Abstract
At the Neolithic settlement "Pločnik" near Prokuplje in Serbia, the electrical imaging method (ERT) was deployed. At the sounding site S-3, 1D electrical survey revealed a low resistivity layer with a thickness of 0.8 meters and a resistivity of about 30 Ωm. A sharp and steep boundary divides the high resistivity medium and the low resistivity medium, according to the 2D electrical survey. The resolution of the ERT method was tested using 3D forward and inverse modeling to see whether it could distinguish the high resistivity pit from the surrounding high resistivity gravel.
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