Baseline Report Series:21. the Chalk and Crag of North Norfolk
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Parish Share Report
PARISH SHARE PAYMENTS For period ended 30th September 2019 SUMMARY OF PARISH SHARE PAYMENTS BY DEANERIES Dean Amount % Deanery Share Received for 2019 % Deanery Share % No Outstanding 2018 2019 to period end 2018 Received for 2018 received £ £ £ £ £ Norwich Archdeaconry 06 Norwich East 23,500 4.41 557,186 354,184 63.57 532,380 322,654 60.61 04 Norwich North 47,317 9.36 508,577 333,671 65.61 505,697 335,854 66.41 05 Norwich South 28,950 7.21 409,212 267,621 65.40 401,270 276,984 69.03 Norfolk Archdeaconry 01 Blofield 37,303 11.04 327,284 212,276 64.86 338,033 227,711 67.36 11 Depwade 46,736 16.20 280,831 137,847 49.09 288,484 155,218 53.80 02 Great Yarmouth 44,786 9.37 467,972 283,804 60.65 478,063 278,114 58.18 13 Humbleyard 47,747 11.00 437,949 192,301 43.91 433,952 205,085 47.26 14 Loddon 62,404 19.34 335,571 165,520 49.32 322,731 174,229 53.99 15 Lothingland 21,237 3.90 562,194 381,997 67.95 545,102 401,890 73.73 16 Redenhall 55,930 17.17 339,813 183,032 53.86 325,740 187,989 57.71 09 St Benet 36,663 9.24 380,642 229,484 60.29 396,955 243,433 61.33 17 Thetford & Rockland 31,271 10.39 314,266 182,806 58.17 300,933 192,966 64.12 Lynn Archdeaconry 18 Breckland 45,799 11.97 397,811 233,505 58.70 382,462 239,714 62.68 20 Burnham & Walsingham 63,028 15.65 396,393 241,163 60.84 402,850 256,123 63.58 12 Dereham in Mitford 43,605 12.03 353,955 223,631 63.18 362,376 208,125 57.43 21 Heacham & Rising 24,243 6.74 377,375 245,242 64.99 359,790 242,156 67.30 22 Holt 28,275 8.55 327,646 207,089 63.21 330,766 214,952 64.99 23 Lynn 10,805 3.30 330,152 196,022 59.37 326,964 187,510 57.35 07 Repps 0 0.00 383,729 278,123 72.48 382,728 285,790 74.67 03 08 Ingworth & Sparham 27,983 6.66 425,260 239,965 56.43 420,215 258,960 61.63 727,583 9.28 7,913,818 4,789,282 60.52 7,837,491 4,895,456 62.46 01/10/2019 NORWICH DIOCESAN BOARD OF FINANCE LTD DEANERY HISTORY REPORT MONTH September YEAR 2019 SUMMARY PARISH 2017 OUTST. -
Contents of Volume 14 Norwich Marriages 1813-37 (Are Distinguished by Letter Code, Given Below) Those from 1801-13 Have Also Been Transcribed and Have No Code
Norfolk Family History Society Norfolk Marriages 1801-1837 The contents of Volume 14 Norwich Marriages 1813-37 (are distinguished by letter code, given below) those from 1801-13 have also been transcribed and have no code. ASt All Saints Hel St. Helen’s MyM St. Mary in the S&J St. Simon & St. And St. Andrew’s Jam St. James’ Marsh Jude Aug St. Augustine’s Jma St. John McC St. Michael Coslany Ste St. Stephen’s Ben St. Benedict’s Maddermarket McP St. Michael at Plea Swi St. Swithen’s JSe St. John Sepulchre McT St. Michael at Thorn Cle St. Clement’s Erh Earlham St. Mary’s Edm St. Edmund’s JTi St. John Timberhill Pau St. Paul’s Etn Eaton St. Andrew’s Eth St. Etheldreda’s Jul St. Julian’s PHu St. Peter Hungate GCo St. George Colegate Law St. Lawrence’s PMa St. Peter Mancroft Hei Heigham St. GTo St. George Mgt St. Margaret’s PpM St. Peter per Bartholomew Tombland MtO St. Martin at Oak Mountergate Lak Lakenham St. John Gil St. Giles’ MtP St. Martin at Palace PSo St. Peter Southgate the Baptist and All Grg St. Gregory’s MyC St. Mary Coslany Sav St. Saviour’s Saints The 25 Suffolk parishes Ashby Burgh Castle (Nfk 1974) Gisleham Kessingland Mutford Barnby Carlton Colville Gorleston (Nfk 1889) Kirkley Oulton Belton (Nfk 1974) Corton Gunton Knettishall Pakefield Blundeston Cove, North Herringfleet Lound Rushmere Bradwell (Nfk 1974) Fritton (Nfk 1974) Hopton (Nfk 1974) Lowestoft Somerleyton The Norfolk parishes 1 Acle 36 Barton Bendish St Andrew 71 Bodham 106 Burlingham St Edmond 141 Colney 2 Alburgh 37 Barton Bendish St Mary 72 Bodney 107 Burlingham -
