In geology, cross-bedding refers to inclined sedimentary structures in a horizontal unit of rock. These tilted structures are deposits from bedforms such as ripples and dunes, and they indicate that the depositional environment contained a flowing fluid (typically, water or wind). This is a case in geology when original depositional layering is tilted, and that the tilting is not a result of post-depositional deformation.
Cross-bedding structures are formed in bedforms such as ripples and dunes by the motion of sediment due to a flowing fluid. Sediment grains bounce up the windward/upstream ("stoss") side of a ripple, and then tumble down the lee side.
Cross-bedded sediments are recognized in the field by the many layers of "foresets", which are the series of layers that form on the lee side of the bedform (ripple or dune). These foresets are individually differentiable because of small-scale separation between layers of material of different sizes and densities.
Cross-bedding can also be recognized by truncations in sets of ripple foresets, where previously-existing stream deposits are eroded by a later flood, and new bedoforms are deposited in the scoured area.
The direction of motion of the cross-beds can show ancient flow or wind directions. The foresets are deposited at the angle of repose (~34 degrees from the horizontal), so geologists are able to measure dip direction of the cross-bedded sediments and calculate the paleoflow direction. This is important in reconstructing past climate and drainage patterns: sand dunes preserve the prevalent wind directions, and current ripples show in which direction the rivers were moving.