HW_Turkey Earthquake
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Astronomy
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Apr 3, 2024
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EES 0836
Earthquakes on the North Anatolian Fault System
Disasters: Geology vs. Hollywood
Introduction
You are part of a team of scientists sent by the United States Geological Survey (USGS) to Turkey to in-
vestigate the hazard of earthquakes along the North Anatolian Fault System (NAF). As a geoscientist, your goal is to address key questions, including:
●
Where do earthquakes occur?
●
Is there some information we could use to forecast the location of the next event? ●
What should we be planning for next?
Learning Objectives
●
Analyze past events to forecast where future events occur. (1, 2, 5, a, b, c)
●
Identify locations where city planners should prepare for future earthquakes. (1, 2, 5, a)
Part 1: Forecasting earthquakes
We know where plate boundaries are, and we know that earthquakes occur at these boundaries. But our ability to forecast when they will occur has remained a challenge for geologists.
1.
What are some methods for forecasting earthquakes?
Some methods for forecasting earthquakes include looking out for precursors which will occur before an earthquake happens. Some of these include a change in the magnetic field, or by look-
ing at the seismic gaps which would tell areas that have had earthquakes occurred along the faults. One final method is by looking at the seismic waves that have occurred which can help identify when exactly the earthquake will occur.
2.
Of the methods you listed, what do you think is the most promising method to use in the future? Explain your thinking.
EES 0836
Looking at the seismic gaps would be the most helpful. This is because these will tell where earthquakes have occurred in the past, which would most likely be the most accurate in helping to
predict when and where they will happen again.
Part 2
: The data
People have lived in Turkey for millennia with a rich set of historical writings and records of events. These historical accounts of disasters, and in some cases, the actual destruction of towns leading to refugee migrations, provide an unusually long record of earthquake occurrence. In this part of the activity,
we will be plotting the amount of fault slip from events throughout the 1900’s and trying to forecast the location of future events.
Just looking at the data included, it is difficult to see if there is any information to glean from it. To help us organize the data, we will be plotting the events from the data set into a format that would help us visu-
alize the information more effectively. Data Set 1: Date (years)
Position (km) parallel to fault
Data source/type
1967
-410 / -330
Historical Account + Geo mapping
1957
-335 / -305
Historical Account + Geo mapping
1951
-195 / -130
Historical Account + Geo mapping
1944
-305 / -130
Historical Account + Geo mapping
1943
-130 / 140
Historical Account + Geo mapping
1942
155 / 185
Historical Account + Geo mapping
1939
95 / 440
Historical Account + Geo mapping
How to Plot: Referring to Data Set 1, the column on the left shows the years, and the middle column contains the movements during that particular earthquake. On the provided table on the next page, plot these coordi-
nates along with their years. Accuracy matters, but don’t worry too much about precision. The informa-
tion, once plotted, should be clear enough. Just make sure you work in pencil in case you need to erase. ●
Locate the approximate year on the Y axis.
●
Then put a dot where the left coordinate is located and another where the right coordinate is lo-
cated. ●
Connect the dots for that event. ●
1967’s earthquake is completed for you.
●
After plotting the data, answer the following questions.
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