no, the process only happens to igneous rocks
Metamorphic
A metaphorphic rock is a rock that undergoes changes to become a different type of rock. The rock changes due to extreme pressure wich makes them heat up, and change types.... i hope this helps :)
Great pressure and heat, but short of the temperature that would completely melt the rock.
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there are 4 bill bob and jerry and the one in abi's head she likes to call a brain Igneous, Sedimentary, and Metamorphic.
No. It's the Metamorphic rocks that melt and become magma.
No, sedimentary is formed by compression. Metamorphic is created by heat and pressure. Sedimentary can be melted to create metamorphic.
yes
Metamorphic
Igneous rocks-after having the chance to cool down after a melt (metamorphic rocks need pressure as well)
Sedimentary and Igneous rocks are not metamorphic rocks. Metamorphic rocks however are igneous or sedimentary rocks that have undertaken metamorphism (In extreme heat and/or pressure the minerals are forced to recrystalize) and become metamorphic rocks. If the heat/pressure causes the rock to melt into liquid rock than it is no longer metamorphi, it is igneous. Hope this helps :)
Metamorphic rocks become igneous rocks by melting from heat and pressure, remnants of which may cool from melt (magma) and become components of igneous rock.
metamorphic
metamorphic
Nope, because they are created when the Earth pressurizes and heats it (but not to the point of melting). Igneous rocks are created when rocks melt.
When metamorphic rocks are heated, the minerals within the rock may undergo recrystallization, transforming into new minerals. This process can lead to the development of new textures and structures in the rock. However, excessive heat can cause the minerals to melt and reform as igneous rocks.
No, rock does not melt when it is changing into metamorphic rock. Metamorphic rocks form from pre-existing rocks, such as sedimentary or igneous rocks, through a process called metamorphism. This process involves changes in temperature, pressure, or the presence of fluids, which cause the minerals in the rock to recrystallize without melting.