Minutes of Committee Meeting 10 October
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The Mill Cottage the Mill Cottage Cockercombe, Over Stowey, Bridgwater, TA5 1HJ Taunton 8 Miles
The Mill Cottage The Mill Cottage Cockercombe, Over Stowey, Bridgwater, TA5 1HJ Taunton 8 Miles • 4.2 Acres • Stable Yard • Mill Leat & Stream • Parkland and Distant views • 3 Reception Rooms • Kitchen & Utility • 3 Bedrooms (Master En-Suite) • Garden Office Guide price £650,000 Situation The Mill Cottage is situated in the picturesque hamlet of Cockercombe, within the Quantock Hills, England's first Area of Outstanding Natural Beauty. This is a very attractive part of Somerset, renowned for its beauty, with excellent riding, walking and other country pursuits. There is an abundance of footpaths and bridleways. The village of Nether Stowey is 2 miles away and Kingston St A charming Grade II Listed cottage with yard, stabling, 4.2 Acres of Mary is 5 miles away. Taunton, the County Town of Somerset, is some 8 miles to the South. Nether Stowey is an attractive centre land and direct access to the Quantock Hills. with an extensive range of local facilities, which are further supplemented by the town of Bridgwater, some 8 miles to the East. Taunton has a wide range of facilities including a theatre, county cricket ground and racecourse. Taunton is well located for national communications, with the M5 motorway at Junction 25 and there is an excellent intercity rail service to London Paddington (an hour and forty minutes). The beautiful coastline at Kilve is within 15 minutes drive. Access to Exmoor and the scenic North Somerset coast is via the A39 or through the many country roads in the area. The Mill Cottage is in a wonderful private location in a quiet lane, with clear views over rolling countryside. -
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. -
Taunton Rock Trail FURTHER CONTACTS E X P L O R E T H E H I D D E N S E C R E T S F R O M T I M E S P a S T
Taunton Taunton Rock Trail FURTHER CONTACTS E x p l o r e t h e h i d d e n s e c r e t s f r o m t i m e s p a s t Rock Trail The Museum’s displays of geological interest are currently being revised. They include: local minerals, invertebrate marine fossils, Lower Jurassic marine vertebrates and Pleistocene (Ice Age) mammals from The Taunton Rock Trail provides the famous bone caves of the western Mendips. The an excellent introduction to the reserve collections are extensive, numbering in excess of 40,000 specimens of rock, minerals and geology around Taunton. fossils. Books can be purchased at their shop near Building stones provide one of the entrance. the best ways of getting to know the local rocks as Taunton Castle, Castle Green, Taunton TA1 4AA. Tel:01823 320200. www.somerset.gov.uk/museums there are now so few accessible exposures available Telephone for opening times. for study. The trail only touches upon a selection of rock types that illustrate the local geology. Somerset Studies Library Emphasis is placed on description rather than The Reference Library, located in Paul Street, has a explanation. Geology is an observational science. selection of geological memoirs, articles and maps besides a wealth of other material on Somerset topics. Study of the textures, colours and structures of the It is open 9.30-5.30 except Wednesday and Friday until various rock types is an essential first step in 7.00 and Saturday 4.00. recognising them. A small x10 hand lens (held close Paul Street, Taunton TA1 3XZ. -
Download Somerset
Somerset by G.W. Wade and J.H. Wade Somerset by G.W. Wade and J.H. Wade Produced by Dave Morgan, Beth Trapaga and the Online Distributed Proofreading Team. [Illustration: A MAP OF THE RAILWAYS OF SOMERSET] [Illustration: THE PINNACLES, CHEDDAR] SOMERSET By G.W. WADE, D.D. and J.H. WADE, M.A. _With Thirty-two Illustrations and Two Maps_ page 1 / 318 "Upon smooth Quantock's airy ridge we roved." London Methuen & Co 36 Essex St. Strand [Illustration: Hand drawn Routes of the Somerset & Dorset Railway] PREFACE The general scheme of this Guide is determined by that of the series of which it forms part. But a number of volumes by different writers are never likely to be quite uniform in character, even though planned on the same lines; and it seems desirable to explain shortly the aim we have had in view in writing our own little book. In our accounts of places of interest we have subordinated the historical to the descriptive element; and whilst we have related pretty fully in the Introduction the events of national importance which have taken place within the county, we have not devoted much space to family histories. We have made it our chief purpose to help our readers to see for themselves what is best worth seeing. If, in carrying out our design, we appear to have treated inadequately many interesting country seats, our excuse must be that such are naturally not very accessible to the ordinary tourist, whose needs we have sought to supply. And if churches and church architecture seem to receive undue attention, it may be page 2 / 318 pleaded that Somerset is particularly rich in ecclesiastical buildings, and affords excellent opportunities for the pursuit of a fascinating study. -
