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How can three stations help locate an earthquake?

An earthquake sends out different kinds of waves that arrive at a station at different times. The gap between P-wave and S-wave arrivals helps estimate distance, but distance alone leaves many possible locations. Combining observations from several stations narrows the search for the epicenter.

8–10 min

Questions you could explore

  • Why is a distance estimate not yet a location?
  • How might uncertain arrival times affect the result?

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Earth and weather

How can lines on a map show a steep hill?

A flat map can warn you that a route climbs sharply before you ever see the hill. Contour lines join places of equal height, and their spacing adds information about how quickly the ground rises.

2–3 min
Earth and weather

How can an earthquake alert arrive before strong shaking?

An earthquake alert can beat the strongest shaking to a distant location even though the earthquake has already started. Detection and communication can travel ahead of the damaging waves, but nearby places may receive little or no warning.

4–5 min
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