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1 How to Use This Presentation
To View the presentation as a slideshow with effects select “View” on the menu bar and click on “Slide Show.” To advance through the presentation, click the right-arrow key or the space bar. From the resources slide, click on any resource to see a presentation for that resource. From the Chapter menu screen click on any lesson to go directly to that lesson’s presentation. You may exit the slide show at any time by pressing the Esc key.

2 Standardized Test Prep Image and Math Focus Bank
Resources Chapter Presentation Bellringers Transparencies Standardized Test Prep Image and Math Focus Bank CNN Videos Header – dark yellow 24 points Arial Bold Body text – white 20 points Arial Bold, dark yellow highlights Bullets – dark yellow Copyright – white 12 points Arial Size: Height: 7.52" Width: 10.02" Scale: 70% Position on slide: Horizontal - 0" Vertical - 0" Visual Concepts

3 Chapter 4 Table of Contents Section 1 The Rock Cycle
Rocks: Mineral Mixtures Table of Contents Section 1 The Rock Cycle Section 2 Igneous Rock Section 3 Sedimentary Rock Section 4 Metamorphic Rock Header – dark yellow 24 points Arial Bold Body text – white 20 points Arial Bold, dark yellow highlights Bullets – dark yellow Copyright – white 12 points Arial Size: Height: 7.52" Width: 10.02" Scale: 70% Position on slide: Horizontal - 0" Vertical - 0"

4 Chapter 4 Section 1 The Rock Cycle Bellringer Most of us try to recycle the items we use in our daily lives to minimize the pollution we cause. In a way, the Earth also recycles through the rock cycle. How can a rock be recycled? How long would recycling a rock take? What would a rock look like before, during, and after the process of recycling? Record your thoughts about these questions in your science journal. Header – dark yellow 24 points Arial Bold Body text – white 20 points Arial Bold, dark yellow highlights Bullets – dark yellow Copyright – white 12 points Arial Size: Height: 7.52" Width: 10.02" Scale: 70% Position on slide: Horizontal - 0" Vertical - 0"

5 Objectives Chapter 4 Describe two ways rocks have been used by humans.
Section 1 The Rock Cycle Objectives Describe two ways rocks have been used by humans. Describe four processes that shape Earth’s features. Describe how each type of rock changes into another type as it moves through the rock cycle. List two characteristics of rock that are used to help classify it. Header – dark yellow 24 points Arial Bold Body text – white 20 points Arial Bold, dark yellow highlights Bullets – dark yellow Copyright – white 12 points Arial Size: Height: 7.52" Width: 10.02" Scale: 70% Position on slide: Horizontal - 0" Vertical - 0"

6 Chapter 4 Section 1 The 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. Header – dark yellow 24 points Arial Bold Body text – white 20 points Arial Bold, dark yellow highlights Bullets – dark yellow Copyright – white 12 points Arial Size: Height: 7.52" Width: 10.02" Scale: 70% Position on slide: Horizontal - 0" Vertical - 0"

7 Chapter 4 Section 1 The Rock Cycle
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8 The Value of Rock Chapter 4
Section 1 The 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. Header – dark yellow 24 points Arial Bold Body text – white 20 points Arial Bold, dark yellow highlights Bullets – dark yellow Copyright – white 12 points Arial Size: Height: 7.52" Width: 10.02" Scale: 70% Position on slide: Horizontal - 0" Vertical - 0"

9 Processes That Shape the Earth
Chapter 4 Section 1 The 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. Header – dark yellow 24 points Arial Bold Body text – white 20 points Arial Bold, dark yellow highlights Bullets – dark yellow Copyright – white 12 points Arial Size: Height: 7.52" Width: 10.02" Scale: 70% Position on slide: Horizontal - 0" Vertical - 0" Resources

10 Processes That Shape the Earth, continued
Chapter 4 Section 1 The Rock Cycle Processes That Shape the Earth, continued Weathering, Erosion, and Deposition The process in which water, wind, ice, and heat break down rock is called weathering. Weathering is important because it breaks down rock into fragments of which sedimentary rock is made. Header – dark yellow 24 points Arial Bold Body text – white 20 points Arial Bold, dark yellow highlights Bullets – dark yellow Copyright – white 12 points Arial Size: Height: 7.52" Width: 10.02" Scale: 70% Position on slide: Horizontal - 0" Vertical - 0"

