• Theodore Roosevelt National Park

    Theodore Roosevelt

    National Park North Dakota

There are park alerts in effect.
show Alerts »
  • Road Closures

    The Scenic Drives in the North and South Units may be closed due to winter weather conditions. For current road status, click on the link below: More »

  • North Unit Road Closure

    The North Unit Scenic Drive will be closed at the Caprock Coulee parking area while repairs are in progress. Repairs may be delayed because of weather conditions, but are expected to be completed by May 15.

Fossils

champsosaurus gigas

Champsosaurus gigas on display at the South Unit Visitor Center.  This fossil crocodilian once inhabited western North Dakota when its climate was swampy.

NPS Photo

Note: Collecting fossils, petrified wood, rocks, or any other materials in Theodore Roosevelt National Park is prohibited by law.

If you have ever stood in the badlands on a hot, dry summer day or a freezing, blustery winter day, a warm, wet, and humid swamp might be the most opposite type of climate and environment you could imagine. Despite its stark contrast with today, fossil evidence in Theodore Roosevelt National Park strongly suggests that a swampy environment is exactly what used to be here in today's badlands. The fossil record shows that in the Paleocene Epoch, just after the time of the dinosaurs, this area was a vast swamp teeming with turtles, crocodilians, and bald cypress trees. A three-year cooperative paleontological survey conducted in Theodore Roosevelt National Park by the North Dakota Geological Survey shed light on this part of North Dakota's geologic history.

The fossilized remains of a crocodile-like reptile named Champsosaurus were excavated from a hillside in the South Unit in October 1995 by Dr. John Hoganson, paleontologist with the North Dakota Geological Survey, and his assistant, Jonathan Campbell. The ancient reptile once inhabited the fresh waters in what is now western North Dakota about 55 million years ago during the Paleocene epoch. At that time, the climate was subtropical, similar to that of present day Florida.

 

The long, narrow snout and large powerful back legs would have enabled the Champsosaurus to feed on fish, snails, mollusks and turtles. Paleontologists believe that this ten-foot-long predator spent much of its time submerged in water waiting for prey, much like modern crocodiles. Champsosaurus could lunge from the bottom using its powerful back legs. A turtle shell with bite marks also found during this survey provides a vignette of life from this era.

 
Prehistoric Swamp Mural

The Fossil Lake Wannagan mural depicts an artist's rendering of the swampy environment preserved in Theodore Roosevelt National Park's fossil record.  The mural, on display in the South Unit Visitor Center, includes reptiles, birds, fish, swamp trees, and extinct mammals such as multituberculates and condylarths.

NPS

During the paleontological inventory, more than two hundred fossil sites were identified and mapped from the rock layers known as the Sentinel Butte and Bullion Creek formations. The sites contained two other partial Champsosaur skeletons plus numerous freshwater mollusk remains, turtles (snapping and soft-shelled), parts of crocodiles and alligators, and plant fossils. The most common fossil found was petrified wood, including large tree stumps measuring seven to eight feet in diameter. It is believed that most of these trees were conifers, such as bald cypress and sequoia.

The paleontological investigation enhanced our view of the park's geologic story. By identifying what creatures and plants existed here, one can get an impression of what life was like millions of years ago. With a clearer picture of the past, we gain a better perspective on this continuously changing environment.

Why did the swamp disappear? Why is the landscape so rugged today? Read more about Geology of Theodore Roosevelt National Park.

Did You Know?

Cannonball concretions

Cannonball concretions can be found along the North Unit Scenic Drive. They were formed by the selective precipitation of mineral-rich groundwater and are nearly spherical because the sandstone in which sand grains were cemented together was of uniform permeability. More...