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The English Channel breaches the symmetry of the basin on its northern side, interrupting the completeness of the concentric zones. The basin of the Seine presents no striking relief contrasts.
Within 30 miles of its source the river is already below 800 feet, and at Paris, 227 miles from its mouth, it is only 80 feet above sea level.
Winter floods are rarely dangerous, but in January 1910 exceptionally heavy rainfall caused the river to rise above 28 feet at Paris, flooding the extensive low-lying quarters along its ancient meander loop (the Marais).
To match this high level it is necessary to go back to February 1658; but in January 1924 and also in January 1955 the river again rose to more than 23 feet in Paris.
The water of the Seine is an important resource for the riverine population.
The broad estuary opens rapidly and extends for 16 miles below Tancarville to Le Havre; it experiences the phenomenon of the tidal bore, which is known as the From its source to Paris, the Seine traverses concentric belts of successively younger sedimentary rocks, infilling a structural basin, the centre of which is occupied by the limestone platforms of the Île-de-France immediately surrounding Paris.
The river is 485 miles (780 kilometres) long and with its tributaries drains an area of about 30,400 square miles (78,700 square kilometres).
It is one of Europe’s great historic rivers, and its drainage network carries most of the French inland waterway traffic.
Since the early Middle Ages it has been above all the river of The Seine rises at 1,545 feet (471 metres) above sea level on the Mont Tasselot in the Côte d’Or region of Burgundy but is still only a small stream when it traverses porous limestone country beyond Châtillon.
Flowing northwest from Burgundy, it enters Champagne above Troyes and traverses the dry chalk plateau of Champagne in a well-defined trench.
As it enters Paris, it is joined by its great tributary the Marne on the right, and, after traversing the metropolis, it receives the Oise, also on the right.