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The extinction of the dinosaurs at the end of the Cretaceous period has long been attributed to a massive asteroid impact. However, a closer examination of the fossil record and geological evidence suggests that volcanic activity, specifically the Deccan Traps in India, was the primary cause. First, the timing of the Deccan Traps eruptions aligns more precisely with the extinction event. Radiometric dating shows that the main phase of volcanic activity occurred over a relatively short period, coinciding with the iridium layer that marks the extinction. Second, volcanic emissions of sulfur dioxide and carbon dioxide would have caused severe climate changes, including rapid global warming and cooling, which could have stressed dinosaur populations long before any asteroid strike. Third, the fossil record indicates a gradual decline in dinosaur diversity over the last few million years of the Cretaceous, consistent with the prolonged environmental stress from volcanism, rather than a sudden catastrophic impact.

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