activity 4 locating an earthquake epicenter answer key

Use the process of triangulation to locate an earthquake's epicenter. Lab 8 - earthquake lab - Lab: Locating the Epicenters of Earthquakes To do this, have the students use, Find the epicenter of the earthquake on the map (. Use the graph to answer the questions that follow. Click for facts and worksheets in PDF! Have students click on the Earthquakes Living Lab hyperlink in the top left in the earthquakes section. 4. fault - a fracture in Earth's crust where the rocks on either side have moved. Activity 4: Locating an Earthquake Epicenter, The three basic types of seismic wave generated by an earthquake at its focus are P, waves, Swaves, and Surface waves. Civil engineers, who design houses, apartment buildings, schools, skyscrapers, bridges, highways, tunnels, water treatment facilities, factories and other structures, may use this data to help them create safer structures that are less likely to sustain damage during earthquakes. How many minutes elapsed between the arrival of the first P wave and the last measurable Figure 2. In this activity, the epicenter of the earthquake is in the center of Los Angeles, CA. farther from the epicenter of an earthquake? Click on New Document and select the file importing option: upload Locating the epicenter of an earthquake worksheet answer key from your device, the cloud, or a protected link. If the lag time were measured at a location closer to the epicenter, The period of a wave is the time between two adj, How does the period of the P waves compare to t. Use data from seismograms to locate the epicenters of earthquakes. In order to determine the location of an earthquake epicenter, seismographs from at least three different places are needed for a particular event. 0000001746 00000 n Collect any giveaways for the students, such as earthquake posters or plate tectonic fliers. Most of these earthquakes are small tremors that cant be felt by people, but occasionally an earthquake occurs on a large magnitude that causes millions of dollars in property damage and kills hundreds to thousands of people. 13 4 locating an earthquake epicenter geosciences libretexts . 0000001893 00000 n 1. Once three seismographs have been located, find the time interval between the arrival of the P-wave . We have answers to the most popular questions from our customers. Then locate and click the link in the center of the page under the question: "How is an earthquake epicenter located and how is magnitude determined"? (i. Answer the following questions in the spaces provided. As the drum rotated, the Analyze and interpret data on natural hazards to forecast future catastrophic events and inform the development of technologies to mitigate their effects. HS-PS4-1. Learn from this informative and clear video.Brought you by award-winning Once each student has constructed his or her circle on the map, mark with an X, the epicenter of the earthquake. Quick Tips. [N'. (Grades Earthquakes Living Lab: Finding Epicenters & Measuring Magnitudes. 6. endstream endobj startxref Success is figuring out that the epicenter is just off the coast of Chile, where the three circles intersect. Practicing this technique, the students work several problems on a map of the US. How does the period of the P waves compare to the period of the surface waves? The period of a wave is the time between two adjacent wave peaks. You will analyze the records and locate the earthquake using a method known While earthquake locations are normally done with a computer that can quickly determine the paths of seismic waves through the Earth to many seismic stations, 15 Introduction to Geology Chapter Worksheet . P and Swaves are body waves and travelthrough the interior of the earth. 0000033429 00000 n (5 minutes) Discuss how gathering information on epicenters can be applied. 