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12 October 2011 Thirty-Fourth Mayor's Report to the Assembly
London Assembly MQT – 12 October 2011 Thirty-fourth Mayor’s Report to the Assembly This is my thirty-fourth report to the Assembly, fulfilling my duty under Section 45 of the Greater London Authority Act 1999. It covers the period 1 September to 28 September 2011. Executive Summary Bernard Hogan-Howe appointed as the new Commissioner of the Metropolitan Police. On 12 September, after interviewing the final four candidates with the Home Secretary, Bernard Hogan-Howe was appointed the new Commissioner of the Metropolitan Police. Londoners deserve strong and dynamic leadership at the helm of the country’s largest and most industrious police force, and I’m pleased to welcome the appointment of Bernard as the man who will deliver the firm, strategic lead our great city needs. Improving the Management of Disruptive Roadworks On 21 September, I announced a new onslaught on disruptive roadworks on London's streets by asking Londoners to "name and shame" those companies who blight London with disruptive or neglected roadworks, causing hours of unnecessary frustration to journeys every day. I urged Londoners to use a new reporting system to tell Transport for London (TfL) when roadworks are not up to scratch so they can take action with the relevant organisations and get things moving again. To help Londoners report disruptive or badly managed roadworks, TfL and I have updated the 'Reportit' system on the TfL website, to allow people to identify and report issues quicker. By visiting www.tfl.gov.uk/roadworks, or by tweeting @report_it with the hashtag #roadworks, complaints can be sent directly to the highway authority responsible, ensuring that direct and swift action can be taken. -
Download Directions
Directions Spectrum, 15 Stratton Street, Mayfair, London, W1J 8LQ. United Kingdom. By London Underground Spectrum’s office is a one minute walk from Green Park tube station, which can be accessed directly from the Piccadilly, Victoria and Jubilee lines. Take the right hand exit from the tube station onto Stratton Street (opposite Langan’s Brasserie) and turn right. As Stratton Street bears round to the right, Spectrum’s office at 15 Stratton Street is located in the left hand corner. There is a large green flag hanging outside the building with the signage “Green Park House”. From London mainline train stations Waterloo: Take the Jubilee line (north) to Green Park. Paddington: Take the Bakerloo line (south) to Oxford Circus. Take the Victoria line (south) to Green Park. Euston/Kings Cross/St. Pancras: Take the Victoria line (south) to Green Park. Victoria: Take the Victoria line (north) to Green Park. From London airports Heathrow Airport: take Heathrow Express train (20 minutes) to Paddington station. Take the Bakerloo line (south) to Oxford Circus. Take the Victoria line (south) to Green Park. City Airport: take Docklands Light Railway (DLR) to Canning Town (7 minutes). Take Jubilee line to Green Park (18 minutes). Gatwick Airport: take Gatwick Express train (30 minutes) to Victoria station. Take the Victoria line (north) one stop to Green Park (2 minutes). Parking There are parking meters located around Berkeley Square. The nearest NCP car park is located in Carrington Street. If arriving by private car, please be aware that the office is within the Congestion Charging Zone. For further information, please visit: www.cclondon.com . -
Old Market Character Appraisal Is Available Deadline of 21 February 2008
