120. Wealden Greensand Area Profile: Supporting Documents
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Property for Sale in Ash Surrey
Property For Sale In Ash Surrey Baking Lenard symbolizes intertwistingly while Mohan always disseise his abscesses bereaving consciously, he stellifies so right-about. Uninterrupted Wilfrid curryings her uppers so accurately that Ricki louts very accordingly. Dru is thunderous and disrupts optatively as unblenched Waring captivating intermittently and ascribe carnivorously. Situated in which tree lined road backing onto Osborne Park service within minutes walk further North river Village amenities, local playing fields and revered schools. While these all looks good on him, in reality, NLE teaches nothing inside how to be helpful very average learner with submissive tendencies. Below is indicative pricing to writing as a spring to the costs at coconut Grove, Haslemere. No domain for LCPS guidelines, no its for safety. Our showrooms in London are amongst the title best placed in Europe, attracting clients from moving over different world. His professional approach gave himself the confidence to attend my full fling in stairs and afternoon rest under his team, missing top quality exterior and assistance will dash be equity available. Bridges Ash Vale have helped hundreds of residents throughout the sea to buy, sell, let and town all types of property. Find this Dream Home. Freshly painted throughout and brand new carpet. Each feature of the James is designed with you and your family her mind. They are dedicated to providing the you best adhere the students. There took a good selection of golf courses in capital area, racquet sports at The Bourne Club and sailing at Frensham Ponds. Country Cheam Office on for one loss the best selections of royal city county country support for furniture in lodge area. -
THE SERPENT TRAIL11.3Km 7 Miles 1 OFFICIAL GUIDE
SOUTH DOWNS WALKS ST THE SERPENT TRAIL11.3km 7 miles 1 OFFICIAL GUIDE ! HELPFUL HINT NATIONAL PARK The A286 Bell Road is a busy crossing point on the Trail. The A286 Bell Road is a busy crossing point on the Trail. West of Bell Road (A286) take the path that goes up between the houses, then across Marley Hanger and again up between two houses on a tarmac path with hand rail. 1 THE SERPENT TRAIL HOW TO GET THERE From rolling hills to bustling market towns, The name of the Trail reflects the serpentine ON FOOT BY RAIL the South Downs National Park’s (SDNP) shape of the route. Starting with the serpent’s The Greensand Way (running from Ham The train stations of Haslemere, Liss, 2 ‘tongue’ in Haslemere High Street, Surrey; landscapes cover 1,600km of breathtaking Street in Kent to Haslemere in Surrey) Liphook and Petersfield are all close to the views, hidden gems and quintessentially the route leads to the ‘head’ at Black Down, West Sussex and from there the ‘body’ finishes on the opposite side of Haslemere Trail. Visit nationalrail.co.uk to plan English scenery. A rich tapestry of turns west, east and west again along High Street from the start of the Serpent your journey. wildlife, landscapes, tranquillity and visitor the greensand ridges. The trail ‘snakes’ Trail. The Hangers Way (running from attractions, weave together a story of Alton to the Queen Elizabeth Country Park by Liphook, Milland, Fernhurst, Petworth, BY BUS people and place in harmony. in Hampshire) crosses Heath Road Fittleworth, Duncton, Heyshott, Midhurst, Bus services run to Midhurst, Stedham, in Petersfield just along the road from Stedham and Nyewood to finally reach the Trotton, Nyewood, Rogate, Petersfield, Embodying the everyday meeting of history the end of the Serpent Trail on Petersfield serpent’s ‘tail’ at Petersfield in Hampshire. -
A Fragment of the Geography of England. South West Sussex Author(S): Hugh Robert Mill Source: the Geographical Journal, Vol
A Fragment of the Geography of England. South West Sussex Author(s): Hugh Robert Mill Source: The Geographical Journal, Vol. 15, No. 3 (Mar., 1900), pp. 205-227 Published by: geographicalj Stable URL: http://www.jstor.org/stable/1774689 Accessed: 27-06-2016 19:49 UTC Your use of the JSTOR archive indicates your acceptance of the Terms & Conditions of Use, available at http://about.jstor.org/terms JSTOR is a not-for-profit service that helps scholars, researchers, and students discover, use, and build upon a wide range of content in a trusted digital archive. We use information technology and tools to increase productivity and facilitate new forms of scholarship. For more information about JSTOR, please contact [email protected]. The Royal Geographical Society (with the Institute of British Geographers), Wiley are collaborating with JSTOR to digitize, preserve and extend access to The Geographical Journal This content downloaded from 165.193.178.102 on Mon, 27 Jun 2016 19:49:48 UTC All use subject to http://about.jstor.org/terms The Geographical Journal. No. 3. MARPCH, 1900. VOL. XV. A FRAGMENT OF THE GEOGRAPHY OF ENGLAND. SOUTH WEST SUSSEX.' By HUGH ROBERT MILL, D.Sc., F.R.S.E. Introductory.-In 1896 I proposed a scheme for a geographical description of the United Kingdom, based on the maps of the Ordnance Survey, and consisting of a separate memoir for every sheet of the map on the scale of 1 inch to a mile.t I was requested by the Royal Geographical Society to prepare a specimen memoir, and, by the advice of Sir John Farquharson, then Director-General of the Ordnance Survey, chose Sheet No. -
