Late Pleistocene channel–levee development on Monterey submarine fan, central California

@article{Normark1998LatePC,
  title={Late Pleistocene channel–levee development on Monterey submarine fan, central California},
  author={William R. Normark},
  journal={Geo-Marine Letters},
  year={1998},
  volume={18},
  pages={179-188}
}
  • W. Normark
  • Published 1 September 1998
  • Geology
  • Geo-Marine Letters
Much of the modern upper (proximal) Monterey fan is a channel–levee complex, the Upper Turbidite Sequence (UTS), that was deeply eroded after the channel breached a volcanic ridge to reach a deeper base level. Ages of sediment samples collected with the ALVIN submersible from the deepest outcrop within the channel–levee system, 390 m below the adjacent western levee crest, indicate that the UTS deposits accumulated at ≥1 m ka−1 during the last 500 ka. Neogene and Early Pleistocene sediment… 
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