European Journal of Earth Science and Geology (EJESG)
Ocean level – geomagnetic extremity connection as result of revolution geodynamics
(This article belongs to Vol - 01, Issue - 02)
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Abstract
The general inclinations of ocean level and geomagnetic extremity advancement spoken to by their individual polynomial pattern lines are metrically compatible and generally incidental at the principal request and prevailingly at the second request periodicities. Our examination uncovers sequential connection of ocean level highs and lows with the calm and disturbed conditions of geomagnetic field, both causally identified with the thickness subordinate turn compelling of maritime/mainland outside layer and the internal/external center masses individually. Their connection along these lines affirms the job of revolution irritations as a typical pacesetter of the World's surface and inside proceduresISO CERTIFIED

European Journal of Earth Science and Geology (EJESG)
ISSN 2190-0977
Published by SDIP, London, United Kingdom.