In this Letter, the tensorial nature of the nonequilibrium dynamics in nonlinear mesoscopic elastic materials is evidenced via multimode resonance experiments. In these experiments the dynamic response, including the spatial variations of velocities and strains, is carefully monitored while the sample is vibrated in a purely longitudinal or a purely torsional mode. By analogy with the fact that such experiments can decouple the elements of the linear elastic tensor, we demonstrate that the parameters quantifying the nonequilibrium dynamics of the material differ substantially for a compressional wave and for a shear wave. This result could lead to further understanding of the nonlinear mechanical phenomena that arise in natural systems as well as to the design and engineering of nonlinear acoustic metamaterials. DOI: 10.1103/PhysRevLett.116.115501 Nonlinear mesoscopic elastic materials [1] exhibit unique and interesting properties related to nonlinear and nonequilibrium dynamics that are relevant to various natural and industrial processes ranging in scales and applications, e.g., the onset of earthquakes and avalanches in geophysics [2][3][4], the aging of infrastructures in civil engineering [5,6], the failure of mechanical parts in industrial settings [7][8][9], bone fragility in the medical field [10][11][12], or the design of novel materials, including nonlinear metamaterials, for shock absorption, acoustic focusing, and energy-harversting systems [13]. These properties include the dependence of wave speed and damping parameters on strain amplitude [5,14,15], slow relaxation [16,17], and hysteresis with end-point memory [18][19][20]. Consolidated (see the work referenced previously) and unconsolidated granular media [21][22][23][24] are of particular interest for laboratory-scale experiments because they can provide reference measurements to study or engineer these properties. The latter, when consisting of disorded bead pack or granular crystal lattices, serves as a simplified paradigm for understanding the key mechanisms responsible for nonequilibrium dynamics whereas the former provides a more complex but faithful representation of realistic systems.In consolidated granular media, nonequilibrium dynamics is thought to originate from the microscopic-sized imperfections (e.g., microcracks, debonding at interfaces, grain contacts, etc.) in the "soft" bond system that connects together mesoscopic-sized "hard" elements (e.g., grains or crystals) [25], with experimental evidence recently presented for thermally damaged samples of concrete [26]. These micro-and mesoscopic features are typically distributed throughout the sample and affect its dynamic response at a macroscopic scale through a process of homogenization, thus offering a rich multiscale problem in material physics. Nonequilibrium dynamics has been quantified experimentally in nonlinear mesoscopic elastic materials, through the nonclassical nonlinear elastic parameter α, by resonant experiments in which a slender bar with free boundary conditions...