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The Malpasset Dam was an arch dam (convex surface facing upstream) on the Reyran River, north of
Fréjus Fréjus (; ) is a commune in the Var department in the Provence-Alpes-Côte d'Azur region in Southeastern France. In 2019, it had a population of 54,458. It neighbours Saint-Raphaël, effectively forming one urban agglomeration. The north of ...
on the
French Riviera The French Riviera (known in French as the ; oc, Còsta d'Azur ; literal translation " Azure Coast") is the Mediterranean coastline of the southeast corner of France. There is no official boundary, but it is usually considered to extend fro ...
. It collapsed on 2 December 1959, killing 423 people in the resulting flood. The breach was caused by a tectonic fault in the impermeable rock base, which had been inadequately surveyed. Nearby road-building works, using explosives, may also have contributed to the disaster.


Construction

The dam was a doubly curved equal angle arch type with variable radius. It was built to supply drinking and irrigation water for the region. Construction began in April 1952 and was finished in 1954. Another source reports that construction began as early as 1941. Delays due to lack of funding and labor strikes interrupted construction a few times. The project was led by well-known French engineer André Coyne. Construction cost 580 million francs (by 1955 prices), and was funded and owned by Var département. Concurrent with the dam construction, the
A8 autoroute The A8 autoroute, also known as La Provençale, is a -long highway in France that runs between Aix-en-Provence and the A7 to the Côte d'Azur. Route The A8 is an extension of the A7 starting to the west of Aix-en-Provence at La Fare-les-Olivi ...
was also being built further down the course of the Reyran from the dam location. The dam was supposed to regulate the rate-of-flow of the river that it was near and to store 50 million cubic metres of water for agriculture, and domestic use and for the tourism sector of the area. The dam was 222 metres in width, 66 metres high, and had a thickness of 6.78 metres at the base and 1.5 metres at the rim.


Disaster

, native_name_lang = fr , english_name = , time = 21:13 , timezone = CET , duration = , date = , venue = , location = , coordinates = , also_known_as = , type = Dam failure , motivation = , theme = , cause = Excess water level due to heavy rainfall , first_reporter = , filmed_by = , outcome = , casualties1 = , casualties2 = , casualties3 = , reported deaths = 423 , reported injuries = 83 , reported missing = , reported property damage = 425 million euros of 2010 , burial = , displaced = , inquiries = , inquest = , coroner = , arrests = , suspects = , accused = , convicted = , charges = , trial = , verdict = , convictions = , sentence = , litigation = , url = , website = , notes = Signs of an imminent collapse began in November 1959: a "trickle of clear water observed high on the right ide and then cracks noticed later in the month in the concrete apron at the dam toe. The dam was breached at 21:13 on December 2, 1959. The break was partially due to rainfall and thus the rising level of water; by noon on 2 December 1959 the reservoir had reached its maximum level. The guardian André Ferro asked for permission to release the excess water and was denied the ability to do so until 6pm of that day. By then, the amount of water was so high that it took three hours to release only a few centimetres of water. The entire wall then collapsed with only a few blocks remaining on the right bank. Pieces of the dam are still scattered throughout the area. The breach created a massive dam-break wave, or wall of water, high and moving at , destroying two small villages, Malpasset and Bozon, the highway construction site, and in 20 minutes, still standing high, reaching Fréjus. The water was recorded traveling at speeds up to with large chunks of the concrete wall some weighing up to . Various small roads and railroad tracks were also destroyed, water flooding the western half of Fréjus and finally reaching the sea. It was reported that the death toll of the dam breach was 423, with 135 children under the age of 15, 15 minors between 15 and 21 years old, 134 men, 112 women, and 27 individuals who were never identified. Additionally, 79 children were orphaned and 83 people were injured. Other damage included 155 buildings destroyed, 796 buildings damaged, and destroyed, the amount of destruction totaling about 425 million euros in 2010 terms. The damage amounted to an equivalent total of US$68 million. The event also ushered in the practice of posthumous marriage in France for civilians as many women who lost their fiancés were granted the right to marry them after death. Some 1959 postage stamps had a flood surcharge imprinted on them, to raise money for flood victims.


