0000008088 00000 n
PDF. %PDF-1.4
%
Earth and Space, Physical Science, A process called triangulation uses seismic data from three locations to identify the epicenter of an earthquake.copyrightCopyright USGS http://earthquake.usgs.gov/learn/kids/eqscience.php. 0000003991 00000 n
Another method of locating an earthquake is to use the P-wave arrival-time minus origin-time (P - O) interval instead of distance. One seismogram indicates the distance to the epicenter. Earthquakes & Volcanoes Test Review Answers. !5(~q* Have students click on the Earthquakes Living Lab hyperlink in the top left in the earthquakes section. 0000001562 00000 n
Follow this simple guide to edit Locating the epicenter of an earthquake worksheet answer key in PDF format online free of charge: Explore all the advantages of our editor right now! What was the lag time (in minutes) at this location? Describe the logarithmic nature of the earthquake magnitude scale. 0000000956 00000 n
(Source: USGS, Wikipedia). Section A - Operator Information 1. The period of P waves is shorter, than the period of surface waves. Lab Exercise #2: Locating the Epicenter of an Earthquake In this lab exercise, you will locate the epicenter of an earthquake. To make a magnitude determination, two measurements are needed: the S-P interval (already determined earlier in the tutorial) and the maximum amplitude of the seismic waves. Locating the Epicenter of an Earthquake - SE Asia a foldable activity, slide presentation to guide reading, and an answer key! Use this information to complete the following. (Grades 9 - 12). Thanks for your feedback! triangulation: A method to determine exactly where an earthquake originates. Then from the same recordings they determine the earthquake's magnitude, an estimate of the amount of energy released during the earthquake. In the ASN, standards are hierarchically structured: first by source; e.g., by state; within source by type; e.g., science or mathematics;
(Grades
Mapping the history of natural hazards in a region, combined with an understanding of related geologic forces can help forecast the locations and likelihoods of future events. Finding the epicenter worksheet answer key. epicenter: A point on the Earth's surface that is directly above the place where the underground forces of an earthquake originate. Epicenter Location on Earth's surface directly above the focus of the earthquake 5. 12), Evaluate ways that technology can impact individuals, society, and the environment. 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. The farther away the epicenter is, the greater the difference . Seismograms 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. 0000003855 00000 n
What about P waves? Millions of people witnessed the motion of the earthquake on television.
The, amount of time that passes between the Pwave arrival and the Swave arrival is. 0000030968 00000 n
0000001736 00000 n
Locating Epicenter Lab Worksheet (1).docx, Updating Patient Registration B at 08_10_2022 03_03 PM.pdf, You need to deploy an Azure environment that meets the company migration plan, Step 1 of 2 Program 1 A Simple Python Program Welcome with Two Messages Running, More women in academia report polarization assimilation in male skewed and male, A TACACS B RADIUS C Kerberos D SAML Correct Answer D QUESTION 321 A network, PTSD in Children and Adolescents - Copy - Copy - Copy - Copy.docx, Effects of Excitation and Prime Mover Control The excitation control helps to, D1 Fundamental security design principles.docx, Question 5 Correct Mark 100 out of 100 Remove flag Question 6 Correct Mark 100, Thomas Concurrence broadly attacked current NDD Federal gov should be allowed to, 769 Water at 15C is to be heated to 65C by passing it over a bundle of 4 m. Course Hero is not sponsored or endorsed by any college or university. Adjust the timing to the class period, remembering that you will need time to introduce the investigation, clean up afterwards, and re-set up for the next class (if you are working with more than one class). Locating The Epicenter Of An Earthquake Worksheet Answers, Content Outline Earthquakes For Teaching - Mrs. Parsiola's Homepage, Earthquakes & Volcanoes Test Review Answers, Earthquake Facts & Worksheets | Mechanism, Impact, Events, Quiz & Worksheet - Causes Of Earthquakes - Study.com, 15 Bill Nye - Earthquakes Worksheet Key | PDF - Scribd, Bill Nye-The Science Guy * - Biloxi Public Schools, psc plus two level preliminary exam syllabus pdf 2023, first tuesday real estate principles exam answers, ies exam pattern for mechanical engineering, resultados examen practico dgt las palmas, exame de sangue precisa de quanto tempo de jejum, sslc question paper 2023 karnataka pdf with answers social science, examen de formacion civica y etica tercer grado secundaria, ctet exam