Journal article Open Access

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

Normark, W. R.


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        <foaf:name>Normark, W. R.</foaf:name>
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    <dct:title>Late Pleistocene channel–levee development on Monterey submarine fan, central California</dct:title>
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    <dct:description>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 accumulation on the fan prior to the UTS was much slower (</dct:description>
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