Activity Pasta Quake

Similar documents
Earthquakes and Seismic Waves Lesson 4 2

Earthquakes!! Be sure to fill in your notes sheet as you go through the power point!

How to Use This Presentation

A Violent Pulse: Earthquakes. Lecture #2

Plate Tectonics and Earth s Structure

Read & Learn Earthquakes & Faults

20.1 Earthquakes. Chapter 20 EARTHQUAKES AND VOLCANOES. Earthquakes and plate boundaries 500 UNIT 6 EARTH S STRUCTURE

Earthquake Investigation

Once you have opened the website with the link provided choose a force: Earthquakes

An entire branch of Earth science, called, is devoted to the study of earthquakes.

they help tell Earth s story! Regents Earth Science With Ms. Connery

Slide 1. Earth Science. Chapter 5 Earthquakes

Activity Pacific Northwest Tectonic Block Model

Earthquakes Modified

Plotting Earthquake Epicenters*

What causes an earthquake? Giant snakes, turtles, catfish, and spiders?

Seismic Waves. 1. Seismic Deformation

Three Fs of earthquakes: forces, faults, and friction. Slow accumulation and rapid release of elastic energy.

LAB. Balboa Heights, Panama. Boulder, Colorado. Mexico City, Mexico. Data Table. Difference Between P-wave and S-wave. S-wave Arrival Time

I. Locations of Earthquakes. Announcements. Earthquakes Ch. 5. video Northridge, California earthquake, lecture on Chapter 5 Earthquakes!

22.5 Earthquakes. The tsunami triggered by the 2004 Sumatra earthquake caused extensive damage to coastal areas in Southeast Asia.

I. What are Earthquakes?

Internal Layers of the Earth

ES Ch 19 Earthquakes 1

Section 19.1: Forces Within Earth Section 19.2: Seismic Waves and Earth s Interior Section 19.3: Measuring and Locating.

FOURTH GRADE HAZARDS 1 WEEK LESSON PLANS AND ACTIVITIES

AIM: What are the features of Earthquakes and where are they located? Do Now: What are some words that are associated with earthquakes?

Name Date Class. radiate in all directions, carrying some of the. of plate boundaries have different usual patterns of.

Epicenter - a point, directly above the true center of disturbance, from which the shock waves of an earthquake apparently radiate.

Integrated Science I: Locating earthquake epicenters. Name Per Date

INTRODUCTION TO EARTHQUAKES

How Do Seismic Waves Travel Through Earth?

Earthquakes. Earthquakes and Earth s Interior Earth Science, 13e Chapter 8. Elastic rebound. Earthquakes. Earthquakes 11/19/2014.

Identifying the causes and effects of earthquakes

Earthquakes. Photo credit: USGS

Earthquakes How and Where Earthquakes Occur

Activities SeismicWaves and SeismicEruption

Activity Cupcake Geology

Section Forces Within Earth. 8 th Grade Earth & Space Science - Class Notes

Determining the Earthquake Epicenter: Japan

Elastic rebound theory

Please be sure to save a copy of this activity to your computer!

5. EARTHQUAKES AND EARTH S INTERIOR

C) 10:20:40 A) the difference between the arrival times of the P -wave and the S -wave

Wheels Radius / Distance Traveled

Earthquakes. Chapter Test A. Multiple Choice. Write the letter of the correct answer on the line at the left.

Earthquakes in Ohio? Teacher Directions and Lesson

Forces in Earth s Crust

Earthquakes. Earthquakes and Plate Tectonics. Earthquakes and Plate Tectonics. Chapter 6 Modern Earth Science. Modern Earth Science. Section 6.

Seismic Waves NOTES.notebook. January 05, lithosphere. limit. elastic. fault. movement. Fault. fault. all. Seismic waves focus. interior.

A. Locate the Epicenter

LAB 9: Earthquakes & Seismic Activity

Module 7: Plate Tectonics and Earth's Structure Topic 4 Content : Earthquakes Presentation Notes. Earthquakes

How Do Scientists Find the Epicenter of an Earthquake?

