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History Established on June 27, 1955 as part of Alberta's 50th Jubilee Year with the goal of protecting the fossil beds, the first warden was Roy Fowler.

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Presentation on theme: "History Established on June 27, 1955 as part of Alberta's 50th Jubilee Year with the goal of protecting the fossil beds, the first warden was Roy Fowler."— Presentation transcript:

1 History Established on June 27, 1955 as part of Alberta's 50th Jubilee Year with the goal of protecting the fossil beds, the first warden was Roy Fowler (1902-1975), a farmer and amateur fossil hunter. The park was established as a UNESCO World Heritage Site on October 26, 1979 both for its nationally significant badlands and riverside riparian habitats, and for the international importance of the fossils found here. Until 1985, discoveries made in the park had to be shipped to museums throughout the world for scientific analysis and display, including the Royal Ontario Museum in Toronto, the Canadian Museum of Nature in Ottawa, and the American Museum of Natural History in New York. This changed with the opening of the Royal Tyrrell Museum of Palaeontology 100 kilometers upstream in Midland Provincial Park adjacent to Drumheller.

2 Dinosaur Provincial Park Visitor Centre The Dinosaur Provincial Park Visitor Centre features exhibits about dinosaurs, fossils, and the geology and natural history of the park. There is a video theater, fossil prep lab area, and a gift shop. Public programs are offered in the summer. John Ware's Cabin is a restored early 20th century cabin that was used by John Ware, an African-American cowboy and important figure in Alberta's ranching history. The cabin is located near the visitor center and is open on select days in the summer.[1]

3 Geology The sediments of Dinosaur Provincial Park span 2.8 million years and three formations: the terrestrial Oldman Formation at the base of the strata, the terrestrial Dinosaur Park Formation above, and the marine Bearpaw at the top. The Dinosaur Park Formation, which contains most of the fossils from articulated skeletons, was primarily laid down by large rivers in very warm temperate coastal lowlands along the western margin of the Western Interior Seaway. The formation dates to the Late Campanian, about 75 million years ago. The Dinosaur Park Formation spans about 1 million years.

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