A dense sphere of solid iron and nickel at the center of the Earth is the ...

Explore the comprehensive Geosphere Test. Prepare with flashcards and multiple choice questions, each with detailed explanations. Master the subject and succeed on your exam!

Multiple Choice

A dense sphere of solid iron and nickel at the center of the Earth is the ...

Explanation:
The inner core is a solid sphere of iron and nickel at Earth's center. The immense pressures there keep iron in a solid state even at very high temperatures, so it forms a dense, solid ball. Surrounding it is the liquid iron–nickel outer core, which moves and convection in that liquid generates Earth's magnetic field. Outside the core lies the mantle, a thick layer of silicate rock, and the crust is the thin outer shell. Seismic evidence supports this layered picture: S-waves don’t travel through the liquid outer core, helping reveal the presence of a liquid layer around the solid center, while P-waves reveal transitions between the solid inner core, the liquid outer core, and the mantle.

The inner core is a solid sphere of iron and nickel at Earth's center. The immense pressures there keep iron in a solid state even at very high temperatures, so it forms a dense, solid ball. Surrounding it is the liquid iron–nickel outer core, which moves and convection in that liquid generates Earth's magnetic field. Outside the core lies the mantle, a thick layer of silicate rock, and the crust is the thin outer shell. Seismic evidence supports this layered picture: S-waves don’t travel through the liquid outer core, helping reveal the presence of a liquid layer around the solid center, while P-waves reveal transitions between the solid inner core, the liquid outer core, and the mantle.

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