3000 miles. %PDF-1.4 % PDF. Introduction: Before student pairs look at the Earthquakes Living Lab, direct them to complete the Engage section of the Finding Epicenters and Measuring Magnitudes Worksheet, which asks them to apply any prior knowledge and/or speculate as to what the Richter magnitude scale is and what an epicenter is. USGS Earthquake Hazards Program If a quake is near the seismograph, the S-waves arrive shortly after the P-waves. hWmo9+[+UH EkNB|6YiaVJ=cRh7{T1R,5LI1$K=s)XR&87@&$LTPLutlcyNuzjf--\?qaXZM&HM.Eg"HnTqSWqN0&~2kf0 Md|d&:zhe)7I? To locate the epicenter of the earthquake, seismologists use the . (Listen to student ideas.) El trmino tambin puede hacer referencia al ttulo o nombre de alguien a quien se diri, Online Education Strategies (UNIV 1001 - AY2021-T), Advanced Care of the Adult/Older Adult (N566), Advanced Design Studio in Lighting (THET659), Introduction to Health Information Technology (HIM200), Biological Principles II and Lab (BIOL 107/L), PHIL ethics and social responsibility (PHIL 1404), Foundational Concepts & Applications (NR-500), Introduction To Project Management Software (CSBU539), Professional Application in Service Learning I (LDR-461), Advanced Anatomy & Physiology for Health Professions (NUR 4904), Principles Of Environmental Science (ENV 100), Operating Systems 2 (proctored course) (CS 3307), Comparative Programming Languages (CS 4402), Business Core Capstone: An Integrated Application (D083), BSC 2085-Study Guide - Dr. Alfonso Pino - Online course, Lecture notes, lecture all lectures - lecture notes from professor alan klein, Full Graded Quiz Unit 3 - Selection of my best coursework, EES 150 Lesson 2 Our Restless Planet Structure, Energy, & Change, General Chemistry I - Chapter 1 and 2 Notes, 1-2 Short Answer- Cultural Objects and Their Culture, Historia de la literatura (linea del tiempo), ACCT 2301 Chapter 1 SB - Homework assignment. Lab Exercise #2: Locating the Epicenter of an Earthquake In this lab exercise, you will locate the epicenter of an earthquake. The Richter scale was created in the 1930s to assign a single number to quantify the energy released during earthquakes. 01. Last updated November 26, 2013. How Can I Locate the Earthquake Epicenter? | Michigan Technological While no one can predict earthquakes, knowing the intensities, frequencies and locations of past earthquakes and fault planes helps us to better anticipate the locations and forces to expect, so we can do our best to prepare our communities and infrastructure to withstand them safely. pen recorded the arrival of P, S, and surface View Notes - Locating_an_epicenter_activity from SCIENCE Earth Scie at Toms River High North. The, amount of time that passes between the Pwave arrival and the Swave arrival is. Locating_an_epicenter_activity-MB.pdf - Activity 4: Locating an The magnitude determination is based on seismic data. Run through the investigation yourself and record the data, just to see how long it takes. How is the magnitude of an earthquake determined? Finding the Epicenter. 0000001408 00000 n Lab Activity Locating Epicenters Flashcards | Quizlet approximate period of the surface waves in seconds? A circle is drawn from each of the three different seismograph locations, where the radius of each circle is equal to the distance from that station to the epicenter. After reading about earthquakes, open a new window to an Earthquake Simulator at, Follow the simulation instructions. Continue the discussion with the following questions (or assign these questions as homework): Have student groups explore one or more of the other two regions (Southern California and Japan) provided in the Virtual Earthquake simulation. m>r/Q[6 In the ASN, standards are hierarchically structured: first by source; e.g., by state; within source by type; e.g., science or mathematics; 0000001978 00000 n El trmino tambin puede hacer referencia al ttulo o nombre de alguien a quien se di, Practica II - De Psicologian membrete es aquello que se ubica en el sector superior de una pgina, mencionando el ttulo o el nombre de un individuo, una empresa, etc. Contact the teacher to find out the length of the class period, as well as how many copies of handouts and sets of materials you need to bring. Use mathematical representations of phenomena or design solutions to describe and/or support claims and/or explanations. Focus (aka Hypocenter) is the location in the Earth where the earthquake starts. Describe the process of triangulation to locate an epicenter. 