Clay minerals adversely affect the selective flocculation of iron ores. The effect of montmorillonite on a hematite-quartz mixture was studied. Montmorillonite, particularly in the presence of Ca++, caused indiscriminate dispersion of the pulp. Three possible mechanisms were postulated, namely, card-house structure formation, adsorption of dissolved species from montmorillonite, and montmorillonite-hematite interaction. It was determined that hetero-coagulation of montmorillonite on hematite was responsible for the behavior. Flocculation tests, montmorillonite abstraction tests, starch adsorption tests, zeta potential measurements, and surface analysis techniques were used to ascertain the montmorillonite-hematite interaction and to account for the manner in which it affected selective flocculation.