Sunday, November 18, 2007
The Thames is a river flowing through southern England, and one of the major waterways in England. While perhaps best known because its lower reaches flow through central London, the river flows through several other significant towns and cities, including Oxford, Reading and Windsor.
The river gives its name to the Thames Valley, a region of England centred around the river between Oxford and West London, and the Thames Gateway, the area centred around the tidal Thames and the Thames Estuary to the east of London.
History
Until around half a million years ago, the Thames flowed on its existing course through what is now Oxfordshire, before turning to the north east through Hertfordshire and East Anglia and reaching North Sea near Ipswich. At the end of the ice age, the ice started to melt and huge amounts of water entered this river system, causing it to cut down a new route through the chalk at the site of the Goring Gap, near the Oxfordshire village of Goring-On-Thames between Oxford and Reading. This created a new river route flowing down through Berkshire and on into London.
At the height of the last ice age around 12000 years ago, Britain was connected to mainland Europe via a large expanse of land known as Doggerland. At this time, the Thames was much larger than it is today, with its source rising much further west in present-day Wales. The river's course continued out into Doggerland, where it met the Rhine. Thus the two rivers were at one time part of the same river system.
Geological history
The Thames provided the major highway between London and Westminster in the 16th and 17th centuries. The clannish guild of watermen ferried Londoners from landing to landing and tolerated no outside interference.
The River Thames has frozen over in cold weather throughout history. One of the earliest accounts of the Thames freezing over comes from A.D. 250 when it was frozen hard for nine weeks. Hubert Lamb and other historians have found that the Thames froze in the years AD 923, AD 998, and for seven weeks in 1061. It has also completely frozen over during these severe winters of (paradoxically) the Medieval Warm Period: 1149 - 1150, 1204 - 1205, 1269 - 1270, 1281 - 1282, 1309 - 1310, 1407 - 1408, 1409 - 1410, 1434 - 1435, early 1506, 1513 - 1514, 1516 - 1517, and 1536 - 1537. (12 times in total)
Between 1400 and the nineteenth century there were a total of 23 documented winters in which the Thames froze over at London during a period that became known as the Little Ice Age. This led to the first Frost Fair in 1607, complete with a tent city set up on the river itself and offering a number of amusements, including ice bowling. After temperatures began to rise again, starting in 1814, the river has never frozen over completely. The building of a new London Bridge in 1825 may also have been a factor; the new bridge had fewer pillars than the old, so allowing the river to flow more freely, thus preventing it from flowing slowly enough to freeze in cold winters.
Human history
The river's name appears always to have been pronounced with a simple "t" at the beginning; the Middle English spelling was typically Temese and Celtic Tamesis. The "th" lends an air of Greek to the name and was added during the Renaissance, possibly to reflect or support a belief that the name was derived from River Thyamis in the Epirus region of Greece, whence early Celtic tribes are thought to have migrated. However, most scholars now believe Temese and Tamesis come from Celtic (Brythonic) Tamesa, possibly meaning 'the dark one'. The modern Welsh name for the river which may stem from this earlier tradition is Tafwys.
Indirect evidence for the antiquity of the name 'Thames' is provided by a Roman potsherd found at Oxford, bearing the inscription Tamesubugus fecit (Tamesubugus made this). It is believed that Tamesubugus's name was derived from that of the river.
Origin of the name
Geography
The Thames has a length of 346 km (215 miles). Its usually quoted source is at Thames Head (at grid reference ST980994), about a mile north of the village of Kemble and near the town of Cirencester, in the Cotswolds. However, Seven Springs near Cheltenham, where the river Churn rises, is also sometimes quoted as the Thames' source, as this location is furthest from the mouth both in distance along its course and as the crow flies. The springs at Seven Springs also flow throughout the year, while those at Thames Head are only seasonal.
The Thames flows through Ashton Keynes, Cricklade, Lechlade, Oxford, Abingdon, Wallingford, Goring-On-Thames, Reading, Henley-on-Thames, Marlow, Maidenhead, Windsor, Eton, Staines and Weybridge, before entering the Greater London area.
From the outskirts of Greater London, the river passes Hampton Court, Kingston, Teddington, Twickenham, Richmond (with the famous view of the Thames from Richmond Hill), Syon House and Kew before flowing through central London. In central London, the river forms one of the principal axes of the city, from the Palace of Westminster to the Tower of London and was the southern boundary of the mediaeval city.
Once clear of central London, the river passes between Greenwich and the Isle of Dogs, before flowing through the Thames Barrier, which protects central London from flooding in the event of storm surges. Below the barrier, the river passes Dartford, Tilbury and Gravesend before entering the Thames Estuary near Southend-on-Sea.
Course of the river
The whole of the river drains a catchment area of some 4,994 square miles (12,935 km²) or 5,924 square miles (15,343 km²) if the River Medway is included as a tributary.
Catchment area and discharge
Innumerable brooks, canals and rivers, within an area of 3,841 square miles (9,948 square km), combine to form 38 main tributaries feeding the Thames between its source and Teddington. These include the rivers Churn, Leach, Cole, Coln, Windrush, Evenlode, Cherwell, Ock, Thame, Pang, Kennet, Loddon, Colne, Wey and Mole.
Between Maidenhead and Windsor, the Thames supports an artificial secondary channel, known as the Jubilee River, for flood relief purposes.
More than half the rain that falls on this catchment is lost to evaporation and plant growth. The remainder provides the water resource that has to be shared between river flows, to support the natural environment and the community needs for water supplies to homes, industry and agriculture. During heavy rainfall events the Thames occasionally receives raw sewage discharge due to sanitary sewer overflow.
The non-tidal section
About 55 miles from the sea, at Teddington, the river begins to exhibit tidal activity from the North Sea. This tidal stretch of the river is known as "the Tideway". London was reputedly made capital of Roman Britain at the spot where the tides reached in AD 43 but this spot has moved up river, in the 2000 years since then, because of the glacial rebound effect. At London, the water is slightly brackish with sea salt. Below Teddington, the principal tributaries include the rivers Brent, Wandle, Effra, Westbourne, Fleet, Ravensbourne (the final part of which is called Deptford Creek), Lea, Roding, Darent and Ingrebourne.
The average discharge of the Thames grows up to approximately 66 m³/s at the end of its non-tidal section, at Kingston upon Thames, a figure which is exceeded by some other British rivers (e.g., the Severn and the Tay). Indeed, if the Thames were not a tidal river, its average discharge in the centre of London would be somewhere between 80 and 100 m³/s, and the Thames would look like a small river, not the large river we can see today by Westminster, the Houses of Parliament or the City.
Some low-lying areas beside the tidal section of the Thames are liable to regular flooding at spring tides. However, in recent years, the flooding has been occurring more frequently at unusual times. One such example exists at Chiswick Lane South in London's W4 postal district, where the river now bursts its banks almost daily between March and September.
The tidal section
The Thames is navigable from the estuary as far as Lechlade in Gloucestershire. Between the sea and Teddington Lock, the river forms part of the Port of London and navigation is administered by the Port of London Authority. From Teddington Lock to the head of navigation, the navigation authority is the Environment Agency.
The river is navigable to large ocean-going ships as far as the Pool of London and London Bridge. Today little commercial traffic passes above the docks at Tilbury and central London sees only the occasional visiting cruise ship or warship, moored alongside HMS Belfast and a few smaller aggregate or refuse vessels, operating from wharves in the west of London. Both the tidal river through London and the non-tidal river upstream are intensively used for leisure navigation.
There are 45 locks on the River Thames. See Locks on the River Thames for a full list of all locks.
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