The Value of Original Natural Stone in the Context of Architectural Heritage
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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 -
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. -
Somerset Geology-A Good Rock Guide
SOMERSET GEOLOGY-A GOOD ROCK GUIDE Hugh Prudden The great unconformity figured by De la Beche WELCOME TO SOMERSET Welcome to green fields, wild flower meadows, farm cider, Cheddar cheese, picturesque villages, wild moorland, peat moors, a spectacular coastline, quiet country lanes…… To which we can add a wealth of geological features. The gorge and caves at Cheddar are well-known. Further east near Frome there are Silurian volcanics, Carboniferous Limestone outcrops, Variscan thrust tectonics, Permo-Triassic conglomerates, sediment-filled fissures, a classic unconformity, Jurassic clays and limestones, Cretaceous Greensand and Chalk topped with Tertiary remnants including sarsen stones-a veritable geological park! Elsewhere in Mendip are reminders of coal and lead mining both in the field and museums. Today the Mendips are a major source of aggregates. The Mesozoic formations curve in an arc through southwest and southeast Somerset creating vales and escarpments that define the landscape and clearly have influenced the patterns of soils, land use and settlement as at Porlock. The church building stones mark the outcrops. Wilder country can be found in the Quantocks, Brendon Hills and Exmoor which are underlain by rocks of Devonian age and within which lie sunken blocks (half-grabens) containing Permo-Triassic sediments. The coastline contains exposures of Devonian sediments and tectonics west of Minehead adjoining the classic exposures of Mesozoic sediments and structural features which extend eastward to the Parrett estuary. The predominance of wave energy from the west and the large tidal range of the Bristol Channel has resulted in rapid cliff erosion and longshore drift to the east where there is a full suite of accretionary landforms: sandy beaches, storm ridges, salt marsh, and sand dunes popular with summer visitors. -
Effectiveness of Nanolime As a Stone Consolidant
materials Article Effectiveness of Nanolime as a Stone Consolidant: A 4-Year Study of Six Common UK Limestones Stelios Tzavellos 1, Giovanni L. Pesce 2 , Yu Wu 1, Alison Henry 3, Simon Robson 2 and Richard J. Ball 1,* 1 BRE Centre for Innovative Construction Materials, Department of Architecture and Civil Engineering, University of Bath, Bath BA2 7AY, UK 2 Department of Architecture and Built Environment, Northumbria University, Newcastle upon Tyne NE1 8ST, UK 3 Building Conservation & Geospatial Survey, Technical Conservation Department, Historic England, The Engine House, Fire Fly Avenue, Swindon SN2 2EH, UK * Correspondence: [email protected]; Tel.: +44-01225-386944 Received: 23 July 2019; Accepted: 14 August 2019; Published: 22 August 2019 Abstract: Protecting stone buildings from weathering and decay is a major challenge in the conservation of built heritage. Most of the stone consolidants currently available are well suited to silicate stones, but are less compatible with limestone. In this paper we present for the first time the results over a 4-year period of various consolidation treatments carried out using nanolime on 6 of the most representative and significant stones used in historic buildings in the United Kingdom. Tests investigated the influence of stone type, environmental conditions and pre-treatments on the effectiveness of the consolidation treatment. A comprehensive and rigorous testing programme was carried out to evaluate the short (12 weeks) and longer-term (4 years) effects. Stone samples were characterised before and after treatment using light and electron microscopy, sorptivity tests and a novel methodology employing drilling resistance to interrogate the near surface effects. -
This Walk Has Been Commissioned by Artangel As Part of A
Urban Geology in London No. 29 This walk has been commissioned by Artangel as part of a programme of events surrounding artist Katrina Palmer’s project on the Isle of Portland and on BBC Radio 4, End Matter. This takes place in April-May 2015. The walk took place on 30th May 2015. London does not have a good local building stone. The Roman and Medieval city was built of Kentish Ragstone and Reigate Stone. Later, the abundant clays and brickearths of the local geology were exploited and stock brick became the city’s main building material. Bath Stone was brought in for some structures. However monumental buildings befitting of a capital required something special, and Portland Stone from Dorset became popular in the early 17th Century and remains London’s iconic stone to this day. There are thousands of buildings in London built of Portland Stone and many others in the maJor cities of the British Isles. One may consider St Paul’s Cathedral, the maJority of the buildings on Whitehall including the Cenotaph and the Banqueting House, The Royal Naval College at Greenwich, The Bank of England, The British Museum, The National Gallery and indeed my home institution, University College London. The stone has also been exported world-wide, mainly to commonwealth countries and the USA. Here we may count amongst several Portland Stone structures the United Nations Building (1952) in New York City. Auckland’s War Memorial Museum in New Zealand probably represents the use of this material most distant from the source. Portland Stone is also the standard for the Commonwealth war grave memorials. -
