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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.
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Pages in category "Geography of the River Thames" The following 20 pages are in this category, out of 20 total. This list may not reflect recent changes. B.
River Thames catchment area. The Goring Gap is a topographical feature on the course of the River Thames.The Gap is located in southern England where the river, flowing from north to south, cuts through and crosses a line of chalk hills in a relatively narrow gap between the Chiltern Hills and the Berkshire Downs.
River Quaggy: 69 square miles (180 km 2) Tidal reach: Deptford Creek River Neckinger or the Neckinger Channel: Shad Thames: north Southwark: 0.8 miles (1.3 km) (about; longer old catchment drains to other surface and combined water conduits)
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.
In the upper reaches of the Thames, the river depth was raised by dams and in the lower reaches it was raised by embankments, so gradually most fords were lost. [1] At least one regular ford remains, at Duxford. Many of the present road bridges over the river are on the sites of earlier fords, ferries and wooden structures.