Lecture Outline Wednesday-Monday April 18 23, 2018

2.3 Notes: Earthquake Damage Can Be Reduced

Activity Template. Drexel-SDP GK-12 ACTIVITY. Subject Area(s): Sound Associated Unit: Associated Lesson: None

Earthquake Lab Introduction: Purpose: Method: Equipment needed: Fundamental Concepts and Key Terms:

11/30/16 EARTHQUAKES ELASTIC LIMIT FAULT FORCE AND PLATES WHAT DO YOU NOTICE?

Earthquakes. Pt Reyes Station 1906

Earthquakes Earth, 9th edition, Chapter 11 Key Concepts What is an earthquake? Earthquake focus and epicenter What is an earthquake?

Earthquakes 11/14/2014. Earthquakes Occur at All Boundaries. Earthquakes. Key Aspects of an Earthquake. Epicenter. Focus

Earthquakes and Earth s Interior

Earthquakes. Building Earth s Surface, Part 2. Science 330 Summer What is an earthquake?

Figure 12.1: The 1964 Alaska earthquake was the longest ever recorded and the largest ever recorded in the United States.

Activity Plotting Earthquake Epicenters an activity for seismic discovery

Figure Diagram of earth movements produced by (a) P-waves and (b) S-waves.

Mondo Quake in Pacific Northwest? By Leander Kahney

Activity Turbidites in a Jar

Dangerous tsunami threat off U.S. West Coast

LECTURE #5: Plate Tectonics: Boundaries & Earthquake Science

Earthquake Epicenters

The Size of an Earthquake. Intensity of Shaking (Robert Mallet, 1857) Calculation of Earthquake Magnitude (Charles Richter, 1935)

Dynamic Crust Regents Review

Geology 101 Study Guide #4

San Andreas Movie Can It Happen?

Earthquakes, an overview. Christa G. von Hillebrandt-Andrade Puerto Rico Seismic Network University of PR-Mayagüez

Earthquakes & Volcanoes

Anatomy of an Earthquake Focus (or hypocentre): the center of energy release.

Earthquakes.


Earthquakes.

Released Science Inquiry Task Location Grade 11

By: Tiffany Norton Ashleigh Ibos

Earthquakes. Forces Within Eartth. Faults form when the forces acting on rock exceed the rock s strength.

Lesson 4: Earthquakes and Moving Plates

Cascadia EarthScope Earthquake and Tsunami Education Program (CEETEP)

Objective: You will learn to interpret a seismogram and, using differences in seismic waves, locate the epicenter of an earthquake.

Forces in the Earth s crust

Directed Reading. Section: How and Where Earthquakes Happen WHY EARTHQUAKES HAPPEN. Skills Worksheet. 1. Define earthquake.

Science Starter. Describe in your own words what an Earthquake is and what causes it. Answer The MSL

Earthquakes. Earthquake Magnitudes 10/1/2013. Environmental Geology Chapter 8 Earthquakes and Related Phenomena

Chapter 6: Earthquakes

Magnitude 7.6 & 7.6 PERU

Figure 2-1. Diagram of earth movements produced by (a) P-waves and (b) S-waves.

on the earthquake's strength. The Richter scale is a rating of an earthquake s magnitude based on the size of the

Measuring the Size of an Earthquake

An Earthquake is a rapid vibration or shaking of the Earth s crust created by a release in energy from sudden movement of a part of a plate along a

Magnitude 7.0 PERU. This region of the Andes is a sparsely populated area, there were no immediate reports of injuries or damage.

EARTHQUAKE INTENSITY AND MAGNITUDE

Transcription:

