Mapping the Hidden Plate: teacher key
Earthquakes, grade 11 edition, written for 11th grade. Nobody can see an earthquake, so seismologists reason from wave arrival times and instruments. They can place and size a quake and give its odds, but they cannot name the day.
Read the book. Print this page for the key.
Questions and answers
- How do seismologists locate an earthquake?
- By guessing a source and shrinking the difference from real arrival times (answer)
- By photographing the fault from above
- By asking people to report the date
- At a transform boundary, what do the two plates do?
- They slide past each other sideways (answer)
- They push apart and make new crust
- One sinks under the other
- Which is early warning, not prediction?
- Naming the date of the next quake
- A ShakeAlert signal sent after a quake has started (answer)
- A cloud that looks strange
- What does Richter's scale measure?
- The largest wiggle on a record (answer)
- People's reports of shaking
- How deep the ocean is
- In this passage, what does inertia explain?
- Why the mass on a spring stays put when the ground shakes (answer)
- Why plates are 70 kilometers thick
- Why tsunamis move fast
Words
- seismograph: shaking recorder
- subduction: plate sinking under
- epicenter: spot above start
- intensity: local shaking
- liquefaction: ground turning soupy
- inertia: staying put