Scheme Assessment Report Volume 2 Appendices
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Dartford Antiquities
http://kentarchaeology.org.uk/research/archaeologia-cantiana/ Kent Archaeological Society is a registered charity number 223382 © 2017 Kent Archaeological Society ( 304 ) DAETFOED ANTIQUITIES. NOTES ON BEITISH EOMAN AND SAXON EEMAINS THEBE EOUND. BY E. C. J. SPURRELL. STONE IMPLEMENTS. WHEN the Kent Archaeological Society met at Dartford, in 1868, the knowledge and study of the more ancient stone implements was in an early stage; almost in its infancy, being, so far as this country was concerned, barely ten years old. And as those stone implements were not commonly accepted as the work of man, they were looked upon doubtfully by the old antiquary: and because one class of them came out of deep cuttings in the ground, and from stalagmite caverns, they were left to geologists as " fossils; " regarding that word as dismissing the matter into the domain of geology. Yet, for all that, the recognition of the earliest palaeolithic implements, as human workmanship is due to Englishmen's acumen; and although the study was revived in Erance, it was consolidated into a science by the investigation of Englishmen once agaim In our own district, that is, about ten miles round Dartford, quite as much attention has been paid to the matter as in any spot in the world, and with a greater success than anywhere else in determin- ing certain controverted points; such as the reality of human agency in the formation of implements, and the larger grasp of the subject consequent on the minute search which has traced them continuously through a greater range in elevation and consequently of age. -
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. -
Shorne Woods Country Park Management Plan 2015-2020
MANAGEMENT PLAN 2015-2020 KENT COUNTY COUNCIL Shorne Woods Country Park Management Plan 2015-2020 Updated: November 2018 by Tim Bell- Head Ranger 851561 – SHORNE WOODS COUNTRY PARK 1 MANAGEMENT PLAN 2015-2020 KENT COUNTY COUNCIL 1 EXECUTIVE SUMMARY .............................................................................. 5 1.1 BACKGROUND INFORMATION ............................................................. 5 1.2 VISION FOR THE SITE ........................................................................ 6 1.3 CONSERVATION MANAGEMENT .......................................................... 6 1.4 HERITAGE MANAGEMENT .................................................................. 9 1.5 VISITOR MANAGEMENT ....................................................................11 1.6 EDUCATION .....................................................................................12 1.7 SITE MAINTENANCE .........................................................................12 1.8 HEALTH AND SAFETY .......................................................................13 1.9 COMMUNITY INVOLVEMENT ...............................................................15 1.10 FINANCIAL OVERVIEW ......................................................................17 2 BACKGROUND INFORMATION .............................................................. 19 2.1 LOCATION AND SITE DESCRIPTION ....................................................19 2.1.1 Contact Details ...........................................................................19 -
K E N T a Rc H a E O Lo G I C a L S O C I E
KE N T ARC H A E O LO G I C A L SO C I E T Y nnIssue numberee 67 wwss ll ee tt tt ee Winter r2005/6r Inside 2-3 KURG Library Notes GOING UNDERGROUND Tebbutt Research Grants KHBCRequire Recruits Letters to the Editor 4-5 What’s on 6-7 What’s on Happy Birthday CAT CATKITS 8-9 Notice Board 10-11 Bee Boles Cattle Droving 12-13 Wye Rural Museum YACActivities 14-15 Thanet Pipeline Microfilm Med Records New Books 16 Hunt the Saxons THE KENT UNDERGROUND RESEARCH GROUP HAVE SURVEYED SITES THROUGHOUT THE COUNTY FROM ROMAN WELLS TO WORLD WAR TWO BUNKERS www.kentarchaeology.org.uk KE N T UN D E R G R O U N D RE S E A R C H GR O U P URG is an affiliated group of the KAS. We are mining historians – a unique blend of unlikely Kopposites. We are primarily archaeologists and carry out