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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. -
Historic Environment Action Plan West Wight Chalk Downland
Directorate of Community Services Director Sarah Mitchell Historic Environment Action Plan West Wight Chalk Downland Isle of Wight County Archaeology and Historic Environment Service October 2008 01983 823810 archaeology @iow.gov.uk Iwight.com HEAP for West Wight Chalk Downland. INTRODUCTION The West Wight Chalk Downland HEAP Area has been defined on the basis of geology, topography and historic landscape character. It forms the western half of a central chalk ridge that crosses the Isle of Wight, the eastern half having been defined as the East Wight Chalk Ridge . Another block of Chalk and Upper Greensand in the south of the Isle of Wight has been defined as the South Wight Downland . Obviously there are many similarities between these three HEAP Areas. However, each of the Areas occupies a particular geographical location and has a distinctive historic landscape character. This document identifies essential characteristics of the West Wight Chalk Downland . These include the large extent of unimproved chalk grassland, great time-depth, many archaeological features and historic settlement in the Bowcombe Valley. The Area is valued for its open access, its landscape and wide views and as a tranquil recreational area. Most of the land at the western end of this Area, from the Needles to Mottistone Down, is open access land belonging to the National Trust. Significant historic landscape features within this Area are identified within this document. The condition of these features and forces for change in the landscape are considered. Management issues are discussed and actions particularly relevant to this Area are identified from those listed in the Isle of Wight HEAP Aims, Objectives and Actions. -
Neolithic & Early Bronze Age Isle of Wight
Neolithic to Early Bronze Age Resource Assessment The Isle of Wight Ruth Waller, Isle of Wight County Archaeology and Historic Environment Service September 2006 Inheritance: The map of Mesolithic finds on the Isle of Wight shows concentrations of activity in the major river valleys as well two clusters on the north coast around the Newtown Estuary and Wooton to Quarr beaches. Although the latter is likely due to the results of a long term research project, it nevertheless shows an interaction with the river valleys and coastal areas best suited for occupation in the Mesolithic period. In the last synthesis of Neolithic evidence (Basford 1980), it was claimed that Neolithic activity appears to follow the same pattern along the three major rivers with the Western Yar activity centred in an area around the chalk gap, flint scatters along the River Medina and greensand activity along the Eastern Yar. The map of Neolithic activity today shows a much more widely dispersed pattern with clear concentrations around the river valleys, but with clusters of activity around the mouths of the four northern estuaries and along the south coast. As most of the Bronze Age remains recorded on the SMR are not securely dated, it has been difficult to divide the Early from the Late Bronze Age remains. All burial barrows and findspots have been included within this period assessment rather than the Later Bronze Age assessment. Nature of the evidence base: 235 Neolithic records on the County SMR with 202 of these being artefacts, including 77 flint or stone polished axes and four sites at which pottery has been recovered. -
Solent Connectivity May 2020
