Alisocysta Margarita Zone, 213-14, 220 Angulata Zone, 244
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1 Chapel Row, Branscombe, Seaton, Devon, EX12 3AZ
1 Chapel Row, Branscombe, Seaton, Devon, EX12 3AZ An outstanding Grade II Listed end of terrace cottage currently let as a successful holiday cottage. Sidmouth 5 miles Honiton 8.6 miles • Three Bedrooms • Sitting Room With Inglenook • Kitchen/ Dining room • Bathroom and downstairs shower room • Private Gardens • Established holiday let • Character Offers in excess of £325,000 01404 45885 | [email protected] Cornwall | Devon | Somerset | Dorset | London stags.co.uk 1 Chapel Row, Branscombe, Seaton, Devon, EX12 3AZ SITUATION OUTSIDE A charming thatched cottage set the highly regarded The garden predominately laid to lawn with mature coastal village of Branscombe with its well-regarded hedging and a stone path. The parking area across the village school, two popular public houses and stunning road has parking for around 2 cars. beach. This delightful part of East Devon which has been designated an Area of Outstanding Natural Beauty forms SERVICES a major part of the Jurassic coast, a World Heritage site, Mains water, electricity and drainage. renowned for its dramatic cliffs and golden beaches. DIRECTIONS From the A3052 at Branscombe Cross travel south, sign There is a range of good independent schools in the area posted to Branscombe and Bulstone, continue on this with the revered Colyton Grammar School within easy road, passing the Fountain Head pub, for 1.7 miles and reach. The nearby Sidmouth provides for most everyday the property is on the left. requirements, including schools, shops, banks, post office, library, theatre and cinema. Honiton lies inland and offers a main line rail service to London Waterloo. Exeter is approximately 21 miles to the west with further amenities, a main line rail link to London Paddington, the M5 motorway and an International airport. -
Review the Mineralogy of Suspended Matter, Fresh and Cenozoic Sediments in the fluvio-Deltaic Rhine–Meuse–Scheldt–Ems Area, the Netherlands: an Overview and Review
Netherlands Journal of Geosciences — Geologie en Mijnbouw |95 – 1 | 23–107 | 2016 doi:10.1017/njg.2015.32 Review The mineralogy of suspended matter, fresh and Cenozoic sediments in the fluvio-deltaic Rhine–Meuse–Scheldt–Ems area, the Netherlands: An overview and review J. Griffioen1,∗,G.Klaver2 &W.E.Westerhoff3 1 TNO Geological Survey of the Netherlands, P.O. Box 80 015, 3508 TA Utrecht, the Netherlands and Copernicus Institute of Sustainable Development, Utrecht University, P.O. Box 80 115, 3508 TC Utrecht, the Netherlands 2 Formerly BRGM, Laboratories Division, 3 av. C. Guillemin, BP36009, 45060 Orleans, France; Le Studium, CNRS, Orleans, France; TNO Geological Survey of the Netherlands, P.O. Box 80 015, 3508 TA Utrecht, the Netherlands 3 TNO Geological Survey of the Netherlands, P.O. Box 80 015, 3508 TA Utrecht, the Netherlands ∗ Corresponding author. Email: jasper.griffi[email protected] Manuscript received: 18 March 2015, accepted: 13 October 2015 Abstract Minerals are the building blocks of clastic sediments and play an important role with respect to the physico-chemical properties of the sediment and the lithostratigraphy of sediments. This paper aims to provide an overview of the mineralogy (including solid organic matter) of sediments as well as suspended matter as found in the Netherlands (and some parts of Belgium). The work is based on a review of the scientific literature published over more than 100 years. Cenozoic sediments are addressed together with suspended matter and recent sediments of the surface water systems because they form a geoscientific continuum from material subject to transport via recently settled to aged material. -
A CRITICAL EVALUATION of the LOWER-MIDDLE PALAEOLITHIC ARCHAEOLOGICAL RECORD of the CHALK UPLANDS of NORTHWEST EUROPE Lesley