Activity Pasta Quake Model of Earthquake Magnitude. Demonstration & Student Worksheets Learn about earthquake magnitude by breaking different size bundles of uncooked spaghetti noodles. Short classroom activity for grades 4 and up emphasizes the difference between magnitudes. Background Intensity or Magnitude? ) iece (1 p M5 M6 (32 pc) M7 ) 4 pc 2 (1,0 Science Standards (NGSS; pg. 287) The severity of an earthquake can be expressed in terms of both intensity and magnitude. However, the two terms are quite different, and they are often confused. Intensity is based on the observed effects of ground shaking on people, buildings, and natural features. It varies from place to place within the disturbed region depending on the location of the observer with respect to the earthquake epicenter. Magnitude is related to the amount of seismic energy released at the hypocenter of the earthquake. It is based on the amplitude of the earthquake waves recorded on instruments which have a common calibration. The magnitude of an earthquake is thus represented by a single, instrumentally determined value. From Molecules to Organisms Structures and Processes: MS-LS1-8 Motion and Stability Forces and Interactions: HS-PS2-1, MS-PS2-2 Energy: MS-PS3-1, MS-PS3-5 Waves and Their Applications in Technologies for Information Transfer: MS-PS4-1, HS-PS4-1, MS-PS4-2, HS-PS4-5 Earth s Systems: HS-ESS2-1, MS-ESS2-2, HS-ESS2-2, MS-ESS2-3 VIDEO: Watch this short video demonstrations of the Pasta Quake activity: DEMO_Pasta Quake_Butler.mov Video 2. Earthquakes & Tsunamis > 3. VIDEOS_Earthquake & Tsunami > DEMO PastaQuake_Butler.mov Web links to other related magnitude activities Interactive Calculate-the-Magnitude activity Jnstructions (Magnitude-WebActivity.pdf) are in the Pasta Quake activity RESOURCES folder. The game can be played at: http://siovizcenter.ucsd.edu/library/tltc/tltcmag.htm Another interactive site to determine magnitude is Virtual Earthquake found at: http://www.sciencecourseware.org/glol/ e-binder for 2014 CEETEP workshop 99

Pasta Quake The San Francisco Treat* Demonstration to learn the concept of magnitude & log scale. Time: 15-20 Minutes Target Grade Level: 4th grade and up Content Objective: Students will learn the earthquake magnitude scale by breaking different amounts of spaghetti. Visual scale of the pasta emphasizes the relative differences between magnitudes; each whole step in magnitude. To Do and Notice The following demonstration may also be done in small groups. Hold up one piece of spaghetti. Bend the piece between your hands until it breaks. Notice the work it takes to break the spaghetti. Call this a 5 on the Pasta Magnitude scale (M5). Now ask, What would you need to multiply this single piece of spaghetti by to equal a Pasta Magnitude 6? (The answer is 32.) Hold up the smallest bundle of 32 strands of spaghetti. Bend the bundle until it breaks. Notice the work it takes to break the bundle. If the pasta magnitude scale were like the earthquake magnitude scale, this would be a Pasta Magnitude 6 break. Notice that the bundle is about the diameter of a large/fat drawing pencil (1.2 cm or.47 in). What did you notice? Was it still fairly easy to break? How did the bundle break - all at once or a strand at a time? We will come back to this a little later. We can now find out how large the next bundle of spaghetti representing a Pasta Magnitude 7 would be. We start by multiplying 32 pieces of spaghetti representing Pasta M6 by 32 = 1,024 pieces of spaghetti representing an M7. We can determine the new cross sectional area by multiplying the area of the M6 (1.135 cm 2 ) by 32 which gives us 36.32 cm 2 for an M7. To find out how large this new bundle will be, we will calculate the diameter of the circular area. (Refer to the Pasta Quake Math page.) The new diameter of the Pasta M7 is 6.8 cm or 2.67 in. Hold up the small 32 strand bundle and the large bundle of 1,024 strands of spaghetti. Notice that the scale of magnitude has increased from the cross sectional area of a fat pencil = M6, to a tennis ball = M7. How much energy do you think it would take to break a bundle of spaghetti this large? You can then break the large bundle of spaghetti, or flex it without breaking to show that it takes much more effort to make the bundle break. Holding up the large bundle of pasta, ask What would you need to multiply this bundle by to equal a Pasta M8? Materials 1# package of thin spaghetti or 2# package of regular spaghetti. (The answer is 32.) We start by multiplying 1,024 pieces of spaghetti representing Pasta M7 by 32 = 32,768 pieces of spaghetti representing an M8. We can determine the new cross sectional area by multiplying the area of the M7 (36.32 cm 2 ) by 32 which gives us 1,162.24 cm 2 for a M8. To find out how large this new bundle will be, we will calculate the diameter of the circular area. (Refer to the Pasta Quake Math page.) The new diameter of the Pasta M8 is 38.46 cm or 15.14 in. Hold up a circle with the new 38.46 cm or 15.14 in diameter. Notice that the scale of magnitude has increased from the cross sectional area of a fat pencil = M6, to a tennis ball = M7, to the size of a beach ball = M8. How much energy do you think it would take to break a bundle of pasta this large? Now let s consider a Pasta Magnitude 9 earthquake. How big of a spaghetti bundle do you think this will be? Look around the room for a comparable diameter and make an educated guess based on how the sizes have been progressing. Let s do the math. Once again, we start by multiplying 32,768 pieces of spaghetti representing Pasta M8 by 32 = 1,048,576 pieces of spaghetti representing an M9. We can determine the new cross sectional area by multiplying the area of the M8 (1,162.24 cm 2 ) by 32 which gives us 37,191.68 cm 2 for the M9. To find out how large this new bundle will be, we will calculate the diameter of the circular area. (Refer to the Pasta Quake Math page.) The new diameter of the Pasta M9 is 217.62 cm or 85.38 in, which is also 7.14! Hold up a circle of plastic tarp with this new diameter. Notice that we have changed from the cross section diameter of a fat drawing pencil = M6, to a tennis ball = M7, to the size of a beach ball = M8 and now to a circle with the diameter slightly larger than the height of a door. How much energy do you think it would take to break a bundle of spaghetti this large? Now we can begin to understand the energy involved in a great Cascadia Subduction Zone earthquake 100 *Activity is used with permission from Paul Doherty http://www.exo.net/~pauld/index.html. Worksheets by Roger Groom, Mount Tabor Middle School, Portland Oregon