11 Processes That Shape the Earth, continued
Chapter 4 Section 1 The 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 called erosion. The process in which sediment moved by erosion is dropped and comes to rest is called deposition. Header – dark yellow 24 points Arial Bold Body text – white 20 points Arial Bold, dark yellow highlights Bullets – dark yellow Copyright – white 12 points Arial Size: Height: 7.52" Width: 10.02" Scale: 70% Position on slide: Horizontal - 0" Vertical - 0"

12 Processes That Shape the Earth, continued
Chapter 4 Section 1 The Rock Cycle Processes That Shape the Earth, continued Heat and Pressure 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. Header – dark yellow 24 points Arial Bold Body text – white 20 points Arial Bold, dark yellow highlights Bullets – dark yellow Copyright – white 12 points Arial Size: Height: 7.52" Width: 10.02" Scale: 70% Position on slide: Horizontal - 0" Vertical - 0"

13 Processes That Shape the Earth, continued
Chapter 4 Section 1 The 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. Uplift is 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. Header – dark yellow 24 points Arial Bold Body text – white 20 points Arial Bold, dark yellow highlights Bullets – dark yellow Copyright – white 12 points Arial Size: Height: 7.52" Width: 10.02" Scale: 70% Position on slide: Horizontal - 0" Vertical - 0"

14 Illustrating the Rock Cycle
Chapter 4 Section 1 The 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. The following Visual Concepts presentation show the different ways rock may change when it goes through the rock cycle. Header – dark yellow 24 points Arial Bold Body text – white 20 points Arial Bold, dark yellow highlights Bullets – dark yellow Copyright – white 12 points Arial Size: Height: 7.52" Width: 10.02" Scale: 70% Position on slide: Horizontal - 0" Vertical - 0"

15 Rock Cycle Chapter 4 Section 1 The Rock Cycle
Click below to watch the Visual Concept. You may stop the video at any time by pressing the Esc key. Visual Concept Header – dark yellow 24 points Arial Bold Body text – white 20 points Arial Bold, dark yellow highlights Bullets – dark yellow Copyright – white 12 points Arial Size: Height: 7.52" Width: 10.02" Scale: 70% Position on slide: Horizontal - 0" Vertical - 0"

16 Rock Classification Chapter 4
Section 1 The Rock Cycle Rock Classification Rock can be three main classes based on how the rock is formed: Igneous rock Sedimentary rock Metamorphic rock Header – dark yellow 24 points Arial Bold Body text – white 20 points Arial Bold, dark yellow highlights Bullets – dark yellow Copyright – white 12 points Arial Size: Height: 7.52" Width: 10.02" Scale: 70% Position on slide: Horizontal - 0" Vertical - 0"

17 Types of Rock Chapter 4 Section 1 The Rock Cycle
Click below to watch the Visual Concept. You may stop the video at any time by pressing the Esc key. Visual Concept Header – dark yellow 24 points Arial Bold Body text – white 20 points Arial Bold, dark yellow highlights Bullets – dark yellow Copyright – white 12 points Arial Size: Height: 7.52" Width: 10.02" Scale: 70% Position on slide: Horizontal - 0" Vertical - 0"

18 Rock Classification, continued
Chapter 4 Section 1 The 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. Header – dark yellow 24 points Arial Bold Body text – white 20 points Arial Bold, dark yellow highlights Bullets – dark yellow Copyright – white 12 points Arial Size: Height: 7.52" Width: 10.02" Scale: 70% Position on slide: Horizontal - 0" Vertical - 0"

19 Rock Classification, continued
Chapter 4 Section 1 The 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. Header – dark yellow 24 points Arial Bold Body text – white 20 points Arial Bold, dark yellow highlights Bullets – dark yellow Copyright – white 12 points Arial Size: Height: 7.52" Width: 10.02" Scale: 70% Position on slide: Horizontal - 0" Vertical - 0"

20 Rock Classification, continued
Chapter 4 Section 1 The 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. Header – dark yellow 24 points Arial Bold Body text – white 20 points Arial Bold, dark yellow highlights Bullets – dark yellow Copyright – white 12 points Arial Size: Height: 7.52" Width: 10.02" Scale: 70% Position on slide: Horizontal - 0" Vertical - 0"

21 Chapter 4 Section 2 Igneous Rock Bellringer Do you think rocks that cooled and solidified from lava on the Earth’s surface would look different from those that cooled and solidified from magma inside the Earth? Why? Record your response in your science journal. Header – dark yellow 24 points Arial Bold Body text – white 20 points Arial Bold, dark yellow highlights Bullets – dark yellow Copyright – white 12 points Arial Size: Height: 7.52" Width: 10.02" Scale: 70% Position on slide: Horizontal - 0" Vertical - 0"

