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The River Thames, known alternatively in parts as the River Isis, is a river that flows through southern England including London. At 215 miles (346 km), it is the longest river entirely in England and the second-longest in the United Kingdom, after the River Severn.
The River Lark crosses the border between Suffolk and Cambridgeshire in England. It is a tributary of the River Great Ouse, and was extended when that river was re-routed as part of drainage improvements. It is thought to have been used for navigation since Roman times, and improvements to its navigability were made in 1638 and in the early 18th century, when locks and staunches were built. Special powers to improve the river from Mildenhall to Bury St Edmunds were granted by statute. The upper terminus was on the northern edge of Bury St Edmunds, but a new dock was opened near the railway station after the Eastern Union Railway opened its line in 1846.
The River Avon is a river in the southwest of England. To distinguish it from a number of other rivers of the same name, it is often called the Bristol Avon. The name 'Avon' is loaned from an ancestor of the Welsh word afon, meaning 'river'.
The Kennet is a tributary of the River Thames in Southern England. Most of the river is straddled by the North Wessex Downs AONB. The lower reaches have been made navigable as the Kennet Navigation, which – together with the Avon Navigation, the Kennet and Avon Canal and the Thames – links the cities of Bristol and London.
The River Dearne South Yorkshire, England flows roughly east for more than 30 kilometres (19 mi), from its source just inside West Yorkshire. It flows through Denby Dale, Clayton West, Darton, Barnsley, Darfield, Wath upon Dearne, Bolton on Dearne, Adwick upon Dearne and Mexborough to its confluence with the River Don at Denaby Main. Its main tributary is the River Dove, which joins it at Darfield. The river was one of those affected by the 2007 United Kingdom floods.
The River Lugg rises near Llangynllo in Radnorshire, Wales. It flows through the border town of Presteigne and then through Herefordshire, England, where it meets its main tributary, the River Arrow, to the south of Leominster. It flows into the River Wye downstream of Hereford at Mordiford, around 63 miles (101 km) from its source. Its name comes from a Welsh root, and means "bright stream".
The English River Thames is navigable from Cricklade or Lechlade to the sea, and this part of the river falls 71 meters (234 feet). There are 45 locks on the river, each with one or more adjacent weirs. These lock and weir combinations are used for controlling the flow of water down the river, most notably when there is a risk of flooding, and provide for navigation above the tideway.
The River Loxley is a river in the City of Sheffield, South Yorkshire, England. Its source is a series of streams which rise some 10 miles (16 km) to the north-west of Sheffield on Bradfield Moors, flowing through Bradfield Dale to converge at Low Bradfield. It flows easterly through Damflask Reservoir and is joined by Storrs Brook at Storrs, near Stannington, and the River Rivelin at Malin Bridge, before flowing into the River Don at Owlerton, in Hillsborough. The Loxley valley provided the initial course of the Great Sheffield Flood, which happened after the Dale Dyke Dam collapsed shortly before its completion in March 1864.
Teddington Lock is a complex of three locks and a weir on the River Thames between Ham and Teddington in the London Borough of Richmond upon Thames, England. Historically in Middlesex, it was first built in 1810.
The River Devon is a tributary of the River Trent, which rises in Leicestershire and joins the Trent at Newark in Nottinghamshire, England. In its upper reaches, it supplies Knipton Reservoir, which was built to supply water to the Grantham Canal, and Belvoir Lakes, designed by Capability Brown. It passes under the Grantham Canal, and then through Bottesford, where it is spanned by five railway bridges, only one of which is still used for its original purpose. On the outskirts of Newark, it passes by two Civil War structures, and just before it joins the Trent it becomes navigable, with a marina located on the west bank. Its name is pronounced "Deevon", not as spelt.
Foudry Brook is a small stream in southern England. It rises from a number of springs near the Hampshire village of Baughurst, and flows to the east and then the north, to join the River Kennet to the south of Reading. The upper section is called Silchester Brook, and beyond that, Bishop's Wood Stream. The underlying geology is chalk, covered by a layer of clay, and so it has the characteristics of a clay stream, experiencing rapid increases in level after heavy rain due to run-off from the surrounding land. It passes a number of listed buildings and scheduled monuments, including the site of the Roman town of Calleva Atrebatum or Silchester.
The River Ash is a small, shallow river in Surrey, England. Its course of 10 kilometres (6.2 mi) is just outside Greater London. Work has been carried out to re-align, clear and build up a small, Littleton head of water and create two backwaters. One backwater dates to the medieval period; the other to the 1990s. It flows as one of the six distributaries of the River Colne from the south of Staines Moor immediately south of the Staines Bypass eastwards through the rest of the borough of Spelthorne before meeting the River Thames.
Shepperton Lock is a lock on the River Thames, in England by the left bank at Shepperton, Surrey. It is across the river from Weybridge which is nearby linked by a passenger ferry.
The River Roach is a river that flows entirely through the English county of Essex. It is one of four main streams that originate in the Rayleigh Hills to the west, and flow east. They then flow towards the centre of the Rochford Basin, a circular feature which may have been caused by an asteroid impact in the Late Oligocene or Early Miocene periods. To the east of Rochford, the river becomes tidal, and is governed by the Crouch Harbour Authority. It joins the River Crouch between Wallasea Island and Foulness Island. To the west of Rochford, there is some doubt as to which of the four streams is officially the Roach.
