ID | 111 |
Region | M1 - eastern Mediterranean |
Sub-Region | Levantine |
Cause | EA - earthquake in land |
Volcanic Explosivity Index | -- |
Reliability | 4 - definite tsunami |
Runup | -- |
Intensity Sieberg-Ambraseys scale | 3 - rather strong |
Intensity Papadopoulos and Imamura scale | V - strong |
Earthquake data from Fokaefs and Papadopoulos (2007) and Sbeinati et al.(2005).
Summary in Salamon et al. (2007). An Ms ~6.6 earthquake in southern Lebanon and northern Israel (Ambraseys and Barazangi, 1989; Amiran et al., 1994) on 1759 10 30 03:45 Local Time. Ben-Menahem (1991) mentions a seiche in Sea of Galilee. Paleoseismic study by Daeron et al. (2005) relates the earthquake to the Rachaiya fault, and archaeoseismic investigation by Marco et al. (2005) suggests the surface rupture extended to the Jordan Gorge segment.
Tsunami at Acre and Tripoli from Fokaefs and Papadopoulos (2007), and Sbeinati et al. (2005), Yolsal et al. (2007); Altinok et al., (2011)
According to Salamon et al., (2011) who reports Ambraseys and Barazangi (1989): a seismic sea wave flooded Acre and the docks at Tripoli, but there was no apparent damage. The tsunami is also mentioned by Shalem (1956) and Ambraseys (1962), who locate the tsunami along the coasts of Israel and Lebanon and estimate the waves flooded the streets of Acre to a height of 8' (ft), and Amiran et al. (1994). This is the only case where the inundation height (height of the flooding water above sea level) is documented in historical sources.
Ambraseys and Barazangi (1989) describe a tsunami for each of the two earthquakes in this sequence (October 30th and November 25th), while Amiran et al. (1994) and Soloviev et al. (2000) determined a tsunami for this event only.