Could All Help With Signing My Petition
Seasonal6 mins ago
No best answer has yet been selected by brassmonkey. Once a best answer has been selected, it will be shown here.
For more on marking an answer as the "Best Answer", please visit our FAQ.That's basically it, CT.
The mantle itself is only about 5-10% molten, so is not fluid enough to have sufficient flow velocity to generate an 'electro-magnetic' field.
Secondly, there is very little free iron in the mantle - most being bound up in the form of iron-rich silicates (often in association with magnesium).
The Earth's outer core, however, is mainly iron and is in a molten (fluid) state.
{Note that molten iron is not magnetic in itself - if you heat a bar magnet up to a high enough temperature, it will lose its magnetism. This is known as the Curie point, and occurs at about 500�C (off the top of my head) - whilst the temperature of the outer core is somewhere around 4000�C.}
It was Bullard and someone-whose-name-I-can't-remember that proposed the 'self-exciting dynamo' theory in the core - whereby convected liquid iron moving through a small, residual magnetic field, would produce an electric current, which would then generate its own magnetic field etc etc..
It is still poorly understood, and not entirely described mathematically to a satisfactory degree. Although the principle is feasible and it remains the most likely explanation. Polarity is not critical either, which may help account for the relatively frequent (geologically speaking) polarity reversals.