Newsletter No. 243 June 2017
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Black Country Urban Park Barometer
3333333 Black Country Urban Park Barometer April 2013 DRAFT WORK IN PROGRESS Welcome to the Black Country Urban Park Barometer. Transformation of the Environmental Infrastructure is one of the key to drivers identified in the Black Country Strategy for Growth and Competitiveness. The full report looks at the six themes created under the ‘Urban Park’ theme and provides a spatial picture of that theme accompanied with the key assets and opportunities for that theme. Foreword to be provided by Roger Lawrence The Strategic Context Quality of the Black Country environment is one of the four primary objectives of the Black Country Vision that has driven the preparation of the Black Country Strategy for Growth and Competitiveness through the Black Country Study process. The environment is critical to the health and well-being of future residents, workers and visitors to the Black Country. It is also both a major contributor to, and measure of, wider goals for sustainable development and living as well as being significantly important to the economy of the region. The importance and the desire for transforming the Black Country environment has been reinforced through the evidence gathering and analysis of the Black Country Study process as both an aspiration in its own right and as a necessity to achieve economic prosperity. Evidence from the Economic and Housing Studies concluded that ‘the creation of new environments will be crucial for attracting investment from high value-added firms’ and similarly that ‘a high quality healthy environment is a priority for ‘knowledge workers’. The Economic Strategy puts ‘Environmental Transformation’ alongside Education & Skills as the fundamental driver to achieve Black Country economic renaissance and prosperity for its people. -
The Life & Times of Mortimer Forest
The Life & Times of Mortimer Forest Mortimer Forest Marked trails All Ability Trail - 1.6 km (1 mile) Vinnalls Loop Trail - 4.8 km (3 miles) Whitcliffe Climbing Jack Trail - 4.5 km (9 miles) Car Park Black Pool Loop Trail - 2.4 km (1.5 miles) Whitcliffe Loop Trail - 3.3 km (2 miles) Vinnalls Car Park Black Pool Car Park 1 km Foreword Woodlands are important places for butterflies and moths with 16 of Britain’s butterflies considered woodland specialists and 380 of the larger moths. Butter- flies and moths form an important part of the food chain for bats and birds, have a key role to play as pollinators and are good biodiversity indicators as they respond rapidly to changing environments. The Mortimer Forest is a significant area of woodland because of its size, the range of butterflies and moths that have been recorded, and its location in a larger wooded landscape. I first visited when I carried out survey work for fritil- lary butterflies, which are in serious decline nationally, in the early 1990s and it is somewhere I have grown to appreciate more and more on subsequent visits. While there have been occasional butterfly and moth records from Mortimer Forest since then, the Forest has never had the equivalent levels of recording of other forests of similar size, largely as a result of its rural position and the lack of a local recording group. For the past three years, Butterfly Conservation has been working in close partnership with the Forestry Commission with the aim of engaging with communities and encouraging them to become involved with the surveying of butterflies and moths and with practical conservation work. -
Proposed Black Country UNESCO Global Geopark
Great things to see and do in the Proposed Black Country UNESCO Global Geopark Black Country UNESCO Global Geopark Project The layers lying above these are grey muddy Welcome to the world-class rocks that contain seams of ironstone, fireclay heritage which is the Black and coal with lots of fossils of plants and insects. These rocks tell us of a time some 310 million Country years ago (called the Carboniferous Period, The Black Country is an amazing place with a named after the carbon in the coal) when the captivating history spanning hundreds of Black Country was covered in huge steamy millions of years. This is a geological and cultural rainforests. undiscovered treasure of the UK, located at the Sitting on top of those we find reddish sandy heart of the country. It is just 30 minutes from rocks containing ancient sand dunes and Birmingham International Airport and 10 minutes pebbly river beds. This tells us that the landscape by train from the city of Birmingham. dried out to become a scorching desolate The Black Country is where many essential desert (this happened about 250 million years aspects of the Industrial Revolution began. It ago and lasted through the Permian and Triassic was the world’s first large scale industrial time periods). landscape where anything could be made, The final chapter in the making of our landscape earning it the nick-name the ‘workshop of the is often called the’ Ice Age’. It spans the last 2.6 world’ during the Industrial Revolution. This million years of our history when vast ice sheets short guidebook introduces some of the sites scraped across the surface of the area, leaving and features that are great things to see and a landscaped sculpted by ice and carved into places to explore across many parts of The the hills and valleys we see today. -
