Numerical solutions of Maxwell equations for a model earth with a reasonabl
y conducting channel indicate that the electric field values are intensifie
d within a certain region only(i.e., above the end of the channel), thus ex
plaining the observed selectivity effect. In this region, the electric fiel
d may reach detectable values (5-10mV/km), while the magnetic field still r
emains low (10(-2)nT). The results are compatible with those obtained recen
tly by analytical solutions (Varotsos et al. [1998]). Both the numerical an
d the analytical solutions lead to a natural explanation of the Delta V/L a
pproximate to const criterion. This criterion, however, should not be appli
ed over an area with strongly inhomogeneous electrical structure.