pressure.
The natural process that causes one kind of rock to change into another is called metamorphism. This occurs when existing rocks—igneous, sedimentary, or even other metamorphic rocks—are subjected to intense heat, pressure, or chemically active fluids, leading to changes in their mineral composition and structure. For example, sedimentary limestone can transform into marble through metamorphism.
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.
Burial metamorphism.
Shale is a sedimentary rock that can transform into other types of rock through the process of metamorphism. Under heat and pressure, shale can turn into slate, while further metamorphism can result in the formation of phyllite, schist, and gneiss.
This is an example of metamorphism, which is the process where rocks undergo changes in response to heat, pressure, or other factors without melting. Shale turning into slate is a common metamorphic process that involves the recrystallization of minerals to form a denser, more compact rock with a characteristic foliation.
pressure.
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.
It's called thermonuclear reaction.
They react and cancel each other out. The process is called neutralization and it causes them to cancel out.
Burial metamorphism.
When rocks stack up on each other, regional metamorphism can occur. This type of metamorphism is caused by high pressure and temperature deep within the Earth's crust, typically associated with tectonic activity like mountain building or collisions between tectonic plates. This process can lead to the formation of new minerals and textures in the rocks.
contact metamorphism is what happens when something is really hot. regional metamorphism on the other hand involves much larger packages of rocks.
contact metamorphism is what happens when something is really hot. regional metamorphism on the other hand involves much larger packages of rocks.
Shale is a sedimentary rock that can transform into other types of rock through the process of metamorphism. Under heat and pressure, shale can turn into slate, while further metamorphism can result in the formation of phyllite, schist, and gneiss.
When rocks grind and squeeze past each other due to tectonic forces, dynamic metamorphism can occur. This process can lead to the formation of mylonites, which are fine-grained rocks with a strong foliation formed from the intense deformation.
Types of metamorphism are Contact Metamorphism Regional Metamorphism Cataclastic Metamorphism Hydrothermal Metamorphism Burial Metamorphism Shock Metamorphism (Impact Metamorphism)
contact metamorphism is what happens when something is really hot. regional metamorphism on the other hand involves much larger packages of rocks.