Chapter 8 Resource: Earthquakes and Volcanoes
Transcription
Chapter 8 Resource: Earthquakes and Volcanoes
Glencoe Science Chapter Resources Earthquakes and Volcanoes Includes: Reproducible Student Pages ASSESSMENT TRANSPARENCY ACTIVITIES ✔ Chapter Tests ✔ Section Focus Transparency Activities ✔ Chapter Review ✔ Teaching Transparency Activity HANDS-ON ACTIVITIES ✔ Assessment Transparency Activity ✔ Lab Worksheets for each Student Edition Activity Teacher Support and Planning ✔ Laboratory Activities ✔ Content Outline for Teaching ✔ Foldables–Reading and Study Skills activity sheet ✔ Spanish Resources ✔ Teacher Guide and Answers MEETING INDIVIDUAL NEEDS ✔ Directed Reading for Content Mastery ✔ Directed Reading for Content Mastery in Spanish ✔ Reinforcement ✔ Enrichment ✔ Note-taking Worksheets Glencoe Science Photo Credits Section Focus Transparency 1: Ken M. Johns/Photo Researchers Section Focus Transparency 2: Prof. Sigurdur Thorarinsson/Univ. of Iceland Section Focus Transparency 3: Mehau Kulyk/Science Photo Library/Photo Researchers Copyright © by The McGraw-Hill Companies, Inc. All rights reserved. Permission is granted to reproduce the material contained herein on the condition that such material be reproduced only for classroom use; be provided to students, teachers, and families without charge; and be used solely in conjunction with the Earthquakes and Volcanoes program. Any other reproduction, for use or sale, is prohibited without prior written permission of the publisher. Send all inquiries to: Glencoe/McGraw-Hill 8787 Orion Place Columbus, OH 43240-4027 ISBN 0-07-867148-5 Printed in the United States of America. 1 2 3 4 5 6 7 8 9 10 071 09 08 07 06 05 04 Reproducible Student Pages Reproducible Student Pages ■ Hands-On Activities MiniLAB: Observing Deformation . . . . . . . . . . . . . . . . . . . . . . . . . . . . 3 MiniLAB: Try at Home Modeling an Eruption . . . . . . . . . . . . . . . . . . 4 Lab: Disruptive Eruptions . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 5 Lab: Seismic Waves . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 7 Laboratory Activity 1: Wave Detecting . . . . . . . . . . . . . . . . . . . . . . . . . 9 Laboratory Activity 2: Volcanic Eruptions . . . . . . . . . . . . . . . . . . . . . 11 Foldables: Reading and Study Skills. . . . . . . . . . . . . . . . . . . . . . . . . . 15 ■ Meeting Individual Needs Extension and Intervention Directed Reading for Content Mastery . . . . . . . . . . . . . . . . . . . . . . . 17 Directed Reading for Content Mastery in Spanish . . . . . . . . . . . . . . 21 Reinforcement . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 25 Enrichment. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 28 Note-taking Worksheet . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 31 ■ Assessment Chapter Review . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 35 Chapter Test . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 37 ■ Transparency Activities Section Focus Transparency Activities . . . . . . . . . . . . . . . . . . . . . . . . 42 Teaching Transparency Activity . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 45 Assessment Transparency Activity . . . . . . . . . . . . . . . . . . . . . . . . . . . 47 Earthquakes and Volcanoes 1 Hands-On Activities Hands-On Activities 2 Earthquakes and Volcanoes Date Class Hands-On Activities Name Observing Deformation WARNING: Do not taste or eat any lab materials. Wash hands when finished. Procedure 1. Remove the wrapper from three bars of taffy. 2. Hold a bar of taffy lengthwise between your hands and gently push on it from opposite directions. 3. Hold another bar of taffy and pull it in opposite directions. Analysis 1. Which of the procedures that you performed on the taffy involved applying tension? Which involved applying compression? Copyright © Glencoe/McGraw-Hill, a division of the McGraw-Hill Companies, Inc. 2. Infer how to apply a shear stress to the third bar of taffy. Earthquakes and Volcanoes 3 Name Date Class Procedure 1. Place red-colored gelatin into a self-sealing plastic bag until the bag is half full. 2. Seal the bag and press the gelatin to the bottom of the bag. 3. Put a hole in the bottom of the bag with a pin. Analysis 1. What parts of a volcano do the gelatin, the plastic bag, and the hole represent? 2. What force in nature did you mimic as you moved the gelatin to the bottom of the bag? 3. What factors in nature cause this force to increase and lead to an eruption? Copyright © Glencoe/McGraw-Hill, a division of the McGraw-Hill Companies, Inc. Hands-On Activities Modeling an Eruption 4 Earthquakes and Volcanoes Name Date Class Hands-On Activities Disruptive Eruptions Lab Preview Directions: Answer these questions before you begin the Lab. 1. Why are safety goggles especially important when doing this lab? 2. Based on what you know about the activity from question 1, what can you expect to happen that might resemble a cinder-cone volcanic eruption? Explain. Copyright © Glencoe/McGraw-Hill, a division of the McGraw-Hill Companies, Inc. A volcano’s structure can influence how it erupts. Some volcanoes have only one central vent, while others have numerous fissures that allow lava to escape. Materials in magma influence its viscosity, or how it flows. If magma is a thin fluid—not viscous—gases can escape easily. But if magma is thick—viscous— gases cannot escape as easily. This builds up pressure within a volcano. Real-World Question Procedure What determines the explosiveness of a volcanic eruption? 1. Watch your teacher demonstrate this lab before attempting to do it yourself. 2. Add 15 mL of vinegar to a film canister. 3. Place 1 teaspoon of baking soda in the film canister’s lid, using it as a type of plate. 4. Place the lid on top of the film canister, but do not cap it. The baking soda will fall into the vinegar. Move a safe distance away. Record your observations in the Data and Observations section. 5. Clean out your film canister, and repeat the lab, but this time cap the canister quickly and tightly. Record your observations. Materials plastic film canisters baking soda (NaHCO3) vinegar (CH3COOH) teaspoon 50-mL graduated cylinder Goals ■ ■ Infer how a volcano’s opening contributes to how explosive an eruption might be. Hypothesize how the viscosity of magma can influence an eruption. Safety Precautions WARNING: This lab should be done outdoors. Goggles must be worn at all times. The caps of the film canisters fly off due to the chemical reaction that occurs inside them. Never put anything in your mouth while doing the experiment. Earthquakes and Volcanoes 5 Name Date Class (continued) Table 1 Trial Observations 1 2 Conclude and Apply 1. Identify Which of the two labs models a more explosive eruption? 2. Explain Was the pressure greater inside the canister during the first or second lab? Why? 3. Explain What do the bubbles have to do with the explosion? How do they influence the pressure in the container? 