academic research into the history of underground features and associated industries. To do this, however, we must be practical and thus have the expertise to carry out exploration and sur- veying of disused mines. Such places are often more dangerous than natural caverns, but our members have many years experience of such exploration. Unlike other mining areas, the South East has few readily available records of the mines. Such records as do exist are often found in the most unlikely places and the tracing of archival sources is an ongoing operation. A record of mining sites is maintained and constantly updated as further sites are discovered. -
Capital Space Ltd Land South of Coldharbour Road, Gravesend
Capital Space Ltd Land South of Coldharbour Road, Gravesend Transport Assessment July 2016 Gravesham Borough Council Contents 1 INTRODUCTION .................................................................................................. 1 2 SITE AND LOCAL AREA ........................................................................................ 2 Site Location ....................................................................................................... 2 Local Road Network ............................................................................................ 2 Public Transport .................................................................................................. 3 3 POLICY ................................................................................................................ 4 National Planning Policy Framework .................................................................. 4 Supplementary Planning Guidance SPG 4 Kent Vehicle Parking Standards (July 2006) ................................................................................................................... 4 Gravesham Local Plan Core Strategy (September 2014) ................................... 5 4 BASELINE CONDITIONS ..................................................................................... 6 Existing Traffic Conditions .................................................................................. 6 5 PROPOSED DEVELOPMENT ................................................................................. 7 Overview -
Provisional Checklist and Account of the Mammals of the London Borough of Bexley
PROVISIONAL CHECKLIST AND ACCOUNT OF THE MAMMALS OF THE LONDON BOROUGH OF BEXLEY Compiled by Chris Rose BSc (Hons), MSc. 4th edition. December 2016. Photo: Donna Zimmer INTRODUCTION WHY PROVISIONAL? Bexley’s mammal fauna would appear to be little studied, at least in any systematic way, and its distribution is incompletely known. It would therefore be premature to suggest that this paper contains a definitive list of species and an accurate representation of their actual abundance and geographical range in the Borough. It is hoped, instead, that by publishing and then occasionally updating a ‘provisional list’ which pulls together as much currently available information as can readily be found, it will stimulate others to help start filling in the gaps, even in a casual way, by submitting records of whatever wild mammals they see in our area. For this reason the status of species not thought to currently occur, or which are no longer found in Bexley, is also given. Mammals are less easy to study than some other groups of species, often being small, nocturnal and thus inconspicuous. Detecting equipment is needed for the proper study of Bats. Training in the live-trapping of small mammals is recommended before embarking on such a course of action, and because Shrews are protected in this regard, a special licence should be obtained first in case any are caught. Suitable traps need to be purchased. Dissection of Owl pellets and the identification of field signs such as Water Vole droppings can help fill in some of the gaps. Perhaps this document will be picked up by local students who may be looking for a project to do as part of their coursework, and who will be able to overcome these obstacles. -
Geology of London, UK
