i believe they do yes.
It is foliated
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.
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.
A metamorphic rock that has grains arranged in bands is said to be foliated. Foliated metamorphic rocks show distinct layering or banding due to the alignment of minerals under heat and pressure during formation. Examples of foliated rocks include schist and gneiss.
The presence of aligned minerals in the rock determines if it is foliated or non-foliated. Foliated metamorphic rocks have minerals that are arranged in layers or bands, while non-foliated rocks do not show any preferred orientation of minerals. The amount of pressure and temperature the rock experiences during metamorphism also influences whether it will develop a foliated or non-foliated texture.
Metamorphic rocks with a banded or striped appearance are called foliated rocks. These bands or stripes are formed due to the alignment of mineral grains or the presence of alternating layers of different minerals. Examples of foliated metamorphic rocks include gneiss, schist, 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.
Metamorphic rocks with a layered or banded look are referred to as foliated.
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.
Metamorphic rock with mineral grains arranaged in bands or lamellar planes are called foliated metamorphic rocks.
foliated