At all events, thanks to the work of Clair Patterson, by 1953 the Earth at last had an age everyone could agree on.
Clair Patterson's extensive research provided a significant breakthrough in determining the age of the Earth, leading to a consensus by 1953. His findings were crucial in establishing a widely accepted timeframe that scientists could rely on for further studies related to the planet’s history and formation.
Before Patterson's work, there was much debate and uncertainty regarding the Earth's true age. His contributions helped clarify these discussions, enabling a unified perspective that enhanced the understanding of geological and evolutionary processes throughout history.
