The patterns of faults in the South Silverton mining area are analyzed according to Von Mises' theory of plasticity in plane strain. Initial sections are devoted to standard derivations of basic equations concerning stress, to criteria of failure, and to plastic stress-strain relations in plane strain. Generalized differential equations are derived for slip lines in polar coordinates and applied in the later sections of the report to the two basic problems presented by the Silverton district. The first problem is that of determining the slip-line pattern to be expected if a wedge is compressed in plane strain so that material flows toward the large end. This simulates the inferred mode of deformation in the western part of the district. The orientation of certain faults are used as boundary conditions for solution of the differential equations and the whole of the slip-line field is reconstructed from partial knowledge of the fault system. Equations for the conjugate shears are exponential in form. A compatible velocity field is derived. The second problem is that of constructing the slip-line field generated by radial stresses, in plane strain, within a segment of a ring around the southeast border of the subsided block of the Silverton caldera. The geometry of certain faults is again used to reconstruct the whole theoretical pattern. Although the equations of the slip lines are exponential in form, they represent orthogonal epicycloids and hypocycloids. The distribution of stresses required to form the slip lines in the eastern district are computed. They appear compatible with stresses to be expected due to wedging of a graben area at the northeast corner of the subsided block. Theoretical slip-line fields for both the western and eastern parts of the district are compared with the actual fault pattern. Although there are differences, the agreement is, on the whole, satisfactory.