Conservation Area 16 Old Market Character Appraisal July 2008 www.bristol.gov.uk/conservation SA Hostel WINSFORD STREET FROME BRIDGE 1 PH 32 8 THRISS 26 to 30 E ET 24 2 LLST Old Market Convervation Area 1 2 20 R WADE STREET STRE 1 7 EET 3 Works N HA L AN Mm STREET 14 EST 8 Car Park LTTLE 6 7 RIVER STREET 2.0m 17 City Business Park 3 6 PH 15 to 11 Boundary of Conservation Area 20 PH 10 PH St Nicholas Church St Nicholas PH E STREET Church l Sub Sta Unive GP 1to32 Ho St Nicholas Lawford's G te TLE ANN usersal House 6 1 LIT Library 1to o15 DS GATE Lawford 11 t E Gate WADE STREE A WFOR T 1to18 D Wessex House 13 46 The Old Vica ge 59 4m ta 5 Car Park T 5 50 PH El T 16 City Business Park ub S 16 STREET S 18 19 PH RIVER INGTON ROAD 17 15 1 ELL NSTREET 1to22 W to 3 1 loucester 11 G House GREAT GEORGE STREE Somerset rence House GREAT AN 1to22 Ca TEMPLE WAY H Po ts o use TRINITY ROAD o44 (Community Centre) Friends Meeting TRINITY WALK House EY TCB 1t ERSL Telephone Exchange 1to17 41 ANE El Sub S Holy Trinity TCB to 48 Church Bristol City Mission Tyndall House 1to44 Po ice Station BRICK STREET Police Station 1to CLARENCE ROAD 1 17 22 20 9 Warehouse PH Jude St Coach and Horse 1to40 (PH) 8 E h Ves The 8 2 CLOS 1 sHo 85 1to2 HAYES 8 2 Warehouse 1 St Matthias try 23 25 81 ST MATTHIAS PARK 2 cel 6 1to 12 LANE E Subta 28 Th 90 41 S 40 (PH) 5 Cha 19 39 BRAGG'S 88 he Nave 75 86 3 21 T ER LANE TCB 84 7 T The LB 82 House 8 1 ES Old 1 The Tow r 0 78 Tannery30 UC St Matthias 51a 2 Guild 65 Heritage 16 Park GLO 1 7 12 29 5 7 0 t 3 o 31 62 5 6 495 2 4 10 18 33 -
Portland Stone: a Nomination for “Global Heritage Stone Resource” from the United Kingdom
221 by T. Hughes1 G.K. Lott2, M.J. Poultney3 and B.J. Cooper4 Portland Stone: A nomination for “Global Heritage Stone Resource” from the United Kingdom 1 Slate and Stone Consultants, Ceunant, Caenarfon, Gwynedd LL55 4SA, United Kingdom. E-mail: [email protected] 2 British Geological Survey, Keyworth, Nottingham, NG12 5GG, United Kingdom. E-mail: [email protected] 3 Albion Stone plc, Robert Denholm House, Bletchingley Road, Nutfield, Surrey RH1 4HW, United Kingdom. E-mail: [email protected] 4 Barbara Hardy Institute, School of Natural & Built Environments, University of South Australia, Adelaide, SA 5000, Australia. E-mail: [email protected] Portland Stone, a well known ooidal limestone of Criteria for GHSR recognition Jurassic age from the United Kingdom is here nominated The defining characteristics of a GHSR are succinctly addressed as a suitable “Global Heritage Stone Resource”. in the HSTG “Terms of Reference” that have been approved, following Portland Stone is considered to ideally fit the newly wide consultation, by IUGS at its Executive Committee Meeting in proposed designation as it has been utilised since Roman San Sebastian, Spain in February 2012. times in England and since the Middle Ages in the An approved GHSR nominee must have a cultural history construction of major historic buildings including St encompassing a significant period. The HSTG Terms of Reference advise that this period must be at least 50 years. Also crucial is that a Pauls Cathedral, British Museum and Bank of England GHSR needs to have been utilised in significant works, be they in in London. It was also the preferred building stone of Sir buildings, sculpture or utilitarian applications. -
GEOLOGY of the ROANOKE and STEWARTSVILLE QUADRANGLES, VIRGINIA by Mervin J
VIRGINIA DIVISION OF MINERAL RESOURCES PUBLICATION 34 GEOLOGY OF THE ROANOKE AND STEWARTSVI LLE OUADRANG LES, VI RG I N IA Mervin J. Bartholomew COMMONWEALTH OF VIRGINIA DEPARTMENT OF CONSERVATION AND ECONOMIC DEVELOPMENT DIVISION OF MINERAL RESOURCES Robert C. Milici, Commissioner of Mineral Resources and State Geologist CHARLOTTESVI LLE, VIRGI NIA 1 981 VIRGINIA DIVISION OF MINERAL RESOURCES PUBLICATION 34 GEOLOGY OF THE ROANOKE AND STEWARTSVI LLE OUADRANG LES, VI RG I N IA Mervin J. Bartholomew COMMONWEALTH OF VIRGINIA DEPARTMENT OF CONSERVATION AND ECONOMIC DEVELOPMENT DIVISION OF MINERAL RESOURCES Robert C. Milici, Commissioner of Mineral Resources and State Geologist CHARLOTTESVILLE, VIRGINIA 1 981 FRONT COVER: Fold showing slightly fanned, axial plane, slaty cleav- age in a loose block of Liberty Hall mudstone at Reference Locality 20, Deer Creek, Roanoke quadrangle. REFERENCE: Portions of this publication may be quoted if credit is given to the Virginia Division of Mineral Resources. It is recommended that referenee to this report be made in the following form: Bartholomew, M. J., 1981, Geology of the Roanoke and Stewaitsville quadrangles, Vir- ginia, Vlrginia Division of Mineral Resources Publicatio4 34,23 p. VIRGINIA DIVISION OF MINERAL RESOURCES PUBLICATION 34 GEOLOGY OF THE ROANOKE AND STEWARTSVI LLE OUADRANG LES, VIRG I N IA Mervin J. Bartholomew COM MONWEALTH OF VIRGINIA DEPARTMENT OF CONSERVATION AND ECONOMIC DEVELOPMENT DIVISION OF MINERAL RESOURCES Robert C. Milici, Commissioner of Mineral Resources and State Geologist CHARLOTTESVILLE, VIRG INIA 1 981 DEPARTMENT OF CONSERVATION AND ECONOMIC DEVELOPMENT Richmond, Virginia FRED W. WALKER, Director JERALD F. MOORE, Deputy Director BOARD ARTHUR P. FLIPPO, Doswell, Chairman HENRY T. -
