Earthquake II
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)
described Earthquake II as an event during which
“deposits were ruptured and the buildings collapsed,”
although wall collapse was characterized as "minor
despite the obvious energy of the earthquake." The
underlying occupation was dated "probably" to the
mid- to late-eighth century CE on the basis of related
structures found in the west of site containing
Mahesh Ware pottery.
Interestingly, the authors noted that the “pottery
within layers capping Earthquake II” was “earlier than
that found in the occupation deposit” beneath the
Earthquake II rupture.
Thomas et al. (2007)
concluded that Earthquake II occurred
sometime "after the mid to late eighth century A.D."
They measured 5 cm of left-lateral slip on Fault A
where it displaced wall J.1:26 and reported that
Faults A and E together produced "an accumulated
southwest dip-slip of 42 cm."