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Tectonic plates are constantly in motion, at the same rate a human fingernail grows, which gives reason to believe the landscape of the Crust will continue evolving right before our eyes.

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The contents of the planet we live on prove it to be a dynamic and ever-changing floating rock that we so casually call home.

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On the Oceanic crust, seafloor spreading and subduction zones can be seen forming due to plate collision and separation.

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Since Geoscientists have never been inside the earth to see this for themselves, this research has been conducted using Seismic waves, computer modeling, and analysis of meteorites.

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The outer core is a molten lake of iron and nickel that creates Earth’s magnetic field, while the inner core is a solid version of iron and nickel that serves as Earth’s geologic midpoint.

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Movement and heat from below can cause these plates to shift, which can cause natural disasters like Volcanoes and Earthquakes on Earth’s continental crust.

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Below the Mantle, the core is split into two parts: the inner core and the outer core. It is a large circular mass that is only slightly smaller than Earth’s Moon.

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About eighteen miles down, you will find a thick layer of silicates, called the Mantle. The mantle is made of hard rock although most people believe it is composed of magma.

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The Earth's Crust is split into the Continental Crust and The Oceanic Crust, which are both made of Tectonic Plates that fit together like puzzle pieces.

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Thankfully, the Inner Earth does not hold any advanced civilizations or creatures trying to flee from hell.

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When you look at a picture of our tiny blue dot, it’s hard to imagine layers of molten rock beneath the surface. The Earth is composed of 4 distinct layers: Crust, Mantle, Inner Core, and Outer Core.