Marble is a completely non-foliated rock. lol
Marble will not show noticeable foliation, although it undergoes some pressure during metamorphism. That is because marble composition is almost 100% calcite. Even calcite crystals realign themselves perpendicular to stress direction, the realignment is still unnoticeable. However, if there are platy minerals, such as mica, which is really uncommon, marble should show foliated texture.
Two examples of non-foliated rocks are marble, which forms from the metamorphism of limestone, and quartzite, which forms from the metamorphism of sandstone. These rocks do not have a layered or banded appearance like foliated rocks such as schist or gneiss.
Metamorphic rock can be either foliated or non-foliated. Foliated metamorphic rocks have layered or banded textures, while non-foliated metamorphic rocks lack these layers and have a more uniform appearance. Examples of foliated metamorphic rocks include schist and gneiss, while examples of non-foliated metamorphic rocks include marble and quartzite.
Foliated rocks have visible layers or bands due to the alignment of mineral grains, like in slate or schist. Non-foliated rocks lack this layered structure and have a more uniform texture, like in marble or quartzite.
The main subcategories of metamorphic rock are foliated (such as schist and gneiss) and non-foliated (such as marble and quartzite). Foliated rocks have layers or bands due to the alignment of mineral grains, while non-foliated rocks do not have a layered structure.
Marble is non-foliated.
marble has an non-foliated texture.
Marble is a non-foliated metamorphic rock.
Marble.
Quartzite, marble, and metabasalt are non-foliated metamorphic rocks..................................... i like dots
Marble will not show noticeable foliation, although it undergoes some pressure during metamorphism. That is because marble composition is almost 100% calcite. Even calcite crystals realign themselves perpendicular to stress direction, the realignment is still unnoticeable. However, if there are platy minerals, such as mica, which is really uncommon, marble should show foliated texture.
non-foliated.
The largest two classifications are foliated (e.g. gneiss) and non-foliated (e.g. marble).
Two examples of non-foliated rocks are marble, which forms from the metamorphism of limestone, and quartzite, which forms from the metamorphism of sandstone. These rocks do not have a layered or banded appearance like foliated rocks such as schist or gneiss.
Non-foliated metamorphic rock, like quartzite and marble.
Certain metamorphic rocks that do not exhibit foliation (banding, lamellar texture) like quartzite and marble are described as non-foliated.
The two most common non-foliated metamorphic rocks are marble, formed from the metamorphism of limestone, and quartzite, formed from the metamorphism of quartz sandstone.