All essential characteristics of the earthing conductor (distribution resistance, potential gradients, applied potential, etc.) directly depend on the specific resistance (resistivity) of the soil. Unlike technical conductors that can be considered essentially homogeneous and their resistance can be read quite precisely from technical manuals, geological environments are electrically much more complex and mostly, microscopically and macroscopically, inhomogeneous, and thus their resistance cannot be estimated even within an order of magnitude (tables and graphs in manuals). It is necessary to determine the soil resistance by direct measurements at the very place where the earthing conductor is installed. The transmission capacity and lifespan of power cables, and thus the quality and reliability of the power supply to consumers, directly depend on the ability of the environment to dissipate the heat that develops due to Joule and dielectric losses in the cable. The excess temperature of an underground power cable is proportional to the specific thermal resistance of the environment in which the cable is laid. For common geological environments, thermal resistance ranges from 40 Kcm/W to 400 Kcm/W, and cannot be estimated accurately enough for cable sizing without direct on-site measurements.