North Norfolk District Council (Alby
DEFINITIVE STATEMENT OF PUBLIC RIGHTS OF WAY NORTH NORFOLK DISTRICT VOLUME I PARISH OF ALBY WITH THWAITE Footpath No. 1 (Middle Hill to Aldborough Mill). Starts from Middle Hill and runs north westwards to Aldborough Hill at parish boundary where it joins Footpath No. 12 of Aldborough. Footpath No. 2 (Alby Hill to All Saints' Church). Starts from Alby Hill and runs southwards to enter road opposite All Saints' Church. Footpath No. 3 (Dovehouse Lane to Footpath 13). Starts from Alby Hill and runs northwards, then turning eastwards, crosses Footpath No. 5 then again northwards, and continuing north-eastwards to field gate. Path continues from field gate in a south- easterly direction crossing the end Footpath No. 4 and U14440 continuing until it meets Footpath No.13 at TG 20567/34065. Footpath No. 4 (Park Farm to Sunday School). Starts from Park Farm and runs south westwards to Footpath No. 3 and U14440. Footpath No. 5 (Pack Lane). Starts from the C288 at TG 20237/33581 going in a northerly direction parallel and to the eastern boundary of the cemetery for a distance of approximately 11 metres to TG 20236/33589. Continuing in a westerly direction following the existing path for approximately 34 metres to TG 20201/33589 at the western boundary of the cemetery. Continuing in a generally northerly direction parallel to the western boundary of the cemetery for approximately 23 metres to the field boundary at TG 20206/33611. Continuing in a westerly direction parallel to and to the northern side of the field boundary for a distance of approximately 153 metres to exit onto the U440 road at TG 20054/33633. -
A Walk of Two Midwives: a Circular Walk in North Norfolk
A Walk of Two Midwives: a circular walk in North Norfolk Introduction This walk was inspired by a paper written by Julia Allison, a midwife historian and former General Secretary of The Royal College of Midwives, and I owe many thanks to her for additional information and her enthusiasm for the retrieval and safeguarding of the history of midwifery in the UK. [Please see Midwives of Sixteenth-Century Rural East Anglia, Rural History (2016) 27 (1), 1-19. DOI: 10.1017/S0956793315000138.] The walk begins and ends at the village of Binham, a few miles inland from the north Norfolk coast, and offers a glimpse into the world of Mistress Fiske, a midwife living at Binham, and Margaret Burwood, a midwife living in Wells, in the 16th century. The information below provides some context for the places on the route. Mistress Fiske Mistress Fiske (we do not know her first name) lived in a fair-sized house in Binham. Her husband was a farmer and saffron-grower. Saffron was an important commodity (used as a dye) and was grown widely across East Anglia. Their house had at least two floors and contained a hall, a saffron kiln, a parlour and a number of bedchambers. Julia Allison, citing the papers of Nathaniel Bacon (of whom more later), tells us that in 1599 Mistress Fiske attended, along with her servant, Mistress Calthorpe in Cockthorpe, the village immediately north of Binham. Mistress Calthorpe was the wife of Captain Calthorpe of the local militia. The walk will follow their likely route. Mistress Fiske’s brother-in-law was a ship builder and owner in nearby Wells-Next-The –Sea, where another midwife Margaret Burwood lived during the 16th century. -
STATEMENT of PERSONS NOMINATED Election of Parish