4. Infer If the vinegar were a more viscous substance, how would the eruption be affected? Communicating Your Data Research three volcanic eruptions that have occurred in the past five years. Compare each eruption to one of the eruption styles you modeled in this lab. Communicate to your class what you learn. 6 Earthquakes and Volcanoes Copyright © Glencoe/McGraw-Hill, a division of the McGraw-Hill Companies, Inc. Hands-On Activities Data and Observations Name Date Class Hands-On Activities Seismic Waves Lab Preview Directions: Answer these questions before you begin the Lab. 1. What about this lab makes wearing goggles a good idea? 2. Predict which type of wave will show the most motion in the spring. Explain. If you and one of your friends hold a long piece of rope between you and move one end of the rope back and forth, you can send a wave through the length of the rope. Hold a ruler at the edge of a table securely with one end of it sticking out from the table’s edge. If you bend the ruler slightly and then release it, what do you experience? How does what you see in the rope and what you feel in the ruler relate to seismic waves? Real-World Question Copyright © Glencoe/McGraw-Hill, a division of the McGraw-Hill Companies, Inc. How do seismic waves differ? Materials coiled spring toy yarn or string metric ruler Goals ■ ■ Demonstrate the motion of primary, secondary, and surface waves. Identify how parts of the spring move in each of the waves. Safety Precautions Procedure 1. Use the table in the Data and Observations section to record your observations. 2. Tie a small piece of yarn or string to every tenth coil of the spring. 3. Place the spring on a smooth, flat surface. Stretch it so it is about 2 m long (1 m for shorter springs). 4. Hold your end of the spring firmly. Make a wave by having your partner snap the spring from side to side quickly. 5. Record your observations and draw the wave you and your partner made in the data table. 6. Have your lab partner hold his or her end of the spring firmly. Make a wave by quickly pushing your end of the spring toward your partner and bringing it back to its original position. 7. Record your observations of the wave and of the yarn or string and draw the wave in the data table. 8. Have your lab partner hold his or her end of the spring firmly. Move the spring off of the table. Gently move your end of the spring side to side while at the same time moving it in a rolling motion, first up and away and then down and toward your partner. 9. Record your observations and draw the wave in the data table. Earthquakes and Volcanoes 7 Name Date Class (continued) Table 1 Comparing Seismic Waves Observation of Wave Observation of Yarn or String Drawing Wave Type Conclude and Apply 1. Based on your observations, determine which of the waves that you and your partner have generated demonstrates a primary, or pressure, wave. Record in your data table and explain why you chose the wave you did. 2. Do the same for the secondary, or shear wave, and for the surface wave. Explain why you chose the wave you did. 3. Explain Based on your observations of wave motion, which of the waves that you and your partner generated probably would cause the most damage during an earthquake? 4. Observe What was the purpose of the yarn or string? 5. Compare and Contrast the motion of the yarn or string when primary and secondary waves travel through the spring. Which of these waves is a compression wave? Explain your answer. 6. Compare and Contrast Which wave most closely resembled wave motion in a body of water? How was it different? Explain. Communicating Your Data Compare your conclusions with those of other students in your class. For more help, refer to the Science Skill Handbook. 8 Earthquakes and Volcanoes Copyright © Glencoe/McGraw-Hill, a division of the McGraw-Hill Companies, Inc. Hands-On Activities Data and Observations Date 1 Laboratory Activity Class Wave Detecting Today, scientists use seismographs to observe and record seismic waves. Before the nineteenth century, however, scientists used other types of instruments to study earthquakes. These instruments did not record seismic waves. Instead, they indicated the magnitude or direction of an earthquake in a general way. In the 1600s in Italy, for example, scientists used a device that contained water to observe seismic waves. The amount of water spilling out during an earthquake indicated the amount of shaking. In this lab, you will make a simple earthquake-detecting device and determine how it is affected by seismic waves. Strategy You will model and observe the effects of seismic waves. You will infer how the energy released by an earthquake affects the amplitude, or height, of seismic waves. Materials baking pan large ceramic or stainless steel bowl pitcher of tap water dropper meterstick textbook paper towels Copyright © Glencoe/McGraw-Hill, a division of the McGraw-Hill Companies, Inc. Procedure 1. Work with a partner. Place the baking pan on a flat surface such as a desk or counter. Set the bowl inside the pan. 2. Pour water into the bowl from the pitcher. Fill the bowl to within 1 to 2 mm of the rim. 3. Using the dropper add water to the bowl until the surface of the water arches above the rim (Figure 1). This is your earthquake detector. 4. Model an earthquake by having a partner drop a textbook near the detector from a height of 2 cm. Observe what happens to the water in the bowl. Do waves appear? Does water spill over? Record your observation in the Data and Observations section. Add more water to the bowl with the dropper if any spills out. Then repeat this step, switching roles with your partner. 5. Repeat step 4 several more times. Each time, you should increase the height at which you drop the book by several centimeters. 6. If any water spills outside the baking pan, be sure to wipe it up with the paper towels. Figure 1 Water Earthquakes and Volcanoes 9 Hands-On Activities Name Name Date Class Laboratory Activity 1 (continued) Table 1 Trial Height from Which Book Is Dropped (cm) Observations of Earthquake Detector 1 2 3 4 Questions and Conclusions 1. How are the waves produced by the book landing on the table similar to seismic waves? 2. Could you tell that the waves produced by some of your model earthquakes had greater amplitude than others? Explain. 3. How did you increase the magnitude of your model earthquake? How did increasing the magnitude of the earthquake affect the amplitude of the waves in your detector? 4. How could you use two earthquake detectors to model how the amplitude of seismic waves is affected by the distance the waves travel? Explain. Strategy Check Can you model and observe the effects of seismic waves? Can you infer how the energy released by an earthquake affects the amplitude of seismic waves? 