Eocene Inversion History of the Sandown Pericline, Isle of Wight, Southern England

Total Page:16

File Type:pdf, Size:1020Kb

Eocene Inversion History of the Sandown Pericline, Isle of Wight, Southern England Journal of the Geological Society, London, Vol. 156, 1999, pp. 327–339. Printed in Great Britain Eocene inversion history of the Sandown Pericline, Isle of Wight, southern England A. S. GALE1,2, P. A. JEFFERY2, J. M. HUGGETT1 & P. CONNOLLY3 1School of Earth and Environmental Sciences, University of Greenwich, Medway Campus, Chatham Maritime, Chatham, Kent ME4 4AW, UK 2Department of Palaeontology, Natural History Museum, Cromwell Road, London SW7 5BD, UK 3Department of Geology, Imperial College, Prince Consort Road, London SW7 2BP, UK Abstract: Study of the composition and distribution of derived lithoclast and fossil suites collected from the Selsey, Barton and Becton Formations in Whitecliff Bay, Isle of Wight has enabled a detailed reconstruction of Mid–Late Eocene uplift of 500 m+ on the northern limb of the Sandown Pericline. The stratigraphical distribution of clasts and fossils derived from older formations demonstrates the erosion of progressively older Eocene, Palaeocene and Cretaceous sediments during growth of the structure. The presence of delicate reworked fossils and clasts, together with limited palaeocurrent data support very local derivation from the south. The preservational state of the derived materials is used to identify the diverse processes of erosion and transport. Two phases of uplift (Lutetian, Bartonian), separated by a period of quiescence and peneplanation have been identified; rates of Eocene uplift of about 100 m Ma"1 are postulated to have taken place. Keywords: Eocene, Structural inversion, southern England, derived fossils. The Palaeogene succession in Whitecliff Bay in the east of the septarian concretions within the Selsey Formation, and Isle of Wight has attracted geologists since the nineteenth independently, P.A.J. found Bracklesham Group molluscs century (e.g. Prestwich 1847; Fisher 1862), on account of the high in the Barton Clay. These finds stimulated us to search spectacular, near-vertical exposures of variegated sediments, further, and led to the discovery of beds containing Reading many of which are fossiliferous. More recently, the sedimen- Formation clay clasts in the Becton Sand and other specimens tological work of Plint (1984, 1988) established Whitecliff Bay of fossils and clasts derived from older Palaeogene sedi- as a classical locality in which to study sequence stratigraphy ments in the Selsey, Barton, and lower part of the Becton in alternating estuarine and shallow-marine facies. The section Formations. The high-resolution biostratigraphical and is probably the most stratigraphically complete, and certainly chronostratigraphical framework which exists for the Eocene the best exposed Eocene succession in the Anglo-Paris Basin, in Whitecliff Bay (e.g. Aubry et al. 1988; timescale updated by and has been important in the calibration of Eocene onshore Berggren et al. 1995) enables precise dating of periods of uplift, magneto- and biostratigraphy with the deep ocean record and we have been able to calculate rates of uplift on the (Aubry et al. 1988). The locality has also been used as a Sandown Pericline during the Lutetian–Bartonian interval. reference section in the development of global chrono- The absolute amount of uplift during this interval (minimum stratigraphical and eustatic charts (e.g. Haq et al. 1988; J. of 500 m) is considerable, and may have wider implications for Hardenbol. pers. comm.). the tectonic history of southern England during the Early It has been suggested by various authors that uplift was Tertiary. taking place during the Palaeogene in the Isle of Wight. Daley & Edwards (1971) used evidence from thickness variation and erosional surfaces in the Solent Group (Late Eocene–Early The succession in Whitecliff Bay Oligocene) to identify fold axes in the northern Isle of Wight. This section provides a brief description