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 Rheinfall in 
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The Rhine Falls (Rheinfall in German) is the largest plain waterfall in
Europe.

The falls are located on the Upper Rhine between the municipalities of
Neuhausen am Rheinfall and Laufen-Uhwiesen, near the town of Schaffhausen
in northern Switzerland, between the cantons of Schaffhausen and Zürich.
They are 150 m (450 ft) wide and 23 m (75 ft) high. In the winter months,
the average water flow is 250 m³/s, while in the summer, the average water
flow is 700 m³/s. The highest flow ever measured was 1,250 m³/s in 1965;
and the lowest, 95 m³/s in 1921.

The falls cannot be climbed by fish, except by eels that are able to worm
their way up over the rocks.

The Rhine Falls were formed in the last ice age, approximately 14,000 to
17,000 years ago, by erosion- resistant rocks narrowing the riverbed. The
first glacial advances created today's landforms approximately 500,000
years ago. Up to the end of the Wolstonian Stage approximately 132,000
years ago, the Rhine flowed westwards from Schaffhausen past Klettgau. This
earlier riverbed later filled up with gravel.

K.Raman

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