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The border of Europe and Asia is here defined as from the Kara Sea, along the Ural Mountains and Ural River to the Caspian Sea.While the crest of the Caucasus Mountains is the geographical border with Asia in the south, Georgia, and to a lesser extent Armenia and Azerbaijan, are politically and culturally often associated with Europe; rivers in these countries are therefore included.
The river gives its name to three informal areas: the Thames Valley, a region of England around the river between Oxford and West London; the Thames Gateway; and the greatly overlapping Thames Estuary around the tidal Thames to the east of London and including the waterway itself.
The lock has the deepest fall of all locks on the Thames at 8 ft 9in (2.69m) and is connected to a large island which is one of three at this point. The lock lies at the end of Church Lane in Sandford on Thames. Upstream from the lock, the main weir connects the second island to the opposite bank on the Kennington, Oxfordshire side. This is the ...
Just short of the Nore's easternmost point where it fades into the channels it has a notable point once marked by a lightship on the line where the estuary of the Thames nominally becomes the North Sea. A lit buoy today stands on this often map-marked divisor: between Havengore Creek in east Essex and Warden Point on the Isle of Sheppey in Kent.
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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 Thame / ˈ t eɪ m / is a river in Southern England. A tributary of the River Thames , the river runs generally south-westward for about 40 mi (64 km) from its source above the Buckinghamshire town of Aylesbury to the Thames in south-east Oxfordshire .
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.