22 Objectives Chapter 4 Describe three ways that igneous rock forms.
Section 2 Igneous Rock Objectives Describe three ways that igneous rock forms. Explain how the cooling rate of magma affects the texture of igneous rock. Distinguish between igneous rock that cools within the Earth’s crust and igneous rock that cools at the Earth’s surface. Header – dark yellow 24 points Arial Bold Body text – white 20 points Arial Bold, dark yellow highlights Bullets – dark yellow Copyright – white 12 points Arial Size: Height: 7.52" Width: 10.02" Scale: 70% Position on slide: Horizontal - 0" Vertical - 0"

23 Origins of Igneous Rock
Chapter 4 Section 2 Igneous Rock Origins of Igneous Rock Igneous rock forms when hot, liquid rock, or magma, cools and solidifies. There are three ways magma can form: When rock is heated When pressure is released When rock changes composition Header – dark yellow 24 points Arial Bold Body text – white 20 points Arial Bold, dark yellow highlights Bullets – dark yellow Copyright – white 12 points Arial Size: Height: 7.52" Width: 10.02" Scale: 70% Position on slide: Horizontal - 0" Vertical - 0"

24 Composition and Texture of Igneous Rock
Chapter 4 Section 2 Igneous Rock Composition and Texture of Igneous Rock Light-colored igneous rocks are called felsic rocks. Felsic rocks are rich in elements such as aluminum, potassium, silicon, and sodium. Dark-colored igneous rocks are called mafic rocks. Mafic rocks are rich in calcium, iron, and magnesium. Header – dark yellow 24 points Arial Bold Body text – white 20 points Arial Bold, dark yellow highlights Bullets – dark yellow Copyright – white 12 points Arial Size: Height: 7.52" Width: 10.02" Scale: 70% Position on slide: Horizontal - 0" Vertical - 0"

25 Igneous Rock Formations
Chapter 4 Section 2 Igneous Rock Igneous Rock Formations When magma intrudes, or pushes, into surrounding rock below the Earth’s surface and cools, the rock that forms is called intrusive igneous rock. Intrusive igneous rock usually has a coarse-grained texture because it is well insulated by surrounding rocks and cools very slowly. Header – dark yellow 24 points Arial Bold Body text – white 20 points Arial Bold, dark yellow highlights Bullets – dark yellow Copyright – white 12 points Arial Size: Height: 7.52" Width: 10.02" Scale: 70% Position on slide: Horizontal - 0" Vertical - 0"

26 Chapter 4 Section 2 Igneous Rock
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27 Igneous Rock Formations, continued
Chapter 4 Section 2 Igneous Rock Igneous Rock Formations, continued Igneous rock that forms from magma that erupts, or extrudes, on the Earth’s surface is called extrusive igneous rock. Extrusive igneous rock, commonly found around volcanoes, cools quickly on the surface and contains very small crystals or no crystals. Header – dark yellow 24 points Arial Bold Body text – white 20 points Arial Bold, dark yellow highlights Bullets – dark yellow Copyright – white 12 points Arial Size: Height: 7.52" Width: 10.02" Scale: 70% Position on slide: Horizontal - 0" Vertical - 0"

28 Chapter 4 Section 3 Sedimentary Rock Bellringer Tree rings are formed each year of a tree’s life cycle. Tree rings exist because the weather changes of the seasons are reflected in the tree’s bark as the tree grows. How are layers in sedimentary rock alike or different from rings in a tree? What can geologists infer from examining sedimentary rock layers? Record your response in your science journal. Header – dark yellow 24 points Arial Bold Body text – white 20 points Arial Bold, dark yellow highlights Bullets – dark yellow Copyright – white 12 points Arial Size: Height: 7.52" Width: 10.02" Scale: 70% Position on slide: Horizontal - 0" Vertical - 0"

29 Objectives Chapter 4 Describe the origin of sedimentary rock.
Section 3 Sedimentary Rock Objectives Describe the origin of sedimentary rock. Describe the three main categories of sedimentary rock. Describe three types of sedimentary structure. Header – dark yellow 24 points Arial Bold Body text – white 20 points Arial Bold, dark yellow highlights Bullets – dark yellow Copyright – white 12 points Arial Size: Height: 7.52" Width: 10.02" Scale: 70% Position on slide: Horizontal - 0" Vertical - 0"

