights who accompanied William the Conqueror. Here is our invitation to discover how this system has come about and to experience the fabulous legacy that it has BLENHEIM PALACE bequeathed to the nation. We have included a fascinating array of visits, to houses both great and small, private and public, spanning the centuries from the Norman invasion to the Victorian era. This spring, join Discover Europe, and like-minded friends, for a look behind the scenes of TREASURE HOUSES OF SOUTHERN ENGLAND. (Note: Part II, The Treasure Houses of Northern England is scheduled to run in September.) THE COST OF THIS ITINERARY, PER PERSON, DOUBLE OCCUPANCY IS: LAND ONLY (NO AIRFARE INCLUDED): $4580 SINGLE SUPPLEMENT: $ 960 Airfares are available from many U.S. cities. Please call for details. THE FOLLOWING SERVICES ARE INCLUDED: HOTELS: 8 nights’ accommodation in fi rst-class hotels All hotel taxes and service charges included COACHING: All ground transportation as detailed in the itinerary MEALS: Full breakfast daily, 4 dinners GUIDES: Discover Europe tour guide throughout BAGGAGE: Porterage of one large suitcase per person ENTRANCES: Entrance fees to all sites included in the itinerary, including private tours of Waddesdon Manor, Blenheim Palace and Stonor Park (all subject to fi nal availability) Please note that travel insurance is not included on this tour.
    [Show full text]