Final answer:
The densest materials on the terrestrial planets sink toward the center, creating a core of dense metals. This is due to the pull of gravity on the heavier elements. The terrestrial planets were likely molten at some point in the past.
Step-by-step explanation:
When we look at the internal structure of each of the terrestrial planets, we find that the densest metals are in a central core, with the lighter silicates near the surface. If these planets were liquid, like the giant planets, we could understand this effect as the result of the sinking of heavier elements due to the pull of gravity. This leads us to conclude that, although the terrestrial planets are solid today, at one time they must have been hot enough to melt.