It is foliated
i believe they do yes.
Rocks with alternating bands of light and dark silicate minerals are called gneiss. Gneiss is a metamorphic rock formed under high temperature and pressure conditions, which causes the minerals within it to align in bands or layers.
Metamorphic rock with mineral grains arranaged in bands or lamellar planes are called foliated metamorphic rocks.
Metamorphic rocks that have a banded appearance due to the alignment of minerals are called foliated metamorphic rocks. This banding occurs as a result of directional pressure during metamorphism, causing the minerals to realign and form distinct layers or bands. Common examples of foliated metamorphic rocks include schist and gneiss.
non-foliated.
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.
A metamorphic rock with visible layers or bands is said to be foliated. The layers are due to the alignment of minerals or the presence of alternating light and dark bands. Examples of foliated metamorphic rocks include slate, schist, and gneiss.
It's because of foliation. Foliation is defined as the arrangement of a set of minerals in parallel, sheet-like layers that lie perpendicular to the flattened plane of a rock.
Metamorphic rocks that have a banded appearance due to the alignment of minerals are called foliated metamorphic rocks. This banding occurs when pressure causes the minerals to align perpendicular to the direction of the stress, creating distinct layers or bands. Common examples include schist and gneiss. The foliation reflects the mineral composition and the conditions under which the rock was formed.
Foliated rocks are typically metamorphic rocks that have undergone deformation and recrystallization due to high pressure and temperature, resulting in the alignment of minerals in bands or layers. Common examples of foliated rocks include schist, gneiss, and slate.
Metamorphic is a group of rocks with similar characteristics. There are minerals in the rocks so they could be considered made of minerals but they are not minerals themselves.
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.