Introduction. Turbidites: geological formations that have their origins in turbidity currents deposits, that deposit from a form of underwater avalanche that are responsible for distributing vast amounts of clastic sediment into the deep ocean. .
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Idealised sequence of sedimentary textures and structures
in a classical turbidite, or Bouma sequence (Bouma, 1962).
Evolution of a single event down channel
over a distance of 74 km
Regional correlation of turbidite stratigraphy spanning the Holocene
Noyo canyon is cut by the NSAF and as an epicentral distance of zero → explains thicker turbidite records