87. East Anglian Chalk Area Profile: Supporting Documents
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Lent Term 2007
CAMBRIDGE UNIVERSITY RAMBLING CLUB Lent Term 2007 Welcome back to the Rambling Club. Once again, we invite you to leave the city for a few hours this term, and enjoy the surrounding countryside with us. The pace of our walks is generally easy, as our main aim is to relax and appreciate the local scenery and villages, and we have tried to provide a mixture of walks of different lengths. We usually stop at a village pub en route, but you should bring a packed lunch and a drink anyway as occasionally a walk doesn’t pass a pub, or we find that a pub is closed. Strong boots and waterproof clothing are also recommended. Your only expense is the bus or train fare (given below), plus our £1 annual membership fee. There is no need to sign up in advance to join any of this term’s walks – just turn up at the time and place given. Our meeting points are: Bus/Coach: At the corner of Drummer Street and Emmanuel Street. Train: In the main hall of Cambridge Railway Station. Saturday 20th January: "Swanning around Swavesey" Swavesey Circular 9 miles Contact: Steven For the first walk of term we head to the village of Swavesey, situated close to the River Ouse about 10 miles north-west of Cambridge. From here we'll explore the lakes and waterways of the nearby Fen Drayton Nature Reserve before visiting the village of Fenstanton. After lunch we'll walk along part of the River Ouse on our way back towards Swavesey for the bus home. -
164 Chrishall and Elmdon & Wenden Lofts – 4.5 Miles (7 Kms)
The Hundred Parishes Circular Walks – number 164 Chrishall and Elmdon & Wenden Lofts – 4.5 miles (7 kms) This walk explores parts of two adjacent parishes, mostly on good paths although some stretches can be muddy at times. There are several stiles. The route offers extensive views over unspoilt countryside. It passes two parish churches and a pub so please be prepared, before entering, to either remove muddy boots or wear boot covers or plastic bags. The route passes The Red Cow pub towards the end; if relying on it for refreshment, please check opening times. There are several seats beside the route as it passes through Elmdon. Start and finish: The walk starts from the car park beside Holy Trinity Church, Chrishall. The entrance is from Bury Lane, on the right about ¼ mile north of B1039. Walkers are welcome to use the car park and are encouraged to make a donation just inside the church porch. Ordnance Survey Grid Reference: TL451386 - Postcode: SG8 8QY. The route can be followed on Ordnance Survey Explorer Map 194. A diagram of the route is provided at the end of the description. From the car park, our route turns right up the gravel path towards the church. If it is open, you are encouraged to visit. In any case, please leave a donation in the porch. The church was mainly constructed between the 13th and 15th centuries and has been recognised for its architectural and historic value with a Grade I listing. From the church porch, we go straight ahead across the grass, with the Vicarage on the left, to leave through a small gateway. -
Railfuture Autumn 2013 Rail Users Conference
ISSUE165 February 2015 Internet at www.railfuture.org.uk/East+Anglia TWITTER http://twitter.com/RailfutureEA. RAILFUTURE; EAST ANGLIA BRANCH ANNUAL GENERAL MEETING 28 FEBRUARY 2015 AT 14.00 HRS FRIENDS MEETING HOUSE, SAINT JOHN'S STREET, BURY ST EDMUNDS, IP33 1SJ www.railfuture.org.uk/East+Anglia 1 Railfuture East Anglia Branch Annual Report to Branch Members from Chairman, Peter Wakefield The Branch has continued with its now well established routine of 4 members' meetings per year. These were held in centres that hopefully enable all members to attend at least one gathering and meet the Branch Committee. The average number of attendees last year was 35. Besides members, the general public has been welcomed too. A speaker connected to the railway industry is invited to talk to members as well as the usual business of a meeting being conducted. This year, meetings have been held in Bury