1. Minerals and Rocks

2. What is the difference?
Minerals: nonliving structures with set chemical formulas
Example: SiO2 is quartz
Rocks: made of combinations of minerals
Pair share:
A: Tell B an analogy… a mineral is to a rock as a _______ is to a ______.

3. How rocks are classified
Rocks are organized into groups in two ways:
By the minerals they are composed of
2) How they are formed

4. Igneous rocks Formed when molten rock cools (volcanic)
Extrusive cools at the surface
Example: obsidian
Intrusive cools underground forming crystals
example: granite
Pair share: B tell A a what “ Ex” in “In” mean and how that relates to where these 2 types of rock cool.

5. Sedimentary rocks Form from fragments of older rocks
Whiteboard: Why do you think that fossils are only found in this type of rock?
Form from fragments of older rocks
Layers can be compressed
Minerals in water can seep through and “cement” them together

6. Metamorphic rocks Heated and put under pressure deep in the crust
Undergo chemical changes
Examples:
limestone becomes marble shale becomes slate
Pair share: A: tell B what other things go through metamorphosis and why you think this kind of rock has that name.

7. Rock cycle: takes millions of years
Over time rocks are:
heated and melted
Cooled
Compressed
Undergo chemical changes
Exposed to wind & H20
Pair share: B tell A what igneous rock must go through to become sediment and what metamorphic rock must go through to become magma.

8. Superposition oldest rocks are in the lowest layers (relative dating)

9. Absolute dating
Radioactive dating is a measure of the decay of isotopes Isotopes decay at a known rate - can calculate age using R=Δ/T
White board: What is an isotope?

10. White Board Review 1) What is the difference between minerals & rocks?
2) What are the two ways rocks are classified?
3) How is the absolute age of a rock determined?

11. Summary Main idea Key concepts Important facts
How the facts relate to the main idea