Linked from

The 10 pages that link to Graded bedding, each with the reason it gives.

• SedimentBroader topic: Grain-size grading can record how a sediment-laden flow waned.

• Alluvial fanRelated: Individual fan deposits may fine upward as a flow loses energy.

• TurbiditeRelated: Many turbidites fine upward as the current loses its ability to carry coarse grains.

• Sediment depositionBroader topic: Settling from a waning flow can create this upward-fining pattern.

• Cross-beddingCompared with: Unlike cross-bedding, graded bedding records vertical grain-size change rather than inclined internal layers.

• Submarine fanRelated: Normal grading commonly records waning flow within fan turbidites.

• Sedimentary structuresBroader topic: Grain-size grading can record waning currents and settling from suspension.

• FlyschRelated: Grading often preserves the waning flow that deposited flysch sandstone beds.

• GreywackeRelated: Grading records the settling of mixed sediment as a turbidity current loses energy.

• Soft-sediment deformation structuresRelated: Original grading can reveal whether distorted layers have been overturned or disrupted.