30 Origins of Sedimentary Rock
Chapter 4 Section 3 Sedimentary Rock Origins of Sedimentary Rock Wind, water, ice, sunlight, and gravity all cause rock to physically weather into fragments. Through erosion, these rock and mineral fragments, called sediment, are moved from one place to another. The sediment is deposited in layers, and eventually newer layers cover the older layers. Header – dark yellow 24 points Arial Bold Body text – white 20 points Arial Bold, dark yellow highlights Bullets – dark yellow Copyright – white 12 points Arial Size: Height: 7.52" Width: 10.02" Scale: 70% Position on slide: Horizontal - 0" Vertical - 0"

31 Sedimentary Rock Cycle
Chapter 4 Section 3 Sedimentary Rock Sedimentary Rock Cycle Click below to watch the Visual Concept. You may stop the video at any time by pressing the Esc key. Visual Concept Header – dark yellow 24 points Arial Bold Body text – white 20 points Arial Bold, dark yellow highlights Bullets – dark yellow Copyright – white 12 points Arial Size: Height: 7.52" Width: 10.02" Scale: 70% Position on slide: Horizontal - 0" Vertical - 0"

32 Origins of Sedimentary Rock, continued
Chapter 4 Section 3 Sedimentary Rock Origins of Sedimentary Rock, continued The most noticeable feature of sedimentary rock is its layers, or strata. A single, horizontal layer of rock is sometimes visible for many miles. Header – dark yellow 24 points Arial Bold Body text – white 20 points Arial Bold, dark yellow highlights Bullets – dark yellow Copyright – white 12 points Arial Size: Height: 7.52" Width: 10.02" Scale: 70% Position on slide: Horizontal - 0" Vertical - 0"

33 Composition of Sedimentary Rock
Chapter 4 Section 3 Sedimentary Rock Composition of Sedimentary Rock Sedimentary rock is classified by the way it forms. Clastic sedimentary rock is made of fragments of rocks cemented together by a mineral such as calcite or quartz. Clasitc sedimentary rocks can have coarse-grained, medium-grained, or fine-grained textures. Header – dark yellow 24 points Arial Bold Body text – white 20 points Arial Bold, dark yellow highlights Bullets – dark yellow Copyright – white 12 points Arial Size: Height: 7.52" Width: 10.02" Scale: 70% Position on slide: Horizontal - 0" Vertical - 0"

34 Chapter 4 Composition of Sedimentary Rock, continued
Section 3 Sedimentary Rock Composition of Sedimentary Rock, continued Chemical sedimentary rock forms from solutions of dissolved mineral and water. As rainwater slowly makes its way to the ocean, it dissolves some of the rock material it passes through. Some of this dissolved material eventually crystallized and forms the mineral that make up chemical sedimentary rock. Header – dark yellow 24 points Arial Bold Body text – white 20 points Arial Bold, dark yellow highlights Bullets – dark yellow Copyright – white 12 points Arial Size: Height: 7.52" Width: 10.02" Scale: 70% Position on slide: Horizontal - 0" Vertical - 0"

35 Chapter 4 Composition of Sedimentary Rock, continued
Section 3 Sedimentary Rock Composition of Sedimentary Rock, continued Organic sedimentary rock is made up of the skeletons and shells of sea animals. These remains collect on the ocean floor and eventually become cemented together. Coal is a type of organic sedimentary rock that is formed when decomposed plant material is buried beneath sediment and is changed by increasing heat and pressure. Header – dark yellow 24 points Arial Bold Body text – white 20 points Arial Bold, dark yellow highlights Bullets – dark yellow Copyright – white 12 points Arial Size: Height: 7.52" Width: 10.02" Scale: 70% Position on slide: Horizontal - 0" Vertical - 0"

36 Sedimentary Rock Structures
Chapter 4 Section 3 Sedimentary Rock Sedimentary Rock Structures Many features indicate the way sedimentary rock is formed. The most important feature is stratification. Stratification is the process in which sedimentary rocks are arranged in layers. Strata differ from one another depending on the kind, size, and color of their sediment. Header – dark yellow 24 points Arial Bold Body text – white 20 points Arial Bold, dark yellow highlights Bullets – dark yellow Copyright – white 12 points Arial Size: Height: 7.52" Width: 10.02" Scale: 70% Position on slide: Horizontal - 0" Vertical - 0"

