“…A typical example of such a motion is anisotropic mean curvature flow: given a norm φ on R n (called anisotropy), the equation for the anisotropic mean curvature flow of hypersurfaces parametrized as Γ t reads as β(ν)V = −div Γt [∇φ(ν)] on Γ t , (1.1) where V denotes the normal velocity of Γ t in the direction of the unit outer normal ν of Γ t and β is the mobility, a positive kinetic coefficient [30]. Anisotropic mean curvature flow is called crystalline provided the boundary of the Wulff shape W φ := {φ ≤ 1} lies on finitely many hyperplanes; in this quite interesting case, equation (1.1) must be properly interpreted, due to the nondifferentiability of φ ; see for instance [1,29,52,28,12,13,31,20,32,17,18]. Equation (1.1) (sometimes referred to as the two-phase evolution) can be generalized to the case of networks in the plane, and more generally to the case of partitions of space (sometimes called the multiphase case): here the evolving sets are intrisically nonsmooth, since the presence of triple junctions (in the plane), or multiple lines, quadruple points etc.…”