A microscopic reason of the opalescence phenomenon observed earlier near the α–β phase transition point at 846 K in crystalline quartz is established. It was shown that the opalescence in quartz crystals is of dynamic nature and results from a sharp increase of Raman scattering spectral intensity (Raman opalescence phenomenon) due to huge fluctuations of the destabilizing soft mode responsible for instability of the crystalline lattice. The Raman opalescence of a destabilizing soft mode is estimated experimentally in the x (zz)y light scattering geometry by recording temperature dependencies of spectral Raman intensity I(ω′,T) (ω′=ω0‐Ω=const) at fixed frequencies ω′. The strong intensity increase of Raman scattering intensity (Raman opalescence) observed at the exact phase‐transition temperature in crystalline quartz is explained by taking into account interaction of the destabilizing soft mode with a low‐frequency high‐finesse oscillator.