1. 3.4 – Metamorphic Rocks

2. Videos/Websites http://www.youtube.com/watch?v=Rv96NSPaDDk

3. Do Now
What are the 3 agents of metamorphism?

4. Do Now What are the 3 agents of metamorphism? Heat Pressure
Hydrothermal Solutions

5. Associated
Key Words

6. Vocab Words Hydrothermal Solution Metamorphism
Nonfoliated Metamorphic Rock
Foliated Metamorphic Rock
Vocab Words

7. Metamorphic Rocks
Metamorphic rocks form when existing rocks are changed by heat and pressure.
Metamorphism – to change form.
Rocks produced during metamorphism often look much different then their parent rock.

8. Formation
Most metamorphic changes occur at elevated temperatures and pressures.
These conditions exist at a few kilometers below Earth’ surface and extend into the upper mantle.
Two types of metamorphism
Contact Metamorphism
Regional Metamorphism

9. Contact Metamorphism
Hot magma moves into rock. Magma forces itself into pre-existing rock.
Low-grade metamorphism
Minor changes are done to the rocks.
Ex: Marble

10. Regional Metamorphism
Extreme pressures and temperatures.
During mountain building, large areas of rocks are subjected to these extreme pressure and temperatures.
Large scale deformation and high- grade metamorphism.

11. Agents of Metamorphism
Agents of metamorphism are heat, pressure and hydrothermal solutions.
During metamorphism, rocks are usually subjected to all three of these agents at the same time.
However, the effect of each agent varies greatly from one situation to another.

12. Heat Heat is the most important agent of metamorphism.
Heat provides the energy needed to drive chemical reactions.
Some reactions cause existing minerals to recrystallize.
Other reactions cause new minerals to form.
The heat for metamorphism comes mainly from two sources – magma and the change in temperature with depth.
Magma essentially “bakes” any rocks that are in contact with it.
Temperature with depth occurs within the upper mantle and temperature increases around 20° – 30° C.

13. Pressure (Stress)
Pressure, like temperature, also increases with depth.
Pressure is applied in all directions.
Pressure on rocks causes the spaces between mineral grains to close.
The result is a more compact rock with greater density.
Pressure can also cause minerals to recrystallize into new minerals.
Increases in temperature and pressure cause rocks to flow rather than fracture. Mineral grains rend to flatten and elongate.

14. Reactions in Solution
Water solutions containing other substances that readily change to gases at the surface play an important role in some types of metamorphism.
Hot, water-based solutions that escape form a mass of magma are called hydrothermal solutions.
Promote recrystallization by dissolving original minerals and then depositing new ones.
The rocks overall composition may occur.

15. Classification of Metamorphic Rocks
Classified by texture and composition.
Foliated Metamorphic Rocks
Nonfoliated Metamorphic Rocks

16. Foliated Metamorphic Rocks
When metamorphic rocks undergo extreme conditions, certain minerals will recrystallize with a preferred orientation.
The result is a rock with a layered or banded appearance.

17. Nonfoliated Metamorphic Rocks
Metamorphic rocks that do not have a banded or layered appearance.
Usually only contain one mineral.
Ex: Marble is a nonfoliated rock made of calcite.

18. Classification Chart

19. Group Activity
On page 84, use that table to fill in the blanks on your group paper and place it in your folder when complete.