Listen to Episode 127 on PodBean, YouTube, Spotify, or wherever podcasts are sold!
We’re now taking questions for our End of the Year Q&A! Submit your question here!
In the Upper Great Plains of the United States is a series of ancient sediments that have for more than a century been a premier source of information on the very end of the Age of Dinosaurs. This episode, we discuss the history, science, and significance of the Hell Creek Formation.
In the news
New insights into the evolution of giant ammonites
The Permian extinction was bad for wood-eating beetles
Young pterosaurs might have been more influential than we thought
Tetrapodophis is not a snake, amid other controversies
The Latest Days of the Mesozoic
The Hell Creek Formation is a geologic formation (that is, a distinct layer of rock representing a particular time and environment) which comprises the last 1-2 million years of the Cretaceous Period – the end of the “Age of Dinosaurs.”

The formation is named after a stream called Hell Creek in Montana. It was in the valley of Hell Creek that famed fossil hunter Barnum Brown became the first to formally study what he named the “Hell Creek beds.” When he first visited the valley in 1902, he found fossils of plants, invertebrates, and vertebrates, including the fossils that would go on to become the first official record of Tyrannosaurus rex.
Over the years, the Hell Creek Formation has become one of the best places in the world to study the end of the Mesozoic Era. The formation is rich in fossils, especially dinosaurs, making it a great place to research dinosaur evolution and ecosystem structure. Hell Creek is also one of the premier places to explore the end-Cretaceous mass extinction – in some places, the Hell Creek Formation sits directly underneath the famous K-Pg boundary, with its ample evidence of asteroid impact – and quite a lot of research in this region has been devoted to studying patterns of evolution and extinction before, during, and after the extinction event.

Image by Vladimír Socha, CC BY-SA 4.0
Hell Creek in its Day
The Hell Creek Formation mostly consists of siltstones, mudstones, and sandstones that represent an ancient flat plain crossed by many rivers. These rivers ran west to east, originating from the early Rocky Mountains to the west and emptying into the Western Interior Seaway in the east. The finer sediments were generally deposited on the floodplain during high water levels, and sandstone channels mark the positions of the ancient rivers themselves.
During the latest Cretaceous, between 66-67 million years ago or so, this plain was home to an evergreen woodland with a lush plant community including abundant flowering plants alongside conifers, ferns, and others. Animal fossils from Hell Creek reveal a diverse ecosystem of freshwater invertebrates, insects, fish, amphibians, reptiles, mammals, and of course, dinosaurs, including some of the most famous dinosaurs of all.

Image by Durbed, CC BY-SA 3.0
Learn More
Some recent Hell Creek discoveries and studies include the giant dromaeosaur Dakotaraptor, analysis of Triceratops evolution, research on primate ancestors, and massive mosasaurs in the nearby seaway, just to name a few.
The Tanis Site in North Dakota is a section of the Hell Creek Formation that might preserve the day of the end-Cretaceous asteroid impact.
Saurian is a survival-simulation game that features an impressive recreation of the Hell Creek ecosystem.
The Hell Creek Formation and its Contribution to the Cretaceous-Paleogene extinction (technical, paywall)
—
If you enjoyed this topic and want more like it, check out these related episodes:
- Episode 32 – Naracoorte Caves, Australia
- Episode 67 – The La Brea Tar Pits
- Episode 89 – The Burgess Shale
- Episode 110 – Mazon Creek Fossil Beds
- Episode 14 – The Gray Fossil Site
We also invite you to follow us on Twitter, Facebook, or Instagram, buy merch at our Zazzle store, join our Discord server, or consider supporting us with a one-time PayPal donation or on Patreon to get bonus recordings and other goodies!
Please feel free to contact us with comments, questions, or topic suggestions, and to rate and review us on iTunes