Geometric Asymmetry in Terrestrial Metal Formation: A Unified Field Reinterpretation of Subsurface Resource Distribution

This paper introduces a geometric field-based model for understanding metal formation on Earth. Challenging traditional particle-centric explanations, it proposes that metals arise from asymmetric scattering of vertical field flows emitted by the Earth’s core. These scattered flows resolve as lateral surface currents, forming flattened field-shell structures we observe as metal deposits. This framework explains conductivity, malleability, and magnetism as emergent properties of geometric tension resolution, not atomic bonding or electron diffusion. Drawing comparisons with carbon and crystalline materials, the paper offers a unified theory of material behavior based on how matter responds to environmental field tension. Industrial processes like forging and alloying are reinterpreted as acts of geometric reconfiguration. The model redefines metals as dynamic field phases — surface-tension echoes of unresolved gravitational curvature.