MAGNETIC PROPERTIES OF CENTRAL MEDITERRANEAN OBSIDIANS: AN ARCHAEOLOGICAL FINGERPRINT?
Tykot (2002) has documented in detail the four Italian islands with geological sources of obsidian. We measured the following magnetic properties of 30 geologic obsidian samples collected from outcrops on the islands: low frequency susceptibility per unit mass (median (med)=27 SI, Interquartile range (IQR)=76 SI); high frequency susceptibility per unit mass (med=25 SI, IQR=70 SI); percent frequency effect (med=9.6 %, IQR=22 %); natural remanent magnetization (med=.38 A/m, IQR=1.7 A/m); demagnetization properties; median destructive field (med=980 Oe, IQR=420 Oe); induced remanent magnetization properties; saturation remanent magnetization (med=15 A/m, IQR=63 A/m); and backfield coercivity of remanence (med=68 mT, IQR=37 mT). Bivariate plots and multivariate statistics help to establish the properties that best distinguish the sources.
Preliminary results suggest that magnetic properties can be used to provenance obsidians to islands and some subsources in the central Mediterranean. However, measurement of more samples is required to better define the ranges of the geologic obsidians properties. Once more fully characterized, archaeological obsidian samples that have been geochemically provenanced could be tested to assess the magnetic fingerprinting method.