Changes in Asset Values on Eroding Coasts
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
F!13Il-.-.; A:: It: Identification of Littoral Cells
Journal of Coastal Research 381-400 Fort Lauderdale, Florida Spring 1995 Littoral Cell Definition and Budgets for Central Southern England Malcolm J. Bray, David J. Carter and Janet M. Hooke Department of Geography University of Portsmouth Portsmouth, POI 3HE, England ABSTRACT . BRAY, M.J.; CARTER, D.J., and HOOKE, J.M., 1995. Littoral cell definition and budgets for central southern England. Journal of Coastal Research, 11(2),381-400. Fort Lauderdale (Florida), ISSN 0749 ,tllllllll,.e 0208. Differentiation of natural process units is promoted as a means of better understanding the interconnected . ~ ~ - nature of coastal systems at various scales. This paper presents a new holistic methodology for the f!13Il-.-.; a:: it: identification of littoral cells. Testing is undertaken through application to an extensive region of central ... bJLt southern England. Diverse sources of information are compiled to map 8. detailed series of local sediment circulations both at the shoreline and in the offshore zone. Cells and sub-cells are subsequently defined by thorough examination of the continuity of sediment transport pathways and by identification of boundaries where there are discontinuities. Important distinctions are made between the nature and stability of different boundaries and a classification of types is devised. Application of sediment budget analysis to major process units helps to clarify the regional significance of different sediment sources, stores and sinks. Within the study area, it is shown that sediments circulate from distinct eroding cliff sources to well defined sinks. Natural beaches are transient and dependent upon the continued functioning of supply pathways from cliff sources. Relict cells with residual circulations are identified as a consequence of interference. -
Understanding the Area
2. Understanding the area A special place The Norfolk Coast Area of Outstanding Natural Beauty The Area was legally designated in 1968, following is a protected National Landscape that sweeps around a five-year process of consideration of its landscape quality, most of the coast of Norfolk, England. Comprising 451 statutory assessments by national conservation agencies, square kilometres of intertidal, coastal and agricultural and consultation with a broad range of stakeholders, land that stretches across the territory of three different including local landowners, residents and businesses, local authorities and one county council, the Area is as well as visitors and the wider public14. It runs along just characterised by remarkable natural landscapes, over 90 kilometres of the Norfolk coast, stretching from the and renowned as one of the few lowland areas in the mean low water mark and up to eight kilometres inland; UK to have a genuine ‘wilderness’ quality. It is physically within its boundaries there are a wealth of different split into three separate zones that encompass large natural and manmade landscapes, many rich with wildlife: sections of the coast: heaths and moors, salt marshes and high cliffs, chalk rivers and busy harbours. • The western zone lies just north of King’s Lynn, taking in parts of the Sandringham Estate (including 13. http://www.norfolkcoastaonb.org.uk/mediaps/pdfuploads/pd003377.pdf Sandringham House) and an area of the south-eastern 14. http://www.norfolkcoastaonb.org.uk/mediaps/pdfuploads/pd001161.pdf corner -
Historic Environment Action Plan the Undercliff
