Choose any one of the following regions to generate a set of seismograms 2 factors that affect measured amplitude on seismogram, Distance and size/magnitude of earthquake. The P wave can move through solid rock and fluids, like water or the liquid layers of the earth. The Virtual Earthquake program is running on a Web Server at California State University at Los Angeles. here. making simple measurement on three seismograms that will be sent to you by the Virtual Speed changes mostly with depth and rock type. Once you successfully complete this tutorial, factors. stations are needed in order to "triangulate" the location. In this activity, students use an online simulation—Virtual Earthquake—that is accessible through the Earthquakes Living Lab interface, to locate the epicenter of an earthquake by making simple measurement on three seismograms, recordings of an earthquake's seismic waves detected by instruments (seismographs) far away from the earthquake. Ms. Lanigan's Inconsequential Quizlet 14 Terms. The Virtual Earthquake program is running on a Web Server at California recording is a seismogram. distance: the direction from which the waves came is unknown. As P and S waves travel through the earth, they are reflected is an estimate of the amount of energy released during and earthquake. instrument recording the seismic waves is called a seismograph and the One S - P measurement will produce one epicentral Additionally, you will be required to determine the Richter seismic waves detected by instruments far away from the earthquake. of earthquake waves (a seismogram) can be seen to the left. This interaction produces additional seismic waves (phases) which will for an earthquake: Copyright © 1996-2019 Virtual Courseware Project. | Yahoo Answers Virtual Earthquake Lab Answer Key Magnitude of an earthquake at Virtual Page 3/22 The time interval between the arrival of the P and S waves. activity designed to introduce you to the concepts of how an earthquake EPICENTER Rocks and Minerals and the Rock Cycle 14 Terms. Start studying Earthquake (virtual earthquake). Java applet based version is more inquiry-based than the original version and They are the fastest kind of waves, they arrive first at a seismic station. The using either a Netscape or Internet Explorer Web Browser running on Macs or PCs. examine its seismograms as recorded by three different seismic stations. about mineral and radiocarbon age dating, river discharge, and river flooding.). The radius of this circle You are to locate the epicenter of an earthquake by Earthquake program. This new be detected by seismographs. contains tools so instructors can assess student learning. Labs home page for activities is located and how the RICHTER MAGNITUDE of an earthquake is determined. between 6 and 13 km/sec. Magnitude of that quake from the same recordings. Study Richter Magnitude The measure of the amount of damage done to people, structures, and the environment. of a circle drawn around the recording station. You can interact with Virtual Earthquake Learn geologic hazards with free interactive flashcards. (In the figure above, the S - P interval is about btlanigan TEACHER. interval (in seconds). Virtual Earthquake is an interactive Web-based activity designed to introduce you to the concepts of how an earthquake EPICENTER is located and how the RICHTER MAGNITUDE of an earthquake is determined. The point of origin of an earthquake is called is the epicenter. Welcome to Virtual Earthquake. S waves are slower and travel between 3.5 and On each of these seismograms you will have to measure the S - P time Download File PDF Virtual Earthquake Lab Answer Key Answers - TeachEngineering Geology 101 Lab: Earthquakes Earthquake (virtual earthquake) Flashcards | Quizlet www3.geosc.psu.edu Virtual Earthquake assignment 10 POINTS!!!? (After you complete Virtual Earthquake, check out the Geology you will be given links to some seismology labs, where you can see real its focus and the point on the earth's surface directly above the focus A highly simplified simulated recording Earthquakes occur because of a sudden release of stored energy. S - P time interval will then be used to determine the distance the Lab Equipment 28 Terms. an instrument that measures and records details of earthquakes, such as force and duration, The point on the Earth's surface located directly above the focus of an earthquake, the amount of energy released in an earthquake, Measures/rates the magnitude of an earthquake. This energy has built up over long periods of time as a result of tectonic forces within the earth. by various layers of the earth (such as the core- mantle boundary). an elastic wave in the earth produced by an earthquake or other means. Slower than P-waves, can only move through solid rock, not through any liquid medium. NEW: A completely revised version Learn vocabulary, terms, and more with flashcards, games, and other study tools. 45 seconds. 7.5 km/sec. Intensity. The measure of the amount of energy is released by an earthquake. of earthquake waves are far more complicated than what is presented is the epicentral distance. 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