Magnetic and Quasi-Magnetic Fields: A CRVD Analysis

This document establishes, entirely within the CRVD framework, the distinction between the two field phenomena conventionally gathered under the single label of “magnetism.” The first is genuine, intrinsic magnetism: a property that originates in the internal structure of matter itself, specifically in the enforced asymmetry of the collective electron cloud within a ferromagnetic crystal lattice. The second is the field that standard physics names “the magnetic field of a planet”: a phenomenon that is not an intrinsic property of the body at all, but a geometric image of its interaction with the surrounding electron-bearing environment — the trapping and rotation of free charges inside a spinning gravity well. For this second class, the corrected term adopted throughout this document is the Quasi-Magnetic Field. The document derives the formation mechanics of both classes, applies the triad of causal factors (gravity-well depth, spin rate, and electron feed rate) to Earth, the Moon, Venus, Jupiter, Uranus, and Ganymede, and closes with a comparative table of the governing factors