Earth's magnetic field is primarily generated by the Dynamo theory, which explains that convection of molten iron and nickel in the planetary core, combined with Earth's rotation, creates electric currents and a magnetic field. However, alternative hypotheses exist, such as one proposed by Gregory Ryskin, suggesting that the magnetic field may originate from dynamo action in the world's oceans instead. This alternative theory addresses certain limitations of the standard model, particularly the correlation between geomagnetic reversals and mass extinction events. Ryskin's hypothesis also considers implications for magnetic fields on other terrestrial planets. The ongoing exploration of these theories highlights the complexity of understanding Earth's magnetic field origins.