Collision of Plate Boundaries
Locating the Earthquake Epicenter
* * *Center of an Earthquake
Triangulation Method
Objective: Find the Epicenter of an earthquake using Triangulation Method
Materials:
- hypothetical records of earthquake waves
- Philippine map
- drawing compass and ruler
Triangulation Table
Data. Computation is required!
RECORDING STATION | TIME DIFFERENCE | DISTANCE | COMPUTED |
---|---|---|---|
Batangas | 44.8 | ||
Puerto Princesa | 32 | ||
Davao | 38.4 |
NOTE: Time difference - difference in the arrival time of P-wave and S-wave in seconds.
Things to do in Triangulation
FOLLOW the STEPS ACCORDINGLY
-
STUDY THE DATA
Shown is the difference between the arrival time of P-waves and S-waves.
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COMPUTE THE DISTANCE
Distance from the epicenter from each station using formula
d=(Td/8sec)x 100km
. -
CHOOSE ONE OF THE RECORDING STATION
Measure the computed distance on the map scale. the scale of the map in Figure 3 is 1.5 cm: 200 km.Set your compass for that computed distance
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AGAIN, ON THE OTHER RECORDING STATION
Center your compass, then draw a circle.
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REPEAT STEPS 3 & 4 FOR THE REST OF THE STATIONS.
You should get three circles that intersect or nearly intersect at a point. This intersection is the epicenter.
GUIDE QUESTIONS
Q1. Where is the epicenter of this hypothetical earthquake?
Q2. What difficulty will you encounter if you only have data from two recording stations?
GUIDE QUESTIONS
Q3. The distance-time graph above shows that the S-P interval is aout 10 minutes. What is the distance of the epicenter from the seismic station?
Q4. What do you think is the importance of determining the epicenter of an earthquake?
Determining the location of earthquake epicenters plays a vital role in laying the foundations of plate tectonics.
That's how!
Now you know!
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