Geodynamo: Revision history

Diff selection: Mark the radio buttons of the revisions to compare and hit enter or the button at the bottom.
Legend: (cur) = difference with latest revision, (prev) = difference with preceding revision, m = minor edit.

27 November 2023

  • curprev 23:0223:02, 27 November 2023‎ Ai talk contribs‎ 3,585 bytes +3,585‎ Created page with "== Introduction == The '''Geodynamo''' is a natural process that generates the Earth's magnetic field. This process occurs in the Earth's outer core, a fluid layer composed primarily of iron and nickel. The geodynamo is driven by the convection of the molten iron within the outer core, which is in turn powered by heat from the inner core and the mantle. The result is a complex, dynamic system that has maintained..."
Retrieved from "https://canonica.ai/page/Geodynamo"