Pasta Quake Math The following math shows the calculations used to determine the size of each bundle of spaghetti for magnitudes 6, 7, 8 and 9 to go with the Pasta Quake Magnitude activity. Magnitude increases by a factor of 32. To calculate increasing magnitudes, we will work with the cross section area of bundles of spaghetti. To increase the magnitude, the cross section area in cm 2 is multiplied by 32. We will also find the diameter of the bundle to see how the size of the bundles of spaghetti increases with each magnitude. Working the math: Magnitude 6: A 32 strand bundle of spaghetti = an area of 1.14 cm 2. To determine the diameter of the bundle, divide the area by π (3.14159) =.36 cm 2. the radius.36 cm 2 =.6 cm. And finally multiply by 2 to determine the new diameter.6 cm x 2 = 1.2 cm or 2.67 in. To increase a M6 to M7, multiply the area of M6 1.14 cm 2 by 32 = 36.32 cm 2 Magnitude 7: A 1,024 strand bundle of spaghetti = an area of 36.32 cm 2. To determine the diameter of the new bundle, divide the area by π (3.14159) = 11.56 cm 2 the radius 11.56 cm 2 = 3.4 cm. And finally multiply by 2 to determine the new diameter 3.4 cm x 2 = 6.8 cm or 2.67 in. To increase a M7 to M8, multiply the area of M7 36.32 cm 2 by 32 = 1,162.24 cm 2 Magnitude 8: A 32,768 strand bundle of spaghetti = an area of 1,162.24 cm 2. To determine the diameter of the new bundle, divide the area by π (3.14159) = 369.95 cm 2. the radius 369.95 cm 2 = 19.23 cm. And finally multiply by 2 to determine the new diameter 19.23 cm x 2 = 38.46 cm or 15.14 in. To increase a M8 to M9, multiply the area of M8 1,162.24 cm 2 by 32 = 37,191.68 cm 2 Magnitude 9: A 1,048,576 strand bundle of spaghetti = an area of 37,191.68 cm 2. To determine the diameter of the new bundle, divide the area by π (3.14159) = 11,838.49 cm 2. the radius 11,838.49 cm 2 = 108.81 cm. And finally multiply by 2 to determine the new diameter 108.81 cm x 2 = 217.62 cm or 85.68 in which also equals 7.14 feet. e-binder for 2014 CEETEP workshop 101