of the succession Murray & Wright (1974) recorded Upper Cretaceous micro- exposed in the southern part of Whitecliff Bay, and provides a fossils in the Venus Bed (Headon Hill Formation, Late stratigraphical context to the sediments which were the source Eocene) of Headon Hill, and at the same level found lime- of clasts and fossils reworked into the Mid–Late Eocene. The stone clasts derived from the lower part of the Headon Hill succession is shown in outline in Fig. 1. Formation. Plint (1982, 1984) interpreted sand units in the Bracklesham Group (Wittering Formation, Mid-Eocene) of Chalk Group (Late Cretaceous). The White Chalk Formation Whitecliff Bay as ‘fans’ derived from earlier Eocene formations (Turonian–Campanian) in the Culver–Whitecliff section during inversion of the east–west basement faults which under- includes nearly 400 m of chalk containing numerous flints lie the Isle of Wight monocline. Plint’s (1984, fig. 12) palaeo- (Rowe 1908; White 1921). The succession is terminated by an geographic reconstruction of the Solent region during unconformity. Derived flints are a conspicuous component of deposition of the Bracklesham Group shows eroding Chalk the Palaeogene succession. uplands immediately to the south of the rising monocline, but to date there is no firm evidence of the timing and amount of Lambeth Group (Palaeocene–Eocene). This group is inversion which took place during the Eocene. represented in the Isle of Wight by the continental Reading During study of exceptional foreshore exposures in Formation (about 40 m thick) which is composed dominantly Whitecliff Bay between 1992 and 1996, A.S.G. and J.M.H. of variegated red, grey, purple and white silts and clays which discovered numerous reworked fragments of London Clay show strong pedogenic mottling (Buurman 1989). 327 328 A. S. GALE ET AL. Clay includes a major hiatus 40 m above the base which is overlain by a lenticular conglomerate. Structural history of the Sandown Pericline Whitecliff Bay is situated on the vertical northern limb of the Sandown Pericline (Fig. 2). The presence of east–west faults at depth underlying the steeply-dipping northern limbs of both the Sandown and Brixton Periclines has been suspected for a long time (White 1921). It is now known that the periclines are underlain by two en-echelon faults which are part of a major basement lineament called the Isle of Wight–Purbeck structure (Stoneley 1982; Underhill & Paterson 1998). The structure continues westwards into Dorset and eastwards from the Isle of Wight as the Bembridge–St Valéry Line which extends across the Channel into the Pays de Bray in northern France (Smith & Curry 1975). During the Early Cretaceous (Barremian–Albian), regional extension caused normal movement on the Variscan basement faults defining the northern margin of the Channel Basin, including the structure beneath the Sandown Pericline (Chadwick 1986; Whittaker 1985; Ruffell 1992; Underhill & Paterson 1998). Clasts and fossils derived from the Jurassic rocks forming the footwall are common in the Barremian (Vectis Formation) and Aptian (Ferruginous Sands Forma- tion) sediments of Sandown Bay (Radley et al. 1998), and testify to extensional movement of the structure at least into Early Albian time. Hardgrounds and condensed sections in the Late Cretaceous Fig. 1. Late Cretaceous and Palaeogene succession exposed in Chalk Group of Culver Cliff (immediately south of Whitecliff Whitecliff Bay. The scale on the left of the lithological column is in Bay) have been interpreted as reflecting growth of the hundreds of metres. Sandown Pericline (Mortimore 1986; Mortimore & Pomerol 1997). They identified two periods of inversion, one in the Thames Group (Eocene, Ypresian). The stratigraphy of the Early Coniacian, and another in the Late Santonian–Early Harwich and London Clay Formations in Whitecliff Bay has Campanian. We disagree with this interpretation for several been described by King (1981) and Huggett & Gale (1998). The reasons. Firstly, the White Chalk Formation thickens south- thin (1 