The Stone Industry at Bath Phillip Wooster
BIAS JOURNAL No 11 1978 The stone industry at Bath Phillip Wooster This article is extracted from a longer. study by the author than 10,000 pounds.’ This was a huge sum for the 1730 s but in which he describes the structure and geology of Great it reduced the cost of the stone from 10/- per ton to 7/6 Oolite, or Bath stone, and then traces the history of its delivered to the wharf. Even if the 1800 tons per annum use from Roman times 1-11 Early in the eighteenth century could have been delivered without the tramroad its Ralph Allen was responsible for a new scale of operation in introduction saved Mr Allen £4,500 per year and so paid for the industry when he directed his organising abilities to itself in just two years! Jones11 tells us that at the time of exploiting new methods of transport. Having been the building of the Parades '4 Carriages going the hill concerned in the scheme for providing a waterway route to constant and over the water, 4 ditto loading on the hill, Bristol with the Avon Navigation, opened in 1727, Allen 2 ditto loading block to Dolemeads, 1 ditto spare if any acquired quarries on Hampton Down and Combe Down misfortune should happen, which carriage cost £4O'. above Bath . Bath stone was shipped through Bristol docks for Bristol, Liverpool and London (where the Portland Stone Firms had to reduce the cost of their stone by one third to To make a success of his investment he needed to compete). -
Winchester Stone by Dr John Parker (PDF)
Winchester Stone by John Parker ©2016 Dr John Parker studied geology at Birmingham and Cambridge universities. He is a Fellow of the Geological Society of London. For over 30 years he worked as an exploration geologist for Shell around the world. He has lived in Winchester since 1987. On retirement he trained to be a Cathedral guide. The Building of Winchester Cathedral – model in the Musée de la Tapisserie, Bayeux 1 Contents Introduction page 3 Geological background 5 Summary of the stratigraphic succession 8 Building in Winchester Romano-British and Anglo-Saxon periods 11 Early medieval period (1066-1350) 12 Later medieval period (1350-1525) 18 16th to 18th century 23 19th to 21st century 24 Principal stone types 28 Chalk, clunch and flint 29 Oolite 30 Quarr 31 Caen 33 Purbeck 34 Beer 35 Upper Greensand 36 Portland 38 Other stones 40 Weldon 40 Chilmark 41 Doulting 41 French limestones 42 Coade Stone 42 Decorative stones, paving and monuments 43 Tournai Marble 43 Ledger stones and paving 44 Alabaster 45 Jerusalem stone 45 Choice of stone 46 Quarries 47 A personal postscript 48 Bibliography and References 50 ~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~ Photographs and diagrams are by the author, unless otherwise indicated 2 Introduction Winchester lies in an area virtually devoid of building stone. The city is on the southern edge of the South Downs, a pronounced upland area extending from Salisbury Plain in the west to Beachy Head in the east (Figs. 1 & 2). The bedrock of the Downs is the Upper Cretaceous Chalk (Fig. 3), a soft friable limestone unsuited for major building work, despite forming impressive cliffs along the Sussex coast to the east of Brighton. -
Anglo-Saxon Pits and a Medieval Kitchen at the Queen's College
Anglo-Saxon Pits and a Medieval Kitchen at The Queen’s College, Oxford Andrew Norton and James Mumford with contributions by Leigh Allen, Martin Allen, John Blair, Paul Booth, Dana Challinor, John Cotter, Alison Kelly, David Mullin, Rebecca Nicholson, Cynthia Poole, Ian Scott, Ruth Shaffrey, Wendy Smith, and Lena Strid SUMMARY In July 2008 Oxford Archaeology (OA) carried out an excavation at The Queen’s College (Queen’s) in advance of the construction of a new kitchen basement. The excavation uncovered tenth- and eleventh-century pits indicative of settlement within the north-eastern quarter of the defended town, or within a suburb immediately outside. The foundations of the college’s fifteenth-century west and north ranges were also revealed, and the medieval kitchen was seen to lie partly below its more recent counterpart. Combined with previous archaeological investigations and historical illustrations, the findings provide a near complete picture of the layout of the medieval college. They also supply much information about fellows’ diet. GEOLOGY AND TOPOGRAPHY ueen’s is on the northern side of the High Street, bounded by Queen’s Lane to the north and Qeast, approximately 500 m east of the centre of Oxford (Fig. 1). The site is on the second river gravel terrace at c.62 m OD, the underlying geology Oxford Clay. ARCHAEOLOGICAL AND HISTORICAL BACKGROUND Before the College The area later occupied by Queen’s lay either within or just outside the eastern part of the Anglo- Saxon burh, thought to have been constructed at the turn of the tenth century.1 An evaluation and watching brief carried out within the Provost’s Garden in the west of the college (Fig. -
