“…Further, the combination of geophysical methods offers high resolution, detecting features in the order of a few tens of centimetres depth and/or thickness to several metres. Resistivity methods, and more specifically electrical resistivity tomography (ERT), (Tsokas et al, 1994;Diamanti et al, 2005, Papadopoulos et al, 2007, Tsokas et al, 2008a, Tsourlos and Tsokas, 2011 and ground penetrating radar (GPR) (Savvaidis et al, 1999;Leucci, 2002;Piro et al, 2003;Linford, 2004;Tsokas et al, 2007) are two of the most popular methods for doing so.…”