Small-angle X-ray scattering (SAXS) and transmission electron microscopy (TEM) have been used to study the microporosity and micromineralogy of vitrinite in a high-volatile bituminous coal (Illinois No. 6). Sections were selected from samples that contained representative amounts of vitrinite. Micropores and fine minerals with sizes ranging between l0 and 1000 A were observed. The minerals, primarily silicates, were heterogeneously distributed in layers parallel to the bedding plane of the coal. The radii of gyration, surface area, volume fraction, and size distribution of micropores, mesopores, and fine-size minerals were obtained from an analysis of the SAXS curves. The total volume fraction of these components was determined from the integrated intensity to be 0'09 _+ 0"02 cm 3 cm -3. The size distributions were found to be trimodal with peaks at 30, 100, and 220 A. These peaks are associated with micropores, microminerals, and mesopores respectively. The specific surfaces associated with each peak are 140__. 20, 3 _+ l, and 10_ 3 m 2 g-1, respectively, while the corresponding volume fractions are 0"004 +_ 0"001, 0"026 _+ 0-005, and 0"056 _+ 0"018 cm 3 cm-3 respectively. Comparison of the results from SAXS with those from TEM showed good agreement.