How did the discovery of radioactivity change estimates of Earth’s age?

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Before the discovery of radioactivity, estimates of Earth’s age were significantly underestimated, often ranging from only a few thousand to roughly 100 million years based on flawed assumptions about sedimentation rates, ocean salinity, or cooling thermodynamic models.1

The discovery of radioactivity fundamentally changed these estimates by providing a reliable method for absolute dating. Early 20th-century researchers, such as Bertram B. Boltwood, used uranium-lead systems to calculate mineral ages reaching into the billions of years, an order of magnitude greater than previous estimates. Furthermore, the realization that radioactive decay provides a continuous internal heat source invalidated earlier cooling models, such as those proposed by Lord Kelvin, which had incorrectly assumed the Earth was inert and cooling from a molten state.21

Today, through the isotopic analysis of meteorites and terrestrial samples, scientists have established that Earth is approximately 4.5 to 4.6 billion years old. This shift from a "young" Earth to one of immense geologic antiquity is a cornerstone of modern geochronology.312