Magnetotelluric data from the central Eromanga Basin indicate that one‐dimensional resistivity models are appropriate for the region. The uppermost Jurassic‐Cretaceous Eromanga Basin sequence contains flowing aquifers and has an average section resistivity in the range 1 to 7 ohm m with a mean of 4 ohm m. This overlies the older sedimentary sequences of the Cooper (Permo‐Triassic) and Adavale (Devonian) Basins with resistivities in the range 10 to 400 ohm m, which present good resistivity contrasts for determining sub‐surface morphology at the base of the Eromanga sequence. The depth extent of the older sequences is not well resolved because of the overlying highly conductive layers, but it appears to be greater than that determined from seismic reflection data in the Coonavalla Syncline and Warrabin Trough.