Earthquake Surface Rupture, Fissures, and Tectonic Uplift/Subsidence

Earthquake Surface Rupture, Fissures, and Tectonic Uplift/Subsidence

Earthquake surface ruptures and fissures are localised ground displacements that develop during and immediately after an earthquake, where the fault which hosted the earthquake intersects the Earth’s surface. Surface ruptures represent the upward continuation of fault slip at depth, while fissures are smaller displacements, or more distributed deformation in and around the rupture area (adapted from USGS, no date and PNSN, no date).

Subsidence and Uplift, Including Shoreline Change (Earthquake Trigger)

Subsidence and Uplift, Including Shoreline Change (Earthquake Trigger)

Tectonic uplift and subsidence are the distributed vertical permanent ground deformations (warping) that result from earthquake displacements on a dipping (inclined) fault (Styron, 2019). This includes changes to the shoreline as a result of uplift and subsidence.

Earthquake

Earthquake

Earthquake is a term used to describe both sudden slip on a fault, and the resulting ground shaking and radiated seismic energy caused by the slip, or by volcanic or magmatic activity, or other sudden stress changes in the Earth (USGS, no date).

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