Which risk increases where strike-slip faults intersect aquifers?

💡 Explanation

Induced seismicity risk increases where faults cross aquifers because pressure changes from fluid injection can destabilize the fault and cause earthquakes; therefore, seismicity is increased rather than some pressure equilibrium, which involves fault lubrication.

• Which risk intensifies as alluvial river plains subside?
• Which climatic outcome occurs when intertropical convergence zone weakens?
• Which mechanism causes orographic lift enhancement when prevailing winds encounter strike-slip faults?
• Which outcome arises when strong katabatic winds erode topographic obstructions in glacial valleys?
• Which outcome results when interseismic stress exceeds frictional strength along a subduction zone megathrust fault?
• Which hazard most directly results when large concentrations of tephra are remobilized downslope after initial deposition?