10 Earthquakes and Volcanoes Copyright © Glencoe/McGraw-Hill, a division of the McGraw-Hill Companies, Inc. Hands-On Activities Data and Observations Date 2 Laboratory Activity Class Volcanic Eruptions Some volcanic eruptions consist of violent explosions of gases and tephra, while others involve a relatively quiet flow of lava around a vent. The type of eruption that occurs depends on both the composition of the magma and the amount of gas trapped in it. Thick magma that is rich in silica tends to trap steam and other gases. The more gas in the magma, the greater the pressure that builds up in the volcano. The tremendous pressure that builds in silica-rich magma is released when the volcano erupts explosively. By contrast, magma that contains less silica tends to be less explosive and flow more easily. This type of magma is rich in iron and magnesium and traps smaller amounts of gas. It produces basaltic lava that flows from a volcano in broad, flat layers. In this lab, you will model both basaltic lava flows and explosive eruptions. Strategy You will model and observe how the buildup of pressure in a volcano can lead to an explosive eruption. You will determine how layers of basaltic lava accumulate. Copyright © Glencoe/McGraw-Hill, a division of the McGraw-Hill Companies, Inc. Materials newspaper old paintbrushes (3) balloons (9) sponge empty coffee can marker measuring cup meterstick plaster of paris scissors water piece of thick cardboard (approximately 50 cm ✕ 50 cm) 1 lb. plastic margarine tubs (2) textbooks red, blue, and green food coloring small tubes of toothpaste in different colors wooden paint stirrers (3) (white, green, striped) WARNING: Never put anything you use in a laboratory experiment into your mouth. Procedure Part A—Modeling Explosive Eruptions 1. Work in a group of five or six students. Put on your apron and goggles, and cover your work area with sheets of newspaper. 2. Inflate six of the balloons. Put less air in some of the balloons than in others. You’ll need two small balloons, two medium, and two large. Leave the remaining balloons uninflated. 3. In the coffee can, combine 1 L of plaster mix with 2 L of water. Stir the mixture with a wooden stirrer until the mixture is smooth. You should use a bit more water than the directions on the box suggest. Thinner plaster will be easier to work with. 4. Pour about one-third of the mixture into each of the plastic tubs, leaving the final third in the can. Add several drops of food coloring to each container, and stir. You should end up with three colors of plaster: red, green, and blue. Do this step as quickly as possible since the plaster mix will begin to harden. 5. Using paintbrushes, coat the entire surface of each of the inflated balloons with a thin layer of plaster. Paint the two small balloons blue, the medium balloons green, and the large balloons red. Using any color, paint a band around the center of each of the empty balloons, leaving the ends unpainted (Figure 1). Set the balloons on sheets of newspaper to dry. If you spill any plaster while you are painting, wipe it up with a damp sponge. Earthquakes and Volcanoes 11 Hands-On Activities Name Name Date Class Laboratory Activity 2 (continued) Inflated 6. While the plaster is drying, skip to Part B of the procedure. 7. To model the buildup of pressure inside magma, try to inflate the empty balloons. What do you observe? Record your observation in the Data and Observations section. 8. Spread newspapers on an open area of the floor. With the marker, draw a large X on the center of the paper. To model an explosive eruption, take one of the small, blue balloons and place it on the X. Pop the balloon by stepping on it. Leave the pieces of the plaster in place and pop the second small balloon in the same way. WARNING: Wear your safety goggles throughout this experiment. 9. With the meterstick, measure the distance from the X to the piece of plaster that landed the farthest from it. This distance represents the radius of the debris field. Record this measurement in Table 1 the Data and Observations section. 10. Repeat step 8 using the medium balloons. Measure and record the distance from the X to the piece of green plaster that landed farthest from it. 11. Repeat step 8 using the large balloons. Measure and record the distance from the X to the piece of red plaster that landed farthest from it. 12 Earthquakes and Volcanoes Uninflated Part B—Modeling Basaltic Lava Flows 1. Use the scissors to poke a hole near the center of the piece of cardboard. Widen the hole until it is just large enough for the cap of a tube of toothpaste to fit through it. 2. Make two stacks of books and place the cardboard on top of them so that the hole is suspended about 30 cm above your work surface (Figure 2). 3. Remove the cap from one of the tubes of toothpaste. Stick the cap end of the tube through the hole so that the tube is upright and just the mouth is sticking out the top of the cardboard. Model a basaltic lava flow by slowly squeezing out the contents of the tube. Figure 2 4. Measure the height and diameter of your “lava” flow and record your measurements in Table 2 in the Data and Observations section. 5. To model additional eruptions, repeat steps 3 and 4 using the other two tubes of toothpaste to add to your “lava” flow. 6. Return to step 7 of Part A. Copyright © Glencoe/McGraw-Hill, a division of the McGraw-Hill Companies, Inc. Hands-On Activities Figure 1 Name Date Class Hands-On Activities Laboratory Activity 2 (continued) Data and Observations What did you observe when you inflated the plaster-coated balloons? Table 1 Balloon Size Radius of Debris Field (cm) Small 1 Small 2 Medium 1 Medium 2 Large 1 Large 2 Table 2 Eruption Diameter (cm) Height (cm) 1 2 Copyright © Glencoe/McGraw-Hill, a division of the McGraw-Hill Companies, Inc. 3 Questions and Conclusions 1. The air in your balloons modeled the gases that build up in silica-rich magma. Which balloons (small, medium, or large) modeled magma under the greatest pressure? Explain. 2. What do your results from Part A tell you about the relationship between pressure and the force of an explosive volcanic eruption? 3. What type or types of volcano did you model in Part A? Explain your answer. Earthquakes and Volcanoes 13 Name Date Class Laboratory Activity 2 (continued) 5. a. In Part B, how did the layers of toothpaste accumulate? Did the second and third layers form on top of the first layer or beneath it? b. What does this result tell you about the age of the top layer of basaltic lava on a volcano compared with lower layers? 6. How did the height of the volcano you modeled in Part B compare with its width? What type of volcano has this shape? 7. How did the two types of eruptions you modeled differ from one another? How were they alike? Strategy Check Can you model an explosive eruption due to the buildup of gas pressure? Can you describe how layers of basaltic lava accumulate? 