Question 138735 • 2026-27 AL-Earth and Space Science
Iron-bearing minerals in ocean rocks align with Earth’s magnetic field as the rocks form, preserving evidence of changes in the field’s direction and supporting seafloor spreading. The ages of seafloor rocks also fit the theory: rocks are youngest near mid-ocean ridges and become older farther away. Pillow-shaped rocks form when lava cools underwater, showing that new crust forms on the ocean floor. Matching fossils in different areas support continental drift, not specifically Hess’s seafloor-spreading theory; Earth’s axial tilt and rotation are unrelated.
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