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4.2 Ingeous Rock
Chapter 4.2 Ingeous Rock
Three ways magma can form | 1) When rock is heated 2) When pressure is released 3) When the rock changes composition. |
Igneous Rock | Forms when hot, liquid rock that has cooled and solidified. |
3 Factors that affect magma formation | 1) Temperature: Different minerals melt and cool at different rates. 2) Composition: The mineral content and water content of rocks affect its melting and cooling points. 3) Pressure: When pressure is released from rocks some minerals melt. |
Composition of rocks | What minerals/chemicals a rock is made from determines when it will melt and how fast it will cool. |
Texture of rocks | Texture is determined by cooling rate. Rocks that cool quickly have few crystals and a fine texture. Rocks that cool slowly have a many crystals and a coarse texture. |
Felsic Rocks | Light in color and less dense. Rich in aluminum, potassium, silicon, and sodium. |
Mafic Rocks | Dark in color and more dense. Rich in calcium, iron, and magnesium, but contain little silicon. |
Intrusive Igneous Rock | Coarse in texture, cools slowly inside the earth. |
Extrusive Igneous Rock | Formed when erupting magma, cools quickly and contains very few crystals. |