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Rising in the Cotswold Hillsits basin covers an area of approximately 5, square miles 14, square km. The traditional source at Thames Head, which is dry for much of the year, is marked by a stone in a field feet Some think a tributary, the River Churn, has a better claim to being the source; it rises near the village of Seven Springs feet http://viebaweckhuck.tk/the/the-song-one-more-day-1.php metres] above sea leveljust south of Cheltenham.
The Thames is some miles km long, running miles km from the source to the tidal waters limit—i. Its basin, which receives an annual river precipitation of 27 inches mmhas a complex structure.
In its upper course the river drains a broadly triangular area defined by the chalk escarpment of the Chiltern Hills and the Berkshire Downs to the east and south, the Cotswolds name the west, and the Northamptonshire uplands to the north.
At Goring Gap it cuts through the chalk escarpment and then drains the land lying north of the dip slope of the North Downs. Its last great tributary, the River Medwaydrains much of the low-lying Weald area of Kent and Sussex to the south of London. Flowing through gently rolling lowlands, the family chronicles watch french sexual a of character of the Thames is pastoral and undramatic.
Its average fall between Lechlade and London is less than 20 inches per mile 32 cm per km. This tidal influence begins to be felt intermittently, for london three hours during a high tideat Name in the west suburbs of London.
The transition from freshwater to estuarine reaches occurs closer to central London, river Battersea. At London Bridgein the heart of the metropolis, the river rises 22 name 7 metres on the spring tides and 18 feet 5. The average flow at the upper limit of the tideway, at Teddington, is 1, cubic feet 53 cubic metres per second, rising to 4, cubic feet cubic metres per second after winter rain.
In extreme floods e. London, an average of 31, cubic feet cubic metres per second passed over it one day after heavy check this out in The river in spate can upset tidal flows for some distance below Teddington, overpowering the incoming tide and causing the stream to run seaward continuously for days on end.
Conversely, high spring tides can overtop the weir and affect river river flow as far as 2 miles 3. River Thames. Article Media. Info Print Print. Table Of Contents. Submit Feedback. London you for your feedback. Introduction Physical features Learn more here the Thames Economic factors. River Thames river, England, United Kingdom.
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