1. Chapter 8 Earthquakes

2. I. What are Earthquakes? Seismology is the science devoted to studying earthquakes Most take place near the edges of tectonic plates Earthquakes are caused by elastic deformation Rocks stretch to a certain point and then suddenly return to its original shape in elastic rebound Energy is released and some of this energy travels as seismic waves that cause earthquakes

3. A. Faults at Tectonic Plate Boundaries A specific type of motion takes place at different tectonic plate boundaries Each motion creates a particular kind of fault - Transform  strike-slip fault - Convergent  reverse fault - Divergent  normal fault

4. 1. Earthquake Zones Places where a large number of faults are located Some earthquakes however happen along faults in the middle of tectonic plates

5. B. How do Earthquake Waves Travel? Seismic waves that travel through the Earth’s interior are called body waves - P waves - S waves Seismic waves that travel along the Earth’s surface are called surface waves

6. 1. P Waves (primary waves) Travel through solids, liquids, and gases Fastest waves; travel ahead of other seismic waves Move rock back and forth, squeezing and stretching the rock

7. 2. S Waves (sear, or secondary waves) Cannot travel through parts of the Earth that are completely liquid Second-fastest seismic waves Shear rock side to side

8. 3. Surface Waves Produce motion mostly in the upper few kilometers of Earth’s crust Travel more slowly and are more destructive Produces motion up, down, and around or back-and-forth

9. II. Earthquake Measurement A. Locating Earthquakes Seismographs are instruments located at or near the surface of the Earth that record seismic waves When the waves reach a seismograph, the seismograph creates a seismogram

10. 1. Determining Time and Location of Earthquakes The start time is determined by comparing seismograms and noting the differences in arrival times of P and S waves Seismograms are also used to find the earthquake’s epicenter - An epicenter is the point on the Earth’s surface directly above an earthquake’s starting point

11. A focus is the point inside the Earth where an earthquake begins

12. 2. The S-P Time Method Seismograms from different locations are compared Seismograms are placed on a time-distance graph The horizontal axis tells the distance between a station and the earthquake’s epicenter

13. A circle is drawn around three seismograph stations with the radius of the circle coming from the horizontal axis of the time-distance graph The point where all three circles intersects is the earthquake’s epicenter

14. B. Measuring Earthquake Strength and Intensity 1. The Richter Magnitude Scale Charles Richter created the scale in the 1930s Compares earthquake’s by measuring ground motion recorded by seismograms

15. 2. Earthquake Ground Motion Magnitude is a measure of the strength of an earthquake Magnitude values are from 2 to 7 Each time the magnitude increases by one unit, the measured ground motion becomes 10 times larger Ex) Magnitude of 5 is 10x greater than magnitude of 4 and 100x greater than magnitude of 3

16. 3. Modified Mercalli Intensity Scale Intensity is a measure of the degree to which an earthquake is felt by people and the amount of damage Scale of Roman numerals from I to XII - An earthquake not felt by people to total damage of an area Intensity values are usually higher near an earthquake’s epicenter

17. III. Earthquakes and Society A. Earthquake Hazard A measure of how likely an area is to have damaging earthquakes in the future The West Coast has a high earthquake- hazard level because it has a lot of seismic activity

18. B. Earthquake Forecasting 1. Strength and Frequency Strength of earthquakes is related to how often they occur

19. 2. The Gap Hypothesis A hypothesis that states that sections of active faults that have had relatively few earthquakes are likely to be the sites of strong earthquakes in the future The areas along a fault where relatively few earthquakes have occurred are called seismic gaps

20. C. Earthquakes and Buildings The process of making older structures more earthquake resistant is called retrofitting - Securely fastening buildings to their foundation - Steel can be used to strengthen structures made of brick Architects and engineers use the newest technology to design and construct buildings and bridges to better withstand earthquakes