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:
1. ______________ 2. ______________ 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: A. _____________ occurs when  molten (liquid) rock flows out of the earth as ________________ Extrusions lava
lava magma
And cools __________ quickly
to form fine or no ____________ crystals
gas pockets Vesicular basalt
This rock if full of gas pockets frothy texture (vesicular)
B. To form magma,  ____________ must be melted. minerals
C. Minerals melt at different  ____________ and ___________ temperatures pressures
D. Igneous rocks  of different  ____________  composition
Can form from  the same body of ____________  magma
4.  INTRUSIVE IGNEOUS ROCKS : A. _____________ occurs when molten  rock beneath the surface Intrusions (magma)
cools  ____________ to form _____________ slowly coarse crystals
Granite: Coarse crystals Basalt: Fine crystals (Microscopic views)
 
5.  FELSIC A. Igneous rocks of the continental crust are rich in _________ density _________ colored minerals low light (granitic)
6. MAFIC A. Igneous rocks of the ocean floor are rich in _________ density _________ colored minerals high dark (basaltic)
 
Comparing Oceanic Crust To Continental Crust
Continental Crust: 1. 2. 3. 4. 5. low density light color felsic granitic thick
Oceanic Crust : 1. 2. 3. 4. 5. high density dark color mafic basaltic thin
Complete the Activity Use this diagram in your ESRT to answer the following:   What is the temperature for the interface between the following… inner core and outer core? 6250° C Outer core and stiffer mantle? 5000° C   Stiffer Mantle and athenosphere? 2600° C   Asthenosphere and lithosphere? 750° C
What is the depth of the interface between the stiffer mantle and the outer core? 2900 KM   State the relationship between depth and pressure :As depth increase pressure increases State the relationship between depth and temperature: As depth increases temperature increases
 
When rocks melt, bonds broken. Crystalline solid no longer exists. MELTING ROCKS AND CRYSTALLIZING MAGMA Rock  magma  magma  rock
Hot liquid contains still solid fragments Minerals melt at different temperatures Melting causes changes in magma composition MELTING ROCKS AND CRYSTALLIZING MAGMA Rock  magma  magma  rock
Cooling of hot liquid allows  crystallization of minerals Bonds are re-established Crystalline structure grows until edges touch adjacent crystals Minerals crystallize at different temperatures MELTING ROCKS AND CRYSTALLIZING MAGMA Rock  magma  magma  rock
OK……….. TAKE OUT YOUR  REFERENCE TABLE
 

Np complete