im 100 percent sure its gneiss
Metamorphic rocks like quartzite, marble, and soapstone do not have distinct layers because they are composed of minerals that recrystallize evenly when subjected to heat and pressure, resulting in a homogenous composition. Unlike rocks with distinct layering like schist or gneiss, the minerals in these rocks are not organized into distinct bands or layers during the metamorphic process.
Yes, sedimentary rocks can contain bands or layers of minerals. These bands are often formed through various processes such as sediment deposition, compaction, and cementation. The minerals within these bands can vary in composition and can provide valuable information about the depositional environment and the history of the rock.
The daughter rock of granite is gneiss. Gneiss forms from the metamorphism of granite, where the minerals in the granite recrystallize and align into distinct bands or layers, giving gneiss its characteristic appearance.
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The light bands of rocks are typically composed of minerals like quartz and feldspar. These minerals have lighter color tones such as white, pink, or beige, which contribute to the overall light appearance of the rock.
An arrangement of minerals in flat, wavy, or parallel bands is known as a banded structure or banding. This structure is commonly seen in rocks like gneiss and schist, where different minerals align in layers or bands due to geological processes like metamorphism. The distinct bands are often a result of alternating composition or texture variations within the rock.
Yes, foliated rocks have layers or bands due to the alignment of minerals within the rock. This alignment is a result of the pressure and temperature conditions during the rock's formation, which caused the minerals to orient themselves in a specific direction, creating a layered appearance.
I do believe that the answer is "foliated". However I am not positive, but I do know that... Banding is another word for foliation, which is the grouping of certain minerals with the rock forming parallel bands that are perpendicular to the pressure that causes its formation. Banding of different minerals give some metamorphic rocks a striped appearance, involving the segregation of light and dark minerals into layers. Good luck with your question and I hope that this information has helped.
Metamorphic rocks like quartzite, marble, and soapstone do not have distinct layers because they are composed of minerals that recrystallize evenly when subjected to heat and pressure, resulting in a homogenous composition. Unlike rocks with distinct layering like schist or gneiss, the minerals in these rocks are not organized into distinct bands or layers during the metamorphic process.
no. their both separate bands no. their both separate bands
Gneiss is a type of rock that has parallel bands of dark and light mineral grains. These bands are a result of the rock being subjected to high temperatures and pressures during its formation, causing the minerals to align in distinct layers.
Gneiss undergoes regional metamorphism, which involves high temperatures and pressures over large areas of the Earth's crust. This can result in the reorganization of minerals within the rock, forming distinct layers or bands of different minerals.
by altering bands of minerals
Sedimentary rocks such as sandstone and limestone often exhibit distinct bands or layers due to the deposition of sediments over time. Metamorphic rocks like gneiss and schist can also display banding as a result of intense heat and pressure causing minerals to align in layers.
Yes, sedimentary rocks can contain bands or layers of minerals. These bands are often formed through various processes such as sediment deposition, compaction, and cementation. The minerals within these bands can vary in composition and can provide valuable information about the depositional environment and the history of the rock.
The daughter rock of granite is gneiss. Gneiss forms from the metamorphism of granite, where the minerals in the granite recrystallize and align into distinct bands or layers, giving gneiss its characteristic appearance.
I dov't know