The Wrekin Forest Plan 2015-2020
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How to Find Us
HOW TO FIND US Newport Whitchurch A442 A442 Stafford (A518) Q UEEN SWAY Princess A Royal The Old Hall AD 522 Hospital RO 3 N W IO HITCH School AT URCH ST DRIVE BRJ School Stanley Road W Wellington E UE LL VEN IN EY A Telford G APL TO N AD Shropshire R O O R A H TF1 3LB D T A W VE R RI 5 D H 2 O APLEY 2 N I Telephone: 01952 223117 T 3 C A H Facsimile: 01952 222674 D U M R ERY RD D A LEEGOM A S C S Email: [email protected] T H O U S O D T T DA Shed N OR R H A TR N R Web: www.oldhall.co.uk R NT O City Y E N O E R L N A L A EC E D A D S Y C ROSL N E S D R WREKIN COLLEGE R E D A A C R L RD B V W C T E E Sports H ER R I AD LB T Hall TC VINEYARD RO A H R D U OAD D . R R DINE R TH C R SU S WellingtonH WA T CK D RO L A W IL R H N I N. V B O L Shropshire C E R L E I L Wrekin Y D I D H R G . N College D TF1 3BH E O OA W S K C A R TE T IN RLO R A O I G E RD R E S T T O R T E T: 01952 265600 C E I T V F : 01952 415068 VICTORIA RD G Telford LE REET BE ST M White House Hotel T.C.A.T. -
Proceedings of the Open University Geological Society
0 OUGS Proceedings 5 2019_OUGSJ 26/02/2019 11:45 Page i Proceedings of the Open University Geological Society Volume 5 2019 Including articles from the AGM 2018 Geoff Brown Memorial Lecture, the ‘Music of the Earth’ Symposium 2018 lectures (Worcester University), OUGS Members’ field trip reports, the Annual Report for 2018, and the 2018 Moyra Eldridge Photographic Competition Winning and Highly Commended photographs Edited and designed by: Dr David M. Jones 41 Blackburn Way, Godalming, Surrey GU7 1JY e-mail: [email protected] The Open University Geological Society (OUGS) and its Proceedings Editor accept no responsibility for breach of copyright. Copyright for the work remains with the authors, but copyright for the published articles is that of the OUGS. ISSN 2058-5209 © Copyright reserved Proceedings of the OUGS 5 2019; published 2019; printed by Hobbs the Printers Ltd, Totton, Hampshire 0 OUGS Proceedings 5 2019_OUGSJ 26/02/2019 11:46 Page 35 The complex tectonic evolution of the Malvern region: crustal accretion followed by multiple extensional and compressional reactivation Tim Pharaoh British Geological Survey, Keyworth, Nottingham, NG12 5GG ([email protected]) Abstract The Malvern Hills include some of the oldest rocks in southern Britain, dated by U-Pb zircon analysis to c. 680Ma. They reflect calc- alkaline arc magmatic activity along a margin of the Rodinia palaeocontinent, hints of which are provided by inherited zircon grains as old as 1600Ma. Metamorphic recrystallisation under upper greenschist/amphibolite facies conditions occurred from c. 650–600Ma. Subsequently, rifting of the magmatic arc (c.f. the modern western Pacific) at c. 565Ma led to the formation of a small oceanic mar- ginal basin, evidenced by basaltic pillow lavas and tuffs of the Warren House Formation, and Kempsey Formation equivalents beneath the Worcester Graben. -
PROGRAMME: July – October 2018
PROGRAMME: July – October 2018 MEETING POINTS Sunday Abbey Foregate car park (opposite The Abbey). 9.30 am. unless otherwise stated in programme. Tuesday Car park behind Harvester Beaten Track PH, Old Potts Way. 9.30 am. unless otherwise stated in programme. Thursday Car park behind Harvester Beaten Track PH, Old Potts Way. 9.30 am. unless otherwise stated in programme. Saturday As per programme. Sun 1 Jul Darren Hall (07837 021138) 7 miles Moderate+ Rectory Wood, up Town Brook Valley to Pole Bank, along the top of the Long Mynd to Pole Cottage, before returning via Ashes Hollow to Church Stretton. Tea afterwards at Berry's or Jemima's Tearooms. Walk leader will meet walkers at Easthope car park at 10:00. Meet 09:30 Abbey Foregate. Voluntary transport contribution £2 Tue 3 Jul John Law (01743 363895) 9 miles Moderate+ Cleobury Mortimer, Mamble & Bayton. Rural paths and tracks Meet 09:00 Harvester Car Park. Voluntary transport contribution £4 Wed 4 Jul Peter Knight (01743 246609) 4 miles Easy Meole Brace along the Reabrook and Shrewsbury School overlooking the Quarry. Start 19:00 Co-op Stores Radbrook (SJ476112). Thu 5 Jul Ken Ashbee (07972 012475) 6 miles Easy Powis Castle, once a medieval fortress. Track and field paths, lovely views. This is a NT property so bring your card if you are a member Meet 09:30 Harvester Car Park. Voluntary transport contribution £3 Sat 7 Jul Phil Barnes (07983 459531) 7 miles Moderate Leebotwood to Pulverbatch Bus Ramble via Picklescote taking in two motte and baileys and a, hard to find, church. -
