Purbeck Marble Conservation and Repair Summary
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The Stones of Osterley Park House Ruth Siddall
Urban Geology in London No. 37 The Stones of Osterley Park House Ruth Siddall Osterley Park House was designed and built by Robert Adam (1728-1792) in the late 18th Century, between 1761 and the 1780s. It was commissioned by the Child Family and superseded a Tudor Mansion on the same site. Adam had ‘total design’ control of the construction and interior decoration of the house. This assumes that Adam also had a hand in overseeing if not selecting the building materials used. This brief report summarises the building and decorative stones used in the building, as observed following a visit to Osterley Park House in June 2017. Portico and Courtyard Portland Whitbed is used for the pediment, balustrade, quoins and other stone dressings on the exterior of Osterley Park House. It is also used for paving and for the columns supporting the pediment. This stone is identified by the pale grey colour with darker fossilised shells of oysters, which now weather slightly proud of the surface. Sedimentary bedding alignment can be detected in both columns and in some flagstones due to the concentration of shell beds. Portland Whitbed is the most commonly used of three main building stones extracted from the Portland Limestone Formation which occurs in outcrop and subcrop on the Isle of Portland, a peninsula on the Dorset Coast. Whitbed contains variable fossil content, predominantly in the form of oyster shells with well-preserved, laminated shells and also fragments of the reef-forming algae Solenpora portlandica. Two other units are also extracted as building stone; the Basebed and the Roach. -
Unclassified Fourteenth- Century Purbeck Marble Incised Slabs
Reports of the Research Committee of the Society of Antiquaries of London, No. 60 EARLY INCISED SLABS AND BRASSES FROM THE LONDON MARBLERS This book is published with the generous assistance of The Francis Coales Charitable Trust. EARLY INCISED SLABS AND BRASSES FROM THE LONDON MARBLERS Sally Badham and Malcolm Norris The Society of Antiquaries of London First published 1999 Dedication by In memory of Frank Allen Greenhill MA, FSA, The Society of Antiquaries of London FSA (Scot) (1896 to 1983) Burlington House Piccadilly In carrying out our study of the incised slabs and London WlV OHS related brasses from the thirteenth- and fourteenth- century London marblers' workshops, we have © The Society of Antiquaries of London 1999 drawn very heavily on Greenhill's records. His rubbings of incised slabs, mostly made in the 1920s All Rights Reserved. Except as permitted under current legislation, and 1930s, often show them better preserved than no part of this work may be photocopied, stored in a retrieval they are now and his unpublished notes provide system, published, performed in public, adapted, broadcast, much invaluable background information. Without transmitted, recorded or reproduced in any form or by any means, access to his material, our study would have been less without the prior permission of the copyright owner. complete. For this reason, we wish to dedicate this volume to Greenhill's memory. ISBN 0 854312722 ISSN 0953-7163 British Library Cataloguing in Publication Data A CIP catalogue record for this book is available from the -
Back Matter (PDF)
PROCEEDINGS OF THE YORKSHIRE GEOLOGICAL SOCIETY 309 INDEX TO VOLUME 55 General index unusual crinoid-coral association 301^ Lake District Boreholes Craven inliers, Yorkshire 241-61 Caradoc volcanoes 73-105 Chronostratigraphy Cretoxyrhinidae 111, 117 stratigraphical revision, Windermere Lithostratigraphy crinoid stems, N Devon 161-73 Supergroup 263-85 Localities crinoid-coral association 301-4 Lake District Batholith 16,73,99 Minerals crinoids, Derbiocrinus diversus Wright 205-7 Lake District Boundary Fault 16,100 New Taxa Cristatisporitis matthewsii 140-42 Lancashire Crummock Fault 15 faunal bands in Lower Coal Measures 26, Curvirimula spp. 28-9 GENERAL 27 Dale Barn Syncline 250 unusual crinoid-coral association 3Q1-A