Display listing of nearby tsunami events
Sergey Soloviev studied this event in a trip to Spain in October 1988, and gives his findings in Soloviev et al. (Reference #2130). Weak tsunami waves were recorded by six tide gauges on the south-eastern shore of the Iberian Peninsula. He found the mechanism of this event similar to the earthquake and tsunami of 1954 in the same region. He concluded that the tsunami was "generated by a strong turbidity current caused by the powerful underwater landslide, that was caused by the earthquake on the steep underwater slope of Africa covered abundantly by loose sediments."
Tsunami caused by one or more major underwater slides also producing turbidity currents (Soloviev, r422).
Tide gauge records at Alicante are also available at the Instituto Geogrāfico nacional, Madrid. (reference #4139)
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