Chapter 8.1/8.2

 Earthquake – a vibration of the Earth produced by a rapid release of energy.  Most often caused by slippage along a TRANSFORM FAULT boundary.

 When the fault “snaps”... Energy travels out from the focus in waves like ripples in water.  Waves travel in ALL directions  P waves, S waves, Surface waves

 Two types – BODY waves and SURFACE waves BODY WAVES – waves that travel through the Earth’s interior. BODY WAVES – waves that travel through the Earth’s interior. Two kinds: P-waves and S-waves. Two kinds: P-waves and S-waves.  P-waves (push-pull waves)  Move things forward and back  S-waves (shake waves)  Move things up and down

Seismic Wave Motion with Surface Effects

 Surface Waves – waves that travel along the Earth’s surface Surface waves travel up and down AND side to side AT THE SAME TIME! Surface waves travel up and down AND side to side AT THE SAME TIME!  Surface waves are the MOST DESTRUCTIVE of all the seismic waves

Seismic Wave Motion Seismic Wave Motion

Epicenter: point on surface above earthquake focus

 Elastic Rebound Hypothesis 1. As two plates are sliding past each other, they get STUCK and stop moving. 1. As two plates are sliding past each other, they get STUCK and stop moving. 2. The convection current below DOES NOT STOP, so pressure builds up under the crust. 2. The convection current below DOES NOT STOP, so pressure builds up under the crust. 3. When TOO MUCH pressure has built up the crust plates shift rapidly to release 3. When TOO MUCH pressure has built up the crust plates shift rapidly to release the pressure. This is an EARTHQUAKE! This is an EARTHQUAKE!

 Foreshocks – small earthquakes that come days, weeks or even years before the MAIN quake.  Aftershocks – small earthquakes that follow a MAIN quake.  Aftershocks can cause MAJOR damage (even though they are smaller than the MAIN quake) because the main quake has already weakened all the structures.

 Seismology – the study of earthquake waves Has been going on for almost 2000 years Has been going on for almost 2000 years  Seismograph – the instrument used to measure the strength of an earthquake

 The machine is attached to the Earth  The Earth moves during an earthquake – moving the machine as well.  The hanging weight DOES NOT MOVE!!  Attached to the weight is a pen.  As the paper moves back and forth with the machine, the pen marks the paper, recording the strength of the seismic waves. OKn7kWXM&feature=endscreen&NR=1 OKn7kWXM&feature=endscreen&NR=1

Seismograph Used to measure Seismic Waves

 In order from FASTEST to SLOWEST P-waves(PRIMARY – first) P-waves(PRIMARY – first) S-waves(SECONDARY – second) S-waves(SECONDARY – second) Surface waves(last) Surface waves(last)  The difference in wave speeds give us the information to determine two important measurements: 1. How far away from the seismograph the earthquake is 1. How far away from the seismograph the earthquake is 2. Where the epicenter of the earthquake is 2. Where the epicenter of the earthquake is

 The paper print out from the seismograph  Shows the arrival times of P-waves, S- waves and Surface waves

 November 10, 2010

 How to calculate distance 1. Read seismogram to determine the time interval between 1 st P-wave and 1 st S-wave 1. Read seismogram to determine the time interval between 1 st P-wave and 1 st S-wave 5 minutes 5 minutes

 2. Find on the time-travel graph where 5 minutes is the interval  3. Travel to the X-axis, this is the earthquake distance You now know how far away from the seismograph the from the seismograph the epicenter is. But you DO NOT know the DIRECTION Could be North, South, East or West How do you locate EXACT location of epicenter?

1. Determine the distance from 3 different seismographs 2. Draw circles that have a radius of that distance 3. The ONE PLACE that all 3 circles touch is the epicenter