The iron ore deposit of Kerry (north-western Syria) has been sampled;
by means of the combined use of small-area x-ray photoelectron spectro
scopy (SA-XPS), small-area x-ray induced Auger electron spectroscopy (
SA-XAES), scanning electron microscopy (SEM), energy dispersive spectr
oscopy (EDS), differential thermal analysis (DTA) and thermal gravimet
ric analysis (TGA), the smelting process of the most iron-rich ore has
been studied under a CO atmosphere up to 1570 K. Attention has been f
ocused on the chemical aspects involved during the reduction of the ir
on ore and on the chemical composition of the non-metallic compounds,
i.e. the slags, that result from the smelting process. Furthermore, th
is information has been compared with that obtained from early iron me
tallurgy slags and artefacts found in north-western Syria in order to
locate the geographical source of the iron ore exploited during the ea
rly Iron Age in this region.