Report IOW 5: Chilton Chine to Colwell Chine
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Road Name Town 123456
List of roads treated APPENDIX 1 P1 Priority Snow Clearance Route P1 and P2 Precautionary Salting Routes SALT OUTE P1 OUTE SALT P2 OUTE SALT ROAD CLASS ROUTE NUMBER SECTION ROAD NAME TOWN 123456 ADELAIDE GROVE EAST COWES C R 1 All 1 - - - - - AFTON ROAD FRESHWATER A R 5 Newport Rd to Freshwater Bay - - - - 5 - AFTON ROAD FRESHWATER A R 6 School Green Rd to Newport Rd - - - - - 6 ALBERT STREET VENTNOR A R 3 All - - 3 - - - ALEXANDRA ROAD RYDE B R 1 St Johns Hill to Gt Preston Rd 1 - - - - - ALEXANDRA ROAD RYDE B R 1 St Johns Hill to Easthill Rd 1 - - - - - ALPINE ROAD VENTNOR A R 3 - - 3 - - - ALUM BAY NEW ROAD TOTLAND B R 6 Church Hill to Cliff Road - - - - - 6 ALVERSTONE ROAD NEWCHURCH C R 3 Newport Rd to Forest Rd / All - - 3 - - - ALVERSTONE SHUTE NEWCHURCH C R 3 All - - 3 - - - APPLEFORD ROAD GODSHILL C R 4 All - - - 4 - - APPLEY ROAD RYDE B R 1 Easthill Rd to Marlborough Rd 1 - - - - - APPLEY ROAD RYDE B R 2 Marlborough Rd to Puckpool Hill - 2 - - - - ARGYLL STREET RYDE R 1 All 1 - - - - - ARRETON ROAD ARRETON A R 3 All - - 3 - - - ARRETON STREET ARRETON A R 3 All - - 3 - - - ARTHURS HILL SHANKLIN A R 3 All - - 3 - - - ASHEY ROAD RYDE C R 1 Upton Rd to Smallbrook Lane 1 - - - - - ASHEY ROAD RYDE C R 2 Smallbrook Lane to Brading Down - 2 - - - - ATHERLEY ROAD SHANKLIN C R 3 All - - 3 - - - AVENUE ROAD FRESHWATER A R 6 All - - - - - 6 AVENUE ROAD SANDOWN A B R 3 All - - 3 - - - BARING ROAD COWES R 6 - - - - - 6 BARRACK SHUTE NITON A R 4 All - - - 4 - - BEACHFIELD ROAD SANDOWN B R 3 All - - 3 - - - BEAPER SHUTE BRADING A R 2 All - 2 -
From Francois De Quesnay Le Despotisme De La Chine (1767)
From Francois de Quesnay Le despotisme de la Chine (1767) [translation by Lewis A. Maverick in China, A Model for Europe (1946)] [Francois de Quesnay (1694-1774) came from a modest provincial family but rose into the middle class with his marriage. He was first apprenticed to an engraver but then turned to the study of surgery and was practicing as a surgeon in the early 1730's. In 1744 he received a medical degree and was therefore qualified as a physician as well as a surgeon and shifted his activity in the latter direction. In 1748, on the recommendation of aristocratic patients, he became physician to Madame de Pompadour, Louis XV's mistress. In 1752 he successfully treated the Dauphin (crown prince) for smallpox and was then appointed as one of the physicians to the King. While serving at court he became interested in economic, political, and social problems and by 1758 was a member of the small group of economists known as "Physiocrats." Their main contribution to economic thinking involved analogizing the economy to the human body and seeing economic prosperity as a matter of ensuring the circulation of money and goods. The Physiocrats became well-known throughout Europe, and were visited by both David Hume and Adam Smith in the 1760s. The Physiocrats took up the cause of agricultural reform, and then broadened their concern to fiscal matters and finally to political reform more generally. They were not democrats; rather they looked to a strong monarchy to adopt and push through the needed reforms. Like many other Frenchman of the mid 18th-century, the Physiocrats saw China as an ideal and modeled many of their proposals after what they believed was Chinese practice. -
The Isle of Wight Coast Path Guided Trail Holiday
The Isle of Wight Coast Path Guided Trail Holiday Tour Style: Guided Trails Destinations: Isle of Wight & England Trip code: FWLIC Trip Walking Grade: 3 HOLIDAY OVERVIEW The Isle of Wight Coast Path circuits the island in an anti-clockwise direction and provides a wonderful opportunity to view the island’s beautiful and varied coastline, including the chalk headlands of the Needles and Culver Cliff. The trail is interspersed with pretty coastal villages and Victorian resorts such as Ventnor. It includes some inland walking around Queen Victoria’s Osborne Estate, Cowes and Newtown Harbour National Nature Reserve. WHAT'S INCLUDED • High quality en-suite accommodation in our country house • Full board from dinner upon arrival to breakfast on departure day • The services of an HF Holidays' walks leader • All transport on walking days www.hfholidays.co.uk PAGE 1 [email protected] Tel: +44(0) 20 3974 8865 HOLIDAYS HIGHLIGHTS • A circuit of the Isle of Wight coast • The dramatic chalk headlands of the Needles and Culver Cliff • Stay at Freshwater Bay House TRIP SUITABILITY This Guided Walking/Hiking Trail is graded 3 which involves walks/hikes on generally good paths, but with some long walking days. There may be some sections over rough or steep terrain and will require a good level of fitness as you will be walking every day. It is your responsibility to ensure you have the relevant fitness required to join this holiday. Fitness We want you to be confident that you can meet the demands of each walking day and get the most out of your holiday. -
