The Earth’s Nuclear Core

The nucleus of the earth that is the core of the earth is like a huge nuclear reactor that burns uranium to lighter elements and produces numerous geological phenomena observed on the earth. This nuclear fission reactor generates most of the earth 's heat, energy, and geomagnetic phenomena. There is a good reason to believe that the Earth's center is a huge nuclear reactor with empirical data from the Earth, and there is logical evidence that the theory is correct.

The structure of the earth can be defined in two ways. Mechanical properties such as rheology, or chemical properties. Mechanically, it is divided into lithosphere, asthenosphere, middle ring mantle, outer core, core. In chemistry, the earth can be divided into crust, upper mantle, lower mantle, outer core and inner core. The geological formation of the Earth is deep inside the Earth's surface. Stratification of the earth is estimated indirectly from the refraction of the earthquake and the movement time of the reflected seismic waves. The core does not pass the shear wave and the moving speed (seismic velocity) is different in other layers. According to Snell's law, changes in seismic velocity between different layers cause refraction, such as light bending through the prism. Likewise, the reflection is caused by a significant increase in seismic velocity and resembles the light reflected from the mirror.

What is the structure of the earth, and what is the process of forming the surface of the earth? Think of the earth as an onion with five major levels. The first part of the earth, the inner part is the inner core. This is a solid consisting mainly of iron and nickel. Scientists are located 5,000 kilometers below the surface of the earth, so we can not actually enter the kernel for testing, but we anticipate that the core is solid. The second layer from the inside to the outside is the outer core. The outer core is molten, or molten iron or nickel. It is located between 2891 and 5150 kilometers in the earth. The third layer that occupies the majority of the earth is the mantle. The depth of the basement is 40 to 2900 km. It is made of lava, lighter than the iron and nickel cores, but heavier than the Earth's crust - the fourth and last layer of the earth. The thickness of the crust is 15 to 200 kilometers, made of lightweight material remaining on the surface of the earth.

First, let's see the structure of the earth. The planet consists of three main shells: a very thin brittle shell, a mantle and a core. The core accounts for only 15% of the earth 's volume, but the mantle accounts for 84%. The Earth's crust occupies the remaining 1%. The composition of the Earth's crust is entirely different from that of the whole Earth. The heavy elements are separated towards the center and the light elements are separated towards the surface. This crust consists of approximately 95% igneous and metamorphic rocks, 4% shale, 0.75% sandstone, and 0.25% limestone. The average composition of continental crust is similar to granodiorite (medium to siliceous igneous rock), but the average composition of oceanic crust is basalt (low silica igneous rock).