The State of England's Chalk Streams
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Solent & South Downs Fish Monitoring Report 2015
Solent & South Downs fish monitoring report 2015 We are the Environment Agency. We protect and improve the environment and make it a better place for people and wildlife. We operate at the place where environmental change has its greatest impact on people’s lives. We reduce the risks to people and properties from flooding; make sure there is enough water for people and wildlife; protect and improve air, land and water quality and apply the environmental standards within which industry can operate. Acting to reduce climate change and helping people and wildlife adapt to its consequences are at the heart of all that we do. We cannot do this alone. We work closely with a wide range of partners including government, business, local authorities, other agencies, civil society groups and the communities we serve. Authors: P. Rudd & L. Swift Published by: Environment Agency Further copies of this report are available Horizon house, Deanery Road, from our publications catalogue: Bristol BS1 5AH www.gov.uk/government/publications Email: [email protected] or our National Customer Contact Centre: www.gov.uk/environment-agency T: 03708 506506 Email: [email protected]. © Environment Agency 2014 All rights reserved. This document may be reproduced with prior permission of the Environment Agency. 2 of 77 Foreword Welcome to the annual fish report for the Solent and South Downs area for 2015. This report covers all of the fisheries surveys we have carried out in Hampshire and West & East Sussex in 2015 and is the ninth annual report we have produced in succession. -
A Valuation of the Chichester Harbour Provisioning Ecosystem Services Provided by Shellfish
Rpep A valuation of the Chichester Harbour Provisioning Ecosystem Services provided by shellfish Report for Sussex IFCA and the Environment Agency Title: A valuation of the Chichester Harbour Provisioning Ecosystem Services provided by shellfish Date: January 25th 2018 Authors: Chris Williams, William Davies and Jake Kuyer Client: Sussex Inshore Fisheries and Conservation Authority (SxIFCA) NEF Consulting is the consultancy arm of the leading UK think tank, New Economics Foundation. We help to put new economic ideas into practice. TheNew content Economicss of this report Foundation can be shared isfreely the within UK’s the only organisation people named-powered above as think the client tank.. However, please contact us if you would like to publish the report, or extracts from the report, on a websiteThe Foundation or in any other way.works Unless to explicitlybuild a agreed new otherwise,economy all where publishing people rights remainreally with take NEFcontrol. Consulting. NEF Consulting Limited New Economics Foundation 10 Salamanca Place London SE1 7HB www.nefconsulting.com Tel: 020 7820 6361 [icon] Contents 1. Background and context …………………………………………………………………….…4 Chichester harbour ...................................................................................................................... 5 Conservation significance and status ........................................................................................ 5 Shellfishery context ..................................................................................................................... -
The Lithostratigraphy and Biostratigraphy of the Chalk Group (Upper Coniacian 1 to Upper Campanian) at Scratchell’S Bay and Alum Bay, Isle of Wight, UK
Manuscript Click here to view linked References The lithostratigraphy and biostratigraphy of the Chalk Group (Upper Coniacian 1 to Upper Campanian) at Scratchell’s Bay and Alum Bay, Isle of Wight, UK. 2 3 Peter Hopson1*, Andrew Farrant1, Ian Wilkinson1, Mark Woods1 , Sev Kender1 4 2 5 and Sofie Jehle , 6 7 1 British Geological Survey, Sir Kingsley Dunham Centre, Nottingham, NG12 8 5GG. 9 2 10 University of Tübingen, Sigwartstraße 10, 72074 Tübingen, Germany 11 12 * corresponding author [email protected] 13 14 Keywords: Cretaceous, Isle of Wight, Chalk, lithostratigraphy, biostratigraphy, 15 16 17 Abstract 18 19 The Scratchell‟s Bay and southern Alum Bay sections, in the extreme