Cause

Geological and hydrological studies were conducted in 1946 and the dam location was considered suitable. Due to lack of proper funding, however, the geological study of the region was not thorough. The
lithology The lithology of a rock unit is a description of its physical characteristics visible at outcrop, in hand or core samples, or with low magnification microscopy. Physical characteristics include colour, texture, grain size, and composition. Lit ...
underlying the dam is a metamorphic rock called gneiss. This rock type is known to be relatively
impermeable Permeability, permeable, and semipermeable may refer to: Chemistry *Semipermeable membrane, a membrane which will allow certain molecules or ions to pass through it by diffusion *Vascular permeability, the movement of fluids and molecules betwe ...
, meaning that there is no significant groundwater flow within the rock unit, and it does not allow water to penetrate the ground. On the right side (looking down the river), was also rock, and a concrete wing wall was constructed to connect the wall to the ground. A
tectonic fault In geology, a fault is a Fracture (geology), planar fracture or discontinuity in a volume of Rock (geology), rock across which there has been significant displacement as a result of rock-mass movements. Large faults within Earth's crust (geolo ...
was later found as the most likely cause of the disaster. Other factors contributed as well; the water pressure was aimed diagonally towards the dam wall, and was not found initially. As a consequence, water collected under a wall and was unable to escape through the ground due to the impermeability of the gneiss rock underneath the dam. Finally, another theory quotes a source stating that explosions during building of the highway might have caused shifting of the rock base of the dam. Weeks before the breach, some cracking noises were heard, but they were not examined. It is not clear when the cracking noises started. The right side of the dam had some leaks in November 1959. Between November 19 and December 2, there was of rainfall, and in 24 hours before the breach. The water level in the dam was only away from the edge. Rain continued, and the dam guardian wanted to open the discharge valves, but the authorities refused, claiming the highway construction site was in danger of flooding. Five hours before the breach, at 18:00 hours, the water release valves were opened, but with a discharge rate of 40 m³/s, it was not enough to empty the reservoir in time. Until the Malpasset incident, only four other incidents of arch-type dam breaches were recorded: * Manitou dam, Manitou Springs, Colorado, 1924 at *
Moyie Dam Moyie Dam is a dam on the Moyie River in Boundary County, Idaho. The current high concrete gravity dam was built in 1950, and is owned and operated by the city of Bonners Ferry, Idaho. The city acquired its own hydroelectric facilities in 1921 ...
(the Eileen Dam),
Moyie Springs Moyie Springs is a city in Boundary County, Idaho, United States. The population was 718 at the 2010 census. Geography Moyie Springs is located at (48.724599, -116.193585). According to the United States Census Bureau, the city has a total ar ...
, Idaho, 1925 at * Lake Lanier, North Carolina, 1926 * Purisima dam, California, 1930


See also

*
Vega de Tera disaster The Vega de Tera disaster, (also known as the Ribadelago disaster 'Catástrofe de Ribadelago'' was a flood that occurred on the early morning of January 9, 1959 in the Province of Zamora, Spain. The flood was caused by the failure of a dam, rel ...
– Dam failure in Spain that same year * List of natural disasters by death toll – Floods and Landslides *
List of hydroelectric power station failures This is a list of major hydroelectric power station failures due to damage to a hydroelectric power station or its connections. Every generating station trips from time to time due to minor defects and can usually be restarted when the defect h ...
* List of wars and disasters by death toll – Flood disasters * Vajont Dam * St. Francis Dam


References

* J. Bellier, Le barrage de Malpasset, 1967 * Max Herzog, Elementare Talsperrenstatik, 1998 * Max Herzog, Bautechnik 67 Heft 12, 1990


External links


Cracking of dams

Website dedicated to the disaster of Malpasset
{{authority control Dams in France Reservoirs in France Buildings and structures in Var (department) 1959 disasters in France Man-made disasters in France Arch dams 1959 in France Dams completed in 1954 Floods in France Landforms of Provence-Alpes-Côte d'Azur 1954 establishments in France 1959 disestablishments in France Dam failures in Europe