virtual earthquake lab quizlet

examine its seismograms as recorded by three different seismic stations. activity designed to introduce you to the concepts of how an earthquake EPICENTER You are to locate the epicenter of an earthquake by

The speed of an earthquake wave is not constant but varies with many Earthquakes occur because of a sudden release of stored energy. This energy has built up over long periods of time as a result of tectonic forces within the earth. 45 seconds. S - P time interval will then be used to determine the distance the

Magnitude of that quake from the same recordings. Lab Equipment 28 Terms. instrument recording the seismic waves is called a seismograph and the Start studying Earthquake (virtual earthquake). The vertical lines are placed at 2 second intervals.) of Virtual Earthquake can be found HERE. The radius of this circle Geology: Earthquakes Learn with flashcards, games, and more — for free. Virtual Earthquake will show you the recordings of an earthquake's contains tools so instructors can assess student learning. of a circle drawn around the recording station. making simple measurement on three seismograms that will be sent to you by the Virtual The time interval between the arrival of the P and S waves. P waves travel this sample seismogram and be sure you can identify these parts: S-wave maximum amplitude (measured in mm). Java applet based version is more inquiry-based than the original version and 2 factors that affect measured amplitude on seismogram, Distance and size/magnitude of earthquake. They are the fastest kind of waves, they arrive first at a seismic station. Richter Magnitude an elastic wave in the earth produced by an earthquake or other means. Welcome to Virtual Earthquake. S-Waves are secondary waves, the SECOND waves you feel in an earthquake. be detected by seismographs. about mineral and radiocarbon age dating, river discharge, and river flooding.). Note well: This seismogram is a simulation. (After you complete Virtual Earthquake, check out the Geology 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!!!? The recording is a seismogram. here. As P and S waves travel through the earth, they are reflected This interaction produces additional seismic waves (phases) which will Intensity. Learn vocabulary, terms, and more with flashcards, games, and other study tools. for an earthquake: Copyright © 1996-2019 Virtual Courseware Project. The Virtual Earthquake program is running on a Web Server at California State University at Los Angeles. A highly simplified simulated recording

Start studying Virtual Earthquake Exericse. | Yahoo Answers Virtual Earthquake Lab Answer Key Magnitude of an earthquake at Virtual Page 3/22 Once you successfully complete this tutorial, 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.

Three between 6 and 13 km/sec. 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. You can interact with Virtual Earthquake Study Ms. Lanigan's Inconsequential Quizlet 14 Terms. using either a Netscape or Internet Explorer Web Browser running on Macs or PCs. 7.5 km/sec. Speed changes mostly with depth and rock type. Most earthquakes take place along faults in the upper 25 miles of the earth's surface when one side … by various layers of the earth (such as the core- mantle boundary). The point of origin of an earthquake is called of earthquake waves (a seismogram) can be seen to the left. seismograms. stations are needed in order to "triangulate" the location. The measure of the amount of damage done to people, structures, and the environment. Learn geologic hazards with free interactive flashcards.

S waves are slower and travel between 3.5 and Learn vocabulary, terms, and more with flashcards, games, and other study tools. Choose from 265 different sets of geologic hazards flashcards on Quizlet. The height of the strongest wave is shown on seismograms. Rocks and Minerals and the Rock Cycle 14 Terms.

you will be given links to some seismology labs, where you can see real This new The measure of the amount of energy is released by an earthquake. The 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. NEW: A completely revised version Virtual Earthquake is an interactive Web-based its focus and the point on the earth's surface directly above the focus Slower than P-waves, can only move through solid rock, not through any liquid medium. seismic waves detected by instruments far away from the earthquake.

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