The Chicxulub crater in the Yucatán Peninsula of Mexico provides crucial evidence for understanding the K-T impact. Measuring about 180 kilometers (roughly 110 miles) in diameter, this enormous structure is the result of an asteroid or comet impact.
- The crater's formation coincides with the geological timeline marking the end of the Cretaceous period.
- Studies show significant levels of shocked quartz and other anomalies typically associated with high-impact events.
- The crater's discovery reinforces the theory that a massive extraterrestrial body collided with Earth, causing wide-scale environmental changes.
Today, scientists use advanced technology to study the crater beneath layers of sediment, providing insights into its exact formation and the catastrophic aftermath experienced globally.