The goal of this investigation is to determine how the sedimentation of the magnetorheological (MR) fluid within an MR sandwich beam affects the beam's dynamics. To discover this phenomenon, the authors measured the natural frequency and damping of a beam under several conditions, such as outer-layer stiffness, magnet location, and magnetic field strength, for beams whose MR fluid had sedimented and beams that were shaken to redistribute the fluid within the beam. The collected data was compared to previously measured modal data of the same beams when they were first built. The results show that the beams' natural frequency lowered when the MR fluid sedimented and was shaken, but the damping rose for sedimented and shaken beams.