Mars` core and magnetism
... were converted into heat it would be sufficient to heat the Marsforming material to several thousand degrees above the melting point, and even with the loss of heat by radiation, a magma ocean is likely. This ocean might be transient (surviving for a brief period after each giant impact), or it migh ...
... were converted into heat it would be sufficient to heat the Marsforming material to several thousand degrees above the melting point, and even with the loss of heat by radiation, a magma ocean is likely. This ocean might be transient (surviving for a brief period after each giant impact), or it migh ...