west of the Isle 20 21 of Wight on the Needles promontory, cover the stratigraphically highest Chalk Group 22 formations available in southern England. They are relatively inaccessible, other than 23 by boat, and despite being a virtually unbroken succession they have not received the 24 attention afforded to the Whitecliff GCR (Geological Conservation Review series) 25 site at the eastern extremity of the island. A detailed account of the lithostratigraphy 26 27 of the strata in Scratchell‟s Bay is presented and integrated with macro and micro 28 biostratigraphical results for each formation present. Comparisons are made with 29 earlier work to provide a comprehensive description of the Seaford Chalk, Newhaven 30 Chalk, Culver Chalk and Portsdown Chalk formations for the Needles promontory. 31 32 33 The strata described are correlated with those seen in the Culver Down Cliffs – 34 Whitecliff Bay at the eastern end of the island that form the Whitecliff GCR site. -
Downe Cottage, York Road, Little Driffield
EPC GOES HERE £169,950 Downe cottage, SERVICES Mains water and electricity and drainage are all connected to the property. Central heating is York Road, from a gas-fired boiler. TENURE The property is held under freehold title with Little Driffield vacant possession on completion. COUNCIL TAX Council Tax is payable to the East Riding of Yorkshire Council. The property is shown on the Council Tax Property Bandings List in Valuation Band ‘A’. VIEWING Strictly by appointment with the sole agents on 01377 241919. FREE VALUATION If you are looking to sell your own property, we will be very happy to provide you with a free, no obligation market appraisal and valuation. We offer very competitive fees and an outstanding personal service that is rated 5 star by our fully verified past clients. 56 Market Place, Driffield | 01377 241919 | www.dee-atkinson-harrison.co.uk Disclaimer: Dee Atkinson & Harrison for themselves and for the vendors or lessors of this property, whose Agents they are, give notice that these particulars are produced in good faith, are set out as a general guide only and do not constitute any part of a Contract. No person in the employment of Dee Atkinson & Harrison has any authority to make any representation or warranty whatever in relation to this property. THE ACCOMMODATION COMPRISES OUTSIDE All ON THE GROUND FLOOR Regardless of the property light to the rear and are approached via a pedestrian right of access over the ENTRANCE HALL neighbouring property or through the bungalow. The With single radiator, thermostat for the central heating garden is designed for low maintenance and includes a and telephone point. -
2018-09-14 RHMC Marine Director and Harbour Master's Report and Current Issues
HAMPSHIRE COUNTY COUNCIL Report Committee: River Hamble Harbour Management Committee Date: 24 June 2021 Title: Marine Director and Harbour Master's Report and Current Issues Report From: Director of Culture, Communities and Business Services Contact name: Jason Scott Tel: 01489 576387 Email: [email protected] Purpose of this Report 1. The purpose of this report is to record formally RHHA patrol operations and inform the Duty Holder of significant events and trends having a bearing on the Marine Safety Management System. Recommendation 2. It is recommended that the River Hamble Harbour Management Committee supports the contents of this report to the Harbour Board. Executive Summary 3. This report summarises the incidents and events which have taken place in the Harbour and addresses any issues currently under consideration by the Harbour Master. Contextual Information Patrols 4. The Harbour has been patrolled by the Duty Harbour Master at various times between 0700 and 2230 daily. Mooring and pontoon checks have been conducted daily throughout the period. Issues 6. 6 Monthly Audit by the Designated Person of the Marine Safety Management System – The MSMS was audited by the RHHA Designated Person on 18 May. As part of our drive for continuous improvement, a number of new initiatives will be pursued to ensure that River Users are informed better of trends in the River and also, in so doing, reminded of the Bye Laws. The Designated Person has affirmed continued compliance with the Port Marine Safety Code. 7. Annual Trinity House Audit – An officer of Trinity House conducted an annual light inspection on 22 March to confirm compliance with the River Hamble Harbour Authority’s status as a Local Lighthouse Authority. -