Solent Connectivity May 2020 Continuous Modular Strategic Planning Page | 1 Page | 2 Table of Contents 1.0 Executive Summary .......................................................................................................................................... 6 2.0 The Solent CMSP Study ................................................................................................................................... 10 2.1 Scope and Geography....................................................................................................................... 10 2.2 Fit with wider rail industry strategy ................................................................................................. 11 2.3 Governance and process .................................................................................................................. 12 3.0 Context and Strategic Questions ............................................................................................................ 15 3.1 Strategic Questions .......................................................................................................................... 15 3.2 Economic context ............................................................................................................................. 16 3.3 Travel patterns and changes over time ............................................................................................ 18 3.4 Dual-city region aspirations and city to city connectivity ................................................................ -
Peat Database Results Hampshire
Baker's Rithe, Hampshire Record ID 29 Authors Year Allen, M. and Gardiner, J. 2000 Location description Deposit location SU 6926 1041 Deposit description Deposit stratigraphy Preserved timbers (oak and yew) on peat ledge. One oak stump in situ. Peat layer 0.15-0.26 m deep [thick?]. Associated artefacts Early work Sample method Depth of deposit 14C ages available -1 m OD Yes Notes 14C details ID 12 Laboratory code R-24993/2 Sample location Depth of sample Dated sample description [-1 m OD] Oak stump Age (uncal) Age (cal) Delta 13C 3735 ± 60 BP 2310-1950 cal. BC Notes Stump BB Bibliographic reference Allen, M. and Gardiner, J. 2000 'Our changing coast; a survey of the intertidal archaeology of Langstone Harbour, Hampshire', Hampshire CBA Research Report 12.4 Coastal peat resource database (Hazell, 2008) Page 1 of 86 Bury Farm (Bury Marshes), Hampshire Record ID 641 Authors Year Long, A., Scaife, R. and Edwards, R. 2000 Location description Deposit location SU 3820 1140 Deposit description Deposit stratigraphy Associated artefacts Early work Sample method Depth of deposit 14C ages available Yes Notes 14C details ID 491 Laboratory code Beta-93195 Sample location Depth of sample Dated sample description SU 3820 1140 -0.16 to -0.11 m OD Transgressive contact. Age (uncal) Age (cal) Delta 13C 3080 ± 60 BP 3394-3083 cal. BP Notes Dark brown humified peat with some turfa. Bibliographic reference Long, A., Scaife, R. and Edwards, R. 2000 'Stratigraphic architecture, relative sea-level, and models of estuary development in southern England: new data from Southampton Water' in ' and estuarine environments: sedimentology, geomorphology and geoarchaeology', (ed.s) Pye, K. -
Gazetteer.Doc Revised from 10/03/02
Save No. 91 Printed 10/03/02 10:33 AM Gazetteer.doc Revised From 10/03/02 Gazetteer compiled by E J Wiseman Abbots Ann SU 3243 Bighton Lane Watercress Beds SU 5933 Abbotstone Down SU 5836 Bishop's Dyke SU 3405 Acres Down SU 2709 Bishopstoke SU 4619 Alice Holt Forest SU 8042 Bishops Sutton Watercress Beds SU 6031 Allbrook SU 4521 Bisterne SU 1400 Allington Lane Gravel Pit SU 4717 Bitterne (Southampton) SU 4413 Alresford Watercress Beds SU 5833 Bitterne Park (Southampton) SU 4414 Alresford Pond SU 5933 Black Bush SU 2515 Amberwood Inclosure SU 2013 Blackbushe Airfield SU 8059 Amery Farm Estate (Alton) SU 7240 Black Dam (Basingstoke) SU 6552 Ampfield SU 4023 Black Gutter Bottom SU 2016 Andover Airfield SU 3245 Blackmoor SU 7733 Anton valley SU 3740 Blackmoor Golf Course SU 7734 Arlebury Lake SU 5732 Black Point (Hayling Island) SZ 7599 Ashlett Creek SU 4603 Blashford Lakes SU 1507 Ashlett Mill Pond SU 4603 Blendworth SU 7113 Ashley Farm (Stockbridge) SU 3730 Bordon SU 8035 Ashley Manor (Stockbridge) SU 3830 Bossington SU 3331 Ashley Walk SU 2014 Botley Wood SU 5410 Ashley Warren SU 4956 Bourley Reservoir SU 8250 Ashmansworth SU 4157 Boveridge SU 0714 Ashurst SU 3310 Braishfield SU 3725 Ash Vale Gravel Pit SU 8853 Brambridge SU 4622 Avington SU 5332 Bramley Camp SU 6559 Avon Castle SU 1303 Bramshaw Wood SU 2516 Avon Causeway SZ 1497 Bramshill (Warren Heath) SU 7759 Avon Tyrrell SZ 1499 Bramshill Common SU 7562 Backley Plain SU 2106 Bramshill Police College Lake SU 7560 Baddesley Common SU 3921 Bramshill Rubbish Tip SU 7561 Badnam Creek (River -
