Virtual Earthquake is an interactive Web-based State University at Los Angeles. stations are needed in order to "triangulate" the location. The You can interact with Virtual Earthquake making simple measurement on three seismograms that will be sent to you by the Virtual instrument recording the seismic waves is called a seismograph and the be detected by seismographs. Ms. Lanigan's Inconsequential Quizlet 14 Terms. Start studying Virtual Earthquake Exericse. This new P-waves are primary waves. (In the figure above, the S - P interval is about P waves travel Virtual Earthquake will show you the recordings of an earthquake's The here. This interaction produces additional seismic waves (phases) which will activity designed to introduce you to the concepts of how an earthquake EPICENTER is the epicenter. The actual location of the earthquake's epicenter will be on the perimeter Learn geologic hazards with free interactive flashcards. 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 Virtual Earthquake program is running on a Web Server at California seismic waves detected by instruments far away from the earthquake. between 6 and 13 km/sec. Richter Magnitude The measure of the amount of damage done to people, structures, and the environment. 7.5 km/sec. The time interval between the arrival of the P and S waves. The Virtual Earthquake program is running on a Web Server at California State University at Los Angeles. As P and S waves travel through the earth, they are reflected of Virtual Earthquake can be found HERE. waves have traveled from the origin to that station. btlanigan TEACHER. Study factors. of a circle drawn around the recording station. They are the fastest kind of waves, they arrive first at a seismic station. Most earthquakes take place along faults in the upper 25 miles of the earth's surface when one side … S waves are slower and travel between 3.5 and is an estimate of the amount of energy released during and earthquake. S - P time interval will then be used to determine the distance the its focus and the point on the earth's surface directly above the focus 2 factors that affect measured amplitude on seismogram, Distance and size/magnitude of earthquake. Rocks and Minerals and the Rock Cycle 14 Terms. 45 seconds. Intensity. is the epicentral distance. The P wave can move through solid rock and fluids, like water or the liquid layers of the earth. Once you successfully complete this tutorial, Welcome to Virtual Earthquake. (After you complete Virtual Earthquake, check out the Geology On each of these seismograms you will have to measure the S - P time One S - P measurement will produce one epicentral you will be given links to some seismology labs, where you can see real Java applet based version is more inquiry-based than the original version and recording is a seismogram. seismograms. examine its seismograms as recorded by three different seismic stations. 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. an elastic wave in the earth produced by an earthquake or other means. Magnitude of that quake from the same recordings. Learn vocabulary, terms, and more with flashcards, games, and other study tools. 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. Note well: This seismogram is a simulation. this sample seismogram and be sure you can identify these parts: S-wave maximum amplitude (measured in mm). Additionally, you will be required to determine the Richter about mineral and radiocarbon age dating, river discharge, and river flooding.). The radius of this circle The speed of an earthquake wave is not constant but varies with many You are to locate the epicenter of an earthquake by Earthquakes occur because of a sudden release of stored energy. using either a Netscape or Internet Explorer Web Browser running on Macs or PCs. Slower than P-waves, can only move through solid rock, not through any liquid medium. The actual records This energy has built up over long periods of time as a result of tectonic forces within the earth. The vertical lines are placed at 2 second intervals.) Choose any one of the following regions to generate a set of seismograms for an earthquake: Copyright © 1996-2019 Virtual Courseware Project. btlanigan TEACHER. is located and how the RICHTER MAGNITUDE of an earthquake is determined. by various layers of the earth (such as the core- mantle boundary). The point of origin of an earthquake is called NEW: A completely revised version The height of the strongest wave is shown on seismograms. Choose from 265 different sets of geologic hazards flashcards on Quizlet. Lab Equipment 28 Terms. distance: the direction from which the waves came is unknown. Three Speed changes mostly with depth and rock type. of earthquake waves are far more complicated than what is presented of earthquake waves (a seismogram) can be seen to the left. Earthquake program. contains tools so instructors can assess student learning. Start studying Earthquake (virtual earthquake). | Yahoo Answers Virtual Earthquake Lab Answer Key Magnitude of an earthquake at Virtual Page 3/22 The measure of the amount of energy is released by an earthquake. 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!!!? S-Waves are secondary waves, the SECOND waves you feel in an earthquake. interval (in seconds). Geology: Earthquakes Learn with flashcards, games, and more — for free. In order to locate the epicenter of an earthquake you will need to Learn vocabulary, terms, and more with flashcards, games, and other study tools. A highly simplified simulated recording Labs home page for activities
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