Plasma turbulence is investigated using high-resolution ion velocity distributions measured by the Magnetospheric Multiscale Mission (MMS) in the Earth's magnetosheath. The particle distribution is highly structured, suggesting a cascade-like process in velocity space. This complex velocity space structure is investigated using a three-dimensional Hermite transform that reveals a power law distribution of moments. In analogy to hydrodynamics, a Kolmogorov approach leads directly to a range of predictions for this phase-space cascade. The scaling theory is in agreement with observations, suggesting a new path for the study of plasma turbulence in weakly collisional space and astrophysical plasmas.Turbulence in fluids is characterized by nonlinear interactions that transfer energy from large to small scales, eventually producing heat. For a collisional medium, whether an ordinary gas or a plasma, turbulence leads to complex real space structure, but the velocity space, constrained by collisions, remains smooth and close to local thermodynamic equilibrium (as, e.g., in ChapmanEnskog theory [1].) However, in a weakly collisional plasma, spatial fluctuations are accompanied by fluctuations in velocity space, representing another essential facet of plasma dynamics. The characterization of the velocity space is challenging in computations and in experiments, although Vlasov simulation has revealed complexity in the velocity space, often near coherent magnetic and flow structures [2][3][4]. Here we make use of powerful new spacecraft observations in the terrestrial magnetosheath that reveal this structure with sufficient accuracy to quantify the velocity cascade for the first time in a space plasma.The observations reported here are enabled by the Magnetospheric Multiscale Mission (MMS), launched in 2015 to explore magnetic reconnection. The MMS/FPI instrument measures ion and electron velocity distributions (VDFs) at high time cadence, and with high resolution in angle and energy. High resolution magnetic field measurements are available and four-point observation is available for all instruments. MMS provides characterization of plasma turbulence with unprecedented resolution and accuracy. The spacecraft orbit repeatedly crosses the Earth's magnetosheath, enabling new and important characterizations of plasma dynamics (see e.g. Burch et al. [5]). Here we focus on one traversal of the magnetosheath, and specifically on a quantitative description of the ion velocity space cascade.