Paleomagnetism explains the history of direction and strength of Earth’s magnetic field and the past location of the tectonic plates and applies to the movement of the tectonic plate fragments.
Step-by-step explanation:
The magnetic field in rocks, sediments and archeological materials are observed using Paleomagnetism. The geochronology tool records the change in the magnetic field in the volcanic and sedimentary rock.
The contact between the rigid lithospheric plates is examined to explain the structure of the earth's crust. The lithospheric plates generally move slowly over the underlying mantle.