In the present work, our formerly published analytical model of resistive magnetohydrodynamic (MHD) shock without Hall effect has been extended to include the Hall effect. Original jump conditions at a plane oblique shock, analogous to the Rankine-Hugoniot formulas, with a moderately resistive air plasma downstream are derived. Viscous and Ohmic dissipations are neglected, but the jump of isentropic exponent, caused by molecular dissociations behind the shock, is also included in the model. Then, for an application to atmospheric entry problems, a shock fitting procedure with realistic geometrical configurations and ambient conditions at two altitudes is worked out by the coupling of these MHD jumps with thermodynamic correlations at equilibrium and an electrical conductivity model. Fundamental features put into evidence are the reduction and saturation of the MHD interaction by the Hall effect as the magnetic field increases, and the crucial role played by the ion slip factor in the phenomenon. Paradoxically, the Hall effect arises because of the dominance of the magnetic field over collisions, and eventually it counters the MHD interaction. The validity of the assumption of plasma equilibrium and possible validation experiments for the flight conditions considered are also discussed.