Acanthotriletes sp. 140 Dent Fault 257,263,268,279 Legburthwaite graben 91-2 acritarchs 243,305-6 Derbiocrinus diversus Wright 205-7 Leiosphaeridia spp. 157 algae Derbyshire, limestones 62 limestones late Triassic, near York 305-6 Diplichnites 102 foraminifera, algae and corals 287-300 in limestones 43-65,287-300 Diplopodichnus 102 micropalaeontology 43-65 origins of non-haptotypic palynomorphs Dumfries Basin 1,4,15,17 unusual crinoid-coral association 301-4 145,149,155-7 Dumfries Fault 16,17 Lingula 22,24 Alston Block 43-65 Dunbar-Oldhamstock Basin 131,133,139, magmatism, Lake District 73-105 Amphoracrinus gilbertsoni (Phillips 1836) 145,149 Manchester Museum, supplement to 301^1 dykes, Lake District 99 catalogue of fossils in Geology Dept. Anacoracidae 111-12 East Irish Sea Basin 1,4-7,8,10,12,13,14,15, 173-82 apatite -
Early Cretaceous) Wessex Formation of the Isle of Wight, Southern England
A new albanerpetontid amphibian from the Barremian (Early Cretaceous) Wessex Formation of the Isle of Wight, southern England STEVEN C. SWEETMAN and JAMES D. GARDNER Sweetman, S.C. and Gardner, J.D. 2013. A new albanerpetontid amphibian from the Barremian (Early Cretaceous) Wes− sex Formation of the Isle of Wight, southern England. Acta Palaeontologica Polonica 58 (2): 295–324. A new albanerpetontid, Wesserpeton evansae gen. et sp. nov., from the Early Cretaceous (Barremian) Wessex Formation of the Isle of Wight, southern England, is described. Wesserpeton is established on the basis of a unique combination of primitive and derived characters relating to the frontals and jaws which render it distinct from currently recognized albanerpetontid genera: Albanerpeton (Late Cretaceous to Pliocene of Europe, Early Cretaceous to Paleocene of North America and Late Cretaceous of Asia); Celtedens (Late Jurassic to Early Cretaceous of Europe); and Anoualerpeton (Middle Jurassic of Europe and Early Cretaceous of North Africa). Although Wesserpeton exhibits considerable intraspecific variation in characters pertaining to the jaws and, to a lesser extent, frontals, the new taxon differs from Celtedens in the shape of the internasal process and gross morphology of the frontals in dorsal or ventral view. It differs from Anoualerpeton in the lack of pronounced heterodonty of dentary and maxillary teeth; and in the more medial loca− tion and direction of opening of the suprapalatal pit. The new taxon cannot be referred to Albanerpeton on the basis of the morphology of the frontals. Wesserpeton currently represents the youngest record of Albanerpetontidae in Britain. Key words: Lissamphibia, Albanerpetontidae, microvertebrates, Cretaceous, Britain. Steven C. -
The English Claim to Gothic: Contemporary Approaches to an Age-Old Debate (Under the Direction of DR STEFAAN VAN LIEFFERINGE)
ABSTRACT MARY ELIZABETH BLUME The English Claim to Gothic: Contemporary Approaches to an Age-Old Debate (Under the Direction of DR STEFAAN VAN LIEFFERINGE) The Gothic Revival of the nineteenth century in Europe aroused a debate concerning the origin of a style already six centuries old. Besides the underlying quandary of how to define or identify “Gothic” structures, the Victorian revivalists fought vehemently over the national birthright of the style. Although Gothic has been traditionally acknowledged as having French origins, English revivalists insisted on the autonomy of English Gothic as a distinct and independent style of architecture in origin and development. Surprisingly, nearly two centuries later, the debate over Gothic’s nationality persists, though the nationalistic tug-of-war has given way to the more scholarly contest to uncover the style’s authentic origins. Traditionally, scholarship took structural or formal approaches, which struggled to classify structures into rigidly defined periods of formal development. As the Gothic style did not develop in such a cleanly linear fashion, this practice of retrospective labeling took a second place to cultural approaches that consider the Gothic style as a material manifestation of an overarching conscious Gothic cultural movement. Nevertheless, scholars still frequently look to the Isle-de-France when discussing Gothic’s formal and cultural beginnings. Gothic historians have entered a period of reflection upon the field’s historiography, questioning methodological paradigms. This -
