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Explore the rock cycle in detail, examining the three main types of rocks: igneous, sedimentary, and metamorphic. Igneous rocks form from the solidification of magma or lava, classified as extrusive or intrusive based on their cooling rate. Sedimentary rocks arise from sediments or chemical processes, including clastic, chemical, and organic types. Metamorphic rocks result from heat and pressure altering existing rock, categorized into foliated and non-foliated textures. Dive deeper into geology and learn how these rock types interact in the Earth's crust.
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Rocks 3.1
Igneous Rocks • Form from the solidification of melted minerals (magma or lava). • Magma = melted rock underground • Lava = melted rock aboveground • Extrusive Igneous Rocks – Rocks formed from hardened lava. • Quick cooling results in extrusive igneous rocks with fine-grained or glassy textures. • Intrusive Igneous Rocks – Rocks formed from hardened magma. • Slow cooling results in intrusive igneous rocks with coarse-grained textures.
Sedimentary Rocks Sedimentary rocks may be made of rock fragments—sediments—or by chemical reactions. The classification of sediments is shown below.
3 Types of Sedimentary Rock • Clastic • Sedimentary rocks made of cemented sediments. • Chemical • Form from chemical precipitation. When minerals settle out from a solution, they come together to form chemical rocks. • Organic • Rocks that come from the remains of organic matter. A good example is coal.
Metamorphic Rocks • Formed when heat and pressure changes existing rock. • This can be done 2 ways: • Contact Metamorphism (heat driven) – when magma intrudes into a previously existing rock layer, and “bakes” the surrounding rock. • Regional Metamorphism (pressure driven) – when intense pressure is applied to previously existing rock. Is driven by plate tectonics.
Contact Metamorphism Contact Metamorphism Previously Existing Rock
Regional Metamorphism Pressure Pressure
Types of Metamorphic Rocks Foliated Non-Foliated No banded appearance. • Have a banded appearance.