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As you go deeper and deeper the layers will start to get hotter and thicker.
earthquakes and volcanoes
The crust goes down about 10 kilometers. Continental crust is about 3 billion years old and oceanic crust is about 70-100 million years old.
Sometimes the plates on the earths crust crash into each other, forcing one to go lower. The friction causes the rock to get hotter and hotter until it melts. This is called magma. The magma keeps getting hotter, but it needs somewhere to go, so it surges up through the earths crust, making a hole. That is how a volcano is made. Once the hole is made, magma from the earths core comes to the surface, causing the volcano to spit lava
Below the crust. This varies based on the thickness of the crust and it has to be continental crust for there to be granite. There are some exceptions to this but it is very complex and not very well understood at this time. The crust varies in thickness between ~25km and 70km (Basin and Range province and Himalayan Mountains, respectively).
As you go deeper and deeper the layers will start to get hotter and thicker.
you get hotter and hotter
Because the density of the force increases.
because it gets hotter as you go in to the earths surface. the six miles is only the crust because the mantle is to hot to in to.
We are living on the surface of the Earth's crust. The deeper you would go into the crust, the hotter it would get.
Heat
the weight of the rocks above you...
temperature gets hotter
temperature gets hotter
As you go deeper, there are more rocks above you, and the more rocks you have, the heavier everything above you gets. When something gets heavier, it applies more pressure on an object. Therefore, when you go deeper, pressure on an object increases.
Bitchesf suck fdick
geothermal starts at the outer edge of the earth's crust and gets hotter the deeper you go. The gradual increase in the temperature as the depth increases is called the geothermal gradient. As you proceed through the crust the gradient is gradual. When you break through the upper mantle the temps then rise almost exponentially.