Directorate of Community Services Director Sarah Mitchell Historic Environment Action Plan The Undercliff Isle of Wight County Archaeology and Historic Environment Service October 2008 01983 823810 archaeology @iow.gov.uk Iwight.com HEAP for the Undercliff. INTRODUCTION This HEAP Area has been defined on the basis of geology, topography, land use and settlement patterns which differentiate it from other HEAP areas. This document identifies essential characteristics of the Undercliff as its geomorphology and rugged landslip areas, its archaeological potential, its 19 th century cottages ornés /marine villas and their grounds, and the Victorian seaside resort character of Ventnor. The Area has a highly distinctive character with an inner cliff towering above a landscape (now partly wooded) demarcated by stone boundary walls. The most significant features of this historic landscape, the most important forces for change and key management issues are considered. Actions particularly relevant to this Area are identified from those listed in the Isle of Wight HEAP Aims, Objectives and Actions. ANALYSIS AND ASSESSMENT Location, Geology and Topography • The Undercliff is identified as a discrete Landscape Character Type in the Isle of Wight AONB Management Plan (2004, 132). • The Area lies to the south of the South Wight Downland , from which it is separated by vertical cliffs forming a geological succession from Ferrugunious Sands through Sandrock, Carstone, Gault Clay, Upper Greensand, Chert Beds and Lower Chalk (Hutchinson 1987, Fig. 6). o The zone between the inner cliff and coastal cliff is a landslip area o This landslip is caused by groundwater lubrication of slip planes within the Gault Clays and Sandrock Beds. -
Georgian Farmhouse in Unspoilt Position
Georgian farmhouse in unspoilt position Grove House, Irstead, Norfolk Freehold Entrance hall • Drawing room • Dining room • Kitchen/ breakfast room with Aga • Study • Utility room • Old dairy Studio • Cloakroom/WC • Cellar • Six bedrooms • Family bathroom • Shower room • Outbuildings including barn Garaging • Mooring rights nearby • Mature gardens and grounds in all about 0.48 of an acre The Property traditionally constructed of red Grove House is a most brick and providing garaging attractive Grade II listed and workshop/storage space. Georgian farmhouse of circa The land in all extends to about 1820 with earlier origins 0.48 of an acre. believed to date to the 17th century. The house has elegant Situation and well-proportioned rooms Irstead is a small unspoilt rural typical of the period and lit by hamlet lying between Horning fine sash windows. Much and Neatishead. The village of period detail remains Neatishead is about half a mile throughout the house which and has a community village was acquired by the current shop and traditional pub. There owners in 1991 and who carried is a new village hall which hosts out a sensitive and faithful a number of local events. The programme of renovation and village of Irstead itself is about restoration. a mile and there is access via a boardwalk with fine walks Outside around the periphery of Barton The house is approached by a Broad nearby. The bustling gravelled drive to the east of riverside village of Horning the house which finishes in a (about two miles) has further large gravelled turning and everyday shopping including a parking space to the north of delicatessen, three public the house. -
Parish Registers and Transcripts in the Norfolk Record Office
Parish Registers and Transcripts in the Norfolk Record Office This list summarises the Norfolk Record Office’s (NRO’s) holdings of parish (Church of England) registers and of transcripts and other copies of them. Parish Registers The NRO holds registers of baptisms, marriages, burials and banns of marriage for most parishes in the Diocese of Norwich (including Suffolk parishes in and near Lowestoft in the deanery of Lothingland) and part of the Diocese of Ely in south-west Norfolk (parishes in the deanery of Fincham and Feltwell). Some Norfolk parish records remain in the churches, especially more recent registers, which may be still in use. In the extreme west of the county, records for parishes in the deanery of Wisbech Lynn Marshland are deposited in the Wisbech and Fenland Museum, whilst Welney parish records are at the Cambridgeshire Record Office. The covering dates of registers in the following list do not conceal any gaps of more than ten years; for the populous urban parishes (such as Great Yarmouth) smaller gaps are indicated. Whenever microfiche or microfilm copies are available they must be used in place of the original registers, some of which are unfit for production. A few parish registers have been digitally photographed and the images are available on computers in the NRO's searchroom. The digital images were produced as a result of partnership projects with other groups and organizations, so we are not able to supply copies of whole registers (either as hard copies or on CD or in any other digital format), although in most cases we have permission to provide printout copies of individual entries. -