STATEMENT OF PERSONS NOMINATED North Norfolk Election of Parish Councillors The following is a statement of the persons nominated for election as a Councillor for Aldborough and Thurgarton Reason why Name of Candidate Home Address Description (if any) Name of Proposer no longer nominated* BAILLIE The Bays, Chapel Murat Anne M Tony Road, Thurgarton, Norwich, NR11 7NP ELLIOTT Sunholme, The Elliott Ruth Paul Martin Green, Aldborough, NR11 7AA GALLANT Spring Cottage, The Elliott Paul M David Peter Green, Aldborough, NR11 7AA WHEELER 4 Pipits Meadow, Grieves John B Jean Elizabeth Aldborough, NR11 7NW WORDINGHAM Two Oaks, Freeman James H J Peter Thurgarton Road, Aldborough, NR11 7NY *Decision of the Returning Officer that the nomination is invalid or other reason why a person nominated no longer stands nominated. The persons above against whose name no entry is made in the last column have been and stand validly nominated. Dated: Friday 10 April 2015 Sheila Oxtoby Returning Officer Printed and published by the Returning Officer, Electoral Services, North Norfolk District Council, Holt Road, Cromer, Norfolk, NR27 9EN STATEMENT OF PERSONS NOMINATED North Norfolk Election of Parish Councillors The following is a statement of the persons nominated for election as a Councillor for Antingham Reason why Name of Candidate Home Address Description (if any) Name of Proposer no longer nominated* EVERSON Margra, Southrepps Long Trevor F Graham Fredrick Road, Antingham, North Walsham, NR28 0NP JONES The Old Coach Independent Bacon Robert H Graham House, Antingham Hall, Cromer Road, Antingham, N. Walsham, NR28 0NJ LONG The Old Forge, Everson Graham F Trevor Francis Elderton Lane, Antingham, North Walsham, NR28 0NR LOVE Holly Cottage, McLeod Lynn W Steven Paul Antingham Hill, North Walsham, Norfolk, NR28 0NH PARAMOR Field View, Long Trevor F Stuart John Southrepps Road, Antingham, North Walsham, NR28 0NP *Decision of the Returning Officer that the nomination is invalid or other reason why a person nominated no longer stands nominated. -
The Sedimentology and Palaeoecology of the Westleton Member of the Norwich Crag Formation (Early Pleistocene) at Thorington, Suffolk, England
Geol. Mag. 136 (4), 1999, pp. 453–464. Printed in the United Kingdom © 1999 Cambridge University Press 453 The sedimentology and palaeoecology of the Westleton Member of the Norwich Crag Formation (Early Pleistocene) at Thorington, Suffolk, England A.E. RICHARDS*, P.L. GIBBARD & M. E. PETTIT *School of Geography, Kingston University, Penrhyn Road, Kingston-upon-Thames, Surrey, KT1 2EE, UK Godwin Institute of Quaternary Research, Department of Geography, University of Cambridge, Downing Place, Cambridge CB2 3EN, UK (Received 28 September 1998; accepted 29 March 1999) Abstract – Extensive sections in the Thorington gravel quarry complex in eastern Suffolk include the most complete record to date of sedimentary environments of the Westleton Beds Member of the Norwich Crag Formation. New palaeoecological and palaeomagnetic evidence is presented, which confirms that the Member was deposited at or near a gravelly shoreline of the Crag Sea as sea level fluctuated during a climatic ameloriation within or at the end of the Baventian/ pre-Pastonian ‘a’ Stage (Tiglian C4c Substage). 1. Introduction 2. Late Pliocene to Early Pleistocene deposits in Suffolk The gravel quarry complex at Thorington (TM 423 728) is situated 8 km west of Southwold in northern A stratigraphical table, comparing British nomencla- Suffolk (Fig. 1). This paper will present details of ture with that of the Netherlands, is given in Table 1. observations in the quarry during the period from The earliest Pleistocene deposits that occur in June 1994 to September 1997, which provide signifi- northern Suffolk are the East Anglian Crags, which cant biostratigraphical and sedimentological evidence were deposited at the margins of the southern North for depositional environments associated with the Sea Basin. -