Geology of London, UK Katherine R. Royse1, Mike de Freitas2,3, William G. Burgess4, John Cosgrove5, Richard C. Ghail3, Phil Gibbard6, Chris King7, Ursula Lawrence8, Rory N. Mortimore9, Hugh Owen10, Jackie Skipper 11, 1. British Geological Survey, Keyworth, Nottingham, NG12 5GG, UK. [email protected] 2. Imperial College London SW72AZ, UK & First Steps Ltd, Unit 17 Hurlingham Studios, London SW6 3PA, UK. 3. Department of Civil and Environmental Engineering, Imperial College London, London, SW7 2AZ, UK. 4. Department of Geological Sciences, University College London, WC1E 6BT, UK. 5. Department of Earth Science and Engineering, Imperial College London, London, SW7 2AZ, UK. 6. Cambridge Quaternary, Department of Geography, University of Cambridge CB2 3EN, UK. 7. 16A Park Road, Bridport, Dorset 8. Crossrail Ltd. 25 Canada Square, Canary Wharf, London, E14 5LQ, UK. 9. University of Brighton & ChalkRock Ltd, 32 Prince Edwards Road, Lewes, BN7 1BE, UK. 10. Department of Palaeontology, The Natural History Museum, Cromwell Road, London SW7 5BD, UK. 11. Geotechnical Consulting Group (GCG), 52A Cromwell Road, London SW7 5BE, UK. Abstract The population of London is around 7 million. The infrastructure to support this makes London one of the most intensively investigated areas of upper crust. however construction work in London continues to reveal the presence of unexpected ground conditions. These have been discovered in isolation and often recorded with no further work to explain them. There is a scientific, industrial and commercial need to refine the geological framework for London and its surrounding area. This paper reviews the geological setting of London as it is understood at present, and outlines the issues that current research is attempting to resolve. -
June 2021 103 Last Word - a View from the Field from CPM’S Technical Editor
£3.99 In this issue... Cereals Event returns page 62 Climate positive page 80 Full details and innovations to build back better Excited for opportunities on the carbon journey Crop Doctor page 8 Rethink on blight page 89 Opinion 4 Talking Tilth - A word from the editor. Volume 23 Number 7 6 Smith’s Soapbox - Views and opinions from an Essex peasant….. June 2021 103 Last Word - A view from the field from CPM’s technical editor. Tech Respect returns next issue. Technical 8 Crop Doctor - Septoria low at T2 As flag leaves emerge, Crop Doctor travels from west to east to assess disease. 14 Diagnostics - Instant intelligence Most farms are generating big data but how to interpret it isn’t always clear. 20 Inside traits - Step-on in wheat choice Four new Group 3 varieties may have added a new dimension. 24 Better buying, better selling - Little steps to a potential big profit Doing the little things could make oilseed rape a big earner. 30 Forward-thinking farmers - A crop you can rely on One Suffolk arable business has an OSR system with dependable genetics. 36 Insiders View - A new matrix… A new Clearfield candidate looks like it could change the game for growers. Editor Tom Allen-Stevens 40 Fit for the Future - Traits of success Technical editor KWS’ latest BYDV-tolerant variety looks set to play an important role. Lucy de la Pasture 44 Rotational Resilience - A conventional approach Machinery editor New barleys look to be snapping at the heels of their hybrid counterparts. Charlotte Cunningham Writers 48 Insiders View - Yields to rival the rest A new offering from Senova represents a step-on in barley. -
Outline • Background
Outline • Background Case Study 1 • Landslide Debris (Dorset) Case Study 2 • Engineering NIR Stratigraphy (Hampshire) Case Study 3 • Weathering - London Clay (London) NIR Spectroscopy Background to NIR NIR Thermal Range Spectral Logging • Visible, NIR, SWIR Wavelengths (350-2500nm) • Spectral resolution 1nm • Measurement window 4-24 mm • Limited/no sample contact • No sample prep needed – (lab samples can be crushed) • Measurement time 0.05 secs Spectral Logging Sensitive to most minerals but especially clays Biggest applications: • Mining – mineral exploration • Heritage Conservation (as non contact) • Pharmaceuticals • Biscuits Typical XRD plot for London Clay Typical Lab Spectra • Sensitive to moisture, mineralogy, clay content, organics, plant health, particulate contaminants......... • Relate to