As you go deeper into Earth's crust, the temperature and pressure increase. The rocks become hotter and more compact, leading to changes in their physical and chemical properties. You may also encounter different types of rocks and mineral deposits at various depths.
As you go deeper and deeper the layers will start to get hotter and thicker.
earthquakes and volcanoes
The temperature of Earth's crust increases as you go deeper due to geothermal gradient. It varies depending on factors such as location and tectonic activity, but on average, the temperature increases by about 25 to 30 degrees Celsius per kilometer depth. The temperature difference can affect the physical and chemical properties of rocks and minerals found in each layer of the Earth's crust.
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).
The geothermal gradient in the Earth's continental crust typically ranges from about 20 to 30°C per kilometer depth. This means the temperature increases by 20-30°C for every kilometer you go deeper into the Earth's continental crust.
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.
Heat
the weight of the rocks above you...
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.
Because the density of the force increases.
The pressure increases as you go deeper below the Earth's crust due to the weight of the overlying rock and other materials. As you move deeper into the Earth, the layers above exert a greater force, causing the pressure to rise. This phenomenon is known as lithostatic pressure.
Each relationship between each layer is different. Like the mantle and the outer core. Its like the mantle is solid and it starts to soften and turn to liquid the deeper you go. Or like the outer core and the inner core . The outer core starts to get harder and denser and the deeper you go the solider it gets. Like the mantle and the crust too. The mantle gets a little more solid and becomes the crust.
earthquakes and volcanoes
The pressure would decrease as you moved from the core to the crust.