River Camlad | |
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![]() The river, here forming the English-Welsh border, to the northwest of Chirbury | |
Location | |
Country | Wales, England |
Counties | Powys, Shropshire |
Physical characteristics | |
Mouth | |
• location | confluence with River Severn near Forden |
• coordinates | 52°35′50″N3°10′09″W / 52.5972°N 3.1693°W Coordinates: 52°35′50″N3°10′09″W / 52.5972°N 3.1693°W |
The River Camlad (or just Camlad) is a minor river in Powys and Shropshire. It forms part of the border between Wales and England in places, before flowing into the River Severn. It is notable for being the only river to cross from England into Wales [1] and does so twice.
The river originates in England, in the area between Snead and Lydham, flows west, forming part of the border between Wales and England, before flowing northwest into Wales. It passes through Church Stoke, where the River Caebitra flows into the Camlad. From Church Stoke it flows north, crossing the border back into England, and flows just east of Chirbury before turning west again, and forms the border (for the second time) between England and Wales. It turns northwest into Wales (for the second time) to join the River Severn to the west of Forden. [2]
Early forms include the Kemelet (1227), Kemlet (1256), Kelemet 1274, Camalet and Kenlet (1577) and Camlet (1612). Ekwall proposes the Welsh cwlm meaning "a knot" (which is found in other river names) giving a hypothetical Old Welsh Culmet then Cylmet whence Kelemet, alternatively Cym(y)let from the Old Welsh for "loop". [3]
The River Severn, at 220 miles (354 km) long, is the longest river in Great Britain. It is also the river with the most voluminous flow of water by far in all of England and Wales, discharging an average of 107 m3/s (3,800 cu ft/s) into the Bristol Channel at Apperley, Gloucestershire. It rises in the Cambrian Mountains in mid Wales, at an altitude of 2,001 feet (610 m), on the Plynlimon massif, which lies close to the Ceredigion/Powys border near Llanidloes. The river then flows through Shropshire, Worcestershire and Gloucestershire. The county towns of Shrewsbury, Gloucester and the City of Worcester lie on its course.
Shropshire is a landlocked 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. Shropshire Council was created in 2009, a unitary authority taking over from the previous county council and five district councils, covering Shropshire district. The borough of Telford and Wrekin has been a separate unitary authority since 1998, but remains part of the ceremonial county.
The Staffordshire and Worcestershire Canal is a navigable narrow canal in Staffordshire and Worcestershire in the English Midlands. It is 46 miles (74 km) long, linking the River Severn at Stourport in Worcestershire with the Trent and Mersey Canal at Haywood Junction by Great Haywood.
Montgomeryshire, also known as Maldwyn is one of thirteen historic counties and a former administrative county of Wales. It is named after its county town, Montgomery, which in turn is named after one of William the Conqueror's main counsellors, Roger de Montgomerie, who was the 1st Earl of Shrewsbury.
The River Teme rises in Mid Wales, south of Newtown, and flows southeast roughly forming the border between England and Wales for several miles through Knighton before becoming fully English in the vicinity of Bucknell and continuing east to Ludlow in Shropshire, then to the north of Tenbury Wells on the Shropshire/Worcestershire border there, on its way to join the River Severn south of Worcester. The whole of the River Teme was designated as an SSSI, by English Nature, in 1996.
The Stour is a river flowing through the counties of Worcestershire, the West Midlands and Staffordshire in the West Midlands region of England. The Stour is a major tributary of the River Severn, and it is about 25 miles (40 km) in length. It has played a considerable part in the economic history of the region.
The name Rea Brook can refer to either of two brooks in Shropshire, England.
Wales is a country that is part of the United Kingdom and whose physical geography is characterised by a varied coastline and a largely upland interior. It is bordered by England to its east, the Irish Sea to its north and west, and the Bristol Channel to its south. It has a total area of 2,064,100 hectares and is about 170 mi (274 km) from north to south and at least 60 mi (97 km) wide. It has a number of offshore islands, by far the largest of which is Anglesey. The mainland coastline, including Anglesey, is about 1,680 mi (2,704 km) in length. As of 2014, Wales had a population of about 3,092,000; Cardiff is the capital and largest city and is situated in the urbanised area of South East Wales.
The Shropshire Hills area, in the English county of Shropshire, is designated as an Area of Outstanding Natural Beauty (AONB). It is located in the south of the county, extending to its border with Wales. Designated in 1958, the area encompasses 802 square kilometres (310 sq mi) of land primarily in south-west Shropshire, taking its name from the upland region of the Shropshire Hills. The A49 road and Welsh Marches Railway Line bisect the area north-south, passing through or near Shrewsbury, Church Stretton, Craven Arms and Ludlow.
The River Vyrnwy is a river which flows through northern Powys, Wales, and Shropshire, England. The name derives from Severn, the river of which it is a tributary.
The town of Shrewsbury in Shropshire, England, has a history that extends back at least as far as the year 901, but it could have been first settled earlier. During the early Middle Ages, the town was a centre of the wool trade, and this was a peak in its importance. During the Industrial Revolution, comparatively little development took place in the town, although it did serve as a significant railway town after the development of rail transport in the area. The town today retains much of its historic architecture.
Shropshire's Geology is very diverse and most geological periods of time, and most rock types, can be found within the county. There is also a large amount of mineral wealth in the county, including lead, barytes, limestone, coal and iron, which helped the area develop the industrial revolution west of Clee Hill and, later, in the Ironbridge Gorge area. Quarrying is still active, with limestone for cement manufacture and concrete aggregate, sandstone, greywacke and dolerite for road aggregate, and sand and gravel for aggregate and drainage filters. Groundwater is an equally important economic resource.
Corndon Hill is a hill in Powys, Mid Wales, whose isolated summit rises to 1,683 ft above sea level.
Bettws-y-Crwyn is a small, remote village and civil parish in south-west Shropshire, England. It is close to the England–Wales border and is one of a number of English villages to have a Welsh language placename.
Chirbury is a village in west Shropshire, England. It is situated in the Vale of Montgomery, close to the Wales–England border, which is to its north, west and south. The A490 and B4386 routes cross at Chirbury.
The River Onny is a river in Shropshire, England. It is a major tributary of the River Teme.
The England–Wales border, sometimes referred to as the Wales–England border or the Anglo–Welsh border, runs for 160 miles (260 km) from the Dee estuary, in the north, to the Severn estuary in the south, separating England and Wales.
The River Worfe is a river in Shropshire, England. The name Worfe is said to derive from the Old English meaning to wander which the river is notable for in its middle section. Mapping indicates that the river begins at Cosford Bridge where the Cosford Brook and Albrighton Brook meet.
Ledwyche Brook is a minor river in south Shropshire, England. It is sometimes referred to as the River Ledwyche and spelled variously, including "Ledwich" or "Ledwych". The brook is a tributary of the River Teme.
The Vale of Montgomery is an area of low land straddling the border between Shropshire (England) and the former county of Montgomeryshire, (Wales). The three principal settlements within it are the former county town of Montgomery and the village of Churchstoke, both in Wales, and Chirbury in England. The earthworks of Offa's Dyke run NNW-ESE through the middle of the vale and are followed by the Offa's Dyke Path. The national boundary also follows this monument for 3 km within the vale. The River Camlad rises to the southeast of the vale whilst its tributary the Caebitra rises to its southwest. They combine at Churchstoke and flow north within a gorge along the eastern margin of the vale, before turning west across the north end of the vale to join the River Severn.
Media related to River Camlad at Wikimedia Commons