12), Seek, evaluate, and use a variety of specialized resources available from libraries, the Internet, and the community to find scientific information on Earth's history Before looking at the Earthquakes Living Lab, have pairs complete the, Then guide the teams to the Earthquakes Living Lab via the living lab website at. trailer <<320C1F98F8FF4795B5CCB8D9E9A0B99B>]/Prev 812054/XRefStm 1396>> startxref 0 %%EOF 93 0 obj <>stream The answer is the San Andreas Fault. The epicenter of an earthquake can be found using the difference between the arrival of the Primary and Secondary waves. Another method of locating an earthquake is to use the P-wave arrival-time minus origin-time (P - O) interval instead of distance. All the arcs should intersect at a common point - the epicenter. Subjects: Do you think we will someday be able to prevent earthquakes? different types of seismic waves. Locating_an_epicenter_activity - Activity4 - Course Hero Facility Name Busine Child ren Information Child Name C. Child Social Security Number Type of Case being filed - Check only one category. This investigation is considered generally safe to do with students. The arrival of seismic waves will be recognized by an increase in amplitude look for a pattern change as lines get taller and more closely spaced (ex. 0000001861 00000 n Learn more How Can I Locate the Earthquake Epicenter? Copyright USGS http://earthquake.usgs.gov/learn/kids/eqscience.php. earthquake lab lab: locating the epicenters of earthquakes objective measurable learning outcomes use data from seismograms to locate the epicenters of Skip to document Ask an Expert Sign inRegister Sign inRegister Home Ask an ExpertNew My Library Discovery Institutions Western Governors University Southern New Hampshire University To abbreviate, use the symbol M (a capital M, plain text, no sub/superscripts) expressed to the nearest 0.1. PDF EARTHQUAKES: Epicenter Determination, Seismic Waves, and Hazards - WOU 0000030240 00000 n Thanks for your feedback! 3. epicenter - the point on Earth's surface directly above the focus, or origin, of an earthquake. [*aiLG?+J\QI86~}ooRrr!pm}dk@dBbZPMZlC4C\9^ SM.R\!H+$|+DUzt^w{" %&{KXjT'9yzT^UFe:+f(`PU_9%EW@\)?i qp!\G Z endstream endobj 75 0 obj <>stream The travel-time graph Short for "primary wave" or "pressure wave." %%EOF Describe the logarithmic nature of the earthquake magnitude scale. distance = travel time for S waves Using online resources and simulations available through the Earthquakes Living Lab, students explore the consequences of subsurface ground type and building height on seismic d Seismographs are measuring devices designed by engineers and used by researchers to determine the locations and magnitudes of earthquakes. The time As the drum rotated, t, pen recorded the arrival of P, S, and surface, between arrival of P and S waves is called, epicenter, the longer the lag time measured, velocity, amplitude, and frequency of the. Ask students what fault they think caused this earthquake. Cross), Give Me Liberty! Finding the epicenter of an Earthquake by Ah - Ha Lessons 5.0 (1) $3.00 PDF Activity This lesson teaches the student the process scientists use to locate the epicenter of an EQ. 0000030504 00000 n Locating Earthquake Epicenter Teaching Resources | TPT 1,000 miles from the epicenter of an earthquake? and S waves depends on the distance from the epicenter of the answer the following question. Locating An Earthquake Epicenter Lab Answer Key ?t?s=Yt '_( endstream endobj 76 0 obj <>stream Tips: Make sure students are reading the S waves and not the P waves. 61 0 obj <> endobj xref Scientists and engineers around the globe gather data through observation and experimentation and use it to describe and understand how the world works. 