14 Earthquakes and Volcanoes Copyright © Glencoe/McGraw-Hill, a division of the McGraw-Hill Companies, Inc. Hands-On Activities 4. What were you modeling when you inflated the plaster-coated balloons in step 7 of Part A? Name Date Class Hands-On Activities Earthquakes and Volcanoes Directions: Use this page to label your Foldable at the beginning of the chapter. Volcanoes Earthquakes Both a cone-shaped mountain or hill that spews magma, solids, and gas Copyright © Glencoe/McGraw-Hill, a division of the McGraw-Hill Companies, Inc. can have pyroclastic flows or tremendous amounts of ash intensity measured on a seismograph rocks inside Earth pass their elastic limit, break, and have elastic rebound Earthquakes and Volcanoes 15 Meeting Individual Needs Meeting Individual Needs 16 Earthquakes and Volcanoes Name Date Directed Reading for Content Mastery Class Overview Earthquakes and Volcanoes Directions: Complete the concept map using the terms in the list below. elastic limit magma elastic rebound lava tectonic plate earthquakes volcanoes occur when rocks within Earth’s crust are stressed past their are related to occur when rising 3. ___________ boundaries Copyright © Glencoe/McGraw-Hill, a division of the McGraw-Hill Companies, Inc. 1. 4. erupts through a vent onto Earth’s surface as break and undergo 2. 5. Directions: Use the following terms to fill in the blanks in the paragraph below. magma divergent mantle hot spots tectonic energy Volcanoes often occur at 6. _______________ and convergent plate boundaries. They also occur at 7. _______________ where large, rising bodies of 8. _______________ can force their way through Earth’s 9. _______________ and crust. Like volcanoes, earthquakes also occur at 10. _______________ plate boundaries. They are caused by the 11. _______________ generated by the plates’ movement. Earthquakes and Volcanoes 17 Meeting Individual Needs Locations of many Name Date Directed Reading for Content Mastery Section 1 ■ Class Earthquakes Directions: Write the term that matches each description below on the spaces provided. The vertical, boxed letters should spell the word that answers question 10. 1 V 2 M 3 Meeting Individual Needs 4 M N 5 H Q 6 7 L R 9 1. 2. 3. 4. 5. 6. 7. 8. 9. G type of fault that may form when rocks are compressed the measurement that describes how much energy an earthquake releases the fastest type of seismic wave on the Modified Mercalli scale, a measure of the amount of structural and geologic damage an earthquake causes kind of force that causes a strike-slip fault to form type of seismic wave that causes the most damage type of fault that may form when rocks are pulled apart type of fault that may form when rocks slide past one another in opposite directions instrument used to record seismic waves 10. what can happen when rocks pass their elastic limit, break, and snap back in elastic rebound? 18 Earthquakes and Volcanoes Copyright © Glencoe/McGraw-Hill, a division of the McGraw-Hill Companies, Inc. 8 F Name Date Directed Reading for Content Mastery Section 2 Section 3 Class ■ ■ Volcanoes Earthquakes, Volcanoes, and Plate Tectonics Directions: Complete the following sentences using the terms listed below. hot spot shield composite tephra 1. ____________________ volcanoes such as the Soufriere Hills volcano often form along subduction zones. 2. Bits of rock or solidified lava that fall from the air after a volcanic eruption are called ____________________. 3. The type of volcanic eruption depends on the amount of gases and the composition of the ____________________. Copyright © Glencoe/McGraw-Hill, a division of the McGraw-Hill Companies, Inc. 4. The largest volcanoes are ____________________ volcanoes, which produce basaltic lava. 5. ____________________ eruptions occur when very fluid magma oozes from cracks in Earth’s surface. 6. The Hawaiian Islands did not form at a boundary of tectonic plates, like most volcanoes, but over a ____________________. Directions: Study the following diagrams. Then label the plate boundaries as divergent, transform, or convergent. A 7. A. ____________________ B C C. ____________________ B. ____________________ Earthquakes and Volcanoes 19 Meeting Individual Needs magma fissure Name Date Directed Reading for Content Mastery Class Key Terms Earthquakes and Volcanoes Directions: Write the correct term from the list in the space provided next to each definition below. fault hot spot shield volcano epicenter rift tsunami seismic safe lava seismograph cinder cone volcano seismic wave focus composite volcano magnitude Meeting Individual Needs 1. broad volcano with gently sloping sides 2. long crack that forms as two tectonic plates move apart 3. magma that reaches Earth’s surface 4. point inside Earth where earthquake movement first occurs 5. small volcano formed from tephra 6. the surface of a break in a section of rock 8. steep-sided volcano formed from layers of lava and tephra 9. point on Earth’s surface directly above the focus of an earthquake 10. rising magma that may force its way through Earth’s crust, not at a plate boundary 11. type of building structure that can withstand earthquake vibrations 12. waves generated by an earthquake and measured using the Richter scale 13. the instrument scientists use to record the measurements in question 12 14. the height of the lines recorded on a seismograph, or the amount of energy released by an earthquake 20 Earthquakes and Volcanoes Copyright © Glencoe/McGraw-Hill, a division of the McGraw-Hill Companies, Inc. 7. powerful sea wave caused by an earthquake Nombre Fecha Lectura dirigida para Dominio del contenido Clase Sinopsis Terremotos y volcanes Instrucciones: Completa el mapa de conceptos con los siguientes términos. límite elástico magma rebote elástico lava placas tectónicas terremotos volcanes está relacionada con ocurre cuando las rocas dentro de la corteza terrestre son presionadas más allá de su ocurre cuando al elevarse el(la) los límites entre 3. ___________ Copyright © Glencoe/McGraw-Hill, a division of the McGraw-Hill Companies, Inc. 1. 4. hace erupción a través de una chimenea hacia la superficie terrestre como y se quiebran y experimentan 2. 5. Instrucciones: Usa los siguientes términos para llenar los espacios en blanco. magma divergentes manto focos cálidos tectónicas energía Los volcanes ocurren con frecuencia en los límites entre placas 6. _______________ y convergentes. También ocurren en 7. _______________, en donde grandes masas de 8. _______________ que se elevan pueden forzar su paso a través del(la) 9. _______________ y la corteza terrestre. Como los volcanes, los terremotos también ocurren en los límites entre las placas 10. _______________. Los terremotos son causados por el(la) 11. _______________ generada por el movimiento de las placas. Terremotos y volcanes 21 Satisface las necesidades individuales La ubicación de muchos Nombre Fecha Sección 1 Lectura dirigida para Clase ■ Los terremotos Dominio del contenido Instrucciones: Llena el crucigrama con el término que describe cada clave. Las letras en las cajas oscuras verticales deben darte la respuesta para la pregunta 10. 2 C I Z Satisface las necesidades individuales M A G N I T U D L L A M I E N T P R I M A R I A S U P E R F I C I E N V E R S A A A N O R M A L A F O A 3 4 D E 5 I 6 7 S I S M O G R 8 9 1. 2. 3. 4. 5. 6. 7. 