Igneous Rocks What are they and how do

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Igneous Rocks What are they and how do they form? Mt. Rushmore

Igneous Rocks What are they and how do they form? Mt. Rushmore

Half Dome, Yosemite, CA Ansel Adams

Half Dome, Yosemite, CA Ansel Adams

IGNEOUS ROCKS Some igneous rocks form from cooled lava that has exited Earth’s crust

IGNEOUS ROCKS Some igneous rocks form from cooled lava that has exited Earth’s crust Hawaii

Some Igneous rocks cool from magma inside Earth and later become exposed through pressure,

Some Igneous rocks cool from magma inside Earth and later become exposed through pressure, uplift, and erosion!!! Half Dome, Yosemite, California

Igneous § Think of “ignite” ignite § To light a fire § Igneous rock

Igneous § Think of “ignite” ignite § To light a fire § Igneous rock comes from the heat within Earth: Earth Geothermal

How are Igneous Rocks Classified? Igneous rocks are classified by: § 1. Mineral Composition

How are Igneous Rocks Classified? Igneous rocks are classified by: § 1. Mineral Composition § 2. Crystal Size (Texture)

Igneous Rock Formation Most Igneous rocks form directly from Magma which is hot, molten

Igneous Rock Formation Most Igneous rocks form directly from Magma which is hot, molten rock § Granite is the most common igneous rock, it cooled from magma Igneous rocks can also form from lava

3. First Classification of Magma: Felsic § Is rich in Silica (Si. O 2)

3. First Classification of Magma: Felsic § Is rich in Silica (Si. O 2) § Small amounts of Ca, Fe, Mg (Calcium, Iron, & Magnesium) § Slow-moving, thick= HIGH VISCOSITY (resistance to flowing) § Crystallizes to light-colored minerals § Resulting rocks have relatively low density § Felsic rocks make up the continents

Examples of FELSIC igneous rocks Rhyolite Pumice

Examples of FELSIC igneous rocks Rhyolite Pumice

4. Second Classification of Magma: Mafic § Low amounts of Silica (Si. O 2)

4. Second Classification of Magma: Mafic § Low amounts of Silica (Si. O 2) § Fe and Mg rich (Iron and Magnesium) § Fast-moving, thinner= LOW Viscosity: Fast less resistance to flowing, more fluid § Crystallize to dark-colored minerals § Resulting rocks have relatively high density § Mafic rocks make up the ocean floors

Mafic Igneous Rock examples: Basalt (ocean floor) Gabbro

Mafic Igneous Rock examples: Basalt (ocean floor) Gabbro

5. Crystal Size § It takes time to grow crystals § As magma cools,

5. Crystal Size § It takes time to grow crystals § As magma cools, it crystallizes § If magma cools slowly, slowly what size crystals will form? Large Crystals If Magma cools quickly, small crystals will form because they have little time to grow.

Igneous Rock Obsidian cools so fast that no crystals have time to form A.

Igneous Rock Obsidian cools so fast that no crystals have time to form A. K. A. Volcanic glass Obsidian is dark in color due to iron oxides.

6. Igneous Rocks Intrusive § Igneous rock that crystallizes below Earth’s surface, from magma

6. Igneous Rocks Intrusive § Igneous rock that crystallizes below Earth’s surface, from magma § Intrusive= Inside Earth Granite Large Crystal size Notice how Granite has large crystals, it cooled slowly from magma deep beneath Earth’s surface

Igneous Rocks Extrusive § Igneous rock that crystallizes or forms at Earth’s surface, from

Igneous Rocks Extrusive § Igneous rock that crystallizes or forms at Earth’s surface, from lava § Extrusive= exited Earth Basalt Small Crystal size Notice how basalt has small crystals, it cooled quickly at Earth’s surface