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Published byOswald Hampton Modified over 8 years ago
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Rocks Earth’s crust is made of rock. Rocks are mixtures of minerals and sometimes other materials.
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When studying a rock sample, geologists observe the rock’s: Color Texture Chemical composition
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Most rocks are made up of grains, particles of minerals, or other rocks. Texture is the look that results from: Size Shape Pattern of rock’s grains
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Coarse-grained-- large/easy to see. Fine-grained – small, even microscopic.
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Grains in rock often form a pattern.
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Flat layers (strata)
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Wavy, swirling patterns
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Rows of beads
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Random or no pattern
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Some rocks have NO grain, because they cooled too quickly when they formed.
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There are 3 groups of rocks: Igneous Metamorphic Sedimentary
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Igneous Rocks Formed from the cooling of molten (melted) rock. Examples: pumice, granite, basalt
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Sedimentary Rocks Formed when particles of other rocks, plants, or animals are cemented together. Examples: Sandstone, breccia, siltstone
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Formed when existing rock is changed by heat, pressure, or chemical reactions. Examples: gneiss, schist, phyllite Metamorphic Rocks
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The Rock Cycle
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