Le Mont-Saint-Michel is an island commune in Normandy, France. It is located about one kilometre (0.6 miles) off the country’s northwestern coast, at the mouth of the Couesnon River near Avranches and is 100 hectares (247 acres) in size. As of 2009, the island has a population of 44.
The island has held strategic fortifications since ancient times and since the 8th century AD has been the seat of the monasteryfrom which it draws its name. The structural composition of the town exemplifies the feudal society that constructed it: on top, God, the abbey and monastery; below, the great halls; then stores and housing; and at the bottom, outside the walls, houses for fishermen and farmers.
The commune’s position — on an island just 600 metres from land — made it accessible at low tide to the many pilgrims to its abbey, but defensible as an incoming tide stranded, drove off, or drowned would-be assailants. The Mont remained unconquered during the Hundred Years’ War; a small garrison fended off a full attack by the English in 1433. The reverse benefits of its natural defence were not lost on Louis XI, who turned the Mont into a prison. Thereafter the abbey began to be used more regularly as a jail during the Ancien Régime.
One of France‘s most recognizable landmarks, visited by more than 3 million people each year, Mont Saint-Michel and its bay are on the UNESCO list of World Heritage Sites. Over 60 buildings within the commune are protected in France as monuments historiques. Geography Formation
Now a rocky tidal island, the Mont occupied dry land in prehistoric times. As sea levels rose, erosion reshaped the coastal landscape, and several outcrops of granite emerged in the bay, having resisted the wear and tear of the ocean better than the surrounding rocks. These included Lillemer, the Mont-Dol, Tombelaine (the island just to the north), and Mont Tombe, later called Mont Saint-Michel.
Mont Saint-Michel consists of leucogranite, which solidified from an underground intrusion of molten magma about 525 million years ago, during the Cambrian period, as one of the younger parts of the Mancellian granitic batholith. (Early studies of Mont Saint-Michel by French geologists sometimes describe the leucogranite of the Mont as “granulite”, but this granitic meaning of granulite is now obsolete).
The Mont has a circumference of about 960 metres (3,150 ft) and its highest point is 92 metres (302 ft) above sea level. Tides
The tides can vary greatly, at roughly 14 metres (46 ft) between high and low water marks. Popularly nicknamed “St. Michael in peril of the sea” by medieval pilgrims making their way across the flats, the mount can still pose dangers for visitors who avoid the causeway and attempt the hazardous walk across the sands from the neighbouring coast.
Polderisation and occasional flooding have created salt marsh meadows that were found to be ideally suited to grazing sheep. The well-flavoured meat that results from the diet of the sheep in the pré salé (salt meadow) makes agneau de pré-salé (salt meadow lamb), a local specialty that may be found on the menus of restaurants that depend on income from the many visitors to the mount. Tidal island
The connection between Mont Saint-Michel and the mainland has changed over the centuries. Previously connected by a tidal causeway (a path uncovered only at low tide), this was converted into a raised (permanently dry) causeway in 1879, preventing the tide from scouring the silt around the mount. The coastal flats have also been polderised to create pastureland, decreasing the distance between the shore and the island, and the Couesnon River has been canalised, reducing the dispersion of the flow of water. These factors all encouraged silting-up of the bay.
On 16 June 2006, the French prime minister and regional authorities announced a €164 million project (Projet Mont-Saint-Michel) to build a hydraulic dam using the waters of the river Couesnon and the tides to help remove the accumulated silt, and to make Mont Saint-Michel an island again.
The construction of the dam began in 2009. The project also includes the removal of the causeway and its visitor car park. Since 28 April 2012 the new car park on the mainland has been located 2.5 kilometres (1.6 miles) from the island. Visitors can walk or use shuttles to cross the causeway.
On 22 July 2014 the new bridge by architect Dietmar Feichtinger was opened to the public. The light bridge allows the waters to flow freely around the island and improves the efficiency of the now operational dam. The project which cost €209 million was officially opened by President François Hollande.
On rare occasions tidal circumstances produce an extremely high ‘supertide’. The new bridge was completely submerged on 21 March 2015, by the highest sea level for at least 18 years, as crowds gathered to snap photos.