Magnetic properties of a series of orthopyroxenes, x FeSiO3⋅(1-x) MgSiO3 separated from various kinds of rocks were examined. Paramagnetic susceptibility of the orthopyroxenes was determined from the slope of the straight line part of the magnetization curve, generally expressed as σ=σ0+χH. The following empirical formula was obtained at the room temperature for the molecular magnetic susceptibility of the orthopyroxenes with varying x, i.e. χmol=1.12x×10-2e.m.u/mol. Using this experimental value and assuming that the Fe2+ ions are embedded isolately without any interaction between them in the orthopyroxene crystal, the effective Bohr magneton number of the Fe2+ ion was estimated to be 5.14 from the Curie's law. That this value is within the range of the accepted values of the ferrous ions in the crystal (5.1-5.55) seems to justify the above simple calculation.