CPRE Norfolk Housing Allocation Pledge Signatures – Correct As of 24 March 2021 South Norfolk Alburgh Ashby St Mary Barford &A
CPRE Norfolk Housing Allocation Pledge Signatures – correct as of 24 March 2021 South Norfolk Alburgh Ashby St Mary Barford & Wramplingham Barnham Broom Bawburgh Bergh Apton Bracon Ash and Hethel Brockdish Broome Colney Costessey Cringleford Dickleburgh and Rushall Diss Framingham Pigot Forncett Gissing Great Melton Hempnall Hethersett Hingham Keswick and Intwood Kirby Cane and Ellingham Langley with Hardley Marlingford and Colton Mulbarton Rockland St Mary with Hellington Saxlingham Nethergate Scole Shelfanger Shelton and Hardwick Shotesham Stockton Surlingham Thurlton Thurton Thwaite St Mary Tivetshall St Margaret Tivetshall St Mary Trowse with Newton Winfarthing Wreningham Broadland Acle Attlebridge Beighton Blofield Brandiston Buxton with Lamas Cantley, Limpenhoe and Southwood Coltishall Drayton Felthorpe Frettenham Great Witchingham Hainford Hemblington Hevingham Honingham Horsford Horsham St Faiths Lingwood and Burlingham Reedham Reepham Ringland Salhouse Stratton Strawless Strumpshaw Swannington with Alderford and Little Witchingham Upton with Fishley Weston Longville Wood Dalling Woodbastwick Total = 72 Total parishes in Broadland & South Norfolk = 181 % signed = 39.8% Breckland Ashill Banham Bintree Carbrooke Caston Colkirk Cranworth East Tuddenham Foulden Garveston, Reymerston & Thuxton Gooderstone Great Ellingham Harling Hockering Lyng Merton Mundford North Tuddenham Ovington Rocklands Roudham & Larling Saham Toney Scoulton Stow Bedon & Breckles Swaffham Weeting with Broomhill Whinburgh & Westfield Wretham Yaxham Great Yarmouth -
Pleistocene Till Provenance in East Yorkshire: Reconstructing Ice Flow of the British North Sea Lobe
Busfield, M.E., Lee, J.R., Riding, J.B., Zalasiewicz, J., Lee, S.V. 2015. Pleistocene till provenance in east Yorkshire: reconstructing ice flow of the British North Sea Lobe. Proceedings of the Geologist’s Association 126, 86-99 [ACCEPTED MANUSCRIPT]. Pleistocene till provenance in east Yorkshire: reconstructing ice flow of the British North Sea Lobe Marie E. Busfield1*, Jonathan R. Lee2, James B. Riding2, Jan Zalasiewicz1, Sarah V. Lee1 1Department of Geology, University of Leicester, University Road, Leicester, LE1 7RH, UK 2British Geological Survey, Keyworth, Nottingham, NG12 5GG, UK *Corresponding author. Current Address: Department of Earth Sciences, Royal Holloway, University of London, Egham, Surrey, TW20 0EX, UK. E-mail: [email protected] Abstract The ice flow path and dynamic behaviour of the British-Irish Ice Sheet has been subject to renewed interest and controversy in recent years. Early studies in eastern England argued for interaction with Fennoscandian ice onshore in Britain, instigating re-examination of the sedimentology and provenance of many Pleistocene till successions. These studies instead supported an exclusively British provenance, and are used to predict southward advance of a broadly coast parallel North Sea Lobe. Quantitative lithological and palynological analysis of the Pleistocene till succession in Holderness, East Yorkshire, however, remains to be carried out. We examined the lithologically diverse Skipsea Till in order to reconstruct ice flow pathways to the Holderness coast during the Pleistocene, thereby constraining which areas of substrate were subglacially eroded and entrained prior to deposition. The till yields a diverse range of soft, low-durability and uniquely British allochthonous material, including Permian Magnesian Limestone, Carboniferous limestone and coal, and Carboniferous pollen and spore assemblages that would be unlikely to survive polyphase reworking. -
New Developments on the Quaternary of Norfolk REPORT
