The rock is very visible by strike-slip
The rock gets farther a part from the fault
Along a fault, rock layers can become displaced, offset, or tilted. This is due to the movement of the Earth's crust along the fault line, resulting in different rock layers being shifted relative to each other.
It is folded and uplifted, or subducted into the mantle, depending on the type of convergent boundary.
The magma forms sills and magma chambers.
Energy is released and earthquakes happen.
When plate movement stores energy in the rock along faults, stress and strain build up within the rock mass. Eventually, this stored energy is released in the form of an earthquake when the rocks along the fault slip past each other, causing seismic waves to propagate through the Earth.
sedimentary rock
nothng
rock band 2
They continue on in the rock cycle.
the rock erodes into soil
It goes into the cup.