8. T R A N E N O I N T S I D A S F O R M A N T E D medida que describe la energía liberada por un terremoto tipo de fuerza que forma las fallas transformantes tipo más rápido de onda sísmica tipo de onda sísmica que causa los peores daños tipo de falla que puede formarse cuando las rocas son comprimidas tipo de falla que puede formarse cuando las rocas son forzadas a separarse instrumento que se usa para registrar las ondas sísmicas en la escala modificada de Mercalli, medida de la cantidad de daño estructural y geológico causado por un terremoto 9. tipo de falla que puede formarse cuando las rocas se deslizan una al lado de otra en direcciones opuestas 10. Lo que puede suceder cuando las rocas sobrepasan su límite elástico, se quiebran y vuelven a su sitio debido al rebote elástico. 22 Terremotos y volcanes Copyright © Glencoe/McGraw-Hill, a division of the McGraw-Hill Companies, Inc. 1 Nombre Fecha Lectura dirigida para Dominio del contenido Clase Sección 2 Sección 3 ■ ■ Los volcanes Terremotos, volcanes y tectónica de placas Instrucciones: Completa las oraciones usando los siguientes términos. foco cálido de escudo compuestos tefrita 1. Los volcanes ____________________, como las Colinas Soufriere, se forman frecuentemente sobre zonas de subducción. 2. Los trozos de roca o lava solidificada que caen por el aire después de una erupción volcánica se llaman ____________________. 3. El tipo de erupción volcánica depende de la cantidad de gases y de la composición del(la) ____________________. 4. Los volcanes más grandes son volcanes ____________________, los cuales producen lava basáltica. Copyright © Glencoe/McGraw-Hill, a division of the McGraw-Hill Companies, Inc. 5. Las erupciones de ____________________ ocurren cuando el magma muy líquido se escurre entre las grietas de la superficie terrestre. 6. Las islas de Hawai no se formaron sobre un límite de placas tectónicas, como casi todos los volcanes, sino sobre un(a) ____________________. Instrucciones: Estudia los diagramas. Luego rotula cada uno usando el término correcto. divergente A 7. A. ____________________ transformante convergente B C C. ____________________ B. ____________________ Terremotos y volcanes 23 Satisface las necesidades individuales magma fisuras Nombre Fecha Lectura dirigida para Dominio del contenido Clase Términos claves Terremotos y volcanes Instrucciones: Para cada definición, escoge el término correcto y escríbelo en el espacio dado, a la izquierda de su definición. onda sísmica foco volcán compuesto magnitud 1. volcán ancho con pendientes suaves 2. grieta larga que se forma cuando dos placas tectónicas se separan 3. magma que llega a la superficie de la Tierra 4. punto dentro de la Tierra en donde ocurre por primera vez un movimiento sísmico 5. volcán pequeño formado por tefrita 6. superficie de una ruptura en una sección de roca 7. ola marina poderosa causada por un terremoto 8. volcán de pendientes abruptas formado por lava y tefrita 9. punto en la superficie de la Tierra directamente sobre el foco de un terremoto 10. magma que se levanta y fuerza su paso a través de la corteza terrestre, en lugar de pasar por un límite entre placas 11. tipo de construcción que puede soportar las vibraciones de los terremotos 12. ondas generadas por un terremoto y que se miden usando la escala Richter 13. instrumento que los científicos usan para registrar las medidas de la pregunta 12 14. altura de las líneas que registra un sismógrafo, o cantidad de energía liberada por un terremoto 24 Terremotos y volcanes Copyright © Glencoe/McGraw-Hill, a division of the McGraw-Hill Companies, Inc. Satisface las necesidades individuales falla de dislocación tsunami foco cálido segura contra sismos lava volcán de escudo sismógrafo epicentro volcán de cono de carbonilla Name 1 Date Reinforcement Class Earthquakes Directions: Write the term that matches each description below on the spaces provided. One or two letters have been given as clues for each answer. Rearrange the letters given as clues to find the term that completes the sentence in question 9. 1. ___ ___ ___ ___ m ___ ___ ___ ___ ___ ___ 2. ___ s ___ ___ a ___ ___ 4. e ___ ___ ___ ___ ___ ___ ___ ___ e 5. ___ ___ i ___ ___ ___ ___ ___ __ 6. ___ ___ i ___ a ___ ___ ___ ___ ___ ___ 7. ___ ___ ___ f ___ c ___ ___ ___ ___ ___ Copyright © Glencoe/McGraw-Hill, a division of the McGraw-Hill Companies, Inc. 8. s ___ ___ ___ ___ ___ ___ ___ ___ ___ ___ ___ ___ 1. 2. 3. 4. 5. 6. instrument that records seismic waves seismic sea wave; becomes more dangerous as it gets closer to shore and can be very destructive the point inside Earth where movement from an earthquake first occurs vibrations caused by rocks breaking and moving as a result of a sudden release of energy the point on the surface of Earth located directly above the earthquake focus type of seismic wave that travels the fastest through rock material by causing rocks to vibrate in the same direction as the waves 7. type of seismic wave that travels the slowest and causes most of the destruction 8. type of seismic wave that moves through rocks by causing rocks to vibrate at right angles to the direction of the waves 9. A building able to stand up against an earthquake is considered to be Directions: Complete the following table. Description Forces That Cause Fault Type of Fault Rocks are pulled apart 10. 13. Rocks are sheared 11. 14. Rocks are compressed 12. 15. Earthquakes and Volcanoes 25 Meeting Individual Needs 3. ___ ___ ___ ___ s Name 2 Date Reinforcement Class Volcanoes Directions: Indicate whether each statement refers to a shield volcano (sh), a cinder cone volcano (cc), or a composite volcano (cv). 1. moderate to violent eruptions throwing volcanic ash, cinders, and lava high into the air 2. largest type of volcano 3. a relatively small cone of volcanic material formed from tephra 5. forms along subduction zones 6. buildup of basaltic layers, forming a broad volcano with gently sloping sides 7. forms where magma is being forced up from the extreme depths within Earth, or in areas where Earth’s plates are moving apart 8. Sunset Crater, near Flagstaff, Arizona 9. Mount St. Helens, in Washington 10. a steep-sided mountain composed of alternating layers of lava and tephra Directions: Match the descriptions in Column II with the items in Column I. Write the letter of the correct description in the blank at the left. Column II Column I 11. pyroclastic flow 12. mudflows 13. lava 14. lava rich in silica 15. lava rich in iron and magnesium 16. tephra a. magma when it reaches Earth’s surface b. ash, cinders, solidified lava c. tends to flow easily d. tends to be thicker and is more resistant to flow e. hot, glowing rock flows on cushion of hot gases f. often accompany eruptions, and can be brought on by heavy rain 26 Earthquakes and Volcanoes Copyright © Glencoe/McGraw-Hill, a division of the McGraw-Hill Companies, Inc. Meeting Individual Needs 4. sometimes erupts violently, forming a layer of tephra; sometimes a quieter eruption forming a lava layer Name 3 Date Reinforcement Class Earthquakes, Volcanoes, and Plate Tectonics Directions: Answer the following questions on the lines provided. 1. Describe the lithosphere. Meeting Individual Needs 2. What are rifts? What kinds of eruptions would you expect there? 