As result of the circular motion of the rigid Earth's coating around the first liquid layer of the Earth's mantle, there are seeming changes in the position of the magnetic poles
New theory of tectonic plates movement of the lithosphere of the Earth
Author Bogdan Góralski
Library of the Historical Institute of Warsaw University
Abbreviations used:
oceanic plate OP centrifugal force -F
continental plate CP angular velocity - ω
Earth's upper mantle EUM linear velocity-V
solar system SS angular momentum- L
The Milky Way Galaxy MWG mass of plates of the lithosphere- m
interplanetary magnetic field IMF length of day - LOD
the radius of the rotating mass - r
The solar system travels through the Milky Way Galaxy at about 250 km / second, swirling around the center of the Galaxy once every 200-250 million years. On the way the SS crosses the four spiral arms of the MWG, which are compacted matter of the Cosmos. Passage through the clusters of galactic arm stars is enhanced by the gravitational effects of the MWG arms on the Solar System. This results in periodic changes in the SS geometry and, as a result, changes in the gravitational field SS. The gravitational interaction of the masses of the Solar System changes the position of the Earth's rigid coating, rotating and sliding along the liquid layer of the Earth's interior. The solid metallic inner core moving in the fluid outer core remains motionless in the grip of the magnetic field of the Sun.
As a result of the circular motion of the rigid Earth's coating around the first liquid layer of the Earth's mantle, there are seeming changes in the position of the magnetic poles on the surface of the earth's crust. So far it has been thought that magnetic poles are moving. My concept assumes that the magnetic poles are stable in the grip of the IMF's magnetic field, whereas the rigid earth's coating move around the liquid interior of the Earth.
I have numerous evidence of this phenomenon, including changes in the location of climatic zones on the surface of the Earth, which can only be explained by the cyclical movements of the Earth's shell relative to the ecliptic and the Sun. So precession of the earth's axis does not exist, because the earth's surface rotating by tilting and deviating from the Sun due to the change of gravity.
The northern hemisphere's lithosphere consists of more massive continental plates than of the southern hemisphere lithosphere, which contains more less heavier oceanic plates. The varying gravitational forces of the Solar System more strongly influenced by the heavier lithosphere of the northern hemisphere, causing the earth's coating continuous motion around the stationary, fluid interior of the Earth. This constant movement of the earth's shell causes friction within the Earth, which heats the internal earth masses and keeps them in liquid state. The differences in the Earth's mass distribution result in a change in the position of the earth's coating, which consists of the shell and the upper mantle floating over the Earth's mantle. The location of the Earth's coating is influenced by the gravity of the Moon, the Sun, and the SS planets, as well as the gravity of smaller space objects. Changes in the location of the Earth's shell, which are the result of the above-mentioned interactions, change the moment of inertia of earth masses, resulting in oscillations of the Earth's rotation speed.
Changes in the mass distribution on the surface of the Earth cause in the end seeming changes in the position of the magnetic and geographic poles. Changes in the location of earth's coating relative to the ecliptic are characterized by cyclical changes in the angular velocity of the earth.
Linear velocity of rotation of Earth V (V = ω r - angular velocity "ω", radius of Earth "r"). Linear speed at the equator is 1667km / h, and at the pole zero. If a part of the earth's shell moves closer to the equator, the effect of the centrifugal force on the lithosphere plates increases, which then initiates movement of them on the surface of the Earth. It follows that changing the position of the earth's coating distorts the equilibrium of the placement of the continental plates CP and the ocean plates OP of the lithosphere because when they were at the pole and part of the earth's shell moved closer to the equator, the greater the centrifugal force F = mr ω2, which causes them to move on the surface of the globe, which is caused by huge differences in centrifugal forces acting between the equator and the poles. The differences in forces acting on lithosphere plates result from the difference in radius r - the distance of the spinning mass of the plates from the axis rotating at a high velocity of the globe. This difference increases as the OP and CP slid across the globe from the pole to the equator.