Welcome to the Telford T50 50 Mile Trail
WELCOME TO THE TELFORD T50 50 MILE TRAIL This new 50 mile circular walking route was created in 2018 to celebrate Telford’s 50th anniversary as a New Town. It uses existing footpaths, tracks and quiet roads to form one continuous trail through the many different communities, beautiful green spaces and heritage sites that make Telford special. The Telford T50 50 Mile Trail showcases many local parks, nature reserves, woods, A 50 MILE TRAIL FOR EVERYONE TO ENJOY pools and open spaces. It features our history and rich industrial heritage. We expect people will want to explore this Fifty years ago, Telford’s Development Plan wonderful new route by starting from the set out to preserve a precious legacy of green space closest to where they live. green networks and heritage sites and allow old industrial areas to be reclaimed by wild The route is waymarked throughout with nature. This walk celebrates that vision of a magenta 'Telford 50th Anniversary' logo. interesting and very special places left for everyone to enjoy. The Trail was developed The Trail begins in Telford Town Park, goes by volunteers from Wellington Walkers are down to Coalport and Ironbridge then on Welcome, the Long Distance Walkers through Little Wenlock to The Wrekin, that Association, Walking for Health Telford & marvellous Shropshire landmark. It then Wrekin, Ironbridge Gorge Walking Festival continues over The Ercall nature reserve and Telford & East Shropshire Ramblers. through Wellington, Horsehay and Oakengates to Lilleshall, where you can www.telfordt5050miletrail.org.uk walk to Newport via The Hutchison Way. After Lilleshall it goes through more areas of important industrial heritage, Granville Country Park and back to The Town Centre. -
A Very Rough Guide to the Main DNA Sources of the Counties of The
A Very Rough Guide To the Main DNA Sources of the Counties of the British Isles (NB This only includes the major contributors - others will have had more limited input) TIMELINE (AD) ? - 43 43 - c410 c410 - 878 c878 - 1066 1066 -> c1086 1169 1283 -> c1289 1290 (limited) (limited) Normans (limited) Region Pre 1974 County Ancient Britons Romans Angles / Saxon / Jutes Norwegians Danes conq Engl inv Irel conq Wales Isle of Man ENGLAND Cornwall Dumnonii Saxon Norman Devon Dumnonii Saxon Norman Dorset Durotriges Saxon Norman Somerset Durotriges (S), Belgae (N) Saxon Norman South West South Wiltshire Belgae (S&W), Atrebates (N&E) Saxon Norman Gloucestershire Dobunni Saxon Norman Middlesex Catuvellauni Saxon Danes Norman Berkshire Atrebates Saxon Norman Hampshire Belgae (S), Atrebates (N) Saxon Norman Surrey Regnenses Saxon Norman Sussex Regnenses Saxon Norman Kent Canti Jute then Saxon Norman South East South Oxfordshire Dobunni (W), Catuvellauni (E) Angle Norman Buckinghamshire Catuvellauni Angle Danes Norman Bedfordshire Catuvellauni Angle Danes Norman Hertfordshire Catuvellauni Angle Danes Norman Essex Trinovantes Saxon Danes Norman Suffolk Trinovantes (S & mid), Iceni (N) Angle Danes Norman Norfolk Iceni Angle Danes Norman East Anglia East Cambridgeshire Catuvellauni Angle Danes Norman Huntingdonshire Catuvellauni Angle Danes Norman Northamptonshire Catuvellauni (S), Coritani (N) Angle Danes Norman Warwickshire Coritani (E), Cornovii (W) Angle Norman Worcestershire Dobunni (S), Cornovii (N) Angle Norman Herefordshire Dobunni (S), Cornovii -
Middlewich Before the Romans
