River Isle | |
---|---|
Location | |
Country | England |
County | Somerset |
Region | Somerset Levels |
Cities | Isle Brewers, Ilminster, Knowle St Giles, Chard, Somerset |
Physical characteristics | |
Source | |
• location | Combe St Nicholas, Somerset, England |
• coordinates | 50°55′10″N2°56′23″W / 50.91944°N 2.93972°W |
Mouth | River Parrett |
• location | Somerset, England |
• coordinates | 51°00′32″N2°49′55″W / 51.00889°N 2.83194°W |
Length | 14 mi (23 km) |
The River Isle (also known as the River Ile) flows from its source near Combe St Nicholas, through Somerset, England and discharges into the River Parrett south of Langport near Midelney.
Several small springs merge into the river near Wadeford it then flows north past Donyatt, Ilminster, Puckington, and Isle Abbotts, before joining the Parrett. The first section of the river falls 250 feet (76 m) in 6 miles (9.7 km) and then falls less steeply falling 80 feet (24 m) during the subsequent 8 miles (13 km). [1] As a result, several mills were built on the upper reaches of the river. At least one mill was in existence at the time of the Domesday Book in 1086. These mills were an important part of the local economy connecting with the wool trade. [2]
The road bridge over the river at Knowle St Giles is a Grade II listed building. [3]
A lock was built at the junction with the River Parrett, to maintain water levels, when the Westport Canal was built in the 1830s. The canal joins the river approximately 1 mile (1.6 km) before the confluence with the Parrett. [4]
Chard Reservoir was built by damming the river in the 1840s to provide water for the Chard Canal. [5]
Near Ilton and Puckington, the Isle is joined by Cad Brook. The name of this stream is first attested in a thirteenth-century copy of a perhaps tenth-century forgery of a charter purporting to date from 725, [6] as Caducburne. The name is attested again in the fifteenth century as Cadde. The second element of this name is an Old English word meaning "stream", the origin of the first element is less certain. In 1928, Eilert Ekwall guessed that Caduc was a diminutive form of a personal name Cada, thus meaning "Caduc's stream". [7] By 1936 he had concluded that the name included a rare Old English word for jackdaw, cadac, in which case the river name meant "jackdaw stream". [8] Andrew Breeze has more recently suggested that caduc was actually a Brittonic name for the stream, adopted into Old English with burn as an explanatory addition, related to the Modern Welsh word caddug ("mist, gloom, darkness"). [9]
The stream gave its name to the hamlet of Cad Green. [9] By the 1920s, the stream itself seems to have been called the Ding, [7] but recent maps show Cad Brook, suggesting that Cad Green has in turn given its name back to the stream from which it was named.[ citation needed ]
The River Parrett flows through the counties of Dorset and Somerset in South West England, from its source in the Thorney Mills springs in the hills around Chedington in Dorset. Flowing northwest through Somerset and the Somerset Levels to its mouth at Burnham-on-Sea, into the Bridgwater Bay nature reserve on the Bristol Channel, the Parrett and its tributaries drain an area of 660 square miles (1,700 km2) – about 50 per cent of Somerset's land area, with a population of 300,000.
The River Tone is a river in the English county of Somerset. The river is about 33 kilometres (21 mi) long. Its source is at Beverton Pond near Huish Champflower in the Brendon Hills, and is dammed at Clatworthy Reservoir. The reservoir outfall continues through Taunton and Curry and Hay Moors, which are designated as a Site of Special Scientific Interest. Finally, it flows into the River Parrett at Burrowbridge.
The River Tame flows through Greater Manchester, England. It rises on Denshaw Moor and flows to Stockport where it joins the River Goyt to form the River Mersey.
Chard is a town and a civil parish in the English county of Somerset. It lies on the A30 road near the Devon and Dorset borders, 15 miles (24 km) south west of Yeovil. The parish has a population of approximately 14,000 and, at an elevation of 121 metres (397 ft), Chard is the southernmost and one of the highest towns in Somerset. Administratively Chard forms part of the district of South Somerset.
The River Chew is a small river in England that flows for some 17 miles (27 km) through the North Somerset countryside to form the Chew Valley before merging with the River Avon.
