This document discusses the earth's magnetic field and how it was studied and understood over time. It asks questions about William Gilbert's hypotheses about compasses and the earth's core in the 1500s. The earth functions similarly to a bar magnet, with Gilbert originally thinking the core was made of sulfur but it is actually made of iron and nickel which helps create the magnetic field. The magnetic and geographic poles are not in the same locations. Magnetic declination changes over time and was important for navigators to understand. The earth leaves a record of its magnetic field changes over time in rocks. The magnetosphere is shaped by solar winds and protects the inner Van Allen radiation belts. Solar wind particles enter the atmosphere at the magnetic poles.