Earthquake III
Area J-East in the archaeological site of Aila preserves one of the
most detailed archaeoseismic records along the southern
Dead Sea Transform. Located approximately 500 m north
of the modern shoreline of the Gulf of Aqaba and about
500 m northwest of the later Islamic city of
Ayla, the Nabatean, Roman, Byzantine, and Early Islamic
occupation sequence spans from the first century CE
through the Early Islamic period.
Aila occupies a tectonic setting at
the northern end of the Gulf of Aqaba where
left-lateral motion on the Aqaba Fault is transferred
westward across the Wadi Arabah by a series of
shoreline-parallel normal cross faults. One of these
active faults (CF-5) intersects the western part of
Area J-East, providing a rare opportunity to document
repeated surface faulting, structural damage, repair,
and stratigraphic displacement within a well-dated
archaeological sequence.
Thomas et al. (2007)
report that Earthquake III was preceded by a
mid-seventh- to mid-eighth-century occupation marked
by Umayyad pottery and mudbrick walls founded on stone
footings. They characterized Earthquake III as a major
event, observing that rupture occurred on four fault
strands (B, C, F, and G), all "within the same fault
corridor." While Fault B produced "left-lateral slip on wall
J.1:26 of only 4 cm," dip-slip "for all four
faults measured in Section 3 was 54 cm, suggesting a
major event."
Thomas et al. (2007)
further reported that Earthquake III was overlain by a
mid- to late-eighth-century CE occupation horizon,
indicating that the earthquake occurred sometime
between the mid-seventh and mid- to late-eighth
centuries CE. Chronologically, the event is compatible with one of the
mid-eighth-century CE earthquakes.