The Stroudwater Navigation is a canal in Gloucestershire, England which linked Stroud to the River Severn. It was authorised in 1776, although part had already been built, as the proprietors believed that an Act of Parliament obtained in 1730 gave them the necessary powers. Opened in 1779, it was a commercial success, its main cargo being coal. It was 8 miles (13 km) in length and had a rise of 102 ft 5 in (31.22 m) through 12 locks. Following the opening of the Thames and Severn Canal in 1789, it formed part of a through route from Bristol to London, although much of its trade vanished when the Kennet and Avon Canal provided a more direct route in 1810. Despite competition from the railways, the canal continued to pay dividends to shareholders until 1922, and was not finally abandoned until 1954.
The River Wey is a main tributary of the River Thames in south east England. Its two branches, one of which rises near Alton in Hampshire and the other in West Sussex to the south of Haslemere, join at Tilford in Surrey. Once combined, the flow is eastwards then northwards via Godalming and Guildford to meet the Thames at Weybridge. Downstream the river forms the backdrop to Newark Priory and Brooklands. The Wey and Godalming Navigations were built in the 17th and 18th centuries, to create a navigable route from Godalming to the Thames.
The Cut is a river in England that rises in North Ascot, Berkshire. It flows for around 14 miles (23 km), through the rural Northern Parishes of Winkfield, Warfield and Binfield in Bracknell Forest on its way down to Bray, where it meets the River Thames just above Queens Eyot on the reach below Bray Lock, having been joined by the Maidenhead Waterways.
The River Dove is a river that extends through the Low Valley in Barnsley, England. It flows from Worsbrough Reservoir to its confluence with the River Dearne.
The Pipp Brook is a left-bank tributary of the River Mole, Surrey, England. It rises at two main springs north of Leith Hill on the Greensand Ridge, then descends steeply in a northward direction, before flowing eastwards along the Vale of Holmesdale. It runs to the north of Dorking High Street, before discharging into the Mole at Pixham.
Oldcotes Dyke is the name of the final section of a river system that drains parts of north Nottinghamshire and the Metropolitan Borough of Rotherham in South Yorkshire, England. Historically, it has supported milling, with seven water mills drawing their power from its water, and ran through the grounds of the Cistercian Roche Abbey. It is a tributary of the River Ryton.
References
- ↑ Marsh, T; Hannaford, J, eds. (2008). UK Hydrometric Register (PDF). Hydrological data UK series. Wallingford, Oxfordshire: Centre for Ecology & Hydrology. ISBN 978-0-9557672-2-7. Archived from the original (PDF) on 21 May 2013.
- ↑ Thurrock Flood Risk Assessment Archived 16 August 2011 at the Wayback Machine
- ↑ Maltby E. "River Darent". SuRCaSE project. University of Liverpool. Retrieved 21 December 2010.
- ↑ River Roding fluvial/tidal flood defence project - National Environmental Research Council, 1992
- 1 2 3 4 5 6 7 "HA16 Rivers and Streams" (PDF). Gateway to WildPRO. Wildlife Information Network. 2004. Retrieved 20 December 2010.
- ↑ "Explore georeferenced maps - Map images - National Library of Scotland".
- ↑ https://upload.wikimedia.org/wikipedia/commons/d/db/LondonBeforeHouses.jpg [ bare URL image file ]
- ↑ http://www.spelthorne.gov.uk/article/18090/Other-sites Spelthorne Borough Council: Biodiversity and Conservation: Other Sites
- ↑ Maltby E. "River Kennet". SuRCaSE project. University of Liverpool. Archived from the original on 6 September 2012. Retrieved 20 December 2010.
- ↑ Neal C (2000). "The water quality of a tributary of the Thames, the Pang, southern England". Science of the Total Environment. 251–252. Elsevier: 459–475. Bibcode:2000ScTEn.251..459N. doi:10.1016/S0048-9697(00)00399-5. PMID 10847178.
- ↑ Neal C (2006). "The water quality of the River Thame in the Thames Basin of south/south-eastern England". Science of the Total Environment. 360 (1–3). Elsevier: 254–271. Bibcode:2006ScTEn.360..254N. doi:10.1016/j.scitotenv.2005.08.039. PMID 16253309.
- ↑ Neal C (2006). "River water quality of the River Cherwell: An agricultural clay-dominated catchment in the upper Thames Basin, southeastern England". Science of the Total Environment. 360 (1–3). Elsevier: 272–289. Bibcode:2006ScTEn.360..272N. doi:10.1016/j.scitotenv.2005.08.040. PMID 16253306.
- ↑ Johnes PJ (1991). "Water Quality Trends in the Windrush Catchment: Nitrogen Speciation and Sediment Interactions" (PDF). Sediment and Stream Water Quality in a Changing Environment: Trends and Explanation. 203. International Association of Hydrological Sciences: 349–357. Retrieved 21 December 2010.
- Cove-Smith, Chris (2006). The River Thames Book. Imray Laurie Norie and Wilson. ISBN 0-85288-892-9.
- Fred. S. Thacker The Thames Highway: Volume II Locks and Weirs, 1920. Republished by David & Charles, 1968.