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Chapter 3 TYPES OF: Rocks
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Rocks Rocks Rocks are any solid mass of mineral or mineral-like matter occurring naturally as a part of our planet. Types of Rocks The 3 kinds of rocks are igneous, sedimentary, and metamorphic
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Igneous Rocks formed by the crystallization of molten magma or lava.
Magma is molten material deep beneath the Earth’s surface Lava is molten material above the surface
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Types of Igneous Rocks 1. Intrusive igneous rocks are formed when magma hardens beneath Earth’s surface. 2. Extrusive igneous rocks are formed when lava hardens (above the Earth’s surface).
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How Igneous Rocks are Classified
Igneous rocks can be classified based on their composition and texture. 1. Texture • Coarse-grained texture is caused by slow cooling resulting in larger crystals. • Fine-grained texture is caused by rapid cooling resulting in smaller, interconnected mineral grains. • Glassy texture is caused by very rapid cooling.
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Course-Grained Igneous Texture
Granite
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Fine-Grained Igneous Texture
Rhyolite
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Obsidian Exhibits a Glassy Texture.
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2. Composition What the rock is made of, based on the amounts of light and dark minerals in the rock.
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Porphyritic Igneous Texture
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Basalt
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Classification of Igneous Rocks
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Sedimentary Rocks Formation of Sedimentary Rocks
• Erosion involves the weathering and the removal of rock. • Deposition occurs when an agent of erosion—water, wind, ice, or gravity—loses energy and drops sediments.
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Sedimentary Rock Formation
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• Compaction is a process that squeezes, or compacts, sediments.
• Cementation takes place when dissolved minerals are deposited in the tiny spaces among the sediments.
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3 Types of Sedimentary Rock
Clastic – composed of weathered bits of rocks and minerals Classified by particle size Ex: Shale, Sandstone, Conglomerate, Grand canyon & the wave in Arizona
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Shale with Plant Fossils
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Sandstone
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Conglomerate
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The Wave, Page, AZ
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Grand Canyon, Arizona
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Chemical – When minerals dissolve out of water
Ex: limestone (caves), coal, rock salt
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Fossiliferous Limestone
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Carlsbad Caverns, NM Stalactites Stalagmites
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Organic – Formed by fossils or organic matter within the rock layers
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Classification of Sedimentary Rocks
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Metamorphic Rocks Formation of Metamorphic Rocks
Metamorphism means “to change form.” Igneous and sedimentary rocks change at elevated temperatures and pressures deep within the Earth or during mountain building
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Agents of Metamorphism
Heat Provides the energy needed to drive chemical reactions Pressure Causes a more compact rock with greater density
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Origin of Pressure in Metamorphism
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Hydrothermal Solutions
Hot water-based solutions escaping from magma Dissolves original minerals and then deposits new ones
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Classifying Metamorphic Rocks
Two main categories 1. Foliated Metamorphic Rock Has a banded or layered appearance 2. Nonfoliated Metamorphic Rock Does not have a banded texture
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Classification of Metamorphic Rocks
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Gneiss Typically Displays a Banded Appearance
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Marble—A Nonfoliated Metamorphic Rock
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Fill in the following table using your textbook (pgs. 71-84)
IGNEOUS ROCKS SEDIMENTARY ROCKS METAMORPHIC ROCKS
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