A CRITICAL EVALUATION OF THE LOWER-MIDDLE PALAEOLITHIC ARCHAEOLOGICAL RECORD OF THE CHALK UPLANDS OF NORTHWEST EUROPE The Chilterns, Pegsdon, Bedfordshire (photograph L. Blundell) Lesley Blundell UCL Thesis submitted for the degree of PhD September 2019 2 I, Lesley Blundell, confirm that the work presented in this thesis is my own. Where information has been derived from other sources, I confirm that this has been indicated in the thesis. Signed: 3 4 Abstract Our understanding of early human behaviour has always been and continues to be predicated on an archaeological record unevenly distributed in space and time. More than 80% of British Lower-Middle Palaeolithic findspots were discovered during the late 19th/early 20th centuries, the majority from lowland fluvial contexts. Within the British planning process and some academic research, the resultant findspot distributions are taken at face value, with insufficient consideration of possible bias resulting from variables operating on their creation. This leads to areas of landscape outside the river valleys being considered to have only limited archaeological potential. This thesis was conceived as an attempt to analyse the findspot data of the Lower-Middle Palaeolithic record of the Chalk uplands of southeast Britain and northern France within a framework complex enough to allow bias in the formation of findspot distribution patterns and artefact preservation/discovery opportunities to be identified and scrutinised more closely. Taking a dynamic, landscape = record approach, this research explores the potential influence of geomorphology, 19th/early 20th century industrialisation and antiquarian collecting on the creation of the Lower- Middle Palaeolithic record through the opportunities created for artefact preservation and release. -
Strategic Stone Study a Building Stone Atlas of Cambridgeshire (Including Peterborough)
Strategic Stone Study A Building Stone Atlas of Cambridgeshire (including Peterborough) Published January 2019 Contents The impressive south face of King’s College Chapel, Cambridge (built 1446 to 1515) mainly from Magnesian Limestone from Tadcaster (Yorkshire) and Kings Cliffe Stone (from Northamptonshire) with smaller amounts of Clipsham Stone and Weldon Stone Introduction ...................................................................................................................................................... 1 Cambridgeshire Bedrock Geology Map ........................................................................................................... 2 Cambridgeshire Superficial Geology Map....................................................................................................... 3 Stratigraphic Table ........................................................................................................................................... 4 The use of stone in Cambridgeshire’s buildings ........................................................................................ 5-19 Background and historical context ........................................................................................................................................................................... 5 The Fens ......................................................................................................................................................................................................................... 7 South -
Chapter 2 Physical Characteristics of the Study Area
CHAPTER 2 PHYSICAL CHARACTERISTICS OF THE STUDY AREA 2.1. Location of study area The study area incorporates part of north Hertfordshire, south and mid- Bedfordshire as well as the southwest corner of Cambridgeshire and lies approximately 40 km north of London (Figure 1.1). Coverage of the area by British Geological Survey (BGS) 1:50,000 map sheets is shown in Figure 2.1. 2.2. Bedrock geology The strikes of the solid geological formations are approximately northeast- southwest across the study area (Figure 2.2). The solid geological succession is shown in Table 2.1. To the northwest of the Chiltern Hills the Gault Clay forms a rich agricultural landscape, representing a continuation of the Vale of Aylesbury. Beyond this, running approximately from Bow Brickhill (SP915343) to Gamlingay (TL234525) is a discontinuous ridge formed by the Woburn Sands Formation, part of the Lower Greensand. This prominent ‘Greensand Ridge’, rising to 170 m O.D. at Bow Brickhill, separates the Cretaceous clays from the Jurassic Oxford and Ampthill Clays to the northwest. The oldest formation is recorded in a borehole (TL23NE1) at Ashwell (TL286390), where Devonian strata were reached at a depth of 186.54 m, i.e. 93 m below O.D. (Smith, 1992). Lying just beyond the northern boundary of the present study area, north of the River Ouse, a borehole (TL15NE2) at Wyboston (TL175572) penetrated Ordovician rocks of Tremadoc age at a depth of approximately 230 m (Moorlock et al ., 2003). The Oxford Clay of the Upper Jurassic represents the oldest formation outcropping within the study area. -
