Event I
Haynes et al. (2006)
report that at the archaeological site of Qasr
Tilah, trenching in Trench A.7 across a fault
strand exposed evidence for a ground-rupturing
earthquake, labeled in the trench log as the
MRE (Most Recent Event), which displaced late
stratigraphic units all the way through unit b. The fault trace terminates
only a few centimeters below the present
surface, where it is sealed by unit a, the
modern ground surface, indicating that the
rupture predates the formation of the present
surface.
An
Ottoman musket ball recovered
near the base of unit a provides a chronological
constraint. This artifact indicates that the
earthquake occurred before the end of Ottoman
control in 1918 CE and after the onset of Ottoman rule in 1516 CE.