1. Metamorphic Rocks
Heat + Temperature

2. Recognizing Metamorphic Rocks
Meta = Greek for change
Morphe = Greek for form
Under enough heat, any rock will become igneous;
But if there is enough pressure to keep it solid, it may just change without reaching its melting point!

3. Metamorphic Minerals Talc, Mica and Garnet
Remember Fractional Crystallization? Bowen?
All minerals are stable at certain temperatures and crystallize at different temperatures.
If rocks containing minerals change due to heat + pressure, scientists can tell what conditions created the new minerals.

4. Metamorphic Textures Two main groups:
Foliated
Nonfoliated
Geologists use metamorphic textures and mineral composition to identify metamorphic rocks.

5. Foliated Rocks
Layers and bands of minerals are characteristics of foliated metamorphic rocks.
High pressure  flat, needle- like crystals with long axes perpendicular to the pressure.
Parallel alignment of minerals.

6. Nonfoliated Rocks
Composed mainly of minerals that form with blocky crystal shapes.
Quartzite (sandstone) and marble (limestone) are common examples
Porophyroblasts: new metamorphic crystals that grow large while surrounding minerals remain small.

7. Grades of Metamorphism
Combos of temperature + pressure result in different ‘grades’ of metamorphism.
Low-grade: Low temp and pressure with specific minerals/textures
High-grade: High temp and pressure with specific minerals/textures
Intermediate: between

8. Regional Metamorphism
Temperature and pressure affect large areas of the Earth’s crust.
Ranges in grade from low to high grade.
Results: changes in rock type, foliation and folding/deforming of rock layers in an area.

9. Contact Metamorphism
When molten material— igneous intrusion—comes in contact with a solid rock.
High temp, low to moderate pressure
Much more abundant with intrusive igneous rocks than with extrusive; affects surrounding rocks.

10. Hydrothermal Metamorphism
Super hot water reacts with rock and alters its chemical and mineral composition.
Fluids coming in and out of rock alter mineral composition and texture.
Chemical changes common.
Valuable ores (gold, copper, zinc, lead) can be formed.

11. Economic Importance
Modern life is only as convenient as it is because of naturally occurring Earth materials.
Metamorphic processes create gold, silver, copper and lead as well as many non-metallic resources.

12. Metallic Mineral Resources
Occur mostly in the form of metal ores.
Precipitated through hydrothermal solutions:
Concentrated in veins
Spread throughout rock mass
Most deposits are metal sulfides such as galena or pyrite.

13. Nonmetallic Mineral Resources
Metamorphism of ultrabasic igneous rocks produces the minerals talc and asbestos.
Talc: very soft; used as dusting powder and texture in paints.
Asbestos: not combustible; used in fireproofing / insulating materials.
Graphite: formed by metamorphism of coal!

14. The Rock Cycle Metamorphic rocks form when other rocks change.
Igneous crystallize magma under Earth or on surface.
Sedimentary form from lithified minerals and sediments
Metamorphic change both with temperature and pressure.

15. The Rock Cycle Will rocks stay the same?
Probably not.
Any rock can be changed into any other type of rock.
Continuous changing and remaking of rocks is called the rock cycle.
No one single way; many different ways to convert rocks.