-Premelting of ice within pores in earth materials is shown to depend on the presence of vapor layers. For thick vapor layers between ice and pore surfaces, a nanosized water sheet can be formed due to repulsive Lifshitz forces. In the absence of vapor layers, ice is inhibited from melting near pore surfaces. In between these limits, we find an enhancement of the water film thickness in silica and alumina pores. In the presence of metallic surface patches in the pore, the Lifshitz forces can dramatically widen the water film thickness, with potential complete melting of the ice surface.At the interface between ice and a dissimilar material, interfacial melting can occur. In some cases this melting can become unbounded resulting in complete interfacial melting of ice. This case is here referred to as premelting in the case of the vapor-ice interface. [1, 2] In porous media, premelting of ice is here shown to depend on the presence of diluted gas layers between ice and pore surface as well as on the optical properties of the surface material. This ought to be important to account for in any realistic modeling that aims at understanding how liquid water can be present in frozen pores on icy planets and in permafrost regions. Different surface materials including silica (serving as model for rock composed of quartz), alumina, and gold are studied. We show how enhanced concentrations of liquid water can be induced in pores depending on the nature of the surface materials and the thickness of the vapor layers. Our model system is shown in Fig.