REPORT REPORT New developments on the Quaternary of Norfolk David Keen’s excellent talk to the Society on the Quaternary of the Midlands will no doubt have reminded members of a Foundation Lecture which one of us (RJOH) gave three years ago on the Quaternary of Norfolk. Since then certain developments have occurred which affect the dating of the Norfolk deposits and their correlation with those described by Professor Keen. At the time of the Foundation Lecture (Hamblin, 2000), Oxygen Isotope Stages for the Norfolk glacial sequence were suggested as in Table 1. Uncertainty as to the date of the Lowestoft Formation has now been largely resolved by further work on material from the Hoxnian type section at Hoxne (Grün and Schwarcz, 2000). This places the interglacial deposits at Hoxne in Stage 11, in which case the immediately underlying Lowestoft Till is Figure 1. Bytham Formation terrace gravels at Leet Hill. almost certainly Stage 12. This was already a These contain glacial erratics and till balls, indicating a difficult conclusion to avoid since the Lowestoft glaciation earlier than OIS 12. glaciation extended the farthest south of any glaciation in south-east England, and has long been believed to have accounted for the diversion of the River Thames. Evidence from the terraces of the Thames placed that diversion in OIS 12 (Bridgland, was found, the Happisburgh and Lowestoft are 1994). clearly separate glaciations. Since the Lowestoft glaciation dates from OIS 12, and there is no good The Corton Formation has been re-named the evidence for a global glaciation in Europe in OIS 14, Happisburgh Formation, partly because a more whereas global ice appears to be important in OIS complete sequence is exposed at Happisburgh than 16 (Raymo,1997), we suggested (Hamblin et al, at Corton, and partly to avoid confusion since 2000) that the Corton (now Happisburgh) Corton is also the type site of the Anglian Stage. -
A New Glacial Stratigraphy for East Anglia PRESIDENTIAL ADDRESS
LECTURE REPORTS PRESIDENTIAL ADDRESS Mesozoic outcrops to the northwest, principally the Chalk and Kimmeridge Clay. However, it has generally been believed that the two ice sheets co- A new glacial stratigraphy existed (Hart and Boulton, 1991). for East Anglia In northeast Norfolk, three tills were recognised Summary of one part of the address to the Society on within the North Sea Drift (Table 1; Banham, 1968, Saturday 12th February 2000, by Dr Richard Hamblin 1988), of which the middle one was noticeably more of the British Geological Survey. calcareous than the others. The Lowestoft When I started to plan three Presidential Formation in the area was termed "Marly Drift" as it Addresses for the Society, I decided to leave East was formed almost wholly of reconstituted Chalk. Anglia until last, as new information was appearing During the late 1980s and early 1990s, Jane Hart all the time. Of course as time went on this new and Juha Pekka Lunkka worked on the coast information became more and more difficult to sections as part of their PhD studies (Hart and interpret! Fortunately we were able to "cut the Boulton, 1991; Lunkka 1994). Unfortunately, in gordian knot" during our 1999 fieldwork and I am view of the contorted nature of the deposits, they now in a position to put forward a completely new were unable to agree on the stratigraphy, but I interpretation of the pre-Devensian glacial believe that I have correctly correlated their sequences of East Anglia, and particularly respective nomenclatures with that of Banham in northeastern Norfolk. Table 1. -
Ice-Rafted Erratics with Early Middle Pleistocene Shallow Marine
