This may be due to the overburden load, which is essentially the weight of all the material above the layer of minerals in question squashing them flat. Or it may be due to deformation caused by the movements of tectonic plates which often causes a form of deformation known as shearing where two things slide past each other. When this occurs in ductile rock masses, it acts to flatten and rotate mineral grains so that their long axis is parallel to the shear plane.
When mineral grains are flattened into layers, the rock is said to have a foliated texture. Foliation usually occurs in metamorphic rocks.
Compressional Force.
pressure
Maybe Sedimentary Rocks?
mineral grains arranging into layers.
Foliated is the general descriptive term used to describe the layering or banding of metamorphic rock.
Not exactly. Some metamorphic rocks have foliation, which can appear similar to the layers of sedimentary rock. Foliation develops from mineral grains being oriented by pressure, rather than the deposition of layers.
Mineral grains are crystals or pieces of crystals that vary widely in chemicalcomposition
Metamorphic rock may have coarse, flattened, or aligned mineral grains.
rutherfordium
Yes, and they often are, and appear as foliations.
A banded mineral is a mineral that has grains that are arranged in a particular pattern of flat layers or forms swirls.
no texture
Maybe Sedimentary Rocks?
no texture
Foliated.
A schistose texture.
schist
mineral grains arranging into layers.
Nonfoliated