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© Trunaev E.M. Part 2 The Basic Stages in Earth's
Pre-geological Development Scientific research has uncovered facts at odds with ideas about the structure and evolution of the solar system. The giant planets and their spherical satellites exhibit unexpectedly high thermal activity, though they used to be considered a mix of gas, ice dust or pieces of ice. It appeared that the surface of the majority of the satellites was a firm crust beyond the molten stage, though having obvious attributes of active volcanoes in the past or present. The chemical composition of all these satellites was found to have unusual variety and to highly differentiated, showing the existence of heavy chemical elements of the ferric and other groups, even the in small satellites of the giant planets. However, the real sensation was the detection of magnetic fields, or attributes of residual magnetization, in the mountain rock of all the planets in the Solar System, and the presence of magnetic dipoles on many satellites of the giant planets. A firm basis in natural science attests to these facts; they cannot be understood or explained by traditional cosmogenic theory. The following explanation seeks to resolve these and other essential, important questions of natural science. After fragments of the Vortex
sleeves separated, whirlwinds of second and third orders ("NC" - new
micro-vortex) were generated– future planet cores and their satellites – all of them
developing independently, governed by the common laws of development of cosmogenic
vortexes. As neutral gas proceeds to the center, the concentration of particles in each
whirlwind increases, and the circulatory speed grows exponentially, in some parts of the
spiral reaching 650 km/sec. The energy of particles moving at 650 km/sec is equivalent to
a temperature of 108 degrees Kelvin. With such kinetic energy (kinetic
temperature) electrons are broken off of their orbits in atoms, and gaseous matter
gradually passes into a plasmic state. The plasma is in cosmogenic vortex of alternating
layers of protons and electrons, providing it with a so-called quasineutrality. In the formation of the
magneto-ionic mantle, each “NC” (including our star, the Sun) has a preliminary stage
of formation, starting as rather flat, quickly rotating objects in slowly rotating
spheroids. A certain amount of matter becomes isolated in the cneter of every vortex
through the interaction of the dipole's “trunk” power lines and their particles of
rotating plasma. This matter assumes the form, properties, and functional capabilities of
an adiabatic pseudo-speherical (negative curvature), open, magnetic snare (bottle). [see fig. 3-a]. More complicated chemical structures continued to develop inside the Solar System, right up to the plasma’s complete disintegration and the disappearance of the magnetic field’s dipole. (This has happened with Mercury and the Moon.) It is known that about 1/3 of Earth’s total weight is concentrated in a small, very dense core, which is essentially the remains of the original hydrogen, formed through the differentially rotating plasma. About 2/3 of the mantle’s weight consists of matter "pumped" from the core, thereby giving it a variegated structure. Our planet’s core today is comprised of considerably deteriorated cosmogenic vortex; consequently, the Earth has a moderated magnetic field. The majority of the planet’s matter consists of plasma, hard rock, liquid, and gas, which are located, respectively, in the mantle, the crust, the hydrosphere, and the atmosphere. Some planets still have plasma (in their core), serving as the raw material for the construction of new elements or matter. (Some of this “building-block” material is hydrogen and helium, often called “relics”.) Second-generation hydrogen flows up through fractures to the top of the mantle, then the crust, and finally the atmosphere, bonding with oxygen and ozone to form water. This clarifies how so-called "ozone holes " are formed over deep fractures, especially over the Earth’s southern region (East Antarctica, [see fig. 3-b], where hydrogen is quite abundant.
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