3. What happens at a convergent plate boundary? How does this set up conditions that form volcanoes? Copyright © Glencoe/McGraw-Hill, a division of the McGraw-Hill Companies, Inc. 4. Where do most volcanoes form? How did the Hawaiian Islands form? 5. Where and how do earthquakes form? 6. Describe the convection theory of tectonic plate movement. Directions: Use the drawings to identify the types of plate boundaries. A B C 7. transform boundary ______ 8. convergent boundary ______ 9. divergent boundary ______ Earthquakes and Volcanoes 27 Name Enrichment Class The New Madrid Fault Of all the states, California faces the highest risk of earthquakes. This is due, in part, to a major break in Earth’s crust that runs through the state for approximately 1,050 km. This fracture, the San Andreas Fault, was responsible for the killer San Francisco earthquake in 1906 and countless others since. Meeting Individual Needs Earthquakes in Missouri But a series of three earthquakes between December 16, 1811, and February 7, 1812, took place not in California, but in Missouri, along a quake zone called the New Madrid Fault. All three measured 8.0 on the Richter scale, making them the largest American earthquakes ever. The quakes were so strong that tremors were felt as far east as Boston and Washington, D.C. Aftershocks continued for more than a year. Besides devastating 7,800 to 13,000 km2 of land, the earthquake caused the Mississippi River to reverse its direction temporarily and begin to flow upstream. The earthquake also caused the Mississippi to permanently change its course and create new lakes and islands where there hadn’t been any before. The New Madrid Fault is 70 km wide, 300 km long, and is located near New Madrid, Missouri. It runs primarily through Missouri, Arkansas, Kentucky, and Tennessee. If an earthquake happened, it could affect up to 17 states surrounding the fault zone. For a long time, geologists thought that a New Madrid earthquake was likely to happen only every 1,000 years or so. Earthquake Conference Unfortunately, earthquakes can and do happen anytime, anywhere. Scientists are still unable to predict them, so they’re constantly working on ways to prepare for an earthquake and to minimize the damage to lives and property. In the fall of 2000, representatives from 26 earthquakeprone states met at the first-ever National Earthquake Risk Management Conference. They discussed, among other things, the New Madrid Fault and the need to make people aware that earthquakes don’t just happen in California. Scientists predict that a New Madrid earthquake could result in $20 billion in damages. With increased land development and urban sprawl hitting all the communities located on the New Madrid Fault, it’s likely the human cost would be very high as well. 1. Where could you find information on earthquake preparedness? Is this something you and your family need to think about? Give at least two reasons. 2. When the New Madrid earthquakes of 1811–1812 hit, there were very few people or buildings in the area. Now scientists predict that a similar earthquake would cause damage from St. Louis to Memphis, causing billions of dollars in property damage and the loss of hundreds of lives. What effect would a New Madrid earthquake have on the land itself? 3. List some preventive measures your school could take to prepare for an earthquake. 28 Earthquakes and Volcanoes Copyright © Glencoe/McGraw-Hill, a division of the McGraw-Hill Companies, Inc. 1 Date Name Enrichment Fire and Ice! Iceland is a land of fire and ice. Volcanoes, hot springs, and glaciers create a landscape of hot and cold contrasts. Every now and then, an earthquake shakes things up. The country is located right over the spreading Mid-Atlantic Ridge where the seafloor is tearing apart. A Volcano Zone Copyright © Glencoe/McGraw-Hill, a division of the McGraw-Hill Companies, Inc. Class As the Earth’s plates move apart in a spreading ridge, fissures form. A long fissure zone with many shield volcanoes on its sides runs right through the southeastern and southwestern parts of Iceland. This zone is about 70 kilometers long. This has created many problems for the people of Iceland, since the volcanic eruptions often cause a lot of damage. Some cities have been damaged because they were built near what were erroneously thought to be inactive volcanoes. Because much of Iceland is under ice, many small volcanic eruptions aren’t seen, but they still melt a lot of water. The water is captured in a caldera, the center region of a volcano, where it then spills out every three to four years. These water spills are called jökulhaups (yohkewl-owps) and can cause a great deal of destruction. Putting Volcanoes to Use The people of Iceland have learned to live with their volcanoes. Iceland is one of the most effective countries of the world in capturing the geothermal energy of Earth and using it to make electricity. When water seeps into the cracks of the fissures, it is superheated by magma. The water turns to steam and escapes through the top of the fissure as a geyser. This high-temperature steam is used to rotate turbine blades. In turn, the turbines produce electricity for use by the people. More than 70 percent of the homes in Iceland are heated and lighted by geothermal energy. Iceland is a model for other countries when it comes to geothermal power. Geothermal energy is environmentally clean and will probably last a long time. 1. Why does Iceland have so many volcanic eruptions? 2. How is geothermal energy captured in Iceland? 3. This type of energy is also called hydrothermal energy. Why do you think that is so? Earthquakes and Volcanoes 29 Meeting Individual Needs 2 Date Name Enrichment Class Coming Up: Island Under Construction Hawaii is a favorite vacation spot for people all over the world. Many people enjoy its beaches and pleasant weather. You can visit its eight major islands: Nihau, Kauai, Oahu, Molokai, Lanai, Maui, Kahoolawe, and Hawaii. A New Island Meeting Individual Needs There is another “island” that is fairly large, but most people have never heard of it. It is called Loihi, a Hawaiian word that means “long.” However, you cannot make a reservation to stay at a hotel there, because Loihi is beneath the ocean. It is about 20 miles from the southeast coast of the island of Hawaii and sits on the same hot spot as Mauna Loa and Kilauea, two active Hawaiian volcanoes. Like the other Hawaiian Islands, Loihi is volcanic. But unlike most of the other islands, it is still being formed. Currently, the island is more than 3,000 m high. It has about 969 m to go before it reaches sea level. If it keeps growing at its current rate, it should become visible above the surface of the ocean sometime in the next 10,000 to 100,000 years. Scientists Discover Loihi Loihi is a volcano that is a seamount, or sea mountain. For a long time, scientists knew it existed, but believed it was extinct. They discovered Loihi was actually relatively young and active in 1970, when an expedition of scientists went to investigate a swarm of earthquakes that had occurred there. Swarm is a term used to describe a large amount of earthquake activity. Undersea photographs of Loihi showed new-looking lava formations. Actual samples of the lava had a glass-like crust, which confirmed the lava was new. Keep in mind that “new” in scientific, or geologic, terms can mean as long as several hundred years ago or as recently as yesterday. Loihi Earthquakes In the summer of 1996, the largest swarm of earthquakes ever recorded for the islands occurred at Loihi. About 4,000 earthquakes shook the seamount during a two-month period that summer. Once again, scientists went to Loihi to study the situation. Diving down to the island in a vessel called a submersible, they collected samples of lava. By using radiometry to date the lava, they found that the volcano had erupted at least once, and possibly twice, that year. Scientists have been monitoring Loihi using devices such as a hydrophone, a microphone that works underwater. The evidence the scientists are collecting shows that Loihi continues to erupt and grow. 1. How did scientists recognize that Loihi was still growing? 