0000053998 00000 n 0000031066 00000 n 0000106240 00000 n For this activity, select the "Chile" box. How does distance from the epicenter affect the magnitude (height) of the seismograph reading? Send activity 4 locating an earthquake epicenter worksheet answers via email, link, or fax. We also acknowledge previous National Science Foundation support under grant numbers 1246120, 1525057, and 1413739. However, please review it for the specific setting, materials, students, and conventional safety precautions. The real-world earthquake data is viewable via a graphical interface using a scaling map. Upload a document. activity illustrates how the epicenter of an earthquake is found. When the tension becomes too great, the fault slips, causing an earthquake. Swaves arrive at the seismic station after the Pwaves. This opens a new window to Michigan Techs UPSeis informational site about earthquakes and seismology. Three seismographs are needed. Mark the first arrival of the swave on each seismogram. Triangulation to Locate an Earthquake By Earthquake Hazards Original Thumbnail Medium Detailed Description Triangulation can be used to locate an earthquake. Locating An Earthquake Epicenter Worksheet Answers If your seismograph station is hbbd``b`$C`q9 X_$_g`bdxc`X 1. Answer Key: Lab 5 Earthquakes - Find People EARTHQUAKES: Epicenter Determination and Seismic Waves . 5 4. Before going to the classroom, you will need to: Provide each student, with the following: Earthquakes occur every day all over the United States and all over the world. Y$Kr;V6[;Dq vg~cx:A[^jCssupwD endstream endobj 80 0 obj <> endobj 81 0 obj <>stream X!.43p2t!}SLx-3z.KN4X+H\+vk? H\0y For purposes of this activity, the least complicated and probably most accurate approach is to just use the term "magnitude," without needing to say "on the Richter scale" or "on the moment magnitude scale." located 1,000 miles from the P and S arrivals, you can now locate an earthquake your answers below. Also commonly termed the focus. The uses of technologies and any limitations on their use are driven by individual or societal needs, desires, and values; by the findings of scientific research; and by differences in such factors as climate, natural resources, and economic conditions. One seismogram indicates the distance to the epicenter. A. Seismic waves-waves generated by an earthquake, can move the ground forward and back- answers the question. 0000001736 00000 n Pwaves have the greatest velocity and reach theseismic station first. between arrival of P and S waves is called Q(_?!6YV3B"\'9:4gTp*7^/P.X!skfkJ)1nG#a\{UD+iWM+ rQR]9SFTUPlM#"c:;tnsQPlu]Uyv?Ge}W;8cMA/x}'5clES~+}S+N7}wQ:/BkmI^" 5oqaBC[TRjq4.e}F:SQg{=u\xcg~EaZKReoC?oahJ` 'w endstream endobj 77 0 obj <>stream Finding the epicenter worksheet answer key. 0000004457 00000 n Read through the sections What Is Seismology and What Are Seismic Waves?, Where Do Earthquakes Happen?, and Why Do Earthquakes Happen? to answer the following questions: What is the difference between S and P waves? ' endstream endobj 69 0 obj <> endobj 70 0 obj [85 0 R] endobj 71 0 obj <> endobj 72 0 obj <> endobj 73 0 obj <>stream If you draw a circle on a map around three different seismographs where the radius of each is the distance from that station to the earthquake, the intersection of those three circles is the epicenter. Use mathematical representations to support a claim regarding relationships among the frequency, wavelength, and speed of waves traveling in various media. trailer <<0444DE89825047A1A483C62E98F50868>]>> startxref 0 %%EOF 114 0 obj <>stream What data is used to determine magnitude? A minimum of three seismic stations is necessary to locate an epicenter. What was the lag time (in minutes) at this location? minutes? When seismic data is collected from at least three different locations, it can be used to determine the epicenter by where it intersects. Note the differences in What are those limits? In this 1-to-10 logarithmic scale, each succeeding level representing 10 times as much energy as the last. Scientists use triangulation to find the epicenter of an earthquake. Use of the TeachEngineering digital library and this website constitutes acceptance of our Terms of Use and Privacy Policy. 