What is fault scarps?

Fault scarps are geological features that form as a result of tectonic activity and the movement of tectonic plates. They are usually found at the edges of a fault and are typically steep, linear cliffs or slopes that can reach several tens of meters in height. Fault scarps are formed when the ground on one side of a fault is displaced vertically relative to the other side, creating a visible step or cliff.

The term “fault scarp” is often used to describe the section of a fault that can be seen at the surface, but it can also refer to the entire zone of deformation associated with the fault. The movement of these faults can cause earthquakes and other geological events, and studying fault scarps is an important part of understanding these processes. Scientists use techniques like LIDAR and satellite imaging to map and study fault scarps and their associated features, which can provide valuable insights into the history and future of tectonic activity in a region.