Name: Per: Pasta Quake! Today s Date: Due Date: There are 3 main ways to measure the magnitude of an earthquake. The magnitude is a measurement of earthquake strength based on seismic waves and movement along faults. First, let s review. What are the 3 types of seismic waves? For each, give a brief description. 1. 2. 3. What about exactly where earthquakes happen? Draw a diagram in the space below to show the difference between the epicenter and the focus. Now, match up the 3 main scales to measure earthquakes with their descriptions: 4. Richter Scale Measures the intensity of an earthquake. This is a measure of the strength of ground motion and has a scale of 1 12, but in Roman numerals, it s I XII. One earthquake may have different ratings depending on the damage at different locations. 5. Moment Magnitude Scale Measures the size of the seismic waves as shown on a seismograph. Good for small or close-by earthquakes. 6. Modified Mercalli Scale Measures the total energy released by an earthquake and can be used for all sizes, near or far. This is usually what is used today. 102

Page 2 Name On the Moment Magnitude Scale, each different number is a measure of the total energy released by an earthquake, and it s about 32 times greater between numbers of the scale. We can demonstrate with spaghetti: Pasta Magnitude Scale # of spaghetti pieces broken 3 1/30 4 1 5 32 6 1,024 7 32,768 8 1,048,576 Below is a list of some major earthquakes and their Moment Magnitude ratings: 1811-12 New Madrid (Midwestern US) 7.7 1906 San Francisco, California 7.8 1960 Arauco, Chile 9.5 1964 Anchorage, Alaska 9.2 1971 San Fernando, California 6.6 1985 Mexico City, Mexico 8.1 1989 San Francisco, California 6.9 1995 Kobe, Japan 6.9 7. Which earthquake released about 32 times more energy than the Mexico City quake of 1985? 1964 Anchorage, Alaska 8. Two of the earthquakes released just a little more than 32 times more energy than the 1971 San Fernando quake. They were... 1811-12 New Madrid and 1906 San Francisco 9. The 1964 quake in Alaska released about 32 times more energy than the 1985 Mexic City quake and it released more than 1024 times the energy of which quake? 1989 San Francisco or 1995 Kobe e-binder for 2014 CEETEP workshop 103

TEACHER ANSWER KEY PAGE 1/2 MEASURING Name: Class EARTHQUAKES Today s Date: Due Date: There are 3 main ways to measure the magnitude of an earthquake. The magnitude is a measurement of earthquake strength based on seismic waves and movement along faults. First, let s review. What are the 3 types of seismic waves? For each, give a brief description. 1. P-Waves primary waves fastest, move straight through solids and liquids 2. S-Waves secondary/shear waves second fastest, cannot move through liquids 3. L-Waves surface waves slowest, travels along surface only What about exactly where earthquakes happen? Draw a diagram in the space below to show the difference between the epicenter and the focus. Focus Fault Now, match up the 3 main scales to measure earthquakes with their descriptions: 4. Richter Scale Measures the intensity of an earthquake. This is a measure of the strength of ground motion and has a scale of 1 12, but in Roman numerals, it s I XII. One earthquake may have different ratings depending on the damage at different locations. 5. Moment Magnitude Scale Measures the size of the seismic waves as shown on a seismograph. Good for small or close-by earthquakes. 6. Modified Mercalli Scale Measures the total energy released by an earthquake and can be used for all sizes, near or far. This is usually what is used today. 104

ANSWER KEY PAGE 2/2 On the Moment Magnitude Scale, each different number is a measure of the total energy released by an earthquake, and it s about 32 times greater between numbers of the scale. We can demonstrate with spaghetti: Pasta Magnitude Scale # of spaghetti pieces broken 3 1/30 4 1 5 32 6 1,024 7 32,768 8 1,048,576 Below is a list of some major earthquakes and their Moment Magnitude ratings: 1811-12 New Madrid (Midwestern US) 7.7 1906 San Francisco, California 7.8 1960 Arauco, Chile 9.5 1964 Anchorage, Alaska 9.2 1971 San Fernando, California 6.6 1985 Mexico City, Mexico 8.1 1989 San Francisco, California 6.9 1995 Kobe, Japan 6.9 7. Which earthquake released about 32 times more energy than the Mexico City quake of 1985? 1964 Anchorage, Alaska 8. Two of the earthquakes released just a little more than 32 times more energy than the 1971 San Fernando quake. They were... 1811-12 New Madrid and 1906 San Francisco 9. The 1964 quake in Alaska released about 32 times more energy than the 1985 Mexic City quake and it released more than 1024 times the energy of which quake? 1989 San Francisco or 1995 Kobe e-binder for 2014 CEETEP workshop 105