nORTH
This is called a reverse or thrust fault.
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A reverse fault is caused by compressional forces in the Earth's crust, where rocks are pushed together, causing the overlying rock to move up and over the underlying rock along the fault plane. This results in a reverse fault where the hanging wall moves vertically upward in relation to the footwall.
A reverse fault forms when a hanging wall moves upward due to compressional forces. This type of fault occurs in areas where the crust is being pushed together, causing the hanging wall to move up and the footwall to move down.
A normal fault is the opposite of a reverse fault.
A reverse fault is formed here
The San Andreas fault is a strike-slip fault, where two tectonic plates move horizontally past each other. It is not a reverse fault, where the hanging wall moves up relative to the footwall due to compression.
Trust faults typically have low dip angles. A high-angle thrust fault is called a reverse fault. A reverse fault occurs primarily across lithological units where as a thrust usually occurs within or at a low angle to lithological units.
Trust faults typically have low dip angles. A high-angle thrust fault is called a reverse fault. A reverse fault occurs primarily across lithological units where as a thrust usually occurs within or at a low angle to lithological units.
thrust
A reverse fault
Reverse