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. -
Historic Environment Action Plan South-West Wight Coastal Zone
Island Heritage Service Historic Environment Action Plan South-West Wight Coastal Zone Isle of Wight County Archaeology and Historic Environment Service October 2008 01983 823810 archaeology @iow.gov.uk Iwight.com HEAP for South-West Wight Coastal Zone 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. Essential characteristics of the South-West Wight Coastal Zone include the long coastline and cliffs containing fossils and archaeological material, the pattern of historic lanes, tracks and boundaries, field patterns showing evidence of open-field enclosure, valley-floor land, historic villages, hamlets and dispersed farmsteads, and vernacular architecture. The Military Road provides a scenic and historically significant route along the coast. The settlements of Mottistone, Hulverstone, Brighstone and Shorwell straddle the boundary between this Area and the West Wight Downland Edge & Sandstone Ridge. Historically these settlements exploited both Areas. For the sake of convenience these settlements are described in the HEAP Area document for the West Wight Downland Edge & Sandstone Ridge even where they fall partially within this Area. However, they are also referred to in this HEAP document where appropriate. This document considers the most significant features of the historic landscape, the most important forces for change, and the key management issues. 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 • Occupies strip of land between West Wight Downland Edge & Sandstone Ridge and coast. • Coastline within this Area stretches from Compton to Shepherd’s Chine and comprises soft, eroding cliffs with areas of landslip. -
461 I. Introduction. and Cardita Deltoidea +
Downloaded from http://jgslegacy.lyellcollection.org/ at University of Oregon on June 23, 2016 ON THE F~0CENE AI~D 0LI60OENE OF THE HAMPSHIRE BASIN. 461 45. On the RELATIONS of the EocEnE and OLIa0CEN~ STRATA in the HA~trSHIR~. BASlI~. By Prof. JoH~ W. JuDD, F.R.S., See. G.S. (Read April 26, 1882.) I. Introduction. SI~cx the publication of my paper "On the Oligocene Strata of the Hampshire Basin" *, I have been favoured with many valuable suggestions and criticisms from geologists, both in this and other countries ; and the time has now perhaps arrived when some of the interesting c!uestions thus raised may be discussed with advantage. The great object of my former memoir was to determine the age and relations of a series of marine beds which contain a highly interesting fauna--a fauna presenting the closest affinities with that of a well-defined system of strata very widely distributed in Central Europe. In framing his classification of the Hampshire Tertiaries, the late Prof. Edward Forbes gave no pIace t~ this important series of beds--a fact which does not seam t~ Iiave bt~ea Strfiiciently considered by those among my critics who h~ve ~mm'rea.r ~ay proposed modifi- cation of Forbes's classification as tmaecessary-ahd, therefore, un- warrantable. The history of the discovery of this i~tevestiug marine series does not appear to be generally known. The late Sir Charles Lycll spent his earliest years in the New Forest, residing at Bartley Lodge near Lyndhurst. At that time shelly marls appear to have been in great request among agriculturists, being employed by them as a manure on some of the poorer soils, like the similar materials of the French Fahluns and our own Crags. -
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. -
The Boundary Committee for England Further Electoral
