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Answer:
- They are divided by a layer of partly molten material called the mesosphere.
- inner core
- a continental margin
- They would detect a change in composition from iron-rich minerals to silica-rich minerals.
- spherical
- Scientists detected energy from certain seismic waves that travel only through liquids deep within Earth.
- The weight of the continents continually presses oceanic crust into the asthenosphere.
- the transfer of radioactive materials outward from Earth's interior
1. The main reason scientists divided Earth's core into an outer core and an inner core because they are divided by a layer of partly molten material called the mesosphere.
2. The crust, asthenosphere, the mantle, the outer core, and the inner core.
3. Rock has the highest percentage of iron-bearing minerals in a continental margin.
4. They would detect a change in composition from iron-rich minerals to silica-rich minerals.
5. The shape of Earth's inner core is spherical.
6. Scientists detected energy from certain seismic waves that travel only through liquids deep within Earth.
7. When Earth was still molten, gravity pulled dense elements down to Earth's center.
8. The weight of the continents continually presses oceanic crust into the asthenosphere.
9. The transfer of radioactive materials outward from Earth's interior.
10. The outer core is liquid and the inner core is solid.
11. The brittle lithosphere cracks under pressure from the moving asthenosphere.
12. It is too deep inside Earth to reach by drilling.
13. They have similar textures (brittle).
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