1. The layers of the Earth from outside to inside are inner core, outer core, mantle, crust. \( \qquad \) 2. The inner core has the highest temperature of all layers. \( \qquad \) 3. As you move deeper into the Earth, temperature and density decrease. \( \qquad \) 4. The continental and oceanic crust are the same in thickness. \( \qquad \) 5. Continental crust is mostly composed of granite. \( \qquad \) 6. The lithosphere is molten rock. \( \qquad \) 7. The asthenosphere is composed of molten rock. \( \qquad \) 8. Convection currents occur in the lithosphere and asthenosphere. \( \qquad \) 9. Iron and nickel are found in the mantle. \( \qquad \) 10. The earth is a sphere. \( \qquad \)
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Beyond the Answer
Did you know that the inner core, while indeed very hot (around 9,932°F or 5,500°C), is actually solid due to the immense pressure at that depth? This layer consists mostly of iron and nickel, and its solid state is crucial for generating the Earth’s magnetic field! Just imagine the center of our planet is like an exotic mix of metal soup, hardening under pressure rather than boiling into a liquid. Speaking of layers, the continental crust can be up to 25 miles thick, while the oceanic crust is significantly thinner, around 5 to 6 miles thick! It's interesting to note that the oceanic crust is denser than the continental crust, which is why it sinks lower and forms ocean basins. The huge contrast between these two types of crust can create fascinating geological features like mountains and trenches!