1. Seismic Waves Chapter 15.4

2. Types of Seismic Waves Earthquakes occur when rocks beneath the Earth’s surface move When pressure in the rock builds up because of forces found deep inside the Earth the rock breaks or changes shape, which releases energy in the form of waves These waves are seismic waves, which are the waves produced by earthquakes – Seismic waves include P waves, S waves, and surface waves – These waves ripple out in all directions from the point where the earthquake occurred and can travel from one side of the Earth to the other

3. P Waves P waves, also known as primary waves, are longitudinal seismic waves They are called primary waves because they travel faster than other seismic waves and therefore arrive at distant points before other seismic waves P waves are made up of refractions and compressions of the rock inside Earth P waves compress and expand the ground as they move through it

4. S Waves S waves (secondary waves) are transverse seismic waves with crests and troughs S waves shake the ground up and down and side to side as they move through it S waves CANNOT travel through liquid – Since part of the Earth’s core is made of liquid S waves do not travel directly through the Earth like P waves – Therefore, S waves CANNOT be detected on the side of the Earth opposite of the Earthquake

5. Surface Waves When P waves and S waves reach the Earth’s surface they can create surface waves A surface wave is a combination of longitudinal and transverse waves that travels along the surface of a medium Surface waves move more slowly than P and S waves Surface waves cause more severe ground movements than P and S waves because they combine up and down and side to side motions that can make the ground roll like ocean waves

6. Surface Waves that Occur Underwater Earthquakes that occur underwater can produce huge surface waves on the ocean called Tsunamis – Tsunamis come in all sizes from 2 cm to 30 meters tall – Tsunamis can travel thousands of kilometers – In the deep oceans waves that cause tsunamis may begin at 1 meter high, but as they near land the tsunamis slow down in shallow waters to allow the waves in the back to catch up with the waves in the front and pile on

7. Detecting Seismic waves To detect and measure earthquake waves scientists use seismographs A seismograph records the ground movements caused by seismic waves as they move through the earth – The frame of the seismograph is attached to the ground, so the frame shakes when seismic waves arrive – Seismographs use to have pens attached to the frame that would wiggle back and forth on a roll of paper as the ground shook, but now electronic seismographs are used P waves arrive at the seismograph first followed by slower moving S waves – Scientists can tell how far away the earthquake was by measuring the time of arrival between P and S waves – Scientists can tell where an earthquake occurred by using three seismographs at three different locations

8. Seismographs Seismographs can be used to find valuable resources such as water and oil Geologists will set off explosives at the Earth’s surface Seismic waves from the explosions reflect from structures underground Seismographs are then used to locate the underground resources

9. Research Report: You and a Partner will write an article for a boating magazine about tsunamis Include: Details about what causes tsunamis, why they are dangerous, and explain what is being done to reduce damage from tsunamis Also include pictures You may use Macs and your book for research You will have today and tomorrow to finish – When you are done share it as a Google doc with kajarikl@gmail.com kajarikl@gmail.com