A folliated texture metamorphic rock, like shist.
Foliated metamorphic rock.
A schistose texture.
Foliated
coal
Foliation.
The texture of a rock with aligning parallel platy grains is said to exhibit metamorphic foliation.
foliation
A metamorphic rock
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.
Metamorphic rocks have their grains arranged in parallel layers or bands that are said to be foliated.
A foiliated metamorphic rock is a metamorphic rock that has a texture of parallel alignment of mineral grains. Your Welcome...
No, foliated metamorphic rocks have mineral grains that are aligned in parallel layers or bands due to the pressure and temperature conditions during their formation. This alignment gives foliated rocks their characteristic layered appearance.
The texture of a rock with aligning parallel platy grains is said to exhibit metamorphic foliation.
Foliated.
Metamorphic rocks such as marble and quartzite are said to be non-foliated because their mineral grains are not arranged in parallel layers or bands like in foliated rocks such as slate or schist. This lack of alignment gives non-foliated rocks a more uniform texture and appearance.
Mica.
It is likely a type of metamorphic rock, such as schist or gneiss, which form under high temperature and pressure conditions leading to the alignment of mineral grains into flat layers.
Metamorphic rock with mineral grains arranaged in bands or lamellar planes are called foliated metamorphic rocks.
Metamorphic rocks can have various types of minerals, such as quartz, feldspar, mica, and amphibole, which form grains within the rock. These grains can be elongated or flattened, depending on the degree of metamorphism the rock has undergone. The size, shape, and alignment of these grains provide valuable information about the rock's history and the conditions under which it formed.
foliation
foliation
any of a class of crystalline metamorphic rocks whose constituent mineral grains have a more or less parallel or foliated arrangement.