Stratum 14 Earthquake
Stratum 14 at Tell Hesban ended with a widespread collapse
of bedrock caves and silos, especially in Areas B and D.
Channels, stairs, and passages once connecting underground
systems were tilted or sealed by debris, marking a sudden,
site-wide destruction horizon.
Mitchel (1980) and
Mitchel (1992) attribute this to a strong earthquake
rather than gradual decay. Fills sealing the collapse lack silt or water-laid layers,
showing that they were deposited quickly after the event and
that rebuilding followed soon afterward. Stratum
13 architecture in Areas A and D was founded directly on leveled debris.
Because Stratum 14 material appears in both
primary and
secondary
contexts, chronological reconstruction is difficult.
Mitchel (1992:61)
noted that “coins recovered at Tell Hesban have correlated poorly with associated pottery.”
A coin of
Aretas IV (r. 9 BCE – 40 CE) from Silo D.3:57 provides an apparent 9 BCE
terminus post quem,
possibly excluding the
31 BCE Josephus Quake.
Associated ceramics extend the horizon into the second century CE and possibly beyond,
with many Early Roman (63 BCE – 135 CE) and a few Late Roman (135 – 324 CE) sherds.
Mitchel (1980)
and Mitchel (1992)
both prefer a
terminus ante quem
in the second century CE — a reasonable assessment, given that the few Late Roman sherds may be secondary or intrusive.
While
Mitchel (1980) and
Mitchel (1992) both suggested that the
~130 CE Eusebius Mystery Quake
was the causative event, the wide date range and the
chronological complications introduced by
secondary deposition
suggest an event sometime between the first century BCE and
the early fourth century CE.