“…In certain occasions (Wilson et al, 2006), the ERT technique was used in order to supplement and clarify the results of initially executed one dimensional VES in the same region. The efficiency of the ERT technique in a variety of inshore geological settings is demonstrated by various researchers, including coastal alluvial aquifers (Abdul Nassir et al, 2000;Morrow et al, 2010;Ebraheem et al, 2012;Mas-Pla et al, 2012), coastal deltaic deposits (Maillet et al, 2005;Martínez et al, 2009;Gurunadha Rao et al, 2011), or inland saline environments, e.g., in the Okavango Delta, Botswana (Bauer et al, 2006), in the Dead Sea, Jordan aquifer (Batayneh, 2006), and in Querenca-Silves, south Portugal (Leitão et al, 2014). These authors have utilized various array configurations and electrode spacing intervals, and showed that the method is able to provide a good correlation between specific resistivity values and hydrogeological properties, and thus, to calculate formation factors (Archie, 1942) for the separate aquifer units, by combining groundwater electrical resistivity measurements and bulk formation resistivity distribution.…”