Dinosaur Provincial Park is located about 2 hours drive east of Calgary, Alberta, Canada or 48 kilometres northeast of the community of Brooks.
The park is situated in the valley of the Red Deer River, which is noted for its striking badland topography. It is well known for being one of the greatest dinosaur fossil beds in the world. Thirty-nine dinosaur species have been discovered here and more than 500 specimens have been removed and exhibited in museums across the globe. Its significance justified it becoming a World Heritage Site in 1980.
Geology
The
sediments of Dinosaur Provincial Park span two 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, was primarily laid down by large rivers in subtropical 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.
Paleontology
Dinosaur Provincial Park preserves an extraordinarily diverse group of freshwater vertebrates. Fish include sharks, rays (such as the durophage
Myledaphus), paddlefish, bowfins, gars, and teleosts. Amphibians include frogs, salamanders, and the extinct albanerpetontids. Reptiles include lizards (such as the large monitor
Paleosaniwa), a wide range of turtles, crocodilians, and the fish-eating
Champsosaurus.
The dinosaurs of the park are astonishingly diverse. They include:
Ceratopsia
Hadrosauridae
Ankylosauria
Hypsilophodontidae'
Pachycephalosauria
Tyrannosauridae
Ornithomimidae
Dromaeosauridae
Troodontidae
Classification Uncertain
Birds such as Hesperornithiformes were present, as well as giant Pterosauria related to Quetzalcoatlus. Stagodont marsupials, placentals and multituberculates scurried underfoot.
Nature
The park boasts a very complex ecoysystem including
cottonwoods. It's ecosystem is surrounded by
prairies but is unique unto itself. Choruses of
coyotes are common at dusk, as are the calls of nighthawks. Jackrabbits, deer, and
pronghorn can all be seen in the park; rattlesnakes and
garter snakes are present as well. Curlews and
Canada geese can be seen in the spring and summer. Some of the most northern species of cactus, including
Opuntia (prickly pear) and
Pediocactus (pincushion) are found in the park as well.
History
Established in
1955 as part of Alberta's 50th Jubilee Year with the goal of protecting the fossil bone beds, the first warden was Roy Fowler, a farmer and amateur fossil hunter.
Until 1985 discoveries made in the park had to be shipped to museums throughout the world for scientific analysis and display, including the Royal Alberta Museum in Edmonton. This changed with the opening of the Royal Tyrrell Museum of Palaeontology 100 kilometres upstream in the Midland Provincial Park near Drumheller.
World Heritage Site
The park was established as a
UNESCO World Heritage Site in
1979, both for its scenery and for the importance of the
fossils found here.
See also
External links
Geography of Alberta | Parks in Alberta | World Heritage Sites in Canada
Dinosaurier-Provinzpark | Parc provincial Dinosaur | Dinosaur Provincial Park | Dinosaur Provincial Park | 省立恐龙公园