Equilibrium, nonequilibrium, and ideal gas (7 = 1.4) laminar boundary layers and viscous shock layers over a 10°-half-angle hyperboloid, 50 nose-radii long, have been computed by several investigators for three 20,000-fps cases, one at 100,000 ft altitude and two at 250,000 ft. Their predictions of skin-friction and heat-transfer coefficients and displacementthickness distributions over the body, as well as property profiles across the layer at the ends of the body, are compared. The conditions were chosen to test the ability of the numerical methods to predict nonequilibrium viscous-layer flows near and far from chemical equilibrium and the applicability of boundary-layer theory at low-Reynolds-number conditions. Results show that recently developed finite-difference methods can be used to compute finite rate, chemically reacting flows near chemical equilibrium, and iterations of implicit finite-difference solutions are required for accurate results. At 250,000 ft altitude, higher-order boundary-layer theory is not adequate and a fully viscous shock-layer technique must be used. At the higher altitude, stagnation heat transfer is strongly affected by shock slip.