Approximately 4.4 billion years ago, zircon crystals formed in what is now the Jack Hills region of Western Australia, creating the oldest known pieces of Earth's crust. These microscopic minerals, found in ancient sedimentary rocks, contain oxygen isotope ratios indicating they crystallized in cool conditions compatible with liquid water and oceans. This evidence contradicted earlier theories that early Earth was entirely molten and suggested habitable conditions existed during the Hadean Eon earlier than previously estimated, potentially affecting timelines for life's origin.