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The Metauro River
The story of a river begins with the source, generally on a
mountain, in the form of a rivulet, stream or springs of water fed
by glaciers, snow and rain.Our Metauro, for example, rises in the form
of a rivulet and springs of water that develop in two different areas: On the upper course of The Metauro there is a waterfall
at S. Angelo in Vado, called Cascata del Sasso, where it forms a lake;
there are also some rapids in Urbania and a dam on the affluent Candigliano
in Furlo Gorge.
Its regimen is torrential because it is irregular; in February
its flow is at its highest point, in August at its lowest.
The lower course of the river begins at Fossombrone, through
the alluvional plain formed by its debris, made of pebbles, of sandstones,
calcareous and flintstone rocks.
On the lower course it is possible to see bands and meanders
of the river too.
The Metauro flows into the Adriatic Sea.
Many centuries ago its mouth was a delta, now it is an estuary.
Because of the excessive excavation of pebbles, in fact, it can’t
deposit alluvional material any more.
The plants growing along its banks are white and black poplars
and above, in the mountaneous part, alders. In the plain water plants
may be found, like reeds and flints.
Some notes on the river
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