This is generally what we are working with.
It appears now that the magnetic field strengths and areas change in conjunction with the light and gravity factors according to the change in latitude on the Earth’s surface. During these changes, the harmonic relationships remain constant.
The basic unit for harmonic calculation is the geodetic inch, or one seventy-two thousandth of a minute of arc—one minute of arc being 6,000 geodetic feet (6,076 British feet). If we take the valties 1257 and 1850 lines of magnetic force per square centimetre and make a fractional correction to allow for the curvature of the Earth’s surface (the given square centimetre area would have fractionally curved sides), we can then establish a theoretical field density of 1257.139035 lines of force in one direction, and 1850.900532 lines of force in the other. This will allow the calculation of the field densities for one square geodetic inch in the north and south pole areas, which can be mathematically related to light and gravity factors.
Field A: 1850.900532 lines of force per square centimetre, converts to 12245.69798 lines of force per square geodetic inch.
Field B: 1257.139035 lines of force per square centimetre, converts to 8317.32698 lines of force per square geodetic inch.
