Abstract. Shock wave data, thermodynamic and phase diagram data for ice, porous ice, and water are taken together with a Rice-Walsh-Bakanova equation of_ state to define the shock pressures and impact velocities required to induce incipient melting (IM) (6 GPa), complete melting (CM) (10 GPa), and passage through the vapor-liquid critical point (CP) upon isentropic release (22.5 GPa).