12. Foliation or lineation happens among deformed rocks due to A. pressure and recrystallization of rocks B. eruption of magma from the mantle to the crust C. increase in temperature in the surrounding area D. increase in volume of water as the rocks' depth increases 13. Which of the following relationships is INCORRECT? A. fine grain: slate B. banding: gneiss C. non-foliated: phyllite D. contact heat: hornfels 14. How do temperature and pressure affect metamorphism? A. Pressure and temperature increase as you go up to the crust. B. The deeper the rock depth, the higher the pressure and temperature. C. Foliation happens as there is an increase in the pressure and temperature. D. Magma cannot bake the surrounding rocks due to the difference in temperature.15. Samer is walking down the river when she sees an unknown metamorphic rock. Which of the following characteristic can BEST help her to immediately identify the type of metamorphism that the rock underwent using a magnifying glass? A. foliation B. grain size C. name of the rock D. kind of mineral present in the rock
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Answer
12. A. pressure and recrystallization of rocks
13. C. non-foliated: phyllite
14. B. The deeper the rock depth, the higher the pressure and temperature.
15. A. foliation
Solution
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Bonus Knowledge
Did you know that foliation in metamorphic rocks occurs when intense pressure aligns minerals within the rock, creating a banded or layered appearance? This process is common in rocks like schist and gneiss and showcases the incredible forces at work within the Earth's crust. Every layer tells a story of geological activity, like nature's own scrapbook of pressure and time! On the other hand, understanding how metamorphic rocks form can help us grasp the beauty of their diversity. If a rock has a fine grain, it might be from a low-grade metamorphism, producing slate, while coarser rocks indicate higher-grade conditions. These characteristics not only aid in identifying the rock but also reveal the environmental conditions under which it formed—pretty cool, right?