Martock is a large village and civil parish in Somerset, England. It is situated on the edge of the Somerset Levels, 7 miles (11.3 km) north-west of Yeovil in the South Somerset district. The parish includes Hurst, approximately one mile south of the village, and Bower Hinton, which is located to the west; the village is bounded by Hurst and the A303. Martock has a population of 4,766 and was historically a market town.
The Chard Canal was a 13.5 miles (21.7 km) tub boat canal in Somerset, England, that ran from the Bridgwater and Taunton Canal at Creech St. Michael, over four aqueducts, through three tunnels and four inclined planes to Chard. It was completed in 1842, was never commercially viable, and closed in 1868. The major engineering features are still clearly visible in the landscape.
The name Rea Brook can refer to either of two brooks in Shropshire, England.
Langport is a town and civil parish in Somerset, England, 5 miles (8 km) west of Somerton. The parish, which covers only part of the town, has a population of 3,578. Langport is contiguous with Huish Episcopi, a separate parish that includes much of the town's outskirts.
The River Gwash, occasionally Guash, a tributary of the River Welland, flows through the English counties of Leicestershire, Rutland and Lincolnshire. It rises just outside the village of Knossington in Leicestershire, near the western edge of Rutland. It is about 39 kilometres (24 mi) long.
Ketton is a village and civil parish in Rutland in the East Midlands of England. It is about 8 miles (13 km) east of Oakham and 3 miles (5 km) west of Stamford, Lincolnshire. The 2011 Census recorded a parish population of 1,926, making it the fourth largest settlement in Rutland, after Oakham, Uppingham and Cottesmore. The village has a primary school.
Ilton is a village and civil parish in Somerset, England, situated 8 miles (12.9 km) south-east of Taunton, and 2 miles (3.2 km) north of Ilminster in the South Somerset district. The village has a population of 854. The parish includes the hamlets of Ilford and Cad Green with its 16th-century almshouses.
Coffinswell is a small village in South Devon, England, just off the A380, the busy Newton Abbot to Torquay road. It lies within Teignbridge District Council.
Chitterne is a village and civil parish in the county of Wiltshire, in the south west of England. The village lies in the middle of Salisbury Plain, about 7 miles (11 km) east of the town of Warminster.
The Westport Canal was built in the late 1830s to link Westport and Langport in Somerset, England. It was part of a larger scheme involving improvements to the River Parrett above Burrow Bridge. Langport is the point at which the River Yeo joins the River Parrett and the intention was to enable trade via the port at Bridgwater. It remained in use until the 1870s, but closed when the Somerset Drainage Commissioners took over control of the River Parrett. Despite a petition against closure by local people, the Commissioners ruled that navigation of the canal must cease due to their interpretation of the Act which gave them control of it, leaving the canal to serve as a drainage channel since 1878.
Caughley was a non-nucleated settlement situated two kilometres east of Barrow near Much Wenlock in Shopshire, England, with the River Severn running down its eastern edge and Dean Brook along its south-western edge. It is noted as a site of the production of Coalport porcelain. In 1883, Caughley extended to 332 hectares and in 1931 the population of the township stood at 48.
The Lox Yeo is a short river in North Somerset, England. It rises at Winscombe and flows south west for about 6 kilometres (4 mi) to join the River Axe near Loxton.
The earliest known infrastructure for transport in Somerset is a series of wooden trackways laid across the Somerset Levels, an area of low-lying marshy ground. To the west of this district lies the Bristol Channel, while the other boundaries of the county of Somerset are along chains of hills that were once exploited for their mineral deposits. These natural features have all influenced the evolution of the transport network. Roads and railways either followed the hills, or needed causeways to cross the Levels. Harbours were developed, rivers improved, and linked to sources of traffic by canals. Railways were constructed throughout the area, influenced by the needs of the city of Bristol, which lies just to the north of Somerset, and to link the ports of the far south-west with the rest of England.
Walverden Water is a minor river in Lancashire, England. It is approximately 2.6 miles (4.2 km) long and has a catchment area of 5.04 square miles (1,304.23 ha).