Across
- 3. What is magma that reaches the surface?
- 7. What is the rigid layer of Earth in the mantle that the plates “ride” on?
- 8. What name did Alfred Wegener give the ancient supercontinent?
- 10. What is the state of matter of the outer core?
- 11. What process breaks rocks into smaller pieces?
- 12. What element is second most common in the crust?
- 15. What is the semi rigid part of the middle mantle?
- 19. What type of plate boundary collides?
- 20. What type of rock changes without melting?
- 21. What element is most common in the crust?
- 22. What type of plate boundary slides past?
- 24. What ocean contains the Ring of Fire?
- 26. What theory did Wegener propose?
- 27. What are the broken pieces of Earth's crust called?
- 29. What process moves sediment from one place to another?
- 31. This is when minerals grow between sediments to glue them together to form sedimentary rocks.
- 32. What do plate boundaries often cause?
- 34. What type of igneous rock forms on surface?
- 35. What do oceanic plates do when meeting continental plates?
- 36. What type of current causes mantle movement?
Down
- 1. This is how tightly packed molecules are together.
- 2. What is the largest layer of Earth?
- 4. What form along plate boundaries?
- 5. What type of eruptions provide insight into Earth's interior?
- 6. What rock type composes continental crust?
- 9. What type of spreading occurs at mid ocean ridges?
- 10. What process turns sediment into sedimentary rock?
- 13. What is the hottest layer of Earth?
- 14. What process occurs when sediments settle?
- 16. What is the state of matter of the inner core?
- 17. What type of waves help study Earth's layers?
- 18. What type of igneous rock forms underground?
- 23. What is molten rock beneath the surface?
- 25. What type of plate boundary moves apart?
- 26. This is when sediments are squeezed together to start forming a sedimentary rock.
- 28. What rock type composes oceanic crust?
- 30. What force makes the inner core solid?
- 33. This is the thinnest layer of the Earth.
