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Mont-Saint-Michel

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Mont-Saint-Michel

Mont-Saint-Michel (French pronunciation: [lə mɔ̃ sɛ̃ miʃɛl]; Norman: Mont Saint Miché; English: Saint Michael's Mount) is a tidal island and mainland commune in Normandy, France.

The island lies approximately one kilometre (one-half nautical mile) off France's north-western coast, at the mouth of the Couesnon River near Avranches and is 7 hectares (17 acres) in area. The mainland part of the commune is 393 hectares (971 acres) in area so that the total surface of the commune is 400 hectares (990 acres). As of 2019, the island has a population of 29.

The commune's position—on an island just a few hundred metres from land—made it accessible at low tide to the many pilgrims to its abbey, and defensible as the incoming tide stranded, drove off, or drowned threats on foot. The island remained unconquered during the Hundred Years' War. A small garrison fended off a full attack by the English in 1433. Louis XI recognised the benefits of its natural defence and turned it into a prison. The abbey was used regularly as a prison during the Ancien Régime.

Mont-Saint-Michel and its surrounding bay were inscribed on the UNESCO list of World Heritage Sites in 1979 for its unique aesthetic and importance as a Catholic site. It is visited by more than three million people each year, and is the most-visited tourist attraction in France outside of Paris. Over 60 buildings within the commune are protected as historical monuments.

Now a rocky tidal island, the mount 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, 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 mount has a circumference of about 960 m (3,150 ft) and its highest point is 92 m (302 ft) above sea level.

The tides vary greatly, at roughly 14 metres (46 ft) between highest and lowest 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 bridge and attempt the hazardous walk across the sands from the neighbouring coast.

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