Dorset and East Devon Coast for Inclusion in the World Heritage List
Nomination of the Dorset and East Devon Coast for inclusion in the World Heritage List © Dorset County Council 2000 Dorset County Council, Devon County Council and the Dorset Coast Forum June 2000 Published by Dorset County Council on behalf of Dorset County Council, Devon County Council and the Dorset Coast Forum. Publication of this nomination has been supported by English Nature and the Countryside Agency, and has been advised by the Joint Nature Conservation Committee and the British Geological Survey. Maps reproduced from Ordnance Survey maps with the permission of the Controller of HMSO. © Crown Copyright. All rights reserved. Licence Number: LA 076 570. Maps and diagrams reproduced/derived from British Geological Survey material with the permission of the British Geological Survey. © NERC. All rights reserved. Permit Number: IPR/4-2. Design and production by Sillson Communications +44 (0)1929 552233. Cover: Duria antiquior (A more ancient Dorset) by Henry De la Beche, c. 1830. The first published reconstruction of a past environment, based on the Lower Jurassic rocks and fossils of the Dorset and East Devon Coast. © Dorset County Council 2000 In April 1999 the Government announced that the Dorset and East Devon Coast would be one of the twenty-five cultural and natural sites to be included on the United Kingdom’s new Tentative List of sites for future nomination for World Heritage status. Eighteen sites from the United Kingdom and its Overseas Territories have already been inscribed on the World Heritage List, although only two other natural sites within the UK, St Kilda and the Giant’s Causeway, have been granted this status to date. -
Evaluation of Belgian Clays for Manufacturing Compressed Earth Blocks Lavie A
GEOLOGICA BELGICA (2019) 22/3-4: 139-148 Evaluation of Belgian clays for manufacturing compressed earth blocks Lavie A. MANGO-ITULAMYA1*, Frédéric COLLIN2, Pascal PILATE3, Fabienne COURTEJOIE4 & Nathalie FAGEL1. 1Argiles, Géochimie et Environnement sédimentaires, University of Liège, Quartier Agora, 14 allée du 6 août, 4000 Liège, Belgium. 2Géotechnique, University of Liège, Quartier Polytech, 4000 Liège, Belgium. 3Belgian Ceramic Research Centre, 4 Av. du Gouverneur E. Cornez, 7000 Mons, Belgium. 4Architecture, University of Liège, 41 Boulevard de la Constitution, 4020 Liège, Belgium. * corresponding author: [email protected]. ABSTRACT. This study aims to characterize Belgian clays in order to evaluate their use for manufacture of compressed earth blocks (CEB). Nineteen Belgian clay deposits were sampled in 56 sites and 135 samples were collected and analyzed. The analyses focus on the determination of particle size, plasticity, nature and mineralogy as the main characteristics for assessing the suitability of the raw clays to make CEB. These analyses allow for classifying the sampled clay deposits in three categories: clays that can be used unchanged to make CEB (2 clay deposits), clays that are suitable for the manufacture of CEB but require addition of sand and gravel particles (13 clay deposits) and clays that are suitable for the manufacture of CEB if they are mixed with other raw clays (4 clay deposits). In order to verify the use of these clays, five of them served as a model for making CEB. The strength of these bricks was evaluated by testing for compressive strength and abrasion resistance. The results of these tests confirm the suitability or not of the sampled clays for the manufacture of CEB. -
Earth-Science Reviews
