Origin of Mid-Lithosphere Discontinuities

During the Younger Dryas, the entire lithosphere of the Earth was inverted 180 degrees without changing its rotation and then returned by two close passes of a large body acting on the Himalaya, and the Moon was captured marking the beginning of the Holocene. These inversions of the lithosphere heated the asthenosphere and caused the oceans of the Earth to flow across the continents, covering them with salty ocean-bottom material that began the destruction of the serpentine dinosaur life.
6,000-years BP proto-Venus, was born from an impact on Jupiter, a solid, highly deuterated, low density methane gas hydrate giant planet.
Proto-Venus, called A-diti (un-bounded) in the RigVeda, rampaged through the solar system, ejected Mars, a beautiful planet, 600 million years older than the Earth and full of life, from its ancient Venus-like orbit into an orbit that intersected that of the Earth.
Close passes of the incandescent proto-Venus overturned the lithosphere of the Earth two more times, by tidal impulses on the Himalaya, scorching the Earth from the Sahara to the Himalaya, leaving the iridium layer and destroying all remaining dinosaur life, further deepening and heating the asthenosphere and covering the Earth with two more layers of ocean-bottom material.
Mars then became captured in a geostationary orbit 35,000-km above Mt. Kailas “Indra’s Home on Earth”, the focus of the raised Tibetan-Himalayan anomaly, for 14.4-years at a time and was then released for 15.6-years. This 30-year cycle (a day and a night of Brahma) was repeated 99 times, during which period all the vegetable life-forms on Mars were blasted to the Earth from hundreds of volcanos each time Mars passed through alignments with the Moon or the Sun and Moon combined. This material covered the Earth with 50-km or more of sedimentary rocks, soil, 150-m of water, (forming the many rythmic layers of sedimentary rock) and live sprouts in manna, Soma and Haoma.
Although Mt. Kailas is located at 31 N Latitude, the tidal drag of Mars forced the entire lithosphere to rotate with Kailas remaining in the ecliptic plane, and slowed its rotation to 360 days per year, using the heated and thickened asthenosphere as a bearing and a source of rhyolite for continent building.
During each 14.4-year kalpa, Mars raised each 20-m layer of the Deccan traps from the asthenosphere, but because the silicates in the asthenospheric rhyolite dissolved in the ocean, the Traps are composed of basalt. The tidal drag of Mars slowed the rotation of the lithosphere relative to the mantle (by 24 kmph) and the ample rhyolite flowed as cratons up into the continents, layer by layer, through the sea-bottom layers ,
and given the time between each kalpas (15.6-years), the rhyolite cooled slowly, expanding as low-density granite, raising the stable continents in only 3,000 years, between 3687 and 687 BC.. Thus the low density granite is found only in the continents of the Earth.
The cratons, although homgeneous, have recently been found to have been produced incrementally, just as the Deccan Traps and at the same times..
The direct tidal drag of Mars pulled the Eurasian, Arabian and Indian plates toward Mt. Kailas. Mars’ indirect tide moved the North and South American continents westward forming the Atlantic Ocean, created the subduction zones on their west coasts and formed the Pacific ring of fire. The ebb and flow of the eastern Atlantic, Mediterranean (Messinean salinity crisis) and Red sea toward and away from the tidal bulge surrounding the Himalaya (samudra in the RigVeda) at the captures and releases of Mars created a seaway, currently imagined to be evidence of an ancient Tethys Sea that separated super continents Gondwana and Laurasia.
See “The Cosmic Origin of the Rig Veda” by John Ackerman at Booklocker.com