m) Harwich Formation comprises glauconitic sands wards by over 100 m across the Island (especially marked in and silts deposited in a shallow marine setting. The London the Coniacian), which is more consistent with con- Clay is 135 m thick at Whitecliff Bay, and is made up of sands, tinued extensional movement on the Purbeck–Isle of Wight silts and clays deposited in marine and estuarine environments. structure than it is with inversion. Secondly, the phosphatic The lower part of the London Clay at Whitecliff Bay is clay chalks found in the Late Santonian–Early Campanian of dominated, the upper part sand dominated, but within this Culver (Whitecliff Ledge Chalk of Gale et al. 1987) are known overall trend there are four upward coarsening units (Divisions elsewhere in the Paris Basin only in erosional cuvettes A–D of King 1981). The London Clay contains ferroan (Jarvis 1980). We think that a local erosional basin unrelated carbonate-cemented septarian concretions (Huggett 1995), to the Sandown Pericline was responsible for this local phosphatic concretions and in the uppermost part sideritic facies. concretions. The unconformity between pelagic limestones of the Chalk Group and continental clays of the Reading Formation is a Bracklesham Group (Eocene, Ypresian–Lutetian). This litho- striking lithological and facies change and represents a major logically diverse group comprises four formations, deposited in hiatus with a duration of about 15 Ma. The uplift of the Chalk lagoonal, estuarine and shallow open shelf environments (Plint probably took place in the Danian, because Maastrichtian 1984, 1988; Huggett & Gale 1997). The Wittering Formation chalks are present offshore south of Dorset (Curry 1990) and (55 m) is a heterogeneous unit, including silts, glauconitic movement predates deposition of the Thanet Formation in the sands, laminated sands and clays and a rooted coal. The London Basin which is Thanetian in age. Gentle regional Earnley Formation comprises 30 m of highly glauconitic fos- folding caused a slight dip (a fraction of a degree) to the south siliferous sands (locally 40%+glaucony). The Marsh Farm west to develop in the Isle of Wight, as shown by westwards Formation (15 m) is dominated by dark interbedded sands and overstep of the Chalk (Curry 1965, 1990 fig. 13.2). Subsequent clays.
Recommended publications
  • 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
    [Show full text]
  • (Public Pack)Agenda Document for Policy and Scrutiny Committee
    Public Document Pack Monitoring Officer Christopher Potter County Hall, Newport, Isle of Wight PO30 1UD Telephone (01983) 821000 Name of meeting POLICY AND SCRUTINY COMMITTEE FOR NEIGHBOURHOODS AND REGENERATION Date THURSDAY 7 JANUARY 2021 Time 5.00 PM Venue VIRTUAL (MS TEAMS) Members of the Cllrs M Beston (Chairman), V Churchman, J Jones- committee Evans, J Medland, T Outlaw, C Quirk and S Smart Democratic Services Officer: Sarah MacDonald [email protected] 1. Minutes (Pages 5 - 10) To confirm as a true record the Minutes of the meeting held on 1 October 2020. 2. Declarations of Interest To invite Members to declare any interest they might have in the matters on the agenda. To observe the meeting as a member of the public/press please use the link provided. This link will be made available 24 hours prior to start of the meeting. Please ensure you access the meeting in good time. Guidance on how to access the public meeting can be found HERE. Committee members and pre-arranged attendees will be contacted by Democratic Services to supply the appropriate link to participate in the meeting. Details of this and other Council committee meetings can be viewed on the Isle of Wight Council’s Committee website. This information may be available in alternative formats on request. Page 1 3. Public Question Time - 15 Minutes Maximum Questions must be delivered in writing or by electronic mail to Democratic Services ([email protected]) no later than 5 pm on Tuesday, 5 January 2021. Each question must give the name and address of the questioner.