2. Why do you think Loihi is sometimes called a submarine island? 3. If Loihi reaches sea level in 10,0000 years, what would its average rate of growth per year be? What would its average rate of growth per year be if it reaches sea level in 100,000 years? 4. Do you think other new islands are possible in the Hawaiian chain? Explain. 30 Earthquakes and Volcanoes Copyright © Glencoe/McGraw-Hill, a division of the McGraw-Hill Companies, Inc. 3 Date Name Date Note-taking Worksheet Section 1 Class Earthquakes and Volcanoes Earthquakes A. Earthquakes—large ______________ that move through rock or other Earth materials 1. Elastic rebound—when rocks strain and then break, the broken pieces _____________. a. Rocks __________ slowly over long periods of time. c. Energy is released suddenly when rocks break and _________. d. The movement causes ______________ that move through Earth. 2. _________—the surface of a break in rock a. Normal fault—caused by tension forces, rock above the fault moves ________ compared to rock below the fault. b. Reverse fault—caused by compression forces, rock above the fault moves __________ compared to rock below the fault. c. Strike-slip fault—caused by shear forces, rock on either side of the fault moves ____________________ in opposite directions. Copyright © Glencoe/McGraw-Hill, a division of the McGraw-Hill Companies, Inc. B. Seismic waves—When strained rock’s ____________________ is released, it moves outward from the fault in seismic waves. 1. Focus—the point inside Earth where ____________ along a fault first occurs and energy is released 2. Epicenter—the point on Earth’s ________________ located directly above the focus 3. Seismic waves start at the focus and travel away in _______________________. a. ______________ waves—cause rock to move back and forth in the same direction the waves are moving b. ________________ waves—cause rock to vibrate at right angles to the direction the waves are moving c. ________________ waves—slowest, largest, most destructive waves C. Measuring earthquakes 1. Seismograph—instrument that records an earthquake’s ____________________ 2. If seismic-wave arrival times are recorded from three stations, the ________________ can be determined. 3. Richter scale—measures an earthquake’s size, or magnitude, based on the heights of lines representing the amount of energy released through ____________________ recorded on a seismograph Earthquakes and Volcanoes 31 Meeting Individual Needs b. _____________ energy builds up in them. Name Date Class Note-taking Worksheet (continued) D. Earthquake Damage 1. Modified Mercalli intensity scale—measures an earthquake’s intensity based on the amount of __________________________________ 2. Most earthquake damage is caused by ___________ waves. 3. Tsunamis—when an earthquake occurs on the _______________, the sudden movement pushes against the water and creates powerful waves that can travel thousands of kilometers. E. Seismic-safe structures are able to stand up against an earthquake’s _______________. 2. Underground water and gas pipes are replaced with pipes that will _______________. 3. Highways have cement pillars with spiral _______________ around them. F. Predicting Earthquakes 1. Long-range forecasts predict whether an earthquake is likely to occur in a given area within _____________ years. Section 2 Volcanoes A. Volcanoes—cone-shaped hills or mountains formed by ___________________ 1. When magma flows onto Earth’s surface through a vent, it is called ________. 2. __________—bits of rock or solidified lava dropped from the air after an explosive eruption. 3. Some volcanoes form where Earth’s plates ___________. a. One plate ____________, or is forced underneath, the other. b. Part of the plate that is forced underneath _________, forming magma chambers. 4. Avalanches of hot, glowing molten rock that flow on cushions of hot gases down a side of a volcano are called _____________________. 5. How forceful an eruption is depends on the composition of the _________. a. More silica makes magma _____________________. b. More iron and magnesium make magma _____________________. c. Water vapor trapped in the magma becomes steam and _____________________. 6. The type of _______________ and _______________ contained in the lava determine the type of volcano that forms. 32 Earthquakes and Volcanoes Copyright © Glencoe/McGraw-Hill, a division of the McGraw-Hill Companies, Inc. Meeting Individual Needs 1. Many high-rise buildings stand on huge steel and rubber _______________. Name Date Class Note-taking Worksheet (continued) B. Four types of volcanoes: 1. Shield volcanoes—____________ lava, which flows easily a. Forms a _________ volcano with gently sloping sides b. ___________ type of volcano c. Form where Earth’s plates are ______________ and magma is forced upward between plates 2. Cinder cone volcanoes—high _______ content in the magma Meeting Individual Needs a. Explosive, but _______________, eruptions b. Form a small cone of volcanic material from tephra 3. Composite volcanoes—made of alternating layers of lava and __________ a. Steep-sided mountains b. Form where Earth’s plates are colliding and being forced underneath each other, or ______________ zones. 4. Fissure eruptions—magma that is very _________ a. Oozes from __________ in Earth’s surface Copyright © Glencoe/McGraw-Hill, a division of the McGraw-Hill Companies, Inc. b. Magma flows freely across the land, as _________________. c. Most of Earth’s crust beneath the _________ is flood basalts. Section 3 Earthquakes, Volcanoes, and Plate Tectonics A. Earth’s crust is broken into __________ that move around. B. Most _____________ form where plates are colliding or moving apart. 1. Divergent plate boundaries—where plates move __________ a. Long cracks called _________ form between them. b. ___________ eruptions are common where plates separate. 2. Convergent plate boundaries—where plates ___________ and denser plates subduct, or are forced underneath less dense plates 3. Hot spots—large rising bodies of _________ force their way through Earth’s crust, not at plate boundaries C. Most _______________ occur where plates are colliding or moving apart. Earthquakes and Volcanoes 33 Assessment Assessment 34 Earthquakes and Volcanoes Name Date Chapter Review Class Earthquakes and Volcanoes Part A. Vocabulary Review Directions: Write the correct term in the spaces after each definition. Unscramble the boxed letters to answer question 17. 