Little Wenlock

Buildwas is a village and civil parish in Shropshire, England, on the north bank of the River Severn at grid reference SJ641045. It lies on the B4380 road between Atcham and Ironbridge. The Royal Mail postcodes begin TF6 and TF8. Buildwas Primary Academy is situated on the Buildwas bank road. The school has been running since 1855, and has three classes and a nursery. Buildwas previously had a nine-hole golf course which ran between the River Severn and the site of Ironbridge Power Station. It was open to members of Buildwas Abbey Club.

Buildwas Abbey was a Cistercian (originally Savigniac) monastery located on the banks of the River Severn, at Buildwas in Shropshire, England - today about 2 miles (3.2 km) west of Ironbridge. Founded by the local bishop in 1135, it was sparsely endowed at the outset but enjoyed several periods of growth and increasing wealth: notably under Abbot Ranulf in the second half of the 12th century and again from the mid-13th century, when large numbers of acquisitions were made from the local landed gentry. Abbots were regularly used as agents by Plantagenet in their attempts to subdue Ireland and Wales and the abbey acquired a daughter house in each country. It was a centre of learning, with a substantial library, and was noted for its discipline until the economic and demographic crises of the 14th century brought about decline and difficulties, exacerbated by conflict and political instability in the Welsh Marches. The abbey was suppressed in 1536 as part of the Dissolution of the Monasteries under Henry VIII. Substantial remains of the abbey church and monks' quarters remain and are in the care of English Heritage.

Uriconian rocks are volcanic rocks found in parts of Shropshire, United Kingdom. The name relates to Uriconio, the Latin name for an Iron Age hillfort on the summit of the Wrekin, a hill formed of Uriconian rock. The Uriconian rocks of Shropshire (Wrekin Terrane) are thought to be potentially related to the Longmyndian Supergroup of the Stretton Hills, Shropshire, United Kingdom. Current geological profiling of the terranes suggests that the Uriconian rocks are of Precambrian age (Neoproterozoic Phases 2 and 3). The Uriconian Rocks outcrop to the southeast of the Long Mynd area of the Welsh Borderland Fault System and beyond the Church Stretton Fault which trends northeast-southwest across the area. The Stretton Hills are composed primarily of arenaceous (quartz rich sand) beds assigned to the Longmyndian Supergroup. The Longmyndian rocks are a c.6 km thick group of volcaniclastic and bentonitic sediment horizons. The Uriconian have long thought to be older than the Longmyndian and generally outcrop to the southeast of the latter within northeast-southwest trending lineaments suggesting basement influence for the regional structure.The Uriconian rocks outcrop in areas from Wellington, Shropshire to Primrose Hill on the southwest side of The Wrekin, east of Caer Caradoc and in the Craven Arms Inlier. Primarily the strata exist as fault-bounded slices within splays of, and to the southeast of, the main Church Stretton fault system. The Uriconian rocks comprise both intermediate to acidic and basic (bimodal) volcanic suites that reflect largely intraplate origins for the complex although some subduction signatures have been identified. Further work has led to suggest that the locality of this kind of volcanism is related to marginal basin volcanicity (behind the main arc) influenced by trans-tension brought about by oblique subduction.The Neoproterozoic sediments were deposited on Avalonia in various strike-slip faulted basins and they comprise predominantly volcaniclastic and siliciclastic sediments.

Buildwas railway station was an isolated junction railway station on the Wellington to Craven Arms Railway and Severn Valley Railway. Opened on 1 February 1862. Although the station served both the Severn Valley Railway and Wellington to Craven Arms Railway, it was an interchange station in open countryside with no passenger access except by rail.The station had three platforms, with two platforms at a lower level serving the Severn Valley Railway and one at a higher level serving the Wellington to Craven Arms Railway. At its peak, the station had a total of eleven staff, including the station master. Up to 1923 the area was controlled by two signal boxes, the Station signal box controlling the station area and the Junction signal box controlling the junction between the Severn Valley line and the double track line across the Albert Edward Bridge towards Lightmoor Junction. These were replaced with a single signal box approximately midway between its predecessors in 1923. This box was subsequently enlarged to accommodate a frame containing 113 levers on 9 December 1931. The track layout was altered several times during its existence including the additional CEGB sidings opened in 1932.The planned closure of the northern end of the Severn Valley Line including Buildwas station pre-dated the Beeching report. Following closure, the station was demolished to make way for Ironbridge B Power Station. Coal for the power station was offloaded close to the site of the original station until the power station stopped generating electricity in November 2015.The Telford Steam Railway has aspirations to operate to this site, running over the Albert Edward Bridge to a new terminus on or close to the site of Buildwas station.

