W. R. Normark 1999 <p><span>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</span>⁻¹<span>&nbsp;during the last 500 ka. Neogene and Early Pleistocene sediment accumulation on the fan prior to the UTS was much slower (&lt;0.03 m ka</span>⁻¹<span>), and underlying turbidite systems(?) had substantially different morphologic expression(s).</span></p> application/pdf 10.1007/s003670050066 en Springer Late Pleistocene channel-levee development on Monterey submarine fan, central California article