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Wey Valley
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 catchment area of . Although it is the longest tributary of the Thames (if the Medway is excluded), its total average discharge is lower than that of the Kennet and 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 th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Waverley Abbey
Waverley Abbey was the first Cistercian abbey in England, founded in 1128 by William Giffard, the Bishop of Winchester. Located about southeast of Farnham, Surrey, it is situated on a flood-plain; surrounded by current and previous channels of the River Wey. It was damaged on more than one occasion by severe flooding, resulting in rebuilding in the 13th century. Despite being the first Cistercian abbey in England, and being motherhouse to several other abbeys, Waverley was "slenderly endowed" and its monks are recorded as having endured poverty and famine. The abbey was suppressed in 1536 as part of King Henry VIII's Dissolution of the Monasteries. Subsequently, largely demolished, its stone was reused in local buildings, likely including "Waverley Abbey House", which was built in 1723 in the northern portion of the former abbey precinct. Waverley Abbey House, the ruins of the abbey and the surrounding land are all part of a conservation area. The house is a Grade II* listed ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Weybridge
Weybridge () is a town in the Borough of Elmbridge in Surrey, England, around southwest of central London. The settlement is recorded as ''Waigebrugge'' and ''Weibrugge'' in the 7th century and the name derives from a crossing point of the River Wey, which flows into the River Thames to the north of the town centre. The earliest evidence of human activity is from the Bronze Age. During the Anglo-Saxon and medieval periods, Weybridge was held by Chertsey Abbey. In the 1530s, Henry VIII constructed Oatlands Palace to the north of the town centre, which he intended to be the residence of his fourth wife, Anne of Cleves. He married Catherine Howard there in July 1540 and the palace remained a royal residence until the Civil War. The buildings were demolished in the early 1650s and a new mansion, Oatlands House, was constructed to the east of Weybridge later the same century. Prince Frederick, Duke of York and Albany owned the mansion in the 18th century. The town began to ex ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tributary
A tributary, or affluent, is a stream or river that flows into a larger stream or main stem (or parent) river or a lake. A tributary does not flow directly into a sea or ocean. Tributaries and the main stem river drain the surrounding drainage basin of its surface water and groundwater, leading the water out into an ocean. The Irtysh is a chief tributary of the Ob river and is also the longest tributary river in the world with a length of . The Madeira River is the largest tributary river by volume in the world with an average discharge of . A confluence, where two or more bodies of water meet, usually refers to the joining of tributaries. The opposite to a tributary is a distributary, a river or stream that branches off from and flows away from the main stream. PhysicalGeography.net, Michael Pidwirny & S ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Ock, Surrey
The River Ock is a tributary of the River Wey in Surrey, England. Course The river has two great sources in the west of Hambledon, Surrey, Hambledon and two similar sources in the east of the parish of Witley. The coalescence is north of a zone of gently north-sloping land forming Wheelerstreet, Witley#Enton, Enton Green and the little manor of Tuesley. For centuries the latter comprised a very modest house and farmstead, dwarfed by the adjacent Busbridge Park, the stream of which drains Busbridge#Busbridge Lakes, Busbridge Lakes, the former mid and lower fish ponds, the upper one having been drained on becoming part of that stream. The resulting Ock passes through Ockford, sometimes considered the east of Ockford Ridge, parts of Godalming, before flowing into the Wey in the town centre. The Portsmouth Main Line railway follows much of the course. Watermills The Old Mill in Godalming, originally known as Hatch Mill, made use of the force and speed of the multi-hill-draining ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cranleigh Waters
The Cranleigh Waters or Bramley Wey is a tributary of the River Wey in Surrey. Course The Cranleigh Waters or Bramley Wey rises at a source close to the sources of two tributaries, the Thornhurst Brook and Coneyhurst Gill in the rural north of Cranleigh, each flowing initially southwestwards to Vachery Pond, before turning to run northwards as the border of Wonersh and Bramley to meet the Wey at Shalford.OS Map of English Heritage Listed Buildings and Parks and Gardens Database From the Vachery Pond to the Wey, Cranleigh Waters is closely paralleled by the disused , which crosses the river at Gosden Aqueduct. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Tillingbourne
The River Tillingbourne (also known as the Tilling Bourne) runs along the south side of the North Downs and joins the River Wey at Guildford. Its source is a mile south of Tilling Springs to the north of Leith Hill at and it runs through Friday Street, Abinger Hammer, Gomshall, Shere, Albury, Chilworth and Shalford. The source is a semi-natural uninhabited area. The catchment is situated on sandstone which has a low rate of weathering. The Tillingbourne is in length. Geography The Tillingbourne initially flows northward for down the northern slopes of Leith Hill over a series of weirs and cascades, before turning west to run for through Abinger Hammer and Chilworth towards the River Wey at Shalford. The river is classified as a subsequent stream, since its course is determined by the direction of the stratum of softer rock for the majority of its length. The river has four principal tributaries: the Friday Street stream joins at Wotton House; the Holmbury St Mary str ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Slea, Hampshire