Next the Sea: Eccles and the Anthroposcenic
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Repository@Nottingham Next the Sea: Eccles and the Anthroposcenic David Matless Accepted for publication in the Journal of Historical Geography, May 2018 Abstract This paper considers the Anthroposcenic, whereby landscape becomes emblematic of processes marking the Anthropocene, through a specific site, Eccles on the northeast coast of Norfolk, England. The coast has become a key landscape for reflections on the Anthropocene, not least through processes of erosion and sea level change; the title phrase ‘next the sea’ here carries both spatial and temporal meaning. Through Eccles the paper investigates cultural-historical Anthropocene signatures over the past two centuries. Between 1862 and 1895 a church tower stood on Eccles beach; in preceding decades the tower was half-buried in sand dunes, but emerged after these were eroded by the sea. In 1895 the tower fell in a storm, although fragments remained intermittently visible over the following century, depending on the state of the beach. The paper takes Eccles tower as a focus for the exploration of themes indicative and/or anticipatory of the Anthropocene, including sea defence and geological speculation on land and sea levels, Eccles featuring in Charles Lyell’s Principles of Geology. The tower became a visitor attraction, and discussions around the 1895 fall are examined, in relation to the spectacle of ruin, claims over the site, and anxieties over defence. The periodic beach exposure of bones from the former churchyard prompted reflections on mortality, also present in literary engagements with Eccles by figures such as Henry Rider Haggard. -
WALKING EXPERIENCES: TOP of the WIGHT Experience Sustainable Transport
BE A WALKING EXPERIENCES: TOP OF THE WIGHT Experience sustainable transport Portsmouth To Southampton s y s rr Southsea Fe y Cowe rr Cowe Fe East on - ssenger on - Pa / e assenger l ampt P c h hi Southampt Ve out S THE EGYPT POINT OLD CASTLE POINT e ft SOLENT yd R GURNARD BAY Cowes e 5 East Cowes y Gurnard 3 3 2 rr tsmouth - B OSBORNE BAY ishbournFe de r Lymington F enger Hovercra Ry y s nger Po rr as sse Fe P rtsmouth/Pa - Po e hicl Ve rtsmouth - ssenger Po Rew Street Pa T THORNESS AS BAY CO RIVE E RYDE AG K R E PIER HEAD ERIT M E Whippingham E H RYDE DINA N C R Ve L Northwood O ESPLANADE A 3 0 2 1 ymington - TT PUCKPOOL hic NEWTOWN BAY OO POINT W Fishbourne l Marks A 3 e /P Corner T 0 DODNOR a 2 0 A 3 0 5 4 Ryde ssenger AS CREEK & DICKSONS Binstead Ya CO Quarr Hill RYDE COPSE ST JOHN’S ROAD rmouth Wootton Spring Vale G E R CLA ME RK I N Bridge TA IVE HERSEY RESERVE, Fe R Seaview LAKE WOOTTON SEAVIEW DUVER rr ERI Porcheld FIRESTONE y H SEAGR OVE BAY OWN Wootton COPSE Hamstead PARKHURST Common WT FOREST NE Newtown Parkhurst Nettlestone P SMALLBROOK B 4 3 3 JUNCTION PRIORY BAY NINGWOOD 0 SCONCE BRIDDLESFORD Havenstreet COMMON P COPSES POINT SWANPOND N ODE’S POINT BOULDNOR Cranmore Newtown deserted HAVENSTREET COPSE P COPSE Medieval village P P A 3 0 5 4 Norton Bouldnor Ashey A St Helens P Yarmouth Shaleet 3 BEMBRIDGE Cli End 0 Ningwood Newport IL 5 A 5 POINT R TR LL B 3 3 3 0 YA ASHEY E A 3 0 5 4Norton W Thorley Thorley Street Carisbrooke SHIDE N Green MILL COPSE NU CHALK PIT B 3 3 9 COL WELL BAY FRES R Bembridge B 3 4 0 R I V E R 0 1 -
NORFOLK. • Witton & Worstead
