ROCKS Are classified according to the environment in

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ROCKS

ROCKS

Are classified according to the environment in which they _____ form

Are classified according to the environment in which they _____ form

Types of Rocks: igneous ________ sedimentary ____ metamorphic

Types of Rocks: igneous ________ sedimentary ____ metamorphic

IGNEOUS ROCKS

IGNEOUS ROCKS

Where Does Igneous Rock Form?

Where Does Igneous Rock Form?

I. FORMATION OF IGNEOUS ROCKS

I. FORMATION OF IGNEOUS ROCKS

A. Igneous rocks form directly from the solidification _______ and crystallization _______

A. Igneous rocks form directly from the solidification _______ and crystallization _______

of _____molten liquid rock to form _______ solid rock

of _____molten liquid rock to form _______ solid rock

FOUNTAINING

FOUNTAINING

FISSURE ERUPTION

FISSURE ERUPTION

LAVA FLOW

LAVA FLOW

LAVA FLOW OVER A ROAD

LAVA FLOW OVER A ROAD

LAVA FLOW THROUGH FORREST

LAVA FLOW THROUGH FORREST

Kilauea, HI 2003

Kilauea, HI 2003

Kilauea, HI , 2003

Kilauea, HI , 2003

Mt. ST. Helens

Mt. ST. Helens

Volcanic crater

Volcanic crater

crazy vulcanist

crazy vulcanist

SKY LIGHT

SKY LIGHT

crystallization B. _______ is the process when a liquid rock cools,

crystallization B. _______ is the process when a liquid rock cools,

and it changes to a solid made of INTERGROWN CRYSTALS __________

and it changes to a solid made of INTERGROWN CRYSTALS __________

GRANITE MICROSCOPIC VIEW

GRANITE MICROSCOPIC VIEW

2. CLASSIFICATION OF IGNEOUS ROCKS:

2. CLASSIFICATION OF IGNEOUS ROCKS:

A. 2 characteristics that are used to classify igneous rocks:

A. 2 characteristics that are used to classify igneous rocks:

texture 1. _______ mineral composition 2. _______

texture 1. _______ mineral composition 2. _______

B. Texture of an igneous rock describes the

B. Texture of an igneous rock describes the

_____, size _____ shape and arrangement ______ of the mineral crystals it was made

_____, size _____ shape and arrangement ______ of the mineral crystals it was made from.

size C. The ______ of the crystals depends on the Rate of _______ cooling

size C. The ______ of the crystals depends on the Rate of _______ cooling _____

Slow cooling = large crystals ______

Slow cooling = large crystals ______

MINERAL CRYSTALS

MINERAL CRYSTALS

GABBRO

GABBRO

Fast cooling = fine crystals ______ Or no crystals (glassy)

Fast cooling = fine crystals ______ Or no crystals (glassy)

GLASSY TEXTURE: OBSIDIAN

GLASSY TEXTURE: OBSIDIAN

BASALT: FINE CRYSTALS

BASALT: FINE CRYSTALS

BASALT MICROSCOPIC VIEW

BASALT MICROSCOPIC VIEW

Granite: Coarse crystals Basalt: Fine crystals (Microscopic views)

Granite: Coarse crystals Basalt: Fine crystals (Microscopic views)

FINE CRYSTAL: RYOLITE

FINE CRYSTAL: RYOLITE

3. EXTRUSIVE IGNEOUS ROCKS: Extrusions A. _______ occurs when molten (liquid) rock flows out

3. EXTRUSIVE IGNEOUS ROCKS: Extrusions A. _______ occurs when molten (liquid) rock flows out of the earth as ________ lava

lava magma

lava magma

And cools quickly _____

And cools quickly _____

to form fine or no crystals ______

to form fine or no crystals ______

Vesicular basalt gas pockets

Vesicular basalt gas pockets

frothy texture (vesicular) This rock if full of gas pockets

frothy texture (vesicular) This rock if full of gas pockets

B. To form magma, minerals ______ must be melted.

B. To form magma, minerals ______ must be melted.

C. Minerals melt at different temperatures ______ pressures and ______

C. Minerals melt at different temperatures ______ pressures and ______

D. Igneous rocks of different composition ______

D. Igneous rocks of different composition ______

Can form from the same body of magma ______

Can form from the same body of magma ______

4. INTRUSIVE IGNEOUS ROCKS: A. Intrusions _______ occurs when molten rock beneath the surface

4. INTRUSIVE IGNEOUS ROCKS: A. Intrusions _______ occurs when molten rock beneath the surface (magma)

cools slowly ______ to form coarse crystals _______

cools slowly ______ to form coarse crystals _______

Granite: Coarse crystals Basalt: Fine crystals (Microscopic views)

Granite: Coarse crystals Basalt: Fine crystals (Microscopic views)

5. FELSIC A. Igneous rocks of the continental crust are rich in _____ density

5. FELSIC A. Igneous rocks of the continental crust are rich in _____ density _____ colored minerals (granitic) low light

6. MAFIC A. Igneous rocks of the ocean floor are rich in _____ density

6. MAFIC A. Igneous rocks of the ocean floor are rich in _____ density _____ colored minerals (basaltic) high dark

Comparing Oceanic Crust To Continental Crust

Comparing Oceanic Crust To Continental Crust

Continental Crust: 1. low density 2. light color 3. granitic 4. felsic 5. thick

Continental Crust: 1. low density 2. light color 3. granitic 4. felsic 5. thick

Oceanic Crust: 1. high density 2. dark color 3. basaltic 4. mafic 5. thin

Oceanic Crust: 1. high density 2. dark color 3. basaltic 4. mafic 5. thin

Complete the Activity Use this diagram in your ESRT to answer the following: What

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

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

MELTING ROCKS AND CRYSTALLIZING MAGMA Rock magma rock When rocks melt, bonds broken. Crystalline

MELTING ROCKS AND CRYSTALLIZING MAGMA Rock magma rock When rocks melt, bonds broken. Crystalline solid no longer exists.

MELTING ROCKS AND CRYSTALLIZING MAGMA Rock magma rock • Hot liquid contains still solid

MELTING ROCKS AND CRYSTALLIZING MAGMA Rock 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 rock • Cooling of hot liquid allows

MELTING ROCKS AND CRYSTALLIZING MAGMA Rock 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

OK………. . TAKE OUT YOUR REFERENCE TABLE

OK………. . TAKE OUT YOUR REFERENCE TABLE