The early Earth experienced melting, causing heavy elements to gravitate toward the center, forming an iron core. While it might be expected that heavy elements like uranium would also sink, uranium is classified as a lithophile, meaning it is chemically active and forms compounds that dissolve in molten rock. This characteristic allowed uranium and thorium to remain in the Earth's crust rather than being drawn into the core. In contrast, chemically inactive heavy elements such as gold, platinum, and iridium preferentially dissolved in iron, leading them to sink into the core and making them rare on the surface. Additionally, the bombardment of the Earth by comets and meteors contributed to the presence of heavy elements in the crust, as evidenced by the iridium found in the Chicxulub crater, which dates back approximately 64 million years.