Schists are metamorphic rocks with parallel alignment of minerals.
A foliated metamorphic rock is a rock that has a layered or banded appearance due to the alignment of minerals in parallel planes. This alignment is typically a result of the rock being subjected to high pressure and temperature conditions during its formation. Examples include gneiss and schist.
Generically it is displaying a metamorphic fabric, specifically a schistosity. If the fabric is well developed it could also be displaying planes of cleavage.
No.
Rock can be changed into metamorphic rock by heat and pressure.
the application of pressure and heat during the rock's formation. This causes the minerals within the rock to reorganize and align themselves in parallel bands. The direction of the pressure determines the orientation of the bands in the metamorphic rock.
crystal
Foliated rock has parallel layers.
A foliated rock is a type of metamorphic rock created when mineral grains flatten and line up in parallel bands. So in other words is a rock that has parallel lines in it and you are able to see them.
A foliated metamorphic rock is a rock that has a layered or banded appearance due to the alignment of minerals in parallel planes. This alignment is typically a result of the rock being subjected to high pressure and temperature conditions during its formation. Examples include gneiss and schist.
Gneissic textured rock.
I think its metamorphic
It has a foliated texture.
Schist is a metamorphic rock that exhibits parallel alignment of mineral grains, giving it a foliated appearance. This alignment is typically a result of regional metamorphism where intense pressure and temperature conditions cause the minerals to recrystallize in a preferred orientation.
Foliated.
The metamorphic rock you are referring to is called foliated rock. Foliated rocks have mineral crystals aligned in parallel layers or bands, resulting from the re-alignment of minerals due to pressure and heat during metamorphism. Examples of foliated rocks include slate, schist, and gneiss.
The parallel alignment of platy grains in a rock is called foliation. Foliation is commonly seen in metamorphic rocks where minerals align in a preferred orientation due to pressure and temperature changes during deformation.
sandstone is a sedimentary rock because of the layers or lines you can see on it