37 Sedimentary Rock Structures, continued
Chapter 4 Section 3 Sedimentary Rock Sedimentary Rock Structures, continued Sedimentary rocks sometimes record the motion of wind and water waves on lakes, oceans, rivers, and sand dunes in features called ripple marks. Structures called mud cracks form when fine-grained sediments at the bottom of a shallow body of water are exposed to the air and dry out. Even raindrop impressions can be preserved in fine-grained sediments, as small pits with raised rims. Header – dark yellow 24 points Arial Bold Body text – white 20 points Arial Bold, dark yellow highlights Bullets – dark yellow Copyright – white 12 points Arial Size: Height: 7.52" Width: 10.02" Scale: 70% Position on slide: Horizontal - 0" Vertical - 0"

38 Chapter 4 Section 4 Metamorphic Rock Bellringer Write a brief description of how cookies are made. How is the mixture of raw ingredients like sedimentary rock? Do the raw ingredients of a cookie look the same after they are done baking? Describe how cookie dough metamorphoses when it is baked in an oven. Header – dark yellow 24 points Arial Bold Body text – white 20 points Arial Bold, dark yellow highlights Bullets – dark yellow Copyright – white 12 points Arial Size: Height: 7.52" Width: 10.02" Scale: 70% Position on slide: Horizontal - 0" Vertical - 0"

39 Chapter 4 Section 4 Metamorphic Rock Objectives Describe two ways a rock can undergo metamorphism. Explain how the mineral composition of rocks changes as the rocks undergo metamorphism. Describe the difference between foliated and non-foliated metamorphic rock. Explain how metamorphic rock structures are related to deformation. Header – dark yellow 24 points Arial Bold Body text – white 20 points Arial Bold, dark yellow highlights Bullets – dark yellow Copyright – white 12 points Arial Size: Height: 7.52" Width: 10.02" Scale: 70% Position on slide: Horizontal - 0" Vertical - 0"

40 Origins of Metamorphic Rock
Chapter 4 Section 4 Metamorphic Rock Origins of Metamorphic Rock Metamorphic rocks are rocks in which the structure, texture, or composition of the rock have changed.All three types of rock can be changed by heat, pressure, or a combination of both. A rock’s texture or mineral composition can change when its surroundings change. If the temperature or pressure of the new environment is different from the one in which the rock formed, the rock will undergo metamorphism. Header – dark yellow 24 points Arial Bold Body text – white 20 points Arial Bold, dark yellow highlights Bullets – dark yellow Copyright – white 12 points Arial Size: Height: 7.52" Width: 10.02" Scale: 70% Position on slide: Horizontal - 0" Vertical - 0"

41 Origins of Metamorphic Rock, continued
Chapter 4 Section 4 Metamorphic Rock Origins of Metamorphic Rock, continued Contact Metamorphism When magma moves through the crust, the magma heats the surrounding rock and changes it. Some minerals in the surrounding rock are changed into other minerals by this increase in temperature. The greatest change occurs where magma comes into direct contact with the surrounding rock. Header – dark yellow 24 points Arial Bold Body text – white 20 points Arial Bold, dark yellow highlights Bullets – dark yellow Copyright – white 12 points Arial Size: Height: 7.52" Width: 10.02" Scale: 70% Position on slide: Horizontal - 0" Vertical - 0"

42 Origins of Metamorphic Rock, continued
Chapter 4 Section 4 Metamorphic Rock Origins of Metamorphic Rock, continued Regional metamorphism occurs when pressure builds up in rock that is buried deep below other rock formations, or when large pieces of the Earth’s curst collide with each other. The increased pressure and temperature causes rock to become deformed and chemically changed. Header – dark yellow 24 points Arial Bold Body text – white 20 points Arial Bold, dark yellow highlights Bullets – dark yellow Copyright – white 12 points Arial Size: Height: 7.52" Width: 10.02" Scale: 70% Position on slide: Horizontal - 0" Vertical - 0"

43 Chapter 4 Section 4 Metamorphic Rock
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44 Composition of Metamorphic Rock
Chapter 4 Section 4 Metamorphic Rock Composition of Metamorphic Rock As rocks undergo metamorphism, original minerals in a rock change into new minerals that are more stable within the new pressure and temperature conditions. Many of these new minerals form only in meta-morphic rock. These are known as index minerals, and are used to estimate the temperature, depth, and pressure at which a rock undergoes meta-morphism. Header – dark yellow 24 points Arial Bold Body text – white 20 points Arial Bold, dark yellow highlights Bullets – dark yellow Copyright – white 12 points Arial Size: Height: 7.52" Width: 10.02" Scale: 70% Position on slide: Horizontal - 0" Vertical - 0"