Taunton Building Stones Walk; Fri 2Nd February 2018 a Leader's
Taunton Building Stones Walk; Fri 2nd February 2018 A Leader’s Perspective Since I retired a few years ago I have been surveying building stones for the Somerset Heritage Trust. As Taunton town centre is a particularly good place for geologists to study building stones a walk here seemed a good way to start the AGM Weekend. Several people had done their homework and brought with them either Hugh Prudden’s book “Geology and Landscape of Taunton Deane “or Eric Robinson’s notes from a previous OUGS outing so I knew I had to concentrate! Taunton is located on Triassic Mercia Mudstone rocks which are unsuitable as a building stone. Rocks of many different lithologies, ranging in age from Devonian to Miocene, occur within a short distance of Taunton (see map) and have been used for the building stone in Taunton over many centuries. This variety of rock types and ages (see Table 1: stratigraphic column for the current BGS terminology and the equivalent traditional names of building stone) and the existence of buildings from many different historical periods mean that Taunton is a particularly good place for geologists to study building stones. We began our walk at the Taunton Castle which today is occupied by the Museum of Somerset. A wall by the approach path to the Castle Gatehouse is constructed of irregular pieces of chert which is used as a building stone in Taunton and southwards into the Blackdown Hills. It is the result of Miocene weathering of the chalk and today is found on the top of the hills and across the lower ground northwards towards Taunton, where it was probably transported in periglacial conditions during the Pleistocene Period. -
RSPB 6Pp Leaflet
Area of Outstanding Natural Beauty JURASSIC CRETACEOUS TERTIARY PLEISTOCENE HOLOCENE • First birds evolve from reptiles • Evolution of flowering plants • First hominids evolve • Ice Age mammals Palaeolithic Mesolithic Neolithic • Widespread shallow seas with ammonites • Extinction of the dinosaurs, ammonites, large marine reptiles • End of last Ice Age • Extinction of mammoths • First crops farmed 200 million years ago 145 million years ago 65 million years ago 2.5 million years ago 750,000 years ago 10,000 years BC 4500 years BC 2000 years BC SOMERSET’S JURASSIC COAST FOSSILS GEOLOGY AND LANDSCAPE The Quantock Hills rise to over 350 metres, an ascent Somerset’s Jurassic Coast stretches from Blue Anchor eastwards beyond Lilstock, and The coast between East Quantoxhead and Kilve has long been known as a good some of the best exposures occur within the AONB area, especially in cliffs around East location to find fossils. Particularly characteristic and numerous fossils are ammonites which passes through hill pastures, coniferous and mixed Quantoxhead and Kilve. Most of the rocks here were formed from sediments deposited (extinct marine snails related to modern-day squids) and bivalves, including clams, forests and sessile oak woodlands to open moorland on the bottom of an ancient seafloor approximately 195 to 200 million years ago. They scallops and oysters. Concentrations of small, ribbed shells (called brachiopods) often summits with heathland. The rocks that form these hills consist of yellow-weathering grey limestones which alternate with units of darker crowded together in large limestone blocks also occur. Occasionally fossils of large are from the Devonian Period of geological time, and are mudstones and shales. -
Somerset County Council Transport Asset Management Plan 2010 Appendices 3 – 5
Somerset County Council Transport Asset Management Plan 2010 Appendices 3 – 5 WWW.SOMERSET.GOV.UK Appendix 4 – Extended tables Appendix 3 Index of tables 3. Goals, Objectives and Policies Paragraph Page 3.1: Meeting Annual Plan and Community Strategy Aims 3.2 13 3.2: Meeting LTP2 Objectives 3.4 12 3.3: Key policy documents 3.9 16 4. Levels of service 4.1: Levels of service definitions 4.20 22 4.2: Indicators and the linkage to levels of service 4.22 23 4.3: Performance measure contribution 4.24 25 4.4: Numerical scoring for level of service standard 4.24 25 4.5.1: Accessibility and economic growth 4.28 26 4.5.2: Environment 4.28 30 4.5.3: Road safety 4.28 32 4.5.4: Demand aspirations 4.28 35 4.5.5: Asset Condition 4.28 39 4.6: Levels of service achieved 4.28 43 5. Inventory and condition assessment 5.1: Management systems 5.8 