Tsunamis (L1-L3)

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Across
  1. 3. This part of the core is solid iron
  2. 4. This wave model's limitation is the depth is the same under the water
  3. 9. This happens at a convergent boundary when two continental plates collide
  4. 11. This is the original point of an earthquake
  5. 13. This variable increases when you increase earthquake magnitude
  6. 15. If this is lower, the tsunami wave height increases
  7. 17. This variable is on the x-axis
  8. 20. This is created at a divergent boundary in the ocean
  9. 21. This part of the core is liquid iron
  10. 22. This boundary is where two plates slide past each other
  11. 23. This is how energy is transferred within the mantle
Down
  1. 1. If this is higher, the tsunami wave height increases
  2. 2. This is the hot liquid layer of the earth below the crust
  3. 5. This layer of the earth combines the crust with the upper solid mantle
  4. 6. This boundary is where two plates move apart
  5. 7. This variable is on the y-axis
  6. 8. This is the distance from the mean to the highest point in a wave
  7. 10. This part of the mantle lies below the lithosphere
  8. 12. This wave model's limitation is that we cannot see the actual amplitude of the waves
  9. 14. This is what a wave does after it hits a barrier
  10. 16. This is the depth that increases tsunami wave height
  11. 18. This boundary is where two plates collide
  12. 19. This type of convergent boundary is where a continental plate meets an oceanic plate