Earth possesses a magnetic field primarily generated by the motion of liquid iron in its outer core, although the exact mechanisms remain poorly understood. The magnetic field is not uniform, leading to variations that affect navigation, such as the drifting of magnetic poles. Some discussions suggest potential links between ocean movements and the magnetic field, but skepticism exists regarding the significance of seawater's conductivity. The field's strength is approximately 30 microteslas at the surface, with variations depending on location, particularly stronger at the poles. Overall, while theories abound, the definitive causes and characteristics of Earth's magnetic field continue to be subjects of research and debate.