An analogue model for studying the behavior of the natural geomagnetic and telluric field variations for the coastline problem is discussed. Measurements of amplitudes and phases for the horizontal electric, the horizontal magnetic, and the vertical magnetic field components for sloping earth–sea interfaces and for a sea over an upwelling conducting zone within the mantle in the form of a step are discussed for both the E and the H polarizations.

You do not currently have access to this article.