metmorphic rack
They're called metamorphic rocks.
Metamorphic rocks are formed from an existing rock (of any of the three types) being subjected to a combination of heat and pressure.
Metamorphic rocks.
A metamorphic rock is a rock that is changed from an already existing form of rock by pressure or temperature
Metamorphic rocks form from existing rocks that undergo a change in temperature, pressure, or chemical environment. This process, called metamorphism, causes the minerals in the original rock to recrystallize and align in new ways, resulting in the formation of a metamorphic rock. Heat and pressure are the main driving forces behind this transformation.
Metamorphic rocks are formed when existing rocks are subjected to high temperatures and pressures, causing them to recrystallize and change form without melting. Examples include marble, slate, and quartzite.
Metamorphic rocks form when existing rocks are subjected to high temperature, pressure, or chemical changes causing the minerals within the rock to recrystallize. This process can occur deep underground due to tectonic forces or during contact with hot magma. Examples of metamorphic rocks include marble, slate, and schist.
Metamorphic rocks form from existing rocks that are subjected to high temperature and pressure conditions, typically found deep within the Earth's crust. This process causes the minerals in the rock to recrystallize and reorganize, resulting in a new rock with different characteristics. Metamorphic rocks can also form through the addition of fluids, which can facilitate chemical reactions and mineral growth.
Metamorphic rocks form when existing rocks are subjected to high temperature and pressure conditions deep within the Earth's crust. This causes the minerals in the original rock to recrystallize and change their structure, resulting in the formation of metamorphic rocks.
a rock
Metamorphic rocks are formed when existing rocks are subjected to high heat, pressure, or chemical changes. This causes the minerals in the rock to reorganize and form new crystals, resulting in a new rock with different characteristics. Metamorphic rocks can have foliated or non-foliated textures, depending on the amount of pressure they were subjected to during formation.
Granite subjected to high temperature and pressure deep within the Earth without melting would likely undergo a process called metamorphism, and would form a metamorphic rock known as gneiss. Gneiss is characterized by its banded appearance due to the reorganization of minerals under intense heat and pressure.