Final answer:
The steps taken to measure the local magnitude (MI) of a shallow earthquake involve recording seismic waves, identifying arrival times of P-waves and S-waves, calculating time differences, determining distance, and applying a logarithmic scale.
Step-by-step explanation:
The steps taken to measure the local magnitude (MI) of a shallow earthquake can be ranked as follows:
- Record seismic waves using seismographs
- Identify the arrival times of P-waves and S-waves
- Calculate the time difference between the arrival of P-waves and S-waves
- Use the time difference to determine the distance from the seismograph to the epicenter of the earthquake
- Apply a logarithmic scale to convert the distance into local magnitude (MI)