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Download the CAS QL3 file Upload your responses to the questions as an assignment submission when they are complete. You have two weeks to complete this assignment.

The link in the file is not working now. Please use this link to get the website where you need to get the data.https://www.memphis.edu/ceri/research/index.phpExamining Earthquake History and Predicting Big Earthquakes

Building a house close to a fault is risky. But how do you estimate the risk? The likelihood of an earthquake

of a certain magnitude in any given year is determined using long-term earthquake records. The longer the

record, the more reliable are the predictions of the earthquake frequencies. Knowing the earthquake

frequencies or recurrence intervals helps us develop communities in earthquake-prone areas. For this

exercise, you will act as the geological consultant hired by the town of New Madrid to determine earthquake

frequencies and recurrence intervals of large earthquakes. You will collect data from the Center for

Earthquake Research and Information (CERI) that has been analyzing earthquake activity in the New

Madrid Seismic Zone and created a catalog of earthquakes since 1974. You will use these data to make

predictions regarding earthquake frequencies and recurrence intervals of large earthquakes. These are the

type of predictions made by geological consultants necessary for city planning and development. This

assignment is worth 30 points with point values indicated throughout the assignment.

A) Gathering the Data

1. First go to the Center for Earthquake Research and Information (CERI) website:

http://www.ceri.memphis.edu. Click on the Seismic Information on the left side of the webpage. In the

section entitled Seismic Information click on CERI Catalog. The resulting web form will allow you to

search for earthquakes based on their time, magnitude, and location. Time is the first option, and you will

examine data over a 35 year time frame by selecting 1975 for the Start Date Year, and 2010 for the End

Date Year. Location is the third option, and you should examine all events in the New Madrid region by

just choosing the RADIAL SEARCH and leaving the default values as is (Latitude: 35.15, Longitude: 90.05, Radius 500 km). The second option is the magnitude, and this is what you will have to adjust

several times to determine how frequent earthquakes of a certain size are.

2. To begin, choose Minimum Magnitude as 1.0 and Maximum magnitude as 1.9. Then click Begin

Search. On the Catalog Results Page, you will see the number of events selected at the top of the page.

You only need the first number, as it also lists a second number that is over 10,000 and simply indicates

the total number of all events in the entire catalog. You should enter the first number in the table below

in the first row and of the first column. You will then need to click the back button in your browser to

return to the Catalog Search Form. Enter the next magnitude range (2.0-2.9) and click to Begin Search

to find the number of events of that size and enter it into the table in the second column of the first row.

Repeat this process for each magnitude range in the table and enter the corresponding number of events

for each magnitude range in the first row. (5 points)

Magnitude

Range

Number of

Earthquakes

from 19752010

Number of

Earthquakes

per Year

Earthquake

Recurrence

Interval in

Years

1.0-1.9

2.0-2.9

3.0-3.9

4.0-4.9

5.0-5.9

6.0-6.9

7.0-7.9

You should find at least one magnitude range with no earthquakes over that 35 year time period. Does

this mean it is not possible for the New Madrid Seismic Zone to have earthquakes of that size? Why or

why not? (1 point)

B) Calculating Earthquake Frequency and Recurrence Intervals

1. Next you will need to calculate the number of earthquakes per year. The first row of our table has the

number of earthquakes between 1975 and 2010, so you need to convert this to the number of earthquakes

over one year. You can do this by dividing each number in the first row by the number of years (end

year minus begin year), and then put this newly calculated value in the second row of the table. Do this

only for magnitude ranges that do not have 0 earthquakes between 1975 and 2010. We will complete the

remainder of the second row in the table later when we figure out how to estimate the number of

earthquakes per year for cases with 0 earthquakes from 1975-2010. (5 points)

For which magnitude ranges do we expect to see at least one earthquake each year in the New Madrid

Seismic Zone? (1 point)

2. To complete your table, calculate the recurrence interval that is the average time interval between

earthquakes of a given magnitude range. This is important for city planners to know, on average, how

often earthquakes of a certain size will occur, and hence how likely infrastructure will need to withstand

an earthquake of that size. The recurrence interval is calculated by taking 1 divided by the number of

earthquakes per year. So for each magnitude range, calculate 1 divided by each number in the second

row of the table and place the newly calculated value in the third row of the table. (5 points)

Magnitude 5 earthquakes are considered important because they can be felt across several states in the

midcontinent and cause moderate damage to structures near the epicenter. How often does a magnitude

5 earthquake occur in the New Madrid Seismic Zone? (1 point)

C) Using Magnitude-Frequency Relationships to Estimate Large Earthquake Likelihood

1. Now plot the Number of Earthquakes per Year versus the Earthquake Magnitude on the graph below.

Note that the Y-axis is logarithmic and that X-axis values indicate the corresponding magnitude range

(e.g., 1 = 1.0-1.9, 2 = 2.0-2.9, etc.). You can use Excel to help you plot the points correctly. (4 points)

2. Researchers have determined that earthquakes follow a common phenomenon in nature called

universality that the likelihood of an event is proportional to the size of the event. Mathematically, this

relationship is called a power-law, which means we can only see the proportional relationship when the

values are plotted logarithmically. This why the Y-axis of our plot is logarithmic, and the X-axis is also

logarithmic because the magnitude value itself is a logarithmic expression for how big an earthquake is

(i.e., a magnitude 7 earthquake is essentially 10 times larger than a magnitude 6 earthquake). So after

plotting the data points on this logarithmic graph, you just need to draw a straight line of best fit through

the data points to establish the proportional relationship between frequency and magnitude for the New

Madrid Seismic Zone. This line is your predictor of the average behavior of the New Madrid faults and

how often they will produce earthquakes of different sizes based on the model of universality. When you

try to draw the straight line, you will find that the line will not go through the middle of every point, but

there will also be one point that is much further away from the trend established by the remaining points.

Go ahead a draw your line to ignore this point. (2 points)

Which magnitude range does this outlier point correspond too and why do you think this point does not

fit with the overall trend? (1 point)

3. Make sure your best fitting line extends (i.e., extrapolates) as far to the right and left as possible so we

can estimate frequency of earthquakes with very large magnitudes that did not occur during 1975-2010.

Based on this line, what is the number of earthquakes per year we should expect for magnitude 6.0-6.9?

(1 point)

Based on this line, what is the number of earthquakes per year we should expect for magnitude 7.0-7.9?

(1 point)

4. As described earlier, the recurrence interval is an important value for city planners to determine how

infrastructure such as buildings should be prepared to withstand earthquakes of a given size. What is the

recurrence interval for the 6.0-6.9 magnitude range? (1 point)

What is the recurrence interval for the 7.0-7.9 magnitude range? (1 point)

5. The New Madrid Seismic Zone is well known not only for the recent small-to-moderate sized

earthquakes, but for a series of large earthquakes in 1811-1812. On the basis of the large area of damage

(600,000 square kilometers), the widespread area of perceptibility (5,000,000 square kilometers), and the

complex landscape changes that occurred, the New Madrid earthquakes of 1811-1812 rank as some of

the largest in the United States since its settlement by Europeans. Because there were no seismographs in

North America at that time, and very few people in the New Madrid region, the estimated magnitudes of

this series of earthquakes vary considerably and depend on modern researchers’ interpretations of

journals, newspaper reports, and other accounts of the ground shaking and damage. The general

consensus is that they were at least magnitude 7 and could have been as large as magnitude 8. Based on

the recurrence interval you just calculated, are we due for an earthquake in the New Madrid Seismic

Zone? Why or why not? (1 point)

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