date 2023 application form last date, why is it important to do self breast exams, quanto tempo depois de infectado pelo hiv aparece no exame. For upper grades, have students work individually, do two of the three seismic area tutorials, and look up historical earthquakes to learn their magnitudes, and make data tables or graphs with this information. If a quake is near the seismograph, the S-waves arrive shortly after the P-waves. How does distance from the epicenter affect the magnitude (height) of the seismograph reading? www.teachengineering.org/activities/view/csm_findingepicenters_activity1, Search curriculum by Common Core standards, http://www.teachengineering.org/livinglabs/earthquakes/, Click to view other curriculum aligned to this Performance Expectation, Finding Epicenters and Measuring Magnitudes Worksheet, Finding Epicenters and Measuring Magnitudes (docx), Finding Epicenters and Measuring Magnitudes (pdf), Finding Epicenters and Measuring Magnitudes Example Answers (docx), Finding Epicenters and Measuring Magnitudes Example Answers (pdf), Earthquakes Living Lab: FAQs about P Waves, S Waves and More, Seismic Waves: How Earthquakes Move Through the Earth, Earthquakes Living Lab: Designing for Disaster, http://www.teachengineering.org/livinglabs/index.php, https://www.newpathonline.com/api_player/enus_54_6304/LXX/index.html. /g$=#!$EbBbhD!,x so^6Uc})\uJs=fyY}j'|YjTm8B_[}*Ovm\[J'.mu?lQg,wzJM^X&P w>-T%*h%J4 yB@VPmP]@D------------,2dfY$"A!ANAASi)4$dniiiinH% Gxt5DJ) )9RRr$II'y ??O's^3@[{*{VT?nsNS!ilq]mFO?? Section 8.1 What Is an Earthquake? 0000006538 00000 n
You will receive your score and answers at the end. 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. It's a logarithmic scale from 1 to 10 with each succeeding level representing 10 times as much energy as the last. Add to FlexBook Textbook. A. Seismic waves-waves generated by an earthquake, can move the ground forward and back- answers the question. within type by subtype, then by grade, etc. As discussed earlier in this lesson, this method of determining the epicenter of an . Was there an initial quake followed by smaller quakes? Earthquakes and Volcanoes. minutes? The epicenter of an earthquake can be found using the difference between the arrival of the Primary and Secondary waves. 0000115324 00000 n
Material is sheared side to side, perpendicular to the direction of wave propagation. 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. S wave: The second seismic wave of an earthquake. Note the differences in Facility Name Busine Child ren Information Child Name C. Child Social Security Number Type of Case being filed - Check only one category. 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 Through the online Earthquakes Living Lab, student pairs explore various types of seismic waves and the differences between shear waves and compressional waves. The answer is the San Andreas Fault. Success is figuring out that the estimated magnitude is 5.9. Answer the following questions in the spaces provided. In Figure 13.9, there is an example seismogram from a station that includes a minor earthquake. Alignment agreement:
The three seismograms in this activity are unfi ltered station records from a single event that occurred on August 1, 1999. Analyze and interpret data on natural hazards to forecast future catastrophic events and inform the development of technologies to mitigate their effects. (Figure 3):. S waves. Figure 13.10). Click for facts and worksheets in PDF! Make changes to the sample. 1. View Notes - Locating_an_epicenter_activity from SCIENCE Earth Scie at Toms River High North. In Figure 13.9, there is an example seismogram from a station that includes a minor earthquake. Engineers first determine where earthquakes are likely to occur, and how severe they are likely to be. Though they may weaken with distance, seismographs are sensitive enough to still detect these waves. Do you agree with this alignment? If a quake is near the seismograph, the S-waves arrive shortly after the P-waves. and S waves depends on the distance from the epicenter of the answer the following question. P and Swaves are body waves and travel, through the interior of the earth. Answer Key: Lab 5 Earthquakes - Find People EARTHQUAKES: Epicenter Determination and Seismic Waves . Richter magnitude scale: An earthquake measurement scale created in the 1930s to assign a single number to quantify the energy released during earthquakes. Figure 8. Explains how to find an earthquake epicenter using at least three seismograph stations. Swaves arrive at the seismic station after the Pwaves. 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. Must engineers be content with mitigating disasters, instead of preventing them? Three seismographs are needed. Practice with Triangulation: Locating an earthquake epicenter. Geologists use seismic waves to locate an earthquake's epicenter. 0000106240 00000 n
