Moon Earth Environment
by Henryk Szubinski
Early Earth evolution of the moon as the sphere that rotated in the fluid space of the Earths oceans and shaped the characteristic IMMERSION FEELING of the TIDAL PULL on Earth ,resulting in the Earths ocean topography as in vectors of alpha = STRETCHING and COMPRESSING=beta as the gamma 3 resulting effect of much of the Lunar details being the types you may observe underwater. The moon has shaped it's Earth interaction into an artificial water environment surface on itself and on the Earth so that the 2 together = the 3rd as the interval between the Earth and Moon.
The vector upwards needed to make the observation of the moon above Earth is also the vector projection that makes the MOON SPHERE exactly visable as from above when placed in the ocean environment so that the observer finds himself above the MOON and looking into the OCEAN DEPTH.
The third vector observation uses the interval between the up and down environment of the immersion reality as the GAIA HYPOTHESIS.
by Henryk Szubinski
Early Earth evolution of the moon as the sphere that rotated in the fluid space of the Earths oceans and shaped the characteristic IMMERSION FEELING of the TIDAL PULL on Earth ,resulting in the Earths ocean topography as in vectors of alpha = STRETCHING and COMPRESSING=beta as the gamma 3 resulting effect of much of the Lunar details being the types you may observe underwater. The moon has shaped it's Earth interaction into an artificial water environment surface on itself and on the Earth so that the 2 together = the 3rd as the interval between the Earth and Moon.
The vector upwards needed to make the observation of the moon above Earth is also the vector projection that makes the MOON SPHERE exactly visable as from above when placed in the ocean environment so that the observer finds himself above the MOON and looking into the OCEAN DEPTH.
The third vector observation uses the interval between the up and down environment of the immersion reality as the GAIA HYPOTHESIS.