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Sediment Gravity Flows. Sediment Gravity Flow Types. Slides and Slumps-mass movement Debris flows-matrix supported flows Grain flows-grain interaction Fluidized flows-fluid escape Turbidity currents-density currents with high sediment concentrations.
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Sediment Gravity Flow Types Slides and Slumps-mass movement Debris flows-matrix supported flows Grain flows-grain interaction Fluidized flows-fluid escape Turbidity currents-density currents with high sediment concentrations
Large Slumps can trigger tsunamies andcause significant damage to offshore infrastructure Slump Scar Slump GeoMap.App
For slumping to occur at a given slope, the shear strength of the sediment must be overcome by shear stress • S(Shear strength) = c + o tan ø, where: c = cohesion o = effective pressure (N-n) N = normal load n = pore water pressure ø = angle of internal friction • Triggered by slope increase and/or a change in normal load (deposition), gradual increase in pore water pressure, or a catastrophic event such as an earthquake that triggers movement
Slumps maintain some amount of stratigraphic integrity (bedding) during transport and deposition
Seismic expression of slumps slump slump
(chaotic seismic facies) slump
Debris flow offshore Texas ridges