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Catchment Board
River boards were authorities who controlled land drainage, fisheries and river pollution and had other functions relating to rivers, streams and inland waters in England and Wales between 1950 and 1965. Background Prior to the 1930s, land drainage in the United Kingdom was regulated by the Statute of Sewers, passed by King Henry VIII in 1531, and several further acts which built upon that foundation. However, the administrative bodies with responsibility for managing the drainage of low-lying areas did not have sufficient resources to do this effectively. Complaints to the Ministry of Agriculture and Fisheries made during the 1920s by existing drainage boards and those who lived and worked in the areas they covered led to the government deciding that a thorough review of the situation should be carried out. A Royal Commission was set up, under the chairmanship of Lord Bledisloe, which produced a final report on 5 December 1927. The report described the existing laws as "vague an ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Drainage Basin
A drainage basin is an area of land where all flowing surface water converges to a single point, such as a river mouth, or flows into another body of water, such as a lake or ocean. A basin is separated from adjacent basins by a perimeter, the '' drainage divide'', made up of a succession of elevated features, such as ridges and hills. A basin may consist of smaller basins that merge at river confluences, forming a hierarchical pattern. Other terms for a drainage basin are catchment area, catchment basin, drainage area, river basin, water basin, and impluvium. In North America, they are commonly called a watershed, though in other English-speaking places, "watershed" is used only in its original sense, that of a drainage divide. In a closed drainage basin, or endorheic basin, the water converges to a single point inside the basin, known as a sink, which may be a permanent lake, a dry lake, or a point where surface water is lost underground. Drainage basins are similar ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lee Conservancy Catchment Board
The Lee Navigation is a canalised river incorporating the River Lea (also called the River Lee along the sections that are navigable). It flows from Hertford Castle Weir to the River Thames at Bow Creek; its first lock is Hertford Lock and its last Bow Locks. Name The Lee Navigation is named by Acts of Parliament and is so marked on Ordnance Survey maps. Constructed elements and human features are spelled Lee, such as the canal system and Lee Valley Park. The un-canalized river is spelled Lea, along with other natural features such as Lower Lea Valley. History The River Lea is a major tributary of the River Thames. It has a long association with navigation, as the marshes of Walthamstow have produced a dugout canoe from the Bronze Age and parts of a Saxon barge. According to the '' Anglo-Saxon Chronicle'', the river was used by Viking raiders, and King Alfred changed the level of the river to strand Guthrum and his fleet. In more peaceful times, it became important for ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Stour, Suffolk
The River Stour () is a river in East Anglia, England. It is long and forms most of the county boundary between Suffolk to the north, and Essex to the south. It rises in eastern Cambridgeshire, passes to the east of Haverhill, Suffolk, Haverhill, through Cavendish, Suffolk, England, Cavendish, Bures, Sudbury, Suffolk, Sudbury, Nayland, Stratford St Mary, Dedham, Essex, Dedham and flows through the Dedham Vale Area of Outstanding Natural Beauty. It becomes tidal just before Manningtree in Essex and joins the North Sea at Harwich. Etymology and usage The name is of ambiguous and disputed origin. On one theory, the name ''Stour'' derives from the Celtic ''sturr'' meaning "strong". However, the hydronym, river-name ''Stour'', common in England, does not occur at all in Wales; Crawford noted two tributaries of the Po River near Turin, spelled ''Stura''. In Germany the ''Stoer'' is a tributary of the River Elbe. According to ''Brewer's Britain and Ireland'' the ''Stour'' is pronounc ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Roding
The River Roding () rises at Molehill Green, Essex, England, then flows south through Essex and London and forms Barking Creek as it reaches the River Thames. Course The river leaves Molehill Green and passes through or near a group of eight or nine villages in Essex known collectively as the Rodings, as their names are 'Roding' prefixed with various different specific names (High, Margaret, Aythorpe etc.). After Chipping Ongar, the river flows under the M25 motorway by Passingford Bridge and Abridge. The river then runs between Loughton and Chigwell, where the Roding Valley Meadows make up the largest surviving area of traditionally managed river-valley habitat in Essex. This nature reserve consists of unimproved wet and dry hay meadows, rich with flora and fauna and bounded by thick hedgerows, scrubland, secondary woodland and tree plantation. The meadows stretch down to the M11 motorway and the Roding Valley tube station is situated close to the area, although Loughton or ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Ouse, Sussex
The Ouse ( ) is a 35 mile (56 kilometre) long river in the English county, counties of West Sussex, West and East Sussex. It rises near Lower Beeding in West Sussex, and flows eastwards and then southwards to reach the sea at Newhaven, East Sussex, Newhaven. It skirts Haywards Heath and passes through Lewes. It forms the main spine of an extensive network of smaller streams, of which the River Uck is the main tributary. As it nears the coast it passes through the Lewes and Laughton Levels, an area of flat, low-lying land that borders the river and another tributary, the Glynde Reach. It was a large tidal inlet at the time of the Domesday book in 1086, but over the following centuries, some attempts were made to reclaim some of the valley floor for agriculture, by building embankments, but the drainage was hampered by the buildup of a large shingle bar which formed across the mouth of the river by longshore drift. In 1539, a new channel for the entrance to the river was cut thro ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Cuckmere
