The mobility conditions of bedload transport in an alpine high-gradient step–pool stream (Rio Cordon) are analysed. Since 1986, a device system at the downstream end section of the stream has been operating in order to monitor the water discharge, suspended sediment and bedload transport. Sediment distribution of bedload transported by various floods has been analysed, and equal-mobility evidence is recognized only for the high-magnitude flows ever recorded (RI > 50 years). The thresholds for size-selective and equal-mobility transport conditions are identified and quantified by using both data provided by the fractional transport rate and by length displacements of marked particles. Size-selective bedload transport seems to dominate when the critical shear stress of the size fractions tau_ci considered is exceeded, whereas the equal-mobility condition is approached as levels of excess shear stress become higher (tau_eq = 1.45tau_ci).