    [Show full text]
  • DINOSAUR SAFARI Experience Sustainable Transport
    BE A WALKING EXPERIENCES: DINOSAUR SAFARI Experience sustainable transport Portsmouth To Southampton Southsea Ferry East Cowes on - Cowes ssenger Ferry Pa / Passenger Southampt Vehicle Southampton - THE EGYPT POINT OLD CASTLE POINT SOLENT GURNARD BAY Cowes Gurnard East Cowes Lymington B 3 3 2 5 OSBORNE BAY Portsmouth - Ryde Passenger Hovercraft Portsmouth - Fishbourne Vehicle/Passenger Ferry Portsmouth - Ryde Rew Street Passenger Ferry THORNESS BAY RIVER MEDINA RYDE PIER HEAD Whippingham HERITAGE COAST RYDE Vehicle/PassengerLymington Ferry - Yarmouth Northwood ESPLANADE NEWTOWN A 3 0 2 1 PUCKPOOL BAY POINT WOOTTON CREEKFishbourne Marks A 3 0 2 0 Corner DODNOR A 3 0 5 4 CREEK & Ryde DICKSONS Quarr Hill Binstead RYDE COPSE Wootton ST JOHN’S ROAD Spring Vale Bridge C L A M E R K I N HERSEY RESERVE, Seaview LAKE WOOTTON SEAVIEW DUVER HERITAGE COAST Porcheld FIRESTONE SEAGR OVE BAY Wootton COPSE Hamstead PARKHURST Common FOREST NEWTOWN RIVER Newtown Parkhurst Nettlestone P SMALLBROOK 0 4 3 3 B PRIORY BAY NINGWOOD JUNCTION 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 P A 3 0 5 5 St Helens Cli End Yarmouth Shaleet BEMBRIDGE Ningwood Newport POINT ASHEY B 3 3 3 0 A 3 0 5 4Norton MILL COPSE Thorley Thorley Street Carisbrooke SHIDE Green CHALK PIT NUNWELL TRAIL B 3 3 9 0 COL WELL BAY WAY FRESHWATER Bembridge B 3 4 0 1 R I V E R YA R EAGLEHEAD AND BRADING GOLDEN P P A S H E Y BLOODSTONE COPSE HILL Wellow
    [Show full text]
  • Isle of Wight Shoreline Management Plan 2
    Isle of Wight Shoreline Management Plan 2 (Review Sub-cell 5d+e) May 2010 Isle of Wight Council, Coastal Management Directorate of Economy & Environment. Director Stuart Love Appendix 1 – DRAFT Policy Unit Options for Public Consultation PDZ1 Gurnard, Cowes and East Cowes (Gurnard Luck to East Cowes Promenade and Entrance to the Medina) (MAN1A) Policy Plan Policy Unit 2025 2055 2105 Comment HTL supports the existing community and allows time for adaptation. Unlikely to qualify for national funding but HTL would allow small scale private defences to be PU1A.1 Gurnard Luck HTL NAI NAI maintained. Moving to NAI reflects the medium to long term increasing risks and need for increasing adaptation. NAI would not preclude maintenance of private defences PU1A.2 Gurnard Cliff NAI NAI NAI Gurnard to Cowes PU1A.3 HTL HTL HTL Parade Recognise that HTL may be difficult to achieve with sea level rise and the community may need to consider PU1A.4 West Cowes HTL HTL HTL coastal adaptation. This will be examined further in the Strategy Study. Recognise that HTL may be difficult to achieve with sea level rise and the community may need to consider PU1A.5 East Cowes HTL HTL HTL coastal adaptation. This will be examined further in the Strategy Study. HTL by maintenance of the existing seawall until the East Cowes Outer PU1A.6 HTL NAI NAI end of its effective life, gradually removing the influence Esplanade of management. Key: HTL - Hold the Line, A - Advance the Line, NAI – No Active Intervention MR – Managed Realignment Medina Estuary and Newport (MAN1B)
    [Show full text]
  • Historic Environment Action Plan Brading Haven and Bembridge Isle
    Directorate of Community Services Director Sarah Mitchell Historic Environment Action Plan Brading Haven and Bembridge Isle Isle of Wight County Archaeology and Historic Environment Service October 2008 01983 823810 archaeology @iow.gov.uk Iwight.com HEAP for Brading Haven and Bembridge Isle INTRODUCTION The Brading Haven and Bembridge Isle HEAP Area comprises land surrounding the former Brading Haven together with the reclaimed land of the haven itself. It includes the settlement of Brading in the west of the Area, St Helens and Nettlestone in the north, Bembridge in the east and Yaverland in the south. Part of this Area, including Bembridge and Yaverland, was for much of its history an island in its own right, cut off from the Wight mainland by arms of the sea at high tide and muddy gulfs at low tide, hence its former name of ‘Bembridge Isle’. A wide area of sea flowed up between Bembridge and St. Helens, past Brading and Yaverland and then joined up with another branch of sea that entered through a gap between Yaverland and Sandown where the boating lake is today. The area between Yaverland and Sandown became known as the ‘Sandown Level’ after it had been drained. A further branch struck off west towards Alverstone. These tidal inlets effectively cut Bembridge Isle off from the rest of the Island until the construction of a causeway at Yar Bridge in the Middle Ages. However, Brading Haven remained as a wide tidal inlet at the mouth of the Eastern Yar River, extending as far inland as Brading, until it was drained between 1878 and 1880, leaving the much smaller area of Bembridge Harbour (Martin 2004a).
