The model of the electrical conductivity distribution within the Bohem
ian Massif to mid-upper mantle depths was derived from magnetotelluric
and magnetic continuum long-period data of the Budkov Observatory (Ge
ophysical Institute, Acad. Sci. Czech Republic., Prague) and from the
ISL (Induction Scale Lengths) data of the Pruhonice Observatory. The r
anges of apparent resistivities in the Bohemian Massif (BM) are compar
ed with those obtained at relevant central European observations. The
conductivity profile is estimated from the resistivity/depth graph cor
responding to substitute perfect conductor inversion.