Authors: D'Eart Ishintreel
This paper presents a mathematical analysis supporting the hypothesis of an inner planet within the Earth, characterized by a quadrupolar magnetic field. We propose that the oblateness of the Earth at the equator obstructs the horizontal component of the magnetic field, resulting in a dipolar magnetic field observed on the Earth's surface. By deriving mathematical equations and considering the geometry and parameters of the inner planet, we demonstrate the feasibility of this alternative model. The implications of this hypothesis for geophysical processes are discussed, along with the experimental and observational challenges associated with validating this hypothesis.
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[v1] 2023-06-23 05:25:52
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