St Edmunds, Colchester (jointly with colleagues from the L&SE Eastern Division) Norwich and Peterborough (jointly with colleagues from the Lincolnshire Branch.) The Branch Committee has met on the same day as the above plus a planning meeting in Cambridge at the end of March. Each member of the Committee has a specific and agreed task. Before each meeting, the newsletter, "RailEast", has been produced and either posted or emailed to all members including Corporate Members. This year, in addition to the above, the Branch organised an all day national Summer conference, on behalf of the Board, in Cambridge. This was well attended and was agreed by attendees as a positive experience. -
ADDENDUM to UTT/ 13/3123/FUL (STRETHALL) (Referred To
ADDENDUM to UTT/ 13/3123/FUL (STRETHALL) (Referred to Committee by Cllr Menell. Reason: Impact on local countryside, visual impact on ancient manor of Strethall and church. Possible destruction of special verges, fauna and flora. Overdevelopment on constrained site. Contrary to policy ENV8, ENV9, and H6) PROPOSAL: New dwelling LOCATION: Ryders Barns, Strethall Lane, Strethall, APPLICANT: Mr Michael Vanoli EXPIRY DATE: 14 January 2013 CASE OFFICER: Tony Boswell This application was considered at the Committee’s last meeting on the 15th of January 2014 and was deferred to allow a site inspection and further information on two points. a) The alignment of the “Icknield Way Footpath” where that passes through the application site. A Statutory Footpath passes through the application site and would not be obstructed by the proposed new house – (although it might be marginally disrupted during construction). That statutory footpath forms part of the modern “Icknield Way Footway”, which is the route now favoured and recommended for use by ramblers and others seeking to follow approximately the route of the historic Icknield Way - rom Ivinghoe Beacon in Buckinghamshire to Knettishall Heath in Norfolk (approximately 110 miles). That historic route predates all of the modern field boundaries and local roads – generally less than 300 years old, and actually pre- dates the roman era. The map below is enlarged from a map published on-line by the Icknield Way Association and shows that ancient route, with the application site also indicated on that same map base. b) It should be noted that the Icknield Way Association were consulted about the current planning application and did not raise any objection. -
THE DEVIL's DYKE, NEWMARKET. Newmarketand
THE DEVIL'S DYKE, NEWMARKET. {READ Arm 13, 1850.] NEWMARKETandits neighbourhood possessed, till within a few years, numerous evidencesof the warlike races which antiently occupied our Island ; but many of the tumuli which studded the country, with fragments of trackways and embankments, have been cleared away, without, it is much to be regretted, even a note of their contents, form, or precise locality. Most remarkable earthworks, however, extending from the woody uplands on one side to the wide expanse of fen on the other, remain to attest the presence and the labours of contending races Camden enumerates five almost parallel dykes or ditches. The first, called Brent Ditch, between Melbourne and Foulmire ; the second about 5 miles long, running from Hinxton, by Hildersham, to Horseheath ; the third,.called Fleam (Flight) Dyke, or from the length of its course, Seven Mile Dyke, from Balsham to Fen Ditton ; the fourth, the greatest and most entire, popularly called the Devil's Dyke, from Woodditton to Reach, a distance of 7 or 8 miles ; and a fifth, the least of all, " shewethe itselfe two miles from hence, betweene Snailwell and Moulton." The courses of the four first of these ditches are shewn on Lysons's map of Cambridge- shire. Brent or Brant Ditch, says that author, is a slight work of the kind, proceeding from Heydon, in Essex, *pointing nearly to Barrington, continuing over part of . Foulmire, till it ends in a piece of boggy ground. The. "Secondditch is seen about a mile south of Bournbridge, lying upon declining ground between Abingdon Wood and Pampisworth, pointing towards Cambridge. -