Purbeck Quarries. OUGS Wessex. March14 2015 Safety
Purbeck Quarries. OUGS Wessex. March14 2015 Safety. Hard hats are required if you go underground in the quarries and perhaps in the Square & Compass pub – low ceilings and beams! At Winspit the quarry edge is unprotected and there is an immediate vertical drop of about 40 feet to the sea. Similarly if you use the Coast Path to overlook the quarry there is a drop to the quarry floor. Keep away from edges. The quarry faces are stable. Morning Landers Quarry. Trev Haysom, Owner Trev will show us around a modern working Purbeck quarry. There will be opportunity to see how the stone is quarried and worked. Landers Quarry is notable as a source of Purbeck Marble. ------------------------------------------------------------------------------------------ Afternoon WORTH MATRAVERS AND WINSPIT. Bob Alderman. OUGS Wessex Worth Matravers, along with Langton Matravers is at the centre of the Purbeck stone industry. At Worth the only active quarry is St Aldhelms Quarry (SY 965 762), behind the Aldhelm’s Head. There are several working quarries between Worth and Langton Matravers. About Worth Matravers. The village of Worth Matravers is notable as an essay in Purbeck stone buildings. The nature of the stone means that if readily forms blocks and in some beds it splits to form thin roofing tiles. Only rarely does it provide beds that allow significant carving. You will note there are few mullion windows. There is a 16th century house in Corfe Castle with Purbeck stone mullions but it is a rare example. Most of the stone, exported from Swanage, was in the form of paving slabs. The rise of the Purbeck Stone industry probably dates from the 12th century when the then Bishop of Winchester used it for his Palace. -
The Geology Durdle Door, Dorset Chalk Stratigraphy, Sedimentology and Tectonic Structure New Marker Beds
Wessex OUGS Field Guide to Durdle Door, Dorset, May 2018 The Geology Durdle Door, Dorset Chalk stratigraphy, sedimentology and tectonic structure New marker beds Durdle Cove, Dorset looking west over Scratchy Bottom and Swyre Head to Bat’s Head. The line of caves at the foot of the cliff in Durdle Cove is formed on the Durdle Cove Thrust (see also Rowe 1901, Plate III, pp. 16-17). Open University Geological Society Wessex Group Field Excursion Sunday 13th May 2018 Leaders: Rory Mortimore and Jeremy Cranmer Field guide prepared by Rory Mortimore www.chalkrock.com Based on the paper Late Cretaceous stratigraphy, sediments and structure: gems of the Jurassic Coast of Devon and Dorset, England just going into press in the Proceedings of the Geologists’ Association, 2018. 1 Wessex OUGS Field Guide to Durdle Door, Dorset, May 2018 Wessex OUGS Field Trip Durdle Door, Durdle Cove, Scratchy Bottom and Bat’s Head Late Cretaceous stratigraphy, sediments and structure: gems of the Jurassic Coast of Devon and Dorset, England Introduction Extraordinary, long-distance litho-marker beds such as the Lewes and Shoreham Tubular Flints and associated marl seams and fossils (Fig.2), recognised in cliff exposures and cliff-fall boulders, are keys to unlocking the stratigraphy and tectonic structures in the Late Cretaceous (Fig.1) of the Jurassic Heritage Coast. Durdle Cove is a special gem exposing the Lewes and Seaford Chalk stratigraphy where these and new marker beds are identified and where sediments and tectonic structures provide clues to timing of movements that produced a Late Cretaceous pericline which grew into a Miocene monocline along the line of the underlying Purbeck Reverse Fault. -
DSWA Dorset News
