activity 4 locating an earthquake epicenter answer key

-

activity 4 locating an earthquake epicenter answer key

Année
Montant HT
SP
Maîtrise d'ouvrage
Maîtrise d'oeuvre

The hypocenter is the point within the earth where an earthquake rupture starts. This is determined by the P-and S-wave arrival times. As you read and complete the activity, take notes so you can complete the. 0000001143 00000 n HTAn Subject Areas: triangulation: A method to determine exactly where an earthquake originates. Draw your signature, type it, upload its image, or use your mobile device as a signature pad. Seismic Waves. Solved ACTIVITY 2B Locating an Earthquake Figure 5 shows - Chegg Use Figure 5 and the travel-time graph in Figure 4 to determine . Ask students what fault they think caused this earthquake. Locating Earthquake Epicenter Worksheet Answer Key 0000001862 00000 n Earthquakes and Volcanoes. Shear wave from earthquake, moving slower than primary waves, through solid material only. 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. Y$Kr;V6[;Dq vg~cx:A[^jCssupwD endstream endobj 80 0 obj <> endobj 81 0 obj <>stream Point on Earth's surface directly above an earthquake's focus. Locating an Earthquake's Epicenter - American Geosciences Institute Analyze and interpret data on natural hazards to forecast future catastrophic events and inform the development of technologies to mitigate their effects. (Figure 3):. Earthquakes Living Lab: Finding Epicenters & Measuring Magnitudes. One seismogram indicates the distance to the epicenter. PDF ActivityEarthquake Location* - Cascadia Earthscope Earthquake and Locating the epicenter of an earthquake worksheet answer key, locating the epicenter of an earthquake worksheet pdf, chapter 7 lab 1 locating epicenters answer key, how many seismographs are needed to locate the epicenter of an earthquake. HTn {0,`K6}(J6]&Q^"!q57y_VQ9fp3/?Mc=KGsrrt:c\$Lh`4}>C>`qcSj0[YpZ_Su(322/N Z./$E )H %C[5ph[BUyGh7|!XPQiDjJ(|BNvylk+g;9G(#Aby>Jcf`XmnwtDD+;Z^I&Sb-4!7oi` L7 endstream endobj 78 0 obj <> endobj 79 0 obj <>stream If you complete all the problems, you should be able to: Identify P, S, and surface waves on a simple seismogram. 01. After this activity, students should be able to: Each TeachEngineering lesson or activity is correlated to one or more K-12 science, Send activity 4 locating an earthquake epicenter worksheet answers via email, link, or fax. Resources. =Cv :~4yrXP 62{_,*Uq/O-oUNBr-$y~:G},#3e^CS6U*_zVGY7ZNUWk2f?? {%!,"{u5E&OOqA_"/uxn-kx+Vz*EQb)Q 0000055643 00000 n S wave: The second seismic wave of an earthquake. However, please review it for the specific setting, materials, students, and conventional safety precautions. Tracings made at three separate seismic stations are needed to locate an earthquake epicenter. 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 If a quake is far from the seismograph, the P-waves arrive long before the S-waves. Three seismographs are needed. 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. technology, engineering or math (STEM) educational standards. 0000005149 00000 n Focus. How Can I Locate the Earthquake Epicenter? | Michigan Technological and S waves to travel any distance up to 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. One seismogram indicates the distance to the epicenter. P and Swaves are body waves and travelthrough the interior of the earth. 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 This is determined by the P-and S-wave arrival times. Quick Tips. What is the time lag for the Seattle, Washington, seismic station? Do you agree with this alignment? Ch Person/Attorney Filing: - Superior Court - Maricopa County - superiorcourt maricopa. Scientists and engineers around the globe gather data through observation and experimentation and use it to describe and understand how the world works. Show students some of the numerous online animations comparing the movements of P and S waves. Finding the Epicenter Determine the epicenter distance from three different seismographs. It's a logarithmic scale from 1 to 10 with each succeeding level representing 10 times as much energy as the last. (Figure 3):. This worksheet focuses on using the p and s graph to find different variables. Locating_an_epicenter_activity - Activity4 - Course Hero The USGS now uses the MMS to estimate magnitudes for all modern large earthquakes. How does the Mad Scientist. 12), Evaluate ways that technology can impact individuals, society, and the environment. 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. Where the 3 circles intersect is the approximate location to the epicenter of the earthquake. Type text, add images, blackout confidential details, add comments, highlights and more. The spot where those three circles intersect is the epicenter (Figure 13.12). Collect any giveaways for the students, such as earthquake posters or plate tectonic fliers. Of the four Earthquakes Living Lab seismic areas, choose the "Chile" box, as shown in Figure 3. !5(~q* aqmd. 0000002009 00000 n Since the 1970s, the use of the Richter magnitude scale has largely been replaced in the scientific community by the moment magnitude scale (MMS). "`B(R6sj [CX7p+s =#;~ `'kA 0000009174 00000 n Locating an Epicenter through Triangulation of Seismic Data- Remote/Hybrid/Live. 0 500 1000 1500 2000 2500 3000 The distance to the earthquake epicenter is then determined using the "Earthquake P-Wave and S-Wave Travel Time" graph. In the ASN, standards are hierarchically structured: first by source; e.g., by state; within source by type; e.g., science or mathematics; PDF Finding Epicenters and Measuring Magnitudes Worksheet What data is used to determine magnitude? The instrument detects and documents the intensity, direction and duration of ground vibrations, which are used to determine the epicenters and strength/magnitudes of earthquakes or other seismic events. When the tension becomes too great, the fault slips, causing an earthquake. Mark the first arrival of the swave on each seismogram. The living lab presents earthquake information through a focus on four active seismic areas and historic earthquakes in those areas. 0000004224 00000 n Activity 4 Locating An Earthquake Epicenter Answers: Fill Out & Sign . Use of the TeachEngineering digital library and this website constitutes acceptance of our Terms of Use and Privacy Policy. Locating An Earthquake Epicenter Worksheet Answers Do limits exist on what science can predict? 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. The Richter scale was created in the 1930s to assign a single number to quantify the energy released during earthquakes. Use this information to complete the following. Privacy Policy, Seismograms from seismic stations in Fresno, CA, Phoenix, AZ, and Las Vegas, NV, A modified travel time curve for S-P wave, A Modified Travel Time Curve for S-P Wave. 0000010002 00000 n Figure 2. Locating Earthquake Epicenters ( Read ) | Earth Science The spot where those three circles intersect is the epicenter (Figure 13.12). Sign, fax and printable from PC, iPad, tablet or mobile with pdfFiller Note-taking Worksheet. Solved Lab Exercise #2: Locating the Epicenter of an - Chegg 3. Review their answers to assess their base knowledge of the subject matter. Though the distance to the epicenter can be determined using a travel-time graph, the direction cannot be told. n{6c&6NK*U;=9i%nF 0000008845 00000 n Focal Depth. S waves. 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. 0000001978 00000 n PDF Example Answers - TeachEngineering If a quake is far from the seismograph, the P-waves arrive long before the S-waves. U.S. Geological Survey, U.S. Department of the Interior. The western U.S. has more faults than the eastern U.S., and therefore the western U.S. has more earthquakes. What is the You will analyze the records and locate the earthquake using a method known 0 by. 0000030240 00000 n Make arrangements so that each student group has a computer with Internet access. Hands-on Activity Earthquakes Living Lab: Finding Epicenters

Mikayla Miller Spin A Yarn Steakhouse, Articles A