Impact Theory
Alvarez and his father Luis W. Alvarez are most widely known for their discovery (with Frank Asaro and Helen Michel) that a clay layer occurring right at the Cretaceous-Tertiary (K-T) boundary was highly enriched in the element iridium. Since iridium enrichment is common in asteroids, but very uncommon on the Earth, they further postulated that the layer had been created by the impact of a large asteroid with the Earth and that this impact event was the likely cause of the Cretaceous–Paleogene extinction event.
This iridium enrichment has now been observed in many other sites around the world. And further, the very large Chicxulub crater was identified and is now regarded as the definitive evidence of a large impact. Consequently, a majority of scientists now accept the impact scenario as the most likely cause for the Cretaceous–Paleogene extinction event which occurred 65 million years ago and eliminated 75% of all species, including all non-avian dinosaurs. His book, T. Rex and the Crater of Doom, details the discovery of the Cretaceous–Paleogene extinction event.
In addition to his interest in extinction events and impacts, Alvarez has contributed to the understanding of Mediterranean tectonics, Roman geology and archeology, and the establishment of magnetostratigraphic correlations.
Read more about this topic: Walter Alvarez
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