Exercises

Question 13.1

Seismographic stations report the following S-wave–P-wave arrival time intervals for an earthquake: Dallas, S-P 5 3 minutes; Los Angeles, S-P 5 2 minutes; San Francisco, S-P 5 2 minutes. Use a map of the United States and the travel-time curves in Figure 13.9 to obtain a rough location for the epicenter of the earthquake.

Question 13.2

Describe two scales for measuring the size of an earthquake. Which is the more appropriate scale for measuring the amount of faulting that caused the earthquake? Which is more appropriate for measuring the amount of shaking experienced by a particular observer?

Question 13.3

How much more energy is released by a magnitude 7.5 earthquake than by a magnitude 6.5 earthquake?

Question 13.4

In Southern California, a magnitude 5 earthquake occurs about once per year. Approximately how many magnitude 4 earthquakes would you expect each year? How many magnitude 2 earthquakes?

Question 13.5

What are the fault mechanisms of earthquakes at the three types of plate boundaries?

Question 13.6

Destructive earthquakes occasionally occur within lithospheric plates, far from plate boundaries. Why?

Question 13.7

At a location along the boundary between the Nazca Plate and the South American Plate, the relative plate movement is 80 mm/year. The last large earthquake there, in 1880, showed a fault slip of 12 m. Should local residents begin to worry about another large earthquake?