The Nice tsunami of 1979 came on October 16. Two
tsunami
A tsunami ( ; from ja, 津波, lit=harbour wave, ) is a series of waves in a water body caused by the displacement of a large volume of water, generally in an ocean or a large lake. Earthquakes, volcanic eruptions and other underwater explo ...
s struck the coast near
Nice
Nice ( , ; Niçard: , classical norm, or , nonstandard, ; it, Nizza ; lij, Nissa; grc, Νίκαια; la, Nicaea) is the prefecture of the Alpes-Maritimes department in France. The Nice agglomeration extends far beyond the administrative c ...
, accompanied by a landslide at the
Nice Airport
Nice ( , ; Niçard: , classical norm, or , nonstandard, ; it, Nizza ; lij, Nissa; grc, Νίκαια; la, Nicaea) is the prefecture of the Alpes-Maritimes department in France. The Nice agglomeration extends far beyond the administrative c ...
, and an aseismic
submarine landslide
Submarine landslides are marine landslides that transport sediment across the continental shelf and into the deep ocean. A submarine landslide is initiated when the downwards driving stress (gravity and other factors) exceeds the resisting str ...
. The two waves struck the coast between the Italian border and the town of
Antibes
Antibes (, also , ; oc, label=Provençal dialect, Provençal, Antíbol) is a coastal city in the Alpes-Maritimes Departments of France, department of southeastern France, on the French Riviera, Côte d'Azur between Cannes and Nice.
The town of ...
(60 miles; 96 km).
[Allaby, M. (2004). A Chronology of Weather. Infobase Publishing.] They reached 3 m high near Nice and 3.5 m
at La Salis (Antibes) and decreased in amplitude from there.
Causes
The origin of these events has been a subject of academic and judicial debate. One hypothesis said that it was the landslide at the
Nice airport
Nice ( , ; Niçard: , classical norm, or , nonstandard, ; it, Nizza ; lij, Nissa; grc, Νίκαια; la, Nicaea) is the prefecture of the Alpes-Maritimes department in France. The Nice agglomeration extends far beyond the administrative c ...
; while the other stated that it was an underwater landslide.
[Seed, H. B. (1988). The landslide at the Port of Nice on October 16, 1979. Earthquake Engineering Research Center, University of California.]
A 0.15 km
3 slide took place off Nice airport while constructing the fill of the new airport, perhaps as a consequence of this work. This landslide would have caused the first tsunami. The material from this slide could have caused a submarine slide that would have caused the second tsunami.
In the second hypothesis, the major natural submarine landslide (~8.7 km
2) that occurred offshore Nice caused a tsunami which would have caused a landslide of the fill of the new airport. This landslide caused another tsunami.
Consequences
Casualty estimates range between 8
and 23. At the construction site, the collapsing fill killed seven people.
The tsunamis inundated a 20-mile section of the coast.
[Dudley, W. C., & Lee, M. (1998). Tsunami!. University of Hawaii Press.] The water travelled up to 150 m inland.
Eleven people were swept away in Nice and one in Antibes.
The airport works were finished, but this event forestalled the construction of a new port for Nice.
References
{{DEFAULTSORT:Nice tsunami (1979)
20th century in Nice
1979 natural disasters
Nice tsunami
1979 tsunamis
Nice tsunami