The River Slea is a tributary of the south branch of the River Wey in Hampshire. Course The river flows east from the confluence of the Kingsley and the longer Oakhanger streams at Kingsley Mill, through the village of Sleaford until it meets the Wey just north of Brockford Bridge. The section between Kingsley Mill and Sleaford is also known as the Oxney Stream. The Slea's main tributary is the Oxney Moss which rises on the west side of Bordon and joins at Sleaford. 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 invertebrates, angiosperm Flowering plants are plants that bear flowers and fruits, and form the clade Angiospermae (), commonly called angiosperms. The term "angiosperm" i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Oxney Stream
The River Slea is a tributary of the south branch of the River Wey in Hampshire. Course The river flows east from the confluence of the Kingsley and the longer Oakhanger streams at Kingsley Mill, through the village of Sleaford until it meets the Wey just north of Brockford Bridge. The section between Kingsley Mill and Sleaford is also known as the Oxney Stream. The Slea's main tributary is the Oxney Moss which rises on the west side of Bordon and joins at Sleaford. 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 invertebrates, angiosperm Flowering plants are plants that bear flowers and fruits, and form the clade Angiospermae (), commonly called angiosperms. The term "angiosperm" i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kingsley Stream
Kingsley Stream is a tributary of the River Slea that lies in Hampshire, England England is a country that is part of the United Kingdom. It shares land borders with Wales to its west and Scotland to its north. The Irish Sea lies northwest and the Celtic Sea to the southwest. It is separated from continental Europe b .... It joins the Oakhanger Stream by Kingsley Mill, south of the village. It is regarded by the Environment Agency as the headwaters of the Slea. References Rivers of Hampshire 1Kingsley {{England-river-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Oakhanger Stream
Oakhanger Stream is a tributary of the River Slea, Hampshire, River Slea that lies in Hampshire, England. Course The source is at Well Head, at the foot of Noar Hill, to the south of Selborne. The initial section towards Selborne is known as the Well Head Stream, the route was diverted in 1894 to provide a supply of water to the village in memory of Gilbert White. At Dorton, on the north side of Selborne, it is joined by the Gracious Street Stream. From Selborne, now known as the Oakhanger Stream, it passes through the village of Oakhanger, Hampshire, Oakhanger then skirts the east side of Shortheath Common and on towards Kingsley Mill where it joins with the Kingsley Stream to form the Rver Slea. Watermills There were, at least, two corn mills on the Oakhanger Stream, the Old Mill in Selborne, a Grade II listed building now used as a private residence, and Dorton Mill, midway between Selborne and Oakhanger, of which no trace is now visible. Water quality The Environment Agency ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Thames Basin
The River Thames ( ), known alternatively in parts as the River Isis, is a river that flows through southern England including London. At , it is the longest river entirely in England and the second-longest in the United Kingdom, after the River Severn. The river rises at Thames Head in Gloucestershire, and flows into the North Sea near Tilbury, Essex and Gravesend, Kent, via the Thames Estuary. From the west it flows through Oxford (where it is sometimes called the Isis), Reading, Henley-on-Thames and Windsor. The Thames also drains the whole of Greater London. In August 2022, the source of the river moved five miles to beyond Somerford Keynes due to the heatwave in July 2022. The lower reaches of the river are called the Tideway, derived from its long tidal reach up to Teddington Lock. Its tidal section includes most of its London stretch and has a rise and fall of . From Oxford to the Estuary the Thames drops by 55 metres. Running through some of the drier parts of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Thames
The River Thames ( ), known alternatively in parts as the The Isis, River Isis, is a river that flows through southern England including London. At , it is the longest river entirely in England and the Longest rivers of the United Kingdom, second-longest in the United Kingdom, after the River Severn. The river rises at Thames Head in Gloucestershire, and flows into the North Sea near Tilbury, Essex and Gravesend, Kent, via the Thames Estuary. From the west it flows through Oxford (where it is sometimes called the Isis), Reading, Berkshire, Reading, Henley-on-Thames and Windsor, Berkshire, Windsor. The Thames also drains the whole of Greater London. In August 2022, the source of the river moved five miles to beyond Somerford Keynes due to the heatwave in July 2022. The lower reaches of the river are called the Tideway, derived from its long tidal reach up to Teddington Lock. Its tidal section includes most of its London stretch and has a rise and fall of . From Oxford to th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
_by_Lewis_Pinhorn_Wood.jpg "Click for more on -> River Tillingbourne")
