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IGNEOUS ROCKS
Where Does  Igneous Rock Form?
I. FORMATION OF IGNEOUS ROCKS
A. Igneous rocks form directly from the _____________ and _____________ solidification crystallization
of _____molten rock to form _______ rock solid liquid
FOUNTAINING
FISSURE ERUPTION
 
LAVA FLOW
 
LAVA FLOW OVER A ROAD
LAVA FLOW THROUGH FORREST
Kilauea, HI 2003
Kilauea, HI , 2003
 
Mt. ST. Helens
Volcanic crater
crazy vulcanist
SKY LIGHT
 
 
 
 
 
 
B. _____________ is the process when a liquid rock cools,   crystallization
and it    changes   to a solid   made of ________ ___________ INTERGROWN CRYSTALS
 
GRANITE MICROSCOPIC VIEW
2.  CLASSIFICATION  OF IGNEOUS ROCKS:
A.  2 characteristics that are used to classify igneous rocks:
[object Object],[object Object],texture mineral composition
 
B. Texture of an  igneous rock describes the
_________, __________ and  ____________ of the mineral crystals it was made from. size shape arrangement
C. The ______ of the crystals depends on the  _______________________ size Rate of  cooling
Slow cooling =   ____________ large crystals
 
MINERAL CRYSTALS
GABBRO
Fast cooling =   ____________ fine crystals Or  no crystals  (glassy)
GLASSY TEXTURE: OBSIDIAN
BASALT: FINE CRYSTALS
BASALT MICROSCOPIC VIEW
Granite: Coarse crystals Basalt: Fine crystals (Microscopic views)
FINE  CRYSTAL:  RYOLITE
3 .  EXTRUSIVE  IGNEOUS ROCKS: ,[object Object],[object Object],Extrusions lava
lava magma
And cools __________ quickly
[object Object],[object Object],[object Object],crystals
gas pockets Vesicular basalt
This rock if full of gas pockets frothy texture (vesicular)
[object Object],[object Object],[object Object],[object Object],minerals
[object Object],[object Object],[object Object],temperatures pressures
[object Object],[object Object],composition
[object Object],magma
4.  INTRUSIVE IGNEOUS ROCKS : ,[object Object],[object Object],Intrusions (magma)
[object Object],[object Object],[object Object],[object Object],slowly coarse crystals
Granite: Coarse crystals Basalt: Fine crystals (Microscopic views)
 
5.  FELSIC ,[object Object],[object Object],[object Object],[object Object],low light (granitic)
6. MAFIC ,[object Object],[object Object],[object Object],[object Object],high dark (basaltic)
 
Comparing Oceanic Crust To Continental Crust
[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],low density light color felsic granitic thick
[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],high density dark color mafic basaltic thin
Complete the Activity ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
[object Object],[object Object],[object Object],[object Object],[object Object]
 
When rocks melt, bonds broken. Crystalline solid no longer exists. MELTING ROCKS AND CRYSTALLIZING MAGMA Rock  magma  magma  rock
[object Object],[object Object],[object Object],MELTING ROCKS AND CRYSTALLIZING MAGMA Rock  magma  magma  rock
[object Object],[object Object],[object Object],[object Object],MELTING ROCKS AND CRYSTALLIZING MAGMA Rock  magma  magma  rock
OK……….. TAKE OUT YOUR  REFERENCE TABLE
 

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