1. Coarse dispersions are thermodynamically unstable because they consist of lyophobic material
2. Brownian motion is not observed due to large size, however sedimentation occurs
3. Caking occurs after sedimentation– weight of sediment forces particles together and overcomes repulsive forces
4. Particles are very close together and potential energy of attraction is strong due to van der Waals forces
5. To overcome attractive forces high energy levels required
6. Any growth or fusion of particles will require more energy to resuspend the sediment
7. Caking more evident with sedimentation of individual particles due to small particles filling voids and forming a dense compacted layer