http://siovizcenter.ucsd.edu/library/TLTC/TLTCmag.htm

**Materials:**

- a frames- and layers-capable browser

- explanation page for the
interactive portion of the activity

- the interactive Richter Scale page (new version here)

- [
*for browsers without frames and layers support*] the Richter Scale print-out page

**Procedure:**

In this activity, you will have the chance to find the Richter magnitude of several earthquakes through the use of an online activity that utilizes frames and layers. If your browser does not support these features, but you do have access to a printer, you can try the alternate exercise, which covers the same material.

Charles Richter is credited with publishing the first method for
assigning a numerical value to an earthquake to represent its
energy. On the suggestion of Harry O. Wood, he called this numerical
value "**magnitude**"; it is generally given to a single
decimal place, an written with a capital **M** (an abbreviation
for magnitude) preceeding it. Determining the magnitude of an earthquake
by Richter's method requires one to inspect a seismogram and
find the difference in time between the P-wave and S-wave arrivals,
as well as the maximum amplitude of the trace deflection on that
same seismogram. Using these two values, and a conversion table
based upon a graph (seen at right) that Richter created from empirical
data, it was possible to calculate the **Richter magnitude**
of an earthquake.

To find the Richter magnitude of an earthquake using this online activity, you will also need a seismogram to work with. There are several different earthquakes to work on, each represented by a single seismogram. Clicking on one of these events in the list at top will bring up that seismogram in another frame. You will see three arrows superimposed on this seismogram.

Your job is to drag these arrows into positions that mark
three specific points: the arrival of the P wave (the red arrow),
the arrival of the S wave (the blue arrow), and the maximum
amplitude shown on that seismogram (the green arrow). Once you
have dragged these arrows into position, you will need to lock
them there, using an obviously-labelled ("Lock Arrows") button. This
will bring up a display showing the numerical values that correspond
to your selections. It also readies the computer to calculate the
Richter magnitude for this earthquake. By clicking on another button,
this one labelled "Compute Magnitude," you tell the computer to find
the Richter magnitude of the earthquake, and display it on the
screen. It will do this graphically, using the **nomograph**
at the bottom of the screen. Record these answers on your own
sheet of paper to compare them to an answer key later.

Full descriptions of each of the frames and features of this activity are given on an explanation page. Though it may not be absolutely vital for completing the activity (the controls are mainly self-explanatory), you should read through this explanation page if you want to understand all of what is going on "behind the scenes".

Go now to the explanation page, or start the online Richter Scale activity!

Your print-out should have three main sections. The uppermost is the title -- "Activity #4: The Richter Scale." Below this is a rectangular area containing a portion of a seismogram of a real earthquake recorded in southern California. The time scale of this seismogram is given directly beneath the rectangle; marks on the rectangle's borders correspond to these numbers, which give hours, minutes, and seconds. Below the seismogram is the third section of the print-out: the Richter Scale nomograph. This graph is name up of three scale bars, labelled below each. The nomograph allows you to find the Richter magnitude of an earthquake by connecting the points that represent two other values (arrival-time difference and maximum amplitude) with a straight line. The point where that line intersects the third and middle scale corresponds to the Richter magnitude of the earthquake.

Just as with the online activity, to find the Richter magnitude
you will need to choose three positions on the seismogram:
the two wave arrivals (P and S),
and the maximum trace deflection, or **amplitude**.

Use what you've learned from Section 3 to select the locations of the P-wave and S-wave arrivals on the waveform recorded within the seismogram rectangle. Remember that the P-wave arrival is the first point (going from left to right) at which the trace deflects from a "resting" position (generally a flat line), and that the S-wave arrival is typically marked by an obvious increase in amplitude and/or an increase in the wavelength of the "wiggles" in the waveform trace. Once you have decided where these arrivals occur, mark them with vertical lines on your paper, making sure they intersect with the borders of the rectangle.

Now translate the points of intersection of the arrival lines into times, using the numerical time scale given just below the seismogram. Estimate these times to the nearest tenth of a second. Subtract the P-wave arrival time from the S-wave arrival time to find the difference in the travel times of these waves, in seconds. Plot this value on the left-hand scale of the nomograph at the bottom of the printed page. Note that this scale is not linear. It is based upon the empirically-derived graph (shown at right) that Richter created from a sample data set of earthquakes in southern California during January 1932.

Next, find the maximum amplitude for this waveform. This is the point on the waveform where the trace is at its greatest distance from the position of rest -- a horizontal line running across the center of the seismogram. It is clearly marked by the flat trace at the left side of the seismogram, before the P wave arrives. Draw a horizontal line through this point of maximum trace deflection, parallel to the top and bottom edges of the seismogram rectangle. Then, using a metric ruler, measure the separation between the line you drew and the line marking the "resting" position of the trace. This distance is the amplitude. Mark this value on the right-hand scale of the nomograph on your print-out. Note that this amplitude scale is logarithmic, not linear, and plot accordingly.

With a point plotted on each side of the nomograph, you are ready to draw a line connecting them. Do this now.

Find the point at which your line intersects the center scale
of the nomograph, labelled "RICHTER MAGNITUDE." Given that
this scale is strictly linear, read off the value of this
point of intersection. This value is the Richter magnitude
of the earthquake recorded on the seismogram; you've
completed the exercise! Now work through the questions
below, ignoring those that focus exclusively upon the online
version of this activity -- the rest are still applicable.

- If you kept track of the magnitudes you
determined for each of these earthquakes, you can now compare
them to this list of magnitudes
determined using the same data and methods.
- Do your results compare favorably to this
list?

- Do your results compare favorably to this
list?
- Which of the arrows -- P, S, or amplitude -- did you feel
was the most difficult to position accurately? (i.e. The position
of which arrow was likely the greatest source of error in
the calculations made to find magnitude?)

- Where in these waveforms did the maximum amplitudes -- the
greatest deflection of the trace from its "resting" position --
tend to occur?
- Does that bode well for a person's chances to take shelter
after they feel the first shaking of an earthquake, but before the
most severe (and damaging) shaking strikes?

- Does that bode well for a person's chances to take shelter
after they feel the first shaking of an earthquake, but before the
most severe (and damaging) shaking strikes?
- The stylus on a standard recording drum used to create
paper seismograms has a maximum lateral range of motion of about
110 mm (55 mm to either side of its "resting" position),
meaning it will "pin" (be unable to move any farther laterally)
for an earthquake that generates a maximum trace deflection of 55 mm
or greater at that particular seismometer. Event #2 in this activity
was of magnitude 5.3 and had a maximum amplitude three times that
size (possible because it was recorded digitally, not on paper,
as was done when the Richter magnitude scale was created)!
- Imagine what would happen if a large earthquake struck
near your small network of seismometers and "pinned" the stylus on
every one of the seismographs creating records of the event;
would you be able to find a Richter magnitude for such an earthquake?

- What are some possible solutions to such a problem?

- Imagine what would happen if a large earthquake struck
near your small network of seismometers and "pinned" the stylus on
every one of the seismographs creating records of the event;
would you be able to find a Richter magnitude for such an earthquake?