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.
A metamorphic rock in which the grains line up in parallel bands is known as a foliated metamorphic rock. This alignment occurs due to the intense pressure and heat that cause the minerals to recrystallize and arrange themselves along planes. Examples of foliated metamorphic rocks include schist and gneiss. The parallel bands give these rocks their distinct layered appearance.
The type of metamorphic rock that has flat layers is called "foliated metamorphic rock." Foliation occurs when pressure causes the minerals in the rock to align in parallel layers or bands. Examples of foliated metamorphic rocks include schist, slate, and gneiss. These layered structures result from the rearrangement of minerals under heat and pressure.
Generically it is displaying a metamorphic fabric, specifically a schistosity. If the fabric is well developed it could also be displaying planes of cleavage.
A planar parallel alignment of different mineral bands in a metamorphic rock is known as foliation. This texture occurs when pressure and temperature conditions cause the minerals to realign and grow in parallel layers, typically due to directional stress. Foliated metamorphic rocks, such as schist and slate, exhibit this characteristic banding, which can enhance their aesthetic and structural properties. The alignment often reflects the history of tectonic forces acting on the rock during its formation.
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.
A metamorphic rock in which the grains line up in parallel bands is known as a foliated metamorphic rock. This alignment occurs due to the intense pressure and heat that cause the minerals to recrystallize and arrange themselves along planes. Examples of foliated metamorphic rocks include schist and gneiss. The parallel bands give these rocks their distinct layered appearance.
It has a foliated texture.
I think its metamorphic
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.