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The Channel River was a prehistoric river flowing between England and France during periods of low sea level during the . Its tributaries included the river Rhine in modern-day Netherlands, the River Thames in modern-day England and other rivers. Over the last 12,000 years rising seas have covered its course, through what is now the English Channel.
A bathymetric study of the morphology of the current Channel floor in 2007 found evidence suggesting that the ridge was eroded by two 'megafloods' between 180,000 and 450,000 years ago. During periods of glaciation the British and the Fennoscandian ice sheets trapped water, preventing it from flowing north, and together with the land bridge to the south formed a glacial lake. The lake grew as the rivers continued to pour into it until it finally breached the southern ridge, creating what the paper called the 'Fleuve Manche', translating to Channel River, flowing through the vast shallow valley of the Channel Basin and into the Bay of Biscay.
This westward-flowing Channel River carried water not only from the rivers that currently enter the Channel (such as the Seine), but also from those that now drain into the southern North Sea, among them the Rhine, Meuse, Thames and Scheldt, making it larger than any river in modern-day Europe.
The erosion from two such breaches left a significant gap in the ridge, so when the ice melted and the seas rose, water covered the area, cutting Britain off. Since the last ice age, around 12,000 years ago, the current Channel formed, and the Strait of Dover is now a wide gap in the ridge, bordered by cliffs of between high on both the Kent and the Pas-de-Calais sides.
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