Creep tests were performed at high temperature (150–770° C) on mono- and polycrystals of uranium in the α and β forms. The variation of the activation energy for creep with temperature led to the establishment of temperature ranges in which different mechanisms were rate-controlling. Micrographie observations made after creep and the stress-dependence of creep rate confirm the hypothesis based on activation energies. Below 325° C, the creep behaviour of mono- and polycrystals is similar. From 325° C to an upper temperature limit which depends on the structural condition of the metal and on its degree of purity, the creep deformation of uranium is controlled by cross-slip. From this limiting temperature up to 520° C, the creep of uranium involves two independent but jointly active mechanisms: these are the motion of screw dislocations by cross-slip and dislocation climb by a diffusion mechanism. Above 520° C and up to the α/β transition, creep of polycrystals is controlled by climb of dislocations out of their slip-planes, following a pile-up process in the case of primary creep and dipole annihilation in the case of secondary creep. For monocrystals, creep depends on the climb of edge dislocations in sub-boundaries which existed before creep, and their rearrangement in these sub-boundaries. In the β phase, creep of polycrystals is controlled by the diffusional climb of dislocations out of their slip-planes.