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PhET Activity for MS-ESS3-2: Earthquake

PhET Activity for MS-ESS3-2: Earthquake

Assessment

Passage

•

Science

•

6th Grade

•

Hard

Created by

Wayground Simulations

FREE Resource

17 questions

Show all answers

1.

MULTIPLE CHOICE QUESTION

3 mins • Ungraded

DIRECTIONS:
1. Click on the 'Execute VirtualEarthquake' button in the center of the page.
Read the introductory text on the first page. Do not select a region yet. Get familiar with the terms P-wave, S-wave, and seismogram.

QUESTION: Are you acquainted with the tools in this simulation?

Yes

No

2.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

DIRECTIONS:
1. Scroll down to the bottom of the page.
2. Click the 'Japan region' radio button.
3. Click the 'Submit Choice' button located at the bottom right.

QUESTION: Why is it important for seismologists to have a network of seismic stations spread across different regions?

To cause more earthquakes for study.
To ensure at least one station is close to any potential earthquake for accurate data collection.
To compete with seismologists in other countries.
To measure the weather at different locations.

Answer explanation

A distributed network allows for data collection from multiple angles and locations, which is essential for accurately locating an earthquake through triangulation.

3.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

DIRECTIONS:
1. Click the 'View Seismograms' button at the bottom center of the page.

QUESTION: Looking at a seismogram, how can you distinguish the P-wave from the S-wave?

The P-wave is always red, and the S-wave is always blue.
The P-wave is the first wave to arrive and has a smaller amplitude than the S-wave.
The S-wave arrives first and has a smaller amplitude.
They both arrive at the same time but have different shapes.

Answer explanation

Primary (P) waves travel faster than Secondary (S) waves, so they always arrive first. S-waves typically carry more energy, resulting in a larger amplitude (more ground shaking).

4.

FILL IN THE BLANKS QUESTION

1 min • 1 pt

DIRECTIONS:
1. Remain on the page displaying the three seismograms.

QUESTION: A seismogram is a graph where the horizontal axis represents ___ and the vertical axis represents the ___ of the seismic waves.

(a)  

Answer explanation

time, amplitude

5.

DROPDOWN QUESTION

1 min • 1 pt

DIRECTIONS:
1. On the 'Pusan' seismogram, read the arrival time of the P-wave (the first wiggle).
2. Read the arrival time of the S-wave (the first large wiggle).
3. Subtract the P-wave time from the S-wave time to get the S-P interval.
4. Enter the calculated value of '50' into the input box for the 'Pusan' station.

QUESTION: The time difference between the P-wave and S-wave arrival is called the (a)   .

S-P interval
epicenter
magnitude
amplitude

Answer explanation

The correct option is 'S-P interval'.

6.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

DIRECTIONS:
1. Do not change the value for Pusan. Now, visually compare the S-P interval (the time gap between the P and S waves) for all three stations.

QUESTION: A seismic station is located very far from an earthquake's epicenter. What would you expect the S-P interval on its seismogram to be compared to a station closer to the epicenter?

The S-P interval would be smaller.
The S-P interval would be larger.
The S-P interval would be exactly the same.
There would be no S-wave.

Answer explanation

Because P-waves and S-waves travel at different speeds, the gap between their arrival times increases with the distance they travel from the epicenter.

7.

OPEN ENDED QUESTION

3 mins • 1 pt

DIRECTIONS:
1. Now, enter the S-P interval for Tokyo as '30'.
2. Enter the S-P interval for Akita as '50'.
3. Click the 'Convert S-P Interval' button.

QUESTION: Explain in your own words why data from only one or two seismic stations is not enough to pinpoint the exact location of an earthquake's epicenter.

Evaluate responses using AI:

OFF

Answer explanation

A good answer should explain that one station can only determine the distance to the epicenter, which defines a circle of possible locations. A second station narrows it down to two possible points where the two circles intersect. A third station is required to eliminate one of those points and identify the single, unique location of the epicenter. This process is called triangulation.

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