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Igneous Rocks Chapter 3.2 ©Mark Place,

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Presentation on theme: "Igneous Rocks Chapter 3.2 ©Mark Place,"— Presentation transcript:

1 Igneous Rocks Chapter 3.2 ©Mark Place, 2007-2008

2 Formation Form when magma or lava cools and hardens.
Magma: inside Earth Lava: outside Earth

3 Where they are made? http://www.indiana.edu/~geol116/week3/maggran.mov
INTRUSIVE IGNEOUS ROCKS Inside Earth

4 EXTRUSIVE IGNEOUS ROCKS * Outside Earth

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6 Texture of the Rocks? Igneous rocks have different textures.
Texture is how a rock looks and feels. Texture is based on the size of crystal grains in the rock.

7 Crystal Size is Determined by:
cooling time

8 crystal size cooling time

9 Large Crystals Indicate
long cooling time Small Crystals Indicate short cooling time

10 SLOW cooling-large enough crystals to see with your naked eye
Intrusive Extrusive form on or near the surface QUICK cooling -small or no crystals form below the surface SLOW cooling-large enough crystals to see with your naked eye

11 Characteristics used to classify igneous rocks

12 Texture glassy } extrusive fine

13 Texture coarse } intrusive very coarse

14 Porphyrytic: When you have a mix of large and small crystal grains.
This rock experienced two cooling situations.

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