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Travel time curves are graphs of

  • A.arrival time plotted against epicentral distance
  • B.amplitude plotted against magnitude
  • C.intensity plotted against depth
  • D.acceleration plotted against period

Answer: A

Correct answer: arrival time plotted against epicentral distance

Travel time curves plot the arrival time of each phase against distance from the epicentre, built up from many recorded earthquakes. They are the working tool for identifying phases on a seismogram and for estimating distance, and their shape is what reveals the earth’s internal velocity structure - the breaks and shadow zones in them are the evidence for the Moho, the mantle transition zones and the core.

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