Shockwaves are propagating disturbances with a long history of study in gas dynamics, fluid dynamics, and astrophysics. We also see examples of shocks in everyday life such as a traffic jam, in which the oncoming traffic has much lower density than the cars within the traffic jam.A classical compression wave involves propagation of a discontinuity in which information is absorbed from both sides in the shock layer. Undercompressive shocks are more unusual; they have special properties, including the transfer of information through the shock and often different stability properties than their compressive cousins. In the past decade, undercompressive waves have been studied in microscale and nanoscale applications in which surface forces dominate the physics in the shock layer. These forces can permit the existence of undercompressive waves, and their utility is just now coming to fruition. In PNAS, Perkinson et al.(1) demonstrate how to use undercompressive shocks in ion-bombarded surfaces to create patterns with steep ridges on a micrometer scale.The traffic jam example is one that can be modeled with a simple 1D, first-order, nonlinear wave equation, or "conservation law," introduced in the mid-1950s (2, 3):Here, u is the material being transported in the direction x and f is the flux of the material. A shock is a solution to such an equation with a discontinuity in u that travels with speed s given by the RankineHugoniot jump condition:Such models can be solved exactly for any choice of states u L and u R on the left and right of the discontinuity. All such shockwaves are compressive, meaning that they satisfy an entropy condition:The speed s of the shock is faster than the characteristics speed f ′(u R ) ahead of it and slower than the speed f ′(u L ) behind it. It was traditionally thought that any physical process described by such a simple 1D model could have only compressive shocks. This fact can be proved rigorously in the case where the physics in the shock layer is "diffusion" or Brownian motion, as is seen in gas dynamics. The modification of Eq. 1 to include linear diffusion in the shock layer isWith diffusion, shock discontinuities are smoothed; however, the basic shock structure, including the speed of the shock as determined by the RankineHugoniot jump condition, is exhibited in smooth traveling wave solutions of Eq. , who showed that it produced undercompressive shocks that could be reproduced in experiments. The model is a conservation law in which u is the slope of the surface and the nonlinear flux function f is the yield function, which gives the average velocity of erosion of the surface as a function of its local slope, and is, in general, nonconvex. Their model has a fourth-order term that models additional smoothing effects such as Mullins-Herring surface diffusion or ion-enhanced viscous flow confined to a thin surface layer. They showed that stable steep undercompressive waves were experimentally viable in ion-bombarded surfaces with common physical parameters.In the case of compressive...