On August 30, 1909, paleontologist Charles Doolittle Walcott discovered exceptionally preserved Cambrian fossils on Fossil Ridge in British Columbia's Yoho National Park. The Burgess Shale, dating to 508 million years ago, contained soft-bodied organisms rarely preserved in the fossil record, including arthropods, worms, and creatures defying modern classification. Walcott returned annually until 1924, collecting over 65,000 specimens for the Smithsonian Institution. The site revealed the diversity of the Cambrian explosion and challenged assumptions about early animal evolution.