The length of Earth's day is constantly growing and the cause of its continuous growth is the gravitational effect of the Moon. Earth Day was 6 hours long when the Earth was formed, and 400 million years ago, the day was 21 hours long, so the speed of rotation of the Earth was much higher, so the centrifugal forces acting on the earth's lithosphere plates were also larger. Higher rotation speeds and greater centrifugal forces shifted lithosphere plates with greater power during subsequent orogene, corresponding to periods of significant change in the Earth's coating position relate to the ecliptic plane. The ancient, seemingly inverse, position of the magnetic poles observed today demonstrates the rotation of the earth's coating, such that the northern and southern hemispheres turn into places.
The Earth's crust, consisting of rigid lithosphere plates floating in a ductile, viscous upper mantle (EUM), is made up of several kilometers basaltic OP plates (5 km in Hawaii) and continental plates CP varying to several tens of kilometers (25 up to 60 km in the California area). The lithosphere, which contains part of the upper mantle of the Earth, travels on the hot and ductile mantle (at a depth of 100-200 km the rock reaches the melting point) probably under constant changes in the centrifugal force resulting from the changing position of the Earth's coating.
Changes in the angular velocity of the Earth are due to continual changes in the location of the Earth's coating. On the massive and irregularly dense coating of the Earth most influence by the variable forces of gravity of the Solar System.
The angular momentum ( L) of the rotary body depends on its mass, dimensions and velocity and the radius of rotation. Mases of lithosphere plates are very diverse and vary in their susceptibility to changes in angular momentum. Continental plates CP are larger, thicker and more resistant to slipping in the ductile and viscous magma of the upper mantle compared to the OP. The OP performs a greater movement than the CP (at the same time) in response to the centrifugal force resulting from the changing position of the Earth's shell. Larger shift oceanic plate in the horizontally direction cause the OP to plunge beneath continental plate CP or submerge beneath other and larger OP. Diving of the ocean plate under the continental plate is caused by the increasing mass of deposits on the older edge of the ocean plate, which is subject to subduction.
L = I x ω - Moment of inertia - I, angular velocity ω => L = I x V / r
The smaller mass, size, and elasticity of the ocean plates (OP) results in greater lability of them during changes of linear velocity changes on the surface of the globe. This causes the OP slides down beneath continental plates which are being more massive (and with higher moving resistance) during moving in the earth's magmatic environment. In this way subduction zones are formed in which fragments of the earth's crust are absorbed by the ductile and hot magma of the earth's mantle. Dipping the OP in the east direction takes place during the acceleration phase, and dipping the OP in the west direction during the delay of the movement. This leads to continual migration of continents which sometimes results in a collision of several continental plates CP, which then large continental plates are formed.
Changeible the Earth's rotational motion is the result of earth coating motion the surface of the globe, consisting of phases of acceleration and delay in different periods, from a day to millions of years, and the consequent multiple of angular momentum changes cause continuous motion of the lithosphere plates on the Earth's surface.
This movement was characterized by periods of increased intensity of tectonics known as orogene, eg Baikal, Caledonian, Hertzian, Himalayan, and alpine. They were correlated with the cooling of the Earth's climate, which indicates the biggest changes in the location of the Earth's coating and the speed of Earth's rotation at these periods. Correlation of cool periods with periods of intense earth's coating shifts and accompanying seeming changes in the location of magnetic poles results from my theory of the climatic mechanism of the Earth (Góralski 2017).
The movement of lithosphere plates may also be due to the movement of magma within the earth's mantle, induced by the more frequent (diurnal) and larger oscillations of the solid metallic inner core moving within the metallic liquid outer core, resulting in the pumping effect of the liquid masses of the outer core on the eccentric pump principle. The denser magma of the lower mantle of the Earth, moving under the influence of movements in the outer core of the Earth, acts on the less dense magma of the upper mantle, which may cause additional movement of the lithosphere plates.