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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. \( \qquad \)

Ask by West Joseph. in the United States
Feb 25,2025

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1. The Earth's layers from outside to inside are crust, mantle, outer core, inner core. 2. The inner core is the hottest layer. 3. Temperature and density increase as you go deeper into the Earth. 4. Continental crust is thicker than oceanic crust. 5. Continental crust is mostly granite. 6. The lithosphere is solid, not molten. 7. The asthenosphere is partially molten, not entirely liquid. 8. Convection currents occur primarily in the asthenosphere. 9. Iron and nickel are present in the mantle. 10. The Earth is roughly spherical.

Solution

Below is an evaluation of each statement: 1. “The layers of the Earth from outside to inside are inner core, outer core, mantle, crust.”   • This ordering is reversed. The correct order from the outside in is: crust, mantle, outer core, inner core.   • Result: False 2. “The inner core has the highest temperature of all layers.”   • The inner core is extremely hot (roughly comparable in temperature to the Sun’s surface) and is the hottest layer even though it is solid.   • Result: True 3. “As you move deeper into the Earth, temperature and density decrease.”   • In fact, both temperature and density increase as you move toward the center of the Earth.   • Result: False 4. “The continental and oceanic crust are the same in thickness.”   • Continental crust is generally thicker (averaging about 30–40 km) than the oceanic crust (typically about 5–10 km thick).   • Result: False 5. “Continental crust is mostly composed of granite.”   • Continental crust is indeed largely composed of silica-rich, granitic rocks.   • Result: True 6. “The lithosphere is molten rock.”   • The lithosphere is the rigid outer layer of the Earth (including the crust and the uppermost mantle). It is solid. The molten or ductile region is the asthenosphere.   • Result: False 7. “The asthenosphere is composed of molten rock.”   • The asthenosphere is a partially molten, ductile region in the upper mantle. Describing it as “molten rock” is an oversimplification since it is not completely liquid, but rather behaves plastically.   • Result: False 8. “Convection currents occur in the lithosphere and asthenosphere.”   • Convection currents primarily occur in the asthenosphere, where the partially molten rock can flow. The lithosphere, though it moves as tectonic plates, is not the region where the convection processes themselves take place.   • Result: False 9. “Iron and nickel are found in the mantle.”   • Though the highest concentrations of iron and nickel are in the core, iron (and to a lesser extent, nickel) is also present in mantle minerals (such as olivine and pyroxene). Thus, they are found in the mantle, even if not in the same proportions as in the core.   • Result: True 10. “The Earth is a sphere.”   • While Earth is more accurately described as an oblate spheroid (slightly flattened at the poles), it is essentially spherical.   • Result: True Summary: 1: False 2: True 3: False 4: False 5: True 6: False 7: False 8: False 9: True 10: True

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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!

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