where would you expect to find graded bedding is a scientific question relevant in geology, particularly sedimentology. Graded bedding typically forms in environments where water or air currents deposit sediment in layers according to particle size. You would find it in river deltas, deep-sea turbidite sequences, or alluvial fans. These layers show a transition from coarse particles at the bottom to finer ones at the top, indicating a slowing of current over time. Graded bedding provides insights into past environments, sediment transport, and stratigraphic correlations in geological studies.