Model with Magnetic Field (IMAGE)
Caption
The bottom-most layer of the moon's mantle melts to form a metal-rich "basal magma ocean" that sits on top of the moon's metal core. Convection in this layer may have driven a dynamo, creating a magnetic field which would have been recorded at the surface by the cooling lunar crust, including the samples brought back by Apollo astronauts.
Credit
Aaron Scheinberg
Usage Restrictions
None
License
Licensed content