45 Texture of Metamorphic Rock
Chapter 4 Section 4 Metamorphic Rock Texture of Metamorphic Rock All metamorphic rock has one of two textures. Foliated Metamorphic Rock Nonfoliated Metamorphic Rock Header – dark yellow 24 points Arial Bold Body text – white 20 points Arial Bold, dark yellow highlights Bullets – dark yellow Copyright – white 12 points Arial Size: Height: 7.52" Width: 10.02" Scale: 70% Position on slide: Horizontal - 0" Vertical - 0"

46 Texture of Metamorphic Rock, continued
Chapter 4 Section 4 Metamorphic Rock Texture of Metamorphic Rock, continued Foliated Metamorphic Rock The texture of metamorphic rock in which the mineral grains are arranged in planes or band is called foliated. Foliated metamorphic rock usually contains aligned grains of flat minerals, such as biotite mica or chlorite Metamorphic rocks can become other metamorphic rocks if the environment changes again. Header – dark yellow 24 points Arial Bold Body text – white 20 points Arial Bold, dark yellow highlights Bullets – dark yellow Copyright – white 12 points Arial Size: Height: 7.52" Width: 10.02" Scale: 70% Position on slide: Horizontal - 0" Vertical - 0"

47 Texture of Metamorphic Rock, continued
Chapter 4 Section 4 Metamorphic Rock Texture of Metamorphic Rock, continued Nonfoliated Metamorphic Rock The texture of metamorphic rock in which the mineral grains are not arranged in planes or band is called nonfoliated. Nonfoliated metamorphic rocks are commonly made of one or only a few minerals. During metamorphism, crystals of these minerals may change in size or the mineral may change in composition in a process called recrystallization. Header – dark yellow 24 points Arial Bold Body text – white 20 points Arial Bold, dark yellow highlights Bullets – dark yellow Copyright – white 12 points Arial Size: Height: 7.52" Width: 10.02" Scale: 70% Position on slide: Horizontal - 0" Vertical - 0"

48 Metamorphic Rock Structures
Chapter 4 Section 4 Metamorphic Rock Metamorphic Rock Structures Metamorphic rock has features that indicates its history. These features are caused by deformation. Deformation is a change in the shape of a rock caused by a force placed on it. These forces may cause a rock to be squeezed or stretched. Folds, or bends, in metamorphic rock are structures that indicate a rock has been deformed. Header – dark yellow 24 points Arial Bold Body text – white 20 points Arial Bold, dark yellow highlights Bullets – dark yellow Copyright – white 12 points Arial Size: Height: 7.52" Width: 10.02" Scale: 70% Position on slide: Horizontal - 0" Vertical - 0"

49 Chapter 4 Rocks: Mineral Mixtures Concept Map Use the terms below to complete the concept map on the next slide. sedimentary clastic extrusive rocks metamorphic regional igneous intrusive Header – dark yellow 24 points Arial Bold Body text – white 20 points Arial Bold, dark yellow highlights Bullets – dark yellow Copyright – white 12 points Arial Size: Height: 7.52" Width: 10.02" Scale: 70% Position on slide: Horizontal - 0" Vertical - 0"

50 Chapter 4 Rocks: Mineral Mixtures
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51 Chapter 4 Rocks: Mineral Mixtures
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52 End of Chapter 4 Show Header – dark yellow 24 points Arial Bold
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53 Chapter 4 Standardized Test Preparation Reading Read each of the passages. Then, answer the questions that follow each passage.

54 Chapter 4 Standardized Test Preparation Passage 1 The texture and composition of a rock can provide good clues about how and where the rock formed. Scientists use both texture and composition to understand the origin and history of rocks. For example, marble is a rock that is made when limestone is metamorphosed. Only limestone contains the mineral—calcite—that can change into marble. Therefore, wherever scientists find marble, they know the sediment that created the original limestone was deposited in a warm ocean or lake environment.

55 Chapter 4 1. In the passage, what does the word origin mean?
Standardized Test Preparation 1. In the passage, what does the word origin mean? A size or appearance B age C location or surroundings D source or formation

56 Chapter 4 1. In the passage, what does the word origin mean?
Standardized Test Preparation 1. In the passage, what does the word origin mean? A size or appearance B age C location or surroundings D source or formation

57 Chapter 4 2. Based on the passage, what can the reader conclude?
Standardized Test Preparation 2. Based on the passage, what can the reader conclude? F Marble is a sedimentary rock. G Limestone is created by sediments deposited in warm ocean or lake environments. H Marble is a rock that is made when sandstone has undergone metamorphism. I In identifying a rock, the texture of a rock is more important than the composition of the rock.

