When rocks are subjected to high pressures, they can change their formation and appearance. This process, which alters the structure of a rock, is called metamorphism.
The conditions that affect physical stability are heat, temperature, compression, pressure, and the molecular structure.
Pressure IS the force of colliding particles, so the more the higher.
Two factors that contribute to the formation of metamorphic rocks are pressure and temperature.
Depending on the rock type, some may explode from excessive heat and pressure. Others may simply melt, if the temperature is hot enough, like that of magma.
Temperature, pressure, availability of source material, and space available for formation all affect the crystallization process of minerals.
The two main factors that affect the temperature at which rocks melt are the composition of the rock and the pressure acting on it. Different minerals have different melting points, so the composition of the rock will determine its melting temperature. Additionally, pressure can increase or decrease the melting temperature of rocks, with higher pressure generally increasing melting temperature and lower pressure decreasing it.
Wind and water can affect rocks by carrying them around and eroding the rocks by such pressure
There are two factors that affect gas pressure. These factors are temperature and volume. Higher volume means lower pressure. Higher temperature means higher pressure.
There are two factors that affect gas pressure. These factors are temperature and volume. Higher volume means lower pressure. Higher temperature means higher pressure.
Gives it higher pressure.
The conditions that affect physical stability are heat, temperature, compression, pressure, and the molecular structure.
The conditions that affect physical stability are heat, temperature, compression, pressure, and the molecular structure.
because the great amount of pressure creates higher density
The higher the blood pressure the faster your heart rate
There is a direct relationship between the temperature at which water boils and the air pressure on it. Higher pressure, higher boiling point. Lower pressure, lower boiling point.
Pressure can effect formation, strength, tightness of packing of rocks and mineral and total geological make-up.
Pressure IS the force of colliding particles, so the more the higher.