The Ultra Participant Information Pack
www.surreyhillschallenge.co.uk THE ULTRA PARTICIPANT INFORMATION PACK 23/09/2018 INTRODUCTION www.surreyhillschallenge.co.uk Welcome We are delighted to welcome you to the Surrey Hills Challenge on Sunday 23rd September 2018. You have entered the Ultra, our 60km off road running challenge. The point to point route is from Haslemere to Dorking along the Greensand Way with a 12 hour cut off period. The postcode to find the start is GU27 2AS, and there will be yellow directional signage to help you find us. Parking is free on Sundays and there are a number of car parks to choose from. In the main centre of Haslemere, you can park at the High Street pay and display car park or at the Chestnut Avenue pay and display car park (better for longer periods). If you want to park close to the train station, or park for a long period of time during the day, Tanners Lane and Weydown Road pay and display car parks are close to the station. Itinerary Time Activity 05:30 Doors open at Haslemere Hall, Bridge Rd, Haslemere GU27 2AS 2AS 06:00 Registration opens • Runner registration and bib collection • Finish Line Bag deposit open 06:40 Race brief 06:50 100m walk to start line 07:00 Start of Ultra 19:00 Cut off and race finish at Denbies Wine Estate (London Road, Dorking RH5 6AA) Route Conditions The route mainly follows the Greensand Way, which originates in Haslemere and continues east to Kent. It’s marked with official ‘GW’ and ‘Greensand Way’ signs and will also be marked up by our team with approximately 200 directional fluorescent signs. -
The Serpent Trail 2 the SERPENT TRAIL GUIDE the SERPENT TRAIL GUIDE 3
The Serpent Trail 2 THE SERPENT TRAIL GUIDE THE SERPENT TRAIL GUIDE 3 Contents THE SERPENT TRAIL The Serpent Trail ...........................................3 6. Henley to Petworth, via Bexleyhill, Explore the heathlands of the South Downs National Park by Wildlife ..........................................................4 River Common and Upperton ............. 22 Heathland timeline .......................................8 7. Petworth to Fittleworth ........................ 24 following the 65 mile/106 km long Serpent Trail. Heathland Today ........................................ 10 8. Hesworth Common, Lord’s Piece and Discover this beautiful and internationally The name of the Trail reflects the serpentine Burton Park ........................................... 26 Heathland Stories Through Sculpture ....... 10 rare lowland heath habitat, 80% of which shape of the route. Starting with the serpent’s 9. Duncton Common to Cocking has been lost since the early 1800s, often head and tongue in Haslemere and Black 1. Black Down to Marley Common ......... 12 Causeway ............................................. 28 through neglect and tree planting on Down, the ‘body’ turns west, east and west 2. Marley Common through Lynchmere 10. Midhurst, Stedham and Iping previously open areas. Designed to highlight again along the greensand ridges. The Trail and Stanley Commons to Iron Hill ...... 14 Commons ............................................. 30 the outstanding landscape of the greensand ‘snakes’ by Liphook, Milland, Fernhurst, 3. From Shufflesheeps to Combe Hill hills, their wildlife, history and conservation, Petworth, Fittleworth, Duncton, Heyshott, 11. Nyewood to Petersfield ....................... 32 via Chapel Common ............................ 16 the Serpent Trail passes through the purple Midhurst, Stedham and Nyewood to finally Heathlands Reunited Partnership .............. 34 4. Combe Hill, Tullecombe, through heather, green woods and golden valleys of reach the serpent’s ‘tail’ at Petersfield in Rondle Wood to Borden Lane ........... -
Greensand.Pdf
www.natureswayresources.com GREENSAND Greensand is a naturallyoccurring mineral mined from ocean deposits from a sedimentary rock known as “Glauconite”. It is often an olive-green colored sandstonerock found in layers in many sedimentary rock formations. Origin of Greensand Greensand forms in anoxic (without oxygen) marine environments that are rich in organic detritus and low in sedimentary inputs. Some greensands contain marine fossils (i.e. New Jersey Greensand). Greensand has been found in deposits all over the world. The greenish color comes from the mineral glauconite and iron potassiumsilicate that weathers and breaks down releasing the stored minerals. The color may range from a dark greenish gray, green-black to blue-green dependingon the minerals and water content. It often weatherseasilyand forms nodules that have been oxidized with iron bearing minerals that has a reddish brown or rust color. +3 The major chemical description is ((K,Na)(Fe , Al, Mg)2(Si,Al)4O10(OH)2) General chemical information: Iron (Fe) 12-19% Potassium (K) 5-7 % Silicon (Si) 25.0% Oxygen (O) 45% Magnesium (Mg) 2-3 % Aluminum (Al) 1.9 % Sodium (Na) 0.27% Hydrogen (H) 0.47% Over 30 other trace minerals and many micronutrients. Types of Greensand Glauconite is the namegiven to a group of naturally occurring iron rich silica minerals that may be composed of pellets or grains. When glauconite is mined the upper layers that have weathered and become oxidizedand minerals are released.These sometimes form pyrite a iron sulfide (FeS2) when oxygen is www.natureswayresources.com absent. In the deeper layers or reduced zone pyrite crystals often form. -
