Of course they can. The overall compositions of the rocks will remain the same (assuming a closed system, which isn't always the case), but mineralogically there will be changes due to metamorphic pressures and temperatures. There are a whole list of minerals which only formed from metamorphic processes.
Blueschist
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the metamorphic rocks are formed by heat and extreme pressure from other rocks
if rock melts it will form magma, which leads to the formation of igneous rocks
Gneiss is a metamorphic rock that meets those criteria.
Gneiss is a metamorphic rock that meets those criteria.
Rocks formed from high temperature and pressure include metamorphic rocks such as marble, schist, and gneiss. These rocks are created deep within the Earth's crust through the transformation of existing rock types under intense heat and pressure conditions.
Rock formed by heat and pressure is called metamorphic rock. It is created when existing rocks are subjected to high temperatures and pressures, causing them to recrystallize into new forms. Examples of metamorphic rocks include marble, slate, and gneiss.
Metamorphic rocks can form from the transformation of pre-existing rocks under high temperatures and pressures. Common parent rocks include shale, limestone, and granite. The minerals present in the parent rocks determine the types of metamorphic rocks that can form.
These rocks are metamorphic rocks. They form when existing rocks (igneous, sedimentary, or other metamorphic rocks) undergo high temperatures and pressure deep within the Earth's crust, causing their minerals to recrystallize and new minerals to form. Metamorphic rocks can have distinct textures and structures depending on the intensity of the heat and pressure they experienced.
Rocks changed by intense pressure and heat become new rocks called metamorphic rocks. These rocks form when existing rocks undergo changes in texture and mineral composition due to high temperatures and pressures. Examples of metamorphic rocks include marble, slate, and gneiss.
Metamorphic rocks change due to heat and pressure. These rocks are transformed from existing rocks that are subjected to high temperatures and pressures, causing them to recrystallize into new forms with different mineral compositions. Examples of metamorphic rocks include marble, slate, and schist.
Slate and marble are examples of metamorphic rocks. They are formed when existing rocks undergo high temperatures and pressures, causing them to recrystallize into new forms with different characteristics.
Igneous, metamorphic, and sedimentary rocks can be changed by high temperatures and pressure, and the resultant rock is called metamorphic, because its form has been changed.
Of course they can. The overall compositions of the rocks will remain the same (assuming a closed system, which isn't always the case), but mineralogically there will be changes due to metamorphic pressures and temperatures. There are a whole list of minerals which only formed from metamorphic processes.
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.