The hypothesis that the Earth's core is Split into Two Halves
The hypothesis that the Earth's core is Split into Two Halves This theory Discovered by: Habiballa Aabker Mohamed [email protected]+201108505785Sudanese: (Republic of Darfur) The Great African Rift Valley: The African Rift is one of the indicators that the Earth's core is split into two sections, extending from the Injiji Valley through Aswan and Oweinat, and passing by Jebel Marra and the Congo. Evidence supporting this lies in the fact that the Earth's core consists of molten iron and—as dictated by physics—contains gold. Since this valley contains gold, it implies that the core—which expels fluids from extreme depths—is secreting gold; indeed, this line is a "gold line." The hypothesis of this split posits that the Earth's interior functions like an electric dynamo. The generated electricity creates repulsive forces within the core, causing it to divide into two halves. Furthermore, this electricity raises the core's temperature; just as connecting electrical poles melts a conductor, this electrical activity causes the Earth's core to remain in a molten state. This explains why temperatures are higher at the Equator: the rift is not static; rather, it is the driving force behind the movement of tectonic plates. Rising temperatures at the Earth's equator and tropics: Many assume that the rise in global temperature at the equator is solely due to the sun being directly overhead—an assumption that is indeed correct. However, from another perspective, the Earth’s rotation causes it to cut across the sun's magnetic field lines most intensely at the equator and the Tropics of Capricorn and Cancer. This generates a massive amount of electricity at the Earth's core; as this electrical energy interacts, it causes the temperature of the iron-rich core to rise drastically, ultimately leading to the melting of the Earth's core.
Authors
- Habiballa Ahmed
Publication Details
- Journal
- Zenodo (CERN European Organization for Nuclear Research)
- Published
- 2026-09-24
- DOI
- https://doi.org/10.5281/zenodo.22942266
- Primary Topic
- Geomagnetism and Paleomagnetism Studies
- Type
- article
- Field-Weighted Citation Impact
- 0.00