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Rocks Rock! What is a rock? • Any solid mass of minerals that occur naturally The Rock Cycle • Interactions among Earth’s water, air, & land cause rocks to change from one type to another. Major Types of Rocks • Classified by their chemical composition & texture • Igneous Rocks • Sedimentary Rocks • Metamorphic Rocks Igneous Rock • Forms when magma cools and hardens • Can occur beneath the surface or as a result of volcanic eruptions Igneous Composition • Minerals: – Quartz – Feldspar – Biotite Mica • Granitic • Andesitic • Basaltic Igneous Texture • Coarse-Grained – SLOW COOLING – LARGE crystals • Fine-Grained – RAPID COOLING – SMALL crystals • Glassy – Cools so fast no crystals can form • Porphyritic – Crystals do not cool at same rate – Large crystals surrounded by small crystals Sedimentary Rock • Exposed igneous or metamorphic rocks undergoes weathering – This means the rock is physically and chemically broken down (by water, air, & living things) into sediments – Clastic Sedimentary Rock = physically broken – Chemical Sedimentary Rock = chemically broken • Sediments are compacted and cemented together to form sedimentary rock Clastic Sedimentary Rocks • Grouped according to SIZE of sediments in the rock • Conglomerate – Rounded, gravel-size or larger • Breccia – Angular sediments • Sandstone – Sand sized sediments • Shale – Very fine-grained sediments (most common type) • Siltstone – Fine-grained rock What are these? (Bio)Chemical Sedimentary Rocks • Usually occurs when water evaporates off leaving a solid product • Limestone (from shells) • Chalk • Coquina (cemented shells) • • • • Rock Salt Chert Flint Rock Gypsum Limestone Coquina Chalk Flint Rock Salt Chert Rock Gypsum Metamorphic Rock • Under extreme pressure & temperature sedimentary or igneous rock will change into metamorphic rock Foliated Metamorphic Rock • Have a layered or banded appearance • Gneiss & schist Non-foliated Metamorphic Rock • Does not have a banded texture • Marble (calcite) • Quartzite • Anthracite Magma • Metamorphic rock can melt to form magma if it is subject to additional pressure and temperature changes