    [Show full text]
  • Metal Detectors on Isle of Wight Council-Controlled Beaches
    Metal detectors on Isle of Wight Council-controlled beaches The council allows metal detecting on any beaches Crown Estate permits (but no other land) it owns or controls. A Crown Estate metal detecting permit is not needed Most of the Isle of Wight’s popular urban beaches (including Ryde, to go metal detecting on Council controlled foreshore, Ventnor, Shanklin and Sandown) are owned by the Isle of Wight but may be elsewhere. Council, and many other stretches of coast are controlled by the It is possible to obtain a permit from the Crown Estate to use a council under lease from the Crown Estate. metal detector on Crown Estate beaches. However, a Crown Estate There are many other beaches, not owned by the council, on permit does not give a detectorist the right to use detecting which metal detectorists may or may not be able to enjoy their equipment on Crown land which has been leased to a third party. hobby lawfully subject to necessary permissions. This map is In the case of beaches controlled by the Isle of Wight Council intended to help metal detectorists by giving guidance on where there is no need for such a permit. In the case of all other beaches council beaches are located. It does not give information about you should check with the landowner or occupier. any other beaches which are not owned or controlled by the council, or other permits you might need. Note To gain permission to use metal detecting equipment on other Many beaches owned and controlled by the council are also beaches, metal detectorists should approach the owner or designated as Sites of Special Scientific Interest, on which occupier of that beach.
    [Show full text]
  • Ventnor and District Local History Society Newsletter 38, October 2018 1 Ventnor and District Local History Society
    Ventnor and District Local History Society Newsletter 38, October 2018 1 Ventnor and District Local History Society Newsletter 38 October 2018 A Victorian Family Christmas This year Ventnor Heritage Centre will be taking part in the fun of Ventnorville, the town’s Winter Jolly, over the weekend of 1–2 December. Our volunteers, with the help of our friends from Vectis Victorians (a Living History Group), are planning a “Victorian Family Christmas Experience” with something for all ages. Volunteers are preparing a special-edition Christmas card for sale, a beautiful Christmas hamper of Island produce will be raffled, there will be a bran tub and other traditional games and activities, as well as musical entertainment. The Museum will be transformed for the occasion with traditional decorations. Everyone is invited to come along and join in the fun, take a glass of Wassail with us and savour the atmosphere of Christmas Past. For more information on Ventnorville and the exciting things that are happening in the rest of the town go to the Love Ventnor website (https://www.loveventnor.co.uk/). Linda Chester, Volunteer Coordinator. New Society Publication: by C.T. Witherby In the summer of 1545, King Henry VIII, already at war researched often come to light. The typescript for this with France, heard that the French might soon attack him book ... is one such.” C.T. Witherby was an active member in England. Portsmouth was a target, along with the Isle of of the Society from the very beginning and a volunteer Wight, and the English fleet was hard pressed, with only steward in the Museum.
