I see what you are alluding to now.
In RE theory, the magnetic field is generated by the dynamo effect of the mantle and core of the earth, and is by definition equidistant from all points on the surface of the earth (approximately). That gives the earth a relatively smooth magnetic field density. In FE theory, the north pole is in one place, relatively close to the "surface" (is there an official FE term for the top side of the world?)
Since that is the case, the magnetic field of the earth should vary with the distance to the north pole, since it is not equidistant from all points on earth. It would be slight, granted, but it would be much stronger at the north pole (which it isn't), as that is as close to the magnetic north pole as you can get in FE theory.
Also, since you said the north and south pole are in the same place, relatively, how would one know if they were at the north or south pole? Wouldn't the compass give false readings?
If I were to fly a plane DUE SOUTH (or directly away from the 'hub'), I would eventually fly off the disk, right? None of this circumnavigation either, I would go to the heart of antarctica.
how does FE theory explain seasons? Season exist due to the earth's axis of inclination relative to the sun. If it were zero degrees, we would have little differentiation of seasons. It is 23.5 degrees, and varies from 22.5 to 24.5 in a long period (something like 25000 years). The intensity of the sun does not change during the different seasons.
I'll stop for now