DSWA Dorset News May 2020 I hope you enjoy this issue of the Newsletter in which I am sharing the results of my exploration into the history of the Isle of Purbeck, its quarries, mines and mellow stone, and characteristic walls. I’ve been helped in this project by Sally Fielding, Dave Rawson, Jon Leyland, the National Trust walling ranger on South Purbeck; Keith Coombs who took some of the photographs; and Trev Haysom, a tenth-generation stone mason with unrivalled knowledge of Purbeck quarrying and its history. Haysom Purbeck Stone has been working in Purbeck since the late 17th century. Purbeck stone and marble Purbeck stone is confined largely to an area of 10 square km to the south and west of Swanage. Twenty operational quarries produce up to 25,000 tonnes annually, just half of that shipped out of Swanage in the boom years of the 18th century and leading up to the Industrial Revolution when there was high demand for building stone in burgeoning towns and cities. The hardest and polishable limestone, known as Purbeck marble, consists of the fossilised shells of freshwater snails (Viviparus) and was first quarried from open pits by Iron Age and Roman artisans. Blue and purple Purbeck marble, quarried along a seam from Peveril Point to Worbarrow Bay, were used in tiles and mosaics at Fishbourne Palace (c.75 CE), near Chichester. Apart from its use in utility objects such as grindstones, and the decorative arts, stone was rare as a building material until the Norman invasion when there was high demand for building castles and churches. -
From the Portland and Purbeck Groups (Tithonian–Berriasian) of Dorset, United Kingdom
New thoracican cirripedes (Crustacea) from the Portland and Purbeck Groups (Tithonian–Berriasian) of Dorset, United Kingdom Andy Galea aSchool of Earth and Environmental Sciences, University of Portsmouth, Burnaby Building, Burnaby Road, Portsmouth PO1 3QL, United Kingdom E-mail: [email protected] Abstract. The first cirripedes from the Portland and Purbeck groups of southern England are described, and referred to two new species, Loriolepas whytei sp. nov and Etcheslepas portlandensis sp. nov. They constitute the first records of cirripedes from the upper Tithonian (uppermost Jurassic) and Berriasian (lowermost Cretaceous) of western Europe. A new family, the Archaeolepadidae, is introduced for the extinct genera Archaeolepas and Loriolepas. Key words. Jurassic, Cretaceous, stalked barnacles, southern England Introduction In 1928, Thomas Withers described the meagre cirripede material from the British Upper Jurassic, consisting of a small number of mostly broken valves washed from the Kimmeridge Clay of Buckinghamshire. In the Lower Cretaceous, the marine pre-Aptian strata had yielded only a single species from the Speeton Clay (Hauterivian) of Speeton, Yorkshire. Recent discoveries by Steve Etches (Etches Collection, Kimmeridge) of magnificently preserved, and locally abundant, cirripedes from the Kimmeridge Clay in Dorset have considerably improved our understanding of the taxonomy, phylogeny and palaeoecology of Late Jurassic forms (Gale 2014, 2018), but they remained unknown from the overlying Portland Group. In 2015, during a field excursion for students of the University of Portsmouth to Freshwater, on the Isle of Portland (Fig. 1) I collected a number of cirripede valves from the Cherty Member of the Portland Stone Formation, and further specimens on a subsequent visit. -
Geology in St Paul's Churchyard and Paternoster Square Ruth Siddall
Urban Geology in London No. 12 Geology in St Paul’s Churchyard and Paternoster Square Ruth Siddall Looking From Newgate Street across Paternoster Square to the Temple Bar and St Paul’s Cathedral. This walk starts at St Paul’s Underground station, and takes in a circuit around the Cathedral via Paternoster Square and St Paul’s Churchyard and back to the tube station via the west end of Cheapside. This area has seen a large amount of redevelopment since Eric Robinson wrote his guides to street geology in this part of the city of London (Robinson, 1984 & 1997; Robinson & Bishop, 1980), including the relocation of two of the City’s monuments into the vicinity. Culturally and archaeologically this is one of the oldest, continuously occupied parts of the City of London, particularly as a religious centre. It was part of the Roman city of Londinium, with the Lud Gate in place in the earliest 