Notes on the Geology and Fossils of the Ludlow District
NOTES ON THE GEOLOGY AND FOSSILS OF THE LUDLOW DISTRICT. By A. SMITH WOODWARD, LL.D., F.R.S., President. (A few ad,'ance coft'es issued /0 11ttlnbtr, in July, ' 901.) NDE R the presidency of a palreontologist it seems appro U priate that the Geologists ' Association should devote its Long Excursion this year to the study of fossils in the field. It becomes more and more evident, as researches progress, that the past history of life on the earth can only be satisfactorily deciphered when the exact stratigraphical position of each fossil has been determined by careful collecting. The variations of an organism in time and space, and its successive migrations, can only be ascertained by more detailed field-work and more precise labelling than has hitherto been customary among palreontolo gists. It is therefore necessary to follow the lead of Lapworth, Buckman, Rowe, Wheelton Hind, Miss Elles, Miss Wood, and others who are inaugurating a new era in the study of British fossils by a most exact and exhaustive method of collecting. The Association, indeed, cannot do better at the present time than attempt to arouse renewed interest in a classic district, which has been much neglected by geologists during recent years, and has scarcely been examined in any respect from the modern standpoint. The classic ground we have chosen to visit is the old country of the Silures, where Murchison originally worked out the details of his Silurian System. Much of it has never been visited by the Association before, and thirty-two years have now elapsed since Ludlow was the centre of one of our excursions. -
Wigmore-NDP-Submission-Doc-Final
Photo credits: Front cover - clockwise from top: St James’ Church, Wigmore– © Copyright Nick Davidson St Giles Church, Pipe Aston - © Copyright Philip Pankhurst and licensed for reuse under the Creative Commons Licence. St Mary’s Church Elton - © Copyright Ian Capper and licensed for reuse under the Creative Commons Licence. St Mary Magdalene, Leinthall Starkes - © Copyright Philip Pankhurst and licensed for reuse under the Creative Commons Licence. Back cover: © Copyright Nick Davidson Contents 1. Introduction and Background 4 2. How is the Neighbourhood Plan prepared? 6 3. Wigmore Group Past and Present 8 3.1 History oF the Wigmore Group 8 3.2 Wigmore Group today 11 4. Key issues For the Wigmore Group Neighbourhood Plan 16 5. Aims, Vision and Objectives oF the Wigmore Group Neighbourhood Plan 19 6. Policies and Proposals 21 6.1 Natural Environment 21 6.2 Housing 26 6.3 Community Facilities 31 6.4 Design and Heritage 33 6.5 Local employment 36 Appendix A. National and Local Policies 39 Appendix B. Statutory Listed Buildings 42 Appendix C. Potential uses oF Community Infrastructure Levy in the 48 Wigmore Group Parishes 1. Introduction and Background 1.1 Welcome to the Wigmore Group Neighbourhood Development Plan (WGNDP). Neighbourhood Development Plans are a new part of the statutory development planning system. Just as local authorities such as Herefordshire Council can produce development plans to promote, guide and control development of houses, businesses, open spaces, so too, now, can parish councils, by preparing a Neighbourhood Development Plan. 1.2 The significance of this is that when the Neighbourhood Development Plan is “made” it will become part of the development plan for the area. -
Application Dossier for the Proposed Black Country Global Geopark
Application Dossier For the Proposed Black Country Global Geopark Page 7 Application Dossier For the Proposed Black Country Global Geopark A5 Application contact person The application contact person is Graham Worton. He can be contacted at the address given below. Dudley Museum and Art Gallery Telephone ; 0044 (0) 1384 815575 St James Road Fax; 0044 (0) 1384 815576 Dudley West Midlands Email; [email protected] England DY1 1HP Web Presence http://www.dudley.gov.uk/see-and-do/museums/dudley-museum-art-gallery/ http://www.blackcountrygeopark.org.uk/ and http://geologymatters.org.uk/ B. Geological Heritage B1 General geological description of the proposed Geopark The Black Country is situated in the centre of England adjacent to the city of Birmingham in the West Midlands (Figure. 1 page 2) .The current proposed geopark headquarters is Dudley Museum and Art Gallery which has the office of the geopark coordinator and hosts spectacular geological collections of local fossils. The geological galleries were opened by Charles Lapworth (founder of the Ordovician System) in 1912 and the museum carries out annual programmes of geological activities, exhibitions and events (see accompanying supporting information disc for additional detail). The museum now hosts a Black Country Geopark Project information point where the latest information about activities in the geopark area and information to support a visit to the geopark can be found. Figure. 7 A view across Stone Street Square Dudley to the Geopark Headquarters at Dudley Museum and Art Gallery For its size, the Black Country has some of the most diverse geology anywhere in the world. -