SHEET 2, MAP 2 Isle of Wight County. Proposed Electoral Divisions in Totland and Freshwater Pier MH W Sconce Point LW Pier M HW W M M H LW M Pier A Fort 3 LW 05 H M 4 ur Victoria st B ea ch T H S B IG H 3 4 S Playing Field Cemy 0 Hurst Castle O 1 W U E T S H T T S H H T D O I A L O R R L Norton Grange N L R O S E L lway Village I NY antled Rai Y A D V N Dism E TE R N A e 3 f R D E 05 A 3054 4 R D YARMOUTH Recreation Ground ok Bro R y Yarmouth C of E rle iv ho e Primary School T r Fort Victoria Country Park Round Tower Point Y a Norton r THE BOUNDARY COMMITTEE FOR ENGLAND E r T te a U H W S w Christchurch Bay o S L T T n E FURTHER ELECTORAL REVIEW OF ISLE OF WIGHT a L e L E M r A N te H A a L W E h C g A i L H P n a L e IL M H Draft Recommendations for Electoral Division Boundaries in the County of the Isle of Wight October 2007 Dismantled Railway Cliff End Fort Thorley Manor Sheet 2 of 9 Albert ay w l i a Holly R ed Farm tl n T ho ma rl s e i y D B ro o k Cliff End B 3401 Thorley D ef E This map is based upon Ordnance Survey material with the permission of Ordnance Survey on behalf of N A L the Controller of Her Majesty's Stationery Office © Crown copyright. -
Coastal Processes Review
Water and Environment Management Framework Lot 3 – Engineering and Related Services West Wight Coastal Flood and Erosion Risk Management Strategy Appendix C - Coastal Processes and Geotechnics Summary August 2015 Document overview Capita | AECOM was commissioned by the Isle of Wight Council in October 2014 to undertake a Coastal Flood and Erosion Risk Management Strategy. As part of this commission, a brief review of coastal processes and geotechnics has been undertaken to inform the option development phase of the Strategy. Document history Version Status Issue date Prepared by Reviewed by Approved by George Batt – Assistant Coastal Jonathan Short Engineer Tara-Leigh Draft for – 1 30th March 2015 Jason McVey – comment Senior Coastal Drummond – Associate Specialist Principal Flood and Coastal Specialist George Batt – Assistant Coastal Updated Jonathan Short Engineer Tara-Leigh following – 2 4th August 2015 Jason McVey – client Senior Coastal Drummond – Associate comments Specialist Principal Flood and Coastal Specialist Scott House, Alencon Link, Basingstoke, Hampshire, RG21 7PP. i Limitations Capita Property and Infrastructure Ltd (“Capita”) | URS Infrastructure & Environment UK Limited (“AECOM”) has prepared this Report for the sole use of the Isle of Wight Council in accordance with the Agreement under which our services were performed. No other warranty, expressed or implied, is made as to the professional advice included in this Report or any other services provided by Capita | AECOM. This Report is confidential and may not be disclosed by the Client nor relied upon by any other party without the prior and express written agreement of Capita | AECOM. The conclusions and recommendations contained in this Report are based upon information provided by others and upon the assumption that all relevant information has been provided by those parties from whom it has been requested and that such information is accurate. -
To Download the Document 'LAF Minutes 07
Minutes & Information resulting from – Meeting 64 1st Newport Scout Hall, Woodbine Close, Newport Thursday 7th March 2019 Present at the meeting Forum Members: Others & Observers: Mark Earp - Chairman Jennine Gardiner-IWC PROW (LAF Secretary) Alec Lawson David Howarth – Observer / IWRA Steve Darch Helena Hewston – Observer / Shalfleet P/C Cllr Paul Fuller Diana Conyers - Ryde T/C John Gurney-Champion John Brownscombe – National Trust Tricia Merrifield Darrel Clarke - IWC Cllr John Hobart Mick Lyons –Havenstreet & Ashey PC Richard Grogan Cllr Steve Hastings John Heather Clare Bennett - CLA Mike Slater Gillian Belben – Gatcombe & Chillerton P/C Penny Edwards 1. Apologies Received, Confirmation of the Minutes of previous meeting, declarations of interest & introductions. Apologies: Stephen Cockett, Geoff Brodie, Jan Brooks, Mike Greenslade, Hugh Walding Confirmation – Done & minutes signed as a true copy Decelerations - None 2. Updates to tasks / matters arising from meeting 6 December 2018 Bus Stops – Mark Earp and a team of four inspected as many rural bus stops as they could. It was felt that by and large these were pretty good but a few do need improvement. All bus stops had a post and a current timetable. There had been grant out for sustainable travel called the “Innovation fund” Mark wondered if anyone had applied for concreate pads, to be funded, at any of the rural bus stop locations? The General Manager for Southern Vectis Mr Richard Tyldsley has been invited to the next LAF meeting. Prior to this LAF members / guests should take time to look at the rural bus stop locations in their areas and using their local knowledge have given feedback to the LAF of any unsafe or redundant ones. -
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 -
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).