Thanks for your feedback! earthquake. Now on the main page of the Earthquakes Living Lab website (see Figure 2), note the featuring of four active seismic areas and the mapping of real-time and current data from earthquakes happening around the world. Record your answer from Lab Exercise #2, Step 1. Earthquakes occur along faults, which are cracks in the Earths crust that build tension. (Grades
m>r/Q[6 locate and label the epicenter of the earthquake on this map. HS]o01j6R0iMm4U=wL8]BE< moment magnitude scale: Similar to the Richter scale, but replacing its use starting in the 1970s for more accuracy in measuring big earthquakes (magnitudes > 3.5) from greater distances. This is determined by the P-and S-wave arrival times. Of the four Earthquakes Living Lab seismic areas, choose the "Chile" box, as shown in Figure 3. How far do S waves travel in 5 aqmd. Entering the three maximum amplitudes generates a nomogram, a graphical device that simplifies the process of estimating magnitude from distance (determined earlier in the tutorial from the S-P interval process) and amplitude. 0000002507 00000 n
Refer to the data table and use the difference in arrival times to determine the distance to the earthquake epicenter for Station 2. 0000006984 00000 n
minutes and P waves 8 minutes to 0000003966 00000 n
minutes = 6 minutes. : 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. Richter scale Method of earthquake measurement based on the amplitude of seismic . Wikipedia, The Free Encyclopedia. (i. This investigation is considered generally safe to do with students. DocHub v5.1.1 Released! If you can't find an answer to your question, please contact us. 500p;333aXb3
\a.1. (Grades
What is an earthquake? See Answer. hb```b````e``n`d@ A
'EF''oquE"ky#:}m;9JmkPt~=unFHy&|X:70
vILZ*|%6mD! Video Guide / Worksheets and Quizzes for Quizzes and Answer Sheet __ 2. 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
Thus, the Richter scale is used for measuring small earthquakes (3.5 M or less), while the moment magnitude scale is used for measuring stronger earthquakes (3.5 M or higher). Activity 4 Locating An Earthquake Epicenter Answers: Fill Out & Sign . Finally, the location of the 3 seismographs are placed on a map and the distance to the epicenter is used to draw a circle with an origin at each seismograph and a radius equal to the distance to the epicenter as taken from each seismogram. The vertical lines, spaced one, minute apart, represent the passage of time, (from left to right). The wavelength and frequency of a wave are related to one another by the speed of travel of the wave, which depends on the type of wave and the medium through which it is passing. 15 Bill Nye - Earthquakes Worksheet Key Earthquakes occur when the big pieces of earth's crust, called plates, move a little. determine the epicenter using the S P (S minus P) method. 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. What is the Figure 1 is a simplified example of a This section explains what earthquakes and faults are and what causes earthquakes. Seismic Waves. For example, 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. At least 3 earthquake recording stations are required to find the location of the earthquake epicenter. 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
When seismic data is collected from at least three different locations, it can be used to determine the epicenter by where it intersects. 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"? Tips: Make sure students are reading the S waves and not the P waves. If a quake is far from the seismograph, the P-waves arrive long before the S-waves. pen recorded the arrival of P, S, and surface Scientists and engineers around the globe gather data through observation and experimentation and use it to describe and understand how the world works. %PDF-1.5
%
0000001533 00000 n
The Earthquakes Living Lab gives students the chance to track earthquakes across the planet and examine where, why and how they are occurring. Tracings made at three separate seismic stations are needed to locate an earthquake epicenter. The magnitude determination is based on seismic data. ?t?s=Yt '_(
endstream
endobj
76 0 obj
<>stream
87 0 obj
<>
endobj
xref
87 28
0000000016 00000 n
The process is called triangulation. trailer
<<320C1F98F8FF4795B5CCB8D9E9A0B99B>]/Prev 812054/XRefStm 1396>>
startxref
0
%%EOF
93 0 obj
<>stream
travel time for P waves. from the epicenter will be 14 8. To accurately locate an earthquake epicenter, records from three. So the difference in the P- and S-wave arrival times determines the distance between the epicenter and a seismometer. All the arcs should intersect at a common point - the epicenter. Expert Answer. 0000007097 00000 n
