The new climatic theory-Climatic effect of Earth's coating movement

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dc.contributor.authorGóralski, Bogdan
dc.contributor.organizationBiblioteka Instytutu Historycznego Uniwersytetu Warszawskiegoen
dc.date.accessioned2019-01-31T09:33:05Z
dc.date.available2019-01-31T09:33:05Z
dc.date.issued2019-01-30
dc.description.abstractThe temperature of the interior of Earth is sustained by the constant friction between the COATING of Earth and its LIQUID CORE. The coating of Earth, consisting of the crust and the upper mantle, is rotating under the influence of the alternating impact of the solar system and is rubbing against a liquid, metallic Earth's outer core, which is a spherical sliding surface for Earth's coating. Changes in Earth’s climate (which are dependent mainly on the heating of its surface) are an evidence that Earth’s coating moves in relation to its core. Climate change resulting from the tilt of the globe in relation to the sun causing the succession of the seasons. On top of this there are circular movements of Earth's coating around the axis of rotation of Earth.en
dc.description.sponsorshipmoja żona i ja
dc.identifier.urihttps://open.icm.edu.pl/handle/123456789/16461
dc.language.isoen
dc.rightsUznanie autorstwa-Użycie niekomercyjne 3.0 Polska*
dc.rights.urihttp://creativecommons.org/licenses/by-nc/3.0/pl/*
dc.subjectnew climatic theoryen
dc.subjectmovement of Earth's coatingen
dc.subjectclimate changesen
dc.subjectshift of Earth's crusten
dc.subjecttrue polar wanderen
dc.titleThe new climatic theory-Climatic effect of Earth's coating movementen
dc.typeworkingPaperen
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