Appendix 5 Defining Reference Conditions for Chalk Stream and Fenland Natural Channels
Appendix 5 Defining reference conditions for chalk stream and Fenland natural channels Chalk stream geomorphology is poorly understood, and under-researched. What studies exist appear to confirm that the majority of UK and European chalk streams have been modified in form and hydraulics by a long history of river management (Sear and others 1999, WRc 2000). The overriding control these modifications exert on the geomorphology and processes operating within the channel, make it difficult to establish what features and physical habitat diversity a natural, unmodified chalk stream should display. In the absence of semi-natural chalk stream habitats from which reference conditions can be determined, the Water Framework Directive specifies the use of palaeoecological information (Logan and Furze 2002). However much of this research is focussed on interpretations of human activity or climatic reconstruction rather than on the specific determination of river form and associated habitats (Davies and Griffiths 2005; French and Lewis 2002). Despite this, it is possible to reconstruct some information of relevance to characterising the floodplain habitats associated with relatively undisturbed chalk streams and rivers. French and others 2005 report a complex suite of landscape changes in the Dry valley and upper reaches of a chalk stream in Dorset. Their results suggest the presence of a relatively wide shallow low sinuosity meandering channel throughout the Holocene into the early historic period, between 30 - 50m in width and 1.5 – 3m in depth with a width:depth ratio of between 10 and 33. The authors stress that the development of each chalk valley is best considered individually rather than to expect a common history of landscape evolution hence the precise form of the channel system and floodplain habitats is also likely to be valley specific. -
Definition of Chalk
1.1: Introduction: 1.1.1: Definition of chalk: Chalk is a soft, white, porous sedimentary carbonate rock, a form of limestone composed of the mineral calcite. Calcite is calcium carbonate or CaCO3. It forms under reasonably deep marine conditions from the gradual accumulation of minute calcite shells (coccoliths) shed from micro-organisms called coccolithophores. Flint (a type of chert unique to chalk) is very common as bands parallel to the bedding or as nodules embedded in chalk. It is probably derived from sponge spicules or other siliceous organisms as water is expelled upwards during compaction. Flint is often deposited around larger fossils such as Echinoidea which may be silicified (i.e. replaced molecule by molecule by flint). Chalk as seen in Cretaceous deposits of Western Europe is unusual among sedimentary limestone in the thickness of the beds. Most cliffs of chalk have very few obvious bedding planes unlike most thick sequences of limestone such as the Carboniferous Limestone or the Jurassic oolitic limestones. This presumably indicates very stable conditions over tens of millions of years. Figure (1-1): Calcium sulphate 1 "Nitzana Chalk curves" situated at Western Negev, Israel are chalk deposits formed at the Mesozoic era's Tethys Ocean Chalk has greater resistance to weathering and slumping than the clays with which it is usually associated, thus forming tall steep cliffs where chalk ridges meet the sea. Chalk hills, known as chalk downland, usually form where bands of chalk reach the surface at an angle, so forming a scarp slope. Because chalk is well jointed it can hold a large volume of ground water, providing a natural reservoir that releases water slowly through dry seasons. -
South East River Basin District Flood Risk Management Plan 2015 - 2021 PART B: Sub Areas in the South East River Basin District
