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Chapter 3: Rocks Table of Contents Section 1: The Rock Cycle.

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Page 1: Chapter 3: Rocks Table of Contents Section 1: The Rock Cycle.
Page 2: Chapter 3: Rocks Table of Contents Section 1: The Rock Cycle.

Chapter 3: Rocks

Table of ContentsTable of Contents

Section 1: The Rock Cycle

Page 3: Chapter 3: Rocks Table of Contents Section 1: The Rock Cycle.

1. Most rock used for building stone contains one or more common minerals, called rock-forming minerals, such as quartz, feldspar, mica, or calcite.

2. When you look closely, the sparkles you see are individual crystals of minerals.

A. What is a rock?—Common Rocks

The Rock CycleThe Rock Cycle

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3. A rock is a mixture of such minerals, rock fragments, volcanic glass, organic matter, or other natural materials.

Page 4: Chapter 3: Rocks Table of Contents Section 1: The Rock Cycle.

1. To show how rocks slowly change through time, scientists have created a model called the rock cycle.

2. It illustrates the processes that create and change rocks.

B. The Rock Cycle

The Rock CycleThe Rock Cycle

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Page 5: Chapter 3: Rocks Table of Contents Section 1: The Rock Cycle.

B. The Rock Cycle

The Rock CycleThe Rock Cycle

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3. The rock cycle shows the three types of rock— igneous, metamorphic, and sedimentary—and the processes that form them. Click image to view movie.

Page 6: Chapter 3: Rocks Table of Contents Section 1: The Rock Cycle.

4. Rocks change by many processes. For example, a sedimentary rock can change by heat and pressure to form a metamorphic rock.

B. The Rock Cycle

The Rock CycleThe Rock Cycle

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5. The metamorphic rock then can melt and later cool to form an igneous rock.

Page 7: Chapter 3: Rocks Table of Contents Section 1: The Rock Cycle.

6. The igneous rock then could be broken into fragments by weathering and erode away.

7. The fragments might later compact and cement together to form another sedimentary rock. Any given rock can change into any of the three major rock types. A rock even can transform into another rock of the same type.

B. The Rock Cycle

The Rock CycleThe Rock Cycle

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Page 8: Chapter 3: Rocks Table of Contents Section 1: The Rock Cycle.

1. The rock cycle shows how rock can be weathered to small rock and mineral grains.

2. This material then can be eroded and carried away by wind, water, or ice.

C. Matter and the Rock Cycle

The Rock CycleThe Rock Cycle

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3. This illustrates the principle of conservation of matter.

4. The changes that take place in the rock cycle never destroy or create matter.

5. The elements are just redistributed in other forms.

Page 9: Chapter 3: Rocks Table of Contents Section 1: The Rock Cycle.

Section CheckSection Check

11Question 1

Which of these is a rock?

A. feldsparB. graniteC. micaD. quartz

Page 10: Chapter 3: Rocks Table of Contents Section 1: The Rock Cycle.

11Section CheckSection Check

Answer

The answer is B. Rocks are mixtures of minerals. Granite is a mixture of feldspar, mica, quartz and other minerals.

Page 11: Chapter 3: Rocks Table of Contents Section 1: The Rock Cycle.

Section CheckSection Check

11Question 2

Weathering and erosion of igneous rocks produces material that can become __________ rock.

A. magmaB. metamorphicC. more igneousD. sedimentary

Page 12: Chapter 3: Rocks Table of Contents Section 1: The Rock Cycle.

11Section CheckSection Check

Answer

The answer is D. Sediments from the weathering of igneous rock form sedimentary rock through compaction and cementation.

Page 13: Chapter 3: Rocks Table of Contents Section 1: The Rock Cycle.

Section CheckSection Check

11Question 3

Which is formed by cooling magma?

A. garnetB. igneousC. metamorphicD. sedimentary

Page 14: Chapter 3: Rocks Table of Contents Section 1: The Rock Cycle.

11Section CheckSection Check

Answer

The answer is B. Igneous rock is formed from cooling magma. Garnet is a mineral found in multiple rock types.

Page 15: Chapter 3: Rocks Table of Contents Section 1: The Rock Cycle.

End of Chapter Summary File


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