
Based on the latest reconstruction of the famous ice age river system, Fleuve Manche, the scientists have calculated that its catchment area was similar to that of the Mississippi.
The Eurasian ice sheet was an enormous conveyor of ice that covered most of northern Europe some 23,000 years ago. Its extent was such that a skier could have traversed 4,500 km continuously across its expanse from the far southwestern isles in Britain to Franz Josef Land in the Siberian Arctic. Its existence had a massive and extremely hostile impact on Europe at the time.
This ice sheet alone lowered the global sea level by over 20 meters. As it melted and collapsed, it caused severe flooding across the continent, led to dramatic sea level rise, and diverted mega-rivers that raged on the continent. A new model investigating the retreat of this ice sheet and its many impacts has just been published in Quaternary Science Reviews.















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