weathering, water movement, vegetation growth Dark Clay Orange Sand 0 2500 nm 0 2500 nm Landslide Debris Particle Size Characterization Upper Group Lower Group Intermediate Group Particle Size Characterization • Possible to predict article composition from 2-3 wavelengths e.g. % clay =130.3-82.754*R(λ 2204 ) +937.388 R(λ 1411 ) Moisture Content Next Steps • Black Venn Study: debris flow mobility – does the mixing of debris flow materials relate to how mobile it is? Debris flow mechanics. • China Bailong Corridor (Zhouqu Debris Flow – Lanzhou Uni): properties of source materials with debris flow mobility. Current Research Projects: Engineering NIR Stratigraphy London Clay (Hampshire Basin) White Cliff Bay - Isle of Wight White Cliff Bay Geological -
Download File 3
REPRESENTATIONS TO MEDWAY COUNCIL LOCAL PLAN 2012 – 2035 Development Options Consultation Document Submitted on Behalf of The Landowners April 2017 REPRESENTATIONS TO MEDWAY COUNCIL LOCAL PLAN 2012 – 2035 Development Options Consultation Document Submitted on Behalf of The Landowners Project Ref: 25973/A5/JM/kf Status: Final Issue/Rev: 01 Date: 03 April 2017 Prepared by: Joshua Mellor Checked by: Andrew Wilford Authorised by: Andrew Wilford Barton Willmore LLP The Observatory Southfleet Road Ebbsfleet Dartford Kent DA10 0DF Tel: Ref: 25973/A5/JM/kf E-mail: Date: 03 April 2017 COPYRIGHT The contents of this document must not be copied or reproduced in whole or in part without the written consent of the Barton Willmore LLP. All Barton Willmore stationery is produced using recycled or FSC paper and vegetable oil based inks. CONTENTS PAGE NO. 1.0 INTRODUCTION 01 2.0 NATIONAL PLANNING POLICY 03 i) National Policy & Plan Making 03 ii) National Policy & Housing Need 05 iii) Duty to Co-operate 05 iv) The Housing White Paper – Fixing Our Broken Housing Market (February 2017) 06 3.0 VISION AND STRATEGIC OBJECTIVES 07 4.0 DELIVERING SUSTAINABLE DEVELOPMENT - OPTIONS 08 i) Objectively Assessed Need 08 ii) Identified Supply of Development Land 08 iii) Options for Growth 09 5.0 LAND SOUTH OF SUNDRIDGE HILL, CUXTON 12 i) Site Suitability - Overall 19 6.0 CONCLUSIONS 21 APPENDICES Appendix 1: Sundridge Hill, Cuxton Location Plan. Appendix 2: Land South of Sundridge Hill – Site Proforma (Medway Council, November 2015). Appendix 3: Accessibility Appraisal (dha transport, March 2017). Appendix 4: Preliminary Ecological Appraisal (KB Ecology, March 2017). -
A Research Framework for the Archaeology of the Extractive Industries
A RESEARCH FRAMEWORK FOR THE ARCHAEOLOGY OF THE EXTRACTIVE INDUSTRIES BIBLIOGRAPHY FOR CHALK EXTRACTION GENERAL Hayes, J W (Rev) 1909 ‘Deneholes and other chalk excavations: their origin and uses’ J Roy Anthropol Inst 39, 44-76 Smith, C J 1980 The Ecology of the English Chalk. Academic Press [includes economic aspects] BERKSHIRE Anon 1970 (no title) Newbury Weekly News 28/8/1970 Anon (nd) M4 Motorway Construction Report, Appendix 1 Underground voids at Furzehill (unpub report) Gray, R and Griffiths, S 1987 The Book of Wargrave. Wimpey Laboratories 1984 Chalk Mine at Lawrence Mead, Kintbury. Report on inspection and proposals for investigation. DORSET Woodward, P J 1987 ‘Romano-British industries in Purbeck: excavations at Norden by Nigel Sunter….’ Dorset Natur Hist Archaeol Soc Monograph Series 6 ESSEX Caiger, N 1976 ‘Caves in South London’ London Archaeol 3, 131-5 [chalk extraction of 'Kentish denehole' type] Chapman, D I and Hammond, P M 1962 ‘A Preliminary Report on Investigation in the Denehole at Hangman's Wood’ Essex Nature 31,11 Clift, J G N 1908 ‘A Criticism of the Hangman’s Wood Denehole Report’ J Brit Archaeol Ass 14, 101-129 Holmes, T V (nd) ‘Denehole at Gravesend’ Essex Nature 15, HERTFORDSHIRE Anon (CSS) 1990 Underground sites. Andrews, R T 1906 ‘Cave Gate, Anstey’ Trans E Herts Archaeol Soc 3.2, 217-19. [Chalk pit and site of shaft, Cave gate Wyddial: Includes plans, section] Anon (CSS) 1986 Caves and tunnels in SE England. 6.14, 50 [Chadwell chalk and flint mine] Fisher, J F & Walsh, J M 1944 ‘An investigation into chalk mining, with reference to a shaft near Kings Langley’ Trans Herts Nat Hist Soc 22.2, 48-51. -
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.