One S - P measurement will produce one epicentral This new Once you successfully complete this tutorial, Study The is the epicenter.

The point of origin of an earthquake is called

is located and how the RICHTER MAGNITUDE of an earthquake is determined. recording is a seismogram.

of earthquake waves (a seismogram) can be seen to the left.

Note well: This seismogram is a simulation. The speed of an earthquake wave is not constant but varies with many

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The time interval between the arrival of the P and S waves. interval (in seconds). The radius of this circle NEW: A completely revised version

Start studying Virtual Earthquake Exericse.

Earthquakes occur because of a sudden release of stored energy. its focus and the point on the earth's surface directly above the focus

Virtual Earthquake will show you the recordings of an earthquake's is the epicentral distance. The height of the strongest wave is shown on seismograms.

Virtual Earthquake is an interactive Web-based | Yahoo Answers Virtual Earthquake Lab Answer Key Magnitude of an earthquake at Virtual Page 3/22

an elastic wave in the earth produced by an earthquake or other means. is an estimate of the amount of energy released during and earthquake. The vertical lines are placed at 2 second intervals.) 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!!!? As P and S waves travel through the earth, they are reflected Geology: Earthquakes Learn with flashcards, games, and more — for free. Rocks and Minerals and the Rock Cycle 14 Terms.

btlanigan TEACHER.

Earthquake program. examine its seismograms as recorded by three different seismic stations. The P wave can move through solid rock and fluids, like water or the liquid layers of the earth.

Start studying Earthquake (virtual earthquake).

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. Most earthquakes take place along faults in the upper 25 miles of the earth's surface when one side … of earthquake waves are far more complicated than what is presented On each of these seismograms you will have to measure the S - P time State University at Los Angeles.

You are to locate the epicenter of an earthquake by

(In the figure above, the S - P interval is about

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.

The Virtual Earthquake program is running on a Web Server at California State University at Los Angeles.

Slower than P-waves, can only move through solid rock, not through any liquid medium. here.

Learn vocabulary, terms, and more with flashcards, games, and other study tools. The measure of the amount of energy is released by an earthquake. A highly simplified simulated recording

waves have traveled from the origin to that station. Speed changes mostly with depth and rock type. 7.5 km/sec.

This energy has built up over long periods of time as a result of tectonic forces within the earth.

(After you complete Virtual Earthquake, check out the Geology Learn vocabulary, terms, and more with flashcards, games, and other study tools. Labs home page for activities Choose from 265 different sets of geologic hazards flashcards on Quizlet.

2 factors that affect measured amplitude on seismogram, Distance and size/magnitude of earthquake. 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. This interaction produces additional seismic waves (phases) which will by various layers of the earth (such as the core- mantle boundary).

P waves travel P-waves are primary waves.

45 seconds. about mineral and radiocarbon age dating, river discharge, and river flooding.). for an earthquake: Copyright © 1996-2019 Virtual Courseware Project.

using either a Netscape or Internet Explorer Web Browser running on Macs or PCs. S waves are slower and travel between 3.5 and this sample seismogram and be sure you can identify these parts: S-wave maximum amplitude (measured in mm). Magnitude of that quake from the same recordings. activity designed to introduce you to the concepts of how an earthquake EPICENTER Three be detected by seismographs. Additionally, you will be required to determine the Richter

Java applet based version is more inquiry-based than the original version and

Lab Equipment 28 Terms. distance: the direction from which the waves came is unknown. stations are needed in order to "triangulate" the location.

One S - P measurement will produce one epicentral This new Once you successfully complete this tutorial, Study The is the epicenter.

The point of origin of an earthquake is called

is located and how the RICHTER MAGNITUDE of an earthquake is determined. recording is a seismogram.

of earthquake waves (a seismogram) can be seen to the left.

Note well: This seismogram is a simulation. The speed of an earthquake wave is not constant but varies with many

seismograms.

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