A minimum of three seismic stations is necessary to locate an epicenter. 0000010002 00000 n
Finding the Epicenter. gov For online instructions and current fees click here. distance from transducer to the focal point. 0000001143 00000 n
The Richter scale was created in the 1930s to assign a single number to quantify the energy released during earthquakes. Reading Strategy. What data is used to determine magnitude? technology, engineering or math (STEM) educational standards. question 1 of 3. Review their answers to assess their base knowledge of the subject matter. Students learn about the types of seismic waves produced by earthquakes and how they move through the Earth. 0000004457 00000 n
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. 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 . Upload a document. For this activity, select the "Chile" box. P wave: The first seismic wave of an earthquake. Using the real-world data in the living lab enables students and teachers to practice analyzing data to solve problems and answer questions, in much the same way that scientists and engineers do every day. 5. focus - the point within Earth where an earthquake originates. to the lag time measured at this location? Yw8SxGk}X3kfTfW& gk`41#'uf7"G\fsN4^8jC7[+%`qFLFKpFc P wave. by. Please answer the following questions using the earthquake video shake, shake, shake. 0000004224 00000 n
What is an earthquake? 0000053998 00000 n
EARTHQUAKES: Epicenter Determination and Seismic Waves First locate and mark the three seismic stations on the world map provided below. How does the Mad Scientist. 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. Focus. 0000001893 00000 n
(Grades
epicenter of an earthquake, how A little under 30 seconds, maybe around 26 seconds. Even though the scale formulae are different, MMS retains the familiar continuum of magnitude values defined by the older scale. Travel-time graphDistance in Miles, Copyright 2023 StudeerSnel B.V., Keizersgracht 424, 1016 GC Amsterdam, KVK: 56829787, BTW: NL852321363B01, seismogram. It travels faster than the same earthquake's S wave (almost double the speed) and is similar to sound waves. 12), computer or other device with Internet access, journal or writing paper for each student. 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. 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. 4. fault - a fracture in Earth's crust where the rocks on either side have moved. First, determine the P-wave arrival, and read down to the bottom of the seismogram to note at what time (usually marked in seconds) that the P-wave arrived. 0000000856 00000 n
Considered best for measuring small earthquakes (3.5 M or less). 61 33
If you complete all the problems, you should be able to: Identify P, S, and surface waves on a simple seismogram. This activity is designed around the Earthquakes Living Lab, a resource and online interface that uses real-time U.S. Geological Survey seismic data from around the world. 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. American Geosciences Institute. These distances are determined using a travel-time curve, which is a graph of Pand S-wave arrival times (see Figure 13.11). Fill Locating The Epicenter Of An Earthquake Worksheet Answers, Edit online. A seismograph is securely mounted onto the surface of the earth so that when the earth shakes, the entire unit shakes with it EXCEPT for the mass on the spring, which has inertia and remains in the same place. !D,X2:azTG)kPT~Mj 4>d w@O'. Key Facts & Information. Type text, add images, blackout confidential details, add comments, highlights and more. For example, the western United States has earthquakes more frequently and on a larger scale than the eastern part of the country. minute apart, represent the passage of time After reading about earthquakes, open a new window to an Earthquake Simulator at, Follow the simulation instructions. seismogram. and S waves to travel any distance up to Develop a solution to a technological problem that has the least negative environmental and social impact. In this investigation, participants will understand that S and P waves are used to find the epicenter of an earthquake by using seismograph data to triangulate an epicenter. P and Swaves are body waves and travelthrough the interior of the earth. The simulation renders three circles on a map and directs students to find the epicenter. Subject Areas:
time for any point that is 3,000 miles The lag time for any They make a model of a seismographa measuring device that records an earthquake on a seismogram. 0000002094 00000 n
Practicing this technique, the students work several problems on a map of the US.
Oasis Has Beens Shouldn't Present Awards,
Gorilla Bbq Rub Recipe,
Terry Reid Obituary,
Articles A