Foliated rocks, and in particular:
* Shale * Schist * Gneiss
It has a foliated texture.
Foliated.
Generically it is displaying a metamorphic fabric, specifically a schistosity. If the fabric is well developed it could also be displaying planes of cleavage.
Foliated rock has parallel layers.
Metamorphic rocks with a layered or banded look are referred to as foliated.
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.
Gneiss is a type of rock that has parallel bands of dark and light mineral grains. These bands are a result of the rock being subjected to high temperatures and pressures during its formation, causing the minerals to align in distinct layers.
stratification
They form sedimentary rocks due to compaction, with grains aligning parallel to each other. Over time, the weight of the overlying layers can cause cementation, binding the grains together to create solid rock.
no texture
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.
A sill is formed when magma is forced into layers parallel to the surrounding rock layers. Sills are characterized by their tabular shape and are often found intruding between rock layers.