Landowner Deposits Register
Register of Landowner Deposits under Highways Act 1980 and Commons Act 2006 The first part of this register contains entries for all CA16 combined deposits received since 1st October 2013, and these all have scanned copies of the deposits attached. The second part of the register lists entries for deposits made before 1st October 2013, all made under section 31(6) of the Highways Act 1980. There are a large number of these, and the only details given here currently are the name of the land, the parish and the date of the deposit. We will be adding fuller details and scanned documents to these entries over time. List of deposits made - last update 12 January 2017 CA16 Combined Deposits Deposit Reference: 44 - Land at Froyle (The Mrs Bootle-Wilbrahams Will Trust) Link to Documents: http://documents.hants.gov.uk/countryside/Deposit44-Bootle-WilbrahamsTrustLand-Froyle-Scan.pdf Details of Depositor Details of Land Crispin Mahony of Savills on behalf of The Parish: Froyle Mrs Bootle-WilbrahamWill Trust, c/o Savills (UK) Froyle Jewry Chambers,44 Jewry Street, Winchester Alton Hampshire Hampshire SO23 8RW GU34 4DD Date of Statement: 14/11/2016 Grid Reference: 733.416 Deposit Reference: 98 - Tower Hill, Dummer Link to Documents: http://documents.hants.gov.uk/rightsofway/Deposit98-LandatTowerHill-Dummer-Scan.pdf Details of Depositor Details of Land Jamie Adams & Madeline Hutton Parish: Dummer 65 Elm Bank Gardens, Up Street Barnes, Dummer London Basingstoke SW13 0NX RG25 2AL Date of Statement: 27/08/2014 Grid Reference: 583. 458 Deposit Reference: -
Location Address1 Address2 Address3 Postcode Asset Type
Location Address1 Address2 Address3 Postcode Asset Type Description Tenure Alverstone Land Alverstone Shute Alverstone PO36 0NT Land Freehold Alverstone Grazing Land Alverstone Shute Alverstone PO36 0NT Grazing Land Freehold Arreton Branstone Farm Study Centre Main Road Branstone PO36 0LT Education Other/Childrens Services Freehold Arreton Stockmans House Main Road Branstone PO36 0LT Housing Freehold Arreton St George`s CE Primary School Main Road Arreton PO30 3AD Schools Freehold Arreton Land Off Hazley Combe Arreton PO30 3AD Non-Operational Freehold Arreton Land Main Road Arreton PO30 3AB Schools Leased Arreton Land Arreton Down Arreton PO30 2PA Non-Operational Leased Bembridge Bembridge Library Church Road Bembridge PO35 5NA Libraries Freehold Bembridge Coastguard Lookout Beachfield Road Bembridge PO35 5TN Non-Operational Freehold Bembridge Forelands Middle School Walls Road Bembridge PO35 5RH Schools Freehold Bembridge Bembridge Fire Station Walls Road Bembridge PO35 5RH Fire & Rescue Freehold Bembridge Bembridge CE Primary Steyne Road Bembridge PO35 5UH Schools Freehold Bembridge Toilets Lane End Bembridge PO35 5TB Public Conveniences Freehold Bembridge RNLI Life Boat Station Lane End Bembridge PO35 5TB Coastal Freehold Bembridge Car Park Lane End Forelands PO35 5UE Car Parks Freehold Bembridge Toilets Beach Road / Station Road Bembridge PO35 5NQ Public Conveniences Freehold Bembridge Toilet High Street Bembridge PO35 5SE Public Conveniences Freehold Bembridge Toilets High Street Bembridge PO35 5SD Public Conveniences Freehold Bembridge -
Sites of Importance for Nature Conservation Sincs Hampshire.Pdf
Sites of Importance for Nature Conservation (SINCs) within Hampshire © Hampshire Biodiversity Information Centre No part of this documentHBIC may be reproduced, stored in a retrieval system or transmitted in any form or by any means electronic, mechanical, photocopying, recoding or otherwise without the prior permission of the Hampshire Biodiversity Information Centre Central Grid SINC Ref District SINC Name Ref. SINC Criteria Area (ha) BD0001 Basingstoke & Deane Straits Copse, St. Mary Bourne SU38905040 1A 2.14 BD0002 Basingstoke & Deane Lee's Wood SU39005080 1A 1.99 BD0003 Basingstoke & Deane Great Wallop Hill Copse SU39005200 1A/1B 21.07 BD0004 Basingstoke & Deane Hackwood Copse SU39504950 1A 11.74 BD0005 Basingstoke & Deane Stokehill Farm Down SU39605130 2A 4.02 BD0006 Basingstoke & Deane Juniper Rough SU39605289 2D 1.16 BD0007 Basingstoke & Deane