No
its foliated
its 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 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.
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.
When a metamorphic rock exhibits a layered or banded appearance, it is said to exhibit foliated texture. This texture is a result of the alignment of mineral grains or the presence of alternating light and dark layers. Examples of foliated metamorphic rocks include gneiss and schist.
Metamorphic rock can be banded and foliated. Banded metamorphic rock has visible layers or bands of different mineral compositions, while foliated metamorphic rock has a layered or sheet-like appearance due to the alignment of minerals. These patterns are a result of the intense heat and pressure the rock undergoes during metamorphism.
MARBLE
A foliated metamorphic rock is a rock that has a layered or banded appearance due to the alignment of minerals in parallel planes. This alignment is typically a result of the rock being subjected to high pressure and temperature conditions during its formation. Examples include gneiss and schist.
Phyllite is foliated.
Foliated or non-foliated. Foliated metamorphic rocks have a layered or banded appearance due to the alignment of minerals, while non-foliated rocks do not exhibit this feature.
Metamorphic rocks have a layered or banded appearance due to the intense heat and pressure they undergo. This sets them apart from igneous rocks, which form from molten material, and sedimentary rocks, which are made from compressed sediments.