Historical Analysis of Exmoor Moorland Management Agreements
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Dear Guest, Peter and Linda Hendrie And
Dear Guest, Peter and Linda Hendrie and family, together with all their Staff, welcome you to The Exmoor White Horse Inn, one of Exmoor’s oldest and finest Country Inns. Our aim is to make your stay with us as comfortable and relaxed as possible, without being intrusive. We pride ourselves on our warm and friendly welcome, and aspire to provide the kind of personal service that one would associate with this kind of establishment. “Your Pleasure is our Business” and help is always on hand from all members of Staff and Management for advice on all aspects related to your holiday on Exmoor, from finding out where the hounds meet to Fly Fishing with our Resident Guide Lewis, Riding over Exmoor on horseback, viewing the wild Red Deer with the Exmoor Safari, Walking and Rambling (Circular Walks Booklets are available from Reception), Clay Pigeon Shooting and Photography, just to mention but a few of the activities that are available. Exmoor, summed up in a nutshell, offers a delightfully varied contrast of beautiful countryside and dramatic scenery for such a relatively small area. On arrival you will be given a leaflet called “Discover Exmoor with Us” and if you have the opportunity we recommend that you try out one of these Routes, which were designed especially for those of you wishing to see Exmoor at its finest. We arrived here at the Exmoor White Horse on November 2nd 1988, and we have aspired to continually improve the quality of Service, Accommodation and the Food, priding ourselves on the friendliness shown by Management and Staff towards you, the Customer. -
A New Geological Model to Explain the Gravity Gradient Across Exmoor, North Devon
A new geological model to explain the gravity gradient across Exmoor, north Devon M. BROOKS, M. BAYERLY & D. J. LLEWELLYN SUMMARY Recent long seismic lines in South Wales and plained by a simple geological model in which the Bristol Channel indicate a structural cul- a thick sequence ofrelatlvely low density Lower mination under the southern part of the Bristol Palaeozoic or late Precambrian rocks occupies Channel, where a layer with a seismic velocity the core of this culmination. The model casts of 6-I km/s approaches to about 2 km of the further doubt on the existence of a major thrust surface. It is shown that the gravity field across under Exmoor. Exmoor and the Bristol Channel can be ex- I. Introduction SEVERAL LONG SEISMIC LINES in the Bristol Channel area, full details of which will be presented in later papers, give evidence of a basal layer of high velocity, in the range from 6. I-6. 3 km/s, which is interpreted as being of Lower Palaeozoic or Precambrian age. This layer, which almost certainly does not represent the same geological formation under all lines, lies at shallow depth under the western part of the South Wales Coalfield, deepens southwards into the northern part of the Bristol Channel and rises rapidly towards the north Devon coast. Figure I illustrates reduced time-distance curves for two of the long seismic lines D and F, whose locations are shown in Fig. 2. On each line, a series of offshore shots was fired into a fixed array of land recording stations. -
Dr Keith Howe the Exmoor Society
LANDSCAPE AND NATURAL CAPITAL IN A NATIONAL PARK: THE CASE OF EXMOOR 5;kl; Dr Keith Howe The Exmoor Society Natural England Landscape Network Autumn Webinar 2, 14 October 20201 CONTEXT ➢ National policy ➢ Exmoor National Park From KEY CONCEPTS & PRINCIPLES ➢ Landscape ➢ Natural capital ➢ Value ➢ The nature of economic decisions ➢ Private and public goods - to SHAPING EXMOOR’S FUTURE LANDSCAPE ➢ Exmoor’s Ambition ➢ Towards a Register of Exmoor’s Natural Capital NEXT STEPS & ISSUES ARISING ➢ Making ELMS work ❑ Economics ❑ Governance ❑ Constraints 2 CONTEXT The Exmoor Society 60th Anniversary & Exmoor National Park Authority Spring Conference (2017) - Dieter Helm’s challenge A Green Future: Our 25 Year Plan to Improve the Environment (2018) - HM Government Landscapes Review (2019) – the Glover report Agriculture Bill (2020) For farmers, the most radical Environment Bill (2020) change for Brexit (2020) agricultural policy since 1846 3 EXMOOR NATIONAL PARK Counties: Somerset 71%, Devon 29% Area: 69,280 hectares = 171,189 acres = 267sq miles (30% of Lake District) Landscape: Moorland or heath c25% of Exmoor National Park, 18,300 hectares of land lying between 305 m (1000 ft) and 519 m (1700 ft) above sea level. Population: Main settlements: Lynton and Lynmouth, Dulverton, Porlock, each c1500; Dunster < 1000, Exmoor total 10,000+ Farms: 559 holdings, 412 full-time commercial farmers (2016) Main farm outputs: In 2014/15, 62% of sheep were finished lamb sales, 16.3% finished cattle sales (majority sold as stores). Farm business income (FBI): Of the 2014/15 aggregate for Farm Business Survey sample, all Exmoor farms; FBI was 17% of gross output, of which; 14.4% Single Farm Payment; 8.1% diversification out of agriculture; 60.2% agri-environment and other payments; minus 53.3% agriculture. -