A Geological Trail in Front of the Last Glacier in South Shropshire By
A Geological Trail in front of the last glacier in South Shropshire By Michael Rosenbaum Figure 1. General view looking north from Mortimer Forest towards Onibury (centre top), across the sandur (fluvioglacial outwash plain) created by the melting of glaciers that came from Wales, eastwards over Clun Forest. One glacial lobe is believed to have come eastwards through the col by Downton Castle (to the left of the above view) and perhaps terminated in the centre of the field of view. Another lobe reached Craven Arms and perhaps then turned southwards towards Onibury (in the centre distance). This landscape has also been modified by erosion as the River Teme, diverted eastwards from Aymestry by a major glacier coming from the Wye Valley to the south, rejuvenated erosion and transportation of weathered material from the Silurian mudstones that underlie the lower ground in the field of view. These alluvial processes were significantly assisted by periglacial weathering, especially solifluction, leaving behind an intricate pattern of small curved steep-sided valleys. A guide prepared on behalf of the Shropshire Geological Society 2007 Published by The Shropshire Geological Society Figure 2. Map of sites described in this Guide, showing distribution of Superficial Deposits and locality numbers (based on Cross, 1971). The Guide follows public roads and footpaths. The use of INTRODUCTION a large scale Ordnance Survey map is strongly Glaciations have taken place a number of times during recommended, such as the Explorer Series Sheet 203 the past 2–2.5 million years. The last to affect the Welsh (1:25,000 scale). Ordnance Survey grid references are Marches was 120,000 to 11,000 yrs BP, called the included to assist location. -
Welcome to Orleton
New to Orleton? A Free Guide to Local Organisations, Services and Facilities produced by Orleton Parish Council (THIS INFORMATION PACK WAS UPDATED ON 15/9/2019) WELCOME TO ORLETON This information pack has been prepared by your Parish Council to help you settle into the village and give you some information on the services and facilities locally available. Orleton Village The village of Orleton is located midway between the historic market towns of Ludlow and Leominster, both some 5 miles away and is surrounded by beautiful Herefordshire countryside with a pretty brook meandering through. About Orleton Village The lovely 13th Century, Norman, St George’s Church is situated at one end of the village and the churchyard provides a tranquil oasis from which to view the beautiful surrounding countryside. It is a thriving, vibrant community with a Shop/Post Office, a Primary School, a Golf Society, two pubs, a Doctor’s Surgery and a very well equipped Village Hall which is home to a variety of clubs and societies, OGGLE (an amateur dramatic group), Evergreens (for older residents of the village), Table Tennis Club, Gardening Club and many more. There is a children’s playground beside the Village Hall making it an excellent venue for children’s parties. The village has excellent public transport links, via the 490 bus to Ludlow, Leominster and Hereford (subsidised by Orleton Parish Council) and is close to the Mortimer Trail, which runs through nearby Mortimer Forest, attracting walkers and cyclists to the area. Tourists are catered for with a number of bed & breakfasts, self catering holiday cottages and caravan parks situated within and around the village. -
Things to See and Do
over the river, where every With its mix of Medieval, and landscape of the area the church. Further afield, spring The Green Man must Georgian and Victorian where you can Meet the but which also make a great t defeat the Frost Queen for architecture, Much Wenlock Mammoth – a full size day out is the Severn Valley there to be summer in the is a must on your ‘to do’ list. replica of the skeleton Railway at Bridgnorth, Clun Valley. This annual Walk along the High Street found at Condover. The The Judge’s Lodgings’ at Church Stretton, nestled in the Shropshire Hills celebration in May is the to browse the galleries, book exhibition also includes Presteigne, Powys Castle, high point of the town’s and antique shops. Visit a film panorama with home of the Earl of Powys, of independent retailers, whether on foot, by bike or famous Green Man Festival, the museum in the Market spectacular views of the near Welshpool, the offering a top-quality even aiming for the sky; the which also includes The Square to discover the Shropshire Hills. After that, fascinating museums of the Michaelmas fair, Bishops Castle shopping experience along Long Mynd enjoys some of Clun Mummers doing battle town’s heritage and links to explore the centre’s 30-acre Ironbridge Gorge and of with a tempting selection of the best thermals in Europe, For 800 years Welsh drovers heritage displays and Visitor in the Square, as well as the modern Olympic Games. Onny Meadows site, which course, the County town of Carding Mill Valley and the Long Mynd Green Man Festival, Clun butchers, bakers, historic so is unrivalled for gliding, brought livestock along the Information Centre. -
