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Texture and metamorphic grade. Schist has visible crystals, while phyllite has crystals too small to be seen with the eye or barely seen. This is a result of schist having higher grade metamorphism.

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Schist is a metamorphic rock that tends to have larger mineral grains and a more layered structure compared to phyllite. Phyllite is also a metamorphic rock, but it has smaller mineral grains and a more silky sheen due to the alignment of mica minerals.

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9mo ago
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Phyllite has a shiny luster look and schist does not.

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15y ago
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Q: What is the difference between schist and phyllite?
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What lists the rocks in order of increasing grain size and increasing grade of metamorphism?

The list that orders rocks in increasing grain size and increasing grade of metamorphism is: shale (fine-grained) - slate (fine-grained) - phyllite (medium-grained) - schist (medium to coarse-grained) - gneiss (coarse-grained).


What mineral is common in schist and gneiss but not common is slate and phyllite?

The mineral common in schist and gneiss but not common in slate and phyllite is garnet. Garnet typically forms in higher-grade metamorphic rocks such as schist and gneiss due to the increased temperature and pressure conditions necessary for its formation.


What foliated metamorphic rock is texturally intermediate between slate and schist?

Phyllite is a foliated metamorphic rock that is texturally intermediate between slate and schist. It exhibits a greater degree of metamorphism than slate but not as much as schist, resulting in a medium-grain texture with a glossy sheen.


Can you describe the 4 rocks formed by metamorphic grade which are Slate Phyllite Schist and Gneiss?

Slate is a low-grade metamorphic rock characterized by fine-grained foliated structure. Phyllite is intermediate-grade metamorphic rock with a greater degree of crystallization and foliation than slate. Schist is a medium-grade metamorphic rock with visible mineral grains and strong foliation. Gneiss is a high-grade metamorphic rock with distinct banding of light and dark minerals and high crystallization.


What is the metamorphic progression of shale?

Shale can transform into slate, then phyllite, followed by schist, and ultimately into gneiss through a series of increasing metamorphic changes. This progression involves the recrystallization of minerals under heat and pressure, resulting in the formation of different textures and new mineral compositions at each stage.