Re-entrant melting (in which a substance's melting point starts to decrease beyond a certain pressure) is believed to be an unusual phenomenon. Among the elements, it has so far only been observed in a very limited number of species, e.g., the alkali metals. Our density functional theory calculations reveal that this behavior actually extends beyond alkali metals to include magnesium, which also undergoes re-entrant melting, though at the much higher pressure of ∼300 GPa. We find that the origin of re-entrant melting is the faster softening of interatomic interactions in the liquid phase than in the solid, as pressure rises. We propose a simple approach to estimate pressure-volume relations and show that this characteristic softening pattern is widely observed in metallic elements. We verify this prediction in the case of aluminum by finding re-entrant melting at ∼4000 GPa. These results suggest that re-entrant melting may be a more universal feature than previously thought. * Re-entrant melting is generally considered an unusual phenomenon 1,2 that is associated with a negative slope of the melting temperature versus pressure line, or the melting curve.An "ordinary" melting curve, rising from low temperatures and pressures, may eventually invert its trend at some maximum temperature, with a change of slope from positive to negative values for increasing pressures. The resulting topology of the melting curve gives rise to re-entrant melting: upon compressing the liquid at temperatures lower than the maximum melting temperature, one observes a liquid-solid-liquid sequence of phases. In other words, the liquid phase, which is stable at low pressures, re-enters at higher pressures.