    [Show full text]
  • The Geological History of the Isle of Wight
    *Manuscript Click here to view linked References The geological history of the Isle of Wight: an overview of the ‘diamond in 1 Britain’s geological crown’ 2 3 4 Abstract 5 6 The geology of the Isle of Wight has attracted both the amateur and professional 7 geologist alike for well over two centuries. It presents a cornucopia of things 8 geological and offers a window into the fascinating story of the geological history and 9 10 landscape development of southern England, as well as an important teaching 11 resource for all levels of study from primary education through to academic research. 12 13 This paper provides a geological framework and a summary of the history of research 14 15 as context for the papers in this issue can be placed. Inevitably, it can only offer a 16 précis of the huge amount of information available, but it is hoped will also give 17 added impetus to further investigation of the literature or, indeed, new research. 18 19 The island offers a field workshop for topics such as lithostratigraphy, sequence 20 21 stratigraphy, tectonics and climate change; studies that are becoming ever more 22 international in their influence. There are 15 Sites of Special Scientific Interest 23 designated because of their geological importance and a number of these are 24 internationally significant. 25 26 27 After a brief discussion on the concealed geology, this paper concentrates on an 28 outline of the near-surface geology on the coast and inland, and introduces a different 29 view on the structure of the Cretaceous and Palaeogene strata.
    [Show full text]
  • Bembridge Sandown
    Island, featuring geology, dinosaurs – and tigers... and – dinosaurs geology, featuring Island, This page This Dinosaur Isle Dinosaur Front cover cover Front Red Cliff and Culver Cliff from Sandown beach Sandown from Cliff Culver and Cliff Red A linear walk over chalk cli#s at the extreme eastern end of the the of end eastern extreme the at cli#s chalk over walk linear A Bembridge to Sandown t'PMMPXBEWJDFBOEMPDBMTJHOT islandbuses.info/things-do/rambles-bus/ t1MBOBIFBEBOECFQSFQBSFE www. or www.iowramblers.com/page44.htm website Enjoy the outdoors the Enjoy All walks in this series can be downloaded from this this from downloaded be can series this in walks All Internet Toilets cafés. cafés. cafés. and pubs of Patrons t,FFQEPHTVOEFSFêFDUJWFDPOUSPM Refreshments Sandown and Bembridge pubs and and pubs Bembridge and Sandown litter home litter of the paths are suitable for families with buggies. buggies. with families for suitable are paths the of t-FBWFOPUSBDFPGZPVSWJTJUBOEUBLFZPVS no stiles, but a hill to climb to get to Culver. Most Most Culver. to get to climb to hill a but stiles, no Protect the natural environment natural the Protect Access information Access There are are There Road, Sandown. Sandown. Road, Start Distance Bus stop, Victoria Victoria stop, Bus miles. 4.7 is available available is and sea fortifications to explore at Culver Down. Down. Culver at explore to fortifications sea and them and follow paths unless wider access access wider unless paths follow and them bus route bus good paths suitable for families, with a monument monument a with families, for suitable paths good t-FBWFHBUFTBOEQSPQFSUZBTZPVëOE to "nd your "nd to Description A linear coastal walk along very very along walk coastal linear A people enjoying the outdoors the enjoying people QR code inside code QR t$POTJEFSUIFMPDBMDPNNVOJUZBOEPUIFS Just use the handy the use Just Bembridge Island Respect other people other Respect most inspiring walks.
    [Show full text]
  • Historic Environment Action Plan Brading Haven and Bembridge Isle
    Island Heritage Service Historic Environment Action Plan Brading Haven and Bembridge Isle Isle of Wight County Archaeology and Historic Environment Service October 2008 01983 823810 archaeology @iow.gov.uk Iwight.com HEAP for Brading Haven and Bembridge Isle INTRODUCTION The Brading Haven and Bembridge Isle HEAP Area comprises land surrounding the former Brading Haven together with the reclaimed land of the haven itself. It includes the settlement of Brading in the west of the Area, St Helens and Nettlestone in the north, Bembridge in the east and Yaverland in the south. Part of this Area, including Bembridge and Yaverland, was for much of its history an island in its own right, cut off from the Wight mainland by arms of the sea at high tide and muddy gulfs at low tide, hence its former name of ‘Bembridge Isle’. A wide area of sea flowed up between Bembridge and St. Helens, past Brading and Yaverland and then joined up with another branch of sea that entered through a gap between Yaverland and Sandown where the boating lake is today. The area between Yaverland and Sandown became known as the ‘Sandown Level’ after it had been drained. A further branch struck off west towards Alverstone. These tidal inlets effectively cut Bembridge Isle off from the rest of the Island until the construction of a causeway at Yar Bridge in the Middle Ages. However, Brading Haven remained as a wide tidal inlet at the mouth of the Eastern Yar River, extending as far inland as Brading, until it was drained between 1878 and 1880, leaving the much smaller area of Bembridge Harbour (Martin 2004a).