3rd Century AD. This Roman gate house survived until 1760 when it was demolished. The first St Paul’s Cathedral was constructed in 604 AD by the Bishop of London, Mellitus. This was replaced (with probable intervening buildings) in 1087 with a new Romanesque cathedral built by Bishop Maurice. In the 13th Century a crypt (still in tact under the current cathedral) and a choir were added, and a cloister and chapter house were added in the 14th Century. In the mid 17th Century, the architect Inigo Jones was surveyor of the fabric and added classical details to the Cathedral. He was succeeded by Sir Christopher Wren who proposed major refurbishments due to have taken place in 1666. -
The Student's Elements of Geology
The Student's Elements of Geology Sir Charles Lyell The Student's Elements of Geology Table of Contents The Student's Elements of Geology.........................................................................................................................1 Sir Charles Lyell............................................................................................................................................1 PREFACE......................................................................................................................................................2 CHAPTER I. ON THE DIFFERENT CLASSES OF ROCKS.....................................................................2 CHAPTER II. AQUEOUS ROCKS. THEIR COMPOSITION AND FORMS OF STRATIFICATION......................................................................................................................................8 CHAPTER III. ARRANGEMENT OF FOSSILS IN STRATA. FRESH−WATER AND MARINE FOSSILS.....................................................................................................................................................14 CHAPTER IV. CONSOLIDATION OF STRATA AND PETRIFACTION OF FOSSILS.......................21 CHAPTER V. ELEVATION OF STRATA ABOVE THE SEA. HORIZONTAL AND INCLINED STRATIFICATION....................................................................................................................................27 CHAPTER VI. DENUDATION..................................................................................................................40 -
Boreal Influence on English Ryazanian Bivalves 285-292 © Biodiversity Heritage Library, 285
ZOBODAT - www.zobodat.at Zoologisch-Botanische Datenbank/Zoological-Botanical Database Digitale Literatur/Digital Literature Zeitschrift/Journal: Zitteliana - Abhandlungen der Bayerischen Staatssammlung für Paläontologie und Histor. Geologie Jahr/Year: 1982 Band/Volume: 10 Autor(en)/Author(s): Kelly Simon R. A. Artikel/Article: Boreal influence on English Ryazanian Bivalves 285-292 © Biodiversity Heritage Library, http://www.biodiversitylibrary.org/; www.zobodat.at 285 Zitteliana 10 285-292 München, l.Ju li 1983 ISSN 0373-9627 Boreal influence on English Ryazanian Bivalves By SIMON R. A. KELLY*) With 6 text figures ABSTRACT In early Ryazanian times a marine embayment extended conditions and contain a bivalve fauna related in part to that of from the Southern North Sea Basin onto the East Midlands the late Portland Beds of the Upper Jurassic, although the Shelf (Spilsby Basin) and slightly later also reached into the sands are separated from these by the Lulworth Beds of late Yorkshire Basin. The sediments on the shelf are predomin Jurassic age. In southern England the Durlston Beds are pre antly glauconitic sandstones with phosphates and sideritic dominantly limestones and marls and contain various bivalve clay-ironstones (upper parts of the Spilsby Sandstone and the faunas ranging from restricted marine to freshwater facies. Sandringham Sands) while those in the Yorkshire Basin are The near marine horizons represent transgression into the clays (lowest part of the Speeton Clay). The associated bivalve Anglo-Paris basin from the north. The more restricted and faunas are marine and show strong affinities with East Green fresh-water environments are typical of European marginal land and Russian Platform faunas.