Chesterton & Sons
t.h. Chesterton & sons Chartered Surveyors ' Auctioneers & Valuers ESTATE AGENTS -: .:: , .i :a¡ ' þ. iì 116 Kensington High Street ;l London Wg 7RW Tel.01-937 1234 rå-l 2 Cale Street Chelsea Green ¡', London SW3 3OU ;1 Tel.01-589 5211 þ ,i I 40 Connaught Street Hyde Park London WZ 2AB YOTJN(i S'I'RDtìT, LOOt(INC; NOR'I'H, JUNIi 189() Tel. O1 -262 7202 26 Clifton Road Maida Vale London W9 1SX Tel. 01 -289 1001 ..:i--. Hornton House Drayson Mews London WB 4LY Tel.01-937 8020 Building Surveying Division 9 Wood Street Cheapside London EC2V 7AR Tel.01-606 3055 Commercial and lndustrial Departments THE KENSINGTON SOCIETY Annual R.port 197 0-7 L The Kensington Society t'.-\'11ìo\ II.R.II. PIìI\CIìSS AI,IC.]D, COLI\TIìSS OI. A:IIII,ONIì I'RIlSli)tlN',l' 'l'IIlì lìI(;II't' I lO\. I,ORD IIURCOll13, t;.c.tr., r<.n.n. VI('Ii-I'IìLSIDEN'TS 'I'IIìi I)O\\I..\(II.]Iì fI.\IìCIIION].]SS OF CIIOLN'IONDIìLEY ,I'IIIi R]" RIì\¡, 'fIIIì I,OIìD BISIIOP OF IitìNSING'ION 't'lIIr) l,AI)Y Sl'OCKS T. COI )NCII, F. r'.r'.s.,r. Nfiss Jean '\lex¡ntler \Ir. \\¡illi¿m Glimes, Jlr'. I lrrr.lr' ,\rrtics Sir John Pope-Ht'nness)', c.B.E., F.Iì..4,., tr.S.r\, 'l'he Ifun. \lr. .Justice lJ¡rrv Tl-rc IIon. NIr. Justice liarminski \lr. \\/. \\:. ììclle¡", F.Iì.III51.s., I-.It.I.tl.¡. trIr. Oliver \'Iessel, c.l.n. Sil Ilugh C'asson, R.I).I., Ir.tr.I.tt.r\, L:rcl¡' Norn"ran, ¡.e. -
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. Oolites in the Green River Formation of Central Utah, and the Problem of Oolite Growth Stuart L. Schoff, DePauw University Oolitic limestone occurs in the Green River formation, of Eocene age, at Manti, in central Utah. A microscopic study of thin sections of the rock suggests conditions under which the oolite originated. As described by Bradley (1), and others, the Green River formation was deposited in a great fresh-water lake, or several lakes—an environ- ment contrasting strongly with the highly saline environment of Great Salt Lake, where oolitic grains are now forming, and less strongly with the marine conditions under which many oolites of the geologic column probably originated. Description.—The oolites are composed of calcium carbonate, chiefly as calcite, with an admixture of silt. Some of the material has been recrystallized, and some is now silicified. The average diameter of the grains is between 0.4 and 0.5 mm. They are circular in cross-section, elongate or oval, triangular, and irregular. In general, the outline con- forms with the shape of the nucleus, if one is present, but there are grains in which the outer zones are eccentric (Fig. 1, A) Uncommonly the oolitic grains contain mineral fragments as nuclei, but, even under high magnification, the centers of most of the grains appear simply as structureless spherical bodies of the same material as the rest of the grain. Hence the nuclei suggest little as regards causes for precipitation of calcium carbonate. Figure 1, B and Figure 2 illustrate grains with two centers of growth. One grain with three centers was noted. -
Chapter 11 Kensington High Street
Chapter 11 Kensington High Street building, Kensington Town Hall adjacent to the High Chapter 11 Kensington Street,as well as Sony and Warners and other High Street smaller offices. 