Linked from

The 24 pages that link to Turbidity current, each with the reason it gives.

• Sediment transportBroader topic: These currents transport large sediment volumes across lake and ocean floors.

• SedimentationRelated: Its deposits record rapid underwater sediment transport and settling.

• Burgess ShaleRelated: Sediment flows rapidly buried organisms on the ancient sea floor.

• SandstoneRelated: These currents deposit thick sand layers that may become deep-marine sandstone.

• Marine sedimentBroader topic: These underwater flows can rapidly deposit thick layers in deep basins.

• Abyssal plainRelated: These flows carry sediment from continental margins into deep basins and spread it across plains.

• TurbiditeRelated: It transports the sediment that settles to form a turbidite.

• Pyroclastic density currentRelated: It provides a fluid-flow comparison for understanding how density contrasts drive motion.

• Sediment depositionRelated: Its deceleration deposits sediment in distinctive submarine layers.

• Continental slopeRelated: These currents transport sediment from the slope into deeper water.

• Graded beddingRelated: Its waning deposits commonly produce upward-fining graded beds.

• Submarine canyonRelated: These flows can erode canyon floors and carry sediment into deep basins.

• Submarine landslideRelated: Landslide debris can evolve into a turbidity current that travels far beyond the initial failure.

• Suspended loadCompared with: It transports sediment in a concentrated, bottom-hugging current rather than ordinary suspended flow.

• VarveCompared with: Such rapid flows can create event beds that resemble layers but are not annual varves.

• Marine geologyRelated: These flows transport sediment from continental margins into deep basins.

• Paleocurrent analysisRelated: Its deposits preserve current indicators used to infer submarine flow paths.

• Submarine fanRelated: These currents commonly carry sediment from submarine canyons onto the fan.

• Continental riseRelated: These flows carry much of the sediment deposited at the foot of continental slopes.

• FlyschRelated: Repeated turbidity currents commonly build flysch's layered sandstone and mudstone sequences.

• SiltstoneRelated: Its deposits can include fine-grained layers containing siltstone.

• Sediment gravity flowBroader topic: Turbulence keeps its grains suspended, producing a distinctive kind of sediment gravity flow.

• GreywackeRelated: These flows commonly carry and deposit the poorly sorted sediment that becomes greywacke.

• SeabedRelated: These currents transport sediment across the seabed and can carve submarine channels.