Metamorphic rock
the metamorphic rocks are formed by heat and extreme pressure from other rocks
Sedimentary Rocks.
Metamorphic rock forms when heat, pressure, or fluids act on existing igneous, sedimentary, or other metamorphic rocks, causing changes in their mineral composition, texture, or structure. Examples of common metamorphic rocks include slate, marble, and gneiss.
B. Metamorphic rock. Metamorphic rock forms from existing rocks that are subjected to high temperatures and pressures, causing them to recrystallize and change in composition without melting.
A rock that forms from other rocks due to heat and pressure beneath the Earth's surface is called a metamorphic rock. Examples include marble, slate, and gneiss.
Metamorphic rocks are formed when existing rocks are subjected to high pressure and temperature deep within the Earth's crust. This process causes the minerals in the original rocks to recrystallize into new forms, resulting in metamorphic rocks like marble, slate, and gneiss.
Metamorphic rocks
Metamorphic rocks are produced from other types of rocks (igneous, sedimentary, or existing metamorphic rocks) under high temperature and pressure conditions. The existing rocks undergo changes in mineral composition and texture without melting. Examples of metamorphic rocks include marble, schist, and gneiss.
Metamorphic rock forms from the recrystallization of pre-existing rocks due to high heat, pressure, or chemical processes. Examples of metamorphic rocks include marble, slate, and schist.
High temperature and pressure can cause rocks to change their forms. This is known as metamorphic.High pressure and high temperature can cause rocks to change forms. This is known as metamorphic.
Heat and pressure causes Metamorphic Rocks to form.
Metamorphic rocks are formed underground through the process of heat and pressure altering existing rocks. When rocks are buried deep in the Earth's crust, they are subjected to high temperatures and pressures that cause their mineral composition and texture to change. This results in the formation of metamorphic rocks from pre-existing igneous, sedimentary, or other metamorphic rocks.