11.1 Introduction 11.1.7 The centre has benefited from comprehensive public realm improvements, that 11.1.1 Kensington High Street has been one of have gained international acclaim. This has put in London’s top retail streets for the last 100 years. place high-quality, York-stone paving, created a The centre lost some of its original raison d’être as central reservation bike park and removed street the biggest concentration of department stores clutter, particularly guard railing. These outside Oxford Street with the closure of Pontings improvements have made crossing the street much and Derry and Tom’s in the early 1970s, and more easier, the pedestrian environment more recently Barker’s. In the seventies Derry and Tom’s comfortable and encouraged higher footfall on the became the home of the legendary Biba emporium northern side of the street (previously footfall was (once described as ‘the most beautiful store in the heavily concentrated on the southern side). world’), making Kensington High Street a fashion 11.1.8 Despite the public realm improvements, destination. With the closure of Biba in the mid people still perceive traffic congestion and the seventies, this role was continued by Hyper Hyper irregularity of the District and Circle Lines to be in the eighties and Kensington Market, which issues. High Street Kensington Station is a major survived until comparatively recently, and remains public transport interchange and the High Street is reflected today in the cluster of young fashion also served by a large number of buses. -
19. Diagenesis of a Seamount Oolite from the West Pacific, Leg 20, Dsdp
19. DIAGENESIS OF A SEAMOUNT OOLITE FROM THE WEST PACIFIC, LEG 20, DSDP Reinhard Hesse, McGill University, Montreal, Canada SAMPLES AND LOCATION of the Caroline Abyssal Plain area. The present estimate of the average subsidence rate for the last 54 million years is Leg 20 recovered the first oolite drilled during the Deep 32 BuB (32m/106y) based on the above data. This is Sea Drilling Project. The oolitic limestone was brought up somewhat less than the figure taken from Sclater et al.'s from 83 and 106 meters subbottom depth in Cores 3 and 4 (1971) general subsidence-rate curve for the north Pacific of Hole 202 on Ita Matai Seamount. Drilling of the (about 40 m/106y for crust as old as early Eocene). seamount was undertaken at the end of Leg 20, when the poor state of repair of the drilling gear prohibited further COLOR, TEXTURE, AND POROSITY drilling in deep water. Water depth at this site is 1515 The oolite is of white yellowish to pale tan color except meters. Thus Cores 3 (45 cm recovery) and 4 (35 cm for the uppermost 10 cm of Core 3, which displays shades recovery) come from a total depth of 1598 and 1621 of gray. meters, respectively. Ita Matai Seamount is located at the Individual ooids displaying a distinct nucleus range in eastern margin of the Caroline Abyssal Plain (Figure 1). The size from 0.12 to 1.45 mm in diameter. Skeletal fragments location of Site 202 is 12°40.90'N, 156°57.15'E. associated with the ooids range up to 3 mm. -
Using the Solid Density to Assess Data Quality
Materials and Structures DOI 10.1617/s11527-015-0767-3 ORIGINAL ARTICLE Porosities of building limestones: using the solid density to assess data quality Christopher Hall . Andrea Hamilton Received: 15 June 2015 / Accepted: 16 December 2015 Ó The Author(s) 2016. This article is published with open access at Springerlink.com Abstract A good knowledge of the volume-fraction the solid density should always be calculated for this porosity is essential in any technical work on porous purpose when the Archimedes method is used. This materials. In construction materials the porosity is check can be useful also when porosities are measured commonly measured by the Archimedes buoyancy by helium pycnometry or by mercury intrusion method, from which the bulk density of the test porosimetry. specimen is also obtained. The porosity and the bulk density together fix the solid density of the specimen, Keywords Porosity Á Density Á Archimedes method Á as only two of the three quantities are independent. Limestone Á Calcite The solid density, although rarely discussed, is determined by the mineralogy of the specimen, and therefore can provide a valuable check on the accuracy 1 Introduction of porosity and bulk density measurements. Our analysis of published data on calcitic limestones Most inorganic construction materials, including the shows that the solid density is generally close to the main building stones, are porous. In research on ideal crystallographic density of calcite. Small devi- mechanics, transport, and durability in these materials, ations can often be traced to variations in mineral the porosity is often used as an explanatory (indepen- composition. However some published porosity–den- dent) variable, and so it is measured and reported as a sity data are inconsistent with the known mineralogy. -