MIDDLEWICH BEFORE THE ROMANS During the last few Centuries BC, the Middlewich area was within the northern territories of the Cornovii. The Cornovii were a Celtic tribe and their territories were extensive: they included Cheshire and Shropshire, the easternmost fringes of Flintshire and Denbighshire and parts of Staffordshire and Worcestershire. They were surrounded by the territories of other similar tribal peoples: to the North was the great tribal federation of the Brigantes, the Deceangli in North Wales, the Ordovices in Gwynedd, the Corieltauvi in Warwickshire and Leicestershire and the Dobunni to the South. We think of them as a single tribe but it is probable that they were under the control of a paramount Chieftain, who may have resided in or near the great hill‐fort of the Wrekin, near Shrewsbury. The minor Clans would have been dominated by a number of minor Chieftains in a loosely‐knit federation. There is evidence for Late Iron Age, pre‐Roman, occupation at Middlewich. This consists of traces of round‐ houses in the King Street area, occasional finds of such things as sword scabbard‐fittings, earthenware salt‐ containers and coins. Taken together with the paleo‐environmental data, which hint strongly at forest‐clearance and agriculture, it is possible to use this evidence to create a picture of Middlewich in the last hundred years or so before the Romans arrived. We may surmise that two things gave the locality importance; the salt brine‐springs and the crossing‐points on the Dane and Croco rivers. The brine was exploited in the general area of King Street, and some of this important commodity was traded far a‐field. -
HISTORY of WORFIELD – the EARLIEST SETTLEMENT. Worfield's History Does Not Begin, As Far As We Can Tell, in Worfield Village I
HISTORY OF WORFIELD – THE EARLIEST SETTLEMENT. Worfield's history does not begin, as far as we can tell, in Worfield village itself. The earliest evidence for settlement in the Parish is at Chesterton. Today Chesterton is a hamlet but to the South of the village is an iron age hill fort of just over 20 acres. There are two ways of accessing the site, either from Chesterton or from Littlegain. From Chesterton walk towards the B4176 until you reach the last house on your left and just beyond that is a public footpath leading to The Walls. From Littlegain leave your car on the grass verge at the top of the lane and walk down the lane, crossing the Stratford Brook. Look carefully and you will find the path leading to the Walls. There are pros and cons of both approaches. The Littlegain approach can be very muddy and there is a very steep ascent to The Walls but to approach from this direction gives you a good impression of the valley and the steps you take from the valley are thought to date from the iron age period. If you do visit please note that metal detecting and digging are, of course, forbidden. Approaching from either direction you will be using one of the original entrances. As you follow the footpath round you will see earthworks – what an achievement to dig these with the most primitive of tools. Erosion and ploughing have levelled the embankment and ditch on the north side but on the east side the ramparts are very impressive. -
Rb-Sr Whole-Rock Isochron Ages of Late Precambrian to Cambrian Igneous Rocks from Southern Britain
J. geol. SOC. London, Vol. 137, 1980, pp. 649656, 6 figs., 1 table. Printed in Northern Ireland. Rb-Sr whole-rock isochron ages of late Precambrian to Cambrian igneous rocks from southern Britain P. J. Patchett, N. H. Gale, R. Goodwin & M. J. Hum SUMMARY:Rb-Sr age data are reported for late Precambrian to Cambrianigneous and metamorphic rocks from the border region of England and Wales. A felsic intrusion from Stanner Hill defines a good whole-rock isochron of 702 f 8 Ma. Uriconian pyroclastic rocks from the Wrekin area give a whole-rock age of 558* 16 Ma, while the late- or post-Uriconian Ercall granophyre from the same area gives a good whole-rock isochron of 533 f 13 Ma. A biotite cooling age from the nearby pre-volcanic Rushton Schist is consistent with these dates and suggests that the region cooled after the close of Uriconian magmatism at 536*8 Ma. All these