All previous attempts at setting a geologic timeline for the solar system have been based on different radiometric dating methods, including some that throw up very unreliable findingsestimates have ranged between 30 million years and 100 million years after the birth of the solar system. However, this time, the scientists used 259 computer simulations of the protoplanetary disk, the band of rocky matter that later made up the four terrestrial planetsMercury, Venus, Earth and Mars. They measured the siderophile (elements such as gold, platinum and iridium that dissolve in molten iron) content on the Earth before the Theia impact, after the Moon-forming event and today, to arrive at the Moons age. This method relies on the well-supported theory that the Theia impact caused siderophiles to sink into Earths iron-rich core from the crust. Given that crust was completely stripped of the siderophiles, whatever of these rare metals is found today in the Earths crust must have come from later impacts. How is the study significant It helps discern which radiometric dating methods are reliable given that some had pegged the age of the Moon close to the new methods figure.