Scientific Basis and Geophysical Consequences of Geomagnetic Reversals and Excursions: A Fundamental Statement

Herndon, J. Marvin (2021) Scientific Basis and Geophysical Consequences of Geomagnetic Reversals and Excursions: A Fundamental Statement. Journal of Geography, Environment and Earth Science International, 25 (3). pp. 59-69. ISSN 2454-7352

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Abstract

Convection in Earth’s georeactor sub-shell is responsible for generating the geomagnetic field and for maintaining the critical balances necessary for stable sub-core nuclear fission. External factors capable of disrupting sub-shell convection are trauma at Earth’s surface, for example by meteorite impact, and electrical energy transfer via Faraday’s electromagnetic induction into the georeactor by changes in the solar wind or in the magnetospheric ring current. Reduced sub-shell convection not only leads to decreased geomagnetic field intensity, but to increased uranium settling out into the sub-core where it undergoes uncontrolled nuclear fission until sub-shell convection is reestablished. Periods of uncontrolled georeactor nuclear fission are responsible for causing geophysical phenomena at Earth’s surface that are associated with geomagnetic reversals and excursions. Anticipated consequences of sub-shell convection collapse include increases in volcanic activity, increases in the number and intensity of earthquakes, warming of the oceans, and diminishment of atmospheric convection resulting in global warming at the surface. The most worrisome potentiality is triggering the eruption of the Yellowstone super-volcano. Changes in solar wind flux, too small to cause geomagnetic field collapse, however, may cause increases in earthquakes and volcanic eruptions. The understanding described here potentially provides a basis for the development of earthquake and volcanic eruption prediction methodologies.

Item Type: Article
Subjects: SCI Archives > Geological Science
Depositing User: Managing Editor
Date Deposited: 16 Feb 2023 06:54
Last Modified: 01 Aug 2024 13:57
URI: http://science.classicopenlibrary.com/id/eprint/278

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