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nothing dencity never changes
The different "layers" are classifications of horizontal sections of the atmosphere, volumes which exhibit different attributes. The high and low pressure regions are areas where the atmosphere is thicker or thinner.
When you have thick layers of rocks rebounding where pressure is released
Temperature will decrease as the altitude increases at all levels due to the thinning of atmospheric gasses.
As you go deeper and deeper the layers will start to get hotter and thicker.
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 decreases
Folding happens when rock layers bend and buckle under pressure. Tilting happens when forces from inside Earth cause rock layers to become slanted.
The temperature decreases
Only the crust. The temperature and pressure increases as you go further down into the earth.
nothing dencity never changes
They melt. Coal turns to diamond.
The deeper you get into the earth, the more weight you have above you. This results in pressure that increases the density of the material below.
The different "layers" are classifications of horizontal sections of the atmosphere, volumes which exhibit different attributes. The high and low pressure regions are areas where the atmosphere is thicker or thinner.
Alluvial soils are transported soils. They are formed of sediments which are brought down by rivers during the passage of their flow. As time passes the sediments get deposited in the form of a layer one upon another. This increases the pressure on the low lying layers of sediments and the temperature in the layers forming the base increases. Then, the process continues for thousands of years and alluvial soil is formed.
On earth, descenting 10 metres is approximately an increase in pressure of 100,000 Pa, 1 atm, 1 bar or 780 mmHg. Water is essentially just little molecules\elements. If the center of the earth is bottom and the eart's crust is the top then water stacks on top of itself like blankets. For simplification let's imagine layers of water 20 feet deep. Every 20 feet you descend in the ocean you are in a deeper layer of water. As you descend deeper and deeper you'll notice that each layer you come in contact with has all the previous layers sitting on top of it. Each layer adds its weight onto the layers below it. 3 Levels deep has two layers above it, 6 Layers deep has 5 layers above it and so forth. The water at each subsequent layer is compressed by this additional weight. This compression is known as pressure in this case water pressure.