Fulbourn Site Assessment Proforma
South Cambridgeshire Strategic Housing Land Availability Assessment (SHLAA) Report August 2013 Appendix 7i: Assessment of 2011 'Call for Sites' SHLAA sites Index of Fulbourn Site Assessment Proforma Site Site Address Site Capacity Page Number Land at Fulbourn Old Drift (south of Site 037 Cambridge Road and north of Shelford 921 dwellings 766 Road), Fulbourn Site 038 Land north of Cambridge Road, Fulbourn 166 dwellings 775 Site 074 Land off Station Road, Fulbourn 186 dwellings 783 Site 108 Land south of Hinton Road, Fulbourn 52 dwellings 794 Land to the South of Fulbourn Old Drift & Site 109 78 dwellings 802 Hinton Road, Fulbourn Site 136 Land at Balsham Road, Fulbourn 62 dwellings 810 Land between Teversham Road and Cow Site 162 92 dwellings 818 Lane, Fulbourn Land at east of Court Meadows House, Site 213 166 dwellings 829 Balsham Road, Fulbourn Site 214 Land off Home End, Fulbourn 14 dwellings 837 Site 245 Bird Farm Field, Cambridge Road, Fulbourn 85 dwellings 845 SHLAA (August 2013) Appendix 7i – Assessment of 2011 ‘Call for Sites’ SHLAA sites Minor Rural Centre Fulbourn Page 765 South Cambridgeshire Local Development Framework Strategic Housing Land Availability Assessment (SHLAA) Site Assessment Proforma Proforma July 2012 Created Proforma Last July 2013 Updated Location Fulbourn Site name / Land at Fulbourn Old Drift (south of Cambridge Road and north of address Shelford Road), Fulbourn Category of A village extension i.e. a development adjoining the existing village site: development framework boundary Description of promoter’s 3,050 dwellings with public open space proposal Site area 76.78 ha. (hectares) Site Number 037 The site lies to the south of Cambridge Road and north of Shelford Road on the south western edge of Fulbourn. -
Locations of Horseheath Records
Locations of Horseheath records Part of Horseheath Village Archives Locations of Horseheath records Cambridgeshire Archives and Local Studies Office Formerly Cambridge Record Office, this holds census, church and parish records along with over 300 other items concerning Horseheath. It is located in the Cambridgeshire County Council Offices, Shire Hall, Castle Street, Castle Hill, Cambridge CB3 0AP Tel.01223 699 399 The Cambridgeshire Collection This is located within the Cambridge Central Library and contains a wide variety of information relating to Cambridgeshire and its people. It includes books, pamphlets, magazines, maps from 1574, illustrations from the 17 th c, newspapers from 1762, press cuttings from 1960 and ephemera of all kinds. The Cambridge Antiquarian Society Photographic Archive is held in the Cambridgeshire Collection, as is the studio portrait archive of the former Cambridge photographers J Palmer Clarke and Ramsey and Muspratt. Family historians have access to many sources listing former residents of the county; directories, electoral rolls, poll books, parish register transcripts, etc. Cambridge University Library List follows. Cemeteries The Monumental Inscriptions in the graveyard of All Saints from the 15th century-1981 are recorded in Cambridgeshire Archives and Local Studies in the Council Offices, Shire Hall, Castle Hill. A copy of the original manuscript of ‘Inscriptions on gravestones and internal monuments’, by Catherine Parsons, 1897 appears in the @all Saints’ Church sewction of Horseheath Village Archives. Census The Census Records from 1841-1911 can be found in the Cambridgeshire Archives and Local Studies Office and at the Family Records Centre in London (see below). The 1881 Census is available in searchable form on www.familysearch.org. -
Cambridgeshire Tydd St
