pressure decreases
As you rise up through the layers of the atmosphere, both the density and pressure decrease. This is because there are fewer air molecules at higher altitudes, leading to lower density and pressure.
As one progresses from the lithosphere towards the inner core of the Earth, the density generally increases. The inner core is the densest layer of the Earth due to the high pressure and temperature conditions, while the lithosphere, being the outermost layer, has lower density materials like rocks and soil.
When rock layers are folded, a geological fold happens. These folds form under various conditions such as stress, hydrostatic pressure, pore pressure, and temperature gradient.
As someone descends through a water column, the pressure increases. This happens because water at higher levels exerts weight on the lower layers of water.
Pressure through layers of crust
They melt. Coal turns to diamond.
sun light bends
the same thing that happens when you divide by zero.
Pressure decreases as you move outward from Earth's interior. This decrease is due to the weight of the rock layers above exerting less force as you move towards the surface. The pressure gradient is part of the reason why we have different layers within the Earth.
Then fluid can travel through the rock, and the rock is said to be "permeable".
Not exactly. Some metamorphic rocks have foliation, which can appear similar to the layers of sedimentary rock. Foliation develops from mineral grains being oriented by pressure, rather than the deposition of layers.
The layers of the Earth in order from lowest pressure to greatest pressure are the crust, mantle, outer core, and inner core. The inner core experiences the highest pressure due to the weight of all the layers above it.