South East River Basin District Flood Risk Management Plan 2015 - 2021 PART B: Sub Areas in the South East river basin district March 2016 Published by: Environment Agency Further copies of this report are available Horizon house, Deanery Road, from our publications catalogue: Bristol BS1 5AH www.gov.uk/government/publications Email: [email protected] or our National Customer Contact Centre: www.gov.uk/environment-agency T: 03708 506506 Email: [email protected]. © Environment Agency 2016 All rights reserved. This document may be reproduced with prior permission of the Environment Agency. Contents Glossary and abbreviations ......................................................................................................... 5 The layout of this document ........................................................................................................ 7 1 Sub-areas in the South East river basin district .............................................................. 9 Introduction ................................................................................................................................. 9 Flood Risk Areas ......................................................................................................................... 9 Management catchments ............................................................................................................ 9 2 Conclusions, objectives and measures to manage risk for the Brighton and Hove Flood Risk Area.......................................................................................................................... -
7714 the London Gazette, 26 November, 1929
7714 THE LONDON GAZETTE, 26 NOVEMBER, 1929. his office at Stoneleigh, and as relates to the Advertiser and the Burnley News of the 20th Parish of Willenhall with the Chairman of and 27th November instant. the Parish Meeting of that parish at his Dated this 25th day of November, 1929. residence at Willenhall. ' Printed copies of the Bill for the intended COLIN CAMPBELL, Town Clerk, Burnley. Act will be deposited in the Committee and SEARPE, PRITCHARD AND Co., Palace Private Bill Office of the House of Commons Chambers, Bridge Street, Westminster,. on or before the 17th day of December next, (188) S.W. 1; Parliamentary Agents. and on and after the 21st day of December next a copy of the Bill may be inspected and copies obtained at the price of three shillings and sixpence each at the office of the under- In Parliament.—Session 1929-30. mentioned Town Clerk, and copies may also be obtained at the said price at the offices of KINGSTON UPON HULL CORPORATION. the undermentioned Parliamentary Agents. OTICE is hereby given that application is. A Notice stating the objects of the intended N intended (to toe made to Parliament in application has been and will be published in the Session 1929-30 by the Lord Mayor Alder- full in the Midland Daily Telegraph on the men and Citizens of the City and County of 20th 'and 27th days of November instant. Kingston upon Hull (hereinafter called " the Dated this 25th day of November 1929. Corporation ") for an Act of which the prin- cipal subject matters are as follows: — FREDERICK SMITH, Town Clerk, 1. -
Flood Risk from Groundwater: Examples from a Chalk Catchment in 2 Southern England 3 4 A.G
1 Flood risk from groundwater: examples from a Chalk catchment in 2 southern England 3 4 A.G. Hughes1, T. Vounaki1, D.W. Peach1, A.M. Ireson2, C.R. Jackson1, A.P. Butler2, J.P. Bloomfield3, 5 J. Finch4 and H.S. Wheater2 6 1 British Geological Survey, Keyworth, Nottinghamshire, UK 7 2 Department of Civil and Environmental Engineering, Imperial College London, London, UK 8 3 British Geological Survey, Wallingford, Oxfordshire, UK 9 4 Centre for Ecology and Hydrology, Wallingford, Oxfordshire, UK 10 11 12 13 14 Correspondence Abstract A.G. Hughes, British Geological Survey, 15 Groundwater flooding has moved up the policy-makers’ agenda as a result of the 16 Keyworth, Nottinghamshire, UK Email: [email protected] United Kingdom experiencing extensive groundwater flooding in winter 2000/ 17 2001. However, there is a lack of appropriate methods and data to support 18 DOI:10.1111/j.1753-318X.2011.01095.x groundwater flood risk assessment. The implications for flood risk assessment of 19 groundwater flooding are outlined using a study of the Chalk aquifer underlying 20 Key