Earth-Science Reviews Predicting shoreline depositional process regimes using insights from palaeotidal modelling --Manuscript Draft-- Manuscript Number: Article Type: Review Article Keywords: Numerical Modelling; Wave; Tide; Fluvial; Palaeotidal; Mixed process; Shoreline; Deltaic; Shelf; Sedimentary Preservation Corresponding Author: Daniel Collins Shell International Ltd London, London UNITED KINGDOM First Author: Daniel Collins Order of Authors: Daniel Collins Alexandros Avdis Martin H. Wells Andrew J. Mitchell Peter A. Allison Howard D. Johnson Gary J. Hampson Jon Hill Christopher D. Dean Matthew D. Piggott Abstract: Tides are a fundamental element of predictive depositional models of ancient shoreline process regimes. These models principally relate ancient tidal potential to shelf width (c. 10–100 km) and shoreline geometry (c. 1–10 km) but rarely consider larger-scale basin physiography (100–1000 km) or variability related to changing shoreline geometry. A refined predictive decision tree for ancient shoreline process regimes is developed based on a review of modern shoreline processes, supported by new insight from numerical palaeotidal modeling studies. Modern depositional shorelines are overwhelmingly wave dominated, suggesting a first-order control of wave fetch and wave-generating wind conditions on shoreline processes. Several numerical palaeotidal modeling studies highlight the following controls on tidal processes: (1) 100–1000 km-scale basin physiography on tidal inflow versus outflow; (2) 10–100 km- scale shelf physiography on shelf tidal resonance potential; (3) tidal amplification (funnelling and shoaling) versus frictional effects in shoreline embayments (1–10 km scale); and (4) palaeogeographic uncertainty, which affects prediction of these latter three controls. The predictive decision tree considers the effects of basin physiography, shelf width and shoreline morphology on wave, tide and fluvial processes separately. -
Site Improvement Plan Sidmouth to West Bay
Improvement Programme for England's Natura 2000 Sites (IPENS) Planning for the Future Site Improvement Plan Sidmouth to West Bay Site Improvement Plans (SIPs) have been developed for each Natura 2000 site in England as part of the Improvement Programme for England's Natura 2000 sites (IPENS). Natura 2000 sites is the combined term for sites designated as Special Areas of Conservation (SAC) and Special Protected Areas (SPA). This work has been financially supported by LIFE, a financial instrument of the European Community. The plan provides a high level overview of the issues (both current and predicted) affecting the condition of the Natura 2000 features on the site(s) and outlines the priority measures required to improve the condition of the features. It does not cover issues where remedial actions are already in place or ongoing management activities which are required for maintenance. The SIP consists of three parts: a Summary table, which sets out the priority Issues and Measures; a detailed Actions table, which sets out who needs to do what, when and how much it is estimated to cost; and a set of tables containing contextual information and links. Once this current programme ends, it is anticipated that Natural England and others, working with landowners and managers, will all play a role in delivering the priority measures to improve the condition of the features on these sites. The SIPs are based on Natural England's current evidence and knowledge. The SIPs are not legal documents, they are live documents that will be updated to reflect changes in our evidence/knowledge and as actions get underway. -
Summer 2014 Free
SUMMER 2014 FREE Robots raise money for a Water Survival Box Page 26 Sea Creatures at Charmouth Primary School Page 22 Winter Storms Page 30 Superfast Mary Anning Broadband – Realities is Here! Page 32 Page 6 Five Gold Stars Page 19 Lost Almshouses Page 14 Sweet flavours of Margaret Ledbrooke and her early summer future daughter-in-law Page 16 Natcha Sukjoy in Auckland, NZ SHORELINE SUMMER 2014 / ISSUE 25 1 Shoreline Summer 2014 Award-Winning Hotel and Restaurant Four Luxury Suites, family friendly www.whitehousehotel.com 01297 560411 @charmouthhotel Contemporary Art Gallery Morcombelake Fun, funky and Dorset DT6 6DY 01297 489746 gorgeous gifts Open Tuesday to Saturday 10am – 5pm for everyone! Next to Charmouth Stores (Nisa) www.artwavewest.com The Street, Charmouth - Tel 01297 560304 CHARMOUTH STORES Your Local Store for more than 198 years! Open until 9pm every night The Street, Charmouth. Tel 01297 560304 2 SHORELINE SUMMER 2014 / ISSUE 25 Editorial Charmouth Traders Summer 2014 Looking behind, I am filled n spite of the difficult economic conditions over the last three or four years it with gratitude. always amazes me that we have the level of local shops and services that we Ido in Charmouth. There are not many (indeed I doubt if there are any) villages Looking forward, I am filled nowadays that can boast two pubs, a pharmacy, a butcher, a flower shop, two with vision. hairdressers, a newsagents come general store like Morgans, two cafes, fish and chip shops, a chocolate shop, a camping shop, a post office, the Nisa store Looking upwards, I am filled with attached gift shop, as well as a variety of caravan parks, hotels, B&Bs and with strength. -