45 5.2: Carriageway asset by district and road class (km) 5.37 49 5.3: Carriageway asset by district and hierarchy 5.39 49 5.4: Length of footway and cycleway by category and district 5.47 50 5.5: Summary of structures 5.54 51 5.6: Highway gullies and kerb offlets as at November 2008 5.71 54 5.7: Ditches and grips 5.71 54 5.8: Summary of verge lengths cut by SCC 5.85 57 5.9: Biodiversity sites requiring ‘special’ attention 5.93 58 5.10: Type and numbers of lighting units 5.101 59 5.11: Signs, road markings and road studs 5.115 62 5.12: SCC signals inventory 5.121 63 5.13: Rights of way network by status 5.125 63 5.14: ProW network assets 5.127 64 5.15: Inventory of cattle grids owned by SCC 5.134 65 5.16: Inventory of arrester beds 5.136 66 5.17: Inventory of safety fencing 5.138 66 5.18: Inventory of depots 5.141 67 5.19: Winter service criteria 5.143 67 5.20: Extent of data collected definition 5.150 68 5.21: Reliability of data collected definition 5.150 69 5.22: Knowledge level matrix 5.150 69 5.23: Combined summary of inventory knowledge and condition 5.150 70 6. -
STRATEGIC STONE STUDY a Building Stone Atlas of SOMERSET & EXMOOR
STRATEGIC STONE STUDY A Building Stone Atlas of SOMERSET & EXMOOR Published August 2011 Derived from BGS digital geological mapping at 1:625,000 scale, British Geological Survey © Somerset & Exmoor Bedrock Geology NERC. All rights reserved Click on this link to visit Somerset’s geology and their contribution to known building stones, stone structures and building stone quarries (Opens in new window . http://maps.bgs.ac.uk/buildingstone?County=Somerset) Somerset Strategic Stone Study 1 INTRODUCTION Quarrying for building stones has occurred in Somerset since at least Roman times, and traces Geologically speaking, Somerset and Exmoor is of this activity can still be seen in the Mendip an extremely diverse area, with rocks varying in Hills. Today the Mendip area still contains very age from the Silurian Period (425 million years large, active limestone quarries although the old). Virtually all the rocks are SEDIMENTARY stone is extracted mainly for aggregate rather METAMORPHIC in origin, with only a few than building purposes. However, the current localised occurrences of INTRUSIVE or volcanic need for local stone for either conservation rocks, this provides a considerable variety of repair or to maintain traditional character in building stones ranging from extremely hard, new buildings seems to be increasing, although highly resistant SILICEOUS FLINTS, CHERTS AND the number of pits and quarries now available QUARTZITIC SANDSTONES, to softer, sandy for these stones is only a fraction of those LIMESTONES, and fissile SLATES useful for roofing worked in former times. and walling. In general terms the geology and occurrence of Somerset and Exmoor’s main building stones can conveniently be considered in four groups: • To the west of the area lie the rolling hills of Exmoor, the Brendons and the Quantocks. -
Dawson, G J, and Wright, P, the Historic Use of Building Stones In
THE HISTORIC USE OF BUILDING STONES IN TAUNTON DEANE G. J. DAWSON AND P. WRIGHT ABSTRACT BACKGROUND This paper describes a survey of building stones In 2015 the Somerset Historic Environment Service carried out in Taunton Deane to support the of the South West Heritage Trust, formerly the buildings conservation work of the South West Heritage Service of Somerset County Council, Heritage Trust. Building stones are identified and identified the need for a survey of the use of the factors that have influenced the selection of traditional building stones in Somerset (Somerset these stones for building are discussed. A very close Historic Environment Service, 2015). The primary correlation between the building stones used and purpose of the survey was to assist the Historic the local geology is demonstrated. Environment Service with preserving the character, appearance and local distinctiveness of towns and villages in the county. This paper describes an initial survey of Taunton Deane. It describes the Fig. 1 Data collection sheet 147 15517 - Somerset Arch Vol 161 - 2018.indb 147 20/09/2018 11:50:36 SOMERSET ARCHAEOLOGY AND NATURAL HISTORY, 2017 methodology and results of the survey and how the War that could be seen from a public road or data may be used by the Trust and others. footpath were included in the survey. Data were collected in the field using the form shown in Figure 1. Except for all churches and significant SURVEY METHOD civic, administrative, educational and historic buildings in Taunton, records were not kept of the The principal data collected during the survey were building stones used in individual buildings. -
Landscape Character Assessment
