What are the characteristics of foliated and non-foliated metamorphic rocks?
Foliation is the repetitive layering of rocks due to intense directed pressure. Foliated rocks are characterized by linear streaks that vary in width. Non-foliated metamorphic rocks do not have these streaks.
It occurs among metamorphic rocks that are subjected to intense directed pressure which causes the minerals within the rock to flatten or realign perpendicularly from the area of greatest pressure.
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Foliated metamorphic rocks have a layered or banded appearance, resulting from the alignment of mineral grains. Examples include slate, schist, and gneiss. Non-foliated metamorphic rocks lack a layered or banded structure and typically consist of one mineral type. Examples include marble and quartzite.
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When evaluating a one-sided limit, you need to be careful when a quantity is approaching zero since its sign is different depending on which way it is approaching zero from. Let us look at some examples.
When evaluating a one-sided limit, you need to be careful when a quantity is approaching zero since its sign is different depending on which way it is approaching zero from. Let us look at some examples.
When evaluating a one-sided limit, you need to be careful when a quantity is approaching zero since its sign is different depending on which way it is approaching zero from. Let us look at some examples.
When evaluating a one-sided limit, you need to be careful when a quantity is approaching zero since its sign is different depending on which way it is approaching zero from. Let us look at some examples.
- How are igneous rocks classified and differentiated from each other?
- What metamorphic rocks are formed from shale?
- How do igneous rocks turn into sediment?
- What can be said about an igneous rock with larger crystals compared to one with smaller crystals?
- How does contact metamorphism differ from regional metamorphism?

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