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Plate Tectonics: The Demise Of Dinosaurs

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Plate tectonics did play a part in discovering what was the demise of the dinosaurs. Walter Alveras and his team were trying to discover why the Earth’s magnetic flip-flopped from south to north and they felt that the answers could be found in sedimentary rock samples. The sedimentary layer of rock was 65 million years old and formed a boundary between the Cretaceous and Tertiary periods, known as the “KT” boundary. This boundary was made of clay and it was a devoid of fossils. Paleontologists had always thought that dinosaur extinction was a slow process. Alveras felt the opposite was true. He felt that the dinosaur extinction was catastrophic and sudden. Alveras and his team were testing for certain elements within this boundary. Iridium

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