Global Journal of Science Frontier Research, A: Physics and Space Science, Volume 23 Issue 1

"Mountain formation is a geological process of formation of mountain structures under the influence of intense upward tectonic movements, whose speed exceeds the speed of processes leading to the leveling of the Earth's surface." This process is commonly explained in this way, but, as already noted earlier, there are no upward movements inside the planet. The most similar phenomenon to mountain formation in the environment is river rapids. There is a flow of water in a river and there is movement of mass under the crust inside the planet. There are big masses moving in both places, there are rapids in a river and mountains on land. The location of mountains is mostly south-north, across the movement of mass inside the planet, the location of rapids is mostly across the flow, but there are exceptions in both places. The analogy is complete. (Fig. 13). The movement of the planet's core mass is constant and multi-millennial. Mountain formation alternates with the destruction and weathering of mountains. Second question: The origin of geosynclines (deep valleys filled with deposits); According to Uyeda, "Many mountain rocks that make up modern mountain ranges originally accumulated on the seabed, and their thickness often exceeded 10,000 meters." If the formation of mountains is possible with the rise of the bottom of a former ocean by several kilometers, why is it not possible to form valleys at the same time? If we look at how gorges are formed, everything becomes clear. Third question: The causes of volcanic eruptions and other magmatic processes; Let's go back to the rotating aquarium. The contents of the aquarium, or rather, its heaviest and densest part, move along the wall, along the boundary of the body. The same occurs inside the planet. Where is this boundary? Maybe this is the Mohorovičić boundary? Yes, it is possible, but if we imagine the inner surface of the aquarium not from a smooth glass, but like, for example, the bottom of a mountain stream, then all kinds of deposits will appear in the form of small fragments, over which bare cliffs rise - in our case, these are the "underground" parts of mountain ranges. Just like in ice when troughs are formed, voids and cracks occur in the Earth's core, through which magma, under the pressure of constantly moving core mass, emerges to the surface. Once a channel has formed, melting and forming a throat, it becomes a place of eruption for many centuries. It is important to note that the pressure of the moving mass will be directed not towards the center of the planet, but towards the external gravitational force, i.e. the Sun and Moon. And moving under the throat, this mass will squeeze out magma like a piston. Fig. 14: The direction of the movement of the mass of substance causing pressure in the area of existing volcanic vents has been added to the illustration from Uyeda's book. The areas of mass accumulation before the earthquake and the area of maximum seismoactivity are indicated 1 Year 2023 55 © 2023 Global Journals Global Journal of Science Frontier Research Volume XXIII Issue ersion I VI ( A ) The New View at the Physics of the Planet Earth

RkJQdWJsaXNoZXIy NTg4NDg=