What is seismites?

Seismites are sedimentary rocks that show evidence of deformation caused by earthquakes or other seismic activity. These deformations can include cracks, folds, and fractures in the rock layers. Seismites are important indicators of past seismic activity and can provide valuable information about the frequency, intensity, and duration of earthquakes in a particular area. They can also be used to track the movements of fault lines and to help predict future seismic activity. Seismites can be found in a range of environments, from deep ocean sediments to terrestrial rock formations, and they are often identified by their distinctive structures and patterns.