1. wave that passes through Earth 1. ___ ___ ___ ___ ___ ___ ___ 2. small, steep volcano with a cone made of tephra 2. 3. vibrations that occur when rocks break due to stress 3. ___ ___ ___ ___ ___ ___ ___ ___ ___ 4. seismic sea wave 4. ___ 5. magma that has reached the surface of Earth 5. 6. number based on seismic wave amplitude 6. ___ ___ ___ ___ ___ ___ ___ ___ ___ ___ ___ ___ ___ ___ ___ ___ ___ ___ ___ ___ ___ ___ ___ 8. structures that can withstand earthquakes 8. ___ ___ ___ ___ 9. bits of rock or solidified lava dropped from the air 9. ___ ___ ___ ___ ___ ___ ___ ___ ___ ___ ___ ___ ___ 11. cone-shaped mountains that spew out lava or gas ___ ___ ___ 11. ___ ___ ___ ___ ___ Assessment ___ ___ ___ 10. instrument used to record earthquakes 10. ___ ___ ___ ___ ___ 12. break in Earth’s rocks caused by stress 12. ___ ___ ___ ___ ___ ___ ___ 7. underground center of an earthquake 7. ___ Copyright © Glencoe/McGraw-Hill, a division of the McGraw-Hill Companies, Inc. ___ ___ ___ ___ ___ 13. long crack where plates diverge 13. ___ ___ ___ 14. large rising bodies of magma not at plate boundaries 14. ___ ___ ___ ___ ___ 15. point on Earth’s surface directly above the focus 15. ___ ___ ___ ___ ___ ___ ___ ___ ___ ___ 16. volcano formed by gentle eruptions of fluid lava 16. ___ ___ ___ ___ ___ ___ ___ ___ ___ ___ ___ ___ 17. The name of a type of volcano: _________________________________________________ Earthquakes and Volcanoes 35 Name Date Class Chapter Review (continued) Part B. Concept Review Directions: Circle the term in parentheses that makes the statement correct. 1. Molten rock inside Earth is (lava, magma, tephra). 2. Subduction takes place at a (convergent, divergent, transform) plate boundary. 3. The Richter scale measures (intensity, duration, magnitude). 4. A broad, shallow volcano with lava sides is a (shield, composite, cinder cone) volcano. 5. Tectonic plates are moved around by (seismic waves, nuclear reactions, convection currents). 6. (Primary, Secondary, Surface) waves are the slowest and largest of the seismic waves and cause most of the destruction during an earthquake. 7. Most earthquakes and volcanic eruptions occur (at the center of the plates, near the equator, at plate boundaries). Directions: Answer the following question on the lines provided. Assessment Directions: Use the following table to answer questions 9 and 10. Distance from Earthquake to Town Time Needed for S-waves to Reach Town Time Needed for P-waves to Reach Town Difference in Time Between the of S- and P-waves Town X 120 km 30 s 20 s 10 s Town Y 960 km 240 s 160 s 80 s 9. Why was the difference in time between the arrival of the P- and S-waves so much greater in Town Y than in Town X? 10. Which town probably suffered the greatest earthquake damage? Why? 36 Earthquakes and Volcanoes Copyright © Glencoe/McGraw-Hill, a division of the McGraw-Hill Companies, Inc. 8. Name the three kinds of faults and describe each of them. Transparency Activities Transparency Activities Earthquakes and Volcanoes 41 Name 1 Date Section Focus Transparency Activity Class Nobody’s Fault at All Transparency Activities 1. What happens during an earthquake? 2. What parts of an earthquake can be measured? 3. Why is it easier to predict where an earthquake will strike than when it will strike? 42 Earthquakes and Volcanoes Copyright © Glencoe/McGraw-Hill, a division of the McGraw-Hill Companies, Inc. The Richter scale was first used to rate the strength of earthquakes in 1935. Since then, we’ve learned a great deal about the causes of earthquakes, but predicting when an earthquake will strike remains tricky. Name 2 Date Section Focus Transparency Activity Class Does the stork bring baby islands? 1. Looking at the photo, how did the island of Surtsey form? 2. What do volcanoes and earthquakes have in common? Transparency Activities Copyright © Glencoe/McGraw-Hill, a division of the McGraw-Hill Companies, Inc. In November of 1963, the Atlantic Ocean got a new island. The island was named Surtsey after Sutur, a mythological fire god. The new island was the result of a volcanic eruption very near Iceland. 3. What unique learning opportunities might scientists have on Surtsey? Earthquakes and Volcanoes 43 Name 3 Date Section Focus Transparency Activity Class Earth Shattering Transparency Activities 1. What do you notice about the locations of the earthquakes shown above? 2. What other geological activity is likely to follow a similar pattern? 3. Give an example of some geological activity that does not occur along these boundaries. 44 Earthquakes and Volcanoes Copyright © Glencoe/McGraw-Hill, a division of the McGraw-Hill Companies, Inc. The dots on this image show places where earthquakes have occurred. The line of dots in the middle of the Atlantic Ocean is the Mid-Atlantic Ridge. As you can see, the area is geologically very active! Name Date 1 Teaching Transparency Activity Class Seismic Waves 16 15 14 13 First S Wave 12 10 rve u eC v a W S First P Wave ve r u C ve a P-W 9 8 7 6 5 5 min 4 3 2 1 0 1,000 Transparency Activities Travel Time (min) Copyright © Glencoe/McGraw-Hill, a division of the McGraw-Hill Companies, Inc. 11 2,000 3,000 4,000 Distance to Epicenter (km) Earthquakes and Volcanoes 45 Name Teaching Transparency Activity Date Class (continued) 1. What instrument records seismic waves from all over the world? 2. What is the name of the scale that gives the magnitude of energy an earthquake releases? 3. What two waves are indicated on the transparency? What do the abbreviations stand for? 4. What is the point on Earth’s surface directly above an earthquake’s focus? 5. What do seismologists study? 6. What do the height of the lines on a seismograph measure? Transparency Activities Copyright © Glencoe/McGraw-Hill, a division of the McGraw-Hill Companies, Inc. 7. Look at the graph to determine the approximate distance to the epicenter if the first P-wave arrives at the recording station two minutes ahead of the first S-wave. 46 Earthquakes and Volcanoes Name Date Assessment Transparency Activity Class Earthquakes and Volcanoes Directions: Carefully review the table and answer the following questions. House Location Earthquakes in Last 10 Years A Oregon 12 2.5 B California 73 5.2 C Illinois 0 0 D Delaware 2 1.1 Average Severity 1. According to the table, which location has earthquakes with an average severity greater than 5.0? AA BB CC DD 2. The most likely cause of the earthquakes in California is ___. F collision of the ocean and land G vibrations from landslides H effects of the weather J faults in Earth’s crust Transparency Activities Copyright © Glencoe/McGraw-Hill, a division of the McGraw-Hill Companies, Inc. Earthquake Activity 3. According to the table, which house has had no earthquake damage in the last ten years? AA BB CC DD Earthquakes and Volcanoes 47