We present a study of the active tectonics of central Asia based on an interpretation of Landsat imagery and supplemented with published field observations and seismic data. Reverse faulting dominates the tectonics of the Tien Shan but is associated with prominent northwest trending right lateral strike slip fault systems. Both types of faulting imply approximately north--south maximum compressive stress. The active tectonics of the Altai and of southern Mongolia are controlled by large-scale conjugate strike slip faulting; left lateral on east--west planes and right lateral on north--northwest planes. This implies that the maximum compressive stress is oriented approximately northeast--southwest. Farther north, strike slip faulting gives way to predominantly normal faulting in the Baykal rift system. We interpret all of the active faulting to be a consequence of lateral displacements of the crust caused by the penetration of the Indian subcontinent of Eurasia. We also interpret the gradual change from thrust faulting and high altitudes in the south and west to normal faulting and lower mean elevations in the north and east to reflect a smooth change in the average state of stress. This suggests that the details of the complex intracontinental deformation in Asia are better described by the deformation of a continuum than by the relative motion of a small number of rigid blocks. Intracontinental rifting in the northeast, in particular, may result from a state of stress analogous to the secondary tension that commonly arises within bounded plastic materials indented by a rigid die.