C D To Long Sutton To Sutton Bridge 55 Cambridgeshire Tydd St. Mary 24 24 50 50 Foul Anchor 55 Tydd Passenger Transport Map 2011 Tydd St. Giles Gote 24 50 Newton 1 55 1 24 50 To Kings Lynn Fitton End 55 To Kings Lynn 46 Gorefield 24 010 LINCOLNSHIRE 63 308.X1 24 WHF To Holbeach Drove 390 24 390 Leverington WHF See separate map WHF WHF for service detail in this area Throckenholt 24 Wisbech Parson 24 390.WHF Drove 24 46 WHF 24 390 Bellamys Bridge 24 46 Wisbech 3 64 To Terrington 390 24. St. Mary A B Elm Emneth E 390 Murrow 3 24 308 010 60 X1 56 64 7 Friday Bridge 65 Thorney 46 380 308 X1 To Grantham X1 NORFOLK and the North 390 308 Outwell 308 Thorney X1 7 Toll Guyhirn Coldham Upwell For details of bus services To in this area see Peterborough City Council Ring’s End 60 Stamford and 7 publicity or call: 01733 747474 60 2 46 3 64 Leicester Eye www.travelchoice.org 010 2 X1 65 390 56 60.64 3.15.24.31.33.46 To 308 7 380 Three Holes Stamford 203.205.206.390.405 33 46 407.415.701.X1.X4 Chainbridge To Downham Market 33 65 65 181 X4 Peterborough 206 701 24 Lot’s Bridge Wansford 308 350 Coates See separate map Iron Bridge To Leicester for service detail Whittlesey 33 701 in this area X4 Eastrea March Christchurch 65 181 206 701 33 24 15 31 46 Tips End 203 65 F Chesterton Hampton 205 Farcet X4 350 9 405 3 31 35 010 Welney 115 To Elton 24 206 X4 407 56 Kings Lynn 430 415 7 56 Gold Hill Haddon 203.205 X8 X4 350.405 Black Horse 24.181 407.430 Yaxley 3.7.430 Wimblington Boots Drove To Oundle 430 Pondersbridge 206.X4 Morborne Bridge 129 430 56 Doddington Hundred Foot Bank 15 115 203 56 46. -
Rye Meads Water Cycle Study\F-Reports\Phase 3\5003-Bm01390-Bmr-18 Water Cycle Strategy Final Report.Doc
STEVENAGE BOROUGH COUNCIL RYE MEADS WATER CYCLE STRATEGY DETAILED STUDY REPORT FINAL REPORT Hyder Consulting (UK) Limited 2212959 Aston Cross Business Village 50Rocky Lane Aston Birmingham B6 5RQ United Kingdom Tel: +44 (0)870 000 3007 Fax: +44 (0)870 000 3907 www.hyderconsulting.com STEVENAGE BOROUGH COUNCIL RYE MEADS WATER CYCLE STRATEGY DETAILED STUDY REPORT FINAL REPORT James Latham/ Dan Author Vogtlin Checker Renuka Gunasekara Approver Mike Irwin Report No 5003-BM01390-BMR-18-Water Cycle Strategy Final Report Date 5th October 2009 This report has been prepared for STEVENAGE BOROUGH COUNCIL in accordance with the terms and conditions of appointment for WATER CYCLE STRATEGY dated April 2008. Hyder Consulting (UK) Limited (2212959) cannot accept any responsibility for any use of or reliance on the contents of this report by any third party. RYE MEADS WATER CYCLE STRATEGY—DETAILED STUDY REPORT Hyder Consulting (UK) Limited-2212959 k:\bm01390- rye meads water cycle study\f-reports\phase 3\5003-bm01390-bmr-18 water cycle strategy final report.doc Revisions Prepared Approved Revision Date Description By By - 2/10/2008 Draft Report Structure JL 1 18/11/2008 First Report Draft JL/DV MI 2 27/01/2009 Draft Report JL/DV MI 3-13 03/04/2009 Final Draft Report as amended by stakeholder comments JL/DV RG 14 09/07/2009 Final Draft Report JL/DV RG 15 10/07/2009 Final Draft Report Redacted JL/DV RG 16 21/08/2009 Final Draft Report JL/DV RG 17 21/09/2009 Final Draft following core project team meeting comments JL/DV RG 18 05/10/2009 Final Report JL/DV MI RYE MEADS WATER CYCLE STRATEGY—DETAILED STUDY REPORT Hyder Consulting (UK) Ltd-2212959 k:\bm01390- rye meads water cycle study\f-reports\phase 3\5003-bm01390-bmr-18 water cycle strategy final report.doc CONTENTS 1 Introduction and Summary of Key Outcomes .................................... -
Chapter 2 Physical Characteristics of the Study Area
CHAPTER 2 PHYSICAL CHARACTERISTICS OF THE STUDY AREA 2.1. Location of study area The study area incorporates part of north Hertfordshire, south and mid- Bedfordshire as well as the southwest corner of Cambridgeshire and lies approximately 40 km north of London (Figure 1.1). Coverage of the area by British Geological Survey (BGS) 1:50,000 map sheets is shown in Figure 2.1. 2.2. Bedrock geology The strikes of the solid geological formations are approximately northeast- southwest across the study area (Figure 2.2). The solid geological succession is shown in Table 2.1. To the northwest of the Chiltern Hills the Gault Clay forms a rich agricultural landscape, representing a continuation of the Vale of Aylesbury. Beyond this, running approximately from Bow Brickhill (SP915343) to Gamlingay (TL234525) is a discontinuous ridge formed by the Woburn Sands Formation, part of the Lower Greensand. This prominent ‘Greensand Ridge’, rising to 170 m O.D. at Bow Brickhill, separates the Cretaceous clays from the Jurassic Oxford and Ampthill Clays to the northwest. The oldest formation is recorded in a borehole (TL23NE1) at Ashwell (TL286390), where Devonian strata were reached at a depth of 186.54 m, i.e. 93 m below O.D. (Smith, 1992). Lying just beyond the northern boundary of the present study area, north of the River Ouse, a borehole (TL15NE2) at Wyboston (TL175572) penetrated Ordovician rocks of Tremadoc age at a depth of approximately 230 m (Moorlock et al ., 2003). The Oxford Clay of the Upper Jurassic represents the oldest formation outcropping within the study area. -
