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Hingston Down Hingston Down HINGSTON DOWN HINGSTON DOWN Hanson Collect & Go is a new, dedicated service for our asphalt collect customers. It allows you to quickly and easily purchase your quality-assured asphalt so you can get to your next job. We have a priority weighbridge and designated bin for hot boxes. Refreshments are available, as well as key tools of the trade including spades, sealants, rakes, brushes and wheelbarrows. HOW TO COLLECT FROM US Our loyalty scheme means you now get more out of every visit. You will receive For standard products in small one stamp per visit when placing an order quantities, such as binder or dense and adhering to site health and safety surface courses, just turn up at our Collect & Go plant. procedures and, for every completed card, we’ll give you a £10 shopping voucher. For large orders, specialist products or out of hours collections, call us on To find out more, visit 0330 123 0763 hansoncollect.co.uk Hingston Down Asphalt Plant Site address Payment options Hanson Asphalt Hingston Down Quarry, Account Delaware Road, Gunnislake, Cornwall, PL18 9AU Credit or debit card on placement Tel: 01822 832 271 of order by calling 0330 123 0763 Local Sales Manager – Rachel Jefferson – 07970 724643 Site facilities Contact us Shop – essential tools of the trade To obtain a quote or place an order call: 0330Milton 123 Abbot 0763 (see list on next page) or additional Lezant Opening times items on request Refreshments – hot and cold Trekenner Monday to Friday 6am – 3pm Alternate weekends served drinks available Chaddlehanger Saturday (by prior arrangement) by Brayford plant or open Peter Tavy Treburley 6am – 11amRezare by local arrangement. Toilet facilities on site Trecombe Sydenham Damerel Tutwell Tavistock Stoke A483 Climsland Luckett Whitchurch Gulworthy Polhilsa Downgate A386 Gunnislake Grenofen Monkscross Maders Kelly Bray St Ann’s Chapel Harrowbarrow Horrabridge Callington Calstock Buckland Rumleigh Monachorum Frogwell Yelverton St Dominick Health and safety Products Our Collect & Go sites can be very busy – A full range of standard products (e.g. hot rolled health and safety is essential. asphalt and pre-coated chippings) are available, along with specialist products like our Tuff, Dura, Duralayer As a minimum, you must wear the following PPE: Multi, Sports and Hanson era® ranges as well as Hanson High-visibility long sleeve jacket Airfields. More information about our asphalt products Safety helmet can be found at hansoncollect.co.uk Gloves Ancillary products Bitukold – 15kg Leotak k140 – 25kg H4 compound – 25kg Leoclean 25ltr, 5ltr and 500ml standard spray Spreader Brush – turks head long and short shaft When on site, please also follow our Asphalt rake – wooden shaft safety guidelines: Asphalt sheet, green jute – 18ft x 12ft Report to the weighbridge before being loaded Use designated vehicle routes, parking areas and Overbonding tape – 25m roll pedestrian walkways Contractor’s wheel barrow Comply with safety instructions given by site staff Thermoplastic road marking white and yellow – 5m Use designated sheeting area/bay to sheet and Square mouth shovel un-sheet your vehicle PPE – safety helmets and glasses, jackets, Switch off your engine and remove the key when trousers and gloves leaving your vehicle unattended Do not use your mobile phone when driving or walking on site Wear ear protection if required in designated areas Do not allow gas cylinders to come into contact with hot substances Before manoeuvring, check the area around your vehicle for people or hazards Seat belts must be worn at all times when inside your vehicle Flashing beacons to be used at all times on site Hanson Asphalt Hingston Down Quarry Delaware Road Gunnislake Cornwall PL18 9AU Tel: 01822 832 271 To obtain a quote or place an order call: 0330 123 0763 Monday to Friday 6am – 3pm Saturday 6am – 11am hansoncollect.co.uk.