Fforest Fawr Geopark James Cresswell (UK)
Fforest Fawr Geopark James Cresswell (UK) Fig. 1. A geological map of the Fforest Fawr Geopark. Copyright the British Geological Society. n 2005, Fforest Fawr Geopark and outcrop in the extreme western resolved the dispute by defining the became the first geopark to be portion of the geopark, between the Ordovician. He recognised that the Iestablished in Wales. As of October towns of Llandeilo and Llandovery fossil fauna in the disputed layers 2013, it was one of 58 geoparks in (Fig. 1). The names of these towns was different from both the Cambrian Europe. The park has been sculpted by may sound familiar to those who and the Silurian. Lapworth divided nearly 500myrs of geological history know something about stratigraphy, up his Ordovician, which is named and contains the highest mountains because they have been used to name after the Ordovices tribe who lived in in southern Britain, the deepest cave stages within the Ordovician and North Wales and mid Wales during in Britain, the finest collection of Silurian periods. In fact, Wales as a Roman times, into the following waterfalls in Britain and 7,000 years whole has played a very major role series: Tremadog, Arenig, Llanvirn, of recorded human occupation. in the naming of geological periods, Caradog and Ashgill, all named after The geopark lies wholly within the with the earliest three periods places in Wales or near the border, Brecon Beacons National Park, since multicellular life began - the where rocks of these ages occur. occupying the central and western Cambrian, the Ordovician and the The Llanvirn is subdivided into the part of the park. -
The Black Country Geological Society
THE BLACK COUNTRY GEOLOGICAL SOCIETY CHAIRMAN CHAIRMAN A. CUTLER, B.Sc. VICE CHAIRMAN P. G. OLIVER, B.Sc., Ph.D., F.G.S. HON. SECRETARY D. J. WRAIGHT HON. TREASURER Mrs. E. BAKEWELL — EW Sl-E" i ,I a S P T EI E 7 Editorial Film Night - Thursday 2.st ApKi1 It is becoming increasingly obvious that] After a late start due to a technical in order for Members to gain maximum hitch. The twenty or so members (includ- benefit from the Society's activities i a ing some new prospective members) were permanent headquarters is required. The able to enjoy two very informative colour availability of Dudley Library is films on Hawaiian Volcanoes, brought along extremely important but there are limit by Doug Bedson. 4tions when it comes the analysis and toning of samples etc, The Society has The particular volcano studied was Kilauea, been offered facilities at Aston a large shield volcano situated on the University, for meetings and it is eastern side of Hawaii, and the film important that this offer is accepted. dipicted the eruption of Kilauea 1KI one A permanent centre in the Black Country of its many vents. The gradual uplift of where a store is available, where a book its lava lake came to a peak on November and map library can be developed and where ll+th 1959 when lava fountains burst Members can Meet at all times is, however, through fissures on the S.W• slopes. essential. The Society now looks to its These incandescent fountains lasted for Members to make all possible enquiries just under five weeks reaching a maximum with the above aims in mind. -
Late Silurian Trilobite Palaeobiology And
LATE SILURIAN TRILOBITE PALAEOBIOLOGY AND BIODIVERSITY by ANDREW JAMES STOREY A thesis submitted to the University of Birmingham for the degree of DOCTOR OF PHILOSOPHY School of Geography, Earth and Environmental Sciences University of Birmingham February 2012 University of Birmingham Research Archive e-theses repository This unpublished thesis/dissertation is copyright of the author and/or third parties. The intellectual property rights of the author or third parties in respect of this work are as defined by The Copyright Designs and Patents Act 1988 or as modified by any successor legislation. Any use made of information contained in this thesis/dissertation must be in accordance with that legislation and must be properly acknowledged. Further distribution or reproduction in any format is prohibited without the permission of the copyright holder. ABSTRACT Trilobites from the Ludlow and Přídolí of England and Wales are described. A total of 15 families; 36 genera and 53 species are documented herein, including a new genus and seventeen new species; fourteen of which remain under open nomenclature. Most of the trilobites in the British late Silurian are restricted to the shelf, and predominantly occur in the Elton, Bringewood, Leintwardine, and Whitcliffe groups of Wales and the Welsh Borderland. The Elton to Whitcliffe groups represent a shallowing upwards sequence overall; each is characterised by a distinct lithofacies and fauna. The trilobites and brachiopods of the Coldwell Formation of the Lake District Basin are documented, and are comparable with faunas in the Swedish Colonus Shale and the Mottled Mudstones of North Wales. Ludlow trilobite associations, containing commonly co-occurring trilobite taxa, are defined for each palaeoenvironment.