    [Show full text]
  • Field Excursion to the Cretaceous and Cenozoic of Redcliff (Sandown) and Whitecliff Bay, Isle of Wight, 5Th January 1992
    Read at the Annual Conference of the Ussher Society, January 1992 FIELD EXCURSION TO THE CRETACEOUS AND CENOZOIC OF REDCLIFF (SANDOWN) AND WHITECLIFF BAY, ISLE OF WIGHT, 5TH JANUARY 1992 A. H. RUFFELL AND M. HARVEY A. H. Ruffell, Department of Geology, Queen's University, Belfast BT7 1NN M. Harvey, Department of Geology, Imperial College, London SW7 2BP The north - south traverse from Redcliff [SZ 612 849] to Whitecliff Bay [SZ discussed by the party, a delta prograding into a lagoon found most support. 643 863] crosses the Isle of Wight Monocline, the site of Cretaceous - At Stop 3 the Shepherd's Chine Member is a succession of finely laminated Cenozoic basin inversion and later folding. On the Redcliff section facies muds and silts with gutter-casts, non- and quasi-marine shell-beds. The shell- developed in Lower to Upper Cretaceous sediments reflect a marine beds form four distinctive coquina limestones that range in thickness from 10 transgression from fluvial and lagoonal environments, through shallow seas to 20 cm. The Shepherd's Chine Member is exposed intermittently along the and into open marine conditions. This succession has an overprint of vegetated slopes above the beach northeast towards Redcliff. The upper 30 transgressive and regressive phases, some of which conform to global models metres of the section is present in a large intact slump block on the intertidal zone of the times of sea-level change: these too are times of tectonic changes in beneath the large landslip of the Atherfield Clay (Figure 2). The Atherfield the Channel Basin, of which the Isle of Wight succession is a part.
    [Show full text]
  • Isle of Wight Newport
    Isle of Wight Newport SCI Celebrity Presentation Evening No SCI festival would be complete without the spectacular festival Friday 8th May - Monday 11th May 2020 finale – the SCI Celebrity Presentation Evening. (May-Day Weekend) In 2019 we were delighted to welcome Ex-Liverpool and England Goalkeeper Chris Kirkland, Ex-Portsmouth and now BBC Sport Pundit Steve Claridge and Ex-Bolton Wanderers and England th Striker Kevin Davies to the Isle of Wight. In 2017 our guest was 15 SCI Isle of Wight former Southampton Legend and current Sky Sports Pundit Matt Le Tissier. Who will the guests be in 2020? There will be a celebrity Mitre Ultimatch Cup presentation evening at each of the 5 holiday parks in 2020. Our Largest & Premier Youth Football Festival Danny Mills John Salako 117 Teams participated in the event in 2019! 120+ teams expected for the festival! Now including Girls Football too! SCI is delighted to once again be staging the 15th SCI Isle of Wight Mitre Ultimatch Cup on the May-Day Weekend 8th – 11th May 2020. The festival is the largest youth football tournament that takes place on the Isle of Wight each and every year. Teams from across England & Wales join SCI for a superb, fun-filled weekend of football & holiday fun at one of 5 holiday parks. Thinking of taking your team abroad but finding the cost prohibitive? Then we can offer you the perfect, cheaper alternative – as the trip to the SCI Isle of Wight Football Festival includes a complimentary ferry crossing – so all players, parents and supporters will feel they have left the mainland behind!! Furthermore, prices start from just £95 per person for the May- Day Weekend.
    [Show full text]