The River Cuckmere rises near Heathfield in East Sussex, England on the southern slopes of the Weald. The name of the river probably comes from an Old English word meaning "fast-flowing", since it descends over 100 m (328 ft) in its initial four miles (6.4 km). It flows into the English Channel, and has the only undeveloped river mouth on the Sussex coast. Description The river has many tributaries at its upper end, the principal one being the River Bull; and its main channel begins at Hellingly. After crossing the Low Weald area of farmland, the Cuckmere cuts through the South Downs in its own valley. It reaches the English Channel at Cuckmere Haven, between Seaford and the Seven Sisters cliff face. The lower part of its course in the floodplain is marked by meandering. The Cuckmere Valley Nature Reserve is located in the lower estuary portion of the river. The valley is very important for nature conservation. It has been designated a Site of Special Scient ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Dee, Wales
The River Dee ( cy, Afon Dyfrdwy, la, Deva Fluvius) is a river in the United Kingdom. It flows through parts of both Wales and England, forming part of the border between the two countries. The river rises in Snowdonia, Wales, flows east via Chester, England, and discharges to the sea in an estuary between Wales and the Wirral Peninsula in England. It has a total length of . History The River Dee was the traditional boundary of the Kingdom of Gwynedd in Wales for centuries, possibly since its founding in the 5th century. It was recorded in the 13th century (in mainstream Middle English orthography, lacking the letters v and w) as ''flumen Dubr Duiu''; the name appears to derive from the Brythonic ''dēvā'': "River of the Goddess" or "Holy River". The river is personified as the war and fate goddess Aerfen. The river name inspired the name of Roman fortress ''Deva Victrix''. It is the only river in the UK to be subject to a Water Protection Zone along its whole length down ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Clwyd
The River Clwyd (Welsh: ''Afon Clwyd'') is a river in Wales that rises in the Clocaenog Forest () northwest of Corwen. Its total length is . It flows due south until, at Melin-y-wig, it veers north-eastwards, tracking the A494 and passing through Derwen, Llanelidan, Pwllglas and Llanfair Dyffryn Clwyd to Ruthin. Here it leaves the relatively narrow valley and enters a broad agricultural vale, the Vale of Clwyd (Welsh: ''Dyffryn Clwyd''). Just south of Denbigh, it is joined by the River Clywedog. This substantial tributary also has its source in the Clocaenog Forest but drains out to the east and north of the forest and passes through Cyffylliog, Bontuchel and Rhewl before its confluence with the main river. Then the Clwyd meanders northwards through the fertile Clwyd valley to St Asaph. Around north of St Asaph, the river is joined by a tributary as large as the main river, the River Elwy. In normal flows at low tide, the waters of these two rivers can be seen flowing sid ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Wampool
The River Wampool is a river flowing through north western Cumbria in England. It is in the ''Waver and Wampool'' (or ''Wampool and Waver'') catchment which includes the towns of Silloth and Wigton. The river is formed at Chalkfoot near East Curthwaite, above which it is known as Chalk Beck. This helps define the western edge of Inglewood Forest. Chalk Beck rises close to Wavergillhead and runs north, meeting Iron Gill and proceeding through a wooded clough to Chalkfoot. Later, the infant River Wampool is joined by Gill Beck at West Curthwaite and Whinnow Beck at Micklethwaite. The river continues northwards through Biglands, where it is joined by Bampton Beck and Wampool, towards Angerton, where it bends westwards, meeting Solway Firth at Anthorn. For much of its length the river forms the boundary between the parishes of Woodside to the west and Thursby and Aikton Aikton is a small village in the north of the English county of Cumbria. The nearest town is Wigton 3 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Waver
The River Waver is a river in Cumbria, England. The river rises at Wavergillhead (as Townthwaite Beck). It is fed by the northwards flowing Thornthwaite Beck and Pow Gill either side of Bolton Wood Lane. The "Little Waver", rising at Catlands Hill, joins at Waterside near Woodrow. The river then takes a northward course via Waverton and Waverbridge, both of which are named for the river, before turning sharply westward at Abbeytown. The river then goes north, running into Moricambe Bay, an inlet of the Solway Firth The Solway Firth ( gd, Tràchd Romhra) is a firth that forms part of the border between England and Scotland, between Cumbria (including the Solway Plain) and Dumfries and Galloway. It stretches from St Bees Head, just south of Whitehaven .... Waver, River {{England-river-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Kent
The River Kent is a short river in the county of Cumbria in England. It originates in hills surrounding Kentmere, and flows for around 20 miles (32 km) into the north of Morecambe Bay. The upper reaches and the western bank of the estuary are located within the boundaries of the Lake District National Park. The river flows in a generally north to south direction, passing through Kentmere, Staveley, Burneside, Kendal and Sedgwick. Near Sedgwick, the river passes through a rock gorge which produces a number of low waterfalls. This section is popular with kayakers as it offers high quality whitewater for several days after rain. The village of Arnside is situated on the east bank of the Kent estuary, just above Morecambe Bay, and a tidal bore known as the Arnside Bore forms in the estuary at this point on high spring tides. The river has been used as a source of power since at least the 13th century. In 1848, the construction of Kentmere Reservoir was completed, which was ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Weaver
The River Weaver is a river, navigable in its lower reaches, running in a curving route anti-clockwise across west Cheshire, northern England. Improvements to the river to make it navigable were authorised in 1720 and the work, which included eleven locks, was completed in 1732. An unusual clause in the enabling Act of Parliament stipulated that profits should be given to the County of Cheshire for the improvement of roads and bridges, but the navigation was not initially profitable, and it was 1775 before the first payments were made. Trade continued to rise, and by 1845, over £500,000 had been given to the county. The major trade was salt. The arrival of the Trent and Mersey Canal at Anderton in 1773 was detrimental to the salt trade at first, but ultimately beneficial, as salt was tipped down chutes from the canal into barges on the river navigation. Access to the river was improved in 1810 by the Weston Canal, which provided a link to Weston Point, where boats could reach ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sep2004.jpg "Click for more on -> River Wampool")