Flooding in the Somerset Levels, 2014 by Christina Mann
GEOACTIVE 549 Flooding in the Somerset Levels, 2014 By Christina Mann A case study about the Relevance to specifications causes, impacts and Exam Link to specification management of flooding board on the Somerset Levels AQA A Unit 1: Physical Geography, Section B, Water on the land, page 13 For a period of three months from http://filestore.aqa.org.uk/subjects/AQA-9030-W-SP-14. December 2013 to February 2014, PDF the Somerset Levels hit the national AQA B Unit 1: Managing Places in the 21st century, The coastal headlines as the area suffered from environment, pages 8–10 http://filestore.aqa.org.uk/subjects/AQA-9035-W-SP-14. extensive flooding. At the height of PDF 2 the winter floods, 65 km of land on Edexcel A Unit 2, The Natural Environment, Section A, The Physical the Levels were under water. This World, Topic 2: River Landscapes, pages 21 and 22 was caused by human and physical http://qualifications.pearson.com/content/dam/pdf/ GCSE/Geography-A/2009/Specification%20and%20 factors. The floods were the most sample%20assessments/9781446911907_GCSE_ severe ever known in this area. Lin_Geog_A_Issue_5.pdf No one was prepared for the extent Edexcel B Unit 1, Dynamic Planet, Section B, Small-scale Dynamic Planet, Topic 6, River Processes and Pressures, page 17 of damage brought by the http://qualifications.pearson.com/content/dam/pdf/ floodwater. Several villages and GCSE/Geography-B/2009/Specification%20and%20 farms were flooded and hundreds of sample%20assessments/9781446911914_GCSE_Lin_ Geog_B_Issue_5.pdf people had to be evacuated. OCR B Unit 562, Key Geographical Themes, Theme 1: Rivers The risk of flooding is likely to and Coasts, pages 12 and 13 increase in the future due to climate http://www.ocr.org.uk/Images/82581-specification.pdf change. -
Download Annex A
Landscape Character Assessment in the Blackdown Hills AONB Landscape character describes the qualities and features that make a place distinctive. It can represent an area larger than the AONB or focus on a very specific location. The Blackdown Hills AONB displays a variety of landscape character within a relatively small, distinct area. These local variations in character within the AONB’s landscape are articulated through the Devon-wide Landscape Character Assessment (LCA), which describes the variations in character between different areas and types of landscape in the county and covers the entire AONB. www.devon.gov.uk/planning/planning-policies/landscape/devons-landscape-character- assessment What information does the Devon LCA contain? Devon has been divided into unique geographical areas sharing similar character and recognisable at different scales: 7 National Character Areas, broadly similar areas of landscape defined at a national scale by Natural England and named to an area recognisable on a national scale, for example, ‘Blackdowns’ and ‘Dartmoor’. There are 159 National Character Areas (NCA) in England; except for a very small area in the far west which falls into the Devon Redlands NCA, the Blackdown Hills AONB is within Blackdowns NCA. Further details: www.gov.uk/government/publications/national-character-area-profiles-data-for-local- decision-making/national-character-area-profiles#ncas-in-south-west-england 68 Devon Character Areas, unique, geographically-specific areas of landscape. Each Devon Character Area has an individual identity, but most comprise several different Landscape Character Types. Devon Character Areas are called by a specific place name, for example, ‘Blackdown Hills Scarp’ and ‘Axe Valley’. -
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. -
