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ROCKS
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Are classified according to the environment in which they _________
form
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Types of Rocks: ________ ________ ________
igneous Types of Rocks: ________ ________ ________ sedimentary metamorphic
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IGNEOUS ROCKS
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Where Does Igneous Rock Form?
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I. FORMATION OF IGNEOUS ROCKS
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solidification crystallization
A. Igneous rocks form directly from the _____________ and _____________ crystallization
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of _____molten rock to form _______ rock
liquid of _____molten rock to form _______ rock solid
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FOUNTAINING
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FISSURE ERUPTION
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LAVA FLOW
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LAVA FLOW OVER A ROAD
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LAVA FLOW THROUGH FORREST
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Kilauea, HI 2003
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Kilauea, HI , 2003
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Mt. ST. Helens
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Volcanic crater
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crazy vulcanist
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SKY LIGHT
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B. _____________ is the process when a liquid rock cools,
crystallization B. _____________ is the process when a liquid rock cools,
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and it changes to a solid made of ___________________
INTERGROWN CRYSTALS
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GRANITE MICROSCOPIC VIEW
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2. CLASSIFICATION OF IGNEOUS ROCKS:
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A. 2 characteristics that are used to classify igneous rocks:
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texture 1. ______________ 2. ______________ mineral composition
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B. Texture of an igneous rock describes the
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size shape arrangement
_________, __________ and ____________ of the mineral crystals it was made from. arrangement
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C. The ______ of the crystals depends on the _______________________
size C. The ______ of the crystals depends on the _______________________ Rate of cooling
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Slow cooling = ____________
large crystals
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MINERAL CRYSTALS
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GABBRO
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Fast cooling = ____________
fine crystals Or no crystals (glassy)
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GLASSY TEXTURE: OBSIDIAN
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BASALT: FINE CRYSTALS
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BASALT MICROSCOPIC VIEW
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Granite: Coarse crystals Basalt: Fine crystals (Microscopic views)
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FINE CRYSTAL: RYOLITE
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3. EXTRUSIVE IGNEOUS ROCKS:
Extrusions A. _____________ occurs when molten (liquid) rock flows out of the earth as ________________ lava
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lava magma
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And cools __________ quickly
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to form fine or no ____________ crystals
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Vesicular basalt gas pockets
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frothy texture (vesicular) This rock if full of gas pockets
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B. To form magma, ____________ must be melted. minerals
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pressures temperatures C. Minerals melt at different
____________ and ___________ temperatures pressures
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D. Igneous rocks of different
____________ composition
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Can form from the same body of ____________
magma
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4. INTRUSIVE IGNEOUS ROCKS:
Intrusions A. _____________ occurs when molten rock beneath the surface (magma)
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cools ____________ to form _____________ slowly coarse crystals
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Granite: Coarse crystals Basalt: Fine crystals (Microscopic views)
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low light (granitic) 5. FELSIC
A. Igneous rocks of the continental crust are rich in _________ density _________ colored minerals low light (granitic)
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high dark (basaltic) 6. MAFIC
A. Igneous rocks of the ocean floor are rich in _________ density _________ colored minerals high dark (basaltic)
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Comparing Oceanic Crust To Continental Crust
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low density light color granitic felsic thick Continental Crust: 1. 2.
3. 4. 5. low density light color granitic felsic thick
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high density dark color basaltic mafic thin Oceanic Crust: 1. 2. 3. 4.
5. high density dark color basaltic mafic thin
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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
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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
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When rocks melt, bonds broken. Crystalline solid no longer exists.
MELTING ROCKS AND CRYSTALLIZING MAGMA Rock magma magma rock When rocks melt, bonds broken. Crystalline solid no longer exists.
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Hot liquid contains still solid fragments
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
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Cooling of hot liquid allows crystallization of minerals
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
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OK……….. TAKE OUT YOUR REFERENCE TABLE
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