If the Earth Planet was a big mass of gas, continuous centrifuge forces trough perpetual revolving had separated chemical elements in discontinuous manner; later, by decreasing temperature around the periphery of sphere some atoms were formed composed a solid initial lithosphere; maybe it was tiny composed by unknown rocks; they were metamorphosed during the same Precambrian. Resulting gas from sphere´s spinning, it went up to the highest extreme (North Pole) and pressure from gas accumulated caused an explosion through the top´s crust. After tremendous outbursts, this fundamental crust was fissured, fractured and faulted in several unpattern figures. The sphere continued its permanent rotation, translation, and more internal movements forming volcanic rocks outside and later, their deformations during Paleozoic such as metamorphism by increasing pressure and temperature on pre-existing rocks. Mantle´s lavas had runaway through the crust´s gaps along some meridians around the surface of sphere impelled by Earth´s rotation permitting blowouts forming extrusive rocks. The first volcanoes group at the top of the Earth acted as a balloon while its air is escaping by simple action and reaction, then steam, ash, and lava were moving outside the planet (as a balloon) it gyrating uncontrollably; perhaps, it was a possible cause for old inversions of poles in our sphere.

Hot gases were expelled to the atmosphere and by simple condensation rain occurred initiating water such as streams, rivers, lakes, and oceans as components of hydrosphere. On surface, volcanic rocks flowed to the South by gravity increasing external lithosphere shape as cream on apple with pointy terminations to the South Pole. (i. e. Africa, India, and South America)

Finally a glance, continental crust in America and Africa moved down of the sphere maybe by gravity. It is easy to find heavy metals in bigger deposits such porphyry cooper in the lower part of South America, gold ore deposits in South Africa, and more. Constant revolve of our sphere caused changes in atmosphere and meteorological conditions, which produced weathering, water, erosion, and sedimentation.