0000002658 00000 n Zip. The farther away the epicenter is, the greater the difference . 12 Earthquake Location Lab Answer Key (PDF) - skislah.edu Web12-earthquake-location-lab-answer-key 1/1 Downloaded from skislah.edu.my on February 15, 2023 by guest 12 Earthquake Location Lab Answer Key Right here, we have countless ebook 12 Earthquake Location Lab Answer Key and collections to check out. hbb2b`b``a I @ endstream endobj 62 0 obj <>/Metadata 55 0 R/Pages 51 0 R/StructTreeRoot 57 0 R/Type/Catalog/ViewerPreferences<>>> endobj 63 0 obj <>/Font<>>>/Fields[]>> endobj 64 0 obj <>/Font<>/ProcSet[/PDF/Text]>>/Rotate 0/TrimBox[0.0 0.0 612.0 792.0]/Type/Page>> endobj 65 0 obj <> endobj 66 0 obj <> endobj 67 0 obj <> endobj 68 0 obj <>stream Have students turn in their answers for the Explain portion of the worksheet. It shows the time required for P PDF Finding Epicenters and Measuring Magnitudes Worksheet to the lag time measured at this location? In order to determine the location of an earthquake epicenter, seismographsfrom at least three different places are needed for a particular event. These distances are determined using a travel-time curve, which is a graph of Pand S-wave arrival times (see Figure 13.11). (Source: USGS). 0000006538 00000 n hb```b````e``n`d@ A 'EF''oquE"ky#:}m;9JmkPt~=unFHy&|X:70 vILZ*|%6mD! When an earthquake strikes, P waves arrive at a seismograph rst and S waves next. 0000001562 00000 n For lower grades, just introduce the concepts of triangulation and the magnitude scale; a thorough understanding of P and S waves is not vital. 15 Bill Nye - Earthquakes Worksheet Key Earthquakes occur when the big pieces of earth's crust, called plates, move a little. and S waves to travel any distance up to Some places are more prone to earthquakes than others. 0000030968 00000 n So next, students compute the magnitude of this same earthquake by looking at the three simplified seismograms again, but this time selecting each's maximum S wave amplitude (height). Subject Areas: If a quake is near the seismograph, the S-waves arrive shortly after the P-waves. The point beneath Earth's surface where rock breaks under stress and causes an earthquake. (Source: USGS, Wikipedia). ya{I;W@DgMN2:UtbT=*+cY1.8Vm(u3Zt"J @9TAjJH@H_F3n7\Srdw~gAR#JQGj`ueS! If a quake is far from the seismograph, the P-waves arrive long before the S-waves. 0000001533 00000 n Ch Person/Attorney Filing: - Superior Court - Maricopa County - superiorcourt maricopa. Earthquake Location 2 Using the skills that you acquired in the picking P and S arrivals, you can now locate an earthquake using real seismic records. The nations most famous fault is the San Andreas Fault, which runs along a north-south trend in southern California, and happens to run directly through Los Angeles. This section explains what earthquakes and faults are and what causes earthquakes. HTn0"H@w=s(vxk8OM1px-{$_!o5|CS7RPr#V(0CUa%ZkuT9t};D Jj=.9,z!#@n5YCu>R88tfFRX=iRK Do you agree with this alignment? 2. So the difference in the P- and S-wave arrival times determines the distance between the epicenter and a seismometer. Take a few minutes to read the information on the left side of this page for the 2010 earthquake off the coast of central Chile. 74 Earthquake Activity: Locating the Epicenter and Time of Earthquake . triangulation: A method to determine exactly where an earthquake originates. DOC Home - Westerville City Schools Millions of people witnessed the motion of the earthquake on television. minutes and P waves 8 minutes to 0000005081 00000 n What data is used to determine magnitude? : an American History (Eric Foner), Principles of Environmental Science (William P. Cunningham; Mary Ann Cunningham), Forecasting, Time Series, and Regression (Richard T. O'Connell; Anne B. Koehler), Chemistry: The Central Science (Theodore E. Brown; H. Eugene H LeMay; Bruce E. Bursten; Catherine Murphy; Patrick Woodward), Biological Science (Freeman Scott; Quillin Kim; Allison Lizabeth), Campbell Biology (Jane B. Reece; Lisa A. Urry; Michael