Which outcome occurs when strain exceeds creep strength?

💡 Explanation

ETS events occur because repeated buildup of stress from tectonic movement eventually surpasses the fault's ability to deform via creep; therefore sudden rupture releases energy as slow earthquakes (ETS), rather than continuous plastic deformation.

• Which risk notably increases as isostatic rebound lags tectonic uplift in fjord formation?
• Which risk increases when a fault's asperities fail?
• In wetlands, which outcome from iron oxidation accelerating?
• Which outcome occurs when mineral saturated water drips?
• Which risk increases when rapidly melting permafrost destabilizes stream banks?
• Which outcome arises when the isostatic rebound causes differential uplift across lake basins?