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Published byOsborne Marsh Modified over 9 years ago
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TAKS Objective 5 The student will demonstrate an understanding of earth and space systems.
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TEKS Objective: 8.12 The student knows that cycles exist in Earth systems. The student is expected to Aanalyze and predict the sequence of events in the lunar and rock cycles.
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Prior Knowledge TEKS 6.6 C – Students identify forces that shape the feature of the earth including uplifting, movement of water, and volcanic activity. TEKS 7.14 B – Student analyze effects of regional erosional deposition and weathering.
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Learning Objectives The student will be able to predict the events in the rock cycle. The student will be able to diagram and explain the rock cycle.
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All rocks are heavy. True or False
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A heavy piece of rock? Think again!
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All rocks are hard. True or False
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False Chalk Pumice Talc
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Rocks never change. True or False
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False Rocks are changed by processes such as: –Melting –Pressure –Heat –Weathering and Erosion
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Teacher Background
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Igneous rocks are formed when magma cools. http://www.fi.edu/fellows/fellow1/oct98/c reate/igneous.htm
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Melting
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Sedimentary rocks are formed when layers of earth have been deposited in the bottoms of bodies of water. Over time these layers are pressed together forming sedimentary rocks. http://www.fi.edu/fellows/fellow 1/oct98/create/sediment.htm
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Weathering and Erosion
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Metamorphic rocks were once sedimentary or igneous rocks that have been placed under tons of pressure and heat. http://www.fi.edu/fellows/fellow1/oct98/c reate/metamorph.htm
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Igneous Sedimentary Metamorphic
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Rock Cycle Diagram
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ENGAGE
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A rock can be a thing of beauty. Photos by Sandra Woodruff
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Explore Explore Chocolate Rocks!
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Explain How did you simulate weathering and erosion? How are sedimentary rocks formed? How are metamorphic rocks formed? How are igneous rocks formed?
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Elaborate Rock Cycle Pictures and Arrows
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Evaluate Draw Your Own Rock Cycle Use the words below. The words may be used more than once. Igneous RockMeltingLithofication Sedimentary RockMagmaCementation Metamorphic RockCoolingCompaction Heat and PressurePressure Weathering & ErosionSediments
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