58 Chapter 4 2. Based on the passage, what can the reader conclude?
Standardized Test Preparation 2. Based on the passage, what can the reader conclude? F Marble is a sedimentary rock. G Limestone is created by sediments deposited in warm ocean or lake environments. H Marble is a rock that is made when sandstone has undergone metamorphism. I In identifying a rock, the texture of a rock is more important than the composition of the rock.

59 Chapter 4 3. What is the main idea of the passage?
Standardized Test Preparation 3. What is the main idea of the passage? A Scientists believe marble is the most important rock type to study. B Scientists study the composition and texture of a rock to determine how the rock formed and what happened after it formed. C Some sediments are deposited in warm oceans and lakes. D When limestone undergoes metamorphism, it creates marble.

60 Chapter 4 3. What is the main idea of the passage?
Standardized Test Preparation 3. What is the main idea of the passage? A Scientists believe marble is the most important rock type to study. B Scientists study the composition and texture of a rock to determine how the rock formed and what happened after it formed. C Some sediments are deposited in warm oceans and lakes. D When limestone undergoes metamorphism, it creates marble.

61 Chapter 4 Standardized Test Preparation Passage 2 Fulgurites are a rare type of natural glass found in areas that have quartz-rich sediments, such as beaches and deserts. A tubular fulgurite forms when a lightning bolt strikes material such as sand and melts the quartz into a liquid. The liquid quartz cools and solidifies quickly, and a thin, glassy tube is left behind. Fulgurites usually have a rough outer surface and a smooth inner surface. Continued on the next slide

62 Chapter 4 Standardized Test Preparation Passage 2, continued Underground, a fulgurite may be shaped like the roots of a tree. The fulgurite branches out with many arms that trace the zigzag path of the lightning bolt. Some fulgurites are as short as your little finger, but others stretch 20 m into the ground.

63 Chapter 4 1. In the passage, what does the word tubular mean?
Standardized Test Preparation 1. In the passage, what does the word tubular mean? A flat and sharp B round and long C funnel shaped D pyramid shaped

64 Chapter 4 1. In the passage, what does the word tubular mean?
Standardized Test Preparation 1. In the passage, what does the word tubular mean? A flat and sharp B round and long C funnel shaped D pyramid shaped

65 Chapter 4 Standardized Test Preparation 2. From the information in the passage, what can the reader conclude? F Fulgurites are formed above ground. G Sand contains a large amount of quartz. H Fulgurites are most often very small. I Fulgurites are easy to find in sandy places.

66 Chapter 4 Standardized Test Preparation 2. From the information in the passage, what can the reader conclude? F Fulgurites are formed above ground. G Sand contains a large amount of quartz. H Fulgurites are most often very small. I Fulgurites are easy to find in sandy places.

67 Chapter 4 Standardized Test Preparation 3. Which of the following statements best describes a fulgurite? A Fulgurites are frozen lightning bolts. B Fulgurites are rootlike rocks. C Fulgurites are glassy tubes found in deserts. D Fulgurites are natural glass tubes formed by lightning bolts.

68 Chapter 4 Standardized Test Preparation 3. Which of the following statements best describes a fulgurite? A Fulgurites are frozen lightning bolts. B Fulgurites are rootlike rocks. C Fulgurites are glassy tubes found in deserts. D Fulgurites are natural glass tubes formed by lightning bolts.

69 Interpreting Graphics
Chapter 4 Standardized Test Preparation Interpreting Graphics Use the diagram below to answer the questions that follow.

70 Chapter 4 Standardized Test Preparation 1. According to the rock cycle diagram, which of the following statements is true? A Only sedimentary rock gets weathered and eroded. B Sedimentary rocks are made from metamorphic, igneous, and sedimentary rock fragments and minerals. C Heat and pressure create igneous rocks. D Metamorphic rocks are created by melting and cooling.

71 Chapter 4 Standardized Test Preparation 1. According to the rock cycle diagram, which of the following statements is true? A Only sedimentary rock gets weathered and eroded. B Sedimentary rocks are made from metamorphic, igneous, and sedimentary rock fragments and minerals. C Heat and pressure create igneous rocks. D Metamorphic rocks are created by melting and cooling.

