A composite consisting of 30 wt% SiC whiskers and a mullitebased matrix (mullite-32.4 wt% ZrO 2 -2.2 wt% MgO) was isothermally exposed in air at 1000°-1350°C, for up to 1000 h. Microstructural evolution in the oxidized samples was investigated using X-ray diffractometry and analytical transmission electron microscopy. Amorphous SiO 2 , formed through the oxidation of SiC whiskers, was devitrified into cristobalite at T > 1200°C and into quartz at 1000°C. At T > 1200°C, the reaction between ZrO 2 and SiO 2 resulted in zircon, and prismatic secondary mullite grains were formed via a solutionreprecipitation mechanism in severely oxidized regions. Ternary compounds, such as sapphirine and cordierite, also were found after long-term exposure at T > 1200°C.