L. Cain; Steven A. Wasserman; Peter V. Minorsky), How many minutes elapsed between the arrival of the first P wave and. hb```f``Rl@ (l"`+uk?0.a~@6Vm;| G3f`75@v@Wz|A4#w9{(` ) !5(~q* MS-ESS3-2. %PDF-1.3 % What about P waves? (, Have any of you ever experienced an earthquake or know anyone who has? Every year, earthquakes cause death and destruction worldwide. Thanks for your feedback! Solved Lab Exercise #2: Locating the Epicenter of an - Chegg Travel-time graphDistance in Miles, Copyright 2023 StudeerSnel B.V., Keizersgracht 424, 1016 GC Amsterdam, KVK: 56829787, BTW: NL852321363B01, seismogram. question 1 of 3. HlRnQ?R\>BjK' Record your answer from Lab Exercise #2, Step 1. 12), computer or other device with Internet access, journal or writing paper for each student. The process is called triangulation. One seismogram indicates the distance to the epicenter. HTAn Last modified July 18, 2012. Student exploration Graphing Skills SE Key Gizmos Explore Learning. 4. Earthquakes can also cause tsunamis, which are very large waves that can damage coastlines and put coastal residents in danger. Locating the epicenter of an earthquake worksheet answer key, locating the epicenter of an earthquake worksheet pdf, chapter 7 lab 1 locating epicenters answer key, how many seismographs are needed to locate the epicenter of an earthquake. 0000003991 00000 n Epicenter. Locating Earthquake Epicenters ( Read ) | Earth Science PDF Locating An Earthquake Epicenter Lab Answers - Full PDF As you read and complete the activity, take notes so you can complete the. Many updates and improvements! 0000001143 00000 n Where the 3 circles intersect is the approximate location to the epicenter of the earthquake. Through the online Earthquakes Living Lab, student pairs explore various types of seismic waves and the differences between shear waves and compressional waves. 3. epicenter of an earthquake, how 6.17: Locating Earthquake Epicenters - K12 LibreTexts Students learn how engineers build shake tables that simulate the ground motions of the Earth caused by seismic waves in order to test the seismic performance of buildings. Seismic stations detect earthquakes by the tracings made on seismographs. Of the four Earthquakes Living Lab seismic areas, choose the "Chile" box, as shown in Figure 3. minute apart, represent the passage of time 83 0 obj <> endobj Lab Lesson 4 - Lab Lesson 4: Earthquakes and Seismology, use slide 6 and answer key slide 7 how can i locate the earthquake epicenter michigan web the epicenter of the earthquake is somewhere on the edge of that circle do the 0000004060 00000 n important in helping seismologists determine the epicenter of the earthquake. 0000005149 00000 n [k0 |`2dGXGGGd00A(60P-e = F5n -f$ C You learned that seismologists determine the distance to the earthquake epicenter using the difference between S and P wave arrival times. All 100,000+ K-12 STEM standards covered in TeachEngineering are collected, maintained and packaged by the Achievement Standards Network (ASN), 0000001675 00000 n The point where your ruler crosses the middle line on the chart marks the magnitude (strength) of the earthquake. Please answer the following questions using the earthquake video - shake, shake, shake. 5. focus - the point within Earth where an earthquake originates. 92 0 obj <>/Filter/FlateDecode/ID[]/Index[83 25]/Info 82 0 R/Length 62/Prev 466624/Root 84 0 R/Size 108/Type/XRef/W[1 2 1]>>stream How might they use this information? Triangulation and Magnitude: Student pairs complete the worksheet, which includes following a tutorial/simulation accessed through the Earthquakes Living Lab. The moment magnitude scale (MMS) was developed in the 1970s as a modification of the Richter scale and is better for measuring big earthquakes but less good for small ones. Then from the same recordings they determine the earthquake's magnitude, an estimate of the amount of energy released during the earthquake. All rights reserved. Notify the classroom teacher of technology needs (overhead projector). 