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Discover the significance of rocks in the natural world, from formation to classification. Learn about the rock cycle and geological processes that shape the Earth's features. Explore the value of rocks as a crucial resource and their role in construction materials. Uncover how weathering, erosion, and deposition contribute to rock formation and transformation. Delve into the classification of rocks based on their composition and texture, including igneous, sedimentary, and metamorphic types.
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Chapter 4: Rocks – Mineral MixturesSection 1: The Rock Cycle
Chapter 4 Section 1The Rock Cycle The Rock Cycle • A rock is a naturally occurring solid mixture of one or more minerals or organic matter. • New rock forms from old rock material constantly. • The series of processes in which a rock forms, changes from one type to another, is destroyed, and forms again by geological processes is called the rock cycle.
Chapter 4 Section 1The Rock Cycle
Chapter 4 Section 1The Rock Cycle The Value of Rock • Rock has been an important natural resource for as long as humans have existed. • Ancient and modern civilizations have used granite, limestone, marble sandstone, slate and other rocks as construction materials. • Rock is also an important ingredient in concrete and plaster, both of which are commonly used in construction.
Chapter 4 Section 1The Rock Cycle Processes That Shape the Earth • Certain geological processes make and destroy rock. • These processes shape the features of our planet. • These processes also influence the type of rock that is found in certain areas. Resources
Chapter 4 Section 1The Rock Cycle Processes That Shape the Earth, continued • The process in which water, wind, ice, and heat break down rock is calledweathering. • Weathering is important because it breaks down rock into fragments of which sedimentary rock is made.
Chapter 4 Section 1The Rock Cycle Processes That Shape the Earth, continued • The process by which wind, water, ice, or gravity transports soil and sediment from one location to another is callederosion. • The process in which sediment moved by erosion is dropped and comes to rest is calleddeposition.
Chapter 4 Section 1The Rock Cycle Processes That Shape the Earth, continued • Sedimentary rock can also form when buried sediment is squeezed by the weight of overlaying layers of sediment. • If the temperature and pressure are high enough, the rock can change into metamorphic rock. • If the rock gets hot enough to melt, this creates the magma that eventually cools to form igneous rock.
Chapter 4 Section 1The Rock Cycle Processes That Shape the Earth, continued • How the Cycle Continues Buried rock is exposed at the Earth’s surface by a combination of uplift and erosion. • Upliftis the movement within the Earth that causes rocks inside the Earth to be moved to the surface. • When uplifted rock reaches the Earth’s surface, weathering, erosion, and deposition begin.
Chapter 4 Section 1The Rock Cycle Illustrating the Rock Cycle • The rock cycle is the continual process by which new rock forms from old rock material. Round and Round It Goes • Rocks may follow various pathways in the rock cycle.
Chapter 4 Section 1The Rock Cycle Rock Classification • Rock can be three main classes based on how the rock is formed: • Igneous rock • Sedimentary rock • Metamorphic rock
Chapter 4 Section 1The Rock Cycle Rock Classification, continued • Each class of rock can be divided further, based on differences in the ways rocks form. • Igneous rock can be divided again based on whether the magma from which it forms cools on the Earth’s surface or below ground.
Chapter 4 Section 1The Rock Cycle Rock Classification, continued • Sedimentary and metamorphic rocks are also divided into smaller groups. • Scientists study rocks in detail using two important criteria: composition and texture.
Chapter 4 Section 1The Rock Cycle Rock Classification, continued • Composition is the chemical makeup of a rock. Composition can describe either the minerals or other materials in the rock. • Texture is the quality of a rock that is based on the sizes, shapes, and positions of the rock’s grains.