before oceans

BEFORE THE DEEPWATER OCEANS

Formation of the deepwater oceans began after the Permian extinction. Before the extinction the lithosphere draped the planet in an unbroken rocky shell, streached flat by internal pressure from transformation of electrons and positrons into atoms by the planetary field and puntuated by volcanoes which increased planetary surface area by thickening the lithosphere.

Before the extinction earth and mars were in geosynchronous orbits between their present orbits, with the same orbital periods and axial tilts when an impact with the moon on a trajectory with the mass and momentum to knock earth and mars out of geosynchronous orbits on trajectories to orbits closer to and further from the sun.

Before the extinction Earth’s climate was temperate with ice ages and boreal forests, compared to after, during the Mesozoic when the climate was tropical without ice ages.

A map of the titanium abundances on the Moon’s surface indicates extremely high concentrations compared to terrestrial rocks. We mimicked the high-Titanium basalts using high-temperature experiments clearly demonstrating how the melt-solid reaction is integral in understanding the formation of these unique magmas.

Titanium deposits, only on the near side of the moon, suggest the moon’s surface may have been heated by atmospheric friction before impacting Earth, and knocking Earth and Mars out of geo-synchroneous orbits, on opposite trajectories into closer and further orbits from the sun.