words the Pang and Lambourn catchments in Berkshire, UK. Groundwater flooding in 21 Q2 ’; ’; ’. the Chalk results from the water table reaching the land surface and producing 22 long-duration surface flows (weeks to months), causing significant disruption to 23 transport infrastructure and households. By analyzing existing data with a farmers’ 24 survey, it was found that groundwater flooding consists of a combination of 25 intermittent stream discharge and anomalous springflow. This work shows that 26 there is a significant challenge involved in drawing together data and under- 27 standing of groundwater flooding, which includes vital local knowledge, reason- 28 able risk assessment procedures and deterministic modelling. -
Rainfall Thresholds for Flow Generation in Desert Ephemeral
Water Resources Research RESEARCH ARTICLE Rainfall Thresholds for Flow Generation 10.1029/2018WR023714 in Desert Ephemeral Streams 1 1 2 1 Key Points: Stephanie K. Kampf G!), Joshua Faulconer , Jeremy R. Shaw G!), Michael Lefsky , Rainfall thresholds predict 3 2 streamflow responses with high Joseph W. Wagenbrenner G!), and David J. Cooper G!) accuracy in small hyperarid and 1 2 semiarid watersheds Department of Ecosystem Science and Sustainability, Colorado State University, Fort Collins, Colorado, USA, Department 3 Using insufficient rain data usually of Forest and Rangeland Stewardship, Colorado State University, FortCollins, Colorado, USA, USDA Forest Service, Pacific increases threshold values for larger Southwest Research Station, Arcata, California,USA watersheds, leading to apparent scale dependence in thresholds Declines in flow frequency and Rainfall thresholds for streamflow generation are commonly mentioned in the literature, but increases in thresholds with drainage Abstract area are steeper in hyperarid than in studies rarely include methods for quantifying and comparing thresholds. This paper quantifies thresholds semiarid watersheds in ephemeral streams and evaluates how they are affected by rainfall and watershed properties. The study sites are in southern Arizona, USA; one is hyperarid and the other is semiarid. At both sites rainfall and 3 2 2 Supporting Information: streamflow were monitored in watersheds ranging from 10- to 10 km . Streams flowed an average of 0-5 • Supporting Information 51 times per year in hyperarid watersheds and 3-11 times per year in semiarid watersheds. Although hyperarid sites had fewer flow events, their flow frequency (fraction of rain events causing flow) was higher than in Correspondence to: 2 semiarid sites for small ( < 1 km ) watersheds. -
Parish/Town Area Vacant Seats Base Expenses Expenditure Electorate
Parish/Town Area Vacant Seats Base Expenses Expenditure Electorate Total Expenditure Grand Total per Elector per Elector Abbotsbury 4 740 £0.06 346 £20.76 £760.76 Affpuddle and Turnerspuddle 9 740 £0.06 379 £22.74 £762.74 Alderholt 9 740 £0.06 2523 £151.38 £891.38 Allington 7 740 £0.06 693 £41.58 £781.58 Alton Pancras 2 740 £0.06 132 £7.92 £747.92 Anderson 1 740 £0.06 75 £4.50 £744.50 Arne 8 740 £0.06 1098 £65.88 £805.88 Ashmore 7 740 £0.06 159 £9.54 £749.54 Athelhampton 2 740 £0.06 29 £1.74 £741.74 Batcombe 2 740 £0.06 83 £4.98 £744.98 Beaminster 11 740 £0.06 2589 £155.34 £895.34 Beer Hackett 3 740 £0.06 81 £4.86 £744.86 Bere Regis 11 740 £0.06 1346 £80.76 £820.76 Bettiscombe 2 740 £0.06 50 £3.00 £743.00 Bincombe 3 740 £0.06 78 £4.68 £744.68 Bishop`s Caundle 7 740 £0.06 329 £19.74 £759.74 Blandford Badbury Heights 1 740 £0.06 906 £54.36 £794.36 Blandford Central 6 740 £0.06 3220 £193.20 £933.20 Blandford Hilltop 2 740 £0.06 731 £43.86 £783.86 Blandford Langton St Leonards 4 740 £0.06 1604 £96.24 £836.24 Blandford Old Town 3 740 £0.06 1596 £95.76 £835.76 Blandford St Mary 7 740 £0.06 1152 £69.12 £809.12 Bothenhampton - Bothenhampton 6 740 £0.06 1299 £77.94 £817.94 Bothenhampton - Walditch 3 740 £0.06 534 £32.04 £772.04 Bourton 9 740 £0.06 707 £42.42 £782.42 Bradford Abbas 7 740 £0.06 765 £45.90 £785.90 Bradford Peverell 7 740 £0.06 323 £19.38 £759.38 Bradpole - Bradpole Village 9 740 £0.06 1712 £102.72 £842.72 Bradpole - Claremont 1 740 £0.06 243 £14.58 £754.58 Bridport North 9 740 £0.06 3541 £212.46 £952.46 Bridport South 9 740 £0.06