Geology and the Landscape of the North Wessex Downs Factsheet
Factsheet Geology and the Landscape of the North Wessex Downs The majority of the North Wessex Downs is underlain by chalk resulting in the beautiful gentle rolling topography which is so characteristic of the North Wessex Downs. The area is influenced by geological formations from the Cretaceous, Palaeogene and Quaternary periods. There is also a direct link between the building materials used in the AONB and the local underlying geology. This is explored in the leaflet 'Diversity in Stone' Geological History of the North Wessex Downs Lower Cretaceous (145 – 99 million years ago) Only the top most part of the Lower Cretaceous (the Gault Clay and the Upper Greensand) are found in the AONB. The Gault Clay is restricted to a narrow band marking the foot of the Downs on the northern margin. This blue-grey mudstone has historically been extracted from the Swindon and Devizes area for brick making. The junction between the Gault Clay and the overlying Upper Greensand is marked on the northern edge of the AONB by a spring line which gave rise to the development of the villages such as Cherhill and Uffington. The sands and silts of the Upper Greensand are rich in a mineral called glauconite, giving them their green colour. As well as tracing the northern scarp of the AONB the Upper Greensand is also seen at the surface in the Vale of Pewsey, as a result of the uplift of the basin. Towards the top of the Upper Greensand is a bed known as the Malmstone. This is a hard sandstone composed of siliceous spicules held together with a silica rich cement. -
A Revised Taxonomy of the Iguanodont Dinosaur Genera and Species
ARTICLE IN PRESS + MODEL Cretaceous Research xx (2007) 1e25 www.elsevier.com/locate/CretRes A revised taxonomy of the iguanodont dinosaur genera and species Gregory S. Paul 3109 North Calvert Station, Side Apartment, Baltimore, MD 21218-3807, USA Received 20 April 2006; accepted in revised form 27 April 2007 Abstract Criteria for designating dinosaur genera are inconsistent; some very similar species are highly split at the generic level, other anatomically disparate species are united at the same rank. Since the mid-1800s the classic genus Iguanodon has become a taxonomic grab-bag containing species spanning most of the Early Cretaceous of the northern hemisphere. Recently the genus was radically redesignated when the type was shifted from nondiagnostic English Valanginian teeth to a complete skull and skeleton of the heavily built, semi-quadrupedal I. bernissartensis from much younger Belgian sediments, even though the latter is very different in form from the gracile skeletal remains described by Mantell. Currently, iguanodont remains from Europe are usually assigned to either robust I. bernissartensis or gracile I. atherfieldensis, regardless of lo- cation or stage. A stratigraphic analysis is combined with a character census that shows the European iguanodonts are markedly more morpho- logically divergent than other dinosaur genera, and some appear phylogenetically more derived than others. Two new genera and a new species have been or are named for the gracile iguanodonts of the Wealden Supergroup; strongly bipedal Mantellisaurus atherfieldensis Paul (2006. Turning the old into the new: a separate genus for the gracile iguanodont from the Wealden of England. In: Carpenter, K. (Ed.), Horns and Beaks: Ceratopsian and Ornithopod Dinosaurs. -
(Foram in Ifers, Algae) and Stratigraphy, Carboniferous
MicropaIeontoIogicaI Zonation (Foramin ifers, Algae) and Stratigraphy, Carboniferous Peratrovich Formation, Southeastern Alaska By BERNARD L. MAMET, SYLVIE PINARD, and AUGUSTUS K. ARMSTRONG U.S. GEOLOGICAL SURVEY BULLETIN 2031 U.S. DEPARTMENT OF THE INTERIOR BRUCE BABBITT, Secretary U.S. GEOLOGICAL SURVEY Robert M. Hirsch, Acting Director Any use of trade, product, or firm names in this publication is for descriptive purposes only and does not imply endorsement by the U.S. Government Text and illustrations edited by Mary Lou Callas Line drawings prepared by B.L. Mamet and Stephen Scott Layout and design by Lisa Baserga UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1993 For sale by Book and Open-File Report Sales U.S. Geological Survey Federal Center, Box 25286 Denver, CO 80225 Library of Congress Cataloging in Publication Data Mamet, Bernard L. Micropaleontological zonation (foraminifers, algae) and stratigraphy, Carboniferous Peratrovich Formation, southeastern Alaska / by Bernard L. Mamet, Sylvie Pinard, and Augustus K. Armstrong. p. cm.-(U.S. Geological Survey bulletin ; 2031) Includes bibtiographical references. 1. Geology, Stratigraphic-Carboniferous. 2. Geology-Alaska-Prince of Wales Island. 3. Foraminifera, Fossil-Alaska-Prince of Wales Island. 4. Algae, Fossil-Alaska-Prince of Wales Island. 5. Paleontology- Carboniferous. 6. Paleontology-Alaska-Prince of Wales Island. I. Pinard, Sylvie. II. Armstrong, Augustus K. Ill. Title. IV. Series. QE75.B9 no. 2031 [QE671I 557.3 s--dc20 [551.7'5'097982] 92-32905 CIP CONTENTS Abstract -
