
Montana And The South Dakota Badlands: A Unique Connection
How the Badlands Connect To Yellowstone
Have you ever gone somewhere new, but it still felt weirdly familiar?
It turns out that if you’re from Montana, you can feel this way in South Dakota too. Let me explain.
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Yellowstone’s Volcanic Legacy Reaches the Badlands
I grew up in South Dakota, so every now and then I catch myself reading up on my old stomping grounds. I was doing just that recently with the Badlands, and I came across something pretty interesting.
The Badlands are basically connected to Yellowstone.
Yellowstone National Park’s volcanic activity didn’t stay put. It spread across a huge area, reaching the Badlands in South Dakota, about 470–500 miles away.
Geological Details From The National Park Service
According to the National Park Service History Website:
The overlying Brule Formation, which is generally thicker in Badlands National Park than the Chadron, is comprised of the lower Scenic and upper Poleslide Members. Together these have a maximum thickness of circa 120 m and are comprised of mudstones, claystones, shales, sandstones, conglomerates, and volcanic ash. Ash derived from the Yellowstone National Park region is a common feature of the Poleslide Member (Clark et al. 1967). In portions of Badlands National Park, the Brule Formation is overlain by generally fine-grained and weakly cemented sediments of the late Oligocene Arikaree Group. The contact between the Sharps Formation of the Arikaree Group and underlying Brule Formation is marked by a distinctive bed of volcanic ash, known as the Rockyford Ash.
I just think that’s kind of wild. No matter where you go, especially out west, you might not be as far from Montana as you think.
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