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A schistose foliation would be found in a metamorphic rock with a large amount of micaceous minerals, creating a flaky texturing with easily cleavable layers. Gneiss is more coarse in texture, not as easily cleavable along planes, and contains less micaceous minerals.

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What is the difference between stratification and foliated rocks?

Stratification results in sedimentary rock due to the deposition of organic and inorganic particles. Foliation is a texture in metamorphic rocks which is a result of heat and pressure, and results in constituent minerals appearing banded or lamellar, due to realignment.


What is the difference between slate and phyllite?

Slate is a fine-grained metamorphic rock formed from the low-grade metamorphism of shale or mudstone, while phyllite is a more intermediate-grade metamorphic rock formed from the metamorphism of slate. Phyllite has a more pronounced foliation and sheen due to increased metamorphic pressure and temperature compared to slate.


Explain the differences between layering in sedimentary rocks and foliation in metamorphic rocks.?

Layering in sedimentary rock is due to seasonal or event based deposition of small rock particles which reflect the environment at the time of deposition. Layering in metamorphic rocks (foliation) is due to the realignment and alteration of minerals from heat and pressure.


What is the biggest time difference in the world between two locations?

The biggest time difference in the world between two locations is 26 hours. This difference occurs between Baker Island and the Line Islands in the Pacific Ocean.


What is the major difference between igneous and metamorphic rocks?

igneous rocks started as melted lava and cooled to be rocks. Metamorphic rock started as a sedimentary rock, and was heated up and put under pressure to create the metamorphic rock. Classic example - igneous = obsidian. Metamorphic = marble (marble is limestone that's been heated and squeezed a lot).

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Do foliated metamorphic rocks break along their outer edges?

Yes, foliated metamorphic rocks tend to break along their layers or foliation planes due to the alignment of minerals during metamorphism. This can result in the rock breaking into thin sheets along its outer edges.