results relate to widespread igneous/metamorphic activityin latest Precambrian to Lower Cambrian time. The Ercall granophyre and Rushton schist are directly overlain by Lower Cambrian sedi- ments and 533* 13 Ma is thus a maximum age for the deposition of these rocks. Rocks underlying themarine Cambrian deposits of rocks comprising the‘Stanner-Hanter complex’, de- southernBritain are exposed ina series of isolated scribed in detail by Holgate & Hallowes (1941). They inliers. Early Rb-Sr mineral and K-Ar dating of these distinguisheda series of intrusiveevents beginning rocks (Moorbath & Shackleton 1966; Lambert & Rex withfine dolerite, followed successively by gabbro, 1966; Fitch et al. 1969)suggested that almostall felsic intrusions and veins, and finally some rare later regions underwent a major thermal event650-600 Ma dolerite dykes. -
WELLINGTON and the WREKIN, Wellington to the Wrekin, One of the Midlands Most Famous Natural SHROPSHIRE Landmarks
An 8 mile circular walk connecting the historic east Shropshire market town of WELLINGTON AND THE WREKIN, Wellington to The Wrekin, one of the Midlands most famous natural SHROPSHIRE landmarks. The journey begins in the centre of medieval Wellington and explores The Ercall (the most northerly of the five hills of the Wrekin range) before following the main track to the summit of its iconic 1334-foot sibling. The trail Strenuous Terrain leaves Wellington following the orange-coloured Buzzard signs indicating the new main route of the long-distance Shropshire Way footpath, which continue all the way to summit of The Wrekin. Returning, the route detours through the town’s Bowring Park and historic Market Square before arriving back at the railway station. 8 miles ADVICE: The heathland atop The Wrekin is a precious landscape that can be easily damaged. Please do not Circular trample on the heather and bilberry and keep dogs on their leads during spring and early summer, when many ground-nesting birds are present. Similarly, the hillfort is 4 hours a Scheduled Ancient Monument (SAM) and visitors are encouraged not to walk on its ramparts. FACILITIES: The walk starts at Wellington rail station, 050419 where tourist information and maps of footpaths in the wider area are available. A cafe is situated on Platform Two and public toilets can be accessed with a key during booking office opening hours. Pay toilets are also located at the adjacent bus station, while free facilities can be found at Wellington Civic Centre in Larkin Way. The route also passes the Red Lion pub on Holyhead Road, while Wellington town centre is home to many catering establishments. -
19A Bus Time Schedule & Line Route
19A bus time schedule & line map 19A Telford - Madeley - Ironbridge - Shrewsbury View In Website Mode The 19A bus line (Telford - Madeley - Ironbridge - Shrewsbury) has 2 routes. For regular weekdays, their operation hours are: (1) Shrewsbury: 7:23 AM (2) Telford Town Centre: 5:45 PM Use the Moovit App to ƒnd the closest 19A bus station near you and ƒnd out when is the next 19A bus arriving. Direction: Shrewsbury 19A bus Time Schedule 32 stops Shrewsbury Route Timetable: VIEW LINE SCHEDULE Sunday Not Operational Monday 7:23 AM Bus Station, Telford Town Centre Coach Central, Telford Tuesday 7:23 AM International Centre, Telford Town Centre Wednesday 7:23 AM St Quentin Gate, Telford Thursday 7:23 AM Miners Arms, Madeley Friday 7:23 AM Station Road, Madeley Saturday 7:23 AM 39 High Street, Madeley Civil Parish Madeley Centre, Madeley Court Street, Madeley Civil Parish 19A bus Info Abraham Darby School, Woodside Direction: Shrewsbury Stops: 32 Belmont Road, Ironbridge Trip Duration: 77 min Madeley Road, The Gorge Civil Parish Line Summary: Bus Station, Telford Town Centre, International Centre, Telford Town Centre, Miners The Square, Ironbridge Arms, Madeley, Station Road, Madeley, Madeley 13 Tontine Hill, The Gorge Civil Parish Centre, Madeley, Abraham Darby School, Woodside, Belmont Road, Ironbridge, The Square, Ironbridge, Museum Of the Gorge Car Park, Ironbridge Museum Of the Gorge Car