Direct numerical simulations of stably and strongly stratified turbulent flows with Reynolds number Re ≫ 1 and horizontal Froude number F h ≪ 1 are presented. The results are interpreted on the basis of a scaling analysis of the governing equations. The analysis suggests that there are two different strongly stratified regimes according to the parameter $\mathcal{R} \,{=}\, \hbox{\it Re} F^2_h\(. When \)\mathcal{R} \,{\gg}\, 1\(, viscous forces are unimportant and l v scales as l v ∼ U / N ( U is a characteristic horizontal velocity and N is the Brunt–Väisälä frequency) so that the dynamics of the flow is inherently three-dimensional but strongly anisotropic. When \)\mathcal{R} \,{\ll}\, 1\(, vertical viscous shearing is important so that \)l_v \,{\sim}\, l_h/\hbox{\it Re}^{1/2}\( ( l h is a characteristic horizontal length scale). The parameter \)\cal R\( is further shown to be related to the buoyancy Reynolds number and proportional to ( l O /η) 4/3 , where l O is the Ozmidov length scale and η the Kolmogorov length scale. This implies that there are simultaneously two distinct ranges in strongly stratified turbulence when \)\mathcal{R} \,{\gg}\, 1\(: the scales larger than l O are strongly influenced by the stratification while those between l O and η are weakly affected by stratification. The direct numerical simulations with forced large-scale horizontal two-dimensional motions and uniform stratification cover a wide Re and F h range and support the main parameter controlling strongly stratified turbulence being \)\cal R\(. The numerical results are in good agreement with the scaling laws for the vertical length scale. Thin horizontal layers are observed independently of the value of \)\cal R\( but they tend to be smooth for \)\cal R\( 1 small-scale three-dimensional turbulent disturbances are increasingly superimposed. The dissipation of kinetic energy is mostly due to vertical shearing for \)\cal R\( 1, the horizontal spectra of kinetic and potential energy exhibit an approximate k −5/3 h -power-law range and a clear forward energy cascade is observed.