The descriptive term is foliated.
Rocks with grains arranged in parallel layers are called sedimentary rocks. These rocks form when sediment such as sand, mud, or organic material is deposited and compacted over time. Examples include sandstone and shale.
Magma that has fallen out a volcano to make sediments through metamorphism.
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.
Foliated rocks, and in particular: * Shale * Schist * Gneiss
Sedimentary rocks are the type of rocks that are mostly arranged in layers. The way in which the layers are arranged is commonly called bedding.
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.
Metamorphic rocks with a layered or banded look are referred to as foliated.
In subject of metamorphic rocks, to be foliated is to have their grains arranged in parallel layers or bands. Non foliated is when the rocks' grains are made randomly in no arranged pattern.Reference:Prentice Hall Earth Science 2009
Formed From Other Rocks Though High Pressure And High Heat . | Example - Foliated Grains Are Arranged In Parallel Layers Or Bands (Stripes) - Non Foliated Rocks , Grains Are Arranged Randomly.
Foliated metamorphic rocks have a layered or banded appearance due to the alignment of mineral grains, while unfoliated metamorphic rocks do not have a layered structure. Foliated rocks form under directed pressure, while unfoliated rocks form under non-directed pressure. Examples of foliated rocks include schist and gneiss, while examples of unfoliated rocks include marble and quartzite.
Foliated metamorphic rocks form through directed pressure and heat acting on existing rocks, causing minerals to align in a preferred orientation. This alignment creates distinct layers or bands within the rock, giving it a foliated texture. Examples of foliated metamorphic rocks include schist, gneiss, and slate.
The parallel crystal arrangement of layers in metamorphic rock is called foliation. Foliation is a common feature in rocks that have undergone intense heat and pressure, resulting in the alignment of mineral grains into distinct layers.