]. More broadly, the stability of flooding fronts is paramount to efficiently displacing the resident pore fluids from a variety of porous media: oil reservoirs, filter beds, fixed beds (regeneration), and aquifer media [Homsy, 1987]. The miscible displacement of pore water by the advancing cosolvent front is affected by the differences in liquid properties, the characteristics of the porous media, and the cosolvent injection rate. A common condition is cosolvent override due to the buoyancy of the cosolvent, and this situation may be exacerbated when the advancing front reaches a NAPL source zone, especially for the case of dense nonaqueous phase liquids (DNAPLs). It is therefore important to understand the factors governing the stability of advancing fronts in order to predict the "stabilized" angle of the front and the time (distance) required for the angle to stabilize if, in fact, the advancing front does stabilize.Flow visualization studies of miscible flooding in quasi-twodimensional models (narrow width tanks, cells, and parallel plates) that allow for gravity-induced behavior under confined