|Elevation||1,335 ft (407 m)|
|Prominence||978 ft (298 m)|
|Parent range||Shropshire Hills|
|Topo map||OS Landranger 127|
The Wrekin // is a hill in east Shropshire, England. It is located some five miles (8 km) west of Telford, on the border between the districts of Shropshire and Telford and Wrekin. Rising to a height of 1,335 feet (407 metres) above the Shropshire Plain, it is a prominent and well-known landmark, signalling the entrance to Shropshire for travellers westbound on the M54 motorway. The Wrekin is contained within the northern panhandle of the Shropshire Hills AONB. The hill is popular with walkers and tourists and offers good views of Shropshire. It can be seen well into Staffordshire and the Black Country, and even as far as the Beetham Tower in Manchester, Winter Hill in Lancashire and Cleeve Hill in Gloucestershire.
The earliest mention of the Wrekin (pronounced locally as REE-KIN) occurs in a charter of 855, as entered in a late 11th century Worcester cartulary, spelled Wreocensetun. Its modern form is believed to have come into modern English by way of Mercian, and that is likely to have been taken from the early Celtic word Wrikon. It is presumed to be etymologically related to the Latin name for the town of Viroconium Cornoviorum - Viroconium="place of werewolves" - (modern Wroxeter; the Cornovii were the Brittonic tribe inhabiting the area), related to similar sounding names such as Wrexham (a charter of 1236 refers to this place as Wrectesham) which was also part of the northwestern edge of the Cornovii Kingdom.
The minor Anglo-Saxon kingdom of the Wreocensæte existed in the area prior to Mercian reign. For several centuries the hill was known as Mount Gilbert, a name given to it by the Normans after a hermit who lived there.
There is an Iron Age hill fort on the summit almost 8 ha (20 acres) in size, to which the name Uriconio originally referred. It is thought the fort was built by the Cornovii tribe and was once their capital.
A more recent addition is the Wrekin transmitting station, used for broadcasting and telecommunications. At the top of the main mast is a beacon which emits a red pulse of light every few seconds at night. A beacon was originally erected on the Wrekin during the Second World War to warn aircraft, and kept in operation until 1960. A new beacon was then installed in 2000, as part of a project to celebrate the new millennium. It is known locally as the "Wrekin Beacon", and is visible for many miles around.
The geology of the Wrekin and its immediate area is complex, consisting of a variety of rocks of a range of ages affected by numerous faults. The crest of the Wrekin's ridge and its northwestern slopes are formed from various rocks of volcanic origin assigned to the Uriconian series, of Precambrian age. The 'Uriconian Volcanics' include rhyolites, tuffs and agglomerates. These rocks – layers of ancient lava flows laid down in a volcanic island arc, similar to modern Japan – are approximately 680 million years old.
Dolerite dykes intruded the extrusive volcanic rocks around 563 million years ago. A variety of the intrusive igneous rock granophyre, known as Ercallite forms the northeastern shoulder of the Ercall. It was put in place around 560 million years ago and is overlain by Cambrian rocks of sedimentary origin. The southeastern side of the ridge is largely formed from sandstones and shales of Cambrian age. They include the early Cambrian Lower Comley Sandstone and Lower Comley Limestones together with the Wrekin Quartzite, outcrops of which also occur to the northwest of the ridge.
The lower ground to the northwest comprises sandstones and mudstones of late Carboniferous and Permian age whilst to the southeast are a succession of rocks of early Carboniferous age including limestone, the Little Wenlock Basalt and the Lydebrook Sandstone.
Structurally, the Wrekin together with the Ercall forms part of the Church Stretton Complex where different geological terranes meet. The Cymru Terrane is to the west with the Wrekin Terrane to the east of the fault system. The fault system trends north-northeast:south-southwest and the line carries on through other geologically important exposures such as those in the area of Caer Caradoc.
Contrary to a common misconception, the Wrekin has never been a volcano in its own right, but is composed mainly of volcanic rocks and is a product of volcanism. Its modern shape, which from certain viewpoints appears to resemble a volcano, has been formed by other natural processes.
The name the Wrekin is also used to refer more generally to the part of East Shropshire around the towns of Telford and Wellington, within sight of the hill. The surrounding area is one of the birthplaces of industry: Ironbridge Gorge is just to the south of the Wrekin hill. Woodland covers much of the hill, the area around the hill and into the Ironbridge Gorge area too. The eponymous Wrekin parliamentary constituency incorporates the hill.
