A metamorphic rock that can form from granite with wavy bands of dark and light layers is called gneiss. Gneiss is characterized by its foliated texture, which results from the high-grade metamorphism of granite, causing the minerals to realign and separate into distinct layers. The wavy bands typically consist of alternating light-colored quartz and feldspar, along with darker bands of biotite or amphibole. This layering gives gneiss its striking appearance and indicates significant geological processes.
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 could be a sedimentary rock or a foliated metamorphic rock exhibiting alternating bands of light and dark minerals.
Yes, granite can exhibit wavy bands of dark and light layers, which are typically the result of variations in mineral composition and the cooling history of the magma from which it formed. These bands, known as foliation, can occur due to the alignment of minerals like mica or variations in the concentration of different minerals such as quartz and feldspar. This unique appearance often results from geological processes such as metamorphism or the intrusion of different magma types. Overall, these wavy patterns contribute to the aesthetic appeal of granite in various applications.
Foliated is the correct answer!!!
Yes, that description fits gneiss rock. Gneiss forms from the metamorphism of granite or other rocks, resulting in distinct wavy bands of dark and light mineral layers. This banding is a key characteristic of gneiss and helps distinguish it from granite.
A metamorphic rock that can form from granite with wavy bands of dark and light layers is called gneiss. Gneiss is characterized by its foliated texture, which results from the high-grade metamorphism of granite, causing the minerals to realign and separate into distinct layers. The wavy bands typically consist of alternating light-colored quartz and feldspar, along with darker bands of biotite or amphibole. This layering gives gneiss its striking appearance and indicates significant geological processes.
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 could be a sedimentary rock or a foliated metamorphic rock exhibiting alternating bands of light and dark minerals.
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.
It is likely a sedimentary rock, where the light layers are composed of a different material or grain size compared to the dark layers. This banding could be due to variations in sediment deposition over time.
Yes, granite can exhibit wavy bands of dark and light layers, which are typically the result of variations in mineral composition and the cooling history of the magma from which it formed. These bands, known as foliation, can occur due to the alignment of minerals like mica or variations in the concentration of different minerals such as quartz and feldspar. This unique appearance often results from geological processes such as metamorphism or the intrusion of different magma types. Overall, these wavy patterns contribute to the aesthetic appeal of granite in various applications.
Gneiss is a metamorphic rock which exhibits foliation (a layered effect). The layers of gneiss are alternating light and dark layers. Usually the lighter layers are rich in quartz and feldspar and the darker layers are rich in biotite mica, hornblende, or tourmaline.
Foliated is the correct answer!!!
A gneiss rock is composed of alternating bands of light and dark silicate minerals, typically formed through high temperature and pressure metamorphism of existing rocks like granite or shale. The light bands are usually composed of quartz and feldspar, while the dark bands are made up of minerals like biotite, amphibole, or pyroxene.
The metamorphic rock texture that has alternating bands of light and dark minerals is called foliation. This texture results from the alignment of minerals due to directional pressure during metamorphism. Schist is a common type of foliated metamorphic rock.
foliated metamorphic rocks. The alternating layers are caused by the alignment and segregation of minerals during the metamorphic process, resulting in a banded or layered appearance. Examples of foliated metamorphic rocks include gneiss, schist, and slate.