Park, Ironbridge, Junction, Buildwas, Kynnersley Lane Jct, Leighton, Kynnersley Junction, Buildwas Arms, Leighton, Garmston Lane Jct, Garmston, Rural Cottages, Upper Longwood, Baxters Farm, Kynnersley Lane Jct, Leighton Eaton Constantine, Crossroads, Lower Longwood, Roman Town, Wroxeter, Mytton & Mermaid Hotel, Kynnersley Arms, Leighton Atcham, Knightsbridge Close Jct, London Road, New College Road Jct, London Road, College, London Garmston Lane Jct, Garmston Road, Armoury Gardens, London Road, Shirehall, Abbey Foregate, The Bell Ph, Abbey Foregate, Newhall Gardens Jct, Abbey Foregate, The Dun Cow, Rural Cottages, Upper Longwood Abbey Foregate, Abbey Church, Abbey Foregate, St. -
Electoral Changes) Order 2009 Sheet 1 of 6
SHEET 1, MAP 1 MAP REFERRED TO IN THE COUNTY OF SHROPSHIRE (ELECTORAL CHANGES) ORDER 2009 SHEET 1 OF 6 This map is based upon Ordnance Survey material with the permission of Ordnance Survey on behalf of the Controller of Her Majesty's Stationery Office © Crown copyright. Unauthorised reproduction infringes Crown copyright and may lead to prosecution or civil proceedings. The Electoral Commission GD03114G 2009. Scale : 1cm = 0.8585 km Grid interval 5km WHITCHURCH URBAN NORTH PARISH WARD WHITCHURCH URBAN SOUTH PARISH WARD H ORT CH N HUR HITC WHITCHURCH WOORE CP W URBAN CP H RC U T CH ES IT W D WH N R BA WA SEE SHEET 6, UR H RIS PA MAP 6 WHITCHURCH SOUTH MARKET WHITCHURCH RURAL CP DRAYTON DUDLESTON DUDLESTON ADDERLEY PARISH WARD EAST HEATH CP NORTON IN PARISH WARD IGHTFIELD CP ST MARTIN'S HALES CP ST MARTIN'S ELLESMERE URBAN E CP L L E WESTON RHYN CP S M E PREES R ELLESMERE E R URBAN U WELSHAMPTON MORETON SAY R CP WHIXALL CP A AND LYNEAL CP CP L C N P TO AY MARKET DR ET WELSH FRANKTON DRAYTON RK CP MA PARISH WARD PREES CP WEST SELATTYNSELATTYN AND AND GOBOWEN GOBOWEN CP TETCHILL PARISH WARD SEE SHEET 2, MAP 2B THE MERES OSWESTRY WEST SUTTON UPON TERN CP WHITTINGTON CP WEMWEM RURAL CP OSWESTRY EAST OSWESTRY COCKSHUTT CP CP WEM CHESWARDINE WHITTINGTON URBAN WESTON- CP HORDLEY CP UNDER- CP LOPPINGTON CP REDCASTLE STOKE UPON TERN CP CP CHESWARDINE HODNET CP SEE SHEET 2, MAP 2A HINSTOCK CP OSWESTRY RURALOSWESTRY CP SOUTH PETTON HODNET WEST FELTON CP CP MORETON CORBET ST OSWALD AND LEE BROCKHURST CP CLIVE CP MYDDLE AND BROUGHTON STANTON UPON HINE -
A Review of the Tectonic History of the Shropshire Area
ISSN 1750-855X (Print) ISSN 1750-8568 (Online) A review of the tectonic history of the Shropshire area 1 James Butler BUTLER, J.B. (1990). A review of the tectonic history of the Shropshire area. Proceedings of the Shropshire Geological Society , 9, 20–34. A review of the tectonic data available for Shropshire, relating this to information which has become available from the exploration of the north-west continental shelf. The tectonic history of Shropshire records short bursts of compression producing folding and wrench faulting as a result of continental collision, followed by longer periods of tension, deposition and reversal of movement along the wrench fault system. The County lies upon the Midland Block, comprising Longmyndian and Charnian rock to which was accreted Island Arc volcanics and related sediments along the line of the Pontesford Lineament in the late Precambrian. The so-called "Caledonian grain" was determined at this time and was reactivated many times subsequently. Sediments were folded during the Taconic pulse in mid-Ordovician, and then continental collision along the Iapetus suture in mid-Devonian intensified the Caledonian grain. At the end of the Devonian, collision occurred to the south of the Midland Block. Pulses during the Carboniferous produced the Hercynian basins and welded the continents into one super-continent: Pangea. Break-up of Pangea was followed by a taphrogenic regime with rifting (Cimmerian) in the Permo-Triassic and early Cretaceous. Compressive forces operated at the end of the Cretaceous with reactivation of old wrench faults. Finally, Styrian compression inverted the Weald-type basins and most likely elevated the Welsh Massif at the same time, some 10 million years ago.