Linked from

The 7 pages that link to Paleocurrent analysis, each with the reason it gives.

• TurbiditeRelated: Turbidite bed structures can indicate the direction of ancient sediment transport.

• SedimentologyRelated: It uses preserved deposits to infer the direction of past transport.

• Cross-beddingRelated: Cross-bed foresets provide measurements of the direction in which bedforms migrated.

• BedformRelated: Bedform deposits preserve orientations that help reconstruct ancient flows.

• Sedimentary structuresRelated: Cross-bedding and sole marks provide common directional measurements.

• Point barRelated: Bar layers can preserve orientations that indicate former channel-flow directions.

• Ripple marksRelated: Asymmetric current ripples can preserve a record of the direction sediment moved.