Severn Valley
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Severn Valley
The Severn Valley is a rural area of the West Midlands region of England, through which the River Severn runs and the Severn Valley Railway steam heritage line operates, starting at its northernmost point in Bridgnorth, Shropshire and running south for 16 miles (26 km) to Ribbesford, a few miles south of Bewdley, Worcestershire in the Wyre Forest. The area is about 25 miles (40 km) due west of Birmingham. There is also use of this term to apply to areas around the River Severn as far south as Gloucester, and as far north as Ironbridge. To the north of Bridgnorth, the land to the sides of the river becomes much steeper, and the upstream part is known as Ironbridge Gorge. From Stourport-on-Severn south to Gloucester, the riverside has a much larger flood plain and loses its distinctive "valley" hillsides found a few miles north in Bewdley. To the south of Gloucester, it becomes the Vale of Berkeley and then the Severn Estuary. History The Severn Valley was under ...
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West Midlands Region
The West Midlands is one of nine official regions of England at the first level of International Territorial Level for statistical purposes. It covers the western half of the area traditionally known as the Midlands. The region consists of the counties of Herefordshire, Shropshire, Staffordshire, Warwickshire, West Midlands and Worcestershire. The region has seven cities; Birmingham, Coventry, Hereford, Lichfield, Stoke-on-Trent, Wolverhampton and Worcester. The West Midlands region is geographically diverse, from the urban central areas of the West Midlands conurbation to the rural counties of Herefordshire, Shropshire and Worcestershire which border Wales. The region is landlocked. However, the longest river in the UK, the River Severn, traverses the region southeastwards, flowing through the county towns of Shrewsbury and Worcester, and the Ironbridge Gorge, a UNESCO World Heritage Site. Staffordshire is home to the industrialised Potteries conurbation, including the ...
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Penda Of Mercia
Penda (died 15 November 655)Manuscript A of the ''Anglo-Saxon Chronicle'' gives the year as 655. Bede also gives the year as 655 and specifies a date, 15 November. R. L. Poole (''Studies in Chronology and History'', 1934) put forward the theory that Bede began his year in September, and consequently November 655 would actually fall in 654; Frank Stenton also dated events accordingly in his ''Anglo-Saxon England'' (1943). 1 Others have accepted Bede's given dates as meaning what they appear to mean, considering Bede's year to have begun on 25 December or 1 January (see S. Wood, 1983: "Bede's Northumbrian dates again"). The historian D. P. Kirby suggested the year 656 as a possibility, alongside 655, in case the dates given by Bede are off by one year (see Kirby's "Bede and Northumbrian Chronology", 1963). The ''Annales Cambriae'' gives the year as 657Annales Cambriae at Fordham University/ref> was a 7th-century king of Mercia, the Anglo-Saxon kingdom in what is today the Midland ...
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Hampton Loade
Hampton Loade is a hamlet in Shropshire, England along the Severn Valley. It is situated on the east bank of the River Severn at , some five miles south of Bridgnorth, and is notable for the unusual current-operated Hampton Loade Ferry, a reaction ferry to the hamlet of Hampton on the west bank. The ferry is responsible for Hampton Loade's name, as ''Loade'' is derived from ''lode'', an old English word for ferry. Hampton Loade station, on the preserved Severn Valley Railway, is actually located on the Hampton side of the river although the whole area is often known locally Hampton Loade due to the presence of the station. There is an unusual bridge close to Hampton Loade: a small private roadway is suspended below two large waterpipe arches, used to pump water from the river to Chelmarsh Reservoir, by the South Staffordshire Water South Staffordshire Water plc known as South Staffs Water is a UK water supply company owned by a privately owned utilities company serving pa ...
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Chelmarsh
Chelmarsh is a village and civil parish in the English county of Shropshire. It lies 4 miles south of Bridgnorth on the B4555 road to Highley. Notable buildings The main feature of the village St. Peter's church. This is an example of the Decorated style and is built on the site of a Norman church, parts of the original building can still be seen. Other notable buildings include the former Chelmarsh Church of England Primary School, built in 1850 which closed its curriculum doors in July 2002; the building has since been converted into a dwelling. Another is Astbury Hall; a stately home with 320 acres. In 1889 it was destroyed by a fire but rebuilt in 1891. Up until 2017 it was the home to Judas Priest star K.K. Downing who transformed it into a golf course. Community It has one pub: 'The Bulls Head' in the main village, and the 'Unicorn' in the hamlet of Hampton, and is also home to Chelmarsh Sports & Social Club and Chelmarsh Parish Hallwww.chelmarshparishhall.co.uk. Che ...
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Quatford
Quatford is a village in the Severn Valley, Shropshire, England. It is located on the A442, just south of the town of Bridgnorth and on the bank of the River Severn. History Quatford is one of the oldest settlements in the area. It was listed in the Domesday Book, the draft of which was finished in 1086. Quatford was settled because of the ease of fording the River Severn. Its name came from it being a ford near Quatt. As the River Severn became deeper a bridge was built at the site instead. In the 11th Century a small castle was built on high ground overlooking the river, but was demolished a few years later. Traces of the motte still remain. Quatford's importance as a crossing of the River Severn was diminished when another bridge was built 2 miles upstream. A settlement was formed at the "bridge north of Quatford", now known as Bridgnorth, which became the major town in the district. North of the village is a mock castle now known as Quatford Castle. It was built circa 1830 ...
