Linked from

The 21 pages that link to Fault (geology), each with the reason it gives.

• Normal faultNarrower topic: A normal fault is a specific fault type, distinguished by its displacement.

• Induced seismicityNarrower topic: Induced earthquakes occur when human-caused stress changes prompt slip on pre-existing faults.

• Strike-slip faultNarrower topic: Strike-slip faults are one kinematic class within the broader family of geological faults.

• EscarpmentNarrower topic: Movement along a fault can displace terrain and create a fault escarpment.

• Slow slip eventNarrower topic: Slow slip is displacement along a fault rather than a separate kind of geological structure.

• AftershockNarrower topic: Aftershocks occur as faults and surrounding crust respond to the main rupture.

• Earthquake nucleationNarrower topic: Nucleation takes place on a fault surface or within its slipping zone.

• Focal mechanismNarrower topic: The mechanism depicts the orientation and motion of a fault during rupture.

• Fault blockNarrower topic: Faults bound blocks and record the movement that separates them.