518 NORTH W ALSHAM, NORFOLK. • Witton & Worstead. Rapping division-Brunstead, Medical Officer & Public Vaccinator, North Walsham Catfield, East Ruston, Happisburgh, Hempstead-cum District, Smallburgh Union, Sidney Hope Harrison Eccles, Hiclding, Horsey, Ingham, Lessingham, Lud M.R.C.S.Eng., L.R.C.P.Lond. Aylsham road ham, Palling, Potter Heigham, Stalham, Sutton, Wal Medical Officer & Public Vaccinator, Southrepps District, cott & W a:xham Erpingham Union, John Shepheard B.A.,M.R.C.S.Eng., L.R.C.P.Lond. Cromer road 1 NORTH WALSHAM SUB-COMMITTEE OF NORFOLK Registrar of Marriages & Deputy for Births & Deaths LOCAL PENSION COMMITTEE. for the Smallburgh District, Ernest W. Gregory, ' The following places are included in the Sub-District: Excelsior house, -King's Arms street Alby, Aldborough, Antingham, Bacton, Banningham, Relieving & Vaccination Officer, Tunstead District & ,Barton Turf, Beeston St. Lawrence, Bradfield, Brum Registrar of Births & Deaths, North Walsham District;, stead, Burgh, Calthorpe, Catfield, Colby, Crostwight, "Smallburgh Union, George Boult Hewitt, Yarmouth rd Dilham, Ea~t Ruston, Edingthorpe, Erpingham, Fel Superintendent Registrar of Smallburgh Union, Fairfax mingham, Gimingham, Gunton, Happisburgh, Hemp Davies. Grammar School road stead-cum-Eccles, Hickling, Honing, Ingham, Ingworth, PLACES OF WORSHIP, with times of Services. Irstead, Knapton, Lessingham, Mundesley, Neatishead, _N orthrepps, North Walsham, Overstrand, Oxnead, St. Nicholas Church, Rev. Robert Aubrey Aitken M.A. Paston, Ridlington, Sidestrand, Skeyton, Sea Palling, vicar & rural dean; Rev. Tom Harry Cromwell Nash Smallburgh, Southrepps, Suffield, Sutton, Swafield, Th.A.K.C. curate; 8 & II a.m. & 3 & 6.30 p.m. ; Stalham, Swanton Abbott, Thorpe Market, Thwaite, mon. wed. & fri. li a.m. ; tues. thurs. -
KING CHARLES CHALLENGE Experience Sustainable Transport RED ROUTE BICYCLE ISLAND ITINERARY #10
BE A KING CHARLES CHALLENGE Experience sustainable transport RED ROUTE BICYCLE ISLAND ITINERARY #10 VERY CONFIDENT ON AND OFF ROAD – NOT TOO TECHNICAL BUT FITNESS ESSENTIAL START/FINISH: CARISBROOK PRIORY, WHITCOMBE ROAD, CARISBROOKE PO30 1YS TIME: 2-3 HOURS – Bridleways and trail riding, with great views and a good experience of country life on the Island DISTANCE: km / ELEVATION GAIN: m 23.5 370 Portsmouth To Southampton s y s rr Southsea Fe y Cowe rr Cowe Fe East on - ssenger on - Pa / e assenger l ampt P c h hi Southampt Ve out S THE EGYPT POINT OLD CASTLE POINT e ft SOLENT yd R GURNARD vercra BAY Cowes e 2 5 East Cowes y Gurnard 3 3 rr tsmouth - B B OSBORNE BAY ishbournFe de r Lymington F enger Ho Ry y nger Po rr ass sse Fe P rtsmouth/Pa - Po e hicl Ve rtsmouth - ssenger Po Rew Street Pa T THORNESS AS BAY CO RIVER MEDINA E RYDE AG K E PIER HEAD ERIT Whippingham E H RYDE N C R Ve L Northwood O ESPLANADE A 3 0 2 1 ymington - TT PUCKPOOL hic NEWTOWN OO POINT A BAY W Fishbourne l Marks A 3 e /P Corner T 0 DODNOR a 2 0 A 3 0 5 4 Ryde ssenger AS CREEK & DICKSONS Binstead Ya CO Quarr Hill RYDE COPSE ST JOHN’S ROAD rmouth Wootton Spring Vale G E R CLA ME RK I N Bridge TA IVE HERSEY RESERVE, Fe R Seaview LAKE WOOTTON SEAVIEW DUVER rr ERI Porcheld FIRESTONE y H SEAGR OVE BAY OWN Wootton COPSE Hamstead PARKHURST Common WT FOREST NE Newtown Parkhurst Nettlestone P SMALLBROOK B 0 4 3 3 PRIORY BAY NINGWOOD JUNCTION SCONCE BRIDDLESFORD Havenstreet COMMON P COPSES POINT SWANPOND N ODE’S POINT BOULDNOR Cranmore Newtown deserted HAVENSTREET COPSE -
Transactions of the Norfolk and Norwich Naturalists' Society
20 NOV 2Q02 I FXCHA^O'-"> 1 Norfolk Bird Report - 2001 Editor: Giles Dunmore Editorial 95 Review of the Year 98 Wetland Bird Surveys for Breydon and The Wash 1 05 Norfolk Bird Atlas 1 07 Systematic List 1 09 Introductions, Escapes, Ferals and Hybrids 248 Earliest and Latest Dates of Summer Migrants 253 Latest and Earliest Dates of Winter Migrants 254 Non-accepted and non-submitted records 255 Contributors 256 Ringing Report 258 Hunstanton Cliffs: a Forgotten Migration Hotspot 268 1 Yellow-legged Gulls in Norfolk: 1 96 -200 1 273 Marmora’s Warbler on Scolt Head - a first for Norfolk 28 Pallas’s Grasshopper Warbler at Blakeney Point - the second for Norfolk 283 Blyth’s Pipit at Happisburgh in September 1 999 - the second for Norfolk 285 Norfolk Mammal Report - 2001 Editor: Ian Keymer Editorial 287 Bats at Paston Great Barn 288 Memories of an ex-editor 298 Harvest Mice: more common than suspected? 