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Stuart Bcckhurst x 2 Senior Scientist (Quality Planning) ) £e> JTH vJsrr U T W J Vcxg locafenvironment agency plan EXE ACTION PLAN PLAN from JULY 2000 to JULY 2005 Further copies of this Action Plan can be obtained from: LEAPs (Devon Area) The Environment Agency Exminster House Miller Way Exminster Devon EX6 8AS Telephone: (01392) 444000 E-mail: [email protected] Environment Agency Copyright Waiver This report is intended to be used widely and the text may be quoted, copied or reproduced in any way, provided that the extracts are not quoted out of context and that due acknowledgement is given to the Environment Agency. However, maps are reproduced from the Ordnance Survey 1:50,000 scale map by the Environment Agency with the permission of the Controller of Her Majesty's Stationery Office, © Crown Copyright. Unauthorised reproduction infringes Crown Copyright and may lead to prosecution or civil proceedings. Licence Number GD 03177G. Note: This is not a legally or scientifically binding document. Introduction 1 . Introduction The Environment Agency We have a wide range of duties and powers relating to different aspects of environmental management. These duties are described in more detail in Section Six. We are required and guided by Government to use these duties and powers in order to help achieve the objective of sustainable development. The Brundtland Commission defined sustainable development 'os development that meets the needs of the present without compromising the ability of future generations to meet their own needs' At the heart of sustainable development is the integration of human needs and the environment within which we live. -
Butterflies of Exmoor Leaflet
. s n o s r a P k r a M y b s o t o h p h t o m l l A . ) e d i u g s i h t f o k c a b e h t n o e r a s l i a t e d ) A N ( ) S ( ) I ( ) D ( . d e s s e s s a t o N ; e l b a t S ; e s a e r c n I ; e n i l c e D g n i w d n i h f o t c a t n o c ( n o i t a v r e s n o C y l f r e t t u B h t i w h c u o t n i t e g ) M ( ) L ( ; t n a r g i M ; e r e h w e s l e e r a R / n o m m o C y l l a c o L f l a h r e t u o o t n w o r b - w o l l e y ; n w o r b r e k r a d d o i r e p t h g i l f k a e P f o s d n a b h t i w n w o r b - y e r g e l a p g n i w e r o f ) R ( ) C ( e s a e l p , s e i l f r e t t u b g n i d r o c e r h t i w d e v l o v n i t e g o t e k i l ; r o o m x E n o e r a R ; r o o m x E n o n o m m o C n o i n a p m o C t e n r u B : d n e r T l a n o i g e R / s u t a t S * e m i t t h g i l f e l b i s s o p / l a n o i s a c c O d l u o w u o y f I . -
Somerset Levels and Moors: Assessment of the Impact of Water Level Management on Flood Risk
Somerset Levels and Moors: Assessment of the impact of water level management on flood risk Report to Somerset Drainage Boards Consortium Charlie Stratford and Mike Acreman Centre for Ecology and Hydrology October 2014 Acknowledgements We would like to thank the following people for their assistance in compiling this document. Name Organisation Phil Brewin Somerset Drainage Board Consortium Nick Stevens Somerset Drainage Board Consortium Iain Sturdy Somerset Drainage Board Consortium Keith Fifield Environment Agency Murray Bush Environment Agency Christopher Matthews Environment Agency Executive Summary The aim of this document is to provide the reader with a robust understanding of the processes that affect surface-water flooding in the area of the Somerset Levels and Moors. Particular attention is paid to the storage of water in the ditch network and adjacent soil body and a key output of this report is an assessment of the role of ditch management in the severity of flood events. The Somerset Levels and Moors consist of low-lying organic peat soils sitting on top of marine silts and clays, and form in effect an impermeable bowl. Rain falling on the surrounding catchments will either infiltrate and recharge the groundwater system or find its way to the network of channels that pass through the Levels and Moors before ultimately entering the Bristol Channel. The area is naturally susceptible to flooding. Extensive drainage was carried out in the 17 th and 18 th centuries with the aim of making the land more accessible and increasing its agricultural value. The drainage network is principally managed to minimise the impact of flooding, enable agricultural production and also provide conditions required for the conservation of the natural and historic environment. -
A River Valley Walk Between Source and Sea Along the Beautiful River Exe the Exe Valley Way a River Valley Walk Between Source and Sea Along the Beautiful River Exe
