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London Stone, Yantlet Creek. The transition between the Thames Estuary and the North Sea has been located at various notional boundaries, including: [1] The Yantlet Line between the Crow Stone (London Stone) on the northern foreshore at Chalkwell, Westcliff-on-Sea and another London Stone off the Isle of Grain, to the south.
The River Thames (/ t ɛ m z / ⓘ TEMZ), known alternatively in parts as the River Isis, is a river that flows through southern England including London. At 215 miles (346 km), it is the longest river entirely in England and the second-longest in the United Kingdom , after the River Severn .
This is a list of rivers of England, organised geographically and taken anti-clockwise around the English coast where the various rivers discharge into the surrounding seas, from the Solway Firth on the Scottish border to the Welsh Dee on the Welsh border, and again from the Wye on the Welsh border anti-clockwise to the Tweed on the Scottish border.
A sketch map of some lost rivers "London Before the Houses", map of pre-urban London from 1884. [1] The position of a mouth of the Effra in the 13th century.. The subterranean or underground rivers of London are or were the direct or indirect tributaries of the upper estuary of the Thames (the Tideway) that were built over during the growth of the metropolis of London.
The original name of the river was the Granta and (unusually) its present name derives from the city of Cambridge (Old English: Grantebrycge) rather than the other way around: After the city's present name developed in Middle English, the river's name was backformed to match.
The Hogsmill River in Surrey and Greater London, England, is a small chalk stream tributary of the River Thames. It rises in Ewell and flows into the Thames at Kingston upon Thames on the lowest non-tidal reach, that above Teddington Lock. The river is 10 km (6 mi) long and has a catchment area of about 73 km 2 (28 sq mi). [1]
The River Rother flows for 35 miles (56 km) through the English counties of East Sussex and Kent. Its source is near Rotherfield in East Sussex, and its mouth is on Rye Bay, part of the English Channel. Prior to 1287, its mouth was further to the east at New Romney, but it changed its course after a great storm blocked its exit to the sea.
The River Neckinger is a reduced subterranean river that rises in Southwark and flows approximately 2.5 kilometres (1.6 miles) through south London to St Saviour's Dock where it enters the Thames. What remains of the river is enclosed and runs underground and most of its narrow catchment has been diverted into other combined and surface water ...