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Igneous Metamorphic Sedimentary
Rocks Igneous Metamorphic Sedimentary
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What is a Rock? A rock is composed of minerals
Can be made of organic material Solid material that forms Earth’s hard surface.
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Igneous Rock
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Igneous Rock Rock that crystallizes from cooling of magma (inside Earth) or lava (on/outside surface of Earth) Characterized two ways – INtrusive or EXtrusive
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Intrusive Igneous Rock
Crystallizes inside of Earth from magma Magma cools slowly (because of the blanket of the Earth’s layers)
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Intrusive Igneous Rock (continued)
Devils Tower, Wyoming Cooling slowly = large interlocking crystals (usually two or more colors) Large crystals = coarse-grained texture
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Igneous Intrusive Rock Samples
Granite Note 3 minerals = mica (black) quartz (smoky) feldspar (pink)
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Extrusive Igneous Rock
Crystallizes outside of Earth from lava – mostly from volcanic activity Lava cools quickly Cooling quickly = tiny or no mineral grains (usually one drab color)
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Extrusive Igneous Rocks (Continued)
Tiny or no mineral grains = fine-grained texture EXTRA : Sometimes has pores or holes from trapped gases
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Extrusive Igneous Rock Samples
Basalt (seafloor) Notice the drab color Notice the holes or pores Pumice Notice the very smooth texture Obsidian (volcanic glass)
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Mafic vs Felsic Mafic igneous rocks - dark in color and have a high density due to high quantities of heavy elements (magnesium, iron, calcium and sodium) basalt (extrusive) and gabbro (intrusive). Felsic igneous rocks – light in color and have a lower density due to high quantities of lighter elements (silicon, oxygen, aluminum, sodium and potassium) Pumice (extrusive) and granite (intrusive)
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Sedimentary Rock How does Sedimentary Rock form?
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#1 #2 #4 #3
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Sedimentary Rock Formed at surface of Earth (in lakes, oceans, rivers) in thin or thick layers (strata) Layering is referred to as stratification Formed from Cementation & Compaction of sediments or Evaporation/Precipitation Only rock type to contain fossils Characterized two ways – clastic or non-clastic
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Clastic Sedimentary Rock
Mineral grains (sediments/fragments) are compacted and cemented together. Example – sand compacted and cemented = sandstone Example – mud/clay compacted and cemented = shale Example – pebbles, sand and mud compacted and cemented = conglomerate
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Clastic Sedimentary Rock Samples
shale field sandstone
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Non-clastic Sedimentary Rock
Two types – Organic Non-clastic or Chemical Non-clastic Organic – made from once living things – plants (coal) or animal life (fossil rich limestone - coquina) Chemical – made from evaporation (gypsum) or precipitation – (CaCO3 – chemical limestone)
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Non-clastic Sedimentary Rock Samples
Coal - organic Chemical limestone Fossil rich limestone - organic Gypsum - chemical
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Sedimentary Features Ripple Marks – left by water or wind in sand, mud, etc. – can be preserved as a rock feature
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Sedimentary Features Mud cracks in today’s puddles can be preserved as rock millions of years from now
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Sedimentary Features Cross bedding – formed in old sand dunes or on off-shore sand bars
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Metamorphic Rock How is metamorphic rock formed?
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Metamorphic Rock Formed deep inside the Earth from intense heat and pressure Any rock type can be changed by metamorphism – depends on how much heat, pressure and original rock type to determine the outcome No melting involved – solid state process (more like softening) Hardest of three types of rock Characterized two ways – foliated or non-foliated
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Foliated Metamorphic Rock
Banding (stripes) or cleavage (flaky) is present Always a change structure and texture of original rock and sometimes a change in the composition. When composition changes – most often a semi to precious gem can be formed.
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Foliated Metamorphic Rock Samples
Gneiss (Previously granite) schist
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Non-foliated Metamorphic Rock
NO Banding and/or NO cleavage Change in structure and texture of original rock Possible change in composition.
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Non-foliated Metamorphic Rock Samples
Quartzite (previously sandstone) Marble (previously limestone)
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