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Investigating Earthquakes

Spinning globe

Learner Outcomes
By completing these activities, the learner will:


Exploration
 
Location of earthquakes around the world Earthquakes occur all over the world. The vast majority are too weak to be felt; but they can be measured using seismographs. 

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National Map of Earthquakes Recorded in the Last 14 Days
US map of earthquakes recorded in the last two weeks
As you can see, most of the earthquakes occuring in the US are in the western portion. This includes:
PacificNorthwest(Washington & Oregon) Montana Washington 
California Yellowstone National Park Alaska (Another Alaska Map)
California and Nevada Utah Hawaii (Island of Hawaii)
Another California  site Wyoming and  Idaho Colorado

Although major earthquakes are infrequent, there are also active regions in southeastern Canada and in the MississippiValley.

More Earthquake Maps on the Web
Seismo-surfing the Internet


Seismograph

Concept Introduction

1. Seismographs are used to measure the magnitude of an earthquake. This is done by measuring the amount of ground movement. The output of a seismograph is a seismogram. Current seismograms can be seen in Los Angeles, CA, Reno, NV, and Orange County, CA.

The three most important parts of a seismogram are:

The difference in arrival times indicates how far away the epicenter is located. This is because P-waves propogate through the Earth much faster than S-waves propogate. Note the first P-wave arrival and the first S-wave arrival as shown on the seismogram below. (Make your own seismogram by clicking here).
P-wave and S-wave seismogram

2. Earthquake epicenters are pinponted by at least three stations calculating radial distance.

Locating EarthquakesDetermine the location of a "virtual" earthquake.

3. The shape of the amplitude disturbance also indicates the type of earthquake. Underground nuclear tests can also be monitored in this way.

Four types of seismograms


Concept Application



Assessment

Extensions