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Classifying Rocks CH 3 Prentice Hall p. 74-77 Rocks • Are made of mixtures of minerals and other materials, although some may contain only a single mineral. – Granite • • • • Quartz Feldspar, Mica Hornblend Characteristics (brainstorm) Group A Group B Rock Color Texture Group C Luster Group D Group E Group F Density Hardness Porous Texture • Size, shape and pattern of rock grains. – Grains- particles of minerals or other rocks. Texture (Grain Size) • Course Grained- Large and easy to see. • Fine Grained- small. Texture (Grain Shape) • Grains vary widely. – Tiny particles of sand. – Look like seeds – Crystals – Smooth / rounded – Jagged Texture (Grain Pattern) • Grains often form patterns. – Some lie in flat layers. – Rows of grains. – Random grains. Texture (No Visible Grain) • Have no grain. – They cool very quickly when they form, gives the rock a smooth, shiny texture like thick glass. (obsidian) – Or made out of extremely small particles of silica that settle out of water. (flint) Origin • 3 Groups- refers to how the rocks formed. Igneous Sedimentary Metamorphic • Forms from cooling molten rock. • Magmabelow the surface. • Lava- above the surface. • Forms from particles of other rocks, remains of plants and animals that are pressed and cemented together. • Forms from pre-existing rock, deep underground. • Changes rock with heat, pressure and chemical reactions. Mineral Composition • Use a microscope to look at the size & shape of crystals to ID (identify) minerals in the rock. • Acid test- tests for carbonates. • Magnetic Test- tests for iron and nickel. Rock Cycle