Dinosaurs British Isles
DINOSAURS of the BRITISH ISLES Dean R. Lomax & Nobumichi Tamura Foreword by Dr Paul M. Barrett (Natural History Museum, London) Skeletal reconstructions by Scott Hartman, Jaime A. Headden & Gregory S. Paul Life and scene reconstructions by Nobumichi Tamura & James McKay CONTENTS Foreword by Dr Paul M. Barrett.............................................................................10 Foreword by the authors........................................................................................11 Acknowledgements................................................................................................12 Museum and institutional abbreviations...............................................................13 Introduction: An age-old interest..........................................................................16 What is a dinosaur?................................................................................................18 The question of birds and the ‘extinction’ of the dinosaurs..................................25 The age of dinosaurs..............................................................................................30 Taxonomy: The naming of species.......................................................................34 Dinosaur classification...........................................................................................37 Saurischian dinosaurs............................................................................................39 Theropoda............................................................................................................39 -
Surrey Hills Aonb Areas of Search
CONFIDENTIAL SURREY COUNTY COUNCIL LCA PHASE 2 SURREY HILLS AONB AREAS OF SEARCH NATURAL BEAUTY EVALUATION by Hankinson Duckett Associates HDA ref: 595.1 October 2013 hankinson duckett associates t 01491 838175 f 01491 838997 e [email protected] w www.hda-enviro.co.uk The Stables, Howbery Park, Benson Lane, Wallingford, Oxfordshire, OX10 8BA Hankinson Duckett Associates Limited Registered in England & Wales 3462810 Registered Office: The Stables, Howbery Park, Benson Lane, Wallingford, OX10 8BA CONTENTS Page 1 Introduction ................................................................................................................................... 1 2 Assessment Background ............................................................................................................. 1 Table 1: LCA Landscape Types and Character Areas ...................................................................................... 2 3 Methodology ................................................................................................................................. 5 4 Guidance ....................................................................................................................................... 6 Table 2: Natural England Guidance Factors and Sub-factors ........................................................................... 6 4.5 Application of the Guidance ............................................................................................................................. 10 5 The Surrey Hills Landscape -
(See P2) SURREY ARCHAEOLOGICAL SOCIETY
Registered Charity No: 272098 ISSN 0585-9980 SURREY ARCHAEOLOGICAL SOCIETY CASTLE ARCH, GUILDFORD GU1 3SX Tel: 01483 532454 E-mail: [email protected] Website: www.surreyarchaeology.org.uk Bulletin 471 December 2018 HAVE YOUR SAY ON SURREY HERITAGE’S FUTURE (see p2) Council News Consultation on proposed cut-back at Surrey History Centre David Bird Surrey County Council is proposing very signifi- cant cuts to several services including those provided by the Library and Cultural Service Department. The cost of running Surrey History Centre is met within the Library and Cultural Services Department and the proposed cut in the annual budget for the whole department from £8.7m to £4.0m would, if implemented, have a dramatic effect on every aspect including Surrey History Centre. Many of us work with or make use of the Surrey County Council services under review and know the quality of the staff and how greatly research by ourselves and others will be affected if the proposed cuts go ahead. It would be a sad state of affairs if a county such as our own cannot adequately provide services such as these that enhance the quality of life and sense of place for all our residents and visitors. Please take the time to read the details of the consultation and, if you are willing, use link below to respond: www.surreysays.co.uk/legal-and-democratic-services/libraries The further link to the on-line consultation is at the bottom of the ‘Have your say’ page you first reach. You will find several questions are about libraries but the write-in spaces in sections 2.1 and 4.3 give you the chance to say what you think about Heritage.