River Team

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River Team
River Team - geograph.org.uk - 836601.jpg
River Team near Gateshead
River Team is located in Tyne and Wear
River Team
Location of mouth within Tyne and Wear
CountryUnited Kingdom
Country within the UKEngland
CountiesTyne and Wear, County Durham
Physical characteristics
 ⁃ location
Confluence with the River Tyne, Dunston, Tyne and Wear
 ⁃ coordinates
54°57′28″N 1°38′14″W / 54.957709°N 1.637177°W / 54.957709; -1.637177Coordinates: 54°57′28″N 1°38′14″W / 54.957709°N 1.637177°W / 54.957709; -1.637177

The River Team is a tributary of the River Tyne in Gateshead, England.


The name Team may have a Brittonic origin.[1] The name may be from the Brittonic root tā-, with a sense of "melting, thawing, dissolving",[1] plus a nasal root determinative, giving a form of *tā-m- or *tā-n-.[1] However, Team has also been associated with the Indo-European *temhx-, "dark" and *tṃh-, "cut" or "be cut".[1]


Its source is near Annfield Plain, where it is known as Kyo Burn. Then changing its name again to Causey Burn as it flows underneath the famous Causey Arch. It then flows past Beamish Museum in County Durham (where it is known as Beamish Burn) then crosses the border into Gateshead flowing through Lamesley. Continuing on into the Team Valley, the river flows through a culvert in the middle of the roundabout underneath the A1 road, it then continues through the Team Valley Trading Estate through a covered culvert, before emerging to the surface halfway along.

It then flows through the site of the 1990 National Garden Festival, before finally discharging into the River Tyne in Dunston. This area is known as Teams, after the river.


The River Team has long been regarded as one of the most polluted rivers in the area due to the discharges from Sewage works near Lamesley and heavy industry in the Team Valley. It is called "The Gut" by the residents of Dunston. However considerable improvements have now been made and the river is relatively clean.


Prior to the last Ice Age, the lower part of the River Team actually formed the lower part of the River Wear, with a combined Tyne-Wear river continuing to the coast from Dunston. The ice diverted the River Wear to its current course towards the coast at Sunderland, with the smaller River Team flowing along its former course towards the River Tyne.


  1. ^ a b c d James, Alan G. "A Guide to the Place-Name Evidence - Guide to the Elements" (PDF). Scottish Place Name Society - The Brittonic Language in the Old North. Retrieved 25 October 2018.