River Isle Explained

River Isle
Subdivision Type1:Country
Subdivision Name1:England
Subdivision Type2:County
Subdivision Name2:Somerset
Subdivision Type3:Region
Subdivision Name3:Somerset Levels
Subdivision Type5:Cities
Subdivision Name5:Isle Brewers, Ilminster, Knowle St Giles, Chard, Somerset
Length:14miles
Source1 Location:Combe St Nicholas, Somerset, England
Source1 Coordinates:50.9194°N -2.9397°W
Mouth:River Parrett
Mouth Location:Somerset, England
Mouth Coordinates:51.0089°N -2.8319°W

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 250feet in 6miles and then falls less steeply falling 80feet during the subsequent 8miles.[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 1miles 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]

Tributaries

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 English, Old (ca.450-1100);: 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", but 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, English, Old (ca.450-1100);: cadac, in which case the river name meant "jackdaw stream".[8] But 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, and that it is related to the Modern Welsh word caddug ("mist, gloom, darkness").[9]

The stream gave its name to the hamlet of Cad Green. By the 1920s, the stream itself seems to have been called the Ding, 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.

Notes and References

  1. Web site: River Isle. Somerset Rivers. 2 September 2011.
  2. Web site: Warren . Derrick . Mills of the Isle . Combe St Nicholas . 2 September 2011 . dead . https://web.archive.org/web/20120331144500/http://www.combestnicholas.org.uk/about_the_parish/Mills%20on%20the%20Isle.htm . 31 March 2012 .
  3. Web site: Road Bridge over River Isle. British Listed Buildings. 2 September 2011.
  4. Web site: River Isle. Somerset Rivers. 2 September 2011.
  5. Web site: Chard Reservoir leaflet . south Somerset Council . 18 November 2010.
  6. Web site: Electronic Sawyer . 2023-05-31 . esawyer.lib.cam.ac.uk.
  7. Eilert Ekwall, English River-names (Oxford: Clarendon Press, 1928), p. 58.
  8. Eilert Ekwall, Studies on English Place-names, Kungl. Vitterhets historie och antikvitets akademiens handlingar, 42:1 (Stockholm: Wahlström & Widstrand, 1936), p. 85.
  9. Andrew Breeze, 'Cad Green, Ilton, Somerset', in Richard Coates, Andrew Breeze, and David Horovitz, Celtic Voices English Places: Studies of the Celtic Impact on Place-Names in England (Stamford: Tyas, 2000), pp. 83-84 [first publ. 'The Name of Cad Green, Ilton', ''Notes and Queries for Somerset and Dorset'', 34 [351 of the continuous series] (2000), 355-56].