Leafy Grove Copse SU39685080 1A 1.83 BD0008 Basingstoke & Deane Trinley Wood SU39804900 1A 6.58 BD0009 Basingstoke & Deane East Woodhay Down SU39806040 2A 29.57 BD0010 Basingstoke & Deane Ten Acre Brow (East) SU39965580 1A 0.55 BD0011 Basingstoke & Deane Berries Copse SU40106240 1A 2.93 BD0012 Basingstoke & Deane Sidley Wood North SU40305590 1A 3.63 BD0013 Basingstoke & Deane The Oaks Grassland SU40405920 2A 1.12 BD0014 Basingstoke & Deane Sidley Wood South SU40505520 1B 1.87 BD0015 Basingstoke & Deane West Of Codley Copse SU40505680 2D/6A 0.68 BD0016 Basingstoke & Deane Hitchen Copse SU40505850 1A 13.91 BD0017 Basingstoke & Deane Pilot Hill: Field To The South-East SU40505900 2A/6A 4.62 -
English Nature Research Report
Maritime Natural Area: MIO. Whitstable to Geological Significance: Notable North Foreland (provisional) General geologicaVgeomorpholugicaIcharactcr: The Whitstable to North Foreland Maritime Natural Area has a varied coastline with relatively low-lying coast in thc cast rising to boulder clay and chalk cliffs towards the Isle of Thanet. Geological Htrtory: This coastline is characterised by the Cretaceous chalk of the Isle oTThanet bounded to the west by clays, silts and sands of the Lower ‘I’ertiary. Upper Cretaceous Santonian chalk (87-83 Ma) is exposed dipping gently to the west from Margatc to the eastern side of Herne Bay. Unconformably overlying the chalk is a sequence of Lower Tertiary scdiments which are exposed in I Ierne Bay; the Palaeocenc Thanet, Woolwicli and Oldhaven Formations overlain by the Eocene London Clay Formation. The Chalk was deposited by a shallow sea which covered much of Northwestern Europe towards the end of the Cretaceous. Sea lcvel fall was followed by the unconformabie deposition of Tertiary Palaeocene and Ikcene sedirnents. Dominantly marine in origin, these scdiments were deposited by a rising, but fluctuating sea, which covered much of Southeast England. Marine conditions were well established by the Eocene leading to the deposition ofthe i,ondon Clay Formation. Thc fossil fauna and flora from the Tertiary rocks indicates a gradually warming climate with sub-tropical conditions established by the Eocene. Subsequent uplilt (associated with the Alpine Orogeny) and resultant erosion removed much of the remaining Tertiary sediments, the next deposition occurring during the Pleistocene. Though not covercd by ice, the area was affectcd by periglacial erosion in a tundra-like environment during the last glaciation (Devensian). -
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). -
Habitats Regulations Assessment for the Portsmouth Site Allocations Document
Habitats Regulations Assessment for the Portsmouth Site Allocations Document Screening Statement Client: Portsmouth City Council UE-0060 Portsmouth CC Site Allocations Report No.: HRA Screening_6_20130219 Version: 6 Status: Draft Final Date: February 2013 Author: SPS/NEJP Checked: SPS Approved: NEJP HRA for the Portsmouth Site Allocations Development Plan Document: Screening Statement February 2013 UE-0060 Portsmouth CC Site Allocations HRA Screening_6_20130219 Contents Executive Summary i E1 Introduction i E2 Scope of the Assessment i E3 Findings ii E4 Conclusions and Consultation Arrangements iii 1 Introduction 1 1.1 Background 1 1.2 Purpose and Structure of this Document 1 1.3 Habitats Regulations Assessment 2 1.4 Portsmouth Local Development Framework 3 2 Methodology 7 2.1 Guidance and Best Practice 7 2.2 Methodology 7 2.3 Consideration of Effects 8 3 European Sites 11 3.1 Scope of the Assessment 11 3.2 Site Descriptions 11 3.3 Qualifying Features 11 3.4 SAC and SPA Conservation Objectives 16 3.5 Conservation Objectives for Ramsar Sites 17 3.6 Key Environmental Conditions Supporting Site Integrity 17 4 Likely Significant Effects 19 4.1 Introduction 19 4.2 Results 19 4.3 In Combination Test 21 5 Commentary 23 5.1 Introduction 23 HRA for the Portsmouth Site Allocations Development Plan Document: Screening Statement February 2013 UE-0060 Portsmouth CC Site Allocations HRA Screening_6_20130219 5.2 Strategically Operating Impacts 23 5.3 Dark-bellied Brent Goose and Waders 24 5.4 Sites Proposed for Allocation 25 6 Screening Statement and