Field XI Earthquake (?) - Iron IIB
Purported archaeoseismic evidence has been reported from the nothern part of Gezer in Field XI. Indicators include a debris layer, displaced
ashlars, through-going joints, and tilted, folded, and displaced walls.
Younker (1991) noted that an excavation
against the outer face of Macalister’s “Tower VII” revealed
a debris layer consisting of fallen ashlar blocks in a bricky fill
containing 8th century BCE sherds
above 10th-century BCE fill.
He suggested that the debris layers may be evidence of both an earlier
8th century earthquake and a later 8th century B.C. Assyrian destruction.
At Macalister’s “Tower VI,” Younker (1991) described displaced ashlars,
through-going joints, and tilted walls. The wall’s original
10th-century BCE construction and its 9th/8th-century BCE remodel—which
“inserted” ashlars as an offset into the upper courses—both appear to
have been destroyed sometime in the 8th century BCE.
Dever (1993) reported that the top of the
inner face of a long section of the outer wall east of “Tower VI” was displaced 50 cm or more outward, and bowed out in a sweeping curve.
He
added that the tops of the wall stones
were tilted down-slope at
an angle of ca. 10–20 degrees.
He also uncovered a tilted Iron Age wall
superimposed on a Late Bronze II wall.
Younker (1991) argued that the damage was
caused by an earthquake rather than slow soil creep, emphasizing that
“several sections of the Outer Wall had been clearly displaced from their
foundations by as much as 10 to 40 cm,” that these “wall sections were
all severely tilted outward toward the north,” and that intact portions
of upper courses “had fallen backwards into the city,” not downslope
beyond the wall. He further observed that the southwest corner of the
9th/8th-century BCE ashlar insert had shifted off its cornerstone, which had been split longitudinally because of the great pressure created
by the lateral movement of the upper courses.
The same pressure
produced fissures in the ashlar stones that penetrated through several
courses.
In contrast, Fantalkin and Finkelstein (2006: 22 n. 3) argued
that the observed tilts could result from long-term fill pressure on the
city wall, which lies along the mound’s slope. They emphasized that the
sections showing deformation were part of a substructure buried from the
outset and thus unlikely to have been affected by a quake, and that no evidence for a seismic event has ever been found in any free-standing building at Gezer.
The chronology of Gezer’s outer walls remains debated, focusing mainly
on whether construction occurred in the 9th or 10th century BCE. Ortiz and Wolff (2017: 7) note that
scholars are divided as to whether there are two phases
(tenth century and a later rebuilding during the ninth or eighth centuries B.C.E.) or only one.