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In geology, shearing occurs when rocks slide past each other horizontally in opposite directions. The kind of fault created by shearing is called a strike-slip fault.
Transform fault or sliding boundary
crack in earths crust where two plates are sliding past each other
Diamonds.
Clastic sedimentary rocks.
Transform fault
Block mountains form when a fault line causes rocks to move past each other. These are also called fault mountains.
Reverse fault
This is known as a normal fault.
In geology, shearing occurs when rocks slide past each other horizontally in opposite directions. The kind of fault created by shearing is called a strike-slip fault.
This kind of fault is called a normal fault and is usually a sign of crustal extension.
It is a transform boundary.
strike slip fault
Transform fault or sliding boundary
crack in earths crust where two plates are sliding past each other
strike-slip faults.
this kind of fault occurs at a transform plate boundaries