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A foliated metamorphic rock when crystals?
A foliated metamorphic rock forms when crystals combine and form visible bands
A foliated metamorphic rock forms when crystals .?
A foliated metamorphic rock forms when crystals combine and form visible bands
A metamorphic rock with visible layers or bands is said to be what?
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.
What is the texture of gneiss?
Gneiss has a foliated texture, meaning it has visible layers or bands of different minerals. These layers are typically arranged in a repetitive pattern, giving gneiss a distinct texture that can vary in appearance depending on the type of minerals present.
Is gneiss foliated or no foliated?
Gneiss is a foliated metamorphic rock, meaning it has visible layers or bands of different minerals. These layers are formed due to the intense pressure and temperature conditions that gneiss undergoes during the metamorphic process.
A foliated metamorphic rock when crystals?
A foliated metamorphic rock forms when crystals combine and form visible bands
A foliated metamorphic rock forms when crystals .?
A foliated metamorphic rock forms when crystals combine and form visible bands
A metamorphic rock that has visible layers or bands?
Schist is a metamorphic rock that has visible layers or bands due to the alignment of platy minerals like mica and chlorite during the metamorphic process. These layers or bands give schist its distinctive foliated texture and can vary in color and composition depending on the minerals present.
A metamorphic rock with visible layers or bands is said to be what?
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.
What is the texture of gneiss?
Gneiss has a foliated texture, meaning it has visible layers or bands of different minerals. These layers are typically arranged in a repetitive pattern, giving gneiss a distinct texture that can vary in appearance depending on the type of minerals present.
Is gneiss foliated or no foliated?
Gneiss is a foliated metamorphic rock, meaning it has visible layers or bands of different minerals. These layers are formed due to the intense pressure and temperature conditions that gneiss undergoes during the metamorphic process.
What type of rock forms when crystals combine and form with visible bands?
The type of rock that forms when crystals combine and create visible bands is called metamorphic rock, specifically a foliated metamorphic rock. An example of this is gneiss, which features alternating layers of different mineral compositions. The banding occurs due to the alignment of mineral grains under pressure and temperature conditions.
Is phyllite foliated or unfoliated?
Phyllite is foliated.
What is a kind of non foliated metamorphic rock?
Metamorphic rocks are rocks that have their grains arranged in parallel layers or bands. Foliated rocks are formed under great pressure and heat, and when they cool they have a banded grain pattern.
WHAT IS A FOLIATED METAMORPHIC ROCK WITH MEDIUM TO COARSE GRAINED CRYSTALS AND WHOSE PARENT ROCK?
A foliated metamorphic rock with medium to coarse-grained crystals is typically schist. Schist is characterized by its well-developed foliation and often contains visible mineral grains, such as mica, garnet, or quartz. Its parent rock is usually shale or mudstone, which undergoes metamorphism under heat and pressure, leading to the alignment of minerals and the development of foliation.
Is marble foliated or non foliated?
Marble is a non-foliated metamorphic rock, meaning it does not have visible layers or banding. It is formed from the recrystallization of limestone under high heat and pressure.
What does foaliated and non foaliated mean?
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.