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Shropshire
Shropshire (; alternatively Salop; abbreviated in print only as Shrops; demonym Salopian ) is a landlocked historic county in the West Midlands region of England. It is bordered by Wales to the west and the English counties of Cheshire to the north, Staffordshire to the east, Worcestershire to the southeast, and Herefordshire to the south. A unitary authority of the same name was created in 2009, taking over from the previous county council and five district councils, now governed by Shropshire Council. The borough of Telford and Wrekin has been a separate unitary authority since 1998, but remains part of the ceremonial county. The county's population and economy is centred on five towns: the county town of Shrewsbury, which is culturally and historically important and close to the centre of the county; Telford, which was founded as a new town in the east which was constructed around a number of older towns, most notably Wellington, Dawley and Madeley, which is today th ...
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Highley
Highley is a large village in Shropshire, England, on the west bank of the River Severn and 7 miles south east of Bridgnorth. The closest cities being Wolverhampton and Birmingham. History Highley began as a rural farming community, including an entry in the Domesday Book, later becoming a significant area for stone quarrying which provided some of the stone for Worcester Cathedral. Coal mining began in the area in the Middle Ages, but in the late 19th century the village was revolutionised by coal mining with large-scale operations beginning in 1878. A period of intense house-building also followed, giving Highley its distinctive red-brick terraced miners' houses. In the 1930s, the mine was extended to the neighbouring village of Alveley across the River Severn and a tunnel and bridge constructed between the two. There are also historical bridging points at Bridgnorth to the north and Bewdley to the south, and in Hampton Loade a private bridge used by the emergency services. ...
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B4555 Road
B roads are numbered routes in Great Britain of lesser importance than A roads. See the article Great Britain road numbering scheme The Great Britain road numbering scheme is a numbering scheme used to classify and identify all roads in Great Britain. Each road is given a single letter (which represents the road's category) and a subsequent number (between 1 and 4 digits). ... for the rationale behind the numbers allocated. 3 digits 4 digits (40xx) 4 digits (41xx) 4 digits (42xx) 4 digits (43xx) 4 digits (44xx) 4 digits (45xx) 4 digits (46xx) References {{DEFAULTSORT:B Roads in Zone 4 of the Great Britain Numbering Scheme 4 4 ...
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Kidderminster
Kidderminster is a large market and historic minster town and civil parish in Worcestershire, England, south-west of Birmingham and north of Worcester. Located north of the River Stour and east of the River Severn, in the 2011 census, it had a population of 55,530. The town is twinned with Husum, Germany. Situated in the far north of Worcestershire (and with its northern suburbs only 3 and 4 miles from the Staffordshire and Shropshire borders respectively), the town is the main administration centre for the wider Wyre Forest District, which includes the towns of Stourport-on-Severn and Bewdley, along with other outlying settlements. History The land around Kidderminster may have been first populated by the Husmerae, an Anglo-Saxon tribe first mentioned in the Ismere Diploma, a document in which Ethelbald of Mercia granted a "parcel of land of ten hides" to Cyneberht. This developed as the settlement of Stour-in-Usmere, which was later the subject of a territorial dispute ...
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Alveley
Alveley is a village in the Severn Valley in southeast Shropshire, England, about south-southeast of Bridgnorth. It is in the civil parish of Alveley and Romsley. The 2011 Census recorded the parish population as 2,098. It is served by bus service 297 (Kidderminster - Bridgnorth) operated by Arriva Midlands. It is most famously known as being the hometown of Jack Jones, a local magician. The Black Death is said to have killed 60% of the village population in 1349. A stone cross, the Buttercross, outside the village dates from the time of the Black Death when it was a place for food to be left for the village when it was quarantined. Churches The Church of England parish church of Saint Mary is 12th-century with a 14th-century south chapel. In the chapel is a very faded 14th-century mural that is thought to represent the Seven Deadly Sins. The upper part of the tower was rebuilt in about 1779. The building was heavily restored in 1878–79 under the direction of Sir Arthur ...
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A442 Road
The A442 is a main road which passes through the counties of Worcestershire and Shropshire, in the West Midlands region of England. __TOC__ Route From Droitwich in Worcestershire it runs towards Kidderminster where it meets the A449 from Worcester. This section of road used to be the B4192 until the late 1970s when it was upgraded to A road status. At Kidderminster, it starts again and then runs north-north-west into Shropshire, via Bridgnorth and Telford (where it crosses the M54 motorway). Through Telford it is known as ''Queensway'', and the ''Eastern Primary'' (EP). It ends where it meets the A53 just outside the village of Hodnet. Before the A53 bypass around the village was built, the A442 continued through Hodnet and joined the A41 near Darliston, south of Whitchurch. This section of road however has now been downgraded: most of it is declassified, but part has been reclassified as part of B5065. History From Droitwich to Low Hill (south of Kidderminster) the road ...
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Sandstone
Sandstone is a clastic sedimentary rock composed mainly of sand-sized (0.0625 to 2 mm) silicate grains. Sandstones comprise about 20–25% of all sedimentary rocks. Most sandstone is composed of quartz or feldspar (both silicates) because they are the most resistant minerals to weathering processes at the Earth's surface. Like uncemented sand, sandstone may be any color due to impurities within the minerals, but the most common colors are tan, brown, yellow, red, grey, pink, white, and black. Since sandstone beds often form highly visible cliffs and other topographic features, certain colors of sandstone have been strongly identified with certain regions. Rock formations that are primarily composed of sandstone usually allow the percolation of water and other fluids and are porous enough to store large quantities, making them valuable aquifers and petroleum reservoirs. Quartz-bearing sandstone can be changed into quartzite through metamorphism, usually related to ...
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