Final answer:
Graded bedding is characteristic of a turbidity current, which is an underwater avalanche of sediment. It represents depositional environments in which transport energy decreases over time.
Step-by-step explanation:
Graded bedding, as shown in the image, is characteristic of a turbidity current. Graded bedding is a sedimentary structure where a change in grain size can be observed within a single bed. It typically represents depositional environments in which transport energy decreases over time. Turbidity currents are underwater avalanches of sediment that move downslope and deposit sediment with graded bedding.