A river valley walk between source and sea along the beautiful River Exe The Exe Valley Way A river valley walk between source and sea along the beautiful River Exe A Guide for northbound and southbound The majority of the route follows footpaths walkers with a sketch map for each stage. and quiet country lanes where there is little traffic but there are brief stretches of busy The Exe Valley Way is a long distance route roads in Exeter and Tiverton. Care should be for walkers exploring the length of this taken at all times when walking on roads. beautiful river valley. It is almost 80km/ 50miles in length, stretching from the South Whilst this booklet does give a broad outline West Coast Path National Trail on the Exe of the waymarked route, it is emphasised Estuary to the village of Exford on the high that it would also be helpful to take an OS land of Exmoor National Park. An additional map along with you, particularly for the 12km/7.5 miles route links Exford to Exe footpath sections. Head, the source of the River Exe, high upon the moor. Most of the route follows beside OS Maps which cover the the River Exe. At the northern end of the Exe Valley Way: route, the route follows the River Barle, a Explorer No. 114 tributary of the River Exe, before rejoining Exeter & the Exe Valley (1:25 000) the Exe at Exford. Explorer OL9 Exmoor (1:25 000) The Exe Valley Way can be divided up into a series of 10 stages, most of which can be walked comfortably by most walkers in half a The Exe Valley day. -
ROYAL FOREST of EXMOOR: RESEARCH FRAMEWORK Exmoor National Park Historic Environment Report Series No 7 the ROYAL FOREST of EXMOOR: RESEARCH FRAMEWORK
Exmoor National Park Historic Environment Report Series No 7 THE ROYAL FOREST OF EXMOOR: RESEARCH FRAMEWORK Exmoor National Park Historic Environment Report Series No 7 THE ROYAL FOREST OF EXMOOR: RESEARCH FRAMEWORK Exmoor National Park Historic Environment Report Series Author: Faye Balmond Design: Pete Rae March 2012 This report series includes interim reports, policy documents and other information relating to the historic environment of Exmoor National Park. Further hard copies of this report can be obtained from the Exmoor National Park Historic Environment Record: Exmoor House, Dulverton, Somerset. TA22 9HL email [email protected], 01398 322273 FRONT COVER: Simonsbath Tower ©Exmoor National Park Authority CONTENTS Page SUMMARY . 1 INTRODUCTION, BACKGROUND AND OBJECTIVES . 1 RESEARCH FRAMEWORK . 3 THE ROYAL FOREST OF EXMOOR (ORIGINS – 1818) . 6 THE RECLAMATION OF EXMOOR FOREST (1818 – 1897) . 8 20TH CENTURY . 11 SOCIAL HISTORY AND OTHER THEMES . 11 DISSEMINATION . 12 REVIEW AND EVALUATION . 13 BILBLIOGRAPHY . 13 THE ROYAL FOREST OF EXMOOR: RESEARCH FRAMEWORK SUMMARY This document sets out the research priorities for the historic environment in the former Royal Forest of Exmoor. The priorities it lists were identified by those with an active interest in this area of Exmoor at a seminar at Ashwick in March 2012. INTRODUCTION, BACKGROUND AND OBJECTIVES A research framework for the former Royal Forest of Exmoor was proposed in an attempt to direct research and address the inability to answer with any degree of certainty some of the most basic questions related to the historical use and operation of this area of Exmoor National Park. The Exmoor Moorland Landscape Partnership Scheme (EMLPS) provided an opportunity to promote further research into the former Royal Forest of Exmoor, with funding available through the ‘Treeless Forest’ project. -
Mineral Resource Information in Support of National, Regional And
Mineral Resource Information in Support of National, Regional and Local Planning: Devon (comprising Devon, Plymouth, Torbay, Dartmoor National Park and part of Exmoor National Park) Commissioned Report CR/05/096N BRITISH GEOLOGICAL SURVEY COMMISSIONED REPORT CR/05/096N Mineral Resource Information in Support of National, Regional and Local Planning Devon (comprising Devon, Plymouth, Torbay, Dartmoor National Park and part of Exmoor National Park) A J Bloodworth, G E Norton, C J Mitchell, R C Scrivener, D G Cameron, S F Hobbs, D J Evans, G K Lott and D E Highley This report accompanies the 1:100 000 scale maps: Devon, Key words North and South (comprising Devon, Plymouth, Torbay, Mineral resources, mineral Dartmoor National Park and part of Exmoor National planning, Devon. Park) Front cover Ball Clay extraction in the Bovey Basin, Devon. Photo by David Highley © BGS NERC 2006 Bibliographical reference BLOODWORTH, A J, NORTON, G E, MITCHELL, C J, SCRIVENER, R C, CAMERON, D G, HOBBS, S F, EVANS, D J, LOTT, G K AND HIGHLEY, D E. 2006. Mineral Resource Information in Support of National, Regional and Local Planning – Devon (comprising Devon, Plymouth, Torbay, Dartmoor National Park and part of Exmoor National Park). British Geological Survey Commissioned Report, CR/05/096N. 16 pp. © Crown Copyright 2006 Keyworth, Nottingham British Geological Survey 2006 BRITISH GEOLOGICAL SURVEY The full range of Survey publications is available from the BGS Keyworth, Nottingham NG12 5GG Sales Desks at Nottingham and Edinburgh; see contact details 0115-936 3241 Fax 0115-936 3488 below or shop online at www.thebgs.co.uk e-mail: [email protected] The London Information Office maintains a reference collection www.bgs.ac.uk of BGS publications including maps for consultation.