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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 Wey drains much of south west Surrey (as well as parts of east Hampshire and the north of West Sussex) and has a total Drainage basin of . Although it is the longest tributary of the Thames (if the River Medway is excluded), its total average discharge is lower than that of the River Kennet and River Cherwell. The river morphology and biodiversity of the Wey are well studied, with many places to take samples and record data. The main tributary is the Tillingbourne, which rises on the western slopes of Leith Hill and flows westwards to join the Wey to the south of Guildford, between Shalford and Peasmarsh.
The steep-sided valley accentuates entering Surrey, between vast masses termed the Lower Greensand Group (south), then down the more easterly valley on both sides (east and west). Reflecting the crumbly nature of this material which has readily eroded, the valley falls from about entering Surrey west of Farnham to lower at Tilford south-east of Farnham and changes from almost v-shaped to a more u-shaped alluvial plain.
The upper parts of the branch were the start of the upper River Blackwater's catchment. Geology for Engineers, F.G.H. Blyth, published by Arnold, third edition, 1952. cited with approval by http://weyriver.co.uk/theriver/wey_north_B.htm and Surrey Nature Partnership in its 2018 Wey Catchment Plan The Wey Stream capture this following cumulative flooding and deposition right up to around Aldershot. A vestige of this is that the upper Blackwater valley proper, north of today's wind gap, is not lower than (Tongham Pool) and of very low gradient. This transported distinctive gravels containing chert, to deposit them north of the gap in the chalky ridge at Farnham. The source rocks of the gravels prove the former extent of the river. Great erosion has occurred in the Wey down to Tilford, along the sinuous, multiple-anabranch Waverley Abbey stretch, through, what Blyth notes as, the "soft strata", of that landscape.
The northern streams drain fingers of a single east–west ridge of Greensand Ridge, their common names, again from east to west, are:
Of varying size, these are long, sandy hills south-east of the upper tip of the Devil's Punch Bowl: Gibbet Hill, Hindhead. One of the northern streams adjoins strips of woodland named Weydown Common and Weycombe.
The south sources are specifically: a wood-surrounded neighbourhood, Kingsley Green (formerly Marsh) in Fernhurst;Ordnance Survey: Surrey: Sheet: XLIV.SE, Revised: 1895 to 1896, Published: 1898
The Wey drains and passes Haslemere's western suburbs then Liphook, Bramshott (including Passfield), Standford and Lindford, and the large parish of Frensham. It combines with the north branch at Tilford, in which parish all three flows have large .
Notable tributaries of the south branch are Cooper's Stream and the River Slea.
During the seventeenth century, the river was made navigable to Guildford and extended in the eighteenth century to Godalming. The Basingstoke Canal and Wey and Arun Junction Canal were later connected to the river. The navigable sections are now owned by the National Trust.
Much of the upper reaches of the river are within the Surrey Hills Area of Outstanding Natural Beauty. The river passes through a variety of habitats including heathland, woodland and watermeadow, resulting in a diversity of wildlife. There are Sites of Special Scientific Interest (SSSI) and Nature reserve along the river.
A broad basin of drain steeply to the river so, as with the Mole, in its natural state, much of the were prone to regular flooding. This has been greatly reduced by flood alleviation measures, upstream lakes such as Frensham Great Pond and, inadvertently, the Wey navigations. The lowest urban areas of Godalming, Byfleet and Weybridge saw extensive flooding in the exceptional winter storms of 2013–14. Recap: Flood-hit communities prepare for further rainfall Surrey Advertiser Group. 12 February 2014. Retrieved 18 April 2014
Water quality of the River Wey in 2019:
Wey South
The Wey South branch stems from two main westward brooks, one now followed by the Portsmouth Direct Line, the other – with longer source brooks – following the Surrey/Sussex boundary, which combine at a point, heading west, where the line first comes as close as 97 metres to the boundary – in the east end of a park, next to one of its three river footbridges. These brooks are fed by six main streams. The farthest are the southern streams. These drain parallel, north, narrow vales between the northerly "fingers" or "ribs" of:
https://maps.nls.uk/geo/explore/#zoom=16&lat=51.07178&lon=-0.72304&layers=6&b=7
Chase Farm marking the furthest point south in [[Surrey]];Ordnance Survey: Surrey: Sheet: XLV.SW, Revised: 1895 to 1896, Published: 1898 and upper fishponds at Wades Marsh marking the Fernhurst/[[Lurgashall]] boundary (both in [[West Sussex]]), next to the summit of Ridge Hill (which is the furthest source).Ordnance Survey: Surrey: Sheet: XL.S, Revised: 1895 to 1896, Published: 1898
Combined river
From Tilford, the river runs through Elstead, Eashing, Godalming, Peasmarsh/Shalford, Guildford, Send, Old Woking, Pyrford, Byfleet, New Haw and forms the historically much more meandering border between Addlestone/Weybridge, today doing so most accurately between Hamm Court and Whittet's Ait respectively. Church of England current ecclesiastical parish boundaries old parish boundary approximate maps Vision of Britain: History of Parliament Trust; University of Portsmouth and Others. From Godalming the river is intertwined with the Wey and Godalming Navigations. The of the navigations' towpath is open to pedestrians. The river joins the Thames at a cascading channel off its Navigation Canal (above Thames Lock) between Addlestone and Weybridge and a weir-fed navigation east of the ait facing the main weir stream of Shepperton Lock.
Tributaries
The River Ock joins at Godalming, Cranleigh Waters and the River Tillingbourne at Shalford and the Hoe Stream at Woking.
History
The river has long been used as a source of power for mills, and many are recorded in the Domesday Book. Between the 17th and 19th centuries there were over 40 mills on the river and more on its tributaries. At various times they have been used for grinding grain, fulling wool, rolling oats, crushing cattle cake, leather dressing, paper production and gunpowder manufacture. Willey Mill, at Farnham, was still in use in 1953. Headley Mill is still in commercial operation. Guildford Town Mill, though no longer used for milling, still harnesses the power of the river to generate electricity.
Natural environment
Wey Valley is a term for the narrowing river basin of the River Wey before it empties into the River Thames.
Water quality
The Environment Agency measure water quality of the river systems in England. Each is given an overall ecological status, which may be one of five levels: high, good, moderate, poor and bad. There are several components that are used to determine this, including biological status, which looks at the quantity and varieties of , and fish. Chemical status, which compares the concentrations of various chemicals against known safe concentrations, is rated good or fail. Text was copied from this source, which is available under an Open Government Licence v3.0. © Crown copyright.
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Further reading
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