Titlebook: Submarine Fans and Related Turbidite Systems; Arnold H. Bouma,William R. Normark,Neal E. Barnes Book 1985 Springer-Verlag New York, Inc 19

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Astoria Fan, Pacific Ocean. Well-developed channels cross the entire fan length; they display classic inner-fan leveed profiles but evolve into distributaries in the midfan area where the gradient decreases sharply. During periods of low sea level, inner- and middle-fan channels funnel sand to distal depositional sites in th

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La Jolla Fan, Pacific Oceanduces three upper fan distributary paths. The position of La Jolla Canyon is controlled by the geometry of a buried hard-rock structure. The northern Newport Canyon channels contain seismically detectable vertical stacks of channel sand bodies. Sediment from northern feeders and the central La Jolla

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Fissure

Monterey Fan, Pacific Oceanannels. The northern Ascension Canyon system is relatively inactive during high sea-level periods. In contrast, Monterey Canyon and its tributaries to the south cut across the shelf and remain active during high sea level. Deposition on the upper fan is controlled primarily by the relative activity

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