Utilisateur
A fault that has not moved for a significant period of geological time.
It no longer has tectonic activity.
Inactive faults no longer generate earthquakes, unlike active faults.
Earthquake rupture.
They provide evidence of past tectonic activity.
Renewed tectonic stress in the region.
Erosion and sediment deposition.
By studying geological features that indicate a lack of recent activity.
That they cannot become active again.
Sedimentary basins.