How is a fault created? – , peru. the sunshine layer of rock exhibits the displacement. a second regular fault is on the proper.
The vector of slip could be qualitatively assessed by finding out any drag folding of strata, which can be seen on both aspect of the fault.
 drag folding is a zone of folding near a fault that seemingly arises from frictional resistance to motion on the fault.
 the route and magnitude of heave and throw could be measured solely by discovering frequent intersection factors on both aspect of the fault (known as a piercing level).
In follow, it’s often solely potential to search out the slip route of faults, and an approximation of the heave and throw vector.