The Wrekin can be accessed from the final junction on the M54 motorway (J7) before it turns into the A5 which continues to Shrewsbury. The hill is then signposted. There is a well-used footpath up the side of the hill which has an entrance at the end of the road off the M54. There is also a small car park and parking bays up the road. Between the Ercall and the Wrekin is a well positioned car park, at Forest Glen, allowing easy access to both areas. The ascent is steep in parts.
Folklore and local custom
A giant called Gwendol Wrekin ap Shenkin ap Mynyddmawr with a grudge against the town of Shrewsbury decided to flood the town and kill all its inhabitants. So he collected a giant-sized spadeful of earth and set off towards the town. When in the vicinity of Wellington he met a cobbler returning from Shrewsbury market with a large sackful of shoes for repair. The giant asked him for directions, adding that he was going to dump his spadeful of earth in the River Severn and flood the town. "It's a very long way to Shrewsbury," replied the quick-thinking shoemaker. "Look at all these shoes I've worn out walking back from there!" The giant immediately decided to abandon his enterprise and dumped the earth on the ground beside him, where it became the Wrekin. The giant also scraped the mud off his boots, which became the smaller hill Ercall Hill nearby. Ironically Shrewsbury is subjected to flooding from the River Severn on frequent occasions naturally.
"All around the Wrekin" or "Running round the Wrekin" is a phrase common in Shropshire, Worcestershire, Staffordshire, Herefordshire, the Black Country, Birmingham to mean "the long way round", in the same way that "round the houses" is used more widely. "To all friends around the Wrekin", meanwhile, is a toast traditionally used in Shropshire, especially at Christmas and New Year.
The amount of inclement weather in the area can also be said to be predicted by the visibility of the Wrekin. The saying being, "If you can see the Wrekin, it's going to rain. And if you can't see the Wrekin, it's already raining".
In 1981 an event was undertaken by local school pupils and adults called "Hands around the Wrekin", whereby a large group of people all held hands, surrounding the hill at the base.
In popular culture
On Wenlock Edge the wood's in trouble;
His forest fleece the Wrekin heaves;
The gale, it plies the saplings double,
And thick on Severn snow the leaves.
The Wrekin is also mentioned in Half Man Half Biscuit's 1987 song, "Rod Hull Is Alive, Why?", with the line: "Halfway up the Wrekin with an empty flask of tea, a fog descends and takes away my visibility..."
In Edward Lear's " A Book of Nonsense" one of the limericks starts with: There was an Old Man of the Wrekin Whose shoes made a horrible creaking
- "BBC Shropshire – The Wrekin". 13 February 2008. Retrieved 2015-04-11.
- Y Cymmrodor Volume 21, p 29,p 59 (1908)
- Delamarre, Xavier (2012). Noms de lieux celtiques de l'europe ancienne. Arles: Editions Errance. p. 273. ISBN 978-2-87772-483-8.
- Wodtko, Dagmar (2000). Wörterbuch der keltiberischen Inschriften: Monumenta Linguarum Hispanicarum, Band V.1. Reichert-Verlag. p. 452. ISBN 978-3-89500-136-9.
- Stevenson (1908). "Monograph on the Name Wrekin". All around the Wrekin. Y Cymmrodor XXI (London: Honorable Society of Cymmrodorion). pp. 58–60. – Appendix I in John Rhys' article All around the Wrekin, pp. 1–62
- "Wrekin beacon will be beaming out again soon". Shropshire Star. 17 January 2014. Retrieved 3 August 2014.
- "Wrekin Introduction". Retrieved 11 September 2010.
- Toghill, P. 2006 Geology of Shropshire 2nd edn Crowood Press
- British Geological Survey 1:50,000 scale geological map sheet 152 Shrewsbury (solid edn)
- "Shropshire – Features – Wrekin up for sale". BBC. 31 January 2005. Retrieved 24 August 2012.
- The Wrekin Giant, BBC Shropshire. Accessed 5 November 2006.
- "All Friends Round the Wrekin". 19 September 2010. Retrieved 23 August 2011.
- Computer generated summit panoramas the Wrekin index. There is an old local claim, supported by a summit toposcope, that there is a line of sight to Snowdon, but the line is blocked by Cadair Berwyn.
- Group dedicated to the Wrekin