Chrishall Grange
Chrishall GranGe CAMBRIDGESHIRE/HERTFORDSHIRE BORDER Chrishall GranGe HEYDON • NR ROYSTON CAMBRIDGESHIRE/HERTFORDSHIRE BORDER Cambridge 12 miles • Saffron Walden 12 miles • Newmarket 20 miles • London 57 miles Whittlesford 5 miles (London Liverpool Street from 60 mins) Royston 7 miles (London Kings Cross from 38 mins) • Stansted Airport 22 miles (All distances and times are approximate) A stunning Grade II* listed country house in an enchanting and accessible rural location Reception Hall • Drawing Room • Dining Room • Sitting Room • Study • Office/Playroom Kitchen/Breakfast Room • Utility Room • Extensive Cellars Master Bedroom Suite with 2 Dressing Rooms and Bathroom • 7 Further Bedrooms • 3 Further Bathrooms 2 Bedroom Cottage • Party Barn with Kitchen and Billiards Room • Garaging Extensive Outbuildings and Machinery Store • Stableyard with 12 Loose Boxes Indoor Riding School • Outdoor Manège Delightful Established Gardens and Grounds • Tennis Court • Swimming Pool Walled Kitchen Garden • Woodland • Paddocks About 28 acres Jackson Stops & Staff Newmarket Savills Cambridge Savills Country Department 168 High Street, Newmarket Unex House, 132-134 Hills Road 33, Margaret Street Suffolk CB8 9AJ Cambridge CB2 8PA London W1G 0JD Jock Lloyd-Jones James Barnett Camilla Foster 01638 662 231 01223 347 147 0207 016 3718 [email protected] [email protected] [email protected] jackson-stops.co.uk savills.co.uk SITUATION Chrishall Grange is superbly located on the edge of a hamlet, 12 miles to the south of Cambridge, the principal city of East Anglia. The house is privately positioned at the end of a long tree-lined drive, sitting well in its land and benefiting from extensive rural views. -
Terra Rossa in the Mediterranean Region: Parent Materials, Composition and Origin
Geologia Croatica 56/1 83–100 23 Figs. 6 Tabs. ZAGREB 2003 Terra Rossa in the Mediterranean Region: Parent Materials, Composition and Origin Goran DURN Key words: Terra rossa, Parent materials, Composi- relict soil formed during the Tertiary and/or hot and humid periods of the Quaternary. However, some recent investigation in the Atlantic tion, Origin, Mediterranean region. coastal region of Morocco (BRONGER & SEDOV, 2002) show that at least some terra rossa previously referred to as polygenetic relict soils should be regarded as Vetusols. In some isolated karst terrain, terra Abstract rossa may have formed exclusively from the insoluble residue of lime- In the past, the term “terra rossa” became quite a common indication stone and dolomite but much more often it comprises a span of parent for all limestone derived red soils in the Mediterranean region. Today, materials including, for example, aaeolian dust, volcanic material or in some classification systems based on the Mediterranean climate as sedimentary clastic rocks which were derived on carbonate terrain via the major soil differentiating criterion, the term terra rossa is used as a different transport mechanisms. BOERO & SCHWERTMANN (1989) name for the soil subclass “Modal Fersiallitic Red soil” when situated concluded that it is of little relevance for the process of rubification on limestones (DUCHAUFOUR, 1982). However, several national whether the primary Fe sources are autochthonous or allochthonous as soil classifications (e.g. Croatian, Italian, Israeli) retained the term long as the general pedoenvironment remains essentially suitable for “terra rossa” for the hard limestone derived red soils. The nature and the formation of terra rossa.