During the grinding of quartz, water is adsorbed from the atmosphere, but this water gave no detectable thermal effect on DTA because it was evolved uniformly up to 1000 ~ However, in conjunction with an iron contaminant, the adsorbed water was involved in an oxidation reaction causing noticeable thermal effects for quartz powdered in a vibration mill constructed of steel parts. When powdered so finely that the ~--/3 inversion peak at 573 ~ had disappeared, annealing caused a partial redevelopment of the peak but recrystallization of disrupted quartz was too small an effect to give any detectable exothermic peak on DTA.We reported previously [1, 2] that when quartz was ground for several hundreds of hours, the disappearance of the c~-/? inversion peak on DTA was caused not by conversion of the quartz to an amorphous phase of silica, but by the formation of a microcrystalline variety of quartz with modified c~-/? inversion characteristics. A dispersion of the inversion over a range of temperature was suggested [1 ], and therefore when thermal effects were observed outside the range of temperature where the e-/~ inversion normally occurs, these were investigated and are reported here. Although the research was mainly concerned with the effect of grinding on the c~-/~ inversion, the findings reported in the present paper relate chiefly to the additional thermal effects of adsorbed water and contamination which occur during grinding.Contrasting with the c~-/? inversion which occurs on every heating, the liberation of adsorbed water or the oxidation of contaminants, if taken to completion during the first DTA run on a given sample, will not produce thrmal effects or a second or subsequent DTA test. However the possible release of stored grinding energy involving the recrystallization of disrupted surface layers on the particles of quartz, discussed by Lindstr6m [3], must be considered. Any broadening of the e -/~ inversion should produce effects, if observeable, both on the initial DTA and subsequent DTA tests of a given sample, unless annealing reduces the strains within the particles to give a sharpening of the e-/~ peak [2].The thermal effects described in this paper are often very small but, nevertheless, they are real in the sense of being reproducible, both on repeated DTA tests and, except in the case of the anomalous effects reported, from one milling test to another involving quartz from various sources. The interpretation of such small