Essay/Short Answer Problems
The crust of the earth when it is subject to tectonic
forces, bends slightly. But, because the crust is rigid, when the stress
or pressure exceeds the strength of the rocks, the crust breaks and snaps
into a new position. Vibrations called seismic waves are generated and
travel both through the earth and along its surface. These seismic waves
cause the movement we call earthquakes.
4. What are some ways you could suggest to make buildings safer during earthquakes?
There is no known way to prevent earthquakes,
but it is possible to lessen the impact. The amount of devastation from
an earthquake can be greatly diminished by building structures using earthquake
resistant design, making the interiors of buildings safe from falling objects,
and educating people about earthquake safety.
5. How is location of earthquakes similar to triangulation? What other physical features are often measured by triangulation?
Given a single seismic station, the seismogram records will yield a measurement of the S-P time, and thus the distance between the station and the event. Multiply the seconds of S-P time by 8 km/s for the kilometers of distance. Drawing a circle on a map around the station's location, with a radius equal to the distance, shows all possible locations for the event. With the S-P time from a second station, the circle around that station will narrow the possible locations down to two points. It is only with a third station's S-P time that you can draw a third circle that should identify which of the two previous possible points is the real one.