Published in Proceedings of the Geologists’ Association (2011) Possible ice-rafted erratics in late Early to early Middle Pleistocene shallow marine and coastal deposits in northeast Norfolk, UK. Nigel R. Larkina*, Jonathan R. Leeb & E. Rodger Connellc a The Natural History Department, Norfolk Museums and Archaeology Service, Shirehall, Market Avenue, Norwich, Norfolk NR1 3JQ, UK [email protected] b British Geological Survey, Keyworth, Nottingham NG12 5GG, UK [email protected] c Geography and Environment, School of Geosciences, University of Aberdeen, St Mary’s, Elphinstone Road, Aberdeen, AB24 3UF UK [email protected] *Corresponding author: email [email protected] telephone 07973 869613 Abstract Erratic clasts with a mass of up to 15 kg are described from preglacial shallow marine deposits (Wroxham Crag Formation) in northeast Norfolk. Detailed examination of their petrology has enabled them to be provenanced to northern Britain and southern Norway. Their clustered occurrence in coastal sediments in Norfolk is believed to be the product of ice-rafting from glacier incursions into the North Sea from eastern Scotland and southern Norway, and their subsequent grounding and melting within coastal areas of what is now north Norfolk. The precise timing of these restricted glaciations is difficult to determine. However, the relationship of the erratics to the biostratigraphic record and the first major expansion of ice into the North Sea suggest these events occurred during at least one glaciation between the late Early Pleistocene and early Middle Pleistocene (c. 1.1−0.6 Ma). In contrast to the late Middle (Anglian) and Late Pleistocene (Last Glacial Maximum) glaciations, where the North Sea was largely devoid of extensive marine conditions, the presence of far-travelled ice-rafted materials implies that earlier cold stage sea-levels were considerably higher. -
The Earliest Record of Human Activity in Northern Europe
The earliest record of human activity in Northern Europe Simon A. Parfitt1, 13, René W. Barendregt2, Marzia Breda3, Ian Candy4, 12, Matthew J. Collins5, G. Russell Coope6, 12, Paul Durbidge7, Mike H. Field8, Jonathan R. Lee9, 12, Adrian M. Lister10, Robert Mutch7, Kirsty E.H. Penkman5, Richard C. Preece11, James Rose12, Christopher B. Stringer12, 13, Robert Symmons13, John E. Whittaker13, John J. Wymer14, & Anthony J. Stuart10, 15 1Institute of Archaeology, University College London, London WC1H 0PY, UK 2University of Lethbridge, Lethbridge, Alberta, Canada TK1 3M4 3Dipartimento di Geologia, Paleontologia e Geofisica, University of Padova, Via Giotto 1, 35100 Padova, Italy 4Department of Geography, Loughborough University, Loughborough LE11 3TU, UK 5BioArch, Biology S Block, University of York, PO Box 373, York YO10 5YW, UK 6Department of Geography, Earth and Environmental Sciences, University of Birmingham, Edgbaston, Birmingham B15 2TT, UK 7Lowestoft Museum, Oulton Broad, Lowestoft NR33 9JR, UK 8Church Cottage, Church Street, Fenny Compton, Warwickshire CV47 2YE, UK 9British Geological Survey, Keyworth, Nottingham NG12 5GG, UK 10Department of Biology, University College London, Gower Street, London WC1E 6BT, UK 11Department of Zoology, University of Cambridge, Downing Street, Cambridge CB2 3EJ, UK 12Department of Geography, Royal Holloway, University of London, Egham TW20 0EX, UK 13Department of Palaeontology, The Natural History Museum, Cromwell Road, London SW7 5BD, UK 1417 Duke Street, Bildeston, Ipswich IP7 7EW, UK 15University of Durham School of Biological and Biomedical Sciences, Durham DH1 3LE, UK The colonisation of Eurasia by early humans is a key event following their spread out of Africa, but the nature, timing and ecological context of the earliest human occupation of northwest Europe is uncertain and has been the subject of intense debate1.