299 Are we under-recording the Norfolk mink population? 301 National Key Sites for Water Voles in Norfolk 304 A Guide to identification of Shrews and Rodents 309 Published by NORFOLK AND NORWICH NATURALISTS’ SOCIETY Castle Museum, Norwich, NRl 3JU (Transactions Volume 35 part 2 October 2002) Please note that the page numbering in this report follows on from part 1 of the Transactions pub- lished in July 2002 ISSN 0375 7226 www.nnns.org.uk Keepsake back numbers are available from David & Iris Pauli, 8 Lindford Drive, Eaton, Norwich NR4 6LT Front cover photograph: Tree Sparrow (Richard Brooks) Back cover photograph: Grey Seal (Graeme Cresswell) NORFOLK BIRD REPORT - 2001 Editorial x On behalf of the Society 1 am pleased to present the annual report on the Birds of Norfolk. -
The Meteorological Magazine Vol
M.O. 548 AIR MINISTRY METEOROLOGICAL OFFICE THE METEOROLOGICAL MAGAZINE VOL. 80, No. 946, APRIL 1951 ESSAY ON FRONTOGENESIS AND FRONTOLYSIS By H. H. LAMB, M.A. Part III Frontolysis.—Frontolysis has tended to be dismissed in meteorological litera ture as a mere counterpart of frontogenesis, to be explained in terms of the same deformation field. The subject is worth separate study. We have already noticed that the frontolytic col seldom arises in practice. Fig. 12, which shows a front, A, lying quasi-stationary between the twin centres of an intense anticyclone over England and France on February 14, 1946, probably typifies an unusually close approach to the frontolytic orien tation of a front in the col. It was not at once clear whether the situation would prove frontolytic, but the intensely anticyclonic conditions ensured that the front would be quiescent. At the time of the chart shown in Fig. 12, the situation had already existed substantially unchanged for more than 24 hours, yet the front A is still marked by a sharp wind discontinuity. Eight hours later a small movement of the front west of Hurn airport brought a wind veer from NE. to S. and eventually to SW. and a sharp deterioration of visibility as the smoke from Bournemouth and Poole was transported in the direction of the airfield. At the same time, the low stratus lifted from about 500 to 1,000 ft. with the arrival of the drier continental air mass. Dew points over France were mainly between 20° and 30°F., and the dry-bulb temperatures show the effect of radiation cooling in the area of clear skies on Fig. -
Bonchurch Landslide, Ventnor Undercliff, Isle of Wight, UK
Geotechnical Study Area G3 Bonchurch landslide, Ventnor Undercliff, Isle of Wight, UK GEOTECHNICAL STUDY AREA G3 BONCHURCH LANDSLIDE, VENTNOR UNDERCLIFF, ISLE OF WIGHT, UK Plate G3 Bonchurch landslide, February 1995, Isle Of Wight , UK 1. BACKGROUND In early February 1995 a large landslide was reported to have occurred in the area known as “The Landslip”, which is situated on the south coast of the Isle of Wight at Bonchurch to the east of Ventnor (see Plate G3 and Figure G3.1). The Landslip area was owned by the Local Authority who first reported the incident to its consulting engineers on 6th February 1995. Early descriptions of the event indicated that a significant area of The Landslip had been affected by the landslide. The event was reported to have resulted in the loss of clifftop land due to the failure of a prominent rear scarp, which marked the landward extent to The Landslip, along with the considerable settlement and disruption of the slopes and amenities within The Landslip. Large quantities of landslide debris were reported to have been deposited on the foreshore, beneath the steep coastal cliffs, as a consequence of the slope movements above (Rendel Geotechnics 1995). Although the description of the events suggested a fairly sudden slope movement, there were no reports of any casualties. The landslide did, however, result in the destruction of a number of public footpaths which form an important amenity in the area. A major concern raised after the event was the potential for further slope instability and landslide extension, particularly upslope of the rear scarp of The Landslip (Plate G3a).