maybe heat can make have the pressure
pressure.
The three agents of metamorphism are heat, pressure, and chemically active fluids. Heat causes recrystallization of minerals, pressure can deform rocks, and chemically active fluids can alter the mineral composition of rocks.
The three agents of metamorphism are heat, pressure, and chemically active fluids. Heat causes minerals to recrystallize, pressure changes the mineral structure, and chemically active fluids can introduce new elements into the rock.
Heat, Pressure, and Chemically active fluids.
The primary agent of contact metamorphism is heat from the intrusion of magma into surrounding rocks. This heat causes changes in the mineralogy and texture of the rocks without significant pressure changes.
The most important agents of metamorphism are heat, pressure, and chemically active fluids. Heat causes minerals to recrystallize, pressure reorients mineral grains, and chemically active fluids introduce new elements to form new minerals. Together, these agents drive the changes in rock composition and texture during metamorphism.
Heat and pressure.
Magmatic intrusionsBurial to great depth by sedimentary overburdenPlate tectonic collision
Pressure, accompanied by deformation, can also cause metamorphism. The application of high pressure over long periods can alter the mineralogy and texture of rocks, leading to metamorphic changes.
Two processes that can cause metamorphism are heat (from deep burial or nearby magma) and pressure (from burial or tectonic forces). These processes can change the mineralogy, texture, and sometimes the chemical composition of rocks, leading to the formation of metamorphic rocks.
Metamorphic rocks are formed by the process of extreme heat, pressure and other chemicals. Two types of metamorphism are dynamic which makes the pressure and extreme heat and thermal which is caused by the heat of magma from a volcanic eruption.
Metamorphism