Ward Beer and Branscombe Reference 21/0302/FUL Applicant
Ward Beer And Branscombe Reference 21/0302/FUL Applicant Mr & Mrs Reid Location Bumbles Locker Fore Street Beer Seaton EX12 3JB Proposal Proposed change of use of shops (A1) to living accommodation (C3) associated with a multi bedroomed self catering holiday let, alterations to the shop fronts, the conversion of existing attic space with the addition of two dormer windows and rear two storey extension to form a new stairwell RECOMMENDATION: Approval with conditions Crown Copyright and database rights 2021 Ordnance Survey 100023746 Committee Date: 5th May 2021 Beer And Target Date: Branscombe 21/0302/FUL 01.04.2021 (Beer) Applicant: Mr & Mrs Reid Location: Bumbles Locker Fore Street Proposal: Proposed change of use of shops (A1) to living accommodation (C3) associated with a multi bedroomed self catering holiday let, alterations to the shop fronts, the conversion of existing attic space with the addition of two dormer windows and rear two storey extension to form a new stairwell RECOMMENDATION: Approval with conditions EXECUTIVE SUMMARY The application is presented to committee as the officer recommendation differs from that of the ward member. The proposal relates to a mixed use property located in the centre of Beer within the defined built-up area boundary and village centre and the designated Beer Conservation Area. The ground floor of the front part of the property has a lawful commercial use, most recently for retail purposes but currently vacant. It is subdivided into 2 no. units a larger unit to the left and smaller unit to the right. The remainder of the ground floor and the first floor of the building are in residential use as a single unit. -
2. General Index
Downloaded from http://pygs.lyellcollection.org/ by guest on September 29, 2021 2. General Index abandoned river courses. Vale of York 40,223-32 anhydrite 50.78.79,81,86,88.143-54 Abbey Crags, Knaresborough Gorge 46,290 Anisocardiu tenera (Antiquicyprina) loweana 39, 117, 130, 131.738-9 Acadian 46,175 ff.; 50,255-65 anisotropy of vitrinites 39,515-26 acanthite 46,135 ankerite 50,87 Acanthodiacrodium cf. simplex 42,412-3 annelida, in Yorkshire Museum 41,402 Acanthodiacrodium rotundatum 45.124 antimony, trace element in galena 44,153 Acanthodiacrodium cf. tumidum 45,124 apatite 44,438 Acanthopleuroceras sp. 42, 152-3 apatite fission-track palaeotemperatures. north-west England 50,95-9 accretionary lapilli, Cwm Clwyd Tuff 39,201,206-7,209,215-6 Apatocythere (Apatocythere) simulans 45, 243 Acheulian handaxes 41,89,94-5 Apedale Fault 50. 196," 198 acid intrusions, Ordovician and Caledonian, geochemical characteristics aplites. Whin Sill 47,251 of 39,33-57 Apollo's Coppice, Shropshire 50,193 acritarchs. Arenig 42. 405 Arachinidiuin smithii 42, 213 acritarchs, Ordovician 47,271-4 Araucarites phillipsii 45,287 acritarchs,Tremadoc 38 45-55; 45,123-7 archaeology, Lincolnshire 41.75 ff. Actinocamax plenus 40,586 Arcomva unioniformis 39.117.133, 134, 138 Acton Reynald Hall, Shropshire 50,193,198,199,200,202,204 Arcow"45,19ff.' adamellite (Threlkeld Microgranite) 40,211-22 Arcow Wood Quarry 39,169,446,448,455,459,470-1 aegirine 44,356 arctic-alpine flora. Teesdale 40.206 aeolian deposition, Devensian loess 40,31 ff. Arenicolites 41,416,436-7 aeolian deposition. Permian 40,54.55 Arenobulirnina advena 45,240 aeolian sands, Permian 45, 11-18 Arenobulimina chapmani 45,240 aeolian sedimentation, Sherwood Sandstone Group 50,68-71 Arenobulirnina macfadyeni 45, 240 aeromagnetic modelling, west Cumbria 50,103-12 arfvedsonite 44,356 aeromagnetic survey, eastern England 46,313,335—41 argentopyrite 46, 134-5 aeromagnetic survey, Norfolk 46.313 Arniocreas fulcaries 42, 150-1 Africa, North, Devonian of 40,277-8 arsenic 44,431 ff.