The Earth's magnetic field does change and the poles are in constant motion, necessitating regular recalibration of magnetic compasses. Geological evidence supports the idea that the magnetic field reverses periodically, although the exact cause of these reversals remains unclear. The shifting of iron within the Earth is believed to play a role in this phenomenon. Research by Dr. Daniel Lathrop from the University of Maryland provides insight into these magnetic dynamics. Understanding the mechanisms behind the magnetic field and its reversals is still an area of active study.