Finding the Finding the EpicenterEpicenter

……I hope you I hope you really like graphs!really like graphs!

Event of an Earthquake RecapEvent of an Earthquake Recap

The Epicenter is the spot on theground directly above where the

earthquake occurred under the ground

When an earthquake occurs, it sends out seismic wave energy in all directions. There When an earthquake occurs, it sends out seismic wave energy in all directions. There are three main waves that form: P-Waves, S-Waves and Surface Waves. Eachare three main waves that form: P-Waves, S-Waves and Surface Waves. EachWave moves the ground differently (as the picture shows above). The P wavesWave moves the ground differently (as the picture shows above). The P waves

always move fastest, then the S-waves and last is the Surface waves. Surfaces waves always move fastest, then the S-waves and last is the Surface waves. Surfaces waves are so slow because they only travel on the surface of the planet but P & S waves can are so slow because they only travel on the surface of the planet but P & S waves can

go right through the middle making their distance/time shorter.go right through the middle making their distance/time shorter.

How a seismograph worksA seismograph is a machine that makes up and down wave lines on a moving paper as the ground moves under the machine. The more the ground moves, the

more the paper moves. The more the paper moves, the bigger the up-down lines will be drawn. The

seismograph shows the three different seismic waves generated by an earthquake.

This chart shows that there are multipleSeismograph stations around the world that

will measure an earthquake when the Seismic wave energy passes by. The fartheraway a station is the longer the actual graph

will be and the shorter the waves will bedrawn. But we are able to make

measurements from the information on thegraph to tell how far away an earthquake

came from.

A station cannot tell the direction an earthquake came from, but if we use the info from A station cannot tell the direction an earthquake came from, but if we use the info from multiple stations, we can pinpoint the actual location of the quake. They draw a circle multiple stations, we can pinpoint the actual location of the quake. They draw a circle with a diameter equal to the distance away an earth was measured to be. All 3 circles with a diameter equal to the distance away an earth was measured to be. All 3 circles will only meet at one exact spot on a map. This spot is the location of the Earthquake!will only meet at one exact spot on a map. This spot is the location of the Earthquake!

Finding Finding MagnitudeMagnitude

Earthquakes are measured by “Magnitude” which measures how “large” the quake is. Basically, the larger the “squiggle” in the seismogram, the greater the magnitude.Once you know the distance from an earthquake, and the amplitude of the seismogram, you can find the magnitude!

As we go up in magnitude, the amount of energy released dramatically increases!Look at this chart of magnitude and how the energy released can be compared…the greater the magnitude of the quake, the more potential damage it can do.

The biggest possible earthquake we can conceive of is measured at a magnitude of10! The biggest we have recorded are in the 9.4 range. These are very rare!