Recommendations for Architecture & Design in Bath
Recommendations for Architecture & Design in Bath January 2011 Introduction This statement has been developed by the Trust’s expert Architecture and Planning Committee who comprise of building historians and built environment professionals who practice (or have practiced) architecture, urban design, conservation, town planning, and engineering, and has been adopted by the board of Trustees. Content has been reviewed by English Heritage, the Georgian Group and the Princes Regeneration Trust. The statement puts forward a set of five recommendations for architecture and design in Bath. Its aim is to provide a clear description of the Bath Preservation Trust’s views on how contemporary architecture should be shaped as the city progresses into the twenty- first century. The statement is made in support of the Trust's charitable objects, which include the mission: “To promote high standards of planning and architecture and to secure the preservation, protection, development and improvement for the public benefit of the character, amenities and buildings of historical, architectural or public interest in and around the City of Bath.” The Recommendations The Trust’s five recommendations are summarised below. They should be read in conjunction with the remainder of this paper which provides the rationale, and explains the recommendations in greater detail. Recommendation 1 new interventions must be informed by a thorough understanding of the significance and vulnerability of the built environment of the World Heritage Site Recommendation 2 historic -
P Gloss.1713
GLOSSARY Abbreviations Agora. The Greek equivalent of the Roman forum, a place of open-air assembly or market. (Isl) refers mainly to Islamic buildings. (Bud) refers Aisles. Lateral divisions parallel with the nave in a mainly to Buddhist buildings. (Hind) refers mainly to basilica or church. Hindu buildings. Terms relating specifically to Jap- Alabaster. A very white, fine-grained, translucent, anese architecture and construction are explained gypseous mineral, used to a small extent as a building within the relevant chapters. material in the ancient Middle East, Greece, Rome the Eastern Empire of Byzantium and, nearer to our Abacus. A slab forming the crowning member of a own day, by certain Victorian architects for its capital. In Greek Doric, square without chamfer or decorative qualities (and biblical associations). In moulding. In Greek Ionic, thinner with ovolo mould- Italy a technique was evolved many centuries ago ing only. In Roman Ionic and Corinthian, the sides are (and still survives) of treating alabaster to simulate hollowed on plan and have the angles cut off. In marble while there seems little doubt that in the past Romanesque, the abacus is deeper but projects less marble was often mistakenly described as alabaster. and is moulded with rounds and hollows, or merely Alae. Small side extensions, alcoves or recesses chamfered on the lower edge. In Gothic, the circular opening from the atrium (or peristyle) of a Roman or octagonal abacus was favoured in England, while house. the square or octagonal abacus is a French feature. Alpa vimana (Hind). Basic form of shrine in south Ablaq (Isl). -
The Building-Stones of Blenheim Palace, Cornbury Park, Glympton Park and Heythrop House, Oxfordshire
The Building-stones of Blenheim Palace, Cornbury Park, Glympton Park and Heythrop House, Oxfordshire By W. J. ARKELL company with Mr. David Green, I examined the exterior of Blenheim Palace in July, 1948, by permission of the Duke of Marlborougb. Mr. IGreen and Mr. Laurence Whistler had informed me that letters from Vanbrugh (mainly unpublished) referred to building stones for the palace from Taynton, Burford, Cornbury, Glympton, Heythrop, Headington, and Bourton-on-the Hill. The results of my examination were surprising, and it seems worth while to record them, together with notes on the other houses, Corn bury, Glympton, and Heythrop, to which the trail led. BLENHEIM PALACE The greater part of the palace visible from the ground (and there is no sign of any change of materials higher up) consists of a cream-coloured oolitic freestone which, especially on the N. front, has turned to a golden yellow on the surface. This stone is peculiar because it is full of fragments and whole specimens of large fossil sea-urchins or sand-dollars (Clypeus). The ooliths are irregular in size and rather coarse, and are harder than the matrix, which weathers marly. Other fossils noticed, besides Clypeus in nearly every block, are occasional Terebratula, Rhynchonella, Pseudolimea, erinea, and one coral (Thecosmilia ?) . This Clypeus stone is used externally, with the minor exceptions noted below, for the whole of the N. and S. fronts, including the great porticos, and for the kitchen court and orangery. In the columns of the kitchen court the stone (not up-ended) is 4 ft. on the bcd, and the squared ashlar stones of the plinth on the two main fronts are of great size.