How could geologists estimate the rate of motion of a fault?

htm. The rate of movement along a plate boundary can be determined by measuring the displacement of rocks or other features along the boundary. ... The San Andreas Fault has cut through this rock unit, dividing it into two parts which are now widely separated on opposite sides of the fault.

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places of higher salinity. there are parts of the ocean where hardly any rain falls but warm dry winds cause lots of evaporation. this evaporation removes water – when water vapour rises into the atmosphere, it leaves the salt behind, so the salinity of the seawater increases. this causes the seawater to become denser.