Approximately
80% of these sediment loads are deposited quickly in the estuary
delta (Bornhold et al., 1986; Saito et al., 2001).
The dynamic behavior of marine sediments is driven by a complex interaction
between oceans and lands interacting over varying spatial and
temporal scales (Talke and Stacey, 2003).
The engineering geological
properties of the Yellow River delta are unstable and geological
hazards are common, including landslides, liquefaction and subsidence,
due to the long-term impact of wave and tidal current on the
silty sediments deposited in the complex sedimentary environment
(Feng et al., 1999).
Approximately80% of these sediment loads are deposited quickly in the estuarydelta (Bornhold et al., 1986; Saito et al., 2001).The dynamic behavior of marine sediments is driven by a complex interactionbetween oceans and lands interacting over varying spatial andtemporal scales (Talke and Stacey, 2003).The engineering geologicalproperties of the Yellow River delta are unstable and geologicalhazards are common, including landslides, liquefaction and subsidence,due to the long-term impact of wave and tidal current on thesilty sediments deposited in the complex sedimentary environment(Feng et al., 1999).
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