Quantock Landscape Partnership Scheme Landscape Character Assessment Final Report February 2019 Acknowledgements Cookson & Tickner would particularly like to thank Bill Jenman (Landscape Partnership Development Officer for the Quantock Landscape Partnership Scheme), Iain Porter (Development Officer for the Quantock Hills AONB Service), Chris Edwards (Quantock Hills AONB Service Manager) and the Quantock Hills AONB Service team for their valued steer, knowledge and input in the preparation of this report. Cookson & Tickner Ltd, Rystwood, Seven Ash, Bishops Lydeard, Taunton TA4 3EX www.cooksonandtickner.co.uk Table of Contents Executive Summary ..................................................................... 1 1. Introduction .......................................................................... 3 2. Understanding Landscape ..................................................... 7 3. The Quantock Hills AONB and its Setting ............................ 15 4. The Natural Landscape ........................................................ 17 5. The Shaping of the Cultural Landscape ................................ 25 6. The Character of the Quantock Landscape ........................... 33 7. River Valley and Agricultural Fringe ..................................... 35 8. Wooded and Farmed Escarpment ........................................ 42 9. Rolling Farmland and Settled Combes ................................. 47 10. Open Hills ........................................................................... 56 11. Lowland Hills to Coast -
Flora of Somerset
A SUPPLEMENT TO THE FLORA OF SOMERSET EDWARD SHEARBURN MARSHALL, M.A., F.L.S. RECTOR OF WEST MONKTON. Uaunton : PUBLISHED BY THE SOMERSETSHIRE ARCH^OLOGICAL AND NATURAL HISTORY SOCIETY. 1914 ; PREFACE. In these pages I have tried to record the various additions or corrections since the pubHcation of Mr. Murray's book ; which, though dated 1896, was not (I beheve) issued until early in the following year. There is a certain fitness in my continuing his work ; for we were intimate friends from the autumn of 1882 until his death, and I had a small share in his Somerset explorations : he was also my first real helper in the study of critical plants. I have generally followed the London Catalogue names and standard of species, which is somewhat more liberal than that of Fl. Som. ; Mr. Murray was accustomed to deal with larger areas, and his point of view was synthetical, rather than analytical. Researches have been carried on for many years in the north-west ; the results are embodied in Mr. J. W. White's Flora of Bristol, in my opinion quite the best and most thorough book of its kind, which appeared in 1912. He has most generously allowed me to make full use of it and—as the reader cannot fail to see—it has been my mainstay. Our friend Dr. C. E. Moss has written an important plant-associations work on the of the county ; and I wish to thank my numerous correspondents for their cordial help. The time has not yet come for a new edition of the Somerset Flora, ; several districts stiU need much closer investigation, and my own scanty leisure is so much occupied by other matters that I have been un- iv ablo to (lovoto a great deal of it to local excursions. -
Landscape Conservation Action Plan; Part 1 Contents Landscape Conservation Action Plan Contents
QUANTOCK LANDSCAPE PARTNERSHIP Landscape Conservation Action Plan; Part 1 Contents Landscape Conservation Action Plan Contents 1 Introduction 4 1.1 Location 5 1.2 The Partnership Board 5 1.3 Vision, Aims, and Objectives 6 1.4 Development and Consultation 9 1.5 Structure of the LCAP 13 2 The Quantock Hills – Somerset’s Secret 14 2.1 Introduction to the Quantocks 14 2.2 Deep Roots; the Geology of the Quantocks 19 2.3 Quantock History; the Development of a Manorial Landscape 27 2.4 The Working Landscape 47 2.5 Quantock Nature 48 2.5.1 Priority Habitats within the LPS area 48 2.5.2 Other Significant Habitats and Widespread Species 53 2.5.3 European Protected Species 55 2.5.3 Designated Sites and Ancient Woodland Inventory 56 2.6 Significance of the Built Heritage 58 3 People and the landscape; access and opportunity 61 The 2018 Quantock Hills User Survey – who comes to the Hills already, 3.1 61 and what do they think of the area? 3.2 Affluence and Deprivation 65 3.3 Barriers to Access 70 What Do People Want? What should the Landscape Partnership Scheme do to help 3.4 73 disadvantaged audiences overcome the barriers to access? 3.5 Potential Audiences; engagement in the medium and long term 74 4 Landscape Character 82 4.1 Landscape Character Assessment 82 4.2 National Character Areas 82 4.2.1 National Character Area 144. Quantock Hills 84 4.2.2 National Character Area 146. Vale of Taunton and Quantock Fringes 85 4.3 The Quantock Landscape Partnership Scheme Landscape Character Assessment 87 4.3.1 River Valley and Agricultural Fringe 89 4.3.2