Abstract. Relaxation times (T1) and lineshapes were examined as a function of temperature through the c~-// transition for z9si in a single crystal of amethyst, and for 29Si and 170 in cristobalite powders. For single crystal quartz, the three z9Si peaks observed at room temperature, representing each of the three differently oriented SiO, tetrahedra in the unit cell, coalesce with increasing temperature such that at the c~-//transition only one peak is observed. 29Si Tl's decrease with increasing temperature up to the transition, above which they remain constant. Although these results are not uniquely interpretable, hopping between the Dauphin6 twin related configurations, el and ez, may be the fluctuations responsible for both effects. This exchange becomes observable up to 150~ below the transition, and persists above the transition, resulting in//-quartz being a time and space average of el and e2. 298i Tl's for isotopically enriched powdered cristobalite show much the same behavior as observed for quartz. In addition, 170 Tl's decrease slowly up to the e-// transition at which point there is an abrupt 1.5 order of magnitude drop. Fitting of static powder ~70 spectra for cristobalite gives an asymmetry parameter (t/) of 0.125 at room T, which decreases to <0.040 at the transition temperature. The electric field gradient (EFG) and chemical shift anisotropy (CSA), however, remain the same, suggesting that the decrease in t/is caused by a dynamical rotation of the tetrahedra below the transition. Thus, the mechanisms of the e-// phase transitions in quartz and cristobalite are similar: there appears to be some fluctuation of the tetrahedra between twin-related orientations below the transition temperature, and the//-phase is characterized by a dynamical average of the twin domains on a unit cell scale.