Which phenomenon initiates turbidity currents along submarine fault scarps during seismic activity?

💡 Explanation

When seismic shaking occurs near submarine fault scarps, liquefaction of sediment happens because grain structure weakens due to increased pore pressure, initiating downslope movement and turbidity currents. Therefore liquefaction results, rather than hydrate release, tsunami propagation, or thermohaline erosion that depend on different triggers.

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