Recommended publications
  • The Distribution of Ammonium in Granites from South-West England
    Journal of the Geological Society, London, Vol. 145, 1988, pp. 37-41, 1 fig., 5 tables. Printed in Northern Ireland The distribution of ammonium in granites from South-West England A. HALL Department of Geology, Royal Holloway and Bedford New College, Egham, Surrey TW20 OEX, UK Abstract: The ammonium contents of granites, pegmatites and hydrothermally altered rocks from SW England have been measured. Ammonium levels in the granites are generally high compared with those from other regions, averaging 36ppm,and they differ markedlybetween intrusions. The pegmatites show higherammonium contents than any other igneous rocks which have yet been investigated. Ammonium contents are strongly enriched in the hydrothermally altered rocks, includ- ing greisens and kaolinized granites. There is agood correlation between the average ammonium content of the intrusions in SW England and their initial "Sr/*'Sr ratios and peraluminosity. This relationship supports the hypothesis that the ammonium in the granites is derived from a sedimentary source, either in the magmatic source region or via contamination of the magma. Introduction Results Ammonium is present as a trace constituent of granitic The granites rocks, in which it occurs in feldspars and micas substituting isomorphously for potassium (Honma & Itihara 1981). The The new analyses of Cornubian granites are given in Table amount of ammonium in granites varies from zero to over 1. They show a range of 3-179 parts per million NH:, with 100 parts per million, and it has been suggested that high the highest values being found in relatively small intrusions. concentrations may indicate the incorporation of organic- Taking the averagefor each of the major intrusions,and rich sedimentary material into the magma, either from the weighting them according to their relative areas (see Table presence of such material in rhe magmatic source region or 4), the average ammonium contentof the Cornubian granites via the assimilation of organic-rich country rocks (Urano as a whole is 36 ppm.
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  • A30 Chiverton to Carland Cross Environmental Statement
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  • Calstock Parish Neighbourhood Development Plan 2018-2030 Consultation Draft Autumn 2018
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  • Cornish Mineral Reference Manual
    Cornish Mineral Reference Manual Peter Golley and Richard Williams April 1995 First published 1995 by Endsleigh Publications in association with Cornish Hillside Publications © Endsleigh Publications 1995 ISBN 0 9519419 9 2 Endsleigh Publications Endsleigh House 50 Daniell Road Truro, Cornwall TR1 2DA England Printed in Great Britain by Short Run Press Ltd, Exeter. Introduction Cornwall's mining history stretches back 2,000 years; its mineralogy dates from comparatively recent times. In his Alphabetum Minerale (Truro, 1682) Becher wrote that he knew of no place on earth that surpassed Cornwall in the number and variety of its minerals. Hogg's 'Manual of Mineralogy' (Truro 1825) is subtitled 'in wich [sic] is shown how much Cornwall contributes to the illustration of the science', although the manual is not exclusively based on Cornish minerals. It was Garby (TRGSC, 1848) who was the first to offer a systematic list of Cornish species, with locations in his 'Catalogue of Minerals'. Garby was followed twenty-three years later by Collins' A Handbook to the Mineralogy of Cornwall and Devon' (1871; 1892 with addenda, the latter being reprinted by Bradford Barton of Truro in 1969). Collins followed this with a supplement in 1911. (JRIC Vol. xvii, pt.2.). Finally the torch was taken up by Robson in 1944 in the form of his 'Cornish Mineral Index' (TRGSC Vol. xvii), his amendments and additions were published in the same Transactions in 1952. All these sources are well known, but the next to appear is regrettably much less so. it would never the less be only just to mention Purser's 'Minerals and locations in S.W.
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  • Department of Mineralogy, University of Oxford. New Occurrences
    SHORT COMMUNICATIONS 501 Within the last few years I have discovered another locality in Corn- wall, Penberthy Croft Mine, St. Hilary, where in a cavity in some decomposed, 'gossany' quartz-galena veinstone I found two small but well-defined prismatic crystals of phosgenite, associated with anglesite, on decomposed galena. The crystals of phosgenite are pale wine-yellow in colour, and of long prismatic habit, the larger of the two being about 8 ram. long and 2 ram. thick: both show well-developed terminal faces of c(001) and several small faces in the pyramid and prism zones, but the latter are in general very striated, with many small vicinal faces, and owing to the positions of the crystals in the cavity it is difficult to make out what most of the faces are. A second occurrence has also been identified, in Cumberland, from the outcrop of the main Driggith-Sandbed vein near Caldbeek, in an old opencast between the two mines: here colourless phosgenite has been found with anglesite in somewhat decomposed, massive granular galena. Department of Mineralogy, ARTIIUR W. G. KINGSRURu University of Oxford. 1 Min. Mag., 1927, vol. 21, p. 221. New occurrences of rosasite in Britain. ROSASITE, (Cu,Zn)2COa(OH)2 , was first described from the Rosas Mine, Sulcis, Sardinia, and has since been recorded from several localities in the U.S.A., at Tsumeb in South-West Africa, and in northern Turkestan. It is probably the zinc-rich end member, with Cu:Zn near 3:2, of an isostructural series with malachite, the X-ray powder-patterns being similar but with different spacings and quite distinct.
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  • Download the Kit Hill Leaflet
    The decline in industrial activity combined with the lack Wildlife of agricultural improvement History Mining and quarrying means that Kit Hill has become Climbing to just over 1000 an oasis for wildlife. As the highest and most distinctive hill in the vicinity, Kit The granite form of Kit Hill originated as molten rock feet (334m) above sea level, Hill may have had religious significance in prehistoric times. which cooled and solidified deep within the earth’s crust. Kit Hill is the highest point of At least 18 burial mounds occur on its slopes, including Stress fractures formed during cooling created conduits Hingston Down ridge, within one beneath the summit chimney, and traces of early field through which mineral-rich fluids flowed. As these fluids the Tamar Valley Area of systems can be seen on aerial photographs. cooled, crystallisation took place forming lodes containing Outstanding Natural Beauty. Prehistoric people left their mark with a Neolithic long metallic ores of tin, copper and tungsten. Apart from small scale cultivation in the Bronze Age barrow (approx. 3000 BC) on the lower eastern slope and The quarrying of granite started through the simple and Medieval times, Kit Hill has only ever been lightly Bronze Age round barrows (2000 -1500 BC), forming part of a exploitation of surface moorstones weathered from the grazed. This, combined with periodic cutting and line of barrows along Hingston Down. surrounding bedrock. Over time this activity gave way to burning of vegetation, has enabled heathland to survive. well-developed industrial-scale bedrock quarries, the latter Characterised by a mix of heathers, gorses, grasses and eventually occupying two main sites on the northern hill bilberry (known locally as whortleberry) this is a precious slopes.
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  • Baseline Report Series: 16. the Granites of South-West England
    Baseline Report Series: 16. The Granites of South-West England Groundwater Systems and Water Quality Commissioned Report CR/04/255 Environment Agency Science Group Technical Report NC/99/74/16 The Natural Quality of Groundwater in England and Wales A joint programme of research by the British Geological Survey and the Environment Agency BRITISH GEOLOGICAL SURVEY Commissioned Report CR/04/255 ENVIRONMENT AGENCY Science Group: Air, Land & Water Technical Report NC/99/74/16 This report is the result of a study jointly funded by the British Geological Baseline Report Series: Survey’s National Groundwater Survey and the Environment Agency’s Science 16. The Granites of South-West Group. No part of this work may be reproduced or transmitted in any form or England by any means, or stored in a retrieval system of any nature, without the prior permission of the copyright proprietors. All rights are reserved by the copyright P L Smedley and D Allen proprietors. Disclaimer Contributors The officers, servants or agents of both the British Geological Survey and the Environment Agency accept no liability *M Thornley, R Hargreaves, C J Milne whatsoever for loss or damage arising from the interpretation or use of the information, or reliance on the views contained herein. Environment Agency Dissemination status *Environment Agency Internal: Release to Regions External: Public Domain ISBN: 978-1-84432-641-9 Product code: SCHO0207BLYN-E-P ©Environment Agency, 2004 Statement of use This document forms one of a series of reports describing the baseline chemistry of selected reference aquifers in England and Wales. Cover illustration Cliffs of jointed granite at Pordenack Point, near Land’s End (photography: C J Jeffery).
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