0000004769 00000 n Use Figure 4.5 and the travel-time graph in Figure 4.4 to determine the distance between each station and THREE SEISMOGRAMS the epicenter. Even though the scale formulae are different, MMS retains the familiar continuum of magnitude values defined by the older scale. (Grades Specifically, seismographs make recordings (seismograms) of the seismic waves generated from earthquakes, providing engineers and other researchers with data that they use to make predictions about future earthquakes. approximate period of the surface waves in seconds? Book: Laboratory Manual for Introductory Geology (Deline, Harris & Tefend), { "13.01:_Introduction" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "13.02:_The_Epicenter,_Focus,_and_Waves" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "13.03:_Seismology" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "13.04:_Locating_an_Earthquake_Epicenter" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "13.05:_Lab_Exercise_(Part_A)" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "13.06:_Hazards_from_Earthquakes" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "13.07:_Lab_Exercise_(Part_B)" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "13.08:_Induced_Seismicity" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "13.09:_Lab_Exercise_(Part_C)" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "13.10:_Student_Responses" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()" }, { "00:_Front_Matter" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "01:_Introduction_to_Physical_Geology" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "02:_Earth\'s_Interior" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "03:_Topographic_Maps" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "04:_Plate_Tectonics" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "05:_Water" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "06:_Climate_Change" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "07:_Matter_and_Minerals" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "08:_Igneous_Rocks" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "09:_Volcanoes" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "10:_Sedimentary_Rocks" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "11:_Metamorphic_Rocks" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "12:_Crustal_Deformation" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "13:_Earthquakes" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "14:_Physiographic_Provinces" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "zz:_Back_Matter" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()" }, [ "article:topic", "showtoc:no", "license:ccbysa", "authorname:delineharristefend", "program:galileo" ], https://geo.libretexts.org/@app/auth/3/login?returnto=https%3A%2F%2Fgeo.libretexts.org%2FLearning_Objects%2FLaboratory%2FBook%253A_Laboratory_Manual_For_Introductory_Geology_(Deline_Harris_and_Tefend)%2F13%253A_Earthquakes%2F13.04%253A_Locating_an_Earthquake_Epicenter, $ \newcommand{\vecs}[1]{\overset { \scriptstyle \rightharpoonup} {\mathbf{#1}}}$ $ \newcommand{\vecd}[1]{\overset{-\!-\!\rightharpoonup}{\vphantom{a}\smash{#1}}} $$\newcommand{\id}{\mathrm{id}}$ $ \newcommand{\Span}{\mathrm{span}}$ $ \newcommand{\kernel}{\mathrm{null}\,}$ $ \newcommand{\range}{\mathrm{range}\,}$ $ \newcommand{\RealPart}{\mathrm{Re}}$ $ \newcommand{\ImaginaryPart}{\mathrm{Im}}$ $ \newcommand{\Argument}{\mathrm{Arg}}$ $ \newcommand{\norm}[1]{\| #1 \|}$ $ \newcommand{\inner}[2]{\langle #1, #2 \rangle}$ $ \newcommand{\Span}{\mathrm{span}}$ $\newcommand{\id}{\mathrm{id}}$ $ \newcommand{\Span}{\mathrm{span}}$ $ \newcommand{\kernel}{\mathrm{null}\,}$ $ \newcommand{\range}{\mathrm{range}\,}$ $ \newcommand{\RealPart}{\mathrm{Re}}$ $ \newcommand{\ImaginaryPart}{\mathrm{Im}}$ $ \newcommand{\Argument}{\mathrm{Arg}}$ $ \newcommand{\norm}[1]{\| #1 \|}$ $ \newcommand{\inner}[2]{\langle #1, #2 \rangle}$ $ \newcommand{\Span}{\mathrm{span}}$$\newcommand{\AA}{\unicode[.8,0]{x212B}}$, status page at https://status.libretexts.org.
Rockledge High School Calendar, Articles A