Our first outing at Theodore Roosevelt NP was a long hike at South Unit of the Petrified Forest loop trail in the Theodore Roosevelt wilderness (read here if you missed it). But that was only a piece of the sprawling 70,400 acres of the breathtaking North Dakota Badlands. The South Unit was close to our home base at Medora Campground (Steve’s review here), but it was a 60-mile drive to the North Unit, our next area of exploration.
Theodore Roosevelt NP map
It was a good thing we visited the badlands areas on different days and at different times, for it gave us a variety of perspectives on the ever-changing mountain hues as the sun moved across the sky. As we approached each unit we were faced with colorful multi-layered mountains.
The layers are very prominent at the North Unit
Early evening at the South Unit
Winding down the scenic roads we began to understand why the badlands had profoundly affected Theodore Roosevelt. This landscape changes rapidly due to erosion by wind and rain. Many multi-colored horizontal stripes in the rocks run for miles. The corrugated cliffs, steep convoluted gullies and dome-shaped hills unfolded before us, and we were both fascinated and in awe of the beauty – so much to take in!
At the North Unit…
…and at the South Unit
Creation of the badlands began over 65 million years ago. It occurred when the newly-arisen Rockies began depositing sediments that streamed here layer after layer. Six hundred thousand years ago the northward-flowing Little Missouri River, which was headed for Hudson Bay in Canada, was diverted east by glaciers. The change in flow eventually formed the rugged terrain that we saw today.
The Little Missouri River cuts through the badlands
With the continuing erosion, colored layers of rock are exposed. They consist of layers of poorly lithified siltstone, claystone, sandstone, and lignite coal that were deposited in a coastal plain environment. When we looked around, common sedimentary sandstone was mostly what we see. But a closer look showed odd shapes and strange formations that we learned result from weathered sandstone that forms a protective cap of rock in some places called “hoodoos.”
With erosion wearing down the less resistant material, a jumble of knobs, ridges, and buttes topped with durable red scoria caps remain
Geologic formations have always fascinated me, and from further reading I learned that the badlands are eroded mainly by “slope wash” not directly by streams and rivers. The soil and rock materials are easily weathered in places where vegetation is thin, forming a loose surface that slips and slides easily downslope during rain showers or when the snow cover melts.
Note the slipping hillside here
Concretions, on the other hand, are spheres of mineral matter once surrounded by rock of a different composition. The concretions in the picture below were formed when a cementing material formed around a center of organic matter such as a leaf, twig, shell or tooth. As the softer material weathers away, the spheres emerge as an apparently separate feature in the landscape. Isn’t that fascinating?
Concretions are commonly, but not always round in shape
A concretion that looks more like a petrified log
The horizontal layers of multi-colored sandstone, clay and shale are complimented by scattered beds of lignite coal and patches of pastel pink scoria. The pinkish color is created when the soft lignite burns in fires usually started by lightning, baking the surrounding clay to this bright color.
A closer look at the formations show bluish-gray layers of weathered volcanic ash that formed excellent marker beds in places. We also saw markers formed by brownish-gray layers of sand containing thin, orange iron-rich bands.
Some strange landscape indeed!
The red color of the rock comes from the oxidation of iron released from lignite coal as it burns
The badlands are a hilly landscape, and as we approached them at the South Unit we were looking down at them from above:
A pose overlooking part of the South Unit
From one of the North Unit pullouts we saw plateaus capped with a blue-black popcorn-like soil called bentonitic clay which added even more color to the hills.
From the rim of “the breaks,” as the descent into the badlands is called, we viewed strips of sparsely-wooded ridges and bluffs.
Steve is searching for the elusive big horn sheep at the North Unit
The badlands may look austere and desolate, but it is home to a dense population of wildlife. Bison and Prairie Dogs cause traffic jams, pronghorns can be seen on the hillside and wild horses munch peacefully in the meadows.
That one weighs about as much as our car!
Pronghorns out for a bit of dinner
We didn’t see any Bighorn sheep until we ran across a park ranger who pointed out several on a distant cliff. He told us that 50% of the sheep here have died of pneumonia recently, and there may not be any left in a year or two. Very sad.
Steve talking with ranger John
It takes a trained eye to spot these resting Bighorn sheep – they really blend into the surrounding rock
And of course I was excited to see several of my feathered friends!
Prairie Dog with a Northern Flicker
Amidst all of the breathtaking landscape in the North Unit is the reality of the oil boom in the Bakken Oil Fields just a few miles north of the park. We were surprised during our drive to the North Unit to see I-85 so busy with big rig traffic and speeding trucks.
While reading about fracking concerns I stumbled onto an interview of a defender of the North Dakota Badlands. It turned out to be none other than the ranger we had met at the park! Click here to learn about the realities of the oil drilling near the park.
Perhaps the best part of our hikes was the absence of one particular mammal – humans! Between the two areas of the park we preferred the North Unit, as it’s in a relatively isolated region and rarely crowded. While there we felt like we were experiencing the gorgeous loneliness of the badlands much as Roosevelt did more than a hundred years ago.
Sunset over the North Dakota Badlands
Next up: Then there’s the SOUTH Dakota badlands!