The Ercall is a small hill in Shropshire, England, between The Wrekin and Wellington. It is an internationally important geological site, part of The Wrekin and The Ercall Site of Special Scientific Interest (SSSI). The hill is managed by Shropshire Wildlife Trust and includes 540 million year old ripple beds and ancient pre-Cambrian lava flows in exposed quarries. Quartzite from the neighbouring Wrekin is also visible. The Ercall bears the marks of extensive quarrying, although the quarries are now disused, safe and open to the public. When the M54 motorway was constructed in 1974, the road was built through the northern end of the hill.

The Wrekin transmitting station is a telecommunications and broadcasting facility on The Wrekin, a hill in the county of Shropshire, England. It includes a 52 metres (171 ft) tall free-standing lattice tower with transmitting antennas attached at various heights. The DTT transmitting arrays add about another 10m to this. It broadcasts digital television, alongside digital and FM (analogue) radio. The station was first proposed in 1966. As The Wrekin is a local beauty spot, many objections had to be overcome and alternative sites analysed before planning consent was given. The transmitter opened in 1975. The building is semi-underground and the tower stands on its roof.

The Wrekin ( REE-kin) is a hill in east Shropshire, England. It is located some five miles (8 km) west of Telford, on the border between the unitary authorities of Shropshire and Telford and Wrekin. Rising above the Shropshire Plain to a height of 407 metres (1,335 feet) above sea level, 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 salient 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 Wrekin Terrane is one of five inferred fault bounded terranes that make up the basement rocks of the southern United Kingdom. The other notable geological terranes in the region are the Charnwood Terrane, Fenland Terrane, Cymru Terrane and the Monian Composite Terrane. The Wrekin Terrane is bounded to the west by the Welsh Borderland Fault System and to the east by the Malvern Lineament. The geological terrane to the west is the Cymru Terrane and to the east is Charnwood Terrane. The majority of rocks in the area are associated with the outcrops that are evident at the faulted boundaries.

The Ironbridge power stations (also known as the Buildwas power stations) refers to a series of two power stations that occupied a site on the banks of the River Severn at Buildwas in Shropshire, England. The Ironbridge B Power Station was operated by E.ON UK but the site is now owned by Haworth Group. The station stands near the Ironbridge Gorge World Heritage Site. Originally powered by coal, they were converted to use 100% biomass fuel. Ironbridge B Power Station stopped generating electricity on 20 November 2015, with the decommissioning process continuing into 2017. The main phase of the 27-month demolition process began at 11:00 GMT on 6 December 2019, commencing with the four cooling towers.

Horsehay is a suburban village on the western outskirts of Dawley, which, along with several other towns and villages, now forms part of the new town of Telford in Shropshire, England. Horsehay lies in the Dawley Hamlets parish, and on the northern edge of the Ironbridge Gorge area. Horsehay used to have four pubs, The Station Inn, The Forester Arms, the All Labour In Vain and the Travellers Joy, however The Station Inn closed down in 2012, and the All Labour In Vain closed in 2014. It also has a Methodist Chapel, a village hall, a post office, and a golf course complete with restaurant.

The Darby Houses museum is one of ten Ironbridge Gorge Museums administered by the Ironbridge Gorge Museum Trust. It is based in the village of Coalbrookdale in the Ironbridge Gorge, in Shropshire, England within a World Heritage Site, the birthplace of the Industrial Revolution. The Darby Houses comprise the adjacent properties of Dale House and Rosehill, both of which were built for members of the Darby family in Darby Road, Coalbrookdale.

The Albert Edward Bridge is a railway bridge spanning the River Severn at Coalbrookdale in Shropshire, England.