Rare Dinosaur from Appalachia Found by Amateur Fossil Hunters

The remains of the dinosaur are on display in McWane Science Center.

Photo courtesy of Jun Ebersole, McWane Science Center

This duck-billed dinosaur — also known as a Hadrosaurid — was probably 20 to 30 feet long as an adult, mostly walked on its hind legs though it could come down on all four to graze on plants with its grinding teeth, and had a scaly exterior. But what set it apart is that it had a large crest on its nose.

“This thing had a big ugly nose,” Erickson said.

That large crest on the nose, plus indentations found in the skull and its unique teeth alerted Erickson and his colleagues from McWane Science Center in Birmingham, Ala., and the University of Bristol in the United Kingdom that the skeleton they had was something special.

The skeletal remains of this 83-million-year-old dinosaur were originally found by a team of amateur fossil enthusiasts alongside a creek in Montgomery County, Alabama in marine sediment. Dinosaurs from the South are extremely rare. A set with a complete skull is an even more extraordinary find. The dinosaur likely was washed out to sea by river or stream sediments after it died. When the group realized they had potentially discovered something of scientific importance, they contacted McWane Science Center in Birmingham, which dispatched a team to the site to carefully remove the remains from the surrounding rock.

After the bones were prepared and cleaned at McWane Science Center and the University of West Alabama, they were studied by a team of paleontologists including Erickson, former FSU doctoral student Albert Prieto-Marquez who is now at the University of Bristol, and Jun Ebersole, director of collections at McWane Science Center. Among the recovered remains of this new dinosaur are a complete skull, dozens of backbones, a partial hip bone and a few bones from the limbs.

It is one of the most complete dinosaur skeletons ever to be found in the eastern United States. Its teeth, which show this dinosaur’s remarkable ability to grind up plants in a manner like cows or horses, were present in early hadrosaurids, allowing them to consume a wide variety of plants as the group radiated around the world.

During the late Cretaceous Period, roughly 85 million years ago, North America was divided in half by a 1,000 mile ocean that connected the Gulf of Mexico to the Arctic Ocean. This body of water created two North American landmasses, Laramidia to the west and Appalachia to the east.

The area of what was considered Appalachia is a bit wider than what we call

Appalachia today. It began roughly in Georgia and Alabama and stretched all the way north into Canada.

The remains were found by amateur fossil hunters who contacted McWane Science Center. They are on display in Jun Ebersole’s lab at the center.

Photo courtesy of Jun Ebersole, McWane Science Center.

“For roughly 100 million years, the dinosaurs were not able to cross this barrier,” Ebersole said. “The discovery of Eotrachodon suggests that duck-billed dinosaurs originated in Appalachia and dispersed to other parts of the world at some point after the seaway lowered, opening a land corridor to western North America.”

Added Erickson: “They just needed to get off the island. From there, they became the cows of the Cretaceous.”

Erickson brought some bone samples and teeth back to his lab at Florida State for further analysis. He found it difficult to pinpoint the exact age of the dinosaur because no growth lines appeared in the bone samples. However, the highly vascularized bones show that it was growing very rapidly at the time of death, akin to a teenager, and stood to get much larger — perhaps 20-30 feet in length, which is typical of duck-billed dinosaurs found elsewhere.

The remains of Eotrachodon are housed at McWane Science Center in Birmingham and are currently on display in Ebersole’s laboratory for the general public to view.

Contacts and sources:
Kathleen Haughney,