Generally, yes, depending on the rock's composition and the altering pressure and temperature.
Metamorphic rocks with a layered or banded look are referred to as foliated.
A banded texture
The Texture term for metamorphic rock which are not banded or layered is non-foliated metamorphic rock. Good examples are marble and quartzite.
A metamorphic rock with definite layers is called a foliated rock. Examples include slate, schist, and gneiss, which form due to intense pressure and heat causing minerals to align in distinct layers. Foliated rocks often have a banded appearance due to this layered structure.
Schistose Structure metamorphic rocks are known as foliated metamorphic rock.
Metamorphic rocks with a layered or banded look are referred to as foliated.
A banded texture
In sedimentary rock it is called striated or stratified. In metamorphic rock it is foliated or gneissic.
Metamorphic rock can be either foliated or non-foliated. Foliated metamorphic rocks have layered or banded textures, while non-foliated metamorphic rocks lack these layers and have a more uniform appearance. Examples of foliated metamorphic rocks include schist and gneiss, while examples of non-foliated metamorphic rocks include marble and quartzite.
The Texture term for metamorphic rock which are not banded or layered is non-foliated metamorphic rock. Good examples are marble and quartzite.
When a metamorphic rock exhibits a layered or banded appearance, it is said to exhibit foliated texture. This texture is a result of the alignment of mineral grains or the presence of alternating light and dark layers. Examples of foliated metamorphic rocks include gneiss and schist.
Layered metamorphic rock is one that has a foliated or banded appearance due to exposure to heat and directed pressure. Examples: phyllite and slate.
Phyllite is foliated.
A metamorphic rock with definite layers is called a foliated rock. Examples include slate, schist, and gneiss, which form due to intense pressure and heat causing minerals to align in distinct layers. Foliated rocks often have a banded appearance due to this layered structure.
Schistose Structure metamorphic rocks are known as foliated metamorphic rock.
Metamorphic rocks with grains arranged randomly are said to be non-foliated. This means they do not have a layered or banded structure like foliated metamorphic rocks. Examples include marble and quartzite.
Quartzite, marble, and metabasalt are non-foliated metamorphic rocks..................................... i like dots