72 Chapter 4 Standardized Test Preparation 2. A rock exists at the surface of the Earth. What would be the next step in the rock cycle? F cooling G weathering H melting I metamorphism

73 Chapter 4 Standardized Test Preparation 2. A rock exists at the surface of the Earth. What would be the next step in the rock cycle? F cooling G weathering H melting I metamorphism

74 Chapter 4 Standardized Test Preparation 3. Which of the following processes brings rocks to Earth’s surface, where they can be eroded? A burial B deposition C uplift D weathering

75 Chapter 4 Standardized Test Preparation 3. Which of the following processes brings rocks to Earth’s surface, where they can be eroded? A burial B deposition C uplift D weathering

76 Chapter 4 Standardized Test Preparation

77 Chapter 4 Standardized Test Preparation 4. Which of the following is the best summary of the rock cycle? F Each type of rock gets melted. Then the magma turns into igneous, sedimentary, and metamorphic rock. G Magma cools to form igneous rock. Then, the igneous rock becomes sedimentary rock. Sedimentary rock is heated and forms metamorphic rock. Metamorphic rock melts to form magma. Choices continued on next slide

78 Chapter 4 Continued from previous slide
Standardized Test Preparation Continued from previous slide H All three rock types weather to create sedimentary rock. All three rock types melt to form magma. Magma forms igneous rock. All three types of rock form metamorphic rock because of heat and pressure. I Igneous rock is weathered to create sedimentary rock. Sedimentary rock is melted to form igneous rock. Metamorphic rock is weathered to form igneous rock.

79 Chapter 4 Standardized Test Preparation 4. Which of the following is the best summary of the rock cycle? F Each type of rock gets melted. Then the magma turns into igneous, sedimentary, and metamorphic rock. G Magma cools to form igneous rock. Then, the igneous rock becomes sedimentary rock. Sedimentary rock is heated and forms metamorphic rock. Metamorphic rock melts to form magma. Choices continued on next slide

80 Chapter 4 Continued from previous slide
Standardized Test Preparation Continued from previous slide H All three rock types weather to create sedimentary rock. All three rock types melt to form magma. Magma forms igneous rock. All three types of rock form metamorphic rock because of heat and pressure. I Igneous rock is weathered to create sedimentary rock. Sedimentary rock is melted to form igneous rock. Metamorphic rock is weathered to form igneous rock.

81 Chapter 4 Math Read each question, and choose the best answer.
Standardized Test Preparation Math Read each question, and choose the best answer.

82 Chapter 4 Standardized Test Preparation 1. Eric has 25 rocks he has collected as a science project for class. Nine rocks are sedimentary, 10 are igneous, and 6 are metamorphic. If Eric chooses a rock at random, what is the probability that he will choose an igneous rock? A 1/2 B 2/5 C 3/8 D 1/15

83 Chapter 4 Standardized Test Preparation 1. Eric has 25 rocks he has collected as a science project for class. Nine rocks are sedimentary, 10 are igneous, and 6 are metamorphic. If Eric chooses a rock at random, what is the probability that he will choose an igneous rock? A 1/2 B 2/5 C 3/8 D 1/15

84 Chapter 4 Standardized Test Preparation 2. At a mineral and fossil show, Elizabeth bought two quartz crystals that cost $2.00 each and four trilobite fossils that cost $3.50 each. Which equation can be used to describe c, the total cost of her purchase? F c  (2  4)  (2.00  3.50) G c  (2  2.00)  (4  3.50) H c  (4  2.00)  (2  3.50) I c  (2  2.00)  (4  3.50)

85 Chapter 4 Standardized Test Preparation 2. At a mineral and fossil show, Elizabeth bought two quartz crystals that cost $2.00 each and four trilobite fossils that cost $3.50 each. Which equation can be used to describe c, the total cost of her purchase? F c  (2  4)  (2.00  3.50) G c  (2  2.00)  (4  3.50) H c  (4  2.00)  (2  3.50) I c  (2  2.00)  (4  3.50)

86 Chapter 4 Section 3 Sedimentary Rock
Header – dark yellow 24 points Arial Bold Body text – white 20 points Arial Bold, dark yellow highlights Bullets – dark yellow Copyright – white 12 points Arial Size: Height: 7.52" Width: 10.02" Scale: 70% Position on slide: Horizontal - 0" Vertical - 0"

87 Chapter 4 Standardized Test Preparation

88 There is no CNN video correlated to this chapter.
The World of Earth Science There is no CNN video correlated to this chapter. Check the One-Stop Planner for a complete listing of CNN videos.


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