There is no absolute trend, since geological faults can thrust older rocks above younger ones, and whole sequences can be turned upside down. However, more often than not, for a single location deeper strata are older.
High water pressure.
In the Heart of the Deep Deep South
Strata.
You can't land on the Great Red Spot; there is nothing solid. If you were to try, you would be whipped around by the winds as you fall. Eventually you will be crushed by the pressure deep in Jupiter's atmosphere.
The pressure of solid rock strata pushes the water to the surface.The pressure of solid rock strata pushes the water to the surface.
Pressure release:Rock deep within earth is under great pressure from surrounding rocks
There is greater pressure the deeper you go in water. So if you go too deep, the pressure in the human lungs will be so great and too much that the persons lungs will collapse.
There is no absolute trend, since geological faults can thrust older rocks above younger ones, and whole sequences can be turned upside down. However, more often than not, for a single location deeper strata are older.
The pressure gets too great and the submarine implodes. The deeper you go under water the more pressure there is.
that changes greatly depending on the strata of the particular areas that you are digging.
Strata - Strata album - was created on 2004-07-27.
pressure of the ground strata around the water pocket
This occurs when moisture goes deep into the soil and can't go further because of rocky strata, leading to landslide
A submarine deep in the ocean is under great pressure, and a space capsule outside the atmosphere is under zero pressure. Both of them are capable of high acceleration, zero acceleration, and anything in between. The pressure is irrelevant.
Each layer is deposited over time as the environment changes over millions of years. The process is deposition of differing sediments, forming strata. When buried at great pressure, the rock is formed, and the strata are evident. Layers may also be caused by lamination of the sediments or through mineral banding (especially in sandstones).
It increases the likelihood of mass movement as the pressure of lower faults, joints and strata has increased.