Bath City-Wide Character Appraisal
Bath and North East Somerset Planning Services Bath City-wide Character Appraisal Supplementary Planning Document Adopted 31 August 2005 Bath City-wide Character Appraisal Contents 1 Introduction 4 2 Designations that Demonstrate the Significance of Bath 4 3 Aims, Objectives and Methodology 5 4 Using the Bath City-wide Character Appraisal 5 5 Cultural and Historical Development of Bath 6 6 The Character of Bath 12 6.1 Landscape, Setting and Views 12 6.2 Influence of River Avon 13 6.3 High Quality Architecture and Urban Design 14 6.4 Height and Scale 16 6.5 Materials 18 6.6 Perceptual and Cultural Influences on the Character of Bath 19 7 Character Areas Location Map of the Bath City-wide Character Areas 21 Area 1: Weston 22 Area 2: Weston Park, Sion Hill and Upper Lansdown 26 Area 3: Fairfield Park and Larkhall 30 Area 4: Newbridge (north) Combe Park and Lower Weston (north) 34 Area 5: Lower Lansdown and Camden 38 Area 6: Grosvenor and Lambridge 42 Area 7: Brassmill Lane, Locksbrook and Western Riverside 46 Area 8: City Centre 50 Area 9: Bathwick 54 Area 10: Widcombe and the Kennet and Avon Canal 58 Area 11: Bathampton 62 Area 12: Twerton, Whiteway, Southdown and Moorlands 66 Area 13: Bear Flat and Oldfield Park 72 Area 14: Pulteney Road 76 Area 15: North Road and Cleveland Walk 80 Area 16: Bathampton Slopes 80 Area 17: Beechen Cliff and Alexandra Park 86 Bath City-wide Character Appraisal Area 18: Entry Hill, Perrymead and Prior Park 90 Area 19: Bathampton Down and Claverton Down 94 Area 20: Odd Down 98 Area 21: Foxhill 102 Area 22: Combe Down 106 8 Rural Fringes Rural Fringe: North of Bath 110 Rural Fringe: West of Bath 114 Rural Fringe: East and South East of Bath 118 Rural Fringe: South of Bath 122 Appendix 1: Earlier Studies Used to Inform the Bath City-wide Character Appraisal 126 Appendix 2: Survey Sheet 127 Notes 130 Bibliography 131 Bath City-wide Character Appraisal 1 Introduction 1.1 Bath has evolved over time in response to political, social and economic conditions and continues to evolve to this day. -
Hartham PSS V3 MW
HANSON UK HARTHAM BATH STONE MINE, CORSHAM NEW MINE ENTRANCE AND ANCILLARY SURFACE FACILITIES Construction of an inclined mine entrance from the surface into existing permitted mine workings, construction of ancillary surface facilities including access to highway, offices, workshop, covered storage, open storage, landscaping and restoration PLANNING SUPPORTING STATEMENT JANUARY 2015 Wardell Armstrong Sir Henry Doulton House, Forge Lane, Etruria, Stoke-on-Trent, ST1 5BD, United Kingdom Telephone: +44 (0)845 111 7777 Facsimile: +44 (0)845 111 8888 www.wardell-armstrong.com DATE ISSUED: January 2015 JOB NUMBER: ST13466 ELECTRONIC REFRENCE: REPORT NUMBER: RPT-010 HANSON UK HARTHAM BATH STONE MINE, NEW MINE ENTRANCE PLANNING SUPPORTING STATEMENT December 2014 PREPARED BY: David Bridgwood Technical Director APPROVED BY: Mike Walker Technical Director This report has been prepared by Wardell Armstrong LLP with all reasonable skill, care and diligence, within the terms of the Contract with the Client. The report is confidential to the Client and Wardell Armstrong LLP accepts no responsibility of whatever nature to third parties to whom this report may be made known. No part of this document may be reproduced without the prior written approval of Wardell Armstrong LLP. ENERGY AND CLIMATE CHANGE ENVIRONMENT AND SUSTAINABILITY INFRASTRUCTURE AND UTILITIES Wardell Armstrong is the trading name of Wardell Armstrong LLP, Registered in England No. OC307138. LAND AND PROPERTY MINING AND MINERAL PROCESSING Registered office: Sir Henry Doulton House, Forge Lane, Etruria, Stoke-on-Trent, ST1 5BD, United Kingdom MINERAL ESTATES AND QUARRYING UK Offices: Stoke-on-Trent, Birmingham, Cardiff, Carlisle, Edinburgh, Greater Manchester, London, Newcastle upon Tyne, Penryn, Sheffield, Truro, West Bromwich.