9. Msaylḥa Bridge (34°16′25″ n 35°41′18″ e) (Figs 13.15–16)
88 For example Maundrell, Journey from Aleppo, 56; Carne, Syria, The Holy Land, 1:45–46; Guérin, La Terre Sainte, 2:84, 93.
89 Pococke, Description of the East, 2.1:97.
90 Robinson Travels in Syria and Palestine, 2:63.
91 Mohamed Reda Sbeinati, Ryad Darawech and Mikhail Mouty, ‘The historical earthquakes of Syria: an analysis of large
and moderate earthquakes from 1365 B.C. to 1900 A.D.’, Annals of Geophysics 48 (2005): 347–453, at 359.
The Roman road from Beirut to Tripoli originally followed the coastline around the headland known as Raʾs al-Shaqʿa (Byzantine Theouprosopon). However, the ad 551 earthquake which also destroyed Roman Beirut also destroyed the coastal road around the headland sending it crashing into the sea. 91 As a result the late Byzantine and medieval route between Beirut and Tripoli was forced to head inland at a point north of Batrūn and through the narrow pass of Msaylḥa. It is clear that the fort was built to control this narrow pass and, in particular, the bridge which is the only historical connection between the coastal road to the south and Tripoli in the north. The date of the fort has recently been questioned, and it is now thought to have been built sometime between the late sixteenth and early seventeenth century, probably in 1624. In any case the structural history of the bridge indicates an early, probably Roman, origin The collapse of the early vault may be connected with the earthquake of ad 551 in which case the rebuilding may date to the medieval period when a secure route was needed to travel north and south along the coast.Petersen (2020:200) showed evidence for an earlier arch on the bridge (Fig. 13.16 - above and here -
Petersen, A. Roman, Medieval or Ottoman: Historic Bridges of the Lebanon Coast in Edbury, P. W., et al. (2020).
Bridge of Civilizations: The Near East and Europe C. 1100-1300, Archaeopress Publishing Limited.
Sbeinati, M. R., R. Darawcheh, and